.^0^$.^./^^^^ ^ (*L /A
FROST & FIRE
VOL 11.
Prinlcihy K Clark
KDMONSroN AND DOUCil.AS, RDINBUIiGH
I.ONllllN . HAMILTON, ADAMS, AND Cll.
fAMBRlnOK . MACMILLAN AND ((1.
DUBI.tX M'O.I.ASIIAN AND (ill. I.
r.l.ASOOW . .lAMKR MACMvlIOSK
Arctic "VTalcr
^
MAP
Sliowiji^ the
PRESEMT POSITION
of a
MARINE CrLAClAU
PERI O D .
-•^Islands
HRl•;■^()^
diiey
ntiinwiutni. / f^CJ^i'E
CONTENTS OF VOL. 11.
CHAPTER XXVIII.
I'AQE
Baltic Current— British Isles ..... 1
CHAPTER XXIX,
Baltic Current 2 — British Isles 2 — Ireland 1 — Connemara —
GaLWAY AXU We.STI'ORT CURA'ES . . . . .18
CHAPTER XXX.
Baltic Current 3— IJritisii Isles 3— Ireland 2— Connemara 2—
North-western and North-eastern Coast.s— Galway, West-
port, AND Derry Veagh Curves . . . .42
CHAPTER XXXI.
Baltic Current i — British Isles 4 — Scotland — Galavay Curve —
Arran ........ 05
CHAPTER XXXII.
Baltic Current 5 — British Isles 5 — Scotland 2 — Westrort Curve
— Ceantire . . . .72
CONTENTS.
CIIATTER XXXni.
PAGE
Baltic Current 6 — Galway and Westport Curves— Argyll, etc. 78
CH AFTER XXXI y.
Baltic Current 7 — Britlsh Isles 6 — Scotland 3— Galway Curve
—Lanarkshire, East Lothian, etc. .... 9:'.
CHAPTER XXXV.
Baltic Current 8 — British Isles 7 — Scotland 4 — Galway Curve
^North-east Coast . . . . .107
CHAPTER XXXVI.
Baltic Current 9 — British Isles 8 — Scotland 5 — Newi-ort Line
— Central Scotland . . . .118
CHAPTER XXXVII.
Baltic Current 10— British Isles 9— Scotland 6— Derry Veaoh
Curve — Caledonian Canal and Northern Scotland . 132
CHAPTER XXXVIII.
Baltic Current 11— British Isles 10 — Scotland 7— Strath Bran,
Beinn Uaish, Sutherland, et('. . . . .151
CHAPTER XXXIX.
Baltic Current 12— British Isles 11— Isle of Man . . 168
CHAPTER XL.
Baltic Current 13— British Isles 12— Yorkshire and Wales, etc. 177
CHAPTER XLl.
Baltic Current 14— 15ritlsii Isles 13— Walks 2 . . 203
(.'ONTENT.S. vii
CHAPTER XLII.
PA(JE
Baltic Current lo — British Isles 11 — P^noland (South) . . 215
CHAPTEK XLII I.
Belleisle Current — America ..... 235
CHAPTER XLIV.
Glacial Periods ....... 249
CHAPTEK XLV.
Deposition — Natural Science — Force — Engines — Tools — Marks 2t>2
CHAPTER XLV I.
Deposition 2 — Time 2 — Temperature — Light — Air — Water —
Winds— Waves— Form . . .268
CHAPTER XLVII.
Deposition 3 — Winds 2 — Waves 2 — W.we-.marks . . . 275
CHAPTER XLVIU.
Deposition 4— Winds 3— Waves 3— Beaches . . .285
CHAPTER XLIX.
Deposition 5— Winds 4— Waves 4— Stre.vm-marks . . 294
CHAPTER L.
Deposition 6— Bedding— Rain-marks . . .303
CHAPTER LI.
Deposition 7— Fossils — Altered Rocks . . . 319
Vlil CONTENTS.
CHAPTER LII.
PAGE
Upheaval— Dykes— Veins— Sublimation . . . 339
CHAPTER LI II.
Upheaval 2 — Rays and Weight 2 — Fusion and Freezing — Metal
AND Slag . . . . . .354
CHAPTER LIV.
Sparks— Volcanic Bombs — Meteorites .... 367
CHAPTER LV.
Tubes and Springs ....... 387
CHAPTER LVI.
Springs, Chambers, Tubes, Craters, and Cones . . . 410
CHAPTER LVII.
Rays 438
CHAPTER LVIII.
Force, Movement, Work, Form ..... 461
ILLUSTEATIONS TO VOL. 11.
Chiefly selected to illustrate farms ickirh result from the action <f
certain forces, and from movements caused hy them. Marks if
Demulatim, Deposition, and Uplieaval : Gravitation, Jladiatiov,
a7id Eotation : Forces : and Will.
Fig. Page
Frontispiece — Map, showmg the present position of a
marine glacial period.
65 6 — A small example of " roclie moutonuee," Wales. Ice and
its marks. 1863.
66 7 — Jointed Tors, Conneniara. ■\
67 10 — Perched block, Connemara. > '
, ,, ,' I ^^tjJ- 18G3.
68 10 — Dropped block, Conneniara. >/
69 1 7 — Forest of Gairloch. Ice-marks on a hUl-slioulder .-^ of gi-ay
qnartz, at about 1350 feet above the sea ; level with the
opposite edge of the glen ^.-^. Methud of mapping stria?.
70 19 — Clocli Corril and the twelve pins of Connemara. Dra%TO
from nature on the wood, 1863. (Eeversed.)
71 25 — Train of blocks near Fumess Lake ; and MoycuUeen Hills.
Ditto.
72 28 — Perched block on rounded tor, Cnoc Ourid, 1200 feet. Ditto.
73 29— Perched block, Cnoc Mordan, 1100 feet. Ditto.
74 64 — Achill Head. A water-mark L- Sea-margin : cliff. 1863.
75 85 — Tors and perched blocks at 1600 feet. Tojj of Beinn Bhreac.
Drawn from natm-e on the wood. 1863.
76 92 — Westport curve. — An ice-mark in Scotland. Stria> ujion a
rock in Loch Fyne, about three miles south-west of Inver-
ary. From a photograph. 1863. ''~".
X ILLUSTRATIONS.
Vig. Piigc
77 lot) — A water-mark ill Icelaml. — Merkiar Fuss near Ilwla. 5tli
August 1861.
78 117 — Granite veins in sliattered beds of altered slate. Railway
cutting at Ualwhinny. Drawn from nature on the block.
(Reversed.) A fire-mark under ice-marks and water-
marks. 1863.
79 150 — Ancient sea-margin. Terraces about 700 feet above the
sea. Loch Roisg. Rocks worn by ice. 1863.
80 158 — West coast of Sutherland. Denudation on a large scale,
and ice-marks. 25th Sept. 1848.
81 167 — Rounded granite boulder in a wood behind TuUoch, rest-
ing on slate, 540 feet above the sea. 1863.
82 184 — Wales. Map, showing the general trend of hollows. Do.
83 19 7 — N.E. corner of Wales. General form of the country ,-^^. Do.
84 200 — Coed Mawr, Wales. Sketch to show the direction of
high stria; parallel to the Snowdon range. Do.
85 214 — Devil's Bridge. A water-mark U • ^'^^
86 221 — Blakeston Tor, Dartmoor ^^. Do.
87 225 — Terraces at Stockbridge. Casting a small fly over heavy
fish. Ancient sea-margins, eddies, and vortices. Do.
88 230 — Eddies and whirling floats. Do.
89 234—" The Scilly Bishops." Lat. 49^ 51' N. The last of the
British Isles. From a sketch made 8th July 1859.
90 248 — Maggoty Cove and Harl)0ur of St. John's. Ice. June 1863.
Waves and Beaches. Denudation and Deposition.
91 261 — A breaking wave. From a photograph. Taken Aug. 1858.
92 272 — Diagram. Wave-forms and wave-marks.
93 279 — Cross-rollers at Isle de Rhe, near Rochelle. From a sketcli
made from the Tour de Balene. November 1859.
94 286 — A breaker. Sketched in Cornwall, 1850.
95 288 — Bolauds Ilofvdi, Iceland. Clift' and talus, beacli and
breaker. Auuu.st 10, 1862.
ILLUSTKATTONS. xi
Fig. Page
96 293 — A snow-Avave in Cliesliiiv. Sketched from nature, after a
strong- breeze of wiiul. January 2n, isofj.
97 298 — Section of a snow-beach. Co})icd from a drift in the south
of England.
98 299 — ^Diagram. Damp sand lieaches packed by air-waves near
a rivulet in Iceland.
99 306 — A working model of a marine formation.
100 311 — Diagram. Stratified .snow-beds forming.
101 312 — Drift-beds on Goat Island, Niagara. 1864.
102 318 — Fossils. St. Louis and Mammoth Cave. 1864.
Uphexival.
103 338 — An ounce of silver, prepared at Newcastle. Rafliation and
form. Fusion and freezing. December 16, 1863.
104 353 — " Sphericity of water." Radiation. A hollow sphere of
fluid. Ditto.
104rt 379 — Sections of volcanic bombs, from Hraundal in Iceland.
Printed from the stones. Radiation and rotation.
Fusion and freezing. Chambered crust and core. Bent
rays. August 20, 1862.
105 400 — Vertical section through a frozen stream of wrinkled slag.
Printed from the stone. Radiation and flow. Fusion
and freezing. 1862.
106 409 — The Geysers from the horse-track. Tubes, cones, and
craters. 1861 and 1862.
107 414 — Tlie Great Geyser boiling over. Eruption, projectiles,
tubes, and cones. Saturday, August 2, 1862.
108 415 — Strokr and Geyser. Tubes, section. Ditto.
109 423 — Sections through the surface of a frozen lava-stream.
Printed from the stones. Radiation and lluw. Fusion
and freezing. Augu.st 23, 1862.
110 450 — Diagram. Centrifugal force.
111 453 — DiaL;ram. Radiation and rotation.
Xll ILLUSTRATIONS.
Fig. I'ago
112 480 — Woocl-eugiaving liy rays. Tlu' sun's path in tlie sky.
18G3.
113 481 — Dittu. Tlie suns path on two cloiuly days. 1MG2, 18G3.
114 481 — Ditto. Solar scale. 18G5.
1 If) 484 — Ditto. The sun's burning power at about twelve degrees
above the horizon for about tliree months. Horizontal
section of a dial. 1859.
IIG 487 — Ditto. The sun's burning power at noon for about three
months. Vertical section on the meridian of a dial.
1859.
1 17 501 — From a photograph of the sun, March 1859, supposed to
be a picture of forms in the solar atmosphere which
result from gravitation, radiation, and rotation. Watch
and dial.
CHAPTER XXVni.
BALTIC CUKKENT — BltlTISH ISLES.
When facts have been gatlierecl, sorted, and piled, the mound
is an obseiTatoiy. When a train of machinery has been
explored, from the dial-plate even to the axis of one small
wheel, the dial may be read though the entire engine may
still be incomprehensible. When an engine has been seen to
■work, the tool-marks may be used as records of work done.
When a creature has been seen to make tracks the old spoor
may be followed. In the preceding pages an arctic current
has been followed ; a pile of facts gathered ; part of an engine
explored ; tool-marks studied ; a spoor learned ; a theory has
been built on a pile of ice ; it will fall to the ground if ill
founded. The way to test it is to work up stream, from delta
to source, from circumference to centre, from the spoor to the
deer, from old ice-marks to melted ice, from tool-marks back
to the wheels which carved out hills and hollows. Old marks
in the British Isles will serve to test the theory of an old
Baltic Current ; and the following j)ages give the result of an
attempt to read and translate the record.
It has been shown that a current probably flowed from
the polar basin through the Gulf of Bothnia, over Southern
Scandinavia and Denmark, and paiis of England, if ever
central Europe was under water ; and if so its tracks should
remain in the British Isles.
If men wish to know from what quarter the wind is
VOL. II. B
2 UALTIC (ITUENT.
blowing they look up to tlie uearest chimney for a stream of
smoke ; to a steeple for a M'eathercock ; to mist on a liLll ; or
to clouds moving freely in air. They do not watch eddies
near the ground which whirl round corners and posts in
streets, or past rocks and glens in hilly countries ; and which
pack sand and whirling autumn leaves in curved ridges and
furrows in every sheltered nook.
The weather-wise look up to some high point in the
general air-current, where the wind is not altered by impedi-
ments. If we wish to know the direction in which the wind
commonly blows, we look for a tree growing in some exposed
place, and note the bend in the trunk and branches (vol. i. pp.
31, 59). It is vain to look at sheltered trees, or at trees in
glens where the wuid eddies and whirls in all directions, while
the main stream blows steadily on above. If we want to find
out the course of an old arctic current wliich brought glacial
drift to grind British rocks, we must in like manner look up.
It is vain to search sheltered glens for marks of a general
system of glacial denudation, and for tracks of polar ice moved
by ocean-currents. If such marks exist they can only he
found at exposed places ; on wide plains ; on hill-tops ; on
high ridges, where trees and plants are bent by the wind.
To find out wlience British glacial drift came, British hill-
tojis near the coast, and far inland, must be searched for
marks, and the marks followed from hill to hill. Marks of
old local glaciers, and old local glacial systems, must be
sought in hollows, for glaciers like rivers How in hollows
down-hill. But marks of ocean-currents and ice-Hoats must
be sought along some ancient sea-level, for ocean-currt'uts
nujve on tlie curves of the globe.
Hunting is healthy pastime, and huuliug for ice-marks
upon liill-to]>s may be coiiibiucd witii otjicv sjKtrt. The spool
BUITISII ISLE8. 3
leads to the haunts of grouse, deer, aud ptarmigan ; to grand
scenery and to regions of fresh air.
In the following pages an attempt is made to show the
result of a search for high ice-marks along some of the curves
on the maps at pages 232 and 496, vol. i.
The spoor. — Before starting on any pursuit, be it the spoor
of an annual or an arctic current, the marks must be learned.
A Highland deer-stalker, an Indian tracker, a Buslmian, or
any practised hunter, will follow a deer where a stranger sees
no track ; and so it is with ice-marks, they must be studied
before they can be followed. An attempt has been made to
show how some ice-marks are now made ; the old marks
relied on are shortly these —
1. Folisliviifj. — Upon certain hard rocks which will take
a fine surface, and over which ice is passing, or has lately
passed ; beneath glaciers, or near them, or near moving sea-
ice ; the stone surface shines when wet, feels perfectly smooth,
and is neither "joint" nor "cleavage plane," nor " bedding."
It is worn, ground, and polislied by the continual passage of
hard heavy ice, clay, and fine sand. As no other natural
engine now produces like w^ork, aud ice always does, a
polished surface "in situ" proves the passage of ice, even
over a hill-top.
2. Strice. — According to the direction in which ice moves,
so is the direction of the mark made. The polished surface
is usually varied by grooves. On the surface of the rock
parallel straight lines of various dimensions are often ruled,
and these lines point out the direction in which the polishing
engine moves. It may not be easy to recognise these marks
at first, and there seems always a lurking wish to show that
they were made by something familiar. It is told that a
numl)er of geologists once met at a quarry, to hold solemn
1 BALTIC CURRENT.
couclave over certain marks on the stone. Much breath and
some brain-work were expended, and no solution of tlie mys-
tery fouml. At the end oi" the meeting a ^A"orkman, who was
ooing h(nne, a])pL'ared above, and slid down the rock with
hob-nailed boots. The denuding engine was seen to make
tracks, and there was an end of this question. "Wlien glaciers
have been seen at work, their tracks are as easily known as
the print of a shoe. Striae are only skin deep ; they do not,
in any way, correspond to the structure of the rock, or if they
do at one jilace, they do not elsewhere. They sometimes
cross each other at small angles ; but so far as each line
extends, it follows a straight course, up one end of a rising
ground, over it, and down the other, or along the sides of a
mound or hollow. These grooves are part of the polished sur-
face, and follow the track of ice. Where they are foimd they
mark out the path like a spoor, and they are of many lands.
3. " Sand-lines." — These are tine as a hair, and are like
the marks of the finest sandpaper ; the}' extend a few inches
only, and are very easily overlooked.
4. " Scores." — These are deeper, and are sometimes made
liy liard gravel, or by points in larger blocks, fixed in moving
ice. Stones have been found under glaciers, fixed in ice, and
[jhuH'd in the end of a new groove. Scores are like a firm line,
cut witli a small gxnige, or a grooving plane with a round
iron. Tlu'y often contain sand-luies, and a pencil Mill rest in
them. They fade gradually away, but many are two or three
feet long. They are often attributed to ploughs and harrows.
0. Grooves. — These are deeper, a walking-stick Avill rest
in tlieni, and some are eight or ten feet long ; some are dinted,
as if a stone liad started and rolled while making tlie groove.
< "ail-whccls get the ci'cdit f>t' tlicsc soniclinics : tlu'V ollen
cHiitain sciMcs imd sand-lines.
BRITISH ISLES. 5
6. Deep (jroovea. — These are long ruuuded hollows n ^
which would fit a man's body. \Mien freshly made or well
preserved, they are fluted, aud often contain grooves, scores,
and sand-lines. They generally occur where great pressure
has been exerted ; on the weather-side of a point ; in the bed
of a river-glacier ; on the weather-side of an island, which has
become a hill ; at a sharp turn in a glen at the dot S, when
moving ice has been forced to curve, and has run full tilt
against the bank, as in Justedal (vol. i. p. 197) and Eomsdal.
Ice can be squeezed into a mould ; so ice under pressure is
forced into hollows ; and stones, sand, and clay, frozen in and
fixed in ice, deepen the groove, and flute the hollow sides.
7. Holloivs ■> — ". — These are but larger grooves, and often
contain all the others, though the smaller marks may be
buried in bogs, or drowned in lakes.
8. Glens ^ — ■. — These are marked on good maps, and many
of them seem to be large ice-grooves worn in rock by glaciers,
local systems, and ocean-currents, as shown above. Many
glens may have been hollows produced by contortions and
disturbances of the earth's crust at first ; but many are
hollows worn by some engine, and these generally retain all
the marks above described, though they may also contain beds
of drift, alluxial plains and rivers, lakes and arms of the sea.
If glens are rats in which ice moved, for the reasons above
given, their direction in a wide tract of country must be con-
sidered in spooring.
Hollows in Southern Scandinavia (chap, xviii.) and in Ice-
land (chap. xx%^) have been attributed above to the passage of
arctic currents, like the stream which has been followed from
Spitzbergen to Xewfomidland. All these are but grooves of
various sizes ^ -, which large engines might cut.
9. Roches Moutonnees. — When any ground surface covers
0 BALTIC flURREKT.
a large area, it is pretty sure to take in rocks of various hard-
ness, wliicli wear unecxually. If a bit of wood is rubbed with
fine sandpaper and a soft pad the grain rises. If a bit of
slate is rubbed, the beds wear unequally. An ice-ground rock-
surface wears unequally, and the rock takes the "niammil-
lated " form which suggested the Swiss name of " muttoned
rocks." Thoy look like bosses, domes, waves, rountU'd tables,
saddle-backs, hog-backs. In Devonshire, rocks of this shape
go by the name of " tors." The word is good ancient British
for " momid ;" so it is used as shorter than the usual glacial
slang terms, " roches moutonnees," and " mammillated sur-
faces." An example on the large scale is drawn on the margin
of the map ; the /\ shape of hills in Gairloch, 4000 feet high,
is there contrasted with the curved shape ^ — ^, which only
reaches to about 2000 feet. Examples symbolized by a convex
curve are given in woodcuts in the preceding pages. This
mark may be used to determine the point on the horizon from
which the grinding force mo>-ed. As a rule, the longest slope
is iq)-stream nr up-liill, and the steepest end dowu-liill or
-QlV
'imillllllllllllUmmmm
Fig. (ij. A Smam. Example ok " Roche Moi'tonnee," Wales.
down-stream. Tlie woodcut was made as an illu.stralion nf
this fact. It shows the form of a small slate " tor" in W'alc.^.
The arrow shows the direction in which ice slid down-hill,
the lines show cleavage, the direction in which the rock breaks ;
the case was selected because the ice-])lane had worked against
the grain of the stone, and had made line woi'k ne\ cftlieless.
10. Jlrolccn Ion. — If the smooth surface ends abnqilly, the
HKITISII ISLES. 7
broken end generally faces the shelter. Juints and bedding
generally weaken the stone vertically, and a force acting hori-
zontally tends to jjnsh, drag, or tear away the end of a worn
ridge, where the resistance is least. After a time the npper
edge of the fracture is worn and rounded off by a force which
works both vertically and horizontally, as heavy sliding ice
does. Another shove breaks off another slice ; and so a rock is
worn and broken, and the fragments pushed and rolled down-
hill or down-stream.
11. Jointed tors. — The weather-end of a ridge is some-
FiG. 60. JoiNTEii Torts, Cunnemara.
times displaced as if the rock had been broken and shaken
loose by a thrust or heavy blow.
The woodcut is from a sketch made near Inver in Con-
nemara.
The rest of the marks in the neighbourhood seem to prove
that ice generally moved from A towards B, and so wore
the granite into long ridges, all pointing one way. In this
case the ends next A have been carried off ; several ridges
are jointed and shaken loose ready to be moved, but the
sheltered end of the ridge next B is still solid.
8 BALTIC CURRENT.
11" such a fracture came to be worn, the steep end Avould
be on the weather-side at first.
So far those marks are all fixtures ; thej^ are in situ : — in the
place where the form was hewn out of the solid rock. They
are tool-marks of glacial denudation, and show the direction
in which the graving-tools worked. Even large hills and
whole countries seem to be hewn into these two forms —
i^A^sides these fixed marks others are used.
12. Quarried blocks. — Large stones are sometimes partly
li(iwn and ground, and partly broken out of the solid rock,
and pushed a few inches or yards from their beds, so that
each block might again be fitted into its place.
The direction in which the stone has been moved is that
in which some force pushed or dragged it, and many of these
blocks are so large that no common stream of water could
well move them.
13. Wandering Uochs. — These are similar stones of all
sorts and sizes, more or less worn or fractured, of the pattern
above described, Init moved further from the quarry. As an
example, granite blocks have been moved some hundred
yards from the granite hills of Arran, and are left npon slate
hills 1200 feet high. They are so placed that they could not
possibly roll to the spots where they are poised ; but they
have been moved so far, that the hole from which the stone
was taken can no longer be identified. Kane gives examples
of similar transport and dejjosition by arctic ice in Greeidaud,
and numerous examples of trans})ort by ice are mentioned
above. The highest wandering boulders yet found at home,
by the writer, are al)ove Loch Ericht, as shown on the margin
of the map (vol. i. ]). 4!)G), and on the shouhler of Len Wyvis.
The last is a large mass of mica-schist droppetl nearly 3000
BRITISH ISLES. 9
feet above the sea, and wholly eut ofl' from any hill of the
same material. Antrim flints have been somehow carried to
the south of Ireland ; zircon syenite, which is found in Nor-
way, has been carried to Galloway ; and rocks supposed to be
of Scandinavian origin have been carried to Poland and
Loudon. If the kind of stone thus transported can be iden-
tified with the parent rock, the direction of movement is
thereby showai. But the mark taken alone is uncertain.
Granite may have come from the polar basin, or from
lands wliich have disappeared. The test is good for land-
glaciers which must flow one way, but bad for ice-floats.
If a similar test were used to discover the prevailing
direction of the wind, it would fail, even though the Avind ma}'
have a prevailing direction. Winds in the British Isles drive
thistle-down, and thistles grow^ where the seed lights. Some
thistles are cultivated, so the direction in which a new variety
spreads from field or garden marks the spoor of the wind. If
there were a constant wdnd, thistles would spread from the
garden down-stream, but thistle-down, which moves every
way, like a British weathercock, would never mark out the
prevailing south-west wind Avhich bends British trees. ^larks
in the solid rock are fixed, and, like the trees, show the pre-
vailing current ; wandering blocks, like flying seeds, may show
eddies and occasional currents, and stray ones may drift
wherever a gale can blow" an ice-float.
14. Perched blocks are wandering blocks, placed upon hill-
tops or hill-shoulders, or balanced one upon the other, or on
" tors" and ridges, on points where they must have been
gently placed by something strong enough to lift tjiem, .
and cany and lay them down. Ice floating over a hill
might drop a stone on the top, or land-ice, grounding at high-
water, might place a stone, and break away wdien the tide
10
liALTIC Criv'REN'l
ebbed. The wootleut was drawn on ilie bloek, uiul represents
a stone perclied neai' Inver in C'onneinara. There are many
Fio. 07. Perched Block, Oonnemara.
other examples in the neighbourhood, but this one is remarl
able, for it looks like a work of art.
M#^
DnoFPED Block, Oonnemara.
15. Dropj)cd blocks. — These seem to have fallen so far as
to break where they fell. The cut was drawn on the wood,
and represents a large mass of granite near tlie police station
at Inver. It is mentioned aaain l)eloAv.
BRITISH ISLKS. 11
15. Trains. — These are rows of large stones, some per-
ched, some dropped and broken, which probably fell from
drifting ice. If so, the Imes pomt out the course of the
mo\dng rafts, and the run of the stream which moved them, but
this test is unceitain. If a Int of a glacier, with a medial
moraine, were launched, and then stranded and melted, the
row of big stones might cross the stream. A slice of ice-foot
might swing any way, and drop its wandering beach so as to
leave a ridge with any bearings (vol. i. p. 404).
16. Drift. — This word applies to confused heaps of stones,
of many kinds, shapes, and sizes ; some larger than hay-
cocks, others as big as casks, kegs, turnips, apples, nuts, and
peas, generally imbedded in sand or clay.
IT. Old moraines are land-ice chips, piled in conical
mounds at the mouths of glens, and composed of stones
which are foimd in situ in higher grounds.
18. A terminal moraine marks the end of an old glacier
(vol. i. p. 181.)
19. A medial moraine is similar stuff in tlie middle of a
rock-groove, generally near the rivulet.
20. A lateral moraine is similar stuff on one or lioth sides
of a glen. Stones on the right come from lulls on the right,
stones on the left from the left.
21. A moraine formed in water must differ in shape
from all these, and samples of aU kinds abound in the Alps,
Scandinavia, Iceland, and the British Isles. True moraines
indicate land-glaciers, and are sure marks, which can easily
be compared with moraines on existing glaciers. Sea-
moraines, formed under water, cannot be compared with
existing sea-glaciers, but their shape may Ije inferred from
models, and from the movements of laud-ice in Spitzbergen,
Greenland, etc. (chaps, xxiii. to xxvi.)
12 HALTU; CUKKENT.
These are all specimens of "drift," but the term is generally
used to express piles of loose rul)l)ish, widely spread OA-er a
whole country or contment, in glens and on plains and hill-sides.
The formation has lately been divided into stratified and un-
stratified, and in America it has been subdivided largely. The
lowest beds are " unstratified," contain scratched boulders, and
rest upon grooved rocks. The upper series are stratified, that
is to say, packed in layers. The deposition of these geological
formations has still to be explained. According to one theory,
the unstratified drift is the debris of land-ice, and the stratified
glacial drift was dropped by floating ice, and packed by
streams of water in a deep sea. It has been argu.ed above
that the drift is the moraine-work of large floating glaciers
like the Arctic Current, with its icebergs and sea-ice.
22. Boulders which belong to these formations are known
by their forms. Those which belong to the lower boulder
clay, which rests upon grooved rocks, are often washed out by
the sea, or by rivers, or picked out by men. They are found
on beaches, in walls, in houses, in fields newly reclaimed.
One side is generally flatter than the rest ; and, when freshly
moveel, the polish on the surface is nearly as fine as the ma-
terial is capable of taking. Stride of all sizes run every way,
but most commonly along the longest axis of the flattest sur-
face. It seems as if the drift were the polishing powder Math
which the rocks were ground, left in the tool-marks of tlie
polishing engine. The drift seems to consist of stones of all
sizes, partially rubbed and ground to clay, frozen into a con
glomerate and pushed onwards, till climate changed and the
ice melted. The worn stones bear marks of each other and of
tlie rock ; the rock bears marks of the drift, and these mark
the direction in which the drift was last moved. If most of
the stones in any patch of drift belong to any known forma-
BRITISH ISLES. 13
tion, the line of inoveiiieut is shown by the nature and posi-
ti(jn of the stones moved. For example, the majority of the
stones in a hill of drift near the sea, at Galway, are hits of
scratched moimtain limestone, and that kind of stone is found
in situ to the north-east. The direction in which this hill
of drift moved w^as from N.E. to S.W., because strise and loose
stones point to the same conclusion. But the hill also con-
tains specimens of many other rocks ; so it may have belonged
to ice which had sailed far, like that which is drifting along
the coast of Labrador, loaded both with foreign and native drift.
23. Weathering. — As all kinds of rock wear when exposed
to the atmosphere, ice-marks on rocks and boulders wear out
when the dressed surface is bare.
First, the fine polished skin gets rough and pitted, as rain
and air and lichens decompose parts of the stone. Then
" striie " wear out in the order of their depth. Then deep
grooves become shallow, from the weathering of their sides
and edges. Then larger grooves, and hollows, and tors, and
ridges between them, assume new shapes. Beds and joints
weather and widen, till an old tor looks like a pile of stones.
Then valleys and hiDs change their form. Eivers dig smooth
pits and jagged angular ruts in hill-sides, and these split, and
crumble, and fall, and join, leaving weathered glens, peaks,
and needles at last. This spoiling process may be watched,
and tlie work may be seen in all stages, in the momitains of
Northern Europe. But still the last bit of an ice-ground
surface may sometimes be found left at the veiy top of a hill,
whose sides have crumbled and fallen away to make heaps of
talus, cliffs, and cairns of stone.
The ridge ..^^ or the peak A is least worn by falling
water, so it lasts longest.
24. Shape. — Because of weathering, old ice-marks are not to
14 BALTIC (UK KENT.
be found without search. But so long as any part of the out-
line of an ice-ground hill retains its shape, a practised eye can
detect ice-work ; and a careful search at likely spots will
generally unearth some one or all of th(>. marks above de-
scribed. Two or tliree will sufhcc to determine the direction
in which ice moved, and a few well-chosen spots will serve
to map out a large district.
25. Hocks. — Different rocks weather in different ways and
at diiferent rates.
It is hopeless to search for any but large marks upon
coarse materials like sandstone. Limestones, unless protected
from rain-water by clay, lose the marks readily. Granites
protected from the air retain even sand-lines, and the finest
polish ; when exposed they become rough, and some kinds
crumble. On some granite-hills in Arran even deep grooves
are obliterated, though slate-hills close to them retain a fine
polish and the whole series of ic(>-marks.
Where quartz rock has not split up, it retahis the finest
marks ; but (juartz rock is vciy lialjle to Ijreak and full a^'ay.
So marks on cpiartz are rare.
Trap, whin, and greenstone, etc., last well, retain striu^ and
lose the polish, but some kinds of tra]) weather easily and
crundjle to dust.
Hard blue clay-slate ap])ears to resist the weather Ijcst of
all. Tec-marks still exist on bare slate-rocks in Wales, Scot-
laud, and Ireland, which could hardly be distinguished from
marks on rocks beneath existing glaciers.
It follows that the best material for inscribed monuments
is the slate which still retains fine sand-lines, made when
British liills were 2000 feet deeper in the sea, or \i\) to their
shoulders in land-ice.
20. ScdrcJiiuf/. — In searching a co\uitr\' for old iee-niaiks,
BRITISH ISLES. 15
it is best to look out for a hill of slate, quartz, or trap, wliieli
has a rounded outline y — ^.
Try the liill-top first for old marks, then beat the sides
about burns, new-made turf-dykes, quarries, and other such
places where the rock has been laid bare. If no marks of a
general movement can be found at the upper levels, try the
glens for the spoor of glaciers, and such small game.
There are few parts of Northern Europe where an old
scratch may not be found by careful searching.
27. Copying. — Eock -surfaces and ice-grooves cannot be
carried away, and specimens are bulky, heavy, and hard to
carry when quarried. Drawings take a long time to make,
photographic apparatus are grievous impediments, but rock-
surfaces may be quickly and accui-ately copied thus : —
Lay a sheet of foolscap on the rock with the longest
edges in the meridian, as nearly as a compass or the sun
will show. Hold the paper fast and rub it wdth a pencil, a
bullet, a coin, a burnt stick, a bit of black coal, or a bit of
heel-ball. The pattern below will be copied : — raised points
dark ; hollows light. The experiment may be tried on the
cover of this book, which is copied from a rubliiug made
from a striated rock beside the " Queen's Drive," on Ai'thuf s
Seat, at Edinburgh. The copy and the original may Ije com-
pared, so as to test the method ; and then other copies, and
descriptions of marks, will have more value if the paper, the
book, and the rock, are fountl to correspond when compared.
When the copy is made mark the north, and from the
centre of a circle draw an-ows pointing at any hill or hollow
which might influence the movements of glaciers ; or currents
of water moving from the horizon to the spot, at the level.
Small outline sketches may be drawn at tlie ends of the
arrows if there is time.
Xotc the name of tlio place ; the names of conspicuous
16 HALTin CURRENT.
points on the liorizon ; their bearings are given by the arrows.
Note the height of the spot by aneroid barometer ; tlie dis-
tance by pedometer from the last place of observation in a
day's walk ; the kind of rock ; tlie dip and strike by clino-
meter and compass ; the slope of trees, and anything else
worthy of note ; and do all this as much as possible without
moving the paper from tlie rock.
The finished sheet is a portable, accurate, pictorial record
of a set of observations at one spot, which may be transferred
to a map, or otherwise combined at leisure. Ranged in order
with dates, each record becomes a page in a journal. The
woodcut below is a reduced copy of a sheet wliicli was thus
prepared, on a rock-surface, on the hill-shoulder which is
represented on the margin of the map at the end of vol. i.
The dark marks within the circle are ridges " — v between
striae ^— ' on a very smooth surface of fine-grained hard
tpiartz rock. The direction in which the engine moved is
shown by the arrow. The loch is Loch Maree in Scotland,
and the sea horizon is open to the W. of K, and to tlie E. of
S. ; to Greenland, and to Scandinavia. To the west are tall
hills of the A pattern, and higher ice-ground rocks of the
- — s pattern ; to the east is a deep ice-ground glen v — • running
parallel to the strife, and beyond it are high hills of the y-^
pattern, and higher hills of the A shape, and numerous ice-
marks, none of which point at the ])eaks.
The dip of the rock is towards I), the white marks in the
rubbing are chinks and fractures.
At this spot on the backbone of Scotland, at 1800 feet
above the present sea-level, ice moved past peaks of the
A pattern over hills of the ^-^ pattern, from tlie direction of
the Baltic towards the Atlantic, horizontally. The spoor is so
fresh that sand-lines need a fine lens to make them out,
Avhile other grooves would hold the mast of a shi]i ; and the
BEITISH ISLES.
17
hill-side is thus worn, for a height of nearly 2000 feet,
throughout an area of many square miles.
If this plan of copying had been devised twenty years
sooner, observations made would have had more value. With
such a plain spoor as this ice-tracking is easy work.
River ElLV. I.och Mar
A A Peaks of Beit
Ghiiis, about 4000 ftet
V 'eatltered quart-
^ — ' Carrie. At 1800
feet marks areper/eet,
from S. 30 E. to N 30
IV. on gray quartz
crossing the mouth oj
the I
A Top of Ben Eith
about ^1x0 feet.
// 'eathered quartz
and talus.
A Heyojtd the gteii.
Top of Ben Siioch,
about ifloo feet.
U 'eathered.
^-^ Pass. Head of
Gleann Bianastte,
HS'^feet. Marks
perfect. N. 60° E. ;
gray quartz.
2isofeet; marks
weathered, N. 60° E.
gneiss. Pass
over the watershed of
Scotland to Dornoch.
--^ Hill .houH,, 18 n
feet; ba, , .
"r^ai: ■
high ma, I.
Mhonaidh and oitann
Bianastle. Nearly paiallrl
to horizontal grooves alt
the way to the bottom of the
glen, about \6oofeet.
---• Pass. Head of Strath
Bran, about 800 fet.
Terraces at Achnasheen.
abotctjQo; watershed of
Scotland. Thence ice-
^tarks follow the run of
the water ttorth eastiuards
to Ben Wyvis and to the
sea at the Conan. Peak {/)
beyond Strath Bran.
■ 09. Forest of Gairloch. Ice-marks on a hill-shoulder ^^ of gray quartz, at aliout
1350 feet above the sea ; level with the opposite edge of the gleti — -.
VOL. IL C
CHAPTEK XXIX.
BALTIC CURRENT 2 — BRITISH ISLES 2 — IRELAND 1 — CONNEMARA
GALWAY AND WESTBORT CURVES.
In the map of the northern hemisphere (end of vol. i.), a series
of curves are drawn from the Pole towards the Equator.
The space between two of these corresponds roughly to
the existing Arctic Current between Spitzbergen and New-
foundland ; and to low grounds in North America which are
strewed with glacial drift, and where many large hollows and
small ice-marks on shore point south-westwards. The space
between another couple of curves includes Novaya Zemlya,
part of Eussia, Scandinavia, Denmark, and the British Isles.
It corresponds to the supposed course of an arctic Baltic
Current, which, according to theory, only ceased to flow south-
west in this tract when the Scandinavian isthmus rose and
turned the stream. In tlie map (vol. i. p. 232), similar curves
are drawn, and one ends in the sea at Galway.
In a systematic attempt to test the soundness of this theory
founded on marks in Scandinavia, a search should begin as
far to the south-west as possible. A stick laid in an ice-
groove on a, hill-to]) points out the way, and it should be
honestly fcjllowed. If it leads to the Jiuirk.s already iiu'ii-
tioned, and the whole series point one way, the Baltic Current
theory may be launclied like a big boulder to find its own
resting-place amtjngst otlu'r rough blocks.
CONNEMARA — GAUVAY AND WESTPORT CURVEh;.
19
The west coast of Ireland is at the tail of the fossil
stream ; so the west of Ireland is the place to search for
marks of ice-floats like those which now cumher the Straits
of Belleisle.
London can be got at from any part of the world, and
the western coast of Ireland is very easily reached from
London, between morning and midnight.
OrH COKRU, AND THE TvVBI.VE PlN.-^ l.)F L'oNNI'
vn fn.in natiuv «n the wocxl, 18(i3. (Reversfd).
Forms characteristic of the action of ice are well seen by
the way. Eunning into Chester by railway, the N.E. corner
(jf Wales appears in profile, and on leaving the station the hills
are conspicuous. They rise gradually from a plain strewed
with glacial drift and water-worn boulders, and from the sea.
They are green and cultivated ; their bones are hid beneath
a skin of clay and soil, and covered by a rich mantle of green
and yellow ; but roimded rocks appear, as the skeleton does in
a living creature. A\^iere a quarry or railway cutting has
20 BALTIC CURRENT — UHlTl.Sll ISLES — IKELAND.
torn a n-nt, or cut a gash, the sandstone frame appears broken
and angular ; Lut the hills are all rounded and smooth.
This is denudation, Lut not the work of water. There is
not one ravine V between Chester and Ehyll, nor is there a
cliff L, though the line runs over a raised Ijeach between the
sea and an old margin all the way.
At Conway the hills are steeper and higher, but the glens
st ill are rounded, and in them fresh iec-marks abound, as will
1)6 shown below.
Near the Menai Bridge glens have the peculiar f(n-ms of
glaciation. Many quarries and cuttings, faults and fractures
in the slate, show that the rounded outlines of these hills and
glens are not due to fracture and disturbance, but to some
wearing action ; and boulders and beds of clay all tell of ice.
The N.E. end of the Snowdon range is seen in profde from
Anglesea. It has a sloping outline -^-n like the north-
eastern corner of Wales ; but the rocks are harder, the slope
is steeper, and some hill-tops are broken and weathered.
Anglesea is all ice-ground. Near Holyhead, amongst
some drifting sand-hills, glaciated rocks rear their heads
amongst the bent. They are smooth and round like the
sand-dunes, and their longest slope, like that of the hills, is
still towards the N.E. The waves which roll in from the
S.W., driven by the wind, have their longest slope towards
the S.W. If Wales were a new country, the shape of it would
suggest the glaciation which is proved by a closer search.
From Dublin to (lalway the country is boggy, low, and
flat. A depression of 500 feet would sink it beneath the
Atlantic.
The first glance at the country about Galway shows the
action of ice. Large boulders piled and scattered broadcast
evevvwhcrc, low vouii(1(m1 hills, lieds of elav stuck full of
CONNEMAKA — GALWAY AND WESTPORT CURVES. 21
rounded stones, wails built of boulders — all suggest glacial
denudation on the large scale ; but no high mountains are to
be seen to account for land-glaciers. Close to the town, on
the beach, but above high-water mark, numerous ground rocks
show smaller ice-marks distinctly. The scores and grooves
point from N.E. to S.W., or thereby. At Blachrocic, the
favourite bathing-place, these guides point out into Galway
Bay, where the track is lost in the Atlantic.
About three miles to the west of the town the sea has
undermined a long round-backed hill. It is broken short off
at the end, leaving a perpendicular cliff about 50 feet high,
with a beach of boulders under it. The hill is called Cnoc-a-
Blilaka or Blake's Hill, and the point Cnoc-na-Carrig or the
Hill of the Stones.
The sea-cliff is a section of the boulder-clay, and ice-work
of the most striking character. A matrix of hard, compact,
bluish-yellow gray clay is stuck full of rounded " subangular"
blocks ; some are three or four feet long, others as big as a
man's head, others small, like apples, nuts, and peas ; and the
beach is made of them. They stand out from the clay where
the rain has washed it down, like plums in an iced pudding.
Every stone is scratched, grooved, and scored ; and the marks
are as plain as if they had just been made with rasps, files,
and sandpaper. ]\Iany surfaces are polished so brightly that
they shine in the sunlight. New-fallen stones, stones i)i situ,
and stones picked out of this cliff, all are polished, ground,
scored, and scratched in many directions, and on all sides.
There are specimens of red and yellow, coarse and fine granite,
fossiliferous dark blue limestone, and other rocks. The hill is
a museum of transported stones, gathered long ago b}' wander-
ing ice, and pushed into Galway Bay.
Near the place, specimens of the same stones, weathered
22 BALTIC CURRENT — BRITISH ISLF.S — IRELAND.
and water-worn, may be compared with these boulders. In
the dykes, where mountain limestone has been weathered,
fossils stand out in relief, showing the minutest detail. In
the cliff where the ground surface has been preserved from
weather by hard clay, fossils can only be distinguished by
tlieir colour. On the beach aw^ay from the cliff, rolled pebbles
are rounder and dinted ; the scratches have disappeared.
Wliere these sea-rolled stones have been weathered, they
retain the finished oval shape which sea-waves gave them,
after ice had blocked them out. The waterworn and the
weathered surfaces are wholly different from the old ice-
mark. Here then, at the most western coast -line of
noi-thern Europe, are the works of ice ; and here too the
prevailing S.W. direction of the wind is pointed out by grow-
ing trees.
If tlie direction of the wind is pointed out by a weather-
cock, and its prevailing direction by a bent tree on a hill, it is
equally well shown on a plain by sand-drifts or grass tufts.
If the direction in which a large ice-system moved is well
shown by grooves upon hill-tops, it is equally well shown
by grooves on a wide plain, where there are no high hills to
interfere with the general movement. So at Gal way the stria?
tell of a general system of glacial action, not of local glaciers.
On the tops of low hills, by road-sides, in fields, and generally
in the neighbourhood, whatever the kind of rock laid bare
may be, grooves have a general N. E. and S.W. direction.
One end of a long stick laid in a groove points N.N.E. or
N. E., and the other end aims a little to the outside of Black
Head, past tlic end of tlie Chii'e mountfiins.
This direction agi'ccs ncitlier with tlie slope of tlie country
ihii- with (he llow (iT ri\cis, iioi' wilb the ]uvseiit run of the
lilies; it (inly agrees with a- system *>\' lai'gi' hnlldws which
CONXEMARA — flALWAY AXD WESTPOHT CURVES. 23
cross Ireland, and are marked as valleys and sea-loclis on the
best Irish map.
The movement was not a result of sliding, for there are
no lulls to the N.E. of Galway from which ice conld slide.
This is no pai-t of a local glacier system, but there are clear
traces of the general movement, which also left its marks on
Scotland, Yorkshire, Wales, and Devon.shire, as will be shown
below.
A good map of Ireland shows the large grooves wdiicli
coiTespond to the ounces on the map. The northern and
southern end of the country is crossed by diagonal valleys,
whose general direction agrees with that of the IMenai Strait,
the Caledonian Canal, the Forth and Clyde Canal, and other
Scotch and English hollows. The ice-stream certainly floated
over the low grounds of Ireland, and part of it poured out
between the mountains of Clare and Connemara, through
Galway Bay.
Curves drawn from Galway in the direction pointed out by
ice-grooves upon hill-tops near the town, cross Ireland by way
of Canick-on-Shannon, the end of Lough Conn, and north of
Belfast Lough. They pass between the Mull of Ceantire and
Portpatrick, into the Firth of Clyde. In Ireland they pass
over a low flat coimtr}^, in the neighbourhood of lakes, canals,
and lines of railway. In Scotland they join a system of large
wide glens, wdiich traverse that country. Let this be called
the Galway curve, and traced back as far as it will lead.
Travelling northwards, other curves should be crossed if
tliis were a general movement. From Galway to Oughterard,
the road .skirts the north-eastern side of a low range of hills
in MoycuUeen, and coasts Lough Corrib. The hills on this
side are all rounded and strewed with large wrecked boulder.s,
but on the other side they are steeper, and the rock is bare.
24 BALTIC CURRENT — BRITISH ISLES — IRELAND.
The low coimtrj" beyond the lake, the shores of the lake,
and the lake itself, all are strewed with enormous stones and
patches of clay. Low down, boulders and gi-avel are every-
where, but the hill-sides are generally rock with a thin cover-
ing of soil or peat, or bare.
Where limestone is the foundation of the country, the
general outline of glacial denudation alone remains. Tlie
rock is furrowed and drilled into the most fantastic shapes,
apparently by water and weather.
When granite is the rock, the general form is nearly the
same, and the surface is still weathered. Crystals stand
up separately, veins stand out and run over the backs of
rounded tors and ridges. The veins are sharp and angular, but
the rocks are all round like Devonshire tors, and the hills to
tlie very top retain shapes into which ice ground them ^ — ^ .
Beyond Oughtcrard a road leads over a low col down into
a wild ti'act of country where the rocks are bare or smothei'ed
in bogs.
Tlie surface is generally weathered, so that stria^ and
gTOOves are hard to find, but wlien the morning sun is shin-
ing across the grooves, the marks come out clearly, as blue
lines of shadow on long ridges of warm gray granite, which
raise their backs in the dark moor.
Low down, at the sea-level, and on liills about 400 I'eet
high, the direction is from KN.E. or N.E. to tlic opposite
points.
At Furncss Lahc, which lies close beneath the IMoyculleen
Hills, grooves, ridges of granite, and trains of large stones,
]ioint the same way.
The cut was sketclied from nature. It shows ]»art of the
Moyculleon Hills, on wliicli ice-marks arc jilaiii, and part of
(lie Idw ((iinilrN-, which is sirowod willi drill and trains of
CONNEMARA — GALWAY AND WESTPOET CURVES.
25
blocks. The district is one of the best samples of an ice-
gi'ound country that is to be found in Western Europe.
These grooves do not aim at the hills ; they run along the
hill-foot, and aim at a large groove ^— ^. A pass about 500
feet high.
At Sgriob Bridge the direction is still the same ; at Inver
Lodge, at Luggccn Lough, at Lough Corrib, the low grooves
Fig. 71. Tr.4in of Blocks near Furness Lake and Moyculi
Drawn from natuie on the wood, 1S63. (Reversed.)
all point nearly one way. They do not aim at moimtains
which surround the low bogs of Connemara and the sea-
lochs, but poiut at glens which lead to the low countiy beyond
the hills, and to great lakes. One of these mountains stands
alone. It goes by the name of Cnoc Ourid, and is about 1300
feet high. It is about two miles from Slian Folagh, which is
X.KE. of it, 2000 feet high, and the end of the Mam Turk
range. A valley more than 1000 feet deep separates Cnoc
Ourid from the higher range, and Shan Folagh is joined to
26 BALTIC CURRENT — BRITISH ISLES — IRELAND.
Mam Turk by a col. To the S.S.W. is a third isohited hill
called Ciioc Mordan, and about 1100 feet high. It is separated
from Cnoc Ourid by a boggy plaiu more than four miles wide,
and but little above the sea-level. To the S.E. is a range
of low hills in Moycidlec7i, which makes one side of a block of
high land, and is separated from Shan Folagh by the glen oi'
Oughterard.
These four high points are well situated for ascertaining
the direction of the general movement, which has so ground
and altered the whole face of this country.
Cnoc Ourid. — In moimting Cnoc Ourid from the north
side from Eusheen Lake, the rock is seen to be upheaved and
strangely contorted. It contains fragments of other rocks,
broken and rounded, and is folded about the fragments in
waving lines. Ice polished the rock across the edge of the
beds, and the surface has been weathered so as to leave the
structure of the rock in low relief Upon ridges and domes
of this gray moss-grown gneiss large boulders are perched.
At the foot of the hill deep grooves are well preserved,
and they point at Mam Turk' and Shan Folagh, past the
shoulder of Cnoc Ourid. Here then are the works of cold and
heat — contorted gneiss, upheaved and altered by fluid granite,
ground down by ice, and weathered afterwards. Five hundred
feet up the hill the rocks are all of the same pattern as those
in the plain below, and on them rest large angular blocks of
gneiss, and smaller boulders of various hard rocks — quartz,
greenstone, etc. These last must have travelled far. Eight
hundred feet up is a large block of gTay trap freshly broken,
and near it is a block unbroken, and perched upon a rounded
saddle of gneiss. Fleveji hundred andsixty feet u]), on the top
of the northern shoulder, striif and grooves arc well ])Vrscr\c(l
on gneiss. They point N.iX.E. at the v\u\ of tlie liigher range
C'ONNEMARA — GALWAY AND WESTPOET CURVES. 27
beyond the valley, aud 8.S.W. out of Camus Bay at the
Atlantic. These marks are unlike those which are made by
river-glaciers ; they are like writing made by a shaking hand,
for they waver and vary slightly in direction, so as to cross
each other at a small angle.
Thirteen hundred feet np, by aneroid barometer, on the top,
the view is wild and desolate. Lakes appear to lie in every pos-
sible direction, in a wilderness of water, stone, and bog, which
fades away into a shallow sea, full of low islands, stones, and
rocks, scattered broadcast in bays and sea-lochs. Galway
Bay is seen over Moyculleen ; Lough Corrib and Lough
Mask, and a wide stretch of low land, are seen past the
shoulder of Shan Folagh. There is no hill far or near to
accomit for glaciation by land-ice at this spot and in this
direction, and yet ice-marks are there, and well preserved. A
stick laid in a groove points S.W. by S. at the shoulder of
Cnoc Mordan, out of Camus Bay, at the sea-horizon, and N.E.
by N. through a notch in the hills, at a sea of lakes and bogs
bomided by a land-horizon as iiat as the sea. The notch is
the col which joins Shan Folagh to the Mam Turk range, and
the nearest hill-top of equal height is beneath the horizon, if
not beyond the sea. Descending the hill on its eastern side,
a block is perched at 1200 feet; and near it, where the wood-
cut was sketched, a solitary goat had perched himself upon a
saddleback of gneiss. His family and friends were scattered
about pickmg up a scanty supper amongst the bare rocks.
Tliey kept peering at the stranger, bleating, stretching their
long necks, wagging their gray beards, and flourishing their
horns over the sky line. The click-click of a span-ing-match
between two old bucks was the only sound besides the sough
of the evening wind, aud tlie red liglit of sunset made tlie old
gray rocks and their gray inhabitants glow like fire.
28 rULTIC CURRENT — BRITISH ISLES — IRELAND.
It was a differeut scene when the block was dropped by
ice 1200 feet above the present sea-level, and when ice floated
over the top of Cnoc Ourid. Tliis hill is joined by a low col
about 500 feet high to a range of low granite and gneiss hills,
on the S.E. At the top of this col the grooves point N.E.
by N. over a wide flat moor, which leads to Lough Corrib
and Lough Alask. There is no high hill in that direction for
many miles. A line drawn on the map passes north of Bel-
fast. Patches of hard yellow clay are deposited in sheltered
hollows on this col, and these contain small boulders of Itlack
Fru. 7i. Perched Block on Rounded Tor, Cnoc Oikid, 1200 t'li t.
limestone, mica schist, very hard tra]», quartz rock, gi'ay
porpliyry, and other rocks which are foreign to this hill, l)u1
which may be found in the direction of the grooves. Tlw
limestone in particular is like rocks near Oiigliterard on the
low shores of Lough Corrib, and the tra}) is like Antrim
trap. The north-eastern slope of Uk- hill and of the col is less
steep than the south-western.
Cnoc Mordan, the second hill, is vww moic isolatt'd. It
makes the north-western horn of Camus Bay, and no hill of
tlie same height is near it.
At the sea-level the stria' are well seen ; they i»oint N.K.
by N., 8.W. by 8. Large granite boulders are scattered about
CONNEMARA — GALWAY AND WESTPORT CURVES.
29
ill the moor. One shaped like a chipped pebble, near Inver-
niore Lake, measures 18 x 12 x 9 feet, and many are still
larger. Ascending the north-eastern slope, the angle is less
steep than the south-western side of Cnoc Ourid. There are
rounded surfaces and perched blocks to the very top. At
GOO feet the grooves are N.W. by N. ; at 700 a groove points
N. and S.
r-^'-i^-^
^
Fig. 73. Perched Block, Cnoc Mordan, 1100 feet. (Rever.sed.)
At 1100 feet above the sea a great angular mass of granite
is stranded upon a shelf, like a boat ready for launching. It
goes by the name of Cloch mor Binnen na gawr — the big
stone of the goat's peak. A lot of bare-footed Celts, two pretty
girls, two men and a small boy, were clustered about when
the sketch was made ; while a party of fishermen out for a
walk took shelter from a S.W. breeze, and smoked under
the lee of a rock. Behind the stone, Cnoc Ourid and Shan
Folagh rose up to the N.E. beyond tlie lakes of Inver and the
endless Ijogs of Connemara.
30 BALTIC CURRENT — BRITISH ISLES — IRELAND.
Tlie top of the hill is flat, Ijoggy, and strewed with small
boulders, and every rock-surface is ground. Grooves are well
marked everywhere, tliough weathered, and their general
direction is N.KE., S.S.W. The hill is very like a small
Dartmoor. Granite tops, which rise out of the moss, are
miniature tors, with joints beginning to open and weather.
The work is the same though it is further advanced in Devon-
shire.
A great change has come over Great Britain since these
rocks were thus ground at a height of 1300 feet, and yet the
marks are so fresh that the change must have happened
recently. Granite weathers and crumbles, but these mountain-
tops upon which tempests beat, and where rain falls in torrents;
mountain-sides, where torrents gather and pour down after every
shower ; river-beds, lake-basins, and sea-margins — all retain
the marks of ice moving diagonally on meridians in a general
south-western direction over this corner of Ireland.
Shan Folagh (the Hill of Flesh) is the third hill in this row.
It is 2000 feet high by the Ordnance map, and by aneroid
barometer. The top is about ten miles from Inver Lodge by
pedometer. It is the eastern end of INIani Turk (the Eange of
the Boar), and the top is isolated.
At 800 feet on the south-western side the rcx'k is stratiticnl
gneiss, dipping at a high angle, and the whole outline of the hill
is rounded ; but the surface on this side is much split and
weathered. The hill is very steep. At the head of the glen,
near the col, the angle is 45°. Few boulders are to be seen,
and few gi'ooves ; but those which do remain at this height
point N.N.E. over the shoulder of the hill at the col which
joins it to the range, and S.S.W. out to sea past Cnoc Ourid
and Cnoc Mordan.
Tliey are ])arall('l to the dee]) glen below them, and to
CONNEMARA — GALWAY AND WESTPORT CURVES. 31
several chains of lakes which are seen in the plain, and they
correspond to marks on the hill-tops at which they point.
From this height it is easy to understand how brittle plates
of ice of great thickness, like those which drift about off
Lal)rador, might float and slide over low hills of granite in
the hollow between Mam Turk and Moyculleen ; for the wide
valley — six or seven miles across — seems almost a plain. In
particular, it is easy to see how ice-floes might split and
ground upon the tops of Cnoc Ourid and Cnoc Mordan ; score
them, break them, stick to them, pick up fragments, and drop
them in the lee.
Supposing these hill-tops to be awash in a frozen sea
moving south-westward, the stream and the ice which it
carried would curl round the hill-tops, as a stream curls round
a big stone, and it would spread out when it had passed the
Straits of Oughterard.
At 1450 feet the tops of Cnoc Ourid and Cnoc Mordan
sink below the sea-horizon of Shan Folagh, and at that level a
groove upon a rounded table of gneiss points S.S.W. over the
top of Cnoc Ourid down Camus Bay at the sea-horizon.
At 2000 feet, on the very top of Shan Folagh, the rock
is gray quartz traversed by white veins. The beds are nearly
vertical ; the surface rounded and polished wherever it has
not broken and split from weathering.
On the north-eastern side of the top, the rocks are polished
and scored in the most remarkable manner, and from their
hardness the surface is exceedingly well preserved. Great
flat tallies, sloping towards the N.N.E. at an angle of 54° or
thereby, are groimd perfectly smooth, and rounded off at the
upi)er edge. Grooves run upwards in various directions, from
N., N.KE., and N.E. by N., and they are xjeculiar. Some marks
are rounded dints, as if the polished rock had been struck and
32 BALTIC CURRENT — BRITISH ISLES — IRELAND.
ground at one spot by sonietliing wliicli was aftenvards pushed
over the hill-top. Bits of this polished surface are easily
picked out, for joints in the stone make it a sort of smooth
mosaic work.
Looking towards places at which these grooves point, there
is no higher land to account for this manifest glaciation. The
grooves point 2000 feet over Lough Mask, or 800 feet over
Slieve Patiy, or level at hills twenty miles off, over glens, and
through deep glens, and over the end of Killary Harlioiu-,
which shines like a glass amongst the dark hills.
These certainly are gi'ooves made by floating ice, whicli
grounded upon this hQl-top, 2000 feet above the present sea-
level, when the whole land was under water.
The whole aspect of the hills seen from this high station
is that of something ground at about this level. MoycuUeen
seems to be a rolling plateau of romided tops, like those which
exist in the valley. Slieve Patry is a block of high land
deeply furrowed by glens, but the top is a smooth even rounded
slope. Beyond it lie Castlebar, Lough Conn, Ballina, and
Sligo. In one direction only, to the northward, higher
mountains seem peaked ; but the northern line, when drawn
on a map from the top of Shan Folagh, passes through a deep
glen forty miles off, beyond Clew Bay. Standing upon glaci-
ated rocks 2000 feet above the sea, and looking at a horizon
54 miles away, it seems almost certain that these ice-groinid
Irish hills rose in the midst of an arctic current which
flowed amongst them and altered their forms. So here tlie
first impression suggested by the shape of the cnmitry is
amply confirmed by closer examination of details.
Glaciers. — A marine glacial period ending in a rise of land
should have produced land-glaciers, and local systems of
marks ; and these marks do in fact remain.
CONNEMARA — PxALWAY AND WESTPORT CURVES. 33
The col and corrie between Shan Folagh and Mam Turk
certainly contained a small glacier, for the marks are there.
The top of the col is bare ice-ground rock, and the glen has
the roimded shape of a glacier valley. There is hardly any
talus, though the rocks split easily. Looking downwards
from the steep slope at the head, the glen seems to fade away
into the boggy plain. There are few large stones in it, and
these seem to have rolled down from broken rocks above them.
Cnoc Ourid seems nearly to fill the mouth of the glen, and
Cnoc Mordan is seen to the right, over the shoiilder of Mam
Turk. Between them are Camus Bay and the sea-horizon
nearly level with the distant hill-tops.
The col was a sea-strait when Cnoc Ourid was awash,
and the glen ought to be full of wrecked drift dropped in the
shelter. It seems to have been swept clean. The hill-sides
are ground from top to bottom, for the glen is a trench dug
transversely through nearly vertical strata.
But when the mouth of the glen is reached, the small
river is found to have cut through a bed of boulders and clay
nearly fifty feet thick. A green hillock is found to be part of
a moraine, and most of the stones contained in the clay seem
to be derived from hills which make the sides of the glen.
Lower down, ice-ground rocks peer up through the brown
moss, and the river washes a grooved rock-surface, which it has
failed to spoil. But this moraine has been washed out of shape.
Shan Folagh was a sunken rock ; then awash ; then a low
island at the end of a point ; then a peninsula with small
glaciers at the isthmus ; tlien a hill in a plain : and then the
glacier seems to have come to a sudden end, for the moraine
stops short in the jaws of the glen. The glacial period pro-
bably ended when the land had risen to a certain point.
At the moraine-level, about 200 feet above the sea, the
VOL. II. D
34 BALTIC CURRENT — BRITISH ISLES — IRELAND.
low hills between Mam Turk and Moyculleeu, and those upon
the borders of Lough Corril), and near Galway, Ballina, and
SKgo, would be like rocks which now fill the sea-loughs ; and
ice might still drift and carry liouldcrs through straits which
are now county Galway, and the glen in which the road has
been made to Inver Lodge.
At the present level of sea and land, the Arctic Current
is shut out by Ireland, Great Britain, Denmark, Scandinavia,
and Lapland, and the Gulf Stream flows up in the lee. If the
sea were 2000 feet higher on this region of the earth's northern
surface generally, the Arctic Current would overflow the dam
which separates the Gulf of Bothnia from the White Sea.
Then the Equatorial Current might be driven elsewhere, and
then the climate would be changed.
When Celts named the "hill of flesh," and the "range of
boars," the " lake of stags," and similar places, they found other
creatures in Connemara than snipes and hares. When they
composed the long poems which Connemara peasants still
repeat, the pastime of their lives and the burden of their
songs were love, war, and hunting ; but before there were ele-
phants, elks, and men, to be hunted and smothered in Irish
bogs ; the wide Atlantic covered the whole land ; and marks
an eighth of an inch deep, made by floating ice on the highest
top of Shan Folagh, have not been worn out by all the rain
which has fallen there since the day of Finn MacCool,
MacArt, IMacTreunmor, and since Shan Folagh peered above
the waves.
Lcaca Donna. — Shan Folagh, Cnoc Ourid, and Cnoc Mor-
dan, being on one side of a strait, the other side is a gneiss
hill, called Leaca Donna, or brown slabs. It makes the
western corner of the block ol' high land in IMoyculleen,
the liighest point of wliic-h is about 1200 feet above
CONNEMARA — GAI.WAY AND WESTPORT CURVES. 35
the sea. The western face of this block is rounded, and
almost bare of soil and vegetation. From the road at Sgi'iob
Lake to the top is about three and a half miles.
At the head of Sgriob, Shan Folagh is seen to the north-
east as a romided, conical, isolated hill. Slieve Patry is seen
past the eastern shoulder as a block of hills with a smooth
sloping top ; and to the westward, in the Moyculleen range, a
wide rounded valley runs half a mile eastwards into the
hills.
About the lake in the low grounds loose blocks of granite
are scattered in every direction, and the rocks are all ground
and scored. The grooves at high-water mark at this spot run
north and south.
At the same level, a mile and a half eastwards, grooves are
well seen ; they point N.E., S.W., and cross the mouth of the
small glen, which seems made to be the habitation of a glacier.
If these grooves were made by land-ice they woidd point due
west out of the glen.
Half a mile nearer to the hills the ground is strewed with
the debris of a small moraine, which makes a curved sweep
across the mouth of the glen. It marks the spot where a
small glacier ended, at about the same level as the Shan Folagh
glacier. This moraine is washed out of shape.
In this sheltered nook a village built of boulders, fields
fenced with rounded stones, green corn, blighted potatoes, and
worm-eaten cabbages, show a better soil than bare granite
and wet peat, which make the plain.
The base of the hill on the right of tliis glen, up to 350
feet, is thickly strewed with large loose blocks. Above that
level — which would join Lough Corrib to the sea, make Moy-
culleen an island, and Ireland an archipelago — the ice-
ground hill is swept bare ; but every here and there perched
3G BALTIC CURRENT— BRITISH ISLES— IRELAND.
blocks riding on granite saddles hang on tlie steep hill-side,
where a good push would send them rolling to the liottom.
The rock generally is rough and weathered, but every here
and there a vein of hard quartz stands up half an inch from
the gneiss. The quartz surface is smooth, polished, shining,
and marked by sand-lines and scores. The edges of the ribs
are still angular. Elsewhere hard patches preserve their
smooth surface for a couple of square yards. At 700 feet
the grooves and finer sand-marks point N.N.E. and S.S.W.
along the face of the hill, past Slieve Patry, over Lough Mask,
at the Firth of Clyde in one direction, and out to sea in the
other.
At 1000 feet a well-marked groove on the top of a shoulder
points N.E. by K, S.W. by S., near Arran in Scotland, and at
the Irish Arran Islands.
At 1130 feet by barometer the hill-top is a boggy rolling
plateau, with low rocky saddlebacks peering up through
black moss. Sea and bog ; hills, islands, lakes and moun-
tains ; Galway Bay, Lough Corrib, and the low grounds of
central Ireland — are spread out like a map, and there is not
a hill in sight to account for tliis glaciation by land-ice.
In tlie foreground of tliis wild landscape a wild group of
figures completed the picture. In a dark wet hollow, where
a stream oozed out of a bog, a thin blue smoke curled up into
the sunlight. Two bare-footed, black-haired girls, dressed in
patched red garments, shaded their eyes from the sun, and
peered doubtfully at the intruder. Three men and a Ijoy,
picturesque and wild, unkempt, bare-footed, ragged, and polite,
paddled al)out in the black peat. Barrels, casks, noggins,
baskets, creels, peats, malt, a copper still, sweet worts, the
wonn in its tub, a pile of potatoes for supper, and the black
holes from whicli tlie whole gear had been dug, showed a
i
CONNEMARA — GALWAY AND WESTPOKT CUKVES. 37
poteen distillery in full work. The Ougliterard ganger — bad
luck to liim — found it out.
From the ice-period to the period of poteen in Conneniara
is a long time, but the weathering of gneiss during that time
has been less than half an inch ; for it can be measured from
the polished surface of a rib of quartz to the rough surface
above which it rises. Space could be turned into time if the
rate of weathering were known. Surely works of human art,
obelisks, pyi-amids, or sculptured stones, might give the rate
of weathering, and so fix the date of the glacial period in Ire-
land.
Thus, on four isolated liill-tops withiii sight of each other,
but far apart, at a height of 2000 feet and at the sea-level, the
Gal way curve is repeated in well-marked ice-grooves upon
fixed rocks in Connemara.
The loiddcrs which ice carried are very remarkable in
this district. They seem to spread like a fan from the pass.
Close to the road-side, near the police barracks at Inver, lies
a great block of granite (p. 10). It measures 36 x 12 x 10
feet, and it rests upon rounded granite, where it fell.
It is broken into seven pieces, which retain their positions.
The upper side is ground like other neighbouring surfaces ;
one end, the rest of the sides, and the fractures, are angular
and unground. It is evident that this great stone was a bit
of the granite surface of the country ; that it was lifted bodily,
carried some distance, and droj)ped where it lies broken.
Perhaps it broke when it fell ; perhaps it split afterwards.
It lies in the jaws of a glen, which was a strait at the foot
of a rounded granite hill, Shan na Clerich (the Clerk's Hill),
which is about 400 feet high. The hiU is scored and ground
all over. Perched blocks are scattered over it ; but all about
it, and chiefly on S.W., or lee-side, enormous blocks of granite
38 BALTIC. CURRENT — BRITISH ISLES — IRELAND.
are thickly strewn. A great many of these are broken, and
most of them are roimded on one side or another. Some few
are rounded on all sides, and chipped at the lower edge, as if
they broke them when they fell down. Sometimes they are
ranged in rows, which point N.E. by N. over the shoulder of
the hill towards the low pass, through which the road leads
from Oughterard.
Nearly all these blocks rest upon bare rock, but here and
there the rock is covered by compact hard beds of gravel and
reddish clay. The gravel is chiefly granite, but the clay
encloses small boulders of greenstone, and quartz rock of
various kinds and coloiirs. These are foreigners, for there are
no rocks of the kind within ten miles at least. Where the
clay has been moved to make roads, the granite-surface beneath
is perfectly preserved in many places. Crystals of quartz and
felspar no longer stand out in relief to give a firm hold to
hob-nailed boots, but crystals and strings of harder rock are all
smoothed to a fine polished surface ; upon this grooves which
a pencil fills and finer marks remain. Hob-nails make abnost
as clear a mark when they slide upon the rock. The polish
on the pillars of the Colosseum is not better preserved, and
the marble of the Parthenon is far more weathered than this
ice-ground Connemara granite where protected by the clay,
which helped to smooth it. All these grooves, great and small,
high and low, point nearly N.E. by N.
There can be no doubt that ice scraped along, carrying
boulders and grinding rocks, and the rocks show whence some
of these boulders came ; others may have come from AntriuL
Amongst the large blocks, and trains of blocks, ridges of
granite of the same kind rise up in the moor. They have
strange weird shapes, and suggest gray monsters crawling
eastwards nut of the moss. They are the sides ^ — v of rock-
CONNEMAKA — (JALWAY AND WESTPORT CURVES. 39
grooves ^ — ^, in which peat-moss gathers and grows, and the
dragons and giant caterpillars and maggots are tors and
ridges, ready to be jointed, quarried, and carried away to
make granite boulders, for the stone is already split.
Some, as in tlie woodcut (p. 7), are actually moved, and
left loose in the place where they were first ground into
shape, and then quarried and pushed out by ice. Tliese are
chiefiy to be found at the north-eastern end of ridges, where
they were struck and shaken.
At other places the angular nest, from which a stone has
been pushed, lifted, or dragged, remains, but the stone has
disappeared. At some places the granite has been worn so
near to a joint that it can be split off' in thin layers. Else-
where it is solid, and the fracture is never round like the
worn surface.
All over the moors and bogs, chiefly on the lee-side of
isolated hills, these blocks are scattered and ranged in rows.
Many are of enormous size. One, near Inver Lake, measures
14 X 11 X 12 feet, and nnist weigh about 130 tons.
Cloch Corril (p. 19) is still larger ; it stands on the bank
of Lough Corril, and it probably came from Shan Folagh,
ten miles off. The circumference is G6 feet, and the height
about 24. The upper side is roimded, the under hollowed
and smoothed. The sides are angular, and coincide with the
natural fractui'e of the stone, for it is splitting up and falling
in large masses, which lie about it, and the rain drips through
it into the hollow beneath. It stands u]3on a romided table of
granite, on which straw is laid ; it is smoked, for fires are
burned beneath it ; and it is rumoured that malt dries there.
The lake is a rock-basin full of big stones, and the strite upon
its islands point tlie usual way, towards Cnoc ]Mordan and
Mam Turk. It is a beautiful spot to look at, and " a fine
40 BALTIC CURRENT— REITISII ISLES — lEEL.VND.
place for brewing poteeu," as a native remarked. It has a
bad name, so it is seldom visited. It is haunted by " each
uisge," the water-horse, and other dangerous beings — so few
people go there except to fish or brew spirits ; heather, blae-
berries, ivy, yew, holly, birch, and oak scrul), flourish upon
the islands ; white goats caper about amongst the stones, and
nibble the bark of the trees ; it is a green spot in the midst
of a wilderness of brown boggy moor, sun-ounded by the dis-
tant blue hills of the "Joyces' country," and the Twelve Pins
of Conneniara. The chief feature in the landscape is the old
gray boulder, M'hich is very like one upon the Unteraar
glacier (vol. i. p. 153). That stone has given shelter to many
a tourist — to Saussure, Forbes, and to masters and students
of glacial action. The Swiss stone rests on ice which is grind-
ing rocks ; the Irish stone upon rocks which are ice-ground.
Ice is carrying one, and ice certainly carried the other.
Sucli a stone must have a legend, and thus the biggest
boulder in Connemara has one of its own. It was the play-
thing of a Celtic hero, Corril, who crushed his fuiger and left
tlie mark in the hollow stone, when he threw it from IMam
Turk at IVlordan, the father of Goll INIacMorna, who stood on
liis own hill about ten miles off.
There can be no doubt that this tract was ground for a
depth of 2000 feet by ice moving from N.E. or N.N.E. to the
opposite points. All marks, from general forms of hill antl
dale, down to minute sand-lines, tell one story. If this be
glacier-work, the snowshed was beyond Scotland. If it be
the work of a current with floats, similar Avork is going on in
corresponding latitudes M'itliiu ten days" sail.
Surely it was sea-ice whicli carried Olocli Corril (j). 19),
and set it gently down <m its base. Suicly i( was a fusible
rait wliicli ]ilant(Ml u block ujion end like a ]»illar on a big
CONNEMARA — GALWAY AND WESTI'ORT CURVES. 41
stone pedestal at the foot of Cnoc Ouricl, on a rock in the
midst of a bog. When the sketch was made on the wood,
two gray horses stood beside the stone, lazily switching their
tails to keep away a host of flies. Wlien it was gently placed
upright on its base, sea-horses, seals, and bears, may have
played about the hill-sides, where goats now browse. There
are "seal-meadows" further south on the opposite coast.
These sea-monsters, and the end of the Irish glacial
period, may have been seen by the ancestors of the men who
are now migrating westward after the glacial period. Celts
owned the land at the earliest historical date, the ice-marks
are as fresh as Eonian and Egyptian sculpture, and all Celtic
tribes in the British Isles, from Cornwall to Sutherland,
people their lakes and seas with water-horses, water-bulls,
dragons, and sea-monsters. Their popular tales speak of ice-
mountains, of hills of glass, of islands with fire about them,
rising from the sea ; of wicked cities and plains sinking
beneath the waves.
According to a Connemara man, Finn and his warriors
once chased a deer till they lost their way, " and all but two
were frozen and starved, so that they died of cold and
starvation." The survivors did many marvellous feats. If
these myths be of native growth, they must surely be tracks
which a recent glacial period has left on human minds. The
belief in mythical sea-monsters, large deer and birds, is fresh
and vivid, plain and clearly marked, amongst all ancient
Britons, as are the ice-marks upon these Irish hills and
plains in Connemara,
CHAPTER XXX.
BALTIC CURRENT 3 — BRITISH ISLES 3 — IRELAND 2 — CONNE-
MARA 2 — NORTH-WESTERN, AND NORTH-EASTERN COASTS —
GALWAY, WESTPORT, AND DERRY VEAGH CURVES.
The broad trail of the Galway curve is well marked.
The fact of glaciatioii iu a certain south-westerly direction
for a height or depth of 2000 feet, and a breadth of thirty
miles, being established at one point on the western coast of
Ireland, the next step is to look to the configuration of the
country. Books on geology — The Antiquity of Man by Lyell,
Jukes' Manual of Geology, and other works of authority — show
that the sea-level has varied greatly on Irish hills. Shells
are found high \\\\ and peat, which grows on shore, is found
below low-water mark ; and for numerous reasons it is taken
to be an established fact that most of Ireland was under
water after its hills had assumed their present general form.
If the contour line of 500 feet is traced, and assumed to be
an ancient sea-level, Ireland becomes an archipelago. Fifteen
groups of islands are disposed about a central strait, which
ends at Galway and Oughterard. If the level of 2000 feet,
the top of Shan Folagh, is taken to be the sea-level, very little
of Ireland remains. (See map. Antiquity of Man, p. 276.)
The western coast at the present sea-level is indented by
a series of bays running northwards and eastwards — Donegal
Bay, Clew Bay, Galway, Shannon, Dingle, Kenmare, Bantry,
etc. Most of the high mountains to the west are on promon-
GALWAY CURVE. 43
tories which separate these bays. If these western mountains
were groups of islands stretching along the lines of movement
already mdicated, it is easy to understand how a north-eastern
current ran amongst them, and to know where to look for
conspicuous ice-marks upon Irish plains and hill-tops.
The nortli-eastern corner of each block of high land ought
to bear the strongest marks of ice drifting south-westwards ;
and curves drawn through glens which were sounds and straits
ought to bear reference to main lines drawn by greater streams
in the widest openings.
The course of a rivulet passing through a row of stepping-
stones ; the run of larger streams which split and join in pass-
ing a salmon weir; the run of the ebb in a sea-loch studded
with rocks and islands ; the curves in the tail of the Gulf
Stream where it passes northwards and eastwards amongst
islands off Hammerfest and the north of Norway ; the Medi-
terranean Current off Gibraltar ; the Baltic Current off the south
of Sweden, and the windings of the Arctic Current off Green-
land and North America, all are illustrations of the move-
ments of an old Arctic Current striking upon Irish hills.
The theory is simple ; but a theory, however formed, is worth
little till it has been well tried. If it stands examination, it
rises in value by every new test.
North-ivestern coast. — A curve drawn below the 500 level
from Galway to Newport joins Clew Bay to Galway Bay, and
cuts off a large block of high land which would be a group of
islands if the sea were less than 500 feet above its present level.
The Twelve Pins of Connemara form part of the group.
Eoads wind about amongst the mountains in this district
and follow the lowest levels, towns are built near the coast ;
so ice-marks which occur near roads and towns must either
•be marks of glaciers sliding from the hills, or of streams flow-
44 BALTIC CURRENT — BRITISH ISLES — IREL.VND.
ing ill shallow soiuids. If a main stream flowed in from the
N.E., about Belfast and Londonderry, it must have found its
way out by glens, into bays, which open to the Atlantic at
Galway, Westport, and Donegal. Ice-marks do follow curves
which agree with this supposed movement of an arctic current
amongst islands.
In travelling from Oiujhtcranl to Clifton, the road leads
along the foot of Mam Turk and the Twelve Pins of Comiemara.
If ice-grooves were made by land-glaciers, they would cross
the road ; if they were made by floating ice and an arctic
current this was a place for an eddy in the stream, and the
grooves should run along the foot of the hills.
At the foot of Mam Turk, in the lee, there are thick beds
of glacial drift ; the large boulders are buried in moss, and tlie
rocks are hidden, but the hill-sides are ground to the very top.
On Hearing Ballynaliincli, after passing a deep glen, the rocks
appear, and grooves point back at Shan Folagh, the promontory
round which a north-eastern stream 500 feet deep must have
turned to reach this spot. The marks run nearly E. and W.
At Ballynahinch Lake, near Canal Bridge, the rock is slate,
and much contorted. The ground surface is well preserved
near the road, and the grooves point E.N.E. along the foot of
the Twelve Pins at the shoulder of INIam Turk. In the other
direction, they point out to sea over the lake, wlierein fisher-
men disport themselves and salmon plunge.
At Clifton, a glen, a hill-side, and well-marked grooves,
point E. and W. out of a de(^p gorge in the mountains at the
sea.
Further on, in a wide boggy plain, a rounded boss of whin-
stone has grooves which point N.W. and S.E. at the end of
the Twelve Pins. Thus, in passing along the foot of the hills
on the lee-side, the grooves turn gradually, till at the point
GALWAY CURVE. 45
they cross the main current at right angles, as eddy-streams
do behind a stone. (See vol. i. p. 127, and map, p. 496.)
From this place the road bends back, and passes up-stream
into a deep gorge at Lcttcrfrack. Here large mounds of boul-
ders are piled below steep mountains, which are swept bare
higher up. A few large boulders are strewed about the foot
of the hills which border Kylemore, and woods of birch and
other trees fringe the lakes, and explain the name of Great-
wood. At the mouth of this pass the drift is arranged in
terraces, and these look like sea-work.
The valley divides the Twelve Pins from Ben Coona, and
after passing a low col the road descends about 300 feet to
the Killaries.
Here a very small depression would join the sea to Lough
]\rask, and make the hills a group of long islands separated
hy narrow sounds.
Up to 700 feet these hill-sides are certainly ice-ground,
and they seem to be ground to the top in the direction of the
valleys. Low down, the rocks are strewed with boulders ;
high up, they are swept clean.
At Lccnan the road comes to the end of a long sea-locli,
and runs up-stream in a deep glen in the direction of Castle-
l)ar and the Ox Mountains, N.E. by N", At the head of the
sea-loch is a mass of drift packed in level terraces.
From Leenan the road follows a deep gorge, with steep
hills on both sides. On the right, cross-glens run far up.
A few moraines cross the mouths of these glens. The rock
is Silurian, a series of beds of conglomerate ; mica-slate and
clay-slate much upheaved. Wliere the road passes out of
the glen, at heights of about 600 and 700 feet, ice-gi'ooves are
exceedingly well preserved on blue slate. The bottom of the
glen elsewhere is full of drift. Here, near the col, the rock is
46 BALTIC CURRENT — BRITISH ISLES— IRELAND.
bare, or covered only by peat. Torrents have cut a few shallow
angular trenches in the steep hill-sides, but here, at the top
of the pass, is evidence of a current 700 feet deeper than the
present sea flowing in from the low centre of Ireland. The
grooves are clear as well-preserved sculpture on a slate
tombstone a year old, and in ascending the hill they turn
gradually round till they get clear of obstructions, and point the
same way as the high Shan Folagh grooves already described.
At the bridge they point E.N.E. over the shoulders of a
hill at the head of the pass.
At 300 feet, a little further on, KE. at a notch. At the
head of the glen, 700 feet, they point N.E. by N. over every-
thing at the Ox Mountains twenty -five miles away and
beyond a glen.
A glance at the map shows that in this district minor
valleys all agree with these marks. From large and small
grooves it seems that the stream, which ran out by Galway
and Oughterard, split upon the hard block of land which is
now the Twelve Pins of Connemara, and glanced off north-
westwards through the Killaries and Kylemore.
Looking back over Slieve Patry, which makes the north-
eastern corner of this block, the outline is smooth and the
slope small, thoiigh the outline is along the strike of strata
which dip away from the ridge on both sides. It seems clear
that little weathering or river-work has been done amongst
these hills since they were last ground by floating ice.
On leaving this glen the road passes across the su])posed
stream, and over a plateau varied by ridges of low hills,
strewed with large blocks.
Near Wcstport these become very numerous. The whole
country is covered with big stones, and wherever the peat
has been cut away the drift appears.
WESTPORT CURVE. 47
Many stones are scored and grooved, walls are museums
of transported stones. Eed sandstone, gray and blue and
black limestone, white quartz, coarse conglomerates, whin-
stones, grits, and granite, are piled up in houses and fences ;
and no ice-groove in the neighbourhood points at the holy
Croagh Patrick, which towers up 2510 feet on the left. It
must have been a tall island when the rest of Ireland was
nearly all drowned.
At Wcstport the head of Clew Bay is reached. A curve
drawn KK, or thereby, 500 feet above the sea-level, passes
up a valley to Castlebar, through a gap in the hills at the end
of Lough Conn, past Ballina, over a flat country to Sligo, and
so through Donegal Bay to Lougli Foyle. (See vol. i. p. 232.)
It cuts off two blocks of high land ; one which ends in
Achill Head, and a second to the north of Donegal Bay,
which ends about Letterkenny and Eossan Point. Let this
be called the " Westport curve," and followed wherever it will
lead.
Westport curve. — If a stream ran in by Lough Foyle, out
by Donegal Bay, branched off through the gaj) at Lough
Conn, between the Ox Mountains and Croagmoyle, and struck
upon Croagh Patrick, the northern shore of Clew Bay would
be in the lee, and the rush would be at the narrows at the
end of Lough Conn ; at Westport ; and at the end of Donegal
Bay. The western mountains — Achill, and those near that
island — would all be sheltered by hills to the east. The road
to Achill is in the supposed lee, and the country supports
theory.
The whole of the northern shore of Clew Bay is thickly
covered by drift, and the hills are clothed to the top with
heather, so that the rock is hidden. The bay is a wide arm
of the sea studded with islands. These seem all to be of one
48 BALTIC CURRENT — BRITISH ISLES — IRELAND.
pattern. They liave rounded slopes towards the head of the
bay, and many are broken short off to seaward. The drift
upon the mainland is piled up in great heaps, mounds, and
beds. Many of the stones are a very coarse conglomerate of
white quartz pebbles, as large as pigeons' eggs. Where these
have been long exposed the cement weathers out, leaving
surfaces wliich resemble a modern sea-beach. But many sur-
faces have been ground, so that one front of a bed of pebbles
is flat and smooth, while the sides are round. Amongst these
are specimens of gray mica schist, red sandstone, and other
rocks, imbedded in hard yellowish clay.
Acliill Island, the Isle of the Cell, is separated from the
mainland by a narrow shallow sound. The low grounds are
covered by very deep peat-mosses, in which bog-pine and bog-
oak abound. Beneath the peat are thick beds of boulders
and clay. Several large hills occupy the rest of the space,
and these end in steep slopes or perpendicular sea-cliffs.
These liiUs have the usual long north-eastern slope and
rounded forms, and piles of drift-like moraines fill up the
ends of mountain hollows. Where rocks do appear they have
the shape of ice-ground rocks, and some few have grooves,
but bare rocks are hard to find in Achill. Crnachan, 2222
feet high according to the survey, and 2200 and odd by
observation, is the highest point.
On the eastern shoulder, at GOO feet, a rock-surlace, very
much weathered, is exposed, and a deep groove, which can
stiU be traced there, points east and west. A few blocks are
perched upon rounded rocks at this spot, and higher up at
800 feet. These are clear ice-marks. At 1000 feet the
ground is covered with large loose stones, laid fiat and closely
packed. They are of many kinds. At 1500 feet stones still
cover the ground, but they are smaller, and some patches of
AVESTI'dljT (Tin'K. 19
yellow cl;iv iH-ip (uit. At the tup tlie gruuiul i,s still thickly
covered with large loijse rounded stones, and tlie roek-surface
is liidden.
To the castivards a small glen has been hollowed ont ot
the slope of the hill, and swept bare. A small lake has
formed beliind a mound, which seems to be the moraine of a
small glacier which once nestled here and swept a trench in
the drift. To the norlh tii.- hill has l)een broken. It has
a steel) scar[)ed face more than 2(H)0 feet high, ahmg which
men and shec]) can barely scrand)le, and at many places the
slopes end in sheer (dills.
The end of Achill is a ridge which projects westward into
the Atlantic. Sheep and shepherds scramble along the face of
the cliffs by paths on which even natives hesitate to venture.
Perched on the verge of this cliff, 830 feet above the Atlantic,
when the wind is high, the whole rock seems to shake and
([uiver. It is a grand specimen of ocean-work, and a striking
contrast to the ice-marks in Connemara. There everything is
round ; here all is angular, the hills are ground from above, Ijut
the clilTs are undermined and Ijroken from below Ijy the sea.
Even where l)lack rocks peer through broken white water off the
extreme point ; where the run of the tide is the strongest, and
Atlantic waves are of the largest size ; even there rock-f(jrms are
sharp and angular. Water- work and ice-work are very different.
On a fine morning after a westerly gale has Idown itself
out, great rolling masses of cloud gather and ground upon
these high western points. They seem to anchor themselves
upon the peaks and stretch slowly away to leeward, lODO
feet above the sea, ilropping .showers as they drift. Their
tall white heads roll upwards and shine like snow in the
sun, while the ribs and keels of these air-shijis, dyed blue
and pur] lie, cast deep indigo shadows on tlie heatlier. As
vol.. 11. K
50 BAT/nc CURRENT — BRITISH ISLKS — IRELAND.
these clouds now drift steadily and ground upon the hill-
tops, so ice once drifted and grounded ; and here, on the lee-
side of a group of hills, boulders which ice carried and dropped
are strewed, 2000 feet above the sea, at the edge of clifis
which the sea is now breakmg down.
Here, too, is evidence of the persistence of ocean-move-
ments which result from the earth's rotation, and from heat and
cold. Where ice-grooves of an arctic current pouit seawards
towards America, the Equatorial Current now brings tropical
seeds to land. The people constantly pick up "nuts," and
they are the "horse-eyes" and "brown purses" which are
the playthings of English children in Jamaica, " fairy eggs"
in the Hebrides, and " Ljusne sten" in Iceland.
In Acliill, according to theory, there ought to be drift in
the lee, and there is so much of it that rock-surfaces are
almost wholly concealed. At Westport and Lough Conn, at
the nortli-eastern end of this high ground, the rock ought to
be swept bare.
On leaving Westport the road passes up-stream over a
low hill about 400 feet high. It separates the bay from the
inland plain, and it stands in the way of a current flowing in
from the N.E. It is swept l)are of drift, and the rock is much
ground. Trees point from W.N.W. and show the usual run
of currents of air ; rock-ridges point W.S.W. out into the bay,
and E.N.E. up a wide valley at the Iom^ lands of central
Ireland. From tliis liill the road descends into a rich, well-
cultivated plain, wliich seems to be made of drift, for rocks
and large boulders are liidden.
At Castlchar rock-surfaces begin to appear, and they seem
to be ground from the N.E.
Thence to CuIIcn Lake the road passes over a tract of low
country, where numerous boulders, large blocks, beds of boukler-
WESTPOT^T CURVK. 51
clay in hollows, and glaciated rocks and ridges abound. Tlie
country is flat and boggy, but the block of high land of whicli
Achill Island forms part is close to the plain. The })lain is
about 300 feet above the sea-level. The hills are about 2000.
Ice-furrows run along the road-side, gradually sweeping round
the foot of the hill till they point at the narrows between
Lough Conn and Lough Cullen. Here, according to theory,
rocks at a north-eastern corner, on a weather-side, and in a
low pass, ought to be much ground, and swept clear of drift ;
and here in fact rocks are as bare as hill-tops in Scandinavia,
or the straits at Oughterard.
It is a beautiful spot. The road Avinds along tlie shore,
and passes between the two lochs, beneath gray rocks, amongst
which berries, heather, fern, and graceful birch-trees find
shelter and room to grow. Distant blue hills are min-ored
in the calm water, and beaches of yellow sand and mica glow
and glitter in the sun like gold and diamonds. High up, on
large bosses, ridges, and tors, great rounded boulders and
rocking-stones hang poised where legends tell that Finn and
his giants cast them, and a pretty salmon river curls under a
bridge and joins the lakes. It is a bit of Sweden planted in
the midst of Ireland, and the same agent has done similar
work in both countries. More conspicuous ice-work could
scarcely be found, and yet there is no indication of land-ice.
Large ridges, and grooves upon them, all point at low lands
along the course which was chosen to make a le'\''el road
through the pass which was a strait at the 500 feet level.
The lines come in from N. N. E. near the river, pass S. S.W.
through the strait, and turn gradually westward as they pass
round the foot of the hill, past Castlebar and over the plain to
the bare hill behind Westport. There the tall cone and saddle-
back of Croagh Patrick l^locks tlie way, and turns the course
irj BATTic rur.HF.XT — r-niTisH tslks — ihei-axt).
of currents of air ; it sccins in liavc tlirown tlie watcr-streaiu
westwards into Clew liay, Id juiu aiiotlicv Inancli wliicli came
in from Louj^li Conn to Newport ; and these two proV)al)ly
droi)ped tlieir burdens of drift in the lee of the hills.
From Balliua to Sligo the road passes u])-stream over a low
Hat country which is generally well cultivated. Large blocks
of stone and smaller bo\dders are scattered about, and stand
up like monuments in the green fields. AVherever the soil is
Ijroken glacial drift appears, and where rivulets have cleared
their beds, the rock-surface below the drift is ground. For
many miles the cone of Croagh Patrick may still be seen past
the shoulder of a hill of Ihe same A pattern, whieh rises west
of Lough Conn, and divides the glens which lead to New])ort^
and Westi)ort.
So two groups of hills in Calway and Alayo api)ear to
record that they were groups of islands in a i'rozen sea which
moved soutli-wcstward.
To tlic right is a block of high land winch reaches to
Knniskillcn ; to the h'i't are the mountains of Donegal Iteyoiid
the l)ay ; and in IVout is the deep gvooxc MJiich crosses Ireland,
and hol.h Donegal I'.ay and Lough Koyle.
According to theory, a N.K. current entered between Innish-
owen and lialiycastle, ami split \\]uni hills alxnit Knniskillen.
The Westjxirt lirancii ran down jiast I'.allyshannou and Sligo,
through Donegal L.ay, and branched dtf into (lew I'ayat Lough
Conn; the othei' Joineil a stream wliicli came in hy Lellast,
and ran out by w;iy of Lou!j,li Mask, Lougli Coirili, Oughterard,
and CJalway. IJotli came lioni Scotland. The I h'vvy and Done-
gal stream came along the north side ol' Ceantire ; the I'xH'ast
and Oalvvay stin^am came tVoni tJie l'"irlh of Clyde, and they were
kept se]»ai'atc by the mountains of Antrim and by 'Ceantire.
in ti'aAclling IVom l;<ill ushni, unit l„ Htm i.slillm lhc.se
WESTI'OKT CURVE. 53
two streams are cross(3(l. The south-western Lank of
Lough Erne is the block of higli land which stretches to
Lough Conn ; the north-eastern bank is low and undulating.
A depression of a few hundred feet would sink tlie plain, and
make these hills islands. They are beds of grit and limestone
nearly horizontal, and from Sligo to Enniskillen the hill-faces
resemble broken sea-clifis. At Enniskillen the eastern side
has the same form, but the low grounds about the foot of the
hills, and the hill-tops, are rounded. The lake itself seems to
be a rock-basin filled with mud, boulders, and water. If an
ice-laden current beat u])on the edge of a stratum of limestone
it would tend to make sea-cliffs.
From E)inishillcn to Lough Foyle the stream is crossed
again by a railway. The country is low and flat, thickly
covered with deep soil and beds of clay and boulders, and no
rocks are to be seen by a passing traveller. At Ballyshannon,
where a salmon stream worthy of Norway is cutting a drain
for Lough Erne through limestone, fossils are weathered out,
and the rock-surface is pitted like that of weathered lime-
stone elsewhere. In the plain the rocks arc hid, stria? can-
not be seen, but the general shape of the country remains,
and it tells of ice. Holluws and low ridges have one general
direction, and point from or towards the bays which here
approach each other and make Donegal a peninsula.
Erom Sf.rahanc to LeUcrhcnny the sea of rolling hills and
glens is crossed at the isthmus. Every here and there a
great round stone in a corn-field, a dam built of boulders,
a gravel-pit, or a bed of clay in a burn, appears to give
evidence in favour of ice-floats. So from the end of Lough
Foyle to Achill Head and Galway the evidence agrees so far.
At the highest point on the road between Letterkenny
and Strabane, 400 feet or thereabouts, the Ijoulders include
54 BALTIC CUKRENT — BRITISH ISLES — IRELAND.
granites of various sorts, gray ami -white (j^iiartz rock, and
traps of various colours. Many of these must have travelled
far : — some perhaps from the Giant's Causeway. The lines
point at Aberdeen, and the granites resemble Aberdeen
granites ; according to theory they may have come thence, but
there is granite close at hand in Donegal.
From Ldterkenny to Givcedor a coast-road makes nearly
half a turn round the north-eastern corner of the Donegal
mountains, or the weather-side of a group of islands.
On leaving Ldterkenny glaciated rocks appear at about
400 feet above the sea-level. Eidges run N.E. and S.AV., but
the rock is too much weathered for small marks. Further
on, at the turn, the rocks are swept bare and much ground,
but it is very difticult to determine the direction. Thence all
the way to Gweedor the rocks near the sea are glaciated, but
broken into low clifts. A range of lofty hills — Muckish, big
and little Ach, and Aracul — stand out from the Deny Veagli
range ; and on the top of the most northern momitain, about
2000 feet high, a bed of fine white sand is worked for glass-
making. It is hard to understand how it got there, or why it
has not been washed away. The road bends south-westwards
along the base of these mountains, which are separated from
each other by deep glens.
If these hills were islands in a north-eastern current, and
exposed to the Atlantic, the inn at Chcccdor would be at the
end of a sea-strait, and in the lee of the stream. The weather-
side has been swept clean ; in the supposed lee a large deposit
of glacial drift is piled at the end of the strait. The heap
crosses the glen l)el(>w the lake, and rises more than 500 feet
on tlie hill-flanks. Small rivulets have made sections, which
show tlicsct low hills to consist of sand, gravel, large and
.small boulders, all mixed coniusodly and resting upon sand-
DEIiRY VEAOH CURVE. 55
stone. The river wliicli drains the lake cuts througli the
mound in a wide gap which looks as if a glacier had ploughed
it out after the land rose. Many of the larger stones in these
mounds are scored. The sweep of the Atlantic and the
prevailing wind is from the S.W. If sea-waves dri^'en by
S.\Y. winds piled such heaps, these would be in the lee at
the north-eastern end of the range, wliicli in fact is swept
clean, so the evidence tells for movement from the N.E.
Aracul is the highest mountain in this tract. After
leaving the inn, glaciated rocks begin to appear close to the
foot of the hill at about 400 feet. The ascent from this side
is very steep. After passing over a series of cairns of
angular quartz blocks which seem to have fallen from the
hill, a steep slope of talus, angle 35°, leads up to the foot of a
large whin dyke. This stands out from the loose stones like
a great cyclopean wall. Xo better specimen of the works of
fire is to be found in Iceland. It runs south through the
hill. In that direction a quarry has been opened which
yields excellent crystalline white marble. It is fine and
white as that of Pentelicus.
At about 2200 feet these clifis are passed, and a steep
slope of stones, with patches of heather, grass, and moss like
green velvet, leads to the top. From this point, on a showery
day, with a S.W. wind, the march of clouds over the Atlantic
is seen in perfection. When a shower is coming, a low ragged
fringe Ijlots out the horizon to windward, and advances
steadily upon the mountain, seeming to eat up the coast-line,
the low country, and the lakes. Then a puff of mist like a
wreath of gray smoke sweeps up the hill-side, and then the
whole cloud sweeps round the top and a sudden darkness
^vraps everything as in a thick veil. The lower world
disappears ; the rain patters down and splashes against the
50 I'.Ai.rir riiiUKXT — lUiiTisii isi.ks— jkki.ami.
stones, and the wind sweeps jiast with ii nishinL; nnist' iik(>
tho sound of the sea. There is nothing Tor it l»iU to crouch
undei- a stone, and smoke the pipe of resignation. In ten
minutes the ck^ud passes on its way ; light (hiwns as suddenly
as it disai»peared ; eoast-line, plain, corn-land, hill and moor,
seem to grow out of the gray sea of mist. The sun wades
out into the blue sky, the tail of the cloud creeps over the
highest }>eak of the hill, the sough of the wind dies away,
and the shower and the (doud are gone.
If the cloud were ice, the wind an arctic current, and the
lain boulders, it is easy to comprehend how rocks would be
iiiaiked, and drift scattered.
(_)n the sides of this particular hill there is no vestige of
ice-work, i'or it is a l»roken ruin. Looking down from the
|M'ak, loose stones, which rains have freshly washed from tlu;
ennnbling sides, radiate in yellow winding strt^ams, like the
Hoods which carried them to lower grounds. This hill is
\\eathered. But lower down, rocks on cols have the familiar
ice-shape, and nearly alltlie lowei' hills to the south are mani-
festly i<;('-ground. On the very top of the highest peak of
Aracul one oidy ]>ateh of the oi'iginal siu'face seems to be
l»reserved. It is a hard gi'ay tpiartz rock alxmt three square
yards in area, and smoothed across Ihejnints. The surface
a]>i)ears to be scored ]\Mv by N., S.W. by S. ; tlie height is
24r.() feet above the sea.
This mark is uncertain, but about 1000 feet lower down ice-
marks are ])lain. On a col about 1500 feet above the sea-level,
iin a knob of hard gray quartz, grooves cross the col from 8.E. to
N.W., in the diniction which a stream would take if it (lowed
through (//riiiraf/h ixud l»i'anehed oil' seawards u])on the cone
of Aracul. In the glen at which lhes(^ groo\'es poini are hea])S
of broken stones piled coidusedly, as if swept there by stn^ams
i)i;i;i;v vkacii cl'uvi:. 'u
or ;i ^lacu'V. Ou tlie (.■ol are several lari^c rounded lumldi^rs
of granite, whieli eontrast slmngely with the angular gi-av
([uartz of tlic lii'dkeu mountains. One great granite pebhle is
nine feet long by six liroad. At a height of about 900 feet, in
tlie pass by the road-side, the rocks are hidden beneath amass
of boulders and clay, and the great bulk of the stones are
foreign to the rocks upon which they rest. At ilvi top of the
pass of Glenveagh, about 1100 feet on the side of Benduich,
are many well-preserved granite surfaces, upon which grooves
point E.N.E. over the shouhler of a hill, at the mouth of the
Caledonian Canal, in Scotland. Many jjerched blocks of large
.size are balanced upon these bare granite rocks. iJurns and
gravel-pits by the road-side sIkjw the whole of the low grounds
in this pass to be paved with drift beneath a carpet of peat-
moss, but the col is swept bare, and high up on the sky-line,
to the south, great stones are poised in ranks, as if the in-
habitants had ranged them there to hurl upon offending
Saxons.
The quartz hills to the north have none of these conspicu-
ous ice-marks ; they are weathered cpiartz peaks, but gi-anite
has withstood the weather, and the hills to the south are
manifestly ice-ground. On one side are talus, soil, and
vegetation ; on the other, bare rock and perched boulders.
Lower down on the weather-side there is little drift and much
glaciation ; jointed tors and long ridges abound, and the hiUs
are rounded to the very top. At Lough Veagh another great
pass runs S.W. through the hills, and here a patch of drift or
a moraine makes a dam and a beautiful lake. At the weather-
end of the next ridge a series of grooves point N". and S., at
an elevation of about 500 feet. Soon after this the north-eastern
end of the Donegal peninsula is passed, ami tlie direction of ice-
gi'ooves changes. They pointed across the stream at the vnd
58 BALTIC CUKKKNT— liltlTISll ISLKS— IKFJ.AND.
of the vn\'^{', where the streams split ; when the end is passed
they i)oiiit along the side of the ridge, and into glens whieli
converge about the head of Donegal Bay. The spoor seems
to record movements like those which are roughly shown on
the margin of the map (vol. i. p. 496).
Here, too, the rock changes — granite is left, flags are
reached, and heather and hog give place to gi'ass and corn-
fields. But still the old rocks, with their old-world inscrip-
tions, peer out all the way down to the sea at Lough
Swilly.
At the holy rock of Tohar-an-dvon, where sick pilgrims
resort from all parts of Ii'eland, from Scotland, and even from
America ; where a garden of planted crutches and walking-
sticks hears flowers and a foliage of hows and rags, the votive
offerings of those who believe that the holy well beside the
rock cured, or will cure, their ailments ; the old rock uj)on
which Irish kings were crowned in the olden time — is an
ice-ground tor ; and here in the low grounds the direction is
once more KE. and S.W.
So the trail is clearly marked for a height etpial to that of
the highest hills in the north and west of Ireland, all the way
from Galway to Gweedor, and the lines all aim diagonally
across meridians, northwards and eastwards, except at places
where a current would split or eddy behind an island, as the
wind now eddies behind the Irish hills.
Tlu'ee curves are thus started from Galway, Westport, and
1 )erry Veagh.
North-easter a cund. — The western coast gives aliroadclear
trail, and it points to the N.E. coast of Ireland. It was
crossed from Galway to Gweedor northwards; the next cast,
like a steady pointer's range, sliould be soutliwards, tlie
other wav.
WESTl'OKT CUKVE. 50
The north-eastern corner of Irehuid is ahout the Giant's
Cnuscivay. From Deny a line of rail leads over a flat, up-
stream to Coleraine, and the first high hill is at Ballycastle.
Looking N. E. from tlie Causeway, on a fine day, the land-
scape fades in the Sound of Jura. A north-eastern line
passes near Loch Awe in Scotland, and clears the land of
Ceantire ; a S.W. line passes over low lauds towards Ennis-
killen and Galway. The rocks of the district are basalt or
chalk, and the boulder clay seems chiefly to contain blocks of
basalt. But on the beach and elsewhere, specimens of various
kinds of granite, of a dark limestone, of sandstone, and of
gray quartz, are found.
Near the top of the cliff ice-striai are well marked upon
whinstone, near a wall. They point N.E. by E. along the
north shore of Ceantire, and S.W. by W. along the shore of
Lough Eoyle. In a field near this spot is a large wandering
block of trap, and near it are several boulders of sandstone,
greenstone, and granite, some of which are grooved. This
direction agTees with the run of tlie flood-tide, which splits
off the Giant's Causeway. One branch pours up Lough
Foyle in the old groove, the other passes outside of Innish-
owen, and so north in an eddy. A depression of 500 feet
would let the flood pour through Donegal Bay. Parallel to
the sea-cliffs, at some distance from the shore, is a line of
submarine cliffs, Avell known to fishermen, who get fish in
the deep water.
If heavy ice were now floating in the Irish Channel, and
grounding upon the top of this lower shelf, some 200 feet
below the sea, ice-floats would make parallel marks similar to
those which now exist on the top of the upper shelf, about
300 feet above the sea. If the upper cliff were under water
half Ireland would be submerged. If it were 2000 feet under
wattji', ami the sea ovi'V Shan Folauli, hiv^c bei;L;s, like those
which now pass Cape Farewell, luiiiht urouml at the Giant's
Causeway. If the depression was general in Europe, the sea-
way would be open to the polar l)asin. (See map, vol. i. p. 232.)
There can he no doubt as to these marks ; they are ice-
grooves crossing each other at a small angle. They are pre-
cisely the same in kind as grooves which are found on the
top of basaltic clifl's, within sight of glaciers, near the edge of
the Arctic Current, at the foot of Snajfell at Stapi in Iceland
(chap. XXV.) There the grooves point at glaciers, basalt, and
lava, and at the top of a volcano ; here they point at low
lands and sounds, where the tide still moves in curves ]iarallel
to the old ice-grooves. And here the ^\•orks of lire are as
manifest as they an; at Staffa and Stapi.
From BallycastU to Cushendal the road passes over a spur
of the Antrim hills, and reaches as high as 800 feet. The
higlier it goes the more drift there is, and at the highest point
the rocks are ground hut weathered. To the N.E. is the INIull
of Ceantirc, so this part of the coast Mas in the lee of the
Scottish Land's End, between two streams or tides which
passed through Lough Foyle to Donegal Bay, and through
Belfast Lougli to Galway Bay.
From Cushendal la Glcn<irm the road coasts along the
sea-margin beneath cliffs of chalk cap])ed with whin. The
contrast of white and l)ri)wii, with all possible shades of green
and blue and ]»urple, on land and st'a, and in the distance,
make these clitfs very l)eautiful. The l)eacli is c()m]tosed of
boulders, chiefly whinstone, but piidv granite is to be seen
here and there.
When rocks whos(f colours are so cons])icuous are thus
placed, transported IVagnieiits are like lliisflc-doM n which a
deer-stalker throws up to lind out the tlirection of a breeze
flALWAY (TRVK. 01
A liit of '• Tiisli liiiK'Stoii.'" used lo I'onn part of a cliihrs
imiSL'UUi, on the opposite coast ; a iliiit is a rare stone heyond
tlie Criant's Causeway. There are none on the opposite coasts
of Scotland — flints were buried witli their owners in Eoss-
shire and in Arran. Boulders on tlie opposite Scotch coasts
are chiefly gray quartz, like hills to the north and east of tlie
Hebrides. But if tlie south-western line is folloAved, Irish
drift is full of chalk and tra}). Professor Jukes says (Mdnvul
of (lfo](i(jij, p. G73) — "Chalk flints and pieces of hard Antrim
chalk are found in the drift in the counties of Duldin and
Wicdvlow, up to heights of one or two hundred feet, and along
the whole eastern and southern coast of Ireland, at least as
far as Baliycottoii Bay, on the coast of Cork."
The tides run both ways, but this drift went S.W., which
again supports a theory of a Baltic current.
Opposite to the Antrim liills at Clamh'hoyc, in County
Down, an isolated hill of slaty quartz rises upon the southern
point of Belfast Lough. The hill is ice-ground, and the stria'
at about r.OO feet point X.E. by N. at Arran, and S.W. by S.
at the shoulder of the Mouriie Mouiilaiiis, in the direction oi'
Gahvay. From "Helen's Tower," on the top of this hill, a
magnificent panorama includes the Isle of Man, and the
opposite coasts from the Mull of Ceantire to Cumberland.
Belfast stands at the head of a long lough, in a hollow
which stretches far inland. The hollow is liounded on the
X.W. by a range of hills, extending south-westward from
Lariie. These are of traj) or clialk, and wliere they are not
broken away in cliffs they are rounded. At 600 feet a large
wandering block of whin stands in a gTeen field, where it
must have been carried. At 1450 feet, on the top of one of
the.^e hills, aiKither largv l»]oek is ]ilaiited. It has lieeii sj.lit
by gunpowder, but the rounded forms of tin; fragments con-
C2 BALTIC CUIJRK.XT — nRITISII ISLES— IRELAND.
trast with the fracture, and betray the origin of the stone.
From this point the gi"ound slopes in all directions, and long-
heather slopes stretch inland towards Lough N"eagh. A long
search on these hill-tops failed to discover a rock-surface.
Some snipes, a grouse, a collie-dog, and a keeper were found,
and the latter, on l)eing questioned, exclaimed, " Wliat, in
heaven's name, do you want with rocks ? " Quarries in the
hill-side show that the rounded forms of these hills are due
to denudation, and the glen gives the same direction as the
grooves at Helen's Tower. The form remains, but the exposed
surface and all small marks have crumbled away.
Another hill of about the same height gave a similar re-
sult. On the side of Cave Hill a large quarry facing Belfast
gives a fine section of the chalk, with its dykes and cover of
trap. A thin bed of red and yellow baked flints divides the
two. The dykes appear to have cooled, and set at the sides
of the fissures through which the melted stone rose, and the
chalk in the walls of the vein of trap is hard and brittle as if
it had lieen heated.
Above the trap is a layer of loose brown earth, containing
numerous rounded stones, chiefly trap. The chalk from this
quarry is used for ballast, and ballast when done with is
thrown overboard ; ships from Belfast sail far, so a lump of
Antrim chalk on a beach must not he taken as evidence of
natural movement in the sea. Al)out 1000 feet up this hill
is a large rounded stone, different from tlu> rock beneath it.
At tlie top, 1300 feet, are more loose stones, but the rock is
liidden. The sea-face is a cliff The chalk has been under-
mined, and the trap has split off and sunk down like the
UntUa-eliff in tlie Isle of Wight, Looking towards central
Ireland from tliis liill-to]), tliei'c is no liigh hind to stop tlic
moV(>ment wliich marked tlie hill at Clandebovt'. The INIourne
GALWAY CURVE. - G3
Mouutaius are there, but they fade away iiiUuid. At GOO feet
the whole land from Belfast to the Mouriie hills would he a
wide strait. It is now the line of various canals and railways,
works which follow level ground and avoid mountains. Far
as the eye can reach is a level horizon or an undulatin<;'
plain.
" When all the lines thus found ruled upon a few Irish hills
are laid down on a map, and carried at the proper level from
hill to hill ; over plain, glen, and sea ; they are found to have
a common general direction. Galway lines point towards
Antrim hills. Lines at Clandeboye point along the south side
of Ceantire at Arran in Scotland. Lines near Westport point
at Lough Conn, and there lines point at Lough Foyle. At the
Giant's Causeway, at the mouth of Lough Foyle, lines point
along the north shore of Ceantire towards Inveraiy and Oban.
At Glen Veagh lines point towards Mull and the Caledonian
Canal. The Imes seem to agree with hollows laid down on
good maps. Either the lines of movement were governed by
the f(jriu of the land, or the form of the land was altered l)y
the movement. But it is admitted that the form of the
rock-surface is a result of denudation, and where ice is work-
ing in earnest now, as it is off Labrador, rocks seem to
crumble like mole-hills before the mighty force. Looking to
the geology of Ireland, harder rocks are in the hills, and softer
generally in hollows. Looking to the ice-marks, it is clear
that ice has worked in Ireland up to a height of 2000 feet.
Taking the whole evidence, it seems that denudation, and
transport of a great mass of debris, have resulted in northern
Ireland from a general south-westerly movement in a current
laden with heavy ice, which continued to flow till land rose
and stopped the movement.
The people of Antrim and the N.E. of Ireland hail from
Cii i'..\i;ri(' (TKiMCNr — r.iiirisii isli;s— ii;klani».
Scdtlaiiil, as (hey say. Tlic lines ilrawii liy icr nii liisli rucks
aim liark at St-otland ; so the next cast must be taken beyond
tlu' sea, and tliis time novlliw ards.
CHAPTER XXXI.
BALTIC CURRENT 4 — BRITISH ISLES 4 — SCOTLAND —
GALWAY CURVE — ARRAN.
The ice-lines on the east coast of Northern Ireland seemed to
converge on Arran, Ceantire, and Loch Linne ; so the Irish
spoor must be followed past the Mull of Ceantire by the
Galway and Westport curves.
Crcdivay curve, Firth of Clyde, Cumbrae. — Steamboats follow
the Galway curve up-stream from Belfast to Ardrossan. On
that coast no observations are recorded, and none were made
on this journey ; but ice-marks abound in Ayrshire.
On the Cumbraes, an arrow on Mr. Geikie's map * points
nearly south, out of the Firth. It is a low-level mark corre-
sponding to the rmi of the ebl).
Arran. — On Arran no arrows are marked by Geikie. The
hills are well seen from the Ayrshire coast, and to them the
high grooves in Connemara and Antrim point.
The high ground forms a block which is still surrounded
with water. The granite mountains differ in shape from the
granite hills of Connemara ; they are higher, and down to
a certain level, about 2000 feet, Goatfell and his giant
brethren are broken weathered peaks A. They are like
jagged mountains which tower above ice in Spitzbergen and
in the Alps. But in Arran, and elsewhere about the Clyde,
hills below 2000 feet are rounded like ice-ground hills
everywhere ^■'~^. Above La ml ash, along glen and a steep
* On the Phenomcim nf (he Glacial Drift of Scotland, l>y A. Geikie ; 1863.
VOL. II. F
GG BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
road lead over to tlic south end of Arrau. At 800 feet, close
to tlie road-side, ice-grooves are weR marked on sandstone ;
they point N.E. by N. and N.E. at the shoulder of the Holy Isle,
and S.W. over the col at Ireland. At this level the stream
would not be mfluenced by the low Ayrshire coast, for 800
feet of water would sink most of the low lauds. To the south
of the road is a hill-top 1350 feet high. Here, on a rock
which has the form of glaciation, a deep groove points N.E.
by N". over the Cumbraes at Ben Lomond. In the other
directions a stick nearly clears the Mull of Ceantire, and
points at Antrim. At this level a stream would be free to
move over Scotland and Ireland.
These marks were not made by land-glaciers, for they do
not point at the high mountains beside them. They seem to
belong to the hollow which crosses the south end of Arran
diagonally, and to a stream which flowed through it.
In the deep glen which rmis south-westward, enormous
masses of diift are piled ; but the drift is not arranged in
conical licaps like a moraine. In the glen which runs N.E. there
is less drift. Trees show the prevailing direction of the wind
to be S.W., for the branches point up-stream in one glen, and
down-stream in the other.
Arran, iccstern coast. — A road coasts northwards along
the back of the island. At a point called Lcaca Bhrcaca
(Speckled Slabs) certam igneous rocks are much weathered,
but ice-ground to a great height. At 200 feet or thereabout,
grooves are distinct ; they rim horizontally along the hill
which faces Ceantire ; at this spot these contour-lines run
N., S. Perched blocks and jointed tors arc numerous up to
the sky-line. In the lee of this point to the south arc great
beds of drift which contain stones of many kinds, but one
pattern. After a long search no flints or Antrim chalk were
GALWAY CURVE — ARRAN. 67
found. North of this promontory, another deep glen leads to
Brodick over a pass, and the coast-land is a wide Hat moor.
Over this a path leads to the King's Caves. Close to tlie
sea is a fine mass of columnar basalt.
At MacJuiri the drift is arranged in ten-aces, which look
like ancient sea-margins, but these are chiefly composed of
glacial drift.
The actual sea-beach, where no ice now forms, is a good
specimen of its class. It is a hollow curved slope of large
stones, with ripples of coarse gravel about high-water mark,
and a calm of sand below it ; but every here and there a
great ice-boulder is planted in the midst of these stone-waves
like a beacon amongst breakers. About Duhhgarrie walls
are a curious study. They are made of big stones found
about the sea-margin ; they were washed out of the drift-
terraces by the sea, and they have been broken by men so as
to show their internal structure. Some blocks are conglomer-
ates, which contain rounded water-worn quartz boulders as big
as turnips, bits of water-worn granite, gray and red sandstone,
and other stones all cemented with a coarse hard reddish
cement. Others are blocks of old red sandstone, which con-
tain large pebbles of water-worn C[uartz with the sand packed
round them, as sand is packed about pebbles on the sea-beach.
Others are blocks of granite very like those which are found
on the beach near the Giant's Causeway, and along the Antrim
coast. There are many chips broken from Arran hills, but
amongst them are no l)its of Antrim flint or chalk.
At the house of Duhhgarrie, at the end of the longest and
deepest glen in Arran, a river is crossed. It rises amongst
the highest hills, 2874 feet. Here is a washed moraine with
conical hillocks and terraces. A little beyond the house the
road passes under a steep bank of brushwood growing on
68 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
glacial drift. A few streamlets have cut scars in this face,
which is about 100 feet high. The bauk contains scratched
and polished stones of all sizes imbedded in fine gray clay,
very ludike the common drift-clay.
This then appears to be a record of the local glacier-
system of Arran, a muse\im of Arran stones brought down to
the sea, and partially arranged by the sea.
At lomacliar the north-western corner of the island is
reached. There a sea-cliff about 150 feet high rises above a
beach of rolled stones and broken crags. This is modern sea-
work, but the rock-surface on the top of the cliff is ice-
groimd. It is so weathered and worn, that it is impossible
to tell the direction with certainty. The rock is contorted
slate, and on it romided blocks of compact granite are perched
at this level.
At a little more than 1000 feet, on the shoulder of a hill
which makes the base of Ben Bhanrigh (the Queen's Hill),
ice-scores are very well preserved on a smooth patch of slate,
wliich appears from under the peat-moss. Tlie direction at
this promontory is again N. and S. A stick aims nearly at
Skipness Point, and at the ]\Iull of Ceantire, along the run of
the coast. A little lower down, and further from the hill,
scores upon similar rocks point N.N.E.
At Wliitcfarlanc, close to the road-side, at less than 100
feet above the sea, strire on slate are very clear. They point
N.E. by N., and so do bcnit trees beside them. Grooves are
tool-marks of ice and water-streams ; trees are shaped by
streams of air ; the equinoctial gale followed the run of the
Arctic Current, and both were driven by the same forces past
this spot m opposite directions.
The Galway curve is carried over Arran at Lamlash at
1300 feet, and past the M'est and nortli-west coriu'rs of Arrau
GALWAY CURVE — ARRAN. ' 69
at more than 1000. To account for these marks by hmd-ice
alone, a glacier must be imagined reaching from 1350 feet to
the sea-bottom, and from Ceantire to the nearest hills of equal
height on the mainland of Scotland. To account for the
marks by floating ice, like that which is working off Labrador
in the same latitude, a change of climate and of sea-level
must be assumed.
The run of the tide in the Sound corresponds to the ice-
lines on the hiU ; the wmd follows the ice-grooves along the
hill 1000 feet higher. A south-westerly breeze, which soon
became an equinoctial gale, and whose path along the sea
was marked by blue squalls and crisp waves, swept the fringe
of a low cloud of sea-mist northwards along the hill at the
high level. Further up the Sound the same south-west wind
curled round the hills and blew from the south-west ; fm^ther
up it blew from the west. In the lee of the mountain the sea-
mist hung and boiled and rolled over and over. A stream of
water of equal depth moving the other way would move
solid floats as the wind moved clouds ; surely the stream did
flow here, and the floating solids have recorded the fact.
In the night, when the breeze became a storm, it was a
Dutchman's hurricane, straight up and down, in the glens. It
sm-ged over the hills like gi-eat rollers on a beach, and plunged
d(jwn u})on the house-tops, as if to crush them ; and ocean-
streams must roll over sunken hills in the same way.
At Cath-mihic-Dhuil, which strangers have baptized Cati-
kill, and at Loch Eanza, are two long glens which held glaciers,
for terraced moraines are near the sea. A lofty ridge divides
the glens, and the hill-top was a good point for high grooves.
Loch Eanza. — L^p to 1300 feet, rocks on this ridge are
ice-ground, but so weathered that the direction is hard to
make out. C)u a shoulder at this level many large boulders
70 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
of granite (some six feet long) are poised on slate saddles.
The smoothest side of these slate knolls points N. N. E., the
broken side S.S.W. The dip has nothing to do with the
shape and fracture. These forms give the direction given
by grooves at 1000 feet, and the wind which followed the
grooves below blew against the fractured side of the rock here.
At 1400 feet, a deep groove in granite again pointed down
wind N.E., over everything in Arran and Bute, up the Firth
of Clyde, at hills about Ben Lomond.
So the Galway curve is here carried over Arran at 1400 feet.
At the top of the ridge, 1800 feet or thereabouts, several
large stones had been moved a few yards from their beds
towards the S.W., but here the granite is weathering fast,
and has weathered so far as to obliterate all small marks.
Gravel as large as peas, scudding before a gale, was form-
ing tiny beaches in front of every heather-bush and peat-bank ;
and rain-drops pattered, and splashed, and rattled against
the hill, driven by the gale. It was bad weather for spooring
on high grounds.
Low Marks. — In the bottom of the glen near Loch Eanza,
about 200 feet above the sea, is a fine section of an ancient
water-washed moraine. It is chiefly composed of granite
gravel swept from the hills, and of very large granite boulders,
which something stronger than wind and water must have
piled there ; but this is not a perfect moraine, the surface had
been worn down. Lower down, stones, sand, and gravel are
ranged in terraces, and packed upon a different principle. The
stones are sorted in sizes, and laid in sloping beds, where the
rivers shot them out during floods and low waters. These are
the washings of moraines an-anged by burns in the sea. At the
iiioiitli of ilic l(»eh ill Ihc soa is a ridge of stones washed iulo
another sliaju', and anaiiged on a different plan, by the ebb
GALWAY CURVE— ARE AN. 71
and flow of the tide, aud by sea-waves. Au old castle stands
on the sea-bar to mark a date, and amongst the gravel at the
point a large block of granite stands firm in the station which
it took up before the castle was built. From Loch Eauza
to the south end of Arran, and along the eastern coast of the
island, similar large granite boulders are planted on the beach ;
and more boulders of the same kind are perched on the top of
the Holy Isle, according to a work on the geology of Arran.*
Thus granite blocks and ice-marks, in situ, can be traced
from the central high hills to the south end of An-an, but
there are traces of two kinds of glaciation. In the glens are
marks of a large local system, but high up on watersheds are
marks of something larger. According to theory these high
marks record the passage of the same arctic current whose
traces were found at Belfast, and in Connemara ; because ice-
grooves point from the E. of K to the W. of S. in this district.
Having carried the Galway curs'-e thus far, the Westport
curve must be carried a stage if possible. Having beat round
Arran, and foimd the spoor as high as 1400 feet, and all
round the coast, the next cast is northwards across the stream
to Ceantire.
* Geology in Clydesdale and Arran, embracing the Marine Zoology and the
Flora of Arran, etc. By James Bryce, M.A., LL.D., F.G.S.
This author says, at p. 15, that he had failed to discover any decided
cases of glacier moraines in An-an. He mentions piles of cMft at the mouth
of Glen lorsa, and at "Catacol," which are mentioned above, as moraines
washed out of shape. Mr. Bryce attributes them to cuireuts of water sweep-
ing these glens when the area was rising from beneath the sea. At pp. 86 and
87, and elsewhere, terminal and lateral moraines are mentioned and described
at higher levels in these Arran glens ; and at p. 89, the combined action of
local glaciers and ice-floats is suggested to account for the disjjersion and
placing of blocks of native granite, which are perched on distant high points
in Arran, such as the Holy Isle at which high grooves above Lamlash point
(see p. 66). The author has failed to notice these and other high marks which
would have helped his argument. This seems to be the work of an able geolo-
gist who changed his first opinion after careful examination and due com-
]>anson with other parts of the country, so his evidence is the more valuable.
CHAPTER XXXII.
BALTIC CURRENT 5 — BRITISH ISLES 5 — SCOTLAND 2 — WESTPOET
CURVE — CEANTIRE.
Between the Galway and Westport cul•^'es is Ceantire, at which
place grooves at the Giant's Causeway pointed. A steamer
runs from Loch Ranza to Campbelton, and thence a road leads
to the lighthouse at the Scotch Land's End. The east coast is
broken and weather-beaten all the way, but the highest hills
are rounded. At Campbelton the hills are very unlike ice-work.
Not a symptom of glacial action could be traced up to the top
of a hill 1100 feet high which rises soutli of the town. But if
the sea were 1000 feet deeper, the town and the country between
the two seas would be about 990 feet under water. This
district has been swept and the surface destroyed l)y the sea.
There is no trace of old ice in the low gi'ounds further
west. A few suspicious boulders at the end of glens may
possiljly be remnants of moraines or drift, but these are few
and far between. Within four miles of the lighthouse, rocks
on high grounds begin to assume the familiar shape, and at
a heiglit of 700 feet, a large block is perched upon a rounded
liill-shoulder to the right of the road. At 900 feet, some
l)l()cks of rounded granite peer through the moss by the road-
side, and beside them are lumps of the crumpled contorted
slate of the country. Fifty yards further, on the north side
of the road, is a well-preserved surface. It is a miniature tor,
and a deep groove on the top of it points nearly Iv and \V.,
at the ]K)tch through wliicli tlie road passes.
WESTPORT CURVE — CEANTIRE. 73
Over the brow to the south of the road, hills rise to a
height of 1260 feet, according to a barometer which passing
gales made an micertam guide for the time. All these tops
have glaciated surfaces, broken short off on the Irish side ;
and the run of hollows and hiU-sides, and of ridges of rock,
nearly agrees with the opposite hollow in which Belfast Lough
now ebbs and flows. But all fine Ihies seemed worn out of
the contorted broken mica-slate. One hill-top after another
was drawn blank. After a long search some very remarkable
grooves were found below the brow, at the very end of tlie
MuU. They are on a point of hard rock at 1080 feet or there-
abouts. Two smooth regular deep grooves, about six feet long,
run parallel to each other, so as to cut out a narrow ridge
upon which a man could ride. One groove is a foot deep,
and two feet wide, the other about the same size. Part of
this rock has split off and fallen, and large blocks of it lie
below the solid point. The fragments are deeply grooved,
and these marks ran parallel to the others, before they split off.
One of these fallen grooves ends suddenly, so that the
hollow would fit a man's head like a stone lielmet. The
grooves cut through the edge of beds in the stone, and the
whole rock is rounded. In profile it has the form of a great
gray leech, and Fair Head in Ireland is seen over the rounded
Imck. A stick laid in one of the grooves points W. K W. just
outside the Ehiims of Islay, along the rmi of the tide, which
hurries past heaving and boiling 1000 feet below. Here then
a stream bearing ice once curled round the Mull, and ran, as
streams now run, from Loch Fyne and the Kyles of Bute,
round Skipness Point, along the Sound of Kilbranuan, and
past the great Scotch rendezvous for modern storms and tides.
These smooth grooves are all the more remarkable from
the shattered rocks which surround them on all sides. It
74 IJALTIC CURRENT — HRITISIl ISLES — SCOTLAND.
remained to be seen if wa\-es and streams make similar marks
at the shore, witliout the lielp of ice, and after a close search
no grooves were found. The coast-line is made up of angular
forms, land-slips, rifts, riv^en cliffs ready to slip, and vast piles
of broken fallen cliffs, amongst which a wild sea raged and
roared, while the wind drove spray, cutting showers of rain,
and hail scudding over land and sea. Abuut the aiguilles
of Mont Blanc (chap, xii.) similar piles of ruin are strewn ;
here all the power of the Atlantic has failed to obliterate high
ice-marks on the brow of the Mull of Ceantire.
From Campbelton to Glenhar the road coasts the Atlantic
for twelve miles along the north shore. The rocks about this
level are all shattered and riven, and the power of ocean-
waves is displayed in the grand tumbling surf which rolls in
upon the sand at Machariehanish Bay. On the land side are
piles of drift, which seem at first to be hills of blown sand,
but the sand covers heaps of large stones. At Glenbar the
mouth of a glen running north-eastwards towards Arran is
passed, and there numbers of large polished and grooved
blocks of hard stone, foreign to the district, had been freshly
dragged from a field, and were piled along the road-side for
building fences. The ice-marks on these were quite fresh.
The Giant's Causeway bears S.W. by W. from this spot, and
is clearly seen on a fine day. Ice-marks at the Giant's Cause-
way pointed N.E. by E. into Glenbar, and along the shore of
Ceantire. There is no Antrim chalk at Glenbar, but there is
granite in Antrim. From this glen to the mouth of West
Loch Tarbert the coast gradually loses the shattered form of
ocean denudation, and smooth ice-worlc is better preserved
as the shelter is reached, llocks are less and less broken as
tlie mainland is a])])roaehed, and as one island breakwater
after anotlicr shuts out the waves. As the western surf
WESTPOET CURVE — CEANTIRE. 75
decreases iu power, and waves get smaller, rifts and geos
become hollows ; cliffs change to ridges and tors ; patches of
drift with stones appear on hill-sides, more large boulders are
seen on the shore, and every rock-fomi points into Loch
Tarbert, and the wide hollow in which it lies, as the direction
from which some grinding force moved. At Fronichean, upon
the top of an isolated hill about 200 feet high, a weathered
surface is preserved, so that the direction can be deter-
mined by deep grooves and other sure marks. At this spot
ice moved from N.E. towards the island of Cara.
At about 100 feet above the clachan the marks are fresh.
The rock is smooth and rounded, and straight grooves on it,
from one and a half to three inches wide, from half an inch to
an inch deep, and some more than six feet long, prove that ice
moved from KKE. at this spot. At 300 feet on the same
hill the general form alone is preserved. The same rock has
weathered, so that waving ribs — the edges of beds of crumpled
slate — rise an inch or more above the surface. At first sight
the fresh grooves would seem to be the work of a small modern
glacier, which slid down a north-eastern hollow from low hills
in Ceantire. The moraine seems just below the village, but
the shape of the hills, deep glens, and the direction of the
grooves, make a modern land-glacier impossible. One surface
has been preserv^ed at one spot by clay, and lately exposed, so
it remains entire beside a bare surface spoiled by weather.
The highest liiU on the road-side is opposite to Ardpatrick,
and is 400 feet high. The surface is bare rock, ground and
weathered. Deep marks here point E.KE. up-stream, at the
mouth of a pass which leads over Ceantire to Skipness, and
W. S. W. past Ardpatrick at the southern point of Islay. A
number of loose stones are scattered on this hill, one of which
is a large block of white quartz.
7G BALTIC CUliRKNT — liUITISII ISLKS— SCOTLAND.
At the end of Ifcsf Luck 'farhcrt, Ceantire is joined to
tlie mainland l)y an isthmus about hall' a mile wide and
some thirty feet high. West Loch Tarbert lies in a deep
hollow about ten miles long, which nearly corresponds to the
strike of rock-beds. On either side of tliis large groove are
hills from 1500 to 2000 feet high. Those to the south-east
make the north-eastern end of Ceantire ; tlie other side of the
groove is a block of high land which ends in another large
groove at the Crinan Canal, and the highest point in the dis-
trict is Slianih Gaoil (the Hill of Love), about which many
songs and legends are repeated. Above the town of Tarbert,
in the middle of the trench, is a long ridge about 600 feet
high. On the top of this ridge are perched blocks, and,
though much weathered, ice-marks abound on the hill. At
one place a long narrow ridge like the back of an animal ends
abruptly where it was broken off ; at another a patch of hard
stone ground smooth has resisted the weather, and marks are
plain. The ridge itself gives the direction. A stick pointed
at Dunskeg in West Loch Tarbert, points down-stream over the
island of Cara at Lough Foyle in Ireland, and up-stream N.E. by
E., over Cowal, past the northern shoulder of high hills near
Ardkinglas ; and every rock-form in the neighbourhood points
the same way. With the sea at this level Ceantire would be
three islands, with sounds near Skipness and at Campbelton.
A stream flowing as the ebb does in Loch Fyne, M'oidd split
on hills east of Tarbert. One branch would join a stream
coming from the Firtli of Clyde, as the ebb does at Skipness
Point, and follow tlu; direction of ice-grooves on the Arran
liills ; another would flow past Tarbert through two narrow
sounds, and join the other streams about Clachan, where ice-
grooves point at the liollow which crosses Ceantire. At
liiffher levels similar streams Avould still follow tliese deci)
WESTrORT CURVE — CEANTIRE. 77
trenches, and flow round islands wluch are hills now. In
walking north-westwards from Tarliert, long parallel ridges
and deep troughs are passed as the hill is mounted. From
Tarbert to the top of the first ridge is about 550 or 600 feet.
Then comes a steep descent of about 500 feet into the next
groove. Then a steep hill rises to 650 feet, and a point is
reached which opens the narrow end of Loch Fyne. Ben
Cruachan is seen to the north, the Ardkinglas hills to the
south, and a wide hollow with hills and glens between these
high points. Eidge follows ridge up to the top of Sliamh
Gaoil, and the whole district seems ice-ground.
All the low hills are of one pattern. At 700 feet are
perched blocks, and more can be seen higher up ; rolled stones
are at the bottom of the glen, and many are foreign to the
rocks on which they rest. Every bare rock in this district,
even rocks below high-water mark, and under water, are
grooved and rounded in the same general direction.
So, after a check at the Mull of Ceantire, the spoor which
was taken up at Westport, at Clew Bay, m Ireland, is fresli
on the mainland of Scotland. It lies in a wide hollow between
the Jura and Arran hills ; between Cruachan and Ben Lo-
mond further inland ; and central Scotland is right ahead.
The track will be taken up there again.
On Mr. Geikie's map arrows point from N.E. to S.W. over
these Argyllshire hills, and the marks are attributed to glaciers
of very large dmiensions sliding off Scotland. According to
the marks now described, ice moved south-westwards as far
as Galway and Westport, in Ireland ; if it was a glacier, it
was 2000 feet thick at Shan Folagli ; it was at least sixty miles
wide on this part of the Scotch coast, and it moved over the
tops of hills, between 1500 and 2000 feet high, in Arran and
Ceantire.
CHAPTEE XXXIII.
lULTIC CURRENT G— GALWAY AND WESTPORT CURVES —
ARGYLL, ETC.
Galway Curves. — The spoor taken up at Gal way, and foimd at
Belfast and in Arran, is fresh in Bute ; but at the low level
of Bute the lines, according to Mr. Geikie's map, follow the
run of the ebb tide, and curve back to the E. of S.
At Greenock a glaciated rock peers out from imder a
garden-wall in a footpath near the town.
So three lines taken uj? in Ireland are landed in three
grooves which cross Scotland.
The Derry Veagli line points to the Caledonian Canal ;
the Westport, Derry, and Tarbert line to Glenorchy ; the Gal-
way, Belfast, and Arran line to the Firth of Clyde : and these
must be followed.
At or near the present sea-level it is easy to trace the
path which ice followed in all the lochs of western Argj^ll.
In crossing from Greenock to Inverary, from the Galway
to the Westport curve, a series of hollows are traversed. It
is plain that land-ice or sea-ice, moving at low levels, could
only slide down, or float up or down, these deep grooves.
Loch Long (the Ship Loch) runs up N.E., and rocks on its
shores are ground from the N.PI as far as Tarbert, where Ben
Lomond stands sentry. A low neck of land divides Loch
Long from Loch Lomond. At the level of sea-shells found
about Paisley, Greenock, etc., the sea would reach Glenfalloch,
ARGYLL, ETC. 79
and surround a large block of high laud in Dumbartonsliire.
At Tarbert the ice-marks do not point at Ben Lomond, but
turn round and point at the shoulder, and at the end of the
loch, where engineers chose Glenfalloch as the lowest pass to
reach Loch Tay. Ben Lomond was not the source of the ice.
A great stream was moved dovra from Glenfalloch, leaving
great stones, to which legends are attached. One is the "Stone
of the Bulls." It was cajDsized and rolled down from the moun-
tains during a mythical fight between two mythical bulls, and
it has been used as a pulpit in later days. High up on the
sky-line, on the shoulder of Ben Lomond, at least 2000 feet
up, more boulders are perched, where they could not have
rolled. They must surely have floated. If these be marks of
ice-floats, the Glenfalloch stream split at Tarbeii; ; one branch
went S.W. down Loch Long, the other round by Dumbarton
to Greenock. The proof must be sought at the head of Glen-
falloch, at the watershed, and that station has not yet been
made good.
At RovMrdennan, on Loch Lomond, where steamers caU, a
point of rock at the water-level has deep conspicuous grooves
which clearly indicate very hea\^ ice passing towards the
Clyde, and groimding or sliding here. The only doubt is
whether the ice was agi'ound in a sea, or high and dry.
Glencrodh. — The Loch Long stream was joined by several
others. A large branch can be traced from Ben lomma to
the col at '• Eest-and-be-Thankful." There the level is about
800 feet, and the question is, What was the sea-level when
the last glacier reached it ? The marks can be followed from
the col two ways ; do-s^ni Glencrodh (the Fold Glen) to the
sea at Loch Long, and down to Ardkingias. The question to
be answered is —
Did the ice slide all the way, or did it slide part of the
80 15.VLTJC CURRENT — GALWAY AND WESirOHT CURVES.
way, to be launched at 2000, or 800, or any sea-level other
than the present ?
Loch Goil. — Loch Goil branches off from Loch Long lower
down, and heavy ice came down that pass from the north.
The rocks are all ground, an<l the weather-side is towards
the pass.
At the mouth of Loch Goil, Clach-an-Turaman (the Stone
of Staggering) is perched upon the sky-line about 100 feet
above the level of the sea. The loch is about 250 feet deep,
and the shape of the bottom is known to herring-fishers, who
say that " it is all in pits and ridges." It is therefore like the
shore. If this be the work of land-glaciers, the ice was at least
600 feet tliick.
At the head of Loch (loil two glens branch — one to the
" Eest," 800 ; the other to Glen Ifrinn, where the col is 630.
A coach and a character convey travellers to Loch Fyne. At
200 feet, and on the top of this pass, are piles of glacial
drift, and at the sea-level on both sides are conspicuous ice-
marks.
But the difficulty is to accoimt for the high drift at 730
feet. No land-glaciers met there, for there are no glens to
hold them.
Loch Uck — Lower down, a third low pass joins Loch Fyne
to the Firth of Clyde, at the Holy Loch and Dunoon.
The shores of Loch Eck are strewed with large Ijoulders,
and grooved. The col is about 100 feet high, and according
to Mr. Geikie's map, the ice moved towards the Clyde from
Loch Fyne.
The question to be solved is the sea-level. At 100 feet
there would be a strait at the Holy Loch ; at 730, a second
strait at Glen Ifiinn ; at 800, Loch Fyne woidd join Locli
Long in a rock-basin called Loch Eestal, and it would meet
ARGYLL, ETC. 81
Loch Lomond at the head of Glen Chonaglas, and at the head
of Glen Fyne. If the sea ever was at that level, there must
be evidence of the fact somewhere, and ice-grooves on water-
sheds may be examined as silent witnesses.
Loch Fyne. — Loch Fyne runs nearly N.E. towards Loch
Tay. Strife are laid down on Geikie's map ; and they are
very conspicuous at low levels. Everywhere along the shores
from end to end, ice-marks are fresh upon rocks near the sea
and awash. The direction of movement was along the run of
the ebb, S.W.
The woodcut on p. 92 is copied from a photograph made
by an able artist. It is a good example of the form of such
rocks.
Inverary. — North of Loch Fjaie, two glens — Glen Aoradh
and Glen Siorrath — rim northwards and eastwards towards
Loch Awe. In these are piles of drift, and in branch glens
which run into them are similar collections of ruljbish at
similar elevations, generally from 600 to 800 feet.
At a place in Glen Aoradh, called Tvllich (mounds), are
great conical heaps of scratched stones, and other glacial
debris, arranged like moraines described above (chap, xxviii.)
On one of these mounds courts were held in the olden time.
The drift extends to the top of the col, which is about 800
feet high, level with "liest-and-l)e-Tliankful." There is nothing
in the shape of the country to suggest a glacier ending at the
head of Glen Aoradh. Ben Cruachan is beyond Loch Awe,
and the drift did not come from that direction. But if the sea
were 1000 feet higher. Loch Awe, Loch Fyne, and Loch Lomond
would all be joined, the sea would reach the foot of the hills
of central Scotland, and all these passes woidd be straits.*
Lorn, Cowal, and Ceantire would be ten islands added to
" For the .slia]'i' nf luhbisli-heaps dropped fioui iiipltiug ii'o, sec vnl. i. ]>, ;3«0,
VOL. 11. 'J
82 BALTIC CUHKENT^ — GALWAY AND WESTPOKT CURVES.
the Hebrides, and the niainlaiul ul" Scothmd would be an
archijjehago at this sea-level.
The river Aoradh has cut sections in the drift, and it
seems to have come round a hill-shoulder from hills and glens
about the upper end of Loch Awe. Above a certaui level,
about 900 or 1000 feet, the hill-tops are bare rock, and striffi
on them point in that direction.
Loch Awe. — Loch Awe runs N.E. and S.W., like the prin-
cipal glens in this district. It points up to Loch Lyddich
and Loch Ericht in central Scotland ; and rocks along the
shores of Loch Awe are ground from that direction.
The general features of the country, then, suggest the
action of some powerful engine which has ground the whole
district, so as to furrow it from N.E. to S.W., and cross-cut it
from N.W. to S.E., leaving a few high points un^round,
A ^^ .^
Above a certain level, about 2000 feet, the tops are riven,
weathered, shattered, bare rocks, as Beinn Copacli ("the
Jagged Hill," which Saxons call the Coljbler, and Celts
Arthur's Seat) ; the Gray Head, and others. Lower hills are
smooth rounded ridges, with the worn strata peeping through
the turf to show that the glens are grooves hollowed out.
Tliey are tool-marks of some graving engine, not fractures
in the earth's crust.
The shattered peaks prove that the glens are not weather-
marks. Itiver-beds prove that tlie glens are not simply
water-marks.
liight down these smooth hill-sides small streams are saw-
ing rough splintery trenches. They are cutting across the
grain into the rounded sides of smooth grooves gouged out
witli siiiuc other tool.
The sea-coast proves that the glens are not tlio marks of
ARGYLL, ETC. 83
ocean-currents. Sea-waves chop like an axe at the root of a
tree, or like a pickaxe at the foundation of a wall ; and the
west coast is a wall of cliffs, wherever the sea has its full
swing.
These west country glens seem to he large ice-grooves ;
the problem is, How came the climate to change, and when
did the change take place? If there were a measure for
river-work, the Highland burns would give one answer. A
stranger, wandering along a smooth hill-side, may see a nar-
row belt of brushwood meandering through the heather. On
coming to the place, he will find an impassable gorge, hidden
amongst the trees. Unless he knows the fords, he may wan-
der for miles, stopped by the work of a rivulet.
Legends tell how Eob Eoy took up his aliodc at a river-
fork of this kind, and called the place his castle. The house
is there still ; and, without the modern bridge, a stranger could
hardly get to it, though the fords are easy, when found.
Further back, it is told that a forfeited earl and a faithfid
guide escaped from hostile Athole men, " who had made a
stable for horses of the Castle of MacCailain." The foes got
near enough to speak, but the strangers could not cross a
burn whose very existence a stranger would hardly suspect.
The river-bed is a fact, if the story be too picturesque for
sober history. It is a deep gash, M'ith vertical sides, cut in
the smooth rounded hollow, which was made before the riAers
began to sa^\" ; and the rivers are sawing through ice-grooves,
which are as fresh as if they had just l)een made in the low
grounds of Argyll.
Westport Curve — high marks. — In order to find out the
course of a general movement in ice and water, sufficient to
accomit fur denudatiun on this scale, it is necessary to get out
of this net\vi)rk of dee]) narrow glens. The t()]i of the steeple
84 RALTIC CURRENT — GALWAY AND WKSTI'ORT CURVES.
is tlie place for the weutlu'i-cock, and liill-t(i})S must l»e sought
for the spoor ol' the Baltic Current.
Dun Chorrc Bhile. — On the north side of Loch Fyne, near
luverary, is a hill which generally goes by the name of Dun
Horrible ; but the name means the hill of the steep Ijriuk. It
is about 950 feet high. The top is isolated, and at the end of a
ridge which separates Glen Aoradh from Glen Siorrath ;
Ben Cruachan is to tlie north, antl the cols are lower than
this hill-top. Loch Fyne, and hills and glens about it ; the
Ceantire hiUs, and many other distant points, are seen from
this spot. With the sea at 800 feet, it was a rock far from
shore. Near the top ore loose blocks which nnist have floated
there, unless they were carried by glaciers or men. The hill it-
self, and rock-surfaces laid bare, have the usual rounded form.
At about 750 feet, weathered rock-tables are bare in the
moor below the to]). Any marks which can be found on them
seem to point at Glen Siorrath and the slioulder of l^einn
Buidhe, beyond which lies Loch Tay. A block of hard stone,
beautifully smoothed and grooved on two sides, lies here ;
and fences are made of boulders gathered on the hill. At this
level, and above it, rocks to the north are ice-gromid all the
way to the head of Glen Aoradh, and marks there turn round
the hill-shoulder into the Loch Awe groove.
These marks lead to central Scotland. I Wit there are
higher marks.
Bcinii Blurac. — The highest point on the ridge whicli
divides Loch Awe from Loch Fyne is Beinn Bhreac (the
Speckled Hill). In ascending to it from Inverary, signs of
glacial action appear eveiywhere. Large grooved stones, v\wx-
juous wandering blocks, patches of drift, contorted beds of
sand, and ofhci' marks, appear in the woods, and amongst the
heather. At 1200 feet, at llic N.K. end i^[ one of llie iiume-
AROVLL, KTC.
85
runs ridges uf whicli the top Ls composed, a well-marked dee^t
groove points X.E. ])y E., into a liollow to the north of Beinn
Buidlie.
Up to 1350 feet, the whole ridge is ice-gronnd, and every
rock-form points at a sea of hills in central Scotland. A
spirit-level and a map show that the passes in the distance are
lower than this point.
At 1550 feet, at the end of the next ridge, weathered
grooves, six feet long, run horizontally along the sides of long-
weathered tors, which rival those of Connemara ; and these
marks all point one way at central Scotland.
From this point to the top, 1650 feet, according to a dis-
turbed barometer, excellent specimens of roches moutonnees,
mth perched blocks, abound. Tlie ciit was sketched on the
wood : it is reversed ; but the form was carefully copied, and
it is characteristic of ice.
If the sea were at 1650 feet, there Avould be a clear course
over Scotland by Strathspey to Scandinavia. Dalwhinny, at
the end of Loch Ericht, is 1169 ; Loch Gany, 1.330 ; and the
highest point on the Perth and Inverness Railway is 1480 feet.
SG BALTIC CURRENT — GALWAY AND WESTPORT CURVES.
And it is to these places tliat liorizontal marks on Beiiiu
Blireac point.
Looking S.W. along the snpposed line of movement, there is
a clear horizon betAveen Jura and Arran along the north shore
of Ceantirc ; and beyond the horizon is a clear way to Loch
Foyle, and thence to Westport, as shown above (chap, xxx.)
Looking N.E. there is a broken horizon between the
vertebrte of Scotland — between Ben Lomond and Ben
Cruachan ; but the way is clear at this level, all the way
to the Bergen glaciers which have been described above
(chajis. xiv. and xv.)
From Beinn Bhreac a magnificent panorama is seen : a
wide stretch of moor and lake, with hills, islands, sounds, and
the wide ocean ; Arran and Ceantire are seen ; Tarbert and
Slianih Ghoil ; the distant smoke of Greenock beyond Cowal
and lloscneath, all the Argyllshire glens and cols above men-
tioned ; and central Scotland right ahead. From this point
the evidence seems complete. These ice-marks were surely
made by sea-ice, of the dimensions described by Lamont,
Dufferin, Scoresby, and others ; moving at this level as sea-
ice moves off Labrador.*
If the other tlieory he taken it will not fit the facts. To
arrive at the to]i of Beinn Bhreac from central Scotland,
land-ice would have 1o clind) for six miles along the back of
■d stcc]) ridge, out of Crlen Aoradh for about 800 feet, if it
stu('k to the ('()! ; for 150(1 feet, if it came straight from Loch
Awe ; and there is no hill to the N.E. high enough to give the
necessary pressure. The hill-top is higher than the water-
shed of central Scotland in passes out of which the ice nmst
* These high marks were first noticed bj' tlie present Duke of Ai-gyll, who, in
] 8.57, wrote a paper on the suhject, and attributed the marks to sea-ice. — Edin.
Nan Phil. Joxirrinl, new series, \-o]. vi., ]). AT)?,.
ar(;yll, etc. 87
have com(» according to the marks wliicli it made CHaeiers
miglit slide down to the sea hy Loch Awe and Loch Fyne ;
but they never climb if they can slide past a hill.
Supposing a solid mass 2000 feet thick to travel along
parallel glens in Scotland, like a sledge in ruts. Let one
runner be in the Caledonian Canal, another in Loch Awe, a
third in Loch Fyne, and a fourth in tlie Clyde. Let the ice-
tract be as large as tlu; largest known, still even that strong
supposition will not carry the ice over the top of Slian Folagli,
2000 feet up, and hundreds of miles away. Nor is there any
apparent reason why such ice should move from N.E. to S.W.
or thereby, from the watershed of Scotland to the west coast
of Ireland.
But if ice floated at tlie level of the highest marks, ice in
Greenland and off Newfoundland explains the puzzle.
It is easy to understand how a prevailing current may
have left marks, as a prevailing wind bends trees. It is easy
to watch clouds floating past those hill-tops at a well-marked
level, and turn them into ice-floes and icebergs, glaciers and
snow, from pictures copied 1>y iiiemory from books and
nature.
The average annual rain-fall in this district is about six
feet. If the rain were snow, as "it is whiles," and the climate
a trifle colder, forty or fifty years would build a snow-heap
more than 2000 feet deep, and glaciers and icebergs might
resume their unfinished work in Argyll. The climate has
changed, and may change again ; a reason for the change is
surely worth seeking. One has been sought in a rise of
Lapland and a Baltic current, and so far the British spoor
looks well, for it points the right way.
Tides. — If high ice-marks are attributed to ice-floats, and
low marks to local glaciers and fjord ice, part of the ice-
SS BALTir CUltKF.NT— CALWAY AND WESTPOUT CURVKS.
[>i'()l)k'iii is sulvetl. The p<jwer.s wliicli luove these lluats on
the opposite coast of Labrador are ocean-currents and local
tides, and their movements regulate the movements of the
ice, as a stream deteraiines the path of froth. Ever since
there was fluid to be moved on the eartli's surface, there
must have been tides, if the laws of nature are permanent
hiws ; so existing tides on the Scotch coast throw light u])on
marks made hj old Scotch ice.
In the tidal chart of the British Isles, given in Keith
Johnston's Phyfiical Atlas, plate 15, the local wave of flood
is shown travelling north-eastwards across the Atlantic from
America towards the Baltic, when it runs foul of Ireland.
There the wave is stopped and divided. It is high water on
the south-western coast of Ireland, and the ebb begins to fl<jw
back. But the wave of flood sweeps on, and curls round till
flood meets flood behind Ireland in the lee, near the Isle of
Man. It is high-water in that channel, and the ebb begins
there, but the wave of flood sweeps on past Cape Wrath and
the Land's End, and the waves meet a second time in the lee,
as waves do behind a stone in a pond. It is high-Avater on
the eastern coast, and a third ebb begins behind Great Britain.
Finally, big waves which travel westwards in pursuit of the
sun and moon, and which are reflected from the shores of
America back to Europe, pass eastwards to Christiania,
Trondhjem, and Gotheborg, where the Baltic Current floA\ ing
out meets the wave of flood and stops it in the narrow sound.
The general principle of this tidal movement is simple
and easily understood, but the details are very intricate.
On the western Scotch coast it takes a lifetime to learn
the tides in a small district. At one point it is said by the
fishermen that seven tides meet. At another, a current swift
as a mill-race pours through a small sound in one direction
ARGYLL, ETC. 89
lur aljout elfvc'ii hours, and after a pause, runs Lack for one
hour. At ancjtlier place Corrie Blireacan whirls round, and
can only be approached at slack water. The famous gulf is
but a wliirlpool like those which whirl behind stones and
posts, and the piers of bridges. It is the offspring of a strong
tide wdiirling aljout steep islands, and there are scores of small
whirlpools in every Scotch and Scandinavian strait.
It is difficult to unravel the maze of the tides at the sea-
level where sea and land are clearly defined, Init it is im-
possible to max) o^^t aU the movements of water l^eneath the
surface. It is hopeless to attempt to follow extinct tides
which flowed through passes amongst archipelagoes of hills,
and at various levels from 3000 feet downwards.
Still, general movements of fossil tides may be inferred,
and some high ice-marks may be referred to them.
At the level of 2000 feet, which would be shown by
contour lines on a Scotch map, if one existed, the flood-tide
which comes in from the S.W. would pass over low lands in
Ireland, and through straits at Loch Laggan, Loch Ericht, Loch
Garry, Loch Tay, etc., in central Scotland, and so on over
Sweden, into the Baltic ; and the ebb would return by tlie
same direct route.
At the level of 1000 feet. Loch Garry and Loch Ericht
would be closed, but Loch Laggan and Loch Tay would be
open, and the tide might still pass that way.
At the level of 500 feet, the Caledonian Canal and the
Forth and Clyde Canal, and Scottish Central Kailway line,
would still be straits, though centml Scotland had become a
single island.
So long as there was a direct passage the waves of flood
would sw^eep through it as they now sweep througli the
Pentland Fii-tli and the Straits of Dover.
90 BALTIC CURRENT — GALWAY AND WESTl'ORT (rEVE>J.
So long as there was an ice-float to be moved ])y tides, the
flood-tide would move it towards Scandinavia, and the ebb
would drive it back towards America, as tides are supposed
to move ice in sounds which cross Greenland (vol. i. p. 395.)
If, when the sea-level was at 3000, 2000, 1000, or 500
feet, there was an arctic current moving south-westward out of
the P>altic, it would help the e1)b to drive the floats aiul breed
glaciers on any Scotch or Irish hills that remained above water.
Now that Lapland is 1400 feet above the sea, there is no
such Baltic current and no British ice.
Inverary nearly corresponds in latitude to Nukasusutok
in Labrador.
Great floes, big icebergs, and fields fifty miles wide, are
moving along the Labrador coast south-eastwards, drivcni by
the reflected current which cannot escape south-westwards
from the arctic basin, because the north-west passage is too
narrow. The Labrador ice is moved by tides and rocked by
Atlantic rollers ; it whirls roimd islands and points and
rocks, but there is a general direction of movement, and there
must 1 )(', a general direction of ice-marks on rocks under water.
So old Scotch floats may have recorded a general move-
ment from N.E. to S.W., though every group of islands and
every change in the level of sea and land would alter the
run of local tides, change tlie drift of ice, and so vary iho
direction of low marks.
Tlio highest marks are, therefore, lirst for getting at general
movements. The Scilly Bishops off Scilly, tlic Dubli lartach
off Mull, the Mealsack ofl* Reykjantes in Iceland, and similar
rocks in the ocean, are washed by ticles, but they do not
change the courses of a tidal wave as Ireland does.
On Slian Folagli in Conneiiiava, at '20(){) feet : on I'.einn
I'.lirear in Ai'uyllsliire, at KlOO f,.,.! ; and on ether isolate<l
ARGYLL, ETC. 91
tops wliicli were solitary rocks if the sea-level ever was so
high, ice-marks do agree with the assumed direction of tides
and currents. The actual jiath of Labrador ice coincides when
copied and transferred to Britain in the map (vol. i. p. 232).
At lower levels in glens and amongst moimtains, in places
where liills made an archij)elago, and the glens a network
of sounds and firths, the marks become an intricate problem,
which would cost an army of observers years to solve. To
these low-level marks the attention of Scotch observers seems
to have been chiefly directed hitherto ; if they will leave the
beaten path and try the hill, they may work out the whole
problem in time.
This at least is plain : If laud rose or sea fell from 2000
feet or any high level so far as to dry glens in central Scotland,
and Beinn Blireac in Argyll, even then glaciers might flow
down straths into sea-loclis in Glenfalloch, Glencroe, and Loch
Long ; in Glen Fyne, Glen Siorrath, Glen Chonaglas, and Glen
Aoradh ; in Glen Orchay and Loch Awe ; in Loch Etive and
Glencoe ; in Loch Nevish, and m similar grooves ; wliile tides
and currents still flowed directly past Edinburgh and Inver-
ness, over low lands in the British Isles.
If there were glaciers on the Arg}dl Bowling-Green when
a cold stream was m the Clyde valley, that branch of the
stream might cany ice grown in Lanarkshire, Dum-
barton, and Arg}'ll, to Connemara ; while the Lochy branch
carried an ice-fleet Imilt about Ben Xevis to be ^^Tecked on
Donegal.
If this really happened, there shoidd be ice-marks to
correspond about Edinburgh and Glasgow, about Inverary
and Dalwhinii}', about Fort-William and Fort-Augustus, and
on hills and watersheds in central Scotland ; and of these
six points one is made good by Beinn Bhreac at Inverary.
92
I'.AI/nc CUKRKXT — (iAIAVAY MU) \VF,«T
At " IJest-aiid-bc-Tliaukful, " a weary pilgrim onrc sat liim
down and sang
"0 king! 0 Peter and Paul I
There's many a stride fnun I'kiiuc to Locliawe."
Above this wild spot, from which a distant lowhind horizon
can be seen through a gap in tlie liills, a tall mountain rises ;
and on its steep ice-groiind sides, fresh moraines hang where
ice left them 1000 feet and more above the present sea.
Where tlic old pilgrim sat, tides surely met since the hills
took their present shape ; and if they did, their way was clear
along this route from Galway to Aberdeen, and to places
further from Lochawe than Eome.
So now to the spoor once more with a cast southwards.
GUnfyiu and
Central
Scotland.
I I -t 11 f7 iM r — \s I MM
St II u] n 1 1 1 11 I li I M al ut tl 1 e n 1
1 II il t Mill IS
CHAPTER XXXIV.
BALTIC CURRENT 7 — BRITISH ISLES G — SCOTLAND 3 — GALWAY
CURVE — LANARKSHIRE, EAST LOTHIAN, ETC.
The last cast was northwards, the next is southwards into
the low lands which were seen from " Rest-and-be-Tliankful ;"
and the next i)oint high on the Galway cui-ve is near Glasgow.
Dcchmoiit. — About eight miles from the town, on the south
bank of the Clyde, is an isolated hill of blue whinstone, called
Dechmont. It is an igneous island in a sandstone sea — an
upthrow in the coal formation. Looking at this hiU from the
N.E., near a bridge over the Clyde, it seems to have been
worn down from the eastward, at right angles to the line of
sight. It is broken down to the westward. It has a rounded
top ; and cliffs on the west and north. In shape it resembles
other hills of the same kind ; for example, Stirling and Salis-
bury Crags in the same glen, and Bren Tor and other tors in
Devonshire.
At the Clyde level, rocks are sandstones covered witli
beds of sand, clay, and glacial drift. Amongst stones taken
from the fields are boulders of hard rock, foreign to the dis-
trict, polished and grooved. Many of these are set up along
the road-side, and marks are so clear on them tliat they can
lie seen from a passing carriage.
]\Iud in the Clyde, which is washed from this district, is
of the same colour as the drift-clav to the south-west, alono
94 BALTIC CURRENT — HRITISH ISLES — SCOTLAND.
the Gahvay curve ; and Lanarkshire boulilers are like Irish
boulders.
Ou the eastern shoulder of Dechmont, a large pile of
stones had been newly dragged from a field by an improving
farmer, m September 1863, and amongst them were large
blocks of crumpled mica-slate, quartz rock, sandstone, and
various kinds of whmstone. Thus glacial drift extends far
up the side of this valley. On the hill-top, at 550 feet, the
blue whinstone is barely covered with soil and turf. There is
no drift, so this hill-top has been swept bare. Close to the
keeper's house, the turf was moved in 18G2, to make room
for a garden, and in 1863 the rock was still exposed. Ice-
marks on it are perfect ; so Dechmont was ice-ground, and
has not lost an eighth of an inch by weatheruig.
There are deep scores with finer sand-marks in them, and all
these point S.E. and E.S.E., at hills on the line of the Caledo-
nian Railway near Lanark. Xorth-Avestward, tlie grooves
aim over Glasgow, down the Clyde. Wherever the turf has
Ijeen moved on this hill, nuirks are fresh, and point in the
same direction. The hill was ground by ice moving over it
from the S.E.
Bent trees on Dechmont point the old way, N.E., at
right angles to these grooves. Water, according to theory,
ought to have followed the track of air. lUit here, ■when the
shape of the land is studied, when the mist of tlie eual-fiehls
of Lanarkshire o^jcus for a moment to show ilislant hills, a
reason appears for a change in direction at this level.
If Dechmont were awash in a current flowing at the 550
I'ct't level, it would l)e a hard rock oil' hard hilly islands,
amongst wliieh tlie Clyde now rises, and off a round-backed
island on Mhich the Kirk of Shotts now stands. If the stream
came bv llic iMi'lh (.r Tav and llic Firtli .'I' F(.rlli, over Onn-
CALWAY CURVE — LANAllKSHIKE, EAST LUTIIIAN, ETC. 95
dee, Perth, and Stirling ; North Berwick, Edinburgh, Carstairs,
Lanark, etc. ; the block of hard high land about Tinto would
turn the stream northwards along the valley of the Clyde, as
far as the next bank, where Cowal now bends the Clyde at
Dunoon. Cowal sends Clydesdale water S.W., to follow the
ebb N.W, roiuid the Mull of Ceantire. On the large scale, it
was the case shown at vol. i. pp. 127, 130, and illustrated Ijy
eveiy stream of moving water and ice.
If the Dechmont marks were made by land-ice, the glacier
was more than 600 feet thick ; a branch slid down Clydes-
dale, and one side of the glacier was beyond the Edinburgh
and Glasgow Eailway.
The low lands of Lanarkshire now drive a busy iron trade.
Coals and iron are dug from behjw ; furnaces, coke-heaps,
and engine-fires darken the air with smoke. Night and day
ringing hammers, machines, and roaring blasts make a cease-
less din ; and at night the very clouds glow in the light of
panting fires, which flare and fade like groups of small vol-
canoes in full work.
Close to the most active centre of artificial igneous action,
at Airdrie, arctic sea-shells have been found in drift at a higher
level than the top of Dechmont. But wheu the sea-shells lived
at Airdrie, Lanarkshire, with all its hidden treasures, was
under water in a wide sea-strait, which crossed Scotland
where the Edinburgh and Glasgow and Caledonian Eailways
now cross, and ocean-currents swung from hiU-side to hill-
side, as the Thames, Clyde, and Forth do from their banks.
The Airdrie bed of arctic shells makes one more link in a
chain of evidence. The marks on Dechmont were made by
floating sea-ice, which was moving in a fjord ; or towards
Galway in Ireland, in a stream which curled round islands,
of which the hi«>h land about the Kirk of Shotts was one.
9C^ BALTIC CUKKENT— ItlMTlSir ISLES — SCOTLAND.
Ill iiiiuiiig i'ur coal and iri>ii tlii' internal structure of tliis
country is learned, and I'roin tliat internal structure one
original surface-forni may be guessed.
It is common to find that a rounded hill consists of a pile
of flat beds of rock, laid one upon the other like a heap of
roofing slates. But the shape of tlie surface has nothing to
do with the structure of the rock. If, in mining, any one of
these beds is followed far enough, a fault or dyke is reached
where a whole series of flat beds has been broken, and the
bits displaced. One side of the fracture or the other is gene-
rally lifted or dropped many feet. In a series of 10 beds No.
1 may be opposite to No 10 ; but if No. 10 has been lifted a
hundred feet up to the place of No. 1, then the side of tlie
broken dislocated fragment ought to be a clifi' a hundred feet
high, with nine beds shown in section. If the broken surface
of Lanarkshire were preserved entire, it would be a land of
flat slopes and sandstone clifts, like an ill-laid pavement, for
the whole of this coal-basin is shattered by faults. The beds
di]) all manner of \\'ays. But this broken surface has not been
preserved.
Lanarkshire is a land of swelling hills and ridges. The
only cliffs in the county are hard trap-cliffs like Dechmont,
and river-banks where running water has done the usual work
of sawing and undermining. The surface has been worn
smooth, and the cliffs ground off". The edges of nine beds, to
correspond to the nine which are found on one side of a vertical
fault, are found by searching along the hill-to]) where the beds
crop out. Cliffs have been denuded.
Here is another link in tlie chain. Tlie whole of Lanark-
shire has been ground down. The sea was up to the level ol'
the Ainlvie shells ; ice moved over the top ..f Dechmont, and
ground the lra]i ; so the great valley was linished by sea-ice,
GALWAY CURVE — LANARKSHIRE, EAST LOTHIAN, ETC. 97
tbougli subteiTanean fire blocked it out, and so prepared a
groove for ice and water to move in.
Tbat seems to be the rough translation of part of the out-
line of the stoiy ; the details have filled many volumes, and
will probably fill many more.
Following the direction of the marks on Dechmont, the
550 feet level leads to the highest hills in the country, which
are nearly 2000 feet above the sea-level about the head of
Clydesdale.
Seven miles in a straight line from Dechmont, at Dalzcll
on the Clyde, a sandstone rock close to the river, 80 feet above
the sea by the Ordnance Survey, is polished and striated.
The direction is S. 55° E
The Clyde here winds about in level haughs, in plains of
clay, earth, and gi-avel ; but where this alluvial deposit was
moved to make a walk in 1863, the old ice-surface was found
perfectly fresh upon the hard sandstone within three feet of
the surface. A line ruled on the Ordnance map points up a
deep wide rock-groove which the Clyde did not make, because
the marks of ice are there ; preserved from the water by the
alluvial beds.
Leaving the Clyde groove at Dalzell, the country to the
north and east rises with a gentle swell. At Wisltaio the rise
is about 350 feet, and a river has dug a V 90 feet deep.
The sandstone cliffs are fractured, and the river-bottom is an
unbroken ripple-marked bed of sandstone. In fields near
Coltness are scratched boulders of quartz, porphyry, limestone,
and other hard rocks. At the road-side are large blocks of
hard igneous rock taken from the drift, some w4tli grooves
more than half an inch deep.
At Camnethan the rise is 480 feet; so- the level of Dech-
mont is passed at a distance of about 10 miles.
VOL. IL H
98 BALTIC CURRENT— mtlTlSII IPT.F.S— SCOTLAND.
Further east, ut Ciirstairs and Clegliorn, tlie height is TH^
hy the survey, 765 hy barometer. ]Iere tlie drift is disposed
ill conical and rounded mounds, like those ^vhich result from
the melting of frozen sand and gravel in water (see vol. i.
p. 380.) The highest point is 918 feet by barometer, and the
form of the surface on this high level is much the same. If
this were first a shoal, then an istlunus, ihifting ice Mould be
apt to ground on it, and this is the place at wliich tlie Decli-
mont grooves point.
Tlie PcnlUdids are about IGOO feet high. Tlu- rode is
much weathered, and ice-marks are obliterated. A rolknl
(juartz pebl)le was jjicked up on the highest hill in the range,
and a scratched boulder was found in a wall at 1200 feet.
The range is chieliy com])osed of volcanic rocks, and the
hill-tops are strangely like volcanic shapes in Icelaiul. I'ai-t
of the Pentland range may, perhaps, be of later dati' tliiui the
Scotch glacial period ; Init on many of these hills ice-marks
are abundant.
IMiudaren mentions other signs of glacial action (in this
I'ange : — A Idock of mica-schi;^-, weighing eight or ten tons,
is at the east end of llimc Jfill, the nearest rocks of the kind
being fifty miles oft', about Loch Vennachar or Loch Earn ;
C(!antire, eighty miles westward ; or Forfarshire, seventy miles
northward. I'ut as all the ice-grooves point i>astward, tlie
block ])robably sailed Iroiii some land lieyond tlie seas, together
witii till' hills of drift which are [)iled up near this track.
i\t 800 or 900 feet, at a ])lace called Wcstu-ahr of Dun-
s//)ic, " dressings" were found hy Maclaren.*
The direction was E. and W.
So at 1000 feet (tlie level of marks on tlu' Arran hills)
fbc (ialway cur\(' is cai'ried over Scotland by the Caledonian
■'• ALT'liiivii'^i <,''n/,uf,,^ J,. 215.
GALWAY CURVE — LAXAlUvSIIIKE, EAST LOTHIAN, ETC. 99
Iiiulway ; tlie hills of Conneinara and the Pcntlands are joined
hy a curve on the map (vol. i. p. 232), and high ice-grooves
coiTespond toleraljly well all the way.
At lower levels this gap in Scotland was blocked by the high
land about the Kirk of Shotts. But the way was open along
the Edinburgh and Glasgow line, and ice followed that curve.
Ediahargh and Glasgov: line. — Two rivers, a canal, many
roads and railways, all follow the path which an ocean-current
may have followed from sea to sea at and above the level of
1000 feet.
To the north of the Edinburgh and Glasgow line, as far as
Castlecary, the north bank of this large groove is a range of
hard hills. These have smooth tops and sides, and they are
scarcely varied by glen or watercourse. The Ljm- grounds
belong to the coal formation ; and the surface of the low
country, ^\•]dch M'as at tlie l»ottom of the sea-strait, is fur-
rowed by ridges and hollows parallel to the rijads, canals,
and railways, and to the range of liills.
Ice did not slide from the hills into the plain. If it had,
furrows would pcnnt at the hills ; but ice made the groo\'es
in passing along the base of the hills, and it seems as if some
grinding machine had passed over the hill-tops also, for the
range is but a large copy of smaller ridges in the plain below
it. All the outlines are curves ^ — v. All the grooves point
from sea to sea.
All the hill-t(jps in this valley are ice-ground, according
to the observations of Maclaren, his predecessors and suc-
cessors. At Binny Crairi, near Linlithgow, grooves and
ridges point E. and W. Craifjlockhart Hill, three miles S.W.
from Edinburgh, is a tor pointing E. and W. It is quoted
as a specimen of crag-and-tail, Init the tail points E., as the
tails of ice-tors do when ice comes from the E.
100 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
When a street iu a populous town is paved with flags
which contain hard nodides, passing feet wear the surface un-
equally. Eipple-marks go first, and at last an old leaving
stone is hollowed out and worn down, till knots of harder
stuff rise like nimiature hills in a rolling plain, on which
puddles gatlier when it rains. The knots are worn and
scratched by sand and hobnails, and they retain marks best,
because they are hardest. The softest bits are "rock-basins."
Eenfrew, Lanark, Ap', Linlithgow, Edinburgh, and Had-
dington, are like the flagstones. They are worn, though not
by the feet of men, and the hard knots are hills of igneous rock
in softer strata, which have been groimd by ice.
The low country is strewed with glacial debris every-
where, and lakes and rivers are like puddles of rain-water
restmg in hollows in streets. Dechmont is like a knot in the
stone. At Edinburgh, Corstorphine Hill and Arthur's Seat
are hard ice-ground knobs which also retain marks.
On Corstorphine Hill conspicuous marks are to be seen
over a space of more than a sqiiare mile. Some grooves are
fifteen yards long and a foot deep. Where the rock has been
newly laid bare in fields, small grooves may still be copied
by rubbing. The direction is E. by N., at a height of about
400 feet. Great weathered rock-tables are to be seen on all
parts of this hill-top. They were noticed by Sir James Hall
many years ago, as mentioned p. 214 of Maclaren's Geology,
1839. The direction of these grooves is confirmed by obser-
vation ; but the cause formerly assigned — a deluge of water
driving stones towards the east — must be abandoned. No
stream of water now makes similar marks without the aid
of ice. There is no sea-beach in the Western Isles, where
Atlantic waves and currents have made marks which could
be taken for ice-marks.
GALWAY CURVE — LANARKSHIRE, EAST LOTHIAN, ETC. 101
On the. Calton Hill are grooves almost obliterated by human
feet. The direction is E. and W. at about 300 feet.
On Arthur's Seat are three sets of marks at least.
One is about 400 feet above the sea, at the side of a steep
path which leads to the hill-top from the Queen's Drive.
Here grooves dive north-eastward into the hill, at an angle
of 22°. If this be an old weathered ice-surface, it has been
covered by the newer igneous rock which makes the top of
the hill. It may be a weathered slickenside.
A second series is lower down on a rock which was laid
bare in making the Queen's Drive. At this spot the fine
surface is almost perfect, and the grooves are very plain. The
movement was from E. by S., S. 78° E., past the hill-side
towards the castle-rock through a gap at the back of "Samson's
Eibs."
Close to these ice-marks, a slickenside has l^een pre-
served. These grooves dive into the hill, and bits of crystal
deposited on them still adhere to the worn surface.
A third set is at the edge of the western cliff of Salisbury
Crags, at a level which would join the two seas by the Edin-
burgh and Glasgow line. Here two sets of cross marks are
well preserved ; but the surface is beginning to split off and
weather. The chief direction was from N". 65° E., or roughly
N.E. by E. These grooves run to the broken edge of the cliff,
where a good push would break off more of the columnar
greenstone. They point over Edinburgh, along the line of the
Caledonian Eailway and the base of the Pentland Hills, at a
low conical mound in the glen S.W. by S. The shape of
the Crags alone would suggest movement in this direction ;
but the marks are sure guides.
The greenstone, together with beds of sandstone which
rest upon it, was at some time lifted up like the lid of a box,
102 BALTIC CUKUF.NT -]'.1;IT1SII ISLES — SCOTLAND.
but since tlu'ii nearly llic wholv ol' the xipiier sandstone layers
liave been rul)bed on". At tbis spot the liard greenstone lias
been reached, and marked by ice passing \vest"\\'ards. The
cross markings point from W.N.W. to E.S.E., from tlie low-
lands of Fife to Ihe Tent lands. If tliis hill rose up in ,a
current flowing i'rom tln' eastward, these and the gvooACs in
the Queen's Di-ive ])oint out the junction of streams Avhieh
split upon Arthur's Seat, and joined in the lee, or these are
marks of heavy ice drifting l)ackwards and Ibrwards in the
local tides.
In any case, they cannot he marks of land-ice, for they
avoid high ranges, and aim over low grounds.
Here seems a fit place to rpiote authority in suj^port of
theory, and the authority in this case carries weight.
Tn his later }ears, Hugh Miller, that type of a Scotch
]>easant — the nuui of vigorous intellect, sturdy limbs, and strong
faith — used to wander from morn till evening on the shores of
the Firth of Forth, seeking to extract the secrets of the boulder-
clays and bi'ick-oarths, and to unravel the old coast-biu's.
The resull of his labours in this direction was publislied in
18(14 by his widow. Xo attem])t was n:iade to account for tlie
ice-period, or the direction in which ice moved ; but Hugh
Miller, as usual, saw a picture of the old ice-world oi' Scotland
through its marks, and showed his vision to others painted in
coloured words.
At page 35* is a woodcut which is not a ])icture, but repre-
sents a fact. It is a rough ])lan of a "boulder ]tavement ;" a
patch of boulder-clay washed (dean by the wa\-es of the Kirth ;
an old ice-pressed sea-bottom of stones scpiee/.ed into clay and
ground in their l)e(l.
* EiUabunjh and !h Xfl,jhhoarhno,l, cf., I'V llii-li Milln'. A. him ;iii.l
Clnilrs IMiiclv, LSGL
OAUVAY CURVE — LAXAEKSIIIIiE, EAST LOTHIAN, ETC. 103
The geologist says —
"The agent was evidently tlie same a.s tlial wliicli grooved and
polished the rocks beneath. It was the ocean-borne icebergal cars of
whiter that rutted these strange subterranean pavements, compared
witli which, those of the buried cities of Vesuvius are as yesterday.
All of them I have seen have their direction and striation east-north-
east— the general direction in the district of lines and grooves of the
rock below."
From ice-marks, old shells, the position of shell-heds, the
shape of contour coast-lines, and other evidence, Hugh Miller
conclvided that a glacial period — the life of arctic sea-shells,
sea-ice, and rock-gi^ding — coincided with a sea-level at least
1000 feet higher on Scotch hills than the present beach. From
the levels of old sea-margins, from the depth of the double line
of sea-caves at the Sutors of Cromarty, and such evidence, he
attempted to deduce a few limits of time, and a rate of change.
Of the reality of the ice-period, and the direction in which
sea-ice moved, lie was satisfied, and his direction corresponds
to the observations above detailed.
North Brnrirk. — Marks on Arthur's Seat point towards
North Berwick.
The Law is an isolated conical hill of igneous rock 017
feet al)Ove the sea, and at the end of this Scotch part of the
Galway curve. The low country is chiefly composed of sand-
stones and beds of whin, and the soil is a mixture of glacial
drift and volcanic debris.
The top of Xortli Berwick Law is much woatliercd, l>ut
grooves are still visil)lc on tlie highest point of the hill.
Looking downwards, all tl:c small rocky islands in the
Firth seem to In- icc-polislied from the direction of the ebli-
tide, but the high grooves were probaltly made from the
north-east. A stick laid in one of the high grooves points
104 BALTIC CURRENT — BRITISH ISLES— SCOTLAND.
like a weathercock on a steeple at places from wliicli ice
came and to wliicli it went. One end points out to sea at
Scandina\'ia, the other towards Ireland along the ice-track
which has thus been followed from Shan Folagli to Xorth
Berwick Law. The bearings in Ireland wore N.E. by N.,
here they are E.N.E.
Because of the shape of the rock-surface there can be no
doubt that ice made these high grooves, and if it was land-ice
the source of the glacier may have been in Scandinavia ; it
cannot have been in Scotland, because of the high marks.
Near the top of North Berwick Law is a strange old thorn
which shows the force of the prevailing S. W. wind. Branches
and trunk stream far away from the root, bowing towards
the N.E., and every exposed tree in the neighbourhood
points the same way. The equatorial current of wind sweeps
over the land from Galway to North Berwick, and winds
amongst the hills like any other stream. An arctic current
of water surely flowed along the same curves in the opposite
direction from North Berwick to Galway. Grooves and trees
tell one consistent story all the way.
If the excellent Ordnance map of the Firth of Forth is set
up where the general sliape of the country can be seen, a
curve drawn from Bergen to North Berwick passes between
the Pentlands and the Lammermuir Hills. Looking down
from the Pentlands this country is seen like a map, and it
would be a sea-l)ottoni at the level of ice-grooves on North
Berwick Law. If a current flowed from N.E. over Scotland
at the 1000 feet level, it would curve round the Fife hills,
as the flood-tide now curves round the East Neulc of Fife on
its way up towards Stirling. The high ice-grooves coincide
with ridges and hollows laid down on the Ordnance map
between the Lammermuir and Ochil Hills. If the map were
GALWAY CURVE— LANAKKSHIRE, EAST LOTHIAN, ETC. 105
laid according to its bearings on the top of North Berwick
Law, the great glen of Scotland wovild coincide Avith the groove
which ice made at one end of it. It seems fair to conclude
that floating ice and ocean-currents — the tools which made
the small groove — also made the big groove which contains
so many ice-marks of so many sorts and sizes.
When the Ordnance map is studied, or when any tract in
this district is seen from a high hill, the form of the wearing
or denudation is seen to differ at different levels on both sides
of the Firth. Down to a certain level (about 800 feet) hill-
glens branch and radiate from high points and ridges. Streams
which flow into the Tweed are like twigs on a branch which
springs from the sea at the English border ; glens in like
manner radiate from the Ochils. But below a certain level,
in the big hollow, all ridges and hollows run in sweeping
curves like mud-l3anks in the Firth, which follow the run of
tides which wear them. These shapes tell of water-work ;
the sea-shells at Airdrie prove the case, the ice-marks speak
for themselves.
Streams of rain-water, which flow into the big glen from
hills which make the sides, are now cutting small cross
furrows to the sea, like those which older streams of water
and ice cut out at the upper level. The Scotch map then
seems to show two distmct forms of denudation — one due to
radiating local systems, the other to a general system of move-
ment from KE. to S.W. The Irish map shows similar forms.
So here is another link in the chain. From Galway to
North Berwick rocks have been worn and grooves made by
ice ; floating in an ocean-current, south-westward ; but high
hills have also been worn, and grooves made in their sides
by land-glaciers sliding in every possible direction, down-
wards, into the sea, from watersheds. The sea-level was a
lor,
liALTIC CUUr.EXT— liinTlSII ISLES-- SC(jTLAXD..
liigli one M'lien tlic liorizuiital marks were made, for tliey
rise high.
The broad track taken up at Galway seems to ])e carried
over one part of Scotland. If followed from North Berwick
the spoor should be found about Stavanger, ^^•llere it was left
in chap, xvii. The next cast is northwards to seek the New-
port ciirve which was left on the top oi' T>v'mn lUireae in
chap, xxxiii.
.V WATHn-MARK IN ICKI.AND. — MlCHKIAH FoSS NKAR Hi'
jtli August 1801.
CHAPTEE XXXV.
BALTIC CURRENT 8 — BRITISH ISLES 7 — SCOTLAND 4 —
GALWAY CURVE — NORTH-EAST COAST.
Scotland — Gahrajj Curve. — If one great glen iu Scotland was
partly hollowed out by ice, and has been so little altered ])y
water and weather as to retain ice-marks half an inch deep,
in many spots ; it is probable that other Scotch glens are but
ice-grooves on a large scale, and that many of them are parts
of curves which record the movements of a general glacial
system whose centre is the North Pole, and A\'hose path, like
that of the present Greenland Current, was like the curve of
the letter P, part of the figure 8 drawn on a meridian.
A glance at a map will show that the Galway cuitc coin-
cides in general direction with man}- of tlie glens which
cross Scotland, with rivers, firths, sounds, and main coast-
lines ; denudation in Scotland as in Ireland has manifest
reference to curves wdiich cross meridians from north-east to
south-w^est or thereby. The Galway cun-e was rim out at
North Berwick ; it can also be followed along the north-
eastern coast. The tract to be searched for the Westport
line found on P)einn Bhreac in Argj'Ushire is somewhere in
central Scotland, about Loch Ericht or Loch Garry ; so the
way is north.
At the level of marks fomid on Dechmont and North
Berwick Law, the OcMl Hills would be a steep island cut off
108 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
from central Scotland by a strait throiigli which the Scottish
Central Railway now passes to Perth.
Stirlinrj, or Windy Gap as it is called in Gaelic, is at one
end of the strait where it joins the ^'alley which now holds the
river Forth ; and here a railway crosses to Loch Lomond,
following the low level. On the castle-rock, IMaclaren
found marks of a movement from the KW. Sir James Hall
foimd dressings which pointed the same way ; but if a
current came from the E., it woidd bend round the foot of the
Ochils.
The Carsc of Stirling is an alluvial plain of rich fiat land,
with sweeping mounds of stratified gxavel and sand rising every
here and there. The stones are small and look water-worn,
and the shape of the country is the shape of a dry river-bed.
Canoes, the skeleton of a whale, shells, and other such marks,
confirm the evidence of form. Tlie battle of Bannockburn
\\'as fouglit upon an old sea-bottom.
The rode on which Stirling Castle is built, the Ahhcy
Craig on which a monument is slowly rising to the memory
of Wallace, and other hills in this tract, are of the same
pattern as Salisbury Crags and Dechmont. They are broken
knobs of hard rock, and they seem to be tors worn from the
Scandinavian side, for they are broken to the westward.
The Scottish Central line passes northwards in the lee of
the Ochils, and at the Bridge of Allan it leaves the plain.
The cuttings are through masses of glacial drift fifty feet thick
at least. The beds are not stratified ; the stones are not sized
and sorted ; but big and little stones of many kinds are con-
fusedly mixed with fine soil. The materials are glacial, but
the surface-form is aqueous.
At Dunblane, 150 feet up ; about Greenloaning, 300 ; and
thence to the watershed, 350, where the Allan is left and water
GALWAY CURVE — NOKTH-EAST COAST. 109
flows towards the Firth of Tay, tlie shape of the country is
like the shape of the Carse of Stirling and the neighbourhood
of Falkirk. It is a large copy of a broad west country sound
when the tide ebbs. Flat fields suddenly end in hillocks,
steep points, and ridges, whose slope is the slope of loose
rubbish. There are piles of drift in the supposed strait
which joined the Firths of Clyde and Tay, and the shape is
that of the model (vol. i. p. 380). Above this drift the hills
are barely covered with turf. They are rocks, but rounded
to the very top.
Seen from Falkirk the Ochils slope down to Fife, but fall
suddenly towards Stirling. Seen against an evening sky from
hills above Dundee, the Scandinavian side of the Ochil hills has
the same general outline ; but the low shoulder is like a great
rolling stormy sea, driven westward by a north-easter, for the
larger form is rex^eated in miniature as ripples copy larger
waves ; all the low ridges slope towards the sea and are steep
to the land. On the weather-side, near Fife and about Perth,
there is less drift, and it is more evenly and thinly spread
over the rocks. So the shape of the Ochils is like that of
smaller tors on which ice-marks remain.
At Auchterarder, 200 feet up, the hills of central Scotland
are seen. When the first snow of winter has whitened the
hill-tops, and a bright sun shines through a clear frosty air,
every mountain form is clearly shown by colour, light, and
shade. The hills are seen to be rounded weathered masses of
stratified rock, with sides furrowed by glens radiating from
the watershed down to a certain level. Below that, ridges
and furrows sweep along the hills. There are visible marks
of vertical and of horizontal denudation on the mountains be-
yond Stratheana.
Weathered edges of the strata, when picked out with snow-
no U.VLTIC CUKRENT — lUtlTISlI ISLES— .SCOTLAM).
(Irii'ls, make the i^ivdi hills like culduivd wooden models.
They owe their convex rounded shoulders and liollow glens
to carving, as models do ; and their structure, like the grain in
wood, has nothing to do with their surface-forms.
Amongst these distant hillsarewell-laiown well-remembered
river-marks. Steej) picturesque gorges, where birches wave,
and heather blooms over gray crags ; where mountain-streams
liruwi and thunder down into black boiling pools, from whicli
they leap Ibaming, till they reach some quiet lake and rest.
There, the broad Tay winds past Taymouth, and the Isla glides
past " the Bonnie House o' Airlie ; " silver threads in a carpet
of green. But these are not the tools Avhich carved these
mountains, glittering like silver in the crisp frosty air. Eivers
might work for millions of years, but they ucxcr could ilo
such work. As A\'ell might an artist scidpture a bust with a
hand-saw.
This work was done witli other tools.
Looking north-east from Auchterarder the horizon is clear
of hills, and the plain of Strathmore fades in the distance.
But on either side; of this IcAxd strait of rich flat land rise
steep islands of rock. The Sidlaw Hills are to the right be-
hind Berth, and the F( »i'farshire hills, on the left, stretch to
the blue horizon, (hi such a day, ^hen a wide tract is seen
like a model, it is easy to fancy the horizontal snow-line to
be a sea-margin, and to follow the coast along the tlark line
where the snow is melted.
The dark lines on a railway map show low grounds ; and
here railways surround two blocks of high land ; they mark
out the base of the Ochils and Sidlaw Hills. There is a tract
of low land all the way from Aberdeen to Greenock ; and if
the sea were at the snow-line, tides might el)l) and ilow along
the east coast of central Scotland and round the coasts of the
(;alway cuhve — north-east coast. 1 1 1
islands of Ocliil and Sidlaw. If the td)l) did in fact pass west-
ward, liearing vast graving-tools, and grinding hills with them,
their marks should be found on the north-eastern islands, and
in particular on the Sidlaw range.
Sidlaiv Hills. — The next large north-eastern island, at the
500 feet level, would he the Sidlaw range, which stretches from
Perth ahnost to Forfar about N. 30° E. The steepest ends of
the hills and broken cliffs face the south and south-west, and
the longest slopes are towards Forfar and Strathmore.
Strathnore, the big glen, runs parallel to the Firth of Tay,
and cuts the Sidlaw range from central Scotland. A railway
follows this old strait over flat land from I'erth to Aberdeen
now ; but at the 500 feet level, Strathmore would be a strait.
A stream, which rises behind Dundee at a low level, flows
into Strathmore, past the northern end of the Sidlaw Hills,
round Ijy Tertli, and S(j dnwu the Firth of Tay past Dundee,
and back to witldn a few miles of its source. The hills which
are thus isolated are about 1000 to 1300 feet higli. They are
chiefly composed of sandstone and bedded trap.
The Carsc of Gownc to the south is a low plain of rieli
clay-land highly culti^'ated. It is \-ery little above the pre-
sent sea-level ; and many marks show that it was under water
at a late period. Eeeds force their way up amongst the corn
from bogs which are now buried. E^'eiy now and then a
rude l)oat, an anchor, an iron ring, or some other mark, turns
up a long way from the present shore.
The air above the Carse is often lieaA'v with water, and,
as the natives say, " In rimy weatlier, M'hen the frost takes
the air, when ye look doon frae the hills, it's just like a
pond." Looking down from a height of 700 feet, on a still
frosty morning, the whole Carse is hidden by a level sea of
mist, above whose distant horizon peer dark islands, in Fife
112 BALTIC CURRENT — BRITISH ISLKS— SCOTLAND.
and Kinross. The Oeliil Hills and the Fife Lomonds are the
islands in this misty sea. From its de])ths vise somids of busy
life — barking of dogs, the crowing of cocks, the low of kine,
the cawing of rooks, the rattle of carts, the buzzing of
steam-ploughs, the distant roar of the train, and the near
voices of men ; but for all that appears to the eye, the Carse
and the low lands of Scotland might be a sea-bottom a
himdred fathoms down. The Carse was a sea-bottom, and
deeper down, since the Sidlaw Hills took their present shape.
Behind Rossie are two wide straths, which at 800 feet
would join Strathmore to the sea. These glens, seen from the
col, seem to run N.E., but below 800 feet they are shel-
tered fi'om the N.E. by hills. The glens make a kind of
bay in the range. At 900 feet, at the head of these glens, and
at 450 feet, at the back of the first range, are collections of
drift. When a field is newly taken in, thousands of large
stones are taken from the red soil. Amongst them are speci-
mens of gray granite, white quartz, contorted gritty stone, blue
limestone with white veins, whinstone, brown trap, hard gray
and white quartz rock, mica-schist, porphyry, greenstone, and
other hard rocks. Many of these are smoothed and grooved.
Similar stones are built into walls, bridges, and houses, and
they are broken up in thousands. This then was a cross
sound amongst the Sidlaw Hills at 800 feet; and at 700 a
sheltered corner in which drift gathered. When the col dried
at 800 feet the glens Avere sea-lochs, dotted with islands, which
are now steep hills.
The hills are all sandstone and trap. The beds dip various
ways, but the dip and fracture do not accord with the shape
of the hills and glens. It is plain that they were carved out;
the question is — By what means?
From one col (800 feet) a steep pull leads to the foot of a
OALWAY CURVE — NORTH-EAST COAST. 113
cliff of igneous rock, ^vliich seems, by its structure, to have
boiled. The old igneous surface on the upper side of one
layer may be seen by moving the next plate. The rock is
like Icelandic lava, a hardened lirown crumpled froth. The
tops of " the Giant's Hill" above the cliff 1350 feet, overlook
Strathniore, and they are rounded knolls. The rock-surface
generally is too much weathered for stripe, but some remain.
They point N. 58" E.
The Kiwjs Scat is the highest point in the range, 1400
feet. The shoulder is manifestly ice-ground, but too much
weathered for marks. The toj) is an artificial barrow of loose
stones, on which the sappers and miners have built their
cairn. At the foot of these hills, which were marked at 1350
feet by ice moving from the N.E., are the piles of drift above
mentioned. On the hills above 1000 feet there is not a boul-
der to be found. But the sea of mist floated up, and settled
upon the King's Seat, and then nothing was visible but a gray
cloud as thick as Icelandic tlioka.
At 800 feet, and some miles nearer to Forfar, a hill-top, at
the head of this basin, called Bala Hill, was dra^ni blank for
ice-grooves, l^ut a polished grooved block of porphyry was
foimd in a field near the top.
Further north, at about 900 feet above the sea, at the foot
of a trap-cliff above the Loch of Lund]/, is a long deep narrow
strath which crosses the range diagonally. Through this
groove distant hills about Glenartney are seen in one direc-
tion, and in the other the coast is clear to Scandinavia. At
this level it would be clear to Galway also. At this spot is
a bare rock- surface about 20 yards square, much weathered
but deeply furrowed in the direction of the glen, N.E. by E.
A steep slope of grass-growm talus 32° and 40° leads to the
top of the cliff, 1150 feet, and from tliis point tlie hills of
VOL. II. I
114 BALTIC CURRENT — r.TJTTISlI ISLES — SCOTLAND.
central Scotland are well seen on a clear day. Ben Ledi,
Ben Vorlich, Ben Mor, Ben Lawers, Scliiehalion, the Cairn-
gorm range, and the Braes of Angus, are all seen beyond
Stratliniore, with its winding rivers and rich corn-land. The
Fife Lomonds and the Ochils are seen beyond the Firth of
Tay. On tlie top of Lundy Hill, near the edge of the cliff,
the rocks are manifestly ice-ground but weathered. Near a
new wire-fence, a surface newly laid bare is better preserved,
and grooves on it point S. 75° E. out to sea at Denmark and
Sweden. Other weathered marks seem to point E. and W.
and others N.E. ; but without a spade to remove the turf,
fresh surfaces are hard to find. None of these high marks
point directly across Strathmore at central Scotland, but they
point along the Sidlaw range, and the glens in it, and join in
with the line marked out by railways. Looking towards
central Scotland, it is seen to be a rounded Ijlock ^ — s, with
conical mountains A rising above it. It is well named Driom
Albain, the back of Scotland.
At about 900 feet, on an isolated top near a keeper's house,
at a place called Wart Well, about four miles south of Lundy
Hill, strife on a trap surface freshly bared by the fall of a tree
point N. 60° E. out to sea. These marks are nearly parallel
to the general run of the tides in the Firth of Tay.
Thus, from about 1.300 feet down to about 900, high grooves
coincide generally with the probable run of the tides, if the
sea were at these levels. At 1300 feet the Sidlaw Hills would
be rocks awash, like the Bell Eock ; at 900 feet they wouhl be
a straggling group of trap islands, some with caps of sand-
stone. At 800 feet the islands would be joined by narrow
ridges. At 800 feet Denmark would be imder water, and
Sweden awash at places to which some grooves point.
Tlie drift is generally below the 900 leet level. Tt is
OALWAY CURVE — NOllTII-EART COAST. 115
foreign to the Sidlaw range, and glacial. It did not cross
Strathniore, and come from central Scotland, because liigli
ice-grooves do not point that way.
The question is : "Whence did it come ? and the gTOOves all
point eastwards to Scandinavia, as similar gTooves did in East
Lothian. At lower levels on the Hill of Dron, at four stations
about 850, 700, 650, and 650 feet high, and three miles apart,
well-marked grooves on trap point up into glens which at 800
feet woidd be bays. Tliese point N. 67° W., N. 78° W., N. 65°
W., N". 65° W., round the hill-shoulder into the shelter ; they
point eastwards out to sea over the Firth of Tay, at Sweden
and the Baltic. The flood-tide now makes a similar curve
round a point close above Dundee, and the ebb returns by
the same path.
It seems then that ice drifted over the Sidlaw Hills when
their tops were, like the Bell Eock, awash, and that it came
from the eastwards and northwards, passing along the
Forfarshire hills, and grounding on Lundy Hill and the Giant's
Hill at 1100 and 1300 feet.
2cl, That the stream split on the Sidlaw range when the
land rose, flowed down Strathniore to the Clyde, and wound
about m straits amongst the Sidlaw islands, grounding floats
on the Hill of Dron, at 900 feet.
3(7, When that hill-top rose the stream curled roimd it
in the lee, beside the keeper's house, and flowed up into the
glens, as the tide now does at a lower level after passing
Dundee.
4^A, ^Vliatever the stream did after that, there seem to
have been no land-glaciers strong enough to remove the
glacial drift wliich is piled in the glens as high as 900 feet.
oth, A\Tien ice had done its work it vanished, and streams
of water sorted the upper part of the rubbish. Eossie
116 BALTIC CUKHENT— Bl;lTISI{ IS^LKS— SCOTLAND.
means promontory, and Eossie cluircli stands on a promontory
of drift, at aliont 200 feet above the sea. The sides have the
slope of rul)lnsli-heaps sorted in water, and the materials are
water-washed glacial drift. The stones were gathered at
home and abroad, and piled in the mouth of the glen on
whose sides are the ice-marks above mentioned.
Wlien the cold period ended the bay in the hills ]-)robal)ly
sent a rapid ebb-tide through the glen beneath the Hill of
Dron, where the burn is now cutting into the point of drift.
On the point stands a cross so old that even the race who
carved the sandstone are forgotten ; yet the ice -sculptures on
the hill-side are fresher than the quaint figures on the cross.
The rich clay-land of the Carse of Gowrie seems to be
fine glacial drift and soil washed out of coarser drift by rivers
and tides, and evenly spread over rough piles of coarser drift,
gravel, and big stones, which are hidden under clay and
mould. The sand is washed further down about Biittonness
and St. Andrews. The rock marked by ice is under the drift,
and shows wherever the covering is moved.
So when the Carse of Gowrie looks " like a pond," and the
Sidlaw Hills are islands in a sea of mist, this part of Scotland
puts on an old winter dress for the time. \Vlien the sun
shines on it a fairer landscape would be liard to find than the
plains and hills whicli lie " atween St. Johnstone's and Bonnie
Dundee."
Ice-]narks then here give evidence of a rise in the land
equal to 1300 feet, suilicient to accoimt for great changes in
climate, and in the course of ocean-currents.
At 500 feet a stream might flow where railways now
point out the lowest ground, south-westward from Aberdeen
through Strathmore, past I'ertli and Dunblane, to Greenock
on the Firth of Clyde ; thence over Bute, past Arran, where
tIALWAY CURVE— NORTH-EAST COAST.
117
ice-marks at 1000 and less than 500 feet point along Ceantire;
thence to Belfast Lough, Galway, and Connemara.
The ice-track then has been followed from Galway to
North Berwick, and to the Sidlaw Hills, and it points thence
to Scandinavia, where the curves are carried into the Baltic
by ice-marks, at levels higher and lower than the Hill of
Lundy and the Hill of Dron, 1150 and 650 feet. At higher
levels tlie curves nmst be sought on higher Scotch hills.
Granite Veins in shattered Beds of altered Slate.
Railway Cutting at Dalwhinny (ii. 121).
Drawn from nature ou the block. Reverseil.
CHArTEll XXXVT.
BALTIC GUUEENT 9 — BRITISH ISLES 8 — SCOTL.VJ^D 5 — NEWPORT
LINE — CENTRAL SCOTLAND.
The next cast is northwards to seek the Newport curve on
the ridge of central Scotland.
Central Highlands. — A new mountain railway leads from
Perth through the central Highlands along tlie line of the old
Higliland road. It follows and crosses a number of theoretical
curves of movement shown on the map (vol. i. p. 232).
It first runs up the valley of the Tay, leaving Strathmore
at Logierait.
Here a groove leads from Aberdeen along the foot of the
Forfarshire liiUs to the west coast by way of Loch Tay, south
of Schiehalion, through Glendochart to Loch Fyne.
The l)ottom of this groove is filled with lakes and flat
alluvial plains, through which noble rivers wind. The sides
ar(3 ice-ground hills, with terraces of drift along their flanks,
and piles of drift opposite to each cross glen which joins the
main line.
Before Scotland lifted her back, at the sea-level indicated
1)y high grooves on Beinn Blireac, near Inverary, and on the
Sidlaw Hills, this was a strait ; and according to the marks
above described, ice then moved in this groove south-westwards
to Tarbert in Ceantire, and the Giant's Causeway in Ireland.
Main roads follow low grounds across Scotland, and
coaches and streams of tourists have succeeded ocean-currents,
NEWPORT LINE — CENTRAL SCOTLAND. 119
icebergs, and boulders; but before the flood of travellers poured
into these glens, a tribe of land-glaciers perched upon the
Highland hills, and slid down from the high mountains into
long sea-lochs. At some sea-level this ice thoroughfare was
barred by a col about the braes of Balquhidder, and thence-
forth ice must have moved north-east along the course now
followed by the Tay and its feeders.
But Scotch ice, grown in Balquhidder, and launched about
Dmidee, might still sail to Ireland through the deeper channel
of the Galway curve, and join a Glenfalloch iceberg launched at
Dumbarton, off Arran in the Firth of Clyde.
Tlie railway follows a branch of the Tay to the Pass of
Killiecrankie, and there, at the GOO feet level, was a sea-loch.
Many of the railway cuttings are through drift, many em-
bankments are piles of drift. In the autumn of 1863 great
boulders, freshly dug from the hill-side, were scattered along
the whole line. Low down, where rock-surfaces were newly
uncovered, they retained their polish. High up on the sky-
line the hill-tops are rounded, and smooth wet rocks shine
like convex mirrors amongst the grass and heather.
At Killiecrankie a second series of glens leads south-
westward to the west coast, passing north of Schiehalion, by
way of Eannoch and the Forest of Glenorchy to Loch Awe,
where marks at 1650 feet point at these glens.
At Struan, north of Blair- Atliol, the railway has passed
the 600 feet level, and here is a conspicuous moraine of which
a cutting gives a section.
From this point the way rises over a col to the end of
Loch Gariy, 1330 feet. The rocks there are ice-groimd and
the soil is glacial drift. Here a third set of glens lead from
Driom XJachdar, the upper ridge of Scotland, and the Cairngorm
range, south-westward by way of Loch Lyddoch to Loch Awe
120
BALTIC CUliRENT — BRITISH ISLES— SCOTLAND.
and Beiiin Blireac, where ice-niavks at 1G50 feet pointed N.E.
by E. With the sea at perched blocks on Beinn lihreac stones
might sail upon ice from Loch Garry to Argyllshire hills. So
the perched blocks on Beinn Bhreac may have come from
Cairngorm, or the hill of the black })ig, which Saxons call
Ben Macdui.
At 1480 feet (1G2U by barometer), the watershed is passed,
and the level of jicrched blocks on Beinn Bhreac is 1650, or
Water now runs north-eastward to Speymouth, and as
soon as this col dried, land-ice must have slid the same way
that water flows.
At this high level in central Scotland hill-tops are
rounded and rocks ice-ground. Here are large piles of
glacial drift, apparently the moraines of glaciers which slid
down small glens on the western side of the railway. The
hillocks are 200 feet high at least, and their sha])e contrasts
with that of drift hills near Dnnltlane.
They consist of large buuldurs, gravel, ami sand, and
amongst the boulders are many of a fine hard gray granite.
These are in such abundance that they have been used to
build bridges and other railway works. There are also
s])ecimens of a very heavy tough comi)act red porphyry, and
blocks of quartz, gneiss, and altered Hags of various colours.
Tlie hills are of the latter rock, which is much shattered and
veined with pink granite. No gray granite is found -in sifir
on this hill.
In a railway cutting opposite to one of these piles of drift,
a (puirtz rock surface has been laid bare. It is ground very
smooth, and grooves on it point N. 38° E. down into Glen
Truim, and S. 38° W. up into the glen. This s})ot is about
1480 feet above the sea.
NEWPORT LINE — CENTRAL SCOTLAND. 121
A little further on a second smaller gleu on the same side
has a smaller pile of ruhljisli in the opening. This glen is
about six miles long and clear of drift high up.
At Dahohinny, at about 1169 feet, a fourth groove is
crossed. It contains Strathspey to the north-east, Loch
P^richt and Loch Awe, and the Sound of Jura, to the south-
west. Witli ice floating at 1650 feet, central Scotland would
be an archipelago intersected by narrow sounds, and this was
a strait 500 feet deep.
So here is the tract in which the line marked on Beinn
Bhreac is to be sought. With Monadh Liath (the hoary
mountain) on one side, Monadh Euagh (the russet range) and
Cairngorm (the blue cairn) on the other ; an arctic current
might pick up Scotch icebergs and Scotch granite boulders
and carry them along the Loch Ericht trench to Inverary, Ben
Bhreac, Ben Cruachan, tlie Jura hills, or Derry Veagli in
Ireland.
At the GOO feet level all these passes would be stopped ;
Strathspey would be a sea-loch ending at Clrantown, and
boulders would have to slide down Strathspey and sail round
by Inverness and tlie Caledonian Canal. If there were no
ice-rafts, when the land rose to any particular level, the
voyages of boulders ended for the time.
A particular kind of boulder, carried to a certain height,
in a particular direction, marks sea-level, movement, and a
cold climate, for it is a float which ice alone can carry.
On the south side of Loch Ericht is a high ridge of gritty
flags and slates traversed by veins of pink granite ; it is a
spur of Driom Uachdar.
In a rock-cutting at Dalwhinny the rock is bare ; on the
hill-top it crops out, and it is seen in burns at other spots,
many miles apart, high and low. The hill would be an island
122 HALTIC UUKKENT — IJIIITISII ISLES— SCOTLAND.
at 1G50 feet. At Dahvhiiiny, boulders uf gray granite al)ound.
They are foreigners who travelled on ice from some other
district, and to get to the end of Loch Ericht they must have
moved up hill if they travelled on land-ice. If they travelled
on sea-ice they mark old sea-levels, and here they mark about
1350 feet at the end of the loch.
They mark higher levels on the spur of Driom Uachdar,
which divides Loch Ericht from Loch Garr}^
At 2000 feet is a round block of granite.
At 2200 is another, and from this stone the sea-horizon
towards Bergen is open north-eastwards beyond Spepnouth.
A pass lies open to Loch Leven on the west coast. At the top
of the ridge was a shallow pool made by a turf washed in
between two small hillocks. At the bottom of the pool was
a plain of fine soft black peat mud, and fine sand washed in
by rain-water. A thrust M^ith a stick demolished the dam
and drained the pool, and changed the bottom into a working
model of Glen Truim and Strathspey. Knobs of peat were
the liills, peat-mud the drift ; tufts of gi'ass and gray moss
were the forests ; the river was a tiny rill of black water. But
the water set off for Speymouth, and the forms of the allu\dal
plains were alike. There were terraces of stratified drift ;
there the river-windings, the Ys and S, the banks of small
stones, high patches, long points, and steep banks of (h'ift
sweeping round steeper and harder slopes. There were glens
of denudation circling round hard islands which became hills
as the water drained away. All these shapes formed in the
moss-hole in a few minutes, and they were all formed long
ago in the big glen below. The model a few yards off, and
the glen stretcliing to the horizon, filled the same space in the
eye, and seemed alike even in size. Kunning water has done
great work amongst the glacial drifts of Strathspey, according
XEWPOKT LINE — CENTItAL SCOTLAND. 123
to the shape of the country, and the lesson taught by tlie
model.
At 2650 feet this hill-top at the head of Strathspey,
and about 1000 feet higher than the col at the western end
of Loch Ericht, is strewed with big stones of gneiss and pink
granite. The flat is rippled by the S.W. wind. Stones are in
the trough, heather in the lee, gray inoss on the weather-side
of these waves ; and far down below, waves driven along the
surface of Loch Ericlit had the same shape. Even winds
leave a spoor where they pass.
This is one great thoroughfare for currents in the loAver
atmosphere, and a whole wood of fir-trees at the inn lean
down towards Strathspey, as if driven by a strong S.W. gale.
The prevailing wind is then an equatorial current moving N.E.
At 2580 feet, within sight of the Cairngorm Hills, are
three large boulders — one of gray granite, one of a veiy coarse
mica-schist with large weathered veins and nodules of wliite
quaitz, and the third is a coarse sandstone grit. The litho-
graph on the margin of the map (vol. i. p. 496) is roughly
done from a hasty sketch made here.
At the same height — six miles from the inn and close
al)ove Loch Ericht — is another boidder of gTay granite beside
a rock of gi'itty flag, traversed Ijy pink granite and white
quartz.
At 2740 feet is another round stone of the gTay granite; at
2800 another three feet long ; at 2850 three more about the
same size ; — and all these contrast strangely with flat stones
amongst which they lie.
At 3150 feet is a cairn on the top of the ridge, and at
this spot is a wide view over central Scotland. Strathspey
is open to the sea. Then come Cairngorm and Beinn-na-jVIuic-
Duibhe, then a hill shoulder ; and beyond the opening Beiun-
124 BALTIC CUKKENT — BRITISH ISLES — SCOTLAND.
y-Gloe. Then comes a wide tract of lower ground open to Fife
and Stirling ; then the shoulder of Ben Lawers and a lot of
near hills, which shut out the distance. Then a notch through
which hills near Loch Tarhert in Ceantire are seen. Then a
near hill ; then a wide opening at the end of Loch Ericlit, Avith
Ben Cruachan rising to the clouds. Then conies the mass
of Ben Alder, v.-ith patches of last year's snow, and Ben
Nevis peering over it. A glen leading down to the sea,
and a col of 800 feet, divide Fort-WilHam from Strathspey
in this direction. To the north, the hills about the Caledonian
Canal are overlooked, and something in a cloud seemed to he
Wy\'is. If boulders mark a sea-level, it is here carried to
aoOO feet at least.
The hills of central Scotland, u\) to this level and a little
higher, are all rounded tops and hog-backed ridges, above
which a few conical tops rise. At this level gray granite
boulders mark floating ice, which might wander amongst
those peaks in any direction. A man may travel on ridges
■^ — ^ or in hollows ' from N.E. to S.W. witliout much
clilubiug ; if he travels in any other direction, he nnist mount
and descend fi*om glen to glen.
A puff of cold wind and a wreath of nust blotted out the
whole of this wide landscape, and Scotland disappeared be-
hind a few drops of water, as it hid under the sea when the
boulder was dropped on the top of Driom Uachdar.
Fifty feet down from the cairn are more round blocks of
gray granite, and they occur all the way down the biirn-side
to the railway, three miles south of Dalwhinny Inn.
Now 1480 feet, the summit-level of this line, would make
Loch Ericht a sea-strait ; and 8100, the highest granite
boulder, would make the strait about 1600 feet deep at the
shallowest part. So the railway Itridge is built of granite
NEWPORT LINE— CENTRAL SCOTLAND. 125
quarried somewhere, and carried l)y ice wliicli floated where
clouds now settle, where grouse crow, and golden plover
whistle and wheel in flocks. Where dun deer and mountain
hares, ptarmigan, sportsmen, keepers, and wanderers now pass
to and fro, amongst green moss and gray stones, ice surely
floated. The railway train passes along the bottom of a strait
which crossed Scotland at Dalwhinny, because transported
gray granite alioimds on hill-tops to the S.W. at a far higher
level than the top of the pass.
Gray granite is found in situ to the N.E. at higher levels.
Opposite to the end of Loch Ericht the drift seems to be
arranged by water. A small proportion of the large stones
retain scratches. They generally have water-worn or weathered
surfaces. From hill-sides to the north these rubl)ish-heaps
are seen to be terraced layers resting upon the solid rock, and
sweeping down into the wide strath in points and knolls
rising one above the other, like drift-terraces in Norway and
Sweden, though on a smaller scale. They are the contour-
lines of the country following the hollowed surface on which
they rest, up to a certain line, beyond which are solitaiy
boulders on bare rock or in heather.
It is very hard to represent these forms truly with a pencil.
For that reason no woodcut is given of sketches done on the
spot. The place is easy to get at and the forms are distinct.
In nature they are marked out by colour, light, and shade,
rather than form; and on a duU day they are lost in the
distance ; Init when the sun shines they come out clearly.
Any one who knows the Highlands knows the aspect of these
dry heathery gravel liills, on which grouse delight to strut and
shout their defiant chorus of " Go back. Go back. Go back,
Cock Cur-r-r-r ! They are "the parallel roads " of a great many
Higliland glens besides Glen Roy. They are the "ancient sea-
12G liALTIC CURRKNT — liKITISU ISLKS — SCOTLAND.
margins" of Chambers, and liere they rise to nearly 1400 feet.
In the middle of Loch Ericht (see map, vol. i. p. 490) are two
bars, similar in shape to bars which cross tideways in narrow
straits ; as at Koseneath, near Greenock ; in Alten Fjord, in
Norway ; at Portland, in the south of England, etc. etc.
The ridge north of Loch Ericht would be an island at
1400 feet, cut off from another lower ridge about 2000 feet
high by a deep glen. In the glen was a glacier. A rock-
surface has been laid bare by a torrent which has washed
away part of a terrace of drift ; enough of gray granite to
make a railway bridge is strewed below. The rock is a
hard fine dark quartz with beds dipping W.N.W. 26°. Grooves
on their edges are horizontal, and point east into Glen
Truim. The terrace of drift is 100 feet thick at least.
On the opposite side of the glen, the burn has dug into the
rock, exposing a set of nearly vertical strata. This, then, is a
fault ; a rift which ice found and smoothed and filled with
glacial drift. Lower down the hummocks of a moraine are
piled in rows opposite to the glen ; Ijut 600 feet higher up, on
the bare hill-top, are perched blocks of gray granite, keeping
watch over Strathspey and Loch Laggan. At their level, and
600 feet lower, the high ridge north of Loch Ericht would
be another long island.
At Kiiigusic another groove with a col only 800 feet high,
according to late measurements, runs S.W. to Fort-WilHaui,
down Glen Spean. The N.E. corner of the island beyond
the fault, and opposite to Laggan Inn, is a gray granite, but
not the granite of the boulders. The tops are bare and
weathered, have the usual rounded form, but retain no small
marks. There are many perched blocks of com])act gray
granite on the highest points, about 2000 feet above the sea.
According to these marks the famous " parallel roads " were
NEWrOKT LINE — CENTRAL SCOTLAND. 127
under water and rose, and if so they do but resendjle terraces
elsewhere. (See cliaps. xxii.-xxvii., etc.)
While basking in the sun in the lee of one of these stones,
far away from any visiljle sign of man, how strange it is to
hear the yell of a steam-engine, and then to watch a streak
skimming like a silver eel, or the mythical white dragon,
through this wide strath, Avliere an icy sea has ebbed and
flowed. It is no wonder that natives stare agape, and
that sheep scamper for their lives, when this fiery steam-
dragon comes yelling and roaring through deer-forests where
lurking stalkers used to speak in whispers.
Strathspey has seen many changes since it was hollowed
out of the rock.
And this is the popular account of the matter got from a
countryman of Hugh ]\Iiller, -svlio was also a fellow craftsman
of the Scotch geologist : —
"Where do you get that gTanite?"
" Oo, they fand a wheen o' t lyin' i' the grund, eneuch to
build a hail toon."
"Is there a quarry?"
"Na, there's nae quarry onyway here, jeest muckle stanes."
" What kind of rock is there here ?"
" Jeest a bastard kind o' a stane."
" WeU, but where did the granite stones come from ?"
" Hoots, they just grew whar they lie."
Chip, chip, chip, and a look of puzzlement.
With a rising land and a rising tenqoerature, with glaciers
shrinking and melting in these Highland glens, moraine after
moraine would be dropped in Strathspey, for the river, the
road and the railway engineer to dig through. The last stone
would be stranded high up on some lofty hill-side. In fact,
tlie Spey winds through a flat plain of rounded stones, and tlie
128 BALTIC CURKENT — BKITISII ISLES — SCOTLAND.
railway cuts through piles wliicli seem to he lateral moraines
re-arranged hy water, while perched hlocks are stranded high
up on hill-sides which l)Ound this large groove.
\Micn this district was the hirthplace of glaciers, it gave
rise to those which flowed from Driom Uachdar into Glen
Truim, and to six -whic]! flowed from Cairngorm and Beinn-
na-Muic-Duilihe, along the valleys of the Dee, Don, Doveran,
Avon, Spey, and Tummel ; and each of these must have left
tracks, hecause in Glen Truim and Strathspey they are con-
spicuous.*
Frothy spots of blood on heather, water oozing into the
footprints of a deer, do not point out the track of a wounded
stag more surely, than moraines in Strathspey map out the
backward course of melting glaciers. But tlie low moraines
are all washed out of shape.
At Boat of Tnsh station, 765 feet, the fresh wound of a
new railway cutting bares the flesh of the country and its
worn bones.
At the fork of two glens, glacial rubl^ish, sand, gravel, and
great boulders, are piled as moraines are piled in beds and
layers, which dip and curve all ways, and rest upon oaeli
other where they were washed off the glacier or iceberg.
Beneath these rubbish-heaps are ground rocks, and behind
the old moraine a shallow loch nestles in a hollow.
At Avicmore, 092 feet (700 by observation), the drift is
flat and terraced, as it is elsewhere, at this level. When the
moraine was whole there was a larger lake bcdiind the dam,
in the flat country which fills the glen higher up.
The grand hills whence this drift may have come tower up-
* Glacial phenomena abont Balmoral have been described 1)y an able local
geologist. They seem to prove the existence of land-glaciers on tlu^ side of
Strathmore, etc.
NEWPORT LINE — CENTRAL SCOTLAND. 129
wards to the mist, with sun and shower, liglit and shade, and
glorious colours of purple and gold, playing on their furrowed
sides. The works of ice in the plain are now arraj'ed in
forests of yellow birch and dark-green pine ; but whoever
has seen ice at work must know these tool-marks and these
chips. On an autumn day, a single snow-patch gleaming
through a cloud is enough to call up a vision of the Alps,
the Folge Fond, or the great ice-floods which hem in Sprengi-
sandr in Iceland. But the sea-level of the mental landscape
rises on the hill flanks.
At Grantown, 731 feet (800 feet up on the hill-side, by
observation), the new line leaves Strathspey and crosses a
ridge 1000 feet high to the ]\Ioray Firth.
It cuts through hills of glacial drift which rest on con-
torted ice-gronnd slates, and other rocks. Woods glowing
with rich autumnal tints; purple heather, yellow corn, and
blue hills, far away beyond the rich strath; the warm rosy
colours of a Scotch moor lit up by the sun — contrast strangely
with the cold gray desolation of the picture which ice-marks
recal so vividly. And yet these Scotch landscapes were like
the hills of Iceland, and the weather and the river Spey have
done little to alter the land since ice and sea left it bare for
plants to clothe.
In descending from the ridge to the sea-level, the whole
character of this country changes. Glens and wide straths,
moraines, and other marks of river-glaciers, are left in the
Spey-groove.
The train approaches a north-eastern corner, and it is like
others in the British Isles. Seen from Wy^ds, it has a regnlar
slope -^ ^. If land-ice grew here, it slid north-west into
the Moray Firth, in a wide sheet like that which covers parts
of Iceland at Ball .Tiikull, Lang Jokull, etc. (chap, xxv.) The
VOL. IL K
130 BALTIC CUKKENT— BRITISH ISLES— SCOTLAND.
whole ot" thu Morayshire side of the Firth is one ridge
from 1000 feet to the sea-level, from the Spey to Inverness.
Above that level, a few A hills — such as the Knock of Brae-
Moray — rise, but they are exceptions. The soil is still drift ;
but the coating of loose debris is more evenly and thinly
spread, and more regularly packed. Layers (jf sand and
gravel are sorted, sized, and generally laid flat one upon the
other above the sandstone rock. The Fiudhorn, and other
rivers, have cut deep gashes in this rock. If land-ice had
moved in the same direction, it would surely have dug
grooves -^ ^ .
At Eafford station, 169 feet above the sea, drift is
arranged in knolls and mounds, and layers dip many ways.
Most of the stones look washed and rolled, and large boulders
are rare. At Forres, the flat plains of JNIorayshire are only
26 feet above the sea ; and thence to Inverness the whole
of the low country bears marks of water-work. But it
was not water-work done by .shallow unfrozen seas, for the
beach at Inverness and the shores of Scotland are not arranged
like the hunnnocky drift-hills and points which rise \ip in this
low tract. Drift-ice might do work of the kind ; and plenty of
glaciers to make icebergs grew between Perth and Inverness
in central Scotland, and on the opposite coast in Norway.
The evidence in this tract seems to prove that central
Scotland was crossed by narrow sounds, through which ice-
floats drifted, as they now do through the straits of Belleisle ;
that the land rose gradually ; and that glaciers on shoi-e have
not been lower than the two moraines near Dalwhinny, since
the sea packed terraces about the end of these moraines.
If after the land had risen to this level (about 1400 feet),
ccnti'al Scotland was an island with a sound passing west-
ward at Stirling, another sound passed westward at Inverness,
NEWPORT LINE— CENTRAL SCOTLAND.
131
and ice-grooves at 1100 feet near Deny Veagli in Ireland
pointed in this direction, as shown above (p. 57).
The Galway and Westport cnrves have both been carried
over Scotland ; the spooring must go northwards again, if tlie
Glenveagh marks are to be found on the Scotch mainland.
INVERNESS AND PERTH JUNCTION RAILWAY.
List of Stations, showing their respective Heights above the Sea-level,
High-water Mark, ordinary. Si^ring-tides (rising 14 feet at Inver-
ness.)
Feet.
Forres . . .26
Rafford . . .169
Dunphail . . 614
Foot of Knock of Brae Moray,
about . . .1000
Grantown . . 731
Broomhill . 656
Boat of Garten . . 706
Aviemore . .692
Boat of Insh . . 765
Kingussie . . 740
Feet.
Newtonmore
764
Dalwhinny
1169
Summit of Dr
imochter
1480
Loch Garry
1330
Struan
615
Blair Athole
421
Pitlochry
334
Ballinluig
202
Guay
186
Dalguise
179
Dunkeld
. 212
ft
4 in.
The heights estimated by the pocket aneroid barometer
agreed pretty well with these heights, which were kindly fur-
nished by a director of this railway.
CHAPTEK XXXVTI.
BALTIC CURRENT 10 — BRITISH ISLES 9 — SCOTLAND 6 — DERRY
VKAGH CURVE — CALEDONIAN CANAL AND NORTHERN SCOTLAND.
Inverness stands at the north-eastern end of a large groove
M'hich crosses Scotland. At 100 feet level the glen which now
holds the Caledonian Canal would be a sea-strait ; at the
500 feet level it would be a deep narrow strait through which
a rapid tide would flow, like that ^\•hieh now boils and seethes
through Kyle Akin, bet\\'een Skye and tlie mainland. North
of Inverness the rocks are a coarse conglomerate. Up to -400
feet great banks of sand, shingle, and large stones, are con-
fusedly piled on the hill-side. This drift contains stones of
many sorts and sizes, granites of various colours, and hard
igneous rocks, mica-schists, and varicuis kinds of quartz.
They have the shape of stones in glacial dril't, lint the surface
of waterworn stones. They look like stones on the beach
near Galway, which have been rolled by sea-waves after
falling out of tlie clay bank, in which similar stones retain
their grooved surface (p. 20). This seems to be water- worn
glacial drift at the end i>f the old strait. The plain bt'low is
of like materials, spread out and laid flat, and a conical i)ile
of loose stones is left in the middh; like the mounds which
workmen leave in a cutting to mark the original level of the
surface from which they have dug. At the head of many a
Scotch glen, at about 600 or 700 feet, a like plain of rolled
drift remains. If rapid tides ebbed and flowed over Inver-
DEERY VEAGH CURVE — CALEDONIAN CANAL, ETC. 133
ness, tliev would dig away Toiii-ua-8]dricli, and the rest of tlie
drift ; but a watershed 100 feet high stops the tide, and tlie
Xess can do little in such hea\y ground. AMierever they
came from, these mounds of large stones were carried, and
they are piled upon ice-gi'ound rocks. The liills have the
usual shape, and enormous fragments of conglomerate have
been moved and dropped where they stand, amongst heather
and trees, 800 feet up, clear of the terraces of rolled drift.
In Geikie's map, lines are marked about the watershed of
this groove. The whole country is glaciated ; and it is mani-
fest that ice can only have moved KE. or S.W. along this dee])
groove, whether it was land-ice or sea-ice.
The next great gi'oove which crosses Scotland from X.E.
to S."W., runs from the Dornocli Firth to Loch Carron.
The intervening district is a large block of high land,
deeply furrowed by glens. On the eastern side, the northern
shore of the Moray Firth is low land in the Black Isle of
Cromarty, and this district is thickly strewed with cbift. It
seems to be glacial and waterworn.
Beyond the Black Isle is the Fu-th of Cromarty, which
ends at DingwaU, below Beinn Uaish or Wyvis, which is a
great block of high ground, with a rolling plateau on the top.
Beyond the Cromarty Firth is a long low tract of drift,
which ends eastward at Tarbert Xess, and beyond that is the
Firth of Dornoch.
Lines of existing and projected railways mark the divi-
sion between hill and plain from Inverness to Dornoch.
From the Firth of Forth to Duncansby Head, the map of
the eastern coast is like the teeth of a Ijlunted saw. The
lines run alternately westward and south-westward, and hills
inland coiTe.spond to the coast-line. Railway lines, in like
manner, rim westward and south-westward in pursuit of low
i;U HALTIC CUKKENT — HItlTISH ISLES — SCOTLAND.
levels. Roads wliicli follow low levels cross this district in
similar directions. Beyond Dornoch, the low coast-land l)e-
coQies a narrow strij) in Snthcrland, wliicli conies to an end
at the Ord of CJaitlnujss, Mhcie the sea washes a line of
eastern clifls.
The hills now trend northward to Thnrso, and westA\-ard to
Cape Wrath ; and Caithness is flat land, with a soil of drift.
If the north-eastern corners of Caithness and Berwickshire
were not blnnteil teeth, St. Ahh's Head, Kinnaird's Head, and
Duncansby Head, would be points of land of the same pattern
as Tarljert Ness and Fife Ness. The whole east coast is a repeti-
tion of the same pattern on different scales, and it is repeated
in miniature in every firth where the tides are wearing the
coast. It seems fair to conclude that tlie shape of the Scotch
coast results from the wearing action of water-streams, which
i\o\v on a fixed principle, and in certain directions. Here
the points aim N.E. and the bays S.W.
In the northern division there are glens to correspond to
notches in the coast-line, and glens which are prolongations
of bays. Deep grooves run up westward at Glengarry, CUen-
moriston, Strathafl'aric, Lovat's Forest, and Strath Conan ; and,
after passing the watershed, glens run westward down to the
coast about the Sound of Sleat, in Knoydart, Glenelg, Loch
Alsh, Kintail, etc.
Further north glens in Sutherland turn north-westwards,
and on the eastern coast they curv(> north. No maj) of
Scothuid gives the true sliapeof these hills and glens. Black's
road and railway map gives some of the main features, and it
shows that the main hollows and passes which cross Scotland
all converge upon the Nics of Norway and the Skagerrak.
Any geological map will show that these forms of denudation
hear no reference to the geology of Scotland. The grooves
DEKRY VEAGH CURVE — CALEDONIAN CANAL, ETC. 135
have nothing to do with dip, or strike, or subterranean dis-
turbance. ]Most of these Scotch glens are tool-marks of some
denuding engine, and the study of their shape is a part of
" superficial geology." Conspicuous ice-marks are in all these
glens, and in all their branches, so far as they are known to
tlie writer. They all seem to have held river-glaciers of large
size, which followed the present run of water from the water-
shed to the low land.
With the sea at the lUOO feet level, this tract would be
crossed by sounds, and the main coast-lines would generally
trend KK, E. byN., or thereby, as coasts and sounds do in
the Hebrides, at the present level of sea and land.
At 1500 feet there would be ample room for the tide to
flow over the low land of Sleat, through Loch Carron and
Strath Bran north of Wyvis, and so along the Sutherland
coast to the Ord of Caithness. The eblj and a north-eastern
arctic current might flow the other way along the same path
as the flood-tide and the Gulf Stream now flow together out-
side of the Hebrides northwards, and the marks should remain.
The most likely place for sea-marks is on the watershed
in passes. Drift accumulates in shallow sounds ; and low
tracts in the Scotch and Scandinavian islands, which join
high hills, are generally composed of terraced drift with recent
shells. If the backbone of Scotland rose from the sea, the
watershed of each glen would be first a shallow sound, and
then a " tarbert," with raised sea-margins. But if the rise
were gradual and general in Scotland, passes would dry in
their order of height ; so the highest terrace is the oldest.
The col at Dalwhinny is at 1480 feet ; so, on this sup-
position, it was dry when the Forest of Gairloch was an island,
and Strath Bran a strait 850 feet deep about Achnasheen.
There the barometer marks 630 feet at an ancient sea-margin.
136 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
"Wlien there Avas a tavbert at the liead of Clleu Dochart, where
the barometer marks 800, there was still a strait G80 feet
deep at Glengarry on the Caledonian Canal, and there was
deep M'ater above Lanarkshire, where sea-shells have been
found in drift at Airdrie. \\lien the sea was at " l)nnnt)ch-
ter," the l*arallel Eoads of Glenroy, about wliicli so nuich has
been written, were sunk 324 feet ; for the highest of that
series is only 1156 feet above the sea*
The ancient sea-margins of the British Isles have been
examined and described by Kobert Chambers, and they lead to
the conchision that the last rise was general, for terraces of
shingle are found at corresponding levels at many distant
points in Britain. A terrace of stratified gravel is a sea-mark
which could not resist a land-glacier ; it would be swept
away by the force which sweeps moraines before it, and grinds
solid rocks ; it is therefore a khid of tlierniometer, and it is
easily distinguished from glacial drift.
Where a terrace is found resting on glacial drift, beneath
wdiich rocks arc marked by ice, there is a series of records.
1. Ice ground the solid rocks and made the marks.
2. Ice dropped the great stones which floated on it, and
which now rest upon the marked rock.
3. Water packed loose gravel in lu)rizontal layers upon
the moraines or drift.
4. Streams cut through the ternices, washed the gravel,
and arranged the mud in hollows lower down.
These records, then, give relative dates for the last glacial
period, and elevation of land.
There has been no land-glacier at the place wdiere a ter-
race of stratified gravel remains, since the terrace was arranged
by water n])on glacial drift. There has been no glacier since
' Aiitiiiuily of Man, jp. 2.'')3.
DERPvY VEAGH CURVE — CALEDONIAN CANAL, ETC. 137
the moraine was stranded in the glen. So the highest terrace
of sea-gravel marks a sea-level at which the land stood after
glaciers had disappeared, and the highest Scotch terraces of
washed drift known to the writer are at Dal whinny, 1169
feet, in Loch Ericht (?), and near the summit level of the new
railway, which is at 1480 feet.
Assuming that this argument is well founded, the record
in Strath Bran proves that the water-level has been at 700
feet since the Scotch hills were clear of ice, and that there
have been no large glaciers since that time in Strath Bran.
For the same reason, because the rubbish at Dalwhinny
is terraced, there has been no land-glacier in Glen Tniim
since the water-level was at 1400 feet ; but there were land-
glaciers as low as 1600 feet near Dalwhinny, and their
moraines have not been washed out of shape.
But if so, and if the rise of land was general in Western
Europe, then the end of the glacial period coincided in level
with the rise of the low isthmus which now joins Scandinavia
to Russia, 1400 feet, and the last cold period in Scotland
coincided mth the level which allowed the Arctic Current to
flow down the Gulf of Bothnia (see map, vol. i p. 232).
Horizontal ice-marks on hill-sides and toj^s, and on water-
sheds in passes above 1400 feet, were probably made l»y
floating ice, at a time when only the highest Scotch hills
were above the sea and smothered in ice.
The nature and direction of ice-marks at high levels is the
foundation on which this theory rests ; and the shape of hills
of drift is another stone on the cairn.
One of the most beautiful of all the Scotch lochs is Loch
Maree in Wester Boss. It lies in a deep trench which runs
north-west along the foot of a block of high land, which
makes the Forest of Gairloch. To the north are lofty hills —
Sk. A
138 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
Sliocli, Beiiiu-aruidli-cluir, and others — wliicli rise to nearly
4000 feet. In the loch are rocky islands on m liieli natural
woods of Scotch fir still survive ; and in deep glens and
corries which furrow the hill-sides, gaunt trees toss their
twisted arms, like the last giants of a departed race. On a
still morning when the eastern sun peeps over the hills and
\inder the mist, it sends a flood of yellow light and heat
streaming westwards, into the level glen at the head of Loch
Maree. Blue peat-reek, which before sunrise followed the
run of the stream down (3very hollow, turns to a golden haze,
and it eddies and curls upwards as the air answers the sun-
power and rises. East and west, north and south, the
smoke of scattered farms sweeps towards the spot where the
light falls and warms the ground, and the chill breath of the
hills comes down the hill-sides like a stream of cold water.
Heat and cold stir the air, and the smoke and the sunliglit
show the currents which a ray of sunlight sets in motion. On
such a morning the hills are like great cones of lapis
lazzuli set in glens of gold and lakes of quicksilver. As
the day wears on the mists rise up and creep slowly round
the highest peaks, till they rise upwards and float away in
shining clouds. Then the blue cones change ; bare white
quartz glitters hi the sun like snow, and Ben Eitli looks as
if it were "ice" in truth.
T(j a height of about 21)00 feet tliese hills arc ice-ground.
It needs but a glance to know tlu- shape, but here all marks
are clear and distinct.
At the Ijottom of tiie glen, at Kinloch Ewe, at 200 feet,
ice-grooves run towards Loch Maree, N. 30° W. These might
be marks of a local glacier.
Thence, for 700 feet uj) the western side, the rock is broken.
At 900 feet glaciation l)cgins. At 1100 feet, at the edge of
DERRY VEAGII CURVE— CALEDONIAN CANAL, ETC. 139
the glen on the west side, a hirge hollow groove three feet
wide, and as smooth as polished marble, contains stride of all
sizes, down to fine sand-marks. They point a little more to the
west, K 40° W. At a higher level than the watershed of the
glen, which is also the watershed of Scotland, and 800 feet
high at Glen Dochart, a tract begins which is not easily
matched. The rock is a very hard stratified quartz — gray
yellow, white, and pale pink — and for several square miles the
rock is bare. It is weathered in some places, and there fossils
rise up half an incli from the surface. The stone looks like a
sugared cake, with chips of almonds stuck into it. Other
beds are weathered into a pattern of round flat lumps, like
small ivory shirt-buttons laid close ; others have larger shapes ;
concentric rings an inch across, which wear away, leaving
concentric ridges and hollows. But the greater part of this
rock is either freshly broken, or ground perfectly smooth. At
1350 feet, on the top of a ridge high enough to clear most of
the cols which join Scotch hills, and close to the foot of Beinn-
a-Ghuis, the marks are perfect. They point N. 20° W.
In that direction they aim over lower hills about the river
Ewe, twenty miles away, and over the sea outside of the Butt
of Lewes ; in the other direction they aim over the head of Glen
Dochart (800 feet), over Strath Bran at a Ijig hill supposed to
be Sgur-a-Mhulin, but found to be further south. There is no
apparent source for land-ice within reach of this spot, except
the high peaks beside it, and the grooves aim past these
hills, which are some of the highest in Scotland.
They were not made by land-ice.
At the same level, 1350 feet, a mile nearer to the foot of
these hills, and opposite to a glen which seems made to he
the home of a glacier, the grooves point N". 56° AV., and here
is a tiny morame, still perfect in shape. It is bare and looks
UO BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
like piles of broken white sugar poured out across the gleu.
Here, near the level of moraines near Dalwhinny, a similar
form tells the same tale. The sea has not been here since the
glaciers melted. At 1800 feet, close to tlie foot of l>einn-a-
Ghuis, the marks point N. 25° W. The sea must have been
here when the marks were made. So the glacial period seems
to have ended when the sea was at the terminal moraines
on the side of Beinn-a-Ghuis at about 1400 feet, and on the
side of Driom Uachdar at about 1400 feet also.
At still greater heights the rocks have the same ground
shape (see cut, p. 17, and map, vol. i. p. 496), but time would
not admit of a closer examination.
It seems to be proved by marks on hills on one side of
Loch Maree, that ice crossed Scotland from the east to the
west at a level of more than 2000 feet. Above that line the
Gairloch hills seem to be conical piles of broken quartz talus
leaning against jagged cliffs and peaks. The shape is ^-^ up
to one level, A above it.
If a stream came from the eastward and split on these
high hills it would sweep off north-westwards, as ice did
according to these marks.
There can be no doubt of the direction. For 100 yards
in length, and 20 in breadth, one great waving sheet of white
quartz is smoothed and grooved on one side, and fractured
on the other, and for several miles rock-surfaces of the same
kind abound. A few blocks of dark trap are scattered about
at this level, but on tliis exposed shoulder there are few
perched blocks. Looking inland from the Gairlocli Forest, an
open gap in the hills about Loch Fannich bears E. by N., and
there is nothing in that direction to stop ice floating at 1800
fe.'t.
Looking througli that gap tlie first land of ('(pial height is
DEKKY VEAGll CURVE— CALEDONIAN CANAL, ETC. 141
ill Scandinavia ; so tliis path, too, is clear, for in Scandinavia
there are grooves on the watershed which point N.E. at about
2000 feet above the sea near Trondhjem (see vol. i. pp. 103,
234).
The next point on this line is on the opposite side of the
glen, where a ridge 2100 feet high is cut off from all neigh-
bouring hills by deep glens. It is cut off from Slioch by
Glen Bianastle ; from the Forest by Kinloch Ewe ; and a
wide deep strath divides it from Ben Dearg to the north-
east. It is called Beinn Mhonaidh.
If a stream at this level came from the east by way of
Fannich it would split on the side of Slioch, which is about
4000 feet high, and run foul of the place last described.
In the bottom of the glen at Kinloch Eioe drift is arranged
in flat terraces up to the 300 feet level. The river is digging
into these banks, and it is building a new set in the loch
three miles down. This is stratified water-work done since
the ice disappeared. But the gravel banks rest in an ice-
groove, for the marks show as soon as the drift is cleared.
At the 1000 feet level the hill-top is above the level of the
col at Glen Dochart, which would make Strath Bran and
Loch Fannich sea-straits.
At 1200 feet the groove which holds Loch Maree is seen
to be a short transverse rut, for the big groove which runs
from sea to sea E. by K is open between Beinn More and
Fin Beinn. A few large perched blocks of gneiss are scat-
tered on the tops at this level, and the wide hollow and the
shape of hiUs and knolls in it, all indicate movement from
the east towards the high hills beyond Loch Maree.
At 1200 feet some weathered grooves on gneiss point
E. by N. The rocks are much weathered, but their shape is
clear. At 1620 feet is a perched block 9 x 9 x'9 feet, and
142 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
iiianv smaller angular blocks of veined gneiss and granite
are balanced upon rounded knobs of gneiss near a small
tarn.
At 2150, on the top of the ridge, are perched Idocks and
grooves pointing N. G5° E. These are almost obliterated, but
they can be made out.
From this point the opposite quartz hills are well seen.
Unless central Scotland was one vast snow-dome, there is
no possible source from which land-ice could reach this spot.
Deep glens surround Beinn Mhonaidh, and the shortest way
to sea from the hills at which the grooves point is behind
Slioch, three or four miles away, and 1500 feet lower down,
where the water runs. At the same level, and a little higher,
the very same kind of rock-surface, and the very same
pattern of smooth hills, are seen in every direction ; but a
little above this 2000 feet level, hill-tops are jagged, conical,
weathered, fantastic peaks, fit rivals to the Lofoten hills, which
have been likened to the teeth of a shark.
On an autumn day when the air is clear, a grander scene
is not to 1)6 found in all Scotland.
When yellow lights, purple shadows, and showers are
chasing each other from hill to hill, rainbows and windgalls,
])riglit clouds antl blue sky, make this wild tract a scene of
wondrous beauty. It is a picture to look at and remember.
But it is easy to map out the glaciers from other pictures
stored in the same memory. Through a gap in the hills is
the way to Bergen. There stand peaks of the pattern of
Bodals Kaabe and Areskutan ; below is a long rounded swell
like the Norwegian Fjeld. Deep down from the rift of Glen
Bianastle comes the distant hushing sound of a mountain-
torrent. It is in the path which ice must have followed if
it came from Scandinavia through Glen Fannich, and ran
KERRY VEAGH CURVE — CALEDONIAN CANAL, ETC. 143
foul of Slioch. It is easy to fill in the whites in this picture,
and it is easy to test its truth when finished.
At the head of Glen Bianastlc, at 1450 feet, tlie rock is
the same quartz which makes the opposite hill-tops in the
forest. The beds dip the same way, and some are weathered
and some polished. At the very edge of the cliff a set of
perfect grooves point from N. 65° E. to S. 65° W. over Loch
IMaree.
At the same level, thirty yards off, similar grooves on gray
quartz point N. 60° E.
In the glen below the cliff at 1200 feet the marks are
quite perfect. Long white ridges and grooves are " for all
the world like a marble chimney-piece," as an astonished
native of Ding^vall remarked. Striae point from N. 50° E.
From this point do^vn to Loch Maree are similar marks
wherever the bed of quartz is the surface.
But at the bottom of the glen a bed of sandstone is
smoothed by water in the bums, and on the side of Slioch,
where strata nearly vertical meet the edge of the sandstone
beds, the hill-side is deeply furrowed by rain. These ruts
aim at the peak, the others run horizontally past the hill.
The burn has cut a rock-trench twenty or thirty feet deep,
but though all this weathering has taken place, many quartz
surfaces have not lost the thickness of a sheet of paper since
ice left them bare.
At 700 feet is a bed of fiat drift apparently arranged ]jy
water amongst old moraine stuff.
At 700 feet the rock is bare, and marks point at right
angles to the shore of the lake. Here a quartz cliff about
1000 feet high is ice-ground to the top, and the opposite hills,
groimd to the level of 2000 feet, tower up beyond the lake.
At 150 feet the shore of Loch JVIaree is a river-delta forming
U4 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
on ;i iiioraiiie, wliicli lias lost the characteristic shape, and
the lake as usual is said to have no bottom. It is veiy deep
and a true rock-basin, for the Ewe escapes through a channel
of rock.
So, looking on these great hills as stones in a stream, ice-
marks at the high level intlicate a current flowing through
sounds, and splitting upon blocks of high land as streams do
on posts ; the floats must have been ice of large dimensions,
but not necessarily larger than drift-ice, in the same latitude.
The plan laid down at the beginning was to follow ice-
marks wherever they might lead. Marks on the top of Beinn
Mhonaidh pointed at quartz hills on the opposite side of Loch
INIaree, and they were followed. IVIarks at the head of Glen
Bianastle led down to the shore of Loch Maree, marks at the
bottom of the glen j)ointed down the stream ; on the shoulder
of Ben-a-Ghuis, opposite to Beinn Mhonaidh, at about 1800
feet, the arrow (see cut, p. 17), carried 55 miles, to the
visible horizon of the highest spot, aimed about Stornoway in
Lewes. The ice-lines were found to wind about the hills, and
finally aim over two blocks of isolated hills 15 or 20 miles off.
This spoor has been followed, and it is very plain on these
distant hills.
The Hill of Clrohan, over which the arrow passes in the
woodcut, is between the post-road to CJairloch and the shore
of Loch Maree. The highest knob of the central eminence in
the midst of this group of small hills is al)Out 1200 feet high.
It is all ice-ground, but weathered. On the S.W. shouhler, at
800 feet, is a shelving rock of great extent ; from which rul)-
bings were taken, first by a gamekeeper and afterwards by a
gentleman who was kind enough to follow the instructions
given at page 15. Allowing 20° for magnetic variation, the
direction is from S. 83" E. at a height of 800 feet.
DERRY VEAGH CURVE — CALEDONIAN CANAL, ETC. 145
Thus, after a flight of nearly 15 miles, the arrow curv^es
westward 48° (A). At a point about 350 feet above the sea,
behind Flowerdale, and near the post-road, marks have the
same direction. These are in the bottom of a hollow, and
cross it diagonally from S. 43° E. (B).
On the other side of the hollow, in the bottom of a wide
shallow valley, which runs nearly north and south, the marks
point from S. 40° E. (E). They do not aim at the hills.
These three spots, ABE, are in the middle, and to one side of
the large glen, which is split by the Hill of Groban, 20 miles
from the watershed at Glen Dochart. At the northern ex-
tremity of the block, beside the road which leads from Gair-
locli to Pool Ewe, the marks point at the sea from 8. 60° E.
(C), which is the direction of the watershed.
Further north, and further from the hills, and out of the
jaws of the glen, another set of marks, perfectly preserved,
give two cross directions — from S. 85° E., and from S.
35" E.
Still further north, and quite beyond the glen, is Meall
]Mor, a hill 600 or 700 feet high, on the north point of
Gairloch, isolated ; and near the western coast-line of this
part of Scotland, a rock on the N.E. shoulder is clearly
marked, and the rubbing shows two distinct movements —
from S. 85° E., and from N. 35° E. (allowing 20° for varia-
tion) (D).
Thus the arrow is carried over the watershed of Scotland,
at about 2000 feet, with the direction N. 65° E., which might
bring it from Scandinavia along the coast of Sutherland. It
is turned aside on the shoulder of Beinn-a-Ghuis, at the same
level ; and is made to glance northwards from S. 25° E., down
a wide and deep groove. Followed for more than 20 miles,
it is found Ijending gradually southwards, and left aiming
VOL. n. L
146 HALTU- crRKENT — BlilTISII ISLES— SCOTLAND.
from east to west and from N. 3.")" E. to 8. 35" W. ncav a
coast wIkhh" cuvrcuts ilow various ways, according to tlie
state of tlie tide. Tides close at hand do in fact flow in
directions wliich correspond to marks upon this last isolated
hill.
All this seems to point at floating glaciers, grown in sea-
lochs, and amongst small islands, moving in cmTents and
tides.
For a perpendicular height of nearly 2000 feet, for a
length of about 25 miles, and a breadth of Hve or six at
least, rocks are marked on one plan. Perpendicular cliffs,
the bottoms of grooves, the tops of ridges, the tops of hills, all
are marked alike : all the smooth sides are towards the water-
shed, all the broken faces towards the sea. All the grooves
have a manifest relation to each other till they get clear of the
glen. It seems plain that this big groove was full of heavy
ice. But there is no great extent of higher gronnd at the
watershed, and there horizontal grooves 1200 feet higher than
the watershed aim past th(> higher peaks from which alone
glaciers could slide.
If the other direction is taken, and the grooves followed,
the same thing appears. From the watershed striae lead
down to the eastern coast, winding seawards in the grooves,
and they are found on hill-sides far above the bottom of the
glen. But at the watershetl there is no possible source for a
land-glacier, and no apparent reason why land-ice of anjA
dimensions should move horizontally over Scotland at 1200
feet above the watershed of glens whi(;h isolate the hill. It
must be remembered that similar marks pass over Scandinavia
at about the same level, and in a similar direction, and that
similar marks are found upon American hills. If these be
marks of land-ice it was unlike any which now exists. If
_n'^'3'<z t^'-^c^L Ciirr-iii^cr- c\^<<^ it*'cU y^ci. /e^/t^ ^cc«-v^
DEERY VEAOH CURVE— CALEDONIAN CANAL, ETC. 147
they l)e marks of sea-ice, tlie Arctic Current explains the
puzzle.*
The head of Glen Dochart is four miles from Kinloch
* While this sheet was passing through the press a new work on this
subject appeared— T/ic Physical Geology and Geogmphy of Great Britain, etc.,
by A. C. Ramsay, F.R.S. : London, Stanford, June 1864. The opinions of tlie
author are well known, and have been adopted by several eminent geologists ;
in particular by the authors of the Geology of Canada, 1863 ; and by Mr.
Geikie, author of an excellent pamphlet on the Phcnome7ia of the Glacial
Drift of Scotland. The theory assumes a period of intense cold, which pre-
vailed throughout all high latitudes, and in all elevated regions of the earth,
simultaneously ; and which caused an enormous growth of ice during one or
more geological periods. But no attempt is made to account for this cold
period. The theory which this volume is intended to illustrate is that the
present time is the "glacial period ; " and that an explanation of ice-marks is
to be found in the present condition of other parts of the globe. The marks
in Scandinavia suggest glaciers on the scale of glaciers in Greenland ; the
marks in Great Britain suggest sea-ice on the scale of Labrador ice ; the
change of climate at one place is accounted for by a change in the course of an
ocean-current, caused by a change in the level of sea and of land. All arc
agreed as to the facts ; the questions left for argument are the cause of the
change which has surely taken place, the nature of the ice which made the
spoor, and the amount of work which this engine has done.
Mr. Eamsay attributes many rock-basins and their lakes to glaciation, and
lew agree with him ; these volumes go further, and attribute these and many
of the main lines of denudation in Northern Europe and elsewhere to glacia-
tion, combined ivith ocean-currents. Mr. Geikie and other observers attribute
marks in Eoss-shire to land-ice. Their difficulty is how to get their glaciers
over watersheds, and account for the cold of the exceptional glacial period.
Mr. Ramsay appears to have proved that glaciation coincided with the deposi-
*tion of certain breccias of Permian age in Britain. The stones are glaciated
stones, that is certain ; their position rests on good authority. If the glacial
period began soon after the coal formation, and has endured till now, the
acknowledged work of denudation gains the aid of an engine which works
faster than streams and waves do. If arctic currents are iiow to be added
to the list, they are l)igger and stronger tools than land-glaciers, and may
have helped to do tlie work, whii'h has certainly licen done somehow.
148 BALTIC CURRKNT — BRITISH ISLES — SCOTLAND.
Ewe and 800 feet above tlie sea. Here tlie rocks are brittle
and broken, and there are no marks.
Loch Roiag is G30 feet np, and from the liead of it to the
S.W. the Applecross hills are seen at the end of a wide strath.
Here is a high col, and here at the head of Loch lJnis<i; are
heaps of drift.
Five miles off, at the lower end of the lake, near Achna-
sheen, are flat terraces of stratified water-worn gravel and
sand, resting on a large lateral moraine, and the moraine is
on grooved rock. Beyond the glen towers Sgur-a-lVIhnlin,
and a range of high hills. The grooves point along Strath
Bran at Ben Wyvis and Loch Carron, so ice did not come
from the high hills.
The terraces stretch far up along the road which leads to
Torridon, and they arc very large.
Tides siu'ely flowed through this strait at al)out 700 feet,
for no small streams could do such heavy work.
The glacier-work was finished, and the drift left, before
the gravel was packed over it. And the river is now winding
along a plain of fine sand and mud which it washes out of
older water-work, and jiacks away in lakes in Strath Bran.
The lateral moraine or the glacial sea-margin, which
l)egins about Loch Eoisg, is followed by the road for about
twenty-five miles to Garve from 630 to 350 feet. Here the
road descends from the high glen and turns away from Ben
Wyvis into the valley of the Blackwater.
The grooves are well marked on rocks all the way from
Achnasheen to the lower end of Loch Garve.
At 630 feet near Achnasheen grooves on gneiss point N.
65° E.
At 530 feet, at the junction of two glens near Locli Liochart,
DERRY VEAGII CURVE — CALEDONIAN CANAL, ETC. 149
and the junction of the river wliich drauis Loch Fannicli,
grooves on gneiss point N. 85° E.
Lower down, at Loch Liochart, at about the same level,
550 feet, weathered grooves on gneiss point N. 82° E.
About this level the high glen ends suddenly in a trans-
verse glen. The drift in the upper groove is arranged in
layers which slope down-hill towards the W.S.W. at an angle
of about 35^. This is like the packing of silt by the ebb (vol.
i. p. 339).
Above the inn at Garve, at about 600 feet, grooves on a
rib of white quartz turn with the glen. They do not point
at W}'\^is or up into Strath Bran. They coast round a hill-
side, carefully avoiding the high hills, as rivers do at the lower
level. They point S. 45' E.
At the end of Loch Gan'e, beside the road, grooves on
contorted gneiss take another turn with the glen. At about
150 feet above the sea, the marks point N. 70° E., and aim at
the shoulder of Wyvis, which bars the way. On this hill-
side are piles of drift, and it seems as though a glacier had
ploughed dowTi to the sea-level through the bed of the Black-
water. Near Contin inn the rocks disappear under plains of
rolled drift.
Now, if these marks were made Ijy a land-glacier, it was
twenty-five miles long at least, and it must have had a large
moraine. That mark ought to be foimd somewhere about the
foot of Wyvis, or about Brahan, or Conan. Biit there is no
large moraine with conical hills. There is glacial drift in
profusion, but the moraine shape is not there.
If Strath Bran held a glacier which flowed north and east
towards Ben Wyvis, stones left by it ought to be blocks of
white and gi-ay quartz and gneiss, fragments of rocks in Strath
Bran, and near it. But there is no such collection of native
150
BALTIC CURRENT — BRITISH ISLES — SCOTLAND
drift here. *. If ever there were true hind-gU\ciers in this dis-
trict, they were launched at a high level, in a sea like that
which is now passing Cape Farewell, near the same latitude,
and which now carries "hea\'y drift ice" and " northern drift"
southwards and westwards in sweeping curves.
A -^ — // 'eaOured hill, ground hill, and flat dri/l. Terraces of ivaUr-tvorn gravel and sand at the
foot of Loch Roisg, near Achnasheen, at about 650 or joo /eel aiimv the sea. Sgur-a-Mhiilin, beyond
Strath Bran. Ice-marks run northeastward to the left along Strath Bran to Ben IVyvis.
'I yAireyue^si;U.^'cu- i^p-^'c^J^^ y^^/^y-^^ ^
i^h'j-
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(ic ixftn y^/rC
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'h''^<nre^ 1y^4^_^
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y^ifa^— 1_ , JLl?^ /fi/if~. MAiin'c^ '.-^ >^T ' >^t^»/xcsi
^'^^c^i^'. ^^ ^^J^'^ -^^-^^^ S^^J-^ >T/tw<s <^^^
CHAPTER XXXVIII.
BALTIC CURRENT 11 — BRITISH ISLES 10 — SCOTLAND 7 — STRATH
BRAN, BEINN UAISH, SUTHERLAND, ETC.
Bcinn Uaish. — In travelling down Strath Bran, the end of the
groove seems barred by the great mountain mass of Wyvis
or Beinn Uaish. The highest point of the hill is nearly 4000
feet above the sea, and the base covers a very wide tract.
Seen from Morayshire, and from the new railway near Inver-
ness, it is a great block '' ^ with a rolling plateau on the top,
and on this high base lofty clouds rest when neighbouring
hills are clear.
From the bridge over the Conan, the movements of floats
of white froth may be studied in the black peat water. The
floats move as the water moves, past the piers of the bridge ;
and such curves described by froth are roughly drawn at page
127 and at the end of vol. i. On Conan Bridge, as on any
sloping road, marks made by streams of water flowing past a
stone may be seen. The forms agree with the movement of
floats. In walking up Wyvis from the south-east, the course
of a supposed north-eastern current, which came doAvn the
western shore of Scandinavia, is crossed. These large forms
should resemble the miniature glens on the bridge, if they are
in any way the work of ocean-currents. The shape of the
land about Wyvis corresponds to hollows made by rain on
sand, and to the curves drawn by froth on the Conan ; and
the floats in the Arctic Current in this latitude are large floes
and deep icebergs loaded with boulders. Here Ijoulders, like
152 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
the hill-forms, seem to record the passage of ice-tioats south
-westward at a high level.
Above Dingwall, in the Avoods behind Tidloch, are
numerous boulders of a peculiar kind of pink granite. They
are not common angular blocks, but large rounded blocks,
like those which abound on the northern shores of the lialtic
(see vol. i. pp. 297, 322).
At 540 feet is one 27 feet round and 8 feet high ; it is
rounded on all sides, and a big tree beside it has bent roimd
it in struggling to grow upright. Near it are others of the
same kind, and these rest upon a foundation of brittle slat}'
sandstone (p. 167).
At GOO feet (the level of Achnaslieen) is a Hat block of
gneiss of the same colour and composition as the granite ;
and this block is scored on the upper surface. It is 9 feet
long by 6 broad.
At 800 feet (the level of tlie col at Glen Dochart) are three
large rounded masses of the same granite.
At 950 feet is another, and at this level the top of Brahan
Hill and Torachilty are overlooked.
At 1100 feet, on the top of tliis hill, are more large granite
boulders on a Avide heathery moor ; and from this spot a deep
s^ ^ groove is seen crossing the ridge of Scotland W. by S.
It is Strath liran. If these boidders mark a sea-level, then
the seaway was oj)en over tlie Avatcrshed of Scothuul.
A corresponding groove runs N.E. along the foot of AVyA'is.
At the same height, four miles inland, is another graniti;
boulder at the head of Strath PefTer, opposite a notch in the
shoulder of Wyvis, Avliich opens Strath Conan above Contin
inn, and Strath r)ran behind Torachilty. The Avatei' in the
glen behind Tidloch runs into the Cromarty Firth ; but at
this leA'cl the tides Avould tlow in iiuni the Firth of l>oni()eli.
STEATH BRAN, BEINN UAISII, SUTHERLAND, ETC. 153
At 750 feet, the burn lias cut tlirough a pile of terraced
drift level with terraces at Achnasheeii. The bank is a cliff
of gray clay, which contains numerous scratched stones,
chiefly gray slaty blocks of various sizes, amongst which are
specimens of granite. In the bed of the stream, where the
largest stones are washed clear of rubbish, many large boulders
of gi'anite are mixed with slaty blocks. But there is no
granite hereabouts in situ.
At 1000 feet, up the side of Wyvis, the rock is laid bare
in a small burn. It is a soft slate dipping 10° south, or there-
abouts.
Thus the shape of Wyvis ^ ^ has nothing to do with the
structure of the rock, but is due to deinidation, and ice has
done part of the work so far. There are blocks of granite on
the hill, and a moraine in the glen. Great part of the moraine
seems to have come from the flanks of Wyvis ; and the corrie
in which the glacier moved is seen on the hill-side -^ ■- . But
granite is foreign.
At 1650 feet is a conical hill called Ciocli Mor. It is a
lump of hard coarse conglomerate left standing in the groove.
The sides are scored ; the greatest length corresponds to the
run of the groove ; the steepest end is down-stream towards
the west ; it is a large tor. In the supposed lee are large
blocks of mica-schist, bits of gray quartz rock, and a l)ig
boulder of gneiss.
At 2600 feet, the sea-horizon is open through a groove to
the north-east.
At 3000 feet, the ground on a shoulder of Wyvis is smooth,
flat, and covered with a velvet carpet of yellow-green moss,
over which mountain-hares have traced a pattern of footpaths.
The rock shows in the edge of the deep corrie which was seen
from below. It is a coarse gritty sandstone wliich splits into
154 BALTIC CUllRENT — liKITISII ISLES — SCOTLAND.
thill Hags ; it dips about 8.W. On this liigh shouLU'i- are
blocks of gneiss, weathering and sjilittiug to bits.
The view over the central district of Scotland is very fine.
All the low hills are seen to have one oven slope to a certain
lieight ^ ^, and above that the tops are of a different pattern
A. The Knock of Brae-Moray is a cone planted upon this
upper level, as Cioch is on the shoulder of Wyvis. The high
hills about the head of Strathspey arc steep conical hills, and
the way over the Toridon hills is open. It is a groove -v ^ ;
and, as shown above, it is ice-ground and terraced.
At 2600 feet, on the shoulder, is a rounded boulder of the
Dovre Fjeld and Fininark pattern, ten feet long, and made of
gneiss. It is visible from Dingwall ; and it must have floated
to the shoulder of Wyvis, unless it flew, or slid upon ice all
the way from the parent rock.
The seaway to Scandinavia along the coast of Sutherland
is clear from this point at this level. Not so the top of Wyvis,
which was hidden in mist.
At 2100 feet rock-surfaces are bare on this side facing the
south. They are rounded but much weathered.
At 2000 feet and lower down glaciated surfaces abound, but
tliey are all weathered. At this level the steep side of the
hill ends, and the base has a longer slope to the head of
Strath Peffer.
At 1100 feet are many granite boulders. And on the top
of a sandstone quarry by the road-side near Dingwall, at the
end of the Cromarty Firth, is a cap of glacial drift which
contains large smoothed scored l)locks of granite, and many
other hard igneous rocks.
In the low grounds tlie whole eountry is covered by
masses of similar stones washed and rolled. It is hard to
find one with ice-marks amongst those which have been
STRATH BRAN, BEINN UAISH, SUTHERLAND, ETC. 155
moved in railway-making and other works. This seems to
be the case of the Galway drift repeated. The boulder-clay
has been disturbed and repacked by water, without the help
of sea-ice, below a certain level, and the scratclied boulders
are water-worn in the plain.
From Beinn Slioch to Wyvis the way to Norway is open,
and floats are stranded at 3000 feet. There are no small
ice-grooves left on Wyvis to point out the way, but glens and
hills are but larger grooves and tors, and here they all point
up the coast of Sutherland towards Molde and Trondhjem,
where the coast-line takes a sweep and curves northwards as
far as the Lofoten Islands beyond the Arctic Circle.
Still following the marks on Wyvis, the Sutherla7id coast
trends N. 48° K, and there are no Scotch hills from which the
Wyvis boulders could have floated at 3000 feet.
At the mound near Dunrobin Castle is a high bluff of
coarse conglomerate, on which small ice-marks cannot be seen,
but there larger grooves are remarkably distinct. The whole
hill-face has been scored horizontally from top to bottom.
The grinding force appears to have come along the coast from
the N.E. as the flood does now. But it may also have come
from the opposite direction with the flood, if tides ebbed and
flowed over this part of Scotland, as they are supposed to do
now over part of Greenland.
The woods of Dunrobin, as far as the river Brora, grow
on vast terraced piles of boulders which do not seem
to be moraines. They rest upon the sides of ice-ground hills
above the sea, as if they belonged to a system far larger than
any land-glaciers which now exist even in Iceland. They
may be marks of the " ice-foot."
These terraced heaps are Like the terraces of Northern
Scandinavia, and they are probably effects of the same
156 BALTIC CUrvKENT — BKITISII ISLES — SCOTLAND,
cause. The stones are of the Scaiidinavian pattern, aud some,
at least, may be of Scandmaviau origm. To decide that pomt
special knowledge is required. If Scotland held together and
sunk and rose as Scotchmen are said to do, in a mass, this
coast was under water when Wyvis and the Gairloch hills
were islands, and Caithness at the bottom of the sea. The
terraces appear to be horizontal.
Leaving Scotland and following the curve of the Scotch
coast up to Scandinavia, the same forms recur all the way
to the North Cape. If summer lost the aid of the Gulf Stream,
winter and his fleets of ice would reign in spite of the mid-
night sun of Scandinavia. But if there were Greenland weather
in Norway, there would be a wintry crop in Northern Scot-
land, and Sutherland might grow icebergs instead of wheat
aud dun deer.
Thus starting at Beimi Eith and Beinn Mhonaiilh, on llie
western coast of Scotland, ice-marks at a level of 2000 feet
lead across Scotland to Wj^ds. There boulders mark a sea-
level of 2GU0 or 3000 feet, and the shape of the country and of
the east coast, existing tides, and other marks, all point one
way. When the line is run out at the North Cape, it coin-
cides with an equatorial current, which is continually flowing
into the arctic basin, along the north-western coast of
Norway. If an arctic current flowed out here, and the Gulf
Stream passed westwards by Panama, the climates of these
northern regions would change.
This curve passes very near Trondhjem where a road crosses
to Sweden. Chambers estimated the height of the col at or
below 2000 feet. He found ice-grooves perfectly preserved
on this watershed, and they jiointed N.E. and S.W.*
North-east from this spot there is no land of eqiial height
* K(liiiliurp;li .louiiial, vol. xii. ii. 75.
STRATH BRAN, BEINN UAISII, SUTHERLAND, ETC, 157
now, unless it be in ISTovaya Zenilya, or about the North ^oTli/ </
Pole. So the boulder on Wy vis may liave sailed over Norway, j--^ /<-/ ^ ^*^^
If it came on land-ice, the nevt5 must have been some- , /j
in similar latitudes, in North America, up the valley of tlie
where beyond Scandinavia, the terminal moraine somewhere ,'"^ f^*i*^ns^
beyond Galway ; and a glacier moved in the same direction, n. ^ — >
St. Lawrence, accordnio- to marks there. A Baltic current is _/ /'„ '
easier to swallow, though it is a large draught. <^^(^^ ^^^^^^
Central Sutherland is a wide rolling plateau, with a few /^T^ ,
tall conical hills rising above the moor. " ^^ //k >^^^^
On the west coast the hills are higher, and they are quoted ^ht-x^ / •v^^
hy the most eminent geologists as proofs of enormous de- ^ItA/^M^ C'-/'~'
nudation. On aU the bare hills ice-marks are conspicuous. ^y /^^t*<A
The sketch copied in the woodcut was made from a yacht c/(^*^i.-^ (^
25th September 1848, on a clear calm day with a transparent ^'■) ^^-^/^^■^
atmosphere, and the outlines are tolerably accurate, though ''^^'^'^^'^^i^mmk,.,
each hill was sketched from a different point, as the yacht ^ /f^^^^y
came opposite to it. The shape of tlie surface in the central "^^^^ tA-^ ^ ,1
districts of Sutherland is like that of the upj)er plateau which Ij^^ iUan'H£JC>
divides the Gulf of Bothnia from the arctic basin -^ . The //"f^ •
shapes of the hills on the west coast are like those of hills y, ^ -r,^—
which now rise through glaciers in Iceland A. /iJL / <:'), IT''
The sharp angular peaks in Sutherland are like weathered ^^^/ / ^/
hills elsewhere. Talus-heaps rest below the cliffs from which j^iu-^—. •
stones fall in every frost, and after every fall of rain rivers (hTH^^^oj^
and mountain-streams add to the heaps, and carry part of a ^ >^ ^ < /
them a stage down-hill. But the low grounds in Sutherland, <yV'~ r- ■//
Scandinavia, and Iceland, are not weathered but ground, and 'C- ? ' /> / {j
they all have one characteristic shape. fi/A^a ' /^
In Iceland there is a tract of ice nearly as large as Suther- ^ / ^ /
land, in which neve and ice cover the whole land like a white 2 , / • ^-—^
pall, but the fringe is a black scolloped border of hills, and ^-^ fn^ii r,
U^^^U-. J^9^c^ ^ -^-^ fac^ 4-^e^ ^U^
158
BALTIC CUr.KKNT — BRITISH ISLES — SCOTLAND.
y
some of these are like ilic hills of
Western Sutlierland.
The ice ilows into the central
liollow of Iceland, but it melts before
two l)road streams meet. For a
distance equal to that which the
woodcut includes, two great banks
of ice hem in Sprengisandr, and the
outline of one is like that of the dark
shadow in the sky of the woodcut.
The ice-banks are advancing towards
the sand, as if towards the sea-coast
of Sutherland. But where a Int of
harder rock has pierced the ice-crust,
it stands up as a long ridge, a steep
rock-spur in the round white ice-
mountain ^ ~". It is ii tor ^ " .
One of these hills in Iceland has
the shape of Suil lUieinn, in the
Moodcut of Sutherland. The ice-
stream is splitting at the col, flowing
along the sides, and meeting again
in the lee. One glance is enough to
show the movement, and the hill
retains ice-marks high above the
present ice-level. This hill is a
great ice-tor, which the Arnefells
Jokull has hewed and is still hewing
out of liedded igneous rock. Suil
l^>heinn is another of the same size
and ])atter)i, and tlie same marks are
on both, 1 hough one is igneous, and
Ihc other sedimentary rock.
STRATH BRAN, BEINN UAISH, SUTHERLAND, ETC. 159
They are long ridges pointing up-stream, tors on a large
scale, mounds left in a rock-cutting, by which to measure the
work done ; and the tool-marks are those of ice.
In the woodcut, Suil Bheinn is seen end on, and it looks
like a pillar.* When the hill is seen from the side, it is a
long steep ridge which ends in a knife-edge, and there are not
many places where it can be scaled. The strata of which it
is made are nearly horizontal, and the same beds recur in hills
to the right, beyond the gaps which are valleys of denudation.
According to Geikie and other geologists, who have explored
this district in more detail, the direction of high ice-grooves
coincides with that of passes and main glens, which run from
south-east to north-west, north of Loch Maree (see woodcut,
p. 17).
About the same latitude, on the opposite side of the
Atlantic, the Arctic Current, after flowing south-west along
the coast of Greenland, eddies round Cape Farewell, and flows
north-west, with all its train of ice-floats. It whirls round
again further north, and flows do^^■n to Newfoundland, along
the curve transferred to the map (vol. i. p. 232). A very slight
modification of that cun-e would make it fit the glens of
Sutherland and Caithness, and ice-marks on high passes in
this district. Tlie curve would then represent an eddy in the
North Sea, and such an eddy might well result from a rise of
land in the path of a Baltic current sweeping round the point
of Norway, as the Arctic Current now sweeps round Cape
Farewell. It is easy to test this theory, by building clay
maps of this part of Europe in any shallow pool with a run-
ning stream.
AMieu tlie land rose, land-glaciers would follow tlie present
river-courses, till they melted and Ijecame rivers. And this
* Si'Jai; Icelandii' for pillar.
IGO IJALTIC CURRENT — BRITISH ISLES — SCOTLAND.
seems to liave been the order of change all the way from Gal-
way to North Berwick, from Maliu Head to Cape Wrath and
John o' Groat's House.
First, cold ocean-currents working denudation on a large
scale ; then local denudation worked liy minor causes acting
from watersheds downwards.
From the sea tlie north coast of Sutherland appears to he
ice-ground, but the sea has dug into the rock, and wild L
cliffs overhang a wild sea.
All down the west coast forms of glaciation recur below a
certain level, above which are forms of M'eathering, and the
sea-cliff is forming at the sea-level.
In the islands it is still the same. In the low island of
Lewes ; in the low lands of Harris ; near the high mountains
of the south end of Harris ; in North Uist, Benbecula (Beinn-
e-jVIhaoil), South Uist, Barra, Skye, Mull, Tyree, Jura, Islay,
and in scores of smaller islands, similar forms recur in rocks
of every description.
In the Long Island, for instance, looking from the north
end of South Uist, the low grounds of Benbecula and North
Uist are spread out like a map. There is a wide plain of
peat and sand, salt and fresh Avater, through which low
hummocks of gray rock and piles of boulders appear. In the
midst of this half-drowned land rise two hills of the same
pattern. They slope to the eastward, and are steep to the west-
ward, and they are groiuul and rounded from t(Ji) to bottom.
Memory and rough sketches are enough to show that these
hills are but large tors, of the pattern of Bren Tor in Devonshire,
and hills in Lapland, with the same bearings. A small de-
pression would make them islands, like those which are
scattered broadcast along the Scotch and Norwegian coasts.
If there be striro on these hills, they will point towards
STRATH BEAN, BEINN UAISH, SUTHERLAND, ETC. 161
the Lofoteu Islands, which they resemble ; but they were
not examined for high grooves.
Outside of Hm-ri^ grooves point N.E. and S.W. along the
western coast near the shore beside a road.
In yikyc, at Loch Corrie Uisge, marks of ice can be traced
to a great height, and down to the sea, as clearly as in Eoms-
dal or Justedal, or in a Swiss or Icelandic glen, where ice is
working. This district has been described by Forbes ; it was
first seen by the writer in 1845, while the impression left by
the Alps was fresh, and the work was then attributed to
land-ice.
In Bona, near the lighthouse at the north-eastern end,
the hills seem ground from the north-east, and thence a sea-
way is open to the Xortli Atlantic.
In Raasay, according to Geikie, all the hills are ice-
ground, as he supposes from the south-west by ice sliding
from Skye.
If the gi'inding resulted from the alternate movements of
tides, the opposite ends of these two long islands may well
show opposite movements. The uttermost rock of Scotland,
the Duhh lartach, has a long reef to the south-west.
In Coll and Tyrce are perched blocks. In jMuU, Colonsay,
Oronsay, Jiira, and in Islay, are all the marks attributed to ice ;
and drift-terraces abound.
The Scaur of Eig, that strangest of all the Western
Islands, is a great wall of trap, with notched sides built
upon a pyramidal base of stratified rocks, and one layer in
this masonry contains fossil wood, immediately imder the
trap-wall. The island is another case of denudation ; it is a
tor in the sea ; and it points up into the Sound of Sle^t
X.E. at Strath Bran and the coast of Sutherland. South-
west of it are Muck, Coll, Tyrce, and the Sycire Mhor reef ;
VOL. n. Ai
162 BALTIC CUKRENT — BKITIRII ISLES — SCOTLAND.
and breakers are ijeyoiid. This is a long ridge partly sunk,
and aiming S.W. outside of Islay and Ireland.
The whole of these islands — all the small ones, and the
main ranges of hills and glens in the large ones — have one
general N.E. and S.W. trend.
Any good map shows the form of tlie eoast. There is no
good map of the hills, hut when the Ordnance map appears,
it will show that all these island-forms hear reference to
grooves crossing meridians diagonally south-westwards, like
the chief passes on the mainland, which no map shows.
Further north, the low Shctlands seem all to be ice-
ground rocks.
Tn Orhncy, farmers find their land full of great loose
stones, and the general shape of the low rocks towards the
north is rounded. At the southern end, the coast-lines are
chiefly cliffs of great height, which the sea is undermining.
So the general shape of this country on a map ; the general
shape of the hills as seen from a distance, minute details on
shore ; the general sha])e of Western Euro})e, and oi' the whole
northern hemisphere, — all seem to point to synnnetrical denu-
dation, and to the action of ice on shore and afloat.
Taking the curves of the Arctic Current from Spitzbergen
to Cape Farewell as a natural curve of motion which might
be rejoeated elsewhere, and is extended south of Newfound-
land, the curve can be apjjlied to the British Isles, as shown
roughly in the map (vol. i. p. 232).
A S.W. curve, which comes out of West Fjord in Norway,
jjasses between the Shetlands and the Faro Islands to Eockall.
Curves which start about the watershed of Lapland, near
Kautokeino, etc., skirt the Norwegian coast, pass over the
Shetlands and Hebrides, and coincide with ice-grooves on the
outside of the Island of Harris.
STRATH BRAN, BEINN UAISH, SUTHERLAND, ETC. 1G3
South-west curves drawnii from south-west ice-grooves on
the watershed of Scandinavia beyond Trondhjem, skirt the
Norwegian coast, and the Scotch coast from the Ord of Caith-
ness, to ice-grooves on hills at Dunrobin in Sutherland ; thence
Strath Bran and small ice-grooves carry the curves over Scot-
land, into the Sound of Sleat. The curve passes Coll and
Tyree and the Sgeire Mhor, into the Atlantic, and even imder
water sunken hills and hollows stretch furtlier in the same
direction.
The same curve, begun about boulders on the Dovre Fjeld,
passes seaward with ice-grooves out of Eomsdal, and enters
the Moray Firth. The Caledonian Canal, the Aluckle Glen and
ice-grooves in it, carry the line over Scotland into Loch Linne,
and it passes Colonsay and Oronsay, which are ice-ground.
There, again, sunken rocks extend in long broken ridges
south-westward into the Atlantic. Strong tides and wild seas
work in the hollows, which hold sounds, amongst these islands.
If the sea were cumbered with heavy ice, as it is off Labrador,
there is water-power enough and to spare in this region, to
work the floating ice-engine which, according to Kane, " rubs
rocks."
Curves begun at the head of the Sogne Fjord, at the foot
of the highest hills in Norway, follow ice-grooves to the sea,
and pass by several local glacier-systems near Bergen. They
fall into a series of deep grooves whicli cross central Scotland,
and in these the curves coincide with ice-marks which cross
the watershed, and touch hill-tops in Argyle ; they recur in
Glen Veagh, Donegal, etc., in Ireland.
Curves drawn from boulders on the Fille Fjeld in Norway
fall in with boulders about Aberdeen, skirt the Sidlaw Hills,
where they coincide with marks on the rock ; pass Perth and
Stirling and Glasgow ; Argyll, An-an, and Ceantire ; the Giant's
164 B.VLTIO CURRENT — BRITISH ISLES — SCOTLAND.
Causeway, Sligo, and Westport ; and there are ice-marks all
the way which seem to correspond to a general movement in
that direction, at a high level.
Cm'ves begmi about the Hardanger glaciers run with ice-
marks for a hundred miles in Scandinavia ; join an ice-mark
on North Berwick Law, and wind their way across Scotland
and Ireland to Connemara and Galway, wdiere the spoor is
lost in the sea. It is there as perfect as if made yesterday,
on limestone rocks laid bare in making a railway near the
coast, and on the top of a quartz hill 2000 feet high.
All these several lines have not been followed expressly
to study ice-marks ; but some have, and the rest are pretty
well known to one who has wandered amongst the hills
whenever he could. There is scarcely a Scotch liill or glen,
in island or in mainland, wdiich does not bear some conspicu-
ous mark of glacial denudation. The low marks seem gene-
rally to bear reference to local glacier systems. The high
marks, from 3000 and 2000 feet down to the sea-level in low
passes, appear to bear niference to a general system oi' liori-
zontal movement in water and floating ice, like that which is
now going on further west.
These tlieories, founded upon observation of glacial action
in Switzerland, Scandinavia, and Iceland, and of ice-marks on
rocks at home and abroad, during twenty-two years, are thus
far supported by facts gathered from books and stated above.
They are also propped up by facts observed and gathered by
the latest writers on this cold subject.
They gain strength from facts stateil by geologists in the
Geological Survey of Canada, 1863 ; by Sir Charles Lyell in
his great work on the AntiqiLity of Man, 1863 ; by Professor
llamsay in numerous papers ; by Mr. Ceikie in his work on
tlio aiarial Drift nf Scotland, 1863, wliicli is perliaps the
STRATH BKAN, BEINN UAISH, SUTHERLAND, ETC. 165
best book of its class which has yet appeared. All these
authorities, and a host of witnesses whom they quote, are
agi-eed that the British Isles are ice-ground, and that the
land has been submerged to a height which would only leave
a few hill-tops above water. The facts are beyond cavil ;
they seem to lead to the following conclusions : —
1st, Because raised terraces and sea-margins are nearly
parallel to the plane of the sea, it is probable that the last
rise of land in Ireland, Scotland, and Scandinavia, was a
general swelling movement, which included a very large
area of upheaval.
2d, That the last cold period in this area, and in parti-
cular in Ireland and Scotland, coincided with a sea-level at
least as high as the highest erratics yet found in Scotland
(on Wyvis and Driom Uachdar at 3000 feet) ; and with the
highest horizontal ice-grooves, which are at about 2000 feet
on Shan Folagh in Ireland, and 2000 feet on hills about
Loch Maree. They may yet be found higher.
3d, That the cold period also coincided with the sea-
level, which is marked by the highest Scotch terrace of
glacial drift. The highest known to the ^^Titer is near Dal-
whinny, at about 1400 feet.
4:th, That ice-marks may have been made in deep water
by ice-floats grounding in 1800 feet, while an "ice-foot"
packed drift in terraces at the sea-level ; because these opera-
tions are now going on further west in similar latitudes.
5th, That the last Scotch glaciers which reached the sea
passed away after the land had risen to the level of the
lowest perfect terminal moraine. The lowest of these yet
found by the writer are opposite to glens north and south of
Loch Ericlit near Dalwhinny, at about 1400 feet. All lower
moraines seem to be washed out of shape.
166 BALTIC CURRENT — BRITISH ISLES — SCOTLAND.
6ih, That this level of 1400 feet, and all other levels
marked above that plane, coincided with a general movement
of cold water from the arctic basin south-westwards, which
was varied by tides and impediments, so as to make eddies
like those drawn on the map, vol. i. p. 496.
7th, That this general movement, varied by local tides
and eddies, continiied while there was a strait left open in
Britain ; now continiies in the Straits of Dover and in the
Pentlaud Firth ; and in the Arctic Current and Gulf Stream,
which alter climate in similar latitudes on opposite coasts.
8th, That the end of the last cold period in Scotland
nearly coincided with the sea-level of 1400 feet, which is
marked by a moraine of conical mounds at Dalwhinny, and
by a terrace of glacial drift, partially water-worn, beside the
moraine.
9th, That this change also coincided with the closiug of
a strait by the rise of land in Lapland, which is now 1500
feet above the sea, according to Von Buch's measurement.
10//i, That a gradual subsidence in the same tract would
let in the current by opening the strait, and would bring
back the period of cold to Scotland wlien land had sunk
al)out 1500 feet to the north of the Baltic.
llth, That many similar changes of equal amount, pro-
duced by the same causes, may have taken place ; and that
the present shape of Scotland, Ireland, and Scandinavia chiefly
results from denudation by currents of air and water, which
still circulate. These are driven by mechanical powers which
still work the engine, and guided by laws M'hich produce
regular movements.
12th, Because these laws seem to govern all known quan-
tities and dimensions, small quantities of earth and water,
and streams whicli men can see and guide, serve to help
STRATH BKAN, BEINN UAISH, SUTHERLAND, ETC. 1G7
them to comprehend movements which they cannot control
or see ; or even comprehend without hard thinking.
IWi, Because Scotch and Irish rocks, exposed to the
weather at 2000 feet above the sea, and at the sea-level, still
retain sand-marks which are perfectly fresh, and less weathered
than Egyptian sculpture 4000 years old, the time which has
elapsed since the end of the last British glacial period must
be short. The occupation of the British Isles Ijy the ances-
tors of races who still dwell there may have coincided with
the existence of glaciers on Scotch hills, and traditions may
be dim recollections of these geological facts.
In the course of this journey from Galway to Dingwall,
from Malin Head to Cape Wrath, the Baltic Current theory
has gained strength. Another cast southwards will try the
hobby ; if he is sound after that run, he may be trotted out
and started, to try his chance with other hobbies.
Fig. 81. Rounded Granite Boulder, in a Wood behind Tullocii, restini; on Slate,
.'■)40 feet above tlip sea (p. ^:)■i).
ClIAPTEK XXXIX.
I'.ALTIC CURIIKNT 12 — BRITISH ISLES 11 — ISLE OF MAN.
A KNOWING old pointer quarters his ground on system, and
his system is worthy of imitation by all who search.
Turned loose on the brown moor on a fine breezy morning,
he capers soberly, and shakes his velvet ears, and licks his
slobbering lips, to express his intense enjoyment of freedom
and fresh air ; and then, with quivering nose breast high, and
wavering tail in full play, he settles steadily to his work. He
takes his line and tacks steadily to windward, crossing and
recrossing the straight line which the human sportsman draws
in the wind's eye. When one beat is finished, a wave of the
keeper's hand conveys the order, and the eloquent tail and
ears tell that their owner knows what to do. Up goes the
head, off goes the pointer down wind at score, that he may
beat to windward again. Having beat the northern half of
the ground on the pointer's zigzag plan, let the middle of the
moor have a turn. The S.W. curve drawn from high grounds
at the head of Stetarsdal, past Stavanger, runs over an ice-
ground country in Norway, passes Berwick, the Solway Firth,
the Cumberland hills, the Isle of Man, Drogheda, and Dublin,
and passes out by the Shannon. If one leg of a pair of com-
passes be placed on the Isle of Man, a large circle, described
about that point, nearly touches Duncansby Head, Cape
Wrath, the Butt of Lewes, Cape Clear, the Scilly Isles, the
mouth of the Thames, and Kinnaird Head. The lighthouse
ISLE OF MAN. 169
Oil tlie Calf of Man is near the centre of the British Isles,
and the island may be taken as a miniature of the whole
group.
The Isle of Man is about thirty miles long and twelve
broad ; and the highest point is about 2000 feet above the
sea. The long axis bears about KE. by N.
The north-eastern end of the hill country is rounded ; the
south-western is broken. To the north-east a long low tract
stretches about eight miles from the hills to the point of Ayre.
At the other end the sea has so undermined the hills, that
cliffs are 350 feet high at Brada Head and elsewhere. Ex-
posed trees point about N.E., so the prevailing wind is from
the S.W. The flood-tide comes from the same direction. Drift
timber, like that which the Gulf Stream lands elsewhere on the
British Isles, is sometimes stranded about the Calf of Man.
So the Mull hills, Brada Head, and the south-western coasts
of the Isle of Man, are exposed to wind, and tide, and ocean-
currents, and to large Atlantic waves, which roll up channel.
The point of Ayre, on the contrary, is sheltered.
Denudation and deposition are still going on ; air and
water are at work ; and the form of the work is conspicuous.
Speaking generally, the coast-line is a shelf quarried out of
contorted silurian and other strata, most of which dip at a
high angle. A vertical cliff, and a shattered plain below it,
form an L notch between high and low water mark. On this
shelf the sea packs chips which it digs from the cliff.
At the sheltered north-eastern end the beach is made of
gravel, fine sand, and clay, and it shelves gradually. The out-
line of the coast is smooth, like that of a mud-bank in a mill-
stream. At the battered end the coast-line is jagged, and
beaches are steep and narrow, and generally made of large
egg-shaped boulders, some as big as a man's head. These are
170 BALTIC CURRENT — BRITISH ISLES.
tools with which waves quavry cliffs, and they bear marks of
work. The general shape of sea-worn boulders is curved ;
but their smooth surface is dinted and pitted by small
hollows. Forty or fifty go to a square inch, and each j)it records
a blow. The water-line at the foot of the cliff is also worn
smooth by the rolling of smooth pebbles at some places ; but
generally the rock is jagged, torn, and broken by the storm of
l)oulders, with wliich hea\y rollers, driven by strong winds,
pelt the cliffs.
If the island has risen from an open sea, there should be
beach-marks of this kind on the hills.
On a clear fine morning, after a slight fall of snow and a
strong wind, the shape of the ground is picked out in lines of
black and white ; and on such a day hills in the Isle of
Man, seen from Douglas Bay, appear to be ruled horizontally
up to a height of about 1200 feet. Low dow^n at least three
notches can be made out on the hills which make the horns
of the bay. The lighthouse is perched on one of these shelves.
At about 150 feet above the sea, at the road-side, on tlie hill
to the N.E. of Douglas, a quarry was open in March 1864.
The rock is silurian slate, dipping at a high angle, the same
as the jagged rocks which form the present sea-beach below
the hill. The cap of the quarry is a thick bed of compact
clay, showing signs of deposition in water. It is arranged in
thin beds where it touches the rock, and it contains ice-
ground stones, which may be contrasted with boulders carried
from the beach. The rock-surface is not broken, but shorn
across the edges of the strata, so that the boundary-line
between rock and clay is an even convex curve ^■^. AVlien
this rock-sui'fuce is laid l)are and washed clean, it is found to
bi; smoothed, grooved, and stvialcd from E.N.E.
So ice liad a sliare in licwiii" out tlicso liills nnd marking
ISLE OF MAN. 171
these beach-lines, and it was not ice sliding from the tops,
but ice moving horizontally along the coast, which made these
marks at Douglas, at 150 feet above the present sea-level.
At about 450 feet above the sea, the road from Douglas
to Laxey passes over the ridge in a groove which runs along
the hills from N.E, to S.W., crossing glens in which the drain-
age of the country now flows.
On the jNIull hills, at the south-western end, at least three
shelves can be distinguished on hill-sides and cliff-faces.
These occur at about the same levels wherever they are
visible, on promontories, etc., according to very rough obser-
vations hurriedly made. To get at the full meaning of these
" terraces of erosion," a careful survey should be made.
There are large boulders, at about 450 feet, at the top of
the ridge, between Douglas and Laxey, and also at Brada
Head, at about 450 feet, which seems to be the level of one
of these rock-shelves which surround the whole island.
There is evidence of an ice-laden sea up to this level at
least. At Laxey are two deep glens which run to the water-
shed. They have the shape of glacier-glens, and they contain
large boulders. The marks of a lai'ge glacier will probably be
found in these rock-grooves when they are examined.
A depression of 500 feet would make the Isle of ]NLan a
row of small conical islands, stretching from N.E, to S.W.
North Bariile, 1842 feet, would be at one angle ; the point of
A}Te would be under water ; Cronck Irey na Lahaa (the hill
of the rise of day, 1445 feet, fifteen miles S.W.) would be at
the other end of an archipelago of twelve islands. At lower
levels, cliffs would still be washed by Atlantic Avaves, but
Laxey Glen would be a long sea-loch.
The top of Snsefell (2024 feet according to maps, a little
more according to observation) is conical but rounded, like
172 BALTIC CURRENT— BRITISH ISLES.
all the other hills iu the island. It is stre"Nved with large
slabs of broken slate and blocks of white quartz, apparently
native rocks. Except the shape of the hill itself, there is no
indication of glacial action at the surface near the top, unless
the large quartz blocks are foreign. The hill is j"oined to
Mullagh Oure (Dun Top) by a col which is about 1400 feet
above the sea, and near about the level of a contour-line,
which is seen from Douglas Bay. In March 1864, a gravel-
pit made for a new road gave a section of the surface-beds.
They consist of blue clay with broken angular slate and
grooved stones, covered by a bod of peat and some washings
from the hill. The rock foundation was hidden. The grooved
stones prove that ice moved at this level on this col. The
new road winds along the hill-sides for several miles, keeping
near the watershed where streams part. The cutting along
the road-way, and numerous gravel-pits, show that the cap
consists chiefly of angular stones broken out of the hills, but
these are mingled with numerous blocks carried from some
distant place. Large angular weathered blocks of granular
quartz rock are the most numerous ; specimens of yellow and
red sandstone and of schorl were found in a day's walk, and
some of the boulders were finely polished and grooved.
At the height of about 1100 feet, on a shelf which is
visible from Douglas Harbour, large rounded boulders are
common in fields, in cottage walls, and elsewhere. Though
the surface has been destroyed by weathering and frosts, there
is still evidence to show that ice floated over the cols where
sandstone was dropped. If the sea were now to rise fifty
feet, it would cut off the Mull hills at Port Erin. If it rose
500 feet, it would sink half the island and make a strait at
Douglas. If it were to rise to 1400 feet, where a foreign
boulder now marks an ancient sea-level, little of tlie island
ISLE OF MAN. 173
would remain above water except eleven hill-tops and two
long ridges. If the rise were general in the British Isles,
nearly the whole of England would be sunk, and the nearest
sandstone island left above water would be in Cumberland.
At the south-western end of the hill countr}', granite and
other boulders are strewed on the hills from Peel up to the
verge of the cliff at Brada Head. There are various kinds,
and as Manx granite appears at the surface in two places
only, some of these must be wandering blocks. They are
found at 400 feet and at higlier levels. The people say that
some of these were carried by Phynnodree, or Hairy Breek,
an outcast fairy with shaggy goat's hair and cloven feet, of
whom many curious Manx tales are told. One block, ac-
cording to popular history, was hurled by Goddard Crovan
at his scolding wife. Fin MacCool and his warriors, giants,
and Druids, and other mysterious people, get credit for
moving these mysterious stones.
The country about Castletown is to the south-west of the
hill country, and would be sheltered from a north-eastern
current. It is well described by an able local geologist.'""
It has the outward form of a plain of drift packed in water.
According to Mr. Gumming, it is a bed of drift containing
bits of insular rock, fragments of the coal-measures of Cum-
berland, stones from the south of Scotland, and chalk-Hints
which may have travelled from Antrim, but which may also
have come from Denmark.
This bed of glacial drift rests upon limestone, which is
striated from the magnetic E., say E. by S. Trains of boul-
ders and other marks indicate an ice-laden current moving
* The Isle of Man, its History, Physical, Ecdesimtical, Civil, and Legend-
ary. By the Rev. George Cuniming. London : John Van Voorst, Pater-
noster Row, 1848.
174 BALTIC CURUENT — BKITISII ISLES.
IVoiu the Sohva}' Firth. To this INlr. Cuiimiiug attributes the
" drift," and tlic ice-iuarks in the Isle of Man. He adds, " The
origin of such a current is at present a mere matter of specu-
lation." He suggests that the chief carrying and grinding
agent which worked on these low grounds was floating ice ;
shore-ice, land-ice, and icebergs moved by tides like those
which noA\' ]wur through the sound of Kitterland. If the low
grounds about Castletown were sunk, and the sea up to the
highest notch on the Mull hills, the same tides which now
flow north and south in the main channel, and east and west
in the small cross sound, would flow east and west over Port
Erin and the limestone district of Castletown. But if the sea
were up to 1400 feet, the Solway Firth would be an open
strait, and a deep sea-way would be open through Ireland
along the curve which leads from Stavanger to Shannon. The
tidal wave which now splits on Ireland would pass directly
to Norway over the British Isles, and ice-floats would move in
the direction of ice-marks, if icebergs moved seaward with the
ebb or south-westward with an ocean-current from the Baltic
past Cumberland and the Hill of Dawn in the Isle of Man.
A cast up-stream leads to the Cumberland hills. Boulders
abound by the Avay-side, along the railway line which crosses
this tract. The mountains are very much ice-ground, accord-
ing to those who have examined them, and in all probability
a local glacier-system once radiated from the watershed of this
tract.
In the lower grounds, between Carlisle and Berwick, drift
and ice-marks abound. The trough Avhich holds the two
main rivers in this tract follows the S.W. curve, and in
Geikie's map a red arrow points about N.E. When hill-sides
are examined at about 1000 and 1500 feet above the sea, the
arrows will probably point the other way.
ISLE OF MAN. 175
A sweep northwards brings the line to that curious set of
curves which are seen in the low lands south of the Pentlands,
from the top of these hills, and which are well show^n upon
the Ordnance majj.
A sweep southwards brings the line round to Morpeth.
The clay which covers the rock near Morpeth and Newcastle
is about ten yards thick, and full of scratched boulders. In
making new coal-pits the rock-surface is laid bare, and it is
said to be scored. A promised rubbing has not appeared, but
in all probability the marks at low levels point south on the
east coast. At high levels they ought to point south-west or
thereby, through gaps in the hills, but this point has not been
made good.
On the other side, down-stream, the whole physical geo-
graphy of Ireland is based upon grooves and ridges, rivers,
lakes, points, and sea-lochs, pointing south-westward. Accord-
ing to Jukes {Manual of Geology, p. 680) —
" Tlie rocks of many parts of Ireland, especially those of the south-
west corner of it, exhibit in great perfection that rounding and polish-
ing which glaciers commiuiicate to the rocks over which they glide.
So perfectly indeed are all, even the hardest rocks, rounded and
smoothed, that the very universality of the process prevents its strik-
ing an eye not instructed in the nature of the phenomenon." . . .
" The surface of the rocks on the slopes and tops of the hills are
traversed also by glacial stria)." . . .
The author shows that Ireland may have been elevated
during the glacial period, so as to be within the climate of
land-glaciers, but that it certainly was submerged during the
glacial period, so as to admit of the passage of ice-floats amongst
a group of Irish islands. " At 2000 feet below the present
level, a few small islets only would be left."
It has been shown above that ice moved in a south-
17G BALTIC CURRENT — BRITISH ISLES.
westerly direction, over the tops of hills in Couueniara, one
of which is 2000 feet high. The map of Ireland, reduced from
the Ordnance Survey, shows that the whole island is grooved
in the same direction, and the shape of it corresponds to the
shape of the Isle of Man.
So a cast round the centre of the Britisli Isles helps to swell
the bag of facts, and feed the Baltic Current with a heavy
feast of hard stones, tough facts, and fossil floods of iced-
water.
CHAPTER XL.
BALTK; CURliKNT 13 — BRITISH ISLES 12 — YORKSHIRE
AND WALES, ETC.
A CURVE begun in Novaya Zenilya, and drawii over Lapland,
near the head of the Gulf of Kandalaksha in the White Sea,
passes near Tornea, runs down the Swedish coast to Sunds-
vall, touches Christiania and Christiansaud, and lands at
Whitby. It crosses Yorkshire, passes Manchester and Liver-
pool, and passes behind Snowdon into Cardigan Bay, skirt-
ing the coast of Ireland from Wexf()rd to Cape Clear.
Part of the country has been descrilted above (chap. xiv.
to XX.), and there ice-marks point to a current moving
south-westwards. In Lyell's Antiquity of Man, p. 270,
glacial phenomena in Ireland are described, and the geolo-
gical survey and former writers are quoted.
Signs of glaciation have been traced to elevations of 2oO(J
feet in the Killarney district. Marine shells have rarely
been met with higher than 600 feet above the sea, and that
chiefly in gravel clay and sand in Wicklow and Wexford.
Above 2500 feet, rocks are rough, below that elevation
smooth, and " drift" has been traced as high as 1500 feet on
hills which reach to .3400 feet. Taking the symbols used
above, the form A characteristic of weathering, is characteristic
of Irish hills down to a level of 2500 feet. Below that level the
characteristic form is - — v. At 1500 feet drift is deposited ;
VOL. II. N
178 I'.ALTFC criiKKNT — lUtlTtSlI ISI.KS.
at 6U0 feet are sea-shells of arctic type in beds of gravel.
Except in a few cases, the transport of erratics is southwards
and westwards, and the prevailing trend of mountain-ranges
is south-westwards. Sir C. Lyeirs map, p. 278, is the best of
its kind, and it shows that currents moving througli the
r.ritish Isles at a level of GOO feet, and governed by the
same laws which affect the present run of tides, might pass
along part of the curves which have been followed thus far.
At 1500 feet, Lapland would be under water, and the way
open from Novaya Zendya to Wicklow, if the submergence
were general in this tract of Europe. Keith Johnston's map
(plate 10, Physical Atlas) shows that volcanic disturbance has
affected areas of equal size in modern times.
If the climate was cold Avhen the districts above men-
tioned were under water ; if glaciers grew in Scotland, Ire-
land, and the Isle of Man ; then it is probable that climate in
England was cold at the same time, and Englisli hills ought to
retain ice-marks.
In Vnrkshire is a hilly tract where the higliest points are
iibout 2000 feet above the sea.
The country is composed of beds of sandstone, shale, car-
boniferous limestone, and suchlike rocks ; disposed horizon-
tally, but broken and shattered and bent, dislocated and
upheaved in many places. Where a stream of running water
has made a bed in the rocks, it has generally cut a deep trench
with steep or perpendicular sides, or the banks have fallen
so as to leave a slope of tains under a cliff. But the whole
district is furrowed by deep glens whose rounded form bears
no sort of resemblance to the beds of streams and torrents
which flow through them, or fall into them. A section
across one of the Yorkshire dales is like a section of an
Irclaiidic glen — a sweei)ing curve, not a stei'p ti'encli — and the
YORKSHIRE AND WALES, ETC. 179
sides are terraced ; each terrace corresponding to a bed of rock.
The dales are deep grooves winding in long sweeping curves,
like dales which now contain glaciers elsewhere ; the hills
are rounded ^^, the glens grooves ^^ ; the terraced sides
are like coasts represented in Parry's Voyages to Baffin's Sea.
These, also, are composed of beds which are nearly horizontal,
and are now undergoing denudation by weathering and ice,
and there glaciers flow through glens with terraced sides.
No small ice-grooves were found in a rapid journey
through the Yorkshire hills, but sandstone and limestone
weather so fast that fine tool-marks speedily wear out. The
dales themselves remain, and they are full of patches of
drift, — of ridges, mounds, banks, and hills of foreign boul-
ders, sand, and clay.
In some glens, as in Wharfdale, small terraces like those
which occur at Melar in Iceland sweep along the hill-sides.
They are not horizontal, so they are not beaches or water-
marks ; they are not the edges of strata, like terraces above
them ; they are about the size of vine-terraces, which are
made on hill-sides near the Ehine, and they sweep round
hollows and promontories in green fields, like works of art.
Where a river has cut through them, their section shows
loose gravel, sand, clay, and stones, disposed like broad steps
upon the rocky foundation of the hollowed dale.
If a local system of land-glaciers filled upper glens, and a
general system of currents worked in from the north-east —
while tides floated field-ice, land-ice, and icebergs up and
down, pushing gravel along the bottom — the forms of these
glens, and of small terraces in them, might be explained by
the known effects of ice elsewhere.
These dales were hollowed out by some wearing process ;
for beds of stone can be followed from glen to glen, and
180 BALTIC CIHKENT — BinTISH ISLES.
from hill to hill, vound, and even through the iiills in the
mines.
They are not tlie work of rivers ; for denudation by
running water is very well exemplified at the lead-washing
floors, and the work differs.
In one process lead-ore and vein-stone are cruslied to
powder, and washed by a stream through a funnel into the
centre of a shallow pit, A machine revolves in the pit,
sweeping the surface of the fallen mud with a heavy coarse
cloth, so as to give it time to separate according to comparative
weight. Heavy lead-ore sinks first and fastest ; lighter mi-
nerals roll further, and sink slower; and when the operation
is finished, there remains a stratified convex mound, whose
outline is a regular curve ^ — ^. When water is poured upon
the top of this dome, it cuts miniature glens in the sides of
the hillock of sediment, as rivers do through hills of sand-
stone ; and each glen has its delta. If rivers dug out the
Yorkshire dales, their forms ought to agree with these. The
miniature glens are, in fact, very like the beds of torrents
in the country ; but they are wholly unlike the dales in which
the torrents flow.
Form asserts the agency of glaciers and ocean-currents,
and denies the agency of rivers in the large denudation of
the Yorkshire dales. The tool-marks are like those of frost
elsewhere. As shown above, a theoretical curve leads near
Christiania, and there the long groove of Gulbrandsdal runs
up to the watershed of Norway at the Dovre Fjeld. The general
sha])(,' of the big Norwegian dale is very like that of the
smaller dales of Yorkshire.
StoJce. — AI)out Stoke, the English watershed is 37u or
400 feet above the sea. The rocks belong to the coal-for-
mation, but a few granite boulders are strewed about the
YORKSHIKE AND WALES, ETC. 181
fields, Xo other ice-marks were found ; but the counti y
is thickly peopled and highly cultivated ; the rock buried
under beds of clay and sand. iNlinton makes china and
encaustic tiles of glacial chips, while coals and iron are
dug from beds 1200 feet below the sea-level, where the
temperature is 68^ in the coal, and the temperature outside
about 49°.
This land was above water when the coals were plants
growing in air ; it Mas under water when sand was poured
over the bed of peat ; it has been up and down while 1500
feet of coal-formation beds were deposited. The whole series
of rocks has been hardened and tilted bodily up and broken ;
and the broken surface has been worn smooth and furrowed.
The worn surface was surely under water when the drift and
clay were dropped there ; and the granite boulder records the
passage of ice at this point on the curve.
The railway gives the line of lowest level, and here Brad-
shaw's Railv:ay Guide and a net of iron roads carry the curve
in any direction ; for there are no hills about Stoke.
Manchester and Liverpool. — At a late meeting of the Man-
chester Geological Society, glaciated rocks were described.
These occur on Bidstou Hill and elsewhere near Liverpool,
at a level of about 200 feet. The direction was N. and S., E.
and "NV., N.W. and S.E. Amongst these low hills, currents
might flow in any direction, as tides do amongst the banks off'
Liverpool, at various states of the tide,
Cheshire — The railway map gives a very intricate pattern
in Cheshire. The country is high and varied by round hills.
Hartford station is about 270 feet above London. Tlie low
grounds are covered with water-worn drift, in which sea-shells
are found. Amongst the stones are granite, chalk-flints, green-
stones, and various hard rocks. Large Idocks of granite, with
182 BALTIC CURKKNT — BKITISH ISLES.
fresh ice-iDavks uii them, are found, and many are broken u])
and iised.
The village of Eaton stands on a hill of bare rock, which
is new red sandstone disposed in horizontal beds. Several
large blocks of granite and greenstone are placed by the road-
side, near wells, and at corners. On some of them the polish
is well preserved, and grooves are fresh. On the top of the
hill, in a sandy lane, a small boulder of green porphyry was
found. It was about the size of a small turnip, subangular,
and with a perfect surface grooved on three sides. The shape
of the rounded sandstone hills bears no relation to dip, fracture,
or bedding. They are carved out by some engine, and ice
certainly passed over the hills at Eaton. The top of the hill
is 340 feet above Oulton. Hollows seem to run E. and \V.
The cax? of the quarry consists of broken flags and sand.
Other boulders of granite and gray quartz with perfect sur-
faces were found in a garden ; and this was the owner's
account of them : —
"Them is what we call marble stones ; they grow in the
yearth, especially in places where they are bringing in new
ground. You see the yearth produces all sorts of things for
the good iii' man. The top produces all manner of vegetables,
and underneath there 's all sorts of mines and minerals for the
good of man, and these stones grow in the yearth amongst the
sand."
So s])oke the village sage.
The sand seems to tell of cold tides flowing in the Vale of
Chester, for sand-pits show mounds of contorted sand-beds,
whose foldings arc hard to unravel, unless they were frozen
and melted like the sand-heap mentioned above (vol. i. ]).
!jS()). A fringe of crystal ice hung in a sandstone ([uany,
and a brittle cru.sl of tliin Hal ice on the mill-dam, was all
YORKSHIRE AND WALES, ETC. \^'^
that remained of Cheshire ice ; but mental eyes looked over
the water to Hamilton Inlet, and saw the pictures which
other men have drawn.
At JVorthwich numerous boulders of large size, specimens
of granite, greenstones, and other hard rocks, are set up in the
town. In fields near the town heaps of small boulders occur.
The whole town is sinking from the constant waste of the
brine springs. About a million of tons of salt pay canal
dues every year. In one dry mine the salt is quarried for a
depth of thirteen feet, in an area of twenty-three acres.
The temperature is 51° at all seasons. The heat of the
earth below, and the weiglit of cold air above, together pro-
duce a constant movement of air. It rises up one shaft and
falls down another. A greater difference of temperature
evaporates water in the salt-pans. Steam rises and water
falls. Steam in the boiler lifts the piston of the steam-
engine which pumps up the brine, and lifts and lowers the
miners and their millions of tons of salt. The same heat-
power, set to lift Cheshire and evaporate the sea ; the same
weight-power, set to condense steam and lower the earth's
crust ; the same natural powers which men chain to their
wheels — seem strong enoiigh to work the natural engine which
ground and polislied granite boulders, and carried them to
Northwich.
It is plain that ice travelled here, it is equally plain that
low ice-marks will not unravel the ice-problem. The Che-
shire boulders did not come from Wales or Yorkshire. They
may have come oiit of Cumberland, but it is possible that they
came from Sweden or Lapland, because zircon syenite was
found in Galloway by Jameson, and at Christiania and in
Lapland by Von Buch, and because boulders are on tlu-
watershed of Kngiand, about Stoke.
ISI
UAI.TIC iTHKKNT— BHITISH ISLKS.
//VE
\nx^ been mapped by the
Or(huuice, jiiul surveyed by
geologists ; it is the scene
of Sir Eoderick ^lurchi-
son's discoveries, and classic
ground. In the book of
the Alpine Club* the glacial
■^ phenomena of Wales are
described by Professor Earn-
say, who states his own
S w ^1/ views, which coincided with
j,,j^, g., those of the best modern
geologists.
It seems tu be atlmitted that sea-ice stranded drift
amongst the Welsh hills at a height of about 2300 feet, that
local land-glaciers ploughed out the drift when the land rose ;
but no attempt seems yet to have been made to account for
the change of climate which destroyed the Welsh glaciers
and turned winter to spring. If England were submerged
2:300 feet, then tlie nearest land to the north-east would be
Scandinavia, and a way open for the curve whose direction is
shown on tlie woodcut.
The Principality i.s an oblong block of high land
whose four sides face the cardinal points. The corner next
Liverpool faces the north-east, the ])oint from which an arctic
current now flows in tin; same latitudes be}'ond the sea.
The corner near Milford Haven faces the south-west, the
point IVom wliich the tides come now; from which the
(■(^uatorial (lulf Stream flows towards our coast, and from
\vhi(;h it is assiimed that a prevailing ecpuitorial current of
air has blown ever since there was an atmosjihere, and will
•'■■ I'iMks. I-assr-s. ;ma ClHci.Ts nftlir 111-1, \\y^. LonKtllilH, LSf.?.
Yorkshire and wales, etc. 185
continue to blow till the state of the atmosphere and the laws
which govern its movements are changed.
The north-western corner of the block is Anglesea, and the
south-eastern is rounded off by the Severn valley.
If a north-east stream flowed from the Cumberland and
Yorkshire hills, it would cross two corners diagonally as south-
western gales do. If the wearing power moved from the south-
west, then the soft rocks of South Wales ought to bear the
strongest marks of abrasion.
In fact the coal-beds are most ground away at the north-
east side of Wales.
From the western side of the block the hollow of Car-
digan Bay seems at first sight to have been scooped out in a
north-easterly direction by south-west waves. In looking at
a map where land only is marked, we are apt to forget that
the sea is but land covered with water. A sea-coast line is
therefore commonly mentioned as a form resulting from
marine denudation, a curved line produced by sea-waves act-
ing unequally upon rocks of various hardness. It seems to
be assumed that a hollow curve like Cardigan Bay was very
slowly scooped out of the edge of a block of high land by
the great rollers which still sweep in from the south-west.
If Cardigan Bay were simply ocean-work of this kind, the
whole coast-line would retain the tool-marks of waves.
The rocks would be steep, broken, and angular, like the
precipice which overhangs the sea at Aberystwith. There
would be heaps of fallen debris and beaches of rolled stones
beneath a bold coast-line, for sea-waves can only act between
wind and water.
The sea does wear away this land, but it works as a pond
does, by undermining and breaking down its banks.
The form of Cardigan Bav is not whollv due to the slow
(^
186 BALTIC CUKKENT — HKIT181I LSLES.
action of Atlantic waves, for the coast is not generally pre-
cipitous. The coast-line is due to the surface-form of the
land, whose valleys and ridges stretch out under the sea,
and Cardigan Bay is part of a large hollow. The surface of
denudation has been broken through by sea-waves at many
places at the sea-level, and there are many sea-clifis ; but the
rock-surface has been preserved else\vhere, and the bottom of
Cardigan Bay is but a continuation of the rocks of Wales.
In particular, at the head of Cardigan Bay a series of deep
glens are continued under water ; and if the fifteen-fathom
line were the coast-line, there would still be a long tjord oH'
Portmadoc, running N.E. and S.W. as the glens do on shore.
Tradition. — Modern geologists are rapidly nearing a con-
chision at which many have arrived. It is held that men, and
certain large animals which no longer exist — great haiiy
elephants, rhinoceroses, elks, cave-bears, and otlier such crea-
tures— existed together in parts of Great Britain and in France,
at a time when the climate of these countries was at least as
cold as it is now in the same latitudes on the Labrador coast.
The oldest of the races who now inhabit Western France
and the British Isles are admitted to be Lapps, Basijues, Celts,
and Cymri. If geologists are right, the ancestors of these
races may possibly have lived in the end of the cold period
where their descendants now live ; or they may have foinid
older races there, whose ancestors had hunted hairy elephants
and wild bulls amongst glaciers in Scotland, Ireland, and
Wales. The race may have witnessed great changes in sea
and land. Lapps have traditions about giants and big beasts.
Al)out Basque traditions little has been published, and that
little does not bear upon this subject.
There arc several collections o! Celtic tvaditioiis. Sir
s Charles Lyell (juoles some British stories in his I'vinciplcs of
A ' ' ~^a/ v/ ^q^ ih.^^ a^vu^ a^ ^ y^-cA^
7^^^ ^(A/v yu^'i^ ci Tk^ U^i^i^ x^'^^^^i^x.^jioLi^
YUKKSHIKE AND WALES, ETC. 187
Geology, and anotlier geologist is about to publish a collection
of Cornish tales, y^ In Cornwall Celtic traditions, which seem Q)
to record changes of sea-level, abound. Celtic and Scandina-
vian traditions, as the oldest of western traditions yet col-
lected, may bear upon late geological changes in the west.
Charts which give the depth of the sea, such as Keith
Johnston's (plate 6), show that a very slight rise or fall of land
or sea would now alter the outline of Wales very materially.
If the land were to sink ninety feet, Aberystwith would be
imder water, and the church-steeple awash in the middle of
a fjord ten or twelve miles long. If the sinking were general,
the majority of Welshmen and Welsh towns would share the
same fate ; and if the land has in fact sunk that much, the
evidence has sunk with it.
If the land were now to rise ninety feet, so as to make the
line of fifteen fathoms the coast-line, great part of the land now
under water in Cardigan Bay would become dry land, and
rounded rocky islands and points which now slope away
beneath the water-line would be rocky knolls and ridges,
like those which rise up through drift and peat-moss in
every Welsh glen.
If like changes were now to take place in Brittany, the
coast-line would alter as much or more in that region. When
land has risen from the sea, the evidence remains for those
who will accept it ; and in Wales the evidence shows that
land has risen about 2300 feet since Snowdon was a mountain.
Sea-shells have been found in the loose soil at a heiglit of
1392 feet, according to Professor Piamsay ; and at 1630 feet,
according to Keith Johnston's Atlas ; and, according to Sir
C. Lyell, stratified drift-beds exist still higher. If these great
changes of level took place suddenly, rapidly, or even
gradually, by fits and starts, at a tiniP when there were
188 BALTIC CURRENT — BRITISH ISLES.
ancient Britons and ancient Gauls, memorable disasters might
result, which tradition may yet vaguely remember.
In Wales and in Brittany there are, in fact, many tradi-
tions which seem to point to such geological changes as a
sinking of land ; to great disasters, and to the existence of
animals which have passed away ; and in all works on geology
evidence is given to support these traditions.
In Wales it is told that Cardigan Bay covers a land which
was thickly peopled by a wicked race who were overwhelmed
by the sea, and sunken forests are at the sea-margin in
Ireland,
In Brittany, according to the popular tale,* the wicked
Princess Dahut, the daughter of King Grallon, and all her
court, were overwhelmed in the city of Keris, near Quimper,
which stood " where now you see the Bay of Douarnenez,"
near Brest. "K^ing. Grallon was a good man, and he was saved
by a saint, whom he had made a bishop. The author of the
Foyer Breton maintains in a note that the ruins of a town
yet exist under water between the Cap de la Chevre and the
Pointe du Eaz.
In Normandy it is told that the tenure by M'hich a certain
abbot held his land was the service of laying a plank for his
superior to walk over from Jersey to the mainland of France.
Mont St. Michel, it is said, was in a great forest when its
owner went to the wars ; when he returned, he tbund it a
rock in a wide plain of sea-sand. The church on the top
saved the rock from the destruction which overwhelmed the
wicked plain. There appears to be some geological evidence
for the existence of the drowned forest.
In England there is a tradition that merchandise was
caiiicd f»ii lioiseback from Winchester to Puckaster Cove iji
* F.iycr I'.rcloii. vnl. i. p. 232.
YORKSHIRE AND WALES, ETC. 189
the Isle of Wight. But there is good evidence to prove that
no great change of sea-level has taken place since the Eoman
invasion.
In Ireland the good O'Donoghue rises once a year, in Ma}-
morning, and rides in procession along the smooth surface of
the Lake of Killarney ; hut there is no evidence to support him.
Near the Isle of 'Sla.n, Fin MacCool and his sunken
country rise once in seven years to the surface, and sink
down again ; but if any one coiild cast a Bible on the land,
the good old times of Fin and his heroes would return, and
his land would remain above water. Geologists suppose that
the channel was in fact dry when big elks lived in the Isle
of Man, where skeletons have been found entire.
In Scotland there are endless traditions of the same kind.
Tales of castles, towns, and houses sunk beneath the waves,
and visible in calm weather ; of islands which appear upon
the western horizon, and sink down again ; of lands where no
land is, discovered in a thick fog by sailors, who find grand-
looldng stalwart men drinking ale from vast cups. They are
the ancient mythical heroes in the " land of youth," and the
"green isle," and the "land under the waves;" and who rise
from time to time to show what men used to be, and what
they still are in " Flathinnis," the abode of heroes.
In Ireland, as in every Celtic country, the same tales of
land rising and sinking abound in endless variety ; and they
prevailed in the days of Queen Elizabeth, for they are recorded
by Giraldus Cambrensis as facts.
In Scandinavia, the wicked city is not droioned, but seven
parishes are smothered under snow and ice, and the church-
bells may still be heard ringing under the glaciers of the
Folge Fond.
Similar traditions of ancient kings — Barbarossa, Arthur,
190 I'.ALTIC CURRENT — lililTISlI ISLES.
etc. — enchanted, with all their warriors, ready to come forth to
battle when summoned, prevail all over Europe, wherever
popular tales have been collected. These myths seem to
resolve themselves into a belief in a spirit-land ; and many
incidents seem to be borrowed from Holy Writ. But popular
imagination has dressed the model in picturesque drapery,
and the figures are often placed in landscapes painted from
nature at home.
The inhabitants of central Europe, and Teutonic races
who came late to England, place their mythical heroes under
ground in caves, in vaults beneath enchanted castles, or in
mounds which rise up and open, and show their buried inha-
bitants alive and busy about the avocations of earthly men.
They find their heroes Avliere they placed their bodies — under
ground. y\
The Celtic races who came early to the west, and to the
coast-line, j)lace Arthur and Fionn, Merlin and Ossian, and
all their following of bards and warriors, and those who
have inherited their attributes, in islands, in lakes, or in a
land beneath the waves of the sea. Perhaps they find them
where they lost them or placed their bodies.*
In jVIorayshire, the buried race are supposed to be under
the sandhills, as they are in some parts of Brittany ; and as a
matter of fact, marks of ancient cultivation constantly appear
in the trough of the sand-waves of jMoray, Where the
adjuncts of a myth fit the countiy and the facts in so
many known ways, they probably fit equally well in the
matter of unknown change in a coast-line.
If Wales sunk ninety feet, after men had taken possession
of it, the line of fifteen fathoms marks off a tract of low
* Tlie savage inhabitants of Tiorra del Fuogo sink tlicii- dond in dcop wiitor,
nci'ordiiK' to .\<lniiinl Fitzrov.
00 ScL. Nial 5 ^^ -
YORKSHIRE AND WALES, ETC 191
countr}' more than twenty miles wide, which was drowned
in Cardigan Bay, as Welsh tradition relates. If France went
down as much after a town was built at the end of a valley
near Brest, the town was drowned as Aberystwith would be,
and the valley became a bay as the Breton tale describes.
If ocean-currents change places, and climates are transferred
for a time, flourishing valleys and mountain pastures might
become the beds of glaciers and snow-heaps, as the Scandina-
vians tell. The Justedal glaciers have in fact advanced and
retired again a short distance, and Swiss glaciers have done
the same in modem times.
All these mythical disasters may be, and very probably
are, records of real events, witnessed by men, and related by
generation to generation ; though the wickedness of the
people, the miracles, the marvels, and the religious features
of the stoiy as now told, may have been invented or added
when Christianity was first taught to a nide people. If Wales
were to sink ninety feet now, the survivors on the mountains
would be apt to quote the destruction of the " cities of the
plain" as a parallel to the destruction of Welsh watering-
places, where the majority of the inhabitants are strangers
who cannot speak Welsh.
In the case of extinct animals, tradition may be true also.
There is a widely-spread popular tale, common to Ireland
and Scotland, and told with many variations. The gist of it
is, that in the days of Fionn there were deer and birds far
larger than any which now exist.
Ossian, it is said, when old and blind, lived in the house
of his father-in-law, or in the house of St. Patrick, and they
were busily writing down all he had to tell them of the his-
toiy of the Feinne. But no one would believe what he said
about the strenath of the men, and the size of the deer, the
192 BALTIC I THKENT — BRITISH ISLES.
birds, the leaves, and the rolls of butter, that there were iu
the " Feinne," the country and age of Fionn.
To convince the unbelievers, the last of the old race
prayed that he might have one more day's hunting, and his
prayer was heard. A boy and a dog, the worst of their class,
came to hiui in the night, and with them he went to some
unknown glen* There, with many strange incidents, it is told
how they found a whistle and a store of arms, and a great
caldron, and how the l»lind hero collected deer and birds by
sounding his whistle, or horn, or " dord." Deer came as big
as houses, or birds as big as oxen. Guided by the boy his
hand drew the bow and slew the quarry, and when the chase
was done they dined as heroes used to dine. A hind-quarter
was brought home, and the bone of an ox went round about
in the marrow-hole of the shank of the creature which (Jssian
had brought from the " Feinne." With endless variations,
this story is told all over Ireland and Scotland ; and it is
firmly believed by a ver}' large class of her Majesty's
Celtic subjects in Ireland, Scotland, and Wales, that there
were giants and monstrous animals in the days of King
Arthur and of Fionn. There is no geological evidence yet for
gigantic men, but peat-bogs, gravel, and caves, are full of the
bones of beasts as big as a small haystack ; and the word
used in the tale, " j^on," means " Elk" as well as bird.
In beds of superficial drift, in caves, in peat, clay, and
gravel, near Torquay, in Wales, in the Isle of Man, in Ire-
land and in Scotland, bones of big British beasts have been
found. Amongst tliem are — cave-bears larger than any
living species, tigers twice the size of those of Bengal, ele-
phants twice as large as tliose commonly found in Africa
* 'I'll!' frloii is iKiiiitcd nut in SuthcrlMiid. in'nr |)ni-*liii. and :it iiitrrni.'-
diatc .sjwt.s. ^
YORKSIIIKK AND WALES, ETC. 193
and Ceylou, two large species of rhinoceros, hippopotami as
bulky as those of Africa, great cave-hyeenas and lions, elk as
tall as horses, gigantic oxen, reindeer of the ordinary size,
and big red-deer with horns like wapiti. Did these or some
or all of them live within the memory of human tradition?
Tradition seems to remember big beasts and ice-clad
mountains, philosophy finds human bones so placed as to
support tradition. The ruins of a drowned town support
the Breton tale which describes its destruction. Thus legends
rest upon piles of old bones ; tradition and geology support
each other, and point the same way. Two separate and
very different routes lead back to a time when men and
elephants were drowned by changes in tlie level of sea and
land, in countries now inhabited by Celts and Cymri, and
the last discovery in France brings men who could carve
good pictures of reindeer, and bones of reindeer of large size,
into one place, where bones and works of human art are
enclosed in slabs of stalagmite.
If the block of land which is now Wales has been up and
down, under water, awash and high and dry ; if arctic and
equatorial streams have spent their force upon it, the surface
must bear their marks.
Supposing an arctic current to break upon the north-
eastern corner of Wales, that corner ought to be worn away
to a slope facing the current, and beds of rock should be
broken short off to form precipices on the south-western
side, if heavy ice was driven over the hills towards the S.W^
It is so in the small scale in all valleys where glaciers
have slid downwards. It is so in the valley of Gwynant
near Beddgelert, and similar action would produce like form
on any scale (see cut, p. fi).
Standing upon Liffh OrmeH Head and looking south-east,
VOL. IL 0
194 BALTIC CURUENT — BKITISH ISLES.
the north-eastern corner of AVtdes is seen in profile, and the
general outline of the country has the form of small rocks
worn down by ice which moved from N.E. to S.W.
To a practised eye the Welsh hills seem to tell their
story of movement from the N.E. as clearly as Welsh trees
do of movement from the S.W. (see vol. i. p. 59).
Looking south-west from the same point, the end of the
ridge, of which Snowdon is the highest point, is seen over a
foreground of bare rocks about 700 feet high, and it is mani-
fest that the outline of the distant ridge of high hills seen in
this direction is something wholly different from the fore-
ground, which is like the rounded hills about IMold and
Wrexham. Those can be seen by looking S.E.
Looking W. and N.W. the outline of Anglesea is some-
thing different from them all. When that island is crossed
it is like a worn grooved slab of stone. From Ormes Head
it seems to be a low uiululating line nearly parallel to tlie
horizon.
If after seeing hills in profile the observer could fly over
tliem, he would gain a better notion of their shape.
In the case of Wales the country has been so admirably
ma[)ped by the Ordnance Survey that to look down upon a
map is almost as instructive as to sail over the country in a
balloon. In the Ordnance map of this district, the high
hills and the low country are seen to have a totally different
configuration.
The Snowdon ridge, 3570 feet high, extends N.E. and
S.\y., and great valleys and corries seem to have been
gouged out of it in every possible direction. But on botli
sides of the ridge the country is furrowed by long grooves,
which run N.E. and S.W. In the deepest of these is the
Menai Strait. Anothei' runs into Cardigan P>av. The
YOKKSHIRE AND WALES, ETC. 195
north-eastern corner of the block has in fact been worn
down by some force acting from tlie KK, and the north-
western corner has been furrowed diagonally in tlie same
direction.
To one used to tlie look of ice-ground hills, the whole
of North Wales, excejit the SnoAvdon range, appears to liave
been first ice-ground in one direction, and then further ice-
ground in all possible directions, l)y local river-glaciers of
great size, which hewed out glens.
The low hills at Little Ormes Head and Llandudno are
much weathered, but they retain their general form. They
are very bare, so that their form can be well seen, but here
and there patches of drift, clay, and boulders, and 1)ig perched
blocks, occur near the top of the hills.
The broad low isthmus which joins Great Ormes Head to
the mainland seems to be chiefly composed of rounded boulders
of all sorts and sizes. It is probably an old moraine ai'ranged
by the sea, and it contains specimens of many kinds of rock
which are not found in the immediate neighbourhood.
Looking down from the ruined battlements of Conway
Castle on a fine evening, after a strong northerly breeze has
nearly blown itself out, the forms of the miniature waves on tlu;
river, and of larger solid wave-marks made at high tide upon
the sandbanks, by larger water-waves, may be seen and com-
pared. They are almost identical : one set is moving, the
other is at rest ; but the wave-mark shows how a wave
moved, and copies it. Looking up to the hill-sides where the
trees are exposed, their form tells of a prevailing wind
which bends them towards the north-east. Looking to the
hills themselves, they have the form of wave-marks, caused
by a north-east wind ; for they have been swept by the force
which carried perched blocks, and arranged the boulders
196 BALTIC CURRENT — URITISII ISLES.
about Llandudno. There is no known force but ice wliich
could so grind rocks and carry sucli stones.
At Chester, Llangollen, AVrexliam, Mold, Holywell, Ehyll,
Abergele, high up and low down, the north-eastern corner of
Wales looks like a block worn down from the N.E.
The hills are much weathered, but they all retain a general
form. Patches of sand, clay, and l)oulders rest in hollows ;
and on hill-tops perched blocks rest at all elevations from the
sea, to about 1000 feet.
About Macs-y-Safn, and this north-eastern corner of Wales
generally, it is hopeless to search for high strioe upon the
limestone rocks ; for they are so weathered as to leave delicate
fossils projecting far above the surface. Eain-water seems
to dissolve limestone like salt. It is vain to search for
strife on grits and sandstones, which crumble at a touch ; but
the whole of these hills have their longest slope towards the
KE. ; in which direction the beds also dip at a higher angle.
The steepest side is generally towards the S.W.
Sometimes the beds are broken, so as to leave precipitous
faces of mountain limestone. Sometimes these edges are
rounded off.
Glens are rounded grooves, and seem to be gouged out of
the rock without reference to bedding ; and every shape in
the country seems to tell of some great mass moving over the
surface of the land, and grinding it down.
There are three stages — first, a low alluvial ])lain, but little
raised above the sea-level, which stretches far up into the
glens ; for example, at Ehyll. This seems to consist of trans-
ported materials. The next stage is a rolling rock-jjlateau,
about 1000 feet above the sea. It is steep towards the N.,
and slopes gradually towards the E. and N.E. In the low
grounds to tlio cast, and on tliis ])lat(^au, arc beds of drill and
YOKKSHIKE AND WALES, ETC
197
Fig. 83. N. E. Corni
boulders. The liills at the 1000 feet level are all rounded.
Even though the slope of the low hills and the dip of the
strata are mucli the
same in direction,
the slope has no-
thing to do -^vith the
dip. Near Ehyll,
the hills slope from
the N.E. at an angle
of about 9°, but the
dip is about 45°.
Above this upper
level, hill-tops are weathered peaks, and mountain-glens
radiate from them, cutting through the upper plateau from
the watershed to the sea.
In the Snoivdon ranye the rocks are harder, and .strite
abound. The valley of the Conway is a great groove, which
runs nearly X. and S., and which certainly contaiued a large
glacier, or heavy fjord ice. The road to Llanberis follows
its course to the foot of Snowdon. The bottom of the groove
is filled with beds of gTavel, sand, clay, and peat, in which
large trees are buried. It is a flat plain, through which
the salmon-stream winds to the estuary, where it meets the
tide ; tree.s, green fields, and neat houses abound ; a railway
train screams and rattles over the plain, and up the glen ; but
there was a big glacier there nevertheless. The railway
cutting has uncovered a rock about twenty-five feet above
the sea-level, and near a ferry above Conway ; and glacial
stride are as freshly mai-ked upon the slate as if they had just
been made.
Above ground, the rocks are weathered and broken down.
Many forests have spi'ung up and died since the ice was
198 BAI.TIC CUKHENT — BIUTISH ISLKS.
there : but under the beds of drift the original surface of
gLicial denudation is nnmistakeably clear. If there was a
glacier at Conway, there may have been others in other AVelsli
glens.
Leaving the valley at Llanriust, a path leads up the
Snowdon side of the valley, past G^^■ydr House, to Coed Mawr
Twll mine. There are numerous ice-marks, boulders, and
suchlike, all the way.
To the left of the path rises a hill called Coed Mmrr,
from which a wide view is obtained. It is the Ehigi to this
range, a kind of outlier, a Hat-topped ridge separated from the
main ridge l)y a hollo\\', and cut off from the rest of "Wales
by deep valleys. At the height of about 1100 feet above the
sea, and on the top of this outlier, the ground is strewed with
loose boulders.
The rocks are well marked with stri;e, and their direction
corresponds to no existing feature of the country. They
neither point down-hill, nor from the ridge, nor along the run
<.)f any valley or ri^•er near them ; they point north-east over
Khyll, and south-west over Traeth Bach in Cardigan Bay ; ])ar-
allel to the JNIenai Strait, to the ridge of Snowdon, and to the
run of the great sound which would cut through Carnarvon-
shire between Moel Siabod (2865 feet high) and Moel Wynn
(2529), and so join Cardigan Bay at the two strands " Traeth
iNIawr" and " Traeth Bach," near Portmadoc, if the sea were
at this level of 1100 feet. A glance at the Ordnance map
shows that the ground in this direction has the form of an
estuary of glaciers passing south-west into Cardigan Bay.
This mark joins in with the curve \\ hieh has been fol-
lowed from Yorkshire, for no land-ice could well move N.K
or S.A\'. ;it Coed IMawr now, uidcss the neve was about the
Pole.
YORKSHIRE AND WALES, ETC. 11)9
Two Imndred feet lower down, in the valley between
Coed Mawr (1100) and Carned Llewellyn (3482), between
the main range and the isolated hill, at a height of about 900
feet, a small lake, Llijn Pencarrcg, has been drained close to
a lead-mine. It was in a rock-basin, for they had to cut
through rock to drain it into the branch of the Con\\'ay
which comes from Snowdon. The bottom is filled with peat,
and where the peat has been removed glacial striations are
fresh and perfect. These point E.N.E. and W.S.W., out into
the valley, through the hollow where the drain was cut. If
ice were now sliding from Carned Llewellyn it might be
caught in the trench and split on the watershed. Part of it
might slide northwards into the Conway valley^ along the
line of the path to Llanrwst, and the rest would swirl
round and move W.S.W. towards Capel Cureg, where it would
meet the Snowdon stream, turn back to Bettws-y-Coed, and
so flow on to Llanrwst by a circuitous path along the river-
course.
If a Carned Llewellyn glacier were so large as to over-
flow the top of Coed Mawr, it would evidently flow S.E. into
the Conway valley ; but the marks upon Coed Mawr are at
right angles to this direction — they point S.W. Moreover
there appear to be a series of shelves higher up which corre-
spond to the stria?, not to the present watershed.
If the Conway glacier, which must have had a source about
Moel Wynn, were large enough to overflow the whole country,
it might possibly move north-east, over Coed Mawr, but it
would have to cross a glen 500 feet deep, at right angles at
Bettws-y-Coed, and then move along a hill-side at a higher
level than tlie opposite side of the Conway valley, about
Llanrwst, which seems impossible. Making every allowance
for land-ice of enormous tliickness, it is still very difficult
-'"11 H.VLTIC CURHKNT — BlilTlSH ISLES.
to explciiu the strite at Coed Mawr witliout the agency of
floating ice.
But if ice floated above 1100 feet, then the Snowdon
range M'as an arcliipelago wlien this mark was made, and
Moel Wynn was an island. But as sea-shells are found 500
feet higher up, and stratified drift 400 feet above the shells,
icebergs may have floated along the Snowdon islands so as to
mark sunken rocks 900 feet below the sea-level. Of 3570
feet of Snowdon there would still remain 1570 above water to
form a base for the land-glaciers which Eamsay describes.
When the land rose the Conway glacier might flow down to
the present sea-level ; ice certainly did move in this trench.
llclf!ts y-Coai.
SO MmI SiaUt.
St rite a/ Cod Ma
On this supposition the strise on Coed Mawr are older
than those which are seen from the train, about 1075 feet
lower down, and those which remain in the lake 200 feet
below the ridge at Coed Mawr. They look far older, and in
this respect resemble otlicis of their class. Looking south-
westward along the line indicated by the stri.T, there is a caveat
YOKKSMIKH AND WALES, ETC. 201
liollow between Moel Siabod and Moel AVyun, beyond which
is Cardigan Bay and its great strand Traeth ^lawr.
When a great smooth Atlantic roller, moving steadily on,
encounters an isolated rock, some twenty or thirty feet higher
than high-water mark, the glassy surface of the wave breaks,
and a torrent of boiling foam, green water, and glittering white
spray, rushes over the stone with a hoarse roar. If water
then left marks they would be parallel to each other, and to
the direction of movement. If a stone or any other loose
object stands upon the rock, it is driven on by the torrent, and
follows the wave till it sinks. But when the crest of the wave
has passed, the rock seems to rise up like a whale, or some
other black monster of the deep. Then for a time the direc-
tion of movement changes — green torrents, streaked with
snowy foam, stream down the black sides of the rock, and
brown sea-weeds flutter and wave in rivulets which radiate
outwards and downwards from the highest point of the rock
in every direction. If these left marks they would radiate as
the streams do. The rivulets Mould make furrows, and flow
in them while there was any water left to flow. But they
leave no such marks. The Dubh lartach, the outermost rock
off the west of Scotland, has a rough jagged surface, though
it rises twenty feet above the sea where waves are as large
as any in the whole world.
"When river-ice drifting down-stream meets a stone, the
ice-surface, like the smooth wave, breaks. It pushes on, up
and over the stone in the direction of the stream which moves
it, but it slides off in many ways. If heavy enough it would
mark the stone.
If ice is moved by a falling tide, a time comes when it no
longer slides over the stone, but splits upon it, and slips past
it, and meets behind it with the stream.
202 BALTIC CUKHEN'T — BRITISH ISLES.
And then if a shower fulls the water streams down the
sides of the stone in every direction, M-hile the stream flows
past as before. If sno^v falls it caps the stone, and when the
tide has ebbed the bed of the stream retains marks of the
current, while the snow is left to tell its own story.
If the blocks of stone which Welshmen call Plynlimmon,
Y Wyddfa, and Cader Idris, were rising stones in the falling
tide of an ice-laden ocean-current, like that w'hich now over-
runs sunken islands off Labrador, they would retain the marks,
for heavy ice does record its movements upon stone, and stone
preserves the record.
The high Welsh hills do retain ice-marks, and they
seem to record that the hills rose up in an icy sea which
moved ice towards the south-west for untold ages, and that
glaciers streamed from their sides when the cold tide fell,
and continued to flow on, until a long age of winter gradually
passed away, after the bed of the cold stream was crossed by
Lapland.
The hills about the head of Cardigan Bay seem to record
that the stream poured out that way, and that the coast-line is
a result, not of waves acting at the present sea-level from the
south-west, but of ocean-streams pouring towards the south-
west, from the arctic basin into the Atlantic.
The deep trench in the fifteen-fathom line tells the same
story. It seems to carry the south-westerly curve over Eng-
land and Wales, and to launch it in the Irish Channel.
The hobby seems none the worse for this rapid burst.
The story told by Scandinavian and Scotch hills is confirmed
by hills in Yorkshire, by stones at Stoke and in Cheshire, by
geologists and their books, by popular tradition, by the map
of Ireland, and Vtv higli ice-marks on Snowdonia.
CHAPTER XLI.
BALTIC CURRENT U— BRITISH ISLES 13 — WALES 2.
Arctic sea-shells found in loose drift at a height of 1392
feet, and boulders, perched blocks, and drift at a height of
2300 feet,* prove that a cold sea has been as high on the flanks
of Snowdon, since rock was ground into something like the
preseiit shape of Wales. High horizontal ice-marks on a hill-
shoulder at 1100 feet seem to prove that the cold sea which
rose so high was cumbered with ice and moved from north-
east to south-west, when the way was last open. If land and
temperature rose together gradually, and the cold period
passed away from Wales when rising land reached a certain
point ; then marks on watersheds at various elevations ought
to record the changes and their order.
Glacial drift, arctic shells, and horizontal ice-grooves,
record the high sea-level and cold weather. Glacial drift
pai-tially waterAvorn, and packed in forms characteristic of
sea-margins, at lower levels amongst the hills, seems to mark
an ebbing sea and warmer weather, a state of things more like
the present state of the beach at Galway (j). 21). Water-
worn drifts at a lower level, terraces, and sea-shells, speak
for themselves. It seems reasonable to assume that during
a gradual change of climate, dwindling glaciers flowed in
* On tlic SiiperfrirrI Arcuiivilnfions nvd Surfncr Markings of Nmih Wnlea.
V.y Professor A. C Rnnisay, F.R.S., F.fi.S. March 26, 1851.
20-t BALTIC CUKKENT — BlilTISH ISLES.
rising glens, long after the greatest cold Lad risen oti' the
sea,
A series of terminal moraines, entirely made of native
rocks, and laid in hollows, mark the retreat of dwindling
glaciers, shrinking iipwards ; while the cold shell of air-tem-
perature and land rose together ; and in Scotland the lowest
perfect moraine seen is at about 1400 feet, the level of the
Welsh shells.
Old strife at Sniefell ]Doint up to, and converge upon, the
high point from wliicli smaller glaciers now diverge (vol. i. p.
432) ; and the same series of events appear to have followed
each other in like order in Wales and in Iceland.
jNIarks made in the bottom of deep glens near the present
sea-level may be marks of comparatively modern glaciers,
which continued to flow into the sea long after hill-shoulders,
with old scars, had risen far beyond the reach of the battle
between sea-water, sea-ice, and Welsh stone, or they may be
marks of fjord ice like that which now works with the tide
in Hamilton Inlet in Labrador.
The old local glacier-system of the Snowdon range has
been well described by abler pens.
Buckland, Darwin, Lyell, Murchison, Kamsay, and a host of
famous men, have piled up a mountain of facts which would be
harder to get over than Y Wyddfa. The former existence of
Welsh glaciers is proved beyond dispute ; and to a practised eye
the record seems patent.
At Capel Cureg ice-ground rocks abound. At the head
of the pass, where the water sheds towards Cardigan Bay, at
a place lower than Coed Mawr, ice-marks rise high, between
Moel Siabod and Snowdon. If ice floated at 1100 feet, this
was a sea-strait, and these may be marks of heavy drift-ice
moving in a groove like the Menai Strait. Two ice-streams
here split. One reached Conway by the road and railway ;
the other went to Beddgelert and Portniadoc. Whether both
reached the present sea-level remains to be proved. It is
certain that the ice was of large size, and it reached Conway.
At the col at the head of the Pass of Llanberis, about
1300 feet above the sea, a cross strait divided the Snowdon
range when shells and drift were deposited upon tlie hill-
sides at 1392 and 2300 feet.* According to the ice-marks,
two glaciers met in this trench, and parted, as glaciers part
now at the Col de Geant. One ice-stream probably split
lower down, and went to Conway and Portmadoc ; the other
stream went towards the Menai Strait, for the marks are
plain in this direction for many miles. Above this col,
Eamsay has tracked old moraines, almost to the peak of
Snowdon. One system thus tracked from Conway to the
highest peak of Wales, the map of the country gives the
shape of the local system. It must have been a herring-
bone pattern of ice, for the glens all radiate like ribs from tlie
backbone of North Wales.
It has been shown above (vol. i. p. 157) that rocks upon the
snowshed of the Alps, on the Strahlek, at 11,000 feet, and in
the midst of land-glaciers, are not ground, but riven and
shattered. It is also sho^\ii (vol. i. p. 167) that rocks on the
snowshed of Mont P)lanc, on the Col de Geant, at 11,146 feet,
and at the source of the largest of European glaciers, are
equally shattered ; although the snow-dome of Mont Blanc,
15,744 feet high, rises 4598 feet immediately over this pass.
From the top of Mont Blanc the Glacier de Boissons
flows continuously down 12,300 feet to a level only 3444 feet
above the sea. This glacier descends 3902 feet below the
* According to Professor Ramsay's paper above quoted, the drift overhangs
tliis pass.
206 BALTIC CrHHEXT— BRITISH ISLKS.
level of the Grimsel Col, which is 7346 above the sea.
According to De Charpentier and Elie de Beaumont, one, and
the highest known, superior limit of the erratic formation is
at the Grimsel Col. There, at the Furca, and on similar
passes in the Alps, at about this level, rocks are rounded.
The top of the Stelvio (9272 feet) is not .shattered but ground
(vol. i. p. 144). The inferior limits of the erratic formation of
the Alps are far beyond the Rhine on one side, and near Turin
and ]\Iilan on the other ; and the question is whether these
stones were carried from the watersheds of the Alps all that
distance upon land-ice, or part of the way on land-ice, and the
rest of it on ice-floats (vol. i. p. 1G9). If the Snowdon ice-marks
were made by land-glaciers, which grew in consequence of a
great elevation of land (which is one theory suggested to
account for them), they ought all to point up-stream, to and
towards some snowshed ; and the snowshed ought to be
shattered when it is narrow, because the Strahlek and Col de
Geant are shattered. According to this theory the snowshed
at Llaiiberis, which is very narrow, ought to be shattered.
The top of the col is in fact rounded.
Tlie highest grooves close to the head of tlie glen are as
deep as grooves made in places where the heaviest glaciers
press hardest, and they seem to be nearly horizontal. If the
ice-work in this district is sea-work — a result of a cold period
caused, not by great elevation, l)ut by a small depression of
land — the marks agree with tlie present state of things on the
opposite coast.
If the col at Llanl)eris was first a deep strait, then
a shallow sound, and then a " tarbert" at the end of a sea-
loch open to the ocean on the west, heavy drift 1000 feet
deep might grind tlie d^ep strait ; lighter drift, 2.'")0 feet, as at
Belleisle, might pass througli the shallow sound ; and heavy
WALES. 207
fjord-ice move liorizontally in tlie sea-loch, as fjord-ice now
does in Hamilton Inlet (chap, xxvi.)
It is certain that this col was a 3ea-strait 1000 feet deep
when drift was packed in ten^aces 1000 feet above the pass, and
that it was a sound at least 92 feet deep, when sea-shells were
buried in drift, where Mr. Trimmer found them at 1392 feet.
It may have been a " tarbert" 300 feet high, when shells
were buried where Professor Ramsay found them at 1000 feet
on Snowdonia.
So far no one has yet found shells in drift on the high
Alps ; no one seems to have sought them ; but judging from
form alone, it seems probable that arctic shells may yet Ije
foimd in superficial deposits at higher levels than the Stelvio
(9000 feet), but not above the level at which cols and peaks
are all shattered — namely, about 11,000 feet.
It seems possible that roimded Alpine passes Avere sea-
straits when they were rounded, and that land-glaciers may
have" been launched from Alpine peaks which were 6672
feet above water when the Stelvio was a " tarbert," and the
Ortles Spitz a tall " stack" in a European ocean whose arctic
current passed Snowdonia.
According to the Baltic Current theory, such a current did
pass this way, and did all the work ; according to other theories,
the whole of the northern hemisphere must have been covered
with one vast sheet of ice during the glacial period.
Wlien the gorge of Llauberis is passed westwards, a wide
plateau begins, where the chief product of the country seems
to be glaciated boulders, but rolled and waterworn. Walls
are made of them, roads are broken boulders, streams run
amongst boulders, and the soil is clay. At this level, about
300 feet above the present sea, most of Anglesea would be
under the sea which helped to roll these stones.
208 n.vLTic cruKKXT — britisii isi. k.s.
The bouldcr-lanJ ends in a series of ste]js and a steep
terrace, wliicli makes one sid(^ of the big groove, over which
the tubular bridge has been thrown. These steps and terraces,
and the groove which holds the Menai Strait, cross the course
of the old Llanberis glacier at right angles. If the Snowdon
glaciers reached the sea at the level of 300 or 400 or 500 feet,
the present tides might move icebergs and hmd-ice N.E. and
S.W. along the coast.
Anglcsea. — The geological structure of Anglesea includes
igneous rocks and sedimentary beds, from the lower silurian
to the coal-measures. In the mines, these beds are seen to be
fractured, twisted, dislocated, and roasted ; the surface con-
sists of rocks of every degree of hardness, of beds dipping
everyway and at all angles, of minerals which fracture, wear,
and weather into all manner of shapes ; but the Avhole sur-
face of the country has one prevailing form. The hills and the
rocks, wherever they appear through drift and peat, have the
same form as the hills and rocks of low ice-ground Scandina-
vian islands ; and they too are ice-ground.
Boulders and clay are everywhere. Travelling at ex-
press S])eed in the railway train, driving or walking, the
marks of ice are manifest. " Tyr Von" is like a slab of
variegated marble roughly ground flat, well scratched, and ill
washed.
The direction of movement was N.E. and S.AV., that of the
tide in the strait, which now looks like a big river shrunk in
its bed ; the grinding-machines were y)robably icebergs and
sea-ice worked by tides and the Arctic Current, with boulders
for polishing-powder (see chap, xxvi.)
All tlie rocks seem to have their longest slopes and
smoothest sides towards the N.1^1, so the machines worked
most from tliat directi(jn, and tlie sea-level was probably
WxVLES. 209
more than 300 feet higlier thau now, about the level of the
boulder plain, when the ice vanished.*
Looking south-east, the side of the Snowdon range whose
end is seen from Llandudno, appears as a long ridge most
worn at the north-eastern end, and furrowed by deep glens
which cross the ridge at right angles. Generally this north-
western corner with its bent trees must leave the impression
of something now swept by a powerful S.W. wind, and formerly
ground by some force which acted from the N.E.
It repeats the story of the north-eastern corner of Wales,
but in a more legible form. It surely was like the corner of
Iceland (chap, xxv.), or Jan Mayen (chap, xxiv.), or Bear
Island (chap, xxiii.), or islands about Hamilton Inlet over the
way (chap, xxvi.)
From Carnarvon the road to Beddgelert first passes
through a boulder country and over terraces, then up the
course of an old glacier, which left notable marks. At
Beddgelert the course of the Portmadoc and Snowdon
glacier is crossed, and thence all the way to Tan-y-Bwlch,
the road crosses a series of large furrows running north-east
and south-west.
In some places the surfaces are beautifully preserved low
down. Many ice-streams seem to have converged here.
Traeth Mawr is seen to the westward, and Moel Wynn is to
the eastward, and there seem to have been large glaciers on
both sides of Moel Wynn which met here. The marshy
plain is probably a heap of drift and glacial debris, a whole
collection of ruined moraines arranged by the sea, like the
plain on which Llandudno stands.
* A ccording to Professor Ramsay, striae in Anglesea were made by floating
ice ; they generally point E. 30° N., and are quite nnconnected with those of
glaciers in Caernarvonshire. —Prt/icr read Marcli 26, 1851.
VOL. II. P
210 I'.ALTIC (TKHENT — HltlTlSH ISI,KS.
From To/t-ij-Bidch the road rises into a valley, which is
strewed with large stones at the height of 700 or 800 feet.
The walls nrQ of Imulders, many of which are grooved, and
tlie rocks and low hills are all rounded to the very top.
Above a certain level, the hills are steep and broken, and
furrowed with larger corries. At the level of the Coed
Mawr striie (1100 feet), this glen would be a strait. On the
map this inland country seems to have been swept south-
wards, as if a N.E. current had split on Diphwys, a range
2050 feet high. The glen may afterwards have been filled by
a Mer de Glace v\'hich was fed from both sides, and overflowed
two ways to Tau-y-Bwlch and to Dolgelley.
The deep glens which meet at Dolgelley all have the form
of glacier-glens, and above Dolgelley at the pass of Bidcli-
llyn-Dach, about 1000 feet above the sea, ice set off south-
wards, and left a large moraine of crumbled slate, to mark
the spot where it finally expired, below Cader Idris. This
is not a perfect moraine, but is washed or weathered out of
shape. Tradition narrates that a giant called Idris sat on the
Cader, his seat, and strode fi'om side to side of this gap. He
was one of " Hyrm Thyrsar," the frost giants of Norse my-
thology, and he has turned to mist ; for he was ice, and he
has melted away.
Thence all the way to Aberystwitli, the hills and glens
have the same general rounded forms, and wherever a quarry
or a broken stone appears, it shows that the form is different
from any which could be produced by weathering or upheaval.
It is neither the form of bedding, jointing, cleavage, nor frac-
ture. It is the form of glacial denudation.
At tlic />r ??//',s Briflfjc, some fourteen miles from Aberyst-
with, a river lias made a mark in a slate rock, which proves
that water could never wear slate into tlu^ form of Welsh
WALES. 211
gleus. A stream working at the bottuin of a curved hollow
has cut its own breadth straight down for ninety feet, and is
cutting backwards for some hundreds more lower down. The
rock is too hard to weather or break easily, and it has not
fallen, so the river-mark is perfectly preserved. Further down,
the valley retains its glaciated form, and higher up, wherever
a valley is left, the upper level of the country is seen to have
one uniform slope from Plynlimmon to the sea -^ ~" .
There is the general form of denudation upon the largest
scale in the outline of the country, and in tlie glens which
run north-east and south-west ; next the form of denuda-
tion by local glaciers, or glacial currents, which scooped out
broad concave glens ; and lastly, a steep straight ditch cut l>y
running water at the bottom of the old ice-groove.
There is no room for doubt as to the tool which made
this drain ; the marks are seen from the water-le\'el up to the
foot of the bridge, and there is no joint or vein in the rock,
for the rock is smooth and polished, and the slate beds are
unbroken in the bed of the stream. At the bottom of the
trench, which the stream has dug ninety feet through slate,
there is not a chink in the stone.
If the rate of wearing could be got at here, it would be
a chronometer. It is not likely that the river worked thus
under ice ; it certainly did not work below the sea, so it
began to dig after the spot had risen. It is now 750 feet
above the sea. The stream was about its present size when
it began at the ninety feet, for the trench is no wider at the
top than it is below. The question then is, How nnich slate
does this river wash off in a year ? By anchoring stones in
the river, and weighing them from time to time, this question
might be solved, and then the upheaval of Wales might be
calculated from the river-mark.
212 BALTIC criiHKNT — BKITISII ISLES.
.Vt IJoitli is a laryc beacli, Mliicli crosses a rock-hollow,
like a sea-daiu.
IJeliind the dam peat and silt-beds have gathered ; in front
of it a bed of yellow sea-sand is smoothed by Atlantic rollers;
and the mound itself is a blue ridge of slate pebbles and
boulders rolled by the sea. These were probably carried
from their parent rocks by the Plynlinmion and Machynlleth
branch glacier from the Plynlimmon and Cemmis junction,
where it joined the Severn valley ice-line, at the watershed.
From Bitrtk near Aberystwith, a railway has been made
across Wales to Shrcwsluiry, and the cutting has not yet
(1863) been overgrown with turf Travelling on this line is
Like studying a geological section. The hills and valleys are
all of one pattern outside, but they are composed of beds
which dip in many directions, and at many angles, and which
are of various kinds. The rock is often covered with glacial
debris, beds of clay, generally yellow, enclosing angular and
rounded blocks of stone of many kinds. There are grits,
white quartz, igneous rocks, and slates. Near Carno, about
700 feet above the sea, these are well seen.
At the height of 1100 feet, this would be a sea-strait. It
may afterwards have been the bed of glaciers which came
from Plynlimmon, s])lit on the watershed, and worked their
way to Shrewsbury and Cardigan Bay.
AVith the well-marked glacial phenomena of the high
iiionulains of North Wales fresh in the mind, a rapid journey
along this line is like reading the history of a glacier. Bare
rocks get covered ; stones get more rounded as the train de-
scends ; tlie colour of tlie clay changes ; confused heaps of
loose rubl)ish are Itetter sorted where they have been washed
in hollows ; there is more variety in the materials after a
greater number of beds have been passed ; and finally, when
WALES. 213
the low plains are reached, the whole is hidden under allu-
vial soil. The work of ice is covered by the work of water
and air, and a green cloak of vegetation is thrown over all.
Then comes the plain, and the town, and archaeology, and
man's history recorded by his works ; old houses, old glass,
old churches — a museum of antiquities. Old English, Nor-
man, Saxon, Eoman, Celtic, and unknown remains — all records
of a series of events, which began here after the other
ended. And yet the sculptured marks of ice which moved
between Snowdon and Conway, and passed over Coed MaM'r
and Anglesea at 1000 feet, and at the sea-level from N.E. to
S.W., are better preserved tlian Koman sculptures from Uri-
conium ; and there are boulders near the Stiper Stones, which
tell their story at least as well as tlie ruined gable of an old
house.
The geological sections of Wales, which liave just been
finished, confirm what has been said alcove.
On the western side of Cader Idris boulder-clay is marked
at 1100 feet; at 1000 on the western side of Snowdon, and
at 1700 feet at Mauchlyn Mawr.
On the eastern side of the hills drift is not marked, but
drift exists in patches everywhere. If the movement was
south-westwards drift ought to be found to the westward of
the high grounds, under the lee of islands which are now
mountains. Sea-waves would tend to wash the drift from the
south-west end, where it abounds most.
The structure of the country shows trap, felspathic ash,
fossiliferous and non-fossiliferous slates, grits, lime, shales, and
coal-fields. There is evidence of fracture, disturbance, and
bending of strata, upon a very large scale, and of volcanic
eruptions. The mines show that the shattered crust has
grated its broken edges to make smooth grooved sides in the
214
BAXTIC CL'1;1;ENT — BKITISH l!?LKS.
cracks. Bits as broad as a paiish aiul ol' uukiiuwu thickuess
have risen, or fallen, or moved horizontally ; and every bit has
moved, for there are slickensides in every mine. The surface
must often have been rough and jagged like that of a broken
flagstone laid upon a soft bed and trodden awry. Some of
the cracks are filled Avith clay and boulders, so they were
open when ice was here. But some great force has now
ground otf all the corners. The geological section gives the
same lines which can be seen in every Welsh quarry, and in
many quarries the surface of glacial denudation yet remains.
The geological map shows no granite in AVales. Granite
boulders are found in Cheshire to the north-east, and the
nearest English granite hill is further to the north and east
than the Cheshire boulders.
If the assumed curve is followed up-stream it joins Wales,
Cheshire, the Skagerrak, and a Scandinavian district where
granite ab(junds, and where ice-marks are conspicuous at high
levels.
So the l)lock of land M'hich we call Wales seems to have
been ground down by an arctic current and by local glaciers,
which gradually disappeared after the land had risen to a
certain level, and of which the last traces are to be found in
the highest i)art of the highest glens. AVhether any of these
traces coincide with any record of man, is the geological
question of the day.
CHAPTER XL 1 1.
BALTIC CUKREiNT 15 — BRITISH ISLES 14— ENGLAND (sOUTH).
A SET of curves, like the rest, drawn from Novaya Zenilya
proper, pass over Eussian Lapland and the White Sea ; Fin-
land, the Gulf of Bothnia, and the Baltic ; the low rocks of
Sweden ; the drift of Denmark, Hanover, Holland, Belgium,
and part of France. In England, curves pass from AVhitby
to Snowdon; from the Wash to the Bristol Chanmd; from the
Thames to the Isle of Wight ; and from Heligoland past Dover,
down the English Channel, and out to sea.
It has been shown above that there is reason to believe
that ice travelled south-westward over Sweden and Finland
(chaps, xviii. xix. xx.) A succinct account of the superficial
geology of Denmark is given by Sir C. Lyell in the second
chapter of his last great work. Means of temperature and
limits of vegetation have been mapped, and a series is pub-
lished in Keith Johnston's Physical Atlas. From facts taken
from these stores, and from personal knowledge, it appears
that the present mean annual temperature in Denmark is
about 46° and 48°, and the forests chiefly beech. In the
upper beds of peat the trees which are preserved are chiefly
beech ; and in this layer human remains are associated
with weapons of iron and other metals. In the next layer
the trees are oak, and works of human art older and
chiefly bronze. In the next the trees are Scotch fir and
liirch, and human implomonts far ruder, and chieHy sloiio.
21G BALTIC CURKENT — BRITISH ISLES.
Beneatli all these are layers of glacial drift, clay, aud
scratched boulders. These several layers seem to indicate a
gradual change of temperature from cold to warm ; thus —
In Bear Island, Greenland, and the north of Labrador, a
mean temperature of 28° now coincides with the deposition of
glacial drift in the sea, and with the polishing of rocks by
land and sea ice.
About the North Cape, Western Iceland, and the south of
Labrador, a mean temperature of 32° now coincides with the
growth of fir-trees and birches on shore, and with the deposi-
tion of glacial drift in the neighbouring seas.
About Stockholm, Christiania, Cape Eace, and Nova Scotia,
a mean temperature of 41° now corresponds to the growth of
oaks, pines, and other forest trees, and of heavy winter-ice on
shore and afloat.
Lastly, about Coi^enhagen an isothermal curve of 44!'
passes north of Scotland and south of Nova Scotia, where sea-
ice now marks rocks, deposits drift, and moves south-west
about lat. 45° in the Bay of Fundy.
If the climate of Europe were now like that of America
there would be -ice-floats on the northern coast of Spain in
winter; the cold of Copenhagen and Halifax would reach
Bordeaux ; while the cold of Labrador, Cape Farewell, and the
North Cape of Norway, would reach Copenhagen.
The glacial drift of Denmark seems to pros'e tliat the
jn'esent climate of lialn-ador did in fact exist about Jutland
when that spot was mider water, and geologists are agreed
that Jutland was an archipelago at no distant date. The
Danish stone, bronze, and iron periods, with their vegetations,
80 far prove a change of climate during the human period,
after the land rosi'.
Accni'diiin to \]\(> Baltic Current theory, the blocking ^^^
ENGLAND (sOUTH). 217
of a northern strait by a rise of land was the first step
in a gi-adual change which is still in progress, for the last
Norwegian glaciers are now dwindling away.
Eivers of all dimensions have deltas ; ocean-streams, espe-
cially when laden with ice, ought also to build submarine
deltas ; the Banks of Newfoundland, about lat. 50", seem to
represent the "northern glacial drift" of the present day:
if so, Denmark, the Dogger Bank, and the drift districts of
eastern England, may be parts of the submarine delta of the
Baltic Current. The direction. of striae, shells, and the nature
of the drift on shore, are the only guides.
The same high authority who states the order of super-
ficial deposits in Denmark also describes the eastern coast of
England (chap, xii.. Antiquity of Man). The " series of docu-
ments " which lie next below the glacial drift in Norfolk and
Suffolk read thus, according to Sir Charles Lyell's trans-
lation of the rocks : —
" The fossil-sliells of the deposits in question clearly point to a
gradual refrigeration of climate from a temperature somewhat warmer
than that now prevailing in our latitudes, to one of intense cokl."
According to the Baltic Current theory, the opening of a
northern strait, by the sinking of land, let in the cold climate,
which is now transferred to Labrador, by the close of the
strait.
The English documents, as read by Lyell, record many
successive changes in the relative level of sea and land in
Norfolk, Suffolk, and Essex. Forest-land has sunk, for beds
of shells are spread above the upright stumps of fir-trees
identical in species with firs now growing ; the sea-bottom
has risen, for trees now grow above the shells, and men spread
shell-marl in the fields, on the top of the English cliffs.
218 ifAi/nr ( tkuknt — uiUTif^n islks.
Through these old buried English tir-woods, elephants,
rhiuoceroses, and other big brutes roamed ; whales, nar-
whals, and sea-horses swam over the same spot when it
sank ; and then came an ice-chapter, which the best of
modern geologists thus translates : —
" Erratics of Scandinavian origin occur chiefly in the lower portions
of the till. I came to the conclusion in 1834 that they had really
come from Norway and Sweden, after ha^ang in that year traced the
course of a continuous stream of such blocks from those countries to
Denmark, and across tlie Elbe, through Westphalia, to the borders of
Holland. It is not surprismg that they should then reappear on the
eastern coast between the Tweed and the Tliames, regions not half so
remote from parts of Norway as are many Eussian erratics from the
sources whence they came." — Antiquity of Man, p. 218.
Tlie Baltic Current theory is thus propped up by a strong
buttress of facts, stated by a great authority to prove some-
thing else. The northern strait, which is supposed to be the
source of change in English climate, is at the head of the
Baltic. When land A\-as sunk in England and in Denmark, a
cold sea carried boulders from Scandinavia to England, in the
direction of the curves above shown (vol. i. p. 232) ; but when
the land rose higher, the transport of Scandinavian stones was
stopped, and soon after that clause in the ice-chapter was
recorded in the till, the glacial period began gradually to
pass from Europe. It is argued that it went to America.
Sir Charles himself suggests, that the " glacial period "
may be nothing but a transfer of existing climates, by causes
now active, but other causes than a Baltic Current.
One more fact may be taken from this storehouse.
At the end of the glacial period, eastern British drift came,
not from Seaiuliiiavia, but a])parent]y from the noitli of
England.
ENGLAND 'S(JUTH). 219
Sir C. Lyell says —
" Patches of the northern drift, at about 20U feet above the Thames,
occur in the neighbourhood of London, as at Muswell Hill near High-
gate. In this drift, blocks of granite, syenite, greenstone, coal-measure
sandstone with its fossils, and other palaeozoic rocks, and the wreck of
chalk and oolite, occur confusedly mixed together. The same glacial
formation is also found capping some of the Essex hills further to the
east, and extending some way do^^Ti their southern slopes towards the
valley of the Thames." — Aiitiquity of Man, p. 16(».
Many of these fragments are not Scandinavian, and may
be of native growth, and the deposition of this drift is sup-
posed to have taken place at a time when nearly the whole of
the low grounds of England were at least 200 feet under the
sea.
According to theor}'-, Scandinavian diift gave place to
English drift when the stream and the local tides changed
theii- direction, after the way from the polar hasin to Mus-
well Hill was blocked by Lapland, now 1200 feet higher,
which rose and sent the cold westward, to the place where
the glacial period has now perched, to feed on rocks in Green-
land.
Passing S.W. from Norwich, glacial drift is said to be
found near the railway between Gloucester and Bristol, and
that line leads to Devonshire. It is vain for a single hand to
attempt to follow drift through all England, so it is best to get
to the hills once more.
Dartmoor is an upthrow of horse-tooth granite of a peculiar
character, which has upheaved and altered surrounding strati-
lied rocks. The granite and the altered rocks are traversed by
numerous veins and faults, in which mines of iron, lead,
copper, tin, etc., are worked. There are numerous dykes of
greenstone and other igneous rocks, which fill up breaches in
220 BALTIC CUHPxENT— BKITISH ISLES.
the earth's crust ; and there are " cross-courses," which are
great cracks filled up with angular fragmeuts of broken rock
and other materials of small value. The crust has been much
Ijrokeu and shaken at various times, for more "heaves" and
"slides," "faidts," "upthrows," and "downthrows," are known
in Devonshire and Cornwall than are to be seen in the cliffs
of Iceland.
There are other evidences of subterranean heat and fire.
There are so-called " hot lodes," where a thermometer marks
90° or 100°. The deepest mines in the district are the hottest,
and volcanic products, carbonic acid gas, and such-like, some-
times escape from veins into the mines.
There are hot springs at Bath still. There is evidence of
upheaval by the agency of heat-force in the geology of the
country, and in the temperature imder ground. There is evi-
dence of denudation by ice above ground.
The hills are about 2000 feet high.
The upper part of Dartmoor is strewed with large; blocks
of granite, many of mIiIcIi differ in stracture from the granite
of the rocks on wliich tliey rest. They resemble ice-borne
boulders in sliape. The soil is peat and decomposed gxanite,
but on the hill-flanks are beds of sand and water-worn boid-
ders. One bed is to be seen at the roadside high above tlie
Dart, near Ashburton. It seems to be water-worn glacial
drift, and the lieiglit is about 200 feet above the sea.
The hill-tops are capped l»y curious granite elevations called
" tors" (heaps or moimds). These, though much weathered,
often retain the characteristic shapes of ice-ground rocks.
The grinding force seems to have acted from tlie north-
cast towards the south-west.
Blakcston Tor, on the south-eastern side of the moor, is a
good specimen of the class.
ENGLAND (SOUTH),
221
The cut is from a sketch made on the spot.
Heytor Rocks, about 1100 feet above Bovey Tracey, are
good samples also. From the internal structure of these
granite hills as seen in a quariy near Heytor, the tors appear
to be weathered remnants of an upper bed of granite, the rest
of M'hich has been ground and broken and pushed away by
some power, acting chiefly from the north-east. Still lower,
layers of granite have also been worn at the edges, so as to
leave a smooth rounded conical hill, strewed with rounded
blocks, and capped by a rounded tor. The granite breaks
into angidar fragments, and weathers into strange shajDes.
The worn surfaces are very clearly seen for about 200 feet
below the top, and a few remnants of grooves can there be
traced. These last are very faint, and much weathered. With-
out other indications, and long practice, they would be wholly
insufficient e\'idence, but taken with the rest, they too point
to ice moving from N.E. to S.W.
If the N.E. is the weather-side, most of the loose stones
ought to be foxmd pushed o^er into the slielter. In fact,
T2'2 BALTIC CL'KRKNT — BRITISH ISl.KS.
most of the loose boulders which are strewed about Dartniuor
are to the westward of the tors, and to the westward of ridges,
and of the range itself. The forms of the hills generally,
when seen from a height, agree with this theory ; they are all
rounded. Whatever their comjiosition may bo, whether they
are " granite," or " killas," or " elvan," igneous or sedimentary,
upheaved or not ; they are steep towards the south-west, and
slope towards the north-east, like hills mentioned above.
On the hill above Wistman's Wood (see vol. i. p. 31) is a
great boulder as big as a house, which seems to be a "tor"
pushed bodily from its base towards the point from which
the prevailing wind now blows, as shown by the trees.
From Shetland and Orkney to Devonshire, at certain ele-
vations, there is a recurrence of the same rock-forms which
are held to be old ice-marks in Scandinavia, Switzerland, and
elsewhere.
Brentor, near Tavistock (sec map, vol. i. p. 232), is at a
lower level. The shape is like that of hills in the valley of
the Forth, with similar bearings. The rock at the top has the
general shape of ice-ground rocks, but it is so weathered,
M-orn, and grass-grown, that notliimr like a groove ^^'as made
out. The general shape of the hill seems to point to a grind-
ing force acting from the direction of Bristol, at a height
of about 700 feet above the present sea-level. Hence this
spoor runs out to sea, unless some of the boulders and loggan-
stones of Cornwall prove to be erratics and perched blocks.
No Cornish ice-grooves are known to the writer. According
to Sir C. Lyell, the southernmost extent of "erratics" in
England is to the north of Dartmoor.*
If ice-floats of former days resembled ice-tloals oil' ]>abra-
ilor now, there may have been an easterly limit, beyniid
' Aiili(iuity i.r.Maii, p. 2811.
ENGLAND (SOUTH). 223
which ice-floats could not pass. But that limit seems to have
included Kent.
In 1860, a party of fishermen were creeping for what they
might find at the bottom of the sea off Margate. They got
hold of something heavy, and thinking that they had netted
an anchor, or something better, they dragged their prize to
land with mucli labour. It was a big rounded stone of the
pattern of those which form terraces about the Tornea. It
was something so foreign to the sandbanks, gravel, and chalk-
cliffs of southern England, and to the experience of the fisher-
men who found it, that they hoisted the stone to the end of
the pier, and there it was shown as a curiosit}^ '
From Muswell Hill and the Thames' mouth, the S.W.
curve leads to Southampton Water.
In many of the chalk-glens of southern England, rich
alluvial flats are flooded to irrigate meadows. The bright
clear sparkling wealth of water in the rivers is divided and
made to spread and wind hither and thither. The green grass
and the water-threads of silver and crystal weave themselves
into a pattern of graceful curves, and this waving, moving,
brilliant, wet carpet, is spread on a yellow floor of flint gi-avel,
peat, and clay, laid in a white chalk-groove. At Stockbridge,
in one of these glens, shoals of trout and greyling are daily
tempted by the best of British flyfishcrs, armed with the best
of London tackle. From constant practice and long acquaint-
ance, these fish and fishermen have learned so much that great
skill spills little blood ; but as a good fencer is a dangerous
foe, the man who kills two Test trout a day is apt to kill most
elsewhere. A stranger used to wild fish finds highly-educated
trout too cunning for his rough hand ; but if fish will not
take, it is well to take to something else.
The old spoor which was found at the North Cape is here.
224 BALTIC CUKRENT — BRITISH ISLES.
This valley, which ends in Southamptou Water, is terraced,
and tlic terraces are as plain as they are in Scandinavia.
From Stockhridgc four shelves are very clearly seen on the
western side of the hollow. The alluvial flat in which the
Test winds is abont a mile wide, and it rests in a chalk-
groove. The solid chalk crops out where the plain ends.
Close above the plain is the first horizontal shelf, and it is
well marked at several places, and on both sides of the glen.
The second shelf is about 100 feet higher ; and the whole
series may be thus roughly expressed. The oidy tool used
was a pocket aneroid : —
Feet.
200 ... . liill-top.
180 .... fifth.
160 . . . . fourth.
150 . . . . third.
100 . . . . second.
10 . . . . first terrace,
o . . . . alluvial plain.
The whole country is cultivated, and there are few hedge-
rows. The colour is uniform — green in spring, yellow in autunni,
brown when the fields are bare. When light is favourable,
and attention directed to the terraced shape of these rounded
chalk-downs, the whole landscape seems pervaded by hori-
zontal lines. Though all the chief outlines are swelling curves
^ ^ s. .- , a great many of the hills have slight notches
) 7 " ^
liewn out at correspouding elevations on both sides ; and
from these, horizontal lines of light and blue shadow mark
the terrace of erosion, which surely marks an ancient water-
level. All theories of lakes are vain here.
The chalk is covered with a very thin layer of soil and
EXGLAND (south). 225
rolled flints. Many of these on the watershed are water-worn
pebbles, like those whicli are found on sea-beaches ; others
are only partially rolled ; others are like flints newly broken
out of the chalk. These stones look like water-work, and
here it must be sea-work. A well-preserved set of terraces
Fir,. S7. Terraces at SiocKBUiLKii;.
Casting a small fly over heavy fish.
occurs near the hill-top to the west of Stockbridge, opposite
to the peat-pits. A hedgerow shows the waving outline of
the hill very distinctly. These terraces are about fifty feet
apart, and might easily pass for works of human skill, " pa-
rallel roads" or fortifications. They seem to be very well pre-
served marine terraces of erosion, and there are ten or a dozen
of various sizes. Lower down the valley they recur. On the
road-side, near a place called Hazlcdown Hill, close to the
watershed of the valley of the Test, three small horizontal
ridges of broken and rolled flints, skinned over with fine turf,
again recur at elevations at which the aneroid liarometer
VOL. II. Q
22G BALTIC CUHRKNT — BKITISII ISLES.
marks the same level — iiainely, heights somewhere between
200 and 150 feet above the level of StockbriJge.
From Hazeldowii Hill the way is clear to the glacial (hiit
on Muswell Hill ; and these terraces carry the sea-level over
London along the line of this last cnrve. It passes from the
mouth of the Thames to Southampton Water ; from the last
patch of British glacial drift yet described by good authority,
down to the English Channel with its broken chalk-cliffs.*
To men who " live at home at ease " all this may seem to
be impossible, or mere vague speculation. A man who has
never seen ice upon the sea, and who thinks that rocks were
created in their present form, is apt to suspect a latent joke
in " sea-margins " in corn-fields. A Londoner who had not
tried to construe a stone, would stare agape at the notion of
ice floating over St. Paul's, or the nearest steeple, where the
weathercock has whirled ever since he M'as born. To such
men all modern geological change seems impossible, and
English ice a myth. But those who ■will accept a rough
translation of a stone record may rest assured that floes and
bergs passed over the site of London, when INIuswell Hill M'as
capped with glacial drift.
The northern "glacial period" is still within easy reach.
The Times of August 4, 18fi3, gives the official report of
the loss of the Anr/lo-Saxon. It narrates that on the 25th of
April 1863, the vessel fell in with ice and foggy weather south
of Newfoundland. The engines were slowed, and as the ice
* It is light to state that a sixteen mile walk to Muswell Hill, without a
guide, and a long search about the foundations of the new building, and else-
where, failed to discover the patch of drift in question. It is there, but it
was found by chance, and it is now buried. If any one sliould fail to discover
marks described in these pages, he may think of the old saw wliich says that
" bail seekers are bad finders."
ENGLAND (SOUTH). 227
became thicker and the fog denser, the engines were stopped.
The vessel drifted till ten on the 26th, wlien the ice being
somewhat less comjjact, she was moved slowly ahead till
two, when clear water was reached. Steam was then set on,
and the vessel went ahead full speed towards Cape Eace :
she was about lat. 46° 54' K, and soon after she ran aground,
and was wrecked in a cold fog at Clam Cove in Newfound-
land.
If she had been on the European coast, she would have
been in the Bay of Biscay off La Eochelle, south of Brittany
and the drowned land of King Grallon. The ice would have
been north of the PjTenees (whose name means " icc-'pcaks"
if it be Celtic) where signs of glaciers abound, she would have
been near the latitude of tlie place where works of human art
were found associated with remains of reindeer.
If she were sailing over Europe, she might have been
over the lake of Geneva, off the high coast of Switzerland, or
in the Sea of Azov, under the lofty Caucasian coast, and north
of the moraines of the Lebanon.
In the Times of June 17, 1864, another wreck in the same
latitude is thus recorded : —
Ice in the Atlantic. — By the arrival of the Allan steamer Peru-
vian we hear of the lo.ss of two ve.ssels belonging to this port — the
Philanthropist and Highlander. The former was on a voyage from
Liverpool to Quebec, and was lost in the ice on the banks of New-
foundland on the 11th of May. The crew were picked off the wreck
by the bark Wolfville, and taken to Quebec. She was a shij) of 805
tons, and was built in St. John, New Brunswick, in 1852. Her pre-
sent owners we have been unable to ascertain, as she very recently
changed hands. The second vessel, the Highlander, was boimd from
Quebec to Fleetwood, and was, says the telegram, " lost near St
George's Bay," but it is supposed through contact with ice. She was a
perfectly new ship, having only been built this season at Quebec, and
was, when lost, on her first voyage, coming over to England, we believe,
228 UALTIC CUREENT — BIMTISH ISLES,
for sale. Both vessels had valuable cargoes, and were fully covered
by insurances, partially if not wholly elfecled in Londi)n. — Liverpool
Courier.
If the Arctic Ciu-reiit came through the English Channel,
the same climate would descend upon the Englisli coast.
Drift, shells, ice-marks, and rounded terraces, record that
a frozen sea, 2000 feet deep, did in fact pass over the sites of
London, Edinburgh, and Dublin ; over Snowdon ; over Scot-
land, Ireland, and Scandinavia ; and some of the highest
marks left are fresher than the scidptured pillars of the
temple of Serapis, which sank in the Bay of Naples, stayed
under water for a time, and rose again.
The force which lifts and lowers land is still active in
Greenland, Iceland, Scandinavia, Labrador, England, Italy,
Sicily.
The same paper which recorded the evil deeds of Jack
Frost in summer 1803, also recorded abortive efforts to
escape made by tlie imprisoned cyclops Fire.
Accounts from Messina of Friday last state that the volcano of
Mount Etna is vomiting fire and lava. A new eruption is threatened
in the direction of Bronte. The inhabitants of Catania are terrified at
the formidable noise and the shower of ashes and stones liilling in that
direction. The population of the moiurtain have made preparations to
quit their dwellings. Their horses are saddled, their cattle gathered
together, and all their household furniture packed up to be ready for
immediate removal. Prayers are being offered in the churches, and
the relics of saints are to be exposed to the piety of the faithful.
Terror prevails among the entire populatinn.
The memory of an English earth({uake is still fresh.
There was a small volcanic eruption in Iceland in 1862.
We live in a period of active geological change, though few
men think al)out Frost and Fire.
ENGLAND (SOUTH). 229
The water-meadows at Stockbridge, like the hills, furnish
occupation for unskilled anglers. Every dry watercourse gives
samples of " denudation" and " deposition" by streams. Eveiy
tame stream gives a lesson which may be used to master the
ways of wild streams, which are too dee]3 to be easily seen
through. In the middle of a weir, about ten yards wide,
behind which was a " head" of water three feet deep, a sluice
was lifted so as to make a strong rush through a still pool
in a lower watercourse.
A certain latent mechanical " water-power," expressed by
the broad arrow at E., was stored up behind the dam. The
same force of gravitation makes rain fall, stops a wagging
pendulum, and works a drop and the surface of the ocean-
pool into spherical forms. By raising a sluice at E., a certain
amount of this power was freed, and set to work on water
at rest in the river-pool.
From one direct force, which tends to produce direct
movement downwards towards the earth's centre in all
latitudes and longitudes, and from the movement expressed
above by the form X) ^ series of very complicated vertical
and horizontal movements resulted in the stagnant pool
below the weir in the Test.
At the head of the pool, at the spot where the falling
water escaped from under the sluice at E., whirling jets
spouted up. In the strongest downward rush, westward
towards W. waves rose highest, curled round, and broke
eastwards, up-stream towards E. A complicated set of
curves, jostling streams and waves, crossed and recrossed
the line of direct movement from E. to W. Surface-waves
rippled and broke on the shore in every direction. At
the tail of the pool was a shallow, and the whole of the
bottom was overgrown with fine water-plants. Each of these
•230
BALTIC CURRENT — BRITISH ISLES.
was a tell-tale to poiut out the course of tlie stream below,
and floats on the surface showed nioveiuents there.
These seemed a movement from every direction.
Because there was a rusli from east to west in tlic middle
of the pool, two edtlit'S whirled opi)osite ways about the points
N. S. in the diagram. The weeds mapped (Hit the currents.
A stick thrown into the rush at E. turneil back wlierc tlie
weeds turned and wliirled round the point N. Two stacks of
dry reeds (expressed by circles and white spots), thrown one
on each side of the rush, revolved in opposite directions about
tht'ir centres of revolution N. S. They described ellipses,
and turned on their axes in the directions shown by arrows ;
and so the floats waltzed over the sunken forest of weeds,
wliich showed like movements at the bottom of the tran-
sparcMit stream. Not one reed had passed over the shalloNv-
wlicii llic cNwiiiii^ flics rose nut of tlio wattM', and trout scciikmI
ENGLAND (sOUTH.) 231
disposed to dine. Tlie experiment was sim})le, any child can
see the result, but all the niatlieniaticians that ever lived
might have found occupation for their lives, in striving to
comprehend the curves that resulted from the action of the
direct force of gravitation which stretches a plumb-line.
No special talents or mental tools were used by philoso-
phers, to discover this natural force of " gravitation ; " it is
something patent and manifest to all, though no human mmd
can account for it, or explain it, or calculate the effects of it.
From the stagnant pool the river Test leads back to the
watershed, and to the rain-cloud which rose out of the sea.
No special talents or mental tools need be used to discover
the second force which tugs at the cable of a fire l)alloon,
beside the force which tightens the cords of the car. The
effects of this force are hard to calculate, the mode of action
is wholly unexplained, but the force is manifest as daylight
itself
The Atlantic is a big pool to cover single-handed ;
arctic currents are heavy streams ; those who venture in are
apt to get out of their depth. From Lapland to Southampton
is a long cast ; but, nevertheless, the small fly has fallen
very near the southern haunts of heavy fish. The last cast
over London and the watershed of the Test may chance to
rouse a shoal of geographers, geologists, and siirveyors, better
worth raising and harder to catch than Test trout ; and this
is the point of the first hook dressed to tempt such readers.
As two sets of floats and two small water-systems revolve
and circulate in eddies, in a small pool, and in the largest
pools that can Ije seen ; so, according to meteorologists and
bent trees ; authority, maps, and observation ; the atmosphere
and local storms, — the largest and deepest streams in our
world whirl and move ; turning opposite ways, on opposite
1'32 BALTIC CUKIJENT— BKITISII ISLES.
sides of the Equator iu the Noitheiu and Southern Hemi-
spheres. The reason seems to he, that two mechanical forces,
which are at rest when evenly balanced, move air opposite
ways when one or the other is in excess.
So also, according to theory founded upon facts, of which
some are stated above, the ocean circulates within narrower
bounds for tlie same reasons. Because it circulates, and tends
to move north and south upon a surface turning eastwards,
main currents move diagonally ; and the coldest and heaviest
tend westwards. For the same reason floats revolve and
circulate about the Poles, as the stacks of withered reeds did
in tlie pool, as froth does in every eddy, as clouds do in the
air ; and as the coldest are also the hardest and the heaviest
of floats, those which tend westwards make the deepest
marks.
It is admitted that this double engine, made of air, water,
and ice, has done the work of " denudation " and " deposition,"
which geologists study, survey, and describe. It is argued
that the tool-marks of each part of the natural engine ought
to be known, and that large work done by regular and con-
stant movements iu air, and water, and ice, ought to be, and
is in fact, symmetrical.
It is easy to build clay-maps in shallow pools, to watch
currents and eddies, study tli(iir action, and seek to apply
knowledge, so gained irom experiment, to larger things. The
])astime is lazy, healthy, and frivolous, as any idle angler can
desire.
The map (vol. i. jt. 41»G) is intended to show that forms which
are attributed to deniulation coincide with general movements
in air and water, some of which correspond to movements in
a river-pool, and wliich seem to make a pattern of curves upon
the rnugli ni()\ijig surface of the globe ; that all the largest
ENGL,AJ^D (south). 233
indentations aboiit the Equator trend westwards, all the cliiel'
coasts on the eastern side of continents, and many mountain-
chains, cross meridians diagonally as currents do. It is
argued that hills and hollows, ruts and ridges, which are less
in proportion than sand-lines on a boulder, may be tool-marks
of a natural graving-engine, worked by fire and frost.
As a mayfly rises from mud, through water into air, and
dies, so the mechanical forces which drive this part of the
engine seem to rise and fall
The world's heat, which is always found when sought
underground, and the sun's heat which is added from without,
evaporate water and expand air ; the power seems to move
water and air to the limit where force radiating from the
earth's centre is expended, or overcome, by force converging
upon the centre, whence rays of heat and force diverged.
In one word, the natural engine seems thus far to be
driven Ijy two opposing forces which bear various names —
" gravitation " and " levitation,"
attraction and repulsion,
condensation and evaporation,
contraction and expansion,
crystallization and dispersion,
weight and heat,
water-power and steam-power,
weights and springs,
freezing and boiling.
Frost and Fire.
The engine seems to be driven by converging and by
radiating mechanical forces, and by the will of Him who
made them, and who said " Let there be light, and there was
light," in the dawn of time.
234
UALTIC CURRENT — BRITISH ISLES.
And so tlie pursuit of nieclmnical I'oiee leads round to
the place from which this long journey began, and a further
searcli r(M|uires a fresh departure.
Fic. SO. "The Scu.ly Bisiioi's." Lat. 41i° 01' N.
The last of the British Isles. From a sketch iiiaile Sth July 1S")9.
The rock above water is higher and longer than the Eddystoiie. The building is pro-
bably the most exposed in the world. Spray goes over the top, which is more than 150
feet above the sea-level. The rock, so far as the sliape of it could be seen or felt, resembles
a Devonshire tor; e.g., Blakeston Tor, p. L"J1. For a contrast in climate in a similar
latitude, see below, and p. 248
CHAPTER XL IT I.
BELLEISLE CURRENT — AMERICA.
In tlie summer of 1864 a holiday \x\\> to North America
was so arranged as to test glacial theories above stated. The
Arctic Current and Gulf Stream were twice crossed, and their
climates felt at sea. Icebergs were seen in July about lat.
49° in the Atlantic. Cape Harrison in Labrador, the Straits
of Belleisle ; the coasts of Newfoundland, Cape Breton, Nova
Scotia, New Brunswick, and of the States, as far south as
Washington, were visited. The curve (see map, vol. i. p. 496)
which passes through the Straits of Belleisle was followed
through Canada and the Western States to St. Louis on the
Mississippi. Various cross-routes and high points on the
Alleghanies were selected, traversed, visited, and examined for
ice-marks ; the Mammoth Cave in Kentucky was visited for
its own sake ; and the following are some of the results : —
Cape Chudleigh, the most northern point in Labrador, is
in lat. 60° 54' N. ; Cape HarrLson is in 55° ; Belleisle in 52°.
The Shetlands correspond to Cape Chudleigh ; Londonderry,
Stranraer, and Newcastle, to places near Cape Harrison ;
Killarney, Cork, Gloucester, and Colchester, to places near
Belleisle. There is no good chart of the Labrador coast. The
interior is unexplored. There are no high mountains and no
glac;iers in the country, so far as it is known to trappers,
Indians, Hshcrmcn, and settlers along the coast. The coast-
236 BELLEISLE CURRENT.
liue is lo\\', rocky, antl glaciated. All the liills, rocks, aud
islands, are rounded. There are few cliffs, and very few
beaches; but vast numbers of rocks, reefs, and islands, and
many long fjords. Hamilton Inlet, for example, is 150 miles
long. The climate is very severe. In July and August 1864
many of the harbours M'ere frozen, and patclies of snow lay
close to the water's edge at places which correspond to
watering-places in North Wales. Heavy pack-ice reached
to the horizon opposite to Hamilton Inlet on the 1st of
August 1864. Between Belleisle and Cape Harrison, islands
of ice were constantly in sight. The largest of these were in
the offing, and resembled isolated rocks, like the Bass or
Ailsa. Some were aground and stationary for a fortnight,
others had moved away when the vessel returned.
It was very difficult to estimate their dimensions, but
many certainly rose 200 feet above the water, and one near
the shore rose 300. Smaller bergs were aground amongst
the islands and in the fjords, and many of these were from 50
to 100 feet high. Smaller fragments, called "growlers," about
the size of ships and boats, were driftmg everywhere, and
bits as big as hogsheads and barrels were rolling in the land-
wash. The temperature of the water was generally about
37° and 40". The air at sea was about 40°, but on rocks and
islands the temperature of the air was far higher in clear
weather. The whole of this drift-ice was working in shore,
gathering in eddies behind points, and shooting off eastwards
where points jutted out into the Arctic Current. The move-
ments were analogous to those of floats in a river — sticks,
leaves, froth, or ice. The coast is now rising between St.
John's in Newfoundland and Cape Harrison in Labrador.
Rocks have been marked, and the marks have risen ; boats
now ground on solid rocks where they floated twenty years
AMERICA. 237
ago ; rocks which were seldom seen now seldom disappear
at high tide ; harbours are shoaling ; beds of common shells
are found high above the sea ; raised beaches are seen on
hill-sides in sheltered corners ; and blocks of foreign rock are
perched upon the summits of islands and on the highest hills
near the coast. The rocks are much weathered, and very
few striae were found. Those which were found aimed up-
stream. At Indian Island, lat. 53° 30', near the lat. of Hull,
they pointed into Davis Straits, at a height of 400 feet
above the sea ; at Red Bay, in the Straits of Belleisle, they
aimed N. 45" E. at the sea-level. In winter the sea is frozen
near the coast to a thickness of 18 inches or more ; in spring
the northern ice comes down in vast masses. In 1864 this
spring drift was 150 miles wide, and it floated past Cape
Eace. From a careful examination of the water-line at many
spots, it appears that bay-ice grinds rock, but does not pro-
duce striation. The tops of conical rocks have been shorn
off. The shape of the country is a result of denudation.
No matter what the dip and fracture of the stone may be,
the coast is generally worn into the shape known as "roches
moutonnees." It is impossible to get at rocks over which
heavy icebergs now move ; but a mass, 150 miles wide, perhaps
3000 feet thick in some parts, and moving at a rate of a mile
an hour, or more, appears to be an engine amply sufficient
to account for striae on rising rocks, which were under water
when sea-shells lived above them, and were buried on them.
A cube of ice cut from a stranded l^erg, and floated in sea-
water, rose one-tenth above the surface. At this rate, a cube
300 feet high is 3000 feet thick, and would ground in 2700
feet of water ; one 30 feet high is 300 feet thick, and will
ground in 270 feet. In winter anchor-ice forms at the bot-
tom ; it must therefore form readily about the Imse of stranded
238 HELLEISLE CURRENT.
bergs. The mass which was 150 miles wide was therefore
a floating glacier, armed, as glaciers are, with stones, gravel,
sand, and mud, moving along a definite course, from N.W. to
S.E., from Cape Chudleigh to Cape Eace, and at a rate which
no glacier equals. Work done by it ought to resemble
glacier-work. At the north end of Newfoundland the stream
parts. One narrow rill flows S.W. through the Straits of
Belleisle, and carries small bergs even to Anticosti in the
Gulf of St. Lawrence ; the main broad stream is shunted
westward, and moves from N.W, to S.E. It was crossed
about lat. 49" on the 16th of July 1864. Numerous lai-ge
bergs were seen ; the temperature of air and water fell when
the stream was entered, and rose again when it was left be-
hind. The streaui was crossed again in November, and the
same change of climate remarked, but no ice was seen on
this voyage. The tail of the stream reaches lat. 36° 10', and
it carries large bergs to these regions, which correspond to
Gibraltar and North Carolina.
If such a current flowed over America, marks left by it
ought to correspond to these movements. Striti? ought to run
from N.E. to S.W., where the stream could flow directly ;
from N.W. to S.E., where it was shunted by land placed as
Newfoundland is now placed.
The summers of 1863 and 1864 were remarkable in Great
Britain and Canada for their unusual warmth ; in Labrador
and Newfoundland they were unusually cold, wet, and dark.
Early in March 1864 the sealing-fleet left St. John's in the lati-
tude of Nantes, tried to force a passage through the pack, and,
failing in that perilous attempt, they worked uj) the coast
inside to Toulinguet, about the latitude of the Scilly Isles. At
tliis promontory a shift of wind drove the ice inshore, and the
whole fleet was beset for a month. About the end of April
AMERICA. 239
this mass of iiortlieni ice got adrift, and broke up. It carried
the fleet with it, and thirty vessels were utterly destroyed,
smashed, and ground up. One was forced up on a pan of ice,
drifted past St. John's, and was rescued about Cape Race by a
tug-steamer sent out for the purpose.
From these facts it appears that a warm summer only
increased the intensity of the cold by setting more ice adrift
in the north ; that a glacial period now exists in English
latitudes ; and that the books above quoted accurately de-
scribe the normal condition of these regions of the earth.
If America were now submerged 3000 or even 2000 feet,
the Arctic Current might flow S.W. to St. Louis on the
Mississippi ; but it would be shunted eastwards by high
grounds in Nova Scotia, New Brunswick, and the Northern
States. According to theory, strite ought to run generally
from KE. to S.W. in the central district ; from N.W. to S.E.
on the Atlantic sliores of the Alleghanies.
Ice-marks in North America appear to coincide with this
theory, so far as they were observed in 1864. They did not
appear to coincide with the other theory published by Agassiz
in the Atlantic ^Magazine of the same year, which supposes
the existence of a glacier, which extended from the North
Pole to Georgia ; but on this point it becomes an inexperienced
writer to speak with diffidence.
Newfoundland extends from 51° 40' to 46° 38' N. lat.
The northern end corresponds to the south of Ireland, the
south of Wales, the country about Bi'istol, Gloucester, Oxford,
and London, Barnet, Epping, St. Albans, etc. The southern
end corresponds to the north of Switzerland, the Jura
Chalons, and the mouth of the Loire. The island corre-
sponds to the south of England and the centre of France.
Bones of large reindeer discovered ' in France were found in
24U BKLLEISLF, CURRENT.
latitudes which now swanu with large reindeer in Newfound-
land. The banks reach lat. 43°, the parallel which crosses
Spain near Valencia and Barcelona. In Newfoundland there
are no high mountains and no glaciers ; the land is Iom', and
furrowed by hollows, which run from N. 30° K, or thereby.
Many of these rock-grooves extend under water, and now
contain large bays and fjords. The dividing ridges form
reefs and headlands, and in many cases the ridges and hol-
lows correspond to the strike. Heavy ices of all kinds and
dimensions drift along the coasts, and over the banks, at all
seasons. On the 2d of June 1863 St. Johns Harbour, in the
latitude of Nantes in France, was filled with heavy drift-ice ;
while the pack extended to the horizon of the signal-station,
which is 540 feet above the sea. A photograph of this
strange scene was taken by a native artist.* If the land
were submerged, the Arctic Current would flow through the
valleys, as part of it now flows through the Straits of Belleisle.
A thousand feet would sink the whole land. Watersheds
between the bays ought to be striated from N. 30° E. to S. 30°
W., or thereby, if drift strise were made by ice drifting in the
Arctic Current over Newfoundland. The whole country is
glaciated ; the shape of it has nothing to do with the dip of
the rock, which is folded and bent. At places ice-marks are
well preserved, but generally the rock-surface is weathered.
No ice-marks were found at watersheds, because rocks in the
interior of Avalon are smothered in bogs, and overgrown with
an almost impassable forest ; no rock was seen on the only
isthmus crossed. The striae which were found were near the
coast, and seem to indicate large land-glaciers moving seawards.
At St. John's, the marks run over the Signal-hill, 540 feet,
iVoni W. and N. 85° W. eastwards ; at Harbour Grace, from S.
* SiM' p. 248.
AMERICA. 241
75° W. down the bay north-eastwards ; at the head of Con-
ception Bay they fill a large hollow, overrun hills, and point
from S. 15° W. northwards. Vast terraces of drift stretch
along the base of rounded hills at the head of Conception
Bay, at Harbour Grace, and at Old Purlican, near the end of
only isthmus crossed. The interior is unexplored, and the
whole is very difticult of access, Indians who use bows and ^^
arrows, and large wild animals of northern type have the /^^/^'^♦a
land in possession ; the coast is occupied by fishermen, and ^^ c^
by merchants who deal chiefly in fish and seal-oil. /^ Wl^
In Nova Scotia and New Brunswick striae seem to indi- ffT/V ^^
cate the passage of sea-ice. A current passing south-west- \,
M-ards from Newfoundland would be turned aside by high ^
grounds near Halifax. Strife in the town of Halifax point N. ^^^^^"^V T
55° W., through a gap which leads to the Bay of Fundy. At rU> Tou^v't
a height of 550 feet above the sea, at the summit-level of the /:i.v/vt cc'qr
VOL. II. R // .
240
BELLEISLE CURRENT.
latitudes which now swunu with large reindeer in Newfound-
land. The banks reach lat. 43°, the parallel which crosses
Spain near Valencia and Barcelona, In Newfoundland there
are no high mountains and no glaciers ; the land is low, and
furrowed by hollows, which run from N. 30° K, or thereby.
Many of these rock-grooves extend under water, and now
the rock, which is folded and bent. At places ice-marks are
well preserved, but generally the rock-surface is weathered.
No ice-marks were found at watersheds, because rocks in the
interior of Avalon are smothered in bogs, and overgrown with
an almost impassable forest ; no rock was seen on the only
isthmus crossed. The stria3 which were found were near the
coast, and seem to indicate large land-glaciers moving seawards.
At St. John's, the marks run over the Signal-hill, 540 feet,
from W. and N. (S5° W. eastwards ; at Harbour Grace, from S.
* See p. 24S.
241
75° W. down the bay north-eastwards ; at the head of Con-
ception Bay they fill a large hollow, overrun hills, and point
from S. 15° W. northwards. Vast terraces of drift stretch
along the base of rounded hills at the head of Conception
Bay, at Harbour Grace, and at Old Purlican, near the end of
the bay, 60 miles off. At the head of the bay, most of this
drift seems to have come from the hills. Opposite to granite ^
hills are numerous blocks of granite ; opposite to sandstone (/^'
and slate hills sandstone and slate boulders abound : and yet ,; /
large islands of ice constantly_drif^ into this bay now, and ., — .
some at least bring loads of stone. Three islands, near 100_ a^^,^ IaaaJ,^ • I '
feet high, were cruising in the bay on the 20th August 18(34. ^^^^ 7l~~'
As coast-ice also picks up and drops stones every year, boulders jj^^^ ^^' ^^
from Greenland, Labrador, and Newfoundland, are certainly „ - '
dropped in Conception Bay ; and probably the banks off the (/ ,a~-X^
coast are strewed with similar mixed drift. Bergs ground on ^^ V^aW
the banks ever}^ year, and some have been seen loaded with Ct^Mi^ '^'r^c^
stones. Striae and drift on shore in Newfoundland indicate t^iA^ \/ i^cvy^^u^
large land-glaciers. The shape of the country seems due to ^*Vuhu^ ^u^c^
some more powerful denuding engine, moving as the Arctic ^ia/ Li^,ca,s
Current now moves ; but no glacial strise were found at the y^ ,
only isthmus crossed. The interior is unexplored, and the
whole is very difficult of access. Indians wdio use bows and ^^^^'^'^
arrows, and large wild animals of northern type have the /^^/^'«^/v^
land in possession ; the coast is occupied by fishermen, and ^^ Qlw£
by merchants who deal chiefly in fish and seal-oil. L^ V^^
In Nova Scotia and New Brunswick stria seem to indi- ^V/ ^/
cate the passage of sea-ice. A current passing south-west- a-'To
wards from Newfoundland would be turned aside by high ^ t/-w-iO^
grounds near Halifax. Stria in the town of Halifax point N. ^^""^^^^ 'Tfc^U/
55° W., through a gap which leads to the Bay of Fundy. At rU) Joli^l ^Icia jf
a height of 550 feet above the sea, at the summit-level of the Cuir^ ^it'M^t*
VOL. II. R /7 . i
242 l!KM,i:iSLF. ri'KKKNT.
railway between Halifax and Windsor, stria- point N. 35" \V.
The current which flows S.W. through the Straits of Belleisle
would continue its direct S.W. course through the Bay of
Fundy, if the low isthmus were gone. At St. John, New
Brunswick, strire in the town and beside the suspension-
bridge point N. 20° K, N., and N. 25° E. The same current
flowing o^'er the north-eastern end of the province would be
turned westward l)y high grounds inland. On a hill near
Fredericton, 100 miles inland, and 300 feet above the sea,
sti'ia? point K 35° W., and N. 87° W. There are no high
]nountains in the province, and these high grooves aim at a
distant horizon. Nova Scotia, Newfoundland, and Cape Breton,
are glaciated throughout, and strewed with mixed drift.
On the Canadian side, stria- at (^)uobec point into the gulf
and up the valley of the St. Lawrence ; the land is terraced,
boulders are perched upon the high grounds, and recent shells
have been found far above the sea. These facts indicate the
passage of sea-ice. The falls of ]\Iontniorenci, near Quebec,
have worn a notch in a t(-rrace of rock, above which marine
shells are found. The size of the notch is a measure of the
time which lias elapsed since the shell-beds and the terrace of
erosion were raised above the sea ; for the river only began to
work at this point when the land rose. This tool-mark is well
seen from the town of Quebec on a clear day, when the notch
is filled with dark shadow, and the terrace is a line of light.
In INIaine, New HamY)shire, Vermont, IMassachusetts, and
New York ; from latitude 45° to 40° 40' ; strite found during
this trip, in the latitudes in which icebergs now abound larther
east, appear to coincide with the proliable run of an arctic
cun'ent flowing over the land 3000 feet above the ]iresent
high-water mark, or less. Such a current wcaild continue; its
course from N.E. to S.W. on the Canadian side, and would
243
be turned westwards by mountains which now separate tlie St.
Lawrence basin from the Atlantic slope. The reflected currents
would flow from X."\V. to S.E., as they do at the northern
end of Newfoundland and off the Lalirador coast. Striie at
high levels point towards tlie Straits of Belleisle, where the
Arctic Current is turned aside, Striie at low levels on the
Atlantic slope converge upon distant mountain-passes, which
woidd be sea-straits meeting in the Gulf of St. Lawrence, if
the land were sufficiently submerged ; and the Arctic Current
would then flow through these passes. Horizontal strire on
the shoulder of the highest peak in this district aim N". 25°
E. and N. 20° E., at 1992 and 2307 feet above the sea. If
these marks on Mount Washington, in lat. 44° 15', were
made by heavy icebergs floating through a strait like Belle-
isle, the nearest land on the horizon was then far away.
Lines produced in the direction of these marks skirt the
sources of the St. John and Penobscot rivers, which flow
into the Atlantic, and of the Chaudiere, which falls inih the
St. Lawrence near Quebec. In this direction the land ^is far
lower than the shoulder of jNIount Washington. Produced in
the other direction, these lines pass over Long Island near
New York. There, glaciation is conspicuous in the latitude
of Madrid, as it is in the park at Stockholm ; l)ut the direction
of movement was different at the low level of New York.
Tavo hundi-ed miles away from the White ^Mountains striae
near the top of the Catskill range, at 1935 above the sea, point
N. 40° E. over low grounds, up the valley of the Hudson,
into the wide pass which now contains Lake George and Lake
Champlain, and which lately contained the bones of a whale
buried in drift. In the other direction, this mark aims into a gap.
On the watershed of the gap, at 2115 feet above the sea, a com-
plicated system of cross marks aim K 77° E., and S. 77° E.
244 15KLLEISLE CUKRKXT.
In the opposite direction, all these point into u holloAv, which
would he a strait passing through the Catskill range west-
wards if the sea were 2200 feet deeper than it is now. These
sets, the highest marks obser\^ed, point N. and E. At lower
levels the marks aim at passes K and W. For a distance of 12
miles, and np to a height of 1800 feet, horizontal stria? on the
Catskill escarpment, and in the low country beneath it, aim at
the lowest ground on the distant horizon, which is between
the Adirondak and Green Mountains, and leads through the
valley of the St. LawTence back to the gulf. This certainly
was a sea-strait when the whale swam in it.
Fifty-seven miles below Albany, on the Hudson, near
high-water mark at Barrytown, opposite to the southern end
of the Catskill range, the strire turn and point N. 8" W. At
Kew York, in the central park and near Broadway, about lat.
40'^ 40', at six different stations, strire aim N. 21", 30", 36°, 37",
a9", 45° W. Some of the stones in this central park contain
large plates of mica, and may have come from the White
Mountains, or from the "azoic" regions about the Adirondaks.
Others may have come from Labrador, for they match rocks
in that country. Further north, on the Atlantic coast, a
system of marks seems to converge upon a chain of lakes
in Maine. A line produced N". 55" W. from Eastport strikes
the Pemadumcook Lake. Lines produced N. 14" W., and N.
28° W. from Portland, avoid the Wliite INIountains, which are
visible at a distance of 90 miles, and strike the Mooselook-
maguntic Lake near Saddleback Mountain, about lat. 45".
These converge upon a low watershed. A line produced N.
25" W. from Boston skirts the western side of tlie White
Mountains, and enters a wide pass which leads to Canada.
If the direction of the highest stria3 of this series be taken
as the direction of the main arctic stream, N. 25" E. to S. 25°
AMERICA. 245
W., it would strike against the White Mountains, Green
Mountains, Adirondaks, and Catskills, and glance westwards to
Eastport, Portland, Boston, Albany, and New York. It would
escape from passes in the main range, as the Arctic Current
now escapes through the Spotted Islands off Labrador, and
through deeps between the sunken banks off Newfoundland.
On the other side of the mountains, marks in the valley
of the St. Lawrence correspond in direction. At Montreal
Mountain, strise point N.E, magnetic ; at Brockville, they
point N. 45'' E. true ; at Niagara Falls N. 20° and N. 5" E. ;
at Buffalo N. 20" and N. 13" E. But, while a general south-
westerly direction is thus marked by strong deep lines, other
lines cross in all directions. At Brockville, for instance, a
deep groove three or four feet wide aims N. 45" E., and all
lines in it down to hair-lines aim in the same direction ;
but on a neighbouring rock a cross system of smaller grooves
aims N.W. almost at right angles to the general direction ;
and at Prescott, the only marks found aimed N. 20" W.
The water-lines of the great lakes and rivers are not striated,
though much worn by winter ice. These variations in a
wide plain accord with the erratic movements of icebergs in
summer, the strong markings seem to agree with the general
combined movement of the spring drift.
So far these fixed marks agree with the probable move-
ments of an arctic current. In order to make the marks, a
polar land-glacier would have to climb more than 2000 feet
out of the Gulf of St. Lawrence, over the shoulder of Mount
Washington. According to other marks it also climbed over
the watershed of the St. Lawrence into the Mississippi basin,
and reached lat. 39°, which seems an impossible feat for land-
ice to accomplish.
Though other observers have found striated rocks south
246 BKLLEISLE CURRENT.
of ]Jullalo, in the central district none were found during
this expedition. All the rock-surfaces found in the Westera
States were either weathered or water-worn, though many
were newly uncovered. Fossils project half an inch at many
spots. But glaciated boulders were found near St. Louis, at
Indianapolis, Lafayette, Fort AVayne, Crestline, Upper San-
dusky, and many other places near the watershed of tribu-
taries of the Ohio and St. Lawrence. Many were found
between lat. 39° and 40°, in Ohio, Indiana, and Illinois. Not
one south of 39° in these states, or south of 41° in Western
Pennsylvania. At St. Louis, Vincennes, Louisville, Cincinnati,
and Pittsburg ; along the banks of rivers, and beside railways,
no single specimen could be discovered. At these places, and
in Kentucky, further south, near lat. 37", the rocks are covered
by thick beds of pure clay and fine sand. South of a line drawn
from lat. 41°, long. 81°, diagonally, south and west, to lat. 39°,
long. 90°, near St. Louis, no glaciated boulders were found. A
short distance north of the line, blocks of Laurentian gneiss
as big as bullocks are scattered broadcast over the flat prairies.
The nearest fixed rocks of the kind are about Lake Superior,
but stones of the very same size, })attern, and material, are on
the top of the Catskill range, on tlie top of the Green INIoun-
tains, on the shoulder of Mount Washington, on the highest
ground near Buffalo, on the liigh grounds near Niagara, at
Brockville, on Montreal Mountain, at Quebec, on hills be-
side the Straits of Belleisle, on islands near Hamilton Inlet in
Labrador. Similar stones are strewed over Newfoundland,
Cape Breton, and Nova Scotia, at the head of the Bay of
Fundy, and all down the Atlantic coast as far as New Yoi'k.
None were found at Philadelphia, Baltimore, Harrisbui'g, oi-
Washington. Water-worn drift abounds at all these jjlaces,
l)ut no striated gneiss boulders were found i here. <^n tlie banks
AMERICA. 247
of the Potomac and at Washington are large stones in ch\y,
but none of those found were striated. At HarrisLurg is a
simihir deposit. Icebergs and rafts of coast-ice are carrying
northern drift stones in the Atlantic, and if America were
submerged the Arctic Current might carry them as far as lat. 39",
long. 90^ for Atlantic bergs reach lat. 37° in long. 47° W. If
a polar glacier carried these stones they ought to be found in
great moraine heaps at the end, but nothing like a terminal
moraine exists in the prairies. For hundreds of miles the plains
are almost as flat as the sea, and where the country rolls, sheets
of drift cover the rolling plain, as snow covers it in winter.
The stones and clay were surely dropped from melting ice-
rafts, as snow is shed from clouds, and as stones are now sown
in the Atlantic : — broadcast. Observations made in America
so far agree with observations made in Europe.
In a series of papers in the Atlantic MontliUj for 18G4,
Agassiz attributes glacial phenomena to polar glaciers which
reached lat. 36° at least, and were 6000 feet thick in lat. 44°.
24G
RKLLEISLE CURRENT.
of BuH'alo, ill the central district none were found during
this expedition. All the rock-surfaces found in the Western
States were eitlier weathered or water-worn, though many
were newly uncovered. Fossils project half an inch at many
spots. But glaciated boulders were found near St. Louis, at
Indianapolis, Lafayette, Fort Wayne, Crestline, Upper San-
dusky, and many other places near the watershed of tribu-
taries of the Ohio and St. Lawrence. Many were found
between lat. 39° and 40°, in Ohio, Indiana, and Illinois. Not
one soutli of 39° in these states, or soutli of 41° in Western
Pennsylvania. At St. Louis, Vincennes, Louisville, Cincinnati,
and Pittsburg ; along the banks of rivers, and beside railways,
no single specimen could be discovered. At these places, and
in Kentucky, further south, near lat. 37", the rocks are covered
by thick beds of pure clay and iiue sand. South of a line drawn
from lat. 41° long. 81°, diagonally, south and west, to lat. 39°,
long. 90°, near St. Louis, no glaciated boulders were found. A
short distance north of tlie line, blocks of Laurentian gneiss
li.
^iffli '^^^mmn
§S5.
-^^■^^i^ri
eg- 5
%^^l
S.O
4 o
'p' S'a- 3 ° .
^•^.
Ig KS K^
AMERICA. 247
of the Potomac and at Washington are large stones in clay,
but none of those found were striated. At Harrisburg is a
similar deposit. Icebergs and rafts of coast-ice are carrying
northern drift stones in the Atlantic, and if America were
submerged the Arctic Current might carry them as far as lat. 39",
long. 90", for Atlantic bergs reach lat. 37° in long. 47° W. If
a polar glacier carried these stones they ought to be found in
great moraine heaps at the end, but nothing like a terminal
moraine exists in the prairies. For hundreds of miles the plains
are almost as flat as the sea, and where the country rolls, sheets
of drift cover the rolling plain, as snow covers it in winter.
The stones and clay were surely dropped from melting ice-
rafts, as snow is shed from clouds, and as stones are now sown
in the Atlantic : — broadcast. Observations made in America
so far agree with observations made in Europe.
In a series of papers in the Atlantic Montldtj for 1864,
Agassiz attributes glacial phenomena to polar glaciers which
reached lat. 36° at least, and were 6000 feet thick in lat. 44°.
A theory espoused by Eamsay, Geikie, Sir W. Logan, Agassiz,
and such men, is worthy of careful investigation. The obser-
vations above recorded seem rather to indicate the action of
polar currents, like those which exist, than the existence of
polar glaciers of these dimensions. The facts above stated may
swell the pile on which a just opinion must be founded at last.
The question turns on the denuding power of the Atlantic drift.
The forms into which the land has been ground by some ice-
engine closely resemble glacier-work ; if the Atlantic drift
is too small to account for the work, the polar glacier is the
only resource. After seeing glaciers and sea-icebergs at work,
and hearing the accounts of those who are familiar with the
polar sea-drift, the writer holds to the opinion expressed above,
and takes his stand on the iceberg for the present.
CHArTEK XLIV. T^S^^,^^^ ^^Cc-u^
GLACIAL PERIODS. V ^^^^-^^^ / ^— ^^
One general conclusion arrived at is, that the mean tempera- ^^
ture at the eartli's surface may now be as cold as it has ever ^^-"^"^^^Yj M^
been, though climate has varied at particular spots. ^^ h^^xyircJi,
In Britain, for instance, tliere has been a recent " glacial ^ct^^l^Zvtov^ o/
period," whose marks are perfectly fresh ; but according to fijjL/^^;^^^^^^ •
theory, partly founded upon these marks, it was a period like ^i
that which now prevails on the banks of Newfoundland and y^ ^^^'^
s of _£
the coasts of Labrador.
Mr. Hopkins (quoted by Lyell, chap, vii.. Principles of ^X^^*^
Geolog^j, 9th edition, 1853) calculated in 1852 that the snow- "-^^ (^t^-f^
line and glaciers woidd reach the sea in Wales and Ireland — ^ JcMyC^^^Ae*^
1. If the Gulf Stream were diverted. /f^^^I^'^^^/(yxM><^
2. If land in Northern Europe were depressed 500 feet. l
3. If a cold current swept over the submerged area simul- .
taueously. Jq iL^/j}
The British marks above described seem to prove that a ^^lw-c^
cold current did sweep south-westwards over Great Britain, '^^^ fltcij,*-^
at a time when the land was submerged about 3000 feet ; and f^/lu ^^'V^<^
that glaciers did reach the sea in these countries till land ^;WiZ^^ .
rose to the level of 1400 feet, or thereabouts.
There has also been a recent glacial period ui North
America, V)ut, according to theory, it was only the marine
climate, which now exists to the east in corresponding lati-
250
tJLACIAL I'KHI
L
tudcs. Sir C. Lyell has poiiitnl out tliat tlir glacial pcriml ol'
tlie Southern Hemisphere comes still nearer to the Equator ;
and if similar conditions prevailed in the northern half of
tlui world, the cold might drift as far there.
In chap, vii., Principles of Gcolojy, it is i»oint('d out that
Captain Cook found snow many fathoms thick extending
ilown to the brink of sea-clilfs in lat. 59° S., which corresponds
to Northern Scotland ; and that he foimd the perpetual snow-
line coincident with the sea-level in lat. 54° S., Avhich corre-
sponds to Yorkshire.
In the Illustrated London News of 18tli June 1864, is a
woodcut and a description of a collision with an iceberg on
the 4th of April 1864, in latitude 54° 40' S. About midway
between Melbourne and Cape Horn, the screw-steamer ' Koyal
Standard,' while sailing with a strong breeze, suddenly ran
into a dense fog, and shortly afterwards she ran against a cliff
" six hvmdred" feet high. After bumping and scraping along
this lloating island for moi'e tlian half a mile, and suffermg
great damage, the vessel rounded the end of the cliff and so
escaped. She made her way under jury-masts to Kio de
Janeiro. In the earlier months of the same year, the Himalaya
and other vessels returning from Melbourne found these seas
" beset with icebergs." At the rate of l-9th above water, this
l)erg was 5400 feet thick, 4800 feet under water, and 600
above. ^ In latitudes corresponding to the Mourne mountains,
the Solway Firth, Cumberland, and Durham, the sea is beset
with hills of ice a great deal thicker than all that is visible of
the British Isles. If the sea were level with the top of Ben
Nevis, a berg of this size might touch the top, scrape the
bottom of Loch Linne, 500 feet below the present sea-level, and
vise 600 feet above wati'r still. /^Changes of climate, and
glacial (louudalioii, which such llcets might accomplish, are
r
I f
v_
AY, JUNE 29, 18G8.
Ou
' TBEDUKE OF EVINBURGH.
Her Majesty's ship Oalatea, Captaia bis Royal Hicbneaa
the Duko of Edinburgh, ILG., left Sydney at 6 30
D.tn. on the 6tb of April, and passed the Snares ofiT
the southern extremity of New Zealand — the 'only land
seen on the pas!»age — at 2 p.m. on the 11th, having
run the first 1,.100 mHes in 4J days. On the 23d of
April, when' in lat. 55 20 S., and long. Ill W.,"eEe
passed a large nat-topped iceberg 450 feet high, and three
quarters of a mile long. On the 24th passed two large ones,
one of them 400 feet high, in form something like a hay-
stack ; the same night another, which, in the absence of i
a moon, was not seen till right abeam, distant only
three miles ; early the next morning sighted ^another |
right ahead, when running 13 knots an hour, and soon after- |
wards passed one on the port bow, and ran between several i
pieces of drift ice, and soon afterwards passed another on i
the starboard bow. In none of these cases did the thermo- I
meter give any warning of approach to danger. The tem-
pera tureo^ the ^a was either the same as that; of the atmo- '
sphere, or higher, but never lower ; in one case it was 3 deg.
higher, and in another 4 deg. The bergs were passed be-
tween long. Ill W. and 105 W. The Galatea passed the Horn
at midnight on the 30th of April, having run the dis-
tance from Sydney in 24J days (allowing for difference of
longitude and change of reckoning). She never got the south-
east trades at all. Crossed the equator in long. 25 16 W,
on the 28th of May, 27J days from the meridian of Cape
Horn. Got the north-east trades in lat. 9 2 > N., long, 26^,
W, on the 1st of June. Had light winds north of the Line,
which fell away to a calm on the 24th, when steam was got
up. On the morning of the 25th fell in with a pilot boat, and
obtained news up to the 15th, got soundings in 85 fathoms
60 miles from the Scilly Islands. Steam was occasionally
used during the passage, for about eight or nine days in all.
Lord Newry, the Hon. E. O.Yorke, Lieutenant Haig, R.E.,
and Mr. Brierly, who went out with the Duke of Edinburgh,
have returned in the ship. Mr. Whatmore, engineer, and
Mr. Tregilgas, engineer (invalided), from Her Majesty's
ihip Challenger, have also had a passage in the ship.
r-
GLACIAL PEKIOUS. 251
not easy to calculate. Sailors, familiar with bergs off New-
foimcUaud, affirm that even these are insignificant to bergs
commonly seen off Cape Horn.
There are plenty of glaciers in New Zealand, about Cape
Horn, and in South America ; and very large icebergs, 150,
'■a -a
^? .1^ Till -
S £5 ^ S. 5 > oO'i
. .„. .„„„^ ?i LUCIllLfl?o^>9lI»0
the climate is now excessively hot.
It is proved that glacial action once extended a great way
from the Swiss mountains ; and that fact has been used to
support the argument for a period of intense cold. But if
ever there was a Baltic cvirrent east of England, Switzerland
was on the other side of it, and the Alps and Pyrenees must
have shared the influence which chilled Scotland.
The highest Swiss mountains are about 15,000 feet above
the sea ; their perpetual snow-line is at about 8500, and glaciers
* 111 his address, Sept. 14, 1864, at Bath, he attributes a ibiiuer extension
of aliniie glaciers to the submergence of laud, now the Sahara, where marine
slirlls have bc.ii found.
,13 Sis 2
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o a ^
GLACIAL PERIODS. 251
not easy to calculate. Sailors, familiar with bergs off New-
foimiUaud, affirm that even these are insignificant to bergs
commonly seen off Cape Horn.
There are plenty of glaciers in New Zealand, about Cape
Horn, and in South America ; and very large icebergs, 150,
250, and 300 feet high, and two miles in circiunference, have
been seen adrift off the Cape of Good Hope between lat. 30°
and 39°. These last were in latitudes which correspond to
Gibraltar, parts of Africa, Syria, Cyprus, Candia, Asia IVIinor,
Persia, Cabool, Japan, and Washington.
Sir Charles Lyell long ago imagined possible distributions
of land and sea which might, as he argues, produce great
general changes of climate over the whole earth.*
Having climbed thus far, some well-established facts
begin to wear a different aspect.
If marks in Scandinavia and Britain do m fact prove that
a cold current changed the climate of Western Europe, then
similar currents may have done as much elsewhere. It is not
necessary to assume a general glacial period in past time,
because marks of ice are found on rocks in countries where
the climate is now excessively hot.
It is proved that glacial action once extended a great way
from the Swiss moimtaius ; and that fact has been used to
support the argument for a period of intense cold. But if
ever there was a Baltic cm-rent east of England, Switzerland
was on the other side of it, and the Alps and PjTenees must
have shared the influence which chilled Scotland.
The higliest Swiss mountains are about 15,000 feet above
the sea ; their perpetual snow-line is at about 8500, and glaciers
* 111 his address, Sept. 14, 1864, at Batli, he attribute.s a former extension
of alpiue glaciers to the submcrgeuce of laud, now the Sahara, where marine
sIr-IIs have l.fuu found.
252 GLACIAL PERIODS.
slide to within 3000 feet of the sea-level now. The mean
temperature below is about 55° ; but if Western Europe were
sunk 3000 feet or more, to the level of boulders on Beinn
Wyvis and Driom Uachdar in Scotland, and on the Dovre-
fjeld in Scandinavia, then the Baltic Current, which carried
Scandinavian boulders into Poland, might also wash the base
of the Alps. They are in the latitude of Nova Scotia, where
the mean coast temperature is 41° instead of 55°. At this
rate the high Alps would still be 10,000 and 12,000 feet
above the sea-level, in regions where Glaisher found snow
falling above England, in June 18G3, when the surface tem-
perature was 66°. Alps 12,000 feet high, with a mean tem-
perature of 41° at the base, and a cold sea passing westwards,
might well breed glaciers large enough to be launched as ice-
bergs if Scotland and Scandinavia were chilled and frozen also.
When the land rose, these alpine glaciers would dwindle if
the climate warmed as the sea fell, but they might take a
long time to shrink to their present size.*
Cold is not easily driven from a fortress of which it has
long held possession. It takes a long time to get the winter's
frost "out of the ground." If the tail of the polar glacial
system passed near the Alps, existing glaciers may be rem-
nants of a large local system, like that which once covered
Scandinavia, and is now dwindling away there.
If the Mediterranean were the receptacle of an arctic
current laden with icebergs launched from the Alps, and drift-
ing over France, Italy, Austria, and low lands then under
the sea, there might be a local glacier system in Syria, and
icebergs in latitudes which correspond to seas off the Cape of
(lood Hope.
* Hitchcock, ;in emiiient American geologist, found wliat he couHidorod to
)m' ancient sea-beaclics, at about 3000 I'cet above tlic sea, in Switzerland.
GLACIAL PERIODS.
253
Hooker found an ancient moraine beside the cedars of
Lebanon, and photographs of the Holy Land show rock-forms
which strongly resemble ice-work.
Still further south, in Africa, snowy mountains now exist.
If the cold stream ran that way, these may have bred glaciers
at the Equator itself.
As described by Captain Grant in a lecture before the
Ethnological Society, in June 1863, the country about the
source of the Nile has a glaciated form. Some parts of it were
said to consist of " flat-topped hills, with outbursts of granite ;
rounded masses are lying upon each other ; there are saddle-
backed hills whose western faces are steep and broken ; and
large loose stones are scattered about." As snow was in sight,
and moraines are in the Lebanon, as the climate of this
raised African plain is temperate now, a glacial period is
possible even about the sources of the Nile.*
In Central Asia is a large system of local glaciers in the
Himalayas, which are well described by Hooker. According
to that traveller these glaciers are now dwindling away, for
their marks extend far beyond their present limits. Are we
therefore bound to assume that the whole world is getting
warmer ?
The snow-line of the Himalayas is now at 15,000 feet,
and the mean temperature at Delhi is 73°. On the coast of
China, in tlie latitude of Delhi, the mean temperature is 64°,
according to Dove's Isotherms. But if Behring's Straits were
wider, the climate on the eastern coast of China would suffer.
There is a cold current there now, it would be colder. Accord-
ing to Kotzebue, there is a striking contrast in the vegeta-
* This guess is left as first printed. It is not founded on any personal
knowledge of the place ; tut as the Sahara is now proved to be a recent sea-
bottom, Alpine or Scandinavian boulders may be found there.
254 GLAf'IAT, PF.mODS.
t'lou on oppusite coasts in lU'living's Straiis, wlio'c no wider
tlian the Straits of Dover ; the Avostcin American coast
is well-wooded, but the eastern Asian coast is V)are and
barren. A current runs inwards on the American side, and
a miniature arctic current is Ixdieved to run out on the Asian
side.
But if Behring's Straits were as wide as the North Atlantic
between Greenland and Scandmavia, so as to spill the Arctic
Current south-westward along the mountains of Chinese
Tartaiy, and over tlie lo-\v grounds of eastern Asia past the
Himalayas, and over India ; then, even tliough the glacier-
system of the Himalayas were lowered nearer to the earth's
centre out of the cold and into the heat, the cold would gain
if the sea were chilled, and the mean temi^erature at the foot
of the hills changed from 73° to 64°, or to some lower tem-
perature.
If mountains 28,000 feet high were lowered to 18,000, and
stood in chilled water, with a climate like that of England at
the coast, then the snow-line would be lowered, and Indian
inountains miglit well breed larger glaciers.
Tliey might even launch icebergs, and send stone- fleets
south-westwards to choke harbours on the African coast, and
do glacial Mvn-k about the sources of the Nile.
In Nortli America a glacial period reached latitudes
wide] I icebergs now reacli in the Atlantic, and it appears
tliat the continent was submerged about 3000 feet during
some part of the "glacial period." Eminent men hold that it
was a period of intense cohl and enormous ghteiers. Tlie
writer l)elieves that it was a period very like the pi'esent,
(hn'ing wliicli tlie Arctic Current has changed its course, and
Iniid has risen and sunk about 3000 feet.
/. / Tlie changes of level required to swamp continents and
GLACIAL PERIODS. 255
change the course of oceaii-cuiTents, are not so large as may
l)e supposed.
500 feet would sink the source of the Volga and drown
the most of Europe.
2850 feet would sink the source of the Danul)e ; 4500
M^ould sink the Elbe ; 1250 feet would sink the lake of Con-
stance ; 800 feet Basle ; 1400 feet the Clyde ; and boulders
are perched on higher European watersheds, in Scandinavia,
Scotland, Wales, Ireland, and central Europe.
At 4575 feet, on the Dovrefjeld, granite blocks are on
mica slate (Von Buch, etc.)
At 3000 feet, on Beinn Wyvis, mica-schist is upon slate.
At 3000 feet, on Driom Uachdar, gray granite is on slate.
All these are at places where transport by local glaciers is
out of the question. On the Jura mountains, erratics derived
from the Alps are common at about 3600 feet, and they too
may have floated on ice-rafts, according to this theory of a
sunken land now raised in Europe.
In Asia, the Ganges runs out of a glacier at 13,000 feet
above the sea. How much would sink China is not ascer-
tained, but most of India would be drowned by a depression
of 4000 feet.
In America, 630 feet would sink Lake Superior, and the
bottom of Lake Ontario is below the sea-level now. If
ancient fossil-shells of marine origm are sea-marks, most of the
high land in the world has been under the sea at some time.
If terraces be sea-marks, there are terraces on Snowdon, and
on the Alps, according to Hitchcock, at 3000 feet ; high up on
the Himalayas, according to Hooker ; and at about 3000 feet
on the "Wliite IN fountains in North America. Sea-shells were
found at 3000 feet on Snowdon, by Mr. Bauragarten, in 1847. ^s
There are cold climates, cjlaciers, and glacial action in
256 GLACIAL PERIODS.
spots all over the world, wherever mountains are high enougli
to reach the cold, so as to catch and condense the clouds.
If such hills stand on the western side of an ocean stretching
nearly from pole to pole, and are washed by a cold stream, as
in Greenland, any quantity of glacier-work yet found may
be accounted for, without assuming any great universal
change of climate at the distance from the earth's centre
which is now high-water mark.
Though climate has changed place, it is not proved that
the snow-line has sunk and risen again everywhere.
One of the last writers who have specially studied this
subject, in speaking of Scotland, says : —
" In whatever way the change was brought about, there can be little
doubt that when the land began once more to rise the temperature had
likcAvise risen."
This accords entirely with what has been said above.
But the following passages from the same page do not : —
" The submergence of a large tract of land would tend to ameliorate
the climate. . . . The depression seems to have been general over the
north of Europe, though probably varying greatly in extent in diflerent
regions." *
According to the theory now submitted to the merciful
consideration of able judges, any depression of land that lets
an arctic or antarctic current flow past an easterm coast will
not ameliorate but spoil a good climate ; and such depressions
in Europe and elsewhere probably caused the last " glacial
period" in Great Britain and Ireland ; perhaps in the Alps
and Pyrenees, Italy, Greece, Syria, India, America, and it
may be in Nubia also.
There is yet another theory which will account for larger
* On the Pfienomena of the Glacial Ih-ift of Scotland, by Archibald Geikie.
Glasgow, John Gray, 99 Hutchison Street. 1863. P. 102.
(ILACIAL PERIODS. 257
glaciers il' icebergs of the dimensions described are too small
to account for the ice-marks.*
It may seem paradoxical, but if the general temperature
of the eaith's upper crust were a little warmer, and solar
radiation the same, there might be more glacial action.
The southern slopes of the Himalayas ought to he warmer
than the northern, and glaciers ought to abound most in the
coldest side, if glaciers resulted from cold alone. It is not so
in fact, because glaciers result from cold and heat. Many
English sportsmen have described these regions. Hooker
gives a reason for the abmidance of glaciers on the warmest
side of the hills ; ]Maury tries to explain like facts, in America
and elsewhere, in his " sailing directions."
There is often a clear hard sky to the nortli, Ijehind the
ridge, when the southern districts are shrouded in mist, and
deluged with rain, below the snow-line. Warm moist equa-
torial winds which sweep over the hot plains of India come
loaded with transparent vapour. AMiile thus expanded, the
vapour only serves to intensify the heat by refracting the
sun's rays Like a lens, but when these hot wet winds meet
the cold air of the high mountains, they are cooled and con-
tract, the vapour is condensed into mist, the lens is spoiled,
and the clouds drop their loads while they screen the snow
from the sun. These big snow-heaps spread an awning of
cloud in the air, to shield them from light.
The winds which pass over the Himalayas have but a
scanty remnant of their store to bestow upon the northern
slopes and high plateaus of central Asia ; they carry little to
the polar regions, to which the cargo was first consigned. To
use Maury's illustration, the wet is squeezed out by cold, as
* For a theory of this kind, see QimrterJij Journal of ScicHCc, 186i ; and a
lecture delivered at the Royal Institution, by Dr. Frankland, .Tan. 29, 1864.
VOL. II. S
258 GLACIAL PElllODS.
water is wrung from a sponge. There is a clear sky on the
northern side, and the snow which does fall there melts
rapidly, or evaporates, because the sun's rays are but little
impeded by clouds in the lens of air.
If there were more water in the air generally, there would
be more clouds ; and these would form most at the coldest
spots, because, in the Himalayas and elsewhere, that is the
result of evaporation and condensation on the largest scale.
A confirmation of this opinion is given by the weather of
1863, 1864. In Britain and Canada the summers were very
warm and bright ; in Labrador and Newfoundland unusually
cold and very misty. There was more evaporation at one
place, and more condensation elsewhere.
If the whole of the sea were frozen, there coidd be few
clouds ; but if the whole world were warmer, there would
be more evaporation everywhere, swifter movements, more
condensation about the Poles, and more glacial action at liigli
levels and latitudes.
The same thing takes place in ScandinaA'ia, apparently
for the same reason.
Warm wet south-westers, loaded with moisture, picked u[i
from the Avarm Gulf Stream, fly over the sea and the low
islands off Scotland, but they begin to drip as soon as they
get to high land. The rain-fall at luverary and Gairloch is
far greater than in the Western Isles and Shetland ; but
when the clouds nnicli the snowy land about Bergen, they
pour. About the glacier districts there are floods and snow-
storms when there is clear Aveatlier close at hand. When tlu^
winds get to the high grounds, about higher watersheds
further to the nortli and east, they have still a remnant of
snow for Sneeluetien, but tluno i.'^ not enough to make snow-
domes and glaciers. The summer sun clears most of Scan-
GLACIAL PERIODS. 259
dinavia, because the sky is generally clear to the east of the
hills, and the sky is clear because Bergen and the west coast
glaciers have cleared it. From Bodals Kaabe, glaciers stream
down almost into the sea ; but there is no glacier worthy of
the name at 8000 feet above the sea further east, and still
further inland, at Sneehaetten and Eoraas (chaps, xiv. to xviii.)
The Bergen glaciers catch the Scotch clouds when they
land, and hold them till they are well-nigh drained.
Sneefell, in Iceland, is another case in point. It stands
far to the west, and has a local glacier system ; it often
gathers clouds from a clear sky, and rivulets pour down from
it while neighbouring tops are clear of mist and snow, and
rivers which flow from them are all but dry. It is a cloud-
condenser, distilling glaciers from the air.
Iceland itself is another example. All the large glacier-
systems are on the south, and in the centre of the island ; no
glaciers approach the sea on the northern coast (chap, xxv.)
Every floating iceberg is surrounded by a veil of mist,
wliicli preserves the cold mass by stopping light. The wetter
and warmer the air is, the thicker is the fog which results.
Fogs on the banks of Newfoundland, near the borders of the
hot and cold water, are peculiarly dense (chaps, xxiii. xxiv.
xliii., etc.)
On a bright day after a shower of snow, the shadows of
posts in Hyde Park are often marked out in lines of snow,
when tlie rest of the ground has been cleared by sunlight.
Of two vessels of water in sunlight and shade, on the opposite
sides of a house, the one on which light falls most loses most
weight by evaporation.
The following is the result of an experiment. l\)th June
lS(i4. — Two glass vessels intended to Imld milk in a dairy,
wove pai'tially filled with garden mould and water, made equal
260 GLACIAL PERIODS.
in weight, and exposed on opposite sides of the same house — on
the north side under a verandah, on the south side on a pillar.
lid Jane. — After about forty-eight hours weighed. Weather
fine ; strong S. W. Ijreezes, and bright sun during the day ; clear
sky at night ; no rain.
Shade . . . . . J>4i ounces.
Light 76
Difference . . . . ISj
Sun-light is a force which lifts water, but it is turned aside
by any screen which casts a dark shade.
But if the whole earth were warmer, the sea would be
warmer and would evaporate faster, to form more clouds, to
give more shade to the ice-condensers, which now exist, in
spite of sunliglit, even on the tops of volcanoes.
If Himalayan, Scandinavian, and Icelandic glaciers exist
because there is a warm sea and a bright sun at the Equator,
it seems to follow that they worJd grow larger, and tliat
polar systems would move faster, and so get further into
warm regions, if more power were applied at the boiler-end
of the caloric engine.
The same result follows if more fuel is burned under a
still, or if colder water is poured on tlie worm ; in either
case the liquor flows faster. If weight be added in one scale,
or taken from the other, the result is the same on the balance.
Because there are large glacier systems in Iceland, close
above boiling water and molten stone, tliere may have
been glacial periods on a far warmer globe. But the present
state of things appears sullicient to account for all glacial
phenomena yet ol)served.
Yet another theory has been started to account for glacial
peiiods. It is assumed that there are regions in space which
i-^
u^-^ ;^" (t--^?
/^r
W^^
^
GLACIAL PERIODS.
2GI
are colder than others, and that the solar system passes through o
these frigid zones at stated periods. These regions are as yet "^^j-wit/ier,
beyond the reach of a mere traveller, and the ice-records ^^ ~^
which he has endeavonred to translate do not seem to reach ^'^^Y^^^^"^ (/ ,
far back or recur at intervals. If anything is to be learned fV ^^^ C^i^
about fossil climates, patient grubbing in mud and ashes ^'^^''"'A'v^^
may do more than soaring at once after astronomers into d^^,
infinite space, r^M^t^iiy^c-i^
The way upwards lies downwards at first. A l>reaker ^/i^/i-t-*- ^IZi
falls headlong, but the spray rises, and the force of the fall ^ft
builds up the sea-beach. We must wade through water to
dry land, and grope in darkness before we can reach light.
O
Fig. 01. A Bre.\king Wave. From a photograph.
THE END OF P.VRT I. — DENUDATION.
i.
^ ^'t.cX^y- U^y/is ^vi/?l M-'/r-e-cy^ y'/'U-^}
fd£7--
\
CHAPTER XLV.
DEPOSITION I.
NATURAL SCIENCE — FORCE — ENGINES — TOOLS — MARKS.
In the preceding pages an attempt lias been made to show
that some branches of geology may be studied experimentally.
Small engines, which are worked by the natural forces
which work natural engines, imitate nature ; and if all me-
chanics are parts of one system, that which is learned from
one engine applies to all. So in studying " dynamical
geology," workmg-models are useful aids.
Men can neither alter the laws of nature nor oppose them
with success ; they nmst obey ; but they can work with
nature's powers by obeying nature's laws. An engineer
cannot stir a boat by stuffing a furnace with ice and a con-
denser with embers ; but by using heat and cold in the natural
order of heat below and cold above, pistons are lifted and
lowered, and steamboats are moved horizontally round the
world. We are too short-lived and short-sighted to see with
bodily eyes large geological movements and changes, which,
in long periods of time, take place in air, sea, and land, about
us ; we cannot even hope to see the whole of the outside of
the ball on which we dwell ; we cannot get at the inside of
it at all. The comprehension of any part of this engine is
out of our reach, because we cannot even see the works. But
models may be worked by the aid of natural forces, and when
the models are cn<^ines of manageable size, their mode of
NATURAL SCIENCE. 263
iictiou is more easily understood. We may learn something
about the large engine, by watching how small ones work.
There are many things which men know but cannot ex-
plain, many facts which we are incapable of imderstandiug.
We cannot explain why we fall in air, sink or swim in water,
and stand upon earth. We know the facts, but do not ex-
plain them by calling a force " gravitation," and by talking of
"gases, fluids, and solids," and their " specific gravities." But
in striving to reach unattainable knowledge, some has been
reached which is power when applied to small engines ; and
which gives some vague notion of the largest engine of all.
Astronomy is learned from the fall of weights, and the flight
of small projectiles. Geology may, in like manner, be learned
from geological toys. Human minds camiot grasp the ideas of
infinite size or smallness, space, time, or number ; but those
who think are driven by facts to perceive that these incom-
prehensible things must be. If there be a limit anywhere,
what is beyond it ?
Men can never understand the great engine which works
in infinite space, for they cannot even comprehend an atom ;
but that is no reason for ceasing to strive. An old Scotch
saw says, "Aim at a go"\vii of gowd, and ye '11 get the sleeve
o't." In stri\ing to understand how mountains have been
made, we may set natural mechanical forces to build and
demolish moleliills ; we can construct and watch our little
engines. In seeking abstract knowledge, things of practical
use — shreds of the golden gown — are found. By experiment,
designedly or accidentally made, men have learned all that
they know about the engine with which they travel through
space ; and they have used their knowledge to make small
useful engines to carry them round the deck of their spherical
rolling ship.
2G4 FORCK.
By geological experiment, human minds may gain more
knowledge of the engine, under hatches, and by imitating it
gain more power. Engines are worked only by using natural
poAvers ; these were found out while searching ; the most
ignorant searcher may cliance to find a treasure, even on
board of this our argosy M'hich circles round the sun.
Water and steam power are treasures, luit only applica-
tions of natural force to human engines.
It took a long time to " invent" a water-mill, and a clock,
and other engines worked by weights. The hydraulic cranes
which now wave their black iron arms like living giants, and
lift and pour out cauldrons of molten iron as a man lifts a
pail of water, have only appeared in modern times ; but gra-
vitation, which works all these engines, had been pouring rivers
and oceans upon the earth, and steering it amongst other
stars, before there were men or millers to use that natui-al
mechanical power. Like it, steam is no human invention,
and its application to engines is nothing new. It is told that
one of the many so-called inventors of steam-engines gained
his first knowledge of steam-power from the clattering lid of
liis mother's kettle. He was but a young discoverer, an
observant scholar and imitator ; and yet his mind has swayed
other minds and inanimate inatter, ever since he applied the
knowledge which descended to him from the first inventor
of kettles, and was left by him as a growing fund to benefit
all engineers. The human inventor did not contrive a force ;
he found one, and so gained power which he use(l. There is,
in fact, no single mechanical principle in any liuman con-
trivance, which had not been applied to some natural engine,
long before the principle was "invented" and "patented" by
men.
Tlie first savage wlio boiled a root unwittingly used steam-
ENGINES. 265
power and burst boilers, in the food which he ate. A human
mind had swayed the movements of matter, and had set a
caloric engine to work when a man had purposely kindled a
fire. But the application of heat-power is far older. What-
ever the antiquity of men, and kettles, and fires kindled by men
to boil kettles, may be, boilmg springs, volcanoes, the world,
heat, and light, are older than men and their weak inventions.
The tool-marks of the old engines record part of their history
on rocks.
In striving to understand the records and the engines, the
best course is to seek after the powers employed, and set
them to work when found.
If the minds of men who only discovered a use for weight
and heat still sway the minds of engineers, and through them
and their engines sway the movements of inanimate matter, a
greater Mind can at least do as much with the universe and
the minds of its inhabitants. Earnest striving to solve pro-
blems in natural science leads to this belief We can neither
see all the face nor reach the works of our own little world, nor
can we hope to understand even that one wheel in the great
engine ; we cannot by searching find out its Maker ; but we
cannot do better than study his works. The more M'e see of
them, the plainer it must appear that such an engine had a
contriver who governs it.
In making geological toys to imitate parts of the engine
of nature, all natural mechanical forces yet discovered may be
employed upon all materials within reach, and all available
wits set to watch results and turn knowledge to practical use.
Millers have learned to use gravitation with water-weights,
in spite of river-floods ; engineers may learn to use the world's
heat, in spite of volcanic eruptions.
It has been done in Italy. If Icelanders would use hot
springs which have worked for centuries, they might have
winter-gardens and hothouses ; they might boil their mutton
for nothing and sell the soup ; they might at least warm their
houses and cow-l»yres, iri'igate their hay-fields, and wash in
the hot water which runs to waste at their doors. If miners
would but direct the natural underground heat-power wliich
moves air in deep mines, they might save human lives, and
the cost of power expended in ventilation. If we could learn
to store up and use the heat-power which lifts water above
ground, and so works all rivers and water-mills, there is
plenty of spare sun-power to work all the heat-machines on
the earth. Magnetism has been pressed and sent to sea as
pilot ; that giant may, perhaps, be set to harder work. Elec-
tricity is errand-boy and link-man, gilder and doctor, and
strong enough for any place. Light paints portraits, kindles
fires, and tells the shape and composition of distant worlds.
Light, too, may be harnessed and set to work in time.
Towards useful discovery the study of natural science
tends ; it can lead to no ill, for the further we go on this path
the nearer we get to truth. Natural science is not taught at
English schools, and so much the worse for those who studied
there. Some school of i>hilosophers taught that the world
stood upon the back of an elephant, and the elephant upon a
tortoise. It was la\\ful to learn this much, Ijut it was impious
to ask what the tortoise stood upon : no one knew that mys-
tery, and no one ought to seek to know it. Once it was
impious to assert that the earth went round the sun. But
now this reign of authority has ended. According to mo-
dern views, unstable ground may be cut from under the
feet of the tortoise, and the sun does not go round the
M-orld, human authority notwithstanding. We may now
seek trutli anywhere and cveiTwhcrc without offence; but
ENGINES. 267
Kiiglisli sclioJars must seek it for themselves if tliey choose
this path.
Natural philosophy is now open to all ; but hitherto it has
been little taught. Any child can and may make experiments.
Every successful eftbrt to find a cause is a fresh gain to all ;
the search for truth can lead to no ill if each step is made
upon solid facts. All paths lead two ways, and study may lead
to error ; but those who travel the wrong way ignore fticts or
misunderstand them. He who sets his cart to drag his horse,
mistaking effects for causes, may travel fast ; but he can never
rise. All inorganic forms which have been accounted for, re-
cord movements ; all movements which have been explained,
have causes. Any attempt to decipher these records and
discover movements, forces, and causes, ought to lead up
towards the great First Cause, whose mind and will contrived
and made the natural engine of the universe. Every fact and
Tmger-post, on every path tried, aims at this central truth, as
the compass aims at the Pole.
An attempt has been made thus far to rise gradually from
small engines and their marks to larger ones, from draughts if^^^^x^^ ^
in a room to trade winds, from raindrops and gutters to ocean- /^Z^ /c /C^;
currents and geological denudation. A further attempt will
be made to show the use of working-models in learning the
unwritten history of great events ; of things which are too
l)ig to be seen by little men ; of changes which occupy longer
time than human lives. The deposition of sedimentary strata,
and their upheaval, follow after the denudation which made
the chips. The way upwards lies downwards at first, for all
paths yet tried lead inwards, and aim at some underground
central force hidden there.
CHAPTER XLVI.
DEPOSITION 2— TIME 2 — TEMPERATURE — LIGHT — AIR —
WATER — WINDS — WAVES — FORM.
Time, — In chap. ix. an attempt was made to show that a rate
of denudation proves the ancient date of a recent series of
events in the geology of Iceland. A rate of deposition is
another measure of past time. If the surface of the world
has l^een gromid down and worn away so as to produce
certain sculptured forms, the chij)S nuist be somewhere, and
the ruljLish-heaps in proportion to the work done, and to the
time spent upon it. We judge of a carpenter by his chips ;
and so we estimate other work. It is manifest that a vast
number of trees have been sawn up at spots in Scandinavia,
because of the heaps of sawdust on shore and below the mills,
in the river and in the river-bed. An old mine is known by
large rubbish-heaps. An old furnace is known by large hills
of cinders. Ancient and long-continued human occupation
of tlie coast of Denmark, is proved by large heaps of oyster-
shells, gnawed bones, and such contents of " kitchen middens."
The evidence for time is equally good if the carpenter has
struck work, or the saw-mill has stopped, or the mine is
" knocked," or the furnace " blown out," or the men who ate
the oysters are eaten by worms.
So it is with sedimentary rocks. They are chips ; and,
from their thickness, it is plain that a great number of engines,
of some kind, have been hewing rocks for a very long time.
TIME. 269
and shooting the rubbish into the sea, to be carried and
packed. So deposition may equal denudation, but cannot
exceed it.
In most cases, the only attainable measure of denuda-
tion, and the only time-keeper, for past time, is the size
of these beds of rubbish. Eiver denudation in Iceland
is older than Icelandic history ; so is glacial denudation.
The discoverers named the land, and the 'ice' did not grow
there in a day. A rate of glacial action has not been found,
and it certainly varies. The machine is working full speed
in Greenland ; it has struck work in Britain ; and it is work-
ing half speed in Scandinavia. Taking the present rate in
Iceland as something like a medium rate for many ages,
the measure of the work done is the quantity of mud now
carried out of the groove in which ice works.
All old fisherman's test for clear water may be used when
a better guage is wanting. Fish will not take a fly in muddy
water, probably because they cannot see it from their haimts
at the bottom ; and the test for fishable water is : " AVade
ye in to yer knees, and when ye can count yer ten taes she'll
fush." In the sea off the west coast of Scotland, shells are
visible in many fathoms. In glacier-rivers in general, and in
large Icelandic rivers in particular, the fisherman's test shows
water as thick as the muddiest of Scotch rivers in the wildest
spate, or the water in London when Faraday dropped his card
on Father Thames, and found him filthy. Wade into the
Hvita up to the ankles, and the bare feet are wholly hidden
from the eyes by white mud. Most of the Icelandic rivers are
like it, and wont " fush " at aU. The Hvita is a broad, deep,
rapid, thick, gray stream, larger than the Thames, and all the
mud is ground by glaciers from igneous rocks. The quantity
of mud in a gallon, and the number of gallons which pass in a
270 FORM.
given time, would give a rough measure of the work oi" denu-
dation accomplished in this basin. If the beds of sediment
could be found and identified, they would equal the groove
made. Beds of rock-chips cannot be referred to the several
grooves whence they were taken ; but chips do not escape
from the world ; and because all sedimentary rocks are chips,
and denudation at the fastest known rate is slow, all history
must be as nothing to the geological time which is measured
by sedimentary rocks. Modern geology deals chiefly with
rubbish-heaps of this kind, with their transport and packing,
and with the order in which the layers are laid. Except in
the case of glacial drift, no attempt is made to trace stones to
parent rocks in position ; but deposition clearly results from
denudation, from transport of materials, sorting and packing ;
and all these operations occupy time.
Form results from movement, and movement from Force.
The forms of sedimentary beds record movements, and the
forces which caused them : and they are thermometers also,
lor they register temperature.
If the packing of a bed of silt records water-work, it also
records some temperature greater than the freezing-point of
water at the earth's surface. rebl)les and grains of sand,
which retain their shapes though cemented together, record
that a temperature less than the melting-point of the stone
has endured at the spot ever since the bed of silt fell through
unfrozen water. The nuiximum limit of temperature at a
particular spot is thus reconled for the Mdiole of the time
during which this particular form lias lasted.
The Forces which pack silt, by moving air and water, are
tlic .same which work denudation, and the engines and tools
TEMPERATURE — ENGINES — TOOL-MARKS. 271
are the same. Loose stones are carried, sorted, and packed
by rivers and land-ice, by ocean-currents and winds, by
waves, and by floats which are strong enough to carry such
weights. The fall of the sediment is a result of gravitation,
the rise of the water results from heat as it appears.
The forms are the tool-marks of these engines, and by
learning the marks, ancient work may be assigned to the
engine which did it, and to the mechanical force which
drives the engine.
In order to learn the marks, the engine may be watched,
or, when any part of it is out of reach, another part may be
watched, and the lesson so learned indirectly. We cannot
get to the surface of the air, but we can watch waves on the
surface of water, and study the barometer ; we cannot get to
the bottom of the sea, but we can watch the air-engine at
work upon snow and sand-drifts on shore, and study the
sea-beach at low tide. AVe can see the tools at work.
Waves. — When a fluid is moved by any force, the smooth
surface takes a form which indicates the direction of move-
ment : if solids are moved by the moving fluid, they too are
packed into corresponding shapes, which may endure to
record what happened at a particular time and place. In
order to recognise work done by an old wave, the thing to
study is an existing wave.
Waves on a stream. — A stream of water, or of any other
fluid, while flowing over an uneven bed, or in a narrow chan-
nel, curls over and forms waves. The water is dragged down-
wards, but it is also thrown upwards and from side to side by
reflection from impediments, and it moves in curves, which
produce wave-forms above, and wave-marks below.
By knowing these wave-forms anglers know where to seek
fish, and boatmen how to avoid stones. In deeper water
272 WAVKS.
similar forms betray reel's and sandbanks ; on diy ground silt-
forms record the passage of currents, and of departed waves,
even waves in the invisible air. In any bed of sedimentary
rock, similar forms record similar movements.
Fio. 92 Wavk-Fukms and Wave-Marks.
We are driven to assume that water, and other fluids, con-
sist of particles, and that they jostle and reboiind ; that the
shapes of waves upon running streams result from the direc-
tions in which force and resistance act upon these particles.
When fluid and solid particles, dry dust, sand, small shot,
and similar materials, are poured down a slope, wave-forms
and movements resemble each other in all the streams. In
sorting dust-shot, a stream is allowed to escape from under a
sluice, and the shot, in rolling down a board, moves like water
in a " lasher." A single ball or a big stone leaps down-hill in
curves, which agree with wave-curves on water-streams.
Waves which the wind drives along the surface of stagnant
water, also resemble curves described by solids. A ball
played on a billiard-table bounds, and rebounds ; jostles other
balls, and moves on the plane as waves do in a pond, or like
tidal waves reflected from continents. We may assume that
fluids consist of particles which also jostle and rebound.
If a marble is driven against one end of a row of marbles,
the driving force and the motion pass from ball to ball
through the series ; and the last ball moves till the force
which moved it is transferred elsewhere ; or, being changed,
disappears. If water consists of particles, then water and
LIGHT, 273
loose sand make a series, ami motion and force pass through
it to the last particle which records the movement when it
stops. Some force — sunlight, for example — moves air ; and
the wind stirs the sea, which stirs sand ; the last grains of
this series take the form of water-waves, on the sea-beach
and in deep water. The sand-form records movement in
water, air, and light, if light lie the force which started this
train.
Water-waves produce waves on sand. Waves in air also
produce like forms in dry dust. Waves of sound are copied
in dry sand spread on a sounding-board, and on water in a
musical glass. I*hotography and photometry record move-
ments in light, or movements caused by light, and philoso-
phers have come to believe that light is but an effect of sys-
tems of waves moving in some unknown fluid, as sound-
waves move in air. Eacli of these things — water, air, and the
fluid whose waves are light — is capable of moving other things.
The moving force which moved the first particles in the
series, of which the last retains the recording form, is the force
which did this work ; if light moves the air, light makes the
ripple-mark on the beach. Are we to stop there ?
In the row of marbles a hand and a human will were in
the series, and the will moved the last marble. In silt-beds
and old stratified rocks, the cham of cause and effect may
seem endless ; but the ultimate cause of the ripple-mark must
be will also, unless there is movement without a cause
somewhere short of the will. Unless there is a will at the
end of the train of machinery, sand, or the sea, or the wind,
or the light of the sun, or some other inanimate thing, moves
without a cause ; which is contrary to experience, and there-
fore cannot be assumed in any train of reasoning. We never
find marbles and billiard-balls, shot and shell, moving with-
VOL. n. T
'^^g^
(^yii .a^/fer~(i^^^^^^^^->5
274 NATUHAL SCIENCE.
out a cause, and most of their movements can be traced back
to lunnan will : why should larger or smaller particles,
worlds, or atoms, move without a cause, more than these ?
Forms which residt from denudation and from deposition
are as figures on a dial-plate which record movements ; from
them the moving force may be sought tlu'ough the works :
the further men can reach the better, if they pause to think
of Him who said. Let there be light, and feel that they are
looking at the works of their Maker, when they study natural
science, and the tool-marks of His engines.
I' . ^
CHAPTER XLVIT.
DEPOSITION 3 — WINDS 2 — WAVES 2 — WAYE-MAKKS.
Because the works of nature are too large for human inspec-
tion, working-models of them help comprehension. Imme-
diate causes are learned by watching the rapid growth of
form. The wind is invisible, but smoke and waves are not ;
and through their visible forms and movements, invisible
movements and forms may be seen.
When wind blows along the calm surface of still water it
does not move in straight lines, horizontally ; it strikes down-
wards, and rolls along, driving the water-surface before it.
On a windy day, where a mountaineer has fired a moor, the
white stream of smoke flying over the brown heath rolls as it
flies. It rolls, and breaks, and surges over the plain, as the
wind does. It flows down hill into a valley, and rolls up the
opposite slope ; and where the smoke strikes visibly, the
brown heath bends before the invisible wind. When some
farmer is burning weeds near a hay-field, the waves on the
sea of green fit into the curves of the smoke-cloud, and the
smoke betrays the immediate cause of the movement, though
it is invisible. Air does not flow in flat sheets or straight
streams, but rolls as water does in a river. Because the river
rolls, sand is packed into the shapes of waves, on water, heath,
and grass, which are driven by rolling streams of air.
When a breeze begins to stir the glassy surface of a lake,
floats move slowly along, while tiny waves and floats rise and
27G DEPOSITION.
fall, advance and slide liaek, as tliey are pushed by the wind,
and pidled down by weight. The surface " ripjiles," and
moves as far as the force can drive it. The far end of a
canal grows deeper when the wmd blows along it. Large
lakes rise to leeward ; high tides coincide with strong gales
at sea. Water is driven by the Avind, and the shape of a
wave suggests that it is moving water driven up over water
at rest, and falling back when the force has done all it can to
pu.sh it over and make a breaker of a rijller.
The force which moved the air is transferred to the water,
and from particle to particle ; and thus a " curl on the water"
grows ; bigger waves grow, and some large ones even move
faster than the wind, and so foretell approaching storms.
The force which is thus transmitted is also reflected, bent
aside, accumulated, dispersed, accelerated, and retarded. So
the forms of waves, and their movements, are complicated
and hard to comprehend.
Horizontal movements. — Waves, moving upon the surface,
are not straight continuous ridges, crossing the path of the
wind ; but short curved ridges, moving and spreading in
many directions. Waves on any puddle are like sea-waves
in this respect.
Barnespool at Eton is a sheltered pool, wallod round, and
spanned by a bridge. When the wind blows strongly from
the west, curved systems of small waves are driven in under
the bridge ; they strike against the walls, and curl round the
jjiers, and they rebound from side to side. The force which
moves the wind is transferred to water, transmitted through
a series of water-particles, bent aside in passing the pier,
reflected from the walls, and finally recorded iipon a mina-
ture beach. These small systems are very complicated, and
as hard to comprehend as larger wave-systems, but they are
WAVES — WAVE-MARKS. 277
lietter seen, because the whole pool can he seen at once. The
waves can be watched from the bridge, bending, crossing, and
re-crossing ; meeting, passing, rebounding from the walls, and
gradually fading away into a calm at the sheltered end of the
stagnant pool. Barnespool was the sole teacher of this science
at Eton.
It is easy to draw and map out these wave-.sy stems, and
to apply the knowledge to larger systems of waves. It is
easy to see how invisible particles of water move, by watch-
ing the movements of solid floats. There is no general move-
ment in the water, but there is a slow drift on the surface.
Apples, orange-peel, bits of ice, and other things which float
deep, advance slowly towards the calm, but they do not move
steadily, or in straight paths. They move as the water does,
up and down, forwards and backwards, descriljing curved
paths, like waltzers or tumblers, wlio whirl and roll while they
advance. The whole of these movements clearly result from
the force which moved the wind, and that is sunlight, according
to modern science. The beach at the end is the tool-mark of
the engine thiven l)y some mechanical force. It is a photo-
graph.
What is true of this puddle is true of larger ponds.
The Scrpentmc, in London, is a larger sheet of water
spanned by a larger bridge, under which waves pass. Waves
at the far end cannot be seen from the bridge, but they can
be followed and watched. The systems move fastest in the
middle ; they are retarded by the sides, and so form loops, as
they do under every arch. At the end, the loops beat upon
a concave dam, and the waves are reflected ; they return and
meet at a focus, where the force which drove them is accumu-
lated. The waves leap highest in the focus of the wall, and
there they disperse, and set olf again, mo\ing back against
278 DEPOSITION.
the wind which drove them forward. At the sides of the
eaual, two systems of breakers cross each other diagonally.
One is the side of the loop which is moving forwards, the
other is the side of the reflected loop which is moving back-
wards. Orange-peel and water-logged apples leap and rock
to and fro, advance and retire, as water-particles must do ;
and ducks in search of food paddle about under the wall,
and use their experience of reflected force to avoid shipwreck.
Force, from which all these complicated movements result,
is still the same ; and the shape of the gravel beach, and piles
of drifted rubbish upon it, record the movement and the force.
The same thing is to be seen wherever there is a beach.
At Weymouth, the waves of a large bay dash against a
concave sea-wall, and rebound. Systems of large size may
be seen advancing from the horizon, and retreating from the
wall ; crossing and recrossing, and meeting in the focus, as
truly as invisible waves of sound and light meet in the focus
of a reflector. The waves driven by an accumulation of
force leap up to form cones and pyramids, and jets of spray ;
and the sea boils.
From the toj) of Portland Island, which makes one horn
of this bay, still larger Atlantic waves are seen moving
rapidly up channel. They are retarded by the ebb, are accele-
rated by the flood ; they are turned aside in passing the Bill
of Portland, curl round into the shelter, and roll into the
bay. They are reflected from the beach; the force is accumu-
lated in the focus, dispersed beyond it ; ships at anchor and
water-logged buoys rock in the sea ; and one side of the Chesil
Bank records these movements, and the amount of deflected
force expended in building this beach behind Portland.
The whole is but an enlarged edition of Barnespool, more
dillicult to see and harder to comprehend, because larger. A
WAVES — WAVE-MAKKS.
279
whole system is seen horn the bridge at Etou ; teu minutes
will carry an observer from one end of the Serpentine to the
other ; but from Weymouth to the Bill of Portland is a day's
march, and the wide Atlantic is beyond.
On Isle de Ehc, near Eochelle, on the coast of France,
stands a tall lighthouse, called Tour de Balene. It stands
upon a sandy point, with well-marked sea-beaches. Outside
the point is a long flat slioal, at tlie end of which stands a
second lighthouse on a ruck which is covered at higli tide.
Big waves rolling in from the Bay of Biscay and the Atlantic
hit upon the end of this shoal. They are most retarded where
the water is shallowest ; and so the long curved ridges become
loops, bend and curl inwards. They do no more than smaller
waves do on points in Barnespool ; but from their greater
size these cross-rollers are very remarkable, and do very re-
280 DErOSITIOX.
markable work. One moving system thus bent on a shoal
beyond the limits of vision appears to be two systems moving
diagonally upon opposite sides of the shoal, the point, and
the lighthouse upon it. The long rollers break and form a
moving netw^ork, whose knots are tall crested " white horses"
advancing directly upon the end of the spit ; while the
meshes are green rollers, crossing each other at right angles,
and breaking heavily on opposite sides of the point.
The bent sea-waves converge and meet at their focus
below the lighthouse, as rays of refracted sunlight converge
and meet in the focus of the lens above. The form of the
sand-spit records this movement, as the Chesil Bank, and
miniature banks in the Serpentine and in Barnespool,
record the movements of smaller waves there. But in this
case the pool is too large to be seen, and harder to under-
stand for that reason.
Tides are but larger waves harder to comprehend, and
driven by a different variety of force. If ordinary sea-waves
result from the radiating force which moves the winds, these
appear to result from the converging force of gravitation,
which drags water towards centres, outside of the circles which
bound the sea. Tide-waves rise under the sim and moon, and
follow them westward ; but they too reboimd, and their vast
and complicated movements have not been fully unravelled.
Wliere tides have been mapped and so brought within
reach of human vision, the movements of tidal waves appear
to agree with those of conmion waves, which are impeded in
wandering over the surface of smaller pools.
It is not necessary to study uncontrollable tides or Atlantic
waves ; a knowledge of this part of the engine may be fished
out of every puddle. The advance of the tidal wave in the
Bay of Fnndy, where tlie rise is from 40 to 75 feet, though it
WAVES — WAVE-MARKS. 281
is one of the grandest sights in nature, is hut a large copy of
the flux and reflux of hroken waves in any creek, or on any
sandy heach.
When something of the movement of waves has been
learned, marks made by waves on sand and gi-avel beaches
are comprehensible ; and similar marks, wherever found, can
be referred to their immediate cause, and their meaning so far
interpreted. Till the movements of waves are studied, their
marks mean nothing, because their language is a foreign speech.
At p. 340, vol. i., a lesson taught by the ebb-tide is set
dowTi as it was learned on a Highland strand ; it is good for
all strands, new and old, if only they retain the tool-marks of
Deposition by waves.
Old ripple-marhs on the millstone grits of Yorkshire, in
quarries near Pately Bridge, are still as perfect as they are on
a strand from which the ebb has just retired. "VMien a new
surface in the quarry is laid bare, ripple-marks are the same
in shape, size, colour, and material, as ripple-marks in the sea.
Tracks of creatures which wriggled, and crawled, and hopped,
and walked about on the wet sand ages ago, are as fresh upon
the stone as similar tracks made within the hour. It was
recorded upon one slab that water had moved first towards
the north-east, and then towards the south-east, or that two
systems of waves had crossed. The surface so marked by
moving water was left dry, marked by moving creatures, and
dimpled by falling drops of rain or by rising bubbles of some
gas. This surface now is solid rock ; thousands like it lie
over it and under it, like pages in a book ; many thick beds
of sandstone are piled like volumes stacked in the corner of a
room. The system stands low in the series of geological
records, but far above the floor. The beds in these quarries
have been shattered, broken, distorted, disturbed, upheaved,
282 DEPOSITION.
criinipled ; big angular rents, fissures, and fractures, are there
as plainly seen as fractures made with gunpowder and sledge-
hammers. Some of the rifts have been filled, and in some of
these are valuable metals, which are worked. Since the veins
were formed, the sides of the crack liave moved, for there are
slickensides in the veins ; they have moved in various direc-
tions, for marks on the smooth surface cross each other where
they have rubbed. Since all these movements took place,
the broken edges of the broken beds have been ground away
and rounded off — " denuded" into the shape of the Yorkshire
hills and dales.
But in spite of all these and many other changes, and of
all the time which has elapsed, the tool-mark of a tiny water-
wave, and the spoor of living creatures, record certain facts in
language too plain to be gainsaid or misunderstood.
Low down in the geological pile of stone books, on a spot
in a crumpled torn page of millstone grit, it is recorded that
long ago there was deposit and packing of silt in fluid water,
which moved as water now moves on the nearest sandbank in
the Huniber ; that plants grew, that living creatures crawled,
and that rain fell from the air. There is no human standard
measure for such denudation and deposition, or fur such time
as tliis ; but tlie Ibriu registers the working of tlie old engine,
which still works.
7Vie climate of Yorkshire is also recorded \\itliin certain
limits. The water was not frozen ; it was not steam, nor was
it too hot for animal and vegetable life. The coal vegetation
which succeeded resembles tropical vegetation of the jiresent
day. It is probable that the climate was warm. Sometimes
an inorganic shape is laid bare in the Yorkshire quarries,
which has no counterpart on cold misty northern shores, and
these shapes tell their story more certainly than fossils. Jl
WAVES — WAVE-MARKS. 283
is only probable that a plant like a palm-tree had a similar
nature ; it is not certain. It was probable that an extinct
elephant lived where the climate was hot ; but it has been
proved by the discovery of woolly hair beside manmioth's
bones, and on tlie skin of a mammoth, which fell out of
frozen ground about Behring's Straits, that the fossil elephants
which lived about the "glacial period" were provided with
natural coverings to resist the cold which prevailed in Eng-
land when English mammoths lived.
The trees of the coal-formation may have flourished in
colder climates, though they are like the tropical vegetation
which now feeds elephants. Xo experiment can test con-
clusions drawn fi-om the shape of a fossil shell, and from the
habits of li\'ing things ; but inorganic forms record facts which
seem never to vary. Frozen mud, mud packed by waves, and
sim-baked mud of the present day, must, so far as we know,
be like mud baked, washed, or frozen, at the time when the
first bed of silt was formed.
Beside, and mingled with ripple-marks, certain inorganic
foims are occasionally laid bare in quarries near Pately Bridge,
which seem to mean baking rather than freezing : a wanu
climate in the place where millstone gTits are found. One
seemed to be a form moulded in sand, partly by air. Dry-
looking white sand, apparently blown by the wind, is scarcely
boimd together, and rests loosely where it fell upon a strange,
brown, rounded form, whose section shows minute bedding.
It seems as if a bank of sand and mud beside a runlet had
been well baked till it cracked, that the edges were rounded
off by tides or floods till a definite form, a tool-mark of
deposition and denudation, was moulded in sand. Then
came a sheet of bro\\Ti mud or a green coat of vegetation,
now reduced to a colour, and over this the drv white sand
284 DEPOSITION.
appears to have diiftcd. Then came a deluge of clean gray
sand, which buried the whole, hid it and preserved it till it
was quarried by Yorkshiremen in search of paving-stones.
The whole document must be read together before the record
is understood.
Itipple-marks are familiar to geologists, but other in-
organic fossil forms have not been luucli noticed, though they
are equally worthy of attention as records. Eipple-niarks
aboimd in sedimentary rocks of all ages. In the old rocks of
Orkney are ripple-marked slates. In the oldest of Welsh
slates, where no trace of life has yet been found, ripples are
perfect. In these old, unaltered, sedimentary beds, which
have been tilted, shattered, baked, and crumpled, the hard
1)lue surface of a flag when newly bared is often ri}»pled as
plainly as the nearest nmd-bank. But in older Canadian
beds which have been more altered, even these marks are
obliterated.
Where the form exists it tells its own tale ; it tells that
the fusing point of the rock has not been reached at the place
since the mark was made ; that the freezing point of the
fluid which packed the sand or mud was not readied wlien
the waves moved. But when the form has been obliterated
at one part of an altered bed, though preserved elsewhere, it
proves that some other force has been at work since the sedi-
luent was packed by waves.
The alphabet of form is to be learned from engines work-
ing on the surface of the globe ; l)ut inscrijttions to be; read
are stored lielow, and some of tln'm are harder to read than
ripple-marks, because they were A\rittcn luiderground.
CHAPTER XLVTIL
DEPOSITION 4 — WINDS 3 — WAVES 3— BEACHES.
The most characteristic wave-mark is a beach. It is a form
like that of waves which beat upon it, one which can only be
understood by watching waves, A more beautiful thing than
a big wave is not to be found in nature. Many a pleasant
dreamy hour has the writer of these pages spent in watching
Atlantic rollers sweeping on from the blue distance to thun-
der in against the Scottish coast. A green glassy ridge comes
rapidly on, glittering in the sunlight ; heaving, growing, swell-
ing, and mounting up, as it comes nearer and nearer ; growing
steeper and steeper as it reaches shallower water. The top
is ever pushing on over the base ; the base is constantly held
by the sea-bottom, and pushed back by the undertow. The
steep ridge of water becomes a wall, and the wall a hollow
curve like a sea-shell, and then the moving hill rolls over
its base, and tons of water fall headlong down with a crash.
The broken water rushes on like a rising tide of white foam,
and leaps up in sparkling fountains of spray, and the flood
drives all that will move up hill till the force is spent. The
falling tide of the undertow rushes back with the force of a
mountain-torrent as broad as the shore is long. Every stone
is moved ; the beach is constantly worn by waterfalls equal to
the height and weight of the wave, and by torrents equal to
the depth and breadth of the undertow. Between high and
low water mark the beach takes the form of a solid wave, be-
286
DEPOSITIOX.
cause pebbles are packed by water-particles Avliicli ti'anst'er the
force wliich moved tlieni to sand and stones. The beacli
driven by water has a curve like the back of a wave driven
by the wind, and each ridge of loose stone leans against a
rock, or rests on the back of the ridge before it. The woodcut is
from a portrait of a heavy rolling Cornish wave which came
from the west, curled round the Land's End, and was returning
westwards, rushing furiously to land against a strong wind, in
a narrow bay with a sandy bottom and a pebbly beach. The
curling head was hurryfng over the base to reach the English
shore, and a silver plume of spray streamed back like a mer-
nuiid's hair, or a horseman's crest.
On the far side of the creek the retarded wave was seen
lagging and breaking before its time on a pile of loose ang-ular
stones, the broken chips of a fallen cliff; and these, as the
WAVES — BEACHES. 287
water burst amongst tlieiii, and roared over tlieni, stirretl and
rolled, and rattled and groaned, and ground themselves to
powder. When the larger tidal wave eblDed, and these
Atlantic waves were driven back, a dry beach remained. It
was the track of the invader who will some day swee^i Eng-
land from the face of the earth, unless some underground ally
lifts her cliffs out of reach of the sea.
This beach was a steep bank of boulders and pebbles, with
a broad slope of gravel and fine sand at the base. The
larger stones were below, driven as far a^the wave could
drive them ; smaller stones were above, tossed up by the recoil
of the blow ; the gravel was at the top of the slope, dragged
there by the undertow ; the sand was lowest and furthest out,
where the force of the downward stream was nearly spent, or
balanced by the advancing wave ; ripple-marks, stream -marks,
and the rest of the smaller tool-marks of deposition by waves,
were on the sand.
A solid wave of sorted stones rested upon the rock where
it broke, and the shape of it was like that of the wave which
was driven by some invisible force. The force which shaped
the beach was that which moved air and water, and the in-
visible wave of force may be like the fluid wave and the beach.
One result of this action is the fonnation of new land.
The sea builds dams, and rain-water fills up the space behind
them with silt. Behind the Chesil Beach, near Portland, a
lake is formed, and rivers are filling it with mud. Near the
Start Point is a similar lake divided from the sea by a broad
wave of boulders. The lake is below an ancient sea-cliff, and
is rapidly filling with mud and reeds ; it is full of fresh-water
fish. At Borth and Traeth Mawr in Wales, are similar beaches.
At the head of BreidfjorS in Iceland are larger beaches of
lava boulders, behind which are pools of sea-water, and fresh-
288
DErosiTiox.
water ponds ; and rivt-rs still How tlirougli oin-nings in this
lava-dam raised by the sea at the far end of a bay.
Near Snoefell is the most remarkable beacli of all. It is
a great black natural mound running across a valley, so as to
dam back the drainage waters, and hold in the ebbing tide.
The crest of the ridge is composed of smooth egg-shaped blocks,
larger than a man's head, tossed about in the wildest confu-
sion at the top, and more neatly packed at the base. The
Sffta// fxfint
Barda Strand
Syssta.
Scahorizon.
Beach.
Shattered rock
Black sand a
-I ,^J-^;^-=i- s/le//s.
Fio. 05. BoLANDS HOFVDI. August 16, 18G'2.
A nlifr of ('{iluniiiav lava, interstratified with ashes, and resting on coarse Iiard breccia of
rolled jiebbles. The talus beneath the cliff is chiefly sand ; it makes an angle of Si"
with the horizon, and is the only pass along this shore.
seaward slope lower down is fine black sand, strewed with
brilliant shells, like those whicli are found in bouldtT-clay.
The back of the mound has a different steeper curve and slope.
The whole is as near the shape of breaking rollers which fall
ui)()ii it as the materials of which it is compos(Hl will admit.
Small stones have been thi'own over the mound like
s])ray, and rest where they fell. Tt is a solid roller, Avliich
WXYES — BEACHES. 289
has not reached the sliorc. The shore of the inland lake is
strewed with pumice, and suchlike volcanic materials, and
is haunted by flocks of l)irds. The whole structure rests upon
a foundation of igneous rock, and is the work of fire arranged
by water. If this beach were found any^vhere ; — in a quarry,
or on a hill-side, it would tell of waves as large as those which
fall upon it : ocean-waves, which may roll without a break
from the South Pole to the beach at Sniiefell.
The district of 3I]/ra Syssla in Iceland seems to be land
formed in this way. Beneath high broken precipices, which
look like sea-clifls, a wide tract of boggy flat land slopes to-
wards the sea. It is traversed by ridges of gravel, which
have the form of dilapidated beaches, and between these the
whole country is a quaking bog, through which occasional
rocks appear. But these old beaches are far higher above the
sea than modern beaches, and they are not horizontal. They
prove that the whole land has risen unevenly. They mark a
late change ; and if similar changes took place in early times,
they too should be recorded somewhere amongst the old beds.
At Malar in the north, at the end of a deep fjord, where
big rollers cannot now come, are similiar raised beaches, with
small moors and bogs resting in hollows amongst the boulders.
In Scandinavia are many similar marks ; and they are found
high up on the Himalayas.
At the head of the large Newfoundland bays, which face
the Atlantic — Conception, Trinity, Bonavista, etc. — beaches of
this pattern form ramparts along the whole shore. Some are
bars imder water, others run from point to point like moles
or breakwaters ; fishing craft anchor behind them, riv'ers form
lirackish pools on the land side, and silt-beds gather in the
still pools. Icebergs drift about in deeper water outside, and
there drop stones carried from C!rcenland. Higher up are
u
290 DEPOSITION.
terraces of larger glaciated Newfoundland and foreign stones,
confusedly mixed with sand, rolled pebbles, and beach-stones.
These in their tmii rest upon glaciated rocks, which have
risen, and are still rising. In winter, bay-ice packs old chips
along the shore. In spring, rivers dig materials from old
terraces to build new deltas behind new sea-beaches. The
bays are like Myra Syssla, the Miry Shire of Iceland, but in
Newfoundland the sea-bottom has not emerged, though it is
rising ; and the low ridges are now parallel to the sea.
Surely these beaches may help to explain the osar aud
kames of the glacial period.
In North America raised beaches abound. They were
first described by Hitchcock, and they are conspicuous on the
White Mountains, Green INIountains, and elsewhere, at great
elevations. They appear to be sea-beaches, formed like those
now forming in the bays of Newfoundland, and ebbed dry in
glens which were bays in the glacial period. Those whicli
were most exi)osed (the highest) are, like the beach at Sna-fell
in Tcoland — confused stone-heajis tossed al)0ut and irregular in
sha[)e. Those which were sheltered by rising points are like
those now forming in the bays of Newfoundland. At the
head of one glen, at Gorham in the White ]\Iountains, a
laminated terrace of fine sand and mud, disposed horizontally,
appears to be a delta formed in still water at the end of a
bay. The formation is about fifty feet thick, and from its
position may be a fresh-water deposit ibrmed in a lake which
burst outwards through a distant terrace, and left the glen
for the railway to occupy. Upon this delta, if such it proves
to be, large glaciated boulders are piled.
The translation of the whole record nuule on (he spot in
1864 is, that ocean-currents, icebergs, and l)ay-ice, drifted
along the course now followed by the Grand Tiunk Itailway,
AVAYES — BEACHES. 291
aud dropped foreign boulders in still bays and straits, which
are now glens and passes amongst the highest of the AUe-
ghauies. The American author who followed Chambers
thought he saw raised beaches in Wales ; and sea-shells have
been found there at 3000 feet. He also thought that he saw
the spoor of the sea in Switzerland at similar heights. Till
sea-shells are found there, and in the White Mountains, there
is room for argument ; but there is little doubt that these so-
called raised sea-beaches are marks of waves in w^ater, in
air, and, it may be, in light.
A ripple-mark is then a copy of a ripple ; a beach copies a
larger wave, and both are marks of deposition, and tool-marks.
This mark is a thermometer like the rest, and it is also a
water-gauge.
The beach is formed at the water-margin. If land rises,
or water sinks, the beach is left high and dr}"-. If land rises
"straight away" from the earth's centre, if one spoke of the
wheel grows longer, the old beach-mark is level there. It is
like a storm-beach ; a higher mark parallel to the lower
beach, and to the sea ; a curve on a higher sphere, further
from the centre. If land rises unequally ; if it bends upwards
like a bubble, or tilts up like the lid of a box, the beach-
mark records that change ; for it was made horizontal.
If the whole sea has sunk down ; if the sea-level is nearer
to the earth's centre and the land where it was, the old Ijeach-
mark must record that fact also : it must be found at the
same level in all parts of the world if the whole sea-level
went down at once.
If the land has risen at one place and sunk at another ;
if it has grown up like a dome, and sunk like a bowl else-
where, the beach-mark records the fact by its distance above
the sea which has a regular curve everywhere.
293 T^EPOSITION.
In reading this larger record, the denuding action of
waves must be considered. On coasts above mentioned no
beaches are formed at exposed points. The rocks are bare ;
but they are broken or sawn, or otherwise worn and marked
between wind and water. Some are drilled, pierced, or blown
up, so as to form pot-holes, caves, and arches ; others are
cliffs, and under some of these are fallen talus-heaps.
It is a question of temperature and tides, rise and fall of
level, whether waves demolish rock, or pack chips at the
w^ater-margin. So if the real beach is found anywhere, a
worn shelf at the same level is not far distant. One is at
the point if the other is in the bay. Woodcuts at page
357, vol. i., are meant to illustrate this fact ; which the author
of "Ancient Sea-Margins in the British Isles" pointed out
long ago. Applied by him to Scandinavian records, the rule
proved that Finmark rose like a bow. If sea-margins were
traced round the world, they might perhaps prove that the
land has waves like the sea.
The changing form of a breaking wave is hard to copy,
its movements puzzle mathematicians ; but these facts appear
to be right so far as they go. The form of a wave drawn by
light may be compared with other fixed forms ; and photo-
graphs of breaking waves, made and bought for the purpose,
have led to these conclusions. The woodcut, p. 2G1, is from
a photograph. With it compare the portraits of snow-waves
(pp. 293, 298), the cuts on pp. 272, 28G, 299. Compare these
with the portraits of clouds, vol. i. p. 33 ; of trees bent by the
wind, pp. 31, 50. Compare the cuts in chaps, v., vi., vii., viii.,
which illustrate movements in air and water, with real waves,
snow-drifts, and beaches ; and these forms will seem to be
copies of movements and records of fence, the spoor of the
sea and the Avind, and natural photographs. The force
WA^T:S — BEACHES.
293
which makes a collection of tluid particles move, and take a
certain form for a time, when transferred to solid particles
makes them move in the saiue way, and take like forms, which
endure. In fluids the form cannot last ; in solids it may.
In the photograph reflected light so acted as to pack solids
in certain forms ; the water-wave was copied in silver by
light-waves, and it has the shape of the beach.
The wave and the beach, like the photograph, may result
from waves in light.
Thus form appears to record that light acted as force,
directly or indirectly, through other materials, — as Ray-
force, which is only perceived where it has accumulated at
the end of a long train.
The cut below is a copy of a natural snow-photograph of
an air-wave made this year.
*
li>. :"'. A snmw-Wave in- Cheshire.
Sketched from nature, January 28, 1865, after a strong breeze of wind.
Horizontal distance from the edge of the snow-breaker to the wall on which
hedge grew, two feet eight inches.
CHAPTEIt XLJX.
DEPOSITION 5 — WINDS 4 — WAVES 4— STREAIM-MARKS.
Taking form to be a record of force, and the force ^\•llicll
makes a ripple-mark and a beach to be Rays, acting through
a chain in Avhich air and water are links only, then similar
marks ought to be found at all links ; for instance, where water
has played no part in packing the chips of denudation.
If water-waves are mriwd liy light acting througli air,
then there must 1k' waves in tlie air, and they too must leave
their mark, if they move solid particles. ]Nfoving ciuTents of
air do in fact produce well-marked forms directly in solid
materials, and these may be compared with thiid wave-forms
and tlu'ir M'ork ; M'itli ri]>ple-marks and sea-l)eaclies, new and
old.
Kijiple-marks and wave-marks iipon a beach only sliow the
last direction in which some force acted ; and marks of tlie very
same pattern are formed upon snow, dust, dry sand, clouds, etc.,
by air. They are also formed by boiling water in hot springs,
and in steam-boilers. Old ripple-marks and wave-marks need
not be the work of a sea like the sea (•!' our times. Tliey only
prove that the marks were made upon beds of solid ])articles by
some licpiid or gas ; and tliat tlie temperature then was some-
where between two extremes — the melting point of the packed
solid, and the freezing point of the fluid which packed it.
Tliese marks do not record that tlmy were made upon .sra-
margins, for they are made by currents of aii' moving at the
M'AVES — i\IAl{KS. 295
hottom of the air-oceau, and they are made at the sea-bottom
as far down as we can see, or feel with a plmnmet. On the
very- top of Eyriks JokuU in Iceland (see vol. i. p. 429),
where the temperature can rarely exceed the freezing point
of water, the snow was found to be beautifully rip])le-
marked by the wind at a height of 6000 feet or more.
The marks proved that the temperature had not exceeded
the melting point of snow since the particles of snow were
arranged, so water was not the fluid which made the mark ;
but the temperature may have fallen to any point be-
tween 32° and the freezing point of air (if it has one), and if
air made tlie mark ; or it might have been made by any other
fluid or gas, if there were a doubt about the composition of
the atmosphere at the top of the hill.
On a lower hill-top in the Faro Islands, in July 1862, at
places where snow had lately melted, bare gravel Mas arranged
in regular ridges and furrows ; sometimes running up and
down hills, but always running nearly north and south, and
always at places fidly ex^Josed to the west wind.
The largest stones were in the hollows, the finest upon tlie
top of the ridges, which is also the case on sea-l)eaches. The
stones were about the size of apples, walnuts, hazel-nut.s, peas,
and small shot. The ridges were about a foot apart, and at
one place the hill-side looked like a ploughed field some
forty yards square. The apparent cause was the flowing of
small streams from melting snowdrifts. But the same form
recurred where that explanation would not suffice — for
example, on level places ; and it never occurred at places
.sheltered from the west wind, even where melting snow-
drifts were on slopes above beds of gravel.
These were tracks of the invisible wind, large ripple-
marks made by air-waves in deep air, on beds of gravel
29G DKI'O^^ITIOX.
loosL'iiL'd liy frosts, and drivt'ii liy i urreiits nioviny i-ashvards
at till' lH,11,,in (.rtlic alin()si)liriv.
Similar forms occur in similar materials, in many parts of
Iceland at lower levels, at Ilelgafell and elsewhere. So the
air has waves for a depth ecpial to the height of the tallest
hill in Iceland, and the sea may have them at the greatest
depth in the ocean. Such marks are common on Scotch
hills, and further south ; and any one who has walked over
a bare hill-top or on the sea-shore in a heavy gale, may have
seen and felt gra\el rolling and Hying before the wind.
This is a mark which a geologist M'ould be apt to attriliute
to water, if he found it in an old rock ; yet water has nothing
to do with it. It simply means that some force moved
gravel from west to oast, and that the temperature has not
been hot enongh to melt gravel since it was so packed. The
form is but a copy of a wave, and in this case it is a copy of
an air-wa^X! at the bottom of the air.
At the Geyser, where water flows from the spring at a
heat of 212° or thereabouts, the stone which it deposits as it
cools is l)eautifully ri])ple-marked in tiny waves, which cross
the direction of the moving stream.
In steam-boilers the earthy material which is deposited
from boilmg water has a ri]iple-marked surface, which shows
the direction of the prevailing movement within the boiler.
A ripple-mark upon a lied of silt, old oi' new, only jiroves
that some force caused motion in some Huid, and in a parti-
cular direction, and that the material moved has not been
greatly alt('red since that time.
The engine set to do the; work inay have been made
of any gas or Huid, at any temperature above its freezing
point ; it may have been air far below zero, or high-pressure
steam ; but the maximum temperature, within certain limits
WAVES — ^[AUKS. 297
of time, at any spot is fixed by a riiiple-niark on any material,
at some point below fusion in the substance marked.
The lowest ripple-mark iu the geological series proves
that the rock upon which it is found is a rubbish-heap, and
that the fusing point of that rock has never been passed
at that place since the rubbish was chipped off and packed.
It does not prove that climate was the same as now at
the surface, or under the sea, which rippled over Laurentian
sand.
Air, the last link in the shorter chain, makes other marks
in packing solids. In England, where snow is the exception,
great snow-waves, solid white rollers, and stationary breakers,
may often be seen after a strong gale. Entangled half-melted
snow-crystals driven by the wind may be likened to silt
moved by water-streams, and the surface of the snow-bed to a
sandbank below the sea. But snow-crystals stick together
more than sand ; and drifted snow-heaps resemble water-waves
more closely than sea-beaches. Snowdrifts are air-marks on
solid water, dust-copies of air-waves. When a strong gale
blows, drifting snow takes the shape of the currents wdiich
move it. Drifts gather to windward and to leeward of anything
which rises above the surface, and so drifts change the direc-
tion of the wind. The wind splits upon a post ; so a point of
snow of a particular shape forms to windward of the post, and
another heap of a different form gathers to leeward in the
shelter.
A heap of snow changes the direction of the wind and
affords shelter; so waves and ridges of snow cross the direction
of the gale, and these roll slowly on piecemeal, taking the form
of rolling waves of air. When a wall or a hedge stops a drift,
the wind whirls the snow over the top, and into the shelter,
and makes a snow model of the curved path.
298 DErOSITION.
It is a copy of a breaker, a suow-beacli arranged by a sea
of air.
In liigli mountains, these snow-waves are often of gigantic
size. They are snow-beaches, the drifts of many winters, and the
work of prevailing winds, which have blown for ages at odd
times, so they are not regular in form ; but in the High Alps,
and in Iceland, snow-beds may be seen curling over high
cliffs, like the crest of a vast roller in act to fall upon a beach.
When snow is drifting, the whirling movement of the air
which models the curved form of the drift is apparent in
the movements of snow-llakes driven over the hills. Of such
Fig. 07. Section of .\ Snow-Beach.
drifts excellent copies are commonly made by the hoJp of
light. But an English snow-drift is as good an illustration
of the principle as the largest snow-heap in the world.
What is true of snow is true of dry sand. The material
will not retain form so well as snow, but the movcnu-nts are
the same, and dry sand records tluin iiniicrrcctl}-.
Sand in water retains form wor.si; tlian it docs in air, lur
it is easier moved in tlic thiid wliicli paitially lloats it ; but
the arrangement of sand by ^^■ind upon dry ground explains
the packing of silt in water where it cannot be reached. It
is ocean-work, but work done by waves in the deep air.
On the sandy plains of Iceland these sand-drifts are
AVAYES— MARKS.
>99
well seen. Loug points and ridges fovni tu windward and to
leeward of every stone post and plant. Large ripple-marked
sand-waves roll over the plain, and stop in every shelter.
The air is filled witli clouds of moving sand, which fly from
drift to drift, and from hill to hill, like spin-drift from the
waves of the sea. Clouds of fine ashes rise up, and float
along hill-sides like mist, and dust gets everywhere. In
the shelter, drifts assume the angle at which dry sand can
rest in still air. To windward is a sloping hill, to leeward a
sand-talus, whose angle is about 32°. But when sand is
wetted, and acquires more cohesion, it copies the form of the
breaking sea-wave more nearly.
Near a pool of water, damp sand forms a perpendicular or
overhanging wall on the sheltered side, and a slope where the
bank is exj)Osed.
Fig. 9S. Damp Sand Beacues packed b\ Aiu-waves neau a Rivilet
All these sand-forms are but modifications of wave-forms,
and copies of air- waves ; and they maybe seen wherever there
is drifting sand.
Near the Findhorn in ^Moray is a curious tract covered
with moving sand-hills.* The sea throws up wet sand, which
dries, and the prevailing south-west wind drives it eastwards
along the coast.
Great yellow hills, 100 feet high, are the sand-waves of
* This district is well described in Wild Sports of the Highlands (chap.
XX.), Joiu-nals of Charles St. John ; Murray, 1846. See also Natural History
and Sport in Moray, by the same author : Edin. 1863.
300 DEPOSITION.
this sandy sea, and though they move \vitli extreme slowness,
they have covered np whok' larms witliin historic times. In
the trough of these waves, oUl wheel-tracks and ploughed land,
the stone implements of a forgotten race of savage Scotchmen,
even golden ornaments, are occasionally laid bare by the wind ;
and the old surface of the "land imder the waves" reappears
for a time. Tt is like the rest of that part of ]\Ioray — a mass
of boulders.
When the wind blows, the movement may lie watched.
Close to the ground yellow streams of fine sand may be seen
waving from side to side, and bounding from point to point, in
curved paths, like the wind which moves them. Wherever there
is a hollow, sand rests in the shelter. The trough of every ripple-
mark fills gradually, but the back of the miniature wave is
constantly wearing away. A grain of sand does not fly or
roll, straight on and continuously ; it moves in curves, and
travels by fits and starts. It is turn about — the lowest grain
beneath the crest of a ripple, then the highest in the trough,
and exposed to the wind. It rolls up the back of the wave,
shoots over, and falls like the crest of a breaker ; and then
more grains fall on it, and shelter it for a time. But while
the upper surface is thus moving to a certain depth, a lower
stratum of damp sand takes time to dry and move. Sand in
motion is rolling over sand at rest, as sea-waves roll over still
water.
The larger hills advance on the same principle. The slope
to windward turns the wind upwards, and loose sand rolls and
ilies up-hill before it, rippling like waves upon an ocean-roller,
till it takes a final leap over the hill-top, and falls into the
shelter. There it may be watched falling and sliding di^wn,
and forming a perfectly regular slope of sand — a talus in the
calm. The base is continually advancing in the same direc-
WAVES — JLA.EKS. 301
tion as the wind, and a succession of strata are being deposited
there at an angle of 32°, Amongst these hills, chiefly in the
hollows, bent, whin, and other plants occasionally, take root
and flourish. They stop the movement where they grow, but
only for a time. The sand-waves march steadily on. The
crest follows the trough ; the whin-bush is buried in the middle
of a hill 50 or 100 feet high ; and by the time the buried
plant comes up behind the wave, it has long ceased to live.
When the wind blows from the east, or from any other point,
the movement changes. The shape of the sand-hills is irregular,
but the prevailing wind is from the west, and form shows it.
This sand-flood, in its eastward course, meets the Findhorn
river flowing north. The water is too wdde to be crossed at a
bound, except in very high gales ; so the sand falls into the
water. The river washes it out to sea, and the sea washes it
up the firth ; treats it according to the fashion of sea-waves,
and throws it up again for the wind to deal with.
When the tide ebbs, the sea-bottom is exposed, and there
is no single form upon diy sand that is not to be found upon
a wet sandbank, when the tide ebbs far enough for the banks
to be seeiL Stream-marks on shore explain old sea-marks.
There is, however, this notable difference between land-
drifts and sea-drifts : — the sea-forms are all flatter and lower,
and the reason is plain. If a conical pile of dry sand is made
in air by pouring sand upon a flat base through a funnel, the
sides will make a certain angle with the horizon, about 32°.
But when dry sand is poured through the funnel into water
tiQ the cone reaches the same height, the sides make a veiy
difterent angle : — the slope is far greater, the base broader, the
sides of the hill less steep. It is still a conical mound, but
it is a flatter cone. So sand-drifts and sand-waves, made by
currents of water in water, are generally less steep than the
302 iiErosiTiox — waves— maiiks.
same furui, made by currents of air in air. Ikit both result
from the force which moves air.
The bottom of the sea cannot be reached directly, but by
feeling with the lead its shape is pretty well known in many
places. It is nowhere ilat, but is ripple-marked everywhere —
varied by hill and dale, by sandbank, shoal, and hollow chan-
nel. Where currents move, sand-forms which result are alike
on shore, in air, on beaches, and in soundings. Snowdrifts
and sandhills show what is taking place at the bottom of the
ocean, and why there are drifting hills and dales even there.
Sedimentary rocks are chiefly old rubbish-heaps packed
in the sea. In the coal-formation beds are worked out, so as
to leave casts of their surface. Beds of ironstone, for example,
are worked in Lanarkshire, and the roof of the mine gives a
sandstone cast of the bed below it, after the bed has been
worked out. In some of these mines the form of the roof is
that of mud-banks now visible at low water in the Firtli of
Clyde. There are domes which covered mounds ; and wedges
which filled hollows like watercourses. The roof and floor
approach each other where the mud was washed away, where
the trough of the mud-wave was.
Similar forms recur in every sedimentary bod. These are
old sea-marks ; they may also be old photographs. According
to the evidence of sand-drifts, snow-drifts, and old rocks, that
which is now going on above water goes on under it, and has
]jeen going on since sand and dust, water and air, were mctved
by sunlight, heat, and gravitation. The surface-forms of old
silt-beds do but record that forces which now woik, liavc
worked air and water engines, and that sunlight, which is a
force, may have worked the tools. The guide to the force is
still form. The tool-mark points out the tool, and that leads
to the engine, and to the power which works it, and to llim
who set the task, and created a power when He made light.
CHAPTEK L.
ItErOSITION G — BEDDING — liAIX-MARKS.
ACCOEDIXG to an old saw, " Because the mountain would not go
to Mahomet, ]\Ialiomet went to tlie mountain." lie did the Lest
he could imder the circumstances, and men who study nature
can do no more. The frog who tried to grow too fast, l)urst
ignominiously ; if he had been content to look at his world
with tadpole's eyes at first, he might have lived to grow and
learn modestly from little things around him. If both ends of
a chain of cause and effect are out of reach, it is best to study
the links which sm-round us, and " creep before we gang."
It is impossible to watch the packing of sQt in the deep
sea, it is possible to watch a similar process in shallow
water and on shore ; on the sea-beach ; amongst the sand-
liills of Moray ; amongst snow-showers and snow-drifts. It
is impossible to watch tlie progress of a tidal wave from Cape
Horn to England ; smaller Atlantic waves are apt to sicken
those who swing over them ; but waves in a puddle may be
watched at ease throughout their course, and from these small
things a large lesson may Ije learned. Because moving water-
mountains go theii" own way, and will not be controlled by
little men, little waves have been summoned from little ponds
to act the part of their giant kin, and work denudation and
deposition on a small scale. This much may suffice to cxi)lain
304 DEl'OSITION.
Avliat was meant by learning to translate old geological records,
by watching geological engines now at work, and liy making
miniature engines in imitation of tbeju.
Air and water are engines which work deposition, and the
chief mechanical power employed about the work is the gravi-
tation which sinks the silt in water, or makes the sand or
snow fall in air. Therefore experiments made with water,
silt, and weight, are but natural operations on a scale suited
to small observers. It is easy to make ripple-marks, and
beaches, and all surface-marks of their class, by stirring a
muddy puddle : it is equally easy to make small geological for
mations grow rapidly, and watch the whole process at home.
One heavy clog on geological study is the impossibility of
watching the progress of work ; 1jut if this difliculty cannot be
overcome it may be circumvented. Gravitation may be set
to work in a glass tank. As an illustration the following
arrangement was made : —
February 12th, 1863. — A glass tank with flat sides was half
fdled with Thames water as supplied in London. A glass
funnel was placed in a retort-stand, so that the end of the
funnel touched the water near one end of the tank. Through
this channel finely divided ]naterials of various colours and
specific gravities were poured in the following order : —
1. "Silver sand;" 2. Coarse granite sand from the Scilly
Isles ; 3. Fine pipeclay mud, squeezed in with a sponge ;
4 Coarse yellow sand ; 5. Silver sand ; 6. Yellow sand ; 7.
Very fine dark river mud, part of a ball in which a nnul-fish
was brought home from the river Zambesi in AlViea. ; 8. Sil-
ver sand ; 0. Zambesi mud; 10. Silver sand; If. Zambesi
mud ; 12. Silver san<l ; l:'. ripechi}- to make a white sur-
face. In spi'eading from the channel through which they fell,
these materials formed themselves into a conical mound (vol.
BEDDIXG — RAIK-MAEKS. 305
i. pp. 378, 380) ; but the base of the heap could not spread
beyond the glass walls, and the edges of the forming layers
were seen through them. Four vertical sections of a stratified
mound were seen forming at different distances from the
channel by which the materials entered, and they varied in
shape, colour, and material. No one of them presented thir-
teen fiat layers arranged in the order in which the materials
were poured ; instead of thirteen beds there were nearly
thirty. A large riv'er brings down mud, sand, gravel, and
larger stones of varying size and weight at various seasons.
An ocean-current may carry various su.bstances at different
geological periods ; it may carry the shells of tropical infu-
soria, or floating moraines ; but whatever the materials may
be, the same gravitation which packs it in the sea worked in
the glass tank, and there the operation could be watched.
At first the water was thick with small suspended particles
of all the materials poured in. To imitate nature, bits of
ice were floated at one end, IST., and sun-light was allowed to
shine on the other, S. (vol. i. p. 68). This arrangement of
temperature moved the miniature engine, and it worked
accordingly. The water about the ice cleared, and a thin layer
of clean cold water floated, because that water was about 33°
(vol. i. p. 75) ; but columns of cold water (about 37°) sank
down from the ice (p. 78), and the falling streams carried
suspended mud rapidly downwards. A\^ierever an iceberg is
melting, the same thing must happen on a larger scale. On
the outer surface of the glass the downward curve of move-
ment was shown by vapour condensed on the glass. Wlier-
ever a cold mass stands in warmer air, like movements and
condensation of vapour result. The curves of temperature
were shown within by clouds of mud, as curves of temperature
are shown l)y clouds in the air (chap, v.) As these mud-
X
306
DErOSITIOX.
clouds fell, layers began to form on the uneven surface below,
and these followed every curve which had resulted from the
method of pouring in the heavier and coarser materials. Hori-
zontal layers of falling silt formed in the water, and sank
gradually, settling upon each othei-, but varying in shape as
the currents of cold water moved them from N. to S. below
while warmer currents moved them from S. to N, aboA'e,
Wave-marks and ripple-marks were formed on the sur-
face of the nmd, and fresh layers were seen to form against
the glass. The heavier particles forced their way through
the falling shower, and these beds, in forming slowly, assumed
ii very complicated structure.
White clay and brown mud separated and mingled, and
took strange branching tree-lOce shapes, like those which
occur in mottled sandstones. These are called " dendritic
concretions," and have been attributed to electrical action ;
in the tank they resulted from mechanical action alone. The
lied of silt, in gathering Aveight, squeezed out the water,
and the water in rising displaced and pushed up the lightest
BEDDING — EAIN-MARKS. 307
particles of mud. Through a leus the opsration was seen ;
some grains were falling slowly, as snow falls in still air,
others were rising in jets and fountains of water squeezed out
by the growing weight above ; others again were drifting
before the currents, as snow and clouds drift before the wind.
When the water cleared, the surface of the mud was a white
surface of deposition with current-marks, the sides of the
mound a section of a small geological formation ; and the
whole operation had been seen from begimiing to end.
Temperature and gravitation had been set to work a small
engine, and it packed silt as the sea does.
By March 24 the surface of the mud was covered with
minute water-plants, green and brown, which grew from their
invisible seeds and spread from centres. About these plants
minute bubbles of gas formed, and more formed beneath the
mud, amongst the sand, and under the plants. In expanding,
these gas-baloons lifted plants, sand, and mud. When the
raising power of the gas had gathered sufficiently, a net of
green, studded with shining balls of gas, and with sand and
mud entangled in the meshes, rose to the surface, and there
hung suspended till the gas escaped. Then the system fell
slowly down again at a new place. As there were currents
in the tank whenever the sun shone, upward, lateral, and
downward movements and transport of inorganic materials
resulted from this minute water vegetation, and from the ar-
rangement of temperature which worked the engine.
Similar action must result from the chemistry of vegetation
and sun-light wherever water-plants grow upon beds of silt ;
and old sedimentary rocks must record movements like those
which were seen in the glass tank.
The tank was kept as a microscopic vivarium, in the hope
of finding some African monster. It was covered with a
308 DEPOSITION.
sheet of glass, but exposed to air aud light ; and by July the
water was peopled willi living creatures hatched in the mud.
They could be seen with the naked eye, and better still with
a lens or microscope. They played and fought and gambolled
in their forest of tiny plants ; they died aud were buried in
the stratified beds of their little world. They were chiefly
home-bred Thames-water monsters ; if any were of African
descent, they were eaten up by hungry English crustaceans,
or overlooked. While these lived, they too helped to shape
the silt-beds above which they swam ; they left their tracks
on the surface, and their dead bodies fell amongst the withered
plants which formed the upper layer in this bedded sedimen-
tary deposit.
By December 22 a layer of water six inches deep had
been lifted up and carried away by the sun ; evaporation was
rapid while the weather was hot, and no condensation — no
rain, had made up the waste. Meantime the vegetation had
become a thick mat on glass and mud, and the water-fleas
were numerous, active, and ravenous. The top of the sand-
heap had risen above water, and had become a circular island,
similar in shape to islands of boiilders in the Baltic, along
the Swedish coast. By stirring the puddle, the island was
worn by miniature waves ; and beaches and terraces were
worn and built, " eroded and deposited" near high-water mark.
As the water fell lower a repetition of the disturbance made
a series like those shown above (vol. i. p. 334).
Lastly, a stream of water poured through the old funnel
cut water courses in the island, and built deltas in the water
about it (chap, x.)
8o within tlic compass of a glass taid< many natural i)he-
nomena may be imitated aud watched : — denudation by
water-streams, tlie habits of crustaceans, the growth of plants,
BEDDING — RAIN-MARKS. 309
the formation of surfaces of deposition, and the deposition
of beds of silt : geology, natural history, and botany.
It is needless to enlarge upon this toy. It is obvious that
a working section of river-mud may be got anywhere by
planting a glass under water ; a glass tumbler and a handful
of mire will show the process of geological deposition at home,
to any one who will condescend to learn from common little
dirty things. It is impossible to get at the bottom of the
sea ; but if sunken mountains be out of reach, it is very easy
to make mole-hills like them in a glass tank, by imitating
nature, and by setting natural forces to work natural engines
of small size.
Having thus taken one small step under water, the next
stride is upwards on land. We cannot get at the bottom of
the sea, but we live at the bottom of a sea of air, and deposi-
tion of strata goes on about us.
The rocks with which geologists now chiefly deal are
stratified sedimentary beds, in which plants and animals were
buried ; most of these are made of chips which were ground
off solid rocks, and fell through water. The formation of
beds by the falling of heavy solid particles of frozen water
through air is a similar process, for it is an effect of gravita-
tion, and it can be watched ; snow-drifts are formed by
streams as sand-banks are. The snow-formation only endures
so long as the temperature is less than 32°, but wliile it lasts
it is a fusible geological formation of sedimentary beds.
Like these, Icelandic strands, deltas, and plains, are made
of fragments of fusible frozen lava, which would certainly
melt again at some high temperature. While they last these
also are parts of a " fusible sedimentary geological formation."
The snow-formation is but the last of a series, fusible at a
lower temperature than those upon which it falls. Sandstone
3 1 0 DEPOSITTON.
beds are like the rest ; beds of a silicious sediment which is
melted in making glass. Lava and silica, like water, become
vapour in a sufficient heat, for they colour flame. Geyser
water holds silica in solution, silicious shells extract it from
sea-water. Snow is but a sediment easier to melt and harder
to freeze than the rest : all sedimentary rocks are fusible : all
their materials sink when cold, solid, and heavy ; flow when
fused ; rise when hot and light. One sedimentary bed packed
by gravitation and a circulating fluid is as good as another
for studying the process of mechanical arrangement, and a
snow-bed is the easiest to get at in the series.
In lofty mountains these sedimentary water-beds may be
seen resting upon sedimentary beds of like form. Avalanches
and landslips fall from lofty cliffs, and their fallen debris
takes the same talus-slope. The mechanical action is the
same, though snow and grit melt and freeze at different tem-
peratures. In Iceland snow-beds occasionally alternate with
beds of ashes, which fall during eruptions, and drift at all
times ; the packing process is the very same, it must still be
the same, at the bottom of the sea. It must have been the
same ever since gravitation worked deposition there, or any-
where.
In some geological books it seems to be assumed that all
strata are deposited flat. It was not so in the model, it is not
so on shore, and it cannot be so on the uneven sea-bottom.
When snow falls on rough ground, it is unequally de-
posited even in a calm, and silt must be unevenly spread for
the same reason.
Let the dark line represent the outline of a sea-bottom, or
of a hilly country, and it is evident that beds of snow or silt
must be deposited irregularly ; at various angles, at different
levels, and in different quantities at different places.
BEDDING — EAIN-MAHKS. 311
Every suow-bed imclulates with the ground Ijeneath it,
and many beds slope because deposited upon a slope. The
snow-shower which forms a bed on the top of a cliff, makes
another at the foot, and a third in the ditch. For that reason.
Fig. 100. Stratified Snow-beds formino.
sloping or separated beds of rock do not necessarily imply
disturbance, for they too may have been deposited upon a
slope, or simultaneously at different elevations. This evi-
dent truth is proved by every streamlet, and on every strand
— where road-dust has been swept into a gutter and left,
where a rivulet flows over sand into a sea, where the tide ebbs
and flows now, and in geological sections of old rocks.
When snow drifts, beds dip down-wind as they form ; when
sand is moved by a river, the beds dip down-stream. In the
upper reaches of the Tana, in Norway, the river meanders
amongst beds of sand, which it covers in floods, and through
whicli it cuts sections at other times ; the beds dip at all manner
of angles, but they all dip one way. The same is true of Ice-
landic river-plains, where travellers may ride for many miles
over deltas of ashes and mud, alternately fording rivers and
riding over dried sand-heaps packed by the winter floods.
On the wide strand about Mont St. Michel, in France, where
the tide ebbs and flows over sands for six or eight miles,
sections made by streams show that stratified beds are not
312
KErOSiTIOX.
deposited as ilat layers in the sea, but may be deposited in
layers sloping opposite ways, where the stream \\hich packs
them ebbs and flows.
At Goat Island, in North America, beds of gravel, etc., are
packed upon glaciated rock, and the form of the packing shows
that water formerly moved towards Buffalo, instead of flowing
i
Goat Island, Ni
from Buffalo to Niagara, as it now does. No. 1, the highest
of the series, dijis down-stream, and was probably packed by
a river. It contains fresh-water shells, and consists chiefly of
gravel and sand.
No. 2 is a bed of stiff clay, containing scratched stones,
many of which are foreign to the district. Because this bed
is horizontal, it is probable that it was formed in still water,
upon a flat base. The lower part of No. 2 is a series -of hori-
zontal beds of gravel, coarse sand, clay, and scratched stones,
the lowest of which rest upon a flat surface of reddish sand.
BEDDING — 1;AIN-M ... 313
No. 3, the sand, contains no stones, but is disposed in
thin sweeping beds, which have a general dip of 15° S.E.
This bed was packed by water, moving south-eastwards ; but
till the packing of silt had been watched in models, in snow-
drifts, on strands, or elsewhere, the record could have no
meaning. No. 4 is a bed of clay containing large blocks of
a kind of rock which is not found to the south-east, but
abounds to the north of the spot. The rock below this bed is
marked with glacial strife, which indicate the passage of
heavy ice towards the south and west. The river Niagara
flows the other way at the foot of the bank, and it has cut a
channel through all these beds of drift, and through some of
the upper beds of glaciated rock. Eeading this old document
by the help of snow-drifts, the meaning seems to be, that
during the time of 4 and 3, water and ice poured as the arrows
point ; that during the period of 2, water was at rest, and things
fell through it ; that during the packing of 1, it flowed as it
now does, from the watershed towards the sea.
At the watershed, near Fort Wayne, some hundreds of
miles away, a similar record confirms the first. A section of
a gravel-pit shows —
1. Gravel and rolled stones ; no stratification visible.
2. Numerous beds of fine sand, liorizontal.
3. Ditto, with occasional small rolled stones, horizontal.
4. A series of beds of sand and gravel, all dipping toivards
the south-west, in all twenty-four feet thick. These indicate a
stream flowing south-westward over this watershed of North
America.
5. A bed of clay, about three feet thick, containing large,
polished, and striated boulders of rocks, which are found in
situ to the north, beyond the great lakes.
6. A bed of fine white sand.
314 DEPOSITION.
The trauslatiou made on tlie spot is given above (pp.
245, 24G) ; the language was learned on the strand described
chap. xxii.
This land in North America seems to be an ancient sea-
bottom. Atlantic currents are sorting tropical infusoria and
glacial debris off Newfoundland ; it is not possible to get at
the bottom of the sea there : but the gravel-pit at Fort
Wayne may explain what is now going on in the Atlantic, if
the strand, the snow-drift, and the glass-tank, have been un-
derstood so far.
If sedimentary rocks were formed m old oceans, this lesson
applies to them all. At Kreuznach, near the Ehine, is a
sandstone quarry, where beds are of different colours, and their
arrangement is very well seen. The section is like No. 3 in
the woodcut, p. 312. But beds which rest on each other dip
opposite ways, and record that water ebbed and flowed, or
changed its course, while the stone was silt falling through
the sea. This so-called "false bedding" is true deposition,
and great currents may have packed large beds on the same
plan. These forms abound in old rocks.
The mechanics of deposition may be learned from models.
The outward form and internal structure of sedimentary rocks
record movements in fluids, and they are registering thermo-
meters within a certain range.
Eyriks JokuU (vol. i. p. 429), and otlicr large mountains
of bedded igneous rock in Iceland, appear to rest upon a thin
bed of sand and cinders. Because of "false bedding" in this
thin layer, it was packed by water which ebbed and flowed ;
if so, Iceland probably rose from the sea. Four or five thou-
sand feet of igneous rock are spread above the bed of tuff,
which is near the level of the lower plain in the woodcut, and
the crust has been l)roken and ground into mountains aiid
BEDDING— EAIN-MARKS. 3 1 5
deep glens. Lava-floods have poured over the surface out of
rifts. But the fusing point of a frozen lava clinker has never
been reached at the bed of tuff since the clinkers froze and
fell there, because the false bedding is preserved, and because
the black glossy cinders retain the shape which they had
when the white ashes were j)acked about them. The form of
a sedimentary bed proves that the fusing point of the material
has not been reached since the bed was packed ; and the rule
holds whether the bed is made of mud, snow, gravel, or Lau-
rentian gneiss ; whether it was packed in a toy on shore or
in the deep sea. A great deal may be learned from little
things ; much may be fished out of dirty puddles ; but every
student who will condescend to make scientific dirt-pies on
the plan here indicated, must set his wits to work out con-
trivances to illustrate his own special study. There is room
enough and to spare in the field, though many are working at
geological deposition and bedded rocks. Let one more familiar
example of learning from little tilings suffice.
Kipple-marks, wave-marks, beaches, and bedding, are
marks made when loose materials were under water or awash.
Other marks can only be made upon x>lastic surfaces in air.
These, like the rest, record facts, but the language must be
learned before a record can be read, and the easiest way of
learning a language is to try to speak it or write it.
A rain-mark was made upon a plastic surface in air, be-
cause haK an inch of water would shelter the surface from the
rain. But in order to learn the meaning of ancient rain-marks
it was necessary to see marks newly made — Sir C. Lyell saw
them in the mud of the Bay of Fundy. It is very easy to
imitate nature in this case also.
Every shower of rain makes its mark on still water. Each
drop makes a dimple and starts a radiating system of circular
316 DKrosiTiox.
waves, wliicli, like other waves, may be refracted, retlected,
and focussed, accelerated or retarded. They meet, and cross,
and jostle, so that the water-mirror becomes a rippling pool.
But when the shower is o\'er the waves cease their gambols,
and the lake is a mirror again. A shower may fall on a
plastic surface — on mud, clay, dry dust, snow, or any other such
material — and there the dimples may retain the shape given by
the falling drop. The mark is a tool-mark, the dint is made
by a drop lifted, carried, and dropped by the engine which
works denudation and deposition ; and the tool-mark may be
so placed as to record very ancient work done by the same
machine. Eain-marks endure when the plastic surface is
baked, frozen, or otherwise hardened.
It is not necessary to travel far in order to learn this language.
The scrapmgs of the streets of London arc chiefly powdered
igneous rocks, ground up to a tough mud by carriage wheels,
and scraped into heaps by scavengers. The wet sludge forms
a surface almost as smooth as that of a lake, and it sets gra-
dually as the water evaporates. After a suunner shower this
smooth mud is often dimpled with regular cups, and each of
these is a cast of a drop of rain, which fell there. Each is a
tool-mark, and a record. Eoad-scrapings bake in the sun,
and freeze hard in winter, and the mud when dry may be
further hardened by baking, so as to resemble some of the old
rocks upon which fossil rain-marks have been found. It is
so far a record. But if the material is fused by greater heat,
the record is spoiled and lost. In the sunnner of 18G2 a
thunder-plump made a very beautiful set of (liiii])l('s on
smooth mud faces, and filled the pockets of cabuien with the
silver of pedestrians, Mdio feared the rain, and thought the
mud a nuisance. One, however, who came from a rainy land
and wears old clothes, watched the shower and the mud, and
I'.EDDING — KAIN-MAKKS. 3 1 7
went home to try whether the shower could not be set to work
for hun.
An old cigar-box was filled with wet plaster-of-paris, and
when the plaster was beginning to set, the box and its smooth
white-faced contents were turned out of doors and watched,
to see what the rain would do to the plaster, and what rain-
marks really meant. They meant that the surface was smooth,
plastic, and above water ; the shape, size, depth, and direction
of each cup recorded the shape and size of a drop, the force
with which it fell, the direction from which it came ; the slab
recorded the number of drops that fell within the area of a
cigar-box during a certain time. When the plaster set it be-
came a register, and it will last till it is destroyed. It is easy
to see how the drops fell, to determine the quarter whence
the wind blew, and the force of it ; and similar marks found
upon old rocks of any age record similar facts. But rain-
marks do not record climate, as some have ai'gued. Hailstones
bury themselves in snow and cold mud, so the climate may
have been cold. Drops which fall from clouds of steam
escaping from a boiler ; scalding drops which fall upon hot
sticky mud, beside the boiling springs at Krabla in Iceland ;
summer rain or winter sleet ; all make the same marks. The
climate in old geological times may have been very different
from existing climates, though rains fell and winds blew
slanting showers down upon smooth plastic mud.
Like other marks, this class register temperature. The
mud was not frozen, for it was soft when the mark was made :
it was warmer than 32° ; it was colder than 212° ; it did not
boU, for the surface was smooth and wet. The fusing point
of the material which retains the mark has not been reached
since the mark was made. Within these limits a rain-mark
registers temperature, and it proves that the whole earth was
318
DEPOSITION.
not covered with water at some unknown date. Like the
ishiud in the glass tank, some part of a brd of silt was above
water when the rain fell.
To get at past climates other marks are used, and they
form a separate branch of study.
■^ 1
Fig. 102. Fossils.
2. Bioken from the limestone wall of 1. From a "weathered" limestone sui-
the Mammoth Cave, Kentucky, near tlu' face lu-eserved under a bed of yellow clay
Uiver Styx." on a hill near St. Louis, on the Mississippi.
These specimens illustrate one denuding action of rain-water. It holds carbonic acid
in solution, and it dissolves insoluble carbonate of lime by transforming it into soluble
bicarbonate. When a limestone rock-surface has thus been dissolved, and worn, and
washed away, insoluble silicious fossils project. These, by their preservation, prove that
a rock-form was not sculptured by mechanical force alone. Tlie hills about St. Louis were
not sculptured by ice, tliongh limestone-hills near Buffalo were. The Mammoth Cave, and
the shapes of hills about it, arc chiefly chemical work, because fossils project from the
sculptured surface of the stone. ,\ -p • . , . y/
/
CHAPTER LI.
DEPOSIirON 7 — FOSSILS — ALTERED ROCKS.
Like otlier shapes, the forms of plants and animals are ther-
mometers.
Because an organism lived, the average temperature where
it lived was, during its life, somewhere between 32° and 212'\
freezing and boiling ; that is, if the extinct thing was made
like most of those which exist. Even lichens will not grow
in extreme cold, and vegetable cells burst in boiling water ;
an animal made partly of albumen and water is frozen in ice,
and is coagulated and cooked when a submarine volcano
makes the sea boil. Living things can resist extreme tempera-
tures for a time ; but nothing now living can long survive
boiling and freezing. Because a sea-plant grew, and a fish
swam, their average climate was probably somewhere between
these limits ; and their shapes are registering thermometers
so far. If species is known, climate may be guessed from the
haunts and habits of living things of the same or like form.
An arctic shell means cold water, a palm-tree warm air, and
things like them similar climates. But organic forms, which
are unlike livmg things, do not so closely record tempera-
tures. Sedimentary beds, with water-marks, rain-marks, and
fossils, together record the former existence of land under
and above water ; with an atmosphere and a climate fit to sup-
port life. Because the fossil form has been preserved, a
320 DEI'OSITION.
stone, or bed of stone, lias not been fused since the materials
took their shape.
Fossils are time-keepers also.
The water-formation exists as solid, fluid, and gas ; solid
snow and ice, fluid water, gaseous steam and vapour.
"SVlien temperature falls to a certain point, a crust of ice
forms and floats upon fluid water, while vapour rises, is con-
densed, crystallizes, and falls as snow. If it falls upon plants
and animals it smothers and preserves them, as silt does, and
far better. If wetted and frozen again, the snow becomes
ice, and the buried plant or animal freezes. Till this forma-
tion is melted, it is an altered crystalline sedimentary forma-
tion containing fossils. The famous frozen Siberian mammoth
was so well preserved in frozen gravel, that dogs fed upon the
flesh when the ice which contained it thawed. In any other
sedimentary bed the skeleton, or a cast of some part of the
creature, might have remained, but the flesh would have
yielded to natural chemistry. That fossil proved that tem-
peratures less than 32° had prevailed at the place from the
date of the mammoth's burial in ice. It was an old forma-
tion, because mammoths have long ceased to live. English
ice now melts every summer ; Arctic ice does not. A perch
preserved in English ice records the date of his death within
a few months, because of the known climate, and implies a
late formation, because his race exists. We know that the
Arctic ice which contains an extinct mammoth, is older ice
than English ice which contains a perch. One is less than
six months old, the other far older, but how much older is
not recorded. We know those facts from observation. If
we did not, the fossils alone would lead to the conclusion that
the perch ice was the newest water formation, because perch
exist and mammoths do not. But if a perch were found in
FOSSILS— ALTERED ROCKS. 321
ice under a mammoth, buried in snow, these relative posi-
tions would prove that some perch lived before the mammoth
died, and that the lowest bed was the oldest in that series,
though it contained fossils of existing species. Like slates
on a roof, these two portions of past time overlap, and their
extent is only known in one direction.
Fossils.
Living Mammoth
Living Perch Perch now alive.
In the first place, relative position proves the relative age
of the fossil ; and when that has been ascertained, the fonn of
the fossil is like an index-number on a page. The uppermost
layer is the newest, unless the series capsized : because snow
and sediment both fall. When two hviman graves were found
above each other under the foundation of an old church, his-
tory gave a date and position older relative dates.
Christian church wall . date known — a.d. ?
Human grave . probably near the time.
Ancient do. older, but uncertain.
If in this case the bones of buried men differed, the lowest
had the type of the oldest race, and such bones thenceforth
mark ancient graves. The buried form became a time-keeper,
for such forms lived before the year a.d. ?, when the
church was founded.
Thus out of form, species, and superposition, vague geo-
logical dates are constructed with fossils, and slowly built up
into a skeleton-history of part of the world's crust. The
study is like turning over the leaves of an old saga, in which
events were recorded year by year. Those which are men-
Y
322 DEl'OSlTKiX.
tioned ill llie uppermost pngf. liappened after those Mliit-li
were first written down ; and when the place of an event has
been learned, it marks the place of others which happenetl
before or after it. Fossils in upper beds died after those
which are buried under them, and the lowest human grave
was first filled.
Position gives the age of a fossil, and then the fossil alone
gives position. A stone is like a torn page which recoi'ds a
known event. If written by a man who was at the battle of
Blenheim, the page must be placed below the "Waterloo page
— for Blenheim soldiers had become extinct before Waterloo ;
and above the page written by the Icelander who described the
battle of Clontarf as a recent event. But the fossil record is
not a history, it is but an index, and by no means complete.
Position even without fossils gives a relative date for beds
of rock.
A bed of snow resting on ice on a pond gives thi'ee dates.
The water was there before the ice formed, and the snow fell
ui)0u the ice — snow is the latest formation, water llie oldest
of these three. In Iceland, beds of silt ai'e on lava in lakes,
ice grows on the lakes, and snow falls on the ice. Of these five
the lava-crust is the oldest, and still older fluid lava once flowed
under the frozen lava-crust.
There is a regular series whose position depends on tem-
perature and specific gravity ; a series liable to disturbance,
and fre(|uently disturbed.
Cold and Wkioiit.
1. AVater as vapour iji the air — condensing and falling.
2. Lava and a'^hes in tlie air— fallin<jt.
FOSSILS — ALTERED HOCKS. 323
?). Water as suow, a bed of sediment^ — at rest.
4. Water as ice, a frozen solid crust — at rest.
5. Water as cold fluid in the lake — at rest.
(). Lava as silt, a bed of sediment — at rest.
7. Lava as a solid frozen crust — at rest.
8. Lava as a hot fluid, which escapes at times.
9. Water as steam, which is always escaping, and struggling
to escape, and has blown up the lava-crust in ]nan}'
places. ^
Heat.
The stone book of sedimentary rocks, with fossil pictures
engraved amongst the leaves, has been rumpled and torn,
pages are missing, leaves were of different sizes at first, whole
volumes are yet unread. It is hard to read the record, and
harder still to understand it. But wherever an organic form
can be traced, it records a climate tit to support organic life,
and proves that the page, though it may be torn and charred,
lias not been destroyed by fire. The fossil form is like a foot-
print in snow, which disappears when the snow melts, though
the melted snow may freeze again. It is like a wrinkle upon
the lava-crust, which ceases to exist when the lava is fused.
But these organic shapes tell more than tool-marks of engines,
however great. They tell of air and water, and their move-
ments ; of heat which kept them from freezing ; of cold which
kept them from boiling ; of gravitation which bound tliem to
earth. But they also tell of life, which made each shape
a separate reproductive system, "whose seed is in itself" — a
system wherein heat and weight play their parts, but are
guided and governed by subtle powers, of which those who
live by them here on earth know absolutely nothing at all.
As a bed of snow is altered by a sufficient heat ; as loose
324 DEPOSITION.
grains of lava-dust may be consolidated by fusing and freezing
— so all sediments may change into solids.
At the Sevres china factory, and at Minton's works in
Staffordshire, and elsewhere, certain clays are mixed with
water till the mixture is like a glacier-river ; the sediment is
washed, allowed to settle, and after a time sludge becomes
mud, and a tough paste. It is then moulded and patted,
twisted and worked into all manner of forms, dried, baked, and
finally burned. When all is done, the sludge has become a hard
flinty brittle substance, with a form which tells part of its
history. One bit was made on a wheel, another pressed in a
mould ; one was baked hard, another burned ; a third too
much fired, half-melted, and so distorted by its own weight.
If the miniature geological formation above described were
made with coloured clays and sands, dried, baked, ajid
burned, the sludge would become stone, and any forms im-
pressed upon the surface, casts of small plants, or creatures
tiiat lived in the tank, or their tracks, or stream-marks made
by currents, would be preserved (chap. 1.)
The forms of sedimentary rocks indicate certain tempera-
tures, an order of succession, and vague dates, for they were
deposited one upon the other long ago, at times when plants
and animals could live, and they have not been fused since.
But there is a wide range of temperature between 212° and
the fusing points of various stones, and many rocks have
been baked and burmul, and partially fused, as china and
bricks and glass are. The lower the rocks are in the geolo-
gical series, the more they bear marks of heat. Therefore,
according to position, a brick-kiln or furnace heat is below,
or was an ancient condition of the upper world.
Beds of slush do not turn to stone without some active
cause ; and the dee])er men go in mines, the greater is the heat
FOSSILS — ALTERED ROCKS. 325
of the earth. When a volcano bursts the crust, earth-light
shines out, and rocks melt like wax in the fire. It is only
by watching human works that we can hope to estimate the
effects of heat upon sedimentary rocks ; but these effects may
be watched at furnaces.
Siicnv becomes glacier-ice by a combination of heat and
pressure ; by softening, kneading, and hardening ; by fusing
and freezing again. — Below 32°.
Clatj becomes brick by kneading and baking. Finer clay
becomes china. About 1100".
Sand becomes glass by fusion with various other sub-
stances. About 1000".
Whinstone was made into a black glassy mineral at Bir-
mingham by fusing it. The difference in the structure of the
mineral was attributed to tlie rate of cooling, which was too
rapid for crystallization. About 1000".
Obsidian is a natural black glass, formed in volcanic
mountains. It seems to line passages in lava through which
hot gases have escaped. The stone is something like a lump
of sugar which has been partially fused in a candle ; and
cavities in lava are commonly varnished with a coat of some
glassy substance of like kind. ? 1000".
Jasper, Uoodstone, and similar glassy minerals, abound in
volcanic countries, and in old igneous rocks. ?
All these are effects of heat.
Limestone of the coal-formation, containing fossils, and
other limestones, are used as fluxes in smelting iron. The
stone melts and runs as lava does. It is often run into
moulds, and when it has time to cool it freezes into an earthy
mineral, with a glassy wrinkled surface, and a crystalline
structure. No trace of a fossil remains after the fusion, and
there would be little sign of fusion if the surface were gone,
and the slag a large bed of stone in a geological series. 3300".
326 DKrosiTioN.
Lavas are like slags ; whinstones are like la\as.
All these are products of heat, of fusion and i'reezing*
The whinstone may have been sedimentary rock because
it is like lava, and lava like slag, which was limestone, and
was perhaps a coral reef, or a bed of shells and silt at the
bottom of an ancient sea.
Fire-clay will not readily yield to heat ; it is easily baked,
but very hard to fuse. One of the Lanarkshire iron-furnaces
was lined with fire-clay as usual, and the first fire was lit
with faggots, amongst which were branches of hazel, and
furze. The furnace worked for many years with the hot-
blast ; thousands of tons of iron and slag were melted in it ;
but at last the walls grew shaky, and it was " blown out" to be
mended and re-made. In breaking out the hearth the work-
men found the shape of a forked branch, and the overseer
sent the curiosity to be examined in Glasgow. The learned
could make nothing of it. It lnol^ed like a l)it of forked stick,
but it was heavy ; it was not wood, but some mineral, so the
chemist wrote back to say that he could make nothing of the
specimen sent. If geologists would take a hint from this
story, and repeat such experiments, they might explain the
mystery of fossils altered in old sedimentiuy rocks. It would
cost nothing to line a furnace with bricks, in which plants
and shells, fish and leaves, had been packed ; the heat of the
furnace is 3300° or more, and the stones would be touch-
stones for temperature recorded in altered rocks.
If there has been a constant succession of life, from the
earliest known fossil species down to the present day, the heat
which baked rocks has never been the general climate of the
u])])er world, since Laurentian times at least. But many
*
Tlu'.se and iiiaiiy otlu'i
■ tcliipciat
urcs ar
(■ quotnl
fVoiii a
'riicniioiiictric;
Tiil.l,-
cuiupil.'.l l.v Dr. A. .^
V Tiiyl.ir.
I,..n.l
..11, ism
: T. iui,
I K. WiUats, [
Cl...„i
isi.lr.
FOSSILS— .VLTEKED ROCKS. 327
setlimeutary beds have Leeu baked since then, and the lowjst
are most altered. The heat certainly was internal lieat, and
the condition of beds which were buried and have been raised
to the surface again would give the temperature of the lower
regions, if a pyrometer scale were made with which to sound
the earth's sedimentary crust.
Beds low in tlie series indicate internal heat, wherever
these beds are found. Snow indicates external cold at all
latitudes and longtitudes. Temperature, as recorded by sedi-
mentary rocks, appears to be arranged in shells about a centre
— heat within and cold without.
It has been argued that " metamorphism" is not neces-
sarily a result of heat, because in some cases the central bed
of a series of three has been altered, while the other two
retain their characteristics.
To use a homely illustration, the same amount of heat
would toast bread and metamorphose the ham of a sand-
wich into lard. When a hot sun shines on the delta of an
Icelandic river in spring it warms a series of beds, which
alternate, and are variously altered by the same temperature.
The foundation is some igneous rock, which was fused at
some time ; on that solid is a pile of loose ashes and dust,
and lava-mud, sorted by the river. In winter this series is
covered with ice, on which rests a layer of ripple-marked
stratified mud. Over this, water has flowed, and frozen, and
packed more silt ; and so the upper beds alternate.
C^ Solar heat. 1. Snow.
.50". July Isotherm. 2. Ice.
36°. Annual ditto. 3. Water.
32°. January ditto. 4. Mud.
32°. Lava under ice. 5. Ice.
3300°. Lava melts. 6. Mud.
O Vulcanic heat. 7. Ice.
8. Mud.
328 DEPOSITION.
When this series is melted by the sun in spring, the ice
fuses and the mud remains. It is abominable ground to
ride over, for hollows cave in where the fused ice has left a
roof of sand. In the mountains it is common to find the
series —
Snow. ")
I Below freezinir,
Snow, y ,^2„
Ashes.
Snow, j
When the heat is sufficient, the snow is altered and " meta-
morphosed " into glacier-ice, but the ashes remain unaltercid.
If a series be made of
Fireclay ;
1 3300",
Limestone, Ironstone, and Fluxes ;
f white heat.
Fireclay,
1 0
and heated till the slag runs, all traces of life will be
obliterated in the central bed, while the other two may con-
tain altered fossils, like the mysterious forked curiosity found
in the furnace in Lanarkshire. So a bed of impure limestone
between two beds of slate may be metamorphosed into crys-
talline marble, by a heat sufficient to fuse limestone and slag,
but only sufficient to bake ripple-marked clay into hard
slate.
So also a bed of sandstone, with alkaline plants, rust, and
lime imbedded in it, might be partially fused into coloured
quartz ; while neighbouring sandbeds, without the alkali,
resisted the heat and hardened without fusing. At lUOU"
flint-glass melts.
In running iron and slag from furnaces, bits of wood, fire-
clay, brick, sandstone, and other such materials, often get
entanuled in the burning stream. Thev are variouslv altered
FOSSILS— ALTERED ROCKS. 329
by a heat of about 3300^ F., but all of them can be identified,
thougli enclosed in ii'on, which flowed over and round about
them. In all these cases the structure depends upon tempera-
ture ; and it seems to follow that a bed of silt may dry up,
and so remain ; or it may be sun-dried ; or baked, or burned,
or fused, by the heat of the earth.
The way to do a thing may be learned by seeing it done ;
the way in which a thing was made may be surmised by
comparing finished works. An altered rock may be com-
pared with a brick, or slag, and if they agree in form and
composition, it is evidence that the rock, like the other sub-
stance, was altered by heat.
If sedimentary rocks have sunk past the brick-kiln to the
smelting-house region below, crusts of lava which welled up
and froze in Iceland, and which now furnish materials for
silt-beds in deltas and in the sea, may once have been sedi-
mentary fossiliferous beds, which, like some ironstones and
fluxes, were silt, and now are metal and slag, because of heat.
So far, theory and models, and the effects of heat in
manufacturing processes agree. Geological facts confirm their
evidence.
Scandinavia, Iceland, Greenland, Labrador, and Xewfound-
laud, are slowly rising or falling — that is to say, in these
regions the solid crust of the earth is swelling or sinking ; re-
ceding from the centre, or approachmg it. But beds of snow
and fields of ice, which form the upper layers of the solid crust,
are not split, torn, dislocated, or smelted, by this movement.
Parts of Europe and North America have risen from the sea,
and yet the layers of soil and sediment next below the winter
snow continue to be soil, sand, clay, gravel, boulder-clays,
and loose materials, packed as they were at first. These beds
have not been much disturbed, or altered from below. The
330 DEPOSITION.
work of geologists who have learned the alphabet of fossils
has been mapped ; and a traveller can now identify tlie
nppermost layer of the conntry on which he stands by tnrn-
ing to a book. He may find out new facts for himself, but
the document has been made out so far that the outline of
the story told Ijy sedimentary fos.'^iliferous beds can be learned
from a translation. There has been a succession of formations
which rest upon each other, each a ruin of older rocks ; and
during that period the outer world was inhabited. There has
been a succession of life ; but when it began, and whether it
was continu.ous or interrupted, remains to be proved.
Tn passing from formation to formation, the most super-
ficial observer must remark a striking difference in the shape
and structure of the rocks themselves. In North America
newer rocks are to the south, the older to the north ; and the
contrast is very striking. In regions where the uppermost
beds ai'e of late age, the country is fiat, and beds are laid
horizontally, or dip very little. They are like beds of snow
and drift which cover them, little disturbed. The saine thing
is true of beds of like age elsewhere. There are many cases
of disturbance recorded in such rocks ; the soil itself has been
disturbed by earthquakes in Italy and in Iceland, and the
ground is there riven and disturbed. Even snow-beds and
ice have been shaken and melted from below in Iceland and
Sicily ; but, generally speaking, beds lately deposited have
been little disturbed and altered. But as the American
traveller works northwards, or the English geologist works
westward, the case alters. In old strata eveiy form tells of
violent disturbance, every stone of great heat. There an;
many sedimentary rocks in which no fossils have yet been
found, many beds in old fossil-bearing strata which contain
no trace of life. ()n(^ (luestioii lelt for ai'ijument is, whether
FOSSILS — ALTEKKD ROCKS. 331
these were deposited in cold water or in water too hot to
support life ?
It is plain, that generally the oldest known fossiliferous
rocks have been much shattered and altered, and that no con-
vulsion within human experience has equalled the amount
of force to which these altered beds have yielded.
The geological sections of Wales are masterpieces of art ;
they show a series of folds and curves upon a vast scale. The
rocks themselves record this part of their history in characters
which a child can read, now that this alphabet is taught in
schools. They retain their sedimentary structure, but many
of them are crumpled, as snow-beds are when they slide from
a house.
In the Isle of Man, at Brada Head, a cliff' 300 feet high is
marked by coloured bands, which sweep and bend, curve and
wave, like roimd text with the flourishing of a writing-master's
pen. The shapes of the hills have nothing to do with this
internal structure ; their forms are tool-marks of denudation.
N"o possible combination of cold streams ever packed silt into
such a form ; no loose silt or hard rock could possibly bend
into these curves without scattering or breaking at the bends.
The rock must have been packed in fiat or sloping layers at
first ; it is now hard and brittle ; but between whiles it has
been plastic, and then it was kneaded and welded like scrap-
iron in a press. No twisted gun-barrel could record the fact
with more clearness. Were these plates so welded when they
were wet or when they were hot ? The structure answers
the question. In this cliff are dykes of igneous rock, which
fill rifts, and the pattern on opposite sides does not fit. Even
in beach stones and pebbles this structure is seen, and tlie
rock looks like stone which has been burned at a furnace.
Waving white lines of quartz meander about in niany a
332 DEPOSITION.
tall cliff on the west of Scotland ; they are followed in all
their windings by lines and bands of other colours, and these
are now edges of crumpled sheets of hard brittle stone. They,
too, must have been soft when they were folded like coloured
glass in the workshop. In Ross-shire, in the forest of Gair-
loch, some beds of quartz rock of similar structure contain
fossils, which only appear when the rock is weathered. So
quartz rock in all probability was a sandbank, though it is
now like half-fused impure distorted flint-glass, which melts
at 1000".
Districts where these old crystalline beds occur show other
signs of great disturbance and great heat. Large dykes and
upthrows of granite, trap, basalt, and other igneous rocks ;
veins, faults, and fissures ; traverse whole districts. IMeasured
along their edges, beds which were deposited upon each other
" conformably and unconformably " are of great thickness ; and
yet, from " Fundamental gneiss to oolite," from " the Minch to
Brora," from " Skye to the Cheviot Hills," the whole patch of
the earth's crust which denuding engines hewed into the
shape of Scotland, was long ago moulded and kneaded like
plates of clay in the potter's hand.* No recurrence of earth-
quakes like those which have been observed by men, could
so crush and alter such thick beds of sediment over such
areas.
In Dana's Geology the Appalachian chain is well and
clearly described. The range includes a series of long wrinkles
and folds, which include rocks of the coal-formation. In
travelling from Pittsbui'g to Ilarrisburg, these folds are seen
in cuttings by the wayside. Beds dipping in one direction
are passed by the train ; sandstones, grits, and coloured beds
* Gi-olor;i(iil Map of Si'otlaiul. IJy Sir K. I. iMurclii.soii ami Aiiliil-aUl
Ocikif. 1861.
FOSSILS— ALTERED ROCKS. 333
succeed each other iu rapid succession, till the anteclinal or
synclinal axis is passed.
The train runs through one side of the bend, fl or \J, and
thence the beds dip the other way. Coloured bands, grits,
sandstones, succeed each other in the reverse order, till the
next fold in the old earth's wrinkled face brings back the
old series of sandstones, grits, coloured bands. The roadside
is like a picture made by the Geological Survey ; the journey
is a day's lesson in contorted rocks. Yet the shape even of
this great mountain-chain is not wholly due to this wrinkling
process. Valleys are not in the hollow curves of the strata
U ; neither are the hills on the top of the folds fl- One great
fault, according to American geologists, left a wall as high as
the Hindoo Koosh, 20,000 feet at least; for on one side of a
crack, over which a man can stride, the highest of upper
Silurian beds faces the lowest of lower Silurian. But the
upper Silurian wall of the raised side of this vast crack was
" denuded," hewn away, and the place where it rose has been
planed smooth, so that masses of grit, caught in the chink
while it was open, are cut through by the surface.
Such changes mean some great force, and the lowest rocks
mean great heat, according to the evidence of burnt stones.
The rocks of Newfoundland are greatly folded and frac-
tured. An able geologist is now engaged upon a survey there.
When his labours are published, we shall know something of
their relative age. They include sandstones, grits, slates, and
numerous beds of granite, but all these are not metamor-
phosed.
The Laurentian rocks of Labrador were supposed to
be " azoic;" they are low in the series, if not the lowest beds
known, and they resemble the old rocks on the Scotch coast.
From Belleisle to Cape Harrison, the land appears to be a
334 DKPOSlTloX.
maze of granite dykes aiul altered roeks. The euuntry looks
as if a sedimentary erust had been smashed up, half-fused
in hot stone, and frozen again.
The only modern natural formation M'liieh bears any re-
sembhmce to this old Laureutiau gneiss, is the water-crust
on tlie sea. Part of it is snow, part flat ice ; but where a
pressure sufficient to smash the crust has been e.xerted, tlie
fluid water has riseu through the faidts, and the whole is
cemented together by frozen water. It is a crust of sedi-
mentary snow and altered snow, now forming; it is broken
up and disturbed ; it has faults, upthrows and downthrows,
ground edges and slickensides, angular conglomerates of
cemented chips, veins and dykes of ice. But underneath
this old ice-crust is a fluid sea, and above it are new-fallen
beds of snow, which rise and fall with the bending crust, when
the tide flows and ebbs. The problem is — Did the shell of
temperature which makes water boil coincide with the for-
mation of any layer of sediment at the bottom of the sea ? and
if so, at what temperature did life begin in Laurentian or
lower beds ? Since they were first made, these old rocks
have been altered by a heat incompatil)le with the life r.\'
anything which now lives on this world.
We liave now reached the period of a water-formation. A
solid crust is formed about the poles, and is forming every-
where ; and if the earth is cooling, the ice-crust will reacli the
e(juator, and descend from the air to the bottonr of the sea.
Th(> solid is forming u}»on a fluid base, and now is the period
of I'apid action and \iiplcnt disturluuRH' in the water-forma-
tion, which hardens at 32° or some degrees lower, at a certain
distance from the earth's centre. Under the iee-formation
water still boils in Iceland at some jioint nearer fn the centre.
If the whole earth is cooling, the jxnnt of ebullition may
FOSSILS — ALTEItKli KOCKS. 335
have beeu further from tlic centre and nearer to the surlaec
in Laurentian times.
When temijerature falls, movements in the water-crust
diminish. There are fewer ice-quakings and sea-eruptions
when the arctic winter sets in. When the ice sets the crast
rests, and the slow deposition of snow is the only apparent
work in progress. But there is fluid beneath, and the crust
sways, and cracks, and groans, to prove that water may still
break the prison which holds it. The water-format i(in is
like the rock-formation even in this ; it has a fauna and
flora of its own. jMinute vegetation reddens snow, birds
and beasts walk on floes, fish and sea-weeds flourish under
them. Esquimaux hunt and fish on the crust of the sea,
and seldom tread on real earth or stone. If the world is
cooling, and cools a little more, the whole sea will be like the
arctic regions. If some glacialists are right, the whole earth
was in a like condition during a glacial period. Snow and
vegetation already begun may spread ; animals may change, and
adapt themselves to new conditions ; Esquimaux geologists, if
any survive, may be driven to speculate on the comparative
age of snow-drifts and altered glacier-ice. They may recognise
certain ancient drifts Vjv works of art contained in them :
the new white snow-stone, by frozen seals and extinct brown
bears ; the old blue snow-stone deposits, by fossil whales,
sharks, lobsters, fish, and other strange marine monsters ; the
lowest altered solid blue ice-beds, by mammoths, seaweeds,
shells ; the lowest beds of all, by conglomerates of different
chemical composition from any water-bed known. Questions
may yet arise as to altered sedimentary highly-crystallized
snow-beds, passing into compact blue ice near ice-dykes : —
whether the beds were altered by pressure, or Ijy a heat
almost sufficient to fuse snow-crystals and fossil flesh, or by
336 DEPOSITION.
some other unexplained natural power, like the nortliern
lights? The ignorant may hold, with the P^squimaux high-
landers found by Eoss, that the whole world is snow and ice,
and that it was so created. Keen arguments may arise
amongst the better informed as to the origin of upthro\vs of
igneous ice — whether the matter rose plastic or fluid, through
a crack, or a hole ; and if it rose at all, why, and whence —
from large or small lakes of fluid ice in the ice-crust, or from
a fluid water-core which reached to the earth's centre ? It
may be argued that, because the coldest air is also the heaviest,
there can be no fluid water under colder ice, for the coldest
water would be sure to sink and freeze first at the earth's
centre. The argument could be settled by experiment ; but
there will be a double crust under the disputants — an upper
crust frozen at 32°, or below zero, resting upon a rock-crust
w^hicli froze at 3000°, or some other temperature, when
the world was younger and warmer, before old age had cooled
its hot blood. And under these two crusts there may still
be fluid water, and fluid lava at deeper depths, if there be
such a thing as internal central heat diminishing by radia-
tion into space. We, who tread upon the upper sedimentary
beds of the rock-crust, wade amongst the snow of the water-
formation, and skate on the winter's ice, find more heat when
we burrow downwards. We see that melted rocks well up
from below in all latitudes and longitudes ; and when they
cool sufficiently, they too form a surface-crust. Surely it is
reasonable to believe that we, and the beds beneatli our feet,
rest upon a crust which froze upon a fluid, and which grows
inwards, as ice does on a pond.
There may be many such crusts, many fhiids, and nuiny
imprisoned gases underneath ; but the greatest heat must be
in the centre, and the last fluid drop there, if there be any
FOSSILS — ALTERED ROCKS. 337
truth in experiment. In every material which is melted and
cooled, fused and frozen, in arts and manufactures, the crust
forms outside about the warmer fluid. Water so freezes in a
spherical bottle. A drop of tallow sets on the outside, and the
fluid interior can he squeezed through the crust when it is
formed. Wax so freezes in a mould, the outside crystallizes
first, and the mside is often poured out to show the crystals.
Slag cools on the same plan. So do metals — solder tin,
bismuth, lead, silver, copper, iron, gold, platinum, irridium.
So does lava. Because all these, and many more, cool on this
same plan, it is probable that the world, whose shattered
crust contains materials which are fused and frozen in the
arts, cooled outside at first, if it ever was fused, and so pre-
pared a foundation on which denuding engines built up chips
and sedimentary rocks, to be the tombs of plants, animals,
and men.
At a certain comfortable club, where travellers and tlieir
guests dine, a luxurious contrivance is placed on a table at
6 P. M. A large double dish of block tin, filled with hot
water, is the base prepared for good things which appear and
disappear later in the evening. While quietly reading the
bill of fare, this engine is apt to startle strangers, for it stirs
the silence of the half-lighted room, like a gong, with a bang.
Tlie upper crust of the hollow dish may be seen to undergo
sudden convulsions. It jerks up at one spot, and when that
jerk is expended, down goes the tin plain for another spring.
Loose cnmibs jump, and gravy is agitated by earthquakes,
while hot springs hiss and sputter through safety valves.
A traveller in search of causes finds red-hot iron under the
double dish, and if he seeks further, he finds that the store of
heat was taken from the kitchen fire. But where did that
heat come from? A book in the library tells how an eiigiueer
VOL. n. z
338
DEPOSITION'.
and a pliilosoplier, wliiiling along a railway, settled the ques-
tion. They held that the heat of huruing coals was solar
heat stored np in plants during the coal-formation : mayha])
it was taken from another store. As the heater cools the
action decreases. Tliere are frequent earthquakes before
dinner ; only a few bangs after it, to rouse the sleepers.
Mayhap the February eruption of Etna, the English earth-
quakes of 1864, the sea-waves off Newfoundland, and such-
like disturbances and upheavals all over the world, are
caused by an old store of terrestrial heat and light now
hidden beneath all sedimentarv rocks in the Avorld.
Vir.. 10;i. An ouiioc of silvor, inciiaro.l at, Ncwcastlt', Dcccnibfi- li;, isc,:i. The ci-ust
icil-liot, ami newly fnizcu ; the iutciior, fluiil, partly gaseous, and white hot; the mass
eooling raiiidly in cold air. Real size. See pp. 350, 352, 358.
The arrows arc intended to show the directions in which two forces acted on shining;
hot projectiles and Inminous sparks thrown off hy tlw metnl, while tlms coolin- l.y radiatioi,
frron within ontw.inls
CHAPTEE LII.
UPHEAVAL I.
DYKES — VEINS — SUBLIMATION.
In the last chapters sediiuentary geology, palieontology, aud a
whole series of rocks, were bored through in search of light.
It would ill become one who knows so little of these sciences
to say more about them. Whether Laurentian gneiss be the
lowest in the series or not, it is low enough to prove tliat
great heat has worked with great force beneath sedimentary
beds which underlie great tracts of the earth's surface. If it
were possible to get lower, nobody could live in the tempera-
tures which fused these rocks. But thoughts may go there
safely, if they can find conveyance ; and the first step in such
a journey is to seek a vehicle for thought.
When snow has fallen on a glass roof it is possible to
stand under it and watch the snow melt. Warm breath does
not melt glass, but it warms tlie roof, and the lowest bed of
snow is fused. It is possible to feel heat flowing away
from the hand up through the glass, and to see the effect of
it on the snow above. A higher temperature would do as
much for sedimentary rocks. . A lamp placed under the glass
cracks it, and melted snow or rain drips through : a greater
heat would do as much for an igneous crust, if there be one
beneath the Laurentian gneiss. In travelling from London to
Cornwall, the edges of a geological series are passed down-
340 UPHEAVAL.
wards. Arrived at the lowest attainable bed at the surface
in tliat direction, rocks are found to be broken as the
glass was. In mines, some cracks are seen to be filled with
various metals. According to one school, lodes were deposited
from solution, and experiments made with solutions have
proved that various metals may be deposited in chinks by
passing currents of electricity through a model. Currents of
electricity do pass through the earth's crust, and the bearings
(jf metallic veins seem to correspond to magnetic currents.
So far experiment confirms a theory which savours of the old
battle between Neptunists and Plutonists, But in volcanic
countries sublimed metals are deposited in chinks ; electricity
may act on metals in the state of vapour as it does on solu-
tions. Experiments are wanting in this direction ; but metals
are found only in small quantities in solution at the sur-
face now. Other materials — dykes and upthrows of igneous
rock — fill larger rifts and holes in Cornish rocks : these rose
hot from below, but Neptunists once believed them to be
precipitates. In Scotland and in Labrador such igneous rocks
form a very large proportion of tlie whole visible crust.
Heavy metals, which fuse and sublime at very high tempera-
tures, may exist in larger quantities in deeper layers, because
they sink deep in fluid slag ; and because these low rocks
were melted.
In Lapland, at Gellivari, a vein of crystalline magnetic
ironstone is seven miles long, and about a mile broad at the
outcrop. At Rutivari, also in Lapland, is another large mass
in a wide glen ; a considerable hill is there made of magnetic
ironstone. At Danemora, in Sweden, a similar mass of iron is
(luarried. At Fahlun, the copper-mine is a vast pit, like the
crater of a volcano. About Lake Superior, in North America,
deposits of iron and copper are on a like scale. In Nova
DYKES — VEINS— SUBLIMATION. 341
Scotia, hollows iu veins of red lieuiatite are luiiig with pen-
dants like icicles. In many of the specimens of iion and
other ores exhibited in 1851 and 1862, in London, the struc-
ture of the ore suggests fusion. Gokl nuggets seem to have
been suddenly cooled while in a state of fusion ; and gold-
bearing quartz looks like burnt stone. If ores were fused
and thrown up like dykes at some places, metallic vapours
may have risen elsewhere, as steam rises through chinks in
igneous rocks in Iceland, and as iron has risen in Elba.
In Yorkshire the smelting of lead-ores caused so much
damage to vegetation in the dales, that smelters were forced
to use their wits and cure the evil. On the tops of the
Yorkshire hills they built chimneys, and from these they
made passages along the hill-sides, down to old furnaces in
the dales. Some of these passages are three miles long.
The smoke from the hearths was passed up to the barren
moors, and there it now escapes harmlessly. The sweepings
of these chimneys were found to contain valuable metals,
which oiJy did harm when out of place. These were sub-
limed at the smelting-house, and they were carried upwards
by the draught. Forty tons of lead were taken out of one
chimney in one year, and arsenic and other metals were also
swept out of the vent. At a distance of three miles, the pro-
portion of condensed metal in the sweepings nearly equalled
the proportion lower down, and the black smoke which es-
capes still carries sublimed metal into the air. In this process
the heat of a small smelting-hearth drove lead a distance of
three miles, and it will drive it much further when the vents
are made longer. It is not possible to get at the roots of
lodes, but it is easy to walk down from the chimney-top to
this smelting-house, and to look in at the fluid metal without
beine consumed.
342 UPHEAVAL.
Lead-ores contain a great deal of silver, and smelted lead
is sent to Newcastle to be refined. There it is possible to see
a working-model of an engine strong enough to work geolo-
gical upheaval, and the mechanical power which works it is
a dazzling white heat. The little engine may throw light into
the darkness of the earth's past history, and down upon strata,
which cannot be reached, beneath Laurentian gneiss.
In separating lead and silver many tons of impure metal
are fused in a row of large iron caldrons. At one stage in the
process, the temperature has to be reduced to about 550°, and
it is done by putting out the fires, by stirring the metal,
and by throwing cold water upon the fluid amalgam.*
Though the boiling point of water is 212", and the metal is
hotter than 550", tlie water does not all fly oft' in steam at
once. Spherical masses roll upon the pool of molten lead,
and these whirl and oscillate, striking and rebounding like
elastic marbles, and apparently dancing on nothing. Their
weight, or their resistance to the force wliicli supports them,
reacts upon the crust which forms under tliem, for the surface
bends where tliey rest ; but they do not touch the lead. IMany
of these are hollow shells of water, supported on a core of
steam, which is constantly forming below, and condensing
above (see p. 353).
Every now and then a water-ball as big as a nmsket-bullet
bursts like a molten shell or breaks. Fragments large as
shot of various sizes then disperse, radiating from centres,
and each fragment becomes a separate rolling spliere. Some
are hollow, some are not, and the steam-chambers vary in
size. These roll hither and thitlier on the hot pool for many
* Dcci'inbcr 16, 1863. For full s<-iciitific descriptions of this jirocosfs, see
./ Minninl of MclaUurgij, hy John A. rhillii)s, Lonclon, 18.''>"i, p. 496. See
;ilso \{vii\\ Elrmfiits of ChrwiMnj, 1830, p. 416.
DYKES — VEINS — SUBLIMATION. 343
minutes, but slowly and gradually the water-spheres diminish
in size and number ; and they all turn to steam and vanish
when they have done their work by taking heat from the
metal to give it to the air. The heat which does this work
is a luminous red heat which acts on photographic plates
like any other light. It seems to be a mechanical force
also.
If a wliite-hot bar of iron is plunged into water, some-
thing of the same kind happens. Little steam rises unless
the bar is plunged so deep that pressure overcomes resistance ;
then steam explodes and scatters the water. A wet finger
may be dipped into a caldron of lead or fluid iron with per-
fect impunity ; there is scarcely a sensation of warmth,
though the metal is hot enough to char a stick, or fry a
beefsteak. When a mass of hot iron is under the steam-
hammer, water is commonly sprinkled on it to clear it of
scales ; it rolls on the iron like shot on a board. But when
the water-spheres are crushed flat by the heavy blow of
the hammer they explode with a loud report. If a wet
stick is tlirust beneath the surface of fluid lead, or if
air is buried by splashing the pool, rapid expansion of
gas follows, and drops of metal are thrown upwards
and scattered by an explosion. If water is thrown on
metal so far cooled as to admit of contact between the two
surfaces, then water takes up heat and turns to steam,
while the metal darkens. In a short time more light from
within supplies the loss of "steam-power," and the metal
brightens. As a hot poker and a wet finger are protected by
gloves of steam from contact with cold water and hot metal,
so water-spheres are guarded and supported and shaped by
the steam which forms between cold water and hot metal.
Hollow spheres float on steam atmos})]ieres, and both are
344 LTHEAVAL.
repelled by strong heat. So heat-rays are force, and the
brightest are the strongest.
But when this ray-power does not equal the opposing
weight-power, as in the case of the blow struck by the steam-
hammer, the fluid sinks through its vapour, takes in a full
charge of heat from the metal, and bursts into steam. Strong
heat, light, or ray-force, may keep two heavy bodies apart in
spite of the whole force of the earth's attraction at its surface ;
repulsion and attraction do, in fact, shape fluids into hollow
sphen^s.
While under these S])ecial conditions, tlie order of the
water series was—
Cold. Dark. Downward force. Attraction.
Air iuul steam.
Thick shell of water. \ i Fluid, less than \
Steam core. , ^ ■ Gas, more than > 2 1 2°.
Thin shell of water. ) ] ( Fluid, less than j
Air and steam. ) '
Heat. )
Crust of lead, dull red. Plastic .solid fieezing.
Melted lead and silver, .v^/vn, Fluid, about 550°.
Heat and bright red light. Fuii;e. Upward force. Repulsion.
The arrangement is unstable, and can only endure for a
time ; but while it lasts the earth's attraction is overcome
by UEruLSiON. A central sphere of hot gas in a .shell of colder
fluid is possible ; to make it last, the centre of gravity and
the centre of heat must nearly coincide, and conthiue so to
coincide. If it so coincides while the mass cools, a drop of
water may become a shell of ice, or a hailstone, or a snow-
crystal, with a structure radiating like rays of force ; but a
drop resting upon a plane is sijueezed out of sha])e by weight
and I'csistance.
The temperature of 550", which tluis changes tlic form
DYKES — VEINS — SUBLIMATION. 345
aud condition of water, is only the freezing-point of pure lead.
At 550° the metal crystallizes like water at 82". Small crystals
form in the mass, and float up like ice forming in a freezing-
pail, others sink like salt. If left to themselves these crystals
form a crust; if stirred they melt, and disperse and crystallize
again.
More crystals form as the temperature falls, and many
sink, for lead is heavier than silver. Some form and stick on
the cooling sides of the vessel ; some unite ; lead and water-
ice alike freeze on iron spoons which are used to stir a freez-
ing mess, for iron is a good conductor. In one case a mea-
sured scale marks 550°, in the other 32°, or 28°, or 14'\ as the
case may be ; the shapes of the crystals differ, but cooling obeys
the same law in this metal amalgam and in salt water. When
crystals form rapidly in the lead, a great iron strainer is
plunged into the pot, and it strains and gathers out a spoonful
of dry granular lead-ice, from which the wet drains and
trickles away. The lead-sludge is thrown into a caldron to
be separately cooked, and passed along the row of caldrons ;
the fluid is left to be enriched, for in that fluid is the silver.
The freezing point of silver is far higher than that of lead ;
Lead melts . . 612"*
Silver . . . 1873"
it takes longer to part with the heat which keeps it fluid.
As water and brine are separated by crystallization at or about
freezing, so lead and silver are parted at or about 550°. As
brine is strengthened by adding brine, and by taking fresh-
Avater ice away, so a pot of metal is enriched by adding a
mixture of lead and sih'er, and Ijy taking out crystals of pure
* There is no certain measure for high temperatures. These anil other
figures are quoted from works of authority, or from statements made by prac-
tical men.
. tliiu Lead crust.
Lead and silver.
v>>v\/v^
o
. about 550".
Kay-foicc.
34G Ul'IIEAVAL.
lead, wetted with liuid aiualyaui. ])uiiiig the cuuliiig of these
metals the upper series is —
Cold. W.ij,'l.t-f..r...
Solid
Fluid
Heat
As cooling goes on a crust forms all around, above, and
below, and against the sides of the iron vessel ; wherever rays
of heat escape; most where they escape most; and a Huid
core is left at last, A large round drop, composed of these
metals, and cooling in space as they cool in a cup, would have
a crust of frozen lead and a hot core of lead and silver, partly
fluid, and crystallizing while cooling by radiation.
When this solution of silver in lead is strong enough,
more heat-povv^er is brought to bear on the mixture, and the
metals work on a different plan. They boil.
Melted amalgam is ladled i\\n\i a pot into a large cup,
made of bone-dust, and hot air and a strong flame are made
to play on the metal surface. The mess sectlies. Thick
fumes of leaden steam are driven off, and fly away, with hot
air and coal-smoke, through the chimney. In Yorkshire
such fumes fly three miles and more. Lead and oxygen com-
bine, and when combined, they stream through the bone
filter as melted litharge ; or they float on the silvei', and flow-
over the edge of the cup. 15ut the boiling point of silver,
like its freezing point, is higher than tliat of lead, and fluid
silver is denser and heavier than fluid litharge; so, while lead
evaporates, and litharge floats and flows away like slag, silver
sinks through the lighter fluid and floats on the strainer, and
the rich broth grows rielier still. As tlie lead boils oil', more
and more of the stock is ladled in, till the " daintv dish is fit
DYKES — VEINS — SUBLIMATION. 347
to set before a king ; " aud then, with an extra force of heat,
the last of the lead is driven away, and the silver-plate is
cooked. The bright metal clears up like the sun breaking
through mist ; and it shines.
In water, lead, and silver, like effects are produced by
various temperatures. The heat which evaporates water
freezes lead ; the heat which evaporates lead only melts silver ;
the force of electric light drives them all away in fumes. At
the highest of these temperatures, and at the pressure of the
atmosphere at the earth's surface now, water, lead, and silver
are gases ; all three are solids at 32°.
Mingled together, and cooling, these fumes or gases would
condense in order, or combine and condense in some new
order. Silver would sink in a fluid oxide of lead. Litharge
would flow on tlie top of red-hot silver, and form a crust of
oxide when it cooled, and water would become ice upon the
heavier solids only after they had both fallen and frozen, and
cooled to 32°. Till that point was reached there could be no
rest for water, for heat would move it in escaping from the
hottest, lowest, and heaviest, through the highest, lightest,
and coldest of tliis series of three fusible solids.
The " working" of this engine is a thing to be seen. It
was seen in Edinburgh class-rooms, in Spain, and elsewhere, in
1839 and 1842 ; at Newcastle it was seen again with a purpose,
after seeing Vesuvius, Hecla, and the Geysers. Seventeen
thousand ounces have been refined in one cake by Pattinson's
process, first invented in 1827 ; 9000 ounces make an ordi-
nary charge. It is a pool four inches deep, two feet and a
lialf wide, and charged with from 1700 to 1800 degrees of
temperature, ami it is a powerful little engine to work wp-
heaval. The pool is perfectly fluid ; it shines with a bril-
liant white light of its own, and reflects other liijht like a
348 UPHEAVAL.
polished mirror. When the hot breath of the furnace plays
on the surface it ripples like water ; when the cup is shaken
tlie sliining mirror is broken up into waves ; when a white-
liot cinder falls on it, rings spread as they do when a stone is
thrown into water ; when the temperature varies within the
cooling mass, gentle currents move hither and thither, and
glowing embers drift on them like fire-ships on a calm tide.
The fluid surface is smooth as glass, and still when undis-
turbed, for silver, quicksilver, and water, when melted, all obey
the laws which govern the movements of fluids ; but of these
three only the hottest shines. A constant play of colours and
a maze of curves play on the surface with every movement
and breath of air. Like a soap-bubble, or oily hot water, the
fluid shining silver has a thin varnish in ra])id movement,
which refracts and distorts the rising light.
There is a great store of latent force in the quiet silver
pool ; it shines, and there is hot oxygen locked up in it.
There is gas ready to expand, and ray-force only waits for
resistance to show its power.
With cold the resistance conies, and the battle rages.
When tlie silver is pure the fire is extinguished, and
freezing speedily begins. First a few crystals form on the
surface, then a network, then a thin skin. If a bit of cold
silver is tossed in about this stage, it floats like a small ice-
berg, and gathers a thin raft about it. The silver-ice may
be pushed about, for it is a floating body ; anil if pushed
down, it rises again high above the fluid. It stands liigher
than ice in water ; far higher than solid lead in fluid lead.
Every point seems to act as a way for heat to escai)e ;
the floats soon take root by spreading below ; and so they
grow and spread, as icel)ei'gs do, in freezing water. At this
stage the lusti'e of raised jxiints fai- exceeds that (tf smooth
DYKES — VEINS — SUBLIMATION. 349
plains ; the rough solid hills are white, hot, and ' tell' light
against smooth thin crusts in the lower regions. These tell
dark in this general blaze of light. "\Mien the cooling has
advanced to a certain point, and a pellicle fomis all over,
a stream of cold air is hlown in to hasten the cooling.
Then the lustre changes from dazzling white to red, the upper
crust thickens, and the action becomes rapid. Molten silver
is within; it is compressed by the forming shell, and hot
oxygen is squeezed out of the mass. The surface at this stage
begins to break up and bubble ; it is upheaved ; silver escapes
where resistance is least, generally near the edge, where the
heat of the cup keeps the crust thin and soft.
At this stage the light of the surface changes colour
rapidly, ^\^^ere the hot interior finds a vent, it is still bril-
liantly wdiite ; where the crust has set, light is bright red ;
where the crust is thick, it is a dark cherry red. Hills now
tell dark against lighter coloured lower grounds, and the
brightest spots are hollows in hill-tops and boiling holes in
the plains. There is great variety in light which shines out
of hot silver while it is freezing, and the same is true of all
other materials which have been w^atched. This light, like
sun-light or any other light, may be refracted and reflected :
a lens forms an image of the silver on a screen ; the image
formed on the palm of the hand is sensibly hot. The metal
is giving off light and heat, wdiich produce their usual effects
at a distance. Similar rays made water-spheres revolve above
dull red molten lead, and white-hot solid iron. The silver
plate is a self-luminous body, like the sun, for the time.
To prevent loss from boiling over at the edge, the work-
men commonly prick the silver plate in the middle ; they
break holes in the ice, and the silver pool wells up like water
in a pond. Then comes the time of rapid upheaval and
350 UPHEAVAL.
disturbance. IMts ui' broken crust rise and tall like tlie
lid of a box, and lutt springs of boiling silver gush out
in shining fountains of glittering light. They freeze as
they overflow, and hollow pillars rise up, growing like
the trees of Aladdin. They rise and grow and branch, and
shed a crop of silver fruit, till they reach the point where
the pressure from without equals the force within, and then,
Avhen the weight equals the heat, when the column of fluid is
balanced by the gas, the tube is sealed by a silver dome, and
that well in the ice is frozen.
All these quaint forms are casts of ray-force. Motion is
arrested suddenly, and fountains are caught flying.
Larger holes give rise to larger tubes, through which boil-
ing silver splashes out. Tubes grow into truncated cones,
and these as they rise gradually narrow, till their limit is
reached. Then they too cool and close, and a silver volcano
is plugged with frosted silver. When the cone is finished, and
tlie vent stopped, smaller vents open in the plain ; and from
these a crop of tubes and cones grow, till a range of hills forms
on a frozen silver sea. There is scarcely a mountain form or
fantastic lava-shape in Iceland, a branching shape in a metal
vein, or an ice-form oft' Labrador, that may not be thus copied
in freezing silver.
Throughout this period, the explosive force within casts
showers of spherical drops whirling into the air, and each of
these for the time becomes a separate system, moving in
obedience to the laws which govern projectiles, and working
itself into shape, because it is moulded by two opposite forces
in obedienc6 to the laws which govern force. These sparks
work in the air, as they fly, while the parent plate works
in its cup ; and many of them cool as hollow shells about
cluunbered intciiois.
DYKES — VEINS— SUBLIMATION. 351
For a full hour a plate of 9000 ounces coutiuued these
displays of volcanic action ; the charge of heat raised
mounds of silver more than six inches above the surface,
and threw silver drops to a distance of more than two
feet. At last the whole mass froze, and then the rapid action
ceased.
But though violent boiling ended then, so far as silver
was concerned, there was still a great store of light, heat, and
force in the solid. The light was cherry red in the hollows,
dark red on the hills, and the light which the crust reflected
was pure. The heat was still felt at a distance, the lustre
was seen in hollows and cracks ; and water thrown on boiled
furiously, or danced as it did on hot lead.
Tlie frozen plate was dragged from the furnace at last and
weighed, and then it was cut into junks with steel chisels,
and heavy sledge-hammers wielded with a will by brawny
arms. It took a great amount of physical force to quarry
this work of heat and cold. The internal structure was sliown
in the section. The mass was hollow, chambered and crystal-
lized like slag, or Icelandic lava, or glacier-ice.
If one of the numerous spheres which were thrown off
by this plate were the subject of inquiry and out of reach ;
if its path were known, its surface seen, its size measured, its
density calculated from its movements, its light analysed, and
its composition unknown ; the data would not give pure silver,
because of the spongy structure of the mass. If planets are
made on the same plan, philosophers may have to revise some
of their conclusions as to other worlds.
When remelted and run into bars and ingots, the silver
takes less room, and has greater density, though many ingots
are chambered still. "When stamped and hammered, the
metal has still greater specific gravity, greater density. It
352 UniEAVAL.
is the same substance, diff(>rciitlv packed by natural iiiecliani-
cal force and by men.
Like tlie water and the lead, the cooling mass, during
l^art of the process, was a solid shell with a fluid core, and
during that time force worked most upheaval. The free pro-
jectiles were spherical, with crusts roughened by radiating
pn)jecti(jns, and with spongy cores.
A world arranged as a core of hot gas in a shell of fluid,
with a solid crust, is possible ; because that arrangement
always recurs in making this experiment. It always results
in certain outward forms, and these endure when the action
has ceased, to show what the nature of the action was. But
till the engine was seen to work, the forms had little meaning.
A portrait of a "specimen of pure silver" is on page 338,
and it was thus prepared : — a bent iron point was dipped into
the silver and came out red-hot, with a frozen crust of white-
hot silver-ice upon it. By dipping, this grew to be a smooth
shining hemispherical half-frozen button, and then it was set
to freeze in a draught. It cooled as the large plate cool(>d
afterwards, but suddenly ; and the fluid interior burst vio-
lently through the crust : the fountains froze as they flew ; and
strange shapes resulted from their movements, and these from
forces. Gravitation acted downwards towards the earth's
centre : radiation from within the silver outwards in all direc-
tions : expansion acted from within, contraction from without :
the radiating forms were casts of distorted rays.
The duration of the rapid action was in proportion to the
size of the mass. A spark cooled as it flew. An ounce cooled
in a few moments. Nine thousand ounces worked for an
hour after the fires were drawn. Seventeen thousand ounces
worked for a much longer time ; the mduntains wert' far larger
and higher, and the erujiliims threatened to blow oll'tlie 1>rick
DYKES — VEINS — SUIiLIMATION.
353
roof of tlit^ arched furnace, tlirougli wliicli a window was opened
to let spectators see tliis silver light do the work of ray-force.
The violence of the action was in proportion to its rapidity.
A charge of force had to be expended, and it escaped cpiietly
and slowly, or suddenly and with explosive violence. A small
mass suddenly cooled, burst, or threw up high projections in
])roportion to its luilk. A like mass more slowly cooled,
worked for a longer time, but did not work exjjlosively.
Of three masses of unequal size — a drop, an ounce, and the
parent mass cooling together in the same temperature — the
smallest cooled first, and had the highest projections ; tlie
larger cooled next, and the largest last.
The first was cold and only reflected light when the second
was still working, and shining through cracks and holes in
its crust ; the third was working and .shining, shedding light
and heat on the other two, Avlien l)oth were cold and dark.
That shining silver plate is an engine on which thoughts
may travel a long way, in as many directions as there are
rays in spheres of light and gravitation.
Solid
Fluid
Metal
Heat and bright red light.
UpTvard ray-/oree.
Repulsion.
CHAPTER LIIT.
ri'IIKAVAL 2— -];AYS and weight 2 — FUSION AND FliERZINU —
METAL AND SLAG.
When so many roads are open it is hard to choose a path.
If light he visible force, the diameter of the sphere within
which it works is twice two of the greatest distances yet
measured from this world to another star ; for light, if it
shines thus far from a ]ioint in space, nmst shine as far in
other directions.
Space and distance on this scale must be left to astrono-
mers. A shorter path will lead a student to the nearest fur-
nace ^\•her^! metals are fused, and there he will hud amplr
room lor him. Stars though visible are out of reach ; our
own little world is too big to be seen ; but at a furnace it is
easy to see and to think ; — to watch small shining bits of our
world fusing, boiling, whirling through the air, freezing and
falling ; to see small work done during minutes, hours, or
days, and to think of material things obeying the same laws
during all time. The scholar may learn one more aljjhabet of
Ibrni Ijy watching solids, iluids, and gases, which are parts of
a great whole, fusing, and freezing, and taking shapes from
forces and their fixed laws.
If any laws govern all matter, tliey ap])ly to all (quanti-
ties, times, and distances alike ; to the lenst as to the greatest,
FUSING AND FREEZING. 355
to sparks and to worlds. Gravitation seems to be a law
which applies to all visible material things ; if visible light
be an opposing force of like general application, these two
may have shaped worlds in obedience to the laws of the
great Lawgiver who made this round world like a little drop.
Modern astronomy rests upon gravitation, which is a law
discovered from the movements of projectiles large and small.
AVliirling worlds and still larger systems of worlds all seem to
obey that one force. If they obey two, and if light is one of
these, a knowledge of a second law may grow from little things.
If natural philosophers will deign to study rubbish by furnace-
light, and make experiments, they may learn to follow ray-
power as far as gravitation in time. That is a way which lies
open beyond the short path which leads to the furnace.
Let a few familiar examples suffice to explain what is
meant by "ray-power." The subject is too large for unskilful
hands and minds to grasp. It is dangerous even to step on
such untried ground.
Gases, fumes, steam ; fluids, hot water, lavas, and suchlike
hot materials are now escaping through sedimentary and
igneous crusts. Since this part of these volumes was first
written, two volcanic eruptions have taken place in Sicily,
one, at least, in Iceland ; the sea Avas disturbed off Ncav-
I'oundland in 1864, and England has several times been
shaken by earthquakes. If lavas make large hills above, they
must leave large hollows below the crust ; it is impossible to
get at these halls, but perhaps they may be seen through small
holes, made on the same plan, by the same working giants,
with the same materials, in small igneous crusts. Chambers
abound in all frozen crusts, and frozen slags are made of
fused rocks ; if geology cannot quarry through the earth's
crust, let her stutly where^'er she can, and begin with slag.
35G rniKAVAL — RAYS AND WEIGHT.
('li;inil»ers in a solid aic avcII so(_-n in Wcnliaiu Lake
ice, in iniimrc ^lass, and in iVozen soda-water within
a bottle, which is a transparent crust of impure glass :
hollows like these may be found by breaking or cutting
through bread, biscuit, pie-crust, plates of sulphur, seal-
ing-wax, tallow, ingots of various metals, and plates of slag
^\■hich are opa(|ue. Larger hollows, of like shape, abound in
lavas which were fused, and whose history is known ; in ores
and in rocks, whose history is not so well known; but many
of these rocks certainly were fused like the slag. Similar
but far larger chand)ers also abound in the crust, from A\'hich
lavas rise and stones are quarried. V>y watching at a furnace,
the growth of a chamber and some of the resulting phenomena
may l)e seen, and the lesson seems good for geological appli-
cation. Many chambers were formed during the freezing
of the Newcastle silver plate (chap, lii.) ; one large steam
chamber, and many small ones, formed in the hot-water sphere
(j). 353). Because outward forms in volcanic countries re-
semble those which always result from the boiling and freez-
ing of water, slag, metals, and other materials, the inward
structure of any frozen crust throws light into dark chambers
under ground. Of several volcanic mountains of like shape
the smallest may be seen to grow, and may be broken up to
see the structure ; or a transparent glass mountain may be
watched while growing, and can be seen through when it has
grown. The best teacher of natural science is experiment ;
so the growth of forms on the earth's crust may perhaps l)e
learned in rubbish heaps by furnace-light.
Silver, cast-iron, mercury, metals, slag, and glass are
smooth and ' flat' as water and other fluids while fused. The
surface for tlie time is like the surface of the sea, part of a
s]i]i('re at the end of a I'ay : it is like a bit iA' a wheel at the
FUSION AND FHEEZING — METAL AND SLAt;. 357
cud of a spuke, ami it takes its shape from gravitation. A
freezing fluid takes many shapes. If slowly cooled, it is Hat
and smooth like ice on a p(jnd. Furnace-refuse left to cool in
the air sets in layers, which would he arched crusts if they
reached to the horizon or covered a sea. But many of tliese
concentric layers are bent and shattered ; projections of various
shapes are on the upper surface, chambers, passages, and holes
are within. Cold slag is like the silver-plate which was seen
to work, and silver hollows were tracked to the surface where
a mound was seen to grow ; to a student wlio knows this
silver alphabet, the outside of a plate of cold slag tells a his-
tory : like the cover of this book, it gives some notion of the
contents. The furnace gives a ready answer to any one wIkj
seeks the meaning of a new form — a new letter in the slag
alphabet. The small heat-engine is at work, and the tool-
marks of ray-force may be learned in that small source of
light, a blast-furnace.
It very soon appears that outward forms record move-
ments in freezing fluids : movements caused by opposing
forces, whatever the freezing or boiling points of the fluids may
be. In chap. viii. an attempt was made to show how trans-
parent water moves, and why. Transparent glass moves like
boiling water, and for the same reason o[)a(|ue slag, whik'
fluid, is mo\'ed by the same forces acting mure power-
fully. The fluid obeys tlie law of gravitation like any other
lluid ; it falls and flows ; and, like other fluids, it boils
and rises when the other force gets the mastery. The out-
ward form of the frozen solid is a record of the struggle, ai d
such forms are l)uilt about rays. The axis of a mound in
slag is perpendicular to the plane of the horizon ; so are the
axes of volcanic mountains set upon the tire of a wheel iliawii
in any direction I'ound the sphere of the woi'ld. In a laic
358 UPHEAVAL — RAYS AND WEICIIT.
book wliicli gives sound information from behind a comic
mask,* it is stated that the edge of a crater in Mexico was
criiwnt'd M'ith icicles pointing upwards. Tliey ^^■ere forms
l)uilt about rays, and prol)ably grew from vajwur caught and
I'rozon \\'hile rising out of tlie bowl. Hoar-frost so forms on
posts, gates, rails, and trees, near wet groimds in England ; it
so forms on the edge of a bowl with water in it ; and in
colder regions, as on the Wliite IMountains in North America,
larger " frost-work " grows about rays which meet within tlie
substance on which the crystals form.t If water condenses,
the form grows by deposition about rays. If w^ater, silver,
glass, metal, or slag freezes slowly and gradually, the crust is
flat and even ; if it cools rapidly or suddenly, the crust is
\meven, and the forms either aim at the eartli's centre, or at
some other point or line about which they grew during a
struggle. In order to catch the meaning of outward forms
thus produced, they must be seen to grow ; they must be
watched, as the silver-plate was at Newcastle.
The cut p. 338 is a portrait of a specimen of pure silver,
which cooled as described above (p. 353). The arrows show
directions in which two forces acted : — Eays from points and
lines within bright hot masses of freezing silver, outwards ;
weight, attraction, gravitation, or some other opposing force,
downwards, towards the earth's centre, like a plumb-line ;
inwards, towards points and lines whence the ray-force
diverged. Such forms alone suffice to explain their growth
when that alphabet is learned ; and slag-forms aw like them
in this respect.
Certain glass vessels are frosted by plunging tough red-
l-h-.to^ri-aplis pul.lislh'd ut New York,
* Tr,
'(irh.
l.y rial
>ni. 1S(;4.
t lu
"■ '•"!
lies (if tl
hcsc l-oniis
lit-li 111
uy l.r
]iun'lias
,m1 in I.on.
FUSION AND FREEZING — METAL AND SLAC;. 359
hot glass into cold water. Steam carries heat rapidly from
the outer layer, and a hard shell forms suddenly. It shrinks
i-apidly and unevenly, breaks, and the bits curl up, while the
hot layer within sticks to the shivered crust, and rises through
a network of cracks. The rest of the cooling goes on slowly
in heated air, and the finished work is smooth within, but
rough, like broken ice, outside. The inside was shaped by
air blown in through a tube ; and if a glass-blower wants to
make a large chamber, he blows in drops of water, which turn
to steam and expand within a tough glass boiler. It expands
like India-rubber, but does not shrink, for it freezes hard.
The structure of transparent glass, and the shapes of chambers
thus formed in it, can be seen through the solid walls. A
soda-water bottle will serve for illustration, and the lesson
may be learned at any glass-house.
In the case of the silver plate, a gas (supposed to be oxygen)
was imprisoned in a fluid, and it acted Like the breath of a
glass-blower. Some of the gas escaped, but part of it was
caught and imprisoned within solid walls of silver, when the
metal had set. In all cases and in all dimensions like action
ought to produce like results. Steam bursts hollow spheres
of water, which dance above hot metal (see p. 353). The
gas either bursts a prison or the prison- walls take the shape
of the imprisoned gas. In the latter case, the chamber is a
cast of the forces which expanded the gas and compressed it.
When a stream of iron flows over wet sand, steam forms and
expands beneath ; the fluid iron upon the sand bubbles like
the boiling water beneath it, and part of the steam bursts
through ; but air and steam are often caught in the freezing
plastic iron while rising through the tough mass. Each hollow
prison then takes the shape of the struggling prisoner. It is
a hollow iron mould of the f(jrce which expanded steam and
360 UrilEAVAL — ItAYS ANT) WEIGHT.
the force which contracted iron ; the shape of it records tlie
struggle for mastery between attraction and repulsion, which
ends only when the two are balanced. But when the prison
has cooled, and steam has condensed, the weight of the whole
atmosphere tends to crush the walls through which imprisoned
heat finds a way. Domes thus formed on blistered steel, hollows
in cast-iron and in other metals, are often crushed and bent
inwards by weight. So ray-force and weight-force together
shape this crust. Things which cannot escape — air, and
water, and other substances — often line such hollows witli
crystals, and so leave open spaces. Other clianil)ers have
porous walls, and the hollows are filled from without long
after they are made ; as caves and mines are partially filled
with ice in cold regions. A slag crust is like the rest : when
suddenly cooled, it is shattered or distorted. Thick plates,
which have long ceased to shine, often burst asimder on the cold
floor of a smelting-house ; and when they do, red light, or the
brighter light of fusion, shines out from the centre of the mass.
Tliough metals and slag are opaque, tliey may be seen
through by the help of air, water, ice, and glass, and l)y tlie
forms which they assume wliile fi'eezing. Perhaps tlie crust
of the earth may be seen through in like manner, by learning
the meaning of outward forms in slag and lava. Luminous
heat expands steam, which moves the lid of a kettle, or
moves the largest engine ; the same force blows a glass bottle,
makes a bubble in metal, and bursts the chamberetl slag
crust, which is made of fused rocks. The same heat melts
lava, and the same forces which shape crusts on lava and
slag may have shattered the earth's crust, as a workman
shatters the crust of a glass Jug with cold water.
The writer spiait much of his childhood amongst rocks
and furnaces, and there gleaned itleas which are now packed
FUSION AND FREEZING— METAL AND SLAG. 361
ill these volumes. One great ploy was to clamber amongst
sea-cliffs, another was to see iron " run." That is a sight
which hears frequent repetition, though many visitors only
see tlie dirt and feel the heat. Turner thought the colour
worthy of his brush, and failed to copy it. Guthrie saw it,
and preached a sermon about it — and even Guthrie failed to
describe the scene. Till bruslus are dipped in light, and
words are real fire, the scene cannot be thus brought home.
But any one who chooses to take the trouble may see a
smelting-house for himself, and a student of natural philo-
sophy will find occupation there. In Lanarkshire, the sky glows
at night with the flaring red light of great fires. They
glow in hollows, and shine from distant hills like stars or
beacons, and the red flames which glow on the clouds leap up
and sink down, panting with regular pulsations, like living
things. Each of these lights may be reached by following a
ray ; and each is a centre of active work, in every sense of
the term. There steam-engines clank, and whistle, and yell,
while men rush hither and thither with iron carts, rattling
over iron-plates, with loads of fuel and iron-ore. These tilt
their loads of stones dug out of the earth's crust into conical,
tall furnaces, whence the light shone upon distant hills and
clouds.
A roaring blast of hot air is blowing furiously at the base
of a heap which grows from above, and the heap burns and
melts. A snow-heap melts below when it rests upon warm
earth ; but here the heap is made of the crust itself. At
Woolwich a heap is made of old iron. The workmen heave
in shot and shell, clanking chain-cables, anchors, old rails,
nails, hoops, clippings, and filings ; with a " one — two — three
— heave;" in goes an old rusty gun which has fought and
gone out of fashion, and down it goes with a crash ; and so
302 UPHEAVAL — RAYS AND WKICIIIT.
the iron heap grows to be a pile oa a hot base. Snow, iron,
and stone, down they all sink alike w'hen they melt ; and
when a charge is fused the base of a furnace is filled with a
fluid, which takes the shape of the cup which holds it, as
snow-\s'ater takes the shape of a lake-basin, or the sea takes
the shape of its bed. But here two separate fluids float on
each other, like oil on water ; one is heavy iron, the other
lighter stone.
The lighter fluid is constantly drawn off, so a river of slag
is pouring all day long from the base of each fm-nace. It is
a miniature lava-stream, and it teaches a lesson which may be
used elsewhere. Morning and evening the heavier iron is
" run." With long l)ars and heavy sledge hammers, bi-awniy
half-naked men attack the base of the hearth. They strike,
and push, and heave with might and main ; and break, and
drdl, and quarry through an outer crust of fire-brick burned
hard as altered rock in a suigle day. The hand may rest on
one side of the brick ; but as the quarrying goes on, a red
heat, tlien a white heat, and lastly the bright light of fusion
is reached. Then out bursts the flood, glowing and shining,
flowing like a river of golden light, scattering a spray of shoot-
ing stars, which hiss and fly and vanish like firewcn-ks at
a festival, or meteors in the sky.
It is a period of rapid action in iron, but it is a period of
short duration at a lurnace. Moulds, called the " sow and
})igs," are prepared in sand ; they are shaped like great ccunbs,
and down these trenches the golden river pours, boiling as it
flows. The light changes at every moment, and the move-
ments change like it. Stars soon cease to fly and shine,
but darker droi)s are thrown up when the metal l)oils, because
air and steam are escaping through it fi'om tlie saud. As
each comb is filled, a clay plug turns the stream, and when
FUSION AND FREEZING— METAL AND SLAG. 3G3
tlie whole cliarge is poured out, the saud floor glows with red
iron-ice formed in ditches of sand. Within a few hours, this
ice is " pig-iron," and by next day it is cold. Cold iron floats
on fliud iron, as ice floats on water.
The forms below are casts of the mould, the upper forms
are casts of the forces which made the iron boil and freeze,
and a broken " pig" shows the inner structure of such a mass.
The case of the silver plate is repeated, and like forms recur
in iron thus manufactured in Lanarkshire and elsewhere.
At many furnaces, the operation is carried a step further.
The pigs are melted again to make malleable iron, and the
fluid is run into large moulds.
When the furnace is tapped, iron and slag pour out to-
gether ; a bright, shining, double river of metal and stone.
It curls round corners, falls over shelves, forms pools below
the falls, and eddies like any other stream. The fisherman's
instinct knows the very spot where a salamander might find
good resting-ground, if there were such fish in that glowing
pool ; there are the very eddies and whirlpools which a wading
fisherman sees meandering past his legs when he wades out
for along cast (p. 225), the eddies which curl behind every post
in a stream of water or air (see vol. i.) But this is a double
stream about to freeze, and form a double crust. When the
mould is filled, bright colours play about the surface ; then it
darkens and curdles, and winds sluggishly as the slag begins
to freeze. Floating stone bergs form and move about as
froth floats on a river ; as icebergs float on the sea ; a crust
begins to form on slag floating on iron, as crusts begin to
freeze on water, on glass, lead, silver, and iron ; and in a few
minutes the slag-crust sets as ice did on the St. Lawrence
when it set this winter. This is the slag period of violent
eruption, the crust breaks, and the fluid core bursts, or wells
slowly up through chinks and round holes, which glow and
3G4 UPHEAVAL — I'.AYS ANH WEIGHT.
sliinc brightly in the red-hot ice. The main stream Hows oil
below, and pours over from pool to pool as before, but the
upper crust coutiuues to grow ou the surface. Flaring sparks
Hy through open chinks, and when caught and cooled they
are cast-iron spheres, with uneven surfaces, and a crust of
oxide. The iron stream below, hotter and heavier than the
upper stream, gradually cools and stagnates as pig-iron did
alone. The stone islands of the upper crust grow together,
and join and form a red-hot solid plain, and though the iron
is hid in this case, the lower crust certainly forms as it formed
in sand when it was the upper crust.
When the iron freezes the slag contracts, darkens, breaks,
and rises into miniature mountain-chains. The first surface,
with all its cones, curves, and wrinkles, and the whole series
of crusts which formed under each other, rise and fall together
slowly ; and all the phenomena of geological upheaval result
from this stage of rapid cooling, in slag resting on cooling
iron. When the iron stream has frozen solid, the upper crust
remains shattered, distorted, and angular ; but also bent, folded,
twisted, and chambered ; it bears the marks of fusion and of
freezing on the surface and in every section, and all this small
work was seen in progress so far. In these two crusts the
time of rapid action ends when the fluid becomes solid, but
there is still a great charge of mechanical force in the hot mass.
The next step in the manufacture is to turn on a stream of
watt;r, and violent action is renewed at once. The water sinks
into the chinks, and rises with all the borrowed power of that
tamed giant steam. Motion which had almost ceased begins
again more violently than before, because this third fusible layer
is more easily boiled, and harder to freeze than the other two
below it, A red heat scarce sufficient to raise iron and slag l)y
ex])anding the solid, throws a broken crust hither and tliiflicr
Ity the help of steam and boiling water. Tlu' solid layers wliicli
FUSION AND FrxEEZlNG — METAT; AND SLAG. 305
lieat the water, cool, contract upon liotter layers within, break,
and let water sinkdeeperto hotter regions below. Steam rushes
up, exploding, hissing, sputtering, scattering broken frag-
ments, tossing heavy plates into the air, bursting chambers,
grinding edges, rounding corners, driving jets of boiling water
high into the air, and filling it with rolling clouds and
Mdiirling drops. At this stage it is hard to see what is going
on, but there is a violent commotion ; and the igneous crusts
are broken up, and partly ground by steam-power, which
gradually wanes, while the iron parts with the charge of ray-
power, which came with it out of the furnace, out of the coals,
out of the sun, if George Stephenson guessed right, or out of
the cooling earth. One very common occurrence about this
stage is the sinking in of the roofs of chambers. The iron con-
tracts, and the slag roofs fall down. The decreasing action is
not regular ; it diminishes quickly at first, very slowly and
gradually at last, in proportion to the ' energy' expended.
The amount of ray-force spent on clouds of steam, in heaps
of sediment, or in hot fountains, is deducted from the store in
the mass of hot iron. Boiling springs sink, lower and lower,
those which spouted two feet rise only one, and after a time
only rise a few inches ; next they well up slowly amongst the
ashes ; and at last the water circulates cpiietly as warm water
does in any vessel, as air does in any room. This hot-spring
period lasts for many hours. There is no visible light, no
violent action, but the power is not all spent, and it was
bright heat at first. At this dull heat ether boils furiously,
and the iron below still has work in hand.
If the water gets to the lower side of a large ingot, so as
to cool that side first, the whole mass bends upwards like a
bow ; and all the upper formations rise upon the arcli, steam-
jets, hot springs, and all. Sometimes an ingot a foot thick
breaks short off like a carrot from this uneven contraction
•■^ni) UriIEAYAL — RAYS AND WEICIIT.
and expansion, and so makes a ' tanlt.' It is the case of the
frosted glass over again, Imt on a larger scale. AMien Loth
sides are at one heat, the bow unbends, and the mound sinks
down slowly. When the upper surface cools, the ends curl
up like a shaving of whalebone laid in a warm hand, or like a
tiat fish laid in a frying-pan. No matter what the substance
may be, expansion and contraction work the engine, and the
same forces must work that larger engine — the earth's igneous
crust — if there be one under sedimentary rocks. Thus at the
end of a short time a bright stream, flowing like a river, and
scattering drops like a spray of light, is changed into rigid,
solid crusts, of metal fit for human use, and of slag only fit
for tlie cinder-heap. The mass stands in water thick with
sediment, which falls in time — a small geological formation of
fusible sedimentary beds under w^ater. In frosty weather the
water freezes in turn, and in very cold weather that crust
splits like the other two. A stranger who had not seen these
changes take place, might find it hard to believe in the wild
vagaries played by hard, cold, ugly, wrinkled, dark-gray solids,
resting in their cinder-heaps now, but lissom and active,
strong and bright, in their vigorous hot youth, when their
bright faces were smooth and soft, before they froze.
When iron ingots and plates of slag thus cooled are broken
up, the shape inside is explained by the movements observed,
and shapes outside can be referred to tliem. The silver plate
was a costly toy, and can only be seen to M-ork at a few
places ; slag-plates are piled in hills and cost nothing.
Lanarkshire roads are made of broken slag. In such a
path, at a hall door, the writer gathered the first-fi'uits of this
branch of education, and there he made his first collection of
igneous rock-forms. Any other child may do as mueli, and
the wisest of pliilosophers may pick up kn(i\vledg(! in tlie
p itli wliich leads to the nearest furnace whence liglil shines.
CHAPTEli LIV.
.SPARK8 — VOLCANIC BOMBS — M ETEORITEH.
If a reader who lias followed thus far, or who happens upon
this page by chance, will look Lack to the " contents," he will
find that this hunt has run a ring. Those who have followed all
the way — if such there be — have been to Spain, Italy, Greece,
Switzerland, Scandinavia, Spitzbergen, Iceland, Greenland,
and America ; all round the British Isles ; high up in the
air, and down through water into the earth, with miners and
geologists for guides. The quany was viewed in the last
chapter, and it went to ground in the cinder-heap whence it
was started. The quarry was terrestrial light, and it is im-
possible to follow it deeper by any direct road.
If a geologist could crack this little round world on which
he lives, and study first the whole outside of the shell, and
then the kernel and the core, within and without ; if he could
cut it in two, like a roll or an orange, a stick or a bone, and
stiuly a whole section at once ; if he could first watch the
growth of it, and then crack it like a pebble, he would under-
stand the structure better than he does. A geologist can do
nothing of the sort ; but every geologist wants to know what
the inside of the world is like, in order that he may the l)etter
understand the outside of it. A great many aide men have
tried to crack that nut. In November (5th and 6tli) 1863, the
^s
3G8 SPARKS.
/0\ Newcastle Daily Journal puhlislied a clever summary of scien-
tific specrilations on this subject, and a woodcut of a section
of the globe, according to the view taken by T. I'. Barkas, the
writer whose signature is attached to the paper in question.
The cut represents a hollow shell. The list of the famous
men who have tried to solve the problem is very imposing,
and it includes teachers and masters of many brandies of
knowledge ; but their opinions differ as much as the several
ways by which they sought to reach their point. In this
mocking age nothing is complete without a ludicrous element ;
so, to relieve the darkness of the earth's interior, and lighten a
hea\y subject. Captain Symmes is introduced to play meiTy-
nian amongst grave and reverend actors on the world's gravest
stage.
" He believed that the interior of the earth was peopled,
and he invited Baron Humboldt and Sir Humphrey Davy to
descend with him into the subterranean recess Ijy an immense
hole which he fancied existed in latitude 82° north, from
which the polar light was supposed to emanate."
Baron Humboldt did not go ; but he says, "According to
conclusions based upon mere analogies, heat probably increases
gradually towards the centre."
No theory ought to be accepted liecause of tlu- author's
authority ; no man's tlieory ought to bo ridiculed till it lias
been tested and luund absurd ; but Humboldt is a bettor guide
than Symmes along underground foot^^'ays, Mliich load step
by step from experiment to conclusion, like ladders which
reach from point to point in a deep dark mine. One leaps in
the dark, the other feels his way cautiously. Parry, Scoresby,
Kane, and others, have been far enough north to ])rove that
Symmes was wi'ong ; all oxporiments yot tried oonlirm tlio
vit'w taken by Humboldt. A student wli.i will not loo]. to
VOLCANIC BOMBS — METEORITES. 309
conclusions, and cannot keep pace with pliilosopiiers wliose
thoughts are mounted on well-built scientific cars, must take
liis own way, and do the best he can t(j reach his ])oint. The
quarry pursued was Light, and it was I'un to grcjund where it
cannot be followed ; luit a student in search of knowledge
may watch a spark flying out of a caldron of lluid iron : he
may study that to begin with, and strive to advance indirectly,
step by step. One who does not mind dust and ashes, and
the risk of burned fingers, may fill his pockets with luminous
drops of metal and slag at any furnace, and crack these like
nuts at home.
Some years ago a great number of sparks were caught fiy-
ing, and others were sifted out of the dust on the fioctr of a
smelting-house in Greenock, to the great wonder of the work-
men, who could not make out " what the gentleman wanted wi'
that dirt." The " gentleman" had just returned from Iceland,
where he had been with the purpose of studying forms wliicli
result from the mechanical action of terrestrial heat and light,
and he wanted to compare certain round stones with frozen
sparks ; lie had come to fill his pockets with dust, in order to
gain light amongst his old friends — intelligent Scotch work-
men— and at his old haunts, beside furnace fires. The round
stones were gathered with the notion that the inside of a round
world, which is hot within and hard without, and travelling
through cold space, might be like the inside of lundnous
sparks of iron and slag, and larger drops of lava, which shone
like stars while they flew through the air at first, and only
ceased to shine when they froze. The student meant to com-
pare all these ^\'ith meteorites, to test his theory as far as he
was able, and to say nothing about it till it was licked intt)
some tangible shape. It has now taken the shape wliich it
wears in these volumes, and readers wlio have had the patience
VOL. II. 2 B
370 SPARKS.
to follow thus far — if sucli there be — may now judge this spark,
which was sifted out of dust and ashes, at home and abroad.
The first step in the comparison was to make the frozen
sparks seem equal in size to the lava-drops ; and with that
end in view, they were placed under a microscope, and draw-
ings made from them.
Like forms have been found upon all such drops. The
surface always appears to be dimpled with cups, and roughened
with projections of various shapes : these resemble forms
which abound upon every plate of slag ; they are miniature
copies of mounds and hollows in cast-iron, from which sparks
and drops were thrown while the iron was hot ; they are like
hills and hollows which may be seen to grow on freezing iron
and slag at any smelting-house ; they are like those which
were seen to grow upon silver at Newcastle and elsewhere.
In one case cones and craters are on the shell of a small
spherical mass ; in others they are on a plane, but the plane
is in reality a portion of a sphere whose centre is the centre
of the earth. The round lava-stones are like the frozen sparks.
Tliey were shot out of cones and craters, and their surfaces are
often pitted and dimpled and roughened with miniature
craters and cones, which, in their turn, resemble shapes which
abound in the lavas, and in the large mountains of Iceland,
and other volcanic regions. The outer forms bear reference
to the interior of the frozen sparks and " volcanic bombs;" the
outer shape of the volcano to the interior of the earth. They
are all shapes built about rays.
The history of " volcanic bombs" may be learned from
passing events. In February 18G5 an eruption broke out in
Sicily, and innueruus writers have described what tliey saw
tlicre. Tlie following are extracts i'rom a letter published in
the Scotsman of the 20th Feltruarv 1805 : —
VOLCANIC BOMBS — METEOIilTES. 371
Hotel pella Corona, Catania,
February 7, 1865.
Having just witnessed an eruption of Mount Etna, I think a short
account of it may be interesting to your readers. The morning of the
2d was ushered in by a temfic thunderstorm accompanied with torrents
of rain and hail. But intelligence is brought us that Etna is in full
eruption ; that the lava has already run so fast and so fur that the road
to Catania is blocked up ; that thousands of peasants have fled from
their home in terror of destruction ; and that a war-vessel has left
Messina, carrying the Prefet and a staff of engineers to the scene, with
the view of saving life and property.
It is almost dark before we reach the steep zigzags leading up from
the main road to Taormina, where we intend to sleep. On reaching a
sudden turn, we see in the clouds a long undulating line of red light.
It is the lava-stream — Etna outlined with a pencil of living fire. And
now the low nuubling of the still distant volcano breaks on the ear,
mixed up with the peals of thmider, which continues to reverberate
among the mountains. As the night deepens, the clouds begin to clear
away, the stream of lava becomes brighter, and the light emitted from
the crater, which was at first but faintly reflected from the clouds above,
becomes more and more brilliant, imtil the whole sky over the mountain
glows with a lurid light. Here and there at difl'erent points bright jets
of flame appear for a few minutes and then vanish. Tliese, we suppose,
arise from the burning of trees set on fire by the lava or the falling
scorioe. Tliere appear to be six craters (juite distinct, but situated near
each other. From all these, in irregular succession, sometimes from
several at a time, there are incessant discharges — huge masses of red-
hot stones and scoriae thrown to an immense height, with volumes of
steam and smoke which reflect the fires from the red-hot cauldron below.
The glowing smoke flickers in the breeze as if it were flame, and through
it and far above it, with the naked eye, we can see the red-hot stones
mount and then fiill slowly back into the abyss.
I regret having omitted to note the time which these stones took t(j
rise and fall, as that might have given an approximate idea of their
size, and the height to which they were ejected. But Taormina is from
twelve to fourteen miles distant in a dii'ect line from the crater, so that
the stones, to be seen at all, must have been enormous. Comparing the
lieight to which they seemed to rise with the appearance which such a
372 Sl'AKK:^.
liuikliiig as St. raul's wlit-u su far niiKivinl ini!j;lit prust-nt, it couUl not
be less than 1000 feet.
Leaving Taormina at nine, -vve drive to Mascali. Tlie weather is a
comiplete contrast to that of yesterday — bright, clear, and calm. As we
pass along among almond trees in full blossom, through orange and
lemon groves gloAnng with their golden fruit, the ground carpeted with
young flax of the brightest green, and see the labourers following their
])eaceful occupations in the fields, it is difficult to realise the idea that
within a few miles a volcano is breaking up the crust of the earth
and spreading a deluge of liquid fire over its surface. A walk of three
hours over a used but not a diflicidt road brings us to the lava. As we
approach, the rumbling sound from the eruption becomes louder and
louder ; but as the sun gains power and brilliancy, the volcano becomes
invisible to the eye. A faint line of smoke along the current of lava,
and a dark cloud hanging over the crater, are the only visible signs
which he gives of his existence — signs which, if met with on a Scotch
mountain, might be passed by as arising from moor burning. The
stream of lava which we visited is said to have flowed from six to eight
miles. The lava, under the influence of the bright sunshine, appears to
consist of blackened scoria3 or cinders. It is only through the chinks,
or wliere the surface is disjilaced by a rolling block, that the fire is
visible. The current, where confined in a narrow gorge, flows rapidly —
that is to say, at the rate of from two to eight feet in the minute, accord-
ing to the steepness of the descent. On the flatter ground, where there
is more obstruction, and where the stream spreads out to a great breadth,
the progress is invisible to the eye. As in a glacier, there is a more
rapid flow in the middle than at the sides, for these sometimes seemed
to be quite fast, while the motion in the centre is distinctly percejitible.
Tlu; portion of the current which is flowing towards Mascali, has a
breadth of some two or three hundred yards, and a depth on its sloping
front of from twenty to twenty-five feet. It may be approached with-
out much inconvenience, and with perfect safety ; for although large
masses are constantly rolling down, there is always time enough to
escape before they reach the bottom. ^Men were busy carrying ott" the
beams of the roof, with the other timber wmk, and filling up the cisterns
with stones. Wlien the Inva comes in conlacl w itii a hxrge body of water,
dangerous explosions take ]ilarr tlirdiii^li its rapid tdUViT'-idn intu stiMin.
The point which the lava lias readied 1 .al.niate In be abcut 2i(i(» feet
VOLCANIC BOMBS — METEORITES. 373
above the level uf the sea, and the crater some 1500 feet higher, or one-
third of the way up the mountain. We followed the stream towards its
suurce, until we were driven off by the heat, the blinding dust, and the
sidphureous suioke. Of the three, the dust was the most troublesome.
Below us we could see the course of the current filling up the hollows
and spreading over the flatter surfaces like a huge black glacier, while
above, confined in a narrow gorge, it came tumbling over a precipice in
a dark mass, relieved by streaks of fire. We waited until night set in,
when the lava began to glow again, and soon assumed the appearance it
presented from Taormina of a river or cascade of fire. On what seems
now to be a glowing mass of living fire men were walking not two
hours ago, for the purpose of getting some trees which had been swept
down by the torrent. One tree we saw carried on shore by two men
who had stood on the lava while they cut it in two. A small prize for
running such a risk ! They returned for a second, but were driven off
by the heat and suffocatuig fumes. An Italian engineer who was on the
mountain took some rough measurements, and calculates that the crater
has already discharged eighty million cubic metres of solid matter, that
the progress of the different branches added together would amount to
seven metres per minute, and the length of the whole to forty-five
English mUes. I consider the estimate of the distance too high ; and
as the eruption began only four days ago, it does not seem to tally with
the other calculations.
The followinn; are extracts from the Times of February 24,
18(3.5 :—
Letters from Sicily, in the j\Ialta papers, give some further
particulars of the eruption, and the progress it has made, A
letter from Catania, on the 12th inst., thus speaks of it : —
" The mountain indulges in a constant roaring, to .which we are gradu-
ally becoming accustomed, but wliich at first kept me awake at night, and
this at a distance of some thii-ty miles ; so you can imagine what it must
have been on the spot which I went to (Monte Crisimo), situated at about
two miles N.E. of the new crater."
Another letter of the same date from the same place
says :—
374 81'AKKS.
" Two nights ago avu could not sleep for the noise, the wind blowing
froni the north. An eye-witness tells nie there were eleven streams of
lava, mostly small."
The following are extracts of other letters from Sicily
relating to the eruption : —
" Aci, Feb. 7.
" The lava issues from four mouths on the south side, and varies
every day in the direction it takes. If the eruption continues it will do
more damage than that of 1859."
"Giarre, Feb. 10.
" Yesterday I visited Piedimonte, out of curiosity, and obser\'ed that
the right branch of liquid lava was advancing with the extraordinary
velocity of about a mile and a half an hour. Great damage has already
been effected by the lava. At the present moment, while I am writing,
all the windows of the house I am living in have been broken by con-
cussion, which was accompanied by eaithquake. Tlie noise is like a
continued cannonading, Avith a discharge from time to time of 100 guns
all at once."
Another letter says : —
" All the world is busy talking and speculating on the effects of an
eruption of Etna which broke out on the north side of the mountain,
about ten days ago, at a place called Monte Frumenti. It is very violent
and threatens to do much damage, as the streams of lava run east and
north, and are progressing with great rapidity. I went up with a party
to see it, and certainly it is one of the grandest spectacles I ever beheld.
Tiiere is an incessant rumbling noise, with, every now and then, loud
explosions resembling the discharge of heavy artillery, when showers of
red-hot stones are thrown to a great height into the air, and either fall
back into one of the craters (for there are three of them in activity), or
are carried away by the streams of molten rock which are constantly flow-
ing. It is certainly one of the finest sights I ever mtnessed ; all other
things appear tame and commonplace when compared with it. Shortly
after the party I was with arrived at the summit near the craters a dense
fog came on, and we were compelled to bivouac for the night, as the
guides refused to undertake the responsibility of conducting us down
until daylight in the morning ; and when we did descend we were con-
VOLCANIC BOMBS— METEOKITES. 375
A'inced of the propriety of tlieir decision, as the road, which we hat!
passed over in the darlc witliout apprehension, ajipeared appalling when
seen by daylight the following morning. From onr bivouac, 6000 feet
above the level of the sea, the scene was magnificent in the highest degree.
The constant thunder of explosions every two or three minutes, and the
streams of lava running doM^n, and, every now and then, setting fire to
trees that stood in their way, was a sight well worth the hardship of a
night's exposure on the hill-side. Some of the streams of lava are a mile
wide, and have extended seven or eight miles already ; as yet the mischief
has not been mucb-^s t^e m'Oiiress of the devastating flood has been con-
.11:1 PiiliilggBi:! IH lll§
action of furnace heat and of terrestrial light will seem t(i 1 n-
identical in character, if different in degree. The lava,
freezing as it flows from the base of the mountain, throws ofl"
a spray of liquid projectiles — " sparks," which rise 1000 feet,
and freeze as they whirl and fly. Like them, and like any
other freezing fluid, the lava-stream freezes on the surface,
and the lava-ice records the rate of cooling by its shape. In
Sicily it is irregular ; in Iceland, where old lava-floods were
larger, the crust is more compact — more like a crust on slag,
374 8PAKKS.
" Two nights ago we could not sleep for the noise, the wind blowing
from the north. An eye-witness tells me there were eleven streams of
lava, mostly small."
The following are extracts of other letters from Sicily
relating to the eruption : —
" Aci, Feb. 7.
" Tlie lava issues from f(nir months on the south side, and varies
.ijypiv l^:>^r in tl.ii <lir.Mtirm it takes. If the eruittion continues it will do
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There is an incessant rumbling noise, with, every now and then, loud
explosions resembling the discliarge of heavy artillery, when showers of
red-hot stones are thrown to a great height into the air, and either fall
back into one of the craters (for there are three of them in activity), or
are carried away by the streams of molten rock which are constantly flow-
ing. It is certainly one of the finest sights I ever witnessed ; all other
things appear tame and commoinilace when compared with it. Shortly
after the party I was with arrived at the summit near the craters a dense
fog came on, and we were compelled to bivouac for the night, as the
guides refused to undertake the responsibility of conducting us down
until daylight in the morning ; and wlieii we did descend Me were cou-
rse«_ (^Vruv.^^ ''^t^^f ^i-tyUt^/- /'tf6}^. 1^1^ ^ ^V^^^^^
VOLCANIC BOMBS— METEORITES. 375
vinced of the propriety of their decision, as the road, which we lia<l
passed over in the dark without apprehension, appeared appalling when
seen by daylight the following morning. From our bivouac, 6000 feet
above the level of the sea, the scene was magnificent in the highest degree.
The constant thunder of explosions every two or three minutes, and the
streams of lava running down, and, every now and tlien, setting fire to
trees that stood in their way, was a sight well worth the hardship of a
night's exposure on the hill-side. Some of the streams of lava are a mile
wide, and have extended seven or eight miles already ; as yet the mischief
has not been much, as the progress of the devastating flood has been con-
fined to the mountainous regions ; but if it once descends to the cultivated
parts, the damage will be incalculable. Government is doing all it can,
by sending troops to assist the people in removing their goods, pumping
out the water from the wells and cisterns to prevent explosions, etc. ;
but it is a sad sight to see the country devastated and overwhelmed l)y
this fiery toiTent, and left desolate for ages. Happy are the countries
that are free from such calamities."
With these fresh descriptions, and an ordinary power of
comparing great things with small, let any one visit the
nearest glass-honse on a day when the metal is melting and
boiling. All that is so well described in Sicily may be seen
in miniature through the opening in the retort — the liquid
fire, the bubbling craters, the hot whirling projectiles. Let
any one watch the sights and sounds aljout a blast-furnace,
to which attention was called in the last chapter, and the
action of furnace heat and of terrestrial light will seem to be
identical in character, if diherent in degree. The lava,
freezing as it flows from the base of the mountain, throws off
a spray of liqviid projectiles — " sparks," which rise 1000 feet,
and freeze as they whirl and fly. Like them, and like any
other freezing fluid, the lava-stream freezes on the surface,
and the lava-ice records the rate of cooling by its shape. In
Sicily it is irregular ; in Iceland, where old lava-floods were
larger, the crust is more compact — more like a crust on slag,
37G SPARKS.
^v]lic'll cooU'J sl()^\•ly. Tlic sjcirks are alike, tliougli vai'inus
ill size and in sliajic. TIu'v sliiiie as they fly ; some Luvst
like rockets, and scatter a shower of golden fire, others shoot
and shine and fall, freeze and glow, and darken on the floor;
and when they are found, these sparks are shaped like little
wuilds. They are frozen drops.
At Hraimdal, in Iceland, a crater is at the npper end of a
glen. It is at the source of an old lava-stream, which flowed
down a hollow for some miles, and froze into clinkers. The
hill may be aboiit 100 feet high, and it is a perfect " cone of
ernption," — a truncated cone, with a funnel-shaped hollow in
the top. The colour is a dusty brick red, and it stands in a
broken-down crater of larger size, and of a different make and
colour. The central mound is a pile of round stones, dust,
and fragments. Some of the stones are as big as a man's
head; others about the size of oranges, potatoes, and nuts; and
most of them are distorted s])heroids, egg-shaped or discoidal.
They are exceedingly hard and tough, and very hea\^. It
took hard blows with a heaAy hanuner to crack these nuts ;
but many were broken on the spot, and a pocketful of speci-
mens were carried during a long day's ride, and brought honu'.
A black specimen was brought home from My^^atn the
year liefore, and these are the stones which had to be com-
pared with furnace sparks.
Ijccause these stones were drops of lava, which cooled by
radiation A\liile revolving in free air, it is certain that the
outside cooled first. The first crust froze, and shrank about a
iluid or viscous hot core. The INTyvatn specimen was some-
what like a split trullle, for the outer crusts tore, as freezing
slag-crusts commonly do under like conditions. A second
crust forniod within the fii'st, and a third under it, and then
all three wore torn, and the hot core Itnlged out. Tlie " faults"
VOLCANIC BOMBS — METEORITES. 377
remain, and their sides show tlie edges of tliree crusts, which
seem to have been soft, for they bulged sideAvays into the
lent. These three crusts differ in colour, though they are
alike in structure; and in this they resemble thicker lava-
crusts, and shattered cliffs, amongst which this lava-ljall was
found. A tap with a hammer l)roke this specimen, shell and
kernel, and so revealed the inner structure of it. It was shot
out by the earth's artillery — by a radiating force, which pro-
jected it from a tube with a chamber ; it was shaped by heat
and cold, by expansion and contraction, by forces acting in
opposite directions, from within and from without, while it
was whirling and flying through the air ; it is a work made
in obedience to the code of laws which seem to apply to all
known objects in nature ; it may be shaped like larger works.
The seedling may be like the old plant ; the structure of this
frozen drop may be like that of the world from which it
sprang. Iron sparks are like it ; cups and cones, faults and
fissures, dykes and craters, Hke those of Iceland, are on the
outside of it. Point a common telescope at the moon, and the
same forms reappear upon the surface of a star which shines
by reflected light, and seems to be no larger than one of the
iron sparks under a microscope.
Sparks and bombs resemble each other in their structure.
They all have crusts and cores, and the whole mass is per-
vaded by tubes and open chambers, of which many communi-
cate with each other, and some with openings in the outer
shell. The outer crusts of broken specimens are built upon
lines which radiate from within ; joints and vertical fractures
in the crusts aU bear reference to points within the mass.
Produced in one direction these lines converge, in the other
direction they diverge. The crusts surround a core as a nut
shell suiTounds the kernel, and tho outer lavers shell off.
378 SI'AKKS.
They are like the earth's igneoiis crust, as seen in clifls ; they
break vertically and also horizontally. The kernel of the
stone is shaped like a sponge, with tubular branching, irregu-
lar passages, and spherical hollows, built about lines which
radiate as heat did, from points M'ithin the mass outwards.
But all the rays are bent in one direction ; like the arrows
in the cut, p. 28, vol. i., or the curves at p. 473, vol. i., and in
the map at the end of that volume. All the specimens from
Hraimdal have crusts with irregular spongy cores, built about
centres of radiation and motion. After trying to copy sections
by various imsatisfactory devices, the stone itself was tried as
a type. Slices were made equal in thickness to a printer's
block ; they were inked and pressed, and here is the result.
These shapes tell of expansion within and pressure
without, and of rotation ; the mass shone while it was form-
ing, and ceased to shine when the crust had formed and
cooled, and such masses whirl as they fly. The first frozen
shell was filled Avith fluid or viscous lava, and with vapours
which shaped hollows in the plastic mass and escaped through
th(;m to holes in the outer crust. The last of the imprisoned
vapour was caught on its way out, the prisons took the shape
of the prisoners, and some of them now are crystals, which
forced the prison-walls to take angular shapes. Surely this
miniature geology may grow. When furnace sparks and vol-
canic bombs agree so well, a student may venture one more
step on the ladder which has led, step by step, to knowledge
and to light.
As a very eloquent, able speaker is apt to say, " Three
courses are open" to every student. One is to follow some
beaten path, and never to venture out of it ; to choose a
leader and follow him, pacing gravely over the same old
ground every day, and learning every inch of it. That school
of peripatetics is numerous, for the ways of these scholars are
VOLfANIC: I{0>[BS — METEORITES. 379
Sections of VoLrANic Bomus, from Hraunpal in Iceland. — Printed from the Stones,
PiTy^^-J"
No. 1 is from a section made at tlie sup-
)iosed equator of a flattened sjiheroidal bomb.
The whole rough surface of it is pitted with
smooth cups : — miniature craters, of which
many end in tubes. As shown in the sec-
tion, many of these ducts communicate with
chambers in the cru.st. Of these some are
associated with rows of small chambers, and
with long in-egiilar passages in the core, which
aim at or meet in a large irregular chamber
near the centre. The ends of numerous radi-
ating and branching passages are seen in all the
sides of this central cavern. The inner surfaces
are smooth, and it is evident that the walls
of the chamber, and of its radiating systems
of ducts and passages, were plastic when they
were shaped by imprisoned vapours struggling
to escape from the centre to the surface. Pits,
cups, tubes, craters, and cones, record tlie
escape of miniature eruptions through the
cnist. If any one system of chambers is fol-
lowed from the outside, the line traced is not
a straight line, but a curved spoke bending
backwards. That form records the direction
in which the stone revolved about its axis.
No. 2 is from a similar section made with the intention of cutting an axis of rotation
at right angles. The surface of this stone is not so much pitted, and one side appears to
have been flattened, as by a blow. The section shows a crust with fewer chambers near the
outside, and a spongy core. The same arrangement of the materials about curved rays is
apparent. From their structure these two stones revolved in the same direction, right
side down the page. Part of the crust of No. 2 split off in the process of cutting.
No. 3 is like the other two in structure, but revolved the other way.
380 SPARKS.
easy and safe. A second course is to avoid roads — to scorn open
gates, gaps, and bridges, guides and leaders, and strive tu be
oiiginal. That is a brilliant, dashing, dangerous course, which
may lead to honour or to failure. Captain Synnnes got a
heavy fall and failed when he made a guess, scorned experi-
ment, and took a header into the earth. The middle course,
in this as in other cases, appears to be safest and best. It is
to follow the best attainable paths quietly and steadily as far
as possible, with the best guides and the best aids, and with
the best comrades, who will travel towards the point aimed
at ; and when the wilderness is reached at last, to choose a
line and take it, and go, best pace, along the best ground
cautiously, like a traveller making his way through a new
country, where all must do the best they can to help them-
selves, for lack of guides, and roads, and cars. Humboldt
got to his point and gained honour, by venturing cautiously
on new ground when he had followed guides and roads as
far as they would lead. In illustration of these three methods
of study a writer may tell a story against himself without
offence.
Some years ago, after a trip to Iceland, it was agreed that
a joint book should be written, and one section of it was to
be written by this hand. With a head full of the subject, the
owner of head and hand set out from Edinburgh for the Carron
Ironworks, intending to watch the pranks of molten stone, as
a key to the forms of old lavas and volcanoes in Iceland. A
heavy cloud had passed over a clear sky the day before, and
a loud clap of thunder had been heard. On getting into the
guard's van to smoke in quiet, it somehow transpired that a
" thunder-bolt had fallen in a field about half-way to Glasgow ."
It so happened that the guard, as he said, was cognizant of the
liill of a meteorite somewhere in England. It fell through the
VOLaVNIC; BOMBS— METEORITES. 381
roof of a barn, and buried itself in the clay floor ; it was dug
out, and it was so hot that the workmen pitched it into a
pond, Avhere, so far as the guard knew, it remained. This
guard had spoken to the guard of another train, w^ho had seen
this new " thunder-bolt" fall while he was passing, and it was
still blazing when the morning train passed. Of all things in
the world, or out of it, a meteorite was the one thing wanted
to compare with volcanic bombs and furnace sparks, and
complete the chapter ; and here, as it appeared, was an
authentic hot aerolite blazing within a few miles. Of course,
it must be got at any cost. The friendly guard made the
ticket all right, and from his box we saw a tall flame, ten feet
high at least, blazing in the field where the lightning had been
seen to fall. It rose from a hole in the earth, about which
fresh turf was scattered, and a great deal of water was flowing
out of the ground. The writer is perfectly well aware that he
will never " set the Thames on fire" himself, and he has little
hope of seeing tliat feat accomplished. To raise such a blaze
out of water did seem beyond the power even of a thunder-
bolt ; but water decomposed and recomposed makes the oxy-
hydrogen blow-pipe and one of the strongest of fires. There
was the flame — a fact to be accounted for somehow^ " Three
courses were open :" to rest content with the information and
leave the facts unexplained ; to leap to a conclusion and hire
a lot of men to dig out the meteorite ; or to go to the place
and investigate. It seemed best to get out at the next station
and walk back along the known road to the field ; then to
clamber through a gap which was seen in tlie hedge, and see
what was to be seen at the spot. The point was reached at
the cost of a wet walk of some miles and a few scratches.
There was the blaze sure enough ; a tall fact ten feet high, roar-
ing; and at the base of it water was welling furioush- out of a
382 srAHKS.
clay-pit, for all the world like a boiling spring in Iceland. A
very simple experiment extinguished the aerolite theory : the
water was quite cold to the touch. " A blower of coal-gas had
been fired by the lightning." That was a jump, and a fall was
the result : the steady school stayed at home ; the middle
course found out the truth. Leaving fire and water to fight
their battle, the wet traveller went to the nearest house and
asked an old woman when the lightning lit the gas. " Od,
man," she said, " it wasna thunner ava ; it was jeest ane
of our lads that fired it wi' a match." The traveller told his
fool's errand to the old dame, who sagely remarked — " It's
jeest like the three craws ;" and then he trudged on through
rain and mire to the nearest furnace, which happened to be an
old haunt in Lanarkshire. There he found what he set out to
seek — sparks. There are two ways of viewing this story.
Here is a great thing beside a little thing — a meteor and a
match — and they may be contrasted or compared. Here is
a big fallacy turned into a little fact, and a man mocking
himself, liut there is a moral in the tale for those who can
see it. There was light at the end of this train, if it were but
a feeble spark, and beyond the match was the will of the man
who lit it. Between them is a great gulf which no man can
leap ; for no philosopher pretends to explain how a man's will
moves his hand, or how that lad thought about lighting the
coal-gas. Beyond them lies that " great ocean of truth" whicli
the greatest of men have seen stretching out before them at
the end of their earnest lives. Sparks of truth were worth
all the trouble of the trip : " the play was worth the candle,"
though it was a burles(|ue.
Though this hunt failed, plenty of meteorites may be seen
at the British INIuseum. A printed catalogue gives a list of
134 specimens of "acreolites," "meteorites consisting for the
Ou Monday, iDe za icst., a luminous body oi a rtsiuaifv-
ahle character passed over this district iti a south-western
direction. It was observed on the northern borders of the
parish, at Poolewe and Gairloch. The time of its appear-
ance was about 3 p.m. Its hinder part seemed enveloped
in a sort of bluish fl ime tapering oflf to a point. During its
course pieces were seen to fly off and disappear instantly.
The most extraordinary feature is that the observers agree |
in describing its path as apparently almost horizontal, and '
at no great elevation. Though the afternoon was clear and I
the sun shining, the course of the meteor was distinctly \
visible. It was not observed by any of the individuals '
throughout its entire course, Uut the distance over which it
travelled, according to the locality of the different ob- \
servers in this district, was about fifty miles, disappearing
apparently about the coast of Skye. I am not aware that I
meteors have been seen in the day-time, and the fact of any i
being observed, would lead t.> the conclusion that they
must be of of very great size and luminosity. '
6.V.t"
""J/^'P^^C^i
382
clay-pit, for all tlie world like a boiling spring in Iceland. A
very simple experiment extinguished the aerolite theory : tlie
water was quite cold to the touch. " A blower of coal-gas had
been fired by the lightning." Tliat was a jump, and a fall was
the result : the steady school stayed at home ; the middle
course found out the truth. Leaving fire and water to fight
their battle, the wet traveller went to the nearest house and
asked an old woman when the lightning lit the gas. " Od,
man," she said, " it wasna tlnmner ava ; it was jeest ane
of our lads that fired it wi' a match." The traveller told his
fool's errand to the old dame, who sagely remarked — " It's
jeest like the three craws ;" and then he trudged on througli
rain and mire to the nearest furnace, which happened to be an
old haunt in Lanarkshire. There he found what he set out to
seek — sparks. There are two waj^s of viewing this story.
Here is a great thing beside a little thing — a meteor and a
match — and they may be contrasted or compared. Here is
a big fallacy turned into a little fact, and a man mocking
himself. But there is a moral in the tale iov those who can
see it. There was light at the end of this train, if it were but
a feeble spark, and beyond the match was the will of the man
who lit it. Between them is a great gidf which no man can
leap ; for no philosopher pretends to explain how a man's will
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On Monday.tne zu inst., a luminous body oi a remai li-
able character passed over this district in a south-western
direction. It was observed on the northern borders of the
parish, at Poolewe and Gaiiloch. The time of its appear-
ance was about 3 p.m. Its hinder part seemed enveloped
in a sort of bluish fl ime tapering off to a point. During its
course pieces were seen to fiy off and disappear tustantly.
The most extraordinary feature is that the observers agree
in describing its path as apparently almost horizontal, and
at no great elevation. Though the afternoon was clear and
the sun shining, the course of the meteor was distinctly
visible. It was not observed by auy of the individuals
throughout its entire course, Uut the distance over which it
travelled, according to the locality of the different ob-
servers in this district, was about fifty miles, disappearing
apparently about the coast of Skye. I am not aware that
meteors have been seen in the day-time, and the (act of any
being observed, would lead t) the conclusion that they
must be of of very great size and luminosity.
fOpL^ Aa^»^
A. Mjbtbob. — The following letter desoribea a
meteor Been in broad sanahine in West Rossshire : — " We
have: witnessed aa extraordinary phenomenon to-day. I was
on one of the parks at the Isle of Ewe trying to shoot
plovers.Johnny and the boy Murdo with me, when the latter
called out ' Look, look!' and we then saw a thing going com-
paratiTcly slowly through the air from aorth-east to south-
west. It was long, something; like a comet, with a pear-
shaped head and a long rather ragged tail, something like
that of a paper kite. It was snowy white, but beautifully
transparent and brilliant as the lime light, and made.jthe
BUD, which was then (at a quarter to 3 o'cloek) shining
gloriously in a cloudless sky, look comparatively dull. It
seemed to U3 to be about 150 yards from the ground, and
not above 200 vanls from the ijlace where we were stand-
j ing, but I suspect this must hare been aa optical illusion.
I I should think we had watched it for about half a minuto
I when it suddenly divided into three parts and then
vanished. On reaching home I was just going to tell M.
about it when she called out she had seen a most extraordinary
Bight, and which proved to have been exactly what we had
Been. One ef my shepherds and one of the workmen saw
it also, and »o doubt hundreds of othoni through the
country.
J C l^i<Lh
6
CiJ^eZs
0^^1A^^>^
ihfXp Tx/UA-y U^^<^ ( &^
^/
r^n-*^X^^
VOLCANIC BOMBS — METEORITES. 383
iiKjst part of various silicates interspersed with isolated part-
icles of uickeliferous native iron, meteoric pyrites (troilite),
&c.," wliicli are exhibited in one case. Of " siderolites,"
"meteorites consisting of nickeliferous native iron in a more
or less continuous or spon(/e-likc state (with schreibersite,
&c.), ca\4ties in which are charged with silicates, &c.," nine
specimens are exliibited. Of " aerosiderites," " masses of
native iron generally nickeliferous and containing phosphides
of nickel and iron (schreibersite), carbon, troilite, &c," 73
specimens are shown. These represent 216 meteoric falls,
previous to August 1, 1803, when the list was printed by
Professor Maskelyne of the mineral department, where all
these may be seen. The heaviest specimen weighs 2800 lbs.
On the 14th of May 1864 a meteorite fell in Jrance.
Mathieu (de la Drome) in his almanac for 1865 gives an
account of tlie fall, and a paper on meteoric stones by Louis
Figuier which gives a great deal of information in a small
space. Chladni, Arago, Humboldt, Herschel, and many other
('minent men, have described these visitants from the outer
world, and in s^jite of learned slow coaches, who long refused
to accept evidence, it is now admitted that from early historic
times small planets and fragments of planets — bodies which
moved in space in obedience to the laws which govern the
movements of the earth, and other members of the solar
system — have passed within reach of the earth's attraction,
and have fallen as stones fell in 1864. The received opinion
is that cold masses, attracted by the earth, are heated by fric-
tion while passing rapidly through the earth's atmosphere,
and shine as .fire-balls and shooting stars, which explode and
faU as hot meteorites at last. The structm-e of many speci-
mens implies that the whole of each mass was fused before
it cooled, and froze, and crystallised, and oxydised, and broke.
«...^ /^...-.^ .--/^7 ^Vw.,-^^^'
384 SI'ARKS.
Besides the collection at the IJritisli JNIuseuiii, aljout 1100
specimens are preserved in uiuseunis in Europe, and the num-
ber is constantly increasing, because attention is directed to
this curious subject. The " Bolide" of 1864 was seen at nearly
the same hour from Paris to the Pyrenees, and ]\I. Adolphe
Bronguiart, who happened to be near Gisors, saw the meteor
pass from west to east at 15 to 20 degrees above the horizon,
and disappear without noise. At Paris and at Gisors it was
seen to the south. In the south it was seen, at eight in the
evening, a globe of fire as big as the moon, followed by a
train of luminous sparks ; it seemed larger as it approached
the ground ; it was seen to burst and scatter a shower of
sparks, leaving a small white cloud, which lasted for some
minutes. At last, the inhabitant* of a region between Nerac
and ISTohic d'Orgueil saw a fire-ball, which seemed larger
than the moon, pass over their heads, revolving on its axis :
it cast off sparks and jets of white vapour in every direction,
and it burst like a shell at last, scattering shining fragments,
which disappeared behind a cloud. An observer maintained
that after the explosion of brilliant sparks he saw a dark red
glol^e continue its course. After an interval of from five to
two minutes, a loud noise was heard by those who saw the
explosion. A shower of stones followed, and fell between the
villages of Nohic, Orgueil, and Mont Bequi. They were hot :
a peasant burned his fingers with one, the grass was singed by
others. About twenty fragments were picked u]), and they
were covered witli a lilack varnish : to produce a like glaze
on a freshly-broken surface the stone had to be heated to a
white heat. This meteorite contains about 5 per cent of car-
bon in the state of graphite, and many solulile salts. It was
seen by so many observers that a map of its course was made,
and its trajectory calculat('(l by M. Lausedat, Professor of the
YOLCAXIC BOMP.S— METEORITES. 385
Ecole rulytechniqiie. Some of the crumbs which fell from
this, the latest of meteorites, are shaped like bits chipped
from the crusts of volcanic bombs. They are chambered and
pierced with holes, and the solid lireaks in two directions,
like the upper layer of the lava-crust shown in the cut p.
429, vol. i. It is therefore possible to compare the structure
of furnace sparks, volcanic bombs, and small planetary bodies,
and upon these three degrees to plant a theory as to the
structure of the earth's interior.
The great majority of meteorites are mere angular frag-
ments.
One specimen at the British Museum is composed of three
fragments, picked up separately, and at considerable distances
from each other, l3ut they fit and form a portion of a shell.
In this they resemble fragments chipped off volcanic l)ondjs.
These broken bits of a crust are covered on all sides l.»y a
vitreous glaze, so in all probability they travelled far after the
larger mass burst.
A great many have marks of fusion on the surface. ^Many
are spongy.
One described by Pallas in 1778, at St. retcrsburg,
weighed about 700 kilogrammes ; it had the form of a large
bomb, a little flattened, and partly covered with a rude ochrous
• rust. The interior was made of soft iron full of holes, like a
coarse sponge. These holes contain grains of olivine as large
as peas. This seems to have fallen entire, and to have the
structure of a volcanic bomb. It is like a furnace spark
which has cooled without bursting.
In the Smithsonian Institution at Wasliington, the so-
caUed " Aiusa" meteorite is preserved. It weighs 1400 pounds,
and is meteoric iron, with specks of a grayish silicious mine-
ral enclosed. It is now in the form of a great rude signet-
VOL. II. 2 (•
386 yPAllKS — VOLCANIC 150M I'.S — METKOlilTES.
rin<^-, l)ut it seems to be a portion of a liollow sphere. Tlie
hollow is iiTegular, and bulges out into concave recesses like
those which commonly occur in ii-on sparks ; like those which
are shown in sections of volcanic bombs. The outer surface
is spoiled, and if ever a crust surrounded this iron core all
traces of it have disappeared. This remarkable meteorite
was found at Sehora, in the Sierra ISIadre, in California, and
it was used for many years as a public anvil. The greatest
diameter is 41 inches. The woodcut in the title-page of this
A'olume is from a rough pencil-sketch made at Washington in
October 1864. In some respects the Ainsa meteorite is like
the woodcut in the paper by Mr. Barkas above quoted.
A comparison of forms in hollow spheres of hot water; in
sparks thrown off by hot silver, iron, slag, and other sub-
stances ; in "bombs" projected from terrestrial volcanoes, and
in meteorites attracted from space ; makes it probable that a
flattened spheroid with a frozen crust, through which luminous
fluids and hot vapours now escape in all directions, may now
have a solid chand^ered spongy core, packed about bent rays,
and about a centre of motion ; made of materials which do
not easily melt, and which freeze at high temperatures.
According to astronomical calculations founded on the earth's
movements, the average density of the whole mass is 5.67,
water being 1. Tlie si)ecific gravity of iron is 7.7, but hollow
iron ships float in water, like pumice-stones, and a spongy mass
of any material might have any apparent density according to
its structure and state of expansion. Chambers may be filled
Avith the hot fluids and gases which radiate through holes
in tlie frozen crust, and sliine willi terrestrial light when they
follow the paths of rays and strive to escape. Jets of vapour
and fountains of sparks so escaped from the fire-ball of 1864,
and they so escape from sliining fnniace 8])arks.
CHAPTEE LV.
TUBES AND SPRIXGS.
Man has been classed as the cooking animal, so most men
have boiled something ; and whoever has Ixjiled anything
must know something of the mechanical force of heat.
Hot solids melt, fluids become vapours, and all increase
in bulk when they have room to expand. Softening and ex-
pansion begin near a source of heat, and spread ; the heat
spreads and radiates as light does from a luminous point ; and
matter moved by heat also spreads and radiates. At a given
distance from a source of heat, expansion and outward move-
ment in any material come to an end, and there contraction
begins or movement stops. Particles attract each other imless
they are kept apart. If sources of light are also sources of
heat, they are centres from which a mechanical force radiates,
and all light appears to be associated with heat, though the
amount may sometimes be too small for measurement.
When water in a kettle is sufficiently heated steam-bubbles
form near the fire. While the upper layers of water are cold
these collapse suddenly to grow again ; the water simmers,
and the kettle is shaken. When the upper layers are warmed
the steam floats up, the bubble expands as it rises ; and at last
it lifts up the surface of the water, bursts through it, and ex-
pands more freely in air when relieved from pressure. In
thus bursting a dome of water, steam drives drops of water
388 TUBES A^•l) SI'ltlNOS.
before it, and these projectiles describe curved paths \vhilc
they rise and fall. They are scattered by radiation, and
attracted by gravitation. The amount of force applied, and
its direction, determine the distances traversed and the curves
described hy these projectiles. The bursting water-dome
starts a whole system of waves, which radiate and spread
horizontall}^ The steam-bubble transfers its charge of heat
and force to the air about it, and it starts a movement which
spreads horizontally and vertically, as sound spreads in the
air. The water particles, which heat separated and drove
upwards, attract each other when the heat has passed on ; the
steam condenses, and drops, attracted by the earth, fall down.
The particles of air, which repelled each other and rose
when heated by steam, attract each other and fall when the
heat has passed on to the next shell of air. And so move-
ment spreads, and circulation goes on about a source of heat
and light. Who is to limit the movement which begins at a
fire under a kettle ?
Whatever the source of mechanical power may be, like
radiating and con^'erging movements must result from radi-
ating and converging forces. A spirit-lamp, a fire, a furnace,
the earth's heat, and the light of the sun, all cause like
radiating movements when iised in the same way.
Water in a transparent glass vessel above a lam]) circulates
like water boiling in a kettle on the fire. Water boiling in
a tray full of sand moves on the same prmciple as water boil-
ing about iron and slag, or about hot lava, or like water in a
spring heated by the earth. The sun's rays, collected with a
burning-glass and thrown upon metal under water, cause the
movements which would result if the metal were heated as
much in any other way.
Whatever the substance may be, radiating and converging
TLBES AND SPRINGS. 389
forces, of sufficieut "energy," produce like movenieiits. Porridge
in a pan, glass in a retort, fluid metals and stones at furnaces,
mud in boiling springs, lava-floods on wet ground, lava-springs
which are volcanoes, all move on one principle ; and some re-
tain forms which register the movements which resulted from
the forces applied. The heat of a lava-drop spinning in air
acts on its surface, and the outside gives a clue to the internal
structm-e of the stone : the heat of the earth acts on its sur-
face, and the forms which result may giA'e a clue to the earth's
structure.
If all sources of heat and all materials be alike in these
respects, then small experiments help to explain the forms
which result from the action of the earth's heat. Materials
which melt and fi'eeze at low temperatures, will serve as well
for illustration and study as those which only melt at furnace
heat.
Oil, water, and mercmy, in a glass vessel, make a series of
three fluid layers, which are portions of concentric shells, and
aie at rest at ordinary temperatures. If the lowest layer is
heated the whole series is disturbed. If cooled so that one
fi'eezes the shapes alter. If water freezes above mercury, in
a closed vessel, the fluid metal beneath the solid ice is forced
into irregular angular shapes, and globules are squeezed up
into the hard crust, where they take the forms of air-bubl)les
compressed in ice. In like manner water and oil in the same
bottle are disturbed by every change of temperature which
freezes the one or boils the other. Water and air at 32°
react upon each other, as iron and air do at 3000°. In both
cases the gas imprisoned within a solid shapes a chamber
whose form records the direction in which forces acted. It is
easy to tell which side of a plate of ice or cast-iron was upper-
most if there be an air-ljulible in it. r>y this rule applied to
390 TUBES AND SPRINGS.
a bit of lava it is easy to tell which side was uppermost, and in
which direction a stream flowed when it froze.
The impression, p. 423, is from a vertical section made
throngh an upper layer of lava, which was flowing from A
to B when it set. It ^-as part of a lava surface near Eeyk-
javik. The ridges are sections of great coils which formed
about the centre, from which a little spring of lava boiled
out, and froze as it spread. The movement was like that of
boiling water, but in this case the boiling fluid curdled and
froze on the surface, and the horizontal waves remain.
At p. 400 is another impression made from a section cut
down through the middle of a set of loops on the surface of a
frozen rill of slag. It boiled up thro ugh a hole in a freezing
crust ; and streams spread as boiling water spreads above a
centre of ebullition. Each riU flowed fastest in the centre,
and froze first at distant points and at the sides, and the
flow is marked by curved loops like string. In these two
cases materials and dimensions differ, but the forms are alike
though produced by terrestrial and furnace heat. Solar heat
properly applied produces the same forms on sealing-wax
or asphalt. Slag can always be seen flowing and freezing,
sealing-wax can be melted at home ; and forms on these
explain lava-forms, and like forms of any dimensions any-
where.
Solder and sealing-wax, lik(3 boiling lava, take a shape
and retain it ; and these and otlier materials, which are easily
managed, serve their purpose as well as iron. Plaster-of-
Paris sinks in cold water, becomes a plastic mud, and then
sets hard ; it is moved by streams and by currents in water,
and when it sets it retains the shape which it took wliile
moving. Water and silt, ])lastei-, sand, or clay, in small
• luautitics, illustrate the action of hot or cold water on larger
TUBES AND SPKINOS. 391
quantities of like materials ; and su models illustrate natural
phenomena.
The Geysers may be compared with a geological toy ; and
forms which result from the earth's heat may be explained
by forms which result from the heat of a lamp applied as
mechanical force.
A working model of a hot spring is very easily made.
Some flat broken plates of slag, and a pile of sand and fine dry
earth, laid upon an iron tray, may rej)resent the country about
the Geysers, wliich consists of shattered strata of lava, volcanic
sands, and loose soil, A pile of broken ice and snow laid on
the heap is placed like glaciers, which crown high mountains
in the region ; and a gas lamp under the tray acts the part of
the earth's heat, which boils water beneath the surface in
Iceland. So far this model imitates a natural arrangement
of a bit of the earth's crust, situated between regions where
the upper tem2:)erature is less than 32°, and the temperature
under groimd is more than 212°, the freezing and boiling points
of water. It is a region of Frost and Fire. Soon after the
lamp is liglited, the pile of ice begins to melt and slide upon
the sand and stones, as glaciers do on sloping hills. A heap
of iron tossed into a furnace melts and slides for the same
reason at a higher temperature ; and ice and iron flow
when they are fluid. The water flows and sinks through
loose sand, and through cracks and holes in the plates of slag ;
and so it finds a way to the lowest depth of the iron vessel.
Iron finds its way through lighter cinders to the bottom of
a furnace ; it sinks through slag as water sinks in oil ; and all
fluids of different specific gravities which do not mix find their
respective levels and take their places in a series, like oil,
water, and mercuiy in a glass. In the model, only one solid
is melted, and a Avet pile of sand and stones remains in a pool
392 TUI5ES AND f^l'KINCS.
of water, supported by an irou tray, which a lamp heats but
cannot melt. So far the heat of fusion enables gravitation to
move ice more speedily from a higher to a lower region. The
melting snows of Iceland form large rivers which reach the
sea ; but great part of the water sinks down through sands
and shattered lavas. The water which sinks where it falls
finally reaches some region where water boils, some lava-crust
which stops it, as a hot iron tray keeps water from sinking
deeper. A column of water, sand, and lava, with a base near
the region whence lava-springs rise, must be intensely heated,
so as to exert a powerful mechanical force, which radiates
from the eartli's centre upwards. At one end of this series
" perpetual snows" crown the hills ; at the other is steam ;
and between these two, water circulates as it does in a tray
full of sand, or in a kettle. When water is boiled in sand,
steam forms below within six inches of unmelted ice upon the
surface, and water boils furiously within a few inches of water
which is scarcely warmed. Shallow water cannot be much
heated so long as ice floats in it ; but sand and stones impede
the movements of water, and steam, and heat. It follows that
the temperature of a hot spring is no measure of its tempera-
ture deep under ground.
But though these movements are retarded, they are still
the same in kind as the movements of water boiling in a
llorence flask. There is circulation ; currents sink and rise,
though snow and ice are at one end and fluid lava at the otlier.
Because hot springs are found in most regions of the earth,
great underground heat is not peculiar to Iceland or to any
district. There is a great store of heat and force within the
earth's crust, ready to act wherever a Aveak point is found.
Currents in water move solids. Sand retards circulation in
hot water, but is equally urged by the Ibrce which it resists.
TUDES AND SPRINGS. 393
When the force accumulates, sand is driven by boiling water,
and steam builds it up into heaps and scatters it in the air.
A heat insufficient to fuse solid sand melts solid ice and turns
it to steam, and so it projects the sand like shot from a steam-
gun. When water is rapidly heated in a narrow tube, steam
forms so as to scatter a column of water like a charge of shot.
AVhen water is heated in a kettle with the lid on, steam formed
below rises to the top, and there expands till it either drives
the water out of the spout or lifts the lid. The mechanics of
the Geyser have been explained by these two modes of action.
According to one theory, the base of a column of water be-
comes so hot that it flashes into steam, and blows out the
charge above it. The other explanation supposes a steam
chamber communicating with the base of the pipe, so as to
force water out of the spout of this giant kettle when the
steam gets up. Both theories may be correct.
In models the latter action commonly results. The melted
ice becomes steam under the slag roof, and forces water out,
while cold water is pressed in by weight. The water is re-
pelled by heat and attracted by gravitation, and so an alter-
nating outward and inward sidelong movement results, be-
cause the slag roof of the steam chamber prevents the steam
from escaping upwards. When a bubble of steam escapes it
carries off a charge of lieat and force, and water enters the
chamber ; when the water is heated sufficiently steam drives
out the water and forces it through sand and chinks in the
slag ; and so, after a short time, jets and fountains of hot water,
steam, and sand, burst through the cold wet surface where ice
remains ; and these, after playing for a moment, stop suddenly
when the steam has blown off, and the boiler is re-fiUed. This
is a result of heat-force, for the height of the jet is decreased
by decreasing the quantity of gas burned, and the action stops
394: TUBES AND SPRINGS.
entirely soon after the gas is tiinied off. Another result is the
packing and sorting of sand. The boiling water sorts coarse and
fine, heavy and light materials, and packs them in stratified
beds ; it drives water fountains through beds of sand, makes
hollows beneath the surface, and it piles mounds of definite
shape upon the top of the heap. In nature, as in this model,
water is dragged down by weight and driven up by heat ; cold
makes it a solid in one region, heat makes steam of it in
another ; it moves from the earth towards the sky, and from
the sky back to earth, as it is heated by the earth's radiation,
or cools by radiation into space. Vapour in air becomes a
cloud, and a snow shower, melts and sinks, turns to steam and
rises again ; and so a cloud becomes a glacier and a geyser in
Iceland, because the world is hot, and space about it cold ;
and the action is the same in a tray full of sand and stones
heated by a gas lamp.
The action of a boiling spring may thus be imitated ; biit
something more is wanting to complete a model. When a
jet of water has forced a way through sand, the loose sand
falls back, and the passage fills. It is so in the model. Near
the foot of Krabla are several large, deep, funnel-shaped hol-
lows in loose volcanic debris. These sandy craters are partly
filled with hot sulphurous gTcen water ; but every shower and
l)reezc of wind disturbs the sand, and the holes tlm)ugh which
water rises are filling rapidly from above. In sandy bays,
where burroM'iiig shells flourish, a certain so-called " spout-
fish" thrusts his long neck through sand when the tide
flows. His mouth is level with the surface, but his body and
shell are far down. When the tide ebl)S and danger
a])))roaches, the shell-fish retires, and in shrinking, spouts
Mater and sand at the foe. lie leaves a sinall crater, but the
next wave lills it, and s<. all trace of the siidul-lish is lost.
TUBES AND SPRINGS. 395
Like this creature, a boiling spring would leave no trace if it
only spouted through holes which filled as fast as they were
made. There may have been springs boiling in ancient sands,
of which no trace remains in sedimentary rocks.
Many of the hot springs in Iceland deposit solids when
the water cools, and these form permanent tubes and craters,
which could be recognised anywhere. Some are deep, still,
hot wells ; some are always surging about ; some are great
foimtaius spouting at short intervals ; some explode occasion-
ally ; — and all these have craters and tubes of definite forms,
wliich result from movements in the water. These forms are
no accidents, for they can be copied in models, and they recur
at different places in Iceland. AVhen the tide flows over the
sand below Granville in France, thousands of sea-wonus
emerge from holes, and their long bodies and active feelers
stretch and w^ave in search of food. \Vlien the tide ebbs,
these creatures shrink back ; but loose sand sticks to their
slimy bodies, and in shrinking each adds a ring of sand to
the tube in which he hides. As multitudes hve together, a
mound of sand, pierced like a sponge, forms at last. Like
these, hot springs add to their tubes by every movement ; and
the form of the tube results from movements in the boiling
water.
Geyser Tales. — Of all these tubes, the best known and
the easiest to get at are the Geysers. They are only seven
days' journey from Leith, and situated near the base of a
volcanic hill somewhat smaller than Ai'thur's Seat ; a cone of
lava is at the top of it ; sand and cinders are on the sides.
To the east is a wide, flat, wet valley, beyond which, some ten
or fifteen miles away, is a low range of hills ; and behind these
the top of Hecla may be seen in clear weather. At the head
of the valley, fur away to the north, are dark, Ixire, high peaks.
300 TURKS AND SP1!1N(;S.
amongst Avliidi are euonnous fields of snow and ice. To the
west, behind the volcanic hill, at a distance of about a mile
from the springs, a range of liigh ground begins, which extends
a day's journey to Thingvalla, and includes a number of high
rocky volcanic peaks, and great lava-floods ; and SkjaldbreiS,
the great centre from which these flowed, is to the north-
west (see p. 409).
To the south-west the wide valley opens out into a great
boggy plain, which reaches to the sea. It is covered Avith
grass and marsh-plants, traversed by large rivers flowing
nearly south-west ; large lakes are in it ; and every here and
there rocky hills spring up in the moor like distant blue islands
in a firth. The whole country rests upon heated strata ; for
in a calm evening the white steam of hot springs may be
seen blowing off at intervals in the marshy plain. To the
east Hecla is still hot, and beyond it lies Skaptar Jokull ; and
hot springs are in that direction. Many are in the plains to
the south ; one is half-way to Thingvalla ; a little geyser is
near Keykjavik ; a spring is near the town itself ; and further
west are many more hot springs. The whole country is
volcanic, even to the Westman Islands, far out at sea ; and
even under the sea volcanic eruptions occasionally break out.
Streams of lava have flowed over beds of loose materials, and
now roof in and confine hot water beneath the surface ; and
so steam is forced to escape through vents, rifts, holes, and
cracks, like those which pervade the upper lava-beds. To the
north also is sullicient evidence of extinct volcanic action :
the land is high and snow-clad, and cold reigns there now ;
but beyond the mountains are many more hot springs.
All these have one thing in common : — they are all in low
grounds near the l)ase ol' \dleanic hills, midway between cold
and heat, ice aud steam ; where the' water which flows IVoui
TUBES AND SPRINGS. 397
tlie jokulls, through ashes and porous strata, shivered lava and
volcanic caverns, stands nearly level with the surface of the
flat marshy ground. Heat is below to boil it, a tough lava to
keep it from sinking deeper ; a region of heat, sufficient to
keep the great kettle boding, is below that ; and a great lid
of mountains is piled over the steam-boiler.
There is then every reason to expect that steam sliould
escape where the weight is least, and that springs should burst
out at the foot of the hills.
The tubes have still to be explained.
Above the great spouting Geyser, distant from it about
100 yards, and on the top of a steep bank of loose sand and
ashes, are several still quiet pools of water which are a few
yards wide, and which look as if they were puddles of rain
collected in hollows at various elevations. An active man
might leap over them ; and the wonder is how water can rest
at all on such porous ground. These are, in fact, springs hot
enough to boil food, and their depth is unknown. The water
is beautifully clear and green, and the sides of the well are
seen through it, darkening as they descend, till they are lost
in a black hole fathoms down. In August 1861, an emerald
green tongue was anchored by a string in one of these wells,
quietly boiling for dinner; while a kettle of soup; with a big
stone on the lid, was simmering up to its ears in hot water on
a natural bridge of stone which spans the pool. Far away
down on a sloping shelf reposed an old copper coffee-kettle,
which some former traveller had dropped in, and the boiling
water was slowly welling up in the middle, rising every now
and then, a smooth greasy mound, like the swirl which a sal-
mon makes when he rises at a fly and wags his broad tail in
derision at the cheat. A small steaming rill, the waste of this
well, and the measure of its supply, trickled steadily down tlie
308 TFliES AND SnUXOS.
l»ank, depositing stone on the ashes. As the eolfee-kettle liad
been on its shelf long enough to gather a crust, it is clear that
this spring, though boiling, boils quietly. It is of great depth,
and sucli a column of water would burst through the loose
ashes of which the ground about the spring consists. Two
such columns could not exist within a few feet of each other
at different elevations, in mere tubes formed in porous soil.
But the columns do so exist, side by side, in these natural wells.
They are enclosed within rough stone tubes, hardly pervious to
water ; and the question is, how these rugged irregular stone
tubes came to be formed at first.
If the question is answered for one tube, the formation of
similar tubes, wherever found, may be referred to the same
agency ; and similar tubes are to be found in all stages of con-
struction in many parts of the world, and more especially in
Iceland.
Rough Stone Tubes. — On the ridge above Thingvalla, to
the eastward of that valley and close to the track, at about
half a day's journey from the " kitchen," on a hill-side, and
below a considerable mountain, in a country whose surface is
wholly composed of bare cinders and lava, there stands a rock
which rises some eight or ten feet above the loose rubbish.
It might be carelessly passed as a clinker which had rolled
down the mountain, and a little way up the opposite slope.
It is in fact the protruding end of a rough stone tube of great
but unknown depth, and it is very like tlie tube of the
kitclien. It contains no water, and apparently never has, for
it is too porous to hold it. So far as the chamber can be
seen it seems to be a large conical hall of rough black lava,
covered by a small conical roof, with a hole in the side through
M'hich a man could creep. All round are scattered traces of
great heat. It is evident that this tube was made of melted
TUBES AND SPRINGS. 399
stones, and that the force which modelled it cast stones out of
it, for there they lie scattered all about it as fresh as if they
had fallen the day before. It is probable that this is a chimney,
which is or once was connected with a subterranean chamber.
Within a mile or two of this tube a roof of lava has fallen
into a cavern, over which the track leads. It is a large hollow
blown in the lava, but no one has explored it. About seven
or eight miles away the plain of Thingvalla has sunk down
over an area of more than a hundred square miles, leaving
broken edges to mark the original level of the roof (vol. i. p.
93). If the lava could be raised up again, and the rifts
mended, there would be a chamber in the valley some hun-
dreds of feet high beneath a roof some hundreds of feet thick
(vol. i. p. 90) ; and if such a lava-boiler were filled with the
lake and boiled, the steam-power would be sufficient to
account for many of the phenomena in the district. In parti-
cular, steam might well blow vertical tubes in soft lava, and
so shape Tintron, with its roof of clinkers and its spreading
lava-waves.
A couple of days' journey to the north is Surtshellr. It
is the best known of Icelandic caverns ; but every lava-flood
in the island seems to be honeycombed with great caves. At
p. 426, vol. 1, is a map which shows the position of Surtshellr ;
and the nearest iron-foundry will show how such horizontal
caverns are formed. The large one extends along the lava-
stream, and is at the edge of a slight fall in the ground. At
page 429 the edge of a broken roof is shown in the foreground,
and here the case of ThingTalla is repeated on a small scale.
The roof having sunk, small cliffs surround a hollow. The en-
trance to the cavern is to the right, and there the roof, though
much shattered, has not fallen. The cavern has been explored
for about a mile ; the roof has fallen in several places, and the
400
TUBES AND SPRINO
cave is partially filled \vitli snow and ice. At furnaces, slag
commonly runs in a trench scraped in ashes. As it flows it
freezes ; first at some considerable distance from the outlet. A
bridge of stone spans the stream, and then the tough surface
gathers behind the bridge, and forms a series of wrinkled
loops, which look like coils of string. This upper crust grows
up stream, while an under crust forms below ; the hot slag
flows on between them, and if the supply is stopped, the fluid
interior of this tube flows away till it cools and stops. When
Fid. lOf). — Vkrtical Section thhuuimi a Fuuzkn Stiikam hi \VkIiNklki> Si-A(;.
rrinteil from the Stono.
Folds oil the surface are like heavy drapery. The stream moved to the left, and fokis
gathered up stream towards the right. The fluid froze at the surface, and crusts and f(dds
which foiTOed under and behind each other can easily be traced from the structure of this
crust (see pp. 300 and 4'.>3).
this happens, the lower end of the tube is filled with tiic same
material which makes the sides and roof The workmen
break up this slag stream to let the fluid escape more freely,
and hundreds of broken pipes about the size of drain-tiles
may be found about any ironwork. It often happens that a
tube of this kind splits along the roof while cooling, and then
^ INGS. 401
sps ;;r; ;n .» '»'»::„:».,■? r;':;r«,.iHm,gh, a„ci the .^e
r-^4S ->;-;t'TX. •i;,^----pperm„.t layer is pris-
-^^- rrri 2^.0.--, -"-:":;';< """S withpe„dan.s
ao-J-'K •»=.•«. .so,»-w^rK" 'J' „a„,,,,t. xhese froze while
»..w»»w .„,,,, u.-.».»"»»™='i;iPf„,,,rf .con ■« The growth of this
"""S «"'"''°°r,rT=X»»°!'=n''"~ '""'Zh- its structure, and
oiSaq A3qx .a,,u.a.. IW^ ^"^^«^ ^"^^ ""^-l!^] Smmoa pi.s s^M ^S.
f -onqT^da^ o, Tionoo aaquiani -noq eqi<uiued CastleS, turrets,
ti;%S '.%."^-»»^S^^^^^^ '«>a by volcanic
-on." ?J~rJryVi?»Vr-n.'.:H pT-?S«.sed in beds, which
b ',= Sao\":>VS° -yo'-Srp^y^iow flows in hollow
of
tiurous va-
II •'•'■» Ua-'""SP«°;J SU°,' 5a,,U,-m Pf chimney, with
:r2::r;JlU".,^.rir.2>„JSrr.- Jra -nd. Far away
f« P"™ US-To, Vtq{s;a"ri"J^'4T,~^ slowing through
■ ::Z:^S^V^^^^^^i^^^ ^e dark crnst
te" rE'".r^.[^S^S»^ ■>- burst
L;,j.dp w»..H;^ri\:rr, jU »!,'»r;; east „ut some of
b.nr4 ie.n?« SHf«»"?^'^>>-">Ssn.phur,
1 paztuSooa. l J ^^^,, ,, S„,ws .- J^ojs^ . ,^,^ jo as.o aq,
'jgiiqw aq^ ^v -op^n^oi ^^r^ naMOiioi at^S« s^a^ 1» ^^
5B0l«aJ"^''^
heco
TUBES
matter, IhT""^ ^hat the '"^"''^^ rather >
"-^^/'s-"^-?<ii^toS!tr^;^oa
is that «
400
cavo
is pavlially fillec, -Uls^^JuKS.njK '- iiilC'S"'
commonly raiis in a trencl- >o Pe.^";5'i.Y,S^"° *'ir„r'''j'°° 'i«>™'i I "•»/«
freezes ; first at so„>e eonsi PuS'iT S*tr2^„f W'^ or«ir,::;» ^ '
bridge of stone spans ii^j^^'^^'S^J^dB'^^^Sff'^k^"'
loops, which look like co/-.4rs ^t■f :jJre\i- -r- s-'-
''« Sl.t„, ;« «;• propert, „r^ 'ftai Willi, i
gainers Denmci tiie
loops, which look like col ;«W .... -«.;. ,J*.-bS„:- f-'v / °'»^"Vi
np stream, while an nml .,"^.u.S'.%t';£. /.'wlid, "SJ'".' «?*r ;,""»';'<> ■
flows on between them
interior of
3tween them, ^/Kh^r^Jf "- ^-th't!e^t'^^--a"Kr N Wat-^,
«- ( B^ referred toVrhitTV''^ to thlZ^^^^^^^^^ t|
-^American ol.i^^'»''«n. As f3>"r, ''°" "f reco.? ; the an.lj
et referred toVb,^!«°/''d to thf S-'"" ''^'^''eea ' =°°'''^in? t,
-«A"ierican OoverJ'!''^"- As t^o t,,, " °^ '<'<=os- i "'« ansC.r
"■;r°'b°!r'-^^''j'C;rbt''' not £4^,"';f ^on of present I'jJ
-a>'ty of Vs°^. '>« cou"? t;"''''1"'=°'1 as -P^^'^' --^^ M
ji-ct being brou-L t ,**"»" bv th ^omp'o- ^^e «var of lJ
•"'''''' no doubt ^' ''"'se cJai>n?°' °'" for the / '"'"^ '^irin- /
KiCi, 105. — Vf;RTIC;l
Folds on th'
ot) "^ ""ritat on u-h T'Posed of fbr' '"esult "^"erates h
"•^' ' .''« honourab « n""°''->- «ame t^'\', "Po° ours I *'"' ''^'^oo
.r'^^l^iiln.^fc-'^ftheirL^^/Jl^/escuer^- /.^-eaffecte,
uApriUs<
gathered iii> stream towards i
which foiTTied under and beh ■ aiJ'i'"'"^?' ''erns nw '" Pointed oni" tu°'*'^"^
crust (sec pp. 300 and 4.:0. ■hti^ai'^? °°'"P .ntr^ *''«" he^ .""' , w ,
this happens, tlie lo.;»« ".wi IS '«C*.t/S'"''"« "f C", ^-••■
materir^vhioh n, rf?^f-^5'f,:iS;n^^
ds of lJ?«''ere"&,A« of S^L 'I'l'^^.S its S"/ | ^*'"- 'vouh
break np this sla, if^^;;»^-,^Wj;r--;-;^s /Gov^,,:^
and hundreds of IJf^i'ere. WeL/^\ of UtH ^"^ong it, „,^'^"; | bama ^ouJc
y be found abo '• "gaJ «h„^ed to X,"^ fheir c^--,ij;^ ^-ould / -nonths in,t
may Oe lOUnCl aDO'-«ffa/«h„^ed t";;Z"f iheirciii,'en^y ^<>nld j ^onths iast
'^''•e;rZ-«« .'■"Howe rtj\, the «an.o ;"
^« ''"'•'•otSJ '.''« benS,",7 P°'"'^-'"i the
"^'-^ '^''ui«itiof';*bich' •" thi ^"'"'"^l
"ion. m / tjio oeutrajl
TUBES AND SPRINGS. 401
a whole series of loops of slag—) ) ) ) ) ) — are torn through
the middle. The roof of Surtshellr is covered with similar
loops and coils, which show the directions of the flow. Tliey are
thick as cables, but exactly like coils on slag (see p. 423). In
many places these wrinkles are torn through, and the whole
roof is shattered. In a section the uppermost layer is pris-
matic; layers below are stratified horizontally ; the under
surface, where it is preserved entire, is hung with pendants
of spongy lava, with a vitreous crust. These froze while
dripping from the newly-frozen roof. The growth of this
horizontal chamber is fully explained by its structure, and
every lava-stream is full of such hollows.
Myvatn. — Vertical chambers also abound at IMyvatn :
many project through the hill-sides near the lake, and have
the most fantastic shapes. They suggest ruined castles, turrets,
and such-like edifices, but they were all built by volcanic
heat. In this region the lavas are disposed in beds, which
have been much broken, and cold water now flows in hollow
chambers beneath lava roofs.
Similar tubes may be seen at an earlier stage of growth.
Vesuvius. — In 1842 there was a tube at the bottom of
the crater of Vesuvius ; smoke and air and sulphurous va-
pours were then rising from it, as from a chimney, with a
loud rushing sound like the noise of a great wind. Far away
down in the earth a dim redness w\as seen glowing through
the smoke : it was earth-light seen through the dark crust.
Heat was converting some material into vapour, in some
underground chamber, and the expanding vapour had burst
through the earth, and made a tube by plastering melted
stone upon the sides. The same force had cast out some of
the spare materials; for half melted and even burning sulphur,
scorched cinders, and bits of lava and pumice, were scattered
VOL. II. 2 D
402 TUHES AND SriUNOS.
about tliG great hollow 1)asiu which suvrounded this hot tube.
The mouth of the hole itself was about the size of a coal-
pit ; and for size, shape, and material, it was extremely like
the empty pipes described above, aud the hot wells above the
Geysers.
It was choking work to get down to the bottom of the
crater of Vesuvius then : shoes were charred, sulphurous
fumes Avere swallowed, in passing over beds which w^ere
visibly burning; eggs were baked for luncheon, and sticks
were burned in red cracks in the lava. No man could have
approached the spot where the giant Fire was at work in his
tube, like a great sea-worm in a sand-bed.
In 1844 a small cone and crater had grown about this
pit, and through it more red-hot stones, and fountains of
dust and vapour, were thrown, as fountains of steam and
drops are thrown by bubbles of steam from boiling water.
The solids either fell within the hollow, and rolled down, to
be again blown out, or they fell outside, and rolled to the side
of the old crater. A small " cone of eruption" was growing
in the crater of the older cone of eruption, which stands in a
still older broken cup which, as it is now believed, grew
under the sea.
A few years later the work could be safely watched from
the upper edge of the crater, and it was thus described : —
The place where the mouth of a stone tube had been in
1842, the bottom of the crater, was filled by a pool of seething
lava, and a small lava river was slowly oozing through the
side of the cone about the level of the pool in the crater.
The stream flowed down outside, and froze as it flowed, as
Avater flows from a s])ring and freezes in winter. But every
now and then the red-hot viscid pool, which was doing its
best to freeze in the l.)asin, got a frcsli supply of heat from
TUBES AND SPRINGS. 403
below. It grew white-hot, and then the whole crater seemed
to fill with a purple haze, and then the surface burst, and a
fountain of hot vapours rushed up into the air through the
hole, carrying with it a thin flake-like stony material, which
fell in showers within and far beyond the edge of the crater.
Lava was then bubbling, and simmering, and boiling over in
the ashes ; heat was blowing a new tube amongst the cinders,
making great stone biibbles and breaking them, and scatter-
ing the fragments far and wide ; and as the finished tul)e
resembled the Icelandic tubes, it is probable that the tubes at
the Geyser were first made like the tube in Vesuvius.
In 1857 lava had risen in the crater of Vesuvius to the
level of the edge, and had formed a plain. On this two small
cones had risen ; they were hollow, and through them hot
vapours escaped ; they were like Tintron with its extinguisher
roof Later a fresh crop of hollow cones grew up ; and then
the plain, with its miniature cones and craters, was burst up
and destroyed.
Tubes radiating from the earth's centre are commonly-
formed by the escape of hot vapours through viscous hot lavas,
and mounds of definite shapes grow about these open tubes,
from overflows of lava and fountains of projectiles which rise
through the tubes.
Filled Tubes. — All these are as it were living specimens
of a common species ; their habits can be studied and their
growth watched, though they are dangerous neighbours.
Extinct varieties of the same tribe — fossil pipes and
chimneys, springs and chambers — also abound ; and they
are as easily known as a fossil bone when the others have
been seen.
In a quarry near the Drachenfells, on the Ehine, near
the top of a conical hill, such a tube was visible in 1846.
404 TUBES AND SPRINGS.
It was made of stuiie uf one kind, and filled with stone
of a different coloui'. It was iu the condition of the tube in
Vesuvius wlien it had filled with a new overfiow of lava, and
such strings are very common in igneous rocks of all ages.
They exist in granite, as well as in lava, and tell their story
of past action by their form, as clearly as fossil bones tell of
extinct life.
Small Natural Tubes. — To understand fossils it is neces-
sary to study living animals, and active volcanoes are not al-
ways within reach. To understand the formation of tubes by
heat the action must be watched ; and there is a veiy lively,
harmless young specimen, whose operations can be watched,
close to the Geysers. A little mud spring is in a hollow to the
north of the Great Geyser ; it is almost hidden amongst the
ashes, and about as big round as a stew-pan : in it the forma-
tion of tubes by hot vapour is going on. The spring M\as be-
trayed by a ploutering, poppling sound, which, to a hungry
Scot with the brevet rank of cook, was absurdly suggestive of
boiling porridge. A vision of a nursery and a rosy maid, a
stew-pan and a fire, rose up as if by magic amongst the cin-
ders ; but there is no porridge to be had in that benighted
land. A deaf French traveller, who was supposed to be dumb,
was startled into speech, and exclaimed, "Chocolate!" The
spring was full of half li<|ui(l boiling tough clay, through
which steam and other hot vapours escaped ; and as the
vapours burst through the surface and rose, tlie nnul ilowed
back and filled up the holes as fast as they were made.
This small tube-making engine was like Vesuvius when the
lava was soft in the crater and vapours were escaping through
it. If the material gets tougher the soft tubes will be finished,
and the poppling will cease, as it had ceased in Vesuvius iu
1842, M'hen the lava was hard though hot, and vapours were
TUBES AND SPRINGS. 405
escaping freely througli a rough tube. In course of time the
mud may be baked into stone, and the tubes will then
resemble larger tubes in the same neighbourhood. They
may become vents for liot vapours, or for hot water, or lastly
they may be filled up with some other material and become
strings like those which abound in all parts of the earth's
crust. The little natural engine is making tubes of the same
pattern as those which are made by larger engines moved by
the same force. By watching it the whole process may be
learned, as the action of a large steam-engine is learned from
a model.
Experiment. — If a small spring thus tells the story of a
l)ig one, the growth may be studied at home. Any material
which will melt and take a new form, and retain it, will
answer the purpose. About a pound of common red sealing-
wax was melted at a slow heat in a tin vessel four or five inches
deep, and the mass was allowed to cool. Cold water was
poured in till the mound of sealing-wax was covered all but
the top. A gas lamp was then placed under the vessel, and a
slow heat applied. The cold water in contact with the sealing-
wax kept the surface tough, while the lamp melted it below,
and in a few moments the wax began to boil on the dry spot.
It not only boiled, but overflowed because of the downward
pressure of the water, and the upward force of its own expand-
ing vapour. But as it boiled over, each successive overflow
cooled and hardened when it met the water; and so a wall
of hard wax grew about a pool of boiling wax. To make the
wall grow higher more water was slowly added, and the circle
rose and kept pace with the rising watt'r. Tlie pressure on
the surface of the wax increased as tlie water deepened, and
the lamp kept the wax boiling in the tulie as it rose. Down-
ward pressure outside forced up the Ihiid, and expansion
40G TUBES AND SPRINGS.
within drove it liiglier ; so the wall grew to be a hard tube
coutaiumg the same materials iu a fluid state. It was like the
Vesuvius lava-tube during an overflow of hot lava. If this
process had been continued to a certaui point, the heat would
have ceased to act, and the tube would have cooled into a
solid pillar ; but the form to be produced in this experiment
was an open tube, so the lamp was extingaiished when the
wall had risen about three inches above the mound of wax.
Gravitation and cold came into play ; the tough surface
of the wax hardened and became a roof which resisted the
pressure of the cold water ; the vapours inside condensed,
and the hot wax diminished in volume, so as to leave hollows
beneath the crust ; the atmosphere pressing upon the fluid in
the hard tube forced it back into the hollows whence it came,
and the hot wax sank in with a rushing sound. Presently-
some crack opened in the cooling roof of the chamber, and
water flowed in and rose up, filled the tube, and replaced the
melted wax. The wax tube had become a water spring.
The outer surface of the tube so made was wrinkled, each
fold corresponduig to an overflow of wax and a rise in the
water. The inner surface was smooth where the air plastered
it against the hard sides. The opening was wider above than
below, and of irregular dimensions ; but generally a horizontal
section was an oval or some rounded figure, while a vertical
section showed chambers and pipes winding about under the
surface of the wax. This experiment explains the making of
larger tubes, and gives some notion of the invisible mechanism
of the great Icelandic fountains. The model tube was joined
to a chamber, and so are the geyser tubes.
Experiment 2. — Plaster-of-Paris will take a form Avhile
plastic, and retain it when it sets ; it is easily moved by
Nvater, and serves well to illustrate tlie M-orkiD.i;- of mud-
TL'BES AND SPlllNGS. 407
springs and the formation of tuLes and cones in la\a. A
shallow tin tray was filled with dry plaster and heated over
a lamp ; an equal hulk of cold water was then poured in,
and it boiled when it reached the tray. The plaster set
ijiiickly ; but, before it hardened, steam had blown a large
clianiber, and pierced two holes in the roof. This contrivance,
when set to work, imitated the action of intermitting hot
springs : water poured over the plaster sank and filled the
chamber ; when it was heated, steam drove water spoutuig
out of the holes which steam first made. The action was like
tliat of a kettle boiling with the lid on, and with water above
the level of the entrance to the spout.
By sprinkling dry plaster over the sm-face while v/ater
was boiling out through these two holes, two craters were
made which differed materially in form. One was like the
Strokr, a deep conical pit ; the other like the basin of the
Great Geyser, a shallow bowl. Tn one, the water was always
far hotter than it was in the other. On breaking up the
model the reason was found. The roof of the chamber was so
formed that steam escaped towards one aperture, when a
certain amount of pressure was overcome. It only escaped
in the other direction after the ^\•ater had been forced out, so
as to dry a lower arch, and so open a passage into the second
tube. As most of the steam went one way, one si)ring boiled
furiously when the other was hardly warmed, though both
opened into the same boiler. The shape of the basin formed
about the tube resulted from the movements of the water.
The hottest radiated most directly from the source of heat,
and so made the steepest walls.
It would be tedious to describe all the plans tried and all
the models made.
Sealing-wax heated under dry sand l)uik'd up, and made
408 TUBES AND SPRINGS.
tubes with cones and craters, from which eruptions of sealing-
wax flowed like lava. When water was poured on, the tubes
became miniature hot springs. When the model was cooled,
tlie same holes and ducts were cold springs when water
poured on liigher points had sunk in. When a mound of
any material rose high enough it was sealed by cold, and
then fresh vents opened near the base of the mound where
resistance was least. At the top of the volcanic hill near the
Geysers is a sealed tube, and probably the hot fountains play
through vents whicli opened below, when the liill was made,
and the power greatly spent.
Similar Forms. — The same thing probably happened
wherever there is a hot spring under a hill, and where^'er
there is an open tiibe or a circular lake, near the base of a
conical hill whose top is of igneous origin.
The same power, though decreasing, would continue to
drive mud or water through tubes till the rocks underneath
cooled. Duddingston Loch below Arthur's Seat, and the
spring in it ; two round lakes below Benknock, in Islay ; r( )uud
lakes at tlie foot of the Jura mountains, and similar forms
elsewhere, may all be traces of the same decreasing igneous
action which raised up hills. Even cold springs flowing
tlirough underground channels may be relics of the same force.
Tubes can ])e made by pouring wet plaster into a hot
tra}'. Steam drives the plaster away, and it grows up a
hollow chambered mound with tubes and basins, each a
miniature hot spring. The movements and the forms whicli
result are like those which resulted IVoni tlie freezing of silver.
The same forms are produced by shaking dry plaster into
l)oiling water, as meal is shaken in to make porridge : the
plaster is moved by currents, and takes a cast of the rny-
ibrce which nioves them. I*otters' clay, paste, porridge,
TUBES AND SPRINGS.
409
asphalt, glass, slag, iron, lava, or any other material through
which vapours can force their way, will take these casts ; and
the form is a record of the force of heat radiating from the
earth outwards. The highest mountains in tlie world contain
tubes ; they pierce the crust in all regions, and they can be
made at will experimentally, by setting radiation and gravi-
tation to work upon fusiljle solids, and vapours which can be
frozen.
In all these examples — in i'urnace-sparks and refuse, in
volcanic bombs and lavas, and in terrestrial volcanoes— radi-
ating tubular forms residt from radiating movements caused
by force radiating from soiutcs of heat and light.
TiiL (jtv brs iRni THE Horse Tr\CK
The lull 111 tliL iiiiiUlk i.s \ukaui( . Fi.iin it tlit top of Hetla ma) bt stcii to the light.
To the loft, beliiii.l the hills, and out of sight, is Skjahlbrcia. Glaciers are amongst tlie
liiUs ill the baekgronii.l. (See pp. 3<'0, 413, and Vi-l)
CHArTEE LVI.
SPRINGS, CHAMBERS, TUBES, CRATERS, AND CONES.
Chambers in a crust often communicate with tlie outside by
tubes ; but these are often partially or wholly filled with
vapours, fluids, and solids, which escape from the interior of a
cooling mass. Sections of volcanic bombs (p. 379) show this
structure ; the growth of it may be watched in models ; and
hot springs in Iceland give samples of this work in all
stages.
These tubes differ from rough stone tubes near them ;
they are smaller, less porous, of regular shapes, and lined with
materials deposited by water. Some are partially filled, others
are choked up.
It has been shown that the Great Geyser and springs about
it probably communicate with the interior through tubes
blown in lava near the base of a small volcano. The cut,
p. 409, shows the position of these springs at the foot of a
hill. The Great Geyser now spouts through a smooth vertical
shaft, which is cliicjfly made of silica deposited by the water.
The mouth of this steam-gun spreads a little near the top,
somewhat like a " bell-mouthed blunderbuss ;" and about
this muzzle is a shallow saucer. The woodcut, vol. i. p. 12,
is from a drawing made in the saucer after an eruption.
Beyond the rim of the " crater" a conical mound spreads and
slopes every way at a small angle. The woodcut, p. 414, is
SrrJNGS, CHAMBERS, ETC. 411
from a drawing made at the base of the mound during the
eruption which emptied the crater, but did not empty the
pipe. The dimensions ascertained by measuring with a sahnon-
line and a fishing-rod are: — breadth of basin, when lilled, 57
feet at the widest place ; breadth of pipe, about 20 feet, but
somewhat less where the walls are vertical ; depth from the
surface of the water in the centre when the crater is full, 75
feet ; ledge upon which a plummet rests on one side, 45 feet.
The diagram, p. 415, is drawn to scale from these measure-
ments. The Strokr or Churn is a conical pit, 36 feet deep.
At about 22i feet is a hole in one of the sides ; at 19 feet is
a hole on the opposite side. Water generally fills the i^it to
Avithin 6 feet of the top ; but after an eruption both side
vents are occasionally seen. The mouth of the pit is sur-
rounded by a raised wall of silicious stone (see title-page, vol.
i.), in a shallow saucer much broken, because it is usually dry
and exposed to frosts and the feet of men and cattle. At the
mouth the pipe is 8 feet wide ; it is less than a foot wide 30
feet clown. A third pipe spouts occasionally ; the mouth is about
the size of a hat, and the hole seems to expand as it descends.
Besides these three, many other smooth pits and pipes, of
various shapes, contain boiling water and mud of various
colours ; and these, within an area of a couple of acres, are
near about the same level. Higher up on the hill-side are
springs which do not boil and spout now ; and still higher,
old tubes are covered or filled, and their sites are marked by
petrified grasses and twigs and ripple-marked stones, like
those which surround the Geyser. All these forms result
from movements in the water, and these from the earth's heat.
The Great Geyser is geuei-ally full up to the brim, and
movements at the surface suggest two forces nearly balanced :
these are weidit and heat. From time to time the water
il2 SPIUNOS, CHAMBERS —
rises a few inches, overflows a little, and sinks quietly down,
to rise again after a pause. It is like mercury in a barometer
when gusts pass. Atmospheric and steam pressure may
regulate these slow movements, and the eruptions. Every day,
sometimes every hour, the kettle simmers. Bubbles of steam
either form in the tube or escape into it somewhere near the
bottom, and these condense suddenly in colder water. The
sound is like that of a blast in a mine — a quick, loud report,
which shakes the ground to a great distance. When fires are
lighted in a steamboat, the noise of simmering is very like tliis
natural artillery : vibration passes through boiler and ship
to water and air about it, and waves spread horizontally
from the sides of the ship. The sound is commonly heard in
houses warmed with hot-water pipes ; and walls are shaken
when bubbles of steam collapse in boilers. Steam may be
watched in a hot spring at Eeykholt. There the water is
very clear, and about three feet dee]) in tlie basin ; bubbles,
large as cricket-balls, rise at intervals out of u hole ; and abo\'e
this vertical tube a dome of water rises on the plane sui-
face. From it water spreads in radiating streams. The pool
is shaken when bubbles collapse ; when they reach the sur-
face a dome bursts, and a fountain of drops and steam spreads
and scatters in tlie air. Tn larger springs the bubbles cannot
be seen, Init they can Ix' heard. They do not always I'eacli the
surface, but they start an n])ward current, which makes a.
dome and flow in the circular pool which fills the crater.
This movement follows the well-known sound of collapsing
steam simmering on a large scale. The radiating flow makes
beautiful curved ])atterns of streams, eddies, whirlpools, and
waves, which are reflected from the sides of the basin. The
brink is wetted by every rise, and dries after every I'all ; and
idtci' each change vapour leaves (he solid which hot water
TUBES, CRATERS, AND COXES. 413
had dissulvL'd. Tlie edge of the crater and the outside of the
cone grow continually, while currents shape the tube and
basin by rising and falling, by spreading and converging. As
in a model, the shape of the tube is a cast of the currents
which move in it.
Of all unpunctual exhibitions the Geysers are the most
provoking. In ISGl the grand fountains went off as a party
of travellers came in sight of the place (p. 409) ; they saw
white clouds of steam three miles away, and that was all they
saw. The tent was pitched and a watch kept; but the
watchers fell asleep, and it is said that the Great Geyser ex-
ploded without rousing the tired sleepers. Every few hours
came the warning — thud, thud, thud — which kept expecta-
tion on the stretch ; but nothing came of it all next day and
all next night. One man was packed up in a bag of mackin-
tosh cloth, and laid out with his face to the spring, to make
sure of one sentry ; but he saw nothing. He looked very
picturesque, somewhat like a mummy extracted from its
wooden case. All next morning the water rose and fell, and
sank and rose again, balancing. Tired of waiting, the party
set off at last, and met a fresh party going to the place. They
arrived in the nick of time, saw" an eruption, and returned
next day. In 1862 the disappointed returned. One party,
who had very little time to spare, rode in hot haste to Hauka-
dal, and saw many eruptions in a few hours. Those who
followed more leisurely waited for three days ; l)ut this time
they did see the show. It was a grand display, and well
worth all the waiting. Instead of ending suddenly or gra-
dually, the steam-salute shot faster and faster ; thuds fol-
lowed each other rapidly, and the whole ground shook ;
then the sound of dashing water, the music of waves,
was added to the turmoil. A great dome rose in the
't ,.,, :;'% —I
SPRINGS, CHAMBERS, TUBES, CRATERS, AND CONES. 415
middle of the pool, and frequent waves dashed over the
edge of the basin, while streams overflowed and drenched
the whole mound. Great clouds of rolling steam burst
out of the water domes, and rose in the still air, swelling
like white cumulus clouds against a hard blue sky. Up they
rose, whirling rings and spheres of vapour driven by the
earth's radiation ; and down they came, showers of drops
dragged back by gravitation. The underground artillery was
silenced, for steam had the mastery of pressure, and the kettle
boiled over. At last the whole pool, 50 and odd feet wide.
— 1 —
Fui. 108. Stroke .\nd Geyser.
rose up a single dome of boiling water and burst, and then
the column in the tube, 70 feet deep and 20 wide, was shot
(jut of the bell-mouthed blunderbuss with a great burst of
steam. The charge scattered as shown in the woodcut ; it
rose about 60 feet, and most of it fell back, and sank in with
a rush ; and so the glittering fountain rose thrice like some
mighty growth. After the last effort, the pool was empty,
and the pipe also for a depth of 6 feet ; the spilt water was
steaming down a stone aqueduct of its own building, and it
41(3 SPRINGS, CIIAMBEES —
tumbled iuto a cold burn in the wet niuir at last. By this
eruption the tube was scoured and smoothed, and something
was added to tlie basin and the mound ; for mutton-bones,
feathers, and suchlike, were covered with a crust in a year.
Each drop, large and small, had its own motion while it flew ;
it described a curved path, revolved, and threw off part of its
mass in steam. If it travelled far enough, it might freeze ; if
hot enough, silica held in solution by water would be left by
steam in the air. Inner surfaces grow inwards, upper and
outer surfaces grow upwards and outwards ; and so this pipe
will choke at last, if the growth continues. The mechanism of
the Great Geyser cannot be seen, because the water is too deep.
The Churn is sometimes emptied so far that the works are seen.
Strokr is a conical oval pit, less than six inches wide
near the bottom. The size of the plummet used makes a
difference in the soundings, and possibly there may be
some small steam-pipe at the end of the cone. The
water is always surging, growling, and frothing about Avitliin
6 feet of the top. Steam rises through a hot colunui 13
feet deep, and never collapses, because there is less pressure
to be overcome ; this well boils, but does not simmer. By
turning a barrowful of turf into the pit, this kettle is made
to boU over ; steam is stopped, the water is stilled for some
minutes, and the mud is greatly heated below. Then a dome
grows and bursts, and wad and water and steam from the gun
grow up like a giant sheaf of corn. First the water in the
well makes a furious swirl, like an eddy from a stricken
whale in shoal water ; and then the column rises and over-
flows slowly with increasing swiftness, till the dome rises
up and bursts, to make way for a steam-bubble as big as a
balloon. Up go the projectiles, and down they come in
showers and streams, to rise again with furious bursts ; and
TUBES, CKATERS, AND CONES. 417
woe betide the spectator who gets within range of this scakl-
ing spray.
After one of these displays the water-level was more than
20 feet from the edge, and then at 19 feet the month of
one tube was seen. From this hole, which was about half a
foot in diameter, boiling water and steam jets squirted into
the pit at intervals ; and it soon tilled to the old level, and
hissed, and growled, and frothed, as before. Another hole
was seen by an Icelander in the opposite side of the pit at
22 feet from the top. The spouting of Strokr is caused
by the shape of a steam chamber, and the mechanism is the
same as that of a closed kettle or the models above de-
scribed (p. 405). The shape of the pit results from the move-
ments of the water, and these result from temperature and
hydraulic pressure. Because the movements are violent and
very irregular this tube is rough, and layers deposited in it
are strangely contorted (see title-page, vol. i.)
In all probability the mechanism of the larger fountain is
built on the same principle of steam chamber and tube. The
lateral steam-pipe in Strokr has a projecting roof ; on the
north side of the Geyser-pipe a plummet rests on some ledge ;*
and when the tube is filling steam-bubbles rise at the place
where they woidd appear if they came from under this roof.
By long practice a fisherman is able to tell what goes on at
the end of his line. An old comrade, a salmon-rod whicli has
earned many a good meal, was used to get a large thermometer
into the middle of the Geyser tube. When the weight was
near the ledge, after it had fallen from it and sunk a few feet
some force appeared to lift it, and drive it about, for it strug-
gled like a fish in a flurry. AMien it was hauled up it had
* Mr. Biyson of Eiliulmiyli was the first to discover this ledge, so far as I
know. His discoveiy was tested afterwards, and the ledge is a faet.
VOL. II. 2 E
418 SPRINGS, CIIAMBEKS —
burst. The explanation suggested by tlie sliape of Strokr, and
by nnnierous models, was tliat steam, or currents of very hot
water, were spouting sideways into the tube under the ledge.
When the plummet sank lower it ceased to stniggle, and
pulled steadily at the rod. According to experiments made
by Mr. Bryson in 1862, the temperatures marked in the
diagram were overcome by the pressure *
A column 37 feet deep prevented the formation of steam
at 253° of Fahrenheit. A deeper colunm of 75 feet made
steam bubbles collapse at the high temperature of 270°, but
soon after this temperature was got the Geyser exploded.
It seems impossible that a layer of lava or of any other ma-
terial only 75 feet thick can still continue hot while the sur-
face has been cool ever since the Geysers were first discovered.
The source from which the heat comes must be far deeper ;
and probably steam rising from great depths heats all these
kettles and makes them boil over.
The Little Geyser spouts occasionally without any ^\•arning,
and rises, 50 feet at least, like a fountain, from its narrow pipe.
The rest of this family bubble and sputter, each on a different
plan.
The Oxhvcr, like the Geyser, is near high ground in a
district of recent violent disturbance, but on the north side of
the island, about 140 miles away. A number of pipes, with
craters and cones formed about them, are near a marsh at the
foot of the hill ; of these, one is called the Bath-house, because,
according to tradition, it burst up through the floor of a house.
* Mr. Biyson's plan of taking the temperature was ingenious. A nuinber
of thermometers were filled but not sealed. These were lowered, and part of
the mercury was spilt. "When it cooled it left an open space. By heating
Uir tulir till the .space was filled again the temperature was got. A common
iii.iNiiiiuin thermometer made for a high temperature (260°) burst or was
su.ashrd ill tlic first trial.
TUBES, CRATERS, AND CONES. 41 'J
The woodcut, vol. i. p. 16, is from a sketch made in 1861. It
is a small copy of the Geyser, and the water balanced in the
same way while dinner was cooking in the overflow. Close to
tliis pipe, in the same stone mound, is a copy of Strokr, a rough
warty irregular basin, with a wall about a conical pit, in which
water seethes furiously within about six feet of the top. The
Badstua explodes occasionally when the steam gets up ;
the other is always expending all the force it borrows from
some chink or hole in a steam chamber under groiuid. A
third pit is called the Oxwell, because an ox fell in and was
boiled. Bouillon came with the first eruption, bouilli at the
second, and a third effort cast out bones. This well is within
100 yards of the other two, has an intermediate shape and
depth, and works on a different plan. The shallow conical
miniature churn is always boiling furiously. The deeper
Oxwell boils over at intervals of ten minutes : the basin is
rough, and the tube somewhat conical. The deepest of this
set — the Bath-room — simmers and shoots underground, and
balances on the steam, but explodes occasionally when the
steam gets up. The shape of it is like that of the larger pipe,
which j)lays on the same plan.
The level of the Kitchen, above described (p. 397), is con-
siderably higher than the level of the Geyser, and therefore
steam has a greater pressure to overcome. The water balances,
but neither seethes nor simmers, nor boils over. The shape of
it differs, for it has reached old age. The sides of the tube
are never above water, so they gain nothing by evaporation,
and grow slowly iiiwards. The waste is small, so the pipe
must be narrow below. The chief growth is at the inner edge
of the highest layer, where the stone is alternately wet and
dry, and for that reason the large rough tube of the Kitchen
is roofing itself with a slab. A bridge spans the pool already,
420 SPRINGS, CHAMBEKS —
iiud the eilges are growing horizontally. AVhen this flat roof
is built, it will either burst or keep down the steam in a closed
chamber of large size. ]\Iany such caverns are hidden under
loose rubbish. About the Kitchen, holes open occasionally,
and betray them ; and, on a still cold evening, white columns
of vapour rise up and hover like ghosts of buried Geysers above
their hidden tombs.
So far, one result of terrestrial radiation is to build cluim-
bers, tubes, basins, and truncated cones, with materials held
in solution by hot water, brought from below to the surface,
and deposited there at low temperatures. The same action
carried further makes a sealed cone. Near Eeykholt, about
50 odd miles to the N.W. of the Geysers, a spring has built
a mound in the middle of a cold river. Steam rises through
the gravel, and the spring boils furiously, and boils over every
few minutes. It rises through tubes with small basins at the
top of a steep gray mound some 10 or 12 feet high. Neigh-
bouring hills, which make one side of the strath in which
the river flows, are made of bedded trap, the beds dipping
towards central high hills to the east of the place. A fault
cuts vertically through these beds, and it seems to run to-
wards the place where this hot spring has bidlt a stone
mound in cold Avater. Some few miles away, a whole cluster
of springs have been spouting for many years, and at Eeykholt
is the bath in which Snorro bathed centuries ago. Opposite
to the spring is another " fault " in the old beds. In No.
1, p. 379, a whole system of " faidts " may be traced from the
crust to the centre of a stone, and many of these pass through
cliambers which were hot. The terrestrial heat which boils
(dl these springs may be at a great depth, and faults may be
ducts for superheated steam. The hot region certamly is
lower than the sea-level. A large spouting spring is close to
TUBES, CRATERS, AND CONES. 421
the sea at the southern shore of the great bay of Faxefjordr.
No near ground is high enough to account for this fountain,
and the sea wouhl have cooled this point long ago. The fires
which work these engines at so many distant points must be
far down, and the power the same which builds mountains.
Sixty miles about north from Eeykjanes, Snte fells JokuU is
built on the end of a point. It is 5808 Danish feet high, and
the shape of it is very like that of a mound built by a hot
spring. A sketch of Sntefell is at p. 85, vol. i. All these
forms, which are seen growing slowly about hot springs —
chambers, tulies, craters and cones, domes and streams —
aboimd in lava and in mountains in Iceland.
At Myvatn, in the north of Iceland, is a cluster of extinct
volcanoes. These rise 6 feet, or 10 or 12, or 50 or 60; and
near them are mountains of like shape, which would cover
half the site of London. Fifty or sixty of the small hOls are
within a square mile, and great streams and lakes of frozen
lava cover neighbouring districts as big as small counties.
Some of these are bare ; others are covered by sandy and
marshy plains, by large lakes of water, and by dry deserts
of gravel and sand. Through these, large glacier-rivers cut
channels, and they build stratified deltas, pack silt, and make
sections. A few days spent in this country are worth whole
years of geological study elsewhere. It would be easy to cut
through many of the small mounds ; but their structure is so
evident, and so many samples of them in all states of growth
and decay abovmd, that to dig w^ould be loss of labour.
In the first place, many chambers are open.
Close to the small cones — so near as to make it evident
that one set of forces shaped the whole — the upper crust of the
lava was blown into small domes, like bubbles blown on
metals or on boiling water. Many of these domes are broken,
422 SPRINGS, CIIAMr.KrvS—
so lliiit. hollows beneath can he se(Mi. When snow covers
tliis tract in winter, swelling forms remain to show what is
beneath ; and if the earth has an igneous crust, upthrows in
sedimentary rocks may, in like manner, betray buried cham-
bers of like origin. Silt-beds are now forming in the lake,
above molten lava-domes, and the sea and its sedimentary
formations may cover larger hills of the same kind. The
whole of a large undulatmg plain near My^^atn is thus cham-
bered. Near a church on the west side, a track leads over a
series of vaults, most of which are split at the crown of the
arch, and through these rifts water is seen flowing over the
next layer of a series. A section of one of these vaults is
exactly like a low flat bridge spanning a pool, but it is part of
a bubble, formed as bubbles form on the Geyser before it ex-
plodes, or on a kettle when it boils. The upper crust is three
to four feet thick ; the surface is wi'inkled ; the roof of the
chamber is smooth ; and a section of it shows a series of
bent layers like those which roof in Surtshellr (vol. i. p. 429).
The floor is rough and w^rinkled like the outer surface. The
dome was blown while the floor was fluid, and the floor flowed
and froze after the roof was made. If t^^•o concentric shells
have tlnis formed, any number of them may exist at any
depths, and chambers may bo of any size. The crust of the
earth may be like the crusts of the stones, p. 379. If such
large chambers exist, it must be a question of power and re-
sistance— heat and the strength of the boiler — whether the
roof shall bend or burst, leak, yield, or resist.
The same lava-domes, the same vaulted lava-ice, abounds
at Rcykjalid, on the other side of Myvatn. A stream poured
over some rough ground, and froze to a thickness of four or
five feet : it poured on below, and left the ice stranded. It is
rough and broken, cracked, starred, and uneven, like " blind
TUBES, CRATERS,
AND CONES.
423
aownwards (in the impressions on this page). See p,. ^^^^^^^^^ „, ,,,„,..
right, and show the characteristic fom of a lava flow of smaU size.
42-i SI'RINOS, C'lIAMHKKS —
ice" on a })(iik1, or ice strandtHl l)y the ebb ; but here every
movement is recorded by wrinkled folds on the surface. A
little way from this shattered crust the horse-track leads over
a dome-shaped, swelling, wrinkled surface, starred and torn,
but not broken up. Under that roof are chambers, and the
tramp of horses rings hollow as they pace along. Cracks in
these domes show that some upward thrust tore them while
they were tough. These are " craters of elevation " in all
stages of growtli.
The lava at Surtshellr and at Thingvalla has sunk, so as
to make a "crater of depression," if such a phrase may be
used ; and the broken edges at Thingvalla are hundreds of
feet thick. Forms which resulted from freezing can be seen
in section in the rifts.
In Henderson's Iceland is an account of a great eruption
which took place in l78o. At page 225 is this passage : —
" Tlie torrents (of lava) that continued to be poured down proceeded
slowly over the tract of ancient lava to the south and south-west of
Skal, and, setting fire to the melted substances, they underwent a fresh
fusion, and were h(;aved up to a considerable elevation. It also rushed
into the subterraneous caverns ; and, during its progress underground,
it threw up the crust either to the side or to a great height in the air.
In such places, as it proceeded below a tliick indurated crust, where
there M'as no vent for the steam, the surface was burst in pieces, and
thrown up with the utmost violence and noise, to the height of near
180 feet."
Here was an upheaval of a tough surface, and the bursting
of a hard crust, by imprisoned air and steam expanded by
heat, and the action was on a large scale. At page 228 it is
said :- —
" With respect to the dimensions of the lava, its utmost length
from the volcano, along the channel of the Skapta down t(i Hnallsar
in Mcdalland, is about .'iO miles ; and its greatest breadth, in the low
TUBES, CRATERS, AND CONES. 425
country, about 12 or 15 miles. The Hverfisfliot branch may be about
40 miles in length, and 7 at its utmost breadth. Its height, in the
level country, does not exceed 100 feet; but in some parts of the
Skapta channel it is not less than 600 feet high."
A tract of about 1500 square miles was covered with
fluid lava in a few days to a depth equal to the height of
moderate hills, and that amount of matter was pumped out
from under the earth's crust, and flowed over it, leaving, it
must be assumed, an equal hnllow beneath.
It is hard to guess what is the power of an engine whose
boiler may have the dimensions of the Firth of Forth or
the Firth of Clyde, and whose furnace is hot enough to fuse
lava.
If lava-bubbles were blown by steam generated in small
cracks and caverns, what would the steam of the larger cavern
accomplish under the pressure of such a roof ?
In old lava-streams near SkjaldbreiS many samples of
like work may be seen. One great bubble, as big as a cellar,
with a roof two feet thick, has a large open angular gap in the
top. It was burst, and the keystone of the arch was blown
to a distance of ten or twelve yards, where it now rests upside
down. It must weigh some tons.
If domes on a biscuit are reproduced in lava hundreds of
feet thick, similar domes of greater dimensions may build
volcanoes in proportion to their size. The crusts which are
seen in cliffs along the coast of Iceland may roof in caverns
from which Hecla grew ; for cones of like shape grew from
smaller lava-crusts at Myvatn. It is not possible to get at the
works of the big engine, but it is very easy to dissect a little
one ; models can be made and broken ; and cones and craters
near INIyvatn are as easily seen as models.
Chambers abound. Tubes of lava like Tintron (p. 398)
4:2C> Sl'HINOS, (HAMREKS —
also abound in tlic district. Near the church are cones and
craters of eA'ery pattern.
Some are truncated cones, with a conical hollow in tlie
top : these are " cones of eruption" — mere ramparts of black
frothy cinders without one solid block or stream of lava out-
side. The}^ are regular in form, and grass is beginning to
sprout on their smooth sloping sides. Rain is beginning to
furrow the slope ; and in winter the mound is covered with
snow. The little volcano is then like Snrefell, or any other
high cone of eruption. The shape is enough to betray the
extinct volcano in the Andes, or elsewhere. In this case a
circular rampart of ashes conceals the tube through Mdiich a
fountain of vapours and stones played. Vesuvius and Hecla
are like this specimen. It would be easy to cut through the
little mound, but a walk of a few yards does equally well.
One regular truncated cone of eruption, made of loose
cinders, stands with part of the base in the lake, and it has
been tilted bodily to one side, but so quietly that this mound
of loose ashes still retains its shape. It is now covered by a
fine sward. In the centre of the crater, the end of the lava-
tube, through Avhich the fountain played, is seen. Six strange
weird-looking blocks of dark rough lava, like the roof of the
Tintron tube, peep through the turf like a circle of stones
about a hero's grave. These mark the source whence tlie
cinders came — the place where a choked tube is buried under
a circular barrow, which a miniature volcano piled over its
own head before it expired. If the mound were in England
it might pass for a work of art. It is no work of human
skill, but a sample of a cone of eruption — a tool-mark of a
natural engine worked l)y terrestrial radiation. It would lie
easy to dig out the buried tul)0, but a walk of a hundred yards
does better.
TUHES, CRATERR, ANF* CONES. 427
Close at htiiid is another specimen of the trilie, whicli has
not grown so far as to hide the lava core of a cone of erup-
tion. In the middle of a circular mound of loose ashes stands
a truncated cone of lava, with a plain on the top. In the
middle of the plain is a depression, with a set of radiating
cracks, and round the edges of the plain is a raised rim. The
work stopped at the stage which Vesuvius had reached.
When the crater was full to the brim (p. 403), it was like the
basin of the Geyser before an eruption (p. 414) ; and the last
movement was downwards, as in the case of the sealing-wax
tube described above (p. 406).
In the first of these three mounds the tube is hidden by
the stone fountain which rose from it and fell about it ; in
the second the end of the pipe projects ; in the last case the
top of a lava-cone frozen about a lava-spring, the frozen
lava-pool in the lava-crater, and the choked up lava-tube,
stand together in the centre of the ring of projectiles, which
scattered as the drops are scattered from the craters of
springs, or from boiling water anywhere. If the power had
been sufficient to keep this tube open and continue the work,
the ring of ashes would have risen till the edge of the tube
was at the bottom of a funnel, like that which surrounded
the tube of Vesuvius in 1842 (p. 402). But the power
was spent before this hill had grown ; the fountains ceased
to play, the spring froze, and the shape remains to tell its
own history of the works of Frost and Fire. This lava-
mound is about the size of a small glass-house chimney;
but within sight of it is a mountain of the very same
pattern, which, though not so high as Vesuvius, covers more
ground. It would be easy to quarry a hole in this specimen,
and as it sounds hollow, there may be a chamber within the
mound. It would be easy to cut a trench through the circular
428 SrKlNGS, CHAMBERS —
niouiid of aslies, but sections of similar mounds are close at
hand.
At Bonn, on the Ehine, the seven hills are larger specimens
of this class. In 185o the river was crossed from Bonn, and
several of the hills were scaled. They are truncated cones,
with plains on the top, and one at least has part of a circular
rampart about the plain. If these ever were surrounded by-
rings or mounds of projected ashes, they have been washed
away ; but ancient lava-streams which flowed from these old
lava-springs can be traced along the slopes opposite Bonn.
The Castle of Godesberg is on a mound of the same descrip-
tion ; and all these sound hollow, though made of rock At
Myvatn small lava-cones are in all stages of growth, and some
are in fact hollow cones, like Tintron.
Many of these have no mounds of ashes about them ;
others have. One stands in a ring about IGO yards across ;
the lava-cone is about 30 feet high, and it has a circular plain
on the top, with a rim about the edge, and a hollow above the
place where the tube ought to be ; it rings hollow. The sides
are steep, and it was no easy matter to reach the top. The
plain seems to consist of balls of lava as big as grape-shot, set
in frozen lava like plums in pudding, or barley in broth.
Close at hand is another specimen without the roof. It is
about nine feet high, and shaped like a glass-house or a lamp-
shade ; it is made of rough clinkery lava, and rises through a
plain of cinders. Near it is another about the same size and
shape, but one side has broken down, leaving a shell about
three feet thick.
It is easy to creep into these and otliers like thom. In
some the inner surface is smoothed, and groovod, and plastered
by fountains of vapour or fluid, which fiist blew them and
then S])0uted through them, and so rilled the gun. Close to
TUBES, CRATERS, AND CONES. 429
one of these a lava-bonil) was found (p. 370). Near to these
are domes which have burst, bubbles which have not burst,
and frozen lava-sj)rings, with a dome surrounded by frozen
wrinkled streams, which radiate from the source.
The growth of a volcanic mound is thus illustrated by
small samples in all stages, and the mechanism of the small
engine is well seen.
A lake of lava froze while boiling. Chambers formed
under the crust, and hot vapours which made the chambers
struggled to escape from them. In some cases a bubble was
blown ; in some the bubble became a hollow cone ; in other
cases the chamber leaked. Tubes were blown, and through
them springs of lava, or fountains of stony froth and vapours,
were driven by the earth's radiation, as foimtains of steam and
hot water are driven by it through geyser tubes.
Large specimens of like work are in Iceland, and may be
seen in a couple of months.
Near Myvatn is Krabla ; and one set of rocks on that
mountain appears to be parts of a hollow cone of lava,
through which hot vapour escaped and fused the inner sur-
face, to make obsidian. The place was seen late in the even-
ing, and this may be an error.
At the foot of this mountain are many old craters and
many boiling springs, and from it old lava-streams diverge in
many directions.
From the top of any hiU in this neighbourhood scores of
larger cones of eruption may be counted, and small ones may
oe reckoned by hundreds.
In crossing the island from Hecla, by way of Sprengisandr,
still larger specimens rise up through snow and ice on all sides.
Hecla is a cone of eruption, and round the base of it are
enormous tracts of lava, great frozen plains without a blade
■130 SPRINGS, CIIAMBEItS —
of grass, in wliicli strange weird solid fountains of frozen lava
stand up like black monsters where they froze. The base of
Hecla is wide, and the crater is small in proportion ; another
effort would finish the cone, and roof the tube like Tintron.
But the tube is there, though buried ; and as soon as the
power accumulates sufficiently it will burst, as it did a few
years ago. \Miere it will burst is a question of power and
resistance. The last eruption broke out near the top, and a
considerable lava-stream flowed down a hollow, froze sud-
denly, and formed clinkers. The only substance to which
these can be compared is " pulled bread " — crumb torn to
bits and baked hard.*
All down the Sniefell peninsula, on both sides, arc cones
and craters of many shapes ; but specimens like them all may
be found at Myvatn in a morning's walk.
From Helgafell a great yellow mountain is seen. It was
a cone and crater of eruption ; but one side of the crater burst
out, and the fallen rubbish makes a stream of heaps, sorted
apparently by a water-flood. Perhaps a lava-stream did the
work, and is buried under the floats.
At the head of this regiment of volcanoes is the great cone
of Sufefell, with its plains of basalt.
All round Faxefjord are small lava-craters, surrounded by
lava-streams, which rose and flowed every way as from a
spring. One of these is Eldborg (fire castle.) It is made of
lava, disposed in beds which dip every way from the edge
of the crater. The stone is spongy and brittle, and it must
have seethed like Strokr when it overflowed. At the bottom
of this great cup is a boss of hard lava, the crown of a solid
pillar, which froze in the tube. For miles around this frozen
lava-spring streams radiate. The newest are clinkers, piled
* F..r a skctrli of Hecla, si-e titlo-pngc, vol. i.
TUBES, CRATERS, AND CONES. 431
in the wildest confusion. To climlj over tlieni is almost
impossible. Tt is exceedingly dangerous ground, for the stones
are hidden by mosses and lichens, and feet and hands slip into
unseen rifts. The stones move easily, and break ; and the sur-
face cuts like shivered glass. Older and larger streams, which
came from this source, are like other lavas in Iceland — com-
pact, firm stone, with a wrinkled surface. At a guess, the
crater at Eldborg may be about 400 yards wide, and 200 feet
deep. No measurements were taken, but sketches were made.
Most of the valleys which drain into Faxefjord have small
cones of eruption and streams of lava, and in many cases the
cone stands in the middle of a far larger broken-down crater,
of a different colour and make. Each of these would be a
study, but mental pictures alone were brought home from this
region. To the right is a low marshy plain, reaching to the
sea ; to the left, tall cliffs of bedded igneous rock, with faults
and fissures, and all the marks of weathering old and new.
As the day wears on, glen after glen opens in this great sea-
wall; and far away in the distance a bare red mound glows
like a heather hill in autumn. On either side of it are yellow
hills, fragments of the old crater ; and from these, down the
glen, conies a stream, black and gray and green, like a peat-
moss in the Highlands. A turn brings in a bright silvery
stream of water, the river which the lava-stream has driven
to one side. All that will grow in Iceland — birch, fern, moss,
and grass — grows best about these lava-streams. Either the
black colour gathers more heat from the sun, or the debris of
lava makes good soil, or there is a store of earth-heat in tlie
lava which warms the plants like a flue in a hothouse. The
only specimen of mountain ash found in the island was found
near Eldborg, growing on modern lava. But all these are tiny
springs to some of the old giants of their race.
432 SPKINGS, CHAMBERS —
From the Creysers to Bnmar is a ride of aljout forty miles.
The way leads up hills, to the left, in the cut, p. 409. It jiasses
over a small lava-stream, far larger than the largest about Vesu-
vius, and then a goat's track leads out of a glen up a steep slope
through a notch in another range. The dry course of a hum,
or a natural rift in this hill, gives a section of the country. The
hill is made of layers of ashes, plastered over with lava.
The rock is cracked, and full of holes ; and it rings hollow
under foot. To ride over it is like riding over vaidts, and
great hollows are open where the sand has been washed away.
At the top of this strange pass the edge of a lava-flood is
reached, and for the rest of the way to Brunar the track
crosses the stream. One branch of it flowed to Thing-\'alla,
and it seems as if part of it reached at least as far as
Eeykjanes, about seventy miles away. The bottom of the sea
is made of lava, according to the report of fishermen, so there is
no certain limit to tlie flow. At p. 90, vol. i., is a view from
Tliiugvalla. In tlie centre is SkjaldbreiS, and the way from
the Geysers to Brunar crosses the shoulder of that dome from
right to left. As it seems the lava radiated from SkjaldbreiS ;
and that mountain is a frozen spring, the top of the pillar
Avliich froze in the tube from which all this vast flood of
molten stone rose and flowed. But if so, tliore must l)e a
chamber in proportion left somewhere under ground. There
is no cinder-heap about this source ; it overflowed and froze
without spouting, for lava-surfaces are well preserved in all
directions. This hill is from 4000 to 5000 feet high, but no
measurements given in the map.
This w^as a large lawa-spring in its day, but the older
igneous rocks which make the large mountain tracts and the
whole island came out of some larger well and some bigger
cistern. It may be that the broken walls of rock which hem
TUBES, CRATERS, AND CONES. 433
in Faxefjord, and dip away from it with the radiating glens
wliich drain into the Ijord, are remnants of a crater 60 miles
witle. The highest mountains in the world are volcanic,
and tlieir shapes are but large copies of mounds at Myvatn.
A force now active raises molten stone 28,000 feet above the
sea-level, or 28 feet, or tlie same number of inches, according to
the amount of force applied ; but, in all these cases, the force
is the earth's radiation, resisted and controlled by gravitation.
Far out at sea, the Westman Islands are cones of erup-
tion like those which abound all round the coast. Some are
bare ; grass grows on others ; and some are broken all round
by the sea. The cliffs are high, and give beautiful sections of
the structure. There is no room for speculation ; the facts are
there patent and manifest, drawn in coloured lines like a geo-
logical section. The mounds consist of layers of ashes, tuff,
and overflows of lava, which rose from many vents. They
seem bent in every possible direction, but really they slope
away from old craters which were buried by later eruptions,
so they form a complicated pattern of waving lines. Sealed
tubes, pillars of lava now frozen where lava-springs rose,
are seen in the cliffs, with faults, and dykes in the faults.
These are harder than the rest of the mound, and they are
not bedded. Millions of birds rest in shelves weathered out
of the stratified series. No bird can perch on the side of the
hard compact lava, which froze in holes and chinks. One of
these islands, Erlandsey, is a study in itself. No drawing can
give any true notion of its complicated structure as shown in
the cliff; but the form of the truncated cone which rises in
the middle is but a repetition of mounds at Myvatn. Like
forms have been made repeatedly by boiling sealing-wax,
water, and plaster ; and sections made in these models are
miniature copies of the structure of Erlandsey. To describe
VOL. II. 2 F
434 Rl'HlNCiS, CHAMBEUS —
each model of a whole series made, in order to copy each of
the forms described in this chapter, wouUl be waste of time
and space. Let one sample suttice, and let those who take
an interest in the subject cook volcanoes for themselves.
After working at models for many years ; afler tliese last
chapters, written some years ago,had been rewritten and printed ;
the following arrangement was made, with the intention of imi-
tating the forms and movements of hot springs and volcanoes :
An iron pan, 17 by 13 inches wide, and 2 deep, was placed
2^ inches above a gas-burner, with 4 rings, of a diameter
of 9 inches. A layer of fine sand, about half an inch deep,
was spread over the centre of the j)an above the burner, and
a ring of dry plaster-of-Paris was made about the sand. A
jwund of coarse sealing-wax was laid on the sand. The gas
was lit, and the sealing-wax was slowly melted upon the sand.
It boiled, and made a pool of melted wax upon a foundation
pervious to water. In this it resembled the natural arrange-
ment of a sheet of lava upon a bed of dust, which recurs so
often in volcanic countries, and in particular at the place
above described (j3. 432). When all the wax was melted it
was covered m ith a layer of dry plaster, through which the
sealing-wax rose. It raised domes, and burst them, as lava-
domes are burst in Iceland. The crown of the arch was
starred, and then from the middle of the star a bubble of wax
rose, which burst and overflowed, covering the plaster.
This resembles a possible natural arrangement. A bed of
limestone may be covered by hot igneous rocks and burned.
If water then gets to quicklime it will set. The craters thus
formed were " craters of elevation." Copies of like forms
constantly recur in slags and lavas ; and according to Von
Buch and Piazzi Smyth, Monte Somma and the outer ring
of the Peak of Teneriffe were so raised from under the sea.
TUBES, CRATERS, AND CONES.
435
C-
It
tS © «S W'
^
^
®-s S «s " ^ ^+=
-5
o s
C W" --^ ^-rS Ofj . ,
~ ' a^ o ^ ^ ^ <p •>«
*"? ill =1 ^ cl c"
o 1 1 p 11 ^ ^ 1 3 's
I ■§ " s 2 2 1 2 '^ -S -I
In the neighbourhood of the crater the white plaster cracked,
and dykes of red wax rose, while fumes from the wax rose
through the porous plaster, and discoloured it. These fumes
spread in the air, and travelled far ; for the smell of wax per-
vaded the house. In aU volcanic countries fumeroles abound.
In particular, near the Geysers, fumes rise and are condensed
amongst the ashes. By adding cold water the temperature
was kept about 60° to 100°. Plaster does not melt at 212°,
^^ „
45 2 tc 2 '-5 "to I
"= « fc * * 3*
.2 *t5^ s ^ ,
-J3 -i:; T-< ^ -G rs I
a> Hj ^ CO u --<i
434 Sl'RlNOS, CHAMBERS —
1^.
rose, -wliicli burst and ovei-flowed, covering the plaster.
This resembles a possible natural arrangement. A bed of
limestone may be covered by hot igneous rocks and burned.
If water then gets to quicklime it will set. The craters thus
formed were " craters of elevation." Copies of like forms
constantly recur in slags and lavas ; and according to Von
Buch and Piazzi Smyth, Monte Somraa and the outer ring
of the Peak of Teneri ffi^ wore so raised from under the sea.
TUBES, CHATERS, AND CONES. 435^
To get more power, water was now poured in round the
edge of the pan, and more plaster was dusted in, to keep the
wax in the middle. Wlien this charge had set, there remained
a plain of wet plaster, pervious to water, surrounding a lot of
springs of boiling wax, which covered a layer of sand. The
plaster was at rest, but the fusible wax heaved and swelled,
and burst and bubbled, and sank down again, like any
other boiling material from metal to water. By adding
cold water till the level of the wax was reached, these
wax-springs were made to grow and become tubes, as
in the experiment (p. 406). While water on the surface
was at 60°, water below boiled furiously, and steam burst
through the wax, throwing up sand through miniature
tubes, which communicated with steam chambers. In
order to concentrate the power, dry plaster was poured over
all vents but one, and there steam blew off, driving out wax,
which froze in the water when it flowed down. The vessel
was now filled to the brim. The surface water was at 100°,
but steam escaped through several pipes in soft wax, which
boiled up and rose more than an inch above the water. A
thermometer placed in the steam rose to 212°, but probably
the temperature was higher. At this stage, sand, wax, plaster,
and water, were thrown to a considerable distance by steam,
which hissed and sputtered through this miniature crater.
In the neighbourhood of the crater the white plaster cracked,
and dykes of red wax rose, while fumes from the wax rose
through the porous plaster, and discoloured it. These fumes
spread in the air, and travelled far ; for the smell of w^ax per-
vaded the house. In all volcanic countries fumeroles abound.
In particular, near the Geysers, fumes rise and are condensed
amongst the ashes. By adding cold water the temperature
was kept about 60° to 100°. Plaster does not melt at 212°,
43G SPRINGS, niAMRERS —
SO wlien it liad si't a hard slicll was formed about a fusible
mass. Sand neither midts nor sets ; Avithout digging into
the model it is plain that a chamber was thus formed equal
to the amount of wax and sand which was driven to the
j /, J- suiface. Where the roof^was weaj^and^ fusible it sank _m,
// ^ and cones of plaster and mounds of wax sank into the chief
li^. / crater and disappeared. So craters of eruption have disap-
, / ^^ peared after rising above the sea. If there had been enough
c^wv^ '^ of sand a sand cone of eruption would have formed about
Lli^/7^^*'"^ - tiie w\ax tubes. To make a cup and cone, dry plaster w\as
sprinkled about the crater. Steam and boiling w^ater drove
it away from the centre, and the basin and mound of the
Great Geyser were copied in plaster. AMien the first layer
had set, more plaster was sprinkled over the mound, and so
it grew. But when it had grown to a certain height the
boiler burst, and a new crater opened in a starred dome veined
with dykes. Water, wax, sand, and steam, burst out and
broke up the crust, throwing balls of soft wax to a distance.
The boiler could now be filled by pouring water into one
of the craters, and so a good head of steam-power was ke])t
going. By shaking dry plaster over both, two truncated
cones, with cups and pipes, grew. Boiling water rising
through wax tubes moved on a definite plan, and sorted the
loose plaster, which set and took a cast of the currents.
When these two mounds had grown so high that the pres-
sure of columns of water in them equalled the strength of the
l)oiler, it burst once more, and a third crater opened at a
low level amongst the plaster. The operation was so far
completed in about two hours, at a cost of about 80 feet
of gas, and the materials. When cooled, water stood at the
same level in all the pipes, and the lowest of the series flowed
as a cold s])ring, if water was poured into any of the rest.
TUBES, CKATKKS, AND CONES. 437
Tliey all commiuiicated with each other, aud met iu a cuiii-
inoii source. But when the model was heated again, water
stood at various levels, and rose in the large tubes far abo\e
the edge of the pan. Moreover, one spring was always hotter
than the rest; it boiled first, and spouted highest of the
series. A model once made works fur a long time, but this
one was doomed to destruction from the first : the toy was
broken by overturning the pan, and the works were dissected.
The layer of sand had disappeared ; part of the wax had taken
the shape of lava clinkers ; part of it was plastered on the
roof and sides of a steam chamber in the plaster, and formed
the lining of long steam-pipes, which wound about through
the mass ; part of it was in the open craters, in choked tubes,
and in hollow cones, which rose through the plaster, but did
not pierce the surface. These were the vents which were
stopped to concentrate the power at one spot. The roof of
the chamber was so shaped that most of the steam must have
gone towards the pipe in which the water was hottest. It
was heated aud forced up by the steam, and the steam took
the easiest way to escape from the gas fire which worked
this engine. So far this model illustrates a theory, formed
upon a careful study of natural forms. On the outside of it
were upheaved strata, dome, overflow, and fountain ; cup,
cone, and pipe ; and these were miniatures of movements
and forms at the Geysers, at Myvatn, and elsewhere. Inside
were tubes and chambers, like those which abound in the
crusts of volcanic bombs (p. 379). The conclusion arrived
at, so far, is that the igneous crust of the earth, and the
mechanism of hot springs of water and lava, are like these
miniatures, and like them were shaped by radiation and gravi-
tation, directed by laws which govern the universe.
CHArTER LVII.
RAYS.
A mental quality, which phrenologists term cansality, drives
men to seek causes. In 1851 and 18G2 this turn of mind
drove many visitors into the department of machinery in
motion ; they were attracted by sights and sounds and smells
which repelled others. It may or may not be true that certain
bumps on their heads were large ; they certainly had like
tastes, and they formed a class. Amongst them were members
of all classes in society, drawn together by a common wish to
learn how things are made, and to see work done. One who
haunted the world's fair got to know where to find faces, with
certain trains of thought mirrored upon them. Simple
wonder, with round eyes, staring agape, was in faces clustered
about the big diamonds ; amongst the engines, even wonder
looked somewhat wise, or seemed to try.
The rattling, grinding, clashing, grating, thumping discurtl
of many engines spread from the place. Following sound, a
door was reached, and there a beam of electric light struck fidl
into the eyes like a stinging dart. To look wms more painful
than i)leasant. Most men blinked and rubbed their dazzled
eyes, looked puzzled, and stepped out of the line of fire as
soon as they could. Some who looked too long injured their
sight. All around was a noisy maze of wheels and axles,
strings and liaiids, rods and ])istons, wliirling and turning,
AVOltK, ENGINES, FORCE, IDEAS. 430
risiuy and falling, advancing and retiring, moving and hard
at work. ISTo visitor ever hoped to comprehend all the engines
which moved and worked in that one departinent ; but every
one who chose to think could find whole trains of causes
there. Those who went far enough found out that the com-
missioners supplied steam-power to the exhibitors gratis.
Without striving to comprehend the maze, it was easy to
look through it, and see, beyond it all, a furnace-fire, a light,
and a man's thought — three distant links in a vast chain of
causes, but links within reach. Leaving the first idea of
the exhibition, and the spark which kindled the fire, a more
immediate cause of all' the movements was in a boiler-furnace,
and one result of this Fire was Frost.
One engine was making ice all day long. An air-pump
exhausted a vessel so as to lift pressure off ether ; the ether
boiled and expanded, and became vapour, which the air-pump
removed, to be condensed elsewhere. The vessel which held
ether thus boiling at a reduced pressure was under salt water,
in which tins filled with fresh water were plunged. In these
water froze. It froze first next the tin, and the solid crusts
grew towards each other, forcing air before them, so as to
shape chambers and tubes in a transparent shell of ice. The
last drop of fluid was in the middle of each ' shape,' and the
shape of each system of air-bubbles showed the directions in
which force had acted. The furnace-fire became force, and
force was set to draw heat out of water in the vapour of
ether ; and so this engine froze water because water was
boiled. One day a rough-fisted man with big brows and
bright eyes watched the proceedings in silence for some time,
and then remarked promiscuously to all who cared to hear,
" I've seen that mony a time in tlie pits." " That" might be
seen in a coal-pit near Glasgow in 1863. Air was driven
440 FlUE, FOKCE, FliOST, All;, WATElt, WAVES, HEAT.
down to the "face" by a steam-engine. It was compressed in
a pump, and in long pipes ; and heat was stpieezed out of it, for
the pump and the pipes were warm. When the compressed
air escaped below, it expanded and took ujt heat so fast that
vapour froze and became hoar-frost in the coal-pit. So fire
turned into force causes frost in some cases.
Leaving all the spinning, weaving, grinding, rolling,
packing, folding, hammering, squeezing, carving, sawing,
modelling contrivances, which shared in the force of one fire,
certain engines illustrate parts of this book ; for fire and weight,
expansion and contraction, were set to move air and w^ater,
and other substances, with engines.
Amongst the engines were many for blowing air into
furnaces. These howled like a winter storm in a forest, or
roared as they only can roar. A hand with relaxed muscles
fluttered like a flag in the iiozzle of the bellows, and felt
that air is a fluid of sufficient density and weight to do the
work of a hurricane, balance a column of mercury, and w-ork
an engine. Part of the force caused waves in the air, which
produced discordant sounds ; part of it made harmony, for all
the great organs were blown by engines. The force of fire
was so directed as to move air in many ways ; part of the
force produced sound waves in air, part of it moved currents
of air.
Another set (jf engines lifted water. In the middle of
the department, a broad cascade fell over a tall screen, with
aU the dash, and spray, and froth of a burn falling over a
rock. ]>ut this fall had no burn behind it. A centrifugal
pump w^as whirling in a basin ; it lifted water through a
Hat tube, and water fell over the edge back into the pool.
There, from constant friction, the circulating water grew
warm and steamed. Fire, turned into force, caused waves
FIKK, LIGHT, RAYS, MOTION, FOKM. 441
aud circulatiug currents to move, aud part of the force became
sensible heat again.
Part of it became visible light in the electro-magnetic
engine, which cast sharp arrows of light aud rays of sensible
heat through a distant doorway. That light was produced
by the passage of a powerful electric current between carbon
points (see Introduction). These do not touch, but when
they approach each other, they become intensely hot, and
very luminous. Bright crackling sparks then fly off at some
angle to the course of the current, and these sparks describe
paths which depend on the laws which govern the flight of
all projectiles. Many were gathered when cool. Under a
microscope, they appear as minute black globules with a
lustrous glassy surface, with cups and cones and craters, like
other sparks. Some of these adhere to carbons which have
cooled, and they .too are spherical.* After many complicated
changes, force caused, or became radiant light, heat, and mo-
tion. Force and light radiated from luminous spheres, and
from sparks thrown off from a luminous current.
Another variety of the same light was produced by passing
tlie current along a stream of falling mercury, f Thin as a wire,
it flowed continuously till the electric current took the same
path, and then the stream burst and shone. Globules and
jets of vapour dashed outward.s, driven by radiation. This
light has a strange ghastly colour, and tlie spectrum is peculiar ;
the breath of it is poison, so it has to be shown tlirough a
glass ; the fumes condense on the glass, and obscure the
light, as earth-light is hidden by the earth's crust. By these
electric lights all the chemical and other results of photo-
graphy are produced. One furnace-fire was a source of rays :
rays took many shapes : light, heat, cold, waves, sound, elec-
" May 27, 18(52. Holmes' light. f Way's li<;lit.
* U2 WILL.
tricity ; galvauic, magnetic, and chemical action ; actinism,
fusion, sublimation, motion, condensation, freezing, repulsion,
attraction, work, and recording forms, were all found at this
one focus — this one luminous point in a maze of engines —
this source of rays.
The forms resulted from the turning of a wheel ; from
force, from a spark, and from human will ; for the action
stopped when the steam was turned off at the end of each day.
From these engines, and their work, it appears that radia-
tion and gravitation are mechanical powers which men can
set to move and shape gases, fluids, and solids, including all
matters yet found in the earth or in meteorites, and all those
which spectrum analysis has found in the sun. In the de-
partment of machinery in motion, gravitation and light, force
and human will, could be seen through an incomprehensible
maze of engines : — without knowing all that sprang from one
thought, and all that made it grow, this much could be seen.
The source of motion, the origin of force, is out of reach ; but
through all the tangled mazes of the incomprehensible engines
which move in space, gravitation and light, force and Divine
will, may be seen even with dazzled eyes.
One remote cause of motion seems to be in rays of light. /\
tr' A certain clever maker of filters used to attract custom by
filling his windows, near Temple-Bar and in liegent Street,
with all maimer of quaint waterworks. One contrivance was
a fountain, on which a striped ball hung suspended under a
glass shade. It hung o\\ one side of the water-pillar, it turned
horizontally round about it, and Avhile it turned slowly with
the sun, or " widersliins," as the case inight be, it also M'hirled
rapidly about an axis of its own, which changed place con-
tinually, but apparently on a definite system, rerhaps the
poles changed also. The ball had tlu'ee distinct movements
Atj^ ^?^ /^^1-W^-^T;-^-^^ rf^ '"^^ "^-v
WEIGHTS, WIIIKLING, AND RAYS. 443
;it least : — rotation aljout its axis, rc\olution of axis about the
axis of the fountain, and revolution of poles about some un-
known point or points. Besides these, the hall and the foun-
tain revolved about the axis of the earth once in twenty-four
liours ; and the earth and this little satellite have been round
the sun many times since the satellite was first observed near
Temple-Bar, more than ten years ago. In these regions
the ground is shaken by heavy traffic ; the engine was dis-
turbed, and the ball fell now and then. When it did the
fountain rose higher, struck and spread upon the dome of
the shade, flowed down the walls of it into a marble cup,
and into a pit, ^^■here it disappeared. Like the water, the
ball fell into this miniature crater and rolled to the bottom of
it ; but there it fell against the fountain, which rose through
a tiny brass pipe in the midst of the pit. Struck on one
side, the rolling ball rolled the other way ; it turned like a
whipped top, and it soon rose again whirling, because one side
of it was lifted faster than the other side fell. It whiiied as
the water circulated from the fountain in the middle towards
the wet circumference where streams flowed down ; and it
rose slowly to a place where attraction and repulsion were
nearly equal, and there it hung balancing. It rose or fell
an inch or two when the engine was disturbed, or when it
was shaken too much the ball fell into the cup ; but, gene-
rally speaking, the ball has kept its place for many years.
To watch it was pleasant pastime for a law student who studied
sparks, but never could see the beauty of " scintilla juris."
Apparently that engine was worked by a single force,
divided and diverted so as to make it act like two opposing
forces. It was a "gravitation engine." The fountain rose
because water in fallmg from a higher to a lower level pushed
water in a bent pipe out of the way, and drove it up. So
444 IJAYS, ENGINES, anh wekihts.
the fountain was repelled by the earth's attraetiun turned
back by the euguieer who had learned to manage this force.
But some other force had lifted the weight ; so this engine
worked by two forces, and the sun's rays helped the earth's
rays to lift the ball when it fell. The hand which winds it
lip moves a clock, so light made this fountain play.
The ball whirled for the same reasons, but the man who
made it Avhiii could not comprehend its movements, and no
man does.
One of the best mathematicians of the day is wont to
encourage and amaze "young men from the country" by
showing them, at the first of a series of lectures on physics,
a series of mechanical tricks which are explained by known
laws of force expressed in numbers, or in symbols which
mean numbers. His climax is to spin an egg-shell — a hollow
oval with a big end and a little one — upon a fountain, with this
comment : — " All the mathematicians that ever were cannot
explain that." Nevertheless the youngest members of the
class delight to repeat the experiment, chielly because of the
splash. They can reproduce the movements without fail, and
they can perceive without much eftbrt that the force which
works this engine is the converging force which makes a stone
fall, and stretches a plumb-line at every point on the earth's
surface ; but behind that force is the other w Inch raised the
weight — and it is light.
If so many different movements result from movement
towards one point, and from the action of one force, two
opposite forces may do complicated work. If experiment
precedes the full explanation of it, the most ignorant may
try what forces will do with matter; for the M'isi'st can do no
mt)re when he gets to unknown ground.
Learned geographers, geologists, and fanidus navigators,
Fl.UrnS IN WI[TRLING BASTXS. 445
lately met to settle the best route towards the North Pole. They
differed as to the route, but all agreed that the pole might be
reached. Their question turned on the movements of ice
tloatiug in a revolving circumpolar sea. The best route for a
ship is where the sea is most open, the best for a sledge where
ice is most compact ; and. that question turns on the movements
c^ floating ice, on the law of its gi*owth, and on the shape of the
cup which holds it. The worst route for a ship would be to start
about lat. 36° 10' N., long. 39° W., where the last iceberg was
seen (chap, xliii.), and to sail over the banks of Newfoundland,
where ice abounds, up either coast of Greenland, against the
Arctic Current, through heavy ice there. The best w^ould be to
sail after the warm Equatorial Gulf Stream, past England and
Scandinavia, to Spitzbergen, and seek for open water beyond.
It has been found in that direction (vol. i. p. 363). If the ice
which drifts past to the west of Iceland comes out of the arctic
basin, it seems reasonable to expect to find an equal open space
somewhere in the basin, and the most probable place fbr such
an opening is near the centre of revolution, which is the North
Pole. This was an important subject ; but one of. the ablest
of the able speakers, in addressing a grave assemblage, com-
pared the Ai'ctic Ocean to a whirling mop. A great authority,
who thus compared great things with small, encouraged one
who compared the Arctic Ocean to a top and a whirling mop
in chap, xxvii., to venture further on the same path. The most
ignorant may try experiments, even though he must leave
their explanation to those who are better informed.
A trundling mop is an old and apt illustration of pui^ cen-
trifugal force. If turned slowly it makes little splash ; if rapidly
whirled, water radiates fi'om it, spreading in rings of spray;
each drop sets off at a tangent to some circle described about
the axis of the whirling mass, by some part of it which holds
440 TRUNDLINc; Mol'S.
Oil to the rest with a iirmer gri}). But wlieii tlie mop spins
as a carriage-wheel turns, vertically, drops do not follow-
straight paths. The centre which attracts is not in this
centre of rotation and centrifugal force, l)ut in tlie earth's
centre ; so each drop describes a different curve when a mop
is trundled vertically. The man who can calculate the
paths of these projectiles must be an able mathematician ;
but any child can make the projectiles dmw part of their
own curved paths, and so take a practical lesson in the laws
of force.
At page 96, vol. i., is a drawing made by a drop of ink
on a block of wood. The engraver cut away the bare sur-
face and left the rest. From the shape it is easy to see how
the fluid moved, to see that these drops struck the target on
which they splashed, fairly, at right angles to the plane. In
fact, th(^y fell upon a block laid horizontally to catch them,
which was moved aside a short way to make room for
each new drop. If, instead of thus striking a plane at right
angles, a drop strikes it sideways, it takes another shape,
which gives like information as to movements and directions
of force. To make more woodcuts of this kind woiUd be
waste of trouble and cash, for anyone may drop ink from
a tube and slope white paper at various angles to see the
effect.
A drop is spherical, and if it be laid on paper it draws its
own section, and dries a round spot. If it falls it takes a new
shape ; it becomes a star if it hits fair ; an oval like a leaf
with prickles round the edge if it hits the surface obliquely.
The falling drops threw off little drops, and some of these
are shown in the cut.
The faster it moves, and the more it hits sideways, the
longer is the oval. The drop is moving both along the sui-
Sl'INNINC TOPS. 447
face and towards it ; so, when it moves fast, and hits a sur-
face at a very small inclination, a drop becomes a very long
oval, with a line and a dot in front. So far a drop recorded
one vertical movement and one reflection — a movement caused
by the direct force which makes it fall, and a reflection from
the paper. A fluid may then be made to draw diagrams of
its own movements, and to record the action of forces.
In the case of a mop, turning like a carriage-wheel,
fluid projectiles are moved by two forces at least : by centrifu-
gal force, which projects them at a tangent to a circle, described
vertically about an axis of-jotation ; and by the earth's gra-
vitation, which may be taken to act perpendicularly in ver-
tical parallel lines. The curves which result may be learned
by trundling a mop near to a wall ; by watching mud
drops thrown by wheels against carriage windows ; by
studpng mud upon house windows or walls in a street
through wliich carriages pass. Some years ago a French
philosopher invented a very clever toy called the gyro-
scope, from which, amongst other things, a taste for spinning
tops grew. One man furnished the public with " patent
metal tops," copied from a Japanese pattern, and he made a
small fortune. These tops were set to draw as soon as they
appeared. To get mop curves a hole was made in a white-
washed wall, and a metal top was spun vertically, so that it
whirled near the wall. A saucer of ink was placed under it,
and raised till it covered the whirling edge. The result was
a diagram more than six feet wide, which showed at a glance
how movement along straight lines — tangents drawn from the
circumference of a revolving wheel at right angles to a spoke
— gradually bent into movements towards the earth's centre.
Thousands of drops drew as many diagrams on the wall. It
would cost a lifetime to calculate curves which fluid projec-
448 KXPKDIENTS.
liUis draw in a inoniciit. Tliero they remain, curves drawn in
all angles which two straight lines will make in (ine plane —
curves which var}- as the projecting force varied in direction
and intensity. Two ibrces drt>w these diagrams, hut they did
not oppose each other directly. Something more was wanted.
Some of these tops will spin for ten minutes. When spun
horizontally, projectiles are not so much disturbed by the
earth's attraction. Lines drawn by them curve downwards,
like the ribs of an umbrella ; but they are not bent sidewise.
A top with a disc of paper on it was spun in a concave lens
to keep it on one spot, and a sheet of cardl)oard was placed
horizontally, so that the edge of a circular hole in the middle
of it was close below the edge of the disc. Ink dropped on
whirling paper was thrown off, and fell on the cardboard
obliquely. The result was a diagram in which thousands of
minute drops had become as many long ovals, with long lines
in front. A ruler laid on any one of these touched the edge
of the disc of paper, when it was- pasted over the hole in
which it had revolved. So far the experiment only demon-
strated the well-known effects of centrifugal force on projectiles.
This diagram was drawn by two forces ; but by forces acting
in different planes. Something more was still wanted.
The first point to be illustrated, if possible, was the action
of two forces — one pure centrifugal force, the other a force
acting from the centre of a revolving wheel, as a volcano at
the equator acts on projectiles, along rays. The top, with a
disc of paper, was spun as before, and a drop of black ink was
allowed to fall on it near the centre. It described branching
spirals from KtoW. as it moved to the circumference, and it flew
off at tangents from W. to E. when it got to the edge and was
scattered there. Drops of red ink were then squirted at the edge
of the disc from a point near the centre, with a syringe. In
ROTATION AND RADIATION. 44!)
this case tlie red ink was driven by two forces — by one wliicli
drove it away from the centre along a spoke ; by another
which tended to throw it at right angles to a spoke ; and drops
of red ink showed the direction in which they were moving
when they fell on the plane. A ruler laid on a red drop did
not always make a tangent to the disc, as it did when laid on
a black drop. Within a parallelogram drawn upon a tangent
and a ray, the red lines converged upon the end of tlie i-ay
along which the red ink was projected.
The aim of this spinning was to get opposing forces to act
in one plane ; — centrifugal and centripetal, radiating and con-
verging forces : — and gi-avitation, still acted at right angles
to the other two. Some other expedient was still wanted.
The woodcut is a fac-simile of a disc of paper, on which
black and red ink drew curves, as described above. The
shaded border is red. The drops are fac-similes of drops
which were projected by discs, l)ut to bring them within the
size of a page they were cut out, and pasted on lines which
touch points on the disc, at which drops aimed from consi-
derable distances.
A drop of black ink fell at A, and described the spiral
figures in travelling from the centre to the circumference of
the revolving disc of paper. One portion of the drop travelled
to W, making a turn and a half, and it was projected towards
B. There, if the centre of attraction had also been the centre
of revolution, the drop would have been attracted towards C.
If, instead of falling on the paper at B, it had returned to
C, the path described would have been a curve drawn within
the angle W B C.
A drop of red ink was projected at E in the direction of
the arrow E 2, and part of it travelled to E 3. If it had
VOL. IT. 2 G
IKIZIINI-AI. SkcTKI
BULLET^^. 451
returned to R 4, the curve described would have been con-
tained within the angle E 2, 3, 4
The first might be called a trundling mop curve ; for it is
a result of centrifugal force and gravitation. The second is a
result of three forces, and one was on a ray.
From this diagram it seems to follow that a stone pro-
jected vertically from a volcano at the equator does not move
off at a tangent to the circle described about the earth's axis
by the top of the mountain, but moves off on a line which
divides the right angle made by a tangent and ray. If the
radial and tangential forces produced equal velocities, the line
would divide the right angle equally, and the stone would set
off at an angle of 45° to the plane of the horizon, eastwards.
But at every point in its flight, a stone is pulled sideways
1»y the earth's attraction, as a drop of mud is pulled down
when thrown up by a carriage-wheel. In mop-curves drawn
on a wall straight lines are bent by gravitation. The straight
line is bent into a curve. In the case supposed the curve
described is a result of radiation, centrifugal force, and
gravitation — a combination of force acting in three different
directions : 1, from centre towards circumference ; 2, from cir-
cumference at a tangent in the direction of revolution W R
E ; and 3, from circumference towards the common centre of
attraction and repulsion. In drawing this second diagram,
two of these forces acted in the horizontal plane ; the third at
right angles to that plane. The object aimed at was to get
forces to act, so as to illustrate the action of rays opposed
l)y another force. A volcanic bomb describes a curve like any
other projectile cast in the same direction with equal force :
the path of every projectile is matter of calculation and
of speculation till the experiment is tried ; but without cal-
culation, it seems plain that a bullet aimed at the zenith point
452 VOLCAXIC rUClKi'TlLICS.
from the equator ought to fall to the west of the gun ; from
either pole into the gun ; from any intermediate hititude to
the west, and at some place further from the nearest pole
than the starting-point — south or north : — and west.
In the diagram, p. 450, a drop travelled from the centre to
the circumference of a disc of paper revolving horizontally in
the direction W E E, as the plane of the equator does. Ink
travelled from A through W to B, and would have uioved
towards C in the direction +, if attracted towards the centre.
The point A also moved in the same direction about the axis.
But in travelling on the revolving disc from A to W, the ink
described a backward curve. The paper and every point u])on
it, and ink adhering to it, moved W K E, but ink rolling along
the paper as a bullet flies through the atmosphere moved E E
W. It reached a larger circle on which points moved faster,
at each stage.
A. drop of ink falls perpendicularly. It may be so dropped
as to move towards the axis of a disc revolving vertically in
the direction W E E. In moving from circumference to centre,
it moves forward with the paper, but it describes a curve in
the backward direction E E W, because the paper moves faster
in the opposite direction W E E. As the first curve was drawn
in the direction W throughout, the ink always lagged behind
the paper. But if paper moved faster than ink, the point A
won the race : the gun beat the bullet ; it could not return
to A, but to some point behind it, or to the west.
A drop of ink fell perpendicularly upon the point A, and
a drop thrown up through the axis would return into it. Its
own centrifugal force does not disturb the path of a rifled shot.
Between the equator and poles of a globe, as many discs revolve
as there are planes at rig) it angles to the axis. At lat. 45°,
the plane of revolution and a [)luinb-line make an angle of 45°.
ERUPTIONS
453
A stone aimed at the zenith, driven in the direction E by a
ray-force, is subjected throughout its coiu-se to the centrifugal
force, wliicli acts in the dii-ection T E, or towards the ecjuator.
Fii.. 111. Vkrtk'al Section.
If this reasoning be riglit, the longest slope of cones of erup-
tion in the northern hemisphere ought to be south and west
of the chief craters, and in the southern hemisphere to the
north and west. Polar ice, after passing Spitzbergen, goes not
to Archangel, southwards, but towards St. John's, Newfound-
land, at something like a tangent, to the circle of lat. 80°. It
goes south and also westwards. It describes a backward
cun^e.
The same reasoning applies to volcanic boml)s. Ink, in
moving from the centre towards the circumference of paper,
revolving in the direction W R E, described the cui^e A \V.
Lava shaped itself into like curves in the specimens at p. 379.
Nos. 1 and 2 revolved in the direction W E E, ISTo. ?> in the
454 CONES OK KKUI'TIOX.
directiuu E li AV. The core and trust make backward curves
(in the iuipressiou), like the curve A W in the diagram, p. 450.
Tlie longest axis of chambers, and many systems of chambers
in concentric layers, have the same curved arrangement. If
the earth has a like structure, a majority of craters ought to be
found to tlie west of the chief cones of eruption at the
equator ; in the northern hemisphere to the south and west ; in
the southern hemisphere to the north and west. Oval craters
ought to have like bearings for their longest axes ; and most
of the matter thrown out ought to be found on that side.
In fact, the longest slope of Etna is to the south of the
highest point, and most of the matter thrown out is to the
south, and to the west of the meridian which cuts the highest
crater (15" E.)
The longest slope of the cone of Vesuvius is towards the
[Jay of Naples, about S. 55° W. of the crater, and the broken
ring of Somma is open to the south-west.
The long axis of Hecla, lat. 6-4' N., beai's about S. G0° W.
The broken crater is open in that direction, and the last stream
of lava escaped on that side, and flowed that way.
At Kral)La or Krafla, GG° N"., the longest slope is to the
south and west. Active water-craters and the latest lava-
streams are to the south-west of the highest point, and that
is a renniant of a large crater broken down on the south-west.
The longest slope of Sn;efell has similar bearings, S. 80
\y., neai' lat. 65" N. (See maj), vol. i. p. 85.)
So far as memory and rough notes and sketclies serve,
tlii.s rule liokls good for all the lai'ge craters noticed in Ice-
land. Broken craters on shore are open to the evening sun,
like the Faxefjord. The eastern edge of the crater, which
i^ the muzzle of the gun, is also highest. These big guns
arc not aimed at the zenith, but at some point to the south
DIAGKAMS. 4;")5
and west of it ; and charges of small shot iired from them
have fallen chiefly to the south and west of the tubes from
which they were thrown.
So far, personal observations and experiments agree, and
make a foundation on which to build a theory. Laws of force
apply to matter above the earth, and within it ; to nebulte
and to worlds, to atmospheres and oceans, and to fluids under
crusts ; and to mops, maps, and tops when they spin.
Bodies propelled by rays must obey the same laws which
govern bullets ; and volcanic mountains are chiefly built of
projectiles shot from the earth through tubes by rays of force.
Since these pages were first printed, many rude experi-
ments above-mentioned have been repeated with good machi-
nery used in polishing optical instnmients, and similar fine
work.*
Some eastern artist engraved certain curves on the sun in
the astronomical symbol copied vol. i. p. 21. A board was
made to turn W. S. E. K, in the same direction as the sun,
the earth, and the solar system, that is against the hands of a
watch when the face is to the pole-star.
1. A sheet of paper was nailed on the board, drops of ink
were placed near the centre, and the board was turned. The
ink drew curved rays, bent as they are in the symbol. As a
potter's wheel is one of the oldest of human inventions, per-
haps this method of drawing diagrams is old.
2. A proof of the map p. 232, vol. i., was placed with the
pole in the centre of revolution. Drops of ink were placed
within five degxees of the pole, and the engine w^as started.
A drop placed at 90° E, followed the arctic current on the
map, touching southern capes in Spitzbergen and the Avestern
* I am indebted to Messrs. C. and F. Darker, of 9 Paradise Row, Lambeth,
for permission to use their machinery. April 13, 1865.
point of Ici'huul. A drop placed at 120^ E. described the
curve assigned to the Baltic Current. It touched the northern
end of Xovaya Zemlya, the Waranger Fjord, crossed Scandina-
via, skirted the western coast, and passed Scotland from the
Moray Firth to Barra. A third drop placed 180° E. passed
over the southern end of Novaya Zemlya, and would have
crossed the south of England if a fold in the paper had not
spoiled the curve.
8. A proof of the map at the end of vol. i. was fixed with
a drop of ink on the pole, and spun. It took great speed to
start this drop, hut when it did move it drew curves which
closely resemble, but do not coincide with, curves drawn by
hand on the stone from which the map was printed.
4. To test the effect of speed, three drops in succession
were placed on the centre, and a sheet of paper whirled thrice
at different rates. The curves were not the same, but very
like, and it seemed that the ink liad started from different
circles.
5. To test the eflfect of distance from the centre, a row of
dro]is were placed on a line on a sheet of section paper. All
the curves diffi-red. A second row was placed at equal dis-
tances on a line at riglit angles to the first, and the paper
\vas turned the opposite way. lieverse curves crossed near
the bisection of two of the four right angles. The figures
produced were heart-shaped, or like the ace of spades. Those
wliicli started from the furthest points were least bent.
G. A speed of 1200 revolutions in the minute gave like
results.
7. Opposite curves were made with a pencil l)y ruling a line
against a ruku-, from circumfcirence to centre, and onwards
from centre to circumference (see chap, x.wii.)
As regards a fixed line, the path of the ink was a ray bent
I'lACKAMS. 457
i'onvard by iVictiuii against tlie })aper ; as regards a moving
radius, it was in a ray bent Ijackwards by inert resistance.
As irdc moved on whirling maps, so a bit of Hoating ice
revolves \\itli the earth and makes a curve south-eastwards
on some imaginary fixed line amongst the stars : it is carried
round by friction, and repelled by centrifugal force. As
legards the meridian on the eartli's crust, the ice describes a
backward curve south-westwards, as ink did on the maps.
Some eastern astronomer described like curves on the sun's
disc : they are repeated on ancient sculptured stones in Scot-
land ; and something like the curves drawn by Maury (vol. i.
]). 28) have been found in photographs of the sun (end of vol. ii.)
Centrifugal force acts along a ray, from the centre towards
the circumference of a revolving plane, and friction bends the
ray forwards.
Sticky gum water dropped on a top spreads along rays,
and the path described by each separate drop is but little
l)ent. The paper holds it fast, and carries it round till it gets
to the edge. There it flies off at a tangent, at right angles to
its path on the paper. Ink, which is more fluid and less sticky,
radiates, but the rays are more bent forward when the fluid
is sticky. The paper slips past and under fluid ; and air,
which also radiates from the axis at slower rates, holds ink
back. The path of ink on the paper is more bent. In
both cases the last course along a tangent is derived from
two movements: one along a ray, the other about an axis.
The paper which holds together makes most turns, though
urged by the same force which also urges gum and ink and
air away from the spindle of a top.
This may be shown in many ways. A shallow round card-
board box with upright sides was fixed on a to]) and spun
with it. Burning sealing-wax dropped in took various shapes
458 MODELS.
as it cooled and haixk'Ued. Part of it set in bent rays, wliicli
started from a ring. The outer crust of tlie ring was irregu-
lar. Projectiles thrown from tliis circular mound there set oft'
at tangents to the ring, hit the side of the box, and made
backward curves where they stopped. The front of each
drop was carried forward, and the rest stuck on spots which
followed the first spot struck. The target was crossing the
line of fire, so fluid bullets made long oval marks on the up-
right wall of the box. Any projectile nnist curve back if
cast forward from the edge of a revolving disc through still
air moving with the disc ; and for that reason volcanic pro-
jectiles ought to fall most on the western side of the crater.
By thus watching the effect of rotation on hot wax, some
notion may be got of the packing of the earth's viscid and fluid
interior within a freezing crust. The round crust formed
in a ring, and the fluid was urged towards it by pure centri-
fugal force. Gravitation acted at right angles to this plane ;
the effect of the same force acting towards a point on the axis
is matter of calculation.
Flaming drops of wax thrown beyond the box were caught
on paper. Some M'hicli had cooled were spherical, like iron
sparks ; others which had not cooled so nmch flattened where
they fell ; and the long axis of each was in a tangent to the
rim of the box in the plane of the horizon. In the vertical
plane each projectile described a curve. Other drops fell on
water and froze flat. Their structure was chambered like
other hot sparks. Each had a core within a crust.
So far these movements and forms M't-re produced by a
force which pulled a string at a tangent to the spindle of a
top, and by a radiating force which fused and boiled wax ;
and the last movement was a tangent to the outer circle,
which revolved about the axis.
MODELS. 459
The next step was to try the efiect of rotation, so as to
test theories as to the interior of bodies which revolve while
changing from a fluid to a solid condition. The top and seal-
ing-wax did well enough ; but better machinery did better
work.
1. A circular cardboard box, with upright sides, was spun
with a mass of thick wet plaster-of-Paris in it. The forms
produced were founded on bent rays.
2. The experiment was repeated in vessels of various
shapes, and at varying speed. Forms produced were like those
-which result from whirling water in a glass bottle, but in this
case a plaster cast of the forces employed was taken. While
wet, the plaster was a reflector, so accurate as to suggest the
making of metal reflectors by the same process somewhat
modified.
3. An elliptical cardboard box, with ujjright sides and a
cover, was nailed on and spun half filled with fluid plaster.
One end of the ellipse was three inches from the centre, the other
six inches. The long diameter was nine inches, the short one six.
When the plaster had set most of it was found at the ends. A
circle described about the centre of revolution touched the
base of a curved waU, which reached the lid and filled the most
distant end. At the other end was another wall : it was curved
in plan and in vertical section, but not concentric with the
(ither wall. About the centre of revolution was a low moimd,
from which waves of plaster made backward curves. Enough
was done to prove that a hollow shell of fluid may form inside
a solid sliell, like the w\ater sphere p. 353, and the sparks,
l)ombs, and meteorites mentioned in the last chax)ter. I will
not even attempt to name the curves which were thus pro-
duced by whirling plaster-of-Paris while it was setting, but
immediate causes were plain enough. Centrifugal and cen-
460 MODEl^S.
tripetal forces, an enuiiii', and a man's liand turning- a crank,
were links in tlie chain ; Imt powers wliicli move ])lanels
were in tliat small train (^f whirling wheels.
The aim of all these devices was to sec light throngh
engines. For lack of mental maehincny with which to cal-
culate the effects of ray-force, machinery in motion was set
to draw diagrams and build models. But some other expe-
dient was still wanting to show the action of rays.
CHAPTEli LVIII.
FORCE — MOVEMENT — WORK — FORM.
In the last chapter various rude expedients, used for learning
the effects of rays and rotation, were described. In preceding
cliapters attempts were made to show that certain forms and
movements result from certain forms of force. It has now
to be shown that, under certain conditions, radiation causes
rotation, and forms which result from that ibrm of force.
Blazing wax drop])ed on water cools suddenly, and the
mass radiates. It throws off streams of vapour, and the
recoil moves the parent mass. If the eruption caused by
radiation moves off from the centre westwards, the mass
moves east. When the eruption is at a tangent to the cir-
cumference, or at any angle less than a right angle to the
tangent, the parent mass turns on its axis. In this case, the
movement only lasts for an instant, but it proves that a cool-
ing mass may be made to rotate by a force which radiates
from within.
Camphor set alight and afloat runs about on water, and it
radiates while it burns. Gutta-percha, varnish of various
sorts, and many substances, move about when heated and
free to move. If any substance will float and hold together,
and yet part with some portion of its mass at a low heat, this
action would be better shown by it.
One substance of this kind whirls. Collodion kept for a
462 ruLLODiON.
long time in an ill-corked bottle turns into a brittle jelly. It
floats in water, a viscous mass in a tough crust, a soft core of
ether and collodion in a shell. As soon as the ether begins
to escape, each mass begins to move. A temperature of 60",
sufficient to boil ether, sets up radiation, and ray-force causes
rotation. As soon as rotation begins, the direction of the
escape is determined, and each mass of collodion -whirls so
long as any ether is left in it. When all the force is spent,
the solid renmaut sinks, for it is heavier than water.
A mass becomes globular or lenticular at first, and
moves by fits and starts. ■ This is an effect of heat. In
hot water, the mass becomes a hollow shell, whirls and often
bursts. Placed in sunlight, the masses whirl rapidly ; small
hollow spheres of collodion filled with the vapour of ether
form on the outside and burst, and many of these are thrown
oft'. At each effort, the parent mass takes a fresh start.
Sometimes it rushes oft" whirling in one direction, while the
small mass whirls off the other way. Generally, each mass
rotates, and also revolves about some central point. Small
masses are attracted by large ones, move towards them when
they get near, and are whirled off again when the pace is
sufficient. The pace slackens gradually, and the glolnilar
shape often changes to a transparent cup, through which
chambers and globular masses of fluid collodion and ether
may still be seen. After the force seems to be exhausted in
the shade, a ray of sunshine will set a whole fleet of tops
spinning faster than ever, and generally in the old direction.
After about a couple of hours, the charge of fluid, in a lump
as big as a bean, is s]ient. Then the whirling slops, and the
hard collodion, shrunk and slirivcllcd like a parched pea, sinks.
WJien dried, it is like wrinkled horn. This experiment has
been repeatedly tried, in all weathers, and always with like
WHinLiXG. 463
results. Tlie force is a ray-lbree — the force of heat in the
eartli's atmosphere, wliich drives ether away as the earth's in-
ternal heat drives water out of Strokr, and lava and ashes out
of Etna. In a bright sun the shadow of ether is th^o^^•n on the
liasin through water, and the eruptions can be watched flowing
outwards in streams which curve backwards like sealing-wax
dropped into a whirling box, or ink on a top (p. 450).
A like result is produced by pouring collodion into a cir-
cular tray floating on water. The vessel sails about without
apparent reason, and sometimes it whirls. The mechanical
force which thus overcomes the friction of water, and keeps a
mass whirling for two hours, Avould sufl&ce to spin the same
mass in free space at a greater rate ; and motion once begun
continues there, if astronomers are right.
The principle of this movement, and the immediate cause
of it, are sufficiently plain : to explain and account for the
eccentric paths of bodies of irregular shape, thus whirling in
water, would be a hard task for any one, and is far too hard for
a traveller to attempt. But rules which govern movements
caused by spinning a top must also govern those caused by
ray-force in whirling collodion, and in rotating worlds.
If the collodion turns sunwise — south, west ; north, east —
which it generally does when placed in sunlight, it also
revolves in the same direction about some point. It rotates
sunwise because ether escapes the other way at first, and
probably ether takes that direction because the shell is
thinnest on the shady side where the heat is least, and
evaporation not so fast. There seems to be no fixed rule, for
it often turns " widershins," as the world turns.
Other substances illustrate this action of ray-force. Gutta-
percha floats on water, but gutta-percha dissolved in cliloro-
form sinks. Heated with a burning-glass under water, a mass
464 ROILINC.
boils, leaps up, explodes, and throws oil' small sphevi's ; some
of wliicli hang under the surface, others rise and fall again,
others burst and iloat above the suri'ace of the water. These
discs have chambered interiors in a ring, and their structure,
though complicated, is regular. Kept in a stoppered bottle
this substance is like any other Huid ; exposed to sunlight,
it grows into all manner of quaint shapes, and throws off"
projectiles, while part of the mass evaporates, and the rest
becomes solid. In these small experiments light acted as
force, and caused first radiation, then rotation, and then pro-
jection to a distance at angles somewliere between a tangent
and a radius in the plane of rotation, and at right angles to
the axis, which, in this case, was a ray reaching from the
earth's centre to London.
If ray-force will cause rotation, any rotating body will
serve for illustration ; and for lack of better machinery, a top
was used to see the effect of a. mass rotating in a fluid at rest.
A metal top was spun in shallow water, so that the disc
was in air and the spindle sunk. The vessel was placed on a
solid base, where the sun shone on the water, and light reflected
on the wall showed that water was as still as water ever is.
The whirling spindle set up a system of waves, which refracted
and reflected light, and cast shadows. The top " hummed,"
and while it did waves were small and of strange forms. As
the sound changed, so did the shape of the waves. They were
like waves which accompany sounds made by rubbing the
finger on the edge of a glass. Instantanef)us photography
would copy these, and that experiment may be tried some
day.* Besides these sound-waves, the top started others,
which seemed to set off at tangents, and they spread as rings.
* These fluid forms are better dufiiuHl tliaii cdivcs wliidi arc loiiicd in
siuul by vibmtioiis in metal plates.
WAVES AND STREAMS. 4G5
Lights reflected from tliem seemed to revolve about the top
^V. N. E. 8. W. ; while the spindle turned the other way,
W.8.E.N.W. Li gilts and shadows thrown on a wall made a
complicatetl pattern of curves, turning opposite ways, while
they receded from the shadow of the top rapidly. These
were also reflected from the sides of the vessel towards the
centre.
The revolving spindle also started a system of slow cur-
rents in the water. Burning sealing-wax dropped on the disc
was thrown off, and fell on the water. Discs of wax thrown
oft' by the top floated, and showed movements at the surface.
These had little in common with the wave systems. The
floats moved slowly, in curves, W. S. E. N. W., as the spindle
moved. They also approached the spindle with increasing
velocity, passed it swiftly, and retired, slackening their pace
gradually till they reached a limit, when they returned. They
seemed to describe elliptical patlis. The spindle was in one
focus, and the other moved round it, as the whole system did,
W. S. E. N. W.
The simplest and therefore tlie best plan for showing
these movements and curves, is to spin a metal top in a con-
cave lens. This centre, placed in the middle of a round tray,
filled to the depth of an inch with water, keeps the top near
one spot. "Gold paint" may he got at any artist's shop.
Dropped upon the whirling top, this fine dust is thrown oft'
at tangents, and where it falls it floats. It moves round the
top ill the direction of rotation, but it also approaches the
spindle, whirls round it, and sets off again. The nearer a
grain of dust is to the spindle, the faster it moves. The
pattern produced is like a series of rays bent backwards.
The whole system is moving one way, but the outside does
not keep pace witli the rest, and seems to lag behind. When
VOL. II. 2 H
466 WHIHLINO.
the top begins to lose speed, the spokes Lend the other way,
forwards. But every trial gives a different variety of the
same pattern ; and sometimes eddies near the oxitside turn
the other way.
To unravel tliat tangled skein of wdiirling curves would
be as hard a task as to explain the movements of an ogg-shell
whirling on a fountain ; but the force which pulled a string
and spun the top was a link in the chain of causes whicli
made the puzzle, for the water was a mirror before the top
was spun.
Collodion whirls without any force but the force which
boils ether, and it wliirl,§ fast in sunlight.
In the first contrivance, radiation set up rotation and
kept it up for a long time. In this, rotation arranged a fluid
and floating solids ; two ojjposing forces acted in one hori-
zontal plane, and the earth's gravitation did not directly inter-
fere with the curves. The top scattered projectiles, as it did
on the diagrams above described, but in this case they fell
where thoy could move. Some force, prol)al)ly friction, at-
tracted them towards the spindle, and dragged water and
dust towards one side of the turning cylinder. It raised up a
small mound about it. Centrifugal force drove water away at
tangents to the other side. The whole moved in one direction
about an axis, and separate parts of the system also turned
the same way so long as the top continued to spin.
According to works on astronomy,* the sun and the solar
system also turn one way. If seen from the fixed axis of
* 1. They (the planets) move in the same invariable direction round the
sun ; their course, as viewed from the north side of the ecliptic, being contrary
to the hands of a watch
2. Tlicy describe oval or elliptical ]iaths round the sun — not, however,
differing greatly from circles
3. Their orbits are more or less inclined to the ecliptic
f). They revolve upon tlu'ir axes in the snnie way as the earth
WAVES AXl) STREAMS, 4-07
the sun by an observer with his head towards the nortli, tlie
system would pass towards the left, for it moves as the hands
of a watch move when the back of it is towards the Great
Bear, or the face of it is turned towards the Southern Cross.
In this contrivance movements were similar and in the
same direction. When the top was spim by pulling the
string from the left side of the spmdle, everything turned
"W. S. E. X. W. " against the sun," as sailors say, or " widershins."
Eadiation caused rotation : rotation spread and caused re-
volution about an axis. Centrifugal force repelled, but some
other force attracted the system, and it revolved. Systems
of waves also radiated from the centraL.body, and they seemed
to move fastest from the left side of it, because they started
thence, and were approaching. The waves moved swiftly,
and did not interfere with the other movements.
One aim of these and of many other similar contrivances
was to set up systems of radiating waves, in order to watch
their effect. Light, according to the best authorities, is an
effect of waves analogous to sound-waves. But if there be
waves there must also be something material in which waves
can be propagated. There is no sound when a bell is struck in
the exhausted receiver of an air-pump. But if there be some
medium in space through which light-waves move, it ought
to obey the laws of motion like any other material — like air, or
like water. If these waves of light act as waves of force, then
force, though directed by a spinning top, may work as force
does when it radiates from a whirling star. In this case the
waves moved faster than currents, and bodies of different
weight revolving about the top moved at different rates in
6. Agi-eeably to the principles of gi-avitation, their velocity is greatest at
tliose parts of tlieir orhit which lie nearest the sun
Hind quoted, p. 1.3. A Handbook of Astronomy, by George F. Cham-
bers, F.R.G.S. London, 1861.
AC)6 FOUUE.
different curves. lu the collodion experiment the whirling
resulted from ray-force. It has yet to be proved that rays
of force do accompany rays of light ; and one way to learn
that fact is the old path to a forge.
There sights and sounds prove that force is active. The
sky glows ; the hiss of steam, the dunt and thud of ham-
mers, the crash and clang of iron bars, the rattle of wheels,
fill the air with waves of discord. Thirsty giants in armour,
with vizors of steel wire, stand in a spray of iron sparks near
tlie hanimers. They avo of tlie class who are now on strike,
;iiid they earn their high wages, for their lives are short, if
they are merry while they last. With a loud warning shout,
an eager boy charges up with a white-hot, hissing, sputtering
mass of puddled iron to feed the hammer ; and it may be
that another urchin charges the other way, trailing a red ingot
to feed the rollers. Every one must take care of himself in
this den of fire. A giant in steel boots grips the puddler's ball
with a pair of tongs, and with a dexterous whirl and swing
it flies glowing through the air, and lands on the anvil. There
it is crushed and squeezed till slag flows out of it like water
from a sponge. The mass is chambered like some meteorites.
When the blow comes, sparks radiate like rays from a star ;
and each in turn radiates light, heat, and force ; for the sparks
hiss when they touch water, and they burn skin and clothes.
Great scissors gape, and nibble off the end of a steel bai', as a
horse bites a carrot. Another pair of steel jaws may be found
champing the air at your elbow, and when that mouth gets a
bar to bite instead of a bone, it snaps it off with a crunch, and
gapes for more. Still larger shears shred boiler-plates like
silk. At the rollers, a block goes in and a bar comes out,
streaming with fluid slag squeezed out. The iron comes
chai'ging over iron plates, like a red snake uncoiling ; a boy
i;avs. 469
seizes tlie head, and turns it back, and the l)ar conies out as
thin as an eel or a ribbon. A few more turns and it wouhl
he a wire. It is no place to dream in, but there is plenty to
see 1)y tliis furnace-light.
If the engine is worked by steam-power, then all the force
came out of the boiler-fire, and went towards the earth : if
worked by water-power, rays, which work the atmosphere,
lifted water and poured it into the milldam. So in a forge, as
elsewhere, part of the force used was in rays of light.
When a large casting is to be made, a furnace is tajjped,
and tons of metal are run off into great vessels, lined with clay,
as men run ale from a vat. It ofteu happens that the metal
is too hot for immediate use, and it is allowed to rest for a
while in its great caldron. It is a l)eautiful object. The sur-
face is in constant motion, and it shines and glows. Creamy
red islets form on it, and move rapidly, Avliile shining lanes of
bright metal curl and twine beautiful patterns of coloured
light. The smooth hot fluid is darker tlian the scum next
above it, and the highest points darken before the scum. Every
moment some bright spark flies (jfl", whirling and shining like
a star ; each describes a luminous curve in the air, and some
burst like rockets and scatter a spray of light. There is a
force in the fluid, and it radiates like rays of light.
If it were free to move, iron would revolve, because collo-
dion and other substances move and revolve when they cast
off projectiles.
To cool the iron, cold scrap-iron is sometimes dropped in,
and these masses float deep and melt as ice does in boiling
water, or sink if the solid is heavier than the fluid. These
are sometimes wet, and when they are, water explodes and
drops of iron are cast whirling to great distances by steam.
The power still radiates, but it acts more powerfully on this
470 KAYS.
substuiice. The saine amuuut ul' ray-force produces different
rates of expansion ; but this action, like the first, shapes pro-
jectiles, and throws them away from a hot mass of iron.
It radiates : — it shines, it is hot, and it throws off sparks.
Before iron is run to be made into shot and shell at Wool-
wich, tlie slag which floats in the furnace, like oil on water, is
run from the other side. It pours down and freezes like a
hollow icicle where it falls, but a large mound of it grows be-
ibre the day is done. In it is a magazine of ray-force. While
the mound is hot, it throws off a spray of shining drops. As
the mass cools, these get smaller and do not fly so far. Some
about the size of No. 6 shot were thrown more than twenty
feet at first, but after ten minutes the range was only twcj or
three feet, and in half an hour the distances traversed could
be measured by inches. It w\as a magazine, but not an in-
exliaustible magazine of force.
A ton of iron throws shot and shell through tubes in a
crust, as the earth does. Hot slag does the same ; and when
the slag is broken, the guns may be found aiming at the sky,
as volcanoes do. In some of these, half-made shot may be
found also.
They are generally egg-shaped chambers wdth the small
end uppermost, and tlie slag is often spongy near tlic large
end. After the slag has ceased to fire these volleys the sur-
face turns dusky red, and darkens. If water is thrown on at
this stage the crust blackens and contracts, water boils above
and in cracks, and fluid under the crust often Avells up as a
sliining spring of lava wells up from under the dark crust
in which hot springs boil in Iceland. The projectiles now
are drops of hot water, or fragments urged by steam ; the old
guns are changed into steam-guns ; but force wliich drives the
shot is in the slag, and it radiates. Wljen the crust is broken
RAYS. -171
it sliiues as the earth shines when a lava-spring is driven up
by ray-force.
As the charge of force is expended, the action decreases ;
and when the mass is as cold as the space about it the move-
ment ends. Till that balance is reached the attraction of gra-
vitation is overcome by the opposite force, which radiates
where light shines from a furnace, or from the earth.
AVhere electro-magnetic light, earth-light, and furnace-light
shine, there also force radiates. Lava, silver, iron, slag, all
radiate force, when they radiate light, and the rays of the sun
also are accompanied by mechanical force.
The rays of the sun reflected from the earth's crust and
absorbed by it, by the atmosphere and the ocean, at a distance
of ninety-five millions of miles, or at some other less enormous
distance according to recent discoveries, cause radiating
movements. Solar rays furnish most of the power to engines,
whose tool-marks are denudation and deposition. The same
rays, reflected from a rough convex surface in the moon, and
therefore greatly dispersed, still act as force, for they move
the index of a thermometer. Piazzi Smyth when on the
shoulder of Teneriffe, and above the clouds, got a black bulb
thermometer up to 212° in the sun's direct rays: he got about
half as much heat from the moon as he got from a candle on
a stool at a distance of 15 feet.*
Xo thermometer yet contrived will measure heat reflected
from distant planets ; none will measure heat reflected from
a window in Calais, and radiated from the electric light on
the English coast ; but nevertheless heat-rays cross the Channel
with beams of light.
The air gets colder the higher we go, and hotter as we
descend, but the sun's rays get hotter and brighter as the air
* P. 231. Teneriffe, 1858. London. By C. Piazzi Smyth, ftc. etc.
clears. At p. 487 is a diagram drawn by the sun, wliicii
proves tliat the atinospliere absorbs the light, the heat, the
burning power, and the mechanical force of rays.
If the sun's rays so act at this distance, it seems to follow
that they nmst also act as ray-force at their source in the
sun. If they do so act, then visible forms on the sun's disc
ought to be a legible index. In order to learn that alphabet,
the sun's rays must be set to work.
In order to prove that rays of mechanical force do accom-
pany the sun's rays, they were set to make pictures, to carve
wood, to model wax, and to move machinery.
In the first place, the sun was set to make photographic
portraits of himself, and these are some of the expedients
used instead of an observatory : —
On the flat top of an out-housc in a garden a mirror
was placed in a flower-pot, and so flxed as to reflect the
sun's rays downwards through a hole. The flrst flower-pot
was placed on a second turned upside down, so the sun's
reflected rays passed down through a diaphragm. This
arrangement stood over a hole in the roof, and over it
the lens of a telescope was laid flat. By it the rays were
refracted to a focus in a dark room. The image formed
was about the size of a Bl> shot, and it had to lie mag-
nified. ]]elow the focus an iron retort-stand was placed, and
in it a j-plate lens by iioss was fixed. The second lens
ibrmed a second image. By varying the distance between
lens and object, the size and place of an image can be
vuried. If tin; lens is near the object, the image is far
IViiin it, and larger than tlie object ; when the lens is far from
tilt' object, and rays arc nearly i»aralle], the image formed is
iicHi' the lens, and smaller than the object. The image formed
li\ the iirsl K'ns was smaller than the .^uii, wliieli was tla^
SUN PICTUUF.S. 473
object, because the sun's rays are nearly parallel at this dis-
tance from the sun. From that image rays diverged, visibly
if air was misty or smoky in the room. The second lens,
and a sheet of white paper, were so placed as to form and
catch an image a great deal larger than the object to be mag-
nified, which was the image of the sun in the focus of the
first lens. In short, the photographic lens was an eye-piece.
A common telescope fixed in a window-shutter, and aimed at
the sun, will give a magnified image, by sliding the draw-tube
till the focus is found for any screen, but the vertical arrange-
ment was made with a purpose.
The distances having been found, a sheet of cardboard
with a hole in it was fixed upon the iron shaft of the retort-
stand, and the light was shut oft".
A collodion plate was then substituted for the white paj)er,
and the card was whirled through the beam of light ; so that
light passed through the hole during some fraction of a
second.
A copy of the best result obtained is at the end. It is a
negative on glass, so developed as to whiten it. The collodion
film was covered with a layer of black oil-paint, and backed
with blotting-paper. It tells light on a dark ground, and is
a portrait of the sun drawn by himself in black and white.
The first mirror tried was silvered glass of the ordinary kind,
and it gave a double image ; the second was a sheet of plate-
glass, backed with black paint, to absorb one of tlie reflections.
It is very easy to describe this contrivance ; it was Ijy no
means easy to work it. The sun would not stand still, and
the reflected rays moved ; the image moved ; the place for the
screen changed at every moment ; clouds got in the way at
the instant when all was adjusted ; and when the cloud bad
passed, the sun was out ol' the field till the mirror was set
4 74 SUN PICTURES.
again. Late in the day, the sun got entangled in a tree, and
he hid behind smoky chimneys in the morning, A bright
morning often changed to a cloudy noon. Besides all these
difficulties, the ordinary ills of photography interfered ; and
lastly, when all was done, a tidy housemaid starred the glass
of the picture now engraved.
Fourteen pictures survive, and no two are alike. In those
which have double images curves and other forms are re-
peated with more or less intensity, but the forms are the same.
They do not result from photographic manipulation, but from
something beyond the mirror which doubled the reflection.
Two pictures were taken on one glass, by passing the screen
through the beam of light a second time, after waiting long
enough for the image to move its own breadth. Even these
do not tally, for clouds in the earth's atmosphere and London
smoke interfered ; but enough remained to show that the
forms copied are beyond the clouds, for parts of the forms are
repeated though not tlie whole. In some respects all the
pictures resemble each other.
If developed so as to make a " good negative," the sun's
image is a black spot. If very slightly developed, so as
])arely to show an image at first, details come out when the
collodion is covered with a thick layer of Mdute oil-paint,
and then the picture is safe, though black upon a white
ground. Generally, each picture is surrounded by a ring of
light, which is dark in the negative. One edge is darker
than the other. Edges are often fluted and rough, as if the
image were distorted by waves in the earth's atmosphere.
These waves are easily seen on a hot day, and they impede
telescopic observations ; here they are copied on the edge
of an object of known angular size, so they can l)e measured.
They show that the air is moving like liul water; rising
SUN PICTURES. 475
from the hut gruuiid, which absorbs heat from the sun, and
gives it back to space as ray-force.
The sun's disc is streaked and barred, and spotted in
patterns, and when a series are placed together the patterns
have something in common.
When the strongest side of the ring is to the left, dark
bars, which are bars of light, cross the sun's disc, as spots
do in zones parallel to tlie sun's equator.
Shortly after an eclipse, a photograph of the sun was
taken with a lens, wdiich gave an image about the size of
BB shot. A well-marked band is in this picture. Another
observer noticed a similar appearance, of which he published
an account, I think, in the Photographic Journal, 1858.
The band, or one like it, is well shown on another picture,
two inches in diameter ; and in one about an inch and a half
broad more bands are shown. One small picture has a whole
series of bands. When placed under a microscope, this pic-
ture has several crescent-shaped gibbous spots, whicli, from
their size, may be grains of dust ; but they have the illumi-
nation which they might have if they were bodies within less
than a degree of the sun's disc.
The picture selected for engraving is like Maury's dia-
gram of the winds, copied at p. 28, vol. i. ; like ocean-currents
in the Atlantic, laid down upon a new terrestrial globe lately
published at Berlin. Others are somewhat like portraits of
Venus, Mars, Jupiter and his satellites, made by able astro-
nomers, and published in the Handhooh of Astronomy, by
George F. Chambers, in 1861. In some, lines and patterns
interlace like lines of light on hot fluids, and some patterns are
drawn on the principle of lines drawn from pole to pole on a re-
volving globe. In one, the sun's disc is barred with straight
lines which meet at various angles, and make a pattern like
47'; SUN riCTUKKS.
tliat Ha.sliinn iKtrtlicrii aurora wliich Scotch ])ca.«aiits call the
" Merry-dancers." This very rude photograpliic eye saw rays
which common eyes did not see on the white paper, and it did
not see " spots on the sun," which were consi)icuous objects on
the screen. The conclusion arrived at was that the camera
saw through the sun's atmosphere which dazzles eyes, and
copied the currents in it against a luminous background of
less intensity. Perhaps the black mirror absorbed rays which
are reflected by other mirrors.
A heliostat set to reflect the sun's rays, through a telescope
aimed at the pole, would cure most of the evils wliich beset
this rude observatory, but there was no heliostat handy. The
only telescope owned had a chemical focus, and was sadly
battered ; and so this troublesome work was abandoned as
soon as a result was obtained. Better machinery, constructed
on the same principle, may perhaps be tried soon.*
* Tliu ]ilan devised for observing the sun may be explained in a very IVw
words. It was not carried out for lack of a hill and a heliostat, and lor otlier
leasous. On some hill-side facing the south — say Arthur's Seat, near Edin-
Iiurgh ; Primrose Hill, Highgate, Hampstead, or Sydenham, near London, —
observe the pole-star, and choose a place wduch brings the true north to the
brink of the hill. Mark the place of the eye, and of a sight on the hill-top
due north. About this line of sight, which is a straight line parallel to the
earth's axis, build a passage, or else dig one below it, so .as to make a fixed
tube. At either end of the tunnel place a heliostat, with the axis in the axis
of the tulie, and at tlie other end place a screen at right angles to the axis,
liy changing the angle of the reflectors, any ray may be reflected up or down
the tube, and any arrangement of lenses may be set in the ray. The only
artificial motion reijuired is a clock to turn the heliostat. The earth does the
rest. A V(!ry little sunlight will make an inii)ression, so one lens of small
aperture and long focus would serve for solar jdiotographj'. Amongst the ad-
vantages iif tills |ilaii are steadiness in the whole contrivance, even temiiera-
liuv ill tlic tuhe, and clicapness. The chief cost woulil be that of a pa.ssage
of (Mnuil (liniuiisioiis, if hiiilt, (.!■ tlic cost of diiviiiH- n sliaft tliroiigli the toji
"I Arthur's Seat, it tliat wnv the iilarr chosen.
SUN PirnuiEs. -177
8(.) rude were these experiments, that no record was taken of
tln^ bearings of the plates. The picture selected has l)een
l)lace(l on the page with bearings suggested by itself. As the
sun is turning from west to east, light-waves ought to travel
fastest from the eastern edge, which is approaching, and fastest
from the equator. The image ought, according to theory, to
be brightest at one spot, namely the place where the equator
cuts the advancing limb. That spot has been placed to the
left, and all other forms fit. The darkest parts of the disc
are to the right, where the surface ought to be receding ;
and above and below the equator near the poles, where move-
ment is slower, and light less direct, than it is at lower lati-
tudes. The picture may be a fallacy, but it is so like a fact
that it is placed here to be compared with others.
Everybody knows that the sun will paint his own picture,
but this particular portrait is peculiar.
It joins in with the rest of these whirling diagrams, for it
is drawn on the principle of the whole series. It is a form
which resulted from the whirling of the sun and from solar
radiation ; the forms so copied are like those which result
from the whirling of the world, maps, and to})S.
On the 18th of July 1860, a great many photographic
contrivances were tried. An accovmt of the successful opera-
tions of Mr. Warren de la Eue is in the PliotocjraiMc
Journal for August 1860, p. 297. A scheme tried in London
Two reflections — one towards tlie pole, another in any other direction —
will steady the sun's ray on a point. The raj' may be sent up or down — up a
tall chimney, or down a coal-pit or an old well, or along a dark passage.
The effect of two reflections has not been tried ; but two plane mirrors, one
small lens, and a clock, might be made true as easily as the numerous lenses of
an astronomical telescope, with all its complicated and costly machinery. In
one case, the whole structure follows the sky ; in the other, the ray is turned
into the telescope which the earth turns.
478 SUN PICTURES.
answered tolerably well, tlioiii^h the apparatus used \\'as ol'
the rudest.
A common photographic camera was placed on a stand,
aimed at the sun, focussed carefully with the full aperture ;
and a stop, with a hole about an eighth of an inch in diameter,
was placed in contact with the outer side of the object-glass.
It was found by experiment that the sun's image alone made
an impression on a collodion plate, when the cover was lifted
and rapidly replaced by hand, when the sky was clear.
By waiting a certain time, the sun and the sun's image moved
far enough to separate images on the plate ; and the film kept
wet for half an hour. Having set this instrument with a
plate in position, all the observer had to do was to lift and
replace the cover at regular intervals, without shaking the
camera. The world turned the instrument more steadily
than clockwork. If time is accurately divided, the distance
from image to image is a scale divided by the engine which
keeps the best astronomical time.
At 1.32 i mean time, according to a neighbouring astrono-
mer's clock, the cover was lifted for the first time, and it was
opened and closed seven times, the last at 1.561. The sky was
very cloudy, so the cover was lifted when there was a chance.
The first plate was developed by an assistant, a second was
placed, and the camera was turned a few degrees by 2.0 i,
and so on till 2.58J. In all 38 attempts to take pictures
of the sun were made on seven plates, and of these 35 trials
succeeded. In particular, three out of four trials at
li. ni.
2—30^
2— 33i
2—361
2—39^
SUN PICTURES. 47!l
according to the watch used, and the time corrected from
the neighbour's clock, gave three crescents differently
placed. They are all within half an inch of each other, but
clear and distinct pictures which bear magnifying. The
object aimed at was to catch the " red flames" which were
caught by Warren de la Eue in Spain. In London the
instrument used and the plan tried failed to catch these
forms ; but it caught the eclipse, and it cost very little.
In five of these pictures, taken about the time of greatest
obscviration, the upper horn of the crescent has a tiny dot
beyond it. The relative positions of points and dots vary
slightly, at a regular rate. This is the place to find " Baily's
beads," and these may perhaps be photographs of that pheno-
menon. The passage of the top of some tall lunar mountain
along the sun's edge would make the horn of the crescent
seem blunt or broken. Constellations of collodion " pin-holes"
and " dust-spots" on the film interfere sadly with observations
on this minute scale.
This method succeeds well under ordinary circumstances,
but during the eclipse it produced some curious results.
Some of the crescents came out negative or black ; others came
out positive or transparent. Of four pictures on one plate, 1
is a fiiint negative with a bright edge ; 2 is a good negative
with a bright edge ; 3 is gray all over, but positive ; 4 is
nearly transparent. Of five pictures on another plate, one is
black with a transparent edge ; another is eqiially transparent
in all parts ; the rest vary. Diffused light produces this
effect, but on other occasions eight pictures of the sun have
been taken on the same plate, all of equal intensity.
These photographic expedients are sufficient to prove that
the sun's rays will cause movements in photographic chemi-
cals. Everybody now knows that fact, and everybody wants
It) liiivc ;i. portrait oi' t'voryltody, ex('ei)t the sun, M-liicli seems
uiigi-ateful at least.
It is not so well known Miat llie sun will engrave.
Fic. Ui. \Viic)i]-KN<!RAViN(i BV .Si'Ni.ionT. TiiK Sun's I'ajh in thk Skv.
Lilies eiigi'aved by the sun on a vertical jilaiie of wood jiUiceil in tlio foi-us of a sjil
ice, 1863, about six weeks.
The sun was set to carve wood, and here is a specimen
I'rom a block engraved by the sun. A glass ball was placed
on a stand outside a window, and a wood-engraver's block was
placed to the north of it ; the printing surface was in a ver-
tical plane, and near the focus of the glass ball. The world
turned the block towards the east ; the sun's rays turned on
the centre of the ball, as a compass-needle turns on a pivot ;
and the sun's image in the focus travelled eastwards as the
sun appeared to travel \vest. Where it travelled, there it
left a deep charred spoor. In the morning the imago was
at AV., in the evening at E., and it made a deep hollow
curve. Vij capsizing and turning it end for end, the imjires-
sion is righted, the curve is made convex to tlu; plane of the
horizon, and the sun's path is from E. to W. on the paper, as
it is in the sky to the south. The sun was moving from the
Tropic of Capricorn northwards, so the path varied each day.
The sky was cloudy, so the spoor was broken. The image
moved on a sphere, the surface was a plane ; ho the sun's
round image drilled oval holes.
KNG HAVING.
481
The diagram proves that the sun's rays set up chemical
action, and burn boxwood as a hot iron might ; and that they
also work as mechanical force, for they tore the wood. It
tore along rays which radiate from a centre of growth, but the
strongest man living could not so tear boxwood with his
hands.
Here is another specimen of the same art : Two dotted
lines were drawn by the sun 10th March 1862 and 23d
November 1863, when the sky was dotted with flying clouds.
3. The Svn'.s Path on Two Cloudy Days.
The place where each passed the sun is marked by a dark
space. The place where the sun was, when the cloud had
passed, is marked by a white spot, or liy the beginning of a
white line. In the wood, the white spaces are at the edges
of deep holes and grooves burned
aAvay by hot rays. The curves do
not coincide, because the block was
in difierent positions.
If passing clouds and the sun
thus divide a line, space may Ik-
divided Ijy making light and dark-
ness recur at regular intervals of
time.
Here is a scale made on this principle, April 1865.
A block was placed opposite to a ball of glass, with the
surface within the burning focus. At 4.25 the sun burned a
VOL. II. 2 I
482 DIVIDING.
(lot. Tilt' l)li)ck was tlu'ii moved by turning the stand on
which it was jilaccd, in azimuth. At 4.27 the lens was
uncovered, and it began to burn. At 4.35 it w^as covered,
at 4.37 oi)en ; 4.45 shut, 4.47 open ; 4.55 shut, 4.57 open ;
5.5 shut. It was found that the image was too large to show
divisions, so the table was turned a few degrees, and the lens
uncovered for eight minutes. At 5.13 it was closed, and
after that time the sun was hid by clouds. This scale is
correctly drawn by the movement of the earth ; on a vertical
l>lane, which is a section of a sphere, with the radius of the
burning focus ; and it proves that photographs taken on flat
surfaces must be distorted. Thirty miniites of time are equal
to 71 degrees of the circle on wdiich the sun appears to move.
Eight minutes are equal to two degrees ; and it is evident that
spaces and dimensions are unequal on the block.
The same block was first tried in the focus of a i-plate
lens by Eoss. The sun marked the Idock, but did not
burn the wood so as to make a groove. INfany scales have
been made with the same instrument on collodion plates,
and there is no practical limit to the minuteness of a scale
thus divided. An image of the sun in the focus of the
smallest lens ever made will move a certain angular distance
in a given time, and a collodion film will take impressions of
it. These blocks are only meant to show how the thing may
be done.*
The point to be made good is, that the sun's rays will do
the work of hot iron at a distance of a certain number of
millions of miles from the source, and these diagrams prove
the fact, which anyone can prove with a burning-glass, b}'
* Tlie principle was ajijilifd to drawings made for tlic Liglitliouso Coni-
niissioii, some of which were puhlished in the report 18(11 ; ;niil it is a con-
trivance which mav he nseful, so it is here dcscrihed.
J
DIVIDING. 483
writing his name on a walking-stick, if he chooses to take
that trouble, on a summer's day.
The pattern which results from the whirling of a spindle
in still water is founded on opposite curves : one set is drawn
away from the circumference, the other set towards it on the
opposite side. Such cur^'es are drawn on watch-cases by
engine-turning. As the sun's rays engrave, and the world is
whirling, rays may do the work of a steel point on a surface
moved by the world, instead of a lathe.
In 1857 the Mdeorolorjical Journal printed a paper " on a
new self-registering sun-dial." It is worked on this principle,
and it can be applied to various uses.*
The instnmient is of the simplest description. A ball of
glass is placed upon a truncated cone of lead, in a hemi-
spherical bowl made of wood or .stone, or metal or glass, or
any other substance. The centre of the solid sphere coincides
with that of the hollow hemisphere, and the dimensions are
so arranged as to make the image formed by the glass coincide
M'ith the hollow surface. The common centre — the apex of
the truncated cone — is the " fixed rest " of the lathe, the sun's
image is the cutting point, and the other end of the chisel is
about ninety-five millions of miles away, fixed in the sun, for
it is a double cone of rays of light. The edge of the bowl
must be level, and the instrument placed where the horizon
is visible. To use a photogi-apher's phrase, this is a camera
with an angular aperture of 180°. The image is formed upon
a hemispherical screen, and the high light alone is copied in
the picture. The sun's image in the bowl copies the sun's
* At the end of the paper is this passago ; — " If it were in general use, the
sunny and cloudy regions of the world might be laid down with greater
accuracy, and deductions might perhaps be drawn from direct observations
Viearing on questions of general science foreign to this description of an instru-
484 ENGINE-TUUNING.
apparent path in the blue vault of Hit' sky, and the shadow of
the glass ball moves in the dial, with a burning centre of
brilliant light. If the lilue \ault were a screen, the world's
sliiulow would nio\c round (lie sun in a year, on curves like
those which the sun's image draws on the l)0wl. When
the moon gets in the way, there is an eclipse of the moon.
If the instrument is placed in position when the sun is on
the tropic of Capricorn, the image begins to burn on the
western side as soon as the rising sun has risen high enough
in the eastern sky to clear vapours which absorb light near
Encunk-Ti'kninc by Sunlight.
Here is a section from a block, sawn out parallel to the plane of the horizon from the
meridian westwards. It represents the sun's burning power during the nioniing for about
a quarter of a year, at an altitude of about twelve degrees. The depth of the groove may
be measured by completing the circle, of which an arc remains. The blank near the middle
roi responds to a similar blank on the meridian, and marks foggy weather. (Sec p. 487.)
the horizon. At this position the image makes a shallow
mark. As the day wears on, the image draws a line east-
wards ; it passes the meridian, and rises in the east. At
every step on this path the powers of light vary. The forces
which do work in the atmosphere cannot do it over again
below ; so visible light, heat, and " actinic" power, all vary in
something like the same proportion. The shell of air is
thinnest over liead, and a vertical sun is the most powerful of
ENGINE-TUENING. 485
a]]. The shell of air is thickest and most charged with
vapours and dust towards the horizon, and this sun-dial proves
that the sun's burning power is subject to the same law.
Marks burned at about the same distance from the horizon
are about the same depth, and the deepest are the nearest to
the plumb-line and the bottom of the bowl — namely, marks
made about noon and the longest day. By their chemical
actinometer Bunsen and Eoscoe got the following numbers : —
Total chemical action effected by the sun's rays from sun-
rise to sunset at the vernal equinox —
Melville Island 1306
Reykjavik 2324
Petersburg 2806
Manchester . . . . . 3625
Heidelberg 4136
Naples 5226
Cairo ...... 6437
At Cairo the sun's rays at the vernal equinox are nearer
to the plumb-line than they are at Eeykjavik, and so tliey do
more work on the ground, and less work in the air.
In like manner, rays do most work on the dial when they
have least work to do in the air through which they pass.
They do less work under a yellow haze of London smoke
tlian they do in the country near London, and they do nothing
under a thick cloud. But when the layer of clouds is passed,
forms and movements there j)^'ove that light is accompanied
* Fuller information on this subject will be found in works on light, espe-
cially in papers published by Professor Roscoe. In the Photographic Journal
(June 15, 1860, p. 256) is an able paper, read by Mr. T. R. Wheeler before the
Photographic Society of Blackheath, in which the researches of Bunsen,
Roscoe, and others, are referred to. See also Tcncriffe, illustrated with photo-
stereographs, by C. Piazzi Smyth, a book whioli is very annising as well as
instructive, and expressed in few and simple words. See also papeis on Light,
In- Sir J. Herschel, in Good Words.
480 ENGINE-TrKNINr;.
by luechanical force, -which radiates I'roni chjuds, and makes
them boil. (See chap, v.)
The line drawn on a clear day is part of a spiral on a sphere.
Ne.xt morning the point of the graver begins again on the
west ; each noon finds the sun higher in the sky, and the spoor
of the image lower in the bowl ; each evening finds the sun
further north on the western horizon, and the image furtlier
south on the eastern edge of the hollow surface on which the
burning point revolves about the fixed rest ; and so this engine-
turning goes on for six months till the longest day. Then the
sun's image turns and burns the other half of the spiral design,
crossing its former path. Such lines could be drawn by
moving a rest horizontally while a ball is turned about a hori-
zontal axis ; but the best of turners and rose-engines and
tools could not equal the accuracy of this work. One end of
the lever is ninety-five millions of miles long, and the other
may be an inch, or a thousandtli part of one ; it is at the focus
of the lens.
The object aimed at was gained when the sun had made
a spoor ; but here is the spoor of the sun on the meridian
of Campden Hill fui' the best part of three winter montlis in
1859.
The instrument was set on the top of the engine-house at
the waterworks at Kensington, 200 feet above the sea, with a
clear horizon, where the sun could shine ; and London smoke
was to the east. The image of the sun was at the Tropic of
Capricorn, T, below the edge, II, at noon, and made a shal-
low mark oij the meridian. It druw a groove eastwards, and
passed over the edge ol' (his particular }»lane. As tlie year
wore on, the eipiator of the bowl rose ; and the image cut
grooves daily, each of increasing depth when the sky was
clear. At a certain time, it fell in with a cloudy atmosphere,
ENGINE-TUKNING.
487
and then the work doue at noon was less. Just before the
equator got to the hot point of the gi'aving-tool, the glass hall
was knocked over. It was found resting on the side of the
bowl, with dt.'ep grooves scored from a different centre at
wrong places. As this particular register was spoiled, a bit
of it thick enough to make a printing block—" a slot " — was
sawn out of it, so as to give a section in the plane of the
meridian. The deepest groove is a quarter of an inch, the rest
can be measured from the outer circle described about the
centre of the original hemispherical surface. Of many bowls,
this is the only one spoiled by such an accident ; tlie rest
are kept in case they may be wanted.
488 ENG1NE-TUKNIN(;.
llegisters haxe Leen kept at No. 5 Eiclimond Terrace, by
Mr. John C. llaile, since the Board of Health was abolished.
A shelf was built beside a chimney, and there a new bowl
is placed twice a year. The sun and the world do the rest
of this engine-turning. Some of the results were piib-
lished* as part of a sanitary inquiry. Three diagrams
made from rubbings show that from 21st December 1855
to 21st June 185G, the sun had little burning power, though
radiant heat registered hy a UacTc hidh thermometer tvas con-
ddcraUe. During the next half year the sun had more burn-
ing power, and marked the bowl at more places. During
the next half year the marks burned were the deepest of this
series. In all these the smoke of London to the east is clearly
shown. Twenty bowls, registers for ten years, have thus been
made.
It has been proved in many ways that light has an influ-
ence on vegetable and animal life. Anything that impedes
light is hurtful to ])lants and animals ; therefore London
smoke, which impedes light, does harm ; and these observa-
tions were placed at the end of a report which aimed at cur-
ing the smoke nuisance, amongst other evils.
A small town has sprung up to the west of a garden near
Ix»n(l((n, ill wliicli roses flourished. Smoke and houses have cut
I 'ft ,30 degrees of the ten-rid zone of sunlight from the clearest
pait of tlie sky, and many of the plants which flourished ten
years ago are withered sticks. A green turf has suffered most
where the evening shadows i'all first. Only fungi grow in dark
mines ; and iiiiiieis are a hleat'hed, s1i(ivt-li\('d race. Sick per-
sons kejit in tlu' Mammoth Cave in Kentucky suffered in
' In tho ici»..it to ihcCfiicral Board i.i Ikaltli li> lonuiiisoioiui's appuiiil.d
to inquire into Uio wannijiR and \cnlilKtion of dwclling-.s (ordcicd to he ininlcd.
2rA\\ Aufiust 1.=«,'.7;.
RAYS. 489
the (lark and died. Cave-crickets and eyeless fisli, which
live in that strange region underground, and other cave
creatures elsewhere, are sluggish. Plants turn towards light.
Many kinds open or close when the sun passes a certain me-
ridian, and of these a botanical clock has been made. A
stick or a tree split along the grain splits along a spiral.
Systems of branches do not sprout above each other, but are
ranged in spirals. Fir-cones, pine-apples, and many flowers,
are built on this same pattern. j\Iany creeping plants turn
about trees. Honeysuckle turns with the sun in the northern
hemisphere.
In short, the pattern which results from the whirling of a
spindle in still water — a pattern of bent rays — is the founda-
tion of many patterns, which seem to result from whirling
movements and the force of sunlight, which made collodion
whirl.
Tlie sun's radiation will cause rotation, and so produce cer-
tain forms on the earth ; and in the photographic picture of
the sun forms are like those which result from the whirl-
ing of a spindle in water.
The sun's rays will also model wax.
One plan devised to prove a fact which scarcely needs
proof, was an ai)plication of the principle of the sun-dial,
which engraved blocks in these pages. A sketch of the
arrangement is below the picture of the sun at the end.
The glass ball* in the centre has a radius of 50 mille-
metres ; the focus in air is 22 millemetres beyond the glass ;
and the curve of a picture of the sky formed l)y the lens in
air has a radius of 72 millemetres. Half sunk in water, the
focal distance is lengthened to lo millemetres. So the curve
* Made at Binuingham, Ftbiuary l^'bl, uudei the superintendence of Mr.
•Tames Chance.
4!»0 FORMS.
of ;i picture foriued uiKler water ])y the upper halt' of this
spherical lens has a radius of 87 niillenietres. At a distance
of 3 inches and 4-lOths from the centre of the ball an image
(»f tlie sun melted lilark sealing-wax nuder water. The wax
took a new shape, water circulated about it, and air-bubbles
formed about the wax. At the shorter focal distance of 72
millenietres the sun's image sauk into black wax like a liot
wire.
These movements and changes resulted from the action of
rays which had travelled ninety-fi^'e millions of miles, and
had passed throngli the coldest regions in the earth's atino-
spliere.
Do these rays shine out of the sun as the earth's light
shines out through the earth's crust ; or like furnace light
welling up through freezing metals and stones ? Or do they
.shine in the sun's atmosphere as the "Merry-dancers" shoot
and shine in the northern sky ?
These are questions, — answers can only be reached by ex-
pedients.
To see what the sun's rays will do when they act from
within outwards, two glass basins Avere got, one with a
I'adius of m. 0.072, the other with a larger radius of m. 0.087.*
All the circles wliicli made these spherical surlaees were
drawn on cardboard and cut out. The outer ring rolled up
made a truncated cone for the snudler basin to stand on in
the large one ; tlie inner ring made a similar stand for tlie
* To .Ml-, (het'ii, llie iiKUiiigiT ot tlie glassworks ol' Jle.s.sis. I'owcll, in
Li)ii(l(Jii, [ iiiii iiuk'bted for these aiid other glass coutrivaiices, and for pennis-
hiou to U.SC funiaces in making experiments. A paper puldished in the Liver-
jiool and Manchester Plwlogi-apliic Juurnal in 1858, contains an ;ir(()uut of
some of the scliemes tried to learn the effects of light and heat on plioto-
graphic chemicals. One result is, that suiili;;lit will first M;iikrii, and tlicn
w hiten a negative.
MODELLING. 491
glass ball, aud some plaster-of-Paris made a stand for the
whole contrivance and fixed it.
It was placed in a window with a southern exposure, and
the outer space was filled with water.
By this arrangement an image of the sun was formed
upon the inner surface of a shell of glass, the outside of which
was in contact with a shell of water. Whenever the sun
shone the water circulated about the sun's image, and bubbles
of gas formed all over the outside of the glass.
The outside of the inner glass was then coated with a
layer of black sealing-wax about a tenth of an inch thick,
and covered with a second layer of gi-een sealing-wax varnish,
and with a coat of gold paint. When this triple fusible crust
had hardened the glasses were placed. On March 19, 1862, the
sun only .shone occasionally, and while the sun was behind a
cloud there was no change ; but whenever the sun did appear
there was a violent commotion at the inner surface of the
crust of wax. There were miniature earthquakes, concussions,
detonations, \dbrations, waves, sudden movements which radi-
ated from the sun's image at all angles, from the end of tlie
rav which reached from the sun to the sealins-wax —
On the outside, Inibbles of some gas Q)robably air absorbed
by the water) formed all over the surface, to which they
were attracted. And here a whole subject for inquiry oj^ens,
for the sun's rays affect magnets and electrometers. In the
meantime, rays witliin drove up a dome, and so ])roduced, first
a crater of elevation, then a tube. On ^larch 21, the sun Avas
hidden, and tlie sealiug-wax mountains were at rest. The
2-4th was a bright day with passing clouds. ^Miniature earth-
(piakes were frequent, and the surface was raised up and
492 MODELLINO.
pushed outwards by the rays. Blisters became Ijubliles and
burst ; and when they did, water entered, and increased the
power, by expanding between wax and glass. The outer
crust was charubered, and chambers are now seen through
the glass. The arrangement was left till the lOtli of May
1862, and then moved, after tiying the effect of dry sand
instead of water. The rays drove wax into sand, biit because
the nearest centre of attraction was in the earth, not in the
sun, and because sand did not cool the wax so fast as water
does, the weight of the soft wax dragged it away, and the
glass was laid bare. Rays then split the glass along the path
of the sun's image in this moving panorama of the sky.
The sun is out of reach, and so bright that human eyes
cannot see it ; but in this expedient a ray acted as mechanical
force. It broke glass, it pushed sealing-wax before it, and so
pushed sand ; it moulded forms, like those which are modelled
by the earth's rays in volcanoes ; by furnace rays at foundi'ies ;
by gas lamps used to make models. The sun's rays modt'lk'd
forms like those which a traveller's telescope enables him to
see on the crust of the moon ; like those which a photographic
eye saw in the sun. The ray modelled the forms wliieh
characterise atmospheric, aqueous, and volcanic action ; up-
heaval ; dome and flow ; tube, crater, and cone ; fault and
dvkt'. It set up circulation in sand, in wax, in water, and in
ail'; in solid, iluid, and gas; and yet tlie soui'cc of the ray
of ibrce was in the sun.
Eays from some of the fi.xed stars act on photograi)lii(^
chcmit'als.
While engaged on drawings which wvw judilislicd in llic
vejtort of llir Lighlhouse Connnission in ISiM, it was found
necessary to construct a scale for tlie lii'ld ol' the camera used
to take pictures.
FORM AND FOllCE. 493
A solar scale was niacle and used, but the sun's image
covered too niucli space for accurate measurement. It
occurred to the writer that stars near the pole might draw a
scale, and the experiment was tried.* A small camera with a
" quarter-plate lens" by Eoss, was aimed at the north star,
having been carefully focussed during the day for the sun's
rays. A collodion plate was prepared with extra precautions
against dust, and after a long exposure it was developed and
fixed. The lines drawn, if any, were too fine for the purpose,
so the plate was stowed away in a box for the time. After
four years it was backed with black oil-paint, and carefully
examined with a lens. A certain number of collodion comets
and stars were found ; a certain region of hazy light where
clouds had reflected rays from the sun or moon ; and amongst
these imperfections were two arcs of concentric ciicles, which
must have been drawn liy stars. According to a rudely-made
paper scale, one circle is about 12|, the other 10 degrees from
the centre. All photographs taken on flat plates are distorted,
and in this case the centre of revolution was not in the centre
of the field. The scale was not a success ; but the experiment
proved that rays from flxed stars act as mechanical force, and
move atoms of silver here on earth, after travelling through
distances which human minds cannot realise.
Amongst nebula?, the most distant of all visible objects,
are many forms which closely resemble curves drawn by
whirling engines : for example, the " spiral nebula, 51 m.,
Canum Venaticorum ; and the spiral nebula, 99 m., Virginis,"
of which pictures are given by Mr. Chambers in his " Hand-
hook" and by an American author in " The Oris of Heaven,"
* " It has been clearlj' proved that tlie light of the stars does produce pli<i.
togi-aphic etiects." . . . (On Light, by Sir J. Ilersehel, Good JFoids, April
1865. P. 322.)
494 FORM AND FOKCE.
London, 1858. Without a large telescxipe it is impossible to
try the effect of light from these distant systems ; but their
forms seem to reveal the action of gravitation, rotation, and
radiation, at the limit now reached by human vision.
If a ray will do so much at this distance, it seems probable
that it shines, as earth-light does, from hot fluids and solids
through heated gases ; and if so, the photograph of the sun
has the shape which fits this answer to the problem set.*
Centrifugal movements, which result from the whirling of a
fluid within a solid shell, were illustrated by the expedient
described above (p. 459). Shapes caused by them may be
seen wherever a fluid whirls ; and water whirls in every
stream. " Vortices " may be watched from any bridge.
Whirlpools are deep pits surrounded by curved spokes, and
the bend shows the direction in which the system revolves.
That point is illustrated by expedients described in this
chapter. Wliirlpools in streams of air moving on a whirling
globe are circular storms, and part t)f the solar system of
motion, for they turn as the hands of a watch turn when the
back of it is towards the north star, or the face of itf towards
the Southern Cross : they turn against the shadow on a dial,
against the bright image of the sun, which travels in the centre
of the shadow of a glass ball set in a bowl. They turn
* " It has been lield that as our trade-winds originate in a greater influx of
lieat from without on and near the equator than at the poles, combined with
the earth's rotation on its a.vis, so the maculiferous belts of the sun may owe
their origin to a gi-eater equatorial efflux of heat, combined with the axial ro-
tation of that luminary." — Sir J. Herschel, Good Words, April 1864. P. 280.
t " At the south pole the winds come from the north-west, and consequently
there they revolve .about it with the hands of a watch." (Quoted from Maury's
Sailing Directions, on p. 23, Abstracts of Meteorological Observations, etc.,
edited by Lieut.-Col. H. James, ll.E. London 1855. Blue Book.)
" Tlie wind approaches the North Pole by a series of spirals from the south-
west . . . and consequently a whirl ought to be created thereby, in which
WHIRLING STORMS. 495
" widersliins," and the old engraver who drew the symbol of
the sun (Fig. 4, vol. i.) gave the right curve.
A watch is a northern contrivance, and probably it was
made in imitation of a dial, for it was meant to measure time
and to be looked at from above. The hands move as the
shadow moves on the dial-plate. In the southern hemisphere
the hands of a watch move with the storm, because the watch
face is turned the other way, and the poles of it are reversed
at the antipodes. By reversing the poles of a watch in the
northern hemisphere so as to make the face of it aim at the
south pole of the sky, apparent movement is converted into
real movement : watch-hands and whirlwinds then turn one
way. The hands turn about the spindle as the earth turns
about its axis and about the axis of the sun, as satellites re-
volve about their central bodies, as the storms whirl on their
axes and move upon the whirling surface of the world. The
large engine and the little one, hour hands and seconds hands,
all turn one way.
The whirling sun has an atmosphere, and shapes in this
photograph are like diagrams laid down by philosophers on
maps, after gathering thousands of facts about great whirling
storms. In this planet a ball with a solid crust is spinning,
and water and air about the crust spin with it, and swing in
streams from and towards the axis, crossing the edges of re-
volving discs diagonally in both hemispheres. The principle
the ascending column of air revolves from right to left, or against the hands
of a watch." (P. 22.)
"It is a singular coincidence between these two facts thus deduced and
other facts which have been observed, and which have been set forth by Kedfield,
Reid, Piddington, and others — viz., that all rotatory storms in the northern
hemisphere revolve as do the whirlwinds about the North Pole, viz. , from right
to left ; and that all circular gales in the southern hemisphere revolve in the
opposite direction, as does the whirl about the South Pole." (P. 23.)
49G PATTERNS.
of the nioveinent in ocean aiul atmosphere is tlic same as in
water set in motion by a whirling spindle. The patterns drawn
ought to be alike, and they are. Forms laid down on globes ;
mountains and coasts, and glens and fjords ; and ice-grooves on
hill-tops — tool-marks of denuding engines — agree in direction.
On any sphere revolving, as the earth revolves, in an atmo-
sphere of its own, the pattern outside ought to be founded on
.spirals, crossing each other like the pattern on the rind of a pine-
apple, or on the heart of a sunflower, or on a daisy. It ought
to be a system of curved cross-hatching, like engine-turning on
the case of a watch. That is the pattern which Maury drew in
his diagram of the winds after comparing and collating thou-
sands of meteorological observations. It is the pattern which
the photographic eye saw on the sun.
Commonly the sun's atmosphere seems to be wrapped
about the ball in broad circular bands. On one occasion the
bands were broken up and scattered, as by a storm. The
bands are seen at the eastern limb about the equator ; and
thence they spread towards the poles, in long curved streams,
like cirrus clouds and mackerel sky overhead. The light
formed long ovals and rings, like whirlpools and systems of
bent waves upon water eddying under a bridge, or made to
whirl in a tray by spinning a top. The actual dimensions of
the shapes figured are of no account ; their proportion to the
rest of the disc is the main point. They are reduced by the
lens, and drawn to scale ; and they cover space in proportion
to spaces traversed liy whirling hurricanes and typhoons, and
laid down on a chart in the blue-book quoted above. Eotating
storms travel over the whole world.
Electric storms, disturbances in currents which affect
magnets, are common, and it has been susi)ected that their
occurrence and the appearance of solar spots have some re-
SUN PICTUltKS. 4!J7
liitiou to ciicli other. A series of pliotogra})lis, kept with a
ivgister of magnetie and other observations, may settle
whether certain forms on the siui's disc indicate storms in
tlie sun's atmosphere, wliich are felt on the earth as electric
storms. Mr. Cliaud)ers say.s —
" We may here take occasion to advert to a very remarkable plieno-
menon seen on September 1, 1859, by two English observer.?, whilst
engaged in scrntinising the sun. A very fine group of spots was visible
at the time, and suddenly, at 1 1 h. 18 m., two patches of intensely bright
wliite light were seen to break out in front of the spots. It was at first
thought to be due to a fracture of the screen attached to the object-
.^Ul«s of the telescope; but such was not the case. The patches of light
were e^'idently connected with the sun itself ; they remained visible for
about five minutes, during which time they traversed a space of about
35,000 miles. The brilliancy of the light was dazzling in the extreme ;
but the most noteworthy circumstance was the marked disturbance
which (as was afterwards foimd) took place in the magnetic instruments
at the Kew Observatory simultaneously with the appearance in question,
followed about sixteen hours afterwards by a great magnetic storm." —
(G. F. Chambers, Handbook of Astronomy. London 1861. P. G.)
Amongst eminent men who have turned their attention to
telescopic drawing and photography, Mr. Nasmyth's name is
conspicuous. He holds that the present condition of planets
may throw light upon the former condition of the world.
^Ir. Chambers only states facts ; he says, p. 9 —
'' It has been thought that the prevalence of large masses of spots
might give rise to a depression in the temperature for the time being,
and thus affect the fertihty of the soil. Modern observation, liowever,
would lead us to infer that the contrary was rather the case, an elevation
(if temperature being contemporaneous with the prevalence of spots."
These shapes may indicate changes in a crust now forming
about a tluid, and this observation supports the notion that
the sun's rays are like those which shiiie throiigli the crust ol
the L-arth.
VuL. II. '2 K
498 FORCE AND FultM.
Bright .streaks and spots of light ui'te'ii Itrcak uul where
dark spots have disappeareil. .Sir W. Herschel, on Deceniher
27, 1799, saw a streak of light which was 2-4G", or 77,000
miles in length (Chambers, p. 9).
The shapes of dark spots projected on paper with a good
astronomical telesco])e are suggestive of forms which result
from ebullition in metals, and may indicate the position of
solid projections rising through heated fluids and gases. The
darkest spots are still so brilliant as to affect photographic
plates rapidly.
When a ]iowerful current of electricity passes through
certain materials, the form is changed, and the current is
changed into light and force ; a wire is broken up, fused,
and the drops are scattered as by an ex])losion. They move
off and radiate from the current.
A bell-wire fused by lightning spreads on the ^^•all in
radiating lines ; a tree is split by lightning ; when lightning
falls in a bed of sand, it sometimes fuses the sand into long,
tapering, branching, radiating tubes. Of these, si)ecimens arv
preserved at the British Museum under the name of Fnlgurites.
If the light of the sun be electric light, that form of light is
accompanied by mechanical force, and it radiates in the same
direction as visible light and sensible heat, and actinic rays,
Avhich affect chemicals.
In these last chapter.^ force has been hunted through
engines of many kinds. If the spoor has been truly followed,
light is a power in every engine of human construction, which
turns out work, for the i)ower which winds a clock moves the
hands. The sun's rays help to move air and evaporate water,
so they help to turn all mills ; light of some kind is at the
.source of jiower in steam-cMigincs ; ]»lanl,s Mill not grow with-
out light; animals cannot work without I'ootl ; and the most
RAYS. 499
carnivorous of creatures only extracts power out of fuel
gathered by his prey. A horse in a mill is but a link in a
chain, and rays also are links in it.
The sun's rays may be set to work directly ; they may be
sot to wind up a clock.
Iron floats in mercury, mercury expands when the sun
shines upon the vessel which holds it, and shrinks when the
slin is hid. A column of mercury in an open iron tube with
a bulb will lift an iron weight when the sun shines, and drop
it when the shadow comes ; a very small amount of ingenuity
will apply the power to a piston, a lever, an axle, or a train of
wheels ; an index and a needle would register the force ap-
plied, and might express it in "foot pounds," for the force lifts
a weight.*
The sun's rays evaporate fluids ; vapour of ether may be
passed through a gas meter, and the index will express the
power in cubic feet.f The sun's rays decompose certain fluids,
and make certain gases combine. Bunsen and Eoscoe applied
that power to measure chemical force in light.
The hand which winds a clock moves the train of wheels ;
the force which causes motion, directly or indirectly, is mechani-
cal force ; and the sun's rays have been set to move engines.
The works of philosophers contain a precious essence ;
they contain truths extracted from fruit and flowers, grain and
chaff, gathered by thousands of labourers in a boundless field
of inquiry. This book only contains the gatherings of one
wandering craftsman ; but he has sought for truth, and haply
he may have found some grains to add to the common stock.
* For an explanation of modern viuws on tlie subject of lioat a.s a mode of
motion, see writings by Professor Joule of Manchester, and articles in tlio
Xorth British Review, February and May 186*.
f Neither of these contrivances has yet been made ; one or other may be
set to work before this liook is pulilisheil.
500 RAYS.
One attempt has been to interpret the meaning of form,
to watcli work in progress, so as to learn to distinguish the
tool-marks of natural engines. If the sun's rays work in the
sun as they do on earth, tlicn forms in the sun ought to be a
legibh; index. ]Jead by this ali)habet of foini, rudely made
witli rough expedients, they seem to mean —
That laws of force, Avhieh cause and regulate movements in
gases, fluids, and solids, in the whirling earth, which is only
one of many satellites in one of many systems, are good law
in the atmosphere of the whirling sun, which is only one of
many sources of light and of ray-force.
])Ut if so, wherever light shines there force may radiate,
though the eye is the (jnly organ which feels the force.
Even the shapes of nebuhe may betray mechanical force
in light.
Thus far this book is an attempt to argue through circles :
— an attempt to gain a point by following a ray; and the
n(>xt point by following another. If the attempt be judged
and condemned, the writer can only plead that he has done
his best ; if acquitted of presumption, he will be content.
He hopes to be forgiven for thinking for himself. INIany
spokes have been tried, many a path trodden ; but all paths
tried have ended at one spot. By searchhig backwards from
\vork done, men reach ])ower through engines ; by travelling
far enoiigh thev seem always to reach a source_of light. ]>ut
that is only one centre in an endless train of wheels. Tlip-
_\\ ivvJiULee further js forwards : to use light, and try to see if
there ])e more wheels, engines, and powers betwet'u work done
and tlie will oi' Him who made them all and created Light.
Taken on or about March 22, ISoO, when
March the south pole of the sun is l)est st
if spots were visiltle.
It; to Sir J. Herschel.
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INDEX.
Stiilini;, 108 I
liiiciliirr.it, 1S5; linw it wiiiiUl
AiUiKV Ci:
Aberysf w i
bf .-III. it. i| iiv ,1 .Miikiii},'()f land, 1S7
Adiill Nl.ni.l, 4s: A. lull Head, view of, (it
Adinaslieen, gravel terraces and other ice-
marks, 148, 152
Aotinometer (chemical) of Bunsen and Roscoe,
action shown by, 4S.j
Ai-tini>m frniii fiini.icc fire, 442
A.iivily nlliTi-.-, iKiiaiiieringof iron, 46S
A.i'.isiiii-riti's, tlirir r.nujiosition, 383
AlVirn, .si.ii'AV iii..niitaiii.s in, 253
Agassiz, Ins i!iciii\- i.f a -In.'irr once existing
from tlii- Ni.;tl. i'i.li' t.. (ii iiigia, 239,247
Ainsa nirti i.i iti' iu .--iiiiilis..iiiaii Institute, 385
Air, rolling of, 'J70 ; marks it makes in [lack-
ing solids, 297 ; its density and weight
when moved, 440 ; waves of, on a hot day,
474
Air-bubb'e, what it shows, 389
Air-pumj), in Exhibition, 439
Airdrio, arctic shells at, 95
Allan Wati-r, nature of country, 109
AUegliaiii. -. ri-,.i:ii I.i illi 1, among, 290
Alps, l1 - - ' - • -: ■•:'.■' :.- Ml, 20(5
Altera! I i M . 11 Iiaicntary rocks,
how ■_'. .i|i-:-ts i,.i_l:t iV|i|aiu the nij-stery,
320, 32S
America (North), direction of ice-marks in,
239 ; submerged during part of glacial period,
254 ; newer rocks to the south, the older to
the north, 330
Ancient sea-margins of Highland Glens, 12(3
Anglers study wave-fonus, 271
Anglesea ice-ground, 20 ; as observed from
Ormes Head, 194 ; anciently under sea, 207 ;
its geological structure, 208 ; stri* in, made
by floating ice, 209
Anglo-Saxon (steamer), loss of, in Newfound-
laud, 226, 227
Animal life, influence of light on, 488, 480
Animals, traditions about existence of, 191 ;
formerly existing in British islands, 18(1
Antrim fl'inLs in south of Ireland, 19; iiieces
of chalk found in drift, 61
Anvil, a largi' mctioritc long used as one, "86
Appalachian chain, long wrinkles and folds ii.
332, 333
Applecross hills, 14S
Aracul, whin dykes on, 55 ; (luaitz rock on
highest peak, 5(5
Archipelago, Ireland once an, 42, 62, 59
Aicti(! current and marks of sea-ice on hills of
West Ross-shire, 14(5 ; on west side of At-
lantic, 159 ; actiim of, in Wales, 193 ; traces
of, in forming coast-line of Cardigan Bay,
202 ; along course of Grand Trunk Railway,
290
Arctic regions, animals of which may yet bo
fossilised, 335
Arctic sea shells on Snowdon, 203 ; shell im-
idies c(dd water, 319
Ardjiatrick, ice-marks at, 75
Argyll (Duke of) on sea-ice marks in West
Highlands, g(>
Arran, L-ranitr innnntains of, 05 ; observations
on riii'!:- "f. !''•'■ 7 I
Arseiiii' ill I ill. tals swept out of chimney
of lea. i iMiiiai-, :;l]
Arthur's .Scat, ii-e-marks on, 100
Arthur (King), days of, 190, 192
Asia (Central), on glaciers dwindling away
there, 253
Atlantic waves seen from Portland Island, 278
Atmosphere absorbs mechanical force of rays
of sun, 472 ; of sun, 495 ; bands on, 490
Attraction overcome by repulsion, instance of,
344
Auchterarder, view of hills from, 109
Aurora borealis, pattern on sun somewhat re-
sembling, 475
Autunm-day among hills of W^cst Ross-shire,
142
Avalon, rocks in, concealed by bogs and
forests, 240
Aviemore, glacial drift at, 128
Ayre (roint of), Isle of Man, 169
Badstua, Iceland, 419
' Baily's beads' in sun, 479
Bala Hill near Forfar, 113
Bnllyshannon, salmon stream, fossils, 5:f
50 i
Balmoral, nhu-u-y ti.t.ks at, iillu.l. .1 |,., 1-js
Baltic ( \ivtl,-) nniri, I, sii|.i...s,,| ,-.,ui-s« (.r,
IS; tin -.A lii. ^;iiiir,l >l|, ii.lli, 1.;-,- ; Uu-l>l\,
207 ; llir.HA, l,h K 1.. Mi|.|.M,i, -Is : li.nv it,
iiii-iii wa^ii 111.' ii:isr ..r III,' Ai|'s, ■::,-2
Buhw, illustration of foriiiatiou .,f boulders
in islands of, HOS
BanniK'kburu (battle of) fou-lit on ancient
sea-bottom, lOS
Barkas (T. P.) suuiniary of siieculations on
structure of earth in ' Newcastle Daily
Journal,' 368
Baniespool at Eton, study of waves on pool,
•270, 277
Basic, change of level that would sink, 2rir)
Bath, hot springs at, 220
Uath-hoMsi>, Oxliver. tra.lition of its burst in-
lip, 41S : l,.illi innin, 4I',>
Bay-iiT uiiiM.-, i^.-k, -mT
Beach a l..,,l maik, -J'.il, 277; the most clia
racteristie wiive-iiiark, 28f) ; description ol
one, 2S7; at Breidtjord and Snrefell, Ice-
land, 288
Beaches (ancient), Myra Syssla, 2S9
Bear Island, tciiiiMaa"i iiiv .'.f, 'Jlii
Bears (cavr) round in I'.rilisli Islands, 1!)2
Beddt;.'!.',!, irr marks, -jn:.
Beds(tniiii:iii,in Ml) illustrated, .'iOn
Beech ti. . s ami i.n. sis in Denmark, 2ir)
Hehrin,-s siiiii,. il wider, how they would
afha't I Iniia, ■' I ; ; ,>n ditl'erence of vegeta-
tion on two sirl. „, •jr.4
Beinn aniidli i-har, :\ mountain in W Koss
shire, 13S
Bein Blireac, ice-niai-ks on, 81, s"' ; pauoiamic
view from, 8tj ; probable orit;iu of ikicIkmI
lilocks on, 120
Beinn Copach, or the Cobbler, 82
Beinn-a-Ghuis, marks on, 139 ; sea once at its
foot, 140
Beinn Mhonaidh, 141 ; glens arouml, 142
Beinn-na-Muic Uliuibe, I2H
Belfast, carried blocks near, 01
Belleisle, 235 ; (Straits of) direction of current,
242
Ben Alder and Ben Nevis, 124
Ben Bhanrigh, Arran, ice-marks near, (W
Bon (Jruachan, 124
Ben Eith, in W. Ross-shire, 138
Benknock, Islay, two round lakes at, 408
Ben Tiawcrs, 124
Ben Loinoiiil, pciclicd boiddcrs on, 7i»
Bert;en, .k.u.ls ami rainfall at, 258; gl.-icicis
of, hold clnu.ls, L'..'.!
Bcttws V t'oed, Irir.s of ancient glacier, lIMi
Bianastie ((;i. n), ,,,;,, i ,,..U at, licail of, 14:;
BidstoM Hill, ■ I I, I ,[, ■' o . I .It, ISl
Binny Cr.ai-, ir. k, - 1 li '■''
Birch iu iLani^li j..,,! \...-..^ ■'!.•,; temperatine
they grow in, 2 If.
Biscay (Bay of), waves from, 279
Black Isle of Cromarty, drift on, l.'iS
Bla('krock, marks of ice motion, 21
Blakestou Tor, 220-221
Blast ol hot air iu iron furnaces, 361
Block of ndca schist on Pentl.ands, OS; (a
large one) with a bent tree beside it, l.')2, 167
Blocks of granite at Katon, ice-grooved and
I)oliHheiI, 182
Bloodstone, a glassy volcainc nn'neral, 325
Blower of coal gas, 3S2
! Boatmen study wave-forms, 271
Boats, anchoi-s, etc. , found in Carsc of Cowrie,
Boiling a root, steam-power in, 265 ; living
organisms cannot long survive, 319 ; water
sorts dill'ereut kinds of materials in strata,
394 ; and stewing sounds of Icelandic
springs, 404
Bolands liofvdi, Iceland, 288
Bolide of 1864, a meteorite, its course, 384
Bonavista Bay, Newfoundland, raised beach
at, 289
Bonn, on the Rhine, seven hills arc ancient
volcanic mounds. 428
Borth, beach at. 212 ; cnrions beach at. 2S7
Bott,.m of the sea. how to study it. 271
B.mldcrclav, Cadei Idiis. ,le .•Jl:!
Boulder of tjneiss on |;,n Wvvis, l.>t ; a small
grooved pond, YIN one at Katou, l.vj
Boulders of tl.r Ih - ■
t could
laciers,
(gla.d
Boxw.M.d iMirnI liv sun's r,a\ s, ISI
Brada Head, Isle of Man, clitls at, 169;
boulders at, 171 ; cliff with curved colourp<l
b,ands, 331
Bradshaw's ' Railw.-.v fiuide' referred to, LSI
Brae Mmav. Kn... k of. a hill, 130, 154
Breeze nn ,i Idvr oii^erved, 27.5, 276
BrcidlJMid. Ih a, 1m - of lava boulders at, 287
Brcnloi iM,,i liM .loeU, .shape, 222
Bricks ;mi. I .1 :■, , ■' .
Brine si,Mii - Il \ ailiwich, 183
British .Musi uiH, iiH leorite in, 3S5
Brittaii.N. Iiadition of the overwhelming of a
(dtv in, IS8; how its coastline would be
affected by a rise of the land, l,s7 ; t ladil ion
■about, 188
Brockville striaj, 245
Brongniart on the French meteorite of 1861,
384
Bronze weapons in Danish peat-bogs, 215
Brunar, country between and the Geysers, 432
Brycc (Di.), ' Geology in Clydesdale and Arran'
quoted, 71
Bryson (Mr. Alex.) discovers ledge in gey.ser
tube, 417; his experiments ou taking thi>
tcmi.craturc, 4 IS
Buch (Von.), on Monte Sonima, 4:U
l!ulfalo.stri;c, 24^
Bulls, stone of tin-, its rc.il and mythical
Buusen.'rese;:
Bwlch-Uyu-I),
Cader Idris, ice marks on, 202; traditii
giant, 210
Cairngorm, 123
Cairo, action of sun's rays at, 4S.'i
Caithness, Ord of, 134; Caithness a ll.i
with a soil of drift, 134
INDEX.
)0.5
Caltiloiiiaii ('anal (gkii linMint;), muf a M-a-
stniit, 13-2
Calton Hill, ice-marks on, 101
Canal, roads, railways, and rivers, imw follnw
the patti (.fan anoient ofoan cunvnt, <A>
CaiMl.lMll.iii, sulfa. -1^ drstinvr.l by tlic sea, Ti
Caiiil'li"!- liurniii-, .'Xim-i iiiuait with, 4(;i
Cnia.la, M:rnl,..;ji':il Siiivfyof Canada' irft;rrcil
In, ir,-| ; jr.' marks, '.M-J
('a|iil (.'111.-, i.i' ,^i'..iiii.l rocks at, 204
Carl... II p.iiiits, .•i.'. •trie, current between, pro-
ducing liglit, 441
Cardigan Bay, how apparently fonned, 1.S5,
180 ; how it would be atl'ccted by rise of
land, 18V ; tradition of the land at its bottom
having li.a'ii sunk, 188
Cani.Ml l.l.'wcllyii, l!i!)
Caip.'iit.i's w..ikju.l,m'd by his chips, 268
Carlisli', .hilt ami icf-niarks between Berwick
and Carlisle, 174
Carron Ironworks, 3S0, 382
Carse of Gowrie at a late period under water,
HI, 112; of Stirling, marine objects foun.l
in, 108
Cascade, an artificial <ine in Exhibition, how
kept u]), 440
Casting of iron, 409
Castlcbar, rock-surfaces, .00
Castletown (Isle of Man), country about,
Casts of ironstone be.ls in sandstone, a02
Catania aii.l tli.' bmstiiis out of Mount Etna,
228; n.a.l to, M.Hk.'.l up by lava, H71
Cath-Mihi. niiiiil, -I. IIS which held glaciers,
69
Catskill range, ice-niaiks, 243
Causality, a mental quality, drove visitors in
1851 and 1862 to the department of macliin
ery in Great Exhibition, 438
Cavehill near Belfast, chalk section, 62
Caverns, Icelandic, 399
Ceantire, ice-marks, 72-77 ; onceperhajis three
islands, 76
Celtic traditions, 186, 187; about submerged
lands, 190 ; abotit large animals, 192
Centrifugal force illustrated by a trundling
mop, 445 ; pnmp lifting water, 440
Chalk clitfs capped with whin between Cushen-
dal and Glenarm, 60 ; glens of sovith Eng-
land, alluvial flats in, 223 ; at Stockbridge,
how covered, 225
Chambers in lava, 355; in ice, etc., 356; in
crust and tube communication, 410; (Iwried)
in sedimentary rocks, 422 ; in lava streams,
425
Chambers (George F.) 'A Handbook of As-
tronomy,' quoted for direction of ]>Ianets,
466, 467 ; for portraits of planets, 475 ; re-
ferred to, 494 ; quoted, 497
Chambers (Robert) on ice-grooves on Nor-
wegian watershed, 156 ; ' Ancient Sea-Mar-
gins in British Islands ' referred to, 292
Chaniplain (Lake), whale-bones in drift, 243
Cheshire, character of country, 181 ; boulders,
possible origin of, 183
Chesil Bank, Portland, 278, 287
Chimneys of lead-smelting furnaces, valuable
metals found in, 341
China made by Mintonfrom glacial chips, 181 ;
325
ifacture, 324 ; and clay, tciupcraturt
Chips (rock) form sedimentary rocks, 270
Chudleigh (Cape), Labrador, 235
Cioch Mor, a conical hill, 153, 154
Circulation of water in river eddies, 230, 231 ;
of ocean, 232
Cisterns on Etna and the lava, 372
Clach-an-Turaman, a perched block, 80
Clandeboye, bill at, with ici -luaiks, 61
Clays, working of, inpott.rus, .".l'4 ; tempera
ture, and mode of making into liricks, 325 ;
Clay-maps in shallow pools for tlie stiuleiit of
action of currents, etc., 232
Clay-.slate, ice-marks on, 14
Clew Bay, drift at, 48
Clini.atf, .■ir.-uiiistaii.cs tli.at woul.l change
clini;it.'..rii<iitli.rii iv-i..iis, \-,r. ; of Englan.l
once c.l.l, iT.S; ili,-ni,u.' .il', in Di'iiniark in
human iMii.i.l, -Jir. ; ..f IJiilnin an. I Canada
in 1863-4, compared with that of Labradoi',
238 ; (ancient) of Yorkshire, 282 ; inference
of average, 319
Cloch Corril, great block at, 39 ; legend about,
40
Clock, modern, 264
Clouils over Achill Isl.and, 49 : march of, fiver
Atlantic, 55 ; would be few if ocean w eic all
frozen, 258 ; affect pass.ige and work of sun's
rays, 485
Clyde, mud of, 93 ; change of level that would
sink, 255 ; (Firth of) mud-banks of, imitated
in Lanarkshire mines, 302
Cnoc-a-Bhlaka, Ireland, a museum of trans-
liorted stones, 21 ; naCarrig, or the Hill of
Stones, Ireland, 21 ; Mordan, perched l)lock
on, 29 ; marks of ice on, 30 ; Ourid, Conne-
mara, ice-ni.arks and boulders, 26, 27
Coal-beds in Wales, abrasion of, 185
Coals at Stoke, depth they are obtained from,
181
Coal vegetation of Yorkshire, 282; heat of
burning coals is solar heat stored up by
plants, 338
Cobbler, various names of that hill, 82
Coed Mawr, Wales, bonlders on, 198 ; maiks
on, 200
Col at Llanberis, once a deep strait, etc., 20ii ;
a ' tarbert,' 207
Col de Geant, snow-shed, 206
Coldness of British and French climates in
former ages, ISO
Cold period in Scotland, the time of, 137 ;
(intense) once prevalent in all high Latitudes
and at elevated regions simultaneously.
Prof K.niis.iNs ili..,iy, 147; period (last) in
Irelan.l an.l S. -tl:iii.l, 165; not easily driven
out 111 ijri.uii.l l.uiu possessed by it, 252;
(external) iii.lu/aleil by snow, 327
Coll, perched blocks, 161 ; curve of Arctic
Current, 163
Collier's observation on freezing of water in
Great Exhibition, 439
Collodion, experiments with, 401, 462, 463
Colour (change of) in cooling of molten silver
349
Coltness, travelled boulders at, 97
' Con,' an elk or bird, 192
Conan Bridge, floats of white froth observe.l
from, 151
50G
INDF-X.
liift, 241 ; Xi
fo\iii(llaiid, lai.stiil beach at, "iSi)
wo of (TniitiDn in .rater of Vesm ins, 402,
403 ; one at llraundal described, 37(5 ; in
Con
403 ; one
I
Couti
rest sloiic, 453
change of level that
.11,. 1 .liift, 140, 152
il laaiu lioUows and passes cross-
ing Scotland upon Naes of Norway and the
Skagerrak, 134
Converging mechanical forces, 233
Conway, hills and glens, 20
Conway Castle, waves and wave-marks ob-
served from, 195 ; valley of, 1!)7 ; glacier
once there, 198
Cook (Capt.), on very deep snow found in
Ifltitude of N. Scotland, 250 : perpetual
snow-line at sea level in lat. 54° S., 250
Cooking at a boiling stream in Iceland, 307
Copper-mine of Fahlun, 340
Cojiying rock-suifaces and ice-marks, 15
Cornwall, Celtic traditions recording change
of sea-level, 187
Corrie Bhreacan whirlpool, 80
Corrie Uisge (Loch), marks of ice, KU
Corril, legend of a stone thrown liy the Celtic
hero, 40
Corstorphine Hill, ice-marks on, 100
Courses (three) open to every student, 37^,
Cra:^!
Crat<.i
of 1
rt Hill,
:i.-.. .lowi)...! with icicles, 358;
.•iil:iti..ii ..| (|unntityof matter
ejcr-lr.l l.v, In l..m .bi\ s, :i7:t ; of Vesuvius in
l'S4-J. 4nl'; ilMir^er of visiting, 402; cone of
erujitinn in 1.S44, 402
Craters i.f elevation at Reykjalid, 424 ; jiosi-
tion of niaioritv, 454; direction of projec-
tiles from, 4r.4, 4."i5
Crisinio (.Monte), i>art of Etna, 373
Croagh Patrick, a high hill in Ireland, 47, 51
Croiuaitv Firlli, l.nid about, 133
•Cn.-,^ '■ i.i . ■ ■ "t li:irtiiioor, 220
Cru.'i.l. , I I liii.l, aliighhill,48
Crusl . : i:i I lii, li.nv it may be studied,
;sc.ii ; I..1I,,. 1 :ili. r c-nipfion of Geyser, 41G ;
of eiirtli and <-rusts of stones, 422 ; forma-
tion of, in ancient times, 336 ; in modern ex-
Crystiilliii.. I'eds in districts show great signs
of di^tiiil.:\!i.... .-nid former heat, 332
CrystMli- ili..n .it silver, :^48, 349, 351
Crvst;il> III li..ll..«>, cn-igin of, 360
Cn'llrii Lake, i.e-niarks, 51
Cnnibr.ies, (■..-.
CiiMniiin'^ Ucv. Geo.l, 'The Isle of Man' re-
fencd to, 173; quoted for cause of drift,
Cnshendal and Glenarm, cliffs of chalk be-
tween, 00
Current (jiolar), tracks of ancient in British
Islands, 1 ; (ancienf) .lii. ,li..ii in Au-lesea,
•J(1S; wlien a col, I .,n, .v.. i.| over Great
Hril.'iin, 'JIO: in liilmn <li,iil ; as rillect
ing vegetation on I'illi. r -i.lr, :'-.|
Curve from \(.vaya Z.inly.i d.snil.ed, 177;
tl'aeed from '|..|Kvlii; ■■• Wil. ■-, l''s
Curvesof Ami: n : n , i. , n;3; and
waves verv ~iMi I ;t i . i..ll>vdrops
of ink, 450, l'.^:; .n n,. .• ni -i.n.'s, 457
Cyinri, ancient race, isi;
Daui't (Princess), tradition in Hritlany ot her
being overwhelmed, ISS
Dales in Yorkshire, section like a section of
Icelandic glen, 17.S ; how hollowed out, 170,
180
Dalwhinuv, ice.mirks, l'„'l : ^^lal" f r.Ters..,]
.hitl
Dalzell on tlie Clyde, nu-k (...lisleal ami
striated by ice, 07
Dana's 'Geology' quoted on stnietnre of
Appalachian chain, 332
Daneinora, Sweden, iron quarried at, 340
Danube, what change of level would sink its
source, 255
Darker's (Jlessrs. C. & F.) machinery for
pnli^iiii.j - j.ii. il instruments, 455
Dartiii " I in.l mines of, 219, 222
Deeliii . i \\ hinstone in the coal for-
Dead sunk in deep water by natives of Tierra
del Fucgo, 190
Dee]! grooves, how made, 5
Delhi, mean temperature at, 25:!
Delta of Icelandic river, action of sun and of
cold on, 327, 328
Deltas, submarine, 217; formation of, illus-
tration, 308
Deiulritic concretions result from mechanical
action, 306
Denmark, temperature and forests of, 215 ;
ancient climate, 216
Density (aveKigi') of earth, :iS(j
Denudation, whole northern hemisphere owes
its general sliape to, 162, KiG ; Eig, a case
of, \i;\ : S.-..)ili liiUs and glens show marks
nf, ir.l: l.v iiiiining w.ater, illnslrated by
lea.l wasliiiiL. I so; (river) older than Ice-
Deiiositiou, meciiauics of, may be learneil fi'om
models, 314
Depression over north of Europi', GeiUie on,
256
Dcrry Veagh range, sand on one of, 54
Devil's Bridge, mark made by a river in slate
rock, 210
Dingwall, boulders of pink granite near, l,'i2
Dijilnvvs, traces ntan arrtie enrreuf, 210
Direction, eninni..n -em ral direeli.m of i.^e-
marks in N. Iivlan.l, r.:;
Disturbance in old strata, .-iliO ; shown in ■lis-
tricts with old crystalline beds, 332
Dochart (Glen\ tarbert once at head of, l:'.il ;
rocks at head of, 148
Dogger Bank, a submarine delta, 217
Dolgelley, glacier glens at, 210
Douglas l!ay, Isle of Man viewed from, hori-
zontal lines, 170
Dovretjehl, granite blocks on, 255
'Downthrows' in Devonshire ami Cornwall,
Drachenfells, tnbe in quarry, 4o:l
Prift rtefinc-il, 11 : stintifiril nii.l •.iiistratificd.
l-J; rolli'il) at lii^nd ■ f -- it. ; J, us, 132;
accuiuiilatts ill sli.ill - n' l:;:, ; in
Irelaiul tracd to i:" ; n level,
1V7 ; in Yorkshire, IT': . n w ■ Mi hills
stianded by sea-ico, IS4; (siijk rticial) re-
mnins of cave bears and tigers in, 102 ;
source of, at tlie end of glacial period, 21 s,
2)9 : on ]irairics, 247
Drift-ice, Labrador, 23ij
Drift -terraces at Kinlochewe, 141
Drift-timber about Calf of Man, ICO
Driom Albain, the back of Se.itland, liill so
called, 114
Driom Uachdar, moraines on side, 140;
granite Mocks on, 2.05
Dron Hill of), ice-marks on, llo
Drop, shapes made by, according to the way it
falls, 440
Drops, lessons derived from figures described
by, 451
Dropped blocks. 9
Drowned land of King Grallon, 227
Dubhgarrie, Arran, stones in walls studied, 1)7
Dubh lartach, long reef at, 161 ; a rough rock
off West of Scotland, 201
Dublin, a frozen sea once over the site of, 22S
Ducks on Seqientine, 278
Duiidingston Loch, spring in, 408
Dunblane, nature of country about, 109
Dun Chorre Bhile, a steep hill near Inverarv,
84
Dunrobin Castle, ice-marks near, 10.5
Dust from an eruiition of Etna, 372
Earl, escape of one from his foes, caused I y
nature of glen, 83
Earth's attraction, force of, on stone, 451
Earthquakes in Italy and Iceland, what beds
are ilisturbed by, 330 ; in England, 355
Eastern coast of Scotland from Firth of Fortli
to Duncansby Head, its general appearance,
133, 134
Eclipse of sun, photographic attempts during,
479
Eddies studied at Stockbridge, 229, 230, 231 ;
in molten iron, 3(53
Edinburgh, a frozen sea once over site of,
228
Egg-shell spinning on a fountain, 444
Eig, Scaur of, 161
Elbe, what change of level would sink its
source, 255
Eldborg, lava-crater of, 430; niountaiu-ash
at, 431
Electric light in machine-room, 438 ; produces
all the results of photography, 441 ; storms
and solar spots, 497
Electricity might be applied to many pur-
poses as yet unthonght of, 266
EIei>hants (hairy) once lived in Britain, 187 ;
(ancient), with woolly hair, 283 ; remains
found in British Islands, 192
Elk, gigantic, 193
' Elvan ' of Dartmoor, 222
Encaustic tiles made by Minton from glacial
chips, 181
Engines in Great Exhibition, 438, 439
Engine-turning by sunlight, 484, 486, 487
England, climate once cold in, 178
Kngraving done by tlie sun, 480 482
Enniskillen, .53
Entomostraeous Crustacea, hatched from
nuid, .'iOS
Erieht (Lodi), high teiTaces of drift at, 137
Erlandsry, one of the Westman Islands, 433
Erratics of .Scandinavian origin, their occur-
rence, 218, 219
Eruption of Mount Etna, 371-375
Eruptitms of Geyseis, irregularity of, 413
Esquimaux ehielly live on crust of sea, su])-
posed speculations of Esquimaux geologists,
Estuaiy of glaciers, ground with fonn of, 198
Ether and air-pump, 439
Etna, active in 1863, 228 : eruption of, in 1865,
371-375 ; its longest slope, 454
Evaporation, experiment to show amomit of,
259, 260
Ewe, passage of, through a channel of rock,
144
Eyrik's Jokull, snow on top of, ripple-marked
by wind, 295 ; seems to rest on a thin bed
of sand and cinders, 314
Exhibitioi\ (Great), department of machineiy
visited, 438
Experinu»nts, value of, in seeking abstract
knowledge, 263; best teacher of natural
science, 356
Exposed, and not sheltered places, must be
obser\'ed by the student of old arctic cur-
rents and glacial drift, 2
Fahlun, copper-mine at, 340
' False bedding' often tnie deposition, 314
Fannich (Loch), gap in hills at, 140 ; once a
sea strait, 141
Faro Islanils, gravel arranged in rid^'es and
furrows, 295
' Fault,' a great one observed by American
geologists in the A])palachian chain, 333;
in an ingot of iron, 365, 366
Faults in beds near hot springs, what they
may be, 420 ; in Devonshire and Cornwall,
220
Fauna and flora of water-formation, 335
Faxefjord, small lava-craters round, 430 ;
valleys with cones of eruption and lava-
streams, 431
Faxefjordr (Bay of), spouting spring on
southern shore of, 421
' Feinne,' strong men, large deer and birds
in, 192
Filter-maker at Temple-Bar and in Regent
Street, waterworks of, 442
Findhorn, gashes in rock cut by, 130 ; moving
sand-hills of, 299
Fin Mac-Cool and his sunken country near
Isle of Man, tradition, 189
Finn and his warriors, Connemara legend
of, 41
Fionn, days of, 190-192
Fir-cones arranged s])irally, 489 ; (Scotch) in
Dani.sh peat-bogs, 215 ; temperature it grows
in, 216 ; trees leaning towards Strathspey,
123
Fire kindling heat-power, 265
Fire-ball observed in 1864 in France, 384;
calculation of Lausedat on its course, 384
Fireclay veiy hard to fuse, 326
508
Fiill.s on cast si,l,' n( ScuUatnl, a.-tiou of li.U's
on c'Oiist., 1^1
Fish found in deep water off submarine dills,
N. Ireland, 50
Fisliable water, an old fisherman's tent, 209
Fishermen ott" Margate drag a largo boulder
to land, 2iS
Fishing Test trout at Stockbridge, 223
Flat, strata not always deposited, 310 ;
country is Hat where uppermost beds are
of late age, 330
' Flathinuis," the abode of heroes, Celtic
tradition, IS!)
Flints raiv Ley.. ml r,i.xuV> Canscway, (!I
Floats .if whit.' liclli, iiinM'iiii'iits of, as ob-
ser\i>H ill )<]:irl |.r:,t wain- ..rConan, 151
Flowi'nlalr, i,r-i,i,uks iM-ai-, Uo
Fluid drawinuiliauiaiiis of its own iiiovcmenls,
447; 11 linilcw slull of, niav I'ona inside a
soli<l slR'll, 4.V.1
Flui.ls consist iifpnrti<-lcs, 272
Fog thickened by wetness and warmth of air,
Folge Fond, churcli-bells said to be heard ring-
ing under glaciers of, 18!)
Forest (drowned) near Mimt St. Michel, 188
Forres, water-woili marks at, 130
Fossil record oidy an index, 322 ; wood under
Scaur of ICig, 101
Fossiliferous beds (sedimentary), how they
may have been formed, 329 ; their order of
succession, 330
Fossils projcctiii_' above tin' surface of wea-
thered rocks, ]■«■' ■ (Mli. iuMsjfnmi Mammoth
Cave projcctiii- ti -nilarf of linu'stcnc
rock, 318; aiv n kr, pris, :i2u; pnn.Mplc
on which age is reckoned, .S21
Fountain of a London tilter-maker, 442
Fountains at the Geysers provokingly un-
punctual in their exhibitions, 413
' Foyer Breton ' quoted for a tradition of the
overwhelming of a city in Brittany, 188
France, sinking of a part near Brest, 191
Frankland (Dr.), lecture at Iloyal Institution
referred to, 257
Fredericton, strise at, 242
Freezing of iron, 304 ; sinking in of roofs of
chambers, 305
Freezing of water by air-pump, etc., 43!)
Fronichean, ice-marks at, 75
Frost preserves flesh and soft parts, 320 ; re-
sult of tire, an instance of, 43!)
Frosting of glass, bow clfcrtc^d, 358, 350
Frumenti (Monte), eruption of Etna at, 374
Fulgurites in British Musciun, 41)8
Fumerolcs in volcanic, countries, 435
Fundy (Bay of), 242 ; tidal wave, 280, 281 ;
rain-marks on mud of, 815
Furnace (old) pointed out by largo ciniler-
heaps, 208; student slioulil study fusing of
metals at, .■S5 1 , Iik .-, s^ .mr,. of r.ays, 441, 442 ;
(iron), what may l.r s.m at, 468, 400
Furnaces, engiius for l.louing air into, 440
Furness Lake, Ireland, blocks at, 24, 25
Fusion of ii-on and other ores, 341
(iAiRLocii (Forest of), ice-marks, 1(>, 17 ; onc(
an island, 135 ; fossils in beds of (luart.z rock,
:vn : hills, their nature, 140
(ialwav, hill of drift at, 13; action of i.c
in coniiliy about, 20, 71 ; curve, trail of,
42 40
Ganges nuis out of a glacier, 255
Garden near London, clleel of smoke on, 488
Garve inn and loeh, ice-marks, 149
Gas (hot) in a sliell of e.ddei- lluid, 344
Geikli' (Ai.liili.iM) M)ii the I'lienomena of the
Glaei.il jiiili ill Seotlaiid' quoted, 05,256;
refniiil i... ir.i; a. lopts opinions of Professor
K.inisav 01 his 'i'lienomena of the Glacial
Uiift of tseotlaud,' 147
Gellivari, Lapland, long vein of magnetic iron-
stone at, 340
' Geologieal Map of Scotland,' by Sir R. I.
Mnrehison and A. Geikie, referred to, 332
George (Lake), 'J43
Geyserdepo.sits stone iutiny waves like ripples,
290 ; tubes of Iceland, their situation, 395 ;
one at Reykjavik, 390 ; (Great), position of,
410 ; dimensions of, 411 ; boiling up of, 412-
410
Geysers, how to make a model illustrative of,
3!ll-:i;H ; uieelemies of, tuo tlhoiirs to ,\.
plain, :ili:; : tubes close t... mi ; s.mI,-,! luiies
near, 4llS ; view of, fioiii the hoise I rack, 40li ;
position of, 410 ; tcmiierature of, and source
of heat, 418
Giant's Causeway, marks of ice near, 59
Gigantic beasts, remains of and traditions
about, 192
Glacial action at Borth, 212 ; tracc<l on a rail-
way, 212, 213 ; varies, '209
Glaeial denudation, extensive marks of, in
tilaeial drift beds. Mam Turk, 44 ; Leenan, 45 ;
near ln\erncss, 132; near Dingwall, 154;
higlie.st Scotch terrace at Dalwhinny, 165 ;
in Isle of .Man, 173 ; how caused, 174 ; of
Glacial period, its end coincided in level with
rise of isthmus Joining Kussia and Scandi-
navia, 137 ; the jiresent time, theory of
author of this wiuk, 117 : a recent one in
Britain, 249 : and in .\meri<'a, 249, 2.50
Glaciated locks at Bidston Hill, 181
Glaciation (signs of), in ICillarney district,
177
Glacier action in Wales, 199, 204 ; where two
met and jiartcd, 205 ; de Boissons, Mont
Blanc, 205 ; picture on the memory caused
by a scene in Ross shire, 142 ; tracks in
Strathspey, 128
Glaciers, course ot ancient llo.it inj jlarici'- in
Ross-shire, 140; the last SmM,, ic,; i,;;
ditionsof, 107; formeil dales m '(oiLshiiv,
180; of Central Asia, 2.J3 ; liou ijuy lui^lit
be increased, 254; not the result of cold
ahinc, 257
Glacier-ice, how formed, 325
Glacier-system, Arran, record of, GO, 07, 09
Glaishei(.\lr ), linds simw falling above Eng-
Glass and saiul, teMiju'raturc, 325 ; transparent
fused moves like boiling water, .3.^7; ball
m.ade under care of Mr .lames Chance, 4.s:) ;
made from, W
atchcd stones
IJ^DEX.
509
Gleiiliar, travL-lk'.! blucks at, 74
(jleiiciiHlIi, glacier traces in, 70
Glenelg glen runs westward, 134
Gleiifalloch, traces of ancient ice, 79
Glengarry, deep groove, 134; once a strait at,
130
Glcunioriston, deep groove, 134
Gleuroy (parallel roads of), ancient state, 130
Glentruim, glacier tracks, 128
Glenveagh, perched blocks at head of, 57
Glen in which big animals were hunted, 192
Glens, what they are, 5 ; in Western High-
lands, S3 ; in Sutherland, their direction,
134 ; in northern division of Scotland, cor-
responding ivith notches in coast line, 134 ;
of Yorkshire, their character, 178 ; of Is'orth
Wales, their radiating character, 205
Gneiss (Laureutian), fonuerly subject to high
temperature, 339
Goatfell, Isle of Arran, 65
Goat Island, Niagara, packing of beds of gravel
upon glaciated rock, 312, 313
Goats on Cnoc Ourid, 27
Goddard Crovau, block in Isle of Man said
to have been hurled by him at his wife,
173
Godesberg(Castle of), built on an old volcanic
mound, 428
Gold nuggets suddenly cooled, 341 ; jiaint, ex-
periment with it dropped on a whirling top,
405
Gorham, White Mountains, laminated teirace
at, 290
Granite boulders near Ben Wyvis, 153 ; blocks
on Dartmoor, 220 ; breaking and weathering
of granite, 221 ; hiU, the nearest to Wales,
214
Grant (Capt.) on glaciated country about
source of Nile, 253
Grantown, glacial drift, railway at, 129
Graphite in French meteoric stones, 384
Gravel (terraces of stratified) afford a series of
records, 136 ; arranged in regular ridges and
furrows in Faro Islands, 295
Gravitation, a term that cannot be perfectly
understood, 203 ; studied in a glass tank,
304 ; applicable to all visible material things,
355 ; engine, 443
Green (Mr.) of Messrs. Powell's glassworks, his
assistance, 490
Greenland, mean temperature of, 216
Green Mountains, raised beaches on, 290
Greenock, glaciated rock at, 78
Grimsel Col, highest known limit of erratic
formation, 206
Groban (hill of), ice-ground, 144
Groove crossing Scotland from Dornoch Firth
to Loch Carron, 133
Grooves on rocks, 4 ; nothing to do with dip,
strike, or subterranean disturbance, 135 ; on
hills near Loch Maree, 139
Ground (shaking of), engine in filter-maker's
window disturbed by, 443
Grouse, hills frequente'd by, 125
' Growlers,' fragments of icebergs, 236
Gulf Stream, importance of, to climate of Scan-
dinavia, 156 ; (equatorial), the best course to
the North Pole, 445
Guthrie (Dr.), tried to describe iron melting,
361
Gutta-percha, e.vperiiiient with htatid, 401, 403
Gweedor, 54
Gwynant valley, action of ice, l!i3
Gyroscope, toy invented by a French iihiloso-
pher, 447
H-«M.\TiTE veins with iciclc-likc pendants in
hollows, 341
Haile (Mi-. John C), registers of sun's power
kept by, 4SS
Hamilton Inlet, picture from, extended to
Cheshire, 182, 183; state of, in July and
August 1804, 236
Hamjishire (New), ice-marks in, 242
Hares (mountain), footpaths of, on Ben Wyvis,
153
Harmony produced by air, 440
Harris, direction of ice-grooves, 101, 102
Harrison (Cape), Labrador, 235
Hartford Station, Cheshire, low grounds
about, 181
Hazledown Hill, three ridges at, 225
Heat (marks of), most apparent on rocks low-
est in series, 324 ; (internal) indicated by
lower beds, 327 ; intense heat must have
altered Lam-entian rocks, 334 ; of fusing
metal, nature of, 343 ; from reflection, curi-
ous instance of, 349 ; effects of, 387, 389 ; of
Geysers, probable deep source of, 418 ; and
of other springs, 421 ; in earth's atmosphere
and internal heat, a ray-force, 463 ; rays
travel with beams of light, 471
' Heaves' in Devenshire and Cornwall, 220
Hecla a cone of eruption, 429 ; buried tube
of, 430 ; its long axis, 454
Heidelberg, action of sun's rays at. 485
Helen's Tower, view from, 61
Helgafell, gravel in ridges at, 296 ; yellow
volcanic mountain seen from, 430
Heliostat required to make accurate photo-
graph of sun, 476
Henderson's ' Iceland' quoted for account of
eruption of 1783, 424, 425
Herschel (Sir John), papers on Light in Good
IVords referred to, 485, 493, 494; (Sir W.).
observes bright streak on sun, 498
Heytor Rocks, 221
Highlander (ship), lost off Newfoundland, 227
HiUs (of drift), shape of, important to observe,
137
' Himalaya' and other vessels encounter ice-
bergs in southern seas, 250
Himalayas, system of local glaciers there, 253 ;
winds over, 257
Hippopotamus, remains of, found in Great
Britain, 193
Hitchcock (Prof.), finds sea-beaches at 3000
feet above sea in Switzerland, 252
Hoar-frost, rising of, 358 ; found in coal-pit,
440
Hollows made by arctic currents, 5
Holmes' light in Exhibition of 1862, 441
Holyhead, glaciated rocks, 20
Holy Isle, Arran, perched boulders on, 71
Holy Land, rock fonns in resembling ice-work,
253
Holy rock of Tobar-an doon, resort of sick
pilgrims, 58
Honeysuckle tunjs with the sun, 489
Hooker (Dr.), on local glaciers of HiuialayaN,
510
253 ; finds an aucieiit iiioraiiii; on Lebanon,
253; jjives a ivasnii IVir glaciers being on
wannest si'K' "I lulls, j',:
llopkins (Ml ). n -iim\, line and glaciers
reacliing tli. -^ ;i in Wiirs, i-te., 249
Horizontal liii< s m1 1;iii,u, :ijif at Stockbridge,
•2->i
Horn (Cape), bergs off Cajie Horn nuich larger
than tliose off Newfoundland, 251
' Hut loiU-s' of Devonsliirr mines, -J-JU
Hot sprin-s of Icrlan.l iiiiulit l.c used, 200:
at Batli, -J-JO ; workin- in-Ml,! ,,f, :{;il ; iu an-
cient sands of wliiih u.. na.L iriiiaiiis, 395;
why at the foot of hills in Iceland, 3'J7
Hot region of Iceland lower than sea-level,
Hraundal, Iceland, crater at, 376 ; stones
Hi
in n.-nniaik, -Jlo
rat iiicix^asing i^radually W
Ii'E. motion of am
10, 17; level a
al rn,..| 'muwi-,
\Vai.s, 1
:ient 1
about Loch Ma
eh Mare,' wher
(lloatimj), arli,,
fireat
■titlaudi 137; on l:
in-eut llowinn llii..u
■ar Dingwall, l.'i'J ; in
lier Western Islaii. Is,
0, 171 ; woni out in
nf land in
11, Mr,
of Mai
, travelled block on, tlM
largo deers and birds,
Hnne Hill, 1',
Hunting, a .1
Celtie st.ny
Hvita liver and its white mud, 209
Hytvna(cave , remains found in Great Britain,
193
Hyde Park, shadows of i)osts in, marked out
by lines of snow, 259
Hydraulic cranes, modern, 204
' Hyrm Tliyrsar,' the frost giants, 210
■d), traces of its aeliou iij
luiilton Inlet, Labrador, 204,
ilnntic in 1804, 227; before
Ice (iiular), its uictioii south-westwards, 453 ;
motion of a bit atl'eeted by revolution of
earth, 457 ; engine in Exhibition making,
439
Iceberir, Cdllisimi uf screw steniiirr 'Royal
.Stan. lard' with, L'.'in ; size ol'a lii'-e one in
S. Seas, and uliat il nil :lil .l.i in tlieN. Seas
I ween Ijellcisle and Cape
action on rocks, 237 ; drop
Ic marks of, near Dunrobin,
I y freezing silver, 350
I Loch Maree, 138 ; nature
"iiclusions from proof of,
ins of North Wales, 1U4 ;
tone of Yorkshire, 179; on granite blocks
t Haitr..nl, isl : at Katun, Is-J
iieii! -^ :ii i-.iiuav Valley, I'.is; ,.n Welsh
iiH- • ■ ' - !e I l.iiel In I ir\ i.nsliire at
cii ■ ■ ■• • ~, -■■■^■. ilirertnm in N.
157, 15S ; volcanic eruptiiiii : nu
glaciers on north coast, 2.'i;i ; i : \ , se
from the sea, 314 ; lava-floods i, ^l ; _:Lat
eruption of 1783, 424
Icelanders might use their hot springs, etc. ,
200
Idris, tradition of, in Wales, 210
Igneous rocks in softer strata, how left, 100 ;
dykes of, at Brada Head, and their elleets on
cliff, 331 ; believed'by Neptunists to be pre-
cipitates, 340
' Illustrated London News' (piotcd for cut
and description of collision of a shiji with
India, change of level that would sink, 2,')."j
Indian cosmog(jny, 200
Indian Island, stria; on, 237
Ink, motion of a drop on a block of wood,
440
Inorganic forms recording facts, 283
Interior of earth believed by Captain Symnies
to be lieopled, 308
Invent, what it nieaiis, -JC.-I
Iliver Cnnneiiiira,,! Inl tors at, 7; perched
j|,p.
Irelaiel (u.M coast of), maiUs uf ice-lloats, l;i ;
most, of it once under water, 42 ; JiiUes on
.action of ice on rocks of, 175 ; whole island
grooved in one direction, 170 ; glaciation in,
177 ; traditions of land rising and sinking
itained from, ISl ;
1, 302, 303; when
:e water, W.i : of
10 : loun.Iry, visit
: rmnaceandsub
tri
hrie to describe, 301 ; weajjons in
at-bogs, 215 ; works in Lanaik-
Ironstone (magnetic), long
vari, 340
Islay, ice-marks and terraces
Jas|M
Jcrse
Joule (frolessoi) on heat, referred to, 499
Jukes (I'mlcssor) on glacier roumling and
polishing of Irish rocks, 175; 'Manual of
511
Kensington waterworks, iilisri vatiiius uu sun's
buniiiig imwcr luiidu at, 4Kti, 4S7
Keris, in Brittany, tradition uf its having been
overwhelmed, 1S8
Kettle, powers of steam studied from lid of,
2(54
Killaniey district, signs of glaeiatioii in, 177 ;
tradition abont the good O'Donoghue riding
on suifacr, lS!t
'Killns'nf l>:.rt!i:r..,r, -i-j-J
Killic'iTiiii:: !l' 'I, iro-tracks at, lli)
''' M^r-' . ■: - :, liO
,.-, tl. ■ •■.-. : lit, VM
■ i I , Allan, ii7
I ice-ground liill, 113
- 1 iiier-niarks at, 13b, 141
,11 - II- :hI, 134
Kiiil:iil -l.n luns westward, 134
Kiti-hfii hi-her than level of Geyser, 419
Kitcliin uii'Mi'ns of Denmark sliow long human
nc-L-U]iation, -.'ijs
Knoydart glen runs wistwaiil, 134
Kotzebue on ditlcinicr in \ c-etation on two
sides of liehrin.L's sii.iit, J.'il
Krabla, dro]>s on imnl iVoia boiling sjirings,
317 ; fiuinel-shai'ed hollows in volcanic de-
bris at, 394 ; supposed cone of lava at, 4*29 ;
longest slope, 454
Kreuzuach, near the Rhine, beds of different
colouT-s in quany, 314
Kyle Akin, rapid tide llirouuh, referred to,
132
Labrador, mean temperature of, 216; coast,
nature of, 235, 23G ; Laurentian rocks of,
333, 334
Laggan inn, ice-traces near, 126
Lamlash, ice-grooves on sandstone above, 66
Lanarkshire once under water, 95 ; nature of
county, 96 ; sandstone casts in beds of iron-
stone, 302 ; iron-furnace lined with fire-
clay, 326 ; smelting-fumaces for iron, 361 ;
slag-roads studied by author, 366
Land-glaciei-s, how their presence or absence
in former times may be inferred, 136 ; be-
coming rivers, 159; probably once occupied
upper glens in Yorkshire, 179
Land's Eml, great wave at, 286
Lapland, rise of, as affecting cun'ent, 219 ;
magnetic ironstone in, 340
Lapps liave traditions about giants and big
beasts, 186
Laurentian rocks of Labrador altered by in-
tense heat, 334
liSusedat (Prof.) on cimrse of great French
meteorite of 1864, 384
Lava, how to tell which side of a bit was up-
permost, 390 ; sections of lava figured,
400-423, described, 390 ; of Surtshellr and
Myvatn, 401 ; of Vesuvius, 403 ; tract of
Iceland, 1500 miles square, covered in a
few days with, 425 ; mounds in Iceland,
427, 428 ; chambers in, 355, 356 ; blocks in-
dicating a choked tube, 426 ; craters, Faxe-
fjord, 430 ; Eldborg, 430, 431 ; shapes copied
by freezing silver, 350 ; stones like sparks,
370
Lava-stream on Etna, 371 ; more raiii<l in the
middle, 372 ; at Piedimonte on Etna, 374 ;
setting fire to trees, 375 ; (old) in Iceland,
431
; section thi-ouyli
423 ; vegetation i
suifaee ol' a frozen
Icelaml best about.
Laws moving air opposite ways, 232
Laxey, Isle of Man, boulders near, 171
Layers deposited in pit of Strokr strangely
contorted, 417
Leaca Bhreaca, Arran, igneous rocks iee-
ground, 6ii
Leaca Donna, a hill in Ireland, 34-36
Lead, erystallisiii- of, i-u.O ; how silver is ex-
tracted liMiii it, :;li',, ;-;47 ; oies, smelting of,
destructive to ve,i;etatn)n, 341 ; smelting of,
in Yorkshire, 341 ; silver associated with,
342 ; washing, an illustration of denudation
by running water, ISO
Lebanon, an ancient moraine on, 253
T.' '!j- o;, i,oit!i -,; i, of Geyser-jiipe, 417
1.' I~ : i: :i 1 i.s of old bones, 193
■ar, 54
Level, change of, in Wales, 187; traditions
about, 188 ; of sea and land has often
changed in Easteni Counties, 217 ; changes
in level required to swamp continents not
so great, 255
Lichens will not grow in extreme cold or
heat, 318
Light cnn be liavnessed and s.'t to work, 266;
makes riii|.l.- nmrlc, -^74 : IVoin a si,,: reason-
ing about, left to ;i,stlolloll|rr, .■;,-,l ; ,.|,-|-tric,
438, 441 ; w:iv,s of, -ir,; ; ],ou,-i.s ,.|, vary as
the day wears on, 4.^4 ; inllueiue of, on ani-
mal and vegetable life, 488, 489 ; a power
in every engine of human constniction, 499
Lighthouse Commission, drawings made by
sun, 482
Lightning, effect of, on bell-wire, tree, bed of
sand, 498
Limestone (Irish), 61 ; dissolved by rain-
water, 318; of coal formation used in iron-
smelting, 325
Liochart (Loch) grooves on gneiss, 148, 149
Lions, remains found in British Islands, 193
Litharge, 346, 347
Liverpool, glaciated rocks, tides neai', etc ,
181
Llanberis, glacier once there, scenery arouml,
197 ; col at, 206
Llandudno, low hills with bmdders and
perched blocks, 195; Snowdon, as viewed
from, 209
Llyn Pencam-g, a small Welsh lake,
Liich Alsh, glen runs westward, 134
Loch Awe, ice traces on shores, 82
Loch Eck, boulders on shore of, 80
Loch Ericht, boulders near, 123 ; once
strait, 124
Loch Fj'ne, ice traces on shores, 81, 92
Loch Garrv, ice-marks, 120
LoehOoil," glacial drift, 80
Lorli LonLi, ice-marked rocks on shore,
Lorh of Lundy, 113
Loch-Maree, ice-marks on 1
groove which holds, 141
Loch Ranza, ice-marks, 7ii ; (
block of granite, 71
Loch Tarbert (West), istlinms at
Lodes, theories of depositi(m of,
Loggan stones of Cornwall, 222
199
Is about.
7(i
s, 340
512
INDEX.
Loiuloii, Mo.s aiul icebergs once passed over
site of, -J'.'i;, -J'JS
liiin;^ Island, voc^ks and boulders in, 100
l^oni, OowmI, and Ceautirc, once pcrliaps ten
LouKli Co'rrib, Vioulders on liills near, and on
tlie shores of, -23, 21
Lough Foyle, 53
Lovafs Forest, deep groove, 134
Lundy Hill, ice-ground, 114
Lyell (Sir Charles), 'AntiijUity of Man' re-
ferred to, 104 ; referred to for account of
glacial phenomena in Ireland, 177 ; quoted,
•217, '218, 219 ; on distributions of land and
sea producing changes of climate, 251
Machari, Arran, drift arranged in terraces, 07
Maes-y-Safn, weathered limestone rocks, 195
Magnetic currents seem to have influenced
bearings of metallic veins, 340 ; instruments
at Kew disturbed by bright white light in
front of sun-spots, 497
Magnetism might do other work beside pilot-
ing, 200
Malar, raised beaches at, 289
Malleable iron, 303
Mam Turk, beds of glacial drift, 44
Mammillated surfaces, 6
Mammoth (Siberian) eaten by dogs when icc
was thawed, 320 ; near Behring's Straits,
283 ; Cave, fossils projected from limestone
rock, 318 ; Cave, sick persons and animal
life in, 489
Man (Isle of), obscr\-ations on, 109176; Ire-
land of same shape as, 170 ; tradition suj)-
porting geological evidence of channel
between it and Ireland having once been
ilry, 189
Manclicstir, action of sun's rays at, 485.
M:ips of Scotland do not give true shape of
Sutln'i-lana hills and glens, 134
Marble cliiniiiey-piece, ridges and grooves
like a, 143 ; (liiarry on Aracul, Ireland, 55 ;
stones in Cheshire, 182
Marbles, illustration of force and motion from
game of, 272 , . ..
Maree (Locli), in Western Ross-slurc, its
beauty and environs, 137, 138
Margate, a large boulder found off, 223
Marine formation, exi'eriments illustrating,
304-307 ; terraces at Stockbridge, 225
Mascali near Etna, 372 . , ., .
Maskelyne (Prof.), his list of meteorites in
British Museum, 383
Massachusetts, ice-marks in, 242
Mathieu, on the fall of a meteorite m France
in 1804, 383, 384 . , , ,
Maury, 'Sailing Directions' quoted for __gla-
ciers being on warmest side of hills, 257
Meall Mor on Gaiiloch, ice-marks, 145
Mechanical tricks shown by a mathematician,
'I It
Mcilil. 1 1 uiraii perhaps oncc the receptacle of
Mil an lir .uiicnt, '252
M.ImII.- Islan.l, action of sun's rays at, 485
McMiai 111 iil;;c-, glens formed by ice, '20 ; strait,
191 ; groove, 208
Miiciuy below frozen water, 389
>lerkiar I-'oss, near Hccla, a water-mark, 100
Metal and sla- drops may teach i.lnlosoplitis
<-:,), 1 1, ill ; ..ftlh-structnreof the earth, 309:
(1, .: .1. . ■ 1- .1, li',9
.M,(i: '■■■,. Ml, :J37; theories of the dopo-
mI'mu Ml 1'-|m,, :iio
Mtt ill)' \. iim, tln-ii- bearings coricsiiond to
iiiamirlhTiinvMts, 340
Mrlaiiioi|.liisiii. is it a result of heat? 327-329
Mrtcoric sloiics, their origin, 383; numbers
of, in museums, 384
Meteorite at St. Petersburg described by
Pallas, 385
Meteorites and sparks in a smelting-house,
309 ; at British Museum, 382, 383 ; paper
on, by Figuier, 383
' Meteorological Journal ' for 1857, paper in, on
self-registering sundial, 483
Mica-scliist block on Pentlauds, 98
Miller (Hugh), on ice-marks near Edinburgh,
102, 103
Miners might use heat-power to ventilate
mines, 260
Mines, heat increases according to depth, 324 ;
theories of ' deposition ' of lodes in, 340
Mintnn's potteries at Stoke, 181 ; potteries iii
Statlonlsliiiv, 324
Moilrl to illustrate volcanic action, 434-437
Moel Siabod, Wales, 198
Moel Wynn, Wales, 198 ; once an island, '200 ;
glaciers once on, 209
Molehills may teach how niuuntains were
made, 203
Mont St. Michel, change in sea level at, ISS
Montmorenci (Falls of), iiotcli visible from
Quebec, 242
Montreal stria', 245
Moon, mountain in, seen on eclipse of siui,
479
Mouselookmaguntic Lake, 244
Mop (whirling), Arctic Ocean compared to,
445 ; tluids from, 447
Mop-curves described, 451
Moraine, a perfect one 1350 feet above sea in
Koss-sliire, 139 ; boulders forniing isthmus
near Great Ormes Head, 195 ; crumbled
slate below Cader Idris, 210
Moraines, various kinds, 11 ; mark retreat of
dwindling glaciers, 204
Moray sandliills, tradition, 190
Morpeth, clay ami bould.-rs near, 175
Moss-hole drained, a model on a small scale,
Motion remotely caused by rays of light, 442 ;
of a stone projected from a volcano at equa-
tor, 451
Moulds for iron, 304
Mound at Borth, 212 ; curious beach at Sua;
f.'U, 2S8
Mounds of large stones near Inverness, how
carried, 133; with tubes in Iceland, 427;
aneiiMit ones at Bonn, 428; fonnation of, in
Iceland, 429 .
Mountain-ash tree growing on lava at *.ld-
borg, 431 , r ■
MoycuUeen, hills of, '23 ; hue sample of an ice
ground country, 2')
Mud, quantity of, estimate of work of denii
dation, '270; spring and forniatum ol tiilies
near Great Geyser, 404
Muddy water of glacier-rivers, 209
513
Mull of Ceantire, iciegi-ooves at end of, 73
Muswell Hill, northern drift at, 2 1 9 ; walk to,
in searcli of glacial drift, 226
Myra Syssla, district fonned of old beaclies,
289
Mythical disasters iirobably records of real
"events, 191
Myvatn, a volcanic stone from, 376, 377 ; ver-
tical chambers in lava at, 401 ; cluster of
extinct volcanoes at, 421 ; plain near, cliani-
bered, 422
Xaples, action of sun's rays at, 485
Nasmyth (Mr.) on present condition of planets
throwing light on fonner condition of world,
497
Natural science not taught in English scliools,
266
Xebulte, many resembling curves drawn by
whirling engines, 493 ; betray roeclianical
force in light, 500
New Brunswick, Ice-inarks in, 241, 242
Newcastle, clay and boulders near, 175 ; lead
ore fused at, to extract silver, 342, 347
Newfoundland (l)anks of), what they are, 217 ;
and parts of Europe it corresponds with,
239, 240 ; Indians and quadrupeds of In-
terior, 241 ; bays, raised beaches at their
head, 289 ; rocks of, 333
New York, ice-marks in, 242-244
New Zealand, glaciers in, 251
Niagara Falls, Ice-marks, 245 ; (river), chan-
nel cut by, 313
Nile, country about its source glaciated, 253
Nohic d'Orgueil, shower of stones which fell
at, 384
Norfolk, Suffolk, and Essex, changes in rela-
tive level of sea and land, 217
Normandy, tradition in, of change of sea-level,
188
North Berwick Law, ice-marks on, 103
• Noi-th British Review' for May 1864 referred
to, on the subject of heat, 499
North Cape, mean temperature of, 216
Northwich, boulders, salt-mines, and brine-
springs, 183
Norwegian dales very like smaller Yorkshire
dales, 180
Nova Scotia, ice-marks in, 241, 242 ; hferaatite
veins, with icicle-like pendants in hollows,
341
Nuts or tropical seeds cast up by the sea, 50
Oak trees of peat-beds in Denmark, 215
Obsidian, a natural black glass, 325
Ocean, circulation of, 232 ; w^ork and ice-work
contrasted, AchiU Island, 49
Ochil hills once a steep island, 107 ; ^^ewed
from different points, 109
O'Donoghue, tradition of the surface of Lake
of KiUamey being ridden over by, 189
Olivine, mineral in meteoric stone at St.
Petersburg, 3S5
Ontario (Lake), its bottom below sea-level, 255
Open water near the Pole, where to look for
it, 445
' Orbs of Heaven* referred to, 494
Ordnance map of basin of Firth of Forth, 104,
105
Organic forms and climate, 323
Organs in Exiabition blown by engines, 440
Orkney, great loose stones in, 162
Orines Head (Great), isthmus at, fonned of
boulders, 195 ; (Little), outlines of country
from, 193, 194 ; low hills at, 195
Ornaments (golden) laid bare by wind in
Moray, 300
Oronsay, ice-marks and terraces, 161
Ortles Spitz, once a tall rock in a European
ocean, 207
Ossian, story about, 191
Ox boiled in hot spring, 419
Oxen (gigantic), remains found in Great Bri-
tain, 193
Oxhver, Iceland, 418
Oxwell, Iceland, hot spring, why so called, 419
Pallas, meteorite at St. Petersburg described
by, 3S5
Palm-tree implies wann air, 319
Parallel roads of Highland glens, 125 ; of Glcn-
roy, 136
Particles, acting of force and resistance on, 272
Passages on hill-sides in Yorkshire to remove
smoke of smelting-houses for lead-ore, 341
Pately Bridge, old ripple-marks at, 281 ; curious
inorganic forms at, 283
Pattinson's process of refining silver, 347
Paving-stones at Pately Bridge, how formed,
283, 284
' Peaks, Passes, and Glaciers of the High
Alps ' referred to, 184
Peaks of hills jagged and fantastic like those
of Lofoten liiUs, 142
Peat found below low-water mark, 42
Pentland hills volcanic, ice-marks on, 98
Perch in English ice, illustration, 320
Perched blocks, 9 ; one on Cnoc Ourid, 28 ;
another on Cnoc Mordau, 29 ; CoU and Tyree,
161 ; at Little Omies Head and Llandudno,
195
Permian age (breccias of) deposited, 147
Petersburg, action of sun's rays at, 485
'Philanthropist' (ship) lost off Newfoundland,
227
Phillips (John A.), ' Manual of Metallurgy '
referred to, 342
Photogi-aph of sun, 472, 473, 474, 501
' Photographic Journal,' 1858, quoted for pho-
tograph of sun after an eclipse, 475 ; for Au-
gust 1860, Mr. Warren de la Rue's operations
in photographing sun, 477
' Photographic Journal ' of Liverjiool and
Manchester referred to, 490
Photography and photometry, 273 ; cliemical
and other results of, produced by electric
lights, 441
Phynnodree, a Manx fairy, and his deeds, 173
Pig-iron, 363
Pilgrims resort to holy rock of Tobar-an-doon,
58
Pine-apples an-anged spirally, 489
Pipes about ironworks, how formed, 400
Pittsburg to Harrisburg, structure of country
observed when travelling from, 332, 333
Plants stopping movement of sand, 301
Plaster-of-Paris used as an illustrative model,
390 ; illustrative exiieriment with, to show
how tubes and hollows of hot springs are
formed, 406, 407
VOL. TI.
2l
514
INDEX.
Plynliuiinoii, ioe-niarks on, 20'_'
Pointer-dog quarters his ground on system, 1 68
Polar currents versus jiolar glaciers, 247
Pole might be reached, 445 ; best coui-se for a
ship or a sledge, 445
Polished surface in situ proves passage of ice, 3
Portland Island, waves obseiTcd from, '279
Position and the age of a fossil, 322
Poteen distillery in Ireland, 30
Pottery manufacture, 324
Prairies, drift on, 247
Present time the ' glacial period,' theorj' of
author of this work, 147
Projectile (curve of) followed by volcanic
bomb, 451
Puckaster Cove,tradition of merchandise taken
to, on horseback from Winchester, 18S
Pyrenees, ' ice-peaks,' 227
QuAKRiED blocks, 8
Quarryman and hob-nailed boots, 4 ; conver-
sation with, about travelled granite blocks,
127
Quartz, marks on, are rare, 14 ; rock near Loch
Maree, peculiarities of weathered surface,
139 ; hills, effect of ice on, 140 ; rock pro-
bably once a sandbank, 332 ; lines of mean-
dering in cliffs of W. Scotland were once
soft, 332; (gold-bearing) like burnt stone,
341
Quebec, ice-marks at, 242
Queen's Drive, Arthur's Seat, ice-marks near,
■ 101, 102
Raasav, ice-marks and their direction, 101
Radiating mechanical forces, 233; movements
caused by solar rays, 471
Radiation of heat, 387 ; (terrestrial), eff'ects of,
in building chambers, tubes, etc., 420 ; and
giavitation shaped the igneous cnist of the
earth, 437 ; their power, 442 ; causes rota-
tion, etc., 461 ; (sun's), etfects of, 489, 490
Ralford station, drift at, 130
Railway (Inverness and Perth Junction),
heights of stations above sea, 131 ; cutting
in Wales from Rorth to Shrcwsbuiy, 212
Rainfall in Argyleshire, 87 ; at Invuiary and
Gairloch greater than in Slirtl.ni.I, '.'.'iS ;
marks, modern and anciriit, ::|., :.ir. ; ex-
periment on, 317 ; water, il.siicii lime-
stone rock, 196 ; water liol.ls cailponic acid
in solution, 318
Raised beaches at Myra Syssla and Malar, 289 ;
Newfoundland and United States, 290
Ramsay (Prof.), ' Tlic Phy.sical Geology and
Geography of Great liiilam' idcrrt'd to, 147 ;
o" glacial iihciiMiii.n.i o| Walr^ 184; 'On
the Hupcrflcial Ac. uiiMilat i..iiN ami Suifact
Markings of Nurtli Walc.N' rdcircl t(), 203
Ray-force, 293 ; power, familiar examples of,
355, 360 ; (source of), a furnace tire, 441, 442
Rays of sun, <li-~tances they travel and their
licMli.i-clVccts;, 490
He .i,,|. h, i„ ,r i,| from gravel terraces, 136
Hr^l l:,., , h. :il, 2:J7
Ki'l .'1 II Hi ir), remains found in Brilahi,
I'.i;;
Red llauies on sun, attempt to take by photo-
graphy, 479
Red suow caused by minute vegetation, 335
Reefs in Western Islands, 101
Reflectors (metal), a suggesliim for making of,
459
Refrigeration of Labrador climate, 217
Reid's ' Elements of Chemistry ' referred to,
342
Reindeer, remains found in British Islands
and France, 193
Relative position proves relative age of fossil,
321
' Rest-and-be-thankful,' 81, 92
Reyk,jalid, lava-domes, etc., at, 422
Reykjavik, Little Geyser and spring at, 396 ;
ai.'tion of sun's rays at, 485
Reykholt, spring building a mound in a river
near, 420 ; bath in which Snorro bathed,
420
Rhe (Isle de), cross-rollers at, 279
Rhinoceros, remains of two large species in
British Islands, 193
Rhyll, alluvial plain at, 196
Ripple-marks (old), of Yorkshire and Pately
Bridge, 281 ; of Orkney and Wales, 284 :
need not be the work of the sea, 294 ; on
snow by wind, 295 ; caused by motion in
some fluid, 296
Ripples on surface of water, 276
Rise of land in Scotland, effect on passes,
135 ; in Ireland, Scotland, and Scandinavia,
nature of last, 165; in Wales, 187 ; how in-
dicated, 291 ; in Labrador, 236
River-beds in Western Highlands, 83
River-glaciers in glens of Scotland, 135
Rivers did not form dales in Yorkshire, ISO
Road-dust (depositing of), as ill\istrating for-
matiim of sedimentaiy beds, 311
Rob Roy's Castle, 83
Roches moutonn^e.s, 5, 6
Rock, marks of heat on lower, 324 ; basins and
I, I'l, Pvf'f Ramsay on cause of, 147 ; snr
I ' \ " li for, near Longh Neagh, 02
r; . ; •. n icebergs over, 237; in North
Aiiiih I, in\\ri to the south, older to the
Roisg (Locli), col and heaps of drift nt head of,
148
Roller (Atlantic), its motion and appearance
described, 201 ; studied on Scottish coast,
285
Rona, ice-marks and their direction, 161
Roscoo (Professor), papers on light alluded to,
485
Roses, how affected by smoke and houses,
488
Rossie, two wide ^lens beliiiul, c<>llection.s of
WIN, 1.7 I'iS : iiMHlrh, I,, lIlN^lialeellectsof.
■li.'J- raiiMM l,y ra.iialin,,, ir.I
Rowardennan, ice-grooves on rock, 79
' Royal Standard' (screw steamer), collision
with iceberg, 250
Rubbish-beds, time-keepers, 209
Rnlibisli heaps, rocks with ripple-marks were,
' Riin ' (iron) described, 362, 363
Rutivari, magnetic iron.stone at, 340
INDEX,
515
Sahara, marine shells found in, 251 ; a roccut
sea-bottom, 253
Salisbury Crags, iee-marks on, 101
Salt, quantity paying canal dues annually at
Northwich, 183
Sand for glass-making, Derry Veagh, 54 ; waves
on, produced by water-waves, 273, 275 ;
arranged by wind on dry ground, 298, 300 ;
temperature to convert into glass, 325
Sand and mud washed into lakes in Strath
Bi'an, 148 ; exiieriments on deposition of,
304, 305
Sand-beaches formed by air-waves in Iceland,
299
Sand-beds in Cheshire (contorted), 1S2
Sand-drifts in Iceland, 299 ; in Scotland, 800,
301
Sand-fonn records movement in watci', air,
and light, 273
Sandhills (moving) near the Findhoni, 299 ;
farms covered up by, 300
Sand-lines on polished surface, 4
Sand-mounds at Granville fonned by sea-
womis, 395
Sand-spit formed by waves at Isle de Rhe, 280
Sandstone with ripple-marks, 281
Sawdust indicates numbers of trees sawn in
Scandinavia, 268
Scandinavia, tradition of seven parishes having
been smothered under ice and snow, 189
Scandinavian pattern and origin, stones of, 156
Scaur of Eig, 16
Sohreibersite, a mineral found in meteoric
stones, 383
Scilly Bishops, the last of the British Isles,
234
Scores on polished surface, 4
Scotland (central) once crossed by narrow
sounds, 130 ; traditions of castles and towns
having been submerged, 189 ; large dykes
and upthrows of granite, trap, basalt, etc. ,
in, 332
' Scotsman,' extract from letter in, on Etna,
371
Scottish Central Railway, nature of country it
passes through, 108 ; hills seen from Aueh-
terarder, 109 ; landscapes once like the hills
of Iceland, 129
Scrap-iron used to cool molten iron, 469
Scrapings of Iiondon streets, studies of, 316
Sea, action of, on north coast of Sutherland,
160; on land, 185, ISf. : all tvny.m, there
would be few clouds, 2'is ; In.ttciin .if, made
of lava, 432 ; need nut 1»- the . ;iu^,. df old
rijiple-marks and wave-iiuuks, 294 ; spoor
of, in Switzerland, 291
Sea-bottom at ebb of tide, 301 ; nowhere flat,
302 ; (ancient), in North America, 314
Sea-coast line, how formed, 185
Sea-horses and bears once in Ireland, 41
Sea-ice carried blocks in Ireland, 40
Sea-level has varied greatly on Irish hills, 42 ;
(ancient), of Scotland, i- i linu to Hugh
Miller, 103; a rise of l< i - r. rt, its
effect on northern ]i:ii - ^ 1, 135;
changes in, Cornish tr litnn, ir-^mling,
187 ; ancient, formerly muili higher in
Wales, 203
Sea-margins (ancient) of British Islands show
■ that the last rise of land was general, 136
Sea-marks on watershed in passes, 135 ; (old),
in sedimentary beds, 302
Sea-shells on Snowdon, 187
Sea-strait, glen now holding Caledonian Canal
once a, 132; an ancient one in Wales, 204,
207 ; ancient one in North America, 244
Sea-wonns at Granville, their habits, mounds
of sand, 395
SiMliim llrit .it Toulinguet in 1864, 238 ; beset
f^.;i!n)j-u,i\, cllccts of heat on, illustrative of
390
Searching for ice-marks, 15
Sedimentary beds, formation of, illustrated
by that of snow-beds and deposition of road-
dust, 311 ; rocks, what they teach, 268, 209 ;
formed of chips, 270 ; rocks how formed,
302
Seuora, meteorite found at, 386
Separation of lead and silver, 345
Serapis (Temple of), sank under water and
rose again, 228
Serpentine, London, waves on, studied, 277
Sevres china factory, materials used, 324
Sgeire Mhor reef, 161 ; curve of arctic current,
163
Sgur-a-Mhulin, 148, 150
Shan Folagh, Connemara, marks of an arctic
current around, 31, 32 ; its vai-it)us states at
different epochs, 33
Shell-fish (a burrowing), habits of, illustrative
of hot springs, 394
Shells in drift in Wales, 207 ; (marine) met
with 600 feet above sea in Wicklow, etc.,
177 : (marine) at Falls of Montmorenci, 242 ;
visible in many fathoms water in West Scot-
land, 269 ; extract silica from sea-water,
310 ; marl of eastern counties of England,
217
Shetlands, ice-groniid rocks, li;2
Shingle-teiTaces :it ccuirsiKiii'ling levels at
many distant points in l;iit,iiii, 136
Shower (thunder), study of Loudon mud dur-
ing, 316
Shrewsbury, museum of antiquities, 213
Siderolites, their composition, 383
Sidlaw Hills, 111 ; what they would be at dif-
ferent periods, 114, 115
Silica held in solution by Geyser water, 310
Silt, forces which pack, 270, 271 : (ancient)
deposit and packing recorded, 282 ; packing
of, observed on shore in shallow water, 303
Silver, cooling of an ounce of, 338, 358 ; found
in smelted lead, 342 ; freezing point of, 345 ;
how extracted from lead, 346, 347 ; (pure) a
specimen of, 338 ; how it was prepared.
Skeleton histoiy of world's cnist, fossils, 321
Sk.jaldbreid, old lava-streams at, 425 ; a frozen
lava-stream, 432
Skye, traces of work by land-ice, 161
Slag in iron cooling, 363 ; in iron furnaces,
400 ; on molten iron, contains a magazine of
ray-force, 470; studied when cooling, 470,
471
Slag-forms, 357, 358 ; slag crust, 360
Slate rock at Devil's Bridge worn by river, 210
Sliamh Gaoil near Tarbert, ice-ground, 76
Slickenside, Arthur's Seat, 101 ; in Welsh
mines, 214 ; in veins, 282
)1G
Slides iu Uevoiisliiie and Ctiniwiill, 'iJO
Sliocli, a iinjuiitain in West Ross-sliire, 13S ;
furrows on, 143 ; way to Norway oiien from,
to Wyvis, 155
Slope (iiinKest) of cones of ernption, 453 ; of
Etna, Vesuvius, and Heela, 454
SnaUinj; iron, limestones used in, 325 ; houses
iu r>auarkshire, 361 ; in Greenock, lessons
studied in, 3ti9
Smithsonian Institute, 'Ainsa' meteorite in,
385
Smoke on a heath or field, studies of air mo-
tion, 275 ; nuisance, observations made to
show, 488
Smyth (C. Pianzi), on effect of sun's rays on
Teneriffe, compared with effect of lieat of
moon, etc., 471 ; on the Peak of Teneriffe,
434
Sniefell, a cloud condenser, 259 ; beach at, 288 ;
great cone of, 430 ; longest slope, 454
Snitfells Jiikull, very like in shape to amound
foi ini;<l by a hot spring, 421
Suajfell, Isle of Man, 171 ; surface and struc-
ture of, 172
Suorro, bath at Reykholt in which he bathed,
420
Snow, melting of, on a glass roof, illustration,
339
Snow-bed on ice of a pond, illustration, 322
Snow-beds in Iceland alternating with beds
of ashes, 310
Snow-beds (stratified), undulate with the
ground beneath them, 311
Snow-dome, Central Scotland probably once
a, 142
Snow-drifts, influences of melting, 295 ; are
air-marks, 297 : principle of, 298
Snow-line and glaciers reaching the sea in
Wales and Ireland, conditions of, 249
Snow-models of the curved path of air, 297
Snow-wave in Cheshire, 293
Snow-waves after strong gale, 297 ; gigantic
ones on Ali)s and in Iceland, 298
Snowdon r.iiise from Anglesea, 20 ; sea-shells
found lii-li nil on, 187; ridge, 194; range
onci- an .iirliiiMlago, 200
Snowy niniinlaiiis in Africa, 253
Soda-water bottle, illustration from, 359
Soil and sediment not altered by slow rise or
falling of earth, 329
Solar heat stored in coals, 338 ; system turns
one way, 467 ; photography, how to con-
duct it, 476 ; scale, 481 ; spots and electric
storms, 497
Solids deposited by hot springs in Iceland,
395
Sonmia (Monte), how raised from the sea, 434
Sound waves, coj)ied in dry sand and water,
273 ; absence of, when bell is struck in ex-
hausted receiver of air-]>innp, 467
Sounds, Central Scotland once crossed by
narrow, 130
' Sow and pigs,' moulds for iron, 363
Space, regions in, sujiposed to be colder than
(illicrs, 260, 261
Spaiks in a snieltinghouse, drawn and
studied, 370, 377 ; from electro-magnetic
engine, 441
Speculations (fancied) of a future Esijuimaux
geologist, 335, 336
Spey, course of, 127
Spheres projected from molten silver, 350;
spongy structure of, 351
Spiral arrangements In vegetable kingdom,
489 ; nebulw, 493 ; pattern of winds, of sur-
face of sun, 496
Spoor, 3
Si>ots on sun cause increased temperature on
earth, 498
Sport, how to combine two kinds of, 2
Spout-fish, habits of, 394
Spray from a wave, 286 ; of Geyser, scalding,
417
Spring in Duddingston Loch, 408 ; (hot) near
Reykholt, 420 ; (hot) experiment to ex-
plain formation and movement, 434-437 ;
(mud) in Iceland, observations on, 404,
405 ; (spouting) Bay of Faxef^jordr, 421
Stars, rays from, act on photographic chemi-
cals, 492
Star Point, lake near, 287
Steam and hot metals, 343 ; formation of,
344 ; (violent action of) in iron-furnaces,
364, 365 ; in Geysers and hot spring at Reyk-
holt, 412; of Strokr, 416, 417; formation
of, 387 ; boilers deposit earthy materials in
ripple-marks, 296 ; engine in Strathspey,
127 ; engines in boats, how employed, 262,
263 ; power in Great Exhibition, 439
Still, fuel supplied to, an(i water poured on
the woi-m, an illustration, 260
Stirling, ice-marks on castle rock, 108
Sti])er stones, boulders, 213
Stockbridge, trout and greyling of, 223 ;
shelves at, 224 ; denudation and deposition
at, 229
Stoke, English watershed at, ISO ; Minton's
potteries at, 181
Stone-book of sedimentaiy rocks, 323
Stone implements in peat-bogs of Denmark,
215 ; found under sand-hills in Morayshire,
300
Stones scratclieil, grooved, and scored by ice
near Blackrock, 21 ; (red hot) projected
from crater of Etna, 371 ,
Storm in Arran, 69
St. Abb's Head, 134
St. John's ' Wild Sjiorts of the Highlands' re-
ferred to, 299 ; ' Natural History and Sport
in Moray ' referred to, 299
St. John's Harbour, Newfoundland, in June,
240, 248 ; New Brunswick, 242
St. Lawrence, shores of, ice-marked, 242
St. Louis (hill near), exposed fossil on a
weathered limestone suiface, 318
St. Michel (Mont), observations on sands of
strand near, 311
Strahlek snow-shed, 206
Straits, ancient ones in the West of Scotland,
81
Strata not always deposited flat, 310
Strathaflaric, <leep groove, 134
Stratli Bran (ince a strait, 135 ; its ancient
st;ilr, l:;7; i. ,■ ■„,u.^r^. MS; no glacier in
it. I l;i: .sr. II ii,,,,, ;, liMuliI, 1,52
Str.-lth Cmii.'IM. Jrr|i -,.^„^r, l.'il
Stiat.ln:ain, liilU li(..)und, 109
Stratlunoic, 111
Stratli I'elfer, granite boulder at head of, 152
Strathspey, traces of ice movements, 123
INDEX.
51'
Stream (arctic), at Ne\vfoun(llan(I, '2as ; beJ
cut by in Yorkshire rocks, 178
Street pavement, wearing of, lesson from, 100
Striie on polished surface, 3, 4 ; on rocks of
Snowilon range, 197
Strokr or chum of Great Geyser, 411, 41S,
419
Struan, north of Blair-Atliol, moraine at, 119
Structure of earth, how geologists would like
to study, 367, 368
Subsidence of sea, how indicated, 291
Suil Bheinn in Sutherlandshire, 158 ; its struc-
ture and shape, 159
Sular, Icelandic for pillar, origin of name Suil
Bheinn, 159
Summer (wann) sets ice adrift and intensifies
cold in other places, 239
Sun making iihotograph of himself, 472, 473,
474, 502 ; plan devised for observing, 476;
sun-pictures, 472, 479 ; can engrave, 480 ;
sun's path on two cloudy days, 481 ; can do
the work of hot iron, 482 ; spoor of, for three
winter months, observed at Campden Hill,
486 ; its effects on sealing-wax, 491 ; its rays
act as a mechanical force, 492 ; its atmo-
sphere, 495 ; bands on, 496
Sim's rays set to make pictures, carve wood,
move machinery, etc., 472 ; can wind up a
clock, decompose fluids, etc., 499 ; reflected
and absorbed cause radiating movements,
471 ; forms in a legible index, 500
Sun-dial, a new self-registering one, 483
Sun-light, its influence, and what counteracts
that influence, 260 ; engine-turning by, 484
Sun-power might work heat-machines, 266
Sunshine, j>ower of a ray in spinning drops of
collodion, 462
Superior (Lake), change of level that would
sink 255 ; deposits of iron and copper
around, 340
Surtshellr, Icelandic cavern, 399 ; roof of,
401 ; sinking of lava at, 424
Sutherlandshire glens, their direction, 134 ;
coast, direction of, 155 ; once under water,
156 ; nature of central parts, 157 ; hills of,
158, 159
Sweden, a bit of, planted in the midst of Ire-
land, 51
Siviss mountains, snow-line, glaciers and
glacial action, 251
Switzerland, sea-beaches high up in, 252
Symmes (Captain) believes interior of world to
be iieopled, 368
Tallow, setting of, 337
Tana (River), beds of sands cut by floods,
311
Tan-y-Bwlch, boulders near, 210
Taormina, Etna in eruption viewed from, 371
Tarbert, perched blocks and ice-marks near,
76 ; in Scotland, how formed, 135
Tay and Isla did not carve hills of central
Scotland, 110
Taylor (Dr. A. S.), thermometrical table, 326
Tenijierature of salt mines at North wich, 183 ;
giadual change of, in Denmark from cold to
wann, 2ir. ; (im an) at earth's surface as cold
as it cvor WIS, I'lii ; in which organisms will
live, 310: ffl.rts ..f ri falling, 320; of hot
springs nil iiiia.Mire of temperature deep
under gi'ound, 392; registered by rain-marks,
317
Teneriffe (Peak of), how raised from the sea,
434
' Teneriffe,' by C. Piazzi Smyth, referred to,
485
Terraces of drift at Dalwhinny, 137 ; at Stock-
bridge, resembling those of Scandinavia,
224, 225 ; heights in Asia, America, and
Europe at which they are situated, 255 ; in
Newfoundland, 290
Ten-aoed piles of boulders at Dunrobin, 155
Test River at Stockbridge, 223 ; lessons de-
rived from it, 231
Thermometer, attempt to get a large one into
the middle of Geyser tube, 417
Thermometers, forms of plants and animals,
319
Thingvalla, sunk plain of, 399 ; sinking of lava
at, 424
Thistles, direction of wind from, 9
Thorn (old) tree on N. Berwick Law shows
general direction of wind, 104
Thimderbolt whieh fell between Edinburgh
and Glasgow, what it turned out to be, 382
Tides throw light on marks raised by old
Scotch ice, 88 ; (ancient) near Strath Bran,
148; (cold) once in Cheshire, shown by con-
torted sand-beds, 182 ; (high) from strong
gales at sea, 276 ; and tidal-waves, 280
Tierra del Fuego, how inhabitants sink their
dead, 190
Tigers, remains of gigantic tigers in British
Islands, 192
' Times,' extract from letter in, about erup-
tion of Etna, 373, 374
Tintron, Iceland, how it may have been formed,
399, 403
Tobar-an-doon, the resort of sick pilgrims, 58
Tom-na-Shirich, how it would be affected by a
rapid tide over Inverness, 133
Tool-mark of wave, 281, 282
Top (metal), spinning of, in water, 464, 465 ;
patent metal, 447 ; their spinning, 448 ; ex-
periments with, 449
Tors of Devonshire, 6 ; broken and jointed
tors, 7 ; of Dartmoor, 220
Torridon, terraces, 148 ; hills, 154
Tour de Balene, a lighthouse, view of waves
from, 279
Tracks of ancient creatures on ripple-marks,
281
Traditions tested by geological discoveries,
186-193 ; about movement of boulders in
Isle of Man, 173
Traeth Mawr and Traeth Bach, 198
Traeth Mawr, beach at, 287
Trains of stones, origin of, 11
Trees in exposed places used to know general
direction of wind, 2 ; of coal formation, 283
Trinity Bay, Newfoundland, raised beach at,
289
Troilite, a mineral found in meteoric stones,
383
Tniim (Glen), time since there has been no
land glacier in, 137
Tube — buried lava-tube in Iceland, 426
Tube-making engine at work in Iceland, 404,
405 ; exploration of, by means of an experi
mcnt, 406
518
Tvibos of the Geysers, 395-30S; rough stone
tubes, ;!S>8 ; in volcanoes, 401-403 ; in granite,
404 ; in highest mountains, 409
TuUieli, lieaps of iee-markeJ stones, 81
Tullocli, boulders of pink granite near, 152,
167
Turner (J. M. W.), tried to paint iron-melting,
361
Tyree, perched blocks, 161 ; curve of Arctic
Current, 163
Tyr Von, in Anglesea, ground and scratched
by ice, 208
Uaish (Beinn). See Ben Wyvis
' Umbra,' ' Travels by,' referred to, 358
Underground traditions about heroes, 190
United States, ice-marks in Northern, 242
Upheaval of Wales, how its rate might be cal-
culated, 211 ; (phenomena of geological) may
be studied at an iron-fumace, 364
' Upthrows ' in Devonshire and Cornwall, 220 ;
in sedimentary rocks may indicate chambers,
422
Vapour in India intensifies the heat, 257 ; and
sparks emitted by fire-ball, 386 ; columns
over holes in Iceland, 420
Vegetable life, influence of light on, 488, 489
Vegetation (chemistry of) studied from a small
model, 307; of water-formation, 335; de-
stroyed by smelting of lead-ores, 341 ; in
Iceland, places where it is best, 431
Vermont, ice-marks in, 242
Vesuvius, tube at bottom of crater, 401 ; craters
and lavas of, 402, 403 ; its longest slope, 454
Vine-terraces of the Rhine, terraces in York-
shire resembling, 179
Volcanic disturbance, areas afFected by, Keith
Johnston's map, 178; eruptions in 1863,
228 ; explosions in molten silver, 350, 351 ;
bombs, 370-382 ; action in many parts of
Iceland, 396 ; erujitions (recent), in Sicily
and Iceland, 355 ; highest mountains are,
433
Volcano, effects of, on rocks, 325 ; stone pro-
jected from, its motion, 451
Volcanoes (extinct) at Myvatn, a cluster of,
421
Volcanoes, their fonns and movements imi-
tated, 434-437
Volga, what cliange of level would sink its
source, 255
Wales, liills of N.E. part of, as seen from
Chester, 19; its general character, 184;
rising of land in, 187; sinking of, lyo;
action cif ii'c ;is observed in, 194 ; Or.lnancc,
ninji (if, 1!M ; its weathered hills, bnuldrrs,
and jKicluil blocks, 196; geology of, 213;
liow it has been ground down, 214 ; geologi-
cal sections show tine scries of folds ami
cnrves, 331
Wandiri iig blocks of Arran, above Loch Ericht.
and on Hen Wyvis, 8
Wart well, ici' marks on a trap surface, 114
WasliinL;li.ii (M.>nnt), ice-marks on, 243
Watrli, nioiioii of ha?n1s in northern and
WatclicaM s rn . ,m,| smUi curves by PUginc-
turiiinK, ;iii'l mui : k,> , may do so, 483
Water-streams, their wearingaction on Scotch
coast, 134 ; meadows at Stockbridge, 229 ;
mills, modern, 264 ; weights used by millers,
265 ; was it too cold or too hot in strata
which contain no trace of life, 330, 331 ;
formation, 334, 335 ; state of, in smelting
lead-ore for silver, 342 ; on hot iron under
steam-hammer, 343 ; circulation of heated,
388 ; boiling, near water scarcely warmed,
302 ; lifted by engines, 440
Water-fleas in vivarium, 308
Watershed in passes, sea-marks on, 135 ; in
Ross-sliire, icp-niarks near, 146
W^ave of floo.l, its . ,nii^' , ss ; a great Atlantic
onedescril"i|, I'ul ; a l>)i'aker builds up sea-
beach, 261 ; toinis, iniportance of knowing
them to anglers and boatmen, 271 ; the
progress and breaking of a big one, 285,
286 ; formed land in Iceland, 289
Wave, changing form of breaking, 292 ; marks
need not be the work of the sea, 294
Waves and wave-marks observed from Conway
Castle, 195 ; work done by old waves may
be studied from existing waves, 271 ; growtli
of, 276 : systems of, 277 ; at Weymouth,
278 ; Isle de Rhe, 279 ; their denuding action,
292 ; how their progress may be observed,
Wax, freezing of, 337 ; illustrative experiment
with, 405, 400 ; (liot) experiments on, 457,
458, 461
Wayne (Fort), section of gravel-pit at, 313 ; ex-
plains what is going on in the Atlantic, 314
Way's light, how produced, 441
Wearing away of land by sea, 185 ; of slate
rock in Wales by a river, 211
Weather of 1863 and 1864 in Britain, Canada,
Labrador, and Newfoundland, 258
Weathering of rocks, 13 ; different ways and
rates, 14
Welsh towns, how they would be affected by
a sinking of land, 187 ; hills and their ice-
marks, 202
Western Islands, forms of glaciation and
weathering among, 160
Westmau Islands, volcanic nature of country
about, 396 ; cones of eniption, 433 ; millions
of birds on shelves, 433
Wcstport, big stones at, 46 ; Westport curv'e,
47-53
Wet finger may be dipped into fluid iron or
lead with impunity, 343
Weymouth, waves and systems of waves ob-
served at, 278
Whale skeleton found in Carse of Stirling,
108; bones in drift near Lake Champlaiii,
243
Wharfdale, Yorkshire, peculiar terraces in,
Wheeler (Mr. T. R.), paper in 'Photographic
Journal,' 1S60, referred to, 485
Whinstnne fuseil into a black glass, 325 ; like
lavas, 326
Scodand caused by tides, 89;
ill lluids niid ill air
Wliilefarlane, A nan,
White-hot bar of iroi
servations on, ;!43
White Mountains,
beaches on, 290
1 1 ia' on slate, 68
ilunged into water, ol
L'C-marks, 243 ;
INDEX.
519
Wight (Isle of), tradition about its once Iiaving
been joined to England, 1S8
Will, cause of motion, 274 ; (hunian), what it
can produce, 442
Wind, direction how known, 2 ; near Conway
Castle, prevailing one indicated by the trees,
195 ; motion and progi-ess of, 275
Winds over Himalayas, their influences, 257
iiiiiist Wiinii south-westers, 258
Windows at Giarre broken by concussion of
volcano, :!74
Wishaw, ripple-marked sandstone at, 97
Wistnian's Wood, boulder on hill, 222
Woolwicli, old iron melted at, 36 ; shot and
shell making at, observations on slag, 470
Working models, value of, 275
Worn shelf near a real beach, 292
Wyvis (Ben), a great block of high gi-ouml
topped by a rolling plateau, 133 ; shoulder
of, 149 ; mass of hill, 151 ; shape due to
denudation, 153 ; rock surfaces on, 154 ;
possible sources of its boulders, 157 ; niiia-
schist blocks on, 255
Y Wyddfa, ice-marks on, 202
Yorkshire, hilly tract in, 178 ; dales like Ice-
landic glens, 178, 179 ; drift in, 179 ; dales
not formed by rivers, 180 ; ancient climate
of, 282 ; smelting of lead-ores destroyed
vegetation, 341
ZiRCON-svENiTE, whcrc found, 183
Frhtted hy R. Clark, Edinburgh.
n
7
V
CHAPTER LIX.
CONTAINING OBSERVATIONS MADE SINCE THE PUBLICATION OF
' FROST AND FIRE ;' NOTICES OF LATE EVENTS WHICH BEAR
UPON DENUDATION, DEPOSITION, AND UPHEAVAL ; AND SPECU-
LATIONS WHICH BEAR ON THE BODY OF THE WORK.
Within tliese two years some new facts, which bear on sub-
jects treated in the body of this work, have been learned. If
the reader will turn to page xvi., which explains the plan of
the Table of Contents, he will find references to chapters
which treat of certain grooves upon rocks. These marks seem
to prove that currents loaded with ice once flowed o^^t of the
Arctic basin, along the eastern side of mountains in Scandi-
navia, down the Baltic, over low lands in Russia, Germany,
and Central Europe, past the Alps, and over low lands in
the British Isles, moving generally from north-east to south-
west. This supposed current is named the " Baltic Current,"
and was the equivalent of cold currents which now move on
curves from polar towards equatorial regions. Such currents
move from Spitzbergen along the eastern coasts of Greenland
and North America to the Banks of Newfoundland, and along
the eastern coast of Asia in Behring's Straits. As these cold
currents carry cold climates southwards, so (as it is argued)
did the Baltic Current, till it was turned aside by a rise of
land in Northern Europe. As Greenland now is, so was the
land above water in the Scandinavian peninsula -when ice-
VOL. II. I
504 MARINE OLACIAL PERIODS
bergs sailed over Sweden. As tlie sea-bottom now is off
Labrador and New^foundland, so were the low lands of Britain
and France wlien submerged in the Baltic Current.
The book itself will best show the evidence on which
this theory was founded, liow it was collected and put
together. The main fact relied on is that on high watersheds,
and on isolated hill-tops, up to 3000 feet above the present
sea-level at least, all the way from the west of Ireland to the
north of Xorway, horizontal grooves were found by the
author, which, as a general rule, aim from north-east to
south-M'est, or thereby. In America like marks were found
on high places, which seemed to indicate a former extension
of the curve of the Arctic Current through Canada and the
States ; from the Straits of Bellisle to Niagara and Buffalo
and Fort Wayne, over lands which certainly were submerged
in cold water in late geological times. The maps at the end
of vol. i. and at p. 232 show theoretical curves, and how
far tliey coincide with actual movements in the ocean,
and with marks ^^'hich are taken to indicate like movements
at places now raised far above the sea. It is shown that if
Central Europe were under water, Scandinavia would be in
the same position as Greenland now is with reference to a
cold current, and tliat the Ural Mountains would be on the
warm side of the sea, as Scandinavia now is. Sir Eoderick
Murchison says in his works that Central Europe was in fact
under water, and that no glacial plicnomcna exist near the
Ural Mountains, though they aliound in Central Europe and
in Sweden, and seem to indicate the action of floating and
stranded bergs at sea, and of glaciers on sliore. We know
that such engines are at M'ork on the Mcstern side of tlie
Atlantic, off the eastern coast of Creenland, which is covered
with land-ice. In similar latitudes in Scandinavia the en-
OR POLAR GLACIERS. 505
gine has disappeared, but tool-marks remain ; so facts, and
theory, and authority agree so far.'"'
One difficidty about ice-grooves is the fact that some run
over considerable hills down into rock-basins, and up again,
thus ^ — v^^ .-^■^, and this even in countries far removed from
high hills. A growing school of modern philosophers account
for these marks by supposing glaciers, which reached from
the Poles nearly to the Equator, and covered great part of the
earth with movable crusts of ice during "glacial periods."
They attribute the cold to variations in the ellipse which the
earth describes about the sun, whose rays alone now prevent
the whole sea from freezing. In tliis they are supported by
some astronomers, who calculate the dates of glacial periods,
past and future ; but speculations on the secular cooling of
the sun complicate the question, which turns on the amount
of heat derived from the sun's rays by the earth during a
yearly revolution, at periods past, present, and to come. Be-
cause the big-glacier theory is still new disciples are few ;
but there is nothing unreasonable in it, and it is supported
by some of the most distinguished geologists. It may be
urged in favour of the less advanced theory, which accounts
for ice-marks by existing causes, that in places where hori-
zontal grooves, like vanes on a steeple, ought to show the free
course of the moving body which made the mark, grooves
* See Geology of Eussia in Europe, etc. 1845, p. 556, where Sir Roderick
iliirchison .saj's — " "We still therefore retain our opinions, as expressed in the
text, that the abrasion and striation of the surface were caused by tlieimssage of
iiiasses of drift moved in eccentric directions with reference to the whole area
affected," one cause of movement, as stated in the text, being " waves of trans-
lation. " The cause of the waves sudden upheavals of land in Scandinavia, the
cause of the upheaval siibterranean expansion. The existence of angular blocks
of foreign stone resting upon rounded drift is attributed by Sir Roderick to
icebergs floating from Scandinavia over Gennany and Poland. (See map in the
work (juoteil, and diagrams to illustrate the dejmsitiou of drift by bergs.)
50(j MAKINH GLACIAL PElilODS
generally aim as currents of cold water move in oceans — west-
wanl, and towards the equator 9. The following explanation
for dipping grooves ^-^ ,^ ^ -- — ^ may perhaps suffice. As stated
in the text, large bergs ground in deep water at the north
end of Newfoundland, and there, as they gradually melt, the
current pushes them up a slope along the bottom, towards the
strait. After thus scraping up hill, it may be for a year or
two, bergs scrape through in 40 fathoms, and sail off into the
Gulf of St. Lawrence. It is said that these, and others like
them, can never again touch the bottom in deeper water. They
certainly can not, unless they grow or founder ; but they do
l:)oth. About Newfoundland, and consequently all the way to
.Spitzbergen, overloaded ice sinks, and " anchor-ice " forms at
the bottom, even in deep water, under certain conditions. The
" anchor" is weighed when the load of stones is not too heavy ;
the float rises ; and -when tlie load is too great the float founders.
As water moulds itself into any shape, and is solid when frozen,
anchor-ice binds, and tends to make specifically lighter, and
to lift masses of gravel, sand, boulders, and mud, which lie in
hollows at the bottom ; and ice itself can be squeezed into any
shape from its powers of "regelation." The Arctic Current is
covered every winter by great rafts and floes, in which islands
of ice are entangled ; anchor-ice must form most near the
roots of these bergs ; so ice joins ice, and movable stones grow
together, while water, in moving from the polar basin to the
]>anks of Newfoundland, pushes all that will move over the
fixed bottom. We know that glacier-ice is pushed over and
squeezed into basins in undulating rocks on shore by the
weight of snow behind it ; equal water-power may do as much
for sunken ice frozen to ice-floats. In fact, the direction of
grooves on high places agrees best with the movements of
marine glaciers. Undulating grooves may thus be accounted
OR POLAR GLACIERS. 0U<
for ; so, after two years of study, the author is not prepared to
join the "radicals" and accept their land glaciers. He still
thinks that the present condition of Greenland, and of tlie sea
on the eastern side of Xorth America, and the causes which
now affect climates in and about tlie Atlantic, are sufficient
to account for all the frost-marks which he lias found between
St. Louis on the Mississippi and the Waranger Fjord in
Northern Europe, after many years of careful search.
The idea of climates canied beyond their proper latitudes
by ocean-currents has been approved at the antipodes. A
geologist wrote from New Zealand in 1866 as follows : —
" Wten Robinson Crusoe discovered the footprints in the sand, he
naturally concluded that a man had arrived in his island, and when my
horse shied at a boulder on Belmont Hill, and consequently nearly threw
me over the bank, I perceived the presence of a stranger, and was forced
to think how the boulder got there. The usual carrier of heavy goods
— ice — of coiu-se was first thought of, but the difficulty of supposing a
severe climate in lat. 41, accompanied by a general depression of land,
was so great that I felt disinclined to credit the possibility. A perusal
of the lately-published work entitled Frost and Fire has to my mind
dispersed the fog which hung about the question, and the theoiy of a
polar current V)eing deflected towards the equator appears to show the
possibility of a glacial period even in low latitudes."
The following short paragraph from the Times oi April IG,
1867, and the quotations given, vol. ii. p. 250, show the pre-
sent condition of the Southern Ocean in these latitudes : —
" Icebergs, Hobart Town, February 22. — The ' Harrowby,' from
London, reports that on the 5th of February, in lat. 45 S., long. 127
E., she passed a large number of icebergs, one of them two miles long ;
afterwards sailed through two miles of block-ice drifting N.N.W., the
ice continuing in sight for 24 hoius."
Anxious to test his published conclusions himself, and to
gather new facts on new ground, the author, in the summer
of 1865, travelled round the Scandinavian peninsula, crossing
the isthmus through Eussian Lapland, and crossing Finland
to St. Petersburg (see map, p. 2.32).
508 ritEHISTOltlC MEN
The I'ullowiiig extracts Irom tlie journal were thought
wortliy of the notice of the Ethnological Society, and bear
on the subject of prehistoric European races who ate large
reindeer in the south of France, and made flint weapons to
tight big creatures which are now extinct.
Littvr ti> John CrairfurJ, Esq., rnmlcnt of the Ethnolo;)lca( Societt/, read
Januai-!/ 9th, 1866.
" NiDDRY Lodge, Kensington, W.
" My dear Sir — I send you a few notes from my journal, together
■with the measurements which I took at your rei^uest last autumn.
The oliject of my journey was to examine the watershed of Eutisiau
Lajjjiland for marks of glacial action. My notes contain little infor-
mation on ethnology, because a Lapp is almost as rare and as hard to
find and to catch as a wild deer. I have seen a great many of them
in other parts of Scandinavia, but I confine myself now to the informa-
tion which I gathered for you on my last trip in 1865.
'' Lat. 62° N. — The first Lapp I saw this year was an old Moman
near Laurgaard, in Gulbrandsdal, on the 21st of July. I knew lier to
be a Lapp by lier face, and gave lier the Lapp salutation, ' Bourist,' to
which slie replied at once. She spoke Norwegian, and told me that
slie and her tribe frequent the neighbourhood of Roraas, where they
keep a lieid of deer. She and a man were wandering exactly like
' tinkers' in Scotland, camping l)y the roadside, and working at odd
jobs about the farm-houses. This tribe is the furthest south in Scan-
dina\'ia. I did not measure the old lady, but she was very little, had
very marked features, and a remnant of national costume. These, like
gyjisies, are supposed to be fortune-tellers and conjurors.
" Lat. 68° N. — The next specimen was seen on the 29th of July, and
represents the most western ti-iVie in Scandinavia. He was a Sea Finn in
i'ull dress, and came on board at the southern end of the Lolfotens.
These ishuids answer in position to the Western Isles of Scotland ; so tins
man is equivalent to a Barra Celt. The man was a little higher than
my shoulder, eyes blue, hair light, cheek-bones broad and square, eyes
set witli an upward turn in the corners ; dress, a blue frock with a
br«ad belt fastened round the loins. He speaks Lapp and Norse, and
says he has fished cod for three winters ofi' the islands. His tribe
travel over the mountains to Sweden with a large herd of deer. A
I'jild Finn (mountain Lap])) of his acquaintance once came with his
herd t(, the Lollnlcns, liiit the climate did not suit. There was little
muss, ami much snow in winter, which, ('nuu alternaling danq) and
AND LAPrs. 509
wanatli and frost, freezes so hard that the deer cannot clear it away
witli their feet and horns as they do elsewhere. The Lapp, having
got as far south as he could, moved back and swam his herd over all
the sounds till he got to the narrows, where he crossed to Offoten.
There the winter's snow is dry and dusty, and his beasts could scrape
up a moss-harvest. This range of wandering is equivalent in direction
to a migration from Aberdeen to Barra, and back from Barra to
Aberdeen ; but the distance traversed is far greater. It is about equal
to ten degrees on the meridian. He used no boat, but crossed on
water ' skidor,' which are things like snow-shoes, on which men stand
and paddle themselves over narrow sounds. A considerable numl)er
of families wander about this tract, just within the Arctic Circle, and
close to the largest of the Norwegian glacier districts. I may remark
that a tribe of Indians lately (1864) crossed the Straits of Belleisle,
which are in the latitude of the Straits of Dover and about as wide,
on sea-ice. They landed in Newfoundland to hunt wild reindeer,
which there abound, as they did in prehistoric France. They used no
boats, and some were armed with bows and arrows.
" July 30fh. — Measured a Lapp on board, near Offoten : four feet
eight, dark bluish eyes, small scanty beard, age fifty ; strong, quick,
active ; very dark brown hair, slightly touched with gray ; high cheek-
bones, narrow chin.
" Lat. 69° 30' N., Ju/y 3lst. — At Tromso are many Lapps and a
camp with deer. Did not visit them myself, as I had seen them
more than once. Their portraits are taken by a photographer at
Tromso, which used to be the head-quarters of northenr witches.
An English party who visited the camp took the following heights : —
Man . . 4 ft. lU in.
Do. . . 4 „ 10 „
Woman . . 4 „ 6 „
From this point northwards the population is scanty, and consists of
three distinct races. 1. ' Quains,' who are Finlanders, and farmers
who have migrated northwards, and who still migrate in large numbers.
They cross from Sweden and Eussia in spring to fish in the open sea
off Norway during the winter, and return in autumn to look after
crops. Their yearly migration is equal to about ten degrees of latitude.
In this they resemble the Highlanders of the west of Scotland, who
have fixed haliitations, but nevertheless wander a great deal in search
of employment. The Quains are a tall fair-haired race, very per-
severing, hard to move, but once started very hard to stop. Their
language has a strong relationship to Lapp.
" 2. Norwegians, about whom nothing need be said. They and
their language are very like Scotchmen and Scotch. They wander a
great deal, Imt they use roads, carriages, and steamboats.
510 I'REinSTORIC MEN
" 3. Lapps or Finns, wlio are quick, active, clever, idle, ami avari-
cious, veiy easily moved and turned aside. Tliey will not work even
for a high bribe unless tlie}^ chance to fancy the job ; but, when they
choose, they can and do work hard. They carry heavy back-loads for
others, fish in the sea, in the rivers, and in the lakes, shoot with very
bad rifles, snare birds, row and pole boats, and some even cultivate
grass. The race is no longer pure, but the purest specimens of the
breed are to be found amongst the mountain herdsmen. Along the
coast, Lapps, Finns, Quains, and Norwegians, marry and cross, wear
each other's costumes and speak each other's language ; but, with all
this crossing, the Lapp characteristics are as easily recognised as the
marked features of a Celt are in England.
" Lat. 70° 30' N., Aur/ust 2d. — At Hammerfest saw a great many
Lapps in full costume. All were little, most bandy-legged. The women
were shy and frightened, and ran away from the English party, who
landed from the steamer and walked ten aljreast through the town, followed
by a mixed crowd of Russians, Quains, Lapps, and sailors from all parts.
" Auffust 3t/. — Saw a Lapp camp on Maggero, the most northern
land in Europe. Three smoked tents were pitched close to the sea,
beneath a clitt'. This tribe have deer and boats, and live partly by
fishing. They winter on the main land, and swim their deer over the
sounds. The temperature of the sea was 44°, aii' 46°, and snow lay in
patches close to the water. Tropical beans are conmionly found in
this region, which proves the existence of a warm current, which
makes winter fishing possible, and keeps the sea clear of ice at all
times.
" The steamer runs up a number uf fjords hereabouts, and many
natives came on board. Tliey M'ure the Tana dress : square caps, blue
frocks embroidered with strijies of many colours, tight leggings, and
comagas. These are peaked shoes stutt'ed with hay. They were
generally fair, and tolerably well-grown, being half-breeds between
Quains and Lapps. The water in these fjords was 52° ; air, at H a.m.
13th, 48". Latitude about 71° N.
" A Lapp schoolmaster was on board this day. His father was a
nt)mad, who died at the age of ninety-four. He speaks Lapp, Quain,
and Norsk, and has a smattering of Greek, Latin, German, and French ;
he knows something of geography and * philosophy,' and kept uj) a
hot fire of words with a talking Norwegian who was on board. He
gave as good as he got. Height five feet one, eyes set straight and
Idue, nose aquiline, forehead s(juare and well made, not very high,
cheek-bones broad, chin small. Generally he looked rather like a
<la}>per little Frenchman, and his manner was like that of a mercurial
Gaul. He wan formerly interpreter to the courts, but he never could
lie made to ])ut questions or give answers accuiately. His own chatter
alwavs bniko in, ;uid he was dismissed from that service. This trait
AND LAPPS. 511
Iji'oke out in his couversatious with me. When I asked fur a Lapp
word, he answered with a long, rapid, rambling discourse upon the
value of some letter in the word, and so I let him chatter, and Low,
and grin, and watched him curiously. I was told that he had taken a
vast fancy to me, probably as a good listener. He shook hands
warmly at parting. Lector Friis, Professor of Lapp in the college at
Christiania, was on board. He has more knowledge of Lajips than any
man I ever met, and probably knows more about them than any one now
living. He has a large collection of excellent photographs made this
year (1865), and he has also a large collection of popular tales in Lapjj
vernacular, which it is to be hoped he will pulilish. I mention him,
as the President of the Ethnological Society may wish to cultivate the
acquaintance of a scientific Norwegian gentleman. At Wardd, the town
is built on a low isthmus between low islands of flagstone. The
isthmus is made of coral-sand and shells. The church is built on this
bed, and graves are dug in coral. It is manifest that the whole coast is
rising, and according to numerous records it has risen within historical
times. In digging the foundation of a new house by the road-side, the
men found a deer's horn, a whale's bone, and a honr spoon, about six
feet under the surface, and about thirty above the sea. The upper
ground is made of layers of earth and fish-bones, flesh-bones, and ashes.
The fashion of the day is to build conical huts of turf and sticks, and
to throw the debris of meals and fires on the floor. The hut is only
occupied during part of the year, and it is easily damaged. The fall of
a few huts and the debris of a few hungry generations would soon make
a heap six feet deep, and a street of Lapps would make the " formation"
under which the spoon was found. It was black as ebony from age
and peat, and the fashion of it is the modern fashion. The fort has a
stone with the date 1737. I mention the spoon as a case of modern
kitchen-midden growth with a date marked by the rise of land, and
recorded by written documents and by oral ti-adition.
" Lat. 70° N., August 6th. — Sud Waranger. Lots of Lapps came on
board. Measured some : —
5 ft. li in.
5 » 1 „
5 » 1 „
5 „ 4i „
5 » 4 „
5 „ 4 a mountaineer
4 „ 5| a woman
Hair black, dark brown and waving, fair and curled. Eyes blue, one
man brown. All yellow-skinned. They were strong, square-built,
Itandy-legged, quick and lively, full of fun, curiosity, and chaft'. One
512 I'liEIllSToKIC MEN
of t)ur party Wfiit up ;i iupt' liaiul owv liaiul ; the Lajtps fullowfd suit
iiniawliutely, and did it well.
" Lat. 70° N., August 1th, Pasvik. — Saw the Russian Landsmand
l)ass np the rivei' with three boats manned by ' Skolter Finns.' The men
poled up the rapids with great skill and power, waded and dragged, and
tiually haided boats and baggage over large stones to pass the fall. They
were all little men, but very strongly built. One little fellow was forty-
two inches round the chest, and made like a pocket Hercules. This tribe
is generally fair, with light-blue eyes. The Russian official i)aid nothing,
but ordered whom he would to work for government ; I could get no-
body to work for me, though I offered douljle pay.
'" Lat. 69° 30' N., August Wth. — On the shore of Enare lake, fell in
with a tribe of pure Lapps. The man had hardly any beard, his hair
was long, black, straight, and shiny, his eyes dark-ljrown, his face very
marked, pointed cheek-boues, angular eyes, and small chin ; his figure
slender, spare, stringy rather than muscular. The women were like
him, but fatter and very ugly. They were well and neatly dressed in
their costume. They had deer in the neighbourhood and boats on the
lake-shore. They sold dried fish to a party of Quains, who were travel-
ling back to the Baltic side. The Quains were big, burly, noisy, hardy,
tair men ; the Lapps quiet and grave. The women kept quietly working
at comagas, while the men sauntered about amongst the travellers, and
we left them busily working and idling. Their only shelter was a sail.
Along the banks of this lake are numerous Lapp camps and a few
fixed liouses ; at the southern end are farms A\here corn is grown. These
are probably the most northern of all corn-fields, about 69° N.
" From these settlements we crossed the watershed with a lot of
porters and a reindeer with a pack-saddle. On the hill a herd of deer
came about us, and two were caught and harnessed. They were tamer
than horses turned out to graze on a Highland moor, and they worked
as patiently as any ordinary beast of bunlen. We saw no more Lapps
on the coiu'se of the Kemi river, which we followed to the sea. The
Quaius make their travelling diet of rye-bread and butter, and sleej) on
the ground.
" The climate in which Lapps llourish is that which suits deer and
grows deer-iKisturc. In this unusually fine sunmier the frosts Ijegan in
Kemi Lappmark as soon as the sun began to set. Water was frozen
in our kettle at the south end of the Enare lake, about lat. 69° N., on
the 1 2th of August, and thenceforth it froze every night till we got to
the Gulf of Bothnia, lat. 66° (August 27th). In the day the heat was
intense. Close to the sea, a day's march from the Waranger Fjord,
tliermometer was 82° in the shade. On the 8th of August it was 80°
du the grass at the sea-side; on the 9th, 78°.
" Lat. 70° N. — The vegetation on the high ground between Enare
and the Baltic, at about 1200 to 1400 feet, is gray mr.ss, three inche.-
AND LAPPS. 513
lung at least ; walking on it is like treading on brittle snow. Below
this region is a zone of birch aud scattered pines, and these, lower
down, form vast forests with marshy groimd. Travelling in summer is
on foot and by water on the rivers ; in winter with deer over every-
thing in polks. It is said that the Russian govenunent are about to
make a road to Enare* About 1000 Quains crossed and recrossed to
and from the North Sea to fish this year, di'agged by deer driven by
Lapps. If the traffic is so great now the road will be used.
" After travelling tlirough Finland, it seems to me that the Lapps
are a very diflVrent race, or that the Finns or Quains or Karelsk have
been crossed 'with Scandinavians, Gennans, or Russians. Anyhow, the
Lapps are a marked race amongst Europeans — so marked that a good
specimen could hardly escape notice anywhere.
" It is somewhat remarkable that traditions still survive in the
Highlands of Scotland which seem to be derived from the habits of
Scotch tribes like Lapps in our day. Stories are told in Sutherland
about a 'witch' who milked deer : — A 'ghost' once became acquainted
with a forester, and at his suggestion packed all her plenishing on a herd
of deer, when forced to flit by another and a bigger ' ghost.' The
green moimds in which 'fairies' are supposed to dwell closely resemljle
the outside of Lapp huts. The fairies themselves are not represented
as airy creatiu-es in gauze wings and sjjangles ; but they appear in all
Celtic traditions as small cunning peojile, eating and drinking, living
close at hand in their green mounds, stealing children and cattle, milk
and food, from their bigger neighbours. They are vmcanny, but so are
Lapps. My own opinion is that these Scotch traditions relate to the
tribes who made kitchen-middens and lake-dwellings in Scotland, and
that they were allied to Lapps." t
These extracts may serve for Scandinavian ethnology.
The main object of the journey was to look out for ice-marks
at certain points, and this is the result.
It is hard to condense daily observations extending over
two months and many hundreds of miles, and to give the
results without drawings ; but by the help of old woodcuts
and the map, x)- 32, something may be explained. The first
" Enare triisk, or lake, is one of the largest in Europe. It is very incor-
rectly drawn on maps. It is full of large islands, and al)Out a hundred rniles
long.
t See vol. i. p. 312, for further information as to the habits of the Lapps
who wander from sea to sea about the Arctic Circle in Scandinavia.
514 MARINE TERRACES
point made was Cliristiausand. From a hill above that town,
and from the sea near it, the long gradual glaciated slope of
Southern Norway is well seen. The whole land was ground
by ice ; the question remains what share sea-ice had in shap-
ing these rocks and hills. Every hollow is filled with terraced
plains of rolled drift. In one of these, now 40 feet above the
sea, under the turf of a hay-field, is a layer of sea-shells mixed
with bones and iron nails, and other marks of human art.
The shells are not of an edible kind, and they are old and
worn. This terrace seems to mark a very late rise of land ;
but part of the town is on it, so it is older than the town. In
the Christiania Fjord glaciation is conspicuous, but so are drift-
terraces and other marine phenomena. All up the line of the
new railroad which runs to the Mjosen lake, up to a height of
900 feet and down to 720, all rocks are glaciated, and all the
soil is drift. Along the IMjosen lake terraces are conspicuous
to a great height. At Lillehammer the lake ends, and the
great groove of Gulbrandsdal begins. It is not a fa^dt, it is a
rock-groove dug out of a rolling southward slope, which was
carved out of bedded rocks, which dip northwards. Tlie
bottom of the groove ^^^^ is full of water-worn stuff ; the sides
are scored by ice where the rock is visible ; and high up on
both hill-sides, at corresponding levels, are horizontal terraces
of drift which rest on the glaciated rock. As these terraces
are higher than hills at the foot of the lake, they must be of
marine origin. The highest point reached on the railway was
900 feet above the sea ; the lake is 720. At 990 above the
sea, at Lillehammer, is a well-marked terrace, chiefly made
of enormous glaciated stones, smooth and striated ; many are
about three or four feet long. There is nothing like a lateral
moraine, and no medial moraine is in the bottom of the glen ;
the whole seems to be glacier-stuff rearranged in water. Above
AND HIGH ICE-MARKS. 515
tlie terraces, and on the brow of the hill, at 1000 feet above
the lake and 1720 above the sea, are horizontal ice-grooves.
These aim seawards. At 1900 feet above the sea the whole
country to the south is overlooked, and there horizontal
grooves aim nearly south by compass. This looks like a
sheet of ice filling the whole glen over the brim, and passing
over the whole land ; over this spot, and far beyond the mouth
of the Christiania Fjord ; but these terraces surely indicate the
presence of water after this ice-sheet had melted. So far the
facts confirm theory. "While the land was deep in a cold
stream it was covered by sheets of ice, which plunged down far
under water, as glaciers do in Greenland ; when the land rose,
the cold stream was turned aside, the ice melted, and as the
land continued to rise, the sea sorted and terraced the drift
which the ice dropped. Here the traveller narrowly escaped
tlie fate of Diarmaid, the mythical ancestor of his clan.
" While busily rubbing a sheet of paper to copy an ice-groove, a
very active healthy jiig came to see what was going on, and stuck his
snout against my arm. Gave him a sound cufF on the side of the
head, and thereby roused his ire. He opened his mouth, well armed
with glancing tusks, and looked vicious, so got up off my knees, and
kicked him. The outraged pig squealed, and charged, open-mouthed,
with all his bristles on end. Seized hold of a rail-fence for a spring,
and kicked out backwards at his head as hard as ever I could. By
good luck, the hobnails took him about the eye, and routed him. He
grunted, yelled, turned tail, and fled, leaving me to finish my rubbing,
and gather up my old friends and comrades the compass and clmo-
meter."
In travelling up Gulbrandsdal, aneroid barometer in hand,
it appeared that gTeat flats of drift in the bottom nearly cor-
respond to terraces at the mouth of the valley, and no trace
of a medial moraine was found anywhere. It seemed also
that work done by the great river Lougen is insignificant.
At one spot near Lourgaard is a river-gorge, cut in the rock,
with water-marks in it ; but it is a mere ditch u at the bottom
51 () MARINE TERRACES
of the Itig rock-groove v •, and was probably made after tlio
terraced land rose from the sea. At Toftemoen the country of
sand terraces begins. The glen is still a rock-groove, but on
both sides of it are terraces of very fine sand, up to a height
of 2000 feet. Even the Norwegian landlord said it looked as
if the sea had been there. At Dombaas the road leaves the
valley near the water-parting of two great rivers, and passes
the highest sand terrace. In a road-cutting somewhat lower
down the men had found no shells, and nothing remarkable, ex-
cept a horizontal layer of hardened ripple-marked stone, about
an inch thick, of which great slabs were taken out of the
sand. Under the sand are beds of clay, and of snljangular
gravel, and amongst these beds are large striated boulders.
The bare rock, which dips under this drift terrace, is striated
horizontally, and the whole is far above the water-parting of
the largest glens in Norway. All this seems to prove a rise
of land equal to 2000 feet since the rock was grooved by ice
and the terrace was packed by the sea (chap, xviii.)
As shown in the text, a great many large rivers part from
the Dovrefjeld. One point to be ascertained w^as the direction
of ice-grooves on this main watershed of Norway. Fokstuen
is between 2900 and 3000 feet above the sea on the watershed
of Norway. It is in a large cup-shaped hollow about ten
miles wide every way. It is a " high groove" crossing the dip
of the rock from N.E. to S.W. ; and stria3 in it aim in the
same direction. If the sea were at this level it might flow
without obstruction along the "Galway Curve" (see map, p. 232).
Above Fokstuen, on hills to the eastward, the ground is covered
with fragments of native rock, flat stones about a foot long,
and shorter ones of like pattern, all neatly packed, like slates
on a roof, by the snow. On a hill-top, 4610 feet above the
sea, the view on July 22d was highly characteristic of Norway.
AND HKHI ICE-MARKS. 517
" To the north, about twenty miles away beyond the groove, is the
broken ridge of Sneehsettan, with one deep gorge crossing it. Great
snow-wreaths seem to flow down the sides into the gorge, which must
surely have held a glacier at some time. To the east is a wide roll-
ing sea of brown hills and dales, with yellow sun-gleams and blue
shadows chasing each other northwards. In that direction scarce a
speck of snow remains, for the sun-gleams have chased the snow from
the fjeld. To the west is Eomsdal, a deep blue gorge in a great
spotted mountain-tract of snow-wreaths and rocks, glazed over with a
blue haze of damp sea-air. Southwards is the same rolling plateau, with
the steep A A A A cones of the Rundene and the Gausta Fjeld
on the horizon, and a deep glen crossing through the fjeld from Gul-
brandsdal to Roraas. Below the level of 4600 feet the whole country
is rounded and moulded, and grooved and glaciated. Above it the
mountains are cones and peaks, like the islands off the coast."
So far nothing new was found, but tlie eye had taken in
a great tract of country, and tlie shape of it appeared to he
due to glacial denudation as in Scotland. Taking the hill-side
homewards, at 4430 feet above the sea, and 1530 above the
bottom of the groove at Fokstuen, a square block of white
granite was found near a large smooth block of white quartz,
and a cluster of smaller white stones, all utterly unlike any-
thing to be seen higher up in situ, but like rocks in the valley
lielow. The nearest hill at this level from which granite might
come nnist be fourteen miles off at least. On the opposite hill-
side in this glen, at the same level, are three perfectly horizontal
shelves, which can be traced for several miles. They are
higher than the watershed of the glen, and they are remark-
ably like marine terraces at Quainclubbe (p. 357). Adding
terrace to foreign stone, this seems to mark a water-level of
4400 feet above the present sea coast, but further search must
be made before this can be taken as proved.
No glaciated surface was found in a walk of thirteen miles
up and down Fokoan. The gi'oove, through which the road passes
to Hjterdkin, is all glaciated and strewn with great boulders ;
and as this is at the source of many large rivers, it is not easy
.518
MARINE TERRACES
to account for tlie marks without assuming- that tlu; liollcnv
was a strait during a glacial period.
At Hj\Trdkin ice-marks confirm this view. A section
across the valley may be expressedby A^_^A^^A, three cones
to represent three ridges. The central ridge is not more than
ten yards wide at the top, and at places not more than two or
DIAGRAM TO SHOW THE KELATIVE AI.TITrDES OF PLArES MENTIONED A
three. The sides are very steep, and it rises about 550 feet
above the rivers which flow on each side of it. A great many
large stones are perclied on the top of this pent-house, and it
suggested an island seen on the coast of Labrador in the pre-
vious year. Stria^ as well marked as on the cover of this book
cross this ridge at right angles, and on the opposite side of the
glen above the station, beside tlie road, similar marks aim the
same way, north-east and south-west, at 3390 feet above the
sea, right over the backbone of Norway. The curve wliich
was taken up at Galway and carried over the backbone of
Scotland lies in a great rock-groove on the ridge of Norway —
fresh as if it had been made last week. The groove is seen
passing over deep glens towards tlie Hebrides. The strangest
thing is, that in these hollows where local ghicier-marks ought
AND HIGH ICE-GROOVES. -^19
to Ije, along the sides of these ridges, and elsewhere, no such
marks were to be seen on Dovre (see chap, xviii.)
So far new facts confirm the published theory ; and these
high grooves appear to have been made by floating ice touching
on reefs and points at a time when the land was about 4500
feet lower, or the sea was as much higher. Terraces of erosion,
wandering blocks, and horizontal striie, taken together, make a
strong case.
The next point to be made was the watershed of Russian
Lapland, between the Gulf of Bothnia and the polar basin.
From Dovre to Trondhjem the marks are of one kind :
rocks are rounded, drift is terraced and packed in plains. In
a glen the face of the lowest terrace is marked by many small
V watercourses with a A delta below each. The next in the
series has fewer but larger gaps in it. The highest rampart
is breached by large rounded embrasures ^^ — ■, each with a
small V notch at the bottom, where a streamlet is at work.
Above all is the bare rounded rock ^ — s ; below is the plain
of debris, in which the main stream is at work. The mouth
of a glen is often like an amphitheatre with seats and arena.
From Trondhjem to the North Cape, on board the steamer,
the shape of drift-banks packed in a warm sea can be studied
with certainty. All who navigate the coast believe that the
land is now rising. At Wardo, people lately dead remem-
Ijered that the sea, in heavy weather, passed over an isthmus
on which houses are now built. A little way up the fjord
vessels lately passed between an island and the mainland,
where the land is now dry. The island has become a penin-
sula within the historical period. It is recorded in old Norse
books that large yachts sailed by Hopseidet, which is now a
grass-grown low sandy isthmus about a mile wide. The
Lapps call it a " Sound " to this day. Old authors are quoted
520 MARINE TERRACES
to prove that Scandinavia was an island as late as 1450. Tu
many places beds of recent shells, buried in the nnid in which
they lived, whale-bones, and suchlike dead witnesses, who
cannot be mistaken, prove beyond dispute that the lowest
terraces are marine, and recent. An eye thus made familiar
with these forms cannot well mistake them elsewhere.
The difference between broken rocks and rocks ground or
washed into shape is equally manifest on this wild and very
beautiful coast.
About nndnight on the 31st of July we passed the glaciers
in Lyng's Fjord. Of these, four are well seen. One looked
like a great wide flood of white foam and broken blue water,
surging from side to side down from the hill-top, through a
rock-glen, and finally bursting out to stop as a crystal torrent
of clear blue hard shining ice. The form is the form of swift
movement, but the glacier has hung as if ready to plunge into
the sea, apparently unaltered, for more than twenty years. It
is one of the most beautiful of European glaciers, and comes
close to the sea-level. It is not easy to describe this place
without a woodcut. Below the blue ice is the bottom of the
rock-groove n_--' strewn with stones shed from the glacier
M'hich has retired, and lower down in the same groove is a
steep stair of short terraces, with one long terrace just above
the sea, stretching along the coast on l)oth sides. The water
is deep steep to, and the coast is rock. Another very-
large glacier hangs higher up over the edge of a gi-eat corrie,
and pours rivers into it. The rivers gather and escape over
u stair of flat drift-terraces. It is plain that the drift is the
terminal moraine of a large glacier which has retired, packed
under water, and terraced by the waves of the sea while
the land was rising. The glacier-river has done very little
work since the first terrace rose. Taking all this together.
AND ICE-MARKS. •'521
it seems plain that many of the Alten teiiaces are well-pre-
served marine moraines of melted glaciers sorted by waves and
raised. The diagram, p. 334, is a fair representation of some
of the shapes which abound along this coasting voyage of 540
miles, where the origin of the shape is made perfectly plain.
Eound the North Cape, and to Pasvik in Snd Waranger,
all this becomes clearer. Vegetation is scanty, and the bones
of the country are bare. At Kjolefjord, about lat. 71°, the first
terrace is made of clean shingle, about 30 feet above high-water
mark. On the second a few lichens grow on the stones. A
third, at 140 feet, is grass-grown. It consists of semiangular
rolled stones of larger size, with large angular blocks. At this
level the mouth of the fjord was far wider, and waves had
more power. A fourth terrace is at 170 feet, and covered with
vegetation. Tlie edges of these steps are far apart, and joined
by long slopes, which are marked at intervals of 15 feet or
less by small terraces exactly like similar marks in the south
of England, which are commonly attributed to human art.
Here cultivation is impossible. All these raised beaches are
semibmar, with the convex side towards the hill — ) *.
About the Tana Fjord work done by weathering and rain
on a large scale is very well seen. A Norwegian said, " Is not
that a remarkable dale ? it is just like the half of a kettle ; "
a Highlander would call it "a corrie ;" and the rocks and
stones are so bare of soil that the structure of the hill itself is
as plainly seen as the dale and the branching rivulets that
are gnawing into bedded rock.
At Elvebacken, where Magnus Clerk, an old friend of
many years' standing, now resides, are good samples of work
done by fjord-ice. In the winter of 1864 the ice clasped a
stone which measures 14 feet by 11 in cross girths ; the tide
rose, and the stone was dragged out of a sandy beach, Avhei^o
•■i22 MARINE TERRACES
it left a large hole. It was lifted move than 2 feet, carried
more than 5 yards, and planted on a pile of smaller stones,
where it rests, a marine " roche perclie." The Lapps declare
that they have often watched this process. The sides of the
fjord and rocks in it are strewed with similar stones arranged
by ice ; and at all levels, np to the highest tops, blocks are
perched on rock-saddles, as they are in places mentioned in
the text — e.g. at 4430 feet on Dovre, in Connemara, Lab-
rador, the White Monntains, and at New York.
The effect of warm and cold currents is illustrated by
the effect of the Pasvik river on its banks. On the 8th of
August the water was 58° Fahr. ; it was 50° in a neighbouring
fjord. The river flows northwards out of a large shallow
lake, more than 100 miles long, at the south end of which
corn grows. Along the coast, and on the banks of small rivers
in this region, the hills are bare, but near this warm river
tir-trees flourish, and all manner of flowers grow in a sunny
garden. In M'inter the thermometer goes to minus 60°.
Low rocks which are in the run of the tide and the river
are so polished up hill and down ^-v that it is hard to stand
on their rounded backs. Eubbings were taken from them,
which caimot be distinguished from modern glacier-work in
Switzerland. The shape of the rocks, grooves of all sorts
and sizes, and stones perched on them, are precisely the marks
which are attributed to the big glacier by Agassiz and by his
school, and which are attributed to local glaciers and sea-ice
in the text. Here, in the far north, the marks are marine ;
they rise high where terraces mark old sea-levels, and the
higher and older they are the fainter they get. This tells
against the liig glacier so I'ar.
In Neidan Fjord the terraces are Acry large and numerous,
and reach to 300 feet at least. At points, terraces of erosion
AND ICE-WOKK.
523
correspond in level to terraces of deposition in bays and
hollows.
The rounded rocky hills are traversed by many faults, and
" slips and heaves " seem to have taken place after the rock
was ground into shape, for the outline of the curve is not
continuous, but broken at the fault. As the whole peninsula
has certainly risen, and unequally, this result might be looked
for. Here it is seen because of the nakedness of the land.
From sea to sea the marks found were like those studied
on the coast. At 255 feet is the top of a terrace of sand and
rolled stones. The edge of this step is the beginning of a
wide plain, studded with small stunted birches, and over-
grown with gray moss. More steps lead to 300 feet, where
the rock is bare and is rounded weathered gneiss abounding
in rock-basins which hold small lakes. ISIore plains of
sand and shingle, with rocks cropping out ; more terraces
on hill-sides extend all the way to the big lake, which is
about 360 feet above the sea. The highest point on the
journey is 450 feet. So called " kames and osar," mounds of
shingle, like railway embankments, vary these drift-plains.
The only fresh marks of glaciation seen were at the upper
end of the lake, where the river enters, and that was the
winter work of river-ice.
In lat. 69°, at the south end of the lake, at 800 feet above
the sea, Scotch firs were found, measuring 4 feet 5 inches and 5
feet 6 inches three feet from the ground. Good rye was grow-
ing, and good potatoes, about good farm-houses. The people
are well dressed ; own sheep, cows, horses, and reindeer ;
make butter and cheese ; bake and read. They have books
and maps, and silver goblets ; and seem to be healthy, well-
fed, cheery, good-natured mortals. The coast of Greenland,
in the same latitude, is inaccessible from drift-ice.
^2i marinp: terraces
From the lake to the watershed (15 miles) the way lii\s
through forest, which grows thinner and thinner as the path
rises. At 850 feet above the sea are " Eskar," mounds of
waterworn but weathered and rough stones, and sandy-
banks. Very few rocks were visible, and these were all
rough and weathered. No perched blocks were seen. About
this level is a well-marked raised beach of rolled stones,
packed in a half-moon curve, across the mouth of a shallow
dale. The convex side is towards the hill. The stones were
much weathered and overgrown with lichens, but in other
respects this mound is the counterpart of a raised beach at
Vadso, and of the beaches at Kjijlefjord. The watershed is
1400 feet above the sea ; and not one scrap of grooved rock
was to be found on it. The hills are all rounded mamelons ;
and all rock-surfaces found were crumbling to sand. Not
even a wandering block was to be seen. So the direction in
which ice moved over the watershed of Eussian Lapland
remains undecided.
The following extracts show what a traveller's life is in
these northern regions, while gathering geological and other
facts. It is not a life of ease, but it is very pleasant in fine
weather.
" After landing from the steamer at Sud Waranger, and boating to
the i)hice where we had to begin our walk, at 7.15 p.m. we started.
One girl with her brother, two Lapp lads and a small boy, and (jiie
Qiiain from Kemi, who is servant here in summer ; these and the
Wapus (guide) made up our baggage-train. . . . Having gone one
English mile, halted and brewed coffee. For the rest of the night took
sliort walks and long halts, to drink coffee and smoke, and sing and
wrestle. Ours was a jolly, cheery, laughing, good-humoured train, and
Ihey walked away cheerily with heavy loads. . . .
" About 2 A.M. we got to a small burn, after walking twelve
English miles, and here the Wapus called a halt for a sleep. Having
carried my pack, and gun and shot, witli ]iocketa crammed with odds
ami ends, \ was wry tirrd, bciii^ fairly used up for want of sU^'p and
AND DRIFT. 52;")
solid food. The mosquitoes were in clouds all the way : the buzzing
was like that of "a swarm of bees, and hands and face were drilled full
of holes. My clothes were wet through with perspiration, and though
I had slept by snatches at tlie halts, the rocks were cold, and I got
little rest for two nights. When the fire was lit for the last time, I
tlirew a mackintosh over my head, took my pack for a pillow, lay
down in the smoke, and slept at once. Awoke rather cold about 4 a.m.
toasted my back at the fire, dried my shirt, got a rug out of one of the
imcks, and slept again. At 8, awoke with a start, and found a very hot
sun beating on my head. Eose, cooked the breakfast, went to the burn,
stripped, and lay down in it ; dressed, and then lay under a bush, with
a cloak on top for shade, till it was time to move again.
" What a gallery of pictures that night-march furnished : — The
glorious red sunset about 10, Avith the wild, silent, northern landscape
stretching out to the horizon ; then the gray twilight of midnight, with
the red glare of fires glowing on our wild train ; the good-humoured
Quain girl playing with her black foxy dog ; the Skolter Finn, with his
broad face, and shiny teeth, and fair curly hair ; the blue Lapp pesk of
the other Finn, beside my red box and the brown tent-bag, birch-trees,
and gray rocks all flickering in the firelight. It was a night to remember.
" A i/ff. 11,2 A.M. — Halted for a sleep beside a lake. Lay down on the
ground, with a thin mackintosh under me, wet-footed as I was, and
streaming with sweat. Slept like a top, after a brew of hot coffee. At
5 A.M. awoke, and found a ring of sleepers round the fire. First, my
friend H. ; then a pair of blue legs peeping out of a brown sack ; then
a pair of brown legs and a brown sack ; then a blue petticoat and
a brown one, with a girl's head and figure inside of them, mixed
up somehow with the yellow boots of a boy, her pillow ; then a Lapp,
inside of a pesk, with nothing to be seen of him but a lock of hair ;
then a big stone for his pillow, and the embers of the fire expiring
in the midst of the ring. Poked it up, warmed myself, and lay down
again iii the rain. Rather cool night's quarters these. At 8, turned
out and cooked a young hare, which Fidi, the dog, caught over night.
Then came a whole string of travellers bound inland from the fishing.
Quains in boots, Lapps in pesks, sailors in good stout blue clotli,
with watches and chains ; in short, a caravan on the march, travelling
like ourselves. Air 48° in the morning. After crossing the big Enare
lake in a boat, camped for a day. In the morning peeped intf) the
living-room (of a large comfortable farm-house, built of logs), and found
the floor thickly covered with men. They had no beds, and slept on
deerskins laid on the boards. Many had nothing on but shirts. Air,
outside our tent, 47° ; inside the house, 68° ; but it froze hard in the
night, for the kettle was half-full of ice when we rose. .
'^A/i;/. 14. — At 5.20 P.M. fifteen miles, 1400 feet aliove the sea, topped
the ridge. The view lium this place is indescribalde. East, south, and
526 MAKINE TEHRACliS
wes^t, one vast rolling i)lak';ui stretched out to the horizon, with scarce
a feature in the ^^icture to fix it in the mind, save vastness and sameness.
Gray moss on the near hills laded into blue ; green birches, in near
hollows, faded into pearly gray ; a bright blue sky was overhead, and
a fierce sun beat down on our panting train. Far ahead iu the distance,
a few hills, less consj^icuous than Primrose Hill, were named as land-
marks ; and to the left rose a round-backed knob of a hill, some 500
feet higher than the pass. It was thickly carpeted A\'ith fine long moss,
and shone with a strange silver-gray light in the brilliant sunshine.
Such is Eussian Lapland in summer : not a speck of snow to be seen,
scarce a living creature to be found, not a sound in the air but the
melancholy pix)e of a distant plover, the droning hum of the cloud of
flies, and the breathing of their prey. There we lay, Englishmen, Lapps,
and Quains, and our patient old stag lay with us, panting and rumbling
with his back-load on the ground, and a blanket of flies on his brown
hide. . . At 8 p.m. halted, after walking twenty miles ; stripped and
bathed in a burn, Avhile the men made a fire. Cooked stew, and brewed
coffee for all hands, after my bath ; and while so engaged, spied a stray
deer come wandering up to our horned steed. One of the men caught
him in a trice, and tethered him to a bush. This arrival of a
tame deer from the wild hill stopped all thoughts of deer-stalking.
As the sun went down, the round hills about us glowed with a strange
greenish-gray warm light, unlike the colour of any other hills that I
have seen. The warm sky, and tlie tall trees about our camp, with
men and deer, made a grand picture. The night was so fine and warm
and bright that we lay on the ground in our wrai)s, and did not pitcli
the tent.
" Aiif/. 15. — Awoke at 5, and found the sun shining on a world glit-
tering with hoar-frost, which covered my plaid. The beams came slanting
down our forest-glade, casting long blue shadows on the yellow frosted
moss, and a large herd of dark reindeer, edged with silver and light,
tossed their antlers and browsed on moss, stood and lay in groui).s
amongst the firs and birches close to our bivouac. In the foreground,
round about the smoking fire, lay the men, and the boy rolled up in a
white deerskin pesk. One old fellow, with his pipe in his cheek, sat
blinking at tlie fire, nnninating, and the rest lay rolling and snoring,
witli sunlight and firelight flickering on their veiled figures. Never
was a wild bivouac more beautiful."
On the south side, at about 1200 feet above the sea, is
anotlior lialf-moon battery of rolled stones, with the convex
side aiming at the hill. These two piles of drift seem to prove
that llic watci-shcd was u]) to the shoulders iu the sea, thus :
AND DKIFT. 527
S. beacli, 1200 ) ridge, 1400 ( K beach, 850.
The rock of the country where it appears about this water-
shed is rounded weathered gi-anite. Tlience to the Gulf of
Bothnia the whole land is covered by great flat sheets of
terraced drift. Small rivers flow in sand, and have scarcely
dug a shallow trench ; as they grow larger, the river-bed is
made first of washed gravel, then of larger stones, at last of
big stones, with an occasional straggler as big as a house. At
very distant points the rock has been washed bare. The
rivers, though they are the biggest in the north, and though
they are armed with strong ice-levers worked by vast snow-
floods, have done little work since they began to flow through
this country of marine deposition.
At the head of Kemi lake the ground is full of great stones :
gneiss of various sorts, granites, mica-schists, altered grits,
white felspar, porphpy in large compact blocks, a slaty hard
blue stone, etc. They are chiefly subangular in form, smooth,
but not striated as a rule, though some are. In the distance
to the east are several low, conical hills, arranged in rows, but
no rock was to be seen. The delta formed by the river in
the lake is mud. The river is not strong enough to move
one of the big porph}Ty blocks, but somehow they seem to
have drifted to Elfdal in Sweden at least (vol. i. p. 244).
The Kemi rapids are the biggest in the north of Europe.
They seem to occur at terraces. What a river can do this
river does ; and as the water was very low in August 1865
the work was seen. Stones about the size of turnips are
packed on long projecting bars, which stand at the river-bank
as the teeth of a comb stand to the back. They are like mag-
nified ripple-marks, eight or ten feet high. The oval stones
are all packed one on the other, like scales on a fish.
The banks are high, and when the top is reached it is
528 MARINE TERRACES
found to be the edge of a great plain of drift. In broken
banks the structure of the drift is seen, and it is stratified
sand, with beds of clay and big stones. At the last rapid, the
biggest in all the north, the water was so low that the rock
was attainable. It was slaty and polished, as by a land-
glacier. Eubbings made there and at the Thousand Isles in
Canada the year before cannot be distinguished. *
So far there is much to confirm the notion of a Baltic Cur-
rent when Lapland was submerged, but no high ice-grooves.
Capital roads cross from Tornea to Wiborg in Finland.
Of that country excellent maps exist — and one gives the alti-
tudes in colours. According to this map, the highest laud is
about the sources of the Alten, Tornea, and Kemi rivers, and
is 1400 feet, with higher points about 2000 feet high. About
long. 47° E. the land is about. 800 and 900 feet. The
colours which indicate 700 to 900 follow the outline of the
coast at varying distances. With the sea at 1400 feet Norway
would end at Kautokeino, and a row of islands would extend
eastwards past the place where the half-moon beaches were
found. With the sea at 900 feet Scandinavia would be a
long island, with a hook to the north of the Gulf of Bothnia
reaching down to lat. 64°, and open sea to the east. At each
lower sea-level the hook would grow southwards, and the
isthmus would only close about the White Sea, when the
land was near the present level. Witliout the map the shape
of the country could not be made out Ijy a traveller ; without
seeing the country the map could give no idea of the extreme
sameness and flatness of the wide tracts of marine drift which
extend from Enare to Petersburg. It is not easy to express
it in words. After driving iVom Kemi to Tornea, and tlience
Kora.jdiinialorau cxprditioii iiiadiMii 18(34, sl'c A Short Amcviaai Tramp,
l.y tlu- same ;tntlior an.l |iul.lisl,rr.
AND DRIFT. 529
to Kviopio overland, after steaming through lakes and canals
to Wihorg, and thence to Petersburg, it seemed proved by marks
that great sheets of ice travelled from Kautokeino and these
regions south-eastwards to Wiborg, scoring and grinding rock ;
that after the land was thus ground the debris was packed by
water, and then raised bodily, and terraced as it rose.
The Baltic Current may or may not have passed over Lap-
land at 1400 feet ; no marks were there to show its direction.
But in Finland, at lower levels, ice moved 7iot from north-east
to south-west, but from north-icest to south-cast.
Kuopio is a town in the middle of Finland, and one
picture from it must suffice for description. Near the town
is Puyio Bakke, a hill renowned for the view, the top of which
is said to be 1400 feet above the sea-level. It is 500 feet
above the Great Suamen lake. Half-way up are stratiiied
beds of sand, coarse and fine, with gravel and clay, and large
and small angular stones — all resting upon glaciated rock.
All the way up foreign stones abound — slates, quartz, red
granite, horsetooth granite, blue stone with white veins, mi-
caceous stones, granite enclosing blocks of altered sandstone,
contorted gneiss, rolled stones and glaciated. These prove
that land or sea ice passed here at a high level.
" On the top of this northern Rhigi an enterprising native ha.s
built a small inn, and a tall wooden edifice to get clear of the trees.
The view from this Gazebo is the strangest I have ever seen. No hill
of greater height is visible in any direction ; only one of equal height
to the eastward. It is a long round-backed naked promontory, with a
notch at the end like a terrace of erosion. It is the same which the
evening sun made to glow like red-hot iron last night. Within the
ring of a wide horizon was one great maze of crisp blue water and dark
green pine-forest, with rare specks of yellow corn and light-green grass
in clearings. Land and lake faded away to a hazy blue distance, cut-
ting against a light-gray sky, with a dark-blue vault overhead. The
town at the hill-foot, a mile aw^uy, looked like a wooden toy, with
M'hite, and red, and gray Mooden loofs, glancing in the bright noonday
530 MARINE TERRACES,
sun. With a powerful glass the distance became like the niitklle dis-
tance, and the middle distance like the foregi-ound ; but nothing was
to be made of that strange maze of lake and forest, island and bay,
drift and rock. It is all the same all the way to the North Sea in one
dii-eetion, and to the Ural Mountains in the other, for ought I know ;
and I believe it to be an ancient sea-bottom, raised long enough for
trees and moss to grow on it, and form a few peat-bogs here and
there."
From tins great maze of lakes a canal was cut to the sea
in 1845. The further south one gets, the more conspicuous
are the ice-marks. The whole rock-country about the lakes
appears to be one great rocJie moutonn^e, with soil enough
upon it to nourish moss and trees. Directly the shore is left
the drift-country begins again. The canal is cut through the
edge of a rock-basin. At all places where drift has been
moved and the rock laid bare all the way to the sea, the sur-
faces are perfect samples of glaciation, smooth as the rocks at
Elvebacken. The rock is a very peculiar granite, much used
in St. Petersburg for building churches, and boulders of it
were seen a few days later built into the walls of Konig.sberg,
beyond the Gulf of Finland. This polished rock is worn into
hills and hollows, and buried under flat sheets of terraced
drift, through which the canal descends. The following are
the bearings of rubbings taken along this slope, and they
correspond in direction with many rubbings taken between
Toruea and Wiborg : —
N. 22 W.
N. 33 W
N. 28 W.
N. 33 W.
N. 35 W.
hy conqxiss.
These do not support the Baltic Current. They do not tell
M'ell for the })olar glacier, because they are much fresher
than uiiuks found in tlie north. They are impartial witnesses.
STRLE, AND DRIFT. 531
and so they must be left to tell their own story to those who
care to translate their meaning. For the manners and customs
of the natives of Finland, this extract must suffice : —
" Lat. 66° N., August 23c/. — After dark went out to enjoy the air,
and to smoke. On returning, found two men mother-naked seated one
on each side of the door-step. They had been stewing in the steam-
bath after their work. I had seen them stalking off, like a couple of
gliosts flitting through the twilight, round the farm-houses, as naked as
they were born, half-an-hour before. Now they were taking the cold
stage in the sharp frosty night-air. Told my chum, who went out and
found them still sitting where I left them. When they had enough,
they came in, put on some clothes in the porch, and went to bed.
This house had mahogany chests of drawers, and all manner of luxuries,
and it was haunted liy very large and hungiy tieas."
About a quarter of a circle westwards a movement from
N.W. to S.E. is now going on in similar latitudes in the sea,
because of the shape of the land now above water in these
regions. In passing southwards ice also moves eastwards
along the western shores of Smith Sound, Baffin Sea, Davis
Strait, and the Atlantic as far as Cape Kace ; but it always
hugs the western shore of the sea, be it wide or narrow^
apparently for reasons already given. The result is shown
in a contemporaneous account of land and sea to the west-
ward of the Atlantic and of Davis Strait.
In 1864 and 1865 two attempts were made to reach the
eastern coast of Greenland, for the purpose of forming a settle-
ment and for exploration. The expedition was twice defeated
by ice which hugs the western shore of the Atlantic all the
way below lat. ^&^ or 67*' N. After vainly striving to force
their way through to land, they went down stream round Cape
Farewell, and up to lat. 66° N., long. 61° W. or thereabouts,
where a fishing and trading post was established on the
western side of Davis Strait near Exeter Sound. On the 12th
September 1866, Mr. Taylor, in command of the expedition,
532 A MODERN " GLACIAL PErvIOD."
wi'ote to Messrs. Antony GiVOjs and Sons, the promoters of it,
and to tliese gentlemen the writer is indebted for permission
to quote from a vivid word-picture of life in a modern glacial
period. Tlie land-traveller had some thoughts of joining the
sea-expedition in 18G5, and he has therefore felt something
like a personal interest in the result.
Men who parted in London in 1865 reached different geo-
logical periods in the same latitudes within a few weeks. One
who followed a warm stream found no ice afloat in lat. 71"
N., and there sweltered under a hot sun on shore. " Those who
went westward found open water as far as Iceland, and then
hy steering westward they suddenly entered the " Western
Atlantic Marine Glacial Period^' whicli has covered Greenland
with snow and ice. They followed it to lat. 60", where cur-
rents work northwards and southwards on opposite coasts of
a narrower sea ; and they finally settled on the western shore
of Davis Strait, where, according to theory, the coldest streams
ought to flow. They found a climate " worse than that of the
worst parts of Greenland," for they were in the " Westevn Baffin
Sea Marine Glacial Period," which extends to Newfoundland.
On the 29th of September 1865, ice drifted in and filled
the fjord. On the 3d of July 1866, the same ice made it im-
possible to launch a boat from the shore, or to get in from
the ship, whicli then arrived out. Tliey are never certain of
the ice for a night in summer. There may be none near in
the evening, and next morning ice may be piled up high on
the beach, to the great danger of boats. Photographs taken
in August 1866 show scattered fleets of " growlers" and
small bergs dotted about the sea off Exeter, as they were in
August 1864, about fifteen degrees farther south, off the La-
brador and Newfoundland. In winter, a man who walked
out in leather boots lost a toe, so the rest, who were only used
LATITUDE 66° N. 533
to Greenland cold, made boots of canvas lined with boiler-
felt, and so escaped frost-bite. Claret, placed in a sitting-
room for safety, burst the bottles when the wine froze. On
the l7th December 1865, a thermometer marked 31° F. on
the floor, between two good coal-fires distant from each other
four feet. From December to May, beer, vinegar, and lime-
juice were solid. January 3d, the cold was 53° below zero at
noon. Mercury was solid as lead. Danish corn-brandy was
thick like syrup. Port-wine forced the casks and ran out,
half-solid half-fluid. On the 4th of August 1866, the ther-
mometer was 56° above zero, and that was the maximum
observed. The temperature observed in Lapland about the
same season was 2-1° higher, though about four degrees further
north (see above, p. 512).
One evening in March, the brave lady who followed her
husband to these cold regions espied a bear quietly walking
past the window, within a few yards of the house. The
gentleman went out and bagged the bear, and aU hands feasted
on him for three days. All the domestic animals lacked
proper food, and suffered. The pig had a family, but the cold
crippled them, and they were slain all but one, who was
lame, and for that offence condemned to die when the frost
set in. Geese flourished ; but Esquimaux dogs played havoc
in the poultry-yard. Two sheep grazed for two months about
the houses, and then disappeared. Six months afterwards their
frozen bodies were found in the rugged mountains which sur-
round the station. Goats died one by one. Fowls did pretty
well, and laid many eggs ; but when more fowls were brought
in a ship, the new arrivals ate their own eggs and those of
the old fowls. Of eighteen lives, shared by two cats, one-
half was expended by Esquimaux dogs, and one cat alone sur-
vived in September 1866. Men who settle in glacial periods
534 THE MAIUNE rOLAE GLACIER.
ought surel}' to provide tlieniselves witli spare lives if they
can, for there seems to be small enjoyment in hibernation.
All this time Scandinavians and Icelanders, and their
cattle, were nourishing as far north, and many degrees fur-
ther. Even Greeulanders about Disko were tolerably well
off by comparison. The new settlement suffered most from
cold, apparently because it is planted on a point M'hich juts
out into a stream of cold water and floating ice, which is
moving southwards because it is cold and heavy, and which
hugs its western shore because of the earth's eastward mo-
tion. The result is a local glacial period of greatest intensity
where land is most exposed to a polar current, as it is at
Exeter, near Cape Walsingham. It is manifest that marks
made by this branch of the marine polar glacier must corre-
spond in direction with the movement which, from local
circumstances, now is S. and eastward, instead of S. and
westward as it is elsewhere.
Town manners are not worth describing, country manners
may be.
From TorneS. to Kuopio is 294 English miles.
" Aug. SOfh. — Travelling in country cars 84 miles. Stopped
at 7.30 at dark. This method of travelling is decidedly uncom-
fortable. ]Most of the "ts are mere wooden trays, \A'ith a
board and a back set directly over the wheels, on the edge of
the tray. There is no symptom of a spring of any kind in
many specimens of this instrument of torture. The traveller's
teeth literally rattle ; the pipe is jerked out of the mouth, and
the jaws come together with a loud snap ; the baccy is jerked
out, and the ashes are blown into the eyes ; and everything in
the baggage is shaken, so that screws come undone in tele-
scopes and such-like gear. Moreover, in a country where
peaceable men go armed, it seemed wise to carry tlie gun
TRAVELLING.
535
loose, and it had to be nursed all the way. The seats are
narrow, and boys and men who drive are much inhabited.
Cheek-by-jowl their vicinity is terrible. The pace is about 7
miles or 10 wersts an hour, but every now and then it varies
from 14 to 1. Some brutes run away, some won't stir. One
dun brute looked obstinate as a nmle, and proved that horses
have expressive eyes. When I thrashed hira he went slower,
when I hit hard he kicked. At last, in despair, I braced up
my nerves for combat, and laid on. The horse kicked, I hit
harder ; he stopped and kicked so that he nearly landed both
Failure of the Whale Fishing.— On Thursday
Qorning the whaliag vessels Erik, of London, and Esqui-
naux, of Dundee, arrived in ihe latter port from thewhalo
ishing, at which, unfortunately, they have been most un-
uccessful. The Erik comes home clean, and the Esqui-
maux bringstho prScltice of a single fish — some 10 or 12
uns of oil. The firm to which the Erik belongs— Messrs.
intony Gibbs and Son, London, have a Jishing settlement
F^'etef "^iiud^ but dufinS!lfie last JL2"months it has been"
iost uuproductive. A nuniber^ot seaborses and^bcars were '
xpturedj^ but tlieseT of course wih noT yield any yery^"
irgesujn. Three men and one woman died at the settle-~f
iionti ATtliough the wLaling~esseI Diana, o^ Hull, wa?^
erv near {JEeBettlement, those resident ttierg^ remainea i
)tally ignorant of her condition, rnis is aceoun'Eea tor bl^
leTact tFat thelginter was an exceedm^^tluckose. .^Tli^
asters of the vessel reporE tharflie "ship Tay, of bundee.
as besot in the ice near Coutts' Inlet towards the end o:
ugust. The vessel has not been seen since.and it is feared
lat the crew will have to endure all the horrors of a winte
these cold and inhospitable retpons. Some of the ©the.
lips are expected soon, but a part of the fleet it is believed
ive gone to Cumberland Gulf, in order to still further pro-
cute the fishing. So far as known at present only two whales
ive been caught by the whole Qeet, and should there be no
iprovement at the close of the season the fishing will be
e mostunreniunerative the Dundee companies haveyetex-
srienced. —Express.
h^y. ^Jxe<; '^^^
If
534 THE MAltlNE rOLAK GLACIER.
ought surely to pi-ovide themselves with spare lives if they
can, for there seems to be small enjoyment in hibernation.
All this time Scandinavians and Icelanders, and their
cattle, were flourishing as far north, and many degi'ees fur-
ther. Even Greenlanders about Disko were t&lerably well
off by comparison. The new settlement suffered most from
cold, apparently because it is planted on a point which juts
out into a stream of cold water and floating ice, which is
moving southwards because it is cold and heavy, and which
hugs its western shore because of the earth's eastward mo-
tion. The result is a local glacial period of greatest int^iT^itv
1
TRAVELLINCx. 535
loose, and it had to be nursed all the way. The seats are
narrow, and boys and men who drive are much inhabited.
Cheek-by-jowl their vicinity is terrible. The pace is about 7
miles or 10 wersts an hour, but every now and then it varies
from 14 to 1. Some brutes run away, some won't stir. One
dun brute looked obstinate as a mule, and proved that horses
have expressive eyes. When I thrashed him he went slower,
when I hit hard he kicked. At last, in despair, I braced up
my nerves for combat, and laid on. The horse kicked, I hit
harder ; he stopped and kicked so that he nearly landed both
heels in the cart. Hit him again, and he sent the soles of his
shoes close to my nose. Hit him again, and laid on as hard
and fast as ever I could rain blows on his dun dusty hide, and
kept on till he gave in and boiled up a trot. After that the
beast went faster when he was flogged.
" Sept. 2d. — Halted at 9 at Gumpomaki (in Finland). On
the road met about a dozen men in shirts, or stark naked,
walking out of the station to the steam-bath. It was a sharp
frost. Shouted gulime (cold), and got a laugh and an answer.
They seemed to think it a matter of course to walk stark
naked in the frosty air for a hundred yards, along a road, out
of their common living-room into an outhouse to be steaiued.
Got a fire, and some bread and milk, and slept in my clothes.
Going loj hours on nothing but bread and sweet milk, in the
very worst cars I ever tried. The last had no seat at all ; the
wheels were so low and the horse so tall that the cart sloped
backwards. When I sat in front the sharp board at the edge
cut my dangling legs, and my bent back ached and seemed
about to break short off at every jolt. When I changed with
the old man and sat back, the ropes which bound the luggage
worked into my ribs, and generally it was the mischief and all
to sit in that agricultural post-carriage. A whole tribe of very
VOL. II. 3
536 AUTIIOIUTY.
good-looking, clean, brushed, steamed, well-dressed rosy lads
came into my room and pored over my Ijooks and maps. Set
them to read, and learned a lot of their language. "
The coimtry between St. Petersburg and London was
traversed in 84 hours, and numerous notes were made ; but it
is needless to print them, for the country is well known to
geologists. Part of it is exceedingly like the country beyond
Chicago, and both Central Europe and the central plains of
North America probably were sea-bottoms during a cold period,
or were in the run of cold currents during periods like the
present. The author holds to his opinion, but he is prepared
to adopt the big glacier on sufficient evidence, and all the
more after follo'wing ice-marks from Tornea to Wiborg, and
boulders into Poland, in the autumn of 1865.
On reading marked passages in books, which Sir Eoderick
Murchison had the kindness to send to him, the author
was pleased to find that many of the conclusions at which he
had arrived by looking at facts agreed with the published
conclusions of his distinguished countryman, drawn after
mature study of drift, etc., in Eussia, Scandina>"ia, and else-
where.
In a very able paper on the drift of Sweden the following
])assage occurs : — *
" Oui- future busiuess ;is geologists is not to contend for the exelu-
iiiv^i operation of any one of these causes'' (waves of translation, marine
and other currents, sea-ice and land-ice), " but to endeavour, calmly
and patiently, to work out each case on its own merits, instead of ap-
pealing to one universal cause for the ijroduction of rounded, polished,
abraded', grooved, and striated rock surfiices."
No one theory yet started will sufiice alone to account for
all the glacial phenomena descriljcd in these pages, and in
books of authority. In Finland marks run from N.W. to S.E.
" ]\ 270, Pn>,rn/i>,;/soffI<r OnJo,/in>/ Sorirfi,. A].!'!] 12, ISK).
UPIIEVVAF,. 037
{Proceedings, Oeoloijical Socuii/, April I84i)). In CJothlaiid
the action (of ice) was from N.E. to S.W. (p. 350). Limestone
of npper silurian age is striated in that direction, and the
drift, a gravel of granite and porphyry, is so disposed as to
indicate movement in that direction.
Forty miles south of Petersburg the direction of similar
marks is from N.N.E. to S.S.W. (p. 360, note).
From various phenomena, terraces, etc., it is probable that
all Gothland was submerged when these marks were made,
and in this case Sir Eoderick attributed the transport of
angular blocks to ice-rafts.
Vast waves of translation will not account for the pheno-
mena observed. Near Stockholm the direction is N. by W.
(p. 369). Baltic shells found under osar and terraces prove
that the drift and erratic blocks of the low country in Sweden
are a marine formation.
And so all the work done is l)ut a foundation on which
to build.
Upheaval.
These few observations bear directly upon two chief divi-
sions of the subject of this book — on " Denudation" and on
"Deposition;" but they also bear indirectly on "Upheaval."
Within the area which was revisited for the express purpose
of testing the conclusions which were stated in the text under
these heads, it is possible to study " forms" shaped under
water by certain " engines," but only because marine deposits,
and the worn rocks on which they rest, were pushed away
from the earth's centre, and were raised above the sea-level
and brought within human reach by the action of a subter-
ranean " ray-force." Late events have shown wliat that
"force" is, for it has come to the surface, and it has done
work there since the publicati(jn of Frosf and Fire.
538 KARTII-LTGTIT.
In 1865 an eruption of Etna was described in English
journals and magazines (chap, liv.) In February 186G a new
Greek island rose from the sea in the bay of Thera at San-
torin. The disturbance began on the 31st of January in the
bay, which is an old crater about six miles wide, broken on
the west, and now filled with sea-water. It began with a noise
like a cannonade. Those who have heard and who have felt
the recoil of steam-guns in the Geysirs ; those who know the
meaning of like noises in hot-water pipes and kettles ; those
who have watched battles between fire and water at furnaces ;
and those who will read chap. Ivi., and make models to illus-
trate volcanic action for themselves, can readily understand
this terrible sound. The earth's cold crust was rent hy a force
radiating from within ; sea-water was dragged down by forces
converging upon the earth's centre from without ; cold ihxid
touched hot fluid, and, urged by opposite forces, they acted
and reacted. One became solid, the other a hot vapour.
Steam-bubbles formed above a newly-formed crust of hot
lava, and as they rose into cold water, the water-shells col-
lapsed. Visible "earth-light" shone out M^here it was not
thus converted into mechanical work and audible sound.
Nea Kaimene, which rose in the same l)ay in 1707, was rent,
and the southern half was dragged down by gravitation and
sank considerably. Houses and the main island sank till the
chimney -tops alone remamed above water. Here were
" troubles," " faults," " heaves," " throws," and " slips," pro-
duced by op})Osite forces : the cold outer crust was broken,
and the fragments Avere moved away from and towards a
common centre of radiation and convergence, which in this
case was the centre of the earth. On the 4th of February
the new island appeared, rising visil>ly h-oni the depths with
noises "like the burstiiiir of steam-boilers ;" amidst " flames"
RADIATION, CONVERGENCE, AND WORK. ■'>3'J
visibly slnuiug uuder a vast column of white smoke, which
rose high into the air, and there spread out to form a curled
capital of dark cloud, which spread and drooped like a foun-
tain, or like a tall palm-tree. The "ray" was pushed through
earth and sea into the air. The sea in the bay boiled ; water
and stones were cast into the air ; the sea-bottom rose 420
feet in one ^Dlace, 84 in another ; the island itself grew out
of the sea into tlie air ; in five days it was 150 feet high, 350
long, and 100 broad. The visible part of it consisted of a
rusty black metallic lava, like slag which had boiled up and
cooled near a furnace ; the outer crust was dark and hard,
but rifts in it still shone, for the tough under-crust was red-
hot. A radiating " force," which was luminous when it was
not otherwise employed, pushed a mass from below, which
pushed up that which liad risen above water ; the cold crust
broke, and " earth-light " shone through and fled away to
work through the air into space. A lava-spring rose through
the earth's broken crust and froze ; water sank in and boiled ;
steam and gases blew bubbles in water, which burst, and in
tough lava, which hardened when it cooled ; and so "ray-force"
built a dome at Thera. Thousands like it may be seen in
Iceland, but this one was seen to rise shining ; so all who care
to study " Dymanical Geology " had good illustrations of the
power of "Fire " in 1865 and 1866.
In the Times of April 22, 1866, is an account of similar
mechanical work done by the same forces on a smaller scale.
Three men neglected to "tap" a blast-furnace at Wolver-
hampton at the proper hour. The molten iron in the cup
rose above the level of a pipe which contained water, so the
facing of the pipe and the pipe itself were destroyed. Solids
were melted, and fluids of different temperatures met. Water
touched luminous fluid iron, and darkened the lidit, but the
540 KAVS OF FORCK.
" rays " were only clianged into rays of force. The water, as
steam, spread from the point of contact ; it blew out the
side of the furnace, and then gravitation dragged down the
fragments, and let loose a torrent of iron, which fell on the
men, and they died. Two were burnt and scalded by molten
projectiles ; one was overwhelmed and instantaneously de-
stroyed. In this case, as in eruptions at Santorin and in
Sicily, " work" was done by " rays " of force, which are coinci-
dent in direction with rays of sensible heat, of audible sound,
and of visible " light."
In March 1867 the same force was felt as an earthquake at
Constantinople and Smyrna, and over great part of the ^gean
Sea. On the Gth, INIitylene M'as destroyed by shocks greater
in degree than tlie quivering motion of a table in a ship in
which a simmering boiler is sliaken by the condensation of
bubbles of steam, and greater tlian the trembling of a bed
on the ground at the Geysirs on the sudden collapse of a
steam-shell, but the motion was similar in kind. The sea,
was seen to heave and foam as fluids do on board a steamer
when the fires are lit. When the radiating earth-waves reached
the town, whole blocks of solid stone houses reeled and
tottered, and fell with a crash, burying hundreds of men.
Here, as at Santorin and Wolverhampton, the solid crust was
rent, and gravitation dragged a fragment down. The most
complete ruin fell upon the lower part of the town, where
the earth literally opened and swallowed a broad belt of
building right u]) from the sea to the slope inland. A i)erma-
nent subsidence of the ground took jilace, and the sea covered
the busiest part of the busy town of JVIitylene. About 1300
out of 80,000 inhabitants perished in conseqiience of this
disturbance caused by subterranean force, which at Santorin
Avas hariiilcss wlien it escaped as visilde " liglit." ()n tlie other
WOKK. 541
side of Greece, amongst the Ionian Islands, it has been
noticed that sea-water has been continually flowing into the
earth through rifts at the sea-level. It seems that a stream
has been flowing into a boiler for many years. When the
earth's crust broke at Santorin, and the pipe at Wolverhamp-
ton, when hot and cold fluids met, visible and sensible rays
became rays of active force. It must be the same whether
they meet above ground or under it — in a furnace, in a kettle,
a boiler, a bay, or a cavern of any size.
In the island of Cerigo (according to a paper in the
AtJiencvum of 13tli May 1865) are terraces and raised
beaches more than twelve miles inland, and from 800 to
1000 yards above the present sea-level.
In the island of Cephalonia, close to the place into which
the sea has been flowing for years, earthquakes shook down
whole towns in February and March 1867.
Etna, Stromboli, Vesuvius, Cephalonia, Santorin, Mity-
lene, Smyrna, and Constantinople, are spots scattered over a
space on the earth's crust which has been more or less shaken
from below within the last two years, and the area is about
as large as the northern district which has been quietly lifted
some few feet out of the sea within the historic period, and
which seems to have risen 4400 feet at least. Together they
equal Greenland, which is moving also, and has moved a
great deal. At Santorin the ray-power which did so mucli
" work" in struggling to escape, emerged at last as " light,"
similar to sunlight, and to all lights whose rays include rays
of heat, which are convertible into rays of force. One cliief
aim of this book was to prove by experiment, and to show by
observation and reasoning, that where light shines there also
a force acts in opposition to gravitation ; and that two oppos-
ing forces, which for brevity may be called " Eays" and
542 KAYS AND WORK.
" Weight," do in fact work natiu-al engines, above ground
and under it, as they do engines of man's device.
These disturbances in Southern Europe support con-
chisions previously formed. " Frost" is over-head in the cohl
regions of space ; " Fire" is under-foot, scarce liidden by the
cold dark crust which opens at times to let out a few rays of
" Light."
About the same time the same thing was going on on the
other side of the world : —
" New Volcano in the South Seas. — The following is an extract
from a letter from Mr. J. C. Williams, Her Britannic Majesty's Consul,
Navigator's Islands : — ' A volcano lias broken out at sea, at Manna,
aboiit two miles from the island of Olosega. It was preceded by a
violent shock of earthquake, which commenced on the 5th of Septem-
ber 1866, and on the 12th dense thick smoke rose out of the sea.
Lava was thrown up, discolouring the water for many miles round, and
destroying large quantities of fish. Wherever the ashes fell on the ad-
jacent island they destroyed all vegetation. Vp to the middle of
November dense smoke was still being thrown up, and my informant
says that the smoke rose higher than the neighbouring island, wliich is
over 2000 feet high. We cannot at present ascertain if there is any
Ijank thrown up in the water. Last July we steamed over the place in
Her Majesty's ship Brisk, and there were no signs of shoals or anything
of the kind.' "
Speculation.
Tlius far an attempt has been made to travel from the
known to the unknown ; from facts observed to their causes,
as far as was possible with the limited means of mental loco-
motion which the writer has at his command. The distance
traversed is small indeed, and the onward journey seems to be
endless.
From these new facts a new crop of old conclusions
naturally grows ; but having reached a boundary-fence, there
is e\('i' a strong desire to pass it. In the " bread-basket oi'
tlic wiirld" farmers are ever seeking new pastui'es to i>l(>ugli
SPECULATION. 543
ill the wild prairie ;* they are never content to grow crops
witliin fences. Having arrived at the " great unexplored
ocean of truth," it is very tempting to venture in ; to
cease wading patiently about the shore with steady work-
•^ 'H t- "" -c -•"- "^ * 2 Tc "^ '^ *" ? ^ "o '.i •" = t: o •'" ri ''- -'"^ 3 " o •■-; "^ ^ r- c •-
r . Q- „^ I ^ f, E 1 ": .5 " ^^ q: I ^ 1 35 .-" -5 iT ^ § i^ <^ s 2 ^ ^ : ^ 1 ^
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S O c cs •_ ^ -■ — _ _ _ ^ (0 © ©
i„-.^ ^ „ ?„rf...',':3u'"icu-, iiia't rays, or radiating' waves, orgi'ow-
ing shells of force, are coincident in direction with rays, or
spreading waves of heat and light. Along the devious path
which is mapped out rudely in this book, it was found that
centres of attraction in masses ichich are hot or himinous are
also centres of repulsion.
If that be good natural law, then work is cut out which
the author has neither skill nor power to undertake. He has
no hope of reaching this land himself ; but, like Eobinson
Crusoe, he thought he saw land, with lights on it, far out at
sea, long ago, when he first began to think about " Frost and
* Short Amci-icaa Tramp, p. 295.
542
RAYS AND WORK.
" Weight," do in fact work natural engines, above ground
and under it, as they do engines of man's device.
These disturbances in Southern Europe support con-
clusions previously formed. " Frost" is over-head in the cold
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■ » a<;
3 P
2.§ g.
3_p o
° S 3 -^^<P
3 2 i=^ 3 c g
g^ro ^ p 3
- P o ?S S S^ ci-
&• 3 c £ 3 3 q 3-
g o
Speculation.
Thus fur an attempt has been made to travel from the
known to the unknown ; from facts observed to their causes,
as far as was possible with the limited means of mental loco-
motion which the writer has at his command. The distance
traversed is small indeed, and the onward journey seems to be
endless.
From these neM' facts a new crop of old conclusions
naturally grows ; but having reached a boundary-fence, there
is ever a strong desire to pass it. In the " bread-basket of
tbc world" farmers are ever seeking new pastures to iil(»ugh
SPECULATION. 543
ill the wild prairie ;* they are never content to grow crops
within fences. Having arrived at the " great unexplored
ocean of truth," it is very tempting to venture in ; to
cease wading patiently about the shore with steady work-
men, who make real progress by building safe cause-
ways with hard facts. On such piers of made ground
idlers may walk dryshod ; but many are tempted to plunge
headlong into unknown depths, with the hope of finding
bottom somewhere. A stone brought up by a diver is a
treasure. To reach new ground, though it may be a rock, is
worth some risk. Many a boy has learned to swim by a
plunge ; and a swimmer, who cannot reach new land, may get
near enough to see it, and return to start afresh in a boat of
his own. Even the sensation of independent thought, even
the search for a fact, is worth some hazard.
It seems to follow, from all that has been observed thus
far, that the " upheaving" force, which does so much work
within reach, may also work out of reach, on any scale, in
any place from which sensible or visible rays set out. It
has been found, so far, that rays, or radiating waves, or grow-
ing shells of force, are coincident in direction with rays, or
spreading waves of heat and light. Along the devious path
which is mapped out rudely in this book, it was found that
centres of attraction in masses which are hot or luminous are
also centres of repulsion.
If that be good natural law, then work is cut out which
the author has neither skill nor power to undertake. He has
no hope of reaching this land himself ; but, like Eobinson
Crusoe, he thought he saw land, with lights on it, far out at
sea, long ago, when he first began to think aljout " Frost and
* Short American Travip, p. 295.
544 SPECULATION.
Fire," " cinder-heaps," " sparks," " motion," " work," and
" form ;" and set about building his thoughts into shape.
If all tlie conclusions arrived at be just, then bodies which
reach the earth from outer space may have been driven away
from some distant star by rays ; for stones are driven away
from the earth by shorter and weaker rays of force.
Planets may burst in space, because waves of force radiate
from, their centres of attraction ; for sparks, shells, volcanic
bombs, and meteors which are small planets, are burst by
rays of force under certain conditions.
The sun may give birth to new planets, if the sun's rays,
which do so much work at this distance, are strong enough at
their source to throw sparks and drops far enough, and in fit
directions. The sun, and stars which are distant suns, may
burst, and change into nebuLx;, and show their origin by forms
made visible by rays, which traverse space and do work even
here after their long flight. These are some of the distant
lights, true or false, which first tempted a wanderer out of
bounds to gather facts witli which to build a raft to carry his
thoughts onward.*
The planets and smaller members of the solar system bear
about the same proportion to the sun round Avhich they
move, as dust, sand, and shot of various numbers bear to a
thirteen-inch shell. The proportion and relative distance are
sliown at the Geological Miiseum in Jermyn Street as far as
the earth. Mr. Chambers t gives the proportions in a form
likely to be impressed on the youthfid memory, through taste.
* " Some indeed have sii])poscd the sun to be cohl, but I believe Mr.
Flanistead is not of this opinion, for they may as well affirm culinary fire to
be cold ; for we have no arj^ument of its being hot but tliat it heats and burns
things that approach it, iiiid \\r have the same argument of tlie sun being hot."
—/.//;■ n/mr Tsaac Nnrhni, vol. ii. ]). i!:,r>.
t DK/Ihirso/As/i'onnui./,, p. lit. Loii.lon : ,lobii .Miirniy, \M\.
SPECULATION.
545
The Sun, a globe 2 feet in Jiunieter .
Vulcan, a pin's head at the distance of
Mercury, a mustard-seed .
Venus, a pea .....
The Earth, a pea ....
Mars, a large pin's head
The Asteroids, grains of sand
Jupiter, a moderate orange
Saturn, a small orange
Uranus, a full-sized cherry
Neptune, a plum ....
o
27 feet
82 „
142 „
215 „
327 „
500 to 600
^ mile
■| mile
f mile
1^ mile
moving daily
4| feet.
3 „
2 „
H „
lOi^ inches.
n „
5 „
4
Would a shell of two feet in diameter throw a grape-shot a
mile and a quarter out of the fuze-hole if it were floating in
space? Would it throw a grain of BB 215 feet? How far
would a gun a foot long tlirow a bullet if the earth's attraction
were out of the problem ?
These are questions. It is a fact that whenever a ladleful
of hot liquid iron equal in mass to a globe of two feet in
diameter is left to its own devices at Woolwich, in the place
where shells are cast, it first curdles at the surface, and when
a thin crust has formed there it begins to throw off small
liquid spheres about the size of peas and pin-heads, BB shot
and snipe-dust. It goes on throwing these projectiles to de-
to a certain point it stops. Thenceforth rays of force work
within ; but for a long time after that stage, rays of sensible
heat and of visible light reach far beyond the most distant of
the projected spheres, which cool and darken rapidly in pro-
portion to their mass. When by any accident water or air
gets shut up in a mould, drops of metal as big as oranges,
cherries, and plums, are thrown about, and sometimes they
are blown through the roof with great force.
In theory, if that mass of iron were cooling in space, it
would take the Ibmi of a sphere, and throw off little spheres
5-16 SrECULATION.
to much greater distances, because tlie projecting force of rays
within tlie crust would be the same when opposed by the
forming shell, and because the attraction of the mass alone
would be far less than its attraction combined with that of the
whole earth. "When the mass had cooled in space, it would
cease to throw off sparks, or throw them to short distances ;
and when cold it might revolve on its axis, and round some
centre of attraction, if there were no resistance to overcome
these motions.
So far theory and fact agree. If the sun were a stationary
mass in the condition of iron newly run from a furnace (chap,
liii.), or of silver cooling (chap, lii.), according to analogy
it would throw off projectiles to great distances.
It is a fact that a mass of gelatinous collodion (chap.
Iviii.) free to move in water assumes a circular form, grows a
shell, and through it projects spheres of collodion, fountains of
ether, and columns of vapour. While so doing it revolves on
its axis, and moves about points on the plane of the water,
till the radiating force within the shell is expended, and the
motion set iip by radiation is overcome by friction. It is
also true that dimensions and distances and times all bear some
proportion to each other. The larger the mass of iron, silver,
or slag, the further it throws sparks, and tlie longer it works.
In fact, small projectiles thrown off by rays from re^•olving
masses rotate on their axes as they move. They do not fly off
at tangents, but take some direction which makes another
angle with a ray. Many burst as they move, so that flights
of small projectiles separate at moving points of dispersion.
It is also true that masses composed of materials which
are solid, fluid, and gaseous, at a given temperature, and all
become vapours or solids at higher and lower temperatures,
display more violent action than a mass of one material only.
SPECULATION. ^i7
If tlie sun were iu fact a mass composed of materials
wliicli are solid, fluid, and gaseous, in the condition of the
mass of gelatinous collodion, the silver, the iron, the slag, and
the other materials above mentioned, according to analogy it
would throw off projectiles in proportion to its mass, to
gradually decreasing distances, till it cooled to a certain point ;
and then it woidd continue to throw rays of heat and light
far beyond projectiles which it had thrown off" to cool rapidly
in proportion to their dimensions and materials, and to go on
with similar work on a less scale till their centres of attraction
ceased to be centres of radiation.
"What motions would result from gravitation, the laws of
motion, and the force of rays ?
That is the next question, and by reason of the earth's
vicinity it cannot be answered by any contrivance. It is
matter of calculation, and therefore it must be left for those
who are strong enough to undertake such work. The writer
has come to a fence beyond which he cannot pass without
help.
Since 1865 events have happened which demand some
explanation.
In 18G6 a great meteor was seen passing over the south
of England in broad daylight. Mr, James ISTasmyth saw it
on the 21st of June, when the image of it covered a space in
his eye equal to one degree, or twice as long as the moon
seems to be broad. The advancing end was brilliant red, with
a white envelope, and it dragged after it and left behind it a
fan-shaped, ragged, wavermg train, with white and faint
vapours. On the same day (according to the Times report),
about the same hour, a similar meteor, or the same, was seen
passing over Eotterdam. Like the meteor of 1864 (vol. ii. p.
383), of which fragments were picked up, this clearly was a solid
548 SPECULATION.
mass, wliicli arrived cold irtmi cold outer space, and was
heated in passing through the atmosphere. To use modern
terms, " retarded motion was converted;" or, to put the same
thing into another shape, direct motion, the result of some
previous exertion of force, was converted by an opposing force
into "rays," which diverged from the centre of the mass.
The cold solid became hot — part of it red-hot ; part was
white-hot and fused ; part of it was changed into vapour and
thrown off and left behind the mass, which was solid, liquid,
and gaseous, and radiated force, heat, and light, perceptible at
different distances.
In June of the same year, about ten o'clock one fine sunny
morning, when the citizens of Boulogne were promenading,
the town was startled by a loud noise, which each individual
supposed to be directly overhead. It was therefore at a great
height. A person who heard the sound describes it as
" like one very loud clap, without any warning or subsequent
rattle ; an explosion Like many powder-mills going off at
once." On looking up at the blue sky, this observer saw a
"sliglit puff';" and a gentleman, who happened to be looking
the right way at the right time, saw " a streak," " a kind
of zig-zag line." No powder-mill was blown up, no thunder-
cloud appeared, no fragments were picked up. The chat-
tering below, the excitement and terror caused by the
noise in the air were portentous, and the learned concluded
that a meteor had burst over Boulogne and fallen into the
sea.
The meteor of the previous year was seen to lly and revolve
and burst, and bits of it were picked up liot. In November
1866 a great flight of little planets met the earth in wheeling
about the hot sun tlirough cold space. When their motion
was stop])ed by resistance, force radiated from within the
SPKCULATION. 5i0
masses, which shone and glowed, and burst and vanished
like a display of rockets or a flight of shells.
While these small planets were luminous, their centres of
attraction were also centres of repulsion ; their rays were
strong enough to overcome the opposing forces which held
them together, and some burst.
Museums contain enough of fragments to make part of the
story of a meteorite perfectly plain (vol. ii. p. 380). But what
was the previous exertion of force which sent the meteor out
on its path through cold space ? Whence did it come ? What
paths did the fragments describe after the meteor burst ?
What course would fragments describe if a larger planet were
burst in like manner by the energy of its own rays ?
Given a gun (R — R^) moving in space about a point (A +)
— a shell filled with fluid fired from the moving gun, turning
on its axis, and burst (at E^). Given weights, velocities,
etc. — what paths will radiating drops and fragments describe
with reference to the point (A+) after they part at the moving
point (R^) ?— (vol. ii. pp. 450, 501).
They partake of motion about A+ and the Axis ; — and
from R^ to R^ ; they are driven apart by rays at E". They are
subject to the laws of motion, and they are attracted towards
each other, and towards A+.
The author hardly knows how to express the problem ;
better mathematicians than any within his reach may perhaps
be able to understand his meaning, and solve the c|uestion ;
but, in the meantime, it seems that under possible conditions
a projectile burst at R^ might there be so repelled and
attracted as to satisfy the conditions from which the curved
paths of meteorites, asteroids, and other projectiles about a
point (A+) do in fact result.
If so, then the sun and its train may have formed one
550 SrECULATION.
mass, which may have formed part of a larger mass, and so
ad infinitum. As a possible case of a burst planet, take "Bode s
law," published in 1778 * Take the numbers 0, 3, G, 12, 24,
48, 96, 192, 384, each of which, the second excepted, is double
the preceding number, and add to each 4. The resulting
numbers, 4, 7, 10, 16, (28), 52, 100, 196, 388, approximately
represent the distances of the planets from the sun. In 1778,
there seemed to be a gap at (28), and Bode predicted the dis-
covery of new planets at or about that distance. Since then
eighty-two small planets have been discovered thereabouts.
The smallest are not more than 20 or 30 miles in diameter,
and who is to say how nuich small shot may be mixed with
this charge of grape ?t
Let the point A -i- be the centre of the sun, and the gun
E" a point on the sun's circumference moving about A+ ;
let a mass be thrown off' revolving on its axis, and let it
burst at li'^ (equal to 28). What paths might some of the
fragments describe with reference to A+ under possible con-
ditions ?
The author cannot tell how to set about the solution of his
problem ; but expedients described in chap. Ivii. and the
diagrams, pp. 450 and 453, etc., were all meant to bear upon
* Handbook of Astronomy, Cliaiulicrs, p. 19 ; Murrny, 1861. Rep. Brit.
Associat. 1866, p. 26.
t " Dr. Olbers of Broinon, who disoovered two of tlicin, hazarded the idea
that a large planet which once occupied the same place had been burst in
pieces by some internal force. This opinion, which has been long considered
as a very probable one, has only recently been called in question. M. Lever-
rier considers the opinion of Olbers as contradicted by the great inclination
of the orbit of Pallas, and believes that they have been regularly formed like
the other planets, and by virtue of the same laws."— ii/c of Sir Isaac Navton,
by Sir David Brewster, 1855, vol. i. p. 371.
P>ut how were the otlier \AA\\iiis formed, and by what mcclianical hncsl
SPECULATION. 551
such questious, which must l)e left to matheniaticiaus, if any
think them worthy of attention.
A visit to the British Association, which was formed for
mutual help, encouraged the author to go on, for he found
himself at sea in good company. The president, in speaking
(if gravitation, said —
" But the nebula} present more difficulty, and some doubt has been
expressed whether gravitation, such as we consider it, acts with these
liodies (at least those exhibiting a spiral form) as it does with us.
T'ossibly some other modifying influence may exist, our present ignor-
ance of which gives rise to the apparent difficulty."* — Report, p. 26.
The author does not venture opinions ; he did not raise
his voice amongst his betters ; but diagrams drawn by fluids
moving away from centres over discs of card (p. 450, vol. ii.)
are strangely like portraits of the spiral nebulae (51 M.
Canum Venaticorum, plate 40, fig. 137, in the handbook
i[Uoted above). Admit that rays of force and light are coinci-
dent, that centres of attraction are also centres of repulsion in
masses which are luminous; and " repulsion" must be taken
account of in astronomical calculations, for light pervades the
visible universe.
When the author of this book found himself, at the end
of a long and rapid journey, in the Nottingham theatre, and
there heard the president reading his address on " Continuity,"
he felt that he was in a shoal of swimmers who were not
content to walk dryshod on the safe causeways which their
ancestors had built, but who had built ships and gone afloat
* Another sidereal phenomenon in which we have the appearance of
motion round a centre, is displayed in the spu-al uebulffi discovered by Lord
llosse. That the stars which compose these spirals have been placed there in
virtue of some movement related to the central mass cannot be doubted,
although it is vain for man to attempt the solution of such a proV'lem." — Life
of ^ir Isaac Nciuton, by Sir David Brewster, 1855, vol. i. p. 37S.
VOL. II. 4
552 SP1-:CULATI0N.
to discover new land. He found his tiny cock-boat steering
with a fleet of first-rates, all heading one way. When he
heard that Light was henceforth to be treated as a form of
motion, convertible into other forms, and capable of mecha-
nical work, lie felt that he had somehow fallen in with a fleet
where all eyes were gazing through outer darkness for the
light which had led him to venture so far from land. How
often, within the last dozen of years, had the pith of this pro-
blem risen up in some shape, in some far corner of the
world ? —
" Assuming the unclulatory theory of light to be true, and that the
motion which constitutes light is transmitted across the interplanetary
si)aces hy a highly-elastic ether, then, unless the motion is confined to
one direction, unless there be no interference, unless there be no vis-
cosity as it is now termed, in the medium, and consequently no
friction, light must lose something as light, for all reflecting minds are
n<jw convinced that force cannot be annihilated — the force is not lost,
but its mode of action is changed. If light then is lost as light ....
what becomes of the traiismitted force lost as Jifjht, but existing in some
other fonn ? .... what becomes of heat radiated into sjjace ? What
becomes of the enormous I'orce thus api:)arently non-recurrent in the
same form ? Does it return as palpable motion ? Does- it move, or
contribute to move, sims and planets '\ and can it be conceived as a force
similar to that which Newton s])eculated on, as universally re]mlsi\i',
and capable of being substituted for universal attraction ?*
Wliat IccoDies of heat ? was the problem out of which un-
])ublished papers began to grow more than twelve years ago.
The problem sent the writer often to Norway, twice to Ice-
land, once to America, seeking facts : it made him select em-
l)loyments which promised to yield more facts ; and these led
to photography, lighthouses, mines, and the problem, \Ylwi
becomes of lights As a means of thought, the writer had built
a book with his store of facts, he had launched the paper
' ncpurl „f tlir Provccdiiiijs ,</ /]„• h'ri/i.sji yl.-<.soci,i/inii /'/ .\o//i,i,f/,>nn.
August 18G(;, p. 2it. i;<.1.t, ll;.idni.'l<.', T.'-J I'i.vadilly.
Sl'ECULATION. 553
l»oat, and gone afloat once more ; and now he had ftillen in
with a fleet steering for the same light and heading one
way. Old thoughts seemed to vibrate and chime in accord
with the eloquent words of a captain who was not ashamed
to confess that he too was out on a voyage of discovery and
at sea : —
" We are in no position at present to answer such questions as
these ; Imt I know of no ])rol)lem in celestial dynamics more interest-
ing than thesi'." — Report, i>. 29.
So be it. Let us ask, "What becomes of light?" and
What is the cause uf Ivjht ? for that is the next problem, if
light is a great mechanical force, for it pervades the whole
visible universe.
The whole visible crust of the moon has been shattered
and reconstructed by rays. In the earth's crust all the oldest
rocks have been rent, shattered, and altered by rays : spots on
the earth's surface equal in proportion to the largest craters
in the moon, or to spots on the sun — as for instance Iceland —
are wholly made of rocks which were fluid, and have frozen
into forms which we see on the moon. When we get hold of
a meteor, a volcanic bomb, or a spark, forms on the surface
and interior indicate rays of force.
It is possible to follow rays which join worlds ; to find a
barren rock on which to stand and look at hills, like it, which
can never be trodden by men. It is possible, even in the
midst of the great unexplored ocean, to reason of things of
which men can never be assured while they are bound to their
native earth. Science enables thought to travel out of bounds
on rays of light. By using light we have learned that planets
exist, and how they move ; that forms like volcanoes are on
the moon and the sun and distant planets ; that substances
which exist in the earth, and in meteorites which were small
55i SrECULATION.
planets, also exist in the sun's atmosphere, in comets, and in
distant stars.
Light, which tells all this and more, is like the steam-
hammer which works on any scale. The hammer will forge
a gun, or crack a nut without crushing the kernel. Like it,
rays set to work in coolmg fluids throw dust, drops, and large
volcanic bombs — inches, or feet, or miles. Set to work in
guns, rays throw small shot, grape, and shells. Set to work
in meteorites, they do like work in the atmosphere. If set to
work on the largest scale, the same forces must work on the
same plan. " Continuity " of effect surely means unity of
cause. Surely this same ray-force may have been set to fashion
worlds, and scatter them.
By searching backwards, men reach power through engines ;
by travelling far enough they seem always to reach a source
of light. The way to see further is to use light (vol. ii. p. 500).
There is reason to believe that a great change was seen to
liappen in a distant world in 18G5 — the same in kind as the
bursting of small planets, but greater in degree than the
bursting of a planet as big as the eighty-two asteroids.
From a paper read by Mr. Hind, it appeared that a new
star in Corona Borealis \^■as observed on the 4th of JNIay from
Canada, and on the 13th of May from Europe. On the 20th
it showed a clear disc, Avas uncommonly brilliant, and liad a
reddish tinge. The Canadian observer concluded that it was
" a telescopic star," because it was magnified by his teh.'scope ;
but if it grew large enough to make the divergence of rays
appreciable, the telescope would magnify a star at any distance.
It waxed and waned gradually, but in a very short time.
European astronomers conjectured that this star had burst
forth with astonishing suddenness, because they liad not ob-
served it so soon ; but tliei-i; is reason to believe that it is an
Sl'ECULATION. 555
old star which has long lM>en known as a mere point of light.
The new and brilliant light which thus appeared was analysed
by the new process which has extended human knowledge so
far into remote space, and the result was thus stated : —
" The liglit was coinjxmnd, and liad emanated fi'oin two different
sources. One spectrum was analogous to that of the sun — viz. formed
by the light of an incandescent solid or Iir[uid photosphere, which had
suffered absorption by the vapoiirs of an envelope cooler than itself.
The second spectrum consists of a few Ijriglit lines which indicated
that the light by which it was formed was emitted hy matter in the state
of luminous gas."
This last spectrum further indicated that the gas was hot
hydrogen. The star, like the meteorites, was apparently in
three conditions — solid, fluid, and gaseous — hot and luminous,
a centre of attraction, and also a centre of repulsion from
which rays diverged.
The observers concluded that the phenomena resulted
" from the burning of liydrogen with some other element, and that
from the resulting temperature the photosphere was heated to incan-
descence."
If light be a mode of motion, and a weak distant manifest-
ation of other modes which are greater and stronger at the
source — if it be as the smooth Atlantic swell which breaks on
the shore in a calm, and tells of a distant stoi^m — then here
was something like the explosion of a star by its own rays.
Perhaps, as some thought, it is " a variable star " — one of a
large class which wax and wane periodically ; but if so, a class
of stars may be in a similar state. They may l.ie passing
through periods of rapid action and " catastrophe." They may
be cooling ; forming crusts and darkening ; breaking them,
shining, and darkening periodically. A whole crust, or great
part of it, may be in the condition of the earth's crust at
Stromboli, which forms and bursts, shines and darkens.
55G SPECULATION.
periodically ; or like hot springs iu Iceland which explode
and have exploded for many years, at regular intervals. When-
ever a fresh charge of heat rises from below, and accumulates
sufficiently, it blows a charge of water out of the steam-gun
(vol. ii. p. 418). These wells seem gradually to cool till they
freeze. Stromboli may be sealed up in time ; and like these
a hot star may cool by regular gradations. Slags and metals,
which we can watch at ease, go through periods of rapid
action followed by long periods of slower work, and gradually
failing energy, which ends in repose at last.
Such events may be common ; they are rarely seen ; but
as form is a record of force, the story of a star may be trans-
lated from forms on the moon. If, as in the case put above
(vol. ii. p. 353), sun, earth, and moon, were parts of one hot
mass, of which tlie smallest has cooled most, then perhaps
we may read our world's geological history in the sun, and
future geology in the moon.
At Nottingliam the moon's surface was once more likened
to forms on metals (chap. Hi.), and the conclusion reached
was that great part of the moon's solid surface had been fluid
long after other parts had boiled up, bubbled, burst, and
hardened. From this it was argued that the later fusion could
not from its extent have been fusion of the same materials of
which the burst bubbles, cones, and craters are made. Moun-
tains would melt in a sea of melted hills. It was not so in
the case of the silver plate described above (chap, lii.) ; but
admitting the conclusion, different materials freeze at dif-
erent temperatures. We have mountains of trap in the water,
and water-seas which only freeze at low temperatures. It was
argued that the moon's surface must be greatly heated by the
sun's rays during each lunation. The supposed heat of a
quartz rock on the moon's surface at the end of a lunar day
SPECULATIOX. 557
was variously estimated at something far greater than the heat
of boiling water ; at 340° Fahr. ; and at the heat of red-hot
iron. One auditor felt that he or the speaker was steering a
wrong course ; so, like the owner of the " Foam," in Letters
from High Latitudes, the owner of the cock-boat " Frost and
Fire " cut the tow-rope, and steered for the ice.
He then believed, and, authority notwithstanding, still
believes, that, despite of the sun's rays, the moon's surface is
intensely cold. The belief is founded on the fact that the
highest rocks on this earth, which are in the rarest and clearest
regions of our atmosphere, and rocks which are exposed to the
sun's rays for much longer periods than lunar days — namely,
mountain-tops in polar regions — are not heated during six
weeks, or even during six months, of exposure to the sun's rays,
but are in fact the coldest spots on the earth, covered with
perpetual snow and ice. Moreover, the moon is not self-lumi-
nous, like hot iron, and rays reflected from it barely affect the
most delicate instruments under the most favourable conditions
yet tried. Moreover, it is clear from the structure of certain
stony meteorites that they were cold when they reached the
atmosphere, and that the surface was glazed by heat after the
stone broke in the air. But these may have been exposed to
the sun's rays in open space for untold ages. According to this
cold theory, so-called lunar seas may be metals frozen about
mountains of other metals which do not so readily fuse, or
they may be frozen water. All the simple bases which are
gases when free in our atmosphere at the temperature of our
earth, which is still hot below the surface, may in a colder
world be condensed, like specimens liquified by pressure and
now kept in glass bottles in Edinburgh. They may have sunk
into crevasses, or they may have frozen, like fluid carbonic
acid, which turns to snow. ^Yhile all are at sea, each cap-
55S Sl'ECULATION.
txain must niauagc his (nvn boat, and keep his course as best
he can.
It has been truly said that " science is but the removal of
the unknown to a greater distance," and " that, to a clear eye,
the smallest fact is a window through which thi' infinite may
be seen."
We who are at sea in the great unexplored ocean of
truth, and surrounded by an infinity of thick darkness, can
do little to help each other ; but each, according to his lights,
may remove the dark unknown by some small space. Even
though the result may be less than a spark, the strongest
human light is good for little more out at sea.
This is the sum of all that has been said, and it must find
its own value. It is but a problem after all.
It seems to follow, from all that has been observiid, tliat
there are in nature two opposite forces, or sets of forces.
If there be such a thing as matter, and if it is diffused
through space, and if gravitation alone acts upon it, then
matter ought to be converging on a point of attraction. It
ought to move at increasing velocities in straight lines, like
grains of dry sawdust thrown on still water, oi- like bubbles
of foam, whicli attract eacli other and accumulate in discs.
Matter ought to be gathering into one great sphere com-
posed of concentric layers ; but, so far as we can see, this is
untrue.
If, on the contrary, a force diverges from a point towards
which there is no attraction, then matter is receding from the
point and accumulating at increasing distances as a liollow
shell. But this also appears to be untrue.
If a centre of attraction becomes a centre of re})ulsion,
then facts observed appear to hang together and make a
Aehicle for thought. The larger the sphere accumulated by
SrECULATION.
559
force of attraction, the greater is the force which compresses
the mass.
Is that force of attraction converted into rays of heat and
li;jht, and of force ojyposed to gravitation and hearing some pro-
portion to the mass ?
While two forces are balanced there is always rest ; when
one gets the mastery, motion results. When rays overcome
weight, when fire beats frost, certain results are observed to
follow, and amongst these are — rotation, and projection of
smaller masses, which have independent centres of attraction
and radiation, and which continue the same process, from the
earth and meteors down to the smallest spark.
Is this good law ivherever light shines, or mag shine ?
If so we are no nearer the end.
What is the cause of radiation and gravitation ? What is
force? We cannot even see the next links in the endless
chain of effects and cause ; but through every little fact " a
clear eye may see the Infinite," and acknowledge the will of
Him who made all things, and who said, Let there be light,
in the beginning, when he created the heavens as well as the
earth.
Many minds are avowedly working out of bounds.*
Having for years watched ideas on certain so-called
powers, the writer still firmly disbelieves nine-tenths of the
stories told about mesmerism ; all that he has heard or read
* See books on " Siiiritualism," and ordinary every-day conversation on
suck subjects ; certain chapters in JVew America, Hepworth Dixon ;
Eeichenbach's Eesearches on Magnetism ; Letters on Animal Magnetism, Gre-
gory ; Mesmerism in India, Esdale ; chapters on Mental Phenomena in The
Gay Science, Dallas ; papers on Biology read at Nottingham, 1866, sec. D ;
papers and books by Tyndal, Lyon Playfair, Darwin, Huxley, etc. ; The Reign
of Law ; Frost aiul Fire, vol. i. p. xiv. etc. ; vol. ii. pp. 273, 274, 4-38, etc. ;
text-books on Law, etc.
fHai.\ liJluj
^
500 Sl'F.CULATTOX.
about " clairvoyance," " supernatural furniture," and " spiritual-
ism." He has seen a table turned, and he saw why it turned ;
lie has often heard an honest inquirer after truth unconsciously
tell an arrant knave the answer to a test question, and accept
the answer as evidence of clairvoyance ; he has often detected
self-deception, and by way of experiment he has often deceived
others by the simplest contrivances ; he has found out some
gross humbugs, who were doing real mischief as " spirit-
ualists." But, in spite of all this, he has been convinced, on
evidence which seems conclusive, that some men do in fact
exercise some influence over some others, by which the will
(jf one man for a time controls the sensations, bodily actions,
thoughts, and will of another.
Very instructive experiments are described by Eeichenbach.*
When a strong magnet was approached to the hand of
Mademoiselle Novotny, while cataleptic and insensible, and
even at other times, the hand " adhered so firmly to it," that
she " raised herself in bed," till her body could not be further
bent, when she was " compelled to let it go." She described
her sensations as "an irresistible attraction which she felt her-
self involuntarily compelled to follow, and which, even against
her will, she was forced to obey." The language hovers be-
tween active and passive moods, but other sick girls were
attracted in the same way by magnets and crystals. Some
persons thought that the magnets felt heavier by the weight
of the arms which were raised, and the hands which grasped,
and no doubt they did ; but Eeichenbach clearly means to
tell the exact truth, and he tested his conclusions by experi-
ment. He found —
Isf. That fingers which were attracted by magnets did not
move a grain of iron-filings.
* P. 24, Resmrchcs on M<i<jiuiifii)i. Ijoinloii, 1850.
RPFX'ULATIOX. 501
2*/. That they did not move a magnetic needle freely sus-
pended.
od. That the largest magnet, when hnng to a beam and
balanced, was not attracted towards the hand, which struggled
to rise and grasp it. The tongue of the balance did not stir,
though the learned professor used force equal to ounces or
pounds to hold down the liand of the patient whom the mag-
net attracted. He concluded " that there is nothing ponder-
able in the attraction exercised by the magnet on the hands
and feet of cataleptics." If magnets, crystals, etc., really
acted at all in these cases, they acted on the unknown forces
by which matter acts on mind, mind on matter, or mind on
mind. They did no more than magnetic needles did when
they " solicited" the will of the man who got a telegram from
another whose will set matter moving between them. The
Mill of A, acting through matter over which it has power,
informs, solicits, or commands the will of B, and sets it to
work through matter, which first acts on the immaterial,
and then is acted on by it. But the master who rings a bell,
and gives an order which is obeyed by a servant, works
by the same power, and the gap between mind and matter
still gapes as widely as it did before Eeichenbach w^rote on
Odyle.
As a " subject" the writer himself as yet is unvanquished ;
as an operator he has never gained a single advantage over
the weakest subject ; and he knows that he may have failed
to detect some fallacy in the cases which he now believes to
be genuine. But the deception or delusion, if such it be, is
now so widely spread that it must be noticed on the border-
land between knowledge and utter ignorance.
Even cautious thinkers are driven to ask, What are " laws
of nature?" How comes it that wills govern where laws
^>G2 SPECULATION-.
are said to " reigii ?" How do wills change the order of events,
and construct engines with inert matter, and with them
control material things, and other wills ?
INIen, like other created beings, must, and do in fact, obey
the " laws of nature," which they can neither alter, repeal,
nor resist; but, nevertheless, human will "reigns" within
bounds which enlarge with knowledge. Every voluntary
human act proves that will acts directly on matter ; for a
man's will, so long as it has power, acts directly on the sub-
stance of his body, and that action spreads.
At the will of a glow-worm light radiates, and other crea-
tures see it. At the will of certain fish electric force is set
free, and others feel it and die ; heat radiates from bodies
at every action and at every thought. Articulate waves of
sound, which are words, are produced at will, and words
are audible thoughts. Thoughts take visible form when
written, and thoughts spoken or written spread like waves on
a still pool, which a pebble disturbed, because it was the will
of a boy to " throw a pretty stone into the water" forty years
ago. These tiny waves have lived in a man's memory, and
are now converted into this shape. A merchant's will at
work in London now vibrates fast and far, and gets answer-
ing waves of thought in a visible shape from Calcutta or
from California in a few hours. Two wills at work at
Washington and at St, Petersburg vibrated in accord, and
agreed to exchange Eussian America for dollars or ships.
Then the wills of speakers and hearers, writers and readers,
telegraphers, printers, and thinkers, throughout the civilised
world, set to work to turn thoughts into sounds, and shapes,
words and letters, waves of electric force, flashes of light, new
thoughts, and symbols which spread thoughts far and wide.
These waves will reach the savages at last, and they may
SPECULATION. 5G3
— «or ItQclily ills. Tlic first thought in each series crossed
^•spel a ine!„ I'^'oistrV „^}*'ii-- before it started nerves and
^ j^^ =^Si£!|^S/'-'.Voj', and mental,
^iSr '?*«o St;'r'"^^^^ ?« «o„ ago, and have
••^^SS|FHl:iH^^iV;^;-soles,ne.e.
and brains. But a£'^''eiV£''^. ^^'^'^ '^^n.ctlTfr.'l ^^^^^ ^^^ ^'^"^8'^'^
or thought, or can imagine, cannot even cp^jroach the chasm
which divides mind from matter, and is passed by every new-
liorn thought. The will of the lowest of living creatures must
leap that ditch ; yet mind and matter act and react within
the wisest of men, they know not how.
We cannot pass back over this narrow grip from effect to
cause, so we cannot hope to cross the great gulf which is
beyond it ; but we can perceive that Omnipotence may move
all matter by mere volition. We move matter by mere volition
at the first link of the short chain of cause and effect which
science found, and which we call " laws of nature." Within
bounds, and during a short reign, a man's will governs " laws "
which " reign " over matter. Beyond is the " supernatural,"
and the relation of " laws of nature " to something greater.
For illustration, human laws may suffice. On the outer
shell are unnumbered laws by which the nations of the earth
are governed — a maze of seeming confusion and contradiction.
Under this net of clauses, acts, and codes, are principles. In
the inner layer — which may be seen through the outer net —
many rights are opposed by many ivrongs, for which laws pro-
vide remedies. But all these may be reduced to UIGIIT and
r,G2
SPECULAT[OX.
are sfii
and (
contrc
M
the " 1
nor re
bound
' *ThV'"amekican3 in AiiLWA^-The way ouj^
mmmmM
fh^liij
,T^
regio
SC ff hut'AlTa n to eT;=ute the people.-as they plac.
This 18 altoKcthe? shocking,
hat h,'
]uiniai» sor^time'Igo-^ithdraw our fcioops froiu Alaska alto.
, 5 cett^rTf they cannot govern it ?yithouSWling off th«
man's 1 f^l icVfingered Kakes who give life and diversity to lU
- v^t bLw loj-ered soUtudes.-iVei« Y^rk Tinm. .
..„_. J.* :_-."..>.. ..v^Liuii .-spreads.
dow-worni liirht radiates, and other crea-
^ ft
stances I
At the will of a _
tares see it. At the will of certain fish electric force is set
free, and others feel it and die ; heat radiates from bodies
at every action and at every thought. Articulate waves of
sound, which are words, are produced at will, and words
are audible thoughts. Thoughts take visible form when
written, and thoughts spoken or written spread like waves on
a still pool, which a pebble disturbed, because it was the will
of a boy to " throw a pretty stone into the water" forty years
ago. These tiny waves have lived in a man's memory, and
are now converted into this shape. A merchant's will at
work in London now vibrates fast and far, and gets answer-
ing waves of thought in a visible shape from Calcutta or
from California in a few hours. Two wills at work at
Washington and at St. Petersburg vibrated in accord, and
agreed to exchange Eussian America for dollars or ships.
Then the wills of speakers and hearers, writers and readers,
telegraphers, printers, and thinkers, throughout the civilised
world, set to work to turn thoughts into sounds, and shapes,
words and letters, waves of electric force, flashes of light, new
thoughts, and symbols which spread thoughts far ami wide.
These waves will reach the savages at last, and thoy may
SPECULATION. 563
suffer bodily ills. The first thought iu each series crossed
the gap between will and matter before it started nerves and
muscles, telegraphs, and other trains material and mental,
which will go on quivering and spreading, like the waves on
the still pool which rose and fell forty years ago, and have
now taken the shape of written words. We are taught that
heat is evolved by chemical action in food — that it is con-
verted into other " modes of motion," or " forms of force" —
and is applied as power to living engines, which work, and
which grow, with all their mysteries of bones, muscles, nerves,
and brains. But all that the wisest brains have yet taught
or thought, or can imagine, cannot even approach the chasm
which divides mind from matter, and is passed by every new--
born thought. The will of the lowest of living creatures must
leap that ditch ; yet mind and matter act and react within
the wisest of men, they know not how.
We cannot pass back over this narrow grip from effect to
cause, so we cannot hope to cross the great gulf which is
beyond it ; but we can perceive that Onmipotence may move
all matter by mere volition. We move matter by mere volition
at the first link of the short chain of cause and effect which
science found, and which we call " laws of nature." Within
bounds, and during a short reign, a man's will governs " laws "
which " reign " over matter. Beyond is the " supernatural,"
and the relation of " laws of nature " to something greater.
For illustration, human laws may suffice. On the outer
shell are unnumbered laws by which the nations of the earth
are governed — a maze of seeming confusion and contradiction.
Under this net of clauses, acts, and codes, are principles. In
the inner layer — which may be seen through the outer net —
many rights are opposed by many wrongs, for which laws pro-
vide remedies. But all tlicse mav be reduced to lUciiT and
564 SPECULATION.
WRONG, and these oppositcsto the AVILL of Him whose will is
" Law " and " Eight."
So in material things, those who seek find, first, unnum-
bered forms and a maze of movements which are hard to
unravel. These seem to result from unnumbered forces ; but
those who search further, dig deeper, and look through the
outer maze, find attractions and repulsions forces which may
hereafter be reduced to radiation and convergence, " rays and
WEIGHT." Between them " clear eyes " may once more " see
the infinite," and discern the WILL of Him whose will is
"Law," and w^hose will is also "Force," which moves matter
and shapes it.
In both cases the " reign of law " must come to mean the
reign of the Lawgiver.
, ^aj It seems to be His will to govern His creatioiiby a sequence
^---y^-rV^ L of cause and effect, and to permit His creatures — created
according to his laws — to learn some of them ; and by them.
/ , within bounds, to govern by WILL.
/ J i But what is matter ? Does it exist ? Is it a maze of force.s_
/ ' which can all be reduced to the WILL of Him -who made all
If so, we shall all move towards the same point if we travel
from effect to cause.
Towards intelligent will, as the cause of causes, all roads
tried have led, so far as this traveller was able to go. By this
distant pole-star he set out to steer in the infinite darkness
which covers the unexplored ocean of truth on Avhich he has
now ventured so far out of his depth ; by this light he hopes
to reach land in the end.
And so he leaves this rude chart of his course to better
men, who, like liim, arc setiking ti'ulh. Tiie Ijeiter and tlic
.stronger men are, the nioiv tliey syiiii)athis(' witli the honest
SPECULATION. 565
efforts of weaker brethren ; so tlie author of this book now
ventures to hope for indulgence if he has erred, because he
has worked as honestly and cautiously and as hard as he
could, and because he has always found the gentlest critics
amongst those who know most, and who most deserve the
respect which is due to superior knowledge. If acquitted of
presumption by these, the author will be content.
ADDRESS
SIE WILLIAM ARMSTRONG,
C.B., LL.D., F.R.S., &c.
y/LC Oyo,-iVUu O^ccw^i^ SLe^iX^^ 9hii^_
PRESIDENT
INSTITUTION OF MECHANICAL ENGINEERS.
NEWCASTLE MEETING.
1869.
NEWCASTLE-UPON-TYNE :
PRINTED BY J. M. CARE, 21, LOW FRIAR STREET.
. 1869. ^y 1 *
mi
Ik dr^tti
«9f«
%l
SEW YORK, riJIDAY,
JANUARY 20,
i8?i.
OUTSmK RRADISG MATTKK,
yiEsr Pagu Chisleliarat : Iit'C(^^lections of to Im-
poiJAl Houa.e ol Uefuge; » Tale or Mardcr— Opiulon In
irance: Letter fioni M. Laboul«ye-How to WtttTTir
I'ariB— Mnsica) NotcB-Olp-anlnfrs-Foreii^n -tiossip—
The Land of Rcfngc- A Tale of Sorrow— At Sea la a
Oydone: A Chmttnas of Torn -Europe: La'it NigWs
• 'ftWe Ad>Tn-pa-Difi Kaohaiiah Write Uie Book orZ4cJj^
Hlif-ThoTraueroiuiaUoa of Paris: An Unpleai
hftngc.
Fprirru PAGE-Third and Fonrth EdlUoa roadiji^
aiatter.
DISCOVERY OF GLACIERS ON TKE PACIFIC
COAST.
At the regular mectini? of the ConnQcttfiutt I
Academy, iu New Haven, on \Vodno8<lay
evening layt, an iufonua! but hiftlil/ impor-
tant communicuiioa was made by Mr. Clar-
ence King concerning sorao recent discoYericb
upon the fnraous peaks of the t'ncitic. con«t^
Mount Shasta, Mount Rainier and. >roant Hood.
It would be hardJy fair, witiiout; iiis i);uthori '
ty, to attempt to gi»».-.a-.miai:^fip^<^A.
cotint of tbeso obstirv.itiouB, :bui^,l«».TO
can be no impropriety in r€'portij9§f_ that '
dtiiiafi: tliolast aatumu Mr. King atj^jhi^Ay-
fiociates, in thiee partiop, uijjcovcrcci fcLo c i
i»*tence of active pjlacicr.-* whoro ti^py. havtfl^
never bofore bf^en noticod, on tluv licrtliern '
siopos of Mount Shasta in CaliforniftiiH well
as on Mount Kninier in VVafh'^i"^'- r '
Mount Hood iu Orugnu. Anotlf i
hopes to pnrsua thesy insj^iurios i : ..■ r
-notth as Mount St. Eli5»j.r ' \
ThiB is the first in9t'Ha^v.)a niluot^
all the territory of the United StRt«»><AIa8ka,
of course, excepted.)*' live glaciers'' have boon
louad, though lu tho East, as well as in the
Wofet, tbera ar? TO^iany indications of 'j\&.-
oial a6tion iu former frioloyfical epof^wa "wiKi**
fflaeii^rs now detected (on Moant Slrai>tR,» at
least) Luvo hitherto teo{vi)ed the nofetc«rf>f
thos^wlip have climbed tho p^ ak; bgjagao.
:\l.:li .,..-C^i... ..... ...:Oi. .........: ......il tluj jOlMK|'
ern elope. Mr. King, by his geolo^IcsHt,
r<'8<'arclie8 in tlie -West,' had' .bo^nj
led to sHripei't tlio cxistouce oi a-ctistoi
glaciorH, nad as jmrt of the work of ernlom. ■
tion whicli ke is doiug for tiio United Scates!
gotezTimcmt, lindcr Major-Cfouoral flami-h-
reye, chief of the Engiuoer Corpg, ho planuotl
laet sutnmer. 'a gr'acicr a«arohiu<{ paity," or-
ganized bis company, made th&A3Con*s on the.
northern instead of tho southern elopos, and
haa.boon rewarded by tlie brilliant discoveries
now recorded. Ho himsolf went up Mount
Shasta, with Mr. Clark, while Mr. Emraoag
Mcd Mr. Wilson were exploring Mount Rai-
nier, aud Mr. Hague'went up Mount IIo;>d.
Theso gpnilomnn arc all momtiGrs of the
government patty orgauiii'Al f'acth^ si^fYOyp/
the fortieth paralh'd, and are ntow in New^
Haven workinjr up tho rf'siiU.-^ of Ihoir labors
in the .field. Mr. Jamcrf T. Crarducr, next to
Mjji King in the conduct of the gur^'ey, has
been for many months "j»ast at work in the
«>i»;paration of the topographical " maps
ikii- publication. The report ot thL-j ex-
pedition on thii minini? industry in
Jscv^da and Colorado, by Mi-". Jaraos l».
TFftgHO, UJinincT sncfiaoer, in neasly ready to be
oni'lishod.
Mr. King's career is a good illnstratlon of
the value of the new education as it is .snniq-
t'tncjj fjiifrlitinjjtiy called, or as we prefer to
gay of the value of good trainiutj in modfjrn
■bcieaoe. Hn i3 a young, enthusiastic, active
iind ;n<(aisitire etudent, Tv'ho was graduated a
i'ewVeara ago from the Sheffield Scientific
-J?chc<jl ot Yale College. Hero he had not only
laid'gcixl foundations in Kevoral branches of
.-Vieacc, but uq received a beat tov?ard geo-
logicul invefctigation, and a concopfcion of the
rl^ht methods of research, which led him as
soon as his college diploma was won to push
oat t^ Calltornia. Through Profoysor Brewer,
one of the earliest graduates of the Sheffield
pchool, and ouc of the uicjt successful scienti-
AiO '^ mountaineers " and bvtaaiata in the
country /Mr. Kmg became a " volunteer aa-
cistant " under Professor J. I>. Whitney on
the geological aiirvey . of (Jdlifornia, with-
w'uich Mr; Biower waa connected as botanist.
While in this service ho had tbd energy to
climb to a higher p6infc in the Sierra Neva-
♦ia than had been reached by any
one else, to dipcovev a peak which U
atill regarded by the knowing ones as
tho lol4i(^tjPC^t yet dcteE*»iircd 'u the limi,t8
iERS.
ine of
i
J New-
' occa-
;n any
ilien, I
ying a
h who,
'ed and
linking
, model
mathe-
Watt
?tect a
w that
■ed its
jl heat
I steam
ased in
' sepa-
" he set
a of a
s soon
of the United States. Tliid point is known as |p^„:„pj „
Mount WJiitneT. Hia6e IjIs ronn«f;tiQa with /
, vacuum,
the piston
iide. An
d for thirs
cad of air,
ipplic?.ble ;
Mount WliitP.ey.
the California Furrej tcrmln--. ' '■ '■■--• heea jn Engine,
<ii the iorvico iiflTlo 'Unit cxn
icf'iit in the Purvey'&lreRfiy r titlio
fortieth parallt-l, tfaal ia to say of tiio rogioa
adjacent to tho- Union and Central Pacific
railroads. .
Mr. Gardner, his friend and associate in
tlieae works, a kin;lrcd spirit and an admi-
rable worker, received a part ot his traininj^
in the Renssaiaer School at Troy and a part
in New Haven, and among' their scientific 'G accurate
comrades are several more who have boon flt- ]y steam-
ted in New Haven and elsowhoro for the . ,
•work of scientific explorers, and for the carelul t.lian the
examination of the actual and possible cUarac- ead of his
texietics of that vast western rc-jioa over , i
. I • * • .? J CO! k, in-
vi hich onr coantry men are so rapully gpcead- j
lag. , _ ' ? have no
existence. With ailing health, narrow* pecuiiiarv ji-ipnris,^,
and a temperame^*ugd.t 4.^ ^^^^ EmT-oTo^' tirt: ■Afs;^^'^
many respects, UI Sir,— Oboerying lo r/i* rtwM the reported •rtVaaflWf'il:
I 1 Her ji^Jesty's fihip Me^cuni on the islaml of St. Psal, iM
ne was a man Wnt^^^ ladUa Oce^o, and tho fortunate laoding of the passen-
and he could not JgersuQ^i crew, tboujjh upoD so utterly destitute aod barren
. .a rock, I hasieu to co.uuiuuioate to you, ia the hope of
and fine intellect miti^atiDg pamful aaxietiea of the relatires of the ship,
SUDCrior in static"'^'"''""^' ^" "^"^ ^^ should be assumed that no prorisioDS,
1 ' ' &c., could be landed with the crew, as to the local resource!
those flieilds, Wl for obuiuiQg food aud -water, that some few years since I
. . ^ visited St. Paul's Ulaod, oq tny way to China, being anxious
once Ills severe ^^^ dcterimue Its lon-iiude, which differed in various re-
Dulse to DrOCeed '"""'''' ^^ •"'*" extent of 20 miles. This small island, only a
^ _ few riiilcs !'■ cir'"iiinf»reuce, is cridently the remaiui of hq
a condenser with exiioct volcanic crater, the edge of which has on one side
brokeu duwn, Icaviu^ a water passage from the sea into the
crater, wuich rorms, as it were, a harbour for small ships.
a century ao'O tl AUliough destitute of springs of water, cattle, trees, or
* ' uselul vegetation, yet the astoniihing resources of its sur-
liniSlied and put roundiuj watms m Urge Hsh and erustacea enabled u», whea
W^ntf in •! <?pnlnr fi'*'^'"" lusile the crnter, to procure a vast supply in a few
but it was not
boii«, tiie catch being so great as, indeed, almost to endau-
Dr. Roebuck, net gt^r the larse boats.
, . As to the supply of water, assuminf; that none could
mere WOrkin<T mc ^e landed from the ship and none could be caught by
awiiiogi, &c , I would ob^ervo that no doubt ailvan-
tage would bo takeu of the followiuj remarkable ciroum-
sta'icu :— the soil and the beach on the level the sea ijj
the crai.er ii so hot that, when bathing and standing in the
watT upon th» »and, the feet could not be allowed to sitik
into it beyond an inch or two without pain. The high tern-
perature in tho sod on the beach would euable a supply of
fresh water to bt obtained fi'oin the sea by distillation, by
Kinking «oiaeof the ship's iron tanks or contlensers into the
intensely-bealod ground.
It had a cylin(
stroke of 5 feet ;
described as the
duce, were still
t or supply of fuel for -ulinary purposes, there is a conal. The Engine,
derablo quaatily of driftwood upoa the nlaud although ^
thousao.U of taibs -listaDt from the mainUnd ; but, sliouid I Ot me \ aiue Oi
tLk fail, food could be cooked by cte great keat of the soU . ^^ ^^^ happy
th"..so woQdertuUy provided iatnid-ooeau. I would or.ljr ^ _ f W„f+
add that tl.e island has high, abrupt sides, aud a central ; gemUS Ot Watt.
plateau which is not acted upoa by the heat appareotm the ^^ , ^^ j,t
lower strata, and as many vessels sight the islaud.and others JUiuuii ^
pa38 at so'Be distance fr.,aiit, I doubt not that our country. .^^ cylinder, the
raea have long eince be- ---d. ^^^^.^^^ ^^^^^^^^ ^^ ^^^^^ achieve-
n/'' AKTHUil A. UOUHRANE, Rear-AdmiraL . .
Ciu-/r- _ .uu^e Domiiivp fiavs of mechanical engmeermg.
I TO^HE EDITOR OF THE TIMES. Newcomen, only
Sir,— 1 Lave just, read in your journal the telegram »n« , 1 ,
nouGcinj; the striading of the above vessel on the Inland of y SaW by Wliat
:^t. Paul, in the Indiau Ocean. . . , , . ible for rotative
A.3 tiua singular volca»ic isle is not often visited, adescnp*
tion of it may not be out of place at this moment, partica- tions, comprising,
Urly to the friends and relations of the crew and passen. t> n /-i i ^
,n-s of the iiifated ship. Ball Govcrnor, he
I visited the inland on an outward-bound royaje som« ,le-acting rotative
year'* siuotf, find althouiih it ^aa then uninhabited and . .
bairen, it still offers the means .if sustaining life by meat« purpOSe requiring
of the abundance of lish to be found in the Crater Basin. ,-,porlv itS Orio-lnal
! Thi^ romarKable basin is about two nailea in circuit, and hat "^ °
30 fathoms water in the aiiddle, which depth is maintained ed by man.
until within M feet of the shore. The rocks round thq ,
crater rise to 600 or 700 feet hi-h, and the view from tha tt, WC mUSt COn-
feuuimit is very impre»sive. All round the edges of t^ifl oKoured In the
basin smoke was rising', amid the stone? liaiog the shore, '
indicatiug iliat omoai iering fires atill lurked below. On ,ble in a COQStrUC-
lauding we fouuil the water on the shore of the crater in p -. . 1 in
some pUcea too hot to permit our hands remainiug in it fo» ^ ClCVlCeS TlSCa
Kuy length of time. The temperature by thermometer in ;• iiiechanical COm-
the hottest part was 204 deg. Great fun was created by , . i j. M
atchiiig fish at uue end of our boat, and, without taking in minutC detail,
1 hem off the hook, letting them drop into t*** ''^t water, •ijj.-^ xJq hSid
aud eookiu^ th-^m. Should any of your readers doubt this '
f tat«iiient, I refer them to Horsburff's Sailing Directions ta nOW choOSe frOm
Ihe East, audto Vlemnaiog, ihe Dutch navigator who di*. . „
covered Che island in 16!>7. 'ICe ot mcanS WaS
Should the Mnjiaera have been so unfortunate as to lot* f Tyoo practicable
her stores in attempting to land them in the heavy surf ' ^
that beats upon the shore, coosiderahlo sostenance may b« If "WC glVC dlie
obtained in the Crater Basin, for the fish are plentiful and -it , oniafp
t'wd eatinc, and a natural tish-kettle U always at hand anij '® ^"^iC tO appreciate
boiUng. Seals, alKO, are plentiful. g^j^J ^\^q Sagacity
Tlie entrance to the Crater Basio is about pistol-shot wide,
but across the throat there is a bar composed of pebbles,
lover which nothing larger than a boat can pass, »odIb»-i f -i. -^ mar-
llieve this is the ouly practicable landing-plaoe to be found.
;A strons currr.ut sets over the bar, and at half ebb it ijhe COuld have had
diflScult to jiet h-iats over, but once passed smooth water is -, , ,. i j-
i found in the ba«-- Ito realize belore
I It is to be hopo.^ ♦•'■^refore, that the iufferiogs of thi g existence. It is
I .-rcw "-'! pa-.seiig'*'" 'T the Megajra may have been consider^
'a'-'.v alleviated by the na'ural resources of the place, and i^
1 IS witti a d'"')"* of qn eting aijpr'hetisioos upon thi^ point
thiit I trouble you, with V.iDte remarks. JC,*?/
' I aiii, Sir, yours oneilientlv, iw/ 1
Haro Hotel, Dover. Au^. 4. ROBERT POSTANS.
impossible to contsmplate these results without feelings
of enthusiasm. To appreciate how much we owe to the
Steam Engine, we need only cDusider, for a moment, what
our position would be if we were deprived of its agency.
The factories which clothe all the nations of the earth
would be almost extinguished. The deep mines which
supply nearly all our mineral wealth would be abandoned.
The manufacture of iron would shrink into comparative
insignificance. Horses and sailing ships would again become
our only means of transit. All great engineering works
would cease, and mankind would relapse into that con-
dition of slow and torpid progress, which preceded the
subjugation of steam b}?" Watt.
Having thus, in honour of an inventor, whose name will
grow greater as the world grows older, referred, in general
terms, to engineering progress during the last hundred
years, I need but glance at some of the more recent
achievements in mechanical and constructive art, in order
to shew that the extraordinary advance . of the century
continues unabated. That such is the fact, will at once
be apparent, when I remind you that during the short
period of eleven years, which has elapsed since the Insti-
tution of Mechanical Engineers last held their annual
meeting, in this town, the Atlantic Telegraph Cables, the
Suez Canal, and the great Railway across the American
Continent, exceeding in length the sea passage from Europe
to America, have been added to the engineering triumphs
of the century. Of these, there is but one of which Eng-
land can claim the glory, and that is the first successful
Atlantic Telegraph. The recondite science involved in
that undertaking, the boldness of the enterprise, the perse-
verance displayed after the first ftxilure, and the moral
effects, as yet but partially developed, of its ultimate
success, justify us in regarding the first Atlantic Telegraph
as one of the very greatest and most honourable achieve-
ments of man. But Englishmen may feel additional pride
in reflecting that the successful laying of that cable, as
well as of the subsequent French one, just now completed,
was chiefly due to the fact that there had been previously
completed in this country, a steam-ship of such gigantic
size as to be itself one of the greatest wonders of modern
engineering. Thus it is that one great invention hangs
upon another. First came the Steam Engine, then followed
the great Steam Ship, and finally the Atlantic Cable, which,
without the aid of steam, could never liave been laid.
The Suez Canal presents another example of the direct
application of the Steam Engine to the execution of one of
the most remarkable of modern works, the chief part of the
Canal having been executed by Steam Dredgers, of which
an interesting description was received by this Institution at
the Paris Meeting. In contemplating this undertaking, we
are naturally led to compare it with the great neighbouring
relics of Egyptian antiquity. In quantity of material
moved, the Suez Canal is far more vast than the great
Pyramid. In its moral and intellectual aspect, it is im-
measurably superior. The ancient Avork is a useless monu-
ment of the idle vault}'- of a tyrant ; the modern work will
bear witness to the practical science and utilitarian spirit of
our better times. Surely the world improves as the dominion
of mind over matter is extended.
I should lengthen my observations too much if I were
to review the many new and important applications of
machinery and mechanical processes, effected since our last
meeting here. The manufacture of iron and steel — steam-
cultivation — mining operations — steam locomotion, by land
and water — economy of labour and of time — economy of
fuel — printing — and even the humble business of the semp-
stress, have all been facilitated and promoted by recent
mechanical progress.
The subject of Coal follows, naturally, a notice of the
Steam Engine, and has a special interest for us, in a
locality celebrated, since the earliest days of Coal mining, for
the production of that invaluable mineral. England, with
her innumerable Steam Engines and Manufactories, is more
dependent upon Coal for the maintenance of her prosperity
than any other nation, and the question of the duration of
her Coal Fields, now, very properly, occupies the attention
of a Royal Commission. The investigations of that Com-
mission are not yet completed, but, so far as they have gone,
the results are re-assuring. I concur in the probable accuracy
of the announcement lately made by two of my fellow Com-
missioners, that the total quantity of Coal in this Island will
prove to be practically inexhaustible ; but until the complica-
ted details of quantities collected by the Commission have been
put together, and expressed in totals, it is difficult to judge
with certainty or accuracy on the subject. Although the
duration of our Coal may, geologically speaking, be practically
unlimited, we have still to consider the important question,
how long will England be supplied with Coal, as good and as
cheap as at present ? We have, unquestionably, made greater
inroads into our best and most accessible Coal beds than other
nations have done into theirs; and if foreign Coal should grow
better and cheaper, and ours dearer and worse, the balance
may turn against us as a manufacturing country long before
our Coal is exhausted in quantity. It is clear that our
stock of good Coal is very large, but most of it lies at great
depths, and one of the most important questions the Royal
Commission has to investigate, is the depth at which Coal
can be worked with commei-cial advantage. The chief ob-
stacle to reaching extreme depth is the increase of tcir.pera-
ture which is met as we descend. I am justified, by
ascertained facts, in saying that this rate of increase will, as
as a rule, prove to be not less than 1° Fahrenheit, for every
twenty yards in depth, and there i3 reason to expect that it
wiU be even more rapid at greater depths than have yet been
SI
attained. The constant temperature of the earth, in this
climate, at a depth of 50 feet, is 50° ; and the rate of increase,
as we descend, is to be calculated from this starting point,
Adopting these figures, you will find that the temperature of
the Ciirth will be equal to blood heat at a depth of about 980
yards, and, at a further depth of 500 yards, mineral sub-
stances will be too hot fur the naked skin to touch with ira-
punit}'. It is extreme!}'' difficult to form an opinion as to the
maximum temperature in which human labour is practicable
in the damp atmosphere of a mine, and it is almost equally
difficult to dt-termine how much the temperature of the air,
in the distant parts of an extremely deep mine, can be reduced
below that of the strata with which it is brought in contact.
It is certain, however, that the limit oi practicable depth will
chiefly depend upini the mechanical means which can be pro-
vided for relieving the miners of the severest part of their
labour; for maintaining a supply of sufficiently cool air at
the working faces of the Coal ; and for superseding the use
of horses, which suffer even more than men from highly
heated air. For the relief of labour we must look to coal-
cutting machines; for improvement of ventilation to exhaust-
ing fans ; and for the superseding of horses, to hauling en-
gines driven by transmitted power. The employment of coal-
cutting machines, working by compressed air, convej'ed into
the mine by pipes, is already an accomplished fact ; and when
the difficulties and objections which usually adhere for a con-
siderable time to new mechanical arrangements, are removed
from these machines, they will probably attain extensive
application. One of the earliest attempts at coal-cutting by
machinery, was described by the late Mr. Nicholas Wood, at
the former Newcastle Meeting of this Institution, and all the
really practical results as yet obtained, date from that period.
The cooling influence of the expanding air as it escapes from
these machines, will be a collateral advantage of considerable
importance in the hot atmosphere of a deep mine. The air
It)
discharged from tlie pneumatic coal-cutting machines, now
in use in tlie Hetton Colliery, escapes into the mine at a
temperature of seven degrees below freezing, and the cold air
from each machine appears to be sufficient in quantity to
lower the temperature of the circulating atmosphere by one de-
gree. If, as seems to be probable, six or seven of these machines
can be employed at each Avorhing face, we may, by this means,
lessen the heat by a corresponding number of degrees, and
thus afford very considerable relief. The employment of
compressed air, as a motive power, in substitution of horse
traction, is also quite feasible, and may be expected to become
general in very deep workings. As regards ventih^tion,
the fan machines of the several constructions tried, have
alread}'^ exhibited great superiority over the old method of
ventilating by an iipcast furnace shaft ; and although the
efficiency of the furnace system of ventilation is increased by
depth, there is reason to believe that the fan will maintain its
superiority to greater depths than are likely to be reached in
mining.
Thus far I have spoken of Mechanical Engineering as
applied to purposes of production. I have now to refer to
it as connected with the opposite element of destruction.
When battles were fought hand to hand, war, so far as
Mechanics are concerned, was an affair of muscuhir force, and
was, in that form, the most sanguinary, because combats
were the most close. When other forces were called into
play, inventive appliances became necessar}^ and these, as
they have advanced, have more and more widened the
distances separating combatants, and have thus operated to
prevent that greater sacrifice of life which would have other-
wise resulted from the employment of more destructive
weapons. It is, therefore, not to be supposed that future
wars will be rendered more murderous by the intervention
of the engineer. On the contrary, we may fairly anticipate
that, the more the element of intelligence supersedes that of
11
animal force in military struggles, the more will the barbarity
of war be mitigated. Science naturally sides with civiliza-
tion, and tends to establish a supremacy over barbarism;
and we find this tendency, as in the case of the late Abyssinian
war, not only giving overwhelming superiority to the cause
of civilization, but deciding the issue with the least possible
waste of life. But, whatever our sentiments may be in
regard to war, it would be absurd to contend that Ave ought
to withhold from invention when the object sought to be
attained is the destruction of life and property. It is
our province, as Engineers, to make the forces of matter
obedient to the will of man, and those who use the means
we supply must be responsible for their legitimate applica-
tion.
It will be in the recollection of the members of this
Institution, who visited the Elswick Works on the occasion
of the last meeting at Newcastle, that two or three small
Breech-loading Rifled Guns were shewn to them as novelties
peserving their attention. Those guns had then very
recently received the recognition of the British Government,
and may be regarded as the small beginnings of a system of
ordnance, which has since attained a very extensive adoption
in this and other countries.
It was not until the principle of rifling was adopted for
Military Fire-arms, that these weapons presented much scope
for the mechanician's art; but the introduction of rifling,
and the change in the form of the projectile from a sphere to
a pointed cylinder, brought about a complication of new
conditions which it has required years of research and ex-
periment to meet and satisfy. Passing over the subject of
Rifled Small Arms, which, of late, has called forth a great
amount of ingenuity and skill, I will speak of Artillery, as
being that division of Gunnery with which I am personally
connected.
The most important of all the considerations affecting
12
Modern Artillery is how to obtain the strongest possible tube
mth the least possible weight. Before I state my views as to
the best mode of attaining this object, I must call attention
to the conditions affecting the force to be resisted. When a
charge of powder is fired in a gun, it is converted into gas at
an exceedingly high temperature, and the pressure exerted is
due, even in a greater degree, to the heat, than to the quantity
of gas produced. But the heat evolved is not wholly realized
in augmentation of pressure, a considerable part of it being
absorbed by the material of the gun. The heating of a gun
by firing is an effect familiar to every one, and it affords an
indication, both of the quantity of heat abstracted from
useful effect, and also of the amazingly high temperatare of
the gas before it escapes from the gun. Fifty rounds, fired
in quick succession from a Field-piece, will make it so hot
that it cannot be touched. Since the flame is only in con-
tact with the bore for about the one-hundred-and-fiftieth
part of a second at each discharge, it follows that the
aggregate duration of the flame contact by which the gun is
thus heated, in fifty rounds, only amounts to one-third of a
second. The thin film of heated matter deposited on the
surface of the bore at each discharge, contributes, in some
measure, to this rise of temperature ; but we may regard the
acquisition of heat from this source as fully neutralized by
the cooling of the gun in the intervals occupied by loading.
Thus, then, you will be able to appreciate both the intensity
of the heat of the gas, and the extent of the waste by
absorption. In small guns the area of absorbing surface
surrounding the charge is greater in relation to the mass of
the charge than it is in large guns. Therefore, the waste
caused by the heating of the gun is also relatively greater,
and the gas never attains either the same heat or the same
pressure in the smaller weapon as in the larger. But the
greater heat attained in a large gun adds to pressure not only
directly, by expanding the gas, but indirectly, by accelerating
13
the combustion of the powder. The powder must be re-
garded as fuel burning in a furnace, and the hotter the
furnace is, the quicker the fuel will burn. You will perceive,
then, that the pressui-e of powder-gas per unit of surface is
augmented by increasing the size of the gun, apart from all
considerations regarding the projectile.
But the pressure of the gas is further increased in large
rifled-guns, by the great length of column represented by
their projectiles. The resistance increases witti the length of
the projectile, and the pi'essure rises with the resistance.
Augmentation of pressure is also caused by the rifled pro-
jectile having to acquire motion of rotation, in addition to
that of translation, though the increase of resistance, and of
consequent pressure, due to this cause, is not so considerable, as
is commonly supposed.
For these various reasons, the introduction of the rifled
principle, and the enormous increase of size demanded in
modern ordnance, combine to intensify the pressure to a
degree which taxes our utmost resources to control. The
limit of the pressure actually reached in rifled guns, of the
largest size, when fired with English service powder, is not
yet fully ascertained, but it is probably not less than seventy
thousand pounds on the square inch.
Now comes the question of what construction is best
adapted to resist so inordinate a strain.
It was long since demonstrated by Professor Barlow, that
a cylinder, to possess the greatest possible resistance to a
bursting force, must, when out of action, have its interior in
a state of compression, and its exterior in a state of tension.
He further proved it to be necessary that the internal com-
pression should diminish in an outward direction, and the
external tension in an inward direction, up to an intermediate
zone of neutrality. If these conditions were neglected, he
shewed that in a very thick cjdinder the material, forming
the interior portion, would be stretched to the breaking point
before the exterior portion acquired any considerable tension.
The interior, therefore, would be overstrained, while the ex-
terior would be understrained, and the a^^gregate resistance
would necessaril)'^ be less than if all parts were doing full duty.
This reasoning is the foundation of the argument in favour
of built-up guns, in which every layer of the material is
stretched upon the layei's beneath, and the finished structure
is in the condition of internal compression and external
tension, demonstrated by Barlow, to be that of greatest
strength. The Americans have endeavoured, with partial
success, to realize the advantage of this principle in cast-iron
guns, by cooling the inside first, and allowing the external
portion of the metal to shrink upon the hardened interior. The
Rodman Cast-Iron Gun is made upon this sj'stem, and con-
sidering the nature of its material, has, in some examples at
least, exhibited great power of resistance, though not
sufficient to enable it to be used for heavy ordnance in the
rifled form. Where forged material is used for the fabrica-
tion of Guns, this condition of outward tension and inward
compres>ion, is unattainable, except by the application of the
material in successive layers, each stretched on those below.
Considerations of economy, or convenience, may supervene to
reduce the number of layers, as in the Frazer modification of
coil-made Guns, but theoretical perfection will be most nearly
reached in that Gun which is composed of the greatest
number of layers. To attempt to forge large Guns in single
blocks is a direct violation of established theory, and the
general failure which has attended such attempts is a
practical proof of the truth of the theory.
The next point to consider is the best kind of material for
the fabrication of Guns. In determining this question, the
choice clearly lies between steel and wrought-iron. I say
this with no disparagement of Major Palliser's system of
adapting cast-iron smooth-bore Guns for rifling, by intro-
ducing a tube of coiled wrought-iron, but this method has,
u
hitherto, only been applied with success to Guns which,
though formerly classified as heavy ordnance, are dwarfed
by comparison with the ponderous Guns of the present day.
For these we require the greatest strength we can attain, and
cast-iron cannot possibly be regarded as so efficient for en-
veloping the internal tube as either wrought-iron or steel. In
discussing which of these two materials is best, I shall
be tresspassing on controversial ground. Krupp and AVhit-
worth, both great names in gunnery, though differing
widely in their views in other points, agree in this, that steel
is the right material for the entire Gun. I, on the other hand,
have always advocated wroughl-iron in the form of welded
coil for the chief mass of the Gun, limiting the use of steel to
the internal tube which has abrasion to resist as well as
tensile strain. The expression of my opinions upon this
point may probably not be considered impartial, but I will,
nevertheless, state the grounds upon which my preference of
wrought-iron, thus applied, is based.
It has been found, both in Elswick and Woolwich Guns,
that whenever failure takes place, it almost invariably origin-
ates with that part which is made of steel. It is the steel
tube which is nearly always the first to crack. So also, wiien
the vent-pieces or closing blocks of the breech loading guns
were made of steel, their fracture was alaimingl}- frequent, but
since wrought iron has been substituted such occurrences are
rare. The conclusion, therefore, at which I long since arrived,
and which I still maintain, is, that although steel has much
greater tensile strength than wrought-iron, it is less adapted to
resist concussive strain. This conclusion is in strict harmony
with the fact, that armour-plates made of steel, have proved,
on every occasion of their trial, greatly inferior to plates of
wrought-iron. The experiments wliich I made some years ago,
on the toughening of steel, in large masses, bv immersion,
when heated, in oil, led me to expect that this fragility wouM
be obviated by that process, and I felt sanguine that 1 should
T6
be able by sucb treatment to produce steel armour-plates of
extraordinary resisting power. An armour-plate of steel was
accordingly manufactured for experiment, and was tempered in
a large bath of oil. Its quaility was tried by test pieces cut off
after tempering, and proved by tension and bending. The
result shewed a very high tensile strength, combined with so
much toughness that I was unable to match its bending power
b}'- an}' sample of iron I could compare with it. The plate
was then sent to Portsmouth for trial, in the fullest confidence
of its success, but two shots from a 08- pounder sufficed to break
it in various directions, and it was justly pronounced a failure.
"NVith these experiences before me, it is imp )Sbible that I can
hold any other opinion than that the vibratory action attend-
ing excessive concussion is more dangerous to steel than iron,
and were it not necessary to provide a harder and more homo-
geneous substance than wroupht-iron for the surface of the
bore, I should entirely discard the use of steel from the manu-
facture of orilnunce. I do not mean to contend that very
strong guns ma}' not bt; made of steel, but I am convinced
that failures will be more frequent, and, I may add, more
disastrous, with steel than with iron, when the conditions of
trial are the same. The want of uniformity in the quality
of steel continues to be another serious objection to its use ;
and, in addition to all these considerations, the element of
cost is greatly in favour of the wrought-iron coil construction
over every mode of manufacture in steel.
I will now offer a few remarks upon the interesting
question of the probable future of Guns. Upon the solution
of this question depends the pattern of future ships, and also
the policy of continuing or abandoning the struggle of
Armour Plates against Guns. From my previous remarks
on the increase of pressure with which we have had to
contend as we have increased the size of our Guns, it might
bo inferred that wo were now nearly reaching a limit
which the strength and endurance of our material would not
17
enable us to pass. I am not prepared to say how far we could
have advanced under the recently existing conditions, but,
certainl)^, every increase of size would have been attended with
increase of difficulty. A new light, however, has just dawned
upon the subject, which entirely alters the prospect. It has
become apparent that the powder we have been using can be
so modified as to produce the required effect, with greatly less
strain upon the Gun. It may appear paradoxical that there
should be a limit to the theoretical advantage of increasing the
initial pressure of the gas evolved in the Grun, but the apparent
anomaly will disappear on examination. The action of ex-
panding gas in a Gun is analogous to that of expanding steam
in the cylinder of a Steam Engine, and we all know the advan-
tage, in the case of steam, of having a high pressure to beo-in
with, provided a steam jacket be used to maintain the material
of the cylinder at a temperature equal to that of the entering
steam. But in a Gun we can have no provision analogous to
the steam jacket, and it would appear that it is owing to the
necessary absence of such a provision that there is a limit to
the increase of initial pressure, beyond which no gain of pro-
pelling force is realized. Perhaps I shall not be fully under-
stood, without explaining this curious and important subject
in a more definite manner, and I will, therefore, endeavour to
do so.
The force exerted in a Gun bears a certain relation
to the heat evolved by the gasification of the charge. The
greater the heat the greater the force, for heat is nothing
more than unexpended force. I have already alluded
to the loss of heat by transmission to the Gun, and it is
evident that this transmission must be greatest in amount
when the heat of the gas is highest. By using a slower burning
powder, less heat and pressure are evolved at first, and the
waste of heat in the stage of initial pressure being less,
more heat remains for expansive action. Hence the slower
burning powder is weaker at first, but stronger afterwards,
and althougli the total quantity of gas be only tlie same
and tlic pressure not so great at any point, yet the aggre-
gate pressure throughout the bore may equal that of the
moi'e energetic and more dangerous powder. This would not
be so if the Gun, like the steam-jacketed cylinder, could be
maintained at the maximum temperatui-e of the elistie
medium within, but in the case of the Gun that temperature
would be far above the melting point of its own material. It
is only lately that attention has been strongly directed to the
powder question in England. In Russia and Prussia, where
great efibrts have been made to obtain endurance with large
rifled Guns, powder simiku* in granulated form to that used
in England has long been wholly discarded and sviperseded
by powder stamped into prismatic blocks, which burn more
slowly ; but although we have erred in using a powder for
our new ordnance so violent as to be justly designated
"brutal" by the French, yet we have this satisfaction that
the ordeal which our Guns have sustained with our severer
powder, affords an assurance of strength which we could
not have had if they had only withstood the mild description
of powder with which alone Continental Guns have been suc-
cessfully tried. Attention is now fully awakened to the
subject, and a scientific Military Committee is conducting
experiments upon the force of different descriptions of powder.
In these experiments the pressures exerted in every part
of the Gun are determined, by the use of an instrument of
exquisite delicacy invented by my friend and partner, Captain
Noble. This instrument, which is a happy combination of
mechanical and electrical action, indicates the velocity
attained by the projectile at any number of points in the
gun, and from these velocities the pressures are deduced by
calculation. Thus a diagram of pressure can now be
exhibited for gas in a Gun, as well as for steam in a cylinder,
and I think you will agree with me in regarding this result
as no small triumph of mechanical science.
19
The mitigation of initial pressure -whicli is now known to
be corap.itible with the maintenance of efficiency, opens a
new future for Guns and removes all doubt as to the practi-
cability of increasing their size and power to an extent which
it would be vain to follow on the side of the defence by
increase in the thickness of armour. No present armour-clad
vessel is proof against present Guns, and there is n"t the
slightest probability that future armour will be proof against
future Guns. Ships of the " Warrior" class can already be
pierced with shot or shell, fired at considerable ranges, by
even second-class Guns, and the still stronger ships, now in
course of construction, are pretty sure to be similarly overtaken
in a ver}' few years. Unless armour be invulnerable, it is of
very doubtful advantage as a defence. It will, perhaps, pre-
vent the entrance of shells, containing large bursting charges,
but on the other hand the passage of a shot through the
thick side of an armour-clad, carries with it a mass of frag-
ments that would act with terrible effect on the crew. If we
cannot stop a shot, the next best thing is to facilitate its passage
through. Wooden ships are out of the question because they
are combustible, but we may have ships of iron without the
armour. Whatever weight we carry as armour, we lose as
armament, and if we lessen the offensive power of a ship, by
loading her with armour, we ought to be very suie that the
armour will realize its defensive purpose.
The efficiency of modern ordnance against armour-plates,
is dependent, not only on the power of the Gun, but also upon
the material and form of the projectile. Ordinary cast-iron
proved absolutely useless for projectiles to be used against
thick armour-plates, and until Major Palliser applied the
process of chilling to the manufacture of cast-iron projectiles
there was every reason to believe that hardened steel was the
only material that could be used for this purpose, with effect.
The process of chilling gives extreme hardness to cast-iron,
but in point of toughness, a chilled cast-iron shot is inferior to
20
one of steel. Steel, however, though much less liable to
break is more easily crusher], and this brings me to notice a
curious evidence of difference in the amount of the penetrative
power lost by crushing, and by breaking. A crushed pro-
jectile is always much heated by the blow, but the fragments
of a chilled projectile remain cool. Hence, we see that crush-
ing detracts more from the power of a projectile than break-
ing, because the heat developed in a projectile by striking a
plate is a criterion of the amount of force expended upon the
projectile instead of the plate. We, accordiugl}'-, find that a
Palliser shot breaking, by impact, will, nevertheless, pierce
more easily than a steel shot which remains whole, but yields
to crushing. As to the proper form of head to be gjvcn to
the projectile for piercing armour, you will remember that, a
few years ago, this question was hotly contested between the
supporters of round heads and flat heads ; but, as often
happens, in the case of human contentions, not limited to the
sphere of mechanical engineering, both parties were afterwards
proved to be wrong. When Major Palliser brought forward
his cbilled projectile, he advocated a pointed head, and with
the new material he was found to be right. Major Palliser
has competitors on the Continent, whose claims I cannot pre-
tend to weigh, but in this country, at all events, he is entitled
to the honour of improving both the material and the form
of the projectile, thereby greatly increasing the penetrative
power of our artilleiy, and, at the same time, effecting an
enormous economy in the manufacture of projectiles.
The most legitimate use of instruments of war is for the
purpose of home defence, and I, therefore, proceed with
satisfaction to notice a class of inexpensive vessels requiring
no armour, and adapted to render the heaviest artillery avail-
able for the protection of our shores and harbours. Until
very recently, there seems to have been an impression that
large Guns required large vessels to carry them ; but the
fallacy of this idea has been practically shown by the prov-
i
21
ing barge of tte Elswick "Works, whicli is a mere floating
giin-carriage. This little vessel, which is only sixty tons
burden, is continually used, without difficulty, for the trial of
twelve-ton Guns, at sea, even when the swell is considerable.
This proving barge was the origin of Mr. Rendel's idea of
the now well-known gunboat "Staunch." The Elswick
barge has no steam power, and thus represents the minimum
of size ; but the '" Staunch " is provided with steam power,
both for propulsion by means of twin screws, and for working
her twelve-ton Gun. She is, therefore, somewhat larger than
the Elswick barge, and yet so small as to be very inex-
pensive, and, at the same time, a very difficult mark to hit.
To burden such a vessel with armour would, at once, increase
her size and her cost, thus rendering her more easy to hit,
and more expensive to lose. A simple screen might, perhaps,
be advantageoudy applied as a protection against Shrapnel ;
but thick armour, if used at all, should be reserved for ocean
ships. I have so recently published my views on the subject
of this vessel, that I need not now repeat them further,
merely observing that Guns of the largest size now made,
or ever likely to be made, may be mounted in vessels similar
to the ''Staunch," without increasing their tonnage in rrrore
than a proportionate degree.
Another recent invention, highly favourable to defence, is
the celebrated Gun-carriage of Captain MoncrielF. By the
ingenious arrangement of this Carriage, the recoil of the
Gun operates in a downward direction, and in descending it
lifts a counterweight which, when liberated, after loading,
raises the Gun again to the height necessary for firing
over the edge of a parapet. By this mechanism the Gun
is handled with almost perfect security to the men, and
is, itself, exposed in the smallest possible degree, and
only for a few seconds while being filed. Ko embrasures
being required, the Gun is not restricted in lateral range.
This is the characteristic advantage of the Barbette
system of mounting Gims, which has, ho-^ever, the fatal
ohjection of exposing both Guns and gunners. Embrasures
are always a source of trouble in fortifications. They not
only admit but guide projectiles into the fort at the \eiy
points where Guns arc placed. In iron defences the opening
for the Gun is even more objectionable. Not only does it
weaken the whole structure, but it serves to break up cast-iron
shot, striking on the edge, and thus to occasion terril)le destruc-
tion inside. I may state as a fact, communicated to me by a
Brazilian officer, on whose testimony I rely implicitly, that in
the late Paraguayan war, in which he was CDgaged, he saw
whole gun-crews swept away in the Brazilian Iron-clads, by
common cast-iron round shot, contemptible for piercing even
the weakest armour, but which, striking the edge of the
port, entered the ship in a torrent of fragments. The Mon-
crieff Gun-carriage gives great additional value to earth-
works, and, in fact, may be used in mere pits, which would
be wholly invisible to an enemy. It will probably also prove
to be available, in combination with iron defences, as a means
of avoiding the objection of port-holes, and it will have the
effect of placing muzzle-loading Guns on a par with breech-
loaders, in regard to security and ease of loading. Captain
Moncrieff"'s invention will play a very important part in
defensive operations, and will greatly reduce the expense of
fortifications.
Many other instances may be cited in illustration of the
tendency of mechanical progress to favour defence. Thus,
the increasing size of Guns renders them difficult to
transport for ofiensive use abroad, but creates no impedi-
ment to their defensive application at home. Or, if we
look to the nautical side of the subject, we see that the con-
ditions sought to be attained in war-ships for aggressive
action involve enormous cost, and that the great size of these
vessels makes them favourable targets for the fire of opposing
artillery. On the other hand, the vessels required for coast
23
and harbour defence are of cheap construction, and their small
size and facility of movement give them the advantage of
heing difficult to hit. The j\Ioncrieff Carriage is applicable,
almost exclusively, to defensive purposes ; and the same may
be said of Torpedoes, which, by many ingenious contrivances,
have recently been rendered most formidable obstacles to
naval attacks upon sea-ports. The tendency, therefore, of
mechanical invention, as applied to war, is to discourage
aggression, and thus to maintain peace. "We may, conse-
quently, hope that it will hasten the arrival of a period when
civilized nations will abandon the arbitrament of arms, and
settle their differences by rational and peaceable methods.
But, while I defend the Mechanical Branch of Military
Science from all imputation of serv^ing the cause of war, I do
not forget that it is to the Civil Branch of Mechanical
Engineering that the honour of promoting the friendship of
nations especially belongs. It is by the facilities it gives to
intercourse and exchange, and by the reciprocal benefits
which flow therefrom, that it teaches men how much they
have to gain by peace, and to lose by war.
NEWCASTLE : J. M. CAEK, STEAil FEINTING WORKS, 21, LOW FEIAE STEEET.
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