ae
nent ee eS i ot Se
PRINTED AT THE HERALD OFFICE, NORTH GATE, BATH.
mee ae ad
HEE CAD ntiog.” en
MELE F1i40 UT OA ae PALM Wat rR, cheery
PROCEEDINGS
OF THE
BATH NATURAL HISTORY
AND
ANTIQUARIAN FIELD CLUB.
BATH :
PRINTED (FOR THE CLUB) AT THE HERALD OFFICE, NORTH GATE.
1889,
wrist
TABLE OF CONTENTS.
Vou. VI, No. 1.
1.—CONTINUATION OF THE FUNGI oF Batu, By C. E.
Broome, F.LS. _... vit ats ae we
2.—On AN ABNORMAL FLOWER OF A PENSTEMON, BY
C. E. Brooms, F.L.S. ee ae ois 2
3.—NoTES ON RoMAN PAVING FOUND IN BRIDEWELL
LANE, BY T. BROWNE
4,—THr BouRNEMOUTH Firs ; CONSIDERED AS THE
REMAINS OF AN ANCIENT Forest. WAS THERE
EVER A ForEST OF FIRS ON THE HILLS AROUND
Bato? By tHe Rev. LeEoNARD BLOMEFIELD,
M.A., F.LS., F.G.8., &. ...
5.—THE ALG OF THE BATH THERMAL WATERS, BY
G. Norman, M.B. ... ve
6.—THE Earuiest Map oF Batu, BY EMANUEL
GREEN, F.S.A.
7.—On RECENT DISCOVERIES MADE IN UNCOVERING
THE ROMAN BATHS AT BATH, BY THE ReEv.
Pres. ScARTH, M.A.
8.—UPON SOME SCULPTURE RECENTLY DISCOVERED AT
THE Cross BATH, BY THE Rey. H. H. Winwvop,
M.A., F.G.S, sie ie vi 25 bye
Pace.
35
37
39
53
58
79
U2. CONTENTS.
PAGE.
9,—Nores ON THE OCCURRENCE OF SALT SPRINGS IN
HE CoAL MEASURES AT RADSTOCK, BY J.
McMvrrtnie, F.G.S. ‘os ae fs ot ee
10.—List or Fosst, MAMMALIA FOUND NEAR BATH, BY
rue Rev. H. H. Winwoop, M.A., F.GS. cae ee
11.—SUMMARY OF PROCEEDINGS FOR THE YEAR 1885-86,
By THE SECRETARY... aie ee aoe ca’ Gen
No. 2.
1.—Nores oN THE GEOLOGY OF BRENT KNOLL, BY
Horace B. Woopwarp, F.G:S. ... ii ree
9.—PitAce NAMES DERIVED FRoM PLANTS (IN THE
NEIGHBOURHOOD OF BATH), BY THE Rev. CANON
ELLACOMBE ... dee me sy. ii ao ee
3.—ADDRESS TO THE MEMBERS OF THE BatH FIELD
CLUB IN REFERENCE TO THE DEATH OF C. E.
BROOME, F.LS., BY THE Rev. L. BLOMEFIELD,
‘M.A, F.LS., F.G.S., &c. ... is tds vee
4,—TRACES OF THE SAXON PERIOD IN BATH AND THE
NEIGHBOURHOOD, BY THE REY. PREB. EARLE ... 153
5,—Lerrers ILLUSTRATING THE BATTLES OF CLAVERTON
AND LANSDOWN, BY H. D. Sxrine, M.A. ae
6.—FurRTHER NoTES ON THE CLAVERTON SKIRMISH, BY
H. D. Sxrine, M.A. 453 MG dis + ee
7—Norrs oN THE HAM HILL STONE, BY Hx.B,
WoopwarbD, F,G.S. oF Rr and an Oe
CONTENTS.
_8.—FurtTHEr RESULTS OF METEOROLOGICAL OBSERVA-
TIONS MADE AT THE BATH ROYAL LITERARY AND
SCIENTIFIC INSTITUTION, BY THE REV. LEONARD
BLoMEFIELD, M.A, F.L.S., F.G.S., &, .
9.—SUMMARY OF PROCEEDINGS FOR THE YEAR 1886-87,
BY THE SECRETARY... ad fe Han My
No. 3.
1.—ON SOME OSTRACODA FROM THE FULLERS - EARTH
OoLITE AND BRADFORD CLAY, BY PROFESSOR T.
RuPert JONES, F.R.S., F.G.S., anp C. DAvits
SHERBORN, F.G.S. ...
2.—LANDSLIPS AND SUBSIDENCES, BY W. PUMPHREY ...
3.—THE DESTRUCTION OF THE Two CHURCHES OF ST.
Mary In Batu, By Austin J. Kine
4.—A Barn Pott Tax 2 RicHarp II., py EMANUEL
GREEN, F.S.A. ae a site ka eee
5.—REMARKS ON SOME HEMIPTERA-HETEROPTERA TAKEN
IN THE NEIGHBOURHOOD OF BATH, BY LIEUT.-
Cot. BLATHWAYT, F.L.S. F.Ent.S. a ane
6.—RECENT “ FINDS” IN THE VICTORIA GRAVEL PIT, BY
THE Rev. H. H. Winwoop, M.A., F.G.S. a
7.—NoTE ON WEBBINA IRPEGULARIS (D’ORB.) FROM THE
Oxrorp CLAY AT WrYMOUTH, BY C. DAvIES
SHERBORN, F.G.S. ... Ba oe age ie
8.--SUMMARY OF PROCEEDINGS FOR THE YEAR 1887-88,
BY THE SECRETARY Se LA: wae PHS
196
vu. CONTEN'S.
No. 4.
PAGE.
1.—On CuurcH Doorways, BY THE REV. REGINALD
A; Gayiuy; McA. .«.. se ite aa .. 363
2.—BatH Lay Supsipies, Henry IV. to Henry VIII,
BY EMANUEL GREEN, F.S.A. me ~ ase de
3.—Tue Divinine Rop, py THomas ForpER PLowMAN 411
4,—ListT OF TERRESTRIAL HEMIPTERA - HETEROPTERA
TAKEN IN THE NEIGHBOURHOOD OF BATH, BY
Lizut.-Con. Buatawayt, F.L.S., F.Ent.S. «s ) 432
5.—SUMMARY OF PROCEEDINGS FOR THE YEAR 1888-89,
BY THE SECRETARY we i des .. 435
~
In
SA
\
¥
8 JUN. 92
“OR OCT 13888.
. : ‘ a PROCEEDINGS
BATH NATURAL HISTORY
ANTIQUARIAN FIELD CLUB
NO. I. VOL, VI
‘PRICE . HALF-A-CROWN.
ee SX BATH: ;
ieee THE HERALD OFFICE, NORTH. GATE.
| J. DAVIES, GRAND PUMP ROOM LIBRARY.
1886, 0
Continuation of the Fungi of Bath, By C. E. Brooms, F.LS.
(Read March 18th, 1885.)
Continuing our Notices of the Fungi of the Bath District from
. a Paper read in March, 1883, before the Bath Field Club, we
commence with the 26th Order of Mr. Berkeley’s arrangement in
the Outlines of British Fungology, Spheriacei. The Order is
characterized by producing its fruit, called sporidia, in little sacs,
or asci, which grow in closed vesicles, perithecia, opening by a
round or elongate mouth. This is perhaps one of the most
interesting Orders of the Family Ascomycetes, especially to
Microscopists, owing to the great variety it presents, both in the
outward form and arrangement of the perithecia, and in the
nature of the sporidia which, in this section, often afford good
specific characters, either in their mode of division, coloration,
or in the number contained in each ascus. Spherie are to be
found in all parts of the world. They are most abundant in
temperate climates ; but they are by no means rare in the tropics,
especially insect-spherie, and such forms as approximate to
Xylaria Hypoxylon, the finer states of which occur in the warmer
climates; and it is probable that if tropical countries were
thoroughly investigated, a great number of undescribed species
would be the result. Ceylon has furnished us with conclusive
evidence on this point, thanks to the exertions of my late friend,
Mr. Thwaites, whose contributions to the mycology of that island
have been recorded in the Linnean Journal (Vols. XI., p. 494 and
‘XIV., p. 29). The old unwieldy genus Spheria, of which Fries
described, in his Systema Mycologicum, upwards of 1,000 species
has, since that time, been divided into numerous genera and
‘subgenera by almost every author who has written on the subject.
“Many of these divisions are, however, of doubtful value; we
‘shall, therefore, confine ourselves in the present enumeration to
‘such as appear to be of most value, and are more generally
Vou. 6, No. 1.
2
recognized, Fries divided them in the Systema according to
their simple, or compound habits.
Those in the simple section are either innate in the bark of trees
or plants, or at length emergent by a longer or shorter neck, with
round or elongate mouths, or quite superficial on the surface of
wood or sticks, and these are glabrous, or hairy, or tomentose, and
sometimes seated on a shaggy subiculum. In the compound
section the perithecia are aggregated together in the substance of
wood, or leaves, or in the stems of herbaceous plants, assuming,
at times, a circinate or quincuncial arrangement, or occupying
carbonaceous receptacles which are immersed in the wood. Some-
times they are located in a flat, or globose, stroma, which, in the
more perfect species, assumes a simple or branched, erect form.
To begin, however, with the more simple forms. We have in
them instances of species without any true perithecia as in
the genus Dothidea, where, however, that want is fully compen-
sated by the various forms of fruit which have been traced to it
in its early stages; thus in Dothidea melanops 7'ul. there are
macrostylospores and microstylospores, as well as ascigerous
fruit.
Again in Diatrype stigma Fr. Stictosphzria Noffmanni Tul, we
have conidia lining the interior of irregular cavities of the wood,
or bark, on which it grows; and, on the same stroma, ascigerous
conceptacles containing sporidia of a form very similar to the
conidia.
In Cucurbitaria macrospora Tul. the three forms of fruit are again
to be seen, occupying one stroma. In Melanconis macrosperma
the conidia are shown, in Tulasne’s figure, growing intermixed
with macrostylospores. The conidiiferous tufts of Stigmatea frag-
rariz also present us with a beautiful microscopic object; this species
grows on living strawberry leaves. I cannot pass over without
notice a minute plant, the structure of which is very curious.
It grows on the leaves of Aira czspitosa, a coarse grass known to
the Wiltshire farmers as Bull-polls, it has been described, as a new
3
genus, under the name of Oomyces, on account of its egg-shape.
Madame Libert published it in her exsiccata, as Spheria carneo-
alba Libert. It is about a line high, bluntly conical, and of a
pinkish-yellow colour ; there is an outer, leathery receptacle, trun-.
-eate at top, around the centre of which are four to seven dark
dots ; a cross section shows that these are the mouths of as many
delicate, membranous perithecia which are closely packed in the
outer conceptacle. The perithecia contain a number of elongate,
cylindrical, asci, filled with very long, flexuous sporidia. It has been
placed in a new genus on account of its compound character ; the
outer conceptacle containing free, ascigerous perithecia. In
Pleospora herbarum Pers. and P. polytricha Wallroth., belonging to
the section Denudatz of the genus Spheria, the early states were
considered autonomous plants; but it has been demonstrated that
the canidia of the first constitute the genus Mystrosporium of
Desmaziere, which again appears to give origin to Cladosporium
herbarum Link., a common pest in greenhouses, covering the plants
with a sooty stratum. The conidia of the latter, Pleospora polytricha
Wall., being stipitate, and septate, present an elegant appearance
under the microscope, and probably belong to Acrothecium
simplex B.and Br. Nectria cinnabarina Fr. the conidiiferous state
of which is known as Tubercularia vulgaris Tode., is interesting,
from its common occurrence on dead sticks, covering them with
bright, scarlet spots. Another of the same genus Nectria
inaurata B. and Br. has two forms of ascigerous fruit, a very unusual
occurrence ; it grows on dead twigs of holly. Capnodium and its
allies, as Fumago and others, belong to the Spheriacei since they
produce their more perfect form of fruit in asci, their perithecia
being furnished with a round mouth. To the unassisted eye these
plants appear as a mere sooty stain on the leaves of trees and
shrubs, thus spoiling their appearance. We may mention in this
place that the conidiiferous state of Hypoxylon coccineum Bull.
was described by Persoon as a mould under the name of Isaria
farinosa Pers. ; but it has been since traced.to the Hypoxylon, it is
4
common on decaying Beech. The genus Hypocrea is intermediate
between Nectria and Cordyceps, it is generally effused, and
horizontal in habit, and more remarkable from the moulds which
constitute its early state, or are associated with it, than in its per-
fect form. These moulds were considered autonomous species till
Tulasne traced them to their true position ; they constitute the
genera Botrytis, Verticillium, and others. Hypocrea inclusa B. and
Br. is curious from its place of growth. It is parasitic in the flesh of
a small truffle, Tuber puberulum £.; its presence may be detected
by a minute, rusty spot not larger than the head of the smallest
pin, visible on making a section of the Truffle.
Another species, nearly related, is not uncommon on grasses; it
surrounds the stalk with a bandlike, yellow stroma, crowded with
perithecia. Tulasne has given it the generic name of Epichloe ;
it differs from Hypocrea in the sporidia being linear and
continuous. In habit it resembles the latter. The genus
‘Hypomyces differs from Hypocrea in fruit, and in being generally
parasitic on other fungi. In a Monograph of the genus, Mr.
Plowright observes that Hypomyces luteo-virens attacks the
Agaric on which it is parasitic, at a very early period before it
‘appears above ground, and so distorts it that it is impossible to
say to what species it belongs: most commonly the Hypomyces
do not attack other fungi till they are in a state of decay.
Another species, he says, grows, not on the Agaric itself, but on
the ground under, or near, the spot where it has decayed, the
decay being the result of the growth of an earlier stage of the
Hypomyces; in other words, the Hypomyces, in its conidial
state, first attacks the Host-Fungus, and, by causing its decay,
‘generates the pabulum necessary for the nourishment and perfec-
tion of the higher form of fructification.
The genus Hypomyces is interesting from the various phases
‘through which many of its members pass. As a rule, the
ascigerous, or perfect form is more rare,—the conidiiferous state
the more common. Hypomyces aureo-nitens Tul. was of striking
5
beauty, as it occurred on a damp morning in North Wales, each of
the conidia growing on a branched mucedinous mycelium, was
surmounted by a minute drop of dew, glittering in the sun’s rays
like a diamond. Hypomyces cervinus Tul. is another pretty
microscopic object, its macroconidia, or second form of fruit, are
globose and echinulate ; they may be seen everywhere on decaying
Boleti in autumn, converting them into a mass of yellow powder.
The genus Xylaria has a branched, erect, clavate stroma, the
early state of which, particularly in Xylaria Hypoxylon, often
puzzles beginners ; the tips of the branches are then covered with
a white powder, consisting of conidia, which fall off on being
touched, leading the student to consider the specimen as belonging
to such of the Hymenomycetes as Clavaria; but later on the
branches swell out at the tips, and numerous perithecia are.
developed in their substance, containing asci and ovate, coloured
sporidia, thus showing the true position of the specimen in the
series.
I shall just allude here to a curious fungus belonging to this
section, although # is not British. It occurred on rotting
Bamboo in Ceylon, It has been named Astrocystis, on account
of its starlike habit; in form it resembles a Geaster, having a
double perithecium, the outer coat splitting into several rays,
which become recurved, as in that genus; the inner coat opens
by a more or less, regular mouth, to allow the escape of the
sporidia, which are those of an Hypoxylon. The similarity of
habit may be regarded as an instance of—what is now much
discussed—mimicry in nature ; the structure and true affinities
are here far apart.
The genus Cordyceps, or Torrubia of Tulasne, is one of the
most interesting of the Spheriacei, both from the variety of its
habitats, or places of growth, and from the medicinal properties of
one of the species. I allude to the Ergot of grasses. In a paper
on this plant, published in the Journal of the Agricultural
Society of England (Vol. x., 8-8, part II.), Mr. Carruthers says,
6
“The full grown Ergot is often overlooked in the barn, among the
corn, owing to its fesemblance to the dung of mice ; but it is
worth especial pains in examining the seed to secure immunity
from this parasite”—“ Ergot might supply an interesting text
from which to exhibit the worthlessness of speculation, as opposed
to observation and experiment in dealing with natural science.
Replacing, as it does, the seed of different grasses, and always
attaining, when full grown, a greater size than the normal seed,
it was, at first, thought merely to indicate an extra quantity of
life and vigour in the particular seeds, which exhausted themselves
in the production of the anomalous, horned grain; no special
qualities being then associated with these abnormal productions.
All along, however, the Ergot has been exerting its baneful in-
fluence on men and animals, without being suspected. Through
its agency the inhabitants of whole districts in France had been
visited with intermittent attacks of gangrenous diseases. England
also has records of similar, although not so extensive calamities.
In the same Journal it is stated that the loss to one breeder
of cattle alone, in Shropshire, was £1,200 in three years owing
to this cause. It has been determined that the power of
Ergot in causing muscular contraction extends to all unstriped,
or involuntary muscular fibre, and it has therefore been applied
in treating certain maladies connected with the intestinal canal,
and the arteries, because these organs are chiefly composed of
this kind of muscular tissue. The comparative immunity of
England from disease arising from Ergot is probably owing
to the less quantity of rye grown for seed, and used in
bread, than is the case in France. But its frequent occurrence
on our grasses as on the Bromi, Alopecuri and Festuz, expose
our cattle to very serious losses. Ergot from the seed of
Dactylis glomerata was sown, when gathered in autumn and kept
under a bell glass through the winter ; in the following spring a
large crop of Cordyceps purpurea was produced. Ergot of rye
bought at a chemist’s, although then quite dry, and sown as
7
above, germinated after a like lapse of time producing the same
species, It is fortunate for us that this pest is much less frequent
on wheat and barley than on rye.
Some species of Cordyceps, or Torrubia, attack wasps nee other
insects, and have given origin to what are known as “ vegetable
wasps,” the insects flying about with the fungus attached.
Cordyceps alutacea F7, may be alluded to as showing some of
the difficulties attending the study of this group of Fungi. Fries
regarded it as a Cordyceps from its form and habit; Tulasne,
guided by its fruit, placed it in the genus Hypocrea, considering
it parasitic on Clavaria ligula, clothing that species with a thin
stroma in which the perithecia are immersed ; but it may be said
against that view, that Clavaria ligula has not occurred in
England unaccompanied by its presumed parasite; and as Cor-
dyceps alutacea is not uncommon in our fir plantations, it is
scarcely possible that such would be the case were the Clavaria
equally common. We may therefore fairly conclude that Fries was
right in placing our plant in the genus Cordyceps, and that it is
not merely a parasite on a Clavaria, but an autonomous species.
Cordyceps entomorrhiza is parasitic on the larve of insects, Mr.
Berkeley supposes that the sporidia fall on the caterpillars before
they bury themselves to undergo their pupa change, or if at a later
period they may be washed down through the soil so as to attain
their proper habitat, as is now said to be the case with the
Peronospora of the potato. At all events this must be the case
where such species as Cordyceps capitata Fr. take possession of
Elaphomyces, a subterranean fungus which is buried, sometimes
deep in the ground. When the sporidia reach their proper
habitat they germinate and pierce the skin of the insect, or the
rind of the fungus, and occupy the whole of its body with an
intricate mass of threads. They then throw out branching roots
into the surrounding soil ; from these roots an erect, club-shaped
stroma arises, in which, at length, the perithecia are formed.
Tulasne says that a second form of fruit, conidia, occurs at the
8
base of the stroma of Cordyceps capitata and C. entomorrhiza,
Cordyceps, Robertsii, a’ New Zealand species, parasitic on the
larva of Hepialus virescens, is one of the finest species belonging
to this genus. |
_ In the Order Perisporiacei the sporidia are set free by the
decay of the perithecia, the species not being furnished with a
mouth. Some of the plants belonging to the Order are beautiful
objects for the microscope, but very prejudicial to our crops.
Thus Spherotheca pannosa Lév. covers the leaves and shoots of
roses with a clothlike felt, thus preventing respiration, and causing
the destruction of leaves and flowers. Spherotheca Castagnii
Lédv. is equally destructive of our hop crops. Phyllactinia guttata
Fr. is common on the leaves of various trees. Erysiphe Martii
Lk, attacks our late crops of peas, often destroying them utterly
in dry seasons. These plants are supported on the leaves by very
elegant supports, or fulera,
There remains only the Physcmycetes and Mucorini to be
considered. The first Order is intermediate between Ascomycetes
and Hyphomycetes, agreeing with the former in the free formation
of its sporidia within a, generally globose, closed sac ; with the
latter in its free, fertile, threads which are never compacted into
an hymenium. The species belonging to these Orders, like the
greater part of moulds, grow on decaying substances, and
frequently on such as are used for food. In some instances,
perhaps, the germination of the sporidia induces decay, and
certainly accelerates it. Certain species of Mucor promote
fermentation in fluids, like the true moulds, as Penicillium. In
the genus Syzygites common on decaying Agarics in woods, the
fertile threads throw out little tubercles from their forked
branches—the tubercles soon touch each other and coalesce; a
dissepiment is formed on either side, the two intermediate
membranes are absorbed, and, finally, the united cells swell and
form an irregular sac, which soon produces an abundance of
sporidia ; thus resembling the connecting tubes of Zygnema
9
among Alge. In the genus Acrostalagmus the sporidia grow
from the apex of the peduncle which protrudes into the cyst, 80
that that genus varies somewhat from the character of the Order,
in the absence of free formation of the fruit inacyst. Something
similar occurs in Ascotricha. Enough has, perhaps, been said to
show that these low types of fungi possess some interest, and
exhibit the wonderful variety of form and structure made use of
by nature in her work, affording an inexhaustible field of research
to the Botanist and Microscopist.
We will now proceed with a list of the species belonging to the
Orders at present treated of, which have occurred in our
District, and which carries us through its mycology according to
the arrangement adopted by Fries.
ORDER 26. SPHARIACEI.
Perithecia carbonaceous or membranaceous, sometimes confluent
with the stroma, pierced at the apex, and mostly papillate.
Hymenium diffiuent.
GENUS 288. CorDyceEps.*
Stroma vertical, fleshy. Fructifying head distinct, hyaline or
coloured. Sporidia repeatedly divided, submoniliform.
Cordyceps ophioglossoides Fr. Spye Park, September, 1843,
parasitic on Elaphomyces muricatus.
C—— entomorrhiza Fr. Hartham Park, April, 1843, on
some caterpillar buried in the ground in fir plantations,
C——— nmuilitaris Fr. Hanham Woods, October, 1853.
C—— myrmecophila Cesati. Leigh Woods, Bristol, March,
1879. ;
C———— microcephala Tul. Leigh Wood, July, 1878. C.
Bucknall.
C———— purpurea Fr. Raised from Ergot on _ grasses.
Batheaston, June, 1854.
* Cordyceps, from Kordule, a club, and cephalos, a head
10
C————-pistillarizformis B. and Br, Annals of Natural History.
No. 969, t. 16, fig 22, on dead sticks still attached to a bush.
Batheaston, March, 1860.
C————-alutacea Fr. Lucknam Grove, in fir plantations,
October, 1859.
GENUS 289. HYPOCREA.* 7.
Stroma horizontal. Perithecia tender, hyaline or coloured.
Hypocrea gelatinosa Fr. Langridge, March, 1875.
H rufa Fr, Batheaston, November, 1859.
H vitalbe B. and Br. Batheaston, February, 1859. Annals
of Natural History, No. 829, t. 9, fig 8, on Clematis vitalba.
H delicatula Zulasne. Lucknam Grove, April, 1866;
Ann. des Sciences Nat., Ser. iv., vol. xiii., p. 18.
H farinosa B. and Br. December, 1863. Ann. of Nat. Hist.,
No. 592.
H inclusa B. and Br. Hanham and Leigh Wood ; parasitic
in the flesh of Tuber pubcrulum B. ; November, 1869. Ann.
of Nat. Hist., No. 970, t. 17, fig 23.
H. lenta Fr. St, Catherine’s, November, 1866, on wood.
GENUS 290. HYPOMYCES.¢ Tul.
Parasitic on fungi; mycelium byssoid; perithecia globose,
papillate; asci 8-spored (rarely 2 or 4), without paraphyses ;
sporidia lanceolate or elliptic, rarely obtuse, uniseptate, ejected
in tendrils.
Hypomyces ochraceus Tul. Langridge, April, 1874.
H asterophorus Jul. Leigh Wood (Macroconidia), C.
Bucknall.
H aurantius Tul. Batheaston, March, 1871, Langridge.
* From upo, beneath, and kreas, flesh.
+ From upo, beneath, and muke, a fungus.
11
H torminosus Tul. Leigh Wood, October, 1879. C.
Bucknall. ~
H. luteo-virens Tul. Ashton Court, Bristol, April, 1845 ;
Bathford, December, 1864.
H lateritius Tul. Leigh Woods, September, 1844.
H aureo-nitens Tul. Lucknam Grove, December, 1864.
H Broomeianus Jul. Batheaston, November, 1877.
H——— candicans Plowright. Bathford, October, 1880.
Grevillea xi., 50.
GENUS 291. EPICHLOE.* J*7.
Parasitic on grass, coloured ; perithecia fleshy, immersed in a
mycelioid stroma ; sporidia linear.
Epichloe typhina Berk. on stalks of grass. Bathford, &c., July, i877.
GENUS 292. XYLARIAT Fr.
Vertical, more or less stipitate. Stroma between fleshy and
corky, covered with a black or rufous bark.
Xylaria digitata Grev. Stapleton, June,1879. C. Bucknall.
D.¢ polymorpha Grev. Rudlow, March, 1843.
X—— hypoxylon Grev. Lucknam, &c., October, 1854.
D4 carpophila Fr. Spye Park, October, 1843.
X——— vaporaria Berk, Clitfe Pypard, November, 1863 ; on cow
dung laid in a heap, proceeding from a sclerotioid body.
pedunculata Fr. Wraxall, near Bristol, March, 1845 ;
Bathford Hill, November, 1863.
X——— bulbosa P. Lucknam, October, 1859; Bathford Hill,
in plantations.
Xx
* Epichloe, from epi, upon, and chloe, green grass.
+ Xylaria, from Xulon, wood.
12
GENUS 293. PORONIA.* Fr.
Between fleshy and corky. Fructifying surface margined,
orbicular. Perithecia immersed, vertical.
Poronia punctata Fr. Batheaston, April, 1871; Hanham.
GENUS 294. HYPOXYLON.¢ Bull.
Stroma, corky or brittle, convex or plane, immarginate, at first
clothed with a floccose veil, then with a black crust, distinct from
the matrix. Perithecia vertical or divergent.
Hypoxylon ustulatum Bul/. Batheaston, on old stumps.
H — nummularium Bull. Stapleton, near Bristol, October,
1853 ; Leigh Wood, September.
H————- luteum Fr. St. Catherine’s, April, 1867 ; Warleigh
February, 1862.
— gastrinum Fr. Batheaston, December, 1862 ; Rudlow,
February, 1843.
H-~————- concentricum Grey. Batheaston; common on ash timber.
H———— coccineum Bull. Batheaston, on beech timber.
H
H— multiforme Fr. Batheaston, November, 1875.
H— argillaceum fr. Batheaston, winter, common on
ash sticks.
H—-——- fuscum fr. Very common on sticks.
H————- rubiginosum Fr. On bare trunks, &c.
H———— serpens Fr, Common on dead wood.
H-————— coprophilum Fr. Batheaston, October, 1864; on cow
dung.
H —udum Fr. Leigh Wood, April, 1877. OC. Bucknall.
H————- atro-purpureum Fr. Leigh Wood, April, 1877. C.
Bucknall.
* Poronia, from poros, a pore.
+ Hypoxylon, from upo, beneath, and xulon, wood.
13
GENUS 295. DIATRYPE.*
’ Stroma partly formed from the matrix, and not distinct from
it ; perithecia sunk, elongated above into a distinct neck; and
frequently rostrate.
Dyatrype pantherina (B.) Leigh Wood, April, 1879. C.
Bucknall.
D———— scobina, Nike. Brockley Coombe, May, 1879. C.
Bucknall.
D—— bullata Fr. Batheaston ; common.
D———- undulata Fr. Rudlow, April, 1865 ; on dead sticks.
D————- stigma Fr. Rudlow, January, 1843 ; very common.
D—_— disciformis Fr. Rudlow, January, 1843; very common.
D———— favacea Fr. Spye Park, March, 1859.
D—— verruceformis. Batheaston, March, 1872.
D——- scabrosa Fr. Near Bristol, March, 1872.
D — sordida Fr. Spye Park, February, 1851.
D
quercina Fr. Batheaston ; winter.
D——- ferruginea Fr. Shockerwick, March, 1854.
D——— ceratosperma Fr. Swainswick, March, 1856.
D strumella Fr. Batheaston, April, 1852.
D— corniculata B. and Br. Lucknam, March, 1853.
D——— podoides Fr. Leigh Wood, February, 1877. C.
Bucknall.
D———— aspera Fr. Shirehampton, January, 1878. C.
Bucknall. .
D———- angulata Fr. Shirehampton, March, 1880. C.
Bucknall. .
D — ilicina Che. (Diaporthe). Durdham Down, May, 1878.
C. Bucknall.
-D———— lirella Mont. (Diaporthe). Boiling Wells, Bristol,
June, 1881. C. Bucknall. i
a nS ee ee
* Diatrype, from dia, through, and trupe, a hole. .
14
D——— Laschii Nike. (Diaporthe). Leigh Wood, May, 1883.
C. Bucknall.
D—— euphorbie Che. (Diaporthe). Leigh Wood, May, 1883.
C. Bucknall.
GENUS 296. VALSA.* Fry.
Perithecia carbonaceous, perfect, circinating, elongated into con-
verging necks ; ostiola erumpent, joined together, or ending in a
common disc.
Valsa prunastri Fr. Rudlow, January, 1843 ; on sloe.
V stellulata Fr. Batheaston, March, 1859.
V. syngenesia Fr. Batheaston, March, 1870.
V. detrusa Fr. Wraxall, January, 1845.
V— fibrosa Fr. Rudlow, May, 1843.
V nivea Fr, Bathampton, March, 1864.
V. leucostoma Fr. Batheaston, February, 1851.
V controversa Fr, Leigh Wood, January, 1880. C. Bucknall.
V—— taleola Fr. Shirehampton. C. Bucknall.
V. circumscripta Mont, Near the Avon, March, 1880. C.
Bucknall.
Vv pini Fr, Leigh Wood, December, 1866,
V. profusa Fr. St. Catherine’s, April, 1852.
V—— coronata Fr. Spye Park, February, 1851.
V chrysostroma Fr. February, 1850; on hornbeam.
V—— suffusa Fr. Spye Park, August, 1859.
V—— leiphemia Fr. Rudlow, May, 1843.
V. salicina Fr. Swainswick, January, 1852.
V—— ambiens Fr. Rudlow.
V—— stilbostoma Fr. Rudlow; var. platanoides.
V— — tetratrupha B. and Br. Spye Park, March, 1859 ; on alder.
¥: fenestrata B. and Br. Spye Park, March, 1859.
* Valsa, a word used by Adanson, derivation uncertain.
15
V—— tetraploa B, and Curt. Batheaston, February, 1850.
V. rhodophila B. and Br. Leigh Wood, C. Bucknall
V—— pulchella Fr. Brockley Coombe, January, 1845.
V. quaternata Fr, Near Chippenham, February, 1850 ; on
beech.
V. hypodermea Fr. Batheaston, December, 1851.
V. hapalocystis B. and Br. Batheaston, ‘April, 1850, on plane.
V— bitorulosa B. and Br. Batheaston, December, 1851.
V—tilie Tul. Leigh Wood, May, 1881. C. Bucknall,
V. gastrinoides (Anthostoma) P. and Wr., Grevillea X. 71.
Leigh Wood ; Bristol Fungi, pl. IL, fig. 11. ©. Bucknall.
V—— pustula Desm. Leigh Wood, June, 1882. C. Bucknall ;
Bristol Fungi, fig 9.
V—— conjuncta (Nees) Fr. On Rubus idzus; Batheaston,
February, 1850.
GENUS 297. MELOGRAMMA.* Fr.
Perithecia confluent with the stroma, more or less free above,
destitute of any neck; contents oozing out, and often forming
eirrhi.
GENUS 298. DOTHIDEA.t Jr.
Perithecia none. Nucleus contained in globose cavities,
immersed in the stroma, with a decided neck and papilleform
ostiolum.
Dothidea ribesia P. Langridge, April, 1872; on currant.
D rose Fr. Batheaston, &c. ; common on roses.
D filicina Fr. Leigh Wood, May, 1878. C. Bucknall.
D striefornis Fr. Batheaston, January, 1857.
D rubra P. Rudlow, September, 1843.
2s I 2 AIR ih pa ee me
* Melogramma from Melas, black, and gramma, a letter or mark,
+ Dothidea, from dothien a tumour, and, eidos, a resemblance.
16
D——— ulmi /r. Rudlow, November, 1841.
D——— trifolii Fr. Westbury, Bristol, April. C. Bucknall.
D——— Johnstoni B. and Br. Sandy Lane, May. C. Bucknall.
D chetomium Fr. Batheaston, February, 1851.
D——— graminis Fr. Derry Hill, winter.
D——— brassice Desm. Batheaston, &c.
GENUS 299. ISOTHEA.* 7,
Nucleus without any perithecium, coloured or black, covered by
‘the transformed substance of the matrix, or immersed in it.
Isothea pustula Berk. Batheaston, winter ; on oak leaves,
GENUS 300. HYPOSPILA.t 7.
Perithecia globose, black, mouthless; altogether innate, concealed
by the blackened substance of the leaves, and when that falls
away, splitting across.
GENUS 301. STIGMATEAL Fr.
Parasitic. Perithecia globose, black, innate, slightly prominent.
‘Nucleus firm, at first mouthless, then bursting with a roundish
aperture.
Stigmatea geranii Fr. Batheaston ; on various Geraniums.
S——_—— robertiani Fr. On Geranium robertianum.
GENUS 302. oomMyces§ JB. and Br.
Perithecia erect, contained in a polished, coloured sac, which is
free above. Ostiola punctiform, apical.
Oomyces carneo-albus. B. and Br. Spheria Libert. On leaves
of Aira cespitosa. Batheaston and Bowood, autumn and
spring. Ann. of Nat. Hist., No. 590. Libert excicc, No. 241.
* Jsothea, beautiful.
+ Hypospila, from upo, beneath, and spilon, a stain,
{ Stigmatea, from stigma, a spot or mark,
§ Oomyces, from Oon, an egg, and muke, a fungus.
17
GENUS 302. Necrria.* . Fr.
Stroma none; or, if present, bearing the coloured, naked
perithecia on its surface.
Nectria cinnabarina Fr. Batheaston, common.
N——— coccinea Fr. Batheaston, common.
N——— ccucurbitula Fr. Batheaston, winter.
N——— sinopica Fr. Batheaston, January, 1856, on ivy.
N——— aquifolia Berk. Ashwick, April, 1854, on holly.
N——— inaurata B. and Br. Ashwick, April, 1854, on holly.
Ann. of Nat. Hist., No. 781.
N. citrino-aurantia Lacroiz. Decem., 1873, on willow twigs.
N——— ochracea Fr. Batheaston, Langridge, January, 1872.
N——— aurantia Fr. Batheaston, winter, 1869.
N——— Albertini B. and Br. Bathford, April, 1865.
N—— flavida Fr. Batheaston, March, 1877.
N——— furfurella B. and Br. Batheaston, February, 1869, on old
cabbage stalks. Annals of Nat. Hist., No. 1,331.
N. Peziza Fr. Rudlow, August, 1842, common.
N— sanguinea Fr. Rudlow, February, common.
N. epispheria Fr. Batheaston, winter, on old, decaying
hypoxyla.
N— Rousselliana Mont. Batheaston, March, 1859, on box
leaves.
N——— graminicola B. and Br. Batheaston, April, 1854. Annals
of Nat. Hist., No. 897, fig.
helminthicola B. and Br. Bathford, January, 1859.
Annals of Nat. Hist., No. 896, on Helminthssporia,
N——— ochraceo-pallida B. and Br. Batheaston, February, 1877.
Annals of Nat. Hist., No. 607, on dead elm.
erubescens Desm., on holly leaves. Clifton, Oct., 1879.
C. Bucknall; with a figure. Fungi of the Bristol District.
N—
N.
* Nectria, from necto, to join together, the perithecia of some of the
species being united by a definite stroma.
B
18
N. muscivora B. and Br., on mosses. Bristol. Annals of Nat.
Hist., No. 608.
N. mammoidea P. and Ph. Walton Hill, July, 1881. C.
Bucknall.
N— dacrymycella Nyl. Blaize Castle, May, 1882. C.
Bucknall.
N arenula B.and Br. Batheaston, February, 1851, on Aira
cespitosa. Annals of Nat. Hist., No. 622, with a figure.
GENUS 303. SPH#&RIA.* Hall.
Perithecia black, pierced at the apex, mostly papillate, superficial
or erumpent, without any stroma.
Series J. SUPERFICIALES.
Byssisede,
Spheria thelena Fr. Box quarries on timber underground.
April, 1872. William Broome.
aquila Jr. Batheaston, common on sticks. April.
tristis ode, Batheaston, common on sticks.
March, 1861.
S——— pheostroma Mont. Batheaston, January, 1859.
S————. racodium P. Spye Park, February, 1851.
S
S
S vervecina Desm. Rudlow, Dec., 1842, on the ground
in woods.
S Epochnii B. and Br. Warleigh. Annals of Nat. Hist.,
No. 1,177, with a figure, t. 5, fig 36.
Villosz.
S_———. ovina P. Batheaston, March, 1869, on rotten wood.
g——. brassicee KJ, Batheaston, April, 1869, on cabbage
stalks.
ee i ee
* Spheeria, from sphaira, a sphere.
19
canescens P. Lucknam Grove, April, 1866, on rotten
S
wood.
Ss hirsuta Fr. Batheaston, January, 1869, on wood.
Ss macrotricha B. and Br. Bathampton, February, 1851.
Annals of Nat. Hist., No. 619, with a figure.
S—_—. Chetomium Fda. Batheaston, winter, on Carex
pendula.
SS) eres B. and Br. Spye Park, February, 1850, on dead
carices. Annals of Nat. Hist., No. 621, with a figure.
S exilis_4. and 8. Lucknam Grove, March, 1859, on pine.
S pilosa P. Bathford, December, 1875, on decayed
wood.
8 hispida Tode. St. Catherine’s, January, 1852, on
decayed wood.
S membranacea B. and Br. Langridge, April, 1874, on
wood. Annals of Nat. Hist., No. 1493.
S———-_ barbula B. and Br. Belmont, near Bristol, March,
1859, on pine. Annals of Nat. Hist., No. 870, t. 10, f. 20.
exosporioides Desm. Batheaston, March, 1859, on
dead leaves of Carex pendula.
S——— felina Feks. Batheaston, March, 1869, on dead
stalks of Rubus.
Ss
Ss — cupulifera B. and Br. Langridge, April, 1869, on
decayed elm stumps. Annals of Nat. Hist., No. 1,333, witha
figure.
Ss pellita Fr. Leigh Wood, April. C. Bucknall.
S——— capillifera Currey. Leigh Wood, autumn. C,
Bucknall,
Denudate.
S—— bombarda Batsch. Rudlow, October, 1843, on wood.
S—— spermoides Hoffin. St. Catherine’s, 1869, on wood.
S- papaverea B. and Br. Batheaston, October, 1869, on an elm
stump. Annals of Nat. Hist., No. 612, with a figure
20
S——— moriformis Tode. Rudlow, February, 1843, on wood.
S innumera B. and Br. St. Catherine’s, March, 1871,
on wood,
Annals of Nat. Hist., No. 2,578. Tulasne Carpologia IL. p,
253, t xxxlii—f. 7 to 9. (Cheetospheria).
S- stercoraria Sow. Batheaston, January, 1867, on horse
dung.
s- pomiformis Pers. Rudlow, November, 1841, on old
apple trees. Annals of Nat. Hist., Series iv., Vol. 7, pl. xxi.,
_ fig. 28, conidia.
S——-— obducens Fr. Batheaston, January 7, 1852, on wood.
S——— pulvis-pyrius P. Batheaston, October, 1860, on wood.
S——— rhytidodes B. and Br, St. Catherine’s, January, 1852.
Annals of Nat. Hist., No. 873, with a figure. On ash pollards.
S——— perexigua Lév. Leigh Wood, April, 1877. C.
Bucknall.
Ss pulveracea Ehr. Batheaston, February, 1859.
NS) myriocarpa Fr. St. Catherine’s, May, 1864,
S vesticola B. and Br. Batheaston, December, 1858, on
old cloth. Annals of Nat. Hist., No. 874.
S——— rubicola Currey, M.SS. Batheaston, March, 1869 ; Lin.
Trans. 319.
S—— caudata Currey. L.c., with a figure.
S——— ostioloidea Che. on Hymenochete. Leigh Wood, January,
1878. C. Bucknall; Greville iv., 113.
S———- Stevensoni B. and Br. Stapleton, June, 1882. C.
Bucknall, Annals of Nat. Hist., No. 1,926. Fungi of the
Bristol districts, No, 1,016.
S——— platyspora (Sordaria) Ph. and P. Leigh Down, May,
1879. C. Bucknall.
equorum (Sordaria) Winter in Hedwigia, 1871. Leigh
Down, May, 1878, OC. Bucknall.
S——— merdaria (Sordaria) Fr. Leigh Down, May, 1878. C.
Bucknall,
s
21
S minuta (Sordaria) Winter, 1.c., var. tetraspora. Leigh
Down, January, 1881. C. Bucknall; with a figure, pl. 4,
fig. 6.
S curvula De By. (Sordaria) Hedwigia, 1871. Stapleton,
February, 1881. C. Bucknall,
8 pleiospora Winter, Grev. x., 72. Leigh Down, January.
C. Bucknall ; with a figure.
S——— Winteri Ph. and P. (Sordaria). Leigh Down, January,
1881. C. Bucknall.
bisporula Hans. (Sordaria). Leigh Down, March. C.
Bucknall.
S——— sparganicola PI. in littera (Sordaria). Yatton, July,
1881. C. Bucknall; on Sparganium ramosum.
S——— microspora Ph. and Pl. (Sordaria). C. Bucknall. Leigh
Down, with a figure, December, 1881. Grevillea x., 73.
Ss)
8 polyspora Ph. and Pl, (Sordaria), Grevillea x.,73. Leigh
Down, December, 1881. C. Bucknall,
s intermedia Awd. (Sporormia). Leigh Down, April, 1879.
C. Bucknall.
Pertuse.
S——— pertusa Fr. St. Catherine’s, February, 1852.
S——— brachythele B. and Br. Batheaston, February, 1859, of
dead elder. Annals of Nat. Hist., No. 877, with a figure.
S——— mastoidea Fr. Batheaston, January, 1857.
S——— vilis Fr. Batheaston, January, 1757.
8 pedida B. and Br. Langridge, April, 1859, on beech
wood. Annals of Nat. Hist., No. 1,396, with a figure, pl. x.,
fig. 13.
Series I]. ERUMPENTES.
Ceespitose.
$————- cupularis P. Batheaston, January, 1869.
S Saubinetii Mont. Batheaston, April, 1859, on elm sticks.
22
naucosa Fy. Batheaston, January, 1860.
nigerrima Blox. St. Catherine’s, April, 1867. Parasitic
on various Diatrypes. This seems to be the same thing as
Dothidea Jerdoni.
Obturate.
S——— obliterans B. and Br. Batheaston, on bare fir poles.
Annals of Nat. Hist., No, 890, with a figure.
Ss eulmifraga Fr. Rudlow, winter, 1851.
Lophiostome.
S macrostoma Fr. Spye Park, April, 1859, on holly.
NS caulium Fr. Batheaston, December, 1858.
S Arundinis Fr. Batheaston, March, 1854.
S——— angustilabra B. and Br. Annals of Nat. Hist., No. 881,
with a figure. Leigh Wood, April, 1852. C. Bucknall.
S——— bicuspidata Che. Bristol, near the Avon. C. Bucknall.
Ceratostome.
S rostrata Fr. Batheaston, December, 1866.
8 lampadophora B. and Rr. Combe Hay, May, 1859, on
elm stumps. Annals of Nat. Hist., No. 882, with a figure,
Batheaston, on white thorn.
S——— ligneola B. and Br. Batheaston, on decayed oak.
Annals of Nat. Hist., No. 883, with a figure.
8 ampullacea Che, Leigh Wood, February, 1877. C.
Bucknall,
Series III. sSUBTECTA.
Immerse.
S——— hypotephra B. and Br. Batheaston, January, 1861, on
oak palings. Annals of Nat. Hist., No. 624, with a figure.
Ss - velata P. Leigh Wood, April, 1882. C. Bucknall.
S——— verecunda Currey. Near the Avon, April, 1878. C.
Bucknall.
23
Endophlez.
S—— decedens F7. Batheaston, on hazel.
S——— apiculata Currey. Batheaston, on bramble.
S——— fraxinicola Currey. Brockley Coombe, May, 1869. C.
Bucknall.
S rubelloides Plowright. Cheddar, June, 1882.
S——— melanotes B. and Br. Leigh Wood, December, 1841.
Annals of Nat. Hist., No. 623, with a figure.
Endocaule.
S——— inquilina Fr. Langridge, March, 1853.
S——— phomatospora B. and Br. Batheaston, Nov., 1850, on
potato haulm, Annals of Nat. Hist., No. 647, with a figure.
S———._ spiculosa P. Batheaston, January, 1860, on goose-
berries.
Obtectee RAMEALES.
Ss siparia B. and Br. Spye Park, February, 1850, on birch
twigs. Annals of Nat. Hist., No. 625, with a figure.
S —— = unicaudata B. and Br. Batheaston, February, 1859, on
Clematis Vitalba. Annals of Nat. Hist., No. 885, with a
figure
S——— ssalicella Fr. Near Chippenham, March, 1859, on
willow.
g——— Argus B. and Br. Spye Park, on birch wood, Feb.,
1850. Annals of Nat. Hist., No. 626, with a figure.
S-_—. aucta B. and Br. Spye Park, April, 1852, on alder.
Annals of Nat. Hist., No. 625, with a figure.
gigaspora Desm. Batheaston, February, 1860, on maple.
conformis B. and Br. Spye Park, March, 1850, on
alder. Annals of Nat. Hist., No, 635, with a figure. .
g__-—._ trivialis B. & Br. Batheaston, March, 1854, on hazel.
Annals of Nat. Hist., No. 632, with a figure.
Ss
S
24
S——— peristens B. and Br. Batheaston, March, 1850, on
Rosa canina. Annals of Nat. Hist., No. 637, with a figure.
S——— futilis B. and Br. Batheaston, March, 1857. Annals
of Nat. Hist., No. 638, with a figure.
S———__ oblitescens B. and Br. Spye Park, January, 1851, on
Cornus. Annals of Nat. Hist., No. 887, with a figure.
melina B. and Br, Batheaston, March, 1850, on ash
wood. Annals of Nat. Hist., No. 888, with a figure.
S——— clypeata Nees. Batheaston, Leigh Wood, February,
1845, on Rubus.
S
S——— appendiculosa B. and Br. Batheaston, March, 1850.
Annals of Nat. Hist., No. 613, with a figure, on Rubus
fruticosus,
S——— rusci Wail. Batheaston, winter, on Ruscus aculeatus.
S——— obtecta Currey. Batheaston, November, 1878, on
alder. Annals of Nat. Hist., No. 979, with a figure (=S.
celata Currey-Cke).
S hemitapha B. and Br. Batheaston, Feb., 1852, on oak.
Annals of Nat, Hist., No. 885, with a figure.
S thodobapha B. and Br. Batheaston, April, 1869, on
dead branches. Annals of Nat. Hist., No. 1,334, with a
figure.
S——— quadrinucleata Currey. The Gully, Bristol. C. Bucknall.
S8——— deflectens Karst (Teichospora) Myc. Fennicx, Staple-
ton. December, 1878. C. Bucknall. Grevillea x., 73, with
a figure.
Herbicolz.
S tomicum Lév. Batheaston, January, 1850, on Aira
czespitosa.
S acus Blox. Batheaston, Jan., 1859, on stems of dock. |
Ss clivensis B. and Br. Bristol, near the Avon, April,
1878. C. Bucknall. Annals of Nat. Hist., No. 643, with
a figure. .
25
Caulicole.
S——— _ acuta Moug. Batheaston, on nettle stems.
S——— doliolum P. Batheaston, on herbaceous stems.
S———._ complanata Tode. Rudlow, on herbaceous stems,
winter, 1842,
S——— hematites Roberge. Batheaston, March, 1854, on
Clematis vitalba.
S. acuminata Sow. Rudlow, May, 1843, on thistles.
S——— Thwaitesii B. and Br. Batheaston, January and March,
1864, Annals of Nat. Hist., No. 646, with a figure.
S———-tenebrosa B. and Br. Batheaston, on Arctium lappa,
April, 1859. Annals of Nat. Hist., No. 649, with a figure.
parsnip. Annals of Nat. Hist., No. 643, with a figure.
S——— nigrans Rob. and Desm. Batheaston, June, 1847, on
Dactylis glomerata.
S——— tosta B. and Br. Rudlow, February, 1843, on Epilobicem.
_ Annals of Nat. Hist., No. 648, with a figure.
cariceti B. and Br. Batheaston, December, 1858, on Aira
exspitosa. Annals of Nat. Hist., No. 983, with a figure.
S——— planiuscula B. and Br. Batheaston, June, 1857,
on Umbellifere. Annals of Nat. Hist., No. 891, with
a figure.
S—— rubella P. Clifton, April, 1878. C. Bucknall.
S——— superflua Awd. Durdham Down, May, 1878. C.
Bucknall.
S——— ulnaspora Che. West Town. C. Bucknall.
S——— agnita Desm. Bristol, near the Avon, May, 1880. C.
Bucknall. |
S——— infectoria Fekl. Bristol, near the Avon, May, 1880. C.
Bucknall.
S——— endopteris, Plowright (in littera). Leigh Down, April,
1882 ; Bristol district, Fungi of, on Pteris aquilina, with a
figure. C. Bucknall.
Ss
26
Ss— Ogilviensis B. and Br. Leigh Wood, June, on Senecio
jacobea, Annals of Nat. Hist., No. 642, with a figure. C.
Bucknall. %
S——— herbarum P. Batheaston, on various plants,
S——— typhecola Che. Grevillea v., 21.; Pill, April, 1882. C.
Bucknall.
Foliicole. Rostellate.
S——— setacea P. Rudlow, February, 1843, on oak leaves.
s— tubeformis Tode. Batheaston, March, 1843, Spye Park.
S——— gnomon 7ode. Batheaston, March, 1852.
Ss— avellanee Schmidt. Batheaston, January, 1867.
Ss— ostruthii Fr. St. Catherine’s, December, 1850.
Spherostome.
S——— pheosticta B. Batheaston, January, 1850, on Carex
pendula. Annals of Nat. Hist., No. 651, with a figure.
S——— anarithma B. and Br. Batheaston, June, 1867. Annals
of Nat. Hist., No. 893, with a figure.
sS—— caine B. and Br. Batheaston, January, 1850, on
Carex paniculata. Annals of Nat. Hist., No. 654, with a figure.
S eucrypta B. and Br. Batheaston, January, 1850, on
Carex pendula, Annals of Nat. Hist., No. 652, with a figure.
S——— rumicis Desm. Batheaston, December, 1851, on dock.
8 helicospora B. and Br. Spye Park, Batheaston, June,
1867, on Carices. Annals of Nat. Hist., No. 653, with a
figure.
8 brassicecola B. and Br. Batheaston, on cabbage leaves
(Asteroma brassice Chev). Annals of Nat. Hist., No. 656,
with a figure,
S——— punctiformis Fr. Batheaston, on dead leaves ; winter.
NS) alliarie 4wd. Stoke, near Bristol, April. C. Bucknall.
S——— italica Sace. Clevedon, Mr. Green (Sace, sylloge, No.
1,107, anthostoma),
27
GENUS 304, SPHARELLA.* De Not.
Perithecia membranaceous, immersed or semi-immersed, scarcely
papillate, sporidia elliptical or oblong, two or more celled, rarely
simple, hyaline, pale or colourless.
Spherella maculzformis (P.) Che. Batheaston, on dead leaves.
S — errabunda (Desm.) Awd. Batheaston, May, 1871, on
beech leaves.
s—— carpinea Fr. Batheaston, on hornbeam, Annals of
Nat. Hist., No. 655, with a figure.
S—— _ hedereecola Fr. Batheaston, May, 1851 (Depazea).
S———— dianthi Desm. Batheaston, March, 1851, on carnations.
S———— inequalis Che. Durdham Down, March, 1879. C.
Bucknall.
S————- taxi Che. Leigh Wood, February, 1878. C. Bueknall.
8 — oblivia Cke. Brockley Coombe, May, 1879. C,
Bucknall.
S———— latebrosa Che. Leigh Wood, May, 1879. C. Bucknall.
GENUS 305. MASSARIA.t De Not.
Perithecium subcarbonaceous, Ostiolum papilleform, Sporidia
septate or simple, oozing out and staining the matrix.
Massaria inquinaus Fr. Batheaston, on elm branches.
M fedans Fr, Batheaston, with conidia, February, 1852.
(Sph. amblyospora B. and Br.)
M——— macrospora Desm. Box, March, 1843, on beech.
M eburnea Zul. Batheaston, December, 1858, with conidia
(Septoria princeps B. and Br.) Annals of Nat. Hist., No.
940, with a figure.
M fimeti Fr. Bathford Hill, on rabbits’ dung.
M holoschista (B. and Br.) On alder, Spye Park.
Annals of Nat. Hist., No. 977, with a figure.
* Spherella, a diminutive of Sphzria.
+ Massaria, so named in honour of Dr. Massare, a botanist,
28
GENUS 306. HYPOCREOPSIS.* Winter, Hedwigia, 1875.
Compound ; perithecia immersed in a fleshy red stroma, covered
on the surface by a reddish down; ostiola erumpent, darker ;
asci oblongo-ventricose, subsessile, 4 to 8 spored ; sporidia elliptic,
simple, hyaline. Hedwigia Vol. 5, p. 123.
Hypocreopsis pulchra, Winter. On sheeps’ dung, Bathford Hill,
October, 1874.
GENUS 307. HERCOSPORA.t F*r.
Perithecium subcarbonaceous, cup-shaped, open above, covered
by the bark, and differently coloured ; papilla heterogeneous,
erumpent,
GENUS 308. PYRENOPHORA.S JF’.
Nucleus slowly formed, immersed in a sclerotioid mass which
performs the office of a perithecium, Ostiolum at length slightly’
prominent, Sporidia mulsetiptate.
Pyrenophora pheocomes Fr. Radlow, June, 1843, on Alisma
plantago.
GENUS 309. GIBBERA§ Fr.
Perithecium between waxy and horny, at length free, radiato—
rimose from the centre, always closed.
Gibbera pulicaris /r. On various branches, common.
G——— Saubinetii Mont. Batheaston, on twigs of elm, &e.
GENUS 310. DICHANA|| 7.
Perithecia subcarbonaceous, elliptic, closed, bursting by a longi
tudinal fissure. Nucleus and asci diffluent, innato-erumpent.
Dichena rugosa /r. On living barks of oak and beech.
* Hypocreopsis, from its resemblance to Hypocrea.
+ Hercospora, from erkos, an inclosed space and sporos a seed.
+ Pyrenophora, from puren, a core or kernel, and phoreo, to bear.
§ Gibbera, from gibber, hunch-backed.
|| Dichzena, from dis, twice, and chaino, to crack or gape.
29
GENUS 311. cAPNopIUM.* ont.
' Parasitic, Mycelium ereeping, black, consisting of branched,
articulated, even or monliform threads, Perithecia elongated,
frequently branched, composed of confluent threads, the tips of
which are often free.
Capnodium elongatum 2. and Desm. On pear leaves, common.
C—— sphericum Oke. Leigh Wood, February, 1878. C.
Bucknall.
ORDER 27. PERISPORIACEI.
Perithecia subglobose, always closed, except in decay, mostly
membranaceous. Nucleus never diffluent.
GENUS 312. PERISPORIUM.t 7%.
_ Peridium subglobose, without any manifest thallus or append-
ages. Asci clavate. Spores indefinite.
Perisporium vulgare Cda. Batheaston, on old rope, November,
1864.
GENUS 313. LASIonoTRYS.{ Kye.
Erumpent. Central peridium between fleshy and horny, pro-
liferous, collapsing above, attached to radiating fibres. Secondary
peridia ascigerous. Asci cylindrical.
GENUS 314. SPHZROTHECA.$ Lév.
Mycelium arachnoid. Perithecia globose, containing a single
globose ascus. Appendages numerous, floccose.
Sphzrotheca pannosa Lévy. On the leaves and shoots of roses,
very common.
S$ —————— castagnei Lév. On hops.
* Capnodium, from capnédes, smoky.
+ Perisporium, from peri, around, and sporos, a seed,
t Lasiobotrys, from lasios, hairy, and botrus, a bunch of grapes.
§Spherotheca, fromsphaira, a globe, and theke, a receptacle.
30
GENUS 315. PHYLLACTINIA.* Lév.
Parasitic. Perithecia hemispherical, at length depressed, seated
on a persistent or evanescent membranaceo—granular receptacle.
Appendages straight, rigid, acicular, at length bent back.
Phyllactinia guttata 77. On various leaves, Batheaston, common.
GENUS 316, UNCINULA.t Lév.
Mycelium floccose. Perithecia globose, Appendages rigid,
simple, bifid or dichotomous, uncinate, at length bent upwards.
Uncinula adunca Lév. On poplar and other leaves, common.
U bicornis Lév. On maple leaves and other leaves,
common.
GENUS 317. MiIcROSPH@RA.{ Lév.
Mycelium arachnoid. Appendages straight, dichotomous.
Branchlets swelling at the tip, or filiform.
Microsphera penicillata Lév. Bathford, September, on hazel.
GENUS 318. ERYSIPHE$ edu.
Mycelium arachnoid. Appendages floccose, simple, or irregularly
branched.
Erysiphe tortilis Zév. Rudlow, September, common.
E communis Schlecht, on various leaves.
E— macularis Fr, Batheaston, July, on hops.
GENUS 319. CEPHALOTHECA,|| ekl.
Symb. Mycol. der-theinischen Pilze.
Perithecia simple, free, carbonaceous, very fragile, composed of
* Phyllactinia, from phullon, a leaf, and aktin, a ray or spoke of a wheel.
+ Uncinula, from uncinus, a hook.
t Microsphera, from micros, small, and sphaira, a sphere.
§ Erysiphe, from Erysibe, mildew.
|| Cephalotheca, from cephalos, a head, and theke, a receptacle.
31
_ small pentagonal or hexagonal, radiato-striate cells, globose, and
at first clothed on all sides with villose hairs, then glabrous,
brown or black at the apex; asci at first seated on the tips of
branched threads forming globose clusters, afterwards free,
8-spored. Sporidia heaped together, then free, simple, ovate or
subfusiform ek. I find globose asei seated laterally on irregular
hyphe, filled with globose sporidia.
Cephalotheca sulfurea /kl., on the underside of damp boards in
Mr. Percival’s grapery at Henbury, near Bristol. The ville
are bright, sulphur-coloured, the threads and sporidia pale.
sulphur. Annals of Nat. Hist., No. 1,729, with a figure.
GENUS 320. CH#ZTOMIUM.* Kze.
Perithecium thin, brittle, mouthless. Asci linear, containing
dark, lemon-shaped sporidia.
Chetomium elatum Kze and Schmidt. Leigh Wood, Bristol, Oct.,
1859, on an old, cast-off dress.
C————. graminis Rabenh, Rudlow, November, 1842.
C rufulum £. and Rr. Batheaston, May, 1871, on an
old paper box under a bell glass. Annals of Nat. Hist.,
No. 1,397, with a figure.
C— chartarum Ehb. Batheaston, April, 1862, on damp
paper in a tin box.
GENUS 321. ASCOTRICHA.t Berk.
Perithecium thin, free, mouthless, seated on loose, branched,
conidiiferous threads. Asci linear, containing dark, elliptic,
sporidia. Annals of Nat. Hist., No. 116.
Ascotricha chartarum Berk. Batheaston, June, 1874. The
conidia are at first developed in a mucous (hollow 1) globose:
mass, which at length disappears, on damp paper.
* Chetomium, from chaite, a hair.
+ Ascotricha, from ascos, a sac, and thrix, a hair.
32
GENUS 322. EuROTIUM.* Lk.
Perithecia reticulated, vesicular, coloured, attached to
mucedinous threads, asci delicate. ;
Eurotium herbariorum Zk. Batheaston, on plants in herbaria.
This is considered merely an ascigerous state of Aspergillus.
St. Catherine’s on damp sticks and leaves in the woods.
ORDER 28. ONYGENEI.
Peridium formed of loosely interwoven threads. Sporidia at
length forming a compact, dusty mass.
GENUS 323. ONYGENAS P.
Parasitic on animal substances. Peridium stipitate or sessile,
paper like, at length splitting. Asci delicate. Sporidia at length
forming a dusty mass.
Onygena apus B. and Br. Hanham, on bones buried in the soil
in woods.
FAMILY VI. PHYSOMYCETES.{
Threads free, or only slightly felted, bearing vesicles which
contain indefinite sporidia,
ORDER 29. ANTENNARIEIL.
Threads black, more or less felted, moniliform and equal in the
same felt, bearing here and there irregular sporangia.
* Eurctium, from euros, mouldiness,
+ Onygena, frem onux, a hoof, and ginomai, to spring from.
+ Physomycetes, from phusa, a bladder, and muke, a fungus,
33
GENUS 324. ANTENNARIA.*~ Lh.
Threads felted, black, articulated, often moniliform. Walls of
sporangia mostly cellular. Spores chained together, immersed in
gelatinous pulp.
Antennaria semiovata B. and Br. Hanham, on fronds of Filix mas,
September, 1853. Annals of Nat. Hist., No. 784, with a figure,
_ GENUS 325. ZASMIDIUM.+ Fr.
- Sporangium thin, carbonaceous but brittle, growing on a septate,
byssoid, equal mycelium. Mouth subumbilicate. Spores simple.
Zasmidium cellare. Common in wine cellars, forming brown,
byssoid tufts, rarely forming any fruit.
ORDER 30. MUCORINI.
Threads free, bearing terminal or lateral appendages.
GENUS 326. ascopHoRA.t Tode.
Sporangia collapsing, and at length hanging down over the
fructifying apices like a hood. Fruit sometimes of two kinds.
Ascophora mucedo Tode. On bread, common.
GENUS 327. MucoR.§ Mich.
Threads free, Sporangia at length bursting, but not dependent.
Mucor amethystiuus Berk. Rudlow, October, 1847, on rotting
pears.
M ramosus Bull. Box, October, 1863, on rotten wood.
M mucedo LZ, - On paste, very common.
M fusiger Lk. Rudlow, October, 1843, on rotten Agarics,
* Antennaria, from antenna, a sailyard.
+ Zasmidium, perhaps from zosma, a kind of seaweed.
{ Ascophora, from ascos, a vessel, and phero, to bear.
§ Mucor, mould.
Cc
34
GENUS 328. HYDROPHORA.* Tode.
Threads erect, tubular, sparingly articulate, equal above, ter-
minated by a vesicle which is at first watery and crystalline, then
turbid, and at length indurated and persistent from the conglo-
meration of the spores.
Hydrophora stercorea Tode. On dung, common,
GENLS 329. ENDODROMIA.| Berk
Vesicle very delicate, perforated by the stem, filled with
delicate, branched, radiating threads, and globose spores, with a
nucleus endowed with active motion.
Endodromia vitrea Berk. Hook, f. 1., 1841, iii, t. 1, fig. C.; has
not occurred in the district.
GENUS 330. SPORODINIA.{ Lk.
Stem dichotomously branched. Vesicles solitary, terminal,
at length splitting horizontally. Columella large. Spores
simple, growing on the columella. This genus has not occurred
in our district.
GENUS 331. ACROSTALAGMUS§$ Cda.
Flocci branched. Branches verticillate. Vesicles terminal,
pierced by the threads, from the tips of which the spores are
produced within the cells.
* Hydrophora, from udor, water, and phero, to bear.
+ Endodromia, from endos, within, and dromos, a running about.
t{Sporodinia, from sporos, a seed, and dineuo, to whirl about or
move. Link remarks “continuatio Wild,c. I. p. 94, ‘ Ehrenberg vidit
massam sporulosam e floccis in sporangium moveri.
§ Acrostalagmus, from akros, pointed, and stalagmos, a drop, or a state
of dropping.
35
Acrostalagmus cinnabarinus Cda. Batheaston, on decaying plants,
Verticillium lateritium. One of the Mucedines is found to
be a form of this species, with naked spores. See Corda
Icones c, ii, 15, t. 10, fig 66.
GENUS 332. syzyGiTEs* Jhb.
Threads branched above. Vesicles of separate branches con-
jugating, and forming a distinct sporangium.
Syzygites megalocarpus Ehb. Has not occurred in our district, at
least in its perfect state.
GENUS 333. ENDOGONE.Tt Lk.
Hypogeous. Flocci collected into a globose, spongy mass.
Vesicles globose, solitary, or collected in little fascicles at the ends
of the branches.
Endogone pisiformis Zi, Near Bristol, in woods, autumn. .
Onan abnormal Flower of a Penstemon, By C, E. Broome, F.L.S.
(Read March 18th, 1885.)
A flower of a Penstemon, communicated to me by C. Timmins,
Esq., in May, 1884, presented the following peculiarities :—
The calyx was leafy, the calyx leaves nearly those peculiar to
the species, the corolla was situated closely above the calyx and
was composed of segments partly green and partly blue, one
stamen with its filament was normal; the other four stamens
were converted into distorted green, leafy appendages; the style
* Syzygites, from sun, together, and zugon, a yoke.
+ Endogone, from endon, within, and gone, seed.
36
‘was prolonged into a green stalk about one inch in length, which
was furnished with two leaves of the normal form. About two-
thirds up there was a flower bud, above which the stem was
again continued for about a quarter of an inch, and surmounted
by a whorl of four leaves with an axillary flower bud as before.
The above were the features presented by the specimen sent
me, and they would seem to come under Dr. Master’s case of
prolification of the flower mentioned in page 115 of his
Teratclogy. Where the centre of the flower is occupied by a
bud or branch, the growing point, or termination of the axis,
which ordinarily ceases to grow after the formation of the carpels,
has here taken on new growth. The mixed colours of the corolla,
in the present instance partly green and partly blue, were of
interest as tending to show the true nature of the floral leaves,
viz., that they are merely the ordinary leaves of the plant
converted into petaloid leaves, I do not find the genus
Penstemon among those in which such reversion has been
recorded, it has been observed, however, in other genera belonging
to the order Scrophulariaceew, as Verbascum. Similar transfor-
mations are not uncommon in other orders.
Dr. Masters gives a remarkable instance in a flower of a cherry
in which there was‘a gradual change from the floral to the foliar
condition ; there were five distinct lanceolate sepals, the arrange-
ment of whose veins betokened that they were leaf-sheaths
rather than perfect leaves, ten petals partly foliaceous and sheath-
like as to their venation, one of them funnel-shaped. The
stamens were ten in number, their connectives prolonged into
foliaceous appendages so that the filament represented the stalk
of the leaf. The pistil was entirely absent, and its place was
supplied by a branch with numerous perfectly formed stipulate
leaves. The genus Plantago presents numerous instances of this
kind of transformation, its monstrosities are not uncommon in our
gardens, and that of P. major is frequent in our fields, it is also
common in cultivated roses.
37
It seems probable that the prolification of the parts of flowers
arises from over luxuriance of growth, since a check given to
vegetative development, as by root pruning, &c., tends to the
production of flowers and fruit, as is well known to gardeners,
and the converse doubtless holds true, and plants which increase
freely by scions, &c., are less free to blossom and produce seed.
Notes on Roman Paving Found in Bridewell Lane. By T.
BROWNE, Esq.
(Read March 18th, 1885.)
At the request of our Secretary, I have brought together a few
notes on the fragments of tesselated Roman Pavement that were
found in August, 1884, in digging the foundations for a new
building in connection with the Mineral Water Hospital.
The largest piece was found near the south-west corner, and
under the old front wall of what had been a public-house known
as the “Sedan Chair,” at a depth of about 7ft. Qin. below the
pavement of the lane. The Paving was an irregular fragment
that would be included in a measurement of 6ft. each way. A
careful exploration was made for some distance all round, in hopes
of finding more; but nothing further was discovered. The
original Paving seems to have been largely destroyed in the
making of a drain from the old public-house to the sewer, no
doubt many years ago.
A small fragment was also found at about the same depth near
the north-west corner of the building, and} almost in a line with
the other, and at about the same level.
On comparing the depth at which the Paving was found with
that which was discovered in 1859, when the Blue Coat School
and Mineral Water Hospital were built, it appears that these
fragments are about 3 ft. below the level of the old Roman
38
Paving which was then found, and is still preserved in sifu in the
basement of the Hospital.
The annexed photograph of the large fragment will give
some idea of the patterns of the work. It will be seen that this
was very richly designed, with a series of large octagons
measuring 2ft. 8in, across, and containing in the interior of
each a series of circles in small stones, and between the circles
and the margins were foliated patterns worked in coloured stones.
Apparently there must have been considerable variety of design
in the whole of the original Paving, for we have here only one
complete octagon, and fragments of two others, and the patterns
are different in each. The small squares and triangles filling in
the spaces between the several octagons and the outer borders are
filled in with rows of tesserae with reversed squares of colour.
On the outer border there is a line of dark tiles, and beyond
this again we found a margin of tiles laid herring-bone fashion
and of which three rows could be traced. This was no doubt
intended to fill up the space between the ornamental centre and
the walls of the room ; but no trace of the walls could be found.
The Paving was bedded upon fine red concrete made from
pounded bricks and lime—at least six inches thick, and resting
upon the earth.
The Pavement has been carefully lifted up in pieces, and
secured to a fresh base of cement; and it was found to be in
such a loose, rotten state, and the surface so damaged that it was
most difficult to lift up anything but small portions at a time.
A few of the tesserae have thus got slightly misplaced ; but as a
whole the patterns are nearly as perfect as when first discovered.
A portion has been brought here for the inspection of the
members.
The small fragment of Paving found at the north-west corner
is of a much plainer character, and consists of a series of squares
with dividing lines and border, and was probably from a room
not considered worthy of a more ornamental Paving.
39
The tesserae in both cases appear to consist of pieces of white
and blue lias, red brick or tile, and a purply red sandstone, all
of which were probably obtained not far from Bath. Many of
the stones are decayed and rotten, and would scarcely bear
handling when once uncovered, no doubt from the effect of wet
and corrosion in the ground, and subsequent drying in the air.
Of course the question naturally arises whether these fragments
have any connection with those found some 25 years ago at the
adjoining Hospital and Blue Coat School, and I think there can
be very little doubt that they all belong to the remains of a
Roman building of some importance, but of which no sufficient
remains are left to enable us to form any definite idea of its
extent or plan.
A great many irregular masses of concrete were found on the
site (apart from these fragments) at different points, but they
had been so broken and disturbed that no theory or idea of any
regular plan could be derived from them, although they all
appeared to be similar in character arid. of the well-known Roman
composition. ecg?
The governors of the Hospital have taken great interest in the
discovery of these fragments of Paving, and have had them
permanently preserved in their new building.
The Bournemouth Firs; considered as the Remains of an Ancient
Forest. Was there ever a Forest of Firs on the Hills around
‘Bath? By the Rev. LEONARD BLOMEFIELD, V.A., F.LS.,
F.GS., &c., President.
(Read December 9th, 1885.)
No one who has been at Bournemouth, and noticed the fir trees
that give so peculiar a character to that place—if he take any
interest in the suhject,—can fail to desire some information as to
their origin and history. Yet he would find it difficult to get his
curiosity satisfied, and be obliged, in great measure, to work out
40
the question for himself as he could. During a visit paid to
Bournemouth this last summer (1885) I was surprised to find how
few persons seemed to know much about these firs or cared to
consider the matter. The usual guide books scarce afford any
help, except on one point, to which I shall revert hereafter. They
speak of the firs as having been always there and forming part
of the place, and they go no further. Persons, however, who
say this do not consider of what modern growth the whole place
and its surroundings are, whether as a place of sea-side resort for
the public, or for permanent residence on the part of the large
numbers who have made it their home; nor set themselves to
inquire what was the state of things previously,
As the place appears now, broad roads, equal to any in England,
are seen branching off in various directions with elegant houses
or villas on either side, at intervals, each having its own grounds
and garden; the firs that have been left simply growing by the
sides of the roads, or along the sides of the gardens, where
they often form a boundary, as it were, between two contiguous
properties. These roads and houses are mostly on the cliffs, or
they run back more or less away from the sea; the town—
properly so called—being at the bottom, nearly at sea-level,
and, much like the towns in other watering places, calling for no
particular remark.
What now was the character of the place before all these roads
and buildings came into existence? I was informed by a lady
living in the neighbourhood, that an aged acquaintance of hers
had known the locality ever since the early part of this century,
when hardly a single building had been erected, or the first step
taken towards bringing it into its present condition. It was in
its wild primitive state—an enormous forest of Scotch Firs, with
scarce any break, reaching for miles away from the sea into the
surrounding country. Who, now, planted all these firs, supposing
them for a moment to have been planted? Not one man, nor
many men. Is it likely either that the several owners of the
4]
different properties, over which the forest must have extended in
those days, would have all come to one agreement in this matter ?
Let us bear in mind the contiguity of this forest of firs to the
New Forest in Hampshire. The latter was formerly much more
extensive than it is at the present day. “ By some it is thought
probable that William, instead of actually creating the forest,
simply added to the extent of a vast tract of woodland which
previously existed there.”* Wise, too, states that the forest
“ occupied nearly the entire §.W. angle of Hampshire:’+ if so it
must have been conterminous with the Bournemouth forest, or
mixed up with it. And though the New Forest is more
distinguished at the present day for its oaks, beeches, and birches,
&c. than for its conifere, it must surely have had formerly
a large growth of firs in addition to the trees above mentioned,
or at least in certain parts of the forest. - Lymington
Heath is spoken of in the “New Forest Guide Book,”
as “a vast stretch of heather and gorse extending down to the
“Beaulieu estate, broken here and there by a few barrows and a
« solitary fir tree, presenting a wild, inhospitable and dreary scene.”
To my thinking, these solitary fir trees here and there are the
sole survivors of a much larger number formerly growing in
that part of the forest. According to a statement in the Times
newspaper, “ there are hundreds of thousands of Scotch Firs in the
New Forest at the present time.”{ Probably a large number of
these have been planted, but the circumstance shows how con-
genial the soil and other conditions of the forest are to the
habits of the fir.
As for the firs in the original Bournemouth forest, they must
have been practically innumerable. It is said that even at the
present day, notwithstanding the clearances that have been made,
peng ARE AREF SS
* New Forest Hand Book, 2nd Ed., p. 8. See also Leland, Itineraries,
2nd Ed.,, vol. vi., p. 88.
+ History of the New Forest, p. 20. { Times, September 19, 1885.
42
‘upwards of three million pine trees remain in the different
districts of Bournemouth and its immediate surroundings.”*
The gravels and sands, which cover so large a portion of the
Bournemouth district, seem naturally favourable for the growth
of the Scotch fir, and seedling plants abound everywhere, which
if left to themselves would soon grow up into a thick plantation.
There are a few groups of firs lying some way east or north east
of the pier—one group especially, at the termination of the cliff
road, and just within the one-mile radius, of a somewhat
rectangular form, and reaching quite to the cliffs edge—which
distinctly give the idea of having been self-originated and
undisturbed by man. In this last group, away from all buildings,
the trees present a very uniform appearance. They are near
together, and of a fair height; but from never having been
thinned out, are drawn up into mere poles, with a considerable
brush of foliage at top, the ground underneath being quite bare
of grass or any other herbage.
There are, again, a few trees very much larger than any of the
above; one especially, known to the inhabitants of the
neighbourhood by the name of “The Four Evangelists,” from
its spreading out, a few feet from the ground, into four large
branches. This tree, thought by a friend resident in Bournemouth
to be the largest in the district, stands in the angle formed by
Grove Lane and the road leading from Christchurch to Herne
Court. I measured it with the help of another party, and found
it to be 13 feet and a half in girth, at about three and a half feet
from the ground.t It is between three and four miles from
Bournemouth, and had probably grown up, in times far back,
near the border of an old forest, or in some open space, where
with more light and air, it had room for expansion.
* Fortnightly Review, Sept., 1885, p. 386.
+ Loudon mentions firs in the Scotch forests 18 and 20 feet in girth,
but does not say at what height from the ground, Arboretwm Britannt-
cum. vol. iv. p. 2169.
43
There are other trees under conditions very different from those
of the trees last mentioned ; trees on the edge of the cliff, exposed
to the full force of winter storms, dwarfed, bent and distorted in
various ways; others, below the cliffs, struggling, as it were, for
life amid the shelving sand heaps threatening, to all appearance, to
drag them gradually down into the sea.
I have entered into the above details, as affording strong
ground, in my opinion, for believing that the Bournemouth
firs are true natives of that part of the country,—in
opposition to those who assert that the Scotch fir, though
indigenous in Scotland is not indigenous in England. Let us
now go into this argument which dates back to the well known
statement in Cesar’s Commentaries that there was the same
timber in Britain as in Gaul, except the fir and the beech—
“ preter fagum atque abietem.” This remark of Czsar’s, however,
is of little worth. First, he could have seen scarce anything
of Britain except Kent and the Thames district ;* secondly, in
addition to the fir, he mentions the beech as not found in Britain,
where he is certainly wrong, as witnessed by Windsor, Epping,
Savernake, and many other native woods and forests; thirdly,
firwood is recorded “to have been found under the foundation of
some Roman roads.”+ In truth, firwood is abundant in many of
the ancient mosses in England, and old roots of the Scotch Fir are
found in the bogs of Ireland. In an Article on the Conifere in
the Edinburgh Review it is stated that “remains of the Scotch Fir
“are plentifully distributed in the northern peat bogs ; and that
“the tree appears to have covered large districts, and to have
“flourished continuously on the same spot for long periods of
“time , .. . It has maintained its place, not by the long
* “Cresar’s account (of Britain) is necessarily confined to Kent, the
district known to him.” Scarth’s Roman Britain, p. 5.
+ Notes and Queries, vol. i. (Sixth Ser.), p. 78.
t Withering, British Plants, and other Authors.
44
“endurance of individual trees, but by successive propagation. It
“was the prevailing tree not only in England and Scotland, but
“over much of the north of Europe.” In the sunken forest at
Cromer, in Norfolk, in a deposit of a period immediately preced-
ing the glacial, even the spruce fir is found as well as the Scotch.
This was proved by the cones being submitted to the scrutiny of
the celebrated Robert Brown, the first botanist of his age, who
pronounced them to be those of the spruce.*
The Spruce, however, did not survive the glacial period, and is
consequently, in this country, extinct ; but the Scotch Fir continues
on to the present day, its range being now confined mainly to the
Scotch mountains, though formerly extending to several of the
northern counties of England. Gerard, in his “ Herball,”t
speaking of the ‘‘firre tree,” says—I have seen these trees
“ growing in Cheshire, Staffordshire and Lancashire, where they
“grew in great plenty, as is reported, before Noah’s Flood ; but
“then being overturned and being overwhelmed, have lien since in
“the mosses and watery moorish grounds, very fresh and sound
*See an Article on the Conifere, Edin. Rev., Oct., 1864, p. 347;
also a Lecture by the late Professor Rolleston, on “The modifications
of the externa] aspects of Organic Nature produced by man’s In-
terference,” 1880, p. 13. See, further, Winch’s ‘‘Essay on the
geographical distribution of Plants through the counties of North-
umberland, Cumberland and Durham, 8vo., 1825.” In this essay are
some remarks of much interest on the subject in question. The
author says—“ On some of the elevated moors of this district the
“roots and trunks of very large pines (P. Sylvestris) are seen
protruding from the black peat moss, being exposed to view by the
‘‘water of these bogs having drained off and left the peat bare, but
“this tree is no longer indigenous with us.” He then adds—“It is
“worthy of remark, that the Scotch Fir does not at this day attain
“the size of these ancient pines, though planted in similar moorland
“situations, even though the young trees be protected, and the
“plantations situated at a lower level.”
+ Ed. 2, by Johnson, 1636, p, 1364.
45
“ until this day.” We may smile at a part of this statement, but
what Gerard had seen himself is a direct proof of the matter in
question ; and there are other statements that bear evidence the
same way. Merrett, in his ‘Pinax Rerum Naturalium
Britannicarum,” published in 1666,* under the head of Abies, the
Fir tree, writes—“in Alpibus Scoticis, et quondam in plurimis
Angliz locis Borealibus.”—Ray, in his ‘Synopsis Stirpium
Britannicarum,” first published in 1696, nearly repeats the same
words. Wordsworth, the poet, in a private letter, gave it as his
opinion that the “ Westmoreland mountains were formerly
“covered in some places to their very summits by pines (the
“ Highland Pine).” He speaks of many that had survived, and
were living when he was a boy.t Selby, in his “British Forest
Trees,” considers that formerly the Scotch Fir ‘“ occupied most
‘of the elevated tracts of the kingdom, though the natural
“forests now remaining are confined to the mountainous districts
“ of Scotland.”{ Hooker, in his “* Student’s Flora of the British
Islands, ”§ says of the Pinus sylvestris, “ Highlands, ascends to
2,200 feet, rare in a native state ; formerly native over many parts
of Britain.”
Coming down now to the southern counties of England, we
have important testimony in two local Floras. of comparatively
recent date, ‘‘Mansel-Pleydell’s Flora of Dorset,” published in
1874, and Townsend’s “ Flora of Hampshire,” published in 1883.
It is on the confines of these two counties that Bournemouth is
situated, and in consequence each author has something to say on
the subject of the fir trees.
Mansel-Pleydell speaks of the Scotch Fir as common on heathy
places, but_ considers it a doubtful native of Dorset. Neverthe-
less he states it is to be found in all the four adjacent counties of
Devon, Hants, Somerset and Wilts.||
ill eS as, aa
*P.1, + Notes and Queries, vol. 3 (2nd Ser.), p. 445. {P. 399.
§ 2nd Ed., 1878, p. 368. | Flora of Dorsetshire, p. 232.
46
Townsend, though he too calls the Scotch Fir “a doubtful
native,” speaks of it as ‘‘common on the heaths around Bourne-
mouth,” and shortly afterwards says “there are abundant evidences
that the pine formerly grew wild throughout the county.”
In another place he says—“ it seems to me possible that living
pine trees in some parts of the county may be descendants from
the wild plant.”+
Such is the testimony afforded by botanists, in favour of the
Scotch Fir being indigenous in England as well as Scotland. Other
testimony is afforded to the same effect by local names. ‘Taylor,
in his “ Words and Places,” thinking to confirm Czsar’s statement
above alluded to, ventured the assertion that—“‘In no single
instance throughout the Anglo-Saxon charters do we meet with a
name implying the existence of any kind of pine or fir, a circum-
stance which curiously corroborates the assertion of Cesar, that
there was no fir found in Britain.”{ I have the high authority
of Mr. Earle, the Professor of Anglo-Saxon, for saying that here
“Taylor is wrong ;” and Mr. Earle has kindly looked out for me
several names of places all of which he considers as undoubtedly
derived from the fir: such are Firbank in Westmoreland,—Fur-
becke (or Firbeck) in West Riding, and Firbie (or Firby) and
Furgarth in East Riding, Yorkshire,— Furbie (or Firby or Firsby)
in Lincolnshire,—Furcombe, in the parish of Farnborough, Berks,
—Furlé (or Furleigh) in Sussex, Pevensy Rape.
In addition to the above local names, I mentioned to Mr. Earle
two others in the south of England,—Furland, a tithing of Crew-
kerne in Somerset, and Furland Hill, one of arange of hills between
Brixham and Dartmouth : both of which he had no doubt, were
also named after the fir tree.
But I come now to a still more important fact, in especial con-
nection with the fir trees at Bournemouth. It is the circumstance
* Flora of Hampshire, pp. 321-2.
+ Words and Places, Ed. vi., p. 249:
47
I alluded to in the beginning of this paper as mentioned in the
Bournemouth guide books. We read that “the remains of a
“submerged forest may, under certain conditions of the beach,
“be seen at the mouth of the valley, on the western side of the ©
“pier, This was especially the case in the early months of the
year 1871, when some four or five of the remains of the trees,
“tof which near thirty were at one time exposed, were removed
‘‘ for examination, and were proved to be the Pinus Sylvestris or
“common fir of the district, with an occasional alder, The
“condition and position of these remains prove that at some
“ comparatively remote period the valley extended a considerable
* Jistance beyond its present sea board, and was covered with trees
*‘ of a similar character to those now common to the locality.”*
Of this submerged forest a detailed account has been given
by the late Sir Charles Lyell, in his “Principles of Geology.”+
The forest is said, by him, to have been laid open during a low
spring tide in 1831. ‘It is situated between the beach and a
“bar of sand about 200 yards off, and extends 50 yards along the
“shore, cropping out from beneath a bed of sand and shingle.
“Tt also lies in the direct line of the Bournemouth valley, from
‘the termination of which it is separated by 200 yards of shingle
“and drift sand. Down the valley flows a large brook traversing
“near its mouth a considerable tract of rough, boggy, and heathy
“round, producing a few birch trees and a great abundance of
“the Bog Myrtle (Myrica gale). In that part of the submerged
“peat, which was exposed at low water, were seen twenty or
“more large stumps of fir, from one to two feet in height, the roots
“and bases of which still retain their bark. The sap wood of
“these is soft and spongy, but perfectly white, and exhibiting its
‘‘ original character; the heartwood is exceedingly hard and tough.”
After some other details he goes on to observe that “as the sea
* Sydenham’s Guide to Bournemouth, 15th Ed., p. 76.
+ 12th Ed., vol. iL, p. 536.
48
is encroaching on this shore we may suppose that at some former
“period the Bournemouth valley extended further, and that its
“extremity consisted, as at present, of rough and boggy ground,
“ partly clothed with fir trees.” His conclusion seems to be that
the whole “had been sunk and submerged in modern times by
the undermining of the sandy strata on which the peat and
«trees rested, and did not imply a general subsidence or change of
“level in that part of the coast.”
Another submerged forest, of the same character as that of
Bournemouth, and due to the same causes, is said by Sir Charles
Lyell to occur on the north side of Poole Harbour. In truth,
as stated by Geikie and others, submerged forests occur in places
all round our coasts, testifying to what an extent living forests
must have formerly prevailed in this island. Speaking of the
Scotch Fir in particular, Geikie says—‘“ In ancient times it must
have grown indiscriminately throughout the length and
breadth of Britain, since we meet with it in the English mosses,
as well those of southern as of northern districts.”*
There were, according to Hutchins, some very large forests in
Dorset formerly—one forest is said to have “extended over the
whole island of Purbeck ”+—and we cannot but suppose fir trees
to have abounded there as in the adjoining county of Hants.
Taking all the above facts together, in connection with what
was stated in the earlier part of this paper respecting the number
and condition of the firs still growing at Bournemouth, we can
hardly doubt the existence of an immense forest of firs on this
part of the south coast of England, reaching over long distances
east and west, in prehistoric times ; and which, continuing on by
spontaneous propagation, has remained in great part to the
present day.
But there is another part of this enquiry yet to be considered.
* Great Ice Age, p. 307.
+ History of Dorsetshire, vol. i., p. 171.
49
How far north did this forest extend? As the fir abounds to this
day in the Highlands of Scotland, of course it was not climate
that determined its northern limit. Its advances in that direction
could only have been checked by the progress of civilisation and
agriculture. It is hardly possible to fix the boundary line exactly ;
but as a rude approximation towards it, I interested myself in
tracing on the return journey from Bournemouth to Bath, for
what distance on either side of the line, the firs might still be
noticed. The speed of railway travelling forbids any accurate
observations of this nature; and possibly I may have been mis-
taken in some instances. But certainly the firs were distinctly
seen, though in gradually diminishing numbers, for a very
considerable distance. They were in abundance—large patches
of them here and there—as far as Wimborne; afterwards (but
the patches fewer in number, or the firs only standing here and
there in rows), they were noticed up to Blandford. There is a
manifest reason, however, for their falling off here.
The sands and gravels of the Bournemouth tertiary beds are
exchanged, after a while, for the underlying chalk which is far
more profitable for agricultural purposes, and which must have
long since led to a clearance,of the firs on that account, if on no
other. I have just said that some of the trees may be seen
standing in rows, and it looks as if they had been purposely left
so, when the clearance was made, to serve as a border line between
two contiguous fields or holdings. One can hardly imagine them
to have been planted for such a purpose, as farmers in general
(certainly in the eastern counties) consider low hedges, and not a
row of trees, essential for good corn crops, allowing a free
circulation of air overhead, and thereby in great measure prevent-
ing mildew.
Passing Blandford there was a decided falling off in the number
of the firs for the rest of the journey ; only a few observed here
and there at rare intervals. I am almost sure I saw some at
Templecombe and Wincanton, and others in the vicinity of one
D
50
or two stations nearer Bath. Some of these last might certainly
have been planted ; but taking them in connection with the large
numbers that we had passed on different parts of the line since
leaving Bournemouth, it seemed to myself as if there must have
been originally one continuous growth of firs the whole way ; and
the question occurred to me—Did the firs ever reach to
Bath itself? And then I remembered a few old scattered,
scraggy, forlorn-looking firs growing on Combe Down when I
first came into this neighbourhood five and thirty years ago.
These firs had always been a puzzle to me. Who planted them
there? supposing them to have been planted. Who cared to
set them on a sort of no man’s land, or if not so, strictly speaking—
on an open down, where persons wander at will, and the trees are
subjected to the rough usage of every passer by? No doubt the
trees had a history once, but they looked, when I last saw them,
as if awaiting extinction,—life’s day all but run out. May there
not have been more firs once, and in full vigour? And is it not
possible they may have had some connection, I do not say with
the Bournemouth firs, but with a large growth of firs existing
ages back over all the downs by which Bath is surrounded, and
as truly plentiful and indigenous in those days as in Bourne-
mouth itself, or any other part of Great Britain? The
Combe Down trees, in that case, must have had a long
ancestry, and they alone survive to tell the tale of the
past, reminding one of the solitary firs on Lymington
Heath above spoken of. There is something of sadness felt
on hearing of things in which we take an interest being
found or seen for the last time. The botanist mourns for the
loss of some rare plant no longer to be met with in spots where
he used to gather it. And the tree as well as the flower may
evoke a feeling of this kind; or steps may be taken, as they have
been taken in some cases, to preserve a few individuals still
remaining. The rare and beautiful Ladies’ Slipper Orchis,
formerly met with in many places in the north, is now, I believe,
51
restricted to one wood in Yorkshire, where (I have heard) the
owner of the ground watches over and strictly preserves the
few plants growing there still.
More to our present purpose, however, is a record of the
last Scotch Fir seen in Ireland. It is said that “in ancient
times all Ireland was full of woods on every side;”* and
there is no question but there were formerly forests of
firs there, as well as in England. More+ gives a few
localities in which till lately they were still found ; adding—
“There is one large and old fir tree, supposed to be a last relic
of the ancient forests, still growing on an open bog . . in
Mayo, and which was lately fenced in and carefully ssolannca by
the Earl of Arran, who is the owner of the land.”
I do not propose any such close imprisonment for the few
remaining firs on Combe Down. But I think they should be
looked after, and some record kept as to their existence before
they quite disappear. Babington makes no allusion whatever to
these Scotch Firs in his “ Flora of Bath.” Should not the matter
be taken up by our Club, expressly instituted for the investigation
of the Natural History and Antiquities of the neighbourhood of
Bath? There may be antiquity in trees as well as in stones.
My own botanising excursions have necessarily for many years
been discontinued ; and I was about to ask if some other of our
members would not make it an object of one or more of their
weekly walks to take a general survey of the downs, and to note
what trees they might still find there and the condition they were in.
I have, however, been anticipated in this matter. One of our mem-
bers, Mr. Frederick Inman, on hearing of what I wanted, forthwith
kindly volunteered his services; rambled over all the downs
in turn, and sent me in a statement of what he had found. He
has got together a good many details of much interest, and such
* See “TIreland’s Natural History” by Boate (1652), p. 119
+ “Cybele Hibernica,” -p. 276.
52
as would furnish matter for a separate paper which I hope he
may be induced to give the Club at some future time. I will
only here give a short summary of what he has ascertained.
Setting aside fir trees growing in the proximity of houses, or in
adjacent woods containing other trees besides firs, where it would
be difficult to distinguish between such as were wild and such as
had been planted ; he finds, on the open ground, scattered trees
upon Kingsdown, Banner Down and Lansdown. I have already —
spoken of the Combe Down Firs, and Mr. Broome informs me
that he had seen formerly a few old trees, some merely stumps,
in the vicinity of Sham Castle. On Hampton Down, on the
edge of the hill near the Rifle Butts, where Mr. Inman remembers
to have seen formerly about a dozen trees, only three stumps of
trees are now left. This looks as if the race of old original firs
was dying out. There are several trees scattered about the top
of Banner Down in one place, where the ground looks more “ as
if it had been covered with these trees at one time than any
other place at the top ofthe hill.”
There are no firs on Solsbury Hill. This may, perhaps, be well
explained by Solsbury having been in aneient times, according to
Mr. Earle, ‘‘the site of a well-inhabited and populous British
city,’* which circumstance would necessarily have led to an early
clearance of any natural forest that grew on its summit and slopes.
Taking Mr. Inman’s notes as a whole, I consider there is
evidence to show that these trees once existed in much larger
numbers; and, in connection with all that I have said in the
early part of this paper, sufficient to warrant the question—
“Was there not formerly, in prehistoric times, if not later, a
forest of Scotch firs covering all the hills by which Bath is
surrounded ?”
I cannot but think the answer to this question, if answer be
possible, would be in the affirmative.
* Bath Ancient and Modern, p. 9.
53
The Alge of the Bath Thermal Waters. By G. NoRMAN, Esq., M.B.
(Read December 9th, 1385. )
The interest attaching to the occurrence of Fresh Water Alge in
thermal waters is due, not so much to the discovery of numerous
fresh species, as to the mere fact of the existence of Alge under
such exceptional circumstances, and of their being able to grow
and flourish at a temperature that would be fatal to members of
the same genus or even species taken from a normal habitat. For
instance, if a portion of Oscillaria were taken from the canal or
river in our neighbourhood and subjected to a temperature of 150
degrees it would undoubtedly be killed outright, whilst at the
thermal springs of Karlsbad, Oscillaria grows freely in water of
the temperature of 160°.
Algz have been found in many of the thermal springs of
Europe ; but the most important one both on account of the heat
of the water, and of the variety of genera to be found in it, is that
of Karlsbad, already mentioned. Here the calcareous and silicious
deposits surrounding the spring are covered with Algz which also
line the troughs conveying away the water into the river. In
these various situations a large number of genera and species of
Algz including diatoms are to be found, and some of the species
of Oscillaria and Mastigocladus are peculiar to this water.
At another very hot spring, the Herculesbad of Mehadia in
Austria, no less than nineteen species of Alge have been found,
including five species of Oscillaria. These waters are saline-
sulphurous in character and vary in temperature from 80° to
180°. In the spring itself only a few forms exist, amongst them
the Oscillaria—the others are found in the outflow only.
Closely allied with this is the organic matter found in the sul-
phurous thermal waters of the Pyrenees called “ Sulfuraire de
Fontan” or “Baregine” which has been lately shewn to consist
almost entirely of felted masses of Oscillatoria ; this is especially
seen at Cauterets, where the temperature is as high as 140°.
Numerous Alge have also been observed in and around the
54
margins of the hot springs of Iceland, fully exposed to the
influence of steam and boiling water—they consisted principally
of Oscillatoria and species of Conferve. Dr. Hooker in his
Himalayan Journal describes Conferve as present in the hot
springs of Belcuppee. He says—‘Conferve abound in the
warm stream from the springs and two species, one ochreous
brown and the other green, occur on the various margins of
the tanks themselves and in the hottest water; the brown is
the best Salamander and forms a belt in deeper water than
the green; both appear in broad luxuriant strata, whenever
the temperature is cooled down to 168° and as low as 90°.”
On the same expedition Dr. Thomson and Captain Strachey
found Alge in the springs of Pugha in Tibet, which attain
a temperature of 174°, and at the hot springs of Mormay,
with a temperature of 110°. The Rev. J. M. Berkeley, who
examined these specimens, says of them :—‘The vegetation
in the three sets of springs was very different. As regards the
Conferve, taking the word in its older sense, the species in the
three are quite different, and even in respect of genera there is
little identity ; but amongst the Diatomacez there is no striking
difference except in those of the Behar springs, where three out
of the four did not occur elsewhere. In the Pugha and Mormay
springs the species were either identical with or nearly allied to
those found in neighbouring localities, where the water did not
exceed the ordinary temperature . . . . . The species are
less numerous . . . . . than might be supposed from the
vegetation of those European hot springs which have been most
investigated.”
In America, Horatio Wood describes two new species of Alge,
Nostoc calidarium, and Chroococcus thermophilus, found in the
hot springs of Benton, California, the temperature of which is
160°; and in the Yeliowstone River district are some remarkable
boiling mud springs which are coloured bright green by the mul-
titude of Algz contained in them—this observation was made by
55
Professor Ramsay of University College, Bristol, during the
Canadian meeting of the British Association, and mentioned by
him at a meeting of the Bristol Naturalists’ Saciety.
Lastly, Professor Moseley, whilst naturalist to the Challenger
expedition, obtained Fresh Water Algz from the boiling springs of
Furnas, at 8. Michael’s in the Azores. He describes the Algz as
growing on the sides of clefts in the ground, about a foot
wide from which, sulphuretted hydrogen, steam, and water so hot
as to scald the hands, are discharged in jerks and splashes.
Close to these were shallow pools of hot water, in the bottom
of which were hollow channels from which hot gases and water
were discharged ; the edges of these were green with deposits of
Algz, which, however, were difficult to get on account of the heat of
the water, In another place were swamps of hot mud, with pools
of hot water, too hot to bear the finger in, constantly discharging
gases and surrounded with crystals of sulphur, and here also Alge
were found. He estimates the heat of the water in the hottest
parts to be as high as 194°, and in others from 176°—149° ; but
no accurate observations were made there. About thirty species of
Algz were found, including some new ones; it was doubtful
whether any Oscillaria was amongst the collection.
As regards the Bath Thermal Waters, although they have
been fully and frequently dealt with from historical and medical
points of view, I am not aware of any recorded observations con-
cerning their natural history, with, however, this exception, that
both Harvey and Hassall in their respective manuals of the
‘British Fresh Water Algee” mention one species of Oscillaria
as peculiar to the Bath Waters, viz., O. tenuissima, which is
described as occurring in irregular, broad, velvet-like patches of a
dark green colour. The irregularity of its appearance arises
from the filaments being collected together into little ascending
tufts, apparently rooted in the muddy deposit of the water.
Each tuft proves on examination to consist of simple, uniform,
even filaments, crowded together and quite pellucid, and equally
56
destitute of joints and branches ; their diameter is not more than
the eight or ten thousandth part of an inch. In various parts
of the baths I have found an Alga corresponding very much to
this description, although Cooke, in his recently published
manual of the “ British Fresh Water Algz,” discards this species
with many others, remarking that “the species of Oscillaria are at
present distinguished by very artificial characters, which are by
no means permanent, in which respect the genus is not in a much
better condition than it was forty years ago.”
The observations I have up to the present been able to make
may be classed under three heads, according to locality, viz. :—
1. The Algze of the Roman Bath. 2. The Algz of the King’s
Bath. 3. ‘The vegetation of the Central Well.
1. The Roman Bath.—The conditions under which Alge
grow here are very favourable; the temperature of the water
which is just tepid, and the sheltered position, with exposure to
the sunlight, encourage luxuriance of growth to the utmost.
The consequence is that one species of Cladophora, viz., C.
insignis, has almost monopolised the bath, to the exclusion
of many other species. Professor Nordstedt, to whom a specimen
was sent, says that it is the finest species of Cladophora he has
seen, and rivals the typical specimens in his collection. Growing
upon the Cladophora are numerous diatoms, the principal of which
is Amphiprora paladosa. This is so abundant as to produce the
appearance of a white fringe on the Algze when seen in bright
sunlight. Mr. Grove says it is a remarkably fine specimen, as
large as his typical specimens from the shores of the Tay, and the
frustules look healthy and full of endochrome. Besides this are
found Surirella ovalis, Synedra tenera, Nitzschia amphioxys and
linearis, and a few other minute forms. The only other Alga I
have been able to find has occurred in small, darkish green patches
around the margins of the bath, and may possibly represent the
Oscillaria tenuissima already described.
2. The King’s Bath.—This, I believe, would prove a very
57
productive field for the smaller filamentous and unicellular Algze ;
but owing to the zeal of the caretakers of the bath to prevent
the floor and walls becoming slimy and slippery, by means of
weekly scrubbings and occasional lime washings, the algal
vegetation is very scarce. However, by scraping the sediment
from the floor of the bath when the water has been let out, I
have been able to find portions of several species of Alge ; and
the fact of their being able to grow in spite of the warfare
carried on against them, justifies, I think, the opinion I have
expressed as to the habitat being a favourable one.
The principal genus is a Phormidium, or Lyngbya, as it is now
termed by Cooke, of which there are two species, a larger and a
smaller, probably P. corium and inundatum, also a few filaments
of Nostoc and some unicellular Alge, principally Glzocystis.
On the under sides of the wooden seats in the bath is a plentiful
supply of the fungus Merulius lacrymans, common dry rot.
3. The Central Well.—tThis is the centre of highest temperature
in the baths, the water being generally about 118°, flowing up
directly from the source to fill the King’s Bath. The whole of
the inside wall of the well presents a curious appearance, being
lined thronghout by a thick coating of the fungus Merulius
lacrymans, which itself is stained by the iron deposited by the
mineral water, and pierced by numberless filaments exceedingly
fine in character, of the small Phormidium before mentioned.
Under the microscope this arrangement may be well seen; but
the Alga is so small that it is with difficulty detected by the
naked eye. There are various patches of Algz around the mouth
and outer walls of the well; but none different, as far as I at
present know, from those found in the King’s Bath.
I regret that, owing to the late period of the year at which I
took up this subject, and to the pressure of other duties, I have
been unable to do as much justice to my subject as I should have
wished ; but I propose to continue my observations, and to
supplement this paper on another occasion.
58
The Earliest Map of Bath. By EMANUEL GREEN, F.S.A.
(Read 13th January, 1886.)
In the British Museum there is a manuscript, a quarto volume,
entitled: The Particular Description of England, with the
Portratures of Certaine of the Chieffest Citties and Townes.
Having been given by Sir Paul Methuen to Sir Hans Sloane,
it now reposes in the Sloane Collection, being numbered 2,596.
The author of the book was one William Smith, who, after being
at Oxford, studied heraldry and antiquities, became Rouge
Dragon, and died in 1618. He seems in his wanderings to have
copied the plans of different citics when he found them already
done, and when not so, to have drawn them for himself. The
plans given are all coloured. Bristol, placed with the county of
Gloucester, is labelled :—Measured and laid in Platforme by me,
Wm. Smith, at my being at Bristow, the 30th and 31st July, Ano.
Dom, 1568. Canterbury is dated 1588 ; and as the title page is
dated 1588, it may be fairly assumed that the work was then
finished. It may be mentioned that the volume has been privately
printed ; but so privately and so small an impression that the
fact is barely known.
Bath, described as but a “little Cittie, yet one of ye most
auncientest in England,” is here reproduced. Taking it in hand
as a novelty, as if the sight were quite new, it is seen to be a
walled city. Then comes the desire to know all about those
walls. The Domesday survey does not mention it, as it does a
few other places, as being a walled city. Two years later, in
1088, our histories mention, as Florence of Worcester and other
Chroniclers record, the coming of a party from Bristol in rebellion
against William Rufus, when Bath was burned, plundered and
devastated : William of Malmesbury says, depopulated and the
spoils treasured up at Bristol. These are very strong words.
There is again no intimation in these accounts that it was a
walled city, or that it offered resistance as if it were so. Passing
59
now over some seventy years, we come to a Chronicle of
extreme interest, the Gesta Stephani,* hitherto altogether over-
looked. Covering the time of Stephen, a terrible time,
imperfectly known through our present histories, this Chronicle
is of particular interest, as, contrary to those more known, it
is in Stephen’s favour. Unlike the others too, which treat more
of northern affairs, the western events being but shortly
mentioned and from general rather than personal knowledge,
this one treats the western events fully, the author writing as
having been an eye witness of what he records. Who the author
was is unknown; but he was clearly cotemporary—probably a
Norman—and connected either with the Court or the King.
After describing Bristol and the Castle, and telling us that the
latter, “‘ vast and fearful” to beholders, was made terrible to the
district by a garrison of freebooters and robbers, he adds :—
“There is a city six miles [error for twelve] from Bristol where
the hot springs circulating in channels beneath the surface are
-conducted in channels artificially constructed and are collected
into an arched reservoir, to supply the warm baths which stand
in the middle of the place—most delightful to see and beneficial
for health. The city is called Batta, the name being derived from
a word in the English tongue which signifies Bath, because infirm
people resort to it from all parts of England for the purpose of
washing themselves in these salubrious waters, and persons in
health also assemble there to see the curious bubbling up of the
warm springs and to use the baths.”
The date of this charmingly pretty account is 1138, and it is
the earliest mention of the scene. By a little imagination we can
see Bath, “The” bath back to the Conquest, and had the writer
added that in a gallery hard by minstrels minstreled, we should
have before us almost as perfect a picture as through any much
later description.
* By Sewell.
60
Bath being held for Stephen, the Bristol. men in rebellion
wished to get it, the more especially as it could be easily
fortified (co quod facilis esset ad muniendum) A party therefore
marched out stealthily in the dusk of early morning, carrying
ladders and other implements for scaling the wall (scalis que secum
et aliis machinulis ad murum conscendendum convectis), and took
post under cover of a hollow, while scouts reconnoitred to
choose the most advisable point for attack. Geoffrey Talbot, and
Gilbert de Lacy, his cousin, were selected as scouts, and went out
hoping to do their work unobserved; but the guards within
espying them they sallied out upon them, and after a struggle
secured Geoffrey as their prisoner—took him and put him in
fetters and threw him into their deepest dungeon; Gilbert,
stronger and more wary, escaped and returned to tell of the
mischance. A curious picture this, these resolute citizens struggling
with the two knights, who were, presumably, in the chain armour
of the time. Then one would like to know where this dungeon
was. Determined to liberate Geoffrey, the Bristolians approached
Bath and summoned the Bishop (Robert) to come out and treat
with them, promising him safe conduct and safe return. The
Bishop “dwelling in his house with simplicity,” giving credit to
their words, went out accordingly, when he was quickly seized
and held a prisoner. He was then covered with abuse, and
threatened with hanging unless he released Geoffrey. As soon
as it was known within that the Bishop was captured, the citizens
closed the gates and manned the walls (conclusis portis wd muros
defendendos concurrerant) ; no assistance or succour consequently
could be sent out and the Bishop was obliged to order that
Geoffrey should be set at liberty. The Chronicler endeavours to
excuse this, first, as being a clemency more becoming a bishop,
and also because reason did not require him either to expose
himself to insult, or to sacrifice his life. For Geoffrey, however,
he had no biessing, but duly doomed him to the usual torment.
The Bishop, being free, became emboldened, and charged his
61
captors with violation of their pledge, threatening them with
discomfiture in all future enterprises. To all this they
answered with jeers, and reminded him of his simplicity in
supposing they were pledged ; then throwing back perhaps a little
of the Bishop’s own teaching, they argued that, being already a
perjured lot, their pledges went for nothing.
The robberies and cruelties of the Bristol garrison becoming
too notorious, King Stephen determined to reduce it. Setting
out hurriedly, he unexpectedly arrived at Bath. The Bishop on
his approach went out to meet the royal cavalcade ; and at once
had to soften the King’s anger against himself, for having let
Geoffrey go. After telling his story, how grossly insulted he
had been and well nigh hanged, he was restored to favour, and
the King accompanied him into the city. Stephen examined the
entire circuit of the walls, commanded them to be raised higher
and outworks to be constructed, and marked a special spot very
capable of defence which would defy assault (ideoque muros altius
sustolli, propugnacula in devectum surrigi). Then, says the
Chronicle, he marched to Bristol—‘ the seat of fraud.” The
Bath men, meanwhile, gallantly and vigorously maintained
themselves, using every means to make the walls and ramparts
impregnable (muros et aggeres omni resistendi artificio inexpugnabiliter
firmare.) Keeping the walls always manned, they sometimes
sallied out at night, placing parties in ambush, whilst by day the
country folk and the men at arms overran the Bristol lands,
sometimes appearing in force even at the gates, or setting fire to
churches or houses, or whatever would burn.
Bristol, however, was not taken, and the King marched on to
other work.
Our own records are few for this date. Passing, then, some
seventy years, we come to the reign of King John. The custom
of the Kings to journey with their Courts from place to place
prompts a search for the movements of John, as, after the year
1200, documents may possibly be found. In 1206 some arrange-
62
ments apparently were in progress for a western journey, as the
King sent to the Bishop of Bath and Wells twenty-four palfreys
and twelve stable boys, and also a servant with one horse and one
stable boy. Twelve palfreys and four stable boys were ordered
to be removed from Taunton to Wells; five others and two
stable boys were moved from Winchester to Glastonbury,
and ten others with three stable boys were to be placed at Bath ;
also six mares were paid for three tonells of wine sent from
Bristol to Bath, with nine shillings for carriage.* There is no
record, however, of a visit in this year.
In 1207, the Bailiff of Bath was directed to see if the king had
two dolia of wine at Bath; and presumably he had not as the
Constable of Bristol was ordered to send that quantity to Bath,
and place it in the house, which was the Bishop’s house.t There
seems again to be no record remaining of a royal visit in this year.
In 1209, however, John was at Bath for two days, May 13th
and 14th; but no account of his stay can be found.
In 1212, John paid another visit, being in the city on the 17th
October ; and for this time there happens to be an account of the
petty or smaller expenses. Besides a hundred and fourteen
warreners, of whom two had three farthings per day, there were
twenty-five dogs in the care of a huntsman, costing for two days,
fifteenpence; then there was the huntsman himself at sevenpence
halfpence per day ; and twenty-four keepers who, for the two days’
stay at Bath, had four shillings ; the total being 16s. 10d. There
was also charged for hire of a cart with two horses, bringing fruit
from Gillingham to Bath, from Bath to Bristol, and from Bristol
to Lacock, three days, two shillings. To Odo who stayed a night
at Bath with the wardrobe and the “harness” of the wardrobe,
and one night at Bristol, eightpence. To five carriers of the
wardrobe, five shillings, and to nine others, nine shillings. There
* Close Rolls, 7 John, m. 1. + Close, 9 John, m. 15, m. 12.
+ Itinerary.
63
was also a payment to Agnes, the laundress, of twelvepence ; and
there was an outlay of sevenpence, pro tribus wrinalibus for the use of
the king ; there is another entry, pro wrinalibus et chassiis ad urinalia
imponendi. An entry a little later, not specially relating to
Bath, but giving an idea of what must have been the case, accounts
for fifty-five stable boys who had between them six shillings and
fourpence per day, and sixty-two horses costing for forage, hay,
corn, and shoeing for the night, sixteen shillings and fourpence
halfpenny. Six carters divided twelvepence per day, and fifteen
‘horses consumed sixteen bushels of oats; the charge for a night’s
livery, hay, oats, forage, lights and litter, being three shillings
and twopence.
In 1213, March 13th, John was again at Bath, but the expen-
diture is only briefly recorded. Five shillings were paid for fowl
for the falcons, and five pounds were given between the head
falconer and his associates. A day or two later the falconers were
paid ten mares for flying their birds. Eighty tonells of wine were
obtained from Bristol, thirty-seven at 26/-, and forty-three at 24/-*
This roll is unique, and of extreme interest ; no other record
affords such minute information, even down to the loss of five
shillings when the king played at ‘Tables.” To dwell too long
on it would be out of place, yet, besides the insight into prices, the
picture is ever curious, with the cavalcade, the incessant move-
ment, usually twenty or thirty miles a day; the hounds and
huntsmen ; the falconers and falcons ; then the preparation in
advance, and the hubbub and arrival of the party in the little—
very little city.
In 1216, John was again at Bath, and for the last time. Going.
from Bristol to Hinton, then to Sherbourn, he was at Wells,
27th August; Bath, 28th; Bradford, 29th; and Chippenham,
1st September.t There is no record of the expenditure.
In 1223, Henry III. apparently had an intention to visit the west,
* Rotulus Mise, 14 John. + Close, 18 John.
64
as he ordered the Prior of Bath to repair his houses there, at a cost
of sixty shillings, and to account for the same to the exchequer.*
He appears to have been there, however, in 1235, as a patent was
dated therefrom in that year.t There seems no other record of
the visit, except an entry on the Pipe Roll of the following year
be taken as a result of personal inspection. By this the Prior of
Bath rendered his account for £13 11s.—a considerable sum at
that time,—spent by order of the king in repairing the king’s
houses and the wall around the King’s bath (in domibus Regis in
villa Bathonie que reparatione indigent, et muro circa balneum Regis
ibidem reparandis.{ This is so far the first known mention of the
King’s bath under that name, and it shows the origin of the name
as being not from usage as generally supposed, but from owner-
ship, distinguishing it from the Prior's bath so named from the
same cause.
Henry III. died abroad, having been absent from England for
some years. Edward I. on succeeding, in 1273 made inquiry in
every Hundred concerning the rights or dues of the Crown, and
to discover the neglect in payment or performance during the late
king’s absence. Relating to Bath there are three returns; two
for the city and one for the Hundred “Forinsecum” or outside the
city. The last is sometimes written as the Hundred Forinsecum
de Berton Bathonie ; or, the Hundred Forinsecum Bathonie de la
Berton. In some documents it is noticed as the Barton Regis extra
civitate. By adopting the early mode of contracting, and taking
the first and last syllables of “Forinsecum” we get Forum; and
thus Bath Forum is simply Bath outside the city and has nothing
to do with a forum, as has been stated.
As to Bath City, the juries found that King John had given
the city and the Hundred “ Forinseewm” to the Prior of Bath ;
and then we get a return well showing the utter neglect into
* Close, 7 H.IIL,m.5. 7+ Pat. Roll, 19 H., ITI, m. 5.
t Pipe Roll, 20 H. III., dors.
65
which everything had fallen, and showing clearly how reasonable
the enquiry was. It was found that Henry de Courteney had
built a noble chamber on the city wall, for which he had taken
the stone from the wall. That the miller of the Prior took stone
from the wall for repairing the pool of his mill. That the Prior
took stone for building an almshouse. That he, as also had other
Priors before him, made lime from the walls at the Southgate ;
and other Priors had made lime at the Westgate for eight perches
towards Monksmill; and that the defunct Prior had carried
stones to the Priory, to the damage of the whole city. That the
Master of the Hospital of St. John took stone for his house ;
that Thomas Wlbeyn, William le Commandur, Roger Budde,
William Faber, John Koker and William Cocer carried away
stone from the walls to construct or repair their houses. That
Peter Forester took stone for the pool of his mill, and Thomas
Sweyn took stone to build the house in which Thomas Sweyn his
son lived, and that Gunilla le Marescal’ held a house built of the
stone from the wall: all being declared to the damage of the
city and of the King. It was also found that the King’s own
houses within the gates of the Abbey were deteriorated and
destroyed, and to repair them to their pristine state would cost
ten mares beyond the cost already expended on two houses
within the metes of the Priory. It was also found that Robert
Cherin had a tenement within the city and a meadow without,
for which he kept the gate on the bridge in time of war.*
This is an early mention of such a bridge. No order for repairs
seems to have followed these enquiries, and so the picture here
drawn must have been seen by the King himself when he came
to Bath three years later, on the 15th September, 1276. He
stayed the 16th, and then went on to Keynsham the 17th, and
then to Bristol. He was in Somerset again in 1278, but did not
visit Bath. In 1285, coming now from Bristol, Edward was in
* Hundred Rolls.
66
Bath for four days, the 3rd, 4th, 5th and 6th January, and then went
onto Marlborough.* There seem to be no accounts existing relating
to these visits.
Passing on to another reign, in 1369, 43 Edward III., there
was a prospect of a war with France, and the king was asked to
set his house in order. A petition presented to Parliament,
prayed that all fortresses, cities and towns should be hastily
surveyed and put in “ sauve garde ;” and that a command should
be given to all Mayors and Bailiffs to have their walls, ditches
and gates duly furnished.t This was done accordingly, and a
letter was ordered, 4th June, to be sent to the Mayor of Bath
concerning enclosing the city.t Then came the letter or patent
on 8th July, directed to Nicholas de Berkeleye, chiv., and the
Mayor and Bailiff of Bath, and Henry de Forde. That whereas
the walls and towers of the city are in divers places destroyed
and broken, the walls being threatened with imminent ruin ; and
whereas the ditches around the walls are obstructed by trees and
herbs growing in them, and are used for dungheaps and ordure
(fimos et fimare), and other sordid filthy things thrown therein ;
unless a quick remedy be applied, as well by us as by the said city
and parts adjacent, heavy dangers and damages are likely to
happen immediately or at any moment. Being willing to remove
these damages and dangers, as has been requested, We assign you
to survey the walls and towers and ditches aforesaid, and to
repair and mend the defects existing in the same ; and to clear
the said ditches from the trees and herbs growing in the same ;
and to cut and clear out all sordid matter and filth. And, with
power to compel and distrain ; to cause all those who have land,
tenements and rents in the city or suburbs, or those who are resi-
dent, or carry on business therein and gain by reason of their stay,
to contribute to the said reparation and clearing,—viz., each one
* Itinerary. + Rolls of Parliament, vol. ii., p. 300,
t Pat. 43 Ed. IIL, pt. 1, m. 23.
67
according to his status or ability as reasonably as may be, so that
none have consideration. And to you and each of you we command
that you set about the work with all diligence. We give orders
also to all and singular the men of the city, by tenor of these
presents, that they appear and attend to assist us or our deputy
in making and executing the said work, as by you or others for
us on our part shall be required.*
The way in which cities were taxed in early times is of interest;
but unfortunately no special plan was ordered or granted by this
patent, and the plan adopted is therefore unknown. Patents for
murage, pavage and pontage are found for several other cities,
but not one for Bath. Sometimes such aid was got by taxing all
articles brought through the gates ; thus a cart paid sixpence ;
skins, 1d.; skins of lamb, hare, &c., td. ; salmon, congers and
eels, 4d. One city, 6 Richard II., was granted the privilege of
not sending a burgess to Parliament for five years, the cost saved
to go towards building the walls.+ The payment to a burgess
ranged apparently from two shillings to four shillings per day ;
the sheriffs getting eight shillings.t
In 1377, 1 Richard II., the Commons again prayed, as a
necessary preparation for war, that cities having walls should
repair and make them defensible ; all who had property in them,
Religious houses as well as others, and merchants for their
merchandize, to be reasonably taxed, following the usual custom,
“come y ad estee usee devant cest heure.” This was ordered
accordingly, and a writ issued to the Mayor and Bailiff of Bath
to survey and repair; but coming so soon after the more
imperative order of 1369, it must have been unnecessary, except
perhaps as reviving dormant energy.
A patent issued in 1417 raised hopes that some good account
of the city would be found. It was for repairs of walls, ditches,
ER ES ER te eR Tia RTIG a TOT
* Pat, 43 Ed. IIL, Pt. ii, m. 39. + Colchester, Pat. Pt. ii, m. 26.
+ Rolls of Parliament,
68
gutters, water courses, and stone bridges between the city of Bath
and the town of Bristol, which by constant flux and reflux of
the sea, and inundations and encroachments of the water, and
neglect of reparation were greatly damaged and broken.*
Beyond the above facts there is, however, no further special
allusion to Bath.
These notes clear the way for understanding the early maps.
With a little imagination, a little filling-in of domestic habits and
domestic events, a fairly clear image of the city is seen, including
“The” bath, for the first time back to the Conquest. Whatever
the condition in which the walls and the city were left after
the damage of 1088, both were perfect in 1138, in the time of
Stephen. After this there seems to have been a general easy
neglect, until during the absence of Henry III., say after 1235,
heavy damage was actually done, as declared in 1273, when the
walls appeared waste and the stones the common property of any
who chose to take them. So all remained yet another ninety odd
years, until 1369, when the great reparation was ordered and the
ditches cleared. To this date, 1369, we may feel inclined to
assign the using up of the Roman stones, recorded by Leland
some 250 years later, as seen by him in the walls; and, after
another repairing, these would be the walls seen by ‘“‘The Most
Illustrious Lord the Lord Richard ” when he was in Bath in July,
1658. Thus the medizval period passes, and we come to a time
with which we are more in touch, a time more readily under-
standed of all men, the time of the view or plan now to be
considered.
Giving this plan a glance, it is seen not to be exact, as it shows
the Abbey church without the Abbey or Priory house. The
grounds around the church are represented as all grass, unfor-
tunately so, as Leland writing some thirty-five years earlier,
records that “a great square tower with other ruins” of the once
* Pat. 5 Henry V., m. 34, dors,
The Kings Bath)
RB The Grofs Bath
Thetomon Balk. |]
dhe mucll Bu th
yemor Het Place.
SLOANE MSS. Wo. 2596.
69
existing bishop’s palace on the south-west of the monastery were
then to be seen. Had Smith marked these, supposing they were
there in his time, we should know the exact site of the palace,
the “bishop’s house” of King John’s time. Possibly they were
removed under the Act of 1540, 32 Hen. VIII, cap. 18, for
re-edifying townes, which declared that in Bath, as well as other
cities named, houses had fallen down decayed and so “doo
“lye as desolate and vacante groundis, many replennyshed
“withe unclennes and filthe.” After proclamation made they
were to be re-edified or repaired within three years; but here
re-building would not be likely, and the greater improvement
would be to remove altogether.
On a further examination of the plan it is seen that although
the bridge is shown, the gate is omitted—the great gate with a
stone arch at the centre of the bridge ; recorded in 1273 as being
kept as a service for certain land and a tenement.
Another peculiarity must be noticed, as this Smith’s map
attempts to show the suburb southward over the bridge, this
being the more remarkable as not only does he so but he marks
a church just at the foot of Holloway, at the corner on the left
turning towards Widcombe. What does this mean? Was there
ever a church here? Going first to the dissolution documents and
the accounts of particulars for grants or for leases, there is found full
notice relating to the “ cathedral” and the site of the Priory, and
the Grange, and le Hayes, and le Ham and pasture for three
hundred and twenty-two sheep called the hogflock. Then there
were pastures in Walcot and Barton; and a pasture on Launce-
down with all commons; and pasture for a flock of three hundred
and sixty ewes called the eweflock of Barton.* Selecting Wid-
combe more especially, there was the farm of the manor of
Widcombe and Lyncombe with the lands and feed called Bewchen-
clyff, or Beauchyncliff, or Bychincliff, or Beachynclyffe, with Prior
* Particulars for Leases, Ed. VI., sec. i.
70
park and other meads and pastures.* Going still backwards, the
Valor mentions Stalls with the chapel of Widcombe annexed ; and
earlier still, in the Wells registers the same thing is found. In
1322, Bishop Drokensford’s register mentions the admission of the
Vicar of Stalls with the chapel of Widcombe, with all the tithes of
Widcombe and Lyncombe. So is it in other registers. There is
no record of a church or chapel on the site here marked by Smith.
Smith’s plan may be considered perhaps, not as a map plotted
exactly as a survey, but rather asa view—a bird’s-eye view—“ a
- portrature” as if taken from Beechen cliff. This church may
then be accounted for, the intention being, not to mark exactly a
site, but, after the manner of early maps, to mark that here in
this suburb was another parish ; and this would then be the parish
church of Widcombe. In this case too, as it happens, this was,
ecclesiastically, really a part of Bath. It is not forgotten that there
was the chapel for lepers, the chapel of St. Mary Magdalen in
Holloway. This is found noticed in 1256 as the chapel of St.
Mary “extra civitate Bathonie,” thus perhaps marking it as the
otherwise unrecognised church of St. Mary extra muros, often
mentioned in the local records.* But it need not be confounded
with the site or suggested site of the church now considered.
One note must be made, as from the above documents we get
the origin of the name Beachen cliff—this being Beau Chine cliff,
chine meaning one side of a gorge such as this is; and so from
Beauchine we drop to Beechen or Beachen, as from Beauchamp
we get to Beecham ; without any origin from the beech tree, as
many suppose.
The intention in these notes is not to examine minutely any
differences in the early maps, as that may be better done by one
more capable and with more minute local knowledge ; but there
is yet one point which must be attentively considered, and here
too must be quoted for once, one local author, but quoted only to
* Particulars for Grants, Hen. VIII. + Pat. 40, H. iii, m. 7.
71
criticise. John Wood in his description of Bath, on page 84, vol. i.
of 2nd edition, has given an engraving of what he calls :—“A
“copy of Doctor Jones’s view of the city of Bath, as it was
‘* published in the year MDLXXII.” He gives it boldly as being
a view taken in the reign of Queen Elizabeth to illustrate Jones’s
book, “The Bathes of Bathes Ayde ;” and considering it suitable for
illustrating his own text, he adds—(p. 84) “I have therefore copied
it.” First, here the title to this map is Wood’s own ; with attentive
reading that is clear, and so it must not be confounded or
taken as being the copy of an original, as a hasty general reader
may readily do. On pp. 85-86, Wood has described this map by
the usual method of using capital letters ; and then he has marked
by the use of other small letters or figures of his own, certain
localities which, as he says, are ‘“‘neither named nor referred to by
Dr. Jones.” Thus alluding to a certain house, he writes, ‘‘it stood
by the fig. 5 in Dr. Jones’s view ”—adding—“‘some of the parts of
which view he (Jones) thus described.” Then he refers to the
capital letters as being Jones’s.
Now all this is false. Dr. Jones’s book does not name or refer
to the city, nor does he by means of letters or figures refer to any °
spot or locality in it. There are no such letters in the book, nor
is there any description of or allusion to any such subject as a map.
The treatise is entirely on the baths, as the heading of the four
chapters or books given in the dedication clearly show. The first
book treats of the descent of Bladud, and of the sicknesses the
baths help ; the second book shows the divers opinions concerning
the cause of the waters ; the third expresses things natural and
non-natural, and the signs of the sick for the better consultation
whether the baths will help them or not; and the fourth book
declareth aphorisms and rules how the baths shall be used. Again
in vol. ii., p. 305, Wood says when speaking of Bellot’s hospital,
“it was built on the ground marked “k” in Jones’s view,” thus
conveying two entirely erroneous impressions ; first, that the “k”
on the map is Dr. Jones’s own letter, and also that Bellot’s hospital
72
must have been founded before 1572, the date given for the map,
whereas Bellot’s hospital was not founded until 1609. Again,
writing here in vol. ii. he has forgotten that in vol. i., p. 86, in the
description there, whilst “i” marks the site of Counter’s tower,
and “1” the site of St. Catherine’s hospital, the “k,” which should
come between these letters and mark Bellot’s hospital, is omitted
from the letterpress, although it appears on the engraved map. An
excellent example this of how a thing may be conspicuous by its
absence, as had the ““k” been in its place it must at once have
attracted attention; Bellot’s hospital, as already noticed, not
being in existence. This little fact seems to show that Wood knew
what he was doing; that this omission was deliberately made.
Comparing now this Jones’s map with two other early ones,
Speed’s and Johnson’s, any little differences will be seen.
Speed’s—entitled, ‘‘ The plott of the famous and most wholsom
waters and citie of the Bathe,” was published in a corner of the
map of Somerset as issued in his volume, entitled, ‘“‘ The kingdom
of England described.” Some of his maps are dated 1605, some
1608, some 1610, others are undated. Somerset is undated,
but usually the year 1610 is assigned for it ; yet when the date is
used it should be stated as being only approximate, or else the
figures should be put in brackets to convey that correct impression.
To print such date on the map and so imply no doubt, is to falsify
it, and convey an impression which may be erroneous.
Johnson’s was published in 1634 in his Therme Bathonicz,—an
extremely rare little book which treats not only of the baths, but,
De urbe et Thermis,—and is the first map published in book form,
Wood inlettering his Joneshas shifted two or three letters slightly
at the beginning, but it may be noted that the letter “x” marks
the site of the Leper’s bath, and ‘‘y” the Hot bath, whilst in Speed
these letters are reversed, “y” marking the Leper’s bath and “x”
the Hot bath. Johnson follows Speed exactly except in these two
letters, and just as Wood’s Jones differs here in these two letters
from Speed, so does he differ, to correspond with Johnson. Further,
73
Speed shows the ferry outside the North gate complete, the uprights
being seen on either shore, with the ferry on the river. Johnson
shows only the uprights on the shore, without the ferry, and so
does Wood’s Jones. Here again Johnson differs slightly from
Speed, the difference exactly occurring in Wood’s Jones. Another
peculiarity is that in the Timber green near Gascoigne’s tower ;
the timber lying about as shown in Speed’s, has not been moved in
Johnson, the seven logs shown in the one are still seven logs in
the other, lying too in exactly the same positions. As Johnson
is exactly like Speed, so again is Wood’s Jones exactly like
Johnson. Speed, too, marks some trees such as by Monk’s mill,
with two small houses; Johnson marks the houses, but not the
trees. Here again, as Johnson differs from Speed, so does Wood’s
Jones agree with Johnson.
This so called Jones’s map has been misnamed and misdated ;
it is simply Johnson’s of 1634. ‘There is not, and there never
was a Jones’s map of Bath.
Besides a personal knowledge of several copies of Jones’s
book—a scarce work notwithstanding—the above argument is
founded on or taken from Wood’s 2nd edition, this being
the one usually quoted or referred to, the complete edition
in four parts. The earlier edition or Part i, issued in 1742,
it not often seen, and as being only a part would not be
bought or sought by a general reader. For this reason it has
been overlooked that the 2nd edition is the first in which the
so called Jones’s map appears, for, on referring to the 1st edition
of 1742, Parti, p. 83, the map there given, is given honestly as
Johnson’s. The paragraph describing it actually begins :—‘‘In
“the year 1634, Dr. Thos. Johnson wrote a description of Bath and
“therein inserted a draught of the same, a copy of which I have
“caused to be engraven.” The map is then given as in Johnson
without any heading or name. It is the same map as given in the
2nd edition, but there called Jones’s. The small letters on it
mark the same spots, not only without any reference to Jones or
74
his pretended omissions, but actually with direct allusion to Dr.
Johnson. The letter “‘k” noticed for its absence from the letter-
press in the 2nd edition in the description of the so called Jones’s,
duly and properly appears here in its place in the letterpress as
well as on the map, and marking Bellot’s hospital ; fair evidence
that it was purposely omitted in the 2nd edition.
That the two maps are the same may be seen from the fact that
both have two “ w’s”; one near the Guildhall having no reference,
the other marking the Cross bath. The difference in them is that
Wood has added small figures in the 2nd edition in extending his
references, and also the line on the margin naming it Jones's, for
which, as can be seen by the pressure indent, the plate just
allowed sufficient space.
Wood gives no reason for this alteration, attempts no explana-
tion whatever. Thus he leaves the conclusion open that he
was not misled, but that he supposed the change would not be
noticed. Further, it must be clear, that he either never saw
Jones’s book, or that if he did so, he has wilfully practised a fraud.
Smith’s view now brought to notice, for it is rather a view, a
“portrature,” than a map, is, clearly, independently made. The
walls are shown more bastioned than in the other maps, and the
timber green, although green, is without timber. Whether it were
“measured and laid in platform” like Bristol and at the same
time as Bristol, viz., 1568, cannot be stated. No exact date can be
given for it. If not done in 1568, it may be taken as not done after
1588. Asit is the earliest known thing of the kind, there seems
no great reason why the Bristol date of 1568 should not be given
to it, as no change took place in the form of the city during the
twenty years named. If it cannot be accepted as quite exact, yet
better than any other map since, it conveys a very exact idea
hardly realized by us to-day, of what must have been the original
appearance of this very ancient and pretty, but yet very little, city
of The Bath.
“a (te ee
75
On Recent discoveries made in Uncovering the Roman Baths at Bath.
By the Rev. Preb. ScARTH, M.A.
(Communicated 13th January, 1886.)
In the proceedings of the Bath Field Club, Vol. iv., no. 4, p.
357, will be found an account of the excavations made at the
baths, by Major Davis, who gave some very interesting details to
the Club. This was in 1881, and as further important discoveries
have been made since that date, it is well that an account of them
should find a place in the records of the Field Club.
The Roman sewer had then been fully examined and utilized for
conveying away the waste water from the thermal spring, and this
led to the discovery of the Roman tank for receiving the hot springs,
as described by Major Davis ; but since then the large Rectangular
Bath has been exposed to view, together with the Ambulatory (or
Scholz) which surrounds it, and the three recesses on the north
and south sides of the Ambulatory. The whole seems to have
formed a vast Hall for bathing,—111ft. 4in. long by 68ft. Gin.
wide, and about 6ft. 8in. deep. The bottom of the bath, like
that of the tank or reservoir which received the hot springs, is
covered with sheet lead, and is 73ft. 2in. by 29ft. Gin. The
sheets of lead covering it are about 10ft. by 5ft., and are
supposed to have been laid rather to keep the hot water which
rises through the earth from entering the bath, than to make the
bath water-tight. Six steps lead down into the bath, but do not
appear to have been covered with lead. At the bottom step in
in the N.E. corner, was a bronze sluice, with an opening 13in. by
12in., which may now be seen in the Pump Room; an overflow was
provided also.
The extreme surface of the water, according to Major Davis’s
measurement, was 83ft. 8in. by 40ft. 2in., and formed a parallelo-
gram, except that the N.W. angle was cut off by the steps being
carried obliquely in three tiers for a length of 7ft. Some of the
76
stones of the bath are 10ft. long,—square sockets appear cut in
some of the steps, as if to support a baluster to a handrail.*
At present the offices of the Poor Law Board stand above rather
more than one-third of this bath ; but it is hoped that before long
this building may be purchased, and the offices removed elsewhere,
so as to allow the whole area to be laid open.
Six piers of wrought stone stand on each side of the bath, the
width of the platform surrounding the bath is 14ft. This has
been arched, as the remains of the roofing have been found in
large fragments, composed of hollow tiles, wedge shaped. It is
probable that the whole was orginally covered—the roof of the
central bath being higher than that of the platform surrounding
it. The present piers remain only to the height of 6 or 7ft., and
appear to have been strengthened by additions. Fragments of
the capitals of the pilastres have been found from which the
arches took their spring, and some portious of a frieze, also the
figure of a lion, which seems to have served as an antefix.
Since the large bath above described was exposed to view,
further discoveries have been made at the western end, near to
the large tank or reservoir below the King’s Bath. These consist
of a Hall, 55ft. long by 36ft. wide, in the centre of which is a
circular bath with steps leading into it ; the depth is the same as
the great bath. To the south of this are vaulted chambers, as
may be seen in the plan given in the guide to the Roman Baths,
drawn by Major Davis, to whom very much is due for the spirit
and energy he has shewn in elucidating these remains.
The steps which surround the circular bath and form seats,
are quite perfect, and the bath is now filled with water. To
the south of this a drain has been found by which the over-
flow from the baths was carried off. This circular bath has been
connected with the large Roman reservoir, which also supplied
* See Paper by Major Davis in Trans. of Bristol and Gloucester
Arch, Soe., vol. viii., pt. i, p. 89 and following.
17
the large Rectangular Bath. The short columns supporting the
roof of the Ambulatory which surrounded this circular bath, are
found perfect in one or two instances ; but the arched roof that
‘must have rested on them has been removed.
This circular bath occupies the western end of the large Rectan-
gular Swimming Bath, as the Rectangular Bath, found in the last
century, formed the eastern end.
The workmanship of the circular bath does not seem so massive
or well put together as that of the large bath. They may perhaps
eventually be found to be of different dates, though both are
undoubtedly Roman, and form portions of a grand arrangement
for bathing.
A circular bath is not common in Roman bathing establish-
ments, but semi-circular baths are very common ; and circular
chambers of very large proportions were attached to baths as
Sudatories and halls. This may be seen at Rome in the Pantheon,
which was a circular hall, with chambers attached, for the
purposes of the Sudatorium, or Vapour Bath ; also the same may
be seen at the baths of Dioclesian, where one or more have
been turned to the purpose of a Circular Church.
Contiguous to the Circular Bath, and beyond the Ambulatory
surrounding it, a chamber has been opened, which seems to
have been used for heating purposes. The remains of a
Hypocaust have also been found. It is probable that this
Circular Bath (as well as the Rectangular one) was supplied with
cold water from a spring, not mineral, but which could be used
for ordinary washing or other purposes. Much, however, remains
yet to be discovered, and more must be laid open before the
exact purposes and arrangement of these baths can be accurately
ascertained. The lead coating of the Circular Bath, which
probably also covered the steps or seats that surround it, had been
removed in past times.
Major Davis, in his paper recently read to the Bath Literary and
Philosophical Society, supposes that the entire establishment of
78
the Roman Baths was contained in a parallelogram of 440ft., or
460ft. from east to west, with a width of from 140ft. to 160ft.
from north to south, and the total area would then be nearly
6,500 sq. ft.; but this would not include the outer Courts or
Gardens, and the whole probably covered two acres.
It has also been stated that the area marked by the Medizval
Walls—helieved to stand on the foundation of the ancient
Roman—is too small for a Roman town, and comprehended the
baths only ; but as their circuit is nearly a mile in extent, there
was ample space not only for the forum, baths, and other edifices,
but for a population of considerable extent, knowing how closely
they were packed in ancient times. The area allowed for the
baths seems to be a fair allowance of space, though considerably
less than was assigned to their area in a paper read last year to
the Literary and Philosophical Society, which supposed the area
of the Roman Baths to have extended over the whole space of
the enclosure within the walls, from E. to W.
The Roman Baths only occupied the southern front of the
forum which is now represented by the Abbey Church Yard; but
the space occupied by the ancient forum is much encroached upon
by modern buildings. If the medizeval walls followed the line of
the Roman, they enclosed an area of 224 acres; and if the
Roman Baths extended over 2} acres, their remain 20 acres for
the forum, streets, temples and other buildings of the ancient
town.
We cannot but hope that the investigation of these baths
will be continued, and that their remains may be carefully
preserved, The coins and vessels hitherto found have been few,
considering the extent of the area now laid open; but such
discoveries are always uncertain, as the baths were probably
in use for a limited time after the Roman domination had
ceased, and were well ransacked for articles in later times, before
they became permanent ruins.
The inscribed Metal Plate, of much interest, found in the
he
79
bath, is not yet admitted to be satisfactorily explained. If
access to this plate could be allowed to certain competent
scholars, something more might be known as to the correctness
of the reading.
Upon some Sculpture recently discovered at the Cross Bath. By Ruv.
H. H. WInwoop.
(Read January 13th, 1886.)
In the Bath Herald, of September 12th, 1885, was a letter upon
“ Preshr discoveries at the Baths,” describing the recent “ find” of
a stone with carving on three sides. “At a depth (the writer says)
“ of very nearly 20ft. in the excavations at the Cross Bath, was dug
“up on Tuesday, 8th inst., a stone, 30in. high by about 17in. wide
“and 10in. in thickness,with carving on three sides. The carving on
“the first side is little more than incisive work, the second side is
“sculptured in high relief, the third side is fractured—showing it was
“ attached to other masonry, and the back is a carving in low relief,
«‘ having no connection as to scale with the principal work. The
“incisive carving (No. 1)is a tree with spreading roots and branches,
“the trunk being entwined by aserpent. Two figures occupy the
“front of the stone ; they are headless and almost armless. The
_ “figure of a man partially covered below the waist by some drapery
“is on the right reclining on a bank beneath atree. The figure on
“the left is that of a woman (nude), and is erect reaching something
“from the tree, but the other arm has perished. Between the
« fioures is a vase or wallet. On the back of the stone is a large
“ dog (?) somewhat like the Danish boar hound, except that it has
“a tail like a collie turned up over its back (some architectural
“foliage and that may be another tail), the Sculpture (and now
“ comes the startling theory), I believe to represent the temptation
“and fallof Adam. It is possible that it may be Hercules and the
« Hesperides ; but the male figure is by no means Herculean, The
80
“discovery is the first found in Bath that may be said to be of
“Christian or rather Biblical character, and certainly the only
“important one of similar character found in Britain.” So far for
the letter with its ingenious conclusion. This brought forth one
or two other letters from another antiquary, written from a
distance, in which an equally hasty suggestion was made that the
stone described was probably the portion (lower shaft) of a Saxon
cross of which two other portions were in the Museum of the
Institution.
Having inspected the carved stone myself several times and
looked at the pieces of Sculpture in the Museum, I could not
possibly reconcile either of the above statements with the actual
facts of the case. Not deeming myself sufficiently competent to
controvert the views set forth by two such authorities, a lucky
chance presented itself, or rather a Deus ex Machina appeared in
the person of Professor Sayce, who accompanied me to the Roman
Bath where this interesting stone is fast being injured (if not
destroyed) by exposure to the action of the weather, stated his
impressions as to the Sculpture at the time and has since written
to me on the subject.*
The following communication clears up the whole matter and
brings conviction to every reasonable mind :—
“‘Thave not had time before to write down for you my notions
about the curious altar-like stone found last summer in the Cross
Bath, which we examined together a few weeks ago. I believe it
must have come from a chapel dedicated to Aisculapius, a deity very
likely to be worshipped in the neighbourhood of the hot springs.
The serpent entwined around a staff, which is engraved on one of
the faces of the stone, is his well-known symbol. The dog repre-
sented on another face was also associated with Aisculapius.
* It is but fair to add that on January 8th a note from the writer
of the first letter states that “he has altogether changed his views as
to this Sculpture.” :
81
According to Festus, dogs were employed in the temples of that
god because he had been “suckled” by one of them, and the
monuments of Epidauros, and of the Asklépion at Athens, as well
as the coins of the Magnetes show us the dog in combination
with the serpent. Inscriptions recently discovered at Epidauros
prove that dogs acted there as the ministers of Asklépios.
The piece of Sculpture on the third face of the stone seems to
me to represent Apollo and Kéronis the mother of Asklépios. It
may be compared with a bas-relief, once built into the walls of
Bath, and figured by Guidott who makes out that it depicts a
shepherd and his mistress! On the newly found stone the male
figure seems evidently intended to represent Apollo. Can any
traces of a crow be detected among the branches of the tree above
the head of the reclining female figure ?”
The Rev. Preb. Scarth, having examined the Sculpture and
formed an independent opinion thereon before hearing Professor
Sayce’s interpretation, read the following notes at the Anniversary
dinner of the Club February 18th.
“The statement of Solinus respecting the “Calidi Fontes” in
Britain, “Opiparo exculti apparatu,” has received singular con-
firmation, after an interval of 1,500 years, by the discovery of an
interesting Sculpture in the form of an Altar, but not quite so
massive as Roman Altars of the same dimensions usually are.
“This stone has two Sculptures on opposite sides, front and back,
and one on the side,—the other side seems to have been fixed
into masonry.
“The Sculptures are much defaced, but shew signs of early,
Roman art, being executed with much spirit. The stone has a
plinth which projects, and the subjects are on panels, the figures
being in relief.
“The whole surface of the front face is occupied by two Se
the one standing and the other reclining.
“The standing figure is that of a man extending the right arm,
and. holding what on minute examination is found to be a lamb,
% F
82
above the head of the reclining figure. The reclining figure
rests on one elbow (the left) and extends the right arm, while the
head is turned away, as if to reject the offering. This is a
female figure ; the lower portion of the body is draped, one leg
being extended the other bent,
“Tn the space between these figures is a large bowl, on one side
of which appears to be a serpent.
“On the side of the stone, reaching from the base to the upper
portion, is a tree, around which is coiled a serpent, with the head
downward.
“On the opposite side of the stone, in the upper portion, is a
wide panel, extending over half the surface. On this is a dog
with a bushy tail, in the act of walking; at the back of the dog
is a tree.
“Below this Sculpture in relief, the surface is quite plain,
apparently without any lettering, though, unfortunately, like the
rest of the stone, much injured. The top portion of the stone
projects considerably over the panel.
“In a letter to the Bath Herald (September 12th, 1885) this
Sculpture was considered to be a representation of the fall of our
first parents! but a careful study of the stone at once shews it to
be connected with the Heathen Mythology.
“This was discovered at once by Professor Sayce, es on
examining it, made the suggestion to the Secretary of the Field
Club, in a letter addressed to him, that it was a representation of
Apollo and the nymph Kéronis. Before seeing his communication,
or knowing the explanation he had given, I had on two
examinations of the stone come to the conclusion that it must be
Aésculapius (the Greek Asklepios) offering a lamb to the goddess
Hegiéa. The serpent feeding out of the crater, or large cup, and
the serpent entwined round the tree, are emblems of Aisculapius,
and the dog also is connected with the worship of that god.
Hegiéa was worshipped in the Temple of Adsculapius at Argos,
where these two divinities had a sanctuary ; also at Athens and
a
83
at Corinth ; also the Goddess Hegiéa is usually represented as
feeding a serpent froma bowl or cup. The bowl, or large cup,
upon the Sculpture may also indicate the healing waters of the
Bath Thermal Spring.
The dog also is not only a symbol of Aisculapius, the god of
healing, but represents also the Dog Star, (xuwv) adopted by the
Romans from the Greeks, and indicating the passage of the sun
into the constellation Leo. The season known as the ‘Dies
Caniculares.” The dog may therefore here be an emblem of the
heat of the thermal springs.
It is not unworthy of remark how the “serpent” enters con-
tinually into the ancient Sculptures found in Bath. The drawings
of the Sculptures given by Guidott in his work, formerly to be
seen in the city walls, contain two representations of figures, one
of which, apparently a female, carries two serpents ; this figure is
nude, the other, apparently a male figure, is clothed and carries
one serpent. Two heads are represented as covered with hair
formed of serpents, and serpents are sculptured in the hair and
beard of the head of Medusa, which formed the centre of the
pediment of the temple,—the remains of which are now in the
portico of the Literary and Scientific Institution. All these seem
to be emblematic of the healing properties of the thermal springs,
which have been for so many hundred years celebrated, and
granted, as Solinus expresses it, ‘ad usus mortalium.”
The chief Altars found in Bath are dedicated to the goddess Sul,
or Sul-Minerva. The British goddess being associated with the
Roman. But the Roman Minerva was the same as the Greek
Athena, and Athena was the goddess of health as well as of the
arts and sciences. According to Proclus, a late Roman writer,
H A@HNA NIKH gpocayopeverar cat YIIEIA. Athena or
Minerva is called victory and health, and this leads me to the
conclusion that the Sculpture represents Alsculapius making an
offer to Hegiea, the goddess of health, and that she is the
presiding goddess of the thermal springs.
84
These remarks are only offered until some more satisfactory
explanation can be found for the meaning of a Sculpture which
appears to me to be of no common interest, and which should be
carefully preserved among the other interesting lapidary records
of Roman Bath.
Notes on the occurrence of Salt Springs in the Coal Measures at
Radstock. By J. McMurtrig, F.G.S.
(Read 10th February, 1886 ).
While engaged during the past year in carrying out a deep
sinking in the Coal Measures at Radstock, the writer encountered
certain Salt Springs not previously met with in the parish, and
believing it to be a comparatively rare occurrence in the Carboni-
ferous series, he has thought it of sufficient importance to bring it
under the notice of the Bath Field Club. Had these springs been
met with in working coal near or under the sea, as in the
Whitchaven, Newcastle and other coal fields, their presence would
not have occasioned any surprise ; but their occurrence in an
inland coal field, twenty-one miles from the nearest sea board, is
very remarkable, and it has given rise to much speculative inquiry
as to their probable source.
In order to explain the position in which these Springs were
met with, it is necessary to point out the geological features of
the locality in which they occur, which are probably familiar to
some who have turned their attention to the subject, but may not
be so to others.
Although Radstock is known chiefly in connection with coal,
a geological stranger visiting the place would be surprised to
find that, after examining every hill and valley within the parish
he had entirely failed to discover any trace of Coal Measures, except-
ing those unsightly shale tips which now disfigure what was once a
picturesque rural parish. The explanation of all this is that the
————
85
Carboniferous rocks, having undergone many changes and much
denudation, were in later but still very remote geological times
overlaid by newer formations which now cover the entire surface
of the parish, capping the higher ground with Inferior Oolite and
Lias, while the lower slopes and the bottoms of the valleys are
occupied by the Rheetic beds and Keuper Marls.
The Middle Pit, in which the sinking operations referred to
have been carried on, is situated about 100 yards on the North
side of the Radstock Market Place, and is easily recognised by
its tall, circular stone chimney, which visitors may have noticed
on their right in driving into Radstock from Bath. The shaft,
being situated in the bottom of the valley, did not meet with the
Lias and Rheetic beds, but passed at once into the Keuper
Marls, which are here 89 feet in thickness, and rest on a bed
of Conglomerate immediately overlying the Coal Measures. These
Marls, fed by the rain and streams from above, and resting
on a water-tight bed beneath, yield a large quantity of water ;
but it is ordinary spring water, without any special mineral
ingredient.
It is hardly necessary to state that it is these same Marls
which, in the Midland Counties, yield almost all the Rock Salt and
Brine Springs which we possess in England. Although only about
17G feet in thickness in the Radstock area, the New Red Sandstone
of Cheshire attains a thickness of 1,700 feet; and it is the
upper 700 feet of this formation which contains the Salt Mines
and Brine Springs which, in Worcestershire and Cheshire, yield
annually from 160,000 to 170,000 tons of prepared Salt. But
although geologically identical, no trace of either Rock Salt or
Salt Springs has ever, so far as the writer is aware, been met with
in the Keuper Marls of Radstock.
Immediately under the New Red Sandstone, but not at all
conformable with it, lies the upper or Radstock group of the
Somersetshire Coal Measures, to win which the Middle Pit was
originally sunk, and which has here been worked successfully for
86
many years. The strata comprised in this series yield very little
water, the Conglomerate at the base of the New Red Sandstone
serving as a nearly water-tight covering, through which only a
very moderate quantity of water ever passes. The only feeder
worth naming occurs in a thick bed of Sandstone overlying the
Middle Vein ; but the water produced here and elsewhere in the
series is entirely free from Salt, of which the writer has never
discovered any trace.
The Middle Pit was originally sunk to the lowest seam of the
Radstock group, which was here met with at a depth of 875 feet,
and beneath which there lay an unknown country. The sinking
operations carried on under the direction of the writer began at
that point on the 8th of May, 1884, and having been carried down
through the second or Farrington group of the Somersetshire Coal
Measures, reached a depth of 1791 feet from the surface on the
25th of January last; the ground below this point having since
been proved by a boring to a total depth of 1846 feet. It is not
the object of the present paper to describe the geological features
met with in this exploration, nor to record in any detail the strata
passed through ; but it may be noted that the thickness of barren
ground, intervening between the lowest vein of the Radstock
series and the first workable vein of the Farrington group, was
here found to be 628 feet, and that it contained the well known
beds of Red Shale which invariably lie between the two groups.
It may also be stated in passing, that the result of this sinking
has entirely falsified the expectations of some who had turned their
attention to the subject. It had long been held in certain quarters
that wherever the Farrington veins have been worked beneath
the Radstock series, the former have been thin and inferior ; and
that the Farrington veins are only valuable in the margin outside
the outcrop of the Radstock group. The writer could never see
any good ground for this contention, believing that the range and
thickness of the seams composing the Farrington group could
not be affected by strata by which they were not overlaid for
nan nna =i == -=-=-------=--=-- RADSTOCK SERIES, ------—---~----->
€ ---=-—----------------' FARRINGTON SERIES.
SECTION OF MIDDLE PIT,
RADSTOCK.
ScALe 280FT TO AN INCH.
Pre [ee] |
|New Repo SANDSTONE
=| CONGLOMERATE
=| GREAT VEIN
Top LitTLe VEIN
Mippte VEIN
_|Styvinc VEIN
Bottom LitTLe VEIN
Butt VEIN
DHjOverae Faurt
Styvinc VEIN,
Bottom LitTLe VEIN
But Vein
Nine IncH VEIN
Rep SHALES 177 0 ;|}0
ee SALT SPRING 225 |.3 | 0
a. 2ND SALT SPRING 230 | 5 | 0
\
|
|
“H3ro SALT SPRING 282 1 i)
|
Bottom oF Pit 298 Std.
iS Bottom oF Bore Hote || 307 4} 10 |
87
long ages afterwards. He considered the contention in question
especially valueless, because in all probability the entire area now
occupied by the Farrington group was originally covered by the
Radstock series ; and the fact of one part having been denuded
while another area had escaped denudation, could not in his
judgment affect the thickness of the seams lying beneath.
And without expressing any sanguine opinion as to the com-
mercial value of the undertaking, which a little time will probably
establish, the writer can only say that the result of this sinking,
carried out in the very centre of the Radstock basin, has entirely
disproved the evil predictions referred to; the thickness of coal
proved being fully equal to what has been met with in other parts
of the district.
To return however to the subject of the paper, the strata
immediately under the Radstock series yielded little or no water,
and what little there was appeared to be quite fresh. The Red
Shales already referred to were cut at a depth of 190 feet below
the 9 inch vein, and were found to be 170 feet in thickness,
presenting no feature of special importance. The first indica-
tion of Salt water was in a bed of Sandstone met with at a
total depth of 1353 feet, and it yielded 90 gallons an hour. Ata
depth however of 1385 feet from the surface, and in a bed of Grey
Sandstone, 21 feet in thickness, a much more considerable spring
of water was met with which was found to be highly impregnated
with Salt. In approaching this bed the miners were first warned
of the presence of these Springs, by the water issuing with consider-
able force from the bore holes made for blasting purposes, in
some instances spouting up to a height of several feet, and
evidently indicating considerable pressure. On reaching the rock
from which the water came, it was found to be full of joints and
fissures from which the water issued on all sides in considerable
quantity, amounting at first to 1,000 gallons per hour; but
gradually decreasing until it did not much exceed 400, Although
the water was excessively salt, as members will find who taste the
88
sample produced, an examination of the rock from which it issued
shewed that it contained no trace whatever of Rock Salt.
An attempt was made to stop back the water, which was found
both expensive and troublesome in sinking, and for that purpose
the shaft was lined for 30 feet with iron casting, technically
called ‘“tubbing,” the operation being attended with some
degree of success. In thus damming back the water, it was
necessary to carry a small vent pipe from the casting, as high
up the shaft as the water would rise, in order to carry off any
pent-up gasses; and it was found that the water rose up the
pipe to a height of 102 feet. The pressure under this head of
water was so considerable, that the water forced its way
through joints and fissures in the strata, and did not rise any
higher ; but it is probable that the natural level of the water
may have been much higher than was indicated by the height
of the water in this pipe.
Through the kindness of Mr. Coomber, principal of the
Merchant Venturers’ School in Bristol, whose valuable assistance
the writer is glad to have this opportunity of acknowledging, he
is enabled to supply the following analysis of the water. Writing
on the 5th February, Mr. Coomber states as follows :—
‘“‘T have made a qualitative analysis of your sample.
“There is almost as much matter dissolved in the sample as in
sea water.
“Next to the Chloride of Sodium present (Sea Salt), Lime
Salts occur in greatest quantity. There is a considerable
quantity of Carbonate of Lime held in solution by Carbonic
Acid.
‘Potassium Salts also occur in quantity, Alkaline Carhonate
is present, and perhaps both Potash and Soda are present in
this form.
“There are also present in small quantity Iron, Alumina,
Magnesia, Lithia, Sulphuric Acid and a trace of Phosphoric
Acid.”
89
And Mr. Coomber has supplemented this by the following
more exact analysis received to-day :—
“T regret to say that I have been unable to get an exhaustive
quantitative analysis of your sample of water completed in time
for your paper upon it, but its qualitative examination is complete,
and almost all the weighings made that have any teaching
regarding the sample.
‘The principal constituent of the water is Chloride of Sodium.
Other constituents present in quantity are Lime, occurring both
as Calcium Chloride and as Carbonate of Lime held in solution by
Carbonic Acid.
“Potassium Chloride is also present in appreciable quantity as
well as Silica.
“Lithium and Iron occur in very small quantity, and there are
also present exceedingly small traces of Magnesium and of
Sulphates and Phosphates.
_ “Jodides, Bromides, and Nitrates are entirely absent.
. “The specific gravity of the sample is 1:02899.
“The total weight of the solids dissolved (dried at 180c°), is
1292-34 grains per gallon.
“The weighings that have been made are the following :—
«“ Calcium Chloride ait ... 149-27 grains per gal.
“Carbonate of Lime... me 11:99 i
amount of Potassium, Chloride
and Silica
”
“Sodium Chloride, with a small
broore
1252-75 re
_ The writer does not possess sufficient chemical knowledge to
discuss as fully as he could wish the chemical aspect of the
question; and the analysis having only come to hand this
morning, there has not been sufficient time to give it adequate
consideration; but the following remarks may serve to direct
attention to one or two points in the analysis.
90
The specific gravity may be compared as follows :—
Pure Water being ... ae Me 1-000.
Sea Water is ae aud is 1:027.
Bath Mineral Water is... ... 10025.
And Radstock Salt Springs -- 102899:
Then as to Solids,—the Bath Mineral Waters contain only
144:018 grains, according to Merck and Galloway, while other
writers give even less; but the Radstock Salt Springs yield,
according to Mr. Coomber’s analysis, 1292°34 grains per gallon.
It may be further noted that nearly all the ingredients in the
Bath Mineral Waters are present in these springs, although in
very different proportions.
Soon after this Spring was tapped, it was found, much to the
annoyance of the Engineer in chage, that certain boilers which
were partly fed by the water from tl.is mine had become encrusted
with Salt. A specimen of this encrustation is now produced,
and the quantity of Salt it contains is very remarkable—
considering that the water before reaching the boilers was
diluted with about twenty times its volume of fresh water from
other sources.
As the sinking proceeded, another Salt Spring was met with
about 302 feet below the one I have already described, and at a
total depth of 1,693 feet from the surface. In this instance also
the Spring indicated very great pressure from beneath, for not
only did the water rise some height out of the bore holes, but
the beds of shale in the bottom of the shaft were heaved up bodily
through its agency. No separate analysis of this Spring has been
obtained ; but it was apparently similar in character to the one
previously met with. Its yield was found to be 100 gallons per
hour ; but a corresponding decrease seems to have taken place in
the upper Spring, with which it may possibly be connected, as
the total quantity continued as before at about 400 gallons per
hour, and it has so remained down to the present time.
Although new in Radstock, the occurrence of Salt Springs
91
seems to have been discovered in several previous sinkings to the
same series in other parts of the district.
The writer has not been able to obtain particulars of some of
the earlier shafts, which were sunk many years ago; but he is
indebted to the Managers of various neighbouring Collieries
for the following information on the subject.
At Braysdown Oolliery, where, about the year 1862, the shaft
was sunk from the Radstock to the Farrington series, the
Manager reports as follows :—
“The water found in the sinking to the Farrington series was
a little Salt before we came to the Red Shales; after passing
through these it was and is at the present time intensely Salt ;
it was very much like brine, from the Red Shales down to
where we left off sinking.
“The water is most destructive to iron and steel, destroying
their properties by eating them away, exposing the grain of iron
as if it was wood, and making it very hard and uncertain. It covers
wood with a coat almost like sheet iron, and preserves it from
decay. At the sides of the roads where it runs, it leaves a
thick sediment very much the colour of blood, but perhaps a
little darker. This I believe to be largely composed of iron,
and it is very heavy indeed.
“These Springs of water do not increase with us in any case,
and if they decrease it is very little indeed, having remained
much the same for the last twenty-four years.”
At Foxcote Colliery, where the same ground was afterwards
proved, a similar result was experienced. The then Manager
informs me that “at a depth of 531 feet from the surface, and
in avery hard bed of Grey Sandstone, 33 feet in thickness, he
met with a Spring which yielded 700 gallons per hour. Also
that 87ft. 9in. below this bed he had another Spring, which
yielded 96 gallons per hour; and again, at a point 391 feet
lower down, he cut a third Spring, yielding 80 gallons per hour,
which so increased in going downwards that the sinking had to
92
be abandoned at a total depth of 1,212 feet from the surface.
The water from all these Springs was extremely Salt. The
Manager tested it on several occasions by boiling a gallon of it,
and when the water was boiled away, he had a common tea cup
full of Salt left on each occasion.”
At the Old Mills Colliery, on the other hand, where two
shafts have been sunk through exactly the same ground, although
a good deal of water was met with, it was uniformly fresh ;
and it remains so to this day. In this instance, however,
the circumstances are somewhat different, the Secondary beds
overlying the Coal Measures being very thin, and the shaft
having passed direct from the New Red Sandstone into the
Farrington Measures, without any of the Radstock series
occurring between.
It may be instructive to compare the depths at which these
Brine Springs have been met with in the different localities to
which I have referred, taking the sea level as the datum for
comparison.
Middle Pit. Foxcote. | Braysdown.| Old Mills.
Depth in | Depth in | Depth in | Depth in
Feet Below| Feet Below] Feet Below | Feet Below
Sea Level. | Sea Level. | Sea Level. | Sea Level.
To I. Spring. 1,110 176 708 242 Feet
eA hee we 1,142 264 to (water
pea Clear 1,450 655 1,241 fresh),
As to the probable source.—The frequent occurrence of these
Salt Springs in the Deeper Measures in and around Radstock,
has naturally given rise to some speculation as to their probable
source ; and whatever their origin may be, it seems tolerably
93
certain that they cannot derive their supply from the Keuper
Marls above. In the memoirs of the Geological Survey mention
is made of crystals of Rock Salt occurring in these Marls at
Hallatrow, and at one or two other places, which, apart from
other evidence, may be taken to indicate their identity with the
same formation in Worcestershire and Cheshire, where it is so
rich in Salt; but having examined the New Red Sandstone at
many points in and around Radstock, the writer has never found
~ even an isolated crystal of Rock Salt ; and it may be stated with
tolerable certainty that nothing in the nature of Salt Springs
exists in the Keuper Marls of this neighbourhood.
In proof of this it may be stated, that all the wells in the
lower parts of Radstock and adjoining parishes have been sunk
in these Marls, the water obtained being perfectly suitable for
domestic purposes; and, as already stated, the shaft sinkings
through the same ground shew a like result.
It also seems clear that the source of supply cannot be in the
upper or Radstock Coal Measures, which have been worked
extensively for many years, without any trace of Salt Springs
being met with.
It also seems evident that these Springs cannot have their origin
in the beds of Sandstone from which they flow, for the writer
having observed them very closely has never found the slightest
trace of Salt in those rocks,
It also seems unlikely that these Springs can come from the
Pennant rocks which lie at no great distance beneath, for it is well
known that they contain no Rock Salt; and although they are
commonly very heavily watered, they generally derive their supply
from the rainfall near the outcrop; the water being so pure that
the Bristol Water Company at one time proposed to acquire a
celebrated Spring in an Iron Mine in the Pennant, at Frampton
Cottrell, in order to augment the supply of Bristol.
The more the facts are considered, the more difficult it seems
to be to account for these Springs; the origin of which must
94
probably remain a matter of conjecture. Notwithstanding the
distance from the nearest coast line, and the fact that the outcrop
of the Farrington series is far inland, it is possible that the source
may be the waters of the Bristol Channel, which may find their
way along the lines of faults or other underground fissures to
this inland district. The great difference of level, however,
between these Springs at diffeaent Collieries hardly seems to
favour this theory. But is it not also possible that we have in
these Salt Springs, long hermetically sealed, a remnant of that
ancient sea which swept away the upturned edges of the Coal
Measures, before the New Red Standstone began to be deposited.
In conclusion, the writer would only allude to one or two
circumstances connected with these Springs, which may or may
not have some bearing on their origin. Sir Charles Lyell, in his
Elements of Geology, page 362, remarks that “As in various
parts of the world red and mottled Clays and Sandstones, of
several distinct geological epochs, are found associated with Salt,
Gypsum, and Magnesian Limestone, or with one or all of these
substances, there is in all likelihood a general cause for such
coincidence. Nevertheless, we must not forget that there are dense
masses of Red and Variegated Sandstones and Clays, thousands
of feet in thickness, and of vast horizontal extent, wholly devoid
of Saliferous or Gypseous matter. There are also deposits of
Gypsum and of common Salt, as in the Blue Clay formation of
Sicily, without any accompanying Red Sandstone or Red Clay.”
Now it is a strange coincidence that the beds of Grey Sand-
stone in which these Radstock Springs rise, occur near, and, for
the most part, immediately under the Red and Mottled Shales
which intervene between the Radstock and Farrington series;
but this may be a coincidence only, and it may be questioned
whether either of the theories indicated offers any adequate
solution of the origin of these Springs, which will probably
remain a matter of doubt and uncertainty.
95
By Rev. H. H.
List of Fossil Mammalia Found near Bath.
Wixwoop, F.G.S.
Read 10th February, 1886.
from
alns
d other rem
ia an
the drift deposits in the Bath basin,” was read before our Club
the Paper, on “the Mammali
Since
by the late Charles Moore in 1869, some fresh sections have been
1 additions made to the list
I have, therefore, thought it might be
,» and severa
opened in the gravel beds
of extinct animals.
tabulated
iscoveries in a
useful to record the result of those d
form for the sake of easy reference.
*M01999[[09
S'M “H ‘H
‘uinasny, Weg
‘mIneSsN]L
ywweq sow
*[[098,"M"H’H
‘TUnesny, We
‘munesny WIV
“we YS OW
‘TI8H UAL,
"001909
100 8M ‘HH
‘mnesny Weg
*201499[[09
8’ “H “H
‘unesny Weg
‘wnesny Weg
*U01402T
709 8M “H
"HE ‘wanesnyy
yaeq 10g
TUnesny, WIV
“CHLIsodaa
quagHM
*J9911G 9789489
‘1e[[90 OJ sumo1yBAvd
“x9 "ployysory *|[eyyre'yT
‘uussnd ga ‘xog “ITH
SIPPIAT ‘ornssy 9191[0O
*ployysoay spoq joavry
"xog ‘TH
SIPPIIA “Seanssy 9141/00
*paoyyseig speq [eavsy
_ S68 “WBysy OI
Ieou ‘UOAW JOATI ou
SUIYsy Ul pe]suvjue peo
*paxoyqse. iy
*prlojyysor iy ‘spoq [aav14y
‘od pig
“Wey “TeyywyT “3014
-qnd ploygeroyy ‘pxrozyysor iy
“TG Ae T
‘espliquie’y ‘yIeq
qyeg "a0j10m 7,42 M [1837
qyosioq pues yasiau0g
*SU14jNO pleyaroyy "pros
“JIBS “90'T “JG WOFMON
‘Adojomen §=sqmMooplAy
2 oquiooud'T *pxrozyso. iy
‘TeGALeT spoq [aavsy
“CNOO4 WHGHM
*souImBy
‘som0q
pur q}90} Le;OpT
som0g 29 prox
*eu0q dary
O[BULT 29 OB UL
—spvoy oM,
"029 ‘44093
IB[Oul'e.1g9}19 A.
"4390 xe[OW
*sd@[OUL
pue viqry‘sysny,
“SHIOUdS
*1'8OQ DIEM
‘snuaf nfouos sng
*(SI[ISSOJ)
‘snyjnqny snnbq
"snvndoungy Uosig
"SniuabiWitdd SOT
*199pUlIY
‘SNPUDADZ Snarsag
‘deeyqg ysuyl
‘snqnyosopy snquaoQ
*so1200U
1qy pousoy omy
‘poarey Buoy ‘snu.
-1.40Y 91] SOLBIOULY QT |
snnbyup snydayq
YROWUMD TT 10 snr
UAB Uletd sNY MAT
aNV SONaS
eo
96
Summary of Proceedings for the Year 1885-86.
Mr. PRESIDENT AND GENTLEMEN,
In reviewing the events of the past year, the first fact to
record is the absence again from the Anniversary programme of
the evening’s social gathering. The Committee appointed to
carry this out were unable to do so by difficulties which they
found to be insurmountable ; with the exception of this incident,
a subject of regret to many, the Proceedings of the year may be
considered fairly successful. The Papers read at the afternoon
meetings sustained their usual character, and the attendance was
more encouraging ; though there is still room for improvement in
this respect, as barely one-fourth of the whole number of
members were present. Natural History has been well repre-
sented, and it can not be deemed invidious to others if especial
allusion be made to the admirable paper on the ‘‘ Bournemouth
Firs” by our venerable President. The vigour of his mind and
the lucidity of his pen seem not in the least abated ; and may he
be long spared to us to enrich our ‘‘ Proceedings ” with the results
of his keen observation, accuracy of statement and eloquent
simplicity of language !
AFTERNOON MEETINGS.
The afternoon of March 18th was given up to Mr. Broome who
continued his account of the Fungi of Bath and its neighbourhood,
and contributed another of those valuable papers on Mycology, the
study of which has been his life-long pursuit, and has acquired
for him well earned reputation (vide page 1). This was followed
by a short description of an abnormal flower of Penstemon sent
to him for examination by a member of the Club (vide page 35).
Canon Ellacombe’s remarks on “ Study of Varieties with reference
to Field Club work” was postponed till the Quarterly Meeting on
7th April, when
Excusing himself for having but little to lay before them, and that
97
little not being new, he said, that clubs like the one he was addressing
ought to be a clubof observers, and as their president had oftenimpressed
upon them the duty of observing, he would venture to bring before
them some examples of matters which required their observation.
They need not go out of their way to do this, but everything they
met with in their regular walks or excursions that was a deflection
from a given type, anything abormal or eccentric ought to be at once
catalogued ; by so doing local clubs would do much good. There were
three or four objects he would specially call their attention to as worthy
of this observation. First, Architecture ; It had long been laid down
that an accurate date could be fixed for Norman, Early English,
Decorated, and the Perpendicular styles ; but the conclusion he had at
length arrived at was that though these dates were most valuable, yet
they must be received with great modification. It was often thought
that architects worked by a certain fixed law in Medieval times and
never departed from this law and standard, but he thought architects
then were much like architects now, and they went in for imitations of
a past period. Then as now in their church restorations they were as
reckless as the destroyers of our own day ; in fact, they had not any
hard and fast rule. Though it was difficult to prove the cases in
which architects previous to date had anticipated the style peculiar to
that date, yet in some instances it could easily be traced, eg., Norman
architects by the intersection of two round arches built pointed arches
as much as those of a subsequent period. To come to latter instances ;
why in Decorated architecture should there never he a vertical line as
some suppose? Look at Gloucester Cathedral, there Perpendicular
work was found at least 100 years before the accepted date of that
style. Fan tracery, so distinguishing an English feature, was con-
sidered not to have come in till temp. Henry VII., exceptin Gloucester
Cathedral, where we find it in work of the 14th century (1360). Then
again we have architects directly imitating work of an earlier period ;
take for instance the so-called Norman work at Bradenstoke Priory,
and the Norman work introduced into the Perpendicular wall at
Kilmersdon. To come nearer home take the case of Bitton (his own
church), originally an Ante-Norman building, where the Bishop
Buttons of the 14th century literally smashed up the old Norman work,
the 15th century architects destroyed the old chancel and west front, and
G
98
those of a later period put a Norman corbel table into a Perpendicular
wall. The churches at Dauntsey and Iron Acton contain likewise
copies of older work, and this is very conspicuous in the buildings of
Oxford. Hence the conclusion he wished to impress upon the members
was that the date of a building could not be always determined by the
style of its architecture. He ventured to think that the interest in the
Somerset and Devonshire churches was much lessened by this fact of
many of them being simply an imitation and reproduction of each
other. Then there was another point worthy of observation, the stone
which was found in the old buildings ; beneath the variety in the
stone often lurked a great history, e.g., in one church granite was found
mixed up with the stones peculiar to the neighbourhood. This led to
the discovery that the original founder had property in Cornwall,
whence, doubtless, this foreign material was derived, The mention of
this led him on to the second subject, z.e. (2) Geology. Here every
variety in the strata should be noted. Were the strata always
uniform, one bed following another in regular succession, how little
should we know about the study ; but the variation in their succession
caused by the disturbances and topsy-turvy movements of some of the
beds added go very much to the interest of the study ; the greater the
variations the greater the interest, eg., the disturbances in our
own Mendips, as at Vobster. Though not professing to be a
geologist himself, yet when in the north of Ireland, between Port Rush
and the Giant’s Causeway, he could not fail to be struck with the
varieties in the colour of the rocks—white rocks stained by red
streaks and capped by black. Then there were the varied movements
of a river ; take, for instance, the Avon, which ought naturally to flow
in a straight line, but witness itsmany windings, study the causes of
these windings, follow the turns ; consider why the water retires here
and encroaches there, and you will have a good key to the geology of
the district between Bath and Bristol. Then again the gorge of the
Avon, which drained off the ancient lake which must have existed
there once; viewed from the Hogsback it looked a mere crack in
the rocks, yet consider how this came about, and the vast alteration
in the surrounding country were this gorge to be dammed up, as
it might easily be by some Brunell of the period. Finally, the third
subject he wished to notice was his favourite one (3) Botany. Of this
99
he certainly knew more than Geology. How full was the study of all
sorts of deviations from the accepted forms of classification, both in the
flowers, the leaves, and the roots, called “vegetable monstrosities,”
until Darwin taught us that all these variations were but the gradual
workings of nature pointing back to old forms once existent, or forward
to some evolution about to come. Note every variety, whether of leaf
or flower, accumulate facts, they will all fall into their right place at some
time or other. This was the one of the chief lessons that great observer
taught us, Carnivorous plants notice especially ; they not only killed but
digested the insects. This food was necessary for their existence. The
utricularia, with its fibrous roots and the little bladders at the end has
recently been discovered to be a feeder on fish, these appendages being
used for that purpose. Notice, too, all those plants that are visited by
insects and find out the reason of these visits, The colours of plants
should be observed; the two opinions about them are that they were
originally (1) all green, (2) all yellow. Green, he thought, was the
more ordinary colour, and that most of them arose from green originals ;
the richer colours (the golden autumnal tints) arising from decay and
death. All yellow flowers were entomophilous—fertilised by insects—all
green, anemophilous—or fertilised by wind—according to Sir Joseph
Hooker. The observations of Col. Jones of a few white spots on lady-
ferns led to an important result as to fertilisation. In conclusion, he
would impress upon local clubs the necessity also of noting the
variation in language, local phrases, peculiarities and expressions, which
were fast passing away.
Mr. Browne agreed with Canon Ellacombe as to his remarks
respecting the imitations in some of the churches mentioned, but
the subject was too great a one to deal with on the spur of the
moment.
After some remarks from Mr. Broome, the warm thanks of those
present were given to Mr. Ellacombe for his admirable address
and hope expressed that they might see it in a more permanent
form for their future instruction.
The SECRETARY (Rev. H. H. Winwood) exhibited some fossils,
which he found during a visit last autumn (1884), to the Rocky
Mountains. Having briefly pointed out, on the maps recently
100
published by the Geological Survey of Canada, the geology of those
regions, he said—
The Canadian Pacific Railway, which would shortly connect the
Atlantic Ocean on the east with the Pacific on the west, had lately
opened out a tract of country in the heart of the Rockies hitherto but
little known ; and it was his good fortune to accompany Professor
Selwyn, Dr. Dawson, Professor Boyd Dawkins and other geologists in
a geological ramble down the Kicking Horse Pass in search of some
fossil evidence, which would help to determine the age of the beds.
The Secondary and Tertiary strata, so horizontal in the Prairie country
to the east, became much disturbed and folded at the “foot hills” of
the Rockies, until on approaching the head of the Kicking Horse Pass,
some 5,000 feet high, the older beds—which here come in and are sup-
posed to be of Devonian age—became tilted up in some places quite
vertical, if not reversed altogether. These beds, consisting of
Quartzites and calcareous rocks, were diligently searched for fossils in
vain ; but just after crossing the high trestle bridge over the Kicking
Horse River, on the left of the track a micaceous slab of rock with
apparently an easterly dip had been exposed, and certain markings
thereon like worm tracks attracted his attention ; on examining these
he found also the trace of something evidently organic, which after
some time and trouble was chiselled out. The exact nature of the fossil
he was unaware of at the time, but a short distance further west on
the same side of the track he found a band of calcareous rock six
inches thick, crammed full of portions of ¢rilobites. On returning home
he shewed them to Dr. Hicks, well versed in the Archzan rocks of
England, and was informed by him that the first specimen contained
the tail of a Paradoxides upon it, and that the calcareous fossiliferous
band was full of portions of the same genus, and of Conocoryphe and
other allied forms, thus shewing that these rocks contained a
Primordial fauna, and that they belonged to what Dr. Hicks calls the
Menevian zone, so ably worked out by himself in Wales. He further
stated that in his opinion these beds were not far distant from an
Archean axis. This was a fortunate discovery, as it will enable future
explorers to take these beds as a datum line, and it is expected that Dr.
Dawson, who was then about to survey that portion of the track, will
have by this time been enabled to define the position of the other beds
both eastward and westward. Specimens of the fossils were exhibited.
LLMs Oe eee
101
The first of the winter meetings took place on Wednesday
afternoon, December 9th, when the President (the Rev. L.
Blomefield) read a paper on the Bournemouth firs (vide page 40).
Before beginning his subject he exhibited a nest of the water-
ouzel presented to the institution by Mr. Bankart. This “dipper,”
he said, allied to the thrush and the blackbird, is essentially a
waterbird, whilst the latter are land birds. It may be seen by
the sides of rapid streams, and diving into the water like a moor-
hen. It endeavours to keep at the bottom of the water
as much as possible in search of its food, consisting of
water beetles and fresh water shells. Its nest is built
in the rocky inequalities by the banks of streams, and is
composed of a tangled mass of brown rootlets. The specimen
in question was from the Yorkshire moors. The bird is a
native of Somerset, and especially frequents the rocky streams
on its borders near Devon. The President took the opportunity
of expressing a wish that some one connected with the county
would present a local specimen to the museum in Bath.
The Rey. Canon ELLACoMBE, who had taken the chair, ex-
pressed the pleasure it gave the Club, and especially himself, at
hearing another of the President’s papers, so full of interest and
originality. Though a labour of love to him yet they all felt
that he must have taken no ordinary trouble in preparing it, and
he was glad to see so large an audience on the occasion. He had
never doubted that the Scotch fir was indigenous. The Pinus
pinaster too, associated with the former at Bournemouth, had
been admitted into the English flora. Mentioned in old writers
as the pine apple tree, it had now lost this name when the present
fruit was discovered in America. Owing to the rapid onward
march of the Scotch fir it is a wonder that it has not spread
even further. Kingsley alludes to the way which the pollen of
this tree propagates itself in his charming essay “ My Winter
Garden.” The growth of the Scotch fir on our neigh-
bouring hills was alluded to by many of the members present,
102
and the President said the tracing of its former existence in the
neighbourhood might well be one of the objects of the Club’s
weekly walks.
Mr. NorMAN then gave some notes on the Algz of thermal
waters, with especial reference to those of Bath (vide page 53).
In the discussion which followed, the PRESIDENT congratulated
the writer on his researches into the natural history of our hot
springs, and urged him to continue his observations therein, so
that their natural history, both animal and vegetable, might in
course of time be well known. Some remarks on the temperature
of the water followed, and a wish was expressed that the scien-
tific observations which it was believed were being systematically
carried on should be made public, so that those locally interested
in the question might be able to obtain some trustworthy data as
to the variation, if any, in their volume and temperature.
The third meeting took place on Wednesday, January 13th,
Mr Skrine in the chair, when Mr. GREEN read a paper on “ The
Earliest Map of Bath ”(vide page 58); another of those valuable
historical leaflets with which Mr. Green has favoured the club
from time to time. The orginal, he said, was to be found in the
British Museum. No exact date could be given for it, but it was
made about 1568 by one Wm. Smith, a herald and antiquary,
who in his account calls Bath “A little cittie, yet one of ye most
anncientest in England.”
McMortrig, F.G.S. fe wie Ye ee
10.—List or Fosst, MAMMALIA FounpD NEAR BATH, BY
THE Rev. H. H. Winwoon, F.G.S8. a Lit
11.—SuMMARY OF PROCEEDINGS FOR THE YEAR 1885-86, —
BY THE SECRETARY ee i ae ed
eet Sts 2 FEB 1988
PROCEEDINGS
é OF THE
AND
VOL. VI., NO. II.
| PRICE ~HALF-A-CROWN.
’
' BATH:
“THE: ‘HERALD OFFICE, NORTH GATE.
DAVIES, REND: PUMP ROOM LIBRARY.
3
mics
5 Me by
k '
a ow . ~~ Cee ne ee og) ee ae ee
125
Notes on the Geology of Brent Knoll, in Somersetshire. By
Horace B. Woopwarp, -F.G.8.,* of the Geological
Survey of England and Wales,
(Read March 10th, 1886.)
The conspicuous hill of Brent Knoll rises to a height of about
450 feet above the Alluvium of the Burnham Level between
Highbridge and the Mendip Hills ; its precise height above the
sea-level is 457 feet. Some attention has been given to its
Geological structure, but as it has been differently interpreted,
_ afew remarks on the subject may be of interest. Thus the area
_ occupied by the Romano-British Camp, was regarded by Conybeare
and also by William Sanders as Inferior Oolite,+ while on the
e. - Geological Survey Map (sheet 20) it was originally coloured as
a Marlstone or Middle Lias, the lower portions of the hill being
regarded as Lower Lias. During the re-survey of the district in
1872, it fell to.my lot to examine Brent Knoll, and in the
A - Memoir subsequently published, a section to illustrate the
_ structure of the hill was inserted.t This section represented the
4 Knoll to be capped by a thin layer of the ‘“ Cephalopoda-bed ”
composed of Upper, Middle, and Lower Lias.
No natural section was to be seen at the encampment, but
there were loose blocks of sandy and ferruginous limestone which
= ontained Ammonites; and although too imperfect for specific
_ determination, the specimens were considered by Mr. Etheridge
3 ¢ to belong to a type that characterizes the so-called “Cephalopoda-
Bega This paper is communicated by permission of the Director General
of the Geological Survey,
_ t+ Conybeare and Phillips’ “Outlines of the Geology of England dod
Wales,” pp. 255, 275 ; Sanders’ “ Map of the Bristol Coal Fields,” 1862,
t “Geology of East Somerset,” &c. (Geol. Survey), p. 116.
- Vou. 6, No. 2. ,
126
bed,” which occurs at the top of the Midford Sands in Glouces-
tershire. So far as the divisions of the Lias were concerned,
the identification of Upper Lias was satisfactorily proved by the
presence of Ammonites communis, A. bifrons, &c., on the platform
beneath the Knoll. Here pale earthy and rubbly limestones,
(beds which characterize the lower part of the Upper Lias at
Pennard Hill, and further south at Yeovil and Ilminster), are
turned up in the ploughed fields and may be traced on the brow
of the hill to the west of the Knoll.
The Marlstone rock-bed was probably present in an attenuated
form, although at the time of my first visit I found only “ one
loose block on the hill which might be identified with this bed.”
At Pennard Hill its thickness is from 15 to 18 inches, and at
Glastonbury Tor it is not much more.*
The rarity of sections, however, rendered the interpretation of
the Geology of Brent Knoll far from satisfactory, and I was
glad to have the opportunity of revisiting it in July, 1885, on
which occasion I had the advantage of being accompanied by
Mr. Alfred Gillett, of Street; Mr. J. Edmund Clark, and Mr
Martin F. Woodward.
On approaching the foot of the hill from the Brent Knoll
railway station, our attention was attracted by a spoil heap
thrown up from a well-sinking. This proved to consist of blue
micaceous Shale, and a search disclosed several specimens of
Ammonites margaritatus, together with Belemnites and fragments
of lignite.
This discovery leads to the conclusion that no Lower Lias is
exposed at Brent Knoll, for the well was commenced but a few
feet above the level of the Alluvium which encircles the hill,
and it had been sunk to a depth of 15 or 20 feet, if not more.
* The thickness of “about 15 feet” assigned to the “ Marlstone-
rock,” at Glastonbury Tor, by Dr. Wright, is I feel sure much
exaggerated. See Quart. Journ. Geol. Sce., vol. Xvi., p. 34.
4
.
4
|
ee ee Ne le * a
a ia .
”
=
127
There are, moreover, certain beds exposed in a lane-cutting west
of East Brent Church, that were described by my colleague, Mr.
W. A. E. Ussher, as “hard and rather fine-grained light grey
Limestone, with bluish-grey spots, containing Ammonites.”- These
beds are interstratified with clay, and I formerly regarded them
as Lower Lias,* but they proved on re-examination to contain
Ammonites communis, and thus to belong to the Upper Lias.
This additional evidence confirms the view that no Lower Lias is
exposed at Brent Knoll.
The upper sandy beds of the Middle Lias are not well exposed
in this hill, but they form a comparatively steep scarp, surmounted
by the Upper Lias. Nor are the Midford Sands shown in
section, although portions of the beds are thrown out from many
rabbit burrows. The thin capping of the so-called ‘‘ Cephalopoda-
¥ __ bed,” that had been inferred from the rubble and loose blocks’
of calcareous sandstone of which the walls of the Camp are
formed was again examined and I was fortunate in finding a
specimen of Rhynchonella cynocephala in one of the small
exposures, in re-arranged material on the summit of the Knoll.
Another and fragmentary specimen was also obtained from a
a loose block of calcareous sandstone by Mr. J. E. Clarke.
Considering the nature of the ground, this is the most
satisfactory evidence that could be obtained of the age of the
beds forming the Knoll. Specimens of Serpula also occurred,
‘ and these prevail at the same horizon below the Inferior Oolite
_ in the neighbourhood of Beaminster and Crewkerne.
It should, however, be mentioned that a variety of Rhynchonella
cynocephala has been found by Mr. E. Witchell in the lower beds
of the Inferior Oolite near Stroud,t so that the species has a-
higher range in the Cotteswold district than it is known to have
in Dorsetshire.
_ * “ Geology of East Somerset,” &c., p. 116.
+ “ Geology of Stroud,” 1882, p. 47.
128
The section of Brent Knoll would therefore be the following*:—
**Cephalopoda-bed” and
Midford Sands’ | \ about"2004ee8
Sands
Upper Lias ... Clay and Stone vs >
: Rock bed and Micaceous ) 80
Middle Lias Sands 1 ”
Micaceous Shales and Clays ,, 130 ,,
Hence the section published in the Geological Survey Memoir
is incorrect, with respect to the Lower Lias, which may now be
altered to Middle Lias.
SECTION OF BRENT KNOLL.
Scale three inches to one mile. A
————————
a. Cephalopoda bed. c. Upper Lias. e. Middle Lias Clays.
6. MidfordSands. . d. Mddle Lias Sands.
Comparing Brent Knoll with Glastonbury Tor we find the
same structure with the exception that no traces of hard
beds at the top of the Midford Sands can there be recognized.
The Tor is formed of these Sands, resting on a platform of
Upper Lias Clay and Stone, beneath which come the Marlstone
rock-bed, and the Middle Lias Sands, well shown in some of the
deep road-cuttings. Micaceous clays and sandy Shales beneath
the Middle Lias Sands, are opened up in three briekyards to the
north-west of the Tor; and although I could find no organic
remains in the beds I feel confident they belong to the same
division as the basement beds of Brent Knoll, which contain
Ammonites margaritatus.
' The general sequence of beds forming the Middle Lias of this
district is the following :—
3. Marlstone rock-bed with 4. spinatus, A. margaritatus, &c.
* The estimates of the thickness of each division are based on the
height of Brent Knoll.
129
2. Sands—not usually fossiliferous.
1. Micaceous Sandy Shales and Clays with 4. margaritatus.
These beds may be traced from the Dorsetshire coast inland
through the district north of Yeovil to Brent Knoll.* Whether
the junction of Middle and Lower Lias should be taken at the
base of the beds with A. margaritatus, or still lower, is a question
about which much difference of opinion has been expressed ; but
it is usual now to group the beds with A. capricurnus, A.
Henleyi ; A. Jumesoni, &c., wherever they occur, with the Lower
Lias. The Middle Lias is well developed on the Dorsetshire
coast, but it becomes much thinner towards the Mendip Hills.
The determination of Middle Lias at the base of Brent Knoll
may be of some slight importance to those interested in the
prospects of Coal on the south of the Mendips; at the Knoll
itself a considerable thickness of Middle Lias, as well as the
whole of the Lower Lias being present. The fault which
stretches from the neighbourhood of Wanstrow,} to the south
of Pilton, and brings the Lias north of Glastonbury against the
Red Marls, is concealed beneath the Alluvium north of Meare,
and its continuance in the neighbourhood of Brent Knoll cannot
be indicated with any certainty. It is, however, evident that
Brent Knoll, like Glastonbury Tor, forms part of a basin-shaped
or synclinal structure in the rocks, and a greater thickness of
Lias might be expected in the immediate neighbourhood of these
hills than in the areas further away. |
Concerning the origin of the hill itself, the denudation is
probably due in part to subaérial and in part to estuarine agencies,
Knolls like Brent Knoll and Glastonbury Tor are met with in
many other parts of the south-west of England, but nowhere
* E. C. H. Day. Quart. Journ. Geol. Soc., vol. xix. p. 278, and C,
Moore, Proc. Somerset Arch, Soc., vol. xiii., part 2, p. 119.
+ The inlier marked as “Great Oolite” on the Geological Survey
Map, at Waustrow, is in reality Fulle:’s Earth.
150
else are they so conspicuous from the fact that at these localities
they are further removed from the main mass of Oolites in the
escarpment. Near Bridport, Colmer’s Hill is a well-known Knoll
of Midford Sands and many other outliers of the Sand and
Inferior Oolite are met with in this neighbourhood. Further
north again similar Knolls occur near Montacute and other places
between Ilminster and Castle Cary. Those near South Cadbury
indicate how the severance of outliers from the main mass may
take place.
Subterranean drainage and erosion in the first instance may
lead to the formation of underground channels in the impervious
Lias Clays beneath the porous Midford Sands and the Limestones
of the Inferior Oolite. The Limestones themselves may be in
part wasted by chemical dissolution, and if channels are formed
in subjacent strata, slight subsidences must take place here and
there, and pave the way for the disconnection of portions of the
main Limestones to form outliers. The subsequent more
complete isolation of the severed masses, is due to the superficial
and subterranean denudation by rain and streams. And in the
case of Brent Knoll, as well as in that of Glastonbury Tor (to
some extent), the influence of the estuarine waters that once
spread over the Somersetshire levels, must have helped to com-
plete the denudation. The preservation of both Brent Knoll and
Glastonbury Tor, however, appears to be due to the basin-shaped
arrangement of the strata, and this although slight, has exercised
some influence on the agents of subaérial denudation.
Place-Names derived from Plants (in the Neig des of Bath).
By Rev. CANON ELu ACOME I
(Read March 1 16th. 1886.)
I feel that I ought to apologise to the members of the Club
for offering them a paper on such a hackneyed subject as Place
and Plant-Names; but by limiting the question to the neighbour
as
131
hood of Bath, and so giving a local colouring, I hope my short
paper may have an interest which it would not have otherwise.
The process of naming places by our early ancestors was a
very simple one. Like all uncivilized people they chose out
their settlement in the places best fitted for their mode of life,
looking out for the necessary requirements of water, wood and
shelter. Tacitus described it in his terse way (speaking of the
Germans) “Colunt discreti ac diversi, ut fons, ut campus, ut
nemus placuit—suam quisque domum spatio circumdat” *—
and having so squatted they named the place after the fons,
campus or nemus—giving it one of the many names signifying
stream, or wood, or meadow. But as the squattings increased in
number it was necessary still further to distinguish them, and so
they looked out for some distinctive natural feature which would
mark out their special property, and among these natural
features trees and plants would readily present themselves for
the purpose of place-names.¢ It is these placenames from trees
and plants which form my subject to-night—and I shall try and
show not only that the trees and plants enter largely into place-
names, but also that their use as place-names tells us something
about the plants. I begin with the forest trees—and first with
- The Oak. We are fond of calling this grand tree the British
Oak, and rightly so; there is no doubt whatever that it is a
native tree, and it forms a part of some place-names. In its
present form of Oak it is not much used in this part of the
country.. There is an Oakhill, near Bath, but I fancy that is a
modern name, and there is an Oaksey, near Cirencester, which
we, with a little stretch, can claim as a neighbour. But its
older form of ac, which we retain in acorn, is also retained in
many place-names. We have, in this neighbourhood, Iron Acton
* Germania, c. 16.
+ Names so distinguished are of course not so old as the simpler
forms—and many of them may be comparatively modern.
132
and Acton Turville. Many of you know those places, and would
at once say that neither of them now are remarkable for
abundance of Oaks, and there is no doubt, that not only in those
places but throughout England, the Oak is becoming scarce,
except where preserved in parks or such places. The reason is, as
I suppose, that though the Oak ripens a very large quantity of
fruit (in this respect being unlike the Elm which never ripens
any in England), yet both the acorn and the young tree are
searched for as food for so many animals, that you seldom find
a colony of Oak seedlings except in sheltered and protected
places.* The Oak is seldom planted, as planters now look out for
a rapid growing tree instead of one “datura nepotibus umbram”
—and when cut down it dies, in that respect also being unlike
the Elm, and Poplar, and some other trees, which when cut down
often send up large colonies of saplings from the roots, which not
only soon take the place of the parent tree, but largely extend
its bounds.
The Ash is an undoubted native—and probably less than two
hundred years ago it was the most abundant of the wild trees of
England, and was probably as abundant in the south of
England as it is still in the north. Its great abundance is shown
by the many places named after it. In the last edition of Lewis’
“ Topographical Dictionary ” there are no less than 122 places in
which the Ash forms a distinct part of the name, and there are
perhaps as many in which the word is more or less hidden, and
of these 122 a large portion are in the south of England. In our
neighbourhood we have Cold Ashton, Long Ashton, Steeple
Ashton, Rood Ashton, Ashwick, and others; and we have the
common family name of Nash. But now the Ash is not one of
our most common trees, and the reason is that it has been
pushed out of our hedgerows by the
* Tusser pointed this out long ago :—
“Tf cattle or coney may enter to crop,
Young oak is in danger of losing his top.”
133
Elm. This is not a native tree. Its very name (corrupted from
ulmus) shows its foreign origin, and the fact that it never ripens
its seed in England is another proof of the same. Yet it is now
our commonest tree. In Evelyn’s time Elm trees were not found
in Shropshire and several other counties, and rarely any beyond
Stamford.* It was probably introduced by the Romans, and
must at once have spread rapidly, for though Aubrey said that
there were only three places in England named from the Elm,
yet it would be easy to find more. In Somersetshire there are
two places called Elm, and in my own parish is a family, of long
standing, called Elms or Nelms. These are probably from the
Elm, but I think it doubtful whether some other places such as
_ Elmley, Elmworth, &c., may not have some other origin, because
I find that one of the places so named is in the Isle of Sheppy,
and I feel sure that there never could have been there such a
growth of Elms as to give a name. The whole Isle is almost
treeless. There is an Elm which is a true native, the Wych Elm,
_ but it does not spread like the other Elm, and so is a much less
common tree. I am not aware of any places named after the
Wych, unless Wychnor, in Staffordshire, and Wychwood Forest
_ may be so named ; but if there was any place so named it would
_ be difficult to distinguish it on the one hand from the common
3 Wic, which we have in Wick, Bathwick, Swanswick, &c., and on
:. the other from the Wich which marks the salt works.
There is a village under Lansdown called Beach, and it is
always assumed that it is so named from the tree. It may be so,
q but there are no Beeches there now, and the soil is not that in
___ which you would expect a natural growth of Beeches. The name
__ is certainly an old one, it occurs in the old accounts of the manor
as Le Beche, and I am inclined to look for the derivation of the
mame in another direction. The village lies under that
_ remarkable acutely-pointed headland which we call Derby Point,
* Sylva, C. iv.
134
and I think it very probable that le Beche, is another form of
le Bec, the beak, just as in other parts of the country such a
headland would be called a ness.*
There can be little doubt that the Birch gives the name to
Berkley—its old name Beorca-ley shows this. The Birch is
certainly not the tree of Berkley now, but we must recollect
that when the name was given, the rising ground on which
Berkley stands was a promontory or almost a peninsula jutting
out from the Cotteswold into a vast impenetrable morass, the
drainage of which has completely altered the vegetation, so that
there may well have been Birches there in olden times, which
have now given place to Elms and Oaks. Shakespeare describes
the trees of Berkley as Bolingbroke and Percy saw them from
Stinchcombe Hill, and as he may have often seen them from the
same “wild high hills and rough uneven ways” that Northum-
berland complained of—
“There stands the castle, by yon tuft of trees.”t
but he does not tell us what the trees were.
And near Berkley there is another place named after a tree,
and apparently now misnamed. This is Alderly, which must be
named after the Alders, as many other places are. Alderly now
is at a considerable elevation above the low ground in which we
should look for Alders,{ and so the name probably tells us some-
thing of the history of the place ; that the first settlement was
‘in the lower ground, as most early settlements were for the sake
of water, but that it afterwards migrated to the higher ground,
taking, however, with it its older name. The very same thing
must have happened with Marshfield. Such a name could never
have been given to that dry exposed hogs-back on which the
present Marshfield stands, but it must point to an older
* Compare “ High Beach,” in Epping Forest.
+ Ric: IL, A, 2. s. 3.
t Crassisque paludibus alni nascuntur—Geo. II., 110.
135
settlement in the lower ground adjoining some part of Box
Brook, afterwards deserted for the higher ground. In my own
parish is the hamlet of Oldland. The name is a puzzle, and one
of the many suggestions I have received is that it is Alder-land.
This is rendered rather probable by the fact that it is sometimes
written Aldeland But against it must be set the fact that there
are other Oldlands, all like this in the neighbourhood of an
ancient forest, and the name is said (but I cannot recollect the
authority) to denote land recovered from the forest, and not
subject to the laws of the forest manor.
The mention of Box Brook may at once take us to the Boz.
There is no doubt that the village of Box is not named from the
tree. It is one of those numberless places which are named
from the streams, and which appear in every direction under the
different forms of Axe, Exe, Ix, Ox, Ux, with all sorts of
different initials and terminals—the same word appears in the
centre of Shockerwick in the same parish.* But if Box is not
named from the tree, we may almost (though not quite) certainly
claim it for Boxwell. Many of you will know that remarkable
valley sloping from the Cotteswold, near Dursley, covered with a
wonderful growth of old Eox trees. Any who have not seen it
may be recommended to visit it, for it is within easy reach of
Bath, and it is one of the most remarkable woods I know.
The Lime or Lind may give its name to Lincombe, but though
T have made some little search for the origin of the name, I have
~ not been able to meet with any that would be decisive.
Before quite leaving the forest trees I would just mention that
the reason more places are not named from the trees is that many
of the most common trees are modern. The Plane has not been
much more than 300 years in England. The Spanish Chestnut
is older, but is a complete foreigner. The Horse Chestnut, now
so common, is an eastern tree, unknown in England 200 years
re a aig ee ie se
* On the upper part of the same stream is Okeford.
136
ago. The Fir tree is a native, and gives its name to a few places,
but not in these parts; and the Walnut, by its very name, is a
foreigner. hs
I will now go to somewhat humbler trees. I am surprised that
so few places are named from the Holly or Holm. It must once
have been most abundant, and probably formed the chief
underwood of Kingswood Forest. But I know of no placa
certainly named after it. There are plenty of Holmes, but they
all mean Islands, There is, however, a Holcombe near Bath,
which may have been Holmcombe, and if so, it must have been so
named from the Holly—a valley could not have been named from
an island. I am also surprised to find none named after the
Hazel ; for Evelyn says, “for the place they above all affect.
- . Where quarries of freestone lie beneath.” Yet, though we
have abundance of freestone, I know of no other place named
after the Hazel nearer than Haslebury, in Wiltshire, and
Hasleton, near Cheltenham.
I know of no place near here named after the Elder, but
I mention it because there is a family name, known to some of
us, which may be traced to that tree, I mean the name of
Ellacombe. The old form of Elder was Eller, or Ellern, and
Eller-combe or Ellern-combe would very easily be written
phonetically Ella-combe. Ferguson, however (a good authority
on names), says that Ell or Elli is the old Norse form for the
Alder.* SoIcan take my choice between the Alder and the Elder.
I wish we could say that the different Hayes—Combehay, &c.,
were named after the Hawthorn, but I suppose they are simply
“‘Hagas” (enclosed lands), the same word which afterwards
became “ Hedge.” It is true that the same word also forms the
first syllable of Hawthorn, but we cannot stretch it further. We
can, however, claim the Thorn as the chief component of
Thornbury.
* Ferguson’s “ North Men,” p. 125,
iii,
a
137
Thorns naturally lead us to Gorse and Furze. There is a hill
near Lansdown called Frizen Hill, now generally corrupted to
Freezing Hill, and believed to be so named as being the coldest
part of Cold Ashton, in which parish it lies. I was sorry to see
this mistake perpetuated in two publications of great authority,
the “Ordnance Survey” and the “Proceedings of the Bath
Field Club” *—for it is a mistake. Frizen, or Frysen, is merely
the old form of furzen, and within the memory of man the hill
was an open hill covered with Furze, and I have conversed with
men who helped to grub up the furze that gave the name and
enclose the land, and a lane leading from it is called Gorse Lane.
I know of no place near Bath named after fruits. In some
parts the Apple has given a name to a few places, but not here.
The nearest approach is such a name as Orchardleigh.
But we have places named from the Vine—not parishes, but
fields. I believe there is no parish named from the Vine, but
there are many places that have Vines and Vineyards. Bath is
one, and the position of the Bath Vineyards, facing due south,
with full protection behind and a warm brashy soil, must have
been the best possible for the growth of the Vine. At
Claverton there is another, and I have to thank Mr. Skrine, not
_ only for showing me the old position, in some respects almost
_ better than the Bath one, but also for giving me much interesting
history connected with it. Vineyards have now gone from Bath,
as they have from other parts of England; but I am sure that a
search into the names of fields in many parishes round Bath
_ would bring to light the former existence of many old Vineyards.
It is the same with hops. The time was when it paid the farmer
to grow his own hops, and in many parishes there are fields
called Hop Gardens (there is one at Bitton), but the cultiva-
tion ceased to pay when it was cheaper to buy hops grown on
more favourable soils.
Of more humble plants I can only name the nettle as giving
* Vol. iv., p. 290.
138
names to places. In Somersetshire we have a Nettlecombe, and
there is a Nettlebridge near Radstock, and if it is really so
named from the plant, it is an additional proof of the value
attached to the nettle by our forefathers as the chief fibre plant.
You will recollect in the churchwardens’ accounts of St. Michael’s,
read to us by Mr. Pearson, one entry pro wrticis, and the plant
is often mentioned in the old cookery books as a good vegetable.
I know of no place named after flowers, strictly so called.*
Our ancesters had to look after something more materially useful
than roses and gilly flowers, when they chose their settlements,
(it required a more advanced state of civilisation to name an
“habitation ” after a “ primrose.”) But there is one place near
Bath for which a flower derivation has been claimed; this is
Claverton, and on this name I should like to speak a little more
at length and so conclude. There are many places in England
compounded of Claver, and it is quite possible that in some of
these (as in Claverham, Clavermead), the word may mean Clover,
of which the old form is Claver, thereby preserving its connection
through the French Cleffre with the Latin Clava, a club, a connec-
tion which we now preserve by calling the trefoils on our cards
clubs. {But in Claverton we are prevented from applying this
derivation, because in the Saxon codex the name is certainly
written Clat-ford-tun,t+ and on this name it has been decided,
chiefly by Professor Earle, that Clat is the same as Clote, and that
Clote means the Water Lily, and so the whole name means the
village by the ford of the Water Lily. Professor Earle calls this
‘a pretty example.” I entirely agree with the prettiness, but
I venture to doubt its correctness, and for these reasons :—
Supposing that Clat could be converted into Clote (which is
* Flax Bourton is so named, not from the Flax plant, but from
having belonged to Flaxley Abbey—(Rutter).
+ Charter of Wulfwarn, 694, and ic geaun Wulfmere mynum
yldrad suna thoes landes cet Clatfordtune mid mete and mid mapnum
and mid eallre tilthe.
a
a ay ee
Ee eee
y .
139
doubtful), there is absolute proof that Clote never meant the
Water Lily in the days when Claverton first got its name. Clote
always meant the bur or burdock and nothing else. On this
point there is a complete consensus of all the old writers,
beginning with the early vocabularies, through the early diction-
aries, such as the Promptorium, the Catholicon and the dictionaries
of Cotgrave and Palsgrave, through all the old Herbalists of the
16th and 17th centuries, down to our own day, in which the
name has been almost lost. In all of these the Clote is always
the Lappa, the bur or burdock, and there is not the slightest hint
that the name was ever applied to the Water Lily. But about
forty years ago Mr. Barnes stated in his Poems of Rural Life,
that in Dorsetshire the Water Lily is now called the Clote. It may
be so now occasionally, and the fact is curious as an instance where
a lost name has survived and been transferred to another plant,
but it is no proof as to any such ancient use of the word, and the
loose way in which the English peasant names plants deprives the
fact of any etymological value.* But it was taken up by three
_ different persons, all of good authority—first by Cuckayne.t In
an Anglo-Saxon Leechdom is a remedy against worms—“ take
dock or clote, such as would swim;” and Cockayne, following
Barnes’ lead, thinks that ‘‘Clote that would swim,” may be the
‘Water Lily. But I have no doubt that the “Clote that would
swim” would be the Water Clote, i.e, the water-bur, ditch-bur,
or reed-bur,} especially as the medical qualities do not apply to
* “Throughout our travels in India we were struck with the undue
reliance placed on native names of plants, and information of all kinds,
and. the pertinacity with which each linguist adhered to his own
crotchet as to the application of terms to natural objects and their
pronunciation. It is a very prevalent but erroneous impression, that
savage and half-civilised people have an accurate knowledge of objects
of natural history and a uniform nomenclature for them.”—Hooker,
“Himalayan Journal,” II, 328—note.
+ Cockayne II. 123. Sparganium ramosum.
140
the reputed qualities of the Water Lily, and Protcssor Skeat
approves of this interpretation. The next was Halliwell. In his
dictionary of Archaic words, he has—‘ Clote, the yellow Water
Lily. Chaucer has Clote leaf, explained the leaf of the burdock,
although the present meaning best suits the context *—see
Gerard, p. 674, and Cloten in Walter de Bibblesworth.” Now
having been taught to “verify your references,” especially in the
case of voluminous writers, I went to these two referred to with
this result—Gerard calls the Clote the Bur, and gives no hint
that the Water Lily was so named, but he says of the Water Lily
that “it is good against the pilling away of the haire of the
head,” and that the flowers made into oil coole and refrigerate the
’ temples,” that isall Gerard says. Walter de Bibblesworth wrote a
long poem in the French of his day, the 14th century, and in it
is thist—
Sy vus trovet en toun verger
Ameroke e gletoner
Les aracez de un besagu
E choletz plantez en lour lu.
The poem has an English interlinear gloss and gletoner is
translated Cloten, so the whole is—“ If you find in your garden
Mayweed or Cloten, dig them up with your fork, and plant
marygolds in their place.” I do not think this proves anything,
except, perhaps, that the Cloten there spoken of could not have
been the Water Lily.
The third person I spoke of is Professor Earle. He is a very
great authority, so great that I could not venture to enter the
lists against him myself. All I can do is to enter them by
deputy, by sending against him another professor of equal or
* Chaucer’s words are—
“ A Clote-leaf he had under his hood
For swote, and for to keep his head from hete.”
“ Canon’s Yeoman’s Tale.”
+ Wright, p. 162.
141
greater weight. Professor Skeat, in his notes on Chaucer, refers
to this theory of the Clote being the Water Lily, but soon dis-
misses it as of no value. He refers, however, to Gerard, and on
my writing to him on the subject, he wrote as follows :—
“Tt is not J who refer to Gerard. I only say that Halliwell refers
to Gerard ; and he gives the reference which I copy. I did not look it
up, because I did not believe in it. As to Claverton, it is simply a
ract that either that place, or some other place of like name, is spelt
Clatfordtin in a charter published by Kemble in his ‘Codex
Diplomaticus.’ There is also an A.S. Clatford as a place-name, and
still two parishes named Ciarrorp. But it cannot well mean Clote-
ford, for the reason that if the A.S. word was Cldt, it would now be
Clote ; but it is not ; therefore the A.S. word was Clat (with short a),
_ and it did not mean Clote, but something else. Had it meant ‘Clote,’
_ your place would have been Cléverton with long o.”
Here I might well stop, but my inquiry into this one name has
led me into so many pleasant paths that I should like to conclude
the argument from my own researches. I now feel certain that
Clat or Clote, in Claverton, never had any connection with the
Water Lily for this reason, that the Water Lily did not grow
there when the name was given. I feel certain that there were
no wild Water Lilies, and very few, if any, cultivated ones in the
South of England for many centuries after that date. There is a
botanical reason for this. The plant is a northern one, and
perhaps indigenous in Scotland, but it is of such a rapid growth,
that if it had been long introduced, the still waters of our
_ southern rivers would have been filled with it by this time. I
can recollect the large pond at Warmley when I could pull or sail
on it anywhere. A Water Lily has since then been introduced,
and now the pond is completely choked with them. And that it
was not known as a wild plant is proved by the early writers.
_ The writers of the early Vocabularies found Nympheza in Pliny,
and so tried to translate it, but could make nothing of it; and
the early Herbalists of the 16th and 17th centuries all name it, but
they all copy one from another, and none of them name any wild
L
142
habitat for it. If Turner or Gerard had ever found it, they
would have said so—they are always fond of giving localities ;
Gerard so much so, that he was convicted on one occasion of
planting a rare plant in one locality and then discovering it,
and publishing the locality. In Ray’s time it had reached
Cambridgeshire, but the first notice that I can find of it south of
the Trent is in Blackstone’s “Specimen Botanicum,” 1746. He
names a few places round London, and among them Windsor
Lake. This looks as if the plant might have been introduced
from Scotland to please the Scottish King, James I., or he might
have introduced it himself, for he was fond of introducing rarities.
The whole of what is now Buckingham Palace and Gardens was
planted by him with mulberries to encourage the silk trade.
But to my mind there is a still stronger proof that the
plant was unknown in England, because with the exception of
the Herbalists, the plant is entirely absent from English
literature, either under its name of Water Lily or its other name
of Water Rose. When we consider what a grand plant the
Water Lily is, it seems impossible that it could have escaped the
notice of all our writers, who yet notice so many of our wild
plants. It is not named by Chaucer, Gower, or Spenser, nor by
Shakespeare (who surely must have named it in the death of
Ophelia had he ever seen it); nor by Drayton, who wrote a long
account of rivers; nor by Vaughan, the Silurist, who had a
special eye for all things that grew in or by rivers; nor by
Herbert, Marvell, or Herrick. Not trusting my own research
I applied to Dr. Murray, who is always most helpful, and he at
once sent me all the slips that they had been able to collect,
expressing at the same time his surprise at finding the plant
unnamed except by the Herbalists.* It is named once in a
* There is a passage in Walton’s Angler which apparently proves
the contrary :—‘‘ You are to cleanse your pond, if you intend either
profit or pleasure, once every three or four years. . . . to kill the
he ee
’
os
Nr
143
Scotch Book, “The Complaynt of Scotland,” 1549, but the
plant is Scotch—the first English writer that names it is Byron,
in 1818.* From all this I conclude that Clote does not mean
_ Water Lily, and that Claverton does not owe its name to that
grand flower. If I were asked what the name does mean, I
should say that I do not know—but in lack of a better derivation
‘I should think that we might adopt the well-known rule of
rejecting or paying no attention to initials (consonants), in
; names, and should say that Ulatfordtun is simply At. ford tun,
the farm at the ford, which exactly describes the place. But
this is a mere guess to be taken quantum valeat.
I have only in conclusion to say-that I offer this paper to the
Club not as an exhaustive account of the names of places in the
neighbourhood, but as a slight sketch which others can fill in at
their leisure.+
water weeds, as water lillies, candocks, reate, and bull-rushes that
breed there.”—c. xx. But this chapter was not in the first edition,
4 and is confessedly not original, but a compiled translation from
. _Dubravius and Lebault. The words of Lebault are:—“On si tu
veux avoir proffit de son estang ou de la fosse, tu dois prendre soing
s & la curer de trois en trois ans oster les roseaux, ioncs, et larges ftelles
que 1’6 appelle nymphee de fleurs d’eau,” &c, If the Water Lily was
F as abundant in the streams round London in Isaac Walton’s time as
_ itis now, it seems impossible that he could have overlooked them, both
3 as a keen observer of natural objects and as an angler.
Since writing this I have found that Cowper’s Poem on the Dog
and the Water Lily was published in 1799.
. + I have found in the “Synonoma Bartholomei,” 1387, a strong
confirmation of my opinion that the old writers did not confuse Clote
and Water Lily, he says :—Ungula caballina est duplex, videlicet
_ terrestris que confert ptisicis et ethicis, et aquatica, cnjus flos dicitur
ke nenufar, Ungula caballina campestris, i. clote.”
144
Address to the Members of the Bath Field Club, in reference to the
death of C. E. Broeme, Esq., F.L.S. By Rev. L. BLoMEFIELD,
M.A., F.LS., F.G.S., &c., President.
(Read December 8th, 1886.)
GENTLEMEN,
Before proceeding to any other subject, I am
anxious to address you this afternoon in reference to the great
loss our Club has sustained by the death of Mr. Broome, one of
our original Members. I think some record of so earnest and
hard working a naturalist should appear in our “ Proceedings.”
With a view to this, I have briefly put together the chief
particulars of his life, wishing afterwards to speak of him, as a
friend personally known to myself over a long term of years, and
as a Member of this Club. :
Christopher Edmund Broome was born at Berkhamstead in
1812. His father, Christopher Broome, lived at White Hill,
Berkhamstead, and was a lawyer by profession, and is said to
have been “a strictly just and most excellent kind-hearted man.”
His mother was a Miss Seller, a niece of Lady Knightly, of
Fawesley.
At the age of nine Broome went to a school at Dr. Jamieson’s,
at Kensington. This school, a few months after, being moved to
Heston, near Hounslow, Broome went with it, and remained
there till he was eighteen, in 1830.
It was in this year that his father died ; two years after which
he and his mother went to live at Chelsea, and it was from thence
he went to be the pupil of a clergyman who held the curacy of
Swaffham Prior, in Cambridgeshire, with whom he remained till
he went up to the University. He was entered at Trinity Hall,
Cambridge, October 23rd, 1832, the same college to which his
tutor belonged, and took his degree in January, 1836. In April
of that same year, he married Charlotte Horman, fourth daughter
of the Rey. John Bush, incumbent of Chelsea Old Church.
145
A few months after his marriage he went to liye at Rudloe
Cottage, Rudloe Firs, near Box, a place probably known to some of
~ the Members of this Club, though the house is now pulled down.
Thence, in 1844, he moved, for nine months, to Wraxall Lodge,
near Bristol, and thence again for a few years to Clifton, where
he became very intimate with Thwaites, a botanist of high
reputation and well known in the botanical world, and who was
afterwards Curator of the Botanical Gardens in Ceylon. I
suspect it was at this time that he began to give especial attention
to the Fungi, as he is said ‘to have made, with Thwaites, many
expeditions in the neighbourhood in search of truffles.” It was
in November, 1848, that Broome took up his abode at Elmhurst,
_ near Bath, where he remained for the rest of his life.
I would now speak of my own acquaintance with Broome, who
_ was the oldest friend I had—relatives apart. It arose out of the
circumstance mentioned above, of his coming to be the pupil of a
clergyman who was curate in the next parish to my own
vicarage of Swaffham Bulbeck, in Cambridgeshire. I was
4 intimate with the tutor, and I soon became intimate with the
_ pupil, especially when I found him taking an interest in Natural
History, for which he seemed to have a latent taste, only waiting
to be evoked according as circumstances were more or less
favourable. And circumstances certainly did favour him ; for the
tutor himself, under whom he was placed, was fond of collecting
_ fossils and rare plants for his garden, independent of my own
_ Natural History pursuits, which I had taken up many years
before the pupil came.
____ Nor could any young naturalist have been placed in a richer or
more attractive neighbourhood, in a Natural History point of
view, than that in which Broome found himself. Newmarket
Heath, with its wide expanse of unenclosed land, crossed by the
miles, and only disturbed in places ; this Ditch terminating at one
, extremity in the Woodlands, at the other in the Fens, the latter
146
reaching far and wide, even to Ely and beyond, as well as in
other directions. This whole district not merely abounded in
birds, insects, shells and plants, but in certain localities were to be
found many rare species, of plants especially, seldom met with in
other parts of England. I know nothing in Somerset, within
easy reach from Bath, approaching to the Cambridgeshire Fens in
this respect, except it be Shapwick Moor, as it was formerly,
when Broome and myself twice visited it, and had a most
successful day’s botanising each time, but not as now, when little
of the Moor remains, its chief rarities having in great measure
disappeared with it.
Such was the rich neighbourhood in which Broome found him- .
self situated, and of which he soon availed himself. He set about
collecting insects, plants, and its other natural productions, and
we frequently took walks together. In 1832, as stated above, he
entered the University, where I often met him for a day’s
excursion, or visited him in his college rooms, and where also he
became acquainted with Henslow, Professor of Botany at that
time, and whose botanical excursions, with his class, I think he
often joined. Darwin had taken his degree the January previous
to Broome’s entering the University in October, 1832, and I am
not sure that the latter ever made the acquaintance of that distin-
guished naturalist, who, soon after graduating, left Cambridge to
accompany Captain Fitzroy on the far-famed voyage of the
Beagle.
After Broome left the University we still kept up our
acquaintance, but we only met at intervals in London or else-
where. His frequent change of residence caused an interruption
of all companionship in Natural History excursions, though it left
a place for occasional correspondence. It was not till after he
had fixed his residence at Elmhurst, Batheaston, and myself had
-moved from Cambridgeshire and come to Bath, that we were able
to associate together as formerly for field explorations.
And here I am led to speak of him in connection with the.
|
—
ea
4
“4
147
origin of this Club, and the circumstances that led to it, which
may not be known to all the Members, and which it may be of
interest to put on record. Broome was one of the original
Members of the Bath Field Club, no other remaining now except
Mr. Scarth (Vice-President) and myself. But Broome was more
than an original Member. I should not be far from the truth in
saying—that he was a joint founder of it with myself. True I
originated the idea, but the idea would never have been carried
out but for Broome. It would never have received shape, but
for the circumstance of the weekly walks, which he and I agreed
to take for the investigation of the Natural History of Bath. Of
these walks I proceed to speak.
_ When I first came to this neighbourhood I resided for a time
at Southstoke, near Combe-Down. Broome, having heard that I
was there, took an early opportunity of walking across the Down
and coming to see me, and we were both glad to renew an
acquaintance which had been interrupted for some years previous.
We then arranged that the most agreeable way of keeping up the
acquaintance, having especial regard to the pursuits we had in
common, would be to take weekly walks together in order to
explore the Natural History of the Bath district. Thursday was
the day fixéd on, and the walks, weather permitting, were taken
recularly. It was not long, however, before we were joined by
friends ; two others especially, both now deceased, joined us
regularly— Captain Hewitt and Mr. Mackarness, the latter Father
; 4 of the present Bishop of Oxford, who was then living at Bathford,
‘not very far from Elmhurst. These gentlemen entered warmly
into our project, and it was agreed that we should meet at each
other’s house in turn as a starting point, regard of course being
had to the direction in which we were going and the spot we
wished to visit.
Others also joined in the walks from time to time, until I
thought things were ready for a move towards setting up a club
a similar to the Berwickshire, Tyneside and Cotteswold Field
148
Clubs, the only ones, I believe, then existing, though now
abounding throughout the country. Accordingly I invited all
who were favourable to the scheme to meet me on an appointed
day at the Literary Institution, where, in the room now called
the Lockey Room, after reading over for approval a few rules
which I had drawn up, and which I thought would serve in the
first instance, on the 18th of February, 1855, the “ Bath Natural
History and Antiquarian Field Club” took its beginning.
But to return to him of whom I desire to speak most on this
occasion : Broome was naturally quiet and reserved, and did not
show to advantage in public gatherings. But as a companion in
a walk—a botanising excursion especially—none could excel him,
none make himself more friendly and agreeable.
Broome had an uncommon sharp eye in looking after a plant
known to grow in a particular locality, and which we were in
search of. He seemed to have a sort of instinctive determination
not to leave the place till one of us had found it, unless compelled
by circumstances to do so, and the discovery of the first specimen
rested much oftener with him than with myself. 1 remember
only two instances in which neither of us had any success, and
when we were forced to return home without the prize. In one
of the cases we were led to think afterwards it was a mistake, and
that the plant did not grow there at all; in the other, that the
plant had become extinct in that particular locality.
He was also clever in finding his way about in strange places.
When at a loss about the road or in doubt as to where a par-
ticular path led, I always left the decision to him, feeling sure we
should come right in the end.
It was mostly during our quiet walks alone that we carried on
our botanical researches. The Club’s regular excursions, though
very pleasant in themselves, afford little opportunity for any
steady work in Natural History. I remember once, our late much
esteemed Member, Charles Moore, on its being remarked that he
seldom walked with the Club, gave as a reason that there was
—_
ey hy
s
iS ae Ca ee
149
‘no liberty of action.” Of course when a large party is wending
its way, on foot or by rail, to some pre-arranged place or object of
attraction, gentlemen can hardly be expected to make any long
stand, whilst one stops to search for fossils in a particular stratum
unexpectedly met with—another to look for some particular
plant. Stationary work of this kind is best done at other times.
Accordingly it was apart from the Club, on different occasions,
that Broome and myself collected by degrees all the rarer plants
growing in the Bath district, besides discovering several new ones
not mentioned in Babington’s “ Flora Bathoniensis.”* Fine
specimens of all of them are preserved in the Herbarium, in the
Jenyns Library, at the Bath Literary Institution.
But Broome was not merely a local collector, he was a general
botanist ; he had been in Italy and some other parts of the Con-
tinent, where he had made himself acquainted with foreign plants,
many specimens of which are preserved in his Herbarium. The
particular department. of botany, however, in which he worked
hardest, and to which he had given his chief attention for a long
term of years before his death, was that of Mycology, perhaps the
most difficult class in the Cryptogamia, and one which very few
botanists attempt to take up asa special pursuit. The “ Pro-
ceedings” of our Club are enriched by several of his papers
relating to the Fungi of the Bath district, and a collection of the
same was placed by him many years back in the Duncan Local
Museum.
In the study of this obscure and difficult tribe of plants, he was.
often associated with the Rev. M. J. Berkeley, celebrated for his
works and papers on Mosses and Fungi, and who, as a Crypte-
gamist, stands as high as any name in this country or abroad.
Berkeley, until his health failed, was a visitor at Elmhurst most
* In the supplement to the “Flora Bathoniensis,” published in
1839, Babington mentions Broome as one of the parties from whom he
_. had derived much assistance in his work.
150
years, where I often met him. I had known him ever since he
was at Cambridge, and even in his undergraduate days he began
to take up the study of Mycology with ardour and success.
I have so slight an acquaintance: myself with that branch of
botany, that I am glad to be able to give the testimony of others
as to what Broome did in this way, and the excellence of his
work.
Broome has bequeathed his rich Collection of Fungi to the
British Museum, and I am permitted to make an extract from a
letter written by Mr. George Murray, an assistant curator in the
botanical department of the Museum, to one of our Members, in
which he speaks of Mr. Broome as follows :—“ The great mass
of his work is contained in the long series of ‘ Notices of British
Fungi,’ contributed by him and the Rev. M. J. Berkeley, to the
Annals and Magazine of Natural History. The whole of it, from the
earliest to the latest, is characterised by remarkable accuracy, the
result of faithful, conscientious research, often involving far more
labour than appéars. A mere dry reference may contain the
result of serious scientific labour, and in such matters as that,
Mr. Broome took as great pains to be accurate beyond doubt as
in far more showy researches so to speak. His modesty appeared
in his work. No one but the Rev. Mr. Berkeley can know the
full extent of it, but all students of the subject recognise his
authority and trust it implicitly as of the highest order.
It is impossible to separate the two names, Berkeley and
Broome, they are familiar to all workers in botany, as the very
highest authority on British Mycology, and in the first rank
of workers in this field throughout the world.”
Thus far the letter. Besides working in the field and in his
study, Broome did hard work in yet another way. He was a
successful cultivator of plants, and did much in the garden with
his own hands. His garden was always attractive—to botanists
especially—from its containing many choice or rare plants not
often met with in other gardens. Perhaps the most attractive -
Ag
-
=
a
:
151
part of his grounds was the drive up to his house from the
Bannerdown Road—the borders on each side of the carriage way
displaying an assortment of shrubby and tall herbaceous plants,
many seldom seen in gardens, and presenting in summer, when
in full flower and foliage, a most ornamental drive, not very long,
but such as I never saw elsewhere in this part of the country. I
remember when it was part of a ploughed field. The wonderful
transformation since effected was done under Broome’s immediate
direction, and much of it, I believe, was the work of his own
hands.
In truth, Broome was a hard worker by habit and by rule.
In summer he rose at six, occasionally at five, and worked in his
garden till breakfast, after which he worked in his study, with his
microscope at hand ready for immediate use, as wanted, till
luncheon. ‘Then in the afternoon, he was out for a botanising
walk, if not called into Bath or elsewhere on some special
business; and not unfrequently in summer, the whole day,
between breakfast and a late dinner, was given up to some
excursion or other, when he would walk long distances, taking
little refreshment. He seemed to me, indeed, to eat and drink
very sparingly at all times, and hardly what I should consider
sufficient to meet the daily expenditure of strength and energy
required for the work he did. For, lastly, it was in the evening,
after dinner, that he took to his reading, especially botanical and
other scientific periodicals, by which he kept himself abreast with
the researches and discoveries of others in his own particular
department. Engaged with his books in this way, he would
often sit up, I have been told, till after midnight, sometimes till
after the short hours had commenced.
No wonder that nature resented such an incessant strain upon
her energies. Interruption of health, in some form or other, had
more than once warned him to desist and spare himself a little,
the warning being backed by the solicitation of friends, but it
was to no purpose. In one case, when confined to the couch by
152
an affection of the knee joint, I went up to visit him in his room,
where his table, spread with the usual books and papers and the
microscope at hand, was drawn closely up, though he could do
but little under the circumstances. I reasoned with him as to
the necessity of his breaking off for a while from such occupations,
and giving rest both to his mind and body. But he only said in
reply, “If I am to lie by and do nothing, I may as well die
at once.”
And no doubt it was incessant work—over fatigue of both
mind and body—that brought on the sudden attack that proved
fatal. He had property in Essex, which he visited regularly at
stated times every year, his head quarters in London being
Wood’s Hotel, Furnival’s Inn. He was there the second week of
last month. On the evening of Friday, November 12th, after a
fatiguing day in Essex, in wet weather, he returned to his Hotel
as usual. Soon after he had gone up to his room, he had
a paralytic seizure, and became insensible. In this state he
remained, his consciousness never returning, till the evening
of the following Monday, the 15th, when at 11 p.m. he passed
away. A sudden death to all outward appearance, but not
sudden to himself—he was prepared for it. He had Jatterly
hinted to one or two of his friends that he felt he should not
be here long.
I conclude, gentlemen, with a few words suitable to the
occasion, and suitable to ourselves.
The life and death alike of our much esteemed Member reads
a lesson to us all—a short lesson, but a most important one—
“ Work to the full extent of your powers, but not to the injury of
your health.” Few Members of our Club, I imagine, need to be
cautioned against working too hard for their health’s sake, but
there may be some to whom the first half of this advice might be
given with advantage. When I look over the volumes of our
“ Proceedings,” and compare the few names which stand as
authors of the chief-papers in them, with the hundred names or
153
more in the list of Members, I say to myself, where are the
many ? What are they doing to promote the objects of this Club 9
We can ill spare a man so active at home and abroad as our late
Member. Will no one come forward and take his place? What
may not a man do for science, if he be only active and willing, in
these days of evolution, when the sciences have been so rolled
together that he who works for one, in some degree works for all.
But I have one more thing to say respecting Broome. 1 stated
above that he had bequeathed his collection of Fungi to the
British Museum. I have now to add that he has bequeathed all
~ his other collections of plants, along with the main part of his
botanical library, consisting of about 340 volumes, to the Bath
Royal Literary and Scientific Institution, When we consider
this last bequest, in connection with the Jenyns Library of
Natural History, and the Herbarium of British plants, already in
the Institution, I conceive that hardly any place in England, out-
side London and the Universities, Kew of course excepted, will
henceforth be more favourably circumstanced than Bath for the
study of botany. May there be at least one, if not more, of the
Members of our Club desirous of availing himself of these
resources, which promise so much assistance and success to those
who take up this subject in good earnest. -
But whether botanists or not, whatever be our work in the
study or the field, may we all copy often the indomitable zeal
and industry of our deceased friend. Let us take for our motto
that which was the guiding star of his whole life—‘ Work while
it is day.”
Traces of the Saxon period in Bath and the Neighbourhood. By
Rey. Prebendary EARLE, Professor of Anglo-Saxon.
(Read December Sth, 1886.)
The Rev. Prebendary EAR.z said, before I begin my subject I
think I must say a word or two, in echo of the very kind and
interesting remarks which our President has made upon Mr.
154
Broome. A great deal of what he said I was able to follow in
my mind, and by recalling my own experience to go over the
same ground. Many a time have I enjoyed a walk with Mr.
Broome himself, or with some member of his family, up that
drive of which Mr. Blomefield has spoken, and I remember
perfectly well the circumstances of its making—how it contributed
to the pleasure which Mr. Broome had in it, that it was a son
of his who had been to the Colonies and had come home who
engineered it and planned it for him. I have often gone round
Mr. Broome’s garden with him; I have been with him to
Bitton, and spent a day or half a day among Mr. Ellacombe’s
remarkable collection of trees and plants; for Mr. Ellacombe
is very fond of bringing home and domesticating rare and
wild English plants which are to be found in his garden, as well
as many exotics. It is fresh in my memory that I went up more
than once to Mr. Broome’s room when he was confined to his
sofa, and as Mr. Blomefield has already told you, he was always
at his table with his work before him. I remember that summer
extremely well. He had been with his son to the Alps on a walking
tour, and keeping pace with the activity of the young man, had
done too much, and so he was for some months confined to his
house by a stiffening in the knee. I am sure that I shall be ex+
pressing the sentiments of many when I say that Mr. Blomefield,
in the way in which he has brought his friend and our friend before
our minds in this memoir, has touched a very deep chord in
our feelings and carried us back to many very pleasant
reminiscences, though now tinged with sorrow and _ regret.
And we cannot but rejoice that our President, among his many
high acquirements and rich accomplishments, adds to it that
power of appreciating the value of his friends, which is one of
the most amiable and admirable qualities, and is thereby able to
do justice to his friend, though Mr. Broome is not the only one of
whom ke could speak. He has indeed already spoken of some of
his acquaintances. I have had the pleasure of reading a
M4 - «
ee ee ee TL -* =
~ "2
Se
155
biography by him upon Yarrell, the Ornithologist ; and I think
there is another great name in natural history, one whom he has
this afternoon mentioned, of whom he could give a sketch,
as well as, or perhaps better than any other man living, I mean
the great Naturalist Darwin. All the best and chiefest traces
that I possess of the life and character of Darwin I owe to
conversation with my valued friend, Mr. Blomefield. It is among
the treasures of my memory that I have had the pleasure of Mr,
Blomefield’s acquaintance, When I first came here in the year
1857, Mr. Blomefield was residing at Swainswick, and from that
time to this I have always been able to feel that I had in hima
friend. But if I were to go on as far as my feelings would let
me upon this subject I should never come to the “ traces of the
Saxon period,” and I hope I have not said more than is right on
an occasion which might be allowed, I suppose, to stir up one’s
feelings a little in the pilgrimage of this life.
The subject of the ‘traces of the Saxon period in Bath
and the neighbouring,” I fear, may seem a very distant subject.
One might say it is eight hundred years ago, speaking roundly ;
yes, it is more than eight hundred years ago since the Saxon period
was brought, or supposed to have been brought to a close by the
Conquest ; and then from the time of its close till it began, we
must reckon back a period of 500 years. From the middle of the
sixth to the middle of the eleventh century is what we call the
Saxon period. It seems a long time ago, but it really is so
only in the arithmetical way of calculation in the sound of
figures; it is not long ago for anyone who has cultivated a
consciousness of his relationship to the national life. We have
had, as I may say, but three stages in our life. We have had the
first Colonists’ stage, when we laid out the country and occupied
the fields, and built farm houses and fenced lands, and instituted
agriculture, and had one more struggle in repelling the Danes,
when to a very great extent we received them as additional
Colonists to our country.
156
So the first 600 years is but a chapter in our life passed.
It is an agricultural chapter, and if you want to go back into the
Saxon period you have only to walk out into the lanes and by-ways
of our remote villages and there you may find all you want for
essentials in the Saxon period. Since that time we have had
two great periods ; we have had the period in which we formed
our municipalities, and then we have had since that the period
of our great manufactures and our Colonies, and these second
and third periods have tended to shut out from our view that
great and important Saxon period which is after all the solid
basis of our national history. Now Bath is a spot in which one
might be naturally led to ask whether there are any remains of
this period. There are many reasons why one should look to
Bath as one of a very small number of spots in which you
might expect to find traces of the Saxon period, other places
which might rank with it, but hardly above it, would be such as
Canterbury, or York, or Winchester for various historical reasons.
I feel that there are very few places that a student acquainted
with Saxon periods and literature, on coming to England from a
foreign country to try to see what he could see in England, would
be more likely to visit with curiosity than the neighbourhood of
Bath. For consider, it was first of all a Roman city, and so
was one of those places which was attacked by the Saxons very
early. It was destroyed by the Saxons in the year 577 after the
battle of Dyrham, as recorded in the Chronicle; but it was
not occupied by the Saxons, they were not fond of city life.
They destroyed cities because cities contained populations that
were hostile to them and they could not live peaceably by them.
This city of Bath must have laid for 100 to 200 years in a
state of desolation—a vast city of stones and buildings, but
without inhabitants—and the proofs of this are very various, and
have been remarked upon independently by different observers
and discoverers. That period was even the subject of a record
in the shape of an ancient poem preserved in the Exeter book—
——
oe
oe ee ee
157
the “Codex Exoniensis” —a volume of the Saxon period which is
the one remaining volume of Bishop Leofric’s library that still lies
in his cathedral. In that volume there is a poem which describes
a city in ruins—splendid ruins—with a pool of water of natural
heat in the centre, and which appears to me to indicate no place
in this country except Bath, and in that opinion I have received
the confirmation of very many important authorities. So far for
literature. I am only touching on the literature as indicating
what means we have to expect that the neighbourhood of Bath
should be one that might probably preserve objects of the Saxon
period. We have a considerable number of documents relating
to Bath, documents of various dates during the Saxon period,
and these documents tell of two things —the transfer of land
and the manumission of slaves. In these documents we have
mention of Widcombe, Lyncombe, Northstoke, Priston, Farm-
borough, Corston, Weston, Hampton and Freshford. In short,
an American or New Zealander, or any visitor who had studied
our early literature, might very well come and ask what there
was to be seen in the neighbourhood of Bath; what v:sible and
tangible objects remained in existence in the neighbourhood of
Bath. Let me first mention one or two things that have been
here, but have been removed. There are lying in Cambridge in
the Parker library, that famous library which Archbishop
Matthew Parker bequeathed to his college, Benet College, now
called Corpus Christi, two important books that were formerly
the property of the Abbey of Bath ; one is a volume of
Gospels, in the fly leaves of which were written the manu-
missions of slaves ; and there is also a volume entirely de-
yoted to documents relating to landed property, mostly of
the property of the Monastery of Bath, but also partly of the
Monastery of Abingdon, which I can only account for by sup-
posing that this book was transcribed after the Conquest. I
think that after the Conquest, when religious houses were
very anxious to multiply the proofs of their property, they
M
158
interchanged with one another the compliment of writing
entries of documents in each other’s book, by way of multiplying
the security of the copy. At any rate there are a number of
entries in the Bath book relating to Abingdon, and I cannot
conceive any other explanation of them. Among other things
that may be mentioned as being found in distant places
are the coins. There were a great number of coins struck in
Bath from the time of Athelstan in 925, up to the period of
Edward the Confessor. I think there must have been more than
one monetarius who was licensed to strike coins in Bath.
At any rate there are a great number of coins in existence of
the Saxon period that have the name of Bath on them, but I
am sorry to say there is not one preserved in the place itself. I
asked Mr. Russell, at the Royal Institution, the question this
morning, and he said they had none. The place where I made
the acquaintance of these coins was at Stockholm.
I had the pleasure many years ago of looking over the great
collection of Saxon coins in the museum at Stockholm, and
the memory of it was revived in a recent conversation with
Mr. Arthur Evans, who told me that his father had just
come back from Stockholm, where he had bought from the
Trustees of the Museum there a large number of coins. Mr.
Evans, who is well-known as an authority in numismatics,
especially British and Saxon, had bought a very large number
of Saxon coins, which were superfluous duplicates in the
Stockholm collection. While Saxon coins do exist in- the
world in very large numbers, and while Bath has its place
among the limited number of cities in which they were struck,
it is remarkable that they are all gone from their native place.
There: is not one to be found in our cases here in the Bath
Museum.
I have spoken of the Monastery. We all know that the
present Abbey Church represents it. Of the Saxon building
we have nothing left, but there are some solid traces of the
KO? wrce —e
adh
Pa eee ee ee ee he
2, . x ee
159
Norman edifice which was built by John de Villula upon the
site previously occupied by the Saxon building ; consider-
able remains will be found by those who know where to look
for them. Of the Saxon building there are none, but in this
book at Cambridge which I have mentioned there is informa-
tion about the Saxon Church. It is incidentally mentioned that
the church is of unusually beautiful architecture—mira fabrica—a
wonderful fabric, and such it might naturally be. It was built
in a place in which stone was in abundance without quarrying.
There were all the materials of the Roman city to build a church
with, so that at a time when stone churches were extremely rare
in our country there was a beautiful stone church at the Abbey
of Bath. Of that church we have no part of the architecture
remaining, but I think I can point to certain fragments which
are connected with its history. There are in the Institution two
fragments of two different Saxon crosses ; the cross was an object
‘which the Saxons particularly decorated and ornamented, in fact
we are rather beginning in some of our tomb-stone crosses
to copy the decoration of the Saxon crosses. There are two
pieces of the heads of two different Saxon crosses in the
Institution here, and they both have been figured by Mr.
Poole in his “ Old Crosses of Somerset.” Then there is among
the excavations from the Roman baths a piece of the upper part of
the shaft of a Saxon cress, ornamented with a triquetrous inter-
lacing pattern which is quite unmistakable. It belongs to no
other period at all unless it may possibly be a specimen of the
interlacing work of British crosses. But I believe it is
Saxon. There is also the basement of a Saxon pillar, probably
one of the pillars of the church which was part of this handsome
building I have referred to. These are the chief ecclesiastical
remains that I have been able to see in Bath, but at Bitton (Mr.
Ellacombe says, I have not myself verified it) there is over
the chancel arch—which is Norman—higher up in the wall
and surrounding the Norman arch, visible traces of a previous
160
Saxon chancel arch; at Limpley Stoke there is a very remark-
able Saxon doorway on the south side of the church. It is
a sight that visitors to the church may easily miss, as they may
visit the church and go away and not see it. If they do not
walk all round they will not see it because all the architectural
featuring of Limpley Stoke Church, contrary to the usual plan
of a church, is on the north side. It is by the door on the north
side that the church is entered, and almost all the windows are
on the north side, so that the south side appears to be a blank
wall. But if you take the trouble to walk round the church,
you will see a most perfect bit of Saxon architecture; an old
doorway in its place perfectly complete. There are the jambs
of the door and the arch of rude timber, like stone-work, but
in perfect condition. Mr. Forss who showed it to us (I was
led thither by my friend Mr. Skrine) was himself under the
impression that it was a door that was brought from the Manor
House close by, indeed in the next field. That this door had an
intimate relation with the Manor House, is manifest, in so far
as it was through this doorway that the people of the Manor
House would pass in and out. In this sense it was the door of
the Manor House, but that it had a more material connection
with that house is not at all likely. It is not like anything ina
private house, and there it is where it should be, directly
opposite the north door, It was usual for a church of that
period to consist of one long room, one long parallelogram
crossed by two doors opposite to each other. Limpley Stoke
Church has both these doors in evidence, but the south door
is walled up, and the north door isin use. It is worth anyone’s
while to walk there to see it. But when we speak of church
architecture, there is in this neighbourhood an example, such as
exists nowhere else; a unique example of a Saxon Church that
has been discovered in our own day, and which was brought out
and cleared from the incumbrances of the adjoining buildings
mainly by the activity of Mr. Jones, who was then the vicar. He
—— a
WN Abc iste
e
r
161
laboured at it day after day, till it became to him an object of
affection ; he worked hard at getting the money to pay for the
expense of clearing it, and it has added a very great ornament
to this whole district. To persons that have a taste for historical
knowledge it is an object that is worth going a very long distanee
to see. When we compare it with our historical records—the
only historical records which we can bring to bear upon it—
we are led to think not only that it belongs to the Saxon period
—that is quite certain, a look at it for anyone with a practised
eye is enough for that—but when we go into the records we
find it probable that it belongs not only to the Saxon period, but
hundreds of years back in the Saxon period. It is quite probable
that it is the very little church—the “ Ecclesiola”—stated by
William of Malmesbury, to have been built by Bishop Aldhelm
at Bradford. Now Bishop Aldhelm died in the year 709; —
and while on the one hand the pushing it back to so high an
antiquity seems to render it more difficult to accept, on the other
hand there are evidences of very high probability. In the first two
centuries of our English Christianity there was a nobility about their
architecture it did not afterwards exceed. We do not realise to
how great an extent the fortunes and the improvements, and
even the minds of the people were crippled in the years of the
Danish visitations. The people were impoverished. They were
driven hack into ruined barbarism, so that to say that a Saxon
church was built in the year 700 is not really harder to believe
than to say it was built in the year 900, or even so hard. It is’
certainly harder to strain our convictions to the point of believing
that it should have existed so long, but that it was built in 700 is in
itself more likely than that it was built in 900 or 950. Now for the
chancel archof that church, there is in the wall above, high up, what
I suppose is the most perfect example of sculpture of the Saxon:
period existing. The Saxons never, at their best, arrived at a
perfection of sculpture to be compared to that of the
Greeks ; that we understand perfectly well. It is something
162
that appeals not to our ethestic feelings and imaginations for its
heauty of outline, but something that appeals to us as English-
men, something which we may look at with the same indulgence
and tenderness of feeling as we look at the drawings of our own
children, and in that point of view Saxon sculpture is intensely
interesting. There is found up in that wall what I think may
be taken as a specimen of the palmy period, an example of early
Saxon sculpture, because in a later period they had lost something
of their artistic ability. By the way, let me pause a moment to illus-
trate what I mean about thedifference in thelater period. It isinthe
early period that we have the best worksof art,notinthelate period.
By the early periol I mean the period before the ninth century,
a period in which our national existence was imperilled, out of
which we were drawn by the heroism of Alfred, and this was the
achievement which makes him a great national hero. Well, before
that time, art had gained a higher perfection than it ever gained
afterwards up to the time of the Conquest. One little example.
Of the whole series of Anglo-Saxon coins during that 500 years
_the most beautiful as works of art are the denarii of King Offa
King Offa died in the year 793, and the most perfect works of ait
in the Saxon period are his coins. That is an illustration of
what I mean. The early period is the period of the best Saxon
art, and the later period is a period of recovery from an enormous
shock.
The sculpture to which I have referred represents two
angels, which we may suppose are in a flying or soaring
position, almost horizontal in their figures, and evidently looking
towards some object, inasmuch as they are looking, as it were, to
one another; but in all probability there was the head of the
cross between them, and perhaps the head of the Lord himself,
and these angels must have been, as it were, worshiping,
waiting, tending or serving the crucified one. That is pro-
bably the meaning of the composition of which they are the relics, .
There is another piece of Saxon sculpture of which, however, I am
es LP eS
Rg KW ie
163
not able to say anything as to date (I should rather be disposed
to attribute it to a later period) to be seen at Bristol in
the Chapter House, dug up when some repairs were being
‘done in the Cathedral there. It is really the slab of a stone
coffin, and upon it there is represented the figure of a man,
apparently Christ (as far as I can recollect, 1 have not seen it
for a great number of years), delivering a soul, represented
by a little figure, out of the mouth of the Dragon. This stone is
now in the vestry within the Chapter. You go through the
Chapter House to a door at one corner of the room and into
the vestry, and there this stone is walled up and presents
itself as a picture over the fire-place. Another kind of
Saxon remains which exist in this country very numerously
are the earthen banks made by the Saxons. Now there are
earthen banks which it may be doubted whether they were
made by the Saxons or not. The Wansdyke may be a Saxon
earth work, or it may not, I cannot pretend to say, but there
are certain earth works of which there is no doubt that
they are Saxon, and these are the earth works which represent
the ground plan of the old Saxon gentleman’s house, the Thane’s
house, the house of the landlord, the man of property. I
think that there is probably one of these mounds at English-
combe. I do not speak of a bit of Wansdyke, which runs through
Englishcombe, but I speak of a couple of concentric circles which
are to be seen near the village of Englishcombe. I think they
are the remains of a fortified house. The first and chief idea of
fortification, (perhaps the feature of Saxon times that possesses
most durability), was to make an earthen bank.
Around the group of buildings of which a noble residence
consisted, was carried a bank and ditch, and at a point in this
enceinte a conical mound was raised, of comparatively high
elevation, with a flat top, on which was erected the watch-tower
' which constituted the citadel of the domestic fortress; I am
persuaded there are relics of many such still capable of being
164
traced if they were looked for, in the neighbourhood of ancient
churches and manor houses. Before castles were built of stone,
the strength of the defence lay in the advantage which the bank
gave to the defenders, and in the hindrance it caused to the
besiegers when they would set the citadel on fire.
You may see an illustration of this in the Bayeaux tapestry.
The best extant figure of a wooden fortress, pitched on a conical
and moated mound, is to be seen in that part of the Bayeaux
tapestry which represents the assault on Dinan. Now these
mounds exist in two forms, that which I have already mentioned
of the fortifications of a domestic house, and also in the
other form of the fortifications of a city. There is a very
large one at Oxford near the station. There is one at Tam-
worth, and one at Canterbury. I think there is one, too, at
Leicester. The most perfect example that I have ever seen of
the fortifications of a domestic house is to be seen at a village
called Laughton, about eight miles from Sheffield. The field in
which it is placed is called, I think, the Castle Field.
There is another very good example, only partly preserved, in
Northamptonshire at Earl’s Barton, close to the churchyard. Mr.
Clark, in a work of his published some years ago, gave some
ground plans of various places in which he had observed these
remains of Saxon houses, and when once they are ascertained and.
recognised they are exceedingly interesting, as illustrating the life
of our forefathers.
Turning now to the churches of the neighbourhood, I have no
doubt that Charlecombe was a very old church, as itis reputed to
be. Before the Norman church was built there was, no doubt, a
Saxon chuch there, as there was at Swanswick and a great many
other villages about here. The churches about Bath are very
generally Norman churches, or churches that bear traces of
having been Norman churches. There original form is in some
instances much obscured. At Twerton, for instance, the church
has been subject to many changes, and the only extant evidence
Mth sen
. — eS. Ue ae
165
ofits Norman history is a well-preserved doorway which originally
stood on the south side, but which in the extension of the area of
the church has been unavoidably removed to the north side.
John de Villula, in building the Norman Abbey, drew a large
number of Norman masons here, who were ready to be
employed in similar works in the neighbourhood. Of all these
Norman Churches which were then built, I have always looked
upon Englishcombe Church as being the most perfect specimen,
indeed I always fancy that Mnglishcombe Church was intended
to be a kind of miniature picture of the Norman Abbey.
However, to return to Charlecombe, there is something at Charle-
combe Church I should like to know a little more about. The
yew tree in the churchyard there is said to be older than the
church. Now that is a very interesting saying, for if we could
really verify it as a genuine tradition in any one place that the
yew tree is older than the church, this would be a matter of
historical value. I am strongly of opinion that the yew trees
did not go to the churches, but that the churches came to the
yew trees. The yew trees did not arrive upon the spot first,
they went there in attendance upon the cross. The first thing
that was erected, speaking generally, in our country, was the
cross. I do not say the cross instead of the church, the cross
was the church, and our word church, whatever people may tell
you about its being derived from «vpiaxdv is simply an anglicism
of the Latin word crucem.
When I say that in our own country at the first the cross was
the church, I mean that the people assembled around the cross,
they received the sacraments at the cross, and they were baptized
at the cross. But the question is what the yew trees had to do
with it? When we travel through our country and see the yew
trees in our churchyards, we cannot divest ourselves of the
idea that there is some very considerable reason, hitherto in-
adequately explained, why there are yew tress so constantly in
the churchyards, being sometimes hundreds of years old, for the
166
yew trees in our churchyards are among the highest antiquities
in the vegetable world. Some people have said that yew trees
are poisonous to cattle, and they were planted in churchyards in
order that farmers might not turn their cattle into them. Well,
that does not satisfy me, and I do not suppose that it satisfies
many members of the Club. Another reason was that the
branches of the yew trees made good bows, and that at the time
when our artillery consisted chiefly of bows and arrows, it was
a matter of public interest that yew trees should be cultivated,
and so they were planted in the churchyards. I think the
national interest would hardly have been dependent upon such a
provision as that. Yet another way of explaining it is that the
yew tress succeeded to the cypresses of the classical period as
symbols of mourning.
All this seems to me to be exceedingly fanciful, and does not
bite into the marrow of the case, but one hint I got from Bishop
Hobhouse, and I was very glad, when as J was preparing these
remarks and turning over old memoranda, to come upon the very
date when Bishop Hobhouse communicated the idea to me. His
idea was that they were planted for the shelter and protection of
the worshippers around the cross when as yet they had no roof
over their heads. I felt at once that this touched the truth, and
ever since that time I have continually looked and searched for
evidence with the purpose of ascertaining whether the yew trees
were in the churchyards before the churches were built.. From
the localities in which they are generally found, namely, on the
south side of the chancel, and the east or west side of the south
door, it would seem that they were about and around the spot
upon which the cross stood.
The cross usually stood upon the south side of the line now
occupied by the church and most generally somewhere about the
middle of that line, and the fact that these trees are found on
one side or the other of that spot shows that there was probably
a ring of yew trees round the cross, the best possible protection
167
that could be devised for people too poor to build a church, and
worshipping in the open air. And let me add one word more. Not
only was this word Church made in this island ; but it reflects in
a remarkable manner the condition and circumstances of our
people in the first age of our national Christianity. Before this
time there never had been in Christendom but one word of
general acceptance to express the idea which that word expresses.
We, the English nation, made a second. To the old word
“Ecclesia” we added an equivalent, a new word, Church. And
we not only used this word ourselves, but we propagated it. We
carried it across seas to our kindred who were still heathen, and
we converted them and brought them into the Church. And
this is the true explanation why the German and the Scan-
dinavian nations use the same word as we do, and speak not
of the Ecclessia but of the Church.
We stand in Christendom on a pinnacle in this respect, that
when Christianity seemed to have grown old, to be worn out,
when no extension had taken place for generations in the area
of Christendom, then it was that our people embraced Christi-
anity, and embraced it with such ardour and passion as caused
them to become in the second generation missionaries, to convert
the people in the old Mother Country, and to found Churches
calling them naturally by the new name which reflected the
circumstances of their own conversion, and the manner of their
earliest Christian ceremonial.
Letters Illustrating the Battles of Claverton and Lansdown. By
H. D. Sxrinz, M.A.
(Read January 11th, 1887.)
Some years ago I read a Paper to this Club giving an account
of the Skirmish at Claverton during the Civil War. My main
object was to elicit information on the subject, as the only
historical records which I had then the opportunity of consulting
168
were the brief notice of the engagement in Clarendon’s History of
the Rebellion, the entry in the Claverton Register, the account in
Collinson, and last, but in my opinion most important—that given
in the Rushworth Historical Collections—I had not seen Mr.
Emmanuel Green’s description of the Battle of Lansdown in which
this skirmish was noticed. In the course of last summer I was
able to consult sgme MSS. in the Bodleian Library, part of the
Clarendon Papers (documents sent to Lord Clarendon as materials
to enable him to write his history). These were two letters, one
by Lord Hopton, then Sir Ralph Hopton, the other by Colonel
Slingsby, both of whom held commands in the Royal army.
These letters give a very clear, graphic and consistent account of
what took place ; and a knowledge of the ground and acquaintance
with the roads, both ancient and modern, as given in maps in my
possession, lead me to conclude that we have in these documents
the true history of what actually did take place. In many
important particulars both my own and Mr. Green’s account
require correction. My information had led me to suppose that
Waller was in position on the Warleigh side of the river from
which he had attacked Claverton Manor House, then in the
possession of the Royalists, and that, being repulsed, Waller
retired along the Warleigh valley to Batheaston and Bath. Mr,
Green was of opinion that Waller occupied both sides of the river
and that the Royalists had been first encountered at Monkton
Combe and that the defeated Parliamentarians withdrew through
Batheaston to Bath and Lansdown Hill. He also thought that
there had been a previous skirmish at Claverton when three
Parliamentary and one Royalist soldier were slain and buried in
Claverton churchyard. There is certainly a discrepancy in the
dates here, but I cannot believe there was more than one battle
at this period in this valley of the Avon. The date of the
burial of these soldiers is stated in the Register to be the 30th
June, 1643, whereas the battle described in the following letters
was fought, according to the Mercurius Aulicus, on the 3rd of July
169
that year. The true explanation of the discrepancy of the dates
probably is, that the letters were written and the entry in
the Register made, some time after the event. Humphrey
Chambers, the Rector of Claverton, was a member of the
Assembly of Divines and was probably in London at the
time, and as there is evidence to show that the bodies
were buried without coffins* it may be conjectured that the
funeral may have been hasty and “ without benefit of clergy.”
It appears by these letters that Waller, having heard that the
Royal army coming from the west had reached Bradford, had
taken post with all his forces on Claverton Down ; and having
thrown a bridge across the Avon at Warleigh ferry, and built a
redoubt to protect the bridge and the ford there, had sent a force
of horse and foot and artillery across the river to occupy Monkton
Farleigh Down—so as to be prepared to meet the enemy on
whichever side of the river he might select to march. As a
matter of fact, the Marquis of Hertford and Prince Maurice,
who commanded the Royalists, marched by the road on the right
bank of the river, which was identical as far as Farley Wick
with the present high read from Bradford to Bath. Near the
point of junction of this road with that leading to Warleigh lane,
and about halfamile from Farleigh Down on the way to Bradford
at the foot of a hill, was a small wood which was grubbed about
30 years ago. In this wood Major Davet,t who commanded the
Parliamentary force on Farleigh Down, placed some of his infantry
* Collinson states that these soldiers were buried under the west
wall of the church. There is at present no room west of the church to
bury, but previous to the building the new north aisle there was a
. Space for burial, and in digging a deep grave there early in the century
some bones were found which apparently had been buried without
coffins, and these were removed to the other side of the church, where
tradition now is that these victims of civil war were finally interred,
+ Rushworth’s account.
170
in ambush, and then advanced to meet the Royal army on the
road to Bradford, and after a slight skirmish with their advance
of cavalry withdrew behind the ambush. And the: battle began
which shall be described by the writers of these letters.
I think it will be seen from the letters when read that the
skirmish at Monkton Farleigh* and Claverton was by no means an
unimportant incident of the Civil War, and very possibly had it
been fought a little earlier in the day the Royalists would have
been able to have pushed on to Lansdown hill, and thus to have
completely reversed the conditions of that battle.
Lord Hopton’s Account of the Movements of the Royalist army, 1643.
Clarendon MSS., 1738. (4).
Vpon Sunday the the Army advanced to Bradford,
where they had a passe over the River Avon at theire Comand,
and were on either side within 4 miles of the Enimye’s Quarters.
The same night Sr Wm. Waller aduanced a great part of his
Army, both Horse foote and dragoones over the River vnder
Claverton-house, where besides the fforde, he had made a Bridge,
and a Redoubte on his side to defende bothe, reserving the other
part of his Army with his Ordnance in Battalio on Claverton-
downe. With this part of the Army so drawen over the River,
he advanced in the night and possest himselfe of the high-ground
at Munckton-ffarly and layd an Ambuscade in a woodland-wald-
* It may be some corruboration of the fact of the battle having been
fought near Monkton Farleigh (or rather Warleigh Down, as the Downs
adjoin) that close to the present Bradford road over the Downs near the
Dry Arch the Warley revels used to be held, and tradition said
in memory of a battle fought there—and labourers who had attended
these revels assured me that they frequently turned up human bones
there. = Be
pp TORS. i er me
171
ground in the ffoote of the Hill, and so in the morning he
advanced strong Partyes of Horse; vpon theire out guards of
Horse, which being then strong and well comanded by Major
Lower, he held them vp till the whole Army drew forth, which
then in good order both Horse and ffoote advanced towards the
Enimy.
The Cornish ffoote in an hower or two beate the Enimy out of
theire Ambuscade, and then both ffoote and Horse advanced
vpon theire maine-body on the topp of Munckton-farley hill,
where they durst not to stande them and so they had the chace
of them as farr as Bathe-Easton. In which chace and not before
they discouvered Sr Wm. Waller with his maine Body on the
other side of the water on the topp of Claverton-dowre with his
Bridge and his worke before mentioned. Herevpon Prince
Maurice turn’d the maine of the force of ffoote to gaine that
pass which he did just as it was night, and so Sr Wm. Waller
in the darke retreated into Bathe. By this time many of the
Horse in pursuite of that part of the Enimy that fledd the
other way had passed into the ffields vnder Lansdowne close by
- Bathe, where about 12 at night it was considered by the officers
there present, whereof the principle were the E. of Carnarvon,
Lo-Mohun and Sr Ralph Hopton and Sr Nicholas Slaiing,
whither they should that night drawe to the topp of Lansdowne
or not, and it was considered that they were there but a part of
the Army, and that the rest of the Army being surprized by the
‘night, after that dayes chace might not be in very good posture
to receive concurrent orders; So they resolu’d to drawe back
that night within Bath-Easton-bridge, and to advise with the
Generall to quarter the Army in the best order they could, with
a resolution to drawe out the next morning verie early to try if
they could prevente the Enimy of that high ground of advantage,
which the next morning early they endeavoured with a little
more heate then was altogether expedient, for moveing verie
early with all theire Horse, ffoote, Canon and Baggage towards
172
Lansdowne, by that time they came to the foote of the hill, the
Enimy, by the advantage of his neernes to it, was possest of the
ground, and themselves with the whole Army, especiaily the
Carriages which were most troublesome, engaged in a ffield just
ynder them, out of which there were verie inconvenient wayes
to retreate, to advance noe possibility, and to stay there least of
all, for the Enimye’s Canon played into them, and they had noe
meanes to requite them. So about one in the afternoone the
chiefe Comanders resolved of a retreate. towards Marsfield, and
comitted the order of it to Sr Ralph Hopton, who drawing vp
the Army in the best order he could to face the Enimy, first
sent of the Canon and Carriages with convenient guards by the
“% narrow lanes that went from thence towards Marsfield, and
presently after sent 1000 Muskettiers to line the hedges vpon
the entrance of both those wayes, then he sent off the Army in
parts, remayninge onely to hold vp the Enimy with a strong
forlorne hope of Horse with which at last he marched off without
any loss and drew a strong party of the Enimye’s Horse within
the Ambuscade of Muskettiers, which haveing tasted they
quickly retired. And so the Army came that night safe to
Marsfield sending out theire Parties of Horse everie way to
secure their Quarters.
The next morning earlie Sr Wm. Waller drew out his whole
Army over Lansdowne to that ende which lookes towards
Marsfield and there vpon the verie point of the hill over the
high way suddenly raysed breast workes with faggots and earth,
and sent downe strong partyes of Horse into the field towards
Marsfield, where they lighted vpon a party of Horse and beate
them in. This roused the Army at Marsfield and so about 8
that morning being the 13th of July, 1643, all drew forth, and
within verie short time a light skirmish was engaged with
dragoones in the hedges on eache side; But the chiefe Comanders
of the King’s Army considering that the continuing of that
kinde of fight would be to little effect, but might onely waste
a
173
theire Amunition (whereof they had not plenty) drew off and
retreated in Batalio towards theire Quarter to Marsfield, which
the other Army perceiveing tooke the courage to sende downe
great partyes of arm’d Horse and Dragoones to charge them
both in reare and flancke. Those that came vpon the reare
vsed most dilligence and haveing left theire dragoones in the
ende of the Lane towards the field charged verie gallantly, and
rowted two Bodyes of theire Horse, whereof the last was, by
Prince Maurice his comand to Sr Ralph Hopton winged with
Cornish-muskettiers, who poore men (though the Horse were
rowted betweene them) kept theire ground and preserv’d them-
selues till the E. of Carvarvons Regiment of Horse was drawen
vp to them. In the meane time Sr. Nicholas Slanning wes
comanded with two or three hundred Muskettiers to fall vpon
the reserue of dragoones behinde them, which he performed
verie gallantly and beate them off; And at the same time the
Earle of Carvarvon with his Regiment and the forementioned
Muskettiers charged the Enimyes Horse and totally rowted them.
Presently after this appeared two great Bodyes of the Enimyes
Horse advancing towards theire flanck, which indured a good
charge of two bodyes of the Kings Horse and some volleys of
Muskettiers before they brake, but at last were rowted and
chaced. And then the whole Army in the best order they could
in that broad way that leads to Lansdowne advanced towards
the Enimy sending out as they wente strong partyes of
Muskettiers on eache hand to seconde one another to endevour
vnder the Couvert of the inclosed grounds to gaine the flanck
of the Enimy on the topp of the Hill, which they at last did,
But the Pikes and the Horse with the rest of the Muskettiers
that advanced vp the broade way as the space would beare had
much to doe by reason of the disadvantage of the grounde, the
Enimye’s ffoote and Batteryes being vnder couvert of theire
breast-workes, and theire Horse ready to charge vpon the verie
browe of the Hill, where the Kings forces were five times
N
174
charg’d and beaten back with disorder. There was Sr Bevil
Grenvile slayne in the head of his Pikes, and Major Lower in
the head of a Partye of Horse, and Sr Nicholas Slanings Horse
kild vuder him with a greate shott, and the whole body of
Horse soe discomforted that of 2000 there did not stand aboue
600. Yett at last they recovered the hill, and the Enimy drew
back about demi-culverin-shott, within a stone wall, but there
stood in reasonable good order, and eache part played vpon the
other with theire Ordnance, but neither advanced being both
soundly batter’d. So the night came on, and all things grew
quiett, where Prince Maurice and Sr Ralph Hopton remayning
in the heads of the Troopes all that night, aboute one of the
clocke heard an advancing of Horse and ffoote, but without
drum or trumpet and they presently received a smart vollye
from the Enimye’s Muskettiers, which was answeared with the
like, but being verie darke noe more was done and all things
grew quiett againe. So after an howers silence the chiefe
Comanders before mentioned rightly iudgeing that this might be
the Enimye’s parting blowe, gave a comon souldier a rewarde to
creepe softly towards the place where the Enimy stoode to bring
certaine notice whether they were retreated or no, who found
them gone. By this time it was towards breake of daye, and
in the morning the Comanders founde themselves possest of the
field and of the dead, and of 3 or 400 of the Enimye’s Armes,
and 9 or 10 barrells of theire powder, And so about 9 in the
morning they retired with the Army to Marsfield, where they
rested the next day, principally by reason of Sr Ralph Hopton,
he having bin in the begining of the battell shott through the
Arme and in the ende of it blowen vp with Gun-powder, and
so was verie vnfitt to be removed the next daye.”
175
By Col. Stingshy. Events of the West, ‘ After Stratton field to taking
of Bristol.” Clarendon MSS., 1738. (3).
“Then does the kings Army mooue first and marches to Brad-
ford* within fower miles of Bathe : the next morning our skoutts
brought vs word that the Enemy was drawne into the field horse
and ffoote in the midle way betwixt our quarters ; wee draw out
presently and marche towardes the place, and finds them but a
party and fixed vpon a ground of greate aduantage, yett from
thence (though with a very hott dispute) they were remou’d
with the losse of two small pieces, and neare 100 men. Wee
possessing this ground discouer’d the body of the Enemy drawne
vp in batalia on the other side the Riuer and about two miles
of ; thus had the shifting Rebell deluded vs one day with a party,
hoping to make vs weary with dancing about him, or else to
fight where hee pleas'd: vpon this wee were once resolu’d to
marche directly vp to Lansdowne hill, but afterwardes (consi-
dering the night approaching, the narrow and craggy passage vp
the hill, with the aduantage theire horse might take vpon our
Reare, who: would bee more bold and troublesome hauing a good
Towne for a retreate soe neare them) wee lay all night in the
bottome close by the ffoote of the hill.
The next morning when day appear’d our Enemy did the like
vpon the hill, who as with iudgement obseru’d our motion
and discern’d our intention soe with greate industry and care
eee ek cree ME lake! Ut el Tene ue Ey as
* Mercurius Aulicus . . . the seven and twentieth weeke p. 356.
It was advertised this day, that Prince Maurice hearing of a Partee
which Waller had sent out to obtaine a Passe over Bradford-bridge,
not farre from Bath, sent out an answerable strengh tto deprive them
of it. Who did their work so valiantly like men of courage that they
did not onley gain that Passe for the Princes use, but killed neare an
hundred of the Rebels, and drave the residue into Bath.
176
labour’d all night both to preuent vs, and to serue himselfe of
such an advantage: and indeede that Generall of the Rebells
was the best shifter and chooser of ground when hee was not
Master of the field that I euer saw; wch are greate abilityes
in a Souldier.
Vpon this south side of Lansdowne hee shewes vs his whole
body ; that day wee spent in looking vpon one another; the Enemy
veiwd our whole Army as it stood rang’d in the valley whose
number could not then bee disguis’d, soe that it appear’d too big
to invite him downe to fight: towardes night wee marchd of the
ffeild towardes Marsfeild, vpon our remoouall a lusty party of
the Enemys horse falls on our Reare, who att first bred a litle
trouble, but were att Jast repulsed with losse and shame :
That night wee lay att Marsfeild and next day fought
Lansdowne batle the Rebells being then drawne vp vpon the
North side of the hill.”
After the Rebells are drawn out on North side of the Hill. Col.
Slingsby’s relation of the battle of Lansdown, July Sth, and
that of Roundway, July 13th. Clarendon MSS., 1738. (2).
The night before the battaile att Launsdowne the kings Army
quarter’d att Marsfeild; in the morning betimes Waller sent a
strong party of horse towardes our head quarter, who beate in
all our horse guards, and alarum’d all our quarters: wee instantly
drew into the feild and marched two miles towardes Launsdowne
where wee could see the Rebells Army drawne vp vpon the top
of the hill, he stood vpon a piece of ground almost inaccessible.
In the brow of the hill hee had raised brestworkes in w™ his
Cannon and greate store of smal] shott was placed; on either
fflanke hee was strengthned with a thicke wood w™ stood vpon
the declining of the hill, in w™ hee had putt store of mus-
keiteires ; on his reare hee had a faire plaine where stood rang’d
177
his reserues of horse and ffootte ; some bodyes of horse with
muskeiteires hee bestow’d vpon some other places of the hill,
where hee thought there was any accesse ; thus fortyfied stood the
foxe gazing at vs when our whole Army was rang’d in order of
battle vpon the large Corne feild neare Tughill. In this posture
wee continued about two houres; nothing passing but ‘loose
skirmishes vpon Tughill, betwixt a party of our vantgard and a
party of horse and dragoones of the enemys sent downe the hill
for that purpose. The kings Army found that the Rebells would
not bee drawne to fight but vpon extreame aduantages; and
therefore faced about and marched towardes our quarter in order
as wee had stood w™ the ground would admit of, being a
continuing plaine large feild all the way to Marsfeild ; when wee
had marched neare a mile the whole streneth of Wallers horse
and dragoones descends the hill, and falls vpon our Reare ; wee
faced about againe and aduanced vpon them endeavoring to
regaine our ground where wee were before rangd: w™ wee
gott with muche dificultye and hazard, our horse receiving some
dangerous foiles ; soe that had not our ffootte bin excellent wee
had certainly suffer’d theire: the rebells horse not enduring our
charges of horse and volleys of small shott that fell vpon them
from our approaching bodys of ffootte, they retir’d themselues out
of that feild; but left all theire dragoons vpon the walls and
hedges vpon the farre end of feild the neare Tughill from whence
our ffoote beate them suddenly. The enemys horse being now
forest into the laine that leades ouer Tughill to Lansdowne, were
obseru’d to be in some disorder by reason of the narrow and ill
passage. Prince Maurice therefore takes all our horse and wings
them on both sides the laine within the hedges with smali shott,
and soe smartly fell vpon them, that some run in greate disorder;
but it seemes they had (like prouident souldiers) placed theire
best horse in the Reare who being compeld, turnes about and
fights desperately, and theire giues our horse another foile with
the death of Major Lower, Major James and many others: but
178
our horse being still assisted by the ffootte, att last beate them
downe Tughill, where in the bottome they were cruelly gall’d
by our ffootte that then drew vp thicke vpon Tughill.
Now did our ffootte beleiue noe men theire equalls, and were
soe apt to vndertake anything, that the hill vpon wch the
Rebells stood well fortyfied litle without muskett shott (from
whence they racked ys with their Cannon) could not deterre
them ; for they desir’d to fall on and ery’d lett vs fetch those
Cannon. Order was presently given to attempt the hill with
horse and ffootte: greate partys of Muskeiteires was sent out of
either of our wings to fall into those woodes w® flanked the
Enemye, and in w™ they had lodg’d stoare of small shott for
their defence, the horse were to passe vpp the high way, but were
att first repulsed ; Sr Beuill Grenville then stood on the head of
his Regiment vpon Tughill, who aduanced presently putting all
his shott vpon his left hand within a wall, and cary’d with him
horse on his right hand the ground being best theire for horse,
and hee himselfe lead vp his pikes in the midle: hee gain’d with
muche gallantry the brow of the hill receiving all their small
shott and Cannon from theire brest worke, and three charges of
horse, two of wch hee stood; but in the third fell with him
many of his men: yett had his appearing vpon the ground soe
disorder’d the Enemy, his owne muskeiteires fyring fast vpon
theire horse, that they could not stay vpon the ground longer ;
the Rebells ffootte tooke example by theire horse and quitt theire
brestworks retyring behind a long stone wall that runs acrosse
the downe; our ffootte leps into their brestworks ; our horse
draws vp vpon theire ground: our two wings that were sent to
fall into the two weodes had done theire businesse and were vpon
the hill assoone as the rest.
The Enemy (obseruing our ffront to enlarge it selfe vpon the
hill, and our Cannon appearing theire likewise) began to suspect
himself, and drew his whole strength behind that wall, weh hee
lined well with muskeiteires, and in seuerall places broke down
179
breaches very broade that his horse might charge if theire were
occasion, w™ breaches were guarded by his Cannon and bodyes
of Pikes.
Thus stood the two Armys taking breath looking vpon each
other, our Cannon on both sides playing without ceasing till it
was darke, Leges and Armes flying apace the two Armys being
within muskett shott: After it was darke theire was great
silence on both sides, att wch time our right wing of shott gott
muche nearer theire army lodging themselues amongst the many
litle pitts betwixt the wall and the wood from whence wee gald
them cruelly.
About 11 of ye clock wee receiu’d a very greate volley of
small shott but not mixt with Cannon by which some of vs
iudg’d that hee was retreating, and gaue this att his expiring ;
but the generall apprehension through our Army was that the
Enemy had intention to trye a pushe in the night for theire
ground, wch they had soe dishonorably lost; for wee were
then seated like a heauy stone vpon the very brow of the hill,
weh with one lustye charge might well haue bin rowl’d to
the bottome.
It was not long before wee knew certainly that they were gone.
att theire departure they left all theire light matches upon the
wall and whole bodys of Pikes standing upright in order within
the wall as if men had held them : wee were glad they were gone
for if they had not I know who had within an hower ; but indeede
had our horse bin as good as the Enemys the rebells had never
gone of the feild unruin’d. We kept the ffeild till it was day
light and then plundered it, and sent severall partys of horse
seueral waies, att whose retourne we were inform’d that the
Enemy was in Bathe: at eight of the clocke we marched of
towards Marsfeild.* Upon Tughill one of our ammunicon
waggons tooke fyer, blew up many men and hurt many; especially
* End of Bath, Lansdown.
180
my Lord Hopton, Major Sheldane dyed the next day and was
muche lamented: this disaster encourag’d the Rebells and dis-
courag’d vs. Our horse were bad before but now worse, our
ffoote drooped for theire Lord whom they low’d, and that they
had not powder left to defend him, for as I remember we had
then but nine barrells left : that night wee quarter’d att Marsfeild
being Thursday, the same night the enemy drawes out of Bathe
up to Lansdowue againe ; the next morning being friday we
marched to Chippenham, the same night the Enemy steps into
our quarters att Marsfeild, and now the Country seeing him
following vs begins to disert vs ; soe that wee could gett neither
meale nor intelligence, two necessary things for an Army : wee
lay att Chipenham two nights, but were on Sunday earely ffrighted
from thence by the Enemys neare approache; wee marched to
the Deuizes.
Further Notes on the Claverton Skirmish. By H. D. SkRiNgE, M.A,
An old map shows very distinctly the road I suppose the Royal
Army to have taken, and you will see that at the date of that
map the road joined the present ford road below the Dry Arch.
The maps do not show how far Monkton Farleigh Down extended
towards Bradford, but I think it can hardly have been farther
than the ford road. That road would be the line of communication
between Davet and Waller, and down it must have been the
pursuit of the defeated Parliamentarians; though some may
have scattered over the precipitous and eraggy common towards
Bathford and Bath.
I do not think the line of march I have pointed out can be
disputed ; but it may be well to note that strategical reasons
would be very strongly in favour of its being chosen by the
Marquis of Hertford and Prince Maurice. It was the most
direct, the shortest, and in every respect, from the open country
it traversed, the most suited to the march of an army; and there
MAP ILLUSTRATING BATTLES OF MONCKTON FARLEIGH
AND CLAVERTON.
REDUCED FROM THORPE’S MAP OF BATH AND ENVIRONS, 1742.
z
Ss
I
&
3
Ee}
e
a
SCALE—1# in. to the Mile.
181
was but one little piece of “walled wood ground” where an
ambush could have been laid. Near the spot just named, still
is to be seen by the side of the high road a deep hollow ditch at
one side, evidently the old road which must have been rather
like a Devonshire lane. The other road through Turley, Winsley
and Conkwell would have presented more physical obstacles and
have also been farther ; and besides, the armies would have been
in sight of each other long before they reached Warleigh Woods,
or the line of Monkton Farleigh Down. That they should have
marched on the left bank of the river may be dismissed for still
stronger reasons. It would have been the wrong side for their
purpose of keeping between Waller under fire ; and at Westwood,
Freshford, Limpley Stoke and Monkton Combe were defiles which
might have been defended easily, as the road most of the way
follows the valley of the Avon with steep hills on both sides.
The circumstances mentioned in the letters, that “in the chase
and not befure the Royalists perceived Waller’s army drawn up
on Claverton Down” exactly tallies with the site of the battle as
described by Lord Hopton ; as until the position at Monkton
Farleigh was won, the rise of the ground would prevent the
Royalists from seeing the Claverton Down.
Rushworth giving the authorized Parliamentarian account of
this battle says “that the Royal Army having come within two
miles of Fourd Hill, Waller sent Major Davet to secure the pass at
Fourd Bridge.” Fourd Hill means Bathford Hill. Fourd Bridge
existed at that time, but the real pass was at Warleigh where was
a bridge at the time, and this could be best secured by occupying
the southern end of Fourd Hill—i.c., Monkton Farleigh Down
and Warleigh Hill. Warleigh would have been naturally named
as the locality, but was probably not known to writers, though
Ford or Bathford was well known, and Warleigh is only a part
of the Manor of Ford. In making the attack on Claverton
Redoubt, cannon no doubt would have been employed to support
the attack, and this accounts for the cannon balls found at
Claverton.
182
Note on the Ham Hill Stone. By Horace B,. Woopwapp, F.G.S.,*
of the Geological Survey of England and Wales.
(Read February 9th, 1887.)
The celebrated building-stone of Ham Hill, near Yeovil, offers
but little attraction to the collector of fossils, for he may hammer
away in the quarries all day long, without obtaining any
palzontological reward ; but the stone is not without geological
interest, for it differs considerably from the ordinary beds of the
Inferior Oolite, and its precise position in that series has been a
subject of some discussion,
The ordinary beds of the Inferior Oolite comprise an upper
division of marly, oolitic, and iron-shot limestones ; and a lower
division of sands (known as the Midford Sands) with impersistent
bands and large concretionary masses of calcareous sandstone.
The Ham Hill stone is mainly composed of sand and comminuted
shells. In considering its relation to other divisions of the series,
we must, of course, remember that however persistent the
ordinary or characteristic features of a formation may be in our
country, such features after all are but local portions of the
original formation ; and with regard to marine deposits, were the
full record of each period preserved and open to our inspection;
it would no doubt exhibit as much diversity as do the sea-bottoms
at the present day.
In the case of the Ham Hill stone, we picture a shoal of shifting
sands and broken shells, such as may be found in many areas of
the English Channel or the German Ocean ; and we are thank-
ful, while searching for fossils, to recognise even the fragment
of a Pecten or an Oyster. After contemplating the rock and
endeavouring to picture the conditions under which it was
* Communicated by permission of the Director General of the
Geological Survey
183
formed, it is but natural to inquire into its precise position in
the Inferior Oolite series, and to ascertain what others have said
upon the subject. Unfortunately a study of the literature is
likely at first to create a feeling of perplexity, for those who
have written about the Inferior Oolite of the Yeovil district,
have not agreed in the correlation of its members with those in
other parts of the West of England ; nevertheless, by the aid of
personal observation, we may extract the truth from the several
Geological papers, and ultimately restore comfort to our minds.
Mr. Charles Moore (to whose papers we naturally turn for
information on the Lias and Oolites of Somersetshire) has given
the best account of the strata at Ham Hill; but he did not enter
into the question of their exact equivalents, as his object was
simply to show the intimate connection between the so-called
Midford Sands and the limestones of the Inferior Oolite, in
opposition to the view of Dr. Wright that the sands should be
grouped with the Upper Lias.* On the Geological Survey Map
the Ham Hill stone is coloured the same as the Inferior Oolite
Limestone, but Mr. Bristow, who originally surveyed the area,
has expressed the opinion that the stone is the equivalent of
the upper part of the Midford, or Inferior Oolite Sands, which
contain thin and interrupted beds of limestone.t This is the
true view of the case, and Prof. Buckman claimed to have been
the first to point it out.t Thus layers of stone like Ham Hill
stone appear in the Sands in the railway cuttings near Yeovil
Junction, and in some of the deep road-cuttings or ‘‘hollow-ways”
of Babylon Hill. Lately Mr. W. H. Hudleston has drawn
particular attention to one of these layers opened up in a pit at
Stoford, west of Yeovil Junction. This shelly-layer yielded
Trigonia anguluta, Tancredia, Ammonites (Harpoceras) Moorei,
* Moore, Proc, Somerset Arch, Soc., vol. xiii.
t Damon’s Geology of Weymouth, &c., 1884, p. 219.
{ Proc. Somerset Arch. Soc., vol. xx., p. 162. :
184
and A. radians.* These shelly limestones may be traced in
places to the south and south-west of Yeovil, and there is a large
quarry in stone similar to that of Ham Hill, at North Perrot,
east of Crewkerne.
Although the Ham Hill stone is, as a rule, devoid of recog-
nizable fossils, I have obtained several specimens of Rhynchonella
cynocephala in the beds exposed on the eastern side of the outlier,
in a quarry about half-a-mile south-west of Montacute Church
and this discovery has since been confirmed by the Rev. H. H.
Winwood. This fossil corroborates the stratigraphical evidence
that the Ham Hill stone belongs to the upper part of the
Midford or Inferior Oolite Sands. + While Professor Buckman
recognized the true position of the Ham Hill stone in reference
to the Inferior Oolite series of the neighbourhood, he was not
justified in grouping the upper part of the Sands at Yeovil
with the lower part of the Inferior Oolite limestone of the
Cotteswold Hills. His son, Mr. S. S. Buckman, has pointed
out that although the limestones of Dorset are comparatively
thin, yet paleontologically they represent the whole of the
Inferior Oolite limestones of Cheltenham, and yield the same
succession of Ammonite-zones ; a succession confirmed by the
more recent observations of Mr. Hudleston. Hence the Sands
below the Inferior Oolite limestone in Dorsetshire, Somersetshire
and Gloucestershire are approximately the same, and the term
Midford Sands (given to them by John Phillips) is applicable to
all these areas.
* Proc. Geol. Assoc., vol. ix., p. 190.
+ As mentioned in my Notes on Brent Knoll, a variety of
Rhynchonell1 cynocephala occurs at a higher horizon in the Cotteswold
Hills,
185
Further Results of Meteorological Observations made at the Bath Royal
Literary and Scientific Institution. By the Rev. Lronarp
BLuMEFIELD, M.A., F.LS., F.G.S., &c., President,
(Lead February, 18th, 1887.)
In a former paper read to this Club in November, 1875, and
published in our “ Proceedings,”* I stated the Results of Meteoro.
logical Observations made at the Bath Royal Literary and
Scientific Institution, during ten years commencing with March,
1865, and ending with February, 1875. I stated under what
circumstances these observations had been taken in hand, as also
what had been done previously, or written by others, in reference
to the subject of the Bath climate. This was followed by a
description of the structure erected in the Institution Gardens
for the reception of the instruments employed, the nature and
character of the instruments themselves and the way in which
they were fixed. As the instruments remain unaltered in
character and position, it is unnecessary to repeat here what was
then said on this part of the subject.
Neither is it necessary to say anything further respecting the
situation of Bath and its surrounding hills, or as to any other of
its features ; nor to speak of other places, some in the immediate
neighbourhood, others in the far distance, east and west, of which
as compared with Bath in the matter of climate, I gave some
account in my first paper.
My main object at present is to annex the results of ten years
further observations of the Thermometer and Rain-gauge to those
of the decades preceding. This will cover a period of twenty
years, commencing with January, 1866, and ending with Dec.,
1885. I also give the results of eleven years’ observations of the
Barometer. Very little was said about this instrument in my
first paper, from the circumstance of there being no barometer
rt
* Vol. III, p 205,
186
in the possession of the Institution at that time with which
any trustworthy observations could be made. At the same
time I stated that a much better instrument had recently been
acquired, “a Fortin’s Barometer made by Casella,” with which
observations were commenced on the Ist of January, 1875 ; and
I now proceed, in the first instance, to give the results of eleven
years’ observations, 1875-85, both years inclusive.
It will be seen, on inspecting the accompaning tables, that the
mean height of the Barometer at the Bath Literary Institution
on an average of eleven years is 29°976 inches. This differs
scarcely more than three hundreths of an inch from the result of
ten years’ measurement at the same Institution with the old
instrument, spoken of in my former paper,* and set at 29-944
inches. It also differs but very little (only ‘012 inches) from the
mean height of the Barometer at Exeter, determined by Dr,
Shapter,t on an average of twelve years, to be 29-988 inches.
The observations I made formerly at Swaffham Bulbeck, in
Cambridgeshire, continued for nineteen years, gave a mean of
29°885 inches. Other observations made at the Cambridge
Observatory for ten years gave a result of 29-906 inches.t
Combining these results we shall not be much in error, if we
consider the mean height of the Barometer in the southern half
of England as about 29°950 inches.
In table 2 are given the greatest and lowest heights of the
Barometer in each month of each year from 1875 to 1885. All
these observations, like those in the first table, have been corrected
for temperature and height above the sea. On inspection they
will be found to possess several features of interest.
The highest of all the Barometric observations registered is
30°978 inches, which occurred on January 18th, 1882. The
* See the Club’s “ Proceedings,” vol. iii., p. 211.
+ Climate of South Devon, p. 24,
t Observations in Meteorology, p. 139,
x
ior)
ee
966-68 | L76.63 | £26.62 | £86.66 | 996.62 | 986.68 | 816-66 | G10.0€ | 618.63 | 86-6 | EF6.6z | 160.08 |iudy,
68 |
96-6 poe fe | ee ef ce 310.08 | 8z8.6z | 929.62 /ax1.08 | 269.68 | t16.63 68g
10.08 || st6-68 | 908.08 zet-o¢ | 6¢o.08| 1¢0.0¢ | 126.68 | 920.08 | o¢0.08 | 298.62 | 26.62 | g06.6s | 020.08] F881
66.68 || 988.06 | 098.68] ¢10.08 | 0¢8.63| €40.08 | 168.68 | 166.62 | 000.08 | 070.08 | F26.63 | 20.08 | se6.6a| cee
86.66 || 120.0¢ | s¥6.63 | eeo.ve | sto.0¢ | 128.68 | ze0.0¢ | 200.08 | eet.o8 | 996.68 | 926.68 | 198.68 | v6.6a| 1891
10.08 || 696 081.08 | Or F.08 |
16.68 || 8
96.63 ||
26.68 ||
I
T
VE.0€ | 9L6-0€ | I6I-0€ | 666.62 | 978-6Z | GZB-6G | 008-66 | €60.0E | OLL-6G | 0G0.0E | 199.62 | 670.08 | 6L8T
G6LL.66 | 968 6G | 808.66 | O€0.0E | L91 62 | 9L0-0€ |F96.62 | G6L-6G | 6E8 6% |.9¢0.0E | LOE.0€ | 612.0 | SL8T
1G0.0€ | est-ce 860.0€ | OLL.6Z | 890.08 | Z10.0€ 486.68 |re6.68 L1€0.0€ | 760.0 | 681.0€ | 780.0€ | 976.66 | S181
( 1202]. Dag PUY 6G aingnsadwuay 0) p9p0a.t.0g )
"ER8I-GLSI ‘uajomomg fo syybrozy hpmax pun hyyyuoyy umapy ay; bumoyg—T aay,
g
g
z
L | 696.62 | 866.62 | 0¢6.66 | zt0.08 | 1¢0.08 | 216.6z | 196.68 | goto | o68.68 | ogt-0g | e18.68 | orF-08 | o8et
T A f F . F
¥ :
oe mor)
OTN NL OLN
om © mM wf as fat Sos Po eS Bom es Bb eee
f St
Pes
61G-0€ | €16.0€ | 88.08 | 1EE.08 | LLE. og | 248.08 | 298.08 | 6FP.0¢ 409.08 | 6e90¢ | ¢9¢.0¢ $99. 0g | 281 |
Se
"VNIXVIN
"A00T-C OT wha T eine fH aati ci9n9 oe tascsnoina fn. cheoes Adoiaree. een eee
8PE.66
6FP-66
F88.66
9€2.66 | 968-66 | $40.63 | 696-88
69.66 | €ZL-62 909-66
891.66
006.6G
$99.66
66
99F.66 | G9Z.6G | 168-66 | SGT9.8¢
8€E.6G | ZIE.66 |O0F8-88 | 980.62
$90.66 | Ze.
098.86
FI9-6G | GI8.66 | £26.66 | 8F0-66 | 118.86
G€8.62 | 998.60 | | ron.63 | ¢69.6 | Z98:9z | eercs | 629-68
€61-66 | GGL-66 | OLL.6G | IFS.6@ | 9EP-66 | OFG.66 9IE.66 | FZZ.6Z
aNoge IVI “aay “NV
6S€.66
601-86
09.66
HOUVIY
“VININIP
¥S9-0€ | P8E.0E | S1Z.0&
PRE-O€ | PSE-0€
eviem
1ge.0€ | 969-08 | 161-0€ | TeF.0€
0S¢.0€ | OTL-O€ | S6E-O& | 7SZ.0€ | C1Z.0€ | LEE.o€ GEL-O€ | 8PZ.0€ | 1Z¢-0€ | £99.08
oce.0g | $9¢.0¢ | #8208 | 6z€.0¢ | ¢zz.0¢ | 9¢.o¢ | ¢cor.og | 699.08 | ¢z2.0¢ |#88.08 | 819.08
Egl.og | PE¢.0¢ | oeF.0 | z4¢.0¢ | err.og | soc.oe | 90¢.0¢ | zz¢.0¢ 281.08 | 826-08
OFF.0¢ | €9¢.0¢ | gtF.0g | ro¢.0e | 1F¢.0¢ | F6z.0¢ |¢g9.o¢ | ¢sz.v¢ g0¢.0¢ | 8¢9.0¢
e6r.0€ | srr.o¢ | 029.08 | 6zE.08 9.08 16P.08
6SP.0€
—+—
PGG.08
OLG-.0€ | I16F-0€ | OLT-0€ | F81-0€ | L9T.0€ 896.08 | L8¢.0€8
£68.08 61E.0€ | 88E.08 | GOZ.0E | GLT.0€ 189.0¢
Sel 2
TPL-O€ 102.08
€99.0€ 99T.0€
099.0€ | €TL-0€
9€€.0€ | 8&9.0E
T9F-0€
0ZZ.0€ | ShE.0€
9LE.08 19P.0€ | OLZ-0€ | LL¥.0€
SPE OF OGE OF | SEF-O€ | 6GZ.0E | E8F.0€ | 6EC.08
8ZE.0€ | $69-0€
€16.0€ 1€6.08
LLE.O€ | LLE.OE | 19G.0E | 6FP.O€ | F09.0€ | Ge90E | G9G.08 | PS9.0E
“GS8L-GL8L waz yova fo YPWOTy yova ur ajaMo.vg {0 syybiazy ysanoT pup j8aJvAL— TIT AIAV
“sony ATID
“VINIXVIN
a
@
=
a
cs)
187
lowest is 28°337 inches on December 4th, 1876. The range
consequently during the whole eleven years is 2°641, or rather
more than two inches and six-tenths. The above extremes have
been exceeded in other places on former occasions. Dr. Shapter’s
extreme maximum at Exeter is 30°98, or very nearly 51 inches,
observed in January, 1825; his extreme minimum 28:13,
observed in December, 1821.
I doubt whether the former, the extreme maximum at Exeter,
has ever been exceeded ; but with regard to the extreme mini-
mum, there are a few unquestionable cases on record, in which:
the Barometer has fallen considerably below 28 inches. Howard
mentions a reading of 27°83 inches at Tottenham, on December,
25th, 1821,* a day on which there was a very remarkable
depression of the Barometer over a great part of the kingdom,
noticed at Greenwich and Cambridge and several other places.t
Perhaps the greatest falls on record were two of more recent
occurrence, in one of which the Barometer, at Barrow-in-Furness,
on December 8th, 1886, fell to 27:410 inches ; in the other at
Ochtertyre, Perthshire, on January 26th, 1884, when it fell to
27°333 inches.t
Belville remarks that the great depression of the Barometer
in December, 1821, above mentioned, occurred after “a heavy
rain of some hours’ duration, with the wind S8.E.” He speaks
also of a great depression (28°21 inches) that occurred “at the
close of the great frost of 1814, which in like manner was pre-
ceded by a stormy wind from S.E. and much rain.”
* “Climate of London,” vol. iii., p. 69.
+ Belville’s Manual of the Barometer, pp. 19, 20.
t See “Nature,” vol, xxxv., p. 157; where it is added as remarkable—
“that these two low Barometers, hitherto the lowest observed by man any
where on the land surfaces of the globe after being reduced to sea-level,
should have occurred in the British Islands, and within three years of
each other.”
188
Judging from my own experience, derived from observations
during a long term of years, I should say that sudden thaws,
after frosts of some continuance—and yet more after frosts of
long continuance—are the occasions generally on which occur the
greatest depressions of the Barometer; and, what is more, that
the greatest elevations also, as well as lowest, mostly occur in
winter. This makes it of interest to notice how far this is the
case in the table of maxima and minima during the eleven years
1875—1885. It will be seen on inspection that the maxima
occurred five times in January, twice in December, twice in
October, once in February and once in May. The minima
occurred four times in February, three times in November, twice
in January, once in December and once in April. Perhaps this
will appear plainer when set out as under, alotting the three
usual months to each season :—
SPRING. SUMMER. AUTUMN WINTER.
Maximum... l ae ie 2 Pe etc}
Minimum... 1 nee Ores 3 mee rE
2 0 5 15
Thus, not only are the greatest elevations and depressions
clearly in excess in winter ; but with the two exceptions of one
high elevation in May and one depression in April, there are no
- extremes one way or the other to be found between the months
of February and October.
The mean height of the Barometer for each season on an
average of eleven years, which it may be useful to record, is as
follows :—
Spring sn hs “s 29°958
Summer ae ibe aie 29:°973
Autumn us esis EE 29-961
Winter sie bas See 30°010
——
189
TEMPERATURE.
From the subject of Barometrical observations I pass on to
consider that of Thermometrical observations. I went so fully
into the subject of temperature, considered generally, in my
former paper on the Bath Climate, that it is hardly necessary to
do more here than to combine the results of ten years’ further
observations with those of the first decade. The period, therefore,
now to be considered is one of 20 years, commencing with
1866 and ending with 1885 ; and there is the less occasion, also,
for going much into detail from the results varying but little
in the two cases. I shall confine myself chiefly to a statement of
results as regards the mean temperature of the whole term of
years and the temperature of the seasons.
The mean temperature of the first nine years will be found in
my former paper. The mean temperatures of each of the eleven
last years is as follows :—
ee ——
MEAN MEAN
YEARS, TEMP. YEARS. TEMP.
AGiGeliieit. oc baGieots PASE 2, o cay 48
1876... ... BLS 1882 ... .. 509
1877... .. 508 1883... ... 504
1878... ... 507 ise OT
1879... ww ATS 188... .. 502
1880... 502 Mean 2000 Sowa
eeeeee eee ee eee ee nena EEE
The mean temperature of the whole series of twenty years is
exactly the same as that of the first ten, which in my former
paper is set at 50°5. The variation also between the two
decades, taken separately, does not amount to one-tenth of a
degree ; so we may fairly consider the mean temperature of
Bath, at least in the lower part of the town, to have been
determined with tolerable correctness.
The year of highest mean temperature in the whole series is
1868, when the mean rose to 52°, The year of lowest mean
OG
190
temperature is 1879, when the mean fell to 47°°5, three degrees
below the average, and following the severest winter in the
series—that of 1878-79. .
’ Fourteen out of the twenty years had a mean temperature of
50° or upwards ; the remaining six had a mean below 50°.
With regard to the seasons, next to be considered, the following
table shows the mean temperature of each season, as deduced
from twenty years’ observations, together with the highest and
lowest means observed in each season—also the range :—
SEASONS. MEAN. HIGHEST. | LOWEST.
Spring eae 48°4 512
Summer ... 60°3 63°5
Autumn ... 50°7 52°3
Winter He 41°4 463
The warmest spring, and the hotest summer, in the series
occurred both in the same year, 1868, which year had also the
highest mean temperature of all the years. Of the summer of this
year (1868) I gave a detailed account to the Field Club shortly
afterwards,* and I need say nothing further about it here. No
such hot summer has occurred since in Bath. The nearest
approach to it was the summer of 1876 ; but the spring preceding
that summer was nearly 4° lower than the spring of 1868.
Looking to the summers generally it appears that the mean
temperature of that season was above 60° in sixteen out of the
twenty years, the four exceptions being 1879, and the three
consecutive summers of 1881, 1882 and 1883. In 1879 the mean
temperature of the summer was scarcely above 38°; it was a
notoriously wet and cold year throughout, of which also I gave a
full account to the Field Club in a paper published in their
Proceedings.
* Proceedings of Bath Field Club, vol.i., No. 3, p. 43.
+ Id, vol. iv., No. 3, p. 209.
191
With respect to the range of mean temperature in the several
seasons, it is worth noticing that while the ranges of Spring and
Summer are identically the same, the Autumn range, or
difference between the highest and lowest mean temperatures,
amounts to nearly 4°,—while in the winter season this difference
is greatly augmented, being nearly double that of any of the
others. Whether this is the case in other places I know not, but
it shows the great uncertainty of character that attaches to the
Winter season in Bath, and the matter seems to call for closer
investigation. For which purpose I annex a Table showing the
mean Winter temperature of each of the twenty years to which
this paper relates—
WINTER. MEAN TEMP. WINTER. MEAN TEMP.
1866-7 42°7 1876-7 461
1867-8 40°8 1877-8 42°8
1868-9 46°3 1878-9 364
1869-70 389 1879-80 375
1870-1 38°0 1880-1 39:0
1871-2 42°6 1881-2 43°0
1872-3 41°1 1882-3 43°6
1873-4 42°1 1883-4 44°38
1874-5 39°0 1884-5 43°4
1875-6 412 1885-6 38°1
Analysing the results of the above Table, it will be found
that the coldest winter in the whole series of years was that of
1878-9, when the mean temperature fell to 36°4; the next cold-
est being the winter following, that of 1879-80, scarcely more
than one degree higher than its predecessor, being 37°'5. The
two coldest winters, therefore, in the whole series were two
consecutive winters. a5
The mildest winter in the series was that of 1868-9, following
the very hot summer of 1868,.the mean temperature of that
winter being as high as 46°°3, or ten degrees higher than that of
192
the coldest spoken of above. The next mildest winter in the
series was that of 1876-7, its mean temperature being 46°],
or scarcely less than that of 1868-9.
It may be further remarked—and this perhaps is the result o¢
chiefest importance,—that thirteen out of the twenty winters
had a mean temperature above 40°, while there were but seven
in which the mean temperature did not rise to 40°, the former
being to the latter in a ratio of nearly two to one, so that,
perhaps, we should not be very wide of the truth in coming to
the conclusion that, though Bath winters are more variable than
the other seasons, they are as a rue mild.
I might add that the great range of the mean temperature of
the winter season in Bath, exceeding that of any of the other
seasons, is in keeping with the circumstance spoken of above,
when treating of the Barometer, viz., that the greatest elevations,
as well as the lowest depressions, of that instrument for the
most part occur in winter; for from this it follows that the range
of th Barometer is, as a rule, also greater in winter than in the
other seasons. I now pass to the subject of
RAINFALL.
In the annexed table are given the results of rainfall measure-
ments during the last ten years. Combining these with the
measurements of the preceding decade, 1866—1875, given for
the most part* in Table I. in my former paper on the climate of
Bath, the results of the whole twenty years may be summed up
as follows :—
The mean Rainfall (mean of 20 years) is 32:064 inches. I
* The above reservation has reference to the circumstance of the
first and last years in that Table being incomplete years. ‘The results
now to appear are those derived from the measurements of 20 complete
years 1866—1865.
: oreo | oaot| sore] ore | oor] cove | spac
618.€
L19.96
a>
lo}
Gt
fr
N
c
—
| ‘
|
|
|
|
L
L
| 1e9.8 | LOE
F6L-€ | RBI Ea zoee | stot | e6r-0 | eze.0 | cose | cer | tore | e161 9181
"E88 Yun buyjounusa, pun
‘QL81 Ys burowoumos apmap ay, fo wax yooo we ysuopy yova ur qynfurney
193
spoke in my first paper of the necessity for rain measurements
being continued for a long term of years “in order to determine
the true average fall at any particular place,” and this necessity
is clearly shown in the present instance. The average Rainfall
in the Institution Gardens, as determined by ten years measure-
ment, is set in my former paper at 29:986, or allowing for errors
at 30 inches. Now—at the end of 20 years, it is found to be
32-064inc., or more than two inches in excess of the ten years
measurement.
But this is not the only striking circumstance in the com-
parison of the two decades. It may further be observed that
the excess of rainfall is almost entirely confined to the latter
decade, so that in a general way the first decade may be called
a dry one, and the latter a wet one. In the first decade there
are only three very wet years, or in which the rainfall amounted
to more than 30 inches. In the second there were seven such
years, the fall in 1882 being more than 42 inches. This last
year was the wettest of the whole twenty; and not only that,
but in no other year did the rainfall attain even to 40 inches.
Other wet years were 1866, 1872, and the five consecutive
years 1875—1879, in all which years the rainfall was between
34:953 inches and 37°795 inches.
Thus, in consequence of most of the wet years occurring in the
second decade, the two decades are very unequal in respect of
rainfall ; the mean yearly fall in the first decade (1866—75)
being 30-504 inches, that of the second (1876—85) being 33°573 ;
the difference between the two being 3-069 inches.
The driest year in the whole series was 1870, when the rainfall
did not exceed 27 inches. The only other very dry year was
1875, when the rainfall as measured, was 24°890 inches.
Passing on to the consideration of the seasons. The following
table represents the mean, maximum and minimum rainfall
in each of the four seasons as the result of twenty years’
meaurement :—
194
MEAN, MAXIMUM. MINIMUM,
Spring oe 6 056 10°848 2°737
Summer ... 7°633 15°583 2 592
Autumn ...._~—:10°008 14°302 4°227
Winter Be. 8°785 13°388 4°830
It appears from this that, as a rule, Autumn is the wettest
season, and Spring the driest season in Bath. In the Rainfall
Table, deduced from the first decade, as given in my ‘former
paper, the inter season is shown to be the wettest ; but there is
not very much difference between the autumn and winter falls in
either table, and either season might prove to be the wettest in
any particular year.
Taking the seasons separately in reference to their extreme
character of wet and dry, it may be worth recording that the
greatest spring rainfall (10°848 inches) occurred in 1878, the
least spring rainfall (2-737 inches) in 1883.
The wettest summer (rainfall, 15°583 inches) occurred in 1879 ;
the summer of 1882 (rainfall, 14°701 inches) being nearly as
wet; the driest summer in the series (rainfall, 2592 inches,
occurred in 1870.
The greatest autumn rainfall (14:302 inches) occurred in 1885 ;
the least autumn rainfall (4°227 inches) occurred in 1884.
Hence the driest autumn in twenty years was succeeded by
the wettest.
The wettest winter in the series was 1869, rainfall amounting
to 13°388 inches. The driest winter was that of 1878, rainfall
being 4:830 inches, It is worth noting that 1878 was one of
the five consecutive wet years spoken of above ; but the heavy falls
were in the spring, summer and autumn months, especially in
‘the month of May.
In reference to wet and dry months, it may be observed,
195
Autumn as a rule being the wettest season, that there is not
much difference between the rainfall of September and that of
October ; and this confirms a remark I made in my former paper,
that “on an average, one of the two months of September and
“October is, comparatively speaking, a wet one, and the other a
“dry one. But which is to be wet and which dry is an even
‘“‘chance looking merely to results.”
The highest mean monthly fall in the results of twenty years
is that of January ; and it will be seen again on referring to my
former paper, that this same month presented the highest
mean fall’in the first decade. January, therefore, may well stand
as on an average, the wettest month in the year in Bath;
though September and October (or one of those months in
any single year) may make a near approach to it.
:: The absolutely wettest month during the whole twenty years
was. May, 1878, when the fall amounted to 7-060 inches; a
remarkable circumstance, May and April being the two months,
in which the mean rainfall (nearly the same in each case) is
lower than in any other months of the year. In only five instances
besides the above did it amount to so much as six inches.
The absolutely driest month in the whole series was July,
1885, when the fall was 0:210 inches. There was no month
absolutely without rain.
: This leaves little more to be said on the present occasion. I
have nothing further to state with respect to the temperature,
rainfall and humidity, of Bath compared with other places,
beyond what I stated in my former paper. Nor need I add
anything to what was therein said respecting the general
conditions of the Bath climate. I believe the results given in
that paper are as a whole correct. Of course the longer the term
of years for which the observations are continued, the more
trustworthy they become ; while there are anomalous states of
weather, in one or other of its aspects, sure to recur from time
to time during long periods, which it is of interest to record ;
196
while also they not unfrequently serve to correct former views
as to the causes that combine to bring about the very variable
states of weather characteristic of the English climate.
Summary of Proceedings for the year 1886-87.
Mr. PRESIDENT AND GENTLEMEN,—_
The thirty-first anniversary of the Club was held at the Royal
Literary and Scientific Institution, on Thursday, 18th February,
when after the usual routine business had been transacted, the
subject of the preservation of the recently uncovered Roman
remains was brought to the notice of the members by the Com-
mittee. The injury caused by their exposure to the vicissitudes
of the weather having been insisted on, a memorial to that
effect was adopted for presentation to the Mayor and Corporation
suggesting that some protection should be given to the whole,
either by enclosure beneath a suitable roof or covering, or at least
that the recently discovered “‘Altar” stone and other more delicate
and easily moveable portions of sculpture should be placed
without delay in the Museum, or elsewhere as may be deemed
advisable. This Memorial having been signed on behalf of the
Committee by the President, Vice-President and officers of the
Club was duly sent to the proper authorities, and courteously
acknowledged by the Architect of the works on behalf of the
Baths Committee, with thanks for the suggestion, which should
receive every consideration. With regard to the sculpture he
stated, that the stones lately uncovered had been partially pro-
tected, but that as to the temporary roof over the whole,
advocated by himself, the Committee considered it unnecessary,
unless the Corporation were willing to erect one of a permanent
character, which could not be undertaken before the removal
of the Poor Law Offices.
197
' Seventeen members having been brought together by a three-
lined Whip, the dinner, which had fallen through the year before,
was held at the Grand Pump Room Hotel in the evening, the
vice-president, the Rev. Preb. Scarth, in the chair.
After the usual loyal toasts, Mr. SKRINE, who was called upon
to give the health of the president the Rev. L. Blomefield, said
it was a duty as well as a pleasure to propose such a toast to
them. From the very commencement of the Club’s life, now
some thirty years ago, until the present time, it might well be
said of him éu es Patronus, tu es Parens. Ever ready to lead the
way and encourage the research of any interesting object of
natural history in our neighbourhood, he had earned our respect
and regard by the vigorous exercise of his intellect. If not
able, through physical weakness, to be with the Club in their
excursions and walks, yet his mind showed no lack of its former
strength, witness his recent admirable paper on the *“ Bourne-
mouth Firs,” and the numerous contributions to our “Proceedings.”
Let, then, his unceasing energy excite us never to rest on our
oars, but to work on and do our very best to distribute valuable
information on the subjects which concern the Club, and with
which we may be familiar. Without putting himself forward,
but showing that modesty which becomes a great mind, it may
be truly said of him, nihil tetigit quod non ornavit. Before sitting
down he must also give the health of the Vice-President, so well
known for his antiquarian lore, and so ready at all times to come
forward and support and promote the objects of the Club. He
was glad to see him among them that evening so vigorous and
well. For nearly 30 years he had been connected with the
Club, may he be so for 30 years more!
Mr. ScCARTH, in returning thanks, spoke of the advantage of
such clubs, and said that this one had taken up a portion of
work much needed in the neighbourhood.
* Proc. 1886, Vol. vi., No. 1, p. 39.
198
. After some more appropriate remarks, the health of the .
Treasurer and Secretary was proposed, and Mr. Scarth made
some remarks on the recently discovered “Altar” stone, and stated
that his interpretation of the figures differed somewhat from that
of Mr. Sayce (vide Vol. vi., No. 1, p. 81),
' The Rey. J. B. Medley, the Rector of Orchardleigh, being the
only one able to be present of those gentlemen from whom the
Club had received hospitality and assistance during their excur-
sions, facetiously returned thanks for his health in the character
of the country mouse visiting the town mouse.
AFTERNOON MEETINGS.
The attendance at these meetings has been encouraging, the
small room at the Institution on some occasions being so inconveni-
ently crowded as to induce the Club to migrate on one afternoon
to Christ Church Hall; an experiment not entirely satisfactory
owing to its size and imperfect acoustic properties when only
partly filled.
The afternoon of Wednesday, March 10th, was given up to
Geology and Botany ; the first paper was from Mr. Horace B.
WoopwarbD, of the Geological Survey, on the “Geology of Brent
Knoll” (vide p. 125). Owing to the absence of sections, the struc-
ture of that remarkable hill, rising some 400ft. from the alluvial
flats of the Burnham level, has always been somewhat doubtful,
especially as regards its lower portion. Hitherto the sequence
of the beds has been, Inferior Oolite on the top, Midford Sands
next, then Upper Lias, followed by Middle Lias and Lower Lias
at the base. From recent discoveries made by Mr. Woodward
in 1885, he has now found out from fossil evidence that the
Lower Lias has no existence at the base of the hill; but that
the basal portion consists of Middle Lias Clays. His paper
then went on to show the bearing of this thickness of the Lias
upon the coal question to the south of the Mendips, and concluded
ee
-'*
199
with a descripton of the agencies at work in the formation of
such outlying conical hills as Glastonbury Tor, and the one in
question. Mr. Woodward was unfortunately prevented from being
present himself, but was enabled, by the kind permission of the
Director General of the soak Sue Survey, to forward the paper
for the Club.
Mr. McMurrrie said these notes were an important addition
to our knowledge of local geology, and the Survey deserved
great credit for so readily acknowledging an error they had
formerly made in mapping this knoll—a readiness which had not
been conspicuous on former occasions when the work of amateur
geologists did not exactly accord with their views. As regards
the prospects of coal, of course this discovery of the thickness
of the Liassic beds at this point did not affect the question
as to the existence of coal south of the Mendips, but merely as
to the depth at which it might be won. Bearing in mind too
that the Lias thinned out near the Polden Hills, and that the
New Red Sandstone came in there, the depth might not after all
be so great. Moreover, a sinking for coal would be made nearer
the Mendips. Mr. Skrine (who was in the chair) proposed a
vote of thanks to Mr. Woodward for having given the Club the
benefit of his notes.
Canon ELLACOMBE then read a short paper on “ Place Names
derived from Plants (in the neighbourhood of Bath),” stating
that the process of naming places by our early ancestors was a
very simple one, for like all uncivilised people they chose out
their settlements in the places best fitted for their requirements,
where the necessaries of life, water, wood and shelter could be
most easily procured; and naming their places from some
distinctive natural feature, those of trees and plants would
readily present themselves for the purpose of place-names. It
was then his endeavour to show that trees and plants enter
largely into place-names, and that the latter also tell us something
about plants. Taking forest trees first, how many places derive
200
their name from the British oak, ash, elm, beech, birch, alder,
box, &c.? He knew of no places near Bath, however, derived
from flowers or fruit; but from more humble plants, e.g., the
nettle, several instances were given. Claverton, near Bath, was
supposed by a high authority to have derived its name from the
water lily, and was originally written Clat-ford-tun, or the town
at the ford of the clote or lily. This derivation, though extremely
pretty, he thought was incorrect, for clofe he considered to be the
water-bur, ditch-bur, or reed-bur, and not the water lily. This
view as regards Claverton was not acceptable to Mr. Skrine, who
contended earnestly for the more flowery and poetical derivation,
and had not failed to fortify himself with the following letter
from Professor Earle, who maintained the correctness of his
former view of the connection of Claverton and water lily by
reference to some learned authorities :—
“The argument for the Water Lily claims no higher a rank than pro-
bability, and it is of the nature of such arguments to be in some
degree matter of opinion. My opinion is strong in favour of the
connection of Claverton with the Water Lily.
Our early authorities are Glossaries of Latin and English, ranging
from the 8th to the 12th century. In these we find the word clate
representing various Latin names of plants, Blitum, Tubera, Blitum
vel Lappa, Amorfolia, Philantropium, Cliton, all, so far as we can
gather (for the identity of these plants is obscure), large leaved plants.
The name of all these which we have most confidence in recognising
is Lappa, which is our Burdock, and the fruit of which is still called
clotbur, where I have no doubt clot is the old clate. But the Glossaries
contain another entry besides all the above, viz., Ovylapation “‘aneo
cyunes clate,” ie. one sort of clote; thus informing us that
clate was used very freely for a large diversity of plants, and that all
the above Latin names are not a variety of names for the same or
nearly the same plant, but rather for so many different plants.
The name of clate being then used with so much latitude, we may
claim it for the Water Lily without denying it to the Burdock. And as
one part of the evidence in favour of the Burdock consists in the
201
modern name of its fruit, so the fact, stated by Barnes, that the Water
Lilies of the Stour are called clotes, must be held good evidence for an
ancient connection between clate and Water Lily. For as on the one
hand we cannot regard our Glossaries as a complete record of the case
of clate, so on the other we must remember that the old English of
the Saxon period is now best represented by the dialect of Dorset,
The Saxon form of Claverton is Clat-ford-tin, and there is a Clatford
in Hants near Andover, where the clat is preserved in its early form.
Does not the association in these instances of clate with water speak
in favour of a water plant with big leaves? And does not the natural
fact which you mention of the habitat of Water Lilies in the Avon at
Claverton lend added force to this presumption ?
I think these are the chief points of the argument ; but you know
in twilight men interpret objects diversely, and if Ellacombe likes his
idea better, he has a right to prefer it. One thing, however, I think is
quite out of court, and that is the Clover.”
Notwithstanding this letter, Mr. Ellacombe, in reply, said that
his opinion had not been in the least shaken, and he thought
that the absence of the water lily from old writers, and the fact
that it was unknown in England till within the last 100 years,
were strong arguments in his favour.
The Rey. S. SHaw exhibited a plaster cast of an inscription
found on the N.E. buttress of his tower during the recent
alterations at Twerton. The tower’s date was about the 13th or
14th century, and the inscription was probably not earlier than
the 15th. The inscription was a complete puzzle to antiquaries
and he sought a solution from those present.
On Wednesday, Dec. 8th, there was a large attendance of
members and their friends on the occasion of the President
opening the winter session with an obituary notice of their
late distinguished mycologist. Regretting that age and its
attendant infirmities had prevented him from taking that chair
for a long time past, he said that he was extremely anxious
to come before them that afternoon in consequence of the great
202
loss. their Society had sustained by the death of Mr. Christopher
Edmund Broome. He desired to speak of him as an acquaint-
ance who had been his friend for a large number of years, and
more particularly to speak of him in reference to his connection
with that club. Mr. Broome was the oldest friend he had,
relatives excepted, and he supposed he had known him for nearer
‘60 than 50 years, their acquaintance taking its origin from the
circumstance of his going, when he was a quite a young man, to
be pupil to a clergyman who was curate of the parish adjoining
his own parish in Cambridgeshire. Then he went to Cambridge
University and graduated in 1836, but after leaving the University
they only fell in with each other at intervals. After a time he
took up his residence at Elmhurst, Batheaston, where he was
living when he (the speaker) first came to Bath, in 1850, and
where he resided until his death. Mr. Broome was one of the
original members of the Bath Field Club, of whom none remained
now except the vice-president and the speaker. But Mr. Broome
was more than an original member, and he would not be far from
the truth in saying that he was the joint founder with himself.
It was true he originated the idea, but if it had not been for Mr.
Broome it would never have received its ultimate shape.
Mr. Blomefield then described the origin of the Field Club,
and spoke of Mr. Broome’s great activity in research, and all
matters connected with natural history, and especially botany ;
also of his rare and valuable collections. He described his
great energy and capacity for work, and attributed his death
to incessant labour and over fatigue of both mind and body.
The death of their much esteemed member read a lesson for all
of them, a sharp lesson, but a most important one—to work to
the full extent of their energies, but not to the injury of their
health. Few members of their Club, he imagined, needed to be
cautioned not to work too hard, and he felt there were not a few
to whom the first half of this advice would be given with
difficulty. They could ill spare one so active at home and
———
203
abroad, as their late member—would anyone, come forward .and
take his place? He asked them to take for their motto, that
which was the guiding star of the whole life of their departed
member—‘ Work while it is day.” The President then read
extracts from the will of the deceased, which he had received
from the hon. secretary of the Royal Literary and Scientific
Institution, bequeathing to that Institution all his books (on.the
fly page of which he had written his initials, “'C.E.B,”), consisting
of works on a number of sciences, which were enumerated,
and his’ herbarium; and also stating that if the bequest of
his fungi made to the British Museum was not accepted, it
should be given to the Institution. This, however, had been
accepted. 3 ,
The Rey. Predendary ScARTH also expressed his sincere
sorrow at the loss they had sustained, and thanked the President
for the excellent memoir which he had placed before them. He
further spoke of his ‘personal friendship with Mr. Broome. |
The PRESIDENT then called upon the Rey. Prebendary EARLE
to read a paper on the “Traces of the Saxon period in Bath
and the neighbourhood.” Before doing so, the Prebendary also
said a few words with reference to the remarks of the President
upon the late Mr. Broome, and added that he was sure he
would be expressing the sentiments of many when he said
that Mr. Blomefield’s memoir of his friend had touched a very
deep chord in their feelings. He then passed on to his subject
(vide p. 153).
The third meeting was held at the Institution, on Wednesday,
January 12th, 1887, when, in the absence of Mr. Skrine, the
Secretary read certain “ Letters illustrating the Battles of
Claverton and Lansdown,” one written by Lord Hopton (then
Sir Ralph), the other by Col. Slingsby, both Royalists (vide p. 167).
In the discussion which followed, Mr. GREEN said he had always
felt sorry that Mr. Skrine had made a former. contribution on
this subject, as printed in 1878, without. having read, or-without
204
having noted, the account of the Battle of Lansdown as printed
in 1875. He had, however, perhaps better not remark further
on this. The letter now read to them was not new, as he had
used it very much, practically embodied it, in his Lansdown
paper, and duly gave the reference to it, where it could be found.
Perhaps, again, a notice of this and a comparison should have
now been made, The whole of these MSS. had just then been
arranged, and he thought he was the first who had referred to
them. It seemed that Mr. Skrine, from his minute knowledge of
the roads about Claverton, had detected that the Royalists could
not have been at Monkton Combe as stated; and looking up
this reference had found the place therein written Monkton
Farleigh. The relation of this march from Frome was epitomised,
being introductory, not as giving full particulars, but merely to
bring both forces to Lansdown. The object in view was the
Battle on Lansdown. Writing at the time full of Somerset, the
more familiar name of Monkton Combe had been substituted
and passed unnoticed ; it was evidently wrong, as it placed both
forces on that side of the river. But it was a slip, a clerical
error, not an error affecting any statement or fact. The para-
graph now as it stood, was meaningless and obscure ; Farleigh
not Combe was clearly intended, as by substituting Farleigh for
Combe all became clear and the account read on correctly. The
narrative of the Lansdown fight was taken from his full
manuscript of the Civil War as relating to the whole county, and
probably a reference to this would show the name written
Farleigh*. The Royalists passing round by Bradford bridge were
met at Monkton Farleigh by Waller’s advanced guard which he
had passed over the “ford” below Claverton, his main body
being drawn up on Claverton Down. Beaten back and losing the
* The Secretary has since been informed by Mr. Green that on
referring again to his original MS. of the Lansdown fight he finds
therein— Monkton Farleigh and not Monkton Coombe.”
205
ford, he then retreated his whole force down the hill and through
Bath to Lansdown. The Royalists keeping the opposite side of
the river passed on as related, and rested that night within
Batheaston bridge. He was glad to have the oversight corrected,
although no great harm had been done.
The fourth afternoon meeting was held at the Institution on
Wednesday, Feb. 9th, when the ‘‘ Note on the Ham Hill Stone,”
contributed by Mr. Horace B. Woodward, of the Geological
Survey, was read by the Secretary. The object of the com-
munication was to define the position of that celebrated building
stone in the Inferior Oolite series, the conclusion being that the
Ham Hill stone belongs to the upper part of the Midford or
Inferior Oolite sands. Mr. McMurtTRIBg, in the discussion which
followed, stated that he was not prepared to come to any definite
conclusion as to the exact position of the stone in the Inferior
Oolite series, as his attention had not been especially directed to
those beds. Hitherto the information respecting them afforded
by the Geological Survey was very meagre, and he congratulated
the Club on hearing this contribution to the subject from one so
well qualified to deal with it as was Mr. Woodward, who had
worked so much in our neighbourhood. He reminded the
members what a different aspect these beds put on in different
parts of the country, comparing their facies on the north of the
Mendips with that on the south, where they were more largely
developed and so different in appearance—instancing their thin
representatives in the neighbourhood of Frome and Mells,
‘resting upon the Carboniferous Limestones ; and their thickness
at Doulting and Ham Hill, both of which places were so
celebrated for their building stone. The CuarrMan, in giving
the thanks of the members to the author of the paper, stated
that everyone must be interested in this stone, who had
seen how much it had been used in our churches for
decorative and other purposes, and how durable it was. As
to his own church he stated that there was a tradition that the
P
206
stone for the tower came from a quarry near Langridge and not
far from Battlefields.
The SEcRETARY having been asked for his view respecting
Mr. Woodward’s “Note,” stated that he was not prepared in
any way to criticise it. The brachiopod—Rhynconella cynocephala
—which the writer said he had found in a small section on the
right hand side of the road, on the last rise before coming to the
main quarries, had subsequently been found there by himself on
two occasions, one being during the excursion of the Club to.
Ham Hill last year; and unless the identification of strata by
their fossil contents was an exploded theory, the discovery of
this peculiar shell (of which specimens were shown) certainly
fixed these beds as coming in somewhere at the base of the
Inferior Oolite series. Alluding to the chairman’s remark about
the locality whence the Oolite for the Tower of Bitton Church
came from, he asked for some definite information as to the
quarries whence the Bath Abbey was hewn; Mr. Chas. Moore
had informed him that the now disused quarry (called Shepherd’s)
on the right of the Entry Hill road supplied the material.
Some sections on the black board illustrated the position of the
Ham Hill Stone as compared with the Inferior Oolite beds at
Leckhampton Hill; and a block of the hard nodular bed at the
base of the workable “Gray beds” at Ham Hill, resting im-
mediately upon the Yellow “ Brim Sands” was exhibited. The
Secretary reminding the members that a very large block of
this stone had just been brought to the surface when they visited
the quarries in September last ; Mr. Trask, the owner, who was
then present, stating that it was rather an uncommon thing to
see this bed exposed, and promising to send a specimen to the
Bath Museum. This he has since kindly done.
EXCURSIONS.
Sherborne Abbey and Park, May 4th. The Club was most fortu-
nate in having so fine a day for the first excursion of the season
to Sherborne. Tuesday was simply a perfect May day, and as
the members, comfortably “located” ina saloon carriage, ascended
the slope of the Mendips and found themselves on the watershed
at Maesbury, looking over the Somerset moors, with a bright
sun and a clear sky everywhere around them, they thought that
the ‘merry month of May” was after all not merely a tradition
of the past, but a bright possession of the present. Glastonbury
Tor, to those unfamiliar with the curious freaks of denudation,
stood out like a huge conical tumulus on the horizon, appearing
and disappearing as the train swept down the winding descent to
Shepton Mallet, and the Polden hills were seen, a faint blue
bank in the distance. The trees were hardly yet in full leafage,
and the grass, owing to the cold nights and late season, was very
scanty of growth; but, notwithstanding this, the rich, rolling
Somerset meadows through which the train passed to Temple-
combe looked as only Somerset meadows can look—verdantly
luxuriant. At Sherborne the members were met at the station
by the viear, the Rev. W. H. Lyon and his son, and were at once
conducted by the south porch of the Abbey to the King’s School.
Here one of the masters, the Rev. A. Wood, showed them over
the school whilst the vicar attended the mid-day service in the
Abbey. From the schoolroom, erected within the last eight
years, containing an organ at one end for concerts (music being
one of the fine arts much cultivated at this school), all the
various portions of the buildings were visited in detail. The
boys’ studies—once the cells of the Benedictine monks, whose
monastery formerly stood on the north side of the Abbey, and
has now been appropriated for the use of the school ; the crypt—
with its Norman piers; the old schoolroom—built 1670, with the
statue of King Edward VI. at its east end, transferred from a
208
more ancient schoolroom to its present site, well known to old
Sherborne boys, as they “ capped” the image of royalty—better
known, perhaps, than the Latin lines beneath :—
En! tibi, Flos juvenum, Britonum Decus, Inclytus orbis
Splendor, Appolinei Delicizeque chori,
* Gymnasium hie pueris statuit, gratumque Minerve
Ut gratis discant—discito—gratis eris.
Outside and over the gateway leading to the court in which this
hall stands, the following two Latin lines record the foundation
of the school :—
Edvardi impensis patet hic Schola Publica Sexti,
Grammatice cupidis, nobile Regis opus.
From the hall up to the sick chambers curiously built amid the
stone groining of what was the Lady Chapel, thence to the
admirably fitted up library, the ancient Guesten hall, and through
the chapel to the museum on the opposite side of the road.
Formerly belonging to a silk factory, this well lighted room con-
tains a very good collection of the characteristic fossils of the
neighbourhood, principally from the Inferior Oolite, and has
evidently had more attention bestowed on its contents than most
school museums. Mr. Wood briefly indicated from a geological
section of the neighbourhood the formations recently traversed in
descending order from the Oxford Clay and Cornbrash at Temple-
combe to the Forest Marble, Fuller’s Earth, Fuller’s Earth Rock,
and Inferior Oolite on which Sherborne is built; the only
peculiarity being that the Great Oolite so thick at Bath had
thinned out in this direction altogether, and was probably
represented by the Forest Marble. The Secretary supplemented
Mr. Wood’s remarks with a few words as to the formations
successively passed over on the morning’s journey. Leaving the
Lower Lias of the Bath valley they had passed through the Upper
Lias in the cutting below Devonshire buildings, the Sands of
the Midford tunnel, on to the Inferior Oolite beyond, over the
209
anticlinal of the Mendips, with the Mountain Limestone dipping
successively north and south, until they reached the levels on the
other side, and once more came upon the Lias. He then drew
especial attention to the series of Ammonites from the Sands
and the Inferior Oolite; alluded to the researches of the late
Professor Buckman, so ably continued by his son, which had done
so much to clear up the vexed question as to the true horizon of
the Sands, and he ventured to think that their researches went
far to establish the fact that these Midford or Yeovil Sands put
on a facies more Oolitic than Liassic. Having thanked Mr. Wood
for his kindness in showing them over the famous school, the
members entered the Abbey at the west end under the guidance
of the vicar. Before doing so the remains of an old doorway on
the north side of the present one were pointed out as containing
traces of Saxon work, and attention was called to the picturesque
effect of the painted window at the east end as seen through the
open portal, The contrast from the glare outside to the subdued
light of the interior of this noble Abbey was most restful to the
eye. ‘The richness of the carving in pannelled pier and vaulted
tracery, and the soft blending of the whole in one harmonious
warm tint, due to the quality of the far celebrated Ham Hill
stone, renders this interior probably unequalled in beauty. The
vicar, notwithstanding the sad affliction in the almost total loss
of his eyesight, was an excellent expositor of all the architectural
details. Recently he has had the gratification of taking a pro-
minent part in the restoration of the tower, and pointed out some
Norman pier work on the north wall of the lantern, recently brought
to light. Scarcely any portion now remains to be restored ;
almost everything has been done through the liberality of the
Digby family that was necessary. There still, however, remains
the anomaly of the Lady Chapel being used as a sick ward to be
done away with, and then this Abbey will be even more perfect
than it is now. A visit was paid to the belfry, containing a peal
of eight bells. The tenor, called “Great Tom,” the gift of Cardinal
210
Wolsey, and the smallest of the seven brought from Tournay and
presented to various cathedrals in England, bears the inscription ;
By Wolsey’s gift I measure time for all ;
To mirth, to grief, to church I serve to call.
The bell rung on the alarm of fire, and from its shape giving out
a peculiar sound, has the following inscription :
Lord, quench this furious flame !
Arise! run! help! put out the same.
The panoramic view from the top of the tower, of the park,
town and surrounding neighbourhood, was much enjoyed by the
few who were energetic enough to make the ascent. A cordial
vote of thanks was given to the vicar for his able guidance, the
members parting with him at the south porch and turning their
steps to the park. The lake looked its best in the bright sun-
shine, dotted here and there with swans sailing out from beneath
the shade of the fine overhanging trees. Having inspected the
outside of the house built in the shape of the letter “ H,” the
cross part of which is said to have been erected by Walter
Raleigh, and the architectural features of which have not much
to attract attention, they wandered on to Walter Raleigh’s seat
and tree (an elm), the traditional scene of the pipe and flagon
of beer anecdote—and finally found themselves admitted, by the ©
civility of the gardener, to the precincts of the old castle, Bishop
Rogers’ once famous fortress, now a picturesque ruin, with here
and there traces of the once rich Norman mouldings in column
and window tracery, characteristic of his period. Several of the
members now returned to Bath by an early train, whilst others
remained to dine at the Digby Hotel.
Southerndown and Ewenny Priory, June Sth, 1886.— The
members (14 in number) who met at the G.W.R. station on
Tuesday, June 8th for this excursion were much indebted to
Mr. T. Graham for the arrangements he had made with the
company, whereby they were enabled to break their journey at
211
Cardiff or elsewhere. Leaving Bath by the 10.18 train, and not
finding much to interest them during the earlier portion of the
morning, in spite of the well known custom of the Club to avoid
politics, the burning question of the day ‘‘Home Rule” unavoid
ably cropped up, and a surprising unanimity prevailed with the
representatives of both sides of political thought in the satisfac-
tion felt by the news of the Government defeat by a majority of
30. At the Patchway station, however, interest was concentrated
upon the great works in progress there in connection with the
Severn Tunnel; the deep cuttings at the sides made for the
double line of rail revealing fine sections of Lower Lias and
Keuper Marls. Just beyond the station, and before approaching
the entrance to the new Patchway tunnel, a thin section of the
Rhetic Bone Bed has been exposed lying on the Light Green
Marls. And the “tips” from the blastings in the tunnel show
many interesting specimens of Millstone grit (containing curious
spherical concretions similar to those found in the Lias near
Bitton whilst making the line there, but in this case siliceous) of
Limestone and a coarse and fine Conglomerate. Though goods
trains have passed through the Severn Tunnel from the other
side the passenger traffic is not yet in working order. Passengers,
who are sadly inconvenienced by the present break at New
Passage, anxiously }ook forward to the completion of this great
undertaking which has already cost about two millions of money.
Arriving at Cardiff about 1.30 the members were met by Dr.
Vachell, President of the Cardiff Naturalists’ Society, and Mr.
Gavey, the Secretary, and at once conducted to the Angel Hotel,
whence, after lunch generously provided and most thoroughly
appreciated and an ascent to the roof to see the fine view thence
of the town and neighbourhood, they went to the Museum and
Free Library close at hand. The principal object being to see
the Rheetic and other fossils from the neighbourhood, time did
not admit of more than a cursory glance at the rest of its
contents. At half-past three a start was made for Llandaff, not
212
before cordial thanks were returned by our Vice-President, the
Rev. Preb. Scarth, on behalf of the Club to the representatives
of the Cardiff Naturalists’ Society for the hospitality and courtesy
shown to the members, and a cordial wish that they would give
the Bath Field Club an opportunity of returning their civility,
and of showing them some of the objects of interest in their
own city. Under the guidance of Mr. Storrie, the able and
intelligent Curator of the Museum, some of the party proceeded
on foot to Llandaff, whilst the rest preferred the more easy, if
less dignified, method of riding on a bus. On looking back
after crossing the fine bridge over the Taff, the Marquis of Bute’s
castellated residence was seen standing out clearly defined in
all the minute details of its architecture and guilding against
the back ground of a black thunder cloud. A slight detour was
made from the main road through the Sofia gardens, the out-
lying district of Canton passed through, and a path to the right
led through pleasant fields to Llandaff, distant about a mile and
a half. Before crossing the last stile a lovely view of the
Cathedral was seen, framed as it were in the limbs of a venerable
ash tree, which must have seen 200 winters at least; the crocketed
spire on its S.W. tower and the Perpendicular pinnacles
of the N.W. standing most picturesquely out of the surround-
ing foliage. Entering by the north porch and passing in to
the nave, the simplicity and unity of the interior was the first
and most noticeable feature before the various details unfolded
themselves ; then the eye was attracted by a curious and most
unhappy series of horizontal graduated pipes projecting over the
stalls from the organ, like long and short post horns held by
some invisible hands; then passing on to the colours of the
41st Welsh Fusileers finally rested with pleasure on the view
of the Lady Chapel seen through the fine Norman arch at the
east end of the choir. Mr. Prichard, the Architect and restorer,
being prevented from meeting the members through illness, they
were severally indebted to Mr. Storrie, the Verger, and a “Sketch
EE EE ae
213
of Llandaff Cathedral by John Taylor,” for particulars of the
structure ; from these various sources of information it was
gleaned that the present building was mainly the work of Bishop
Urban, about 1120, whose work may be recognised in the N.
and §S. doorways and the choir arch and some portions of the
external walls. The pillars of the nave and choir and the W.
frent are later, about 1220; the Lady Chapel is still later in date,
and the Chapter House on the S. is advanced Early English,
square with a central pillar. The tower on the N.W. was
built by Jasper, Earl of Pembroke, 1485, and is similar in its
overhanging pinnacles to that of St. Stephen’s, Bristol, and to the
one at Cardiff. The S.W. tower has been recently re-erected,
and the whole of the careful restorations, completed in 1869 under
the skilful hands of Messrs. Prichard and Seddon, give general
satisfaction. There are many monuments, amongst them two are
worthy of special mention, the one at E. end of N. aisle, an
altar tomb with a knight in armour, said to be that of Sir David
Matthew standard bearer to Edward IV. at the battle of
Towton, 1461, and murdered by a Turbervill ; and another at the
N.E. of the nave to Sir William Matthew and Janet his
wife, two fine alabaster figures, 1528—1530. The wood-work of
the stalls, cedar wood inlaid with oak, box and lignum vite, are
very beautiful. As afternoon service was just about to commence,
the members passed by the well, the water of which was level
with the floor, outside round by the cross erected to the memory
of Dean Conybeare and ascended the table land immediately
N. of the Cathedral, and wended their way through Fairwater to
Ely station, about one mile distant ; here the train was taken for
Bridgend, and after a drive of five miles the barren uplands of
Southerndown were reached, and the Marine Hotel and some
neighbouring houses received the members for Tuesday night.
Wednesday, June 9th.—Some of the younger and more
enthusiastic members rose early on Wednesday morning and
found their way to the beach in spite of the stone walls which
214
run down in all directions seawards—small proprietary rights
sadly interfering thereby with the roaming instincts of the free
Briton. Looking upwards from the yellow sands a very fine section
of Lower Lias beds about 250ft. in height are seen from summit to
base. The horizontal reefs extend to low water mark, the
lowest of them being a blue coarsish crystalline limestone, its
outer surface roughened with angular and sub-angular pebbles of
Chert and Mountain Limestone. Fossils seemed scarce in these
lower reefs, but blocks with impressions of Ammonites Bucklandi
were scattered about under the cliff, probably fallen from higher
beds above. The strata were nearly horizontal with perhaps a
slight dip landwards. After an early breakfast a start was made
at 9 a.m. for Sutton, Mr. Storrie, who had come all the way from
Cardiff, kindly acting as guide through the day. Following the
cliff road by the farmhouse of West, before descending to the
sea level a halt was called at a road section on the left, where
the Sutton stone was first seen and many characteristic fossils
were found on the heaps of weathered blocks lying about, e.g.
Pecten Polluw ; Ostrea multicostata ; Cardinia Suttonensis
(Tawney), &e., &c. Passing still further downwards another
section on the right just above some houses was visited, it was
here that the Sutton stone was originally quarried for building
purposes. Standing on one of the “ tips,” now grass grown, the
Secretary gave a short description of the geology of the district,
and the discoveries made here by their late lamented brother
geologist, Charles Moore. ‘They were standing (he said) on
that remarkable formation called the ‘Sutton stone,” so named
from the locality where it was first worked—the question was,
to what particular position in geological sequence these beds
belonged—were they representatives of the Rheetic series ? a view
once held by a very able geologist, now passed away to the
majority, (his friend E. B. Tawney), but a view which he, the
Secretary, knew had been given up at the latter period of his life
—or were they representatives of the Lower Lias—the Ammonites
215
angulatus zone? The latter was the view held by Charles
Moore; than whom no one could be better able to form an
opinion. The Rhetic theory had recently been resuscitated by
Messrs. Tomes and Lucy based principally on coral evidence. A
re-examination of the geology of this district was therefore
necessary, and this excursion had been planned with this object.
A great alteration had taken place in the lithological character of
these beds,—as could be readily seen by comparing the speci-
mens before them with the Lias through which they had passed
on their journey yesterday—this rendered their correlation so
difficult. Those however familiar with the Secondary rocks in the
Mendip area must be struck with the practical identity of these beds
with those at Shepton Mallet, both as to their appearance and fossil
contents—the latter were admittedly Lower Lias. Indeed when~
ever the Liassic beds rested uncomformably on the Carboniferous
Limestone this alteration (as Charles Moore had pointed out) has
taken place. Similar conditions prevailed in this district, on looking
seawards the members would perceive the reefs of Carboniferous
Limestone with the Sutton stone resting uncomformably upon
them, the high range of hills at their back were a like formation
and throughout this neighbourhood those beds resting on these
Palzeozoic rocks were much changed in structure. What caused
this was still an open question, the evidence of igneous rocks
in close proximity could not be adduced as a reason here, as it
had been across the water—however the fact of their alteration
remains, so that the fossil contents of these beds were the only
safe guide to their place in the geological series—members
had an opportunity of winning their spurs.”
The carriages being rejoined below they drove past the mouth of
the Ogmore and on to Ogmore Castle, a picturesque ruin of which
not much beyond the old keep and a portion of the outer walls
remain, situated on the river Ewenny crossed here by stepping
stones. The view of the yellow sand hills at the back across the
Ogmore framed in one of the old windows was most picturesque. A
216
two-mile drive landed the party at Ewenny Priory. Colonel Turber
vill, notwithstanding the early hour of arrival, was ready to
receive the members and to show them over the Priory Church and
grounds. Entering by the S. door into the chancel it was at
once seen that no ordinary hand had been busy with the restora-
tion of this perfect specimen of early Norman work. The
Presbytery or chancel is simply perfect and one of the purest
specimens of Norman work in 8. Wales. The floor has been
recently covered with encaustic tiles, modern reproductions of
the various coats of arms belonging to the noble families of which
traces have from time to time been discovered, the three-light
Norman window at the E. end has been opened and various
other restorations recently carried out. From Colonel Turber-
vill’s description and from the account of the Priory by Mr.
Freeman in the Archzologica Cambrensis, 1857, the following
history was gathered :—
It was originally a Norman fortress built by William de Londres,
one of the twelve knights who with Fitz Hamon invaded
Glamorgan and who built Ogmore Castle. In 1141 it was added
as a cell to the Abbey of St. Peter at Glo’ster. The Priory
belonged to the Benedictines and after the dissolution passed to
the Carne family and afterwards by marriage to the Turbervills.
Freeman considers the Priory Church highly remarkable on
several grounds, and to be one of the best specimens of a fortified
ecclesiastical building—the union of Castle and Monastry in the
same structure— and that it exists very nearly as it was originally
built. The Church was cruciform with central tower very massive
—when perfect there was a nave with N. aisle—N. and S.
transepts, latter only now remaining with eastern vaulted chapels
now destroyed, and presbytery. The nave originally formed and
now forms the parish Church, the choir, the presbytery and their
appendages formed the church of the Priory. The vaulting of
the Presbytery, Freeman writes, is one of the rare instances of
Romanesque on so large a scale in England. Over the two
217
western bays is a barrel vault, the third and eastern has groined
cellular vaulting—the S. transept has three round-headed
lights at the S. end, an arcade of seven arches approached by
a stone newel staircase in the S.W. corner leading to the
tower belfry, and contains the supposed tomb of the founder, on
which is a floriated cross with the following inscription round it :—
“Tei gist Morice de Londres le foundeur,
Dieu lui rend on labeur Am.”
Several other incised slabs of later date are let into the floor
at the S. end. Entering the nave through the S. arched
doorway lately opened out, the massive Norman cylindrical piers,
with plain imposts on the N. side instructive characteristics
of English Norman (as Freeman writes) were pointed out, also
the fine oval Norman font at the W. end, and the 18th century
plain tablet to a local blacksmith in the S. wall adjoining
with the following appropriate inscription :—
“Underneath
“ Lieth the body of David William,
“of this Parish, who died the 16th of
“March, 1742, aged 57.
““ My sledge and hammers lie decay’d,
“My fires extinct, my force allay’d ;
“My vice is in the dust confin’d,
“My coal is spent, my irons gone ;
“ My nails are drove, my work is done.”
Passing through the N. door to the outside the remains of the
N. transept were seen, also the foundations of two of the
chapels E. of that transept. The domestic buildings of the
Priory were on the S. side and remained nearly perfect till about
the beginning of the present century. A large portion of the
enclosing wall remains with two gateways ; on passing out of the
S. door a broken slab with the following portion of an inscrip-
tion has lately been discovered :—
Hic jacet ..... . DeLon. .. +.
218
Evidently the cover of a tomb to one of the De Londres. Colonel
Turburvill having most hospitably invited the members to lunch,
the spare time was occupied in wandering through the grounds
and following the course of the ancient walls; the curious
dovecot in the E. wall, the S.W. gateway, the kitchen
garden enclosed on three sides by the old ramparts and the N.
gateway were the chief objects of interest. The Secretary
likewise in company with Mr, Storrie took a few of the members
more especially interested in the subject to see a geological section
about a mile distant on the Brocastle road, an account of the
result of this visit is appended :—
Brocastle Section—In a paper recently read by Mr. Lucy before
the Cotteswold Naturalists’ Field. Club, and published in their
Proceedings for 1884-1885 (p. 257), an attempt is there made
to revive Mr, Tawney’s theory of the Rhetic age of the Sutton
stone Conglomerate, and to show that Charles Moore was in
error in supposing it to be of Lower Lias age, and had mistaken
one bed for another. In his paper on Abnormal Secondary
Deposits (Quarterly Journal Geological Society, Vol. xxiii., p. 521), a
section is there given at Brocestle, with a description of “a deposit
of Conglomerate” found there resting on the Mountain Limestone
immediately under the soil, the Liassic character of which he
brought forward abundant evidence to prove. At p. 257 of Mr, Lucy’s
paper—with a view of rebntting this evidence of the Liassic age of
the Conglomerate—a statement is made that “it was clear (to the
writer’s mind) that it was merely a large mass of drift ”—whatever
this may mean. It was then to ascertain the accuracy of this view
that the visit was made. About a mile from the Priory on the S.
road to Brocastle, just at the top of a slight rise, and nearly opposite a
road section on the right-hand, a gate on the left led into a field at
the top corner of which, close to the hedge bounding the road on the
S., Moore’s section was found. There could not be any doubt of this,
as the Secretary had the original map used by that Geologist on which
the spot was marked. The quarry having long been disused was of
course much grown over ; but the E. side revealed the section sought
for. There immediately under the. turf.were loose blocks of bluish
219
Conglomerate full of cavities on the exterior, with encrinital plates
attached and apparently bored by zthodomi, some two or three inches
thick ; these were followed on the slope to the N. by thicker beds of
whitish fine grained blocks, having precisely the character of the fine
grained Sutton stone, and containing Lower Lias fossils ; one of the first
blocks, about 1ft. long and 2in thick, revealing when broken open good
specimens of Ostrea liassica Avicula decussata and a perfect tooth of
Acrodus nobilis ; so far for the fossil contents. Mr. Lucy, however,
apparently does not dispute the fact of this deposit containing a Lower
Lias fauna ; but of its similarity in stratigraphical position with the
beds at Sutton. In the opinion of the Geologists present and also that
of Mr. Storrie, who is well acquainted with these beds, the similarity
of these deposits with the Sutton stone could hardly be doubted ; and
the “drift” theory of Mr. Lucy, whatever that might mean, did not
hold good. Charles Moore’s views in this respect were not proved
erroneous, and the legitimate, though at the same time hazardous,
attempt to overthrow observations made by cautious authorities had
not as yet proved successful,
Prebendary ScARTA having after lunch thanked the courteous
host and hostess for their hospitality and the instructive morning
the members had passed under their guidance, the intervening
distance to Bridgend was soon traversed, and the 3.5 p.m. train
received them just in time before the break up of the fine
weather which had so much enhanced the pleasure of the
excursion.
Excursion to Chepstow and Tintern Abbey, Tuesday, July 13th,
1886.—Memories of pleasant places and things need refreshing
sometimes, hence though the Club had previously, in 1864, visited
Chepstow and Tintern, many who had recently become members
were anxious to see those far-famed places for the first time, and
the others were not adverse to revisit those architectural gems
ever revealing something new to wonder at and admire at
every fresh visit. The G.W.R. arrangements necessitated an
early start from Bath and the 8.5 a.m. train for Portskewet
received some twenty members. On the way they were joined by
220
Mr. Charles Richardson, the acting engineer of the Severn Tunnel
works. That costly undertaking of driving a tunnel five miles
long—two-and-a-quarter beneath the water and two-and-a-quarter
on land—thoughnow so farfinishedasto have admitted the passage
of a good’s train, yet is not in sufficient working order for
passenger traffic. The unfortunate bursting out of a land spring
on the Portskewet side having more than once impeded progress,
and now requiring the pumping up of 15 million gallons of water
every 24 hours; a drain which report states has considerably
affected the neighbouring springs, and must also affect the
finances, notwithstanding the contemplated saving of £12,000 per
annum, by the doing away with the present water traffic. Let us
hope, however, that this like other difficulties will be successfully
met by engineering skill! After having duly noted the velocity of
the Severn currents causing a perceptible irregularity inthe level of
the water which in some places seemed to be flowing down hill
near the “Shoots,” the trajectus at all times unpleasant and
especially so at low tide was accomplished, and nothing particular
occurred worthy of record before arriving at Chepstow, except the
pretty peeps of the Wye seen through the intervening masses of
rock as the train wound its way along the right bank. On
alighting of course the first object was the Castle so picturesquely
perched on its inaccessible crag, rising 130 fect in a sheer per-
pendicular wall of Mountain Limestone from the river which
washes its base. Ascending a grassy slope and passing under the
eastern gateway with its grooves for portcullis flanked on either
hand by round towers of Edwardian date, late 13th century, the
first of the four courts was entered. On the right was the
Banqueting hall, the tracery in its windows looking on to the court
indicating early Decorated work, temp. Edward II. Pantry
and buttery are shown at the E. end of this hall and a flight
of stone steps leads to the kitchen. The groining over the steps
is particularly good, also that of the vaulted subterranean store
chamber beneath, with its opening to the Wye and its iron ring
—_—-~
0 a”
‘
221
in the floor to which the rope of the boats bringing provisions to
the inmates was attached from below. Proceeding to the left side
of the first court, the tower where Henry Marten, one of the judges
of King Charles I., was interned and died, was next inspected. The
moulding of the upper part, supposed to be the chapel, shows the
ball flower and is of early English date, the windows facing the
court are much later. Ascending the spiral staircase, the battle-
ments were followed to the fine hall at the upper end of the
first court, supposed once to have been a chapel. The windows
are fine specimens of Decorated work. On the inside face of the
south and west walls, above the holes where the flooring joists were
inserted, there are several apparently Norman arches possibly
some of the original work of Fitz Osborn, the Norman, who is said
to have been the original founder of the Castle in the 11th
century. At the upper end of the hall are remains of some
Early English work, probably of a screen which separated a portion
from the rest and made it into a chapel. Passing outside this
hall, on the river side, a steep ascent led into another court-
yard approached by an outer gate. Having returned to the
first courtyard and enjoyed the shade of a magnificent walnut
tree for a space, the members passed out through the east entrance
and followed the deep ditch on the S., noting by the way at
the bottom of “ Marten’s” tower the peculiar strengthening of the
base which seemed to rest on an inverted arch of hewn stone,
the sides forming the angles of the tower and gradually dying away
in the masonry above. A coach and break met the members at
the top of the moat on the Tintern road, and after a pleasant and
breezy drive through Piercefield Park they commenced the
ascent of the Windceliff by an easy path through the woods at the
back of Moss Cottage. The far-famed view was seen to
advantage. The windings of the Wye through its tree-clad
inland cliffs, the distant islands of the Steep and Flat Holmes,
the Cotteswold hills across the expanse of the Severn on the
horizon, and Chepstow and its Castle almost hidden in the midst
Q
222
of the surrounding deep foliage at their feet, were the prominent
features in a view rarely excelled in beauty. A descent through
the woods was then made, and after paying the usual toll at the
Cottage, the conveyances, which had been sent round to meet
the members, were re-mounted and after a drive of two miles
the much needed lunch, prepared at the Beaufort Arms, was
thought highly necessary before the further prosecution of .
antiquarian research. To those entering the western portal of the
Abbey for the first time the view of the exquisite interior seems
unrivalled ; wall, pier, window and tracery seem so little injured
by time that one almost fancies the roof is only waiting
to be erected to restore the whole to its former state of chaste
beauty, even the large bosses at the intersection of the groining
are there ready to be raised into place—but perhaps its present
state of ruined preservation is better for pilgrims. Founded in
1131 by Walter de Clare, a Norman baron and relative of William
the Conqueror, but little, if anything, remains of that early date ;
all the chief architectural features of the present building date
from the 13th century. Roger de Bigod, Earl of Norfolk, to
whom the de Clare estates descended by marriage, commenced it
in 1269; and 1287 saw it finished for divine service. After the
dissolution in 1537, the monastic buildings and estates fell to the
share of the Earl of Worcester and through him to his descendant
the present Duke of Beaufort. The interor illustrates the
typical arrangements of the Cistercians. The nave which was
given up to the lay brethren has on its south side the remains of
the stone screens which shut out the lay brothers from the monks,
and was entered by a door-way still existing in the N.W. corner.
All the monastic offices are on the N. side; the Chapter House
with its encaustic flooring recently uncovered, the Guest House,
Refectory and elegant vaulted pulpit on its west side for the
reader, the buttery, kitchen, dormitories, and the Cloister Garth.
At the south side of the Garth, near the richly Decorated north
doorway to the nave, are two tombstones on one of which the in-
223
scription ‘‘ Johannes de Lynns;” and on the other “Jacet Henricus
de Lancaut . . . Abbas de Voto,” can be plainly read. The
Cloisters themselves have disappeared, but the well proportioned
windows of the N. aisle, dwarfed purposely for the admission of
the lean-too roof beneath, indicate the line where these originally
ran. Situation and architectural details both combine to make
these ruins some of the most picturesque in England. Passing out
again beneath the beautifully proportioned west window with its
nearly perfect Decorated tracery, a last look was given at the
fine west front with the remains of its Galilee, and then the modern
procession of lay brethren wound their way reluctantly back to
those less interesting but most useful conveyances, the coach and
break, which took them on to the station at Tintern Parva, a
mile distant, whence the train was taken for Chepstow. The
lovely peeps of rock, wood and river, as the train winds its way
to Chepstow, are unsurpassed even by the hitherto celebrated
drive by the coach road. The beauty of the scenery was much
enhanced, too, by the freshness which the recent rains had effected
on the foliage after the long drought of the past June, and every-
thing conspired to render this a most pleasant and successful
archeological excursion.
Ham Hiil and Montacute, Tuesday September 14th, 1886.—Those
who were present at a former excursion to Montacute on
10th October, 1865, may recollect that owing to the bad weather
and other contretemps the day did not leave pleasant memories
in its wake. Neither the house nor the quarries were seen to
advantage. Such remarks, however, could not be recorded of
this the fourth and last excursion of the season. A glorious
summer's day and courteous civility combined to make this
certainly one of the pleasantest and most instructive of the
series. Owing to the length of the programme an early start for
Yeovil by G.W.R. was necessary, and at 10.45 twenty members
and their friends, comfortably packed away in two breaks supplied
by the landlord of the “Three Choughs,” left the Pen Mill
124
station for Ham Hill, . Pleasant was the drive in the balmy
morning air by upland and deep cut hedge-embowered lane, with
distant peeps of church tower, and stately mansion house
embosomed in luxuriant foliage, thechurch of Odcombe conspicious
on the right, and the fine Queen Anne facade of Brympton in
the vale below. Agreeable, too, was the shade from the long avenue
of Scotch firs on either side of the road; though perhaps not planted
by the original makers of the camp, yet planted many years
ago by a former owner of Montacute (?) with excellent taste, and
seemingly rejoicing in the rich nature of the Inferior Oolite Sands
capping the elevated ground on which they grow. Ata sharp
rise of the ground leading to the outer defence of the camp, the
members left the breaks and walked up the road cut through the
steep vallum on the KE. At a small quarry on the right hand,
immediately on passing into the camp, the Secretary called a
halt, and pointing to a particular ferruginous band about six feet
from the top of the section, suggested that a search should there
be made for a small and characteristic shell. Crowbar and
hammer having been plied, many specimens more or less perfect
were soon found of the Rhynconella cynocephala, a brachiopod
marking a certain horizon in the Pisolitic beds of the Inferior
Oolite of the Cotteswold hills. Proceeding onwards from the
corner, ‘‘ too hot” in some respects for the comfort of many, the
more airy plateau of the hill was reached, and a short detour to
the left led to the quarries so widely celebrated for their
building stone, Fortunately the owner, Mr. Trask, was there,
and from him the following facts were elicited. The deep
quarries have only been opened in the present century; the one
above which they were standing, some 90ft. from the top soil to
the bottom of the working, only during the last 30 years. The
stone had been known and utilized for centuries, the original
makers of the camp were acquainted with it, as the use of it in the
S. and W. ramparts plainly showed. The Romans certainly used
it, and the architects from the Norman period down to the
125
present day, as so many of the churches bear witness. The
problem was, how with the bad roads of former days they were
enabled to convey the material so far. As to the details of the
section he referred to the late Mr. Charles Moore’s description,
which is given below in ascending order :—
Feet. Inches.
Inferior Oolite ; Yellow “ Brim Sands” with occasional
concretionary boulders of Sandstone j 80
Bottom bed—hard Nodular bed, not worked ... ee!
Gray bed 2
Ditto 2 6
Ditto 2
Ditto aoe be ar Sai ace C3
The “Yellow beds” closely bedded, varying from 2ft.
to lft. Gin. ode ace Het Si ee 50
“ Ochre ”—consisting of Yellow sands, sometimes passing
into Sandstone... ae: wae tid nas 30
The ‘Gray beds” yield the best weathering stone, and are
separated from the ‘ Yellow beds” by a band about 1ft. thick
containing many pellets of iron ore (Somerset Archeological
and Natural History Society, vol. xiii, 1865-6). Mr.
Trask told us that in working back the quarries many hut
circles had been destroyed containing skulls, burnt earth and
pebbles. During the morning an example of one of these “ finds”
was shown by a workman, consisting of round water worn flint
pebbles, a broken implement, probably portion of 2 polished celt
made of some hard blue stone (? igneous), and some bones of
domestic animals, sheep, &c. The flint pebbles looked
like sling stones. The Secretary thanked Mr. Trask for his infor-
mation, and said he would supplement his remarks by calling their
attention to the numerous fissures and joints running at cross
angles to the beds, facilitating the removal of the large blocks
from their parent bedding. Having accompanied Professor
Boyd Dawkins to these quarries a few weeks ago, he could give
them the substance of the latter’s remarks on these beds. Being
226
composed of comminuted shells, the Professor stated that in his
opinion these beds owed their formation to shallow water and
were probably laid down at a depth not exceeding 150 fathoms.
There was once a time when a walk could have been made from
this hill, without descending any very deep valleys, to Glastonbury
Torr ; but owing to the enormous wearing down that had gone
on in comparatively recent times the intervening rock had been
removed by the action of the sea, rain, river, frosts and carbonic
acid until the hill stood out boldly as at present, a monument of
past denudation. The geological part of the day’s programme
having been finished, a traverse was made to the S.W. entrance of
the camp and the vallum followed to a projecting spur, whence a
magnificent view of the distant Quantocks with the intervening
rich lowlands and numerous church towers scattered about was
obtained. At this point extra strength has been given to the
camp by a series of outworks defending the entrance in this
direction in a manner which even military authorities of the
present day would acknowledge as well and skilfully carried out.
The Secretary, here again referring to the great authorities on
these camps, said that this was one of the largest in England,
being 210 acres in area and three miles round; and that such
strongholds as these, of which there are numerous examples on
all our neighbouring hills, were made by the Neolithic people,
the Non-Aryans who preceeded the Celts, and by whom the
polished stone weapons were made. They were a military
people, and wherever there was a weak point to protect it was
always defended on scientific principles, such as would guide
defenders in the present day. The reasons why these camps
were situated on rising ground was due to the fact that in those
early days the country was divided into small communities, and
when the latter took to fighting among themselves—and the
country was “up” either from domestic feuds or from foreign
invasion—these upland enclosures served as places of refuge to
which they drove their cattle and in which they lived till the
227
clouds rolled by. Generally water was to be had close at hand
or could be temporarily obtained from the rainfall or dew ponds,
asin Wiltshire. These camps were in existence when the Romans
came, and were of course adapted and occupied by them as good
strategical points. Continuing along the W. side, the contour of
the ground was seen to have been much altered by the ancient
quarrying ; the Romans and others seem to have gradually worked
the stone back from the W. face, throwing up the “tips” as
they went eastward and in some places obliterating the ancient
vallum. The heat of the sun taxing the powers of some of the
members a cross cut over the broken-up ground was made
to the N.E. side, and the much needed lunch, brought in the
breaks, having refreshed them for the remaining portion of the
day’s work, the ‘‘Frying Pan” was the next object. This, an
undoubted portion of Roman adaptation, is situated at the N.E.
point of the hill, and was probably originally an amphitheatre ;
the scene of Roman military agitation, as in latter days it has been
utilized by arch agitators of the bucolic stamp. Many unfinished
Roman swords, coins chiefly of the Antonine period, one 50 years
later, and fibule have been found; also a curious row of holed
stones existed close at hand in situ, but during the last ten
years these have nearly all disappeared. One still remains
much broken away, but what their use was is doubt-
ful. Some think they were used for the purpose of tether-
ing horses. The hill having been both geologically and
archeological examined, it now remained to make a steep and
rapid descent to the church of Stoke-sub-Hamdon below, where the
Vicar, the Rev. W. J. Rowland, was kindly ready to receive the
members in his churchyard and point out the peculiarities of his
most interesting church. Proceeding first of all round the out-
side, attention was directed to some Early English work on the N.
wall of the nave, the meaning of which it was not easy to under-
stand. Over this,on the same side, was a good specimen of an
Early Norman narrow-lighted window, with grotesque carving in
228
the headstone forming the arch, at the W. end a fine Decorated
window, on the 8. Norman and Early English windows side by
side. The S. doorway, originally Norman, had been altered to
admit of the insertion over it of a later window. The S. side of
the chancel caused some discussion. Mr. Talbot considered that
the curious Norman corbel table was in its original position, that
the masonry of the walls was Norman work as was evidently that
of the end buttresses ; and that the windows were Early English
and Early Decorated, but altered on the north side of the chancel
in the 15th century. Entering the church by the N. porch the
tympanum of the doorway, originally blocked up by masonry and
discovered as the Vicar told us in 1857, created much interest.
The subject—in the centre a tree with three birds in the branches ;
an archer, half beast half man, on the left, turning backwards
shooting at a lion, with “ Sagittarius” roughly cut below; a lamb on
the right with a cross on back ; beneath, a lion with head turned
to right and tongue out as if wounded, with ‘‘ Leo” cut in like rude
characters—gave rise to many curious explanations (wide Mr.
Talbov’s ‘ Notes” below). Inside, the following facts were gleaned
from the Vicar. Originally a Norman church with chancel and
nave, subsequent alterations had made it cruciform. The chancel
arch, a very fine specimen of Norman work, had probably been
altered, the square abaci apparently being older than the capitals
below, a heavy roll runs completely round the soffit, a peculiarity.
The tower instead of being at the W. end, as was usual, is over
the N. transept, the stand for the hour glass on right of pulpit
was a relic of olden times. The S. transept was a beautiful
specimen of Early Decorated work, and the “ squints” were also
noticeable. In short but few churches in Somerset, so noted for
its churches, equal this in interest, as it is an example of nearly
every style from Early Norman down to our own times.
Mr. Talbot’s notes on the church being of value are here
appended :—
Notes on Stoke-sub-Hamdon Church. By C. H. Tazo.
This church is very picturesque and of great interest, owing to the
229
successive alterations it has’ undergone, and the work of different
periods remaining. It is a cruciform, aisleless building, with a tower
over the north transept and a north porch. The walls of the nave and
chancel are Norman; those of the nave having been raised probably
in the fourteenth century. The original Norman north doorway of
the nave remains, though somewhat concealed in the upper part by
the fourteenth century poreh which has been built against it. This door-
way has a solid tympanum, with curious and interesting carving ; in
the centre is a tree, with three birds in its branches ; on the right, an
Agnus Dei ; and below, on the left, a Sagittarius ; and, on the right, a
lion, identified by an apparently contemporary inscription underneath
—“Sagittarius . . . Leo.” The suggestion, in this and other cases,
that the Sagittarius had reference to King Stephen, appears to me
fanciful ; as also the notion that the carvings typify St. Michael and
the devil ; though the Sagittarius is certainly represented as shooting
at the lion, they may simply be two of the signs of the zodiac. There
are the remains of a corresponding Norman doorway on the south side
of the nave, but it has lost its arch and tympanum owing to the
insertion of a later window over it; so that we cannot tell whether
more signs of the zodiac were carved upon it. There are the remains
of two small original windows in the north and south walls of the
nave, and one in the south wall of the chancel. The chancel walls
retain very interesting original corbel tables. The chancel arch is a
Norman one restored. Above it, on the side next the nave, is a
defaced carved string course, apparently Norman, which would be
parallel to the orginal flat ceiling if the usual Norman arrangement
existed.
On the south side of the chancel, near the east end, is a double
lancet window of the thirteenth century, under one arch internally ;
to the west of this, a lancet of the fourteenth century ; and, to the
west of that again, a low side window, of the same date, with a plain
cusped head. It is obvious that the latter window may have been
exactly similar in the head, and have been reduced to the lancet form
by cutting away the cusps, but it is not absolutely certain.
Exactly the same arrangement seems to have prevailed on the north
side of the chancel, as is shown by the original arches of the windows
remaining internally ; but externally they have been remodelled in
250
the fifteenth century. The east window is an interesting specimen of
Perpendicular. Buttresses were added to the side walls of the chancel,
apparently at the same time.
The north transept and tower over it are of the thirteenth century,
with the exception of the north window, which was inserted in the
fifteenth century. The lower storey has groined vaulting, and there is
a projection on the east side, which may perhaps act as an abutment
to the chancel arch ; but, no doubt, served to enlarge the transept and
to contain an altar internally. All this is of the thirteenth century. In
front of this eastern recess is placed a stone screen of the fifteenth
century, which formerly occupied a different position in the church.
The south transept has ranges of windows in the side walls, of
early fourteenth century character, so close together that their splays
meet, forming an angle, and the whole has much the effect of a con-
tinuous arcade internally. The south window is of a later type,
fully developed fourteenth century work. There is, in the south wall,
a well preserved male effigy in a canopied recess of the same date ; and
piscinas across the S.E, angles in the transept and chancel. The
nave has several good windows inserted in the fourteenth century ;
particularly the west window, under which is a late fifteenth century
doorway. A bracket, affixed to the east splay of one of the windows,
on the south side of the nave, probably carried a statue. The font
is Norman.
The north porch, added in the fourteenth century, is of two stories
with a groined vault to the basement, and a ribbed vault, apparently a
true stone roof, to the upper chamber. Close to this porch, by which
it is partly concealed, in the outer wall of the nave is a feature of the
thirteenth century, not very easy to understand, consisting of tabling
crowned with Early English foliage. A similar, but perfect, example
is said to occur elsewhere. Internally there are remains of early
painting on the splays of the Norman windows, and also remains of
painting on the wall, over the chancel arch—two censing angels ;
probably, the figure of our Lord was formerly in the centre.
On the north side of the chancel there is a male effigy, under a
canopy, which may be of the time of Elizabeth, or, as some think,
later. The arms, on the monument, show that it commemorates a
member of the Strode family, as the same arms occur on a later tablet of
that family against the east wall of the chancel.
231
In the churchyard is an altar tomb, apparently of the fifteeuth
century, probably removed from the church.
There are a number of houses near the church, mostly of late date,
but preserving the ancient traditional character, well preserved and
but little altered.
After thanking the Vicar for his information a short drive took
the members to the W. entrance of Montacute house, where a
cordial reception from Mr. and Mrs. W. R. Phelips enabled them to
see both the exterior and inside of their noble mansion. Passing
beneath “and yours my friends” into the hall, they issued
“through the wide-opening gate,” where “none come too early,
none return too late,” on to the courtyard opposite the W.
entrance. Attention was here directed to the grand Elizabethan
facade with its so called nine worthies writ in stone—Hector, son
of Priam, Alexander the Great and Julius Czsar, three Gentiles ;
Joshua, David and Judas Maccabzus, three Jews ; Arthur the
King, Charlemagne and Godfrey de Bouillon, three Christians.
Beneath the windows, of which there are said to be 365, a
number equal to days in the year, were round hollows—what
was their use? Mr. Talbot thought they were for statues
originally ; the round chimmeys too, were they a part of the
original structure, or a later introduction? Longleat had similar
ones, these the last authority thought were not original. Was John
of Padua the architect, or who? Records are silent; but the
founder of this noble house all know was Sir Edward Phelips,
Knt., Queen’s Sergeant to Elizabeth between 1580 and
1601 ; and in possession of that family it has been ever since.
The eastern facade has had a subsequent addition made to it,
the centre portion between the two wings having been brought
from the house of the Horsey’s, Clifton, May Bank, and inserted
here ; “J. H.” or “C. H.” and the crest of the Horsey family, a
horse’s head, being recognised in the 15th century carving over
the porch and elsewhere. The members then entered the hall, in
which at the N. end is a curious plaster relief of the pratice called
232
“‘ Skimmerton riding,” of which the following is a description :—
“ Riding the Skimmity,”
* “On the left-hand of the bas-relief a man is seen stooping over a
beer barrel, in one arm he is holding a baby which has evidently
been entrusted to his charge by his absent wife. In the meantime he
has been drinking the beer, and apparently in a state of intoxication
is about to draw more, as the hand of his other arm is extended towards
the tap, and a cup to receive it stands underneath. But the wife
returns, and finding him in this condition rates him soundly ; then
while an altercation ensues between them, and she is whacking him
with an old shoe, a third person, supposed to be the school-master from
a scroll of paper in his hand, overhears the quarrel and reports it to
the village. Then follows the procession composed of men and women,
most of whom are carrying an eftigy of the delinquent on a pole and
proclaiming the matrimonial scandal to the surrounding crowd.”
Nore,—The term “skimmerton” is supposed to be derived from the
“skimmers” and ladles which the person riding carries in his hand and
with which he was sometimes belaboured. The Rey. J. B. Medley,
Rector of Orchardleigh, informed the Secretary that during his curacy
at Shepton Beauchamp he once saw (1854) this old use of “‘ Skimmerton
riding.”
From the hall the members ascended the stone staircase to the
long gallery, one of the most striking features of the house ;
supposed once to have been the library it extends the whole
length of the building and has a good oriel window at either
end. A refreshing cup of tea was awaiting their descent to the
hall, and after thanking their host and hostess for their courtesy
the breaks were remounted, and a pleasant ride through the
park brought them to Yeovil in time for the 6.23 p.m. train to
Bath after a most enjoyable day.
The bye-excursion to Dundry, fixed for May 18th—postponed
owing to the rain—came off on October 12th. There were only
five or six members who ventured in spite of a somewhat
unpromising morning to take part in it, and on leaving the
Bristol station had a most unpleasant trudge through muddy
233
roads and blinding rain to the top of the hill. The derivation of
the word—whether from the Saxon Dagian, to dawnor spread light,
according to Bishop Clifford, the Tower of the Church being
on the site of an ancient beacon, or ‘“ Dawn tree”; or whether
from two words Dun and Draegh, signifying “a hill of oaks,”
according to Collinson—was discussed by the way; the chief
conclusion arrived at, however, was that it was not done dry.
As it was impossible to enjoy any view, or to visit the celebrated
quarries; after some needed refreshments were taken at a
friendly Hostelry, the Church was hastily inspected, with its
“Dole stone” and fine cross in the Churchyard, and a rapid
descent made to Bristol.
The other bye-excursions, to West Harptree and Win-
chester, were not carried out; but the long deferred one, to
‘visit the little Saxon Church at Bradford, on the invitation
of Mr. Adye, the architect at present engaged in the
needful structural repairs, was made on Tuesday, December
14th. Owing to the heavy rainfall in the early morning only about
six members were present. These. were met by Mr. Shum at
the Bradford station, and had some of the interesting features of
that picturesque and foreign looking town pointed out to them.
Before crossing the bridge, the house in which Lord Westbury
was born, and the residence, nearly opposite, of the inventor of
the Shrapnell shell, were passed, and the strongly built and
curious little chapel on the south side of the bridge, overhanging
the water, claimed more than a mere passing look. At the
Ecclesiola, Mr. ’Adye met the party, and pointed out the various
repairs to walls and roof, which had elicited the commendation
of Mr. Freeman, and therefore must needs be historically and
architecturally correct. Since the last visit of the club much
has been done, the precincts of the chapel have been cleared
from the tumble-down cumbrous sheds before built against
the south wall and hiding its features; the roof has been
repaired and made watertight, and the walls, which were in a
234
dangerous state and consisted of an outer and inner facing of
masonry with the space between hollow, have been filled in with
Portland cement, thus binding the whole together in a solid mass,
The small round arches have been repaired and completed
wherever it was necessary for structural reasons to do so, and
wherever there was sufficient “springing” left to carry on the
design. On clearing away the structure abutting against the
south side, the foundations of a south porch were found ; and the
pitch of a high roof, corresponding with the height of the wall,
plainly indicated on the outside; an interesting point, thus
showing that the south porch was a fac simile as to height and
dimensions of the existing north porch. Two solid buttresses
have been carried up, resting upon the base of the east and west
walls of this porch, thus marking the site, and acting as a
support to the main wall on that side; though in the opinion of
the architect such support was not needed. Of course it is a
question about which the different schools of thought may
readily dispute, whether this present ugly masonry should
remain breaking the harmony of the south side; or whether
the porch should be restored (hateful word to some!) and
the walls and roofs added. MJntering through the arched
doorway into the nave, the great height of the building
at once arrested attention; and when the eye became
accustomed to the dim light, the irregularity of the details, the
descent instead of ascent into the chancel by a step , the bulging
look of the walls, which might have been original and intended
to be out of ‘plumb line ;” the curious “rundlet,” or reed-like
ornamentation round the chancel arch—the only ornament in the
chapel save the two angels high up in the chancel wall, about which
Professor Earle discoursed to the Club at their last meeting (Vide
p- 162),—all came out at last into prominence. The chancel
appears to have been lit by one deeply-splayed window, high up in
the south wall, and the length of the whole building, corresponded
with the height of the walls, 25 feet. Passing through the north
235
porch, the outside details were inspected, which are equally
interesting with those in the interior. The arched panelling,
all round under the eaves, evidently cut out of the masonry ; the
flat pilasters, “stepped” now on one side of the base, now
on the other, here and there on both sides; the irregularity
of the string courses and the general idiosyncrasy of the
structural details were remarkable. The west front has three
windows pierced in it, and on the inside beneath them it is
stated that they were not found there originally ; here, perhaps,
utilitarian purposes were a sufficient reason for breaking the
otherwise plain western wall facc. Having thoroughly seen this
most instructive building the parish church adjoining was visited ;
and thus in a very small space were seen illustrations of church
architecture, from the eighth century (so some suppose) down
through all the ages to the present nineteenth century garter-like
bands with which some fanciful hand has girt the westernmost
pillars of the north aisle. Having thanked Mr. Adye for his
guidance, the party, taken in hand by Mr. Shum, were shown the
priest’s chapel on Tory hill, admired the beautiful view o’er
woodland and vale below flecked with storm clouds and sunshine,
and descended to the beautifully situated manor house of
Belcombe Brook, and were there most hospitably entertained by
Mr. Shum.
Amongst the walks that to Claverton Down, at the invitation
of Mr. Skrine, to examine the Camp and excavations lately made
there by him, may be recorded. The meeting place was Sham
Castle, on October 26th. About twenty members were present.
The day was fair, cold and bracing, and so nipping and eager was
the wind on that airy height that the party were fain to crowd
under the lee of the Sham Castle, which some must have wished
to have formed a little more real defence against the elements.
Here Mr. Skrine read his paper (Vide p. 236), which was listened
to with attention, and the whole party then ascended to the ram-
parts of the Camp, noting several longitudinal mounds, considered
236
by Mr. Scarth to have been barrows. They struck the line of the
ramparts at the stile leading on to the Down and followed it
round to the Rifle Butts, where the ancient road through the
Camp ha‘ its exit towards the nortli, and where is still the cart
track. The line of the road curving through the Camp was
then followed, Mr. Skrine pointing out the lines of the enclosures
which bordered it. The rampart on the south was then observed,
dividing a field belonging to Major AlJen from the Down, with a
wall on the top of the bank as in prehistoric times. Several of
the enclosures were then pointed out with a reference to the map
of the Camp, and the party entered a field of Mr. Skrine’s, in
which he is carrying on some excavations. The building here
had been partially cleared, showing a solid wall 6ft. thick and
about 3ft. 4in. in height. A small piece of pottery (apparently:
Roman) and a piece of worked flint like a sling stone had been
found on the spot. The members then were guided to
Gainsborough’s Kitchen, a romantic dell in a rocky lane leading
down to a spring, the course of which is the boundary of the manor ;
and then through the wood to Claverton Manor by a charming
road overlooking the Avon valley. At Claverton the Club were
entertained at luncheon by Mr. Skrine in the picture gallery,
after which, on Colonel Chandler’s motion, a hearty vote of
thanks was given to Mr. Skrine for his paper and hospitality.
Hampton Camp.—The ancient camp on Hampton Down which I,
have asked you to explore with me to-day, is by all learned archzologists
considered to have been constructed by the Belgz, the invaders and
conquerors of South Britain, about 200 years B.C.
It was their most important fortress in this part of the country, and
was closely connected with their famous Boundary-Earthwork called’
the Wansdyke. It is very strong by situation, for it crowns a steep’
and wooded hill about 700 feet above the sea, and 600 at least
above the valley of the Avon which it commands. It overlooks a
considerable expanse of country, and was within sight of numerous’
hill forts on the line of the Wansdyke. It was then of considerable.
strategic importance to the Belgz, and was surrounded by an embank-
aoe
237
ment and ditch still to be clearly traced on three sides, north, west
and south. On the east the quarries have destroyed the line of the
ramparts, but probably as the hill on that side seems to have been
scarped and is very precipitous, its ramparts may not have had so much
attention. It is most likely that a wall stood on the top of the bank,
stone being plentiful and near the surface. The old road which passed
through the settlement from south to north and which was part of the
ancient Fosse Road from Seaton to Lincoln is still distinctly traceable.
The interior area of the camp is about 74 acres, and it is divided
into a number of parcels of land of unequal size by low longitudinal
ridges or banks. These are the remains of substantial walls or high
banks, that served to separate the hut dwellings, and the homesteads
or yards of the cattle, belonging to the inhabitants ; and also perhaps
enclosed gardens and fields of arable. The number and size of these
enclosures show that this was a permanent settlement or town, and
not merely a military post, or refuge for the neighbouring villages in
time of war. The cattle would be stabled or yarded at night by
their owners to protect them from wild beasts, or robbers ; and would
be led out to pasture by day in the woods and on the adjacent
downs, under the charge of their herdsmen.
Sir Richard Colt Hoare says that he has repeatedly met with
similar foundations of enclosures on and near the Wiltshire Downs, and
that he had invariably found they were indications of a British village.
The situation of Hampton Down also corresponds with the description
by Cesar of an “oppidum” of the Britons. He says “the Britons
call a town a place with a tangled wood round it and fortified with a
yampart and ditch.” Inside this, as Strabo tells us, they would build
their huts and collect their cattle, but not with a view to remaining
there long. As, however, Hampton Down was on the frontier, it was
no doubt always occupied by a garrison, and was a permanent settle-
ment. I am indebted to Mr. Spackman for the assistance of a map
of the camp which he made by direction of Mr. Scarth, more than
30 years ago, and which I have had reduced. It gives all or nearly
all the enclosures within the camp, some 34 innumber, andsome outside ;
and a recent measurement directed by myself has verified the lines as
on the whole very accurate. No excavation has been made of these
lines ; but some hut circles have been explored by Mr. Scarth. And 1
R
238
have discovered enclosures of a similar kind to them within the camp
in a field of mine called Bushy Norwood, on the south side of the
camp, where I am now carrying on some. excavations to which I
shall invite your attention.
It has, I think, been shown that we have here a considerable camp,
occupying an important military position in pre-historic times.
What traces there may be of Roman occupation I am not prepared
to say, a small fragment of pottery being all I have found by
excavation ; but it is certain that this must have been one of the forts
garrisoned by Ostorius on the Avon and Severn rivers when he marched
against the Silures in South Wales. Mr. Scarth found traces of a
Roman camp on what was Claverton Down; but the plough has
probably obliterated it. We are, however, on the present occasion
dealing with its occupation by the Belg as their frontier fortress,
Now who were the Belge? This is a question which has puzzled a
good many antiquaries; but it is fairly solved by the researches of
the late Dr. Guest, given to the world ina posthumous work of his
“ Origines Celticce.”
He says, “the Belgze were a powerful and aggressive people, but
from what quarter they had intruded themselves into the seats where we
find them settled is a difficult question to answer, Cvesar says that the
country of Gaul was parcelled out among three great tribes—Belge,
Celte and Aquitani—and he makes the Seine and the Marne the
Southern boundary of the Belge. The basin of the Rhone and
Saone with Toulouse the capital was called ‘Provincia’ by the
Romans (‘ Provence’ now), and this was occupied by the Volcse—
another reading of Bole or Belcz the V and B being interchange-
able letters. These Volce were traced also to Ancyra in Asia
Minor, whither the Belge under Brennus some centuries before
had passed from Byzantium. Jerome says, the people of Ancyra
spoke the same language as those of Toulouse. Identity of language
in this case means identity of race.” These Volcz were also called
Tectosages ; the meaning of which, says Guest, is the wayfaring men
who wore cloaks of skins, ze... shepherds or herdsmen ; and curiously
enough the Scythians who drove some of these same Belge from the
basin of the Danube over into Asia, were also called Belew or Tecto
sages. The name being a collective term for their occupation as herds-
men, Dr. Guest pursues the matter by an argument from etymology.
239
Fir-Bolg, the Irish or Gaelic form of the name Belgze, means the men
of the Bolg tribe, Fir, plural of Fear-Men (or say it was an Irish form
of the Latin Vir which would be pronounced Fear) the meaning is the
same. He thinks that the Roman Bubulcus comes from Bolg, or
Buile, againa Gaelic form of the word, and hederives it from the Sanscrit
Palah, or Palakah, protector ; Go-Palah, or Palakah, being cow-herd ;
Greek Bov-moros, Latin Bu-Bulc-us. Supposing this conjecture to
be correct, the name admirably fits the character and occupation of
the Belge who invaded Britain 200 years before the Christian era.
And what does Cwsar tell us of them? Cvsar says that the southern
coasts of Britain were occupied by these tribes, who had crossed over
from Belgium for the purposes of plunder and war, and who had
finally settled there and begun to cultivate the Jand. Dr. Guest
follows up this by saying that they probably landed near Christ
Church, in Hamsphire; and thus possessed themselves of the fine
grazing lands on the banks of the Stour and Avon ; and that they fixed
their first boundary line by a Dyke—called Bokerley Dyke and Combe
Bank—which included Cranborne Chase and part of the new Forest.
They next pushed on beyond Old Sarum and Amesbury to the Downs
of Hants and South Wiltshire. Their third line was the Wansdyke,
which has been traced from the Berkshire Downs through Savernake
Forest to near Portbury Lane and the Bristol Channel. It is plainly
visible near Warleigh on the opposite side of the Avon. The ditch in
every instance faces the N. to keep back the British tribes, of whose
land they had taken possession. There were numerous forts along the
Wansdyke, many of which must have been within sight of Hampton
Down ; English Combe, Maes Knoll, Dundry and Stantonbury camp
on the W., or Bathford Hill, which appears to have been scarped,
though no certain traces of a camp have, so far as I am aware,
been discovered. Many of the forts on the Marlborough Down
from Roundway eastwards would also be in communication, and the
Wansdyke itself was utilised by the Romans as their own road to
Marlborough.
These observations will, I think, have shown the strategic import-
ance of the Hampton Camp. It was the great frontier fortress
settlement of the Belge ; and, as observed before, no doubt permanently
occupied by them. Now assuming Dr. Guest’s conjecture to be correct
as to their name and origin, we shall see that their migrations may have
240
been dictated by the necessity of their occupation. They had out-
grown their own lands in Gaul, or possibly had been driven out by
an inundation of the sea, and sought fresh grazing and arable lands in
the fertile vallies of Southern Britain, where the Downs afforded dry
and safe situations for their fortified settlements ; many of these had
no doubt been occupied by the British tribes who had preceded them,
but were further strengthened by these men who possessed iron and
bronze tools unknown to the early settlers of the stone age. It would
also become necessary to mark out in some definite manner the limits
of their conquests, both to keep their own cattle in and to exclude
those of the neighbouring tribes from their grazing grounds.
That their migration and conquest of South Britain may be thus
explained is no mere theory, but is in accordance with what may be
called the laws of Nature.
In the primitive times it was undoubtedly the case that the owners
of cattle had to move their quarters frequently, their herds and flocks
having out-grown the pastures. Abraham and Lot had “ exceeding
many flocks and herds,” and separated in consequence. And cattle,
if short of food, would certainly move, whether with or without their
master’s leave, and draw them after them “to fresh fields and
pastures new.”
An illustration of this may be drawn from the ranches in N.W.
America ; where, when prairie fires or overstocking has laid the
pastures bare, the herds rush tumultuously down on the homesteads
and wreck them in order to get at the hay and provender stored
within. We find the Belgic tribes had before Czesar’s time occupied
the greater part of Southern Britain, and were his sturdy antagonists
in war.
Dr. Guest considers that the Wansdyke was merely a boundary
fence, and argues that it could not be defended in time of war ; but it
must be borne in mind that the hedge, that most probably surmounted
the bank, would be a very valid obstruction, and one that was certainly
made use of as such by the Romans in that famous dyke constructed
by Drusus from the Rhine to the Danube, a distance of 300 miles, to
repress the incursions of the German tribes. It is called the Pfahl-
Graben, or the hedge-bank and ditch, and is still clearly traceable
from near Coblentz to Ratisbon. This was like the Wansdyke, guarded
at intervals of a few miles by forts garrisoned by Roman soldiers ; one
241
of these, the Saal-Burg, near Homburg, has been carefully explored,
and the foundations of all the usual buildings ina Roman camp are
visible. When first discovered little more was to be seen than
raised mounds, such as we have on Hampton Down. The hedges
had grown into trees and thickets, and formed a thick barrier in many
places ; and the idea was, that if an enemy came through in one place
he would have a difficulty in finding again the hole through which he
had entered the territory, and might be cut off in his retreat by the
garrison of the adjacent forts, which were all within signal notice of
each other.
It seems to me that the Wansdyke, with its numerous forts along the
line, may have suggested to the Romans the means of fortifying their
positions on the Rhine and Danube ;-and also afterwards, the walls in
the North of England to curb the Scots.
The Belgze were far in advance of the ancient Britons in civilisation
and knowledge of husbandry. Whereas the British tribes were wont
to burn the straw, and to store the ears of corn, which they cut from the
stalks, in holes in the earth, the Belge built barns and threshed
their corn and stored it therein. But though nearly as much civilised
as their neighbours on the continent (says Mr. Elton in his origins of
English History) they were simpler in their habits. They had not
learned to build regular towns, though their kinsmen in Gaul had
founded cities with streets and market places. What they called a
town or dunum, was still no more than a refuge in time
of war, a stockade on a hilltop. Their villages were built of
beehive huts with roofs of fern or thatch, But their farms
were laid out in large fields without enclosures, except when
fences were necessary to separate the arable from the pasture.
Such enclosures can, I think, be shown on Hampten Down, and must
have been more than walls of huts and yards, for some are several
acres in extent. It may be that further excavations may show more
clearly the nature of this Belgic settlement and the character of its
ancient inhabitants, but the main facts above related are, I think,
reliable. A building on my side of the camp, the foundations of
which are now being cleared, appears to have been erected for some
peculiar object and to be of a public nature, It is of an oval shape,
and the walls are at least 6ft. thick. The length 93ft., breadth 50ft.
It seems to be connected with what looks like an exterior defensive
242
wall of the settlement on the hither side of the camp. Mr. Scarth
finds on the N, side remains of a temple and several barrows, which
will probably attract the attention of the Club. On the whole I
think the camp deserves very full and serious exploration, and ought
to be included in the ancient monuments protected by the Act of
Parliament.
The weekly walks have been kept up, but the Secretary has
not received any Notes respecting them, and concludes that bodily
exercise, unaccompanied with any particular strain upon the mind
by way of observation, was the chief object. As he is not always
able to join in these walks himself, he wishes members would
from time to time send him some result of their meetings, ¢.9.,
the time of the flowering of plants, the first appearance of
migratory birds, and other events connected with natural history ;
any notices connected with the geology of the district, such as
the opening of new sections and quarries in the rocks, the
occurrence of landslips, so constantly going on around our hills
of more or less magnitude, and lastly the state of preservation
of our momuments both ancient and modern. In connection
with this last subject a communication was received in the
summer from the authorities of the Somerset Archeological
and Natural History Society, requesting to have a report upon
any Ancient Monuments in our neighbourhood which it was
desirable to place under Government protection. In accordance
with this request a report was made and sent to the secretaries
upon the remains of the Wansdyke at Englishcombe and
Claverton Down; also of the Cromlechs opposite Tracey Park,
near Castle Combe, and in Orchardleigh Park. It is right to
mention here, in connection with the preservation of ancient
remains, that the so called altar-stone, of so much archeological
interest, having again been brought out from its temporary
shelter and exposed to the destructive action of the weather,
it was found necessary to call the attention of the Mayor and
Corporation to a former presentation from the Club on this
243
subject. Owing also to a statement made at one of the
Quarterly Meetings of the danger lest some of the interesting
Roman work lately uncovered at the Baths should be interfered
with and obscured by the new buildings in process, your
Secretary was empowered to present the following memorial to
the Town Council :—‘*The Committee of the Bath Natural
History and Antiquarian Field Club having been credibly
informed that a wall has lately been built intersecting some of
the Roman work recently uncovered, respectfully beg the Mayor
and Corporation to make such structural arrangements in
the new work as that any destruction or concealment of
the Roman work by plaster or otherwise may be avoided, in
order that the public may have free access to, and free inspec-
tion of, the valuable system of Baths prevailing at the Roman
period. This was presented by your Secretary on Tuesday,
November 23rd.
The Inscribed Leaden Tablet found in the Roman Bath.
As every reading and every notice of this Table must be of
importance and of value to local archeologists, a record of such
notices may well find a place in our Proceedings. Two new
readings, which will accordingly be acceptable, having recently
appeared, they are here, with the kind permission of the authors,
produced.
But just lately, in the volume of the Archzological Assocation for
1886, Mr. W. de Gray Birch, F.S.A., after remarking that the
characters on the tablet appear to be a mixture of cursive and rustic
letters, assigns the date to a period ranging from the second to the
fifth century after Christ. Mr. Birch considers that the reading
should be from left to right as usual, but that every word is written or
inscribed in reversed order of the letters, a manner quite unique. All
other readers have begun at the right-hand side of the first line, and
so on each line consecutively from right to left ; but that the reading
should be from left to right is clear, as the last line starts from the left
and finishes half way across towards the right.
244
A fac-simile of the tablet given in the Berlin Hermes, Vol. xv.,
March, 1881, shows the inscription clearer than a photograph, and Mr.
Birch thus reads the text as :—
QIHIM. MAIBLIV TIVALOG
VI . CIS TAVQIL OMOC AVQA
ELAT...... VVQMAE TI VA
VL...... ANNIVLEVSVEREPV
—— SXESVNAIRFASVNIREV
ESSILATSVGASVNAITI
MOC SVNAINIMSVTAC
LLINAMREG ANIVOI
No contractions are used except Q for qui. As the whole of the
fourth word could not be got into the first line, it was finished on the
second, and so with the third, fourth, fifth, sixth and seventh lines
which all begin with end parts of words from the lines above them.
The reversed mode of writing is supposed to recommend itself to the
avenging deity.
By this reading the inscription becomes clear and we get an intelli-
gible piece of tragedy. It works out as :—
Q(ui) MIHI VILBIAM JUGOLAVIT (=
jugulavit) sic LiquaT (=liquatur)
Com? (=Comodo, quomodo) aqua. TALE
vu (enus) Q(ui or qua) cUM (sa)LVAVIT
(est or fuit ) VELVINNA EXSUPEREUS
AFRI1(C)ANUS SEVERINUS AGUSTALIS
COMITIANUS MINIANUS CATUS GERMANILLA
JOVINA
“ Mihi” is considered to refer to Germanilla Jovina.
In the Journal no translation is given, but Mr. Birch has kindly
favoured us—his own version being so desirable—and gives the
followiig ;
May he who cut Vilbia’s throat for me melt away like water. It
is (or was) Velvinna who cured her of such a wound. Exsupereus
ii ee
245
Africanus, Severinus, Augustalis, Comitianus, Minianus, Catus, Ger-
manilla Jovina. These names may possibly be those of witnesses ;
and lastly comes Germanilla Jovina as the lady whose servant had
been so nearly murdered.
In a previous volume of the Archeological Association, that for
1885, Mr. Thos. Morgan, F.S.A., has given an account of his reading,
and by his kind permission the following extracts are made. After
remarking that three tablets have been found, only this one having
been described in print, he reads the inscription, taking the words
from right to left, as :—
COLAVIT. VILBIA, M(iniana) MIHI Q(ue)
AQUA. COM. CLI(ens) Qv(in) T(u)s. E(git) c(ommentariensis)
VEL [R] (atiocinator) Iv
AVITE, AMVL(ius) E(t). AEL(ius) (vel) AEL(ianus)
EXPERIVS VELVINNAI(tem) L(avit) V
GVERINVS. AERIANVS. EX
ITIANVS. AGVSTALIS, S(evir)
CATVS MINIANVS, COM
JOVINA, GERMANILL(a)
Translated thus :—Vilbia Miniana, in company (with Jovina the
little sister), bathed in the water four times ; and when Quintus my
client, ancestrally named Amulius and lius or Atlianus, acted as
secretary or accountant. Experius Velvinna also bathed fives times ;
Guerinus Airianus Exitianus member of the Augustal College; as
also Catus Minianus, with Jovina the little sister,
The only conjectural emendations made are, the setting out Amulius
in full in the third line, and the substitution of V for X the fourth
letter from the end, in the fifth line. The reading thus seems to be
the testimonial of a family party who went to take the baths, viz. :—
Catus Minianus the pater-familias, with his wife or daughter Vilbia,
and a little sister Jovina, and their attendants. The words on the
tablet are easily read because the position only of the letters is
reversed ; the letters are written in the right way. This could not
therefore have been a tablet for stamping or printing. Professor
Zangemeister, of Heidelberg, requires an I instead of E in line two,
then Mr. Morgan could read Juit (for egit) ; or if the E be allowed to
remain. then E Commentariis might be preferred as relating to Avite
S
246
Aurelius et Aflius in the third line. Hgit Commentariensis is not
common in inscriptions, though good Latin. The A at the end of the
second line forming the first syllable of Aqua is considered too faint
to do duty as a letter ; omitting it the words would be mihique quacum
cliens Quintus, which makes the sense more explicit, and the sentence
would run :—Vilbia Miniana in company (of the little sister Jovina),
bethed four times (quater), with whom (quacum) my client Quintus
went as secretary, &c. The IV in the second line wants the dash
over it to mark it as a numeral, though this may have disappeared
with age ; if consequently this IV must be read as two letters, then
E CIV might stand for e civibus if Quintus were entitled to citizen-
ship; or IV might mean [VIT if the reading = CoMMENTARIIS
be adopted.
The investigation of the circulation, quality, and quantity
of underground waters being one of the subjects about which our
Society, as one of the corresponding Societies of the British
Association, was requested to acquire information, an applica-
tion was made to the Baths Committee with a view to ascertain
whether any scientific observations had been carried on for a
series of years to dertermine the temperature and volume of the
Hot Springs. In reply to this your Secretary was informed that
the experiments as to the temperature, which appear to have been
carried on merely during the last two years, have been conducted
at the expense of a private physicianin London. It is very much
to be regretted that accurate and scientific observations, in
connection with a subject so vastly important to the welfare of
the city and general public as the variableness or otherwise of
the flow, temperature, and mineral contents of these Hot Springs,
should not be systematically made. One other subject may be
briefly mentioned, the Club having offered to assist the Mayor
in his reception of the Colonial visitors on September 8th and
9th, your Secretary was placed on the Reception Committee,
and was in attendance at the Museum of the Royal Literary and
Scientific Institution during their visit on the latter day, and
briefly pointed out to them the valuable contents of the Moore.
Geological collection.
247
The finances of the Club continue in a fairly prosperous posi-
tion, for though the yearly expenditure exceeds the receipts by
£4, Os. 7d., the Treasurer was able to meet the deficiency by the
balance in hand from past years. The increased expenses arising
mainly in the Printing items, the Committee have been instructed
to consider the question of possible reduction in this quarter.
In conclusion, the past year has been rather an eventful one
in the death annals of the Club, three old members whose
presence used to be so familar have passed away ; the Rev. A.
G. How, General Mulcaster ; and C. E. Broome, Esq. ; the latter’s
absence cannot easily be replaced ; another * (star) has fallen
out of our list, two only now remain, let his and their example
encourage us to work while time is ours!
H. H. WINWOOD,
Hon. Secretary.
Nrsauwed
of FEB 1888
CORRIGENDA.
Page 200, tenth line from bottom, for “aneo” read “ anes.”
Page 201, sixth line from top, before England insert “ the S. of.”
CONTENTS OF NO. IL, VOL
‘ 10:
eee pte
is -1—Nores on THE Grotocy or Brent KNoLL, IN |
f ne Ree SOMERSETSHIRE, BY Horace “B. Woopwarpb, | ;
_2,—Puacr-Names DERIVED FROM PLANTS (IN THE es
react NEIGHBOURHOOD or Batu), By Rev. CANON —
{ ELLACOMBE rot Bienes = Pe aie
3,.—ADDRESS TO THE MEMBERS OF THE BaTH FIELD ~~
Cus, IN REFERENCE To THE Dearu or C. E. ioe
Broome, Esq, F.LS., By Rev. L. BLoMEFIELD, ~
MA, F.LS., F.GS., &e. |
4,—TRACES OF THE SAxoN PERIOD IN. BATH AND THE — y
NEIGHBOURHOOD, BY REV, PREBENDARY EARLE . 153
-3.—LETTERS ILLUSTRATING THE BATTLES OF CLAVERTON
AND LANSDOWN, BY H. D. SkKRINE, M.A.
’ 6.—FurRTHER NOTES ON THE CLAVERTON SKIRMISH, BY
Wan: H. Di Siriwe, -MiAS ye a ea
7, Notes on toe Ham Hin Sronu, sy Horace Bo
eet Woopwarp, F.G.S. =~ a ve way oe ORS
8.—FurTHER RESULTS OF METEOROLOGICAL OBSERVA-
TIONS MADE AT'THE BATH RoyAL LITERARY ©
Sanam AND SCIENTIFIC INSTITUTION, BY Rev. LUONARD
;--* -. Bromeried, M.A., F.LS., F.G.S., &e. ,
- -9,—-SuMMARY OF PROCEEDINGS FoR THE YEAR 1886-87, a
Re ioe RY. TH SRORETARY. 00. {res eae Heer
aa PROCEEDINGS
OF THE
BATH NATURAL HISTORY
NO. 3, VOL. VI.
7]
ha . : ra
x
PRICE HALF.A-CROWN.
. Slap S
rs -
= =o “}
‘
Se BATH:
. THE HERALD OFFICE, NORTH GATE.
' J. DAVIES, GRAND PUMP ROOM LIBRARY,
=
ror rene as a . Pa He Pres
“i ‘ . os 3
= < 3
|
249
On some Ostracoda ‘from the Fullers-earth Oolite and Bradford Clay.
By Professor T. Rupert Jongs, F.R.S., F.G.S., and
C. Davies SHERBORN, Esq., F.G.S.
(Read November | 16th, 1887.)
[Plates i—v.]
Introduction.—In a short paper on Jurassic Microzoa in the
Geological Magazine for June, 1886 (pp. 271—274), we referred
in detail to each of the hand-specimens courteously supplied to
us a few weeks previously by the Rev. H. H. Winwood, F.G.S.,
and H. B. Woodward, Esq., F.G.S., of the Geological Survey.
Amongst them were examples of the Fullers-earth Clays, from
-Midford, containing Ostracoda. These minute bivalved Entom-
ostracan Crustacea are the subject of the present memoir.
The Ostracodes were obtained from the blue and yellow clays
of the Fullers-earth Oolite, as exposed in the sections at Midford,-
near Bath.* One of the two blue clays is directly under the
Great Oolite. Not far beneath is a yellow Fullers-earth Clay ;
and this rests upon the second bed of blue clay. Very few
Microzoa (not 10 per cent.) were found in the yellow bed.
The Rev. H. H. Winwood has also sent us a small piece of
the Fullers-earth Rock,+ from near Bath, as it contained some
Ostracodes. These are rather obscure on account of their embed-
ment in the matrix, but are evidently a Bairdia and a Cytherella,
and are probably of the same species as some of those from
the clays.
Several specimens from the base of the Fullers-earth Oolite,
near the Cotteswolds (see p. 256), have been courteously sub-
* The Clays at Midford are mentioned in H. B. Woodward’s
“ Geology of England and Wales,” 2nd edition, 1887, p. 297.
+ Mentioned in H, B. Woodward’s “Geol. England and Wales,”
“2nd edition, p. 295.
Vou. 6, No. 3.
250
mitted for our examination by Mr..E. A. Walford, F.G.S.
They are figured in the fifth plate issued herewith.
One piece of the Bradford Clay from Bradford (Geol. Mag.,
1886, p. 273) has yielded a few specimens which are also
treated of here.
A bibliographic list of works treating of the Jurassic Ostracoda
(omitting those of the Lias and the Purbeck beds) is given in the
Quart. Journ. Geol. Soc., vol. xl., p. 776. To this list may be
added the paper on the species obtained from the boring at
Richmond, Surrey, described in the same volume, and M. O.
Terquem’s memoir on the Ostracodes. from the Inferior Oolite*
of the Department of the Moselle, in France (Mém. Soc. Géol.,
France, sér. 3, vol. iv., 1885). The latter is elaborate and fully
‘illustrated ; but we are not satisfied with all the generic deter-
minations, and the drawings in some instances leave much to
‘be desired. Another such memoir by M. Terquem treats of the
‘Ostracoda of the Inferior Oolite near Warsaw, 1886.
The figures on the five plates illustrating this present memoir
‘give the valves with the anterior extremities upwards; the
dorsal and ‘ventral margins being on the right and left hand,
as the case may be. Of course, this position is not in accordance
with the natural habit of the animal when swimming; but it is
‘a convenient arrangement in plates, and often adopted. Hence
the height of the valves (from the ventral to the dorsal margin) is
‘occasionally referred to in the text as the (apparent) breadth.
"In every case the specimen has been mounted ona ‘‘ Beck’s
revolving disc,” and drawn under the camera; and thus the several
‘views that we have given of each individual type of a species
“have an assured correctness. :
The Ostracodous Genera mentioned in our note in the Geological
‘ Magazine, June, 1886, have been more accurately determined in
* One figure, p. 100, pl. ‘xviii, fig. 1, seems to approach our C.
pentagonalis, p. 261. Mee ; i
o
251
the present memoir. Their characters have been defined
chiefly in the works of Sars and Brady. We need offer no
remarks except on Cytheridea. In this genus the hinge is con-
structed as described by Jones (Monogr. Tertiary Entom., Pal.
Soc., 1856, p. 41) and Brady (Trans. Zool. Soc., vol. v., 1866,
p. 369), and has the following characters :—Hinge-margin of the
right valve marked with a series cf small tubercles, which are
received into corresponding depressions of the opposite (left)
valve. These tubercles or crenulations are mostly disposed in
two terminal groups, and the intervening portion of the valve-
margin either is plain, or may be marked by minute tubercles
on the left, and corresponding fosse on the right valve.
G.S. B., Zc.
The continuance of the crenulation along the dorsal edge
occurs in Cyprideis, Jones (Monegr. Tert. Entom., p. 21); and, if
worthy of being noticed as a distinctive feature, this name might
have been retained as subgeneric, were it not that Cytheridea
perforata and C. Sorbyana (Monogr. Tert. Entom., pp. 40 and 44)
have it also. Moreover, Cythere lutea, Miiller, is figured by G.
S. Brady as having this hinge-structure in the Trans. Linn. Soc.,
vol, xxvi., pl. xxviii., fig. 5 b, and a simple Cytheridean form of
hinge in Trans. Zool. Soc., vol. v., pl. lviii., figs. 13 c,d. This shows
that ‘merely by the hingement the tests of Cytheridea, Cyprideis,
and Cythere cannot be always clearly separated ; but, for the sake
of convenience in Palzontology, we must use some special terms
for the forms having the different kinds of hinges, as they are among
the few leading characters that we have at command. Thus
those forms having hinges with crenulated teeth and edges are
teferred to Cytheridea, whilst those having the bar and furrow,
‘with teeth (rarely crenulated) at the angles, belong to Cythere.* :
We may also notice that the allied Cytheropteron and Loxoconcha
have sometimes crenulations on or near-their hinges.
* This kind of hinge is definitely described and figured in the
Monogr. Tert. Entom., 1856, p. 23, pl. iii. ; and in the Challenge
Report, 1880, p. 62.
DESCRIPTION OF THE SPECIES.
[In Zoologicul arrangement. |
1. BYTHOCYPRIS WINWOODIANA, sp. 1.
HL. v,, figs. 1. 4,0, .c.
Reniform, nearly symmetrical, sub-convex, smooth ; left valve
overlapping the right on the ventral margin. Edge view,
lanceolate ; end view, compressed ovate.
Named after the Rev. H. H. Winwood, M.A., F.G.S., who
courteously favoured us with some of the material from Midford,
One specimen ; Blue Fullers-earth Clay, Midford.
2. MACROCYPRIS HORATIANA, sp.
Pl. v., figs. 2 a, 0, ¢.
Subreniform, elongate, narrower behind than in front, with a
flattening at the antero-dorsal margin. Not very convex ;
surface perfectly smooth; edge view, lanceolate; end view,
narrow-ovate.
Named after Mr. Horace B. Woodward, F.G.S., to whom we
are indebted for some of the fossil material from Midford.
This species is near M. decora, G. S. Brady, Challenger Report,
p. 44, pl. 1, fig. 3, but it is shorter, blunter, and less arcuate.
Five examples; Blue Fullers-earth Clay, Midford.
3. MACROCYPRIS TERRA-FULLONICH,* sp. n.
Pl. v., figs. 3 a, b, ¢.
Subreniform, posterior end narrower than the anterior.
Ventral margin nearly straight. Well-curved on the dorsal
margin. Surface smooth. Edge view, lanceolate; end view,
vroadly ovate. ,
Four examples ; Blue Fullers-earth Clay, Midford.
* Of the Fullers-earth,
253
4. BAIRDIA JUDDIANA, Jones.
Quart. Journ. Geol. Soc., vol. xl., 1884, p. 767, pl. xxxiv., fig. 18.
/One perfect example of this boldly characterized Bairdia
occurs in the Blue Fullers-earth Clay at Midford. It is well
known to us as occurring in the Lias, and from the Richmond
boring.
5, BAIRDIA TRIGONALIS, Jones.
Quart. Journ. Geol. Soc., vol. xl., 1884, p. 767, pl. xxxiv., fig. 19.
_ Two valves of this species occur in the Blue Fullers-earth
Clay, Midford.
6. BAIRDIA FULLONICA, sp. n.-
Pl. v., figs. 4 a, 6, ¢.
Of the usual subdeltvid outline, evenly convex, smooth, and
delicately punctate. We do not, however, know any form yet
figured that exactly matches these specimens from the Fullers-
earth Oolite. Edge view, lanceolate ; end view, sharp-oval.
Two examples ; Blue Fullers-earth Clay, Midford.
7. Three examples of Bairdia, more nearly approaching to
B. Hilda (Quart. Journ. Geol. Soc., vol. xl., 1884, p. 771, pl. xxxiv.,
fig 20) than to others, occur in the Blue Fullers-earth Clay of
Midford; also a single valve of a Buirdia very near to the
smaller valve of B. Jurassica (loc. cit., fig. 22.)
8. CYTHERE SPHERULATA, sp. 1.
Piva, figs. 6 a, b, ¢.
Broadly sub-oblong and convex, with the antero-dorsal border
very oblique, and the posterior end well rounded. Surface
ornamented with minute tubercles arranged in curved lines,
resembling strings of beads, and becoming straighter, but con-
fused in the dorsal region. Edge view, long-ovate; end view,
sub-cordate or broadly ovate, with flat base.
254
One specimen; Yellow Fullers-earth Clay,* Midford.
The dorsal view (not figured) of this perfect specimen shows
the anterior hinge-tubercles usual in Cythere, and the dorsal
depression (as in Monogr. Tert. Entom., Pal. Soc., pl. iii., fig. 2 ¢),
hence we are inclined to refer tiiis specimen to Cythere.
9. CYTHERE (1) SPECIOSA, sp. n.
Pia, figs: 10°a;"b, 2.
Carapace convex and smooth, sinuous on the dorsal margin,
the anterior hinge being prominent. The ventral margin is
elegantly outlined with an oblique curve. Anterior end nearly semi-
circular ; posterior narrower, with a sharp curve, and distinct
rim. Edge view, sub-sagittate ; end view (like that of pl. ii,
fig. 8), ovate and compressed dorsally, this depression showing
on the front half of the carapace, behind the anterior hinge.
One specimen (unfortunately lost since the drawing was
made) ; Blue Fullers-earth Clay, Midford.
10. CYTHERE CORROSA, sp. 2.
Pl. ii, figs. 12 a, b, ¢.
A short, sub-oblong form, neatly rounded behind, and obli-
quely rounded in front, with the dorsal slope meeting the
prominent anterior hinge, and forming a shoulder, hence the dorsal
edge shows features strongly suggestive of a Cythere. Surface
with a rugose, sub-concentric reticulation. Edge view, ovate,
slightly compressed at the anterior third ; end view, subcordate.
One specimen ; Blue Fullers-earth Clay, Midford.
11. CYTHERE OSCILLUM,T ep. n.
Pi it, figs. 8 a; 0, ¢.
Sub-oval ; angularly curved and rimmed in front; angulate
with a flattened extremity behind. Ventral margin partly
* See Geol. Mag., June, 1886, p. 272.
+ A little mask.
255
straight ; dorsal margin convex. Hinge consisting of strongly
developed, crenulated processes at the angles, separated by a.
furrow, and with corresponding depressions and ridge or bar in
the opposite valve ; thus differing in the character of hingement
from many of the associated Cytheridean forms. '
Surface smooth and convex, but strongly impressed by broad,
sunken areas along the ventral region, and by more irregular
impressions in the dorsal region, there remaining a central,
rounded but broken ridge,
One specimen ; Blue Fullers-earth Clay, Midford.
12. CYTHERE JUGLANDICA, Jones, var. MAJOR, nov.
Pl. iv., figs. 2 a, 0.
This form is like C. juglandica (Quart. Journ. Geol. Soc., vol. xl.,
1884, p. 766, pl. xxxiv., figs. 36 and 37), from the Richmond
boring, in all its essentials, but is much broader (higher).
One specimen from the Bradford Clay, Bradford.*
13. CYTHERE JUGLANDICA, Jones, var: MINOR, nov.
Pl. iv., figs. 3 a, b, ¢.
' This also approximates in all essential features to C. juglandica.
too nearly to allow of any specific distinction. The ventral
ridging is much stronger in this specimen than in either the type
or the var. major ; but, as this only represents the longitudinal
ridges of the meshes in an exaggerated form, the departure from
the type is but slight.
One specimen ; Blue Fullers-earth Clay, Midford.
14. CYTHERE WALFORDIANA, sp. n.
. Pl. v., figs. 9 a, b, ¢. .
Mr. Walford’s specimens were from the Fullers-earth Oolite
in a cutting on the Banbury-and-Cheltenham Railway, about
ej Geol, Mag., June, 1886, p. 273.
256
midway between Notgrove and Bourton-on-the-Water, east of
the Harford-road Bridge, in Gloucestershire and within the
Cotteswolds region. The section has been described by Mr.
Walford in the Quart. Journ. Geol. Soc., vol. xxxix., 1873, p. 225;
and the Ostracoda were obtained by washing the nodules there
described as occurring at the base of the Fullers-earth Blue Clay.
C. Walfordiana is represented by one valve of the usual sub-
oblong form of this class of Cythere. Rather larger than the
majority of the specimens from Midford. The anterior hinge
is distinct ; and near it are two oblique transverse furrows on
the valve, with a triangular swelling between them, having its
apex directed forwards. The anterior margin is thickly rimmed ;
and a coarse reticulation covers the valves.
« We name this species after Mr. E. A. Walford, F.G.S., through
whose kindness we are enabled to. catalogue several new forms
of Ostracoda from the above-mentioned clay found between
Notgrove and Bourton.
15. CYTHERE TRAPEZIOIDES, sp. 1.
Pl. v., figs. 10 a, 4, ¢.
Convex, oblong, with the front hinge strongly expressed,
Obliquely rounded at the ends, and nearly trapezioidal. Posterior
extremity suddenly compressed to a flat narrow rim. An
irregular wrinkling of the surface is observable on some parts of
the valve. The tubules perforating the test, in the subconcentric
pits, falsely appear, in some lights, under the microscope as
projecting spines, a condition observable in other Ostracoda.
From the base of the Fullers-earth Oolite between Notgrove
and Bourton. In Mr, E. A. Walford’s collection.
16, CYTHEREIS FULLONICA,* sp. n.
P). iv., figs. 13 a, b, ¢.
' This little form is of considerable interest, as it is the first or
* Having reference to the Fullers-earth.
257.
oldest known of those allies‘ of Cythere which have been divided
off as Cythereis on account of their quadrate angular features.
The smooth test bears, in addition to the characteristic: posterior
angles, the central tubercle usual in this genus, also a curved
lumpy ridge along the ventral region, and a smaller interrupted
ridge in the antero-dorsal region.
Two specimens from the Blue Fullers-earth Clay, Midford.
17. CYTHEREIS WALFORDIANA, sp. 1.
Pl. v., figs. 12 a, 8, ¢.
. This is near to C. fullonica (pl. iv., fig. 13), but the surface is
somewhat differently sculptured. The anterior ridge is stronger
and more continuous, and ends sharply over the hinge; the
dorsal ridge is not quite so acute posteriorly; the ventral ridge
is somewhat weaker ; and there are two small longitudinal ridges
on the posterior third of the valve. These last are slightly curved,
and one of them bears a small smooth tubercle.
One specimen from the base of the Fullers-earth Oolite between
Notgrove and Bourton. Collected by Mr. E. A. Walford, F.G.S.,
after whom the species is named.
18. CYTHERIDEA ZQUABILIS, sp. n.
PL ih, figs: 1a, 0; .¢.
‘Oblong, with symmetrically rounded and equally compressed
ends; the latter feature giving a truly lanceolate edge-view, longer
than broad, and diminishing each way from the middle. The hinge-
line (seen to the left in figure 1 @) is straight, with feeble angles,
thus associating this form with similar Cytheridew (figs. 3 and 4),
which have this character definitely though weakly marked.
Surface smooth, very convex, especially in the ventral region ;
end view, broadly ovate.
At first sight this species is something like Cythere (?) tenella,
(Quart. Journ. Geol. Soc., vol. xl, 1884, pl. xxxiv., fig. 24) ; but
the present specimen is much larger and more symmetrical.
258
‘ It has also some resemblance to Terquem’s Pontocypris sub-
deltoidea, Mém. Soc. Géol. France, sér. 3, vol. iv., 1885, p. 14,.
pl. ii., fig. 1, as far as the side view is concerned ; but there is:
no real alliance.
: One specimen ; Yellow Fullers-earth Clay, Midford.
19. CYTHERIDEA PUNCTIPUTEOLATA, sp. 1.
Pl. i., figs. 4, a, b, ¢.
This form resembles pl. i., fig. 2, in outline, but is longer and
narrower, more convex’ in the middle, and more compressed
anteriorly. Surface finely punctate, and marked with upwards
of 40 larger pits scattered about. Edge view, acute-ovate, com-
pressed anteriorly ; end view, almost circular. Hingement differs:
from that of pl. i, fig. 2, by not clearly showing crenulations on’
the teeth at the angles; but on this point we are not well satisfied.
~ One specimen ; Blue Fullers-earth Clay, Midford.
20, CYTHERIDEA TERRAI-FULLONICH, sp. 1.
Cytheridea perforata, Terquem (non Reemer). Mém. Soc. Géol.
France, sér. 3, vol. iv., 1885, p. 28, pl., iv., fig. 8.
Pl. i., figs. 5 a, 6, ©.
Broad-oblong, ends rounded, the anterior somewhat compressed
and rather broader than the posterior, which is slightly rimmed.
Surface coarsely reticulate, with large and irregularly rounded,
shallow meshes. Hingement as in pl. i., fig. 2. End view, ovate.
_ Cytheridea spinulosa, G. S. Brady, Challenger Report, 1880, pl.
XXxiii., fig. 6,is probably allied to this form. The name perforata,
having been used by Roemer, we refer M. Terquem’s species to
the form under notice.
Four specimens from the Blue, and two from the Yellow.
Fullers-earth Clay, Midford. One valve, from the base of the
Fullers-earth Oolite, between Notgrove and Bourton, is in Mr. E.,
A. Walford’s collection.
259
21. CYTHERIDEA WINWOODIANA, sp. 1.
Pl. i, figs. 2 a, b, c, d.
Smooth, sub-oblong in outline ; anterior hinge sub-angulate, as
commonly seen in these forms of Ostracoda. Edge view, narrow-
lanceolate, blunted anteriorly; end view, sub-ovate, the valves
not being very convex. Hinge consists of a crenulated tooth at
each end of a shallow groove in one valve, and corresponding
pitted depressions at the extremities of a delicate ridge in the
other. This hingement is common to the greater number of
Ostracoda here to be described, and has therefore been figured
only in a few cases (pl. iii., fig. 11; pl. iv., fig. 9).
Cytheridea Winwoodiana is comparable with Cytheridea sub-
perforata, Jones (Quart. Journ. Geol. Soc., vol. xl., 1884, pl. xxxiv.,
fig. 26) ; but the anterior extremity is less contracted and less
oblique, while the posterior is more fully rounded.
Named after the Rev. H. H. Winwood, M.A., F.G.S., by whose.
kindness we received some of the material from which these:
Ostracoda are here described.
_ Two examples from the Yellow Fullers-earth Clay, Midford.
22. CYTHERIDEA COARCTATA, sp. n.
Pl. i, figs. 3 a, b, ¢.
A narrow, convex, approximately oblong form, with oblique
ends, making it somewhat subrhomboidal. Surface smooth,
marked with a few scattered small pits. Edge view, long-ovate,
compressed at the middle; end view, acute-ovate. A form
perhaps allied to this is the Cytheropsis obliquepunctata, Terquem
(Ménm. Soc. Géol., France, ser. 3, tome iv., 1885, p. 23, pl. iii, fig. 13 ).
One specimen ; Blue Fullers-earth Clay, Midford.
23. CYTHERIDEA PUTEOLATA, sp. 2.
Pl. i, figs. 7 a, 6, ¢. ;
' Also a sub-oblong Cytheridea, having the ventral and dorsal
260
margins nearly parallel ; very convex, especially in: the posterior
third. A slight transverse depression occurs near the middle,
in front of which can be seen the lucid spots of the muscle-
mark, visible externally. These apparently consist of a row of:
four, and there are probably one or two more in front of them.
Surface smooth, with a few very faint ridges in the ventral.
region, and ornamented with scattered shallow pits. Hingement
as in pl. i., fig. 2.
Three examples ; Blue Fullers-earth Clay, Midford.
24. CYTHERIDEA RETORRIDA,* sp. %.
Pl. i., figs. 8 a, b, ¢.
_If compared with pl. i., fig. 5, this form is seen to be less
symmetrical, smaller, and narrower. The dorsal margin also is much
straighter, and the hinge-line is more defined. The posterior
and anterior ends are unequally and obliquely rounded, and the
ventral margin is much incurved. Edge view, narrow acute-
ovate, falling in sharply at the base; end view, ovate. Ornament
somewhat similar to that of pl. i, fig. 5; the carapace has a
dried up, parched, or withered appearance.
One specimen ; Yellow Fullers-earth Clay, Midford.
25. CYTHERIDEA PARALLELA, sp. n.
' Pi. 1, figs. 9 a, 6,2.
_Sub-oblong, with ends obliquely rounded, especially on the
postero-ventral margin. Hinge-line long and distinct. Valves
very convex ; the left valve overlapping the right in the posterior
region, smooth, and ornamented with some shallow, scattered
pits. Edge view, almost lanceolate, the greatest fullness in the
posterior third ; end view, almost circular.
Four or five examples from the Blue Fullers-earth Clay,
Midford.
* Parched.
261
26... CYTHERIDEA ‘SEDATA,* sp. 2.
Pl. i, figs. 10 a, 0, ¢.
Perfectly smooth and unornamented ; much like some of the
foregoing sub-oblong forms in general outline, but less convex.
Anterior end broadly rounded and compressed ; posterior end
more convex, and obliquely rounded, curving to join an incurve
on the ventral margin. Edge view, narrow-ovate ; end view,
compressed-ovate.
One specimen from the Blue, and one from the Yellow Fullers-
earth Clay, Midford.
27. CYTHERIDEA EMINULA,f sp. n.
Pl. i., figs. 11 a, 0, 6.
In general outline this approaches Cythere Blakeana, Jones
(Quart. Journ. Geol. Soc., vol. xl., 1884, pl]. xxxiv., fig. 34), but it
differs from it in ornamentation considerably, having a few scattered
pits instead of a coarse reticulation. Edge view, sharply ovate,
apiculate posteriorly ; end view, ovate. Hingement like that of
pl. i., fig. 2.
Two examples ; Blue Fullers-earth Clay, Midford.
‘28. CYTHERIDEA SUBEMINULA, sp. n.
Lees MOS, 8. Bb
A form nearly allied to C. eminula (pl. i., fig. 11), but squarer,
flatter, and more swollen behind. The surface also differs from
that of C. eminula, in being quite smooth.
One specimen from the base of the Fullers-earth Oolite,
‘between Notgrove and Bourton. In Mr. E. A. Walford’s
‘collection,
29, -CYTHERIDEA PENTAGONALIS, sp. n.
Pl. ii, figs. 1 a, 6, ¢
The dorsal margin of this species has a distinct, but short and
SS ee ee
* Quiet or calm. + Rising slightly,
262
slightly incurved hinge-line ; the anterior margin slopes with a
long curve round to the straight ventral edge, while the posterior
margin has two slopes—one ventral, and one meeting the hinge-
line. These five border-lines give a pentagonal aspect to the
valve. In the edge view the convexity of the valve is nearly
equal, making an acute-oval ; the end view is ovate, somewhat
compressed dorsally. Surface smooth, with small scattered pits.
Hingement as in pl. i., fig. 2.
One specimen ; Yellow Fullers-earth Clay, Midford.
30. CYTHERIDEA SUGILLATA,* sp. n.
Pl. ii., figs. 2 a, b, ¢.
Obovate in outline, almost semicircular anteriorly, more
convex posteriorly ; the three free margins have a broad and
strong rim, that on the ventral margin very nearly hidden by the
convexity of the valve. Surface smooth, but raised into
irregular wales, weals, or broken rolls in the dorsal region, and
into a loosely-reticulate ridge in the ventral region ; the weals
run together posteriorly, but their junction anteriorly is defined
by a small tubercle. Hingement as in pl. i., fig. 2.
Two examples; Blue Fullers-earth Clay, Midford.
31. CYTHERIDEA REFECTA, sp. n.
Pl. ii, figs. 3 a, 5.
A sub-oval Cytheridea, rounded at the ends, broadest posteriorly ;
nearly straight on the ventral margin, somewhat sinuous dorsally,
with the anterior hinge-joint marked by a small tubercle.
Surface somewhat depressed and irregularly undulate, as if it
had been crushed and repaired—this feature, however, appears to
be natural. Edge view, a narrow acute-oval; end view (not
drawn), acute-oval, compressed, and sinuous.
Two or three examples ; Blue Fullers-earth Clay, Midford.
--* * Beaten, with weals or wales. -
263
- 32. CYTHERIDEA VULSA,* sp..n.
Pl. ii., figs. 4a, 6.
Sub-oblong, rounded in front, obliquely rounded behind,
straight on the ventral and dorsal margins. Hinge-line long and
distinct, terminating anteriorly with a faint tubercle. Surface
irregularly convex, depressed and sulcate in the dorsal region,
‘and raised along the ventral region, as if forcibly pinched up.
‘The general appearance, looking at the carapace with the dorsal
‘margin uppermost, is that of a partially melted wax seal,
hanging in a curved lump away from the upper margin, and
showing a furrow at the top.
-. One specimen from the Blue. Fullers-earth Clay, Midford ;
another specimen of this form has been sent to us by Mr. E. A.
Walford, F.G.S., from the base of the Fullers-earth Oolite
‘between Notgrove and Bourton.
33. CYTHERIDEA HORATIANA, sp. n.
Pl. ii., figs. 5 a, b.
This large, smooth, and somewhat oval form, has a short
hinge-line in the middle of an arched dorsal margin, with a
‘strong shoulder. The ventral margin is nearly straight, but
‘sinuous, owing to a slight median convexity. The ends are
‘rounded, rather narrow; the anterior largest, but more com-
pressed than the posterior. The lucid spots of the muscle-mark,
‘seen through the shell, are arranged in a group much the same
.as in other Cytheridew. Hingement the same as in pl. 1, fig. 2.
There is some fine punctation on the surface of the posterior sixth
of the carapace, but it is not shown in the-figure.
We name this species after Mr. Horace B. Woodward, F.G.S.,
to whom we are indebted for some of the material from which
these forms were obtained.. 1 ae
, Three examples ; Blue Fullers-earth Clay, Midford. -
- * Pulled out, or pinched up.
264
34. CYTHERIDEA OBOVATA, sp. “n.
Pl, ii., figs. 6a, 6, ¢.
Smooth and very convex; obovate, the anterior being broader
than the posterior ; nearly symmetrical, but-the dorsal margin is
more rounded than the-ventral. Edge view, long oval; end
view, ovate. A slight notch (not shown in the figure) marks the
junction of the anterior and the ventral margins. The hinge-
ment in the specimen from which our figures are taken is
beautifully perfect, and consists of two crenulated ridges, running
side by side and gradually dying away in the middle third of the
hinge-line. This is precisely the same feature as seen in Cytheridea
pinguis, Jones, Monogr. Tert. Entom., Pal. Soc., 1856, p. 43,
pl. ii, figs. 4¢, 4f.
Two or three examples ; Yellow Fullers-earth Clay, Midford.
The side view of this form seems to have a close resemblance
to that of Terquem’s Bairdia affinis (op. cit. p. 8, pl.-i., fig. 1);
but there is no real affinity between the two.
35. CYTHERIDEA SPINIGYRATA, sp. 2.
Pl. ii, figs. 7 a, b, ¢.
Near Cythere drupacea, Jones (Quart. Journ. Geol. Soc., vol. xl.,
i884, p. 772, pl. xxxiv., fig. 30), but the posterior end is much
broader, and the ornament is more distinctly gyrate, with prickles
instead of pits. It is also denticulate on the front margin.
Swollen in posterior ventral region. Hinge-line distinct, and
longer than in C. drupacea. Hingement, that of pl. i, fig. 2.
Edge-view, long-ovate ; end view, ovate.
One specimen only; Blue Fullers-earth Clay, Midford.
36. CYTHERIDEA SPINIFASTIGIATA, sp. 2.
Pl. ii, figs. 8 a, 0, ¢.
_ This belongs to the same group as the last. It is much swollen
in the ventral region, the swelling hiding the incurved margin.
265
The small notches seen at the anterior hinge are probably due
to fracture. Ornament consisting of delicate longitudinal ridges,
bearing short, sharp spines. Hingement, as in pl. 1,, fig. 2.
One specimen ; Blue Fullers-earth Clay, Midford.
37. CYTHERIDEA SUBTRIGONA, sp. 2.
Pl. ii,, figs. 9 a, 5, ¢.
This form differs from Cytheridea obovata, pl. ii., fig. 6, in
having a narrower anterior, and a broader posterior margin ; and
in being somewhat angular at the shoulder or front end of the
hinge-line. The edge and end views are less convex than those
of C. obovata. Hingement, the same as pl. 1, fig. 2.
Terquem’s Cytheridea fabacea (op. cit. p. 27, pl. iv., fig. 4) is
allied to the form here figured and described.
Three or four examples ; Blue Fullers-earth Clay, Midford.
38. CYTHERIDEA POLITULA, sp. 1.
Pl. v., fige: 7 a, 6G, ¢.
Small, sub-triangular, smooth, and sparsely pitted. Cytheridea
perforata of the Tertiary and Cretaceous formations is allied to
this form. The tubules at the base of the pits appear falsely as
spinules, in some lights, under the microscope.
One specimen from the base of the Fullers-earth Oolite
between Notgrove and Bourton. In Mr. Walford’s collection.
39. CYTHERIDEA BLAKEANA, Jones.
Pl. ii, figs. 11 a, b, ¢.
Cythere Blakeana, Jones, Quart. Journ. Geol. Soc., vol. xl., 1884,
p. 772, pl. xxxiv., figs. 34, 35.
This appears to be the same as Cythere Blakeana from the
Richmond boring. Although slightly narrower posteriorly, it
agrees in the hingement (as in pl. i, fig. 2) and other important
U
266
features. In outline C. Blakeana has some alliance with the recent
Cythere impluta, Brady (Challenger Report, 1880, p. 76, pl. xvi.,
fig. 3), but this latter has a fuller ventral margin, and a more
sharply marked outline.
Two examples ; Blue Fullers-earth Clay, Midford.
40. CYTHERIDEA RENOIDES, sp. n.
Pl. iii., figs. 1 a, b, ¢.
Subreniform, smooth, but pitted with large, shallow, scattered
holes. Ventral margin slightly incurved ; dorsal margin convex,
but with a distinct hinge-line. Ends rounded, the posterior
narrowest. Edge view, bluntly lanceolate ; end view, broad-
ovate. Hingement, like that of pl. i., fig. 2.
G. S. Brady’s figure of Cytheridea papillosa, Bosquet (Trans.
Zool. Soc., vol. v., 1866, pl. lviii., fig. 8), is almost identical in
outline with our figure, but it is broader (higher) than Bosquet’s
species ; and neither of the two agrees with ours in the surface
ornaments and end view.
Four examples from the Blue, and one from the Yellow Fullers-
earth Clay, Midford.
41. CYTHERIDEA PULVINAR,* sp. n.
Pl. iii., figs. 2 a, b, ¢.
A large and sub-ohlong form, both ends broadly rimmed ;
semicircular in front, angular behind, and having both the
ventral and the dorsal margin sinuous and swollen. Surface
smooth ; transversely undulate to a slight degree, and marked
with large shallow scattered pits. Edge view, lanceolate, with
pinched ends; end view, ovate, with blunt ends. Hingement,
as in pl. i., fig. 2.
Three specimens, Blue Fullers-earth Clay, Midford.
* A pillow.
267
42. CYTHERIDEA DOLABRA,* sp. n.
Pl. iii., figs. 3 a, b, ¢.
Dorsal margin straight in the middle, strongly sloping towards
each end from the hinge-angles; the posterior slope incurved
like that of a Buirdia. Ventral margin rounded before and
behind, and incurved in the middle. Surface smooth, but marked
with scattered pits, as in the two foregoing species. Edge view, long
acute-ovate ; end view, acute-ovate. Hingement, as in pl. i.,, fig. 2.
Reuss’ C. notata (Haidinger’s Nut. Abth., vol. iii., 1850, pl. ix.,
fig. 16), approaches this form ; but Reuss’ species has a strong
antero-ventral notch, and a curved transverse mid-dorsal ridge,
dying out towards the antero-ventral region.
Four examples ; Blue Fullers-earth Clay, Midford.
43. CYTHERIDEA TRANSVERSIPLICATA, sp. 7.
Pl, iii., figs. 4 a, 6, ¢.
Broadly curved anteriorly, angulate behind. Dorsal margin
almost straight, but slightly projecting at the anterior hinge.
Ventral margin sinuous, being incurved in the middle. The valve
has somewhat the outline of the sole of a human foot. Surface
smooth, but with numerous small transverse undulations (well
seen in the edge view), and marked all over with large, irregular,
shallow pits. Edge view, bluntly lanceolate, with wrinkled
outline ; end view, oval. Hingement, the same as pl. i., fig. 2.
One specimen ; Blue Fullers-earth Clay, Midford.
44, CYTHERIDEA EGREGIA, sp. n.
Pl. iii., figs. 5 a, }, ¢
Nearly allied to the last, but broader, more oblique anteriorly,
and rather less angular behind. Surface bearing faint cross
* An axe,
268
wrinkles or undulations; not pitted; with a few limited
flattened areas in the anterior and posterior regions. Hingement,
as in pl. i., fig. 2.
One specimen ; Yellow Fullers-earth Clay, Midford.
45, CYTHERIDEA VISCERALIS,* sp. n.
Pl. iii., figs. 6 a, 6, c.
Oblong with oblique ends, subrhomboidal ; truncate in front,
angular behind. Surface punctate, swollen into irregular lumps,
and having a short depression in the antero-ventral region, and
a flattened area along the postero-ventral border.
One specimen; Blue Fullers-earth Clay, Midford. In Mr.
Walford’s collection, there is a specimen from the base of the
Fullers-earth Oolite between Notgrove and Bourton, which we
regard as an immature specimen of this form. It differs from the
figured individual in being smaller, and in having the postero-
ventral swelling more prominent; thus giving the valves a more
triangularly sagittate edge view.
46. CYTHERIDEA STRIBLITA,t sp. 7.
Pl. iii, figs. 7 a, b,c.
Sub-oblong, with rounded anterior margin, and angular
posterior margin; sloping on the postero-dorsal margin, and
flattened at its extremity. Surface smooth, with a few pits ;
irregularly swollen, and partially crossed by a sulcus, it looks
like a dough cake. The hingement is as in pl. 1, fig. 2.
Two specimens; Blue Fullers-earth Clay, Midford
47. CYTHERIDEA IGNOBILIS, sp. 7.
Pl, iii., figs. 9:a, b, ¢.
Neatly sub-oblong, convex; rounded in front, straight at
eee UE EES EEE ESET
* Like bowels. + A twisted cake.
269
upper and lower margins, and bluntly angular behind. This
simple form is covered with minute puncta, amongst which are
sparsely scattered a few pits. Edge view, sub-lanceolate; end
view, acute-ovate. Hingement, as in pl. i., fig. 2.
Two specimens ; Blue Fullers-earth Clay, Midford.
48. CYTHERIDEA VENTROSA, sp. n.
Pl. iii., figs. 10 a, 5, ¢.
Obovate, but angular and lipped behind, and rather narrowed
anteriorly. Convex and quite smooth. Edge view, sharp-oval ;
end view, ovate. Hingement, like that of pl. i., fig. 2.
One specimen ; Blue Fullers-earth Clay, Midford.
49. CYTHERIDEA PURA, sp. Nn.
PI. iii., figs. 11 a, 5, ¢, d.
A delicate and simple form, much like a common type of
Cythere, having a curved dorsal margin, rounded anterior, angular
posterior, and swollen ventral margin, defined at each end by a
slight depression. Altogether, sub-oval, smooth, and convex.
Hingement, as in pl. i., fig. 2. In some respects allied to Cythere
virginea, Jones (Monogr. Cretaceous Entom., Palwontographical
Society, 1848, p. 12, pl. i, fig. 2n). If magnified 75 diameters,
the surface has the appearance of hammered metal.
One specimen ; Blue Fullers-earth Clay, Midford.
50. CYTHERIDEA LIMACIFORMIS,* sp. 2.
Pl. iii., figs. 12 a, 8, ¢.
Ovate-oblong, very convex ; hinge-line distinct ; ventral region
swollen ; posterior end somewhat angular and lipped. There are
some faint ridges parallel with the ventral margin, not well
shown in the figure. Hingement, like that of pl. i, fig. 2.
One specimen ; Blue Fullers-earth Clay, Midford.
* Like a slug (resting).
270
51. CYTHERIDEA TRAPEZOIDALIS, Terquem.
Pl. iv., figs. 1 a, 0.
Mém. Soc. Géol., France, ser. 3, vol. iv., 1885, p. 31, pl. iv.,
figs. 20 a, }, c.
Straight on the dorsal margin, angular behind, with the
postero-ventral slope reaching into the middle of the ventral
margin, giving to the latter an obtuse angle. Both anterior
and posterior margins are lipped. Surface moderately convex,
smooth, but sparsely pitted; and with two or three shallow
transverse sulci in the dorsal region. Hinge-line very long.
Terquem’s figures are not quite equal among themselves, but,
taking the average, we think that they are not unlike the form
here figured and described.
One specimen; Blue Fullers-earth Clay, Midford.
52. CYTHERIDEA PERSICA,* sp. 1.
Pl. iv., fig. 4.
Roughly obovate, much resembling a coarsely marked peach-
stone, rounded in front, angular behind, and lipped at each ex-
tremity. A strong longitudinal keel is developed on the ventral
margin of the valve, and this is repeated, with less intensity, by
the raised ridges of the concentric reticulation on that region.
Edge view (not drawn), compressed ovate, with apiculate ends.
Hingement, like that of pl. 1, fig. 2.
One specimen ; Blue Fullers-earth Clay, Midford.
53. CYTHERIDEA BICARINATA, sp. 2.
Pl. iv., figs. 5 a,b, ©.
Sub-obovate, obliquely rounded in front, angular and lipped
behind. Dorsal margin oblique, with a straight hinge-line,
which is tuberculate externally. The ventral region bears two
* With reference to the stone of a peach.
271
ridges, one of which overhangs and hides the margin. The
surface is more strongly reticulate than shown in the figure 3
it has a low tubercle on the anterior third, and a limited
impression on the posterior region, near the dorsal border.
Edge view, bluntly sub-sagittate ; end view, sub-quadrate.
Four’ examples ; Blue Fullers-earth Clay, Midford,
54, CYTHERIDEA OSTREATA,* sp. n,
Pl. iv., figs. 6 a, b, ¢.
A large and sub-oblong Cytheridea, obliquely rounded in front,
contracted and irregularly angular behind. Dorsal margin
straight; anterior hinge-angle prominent, hinder hinge-angle
hidden by a coarse, irregular growth of shelly matter. Surface
reticulate, with irregular meshes, looking like. oyster-spat. Two
strong ridges runs along the ventral region, the upper of which
turns upwards, and runs parallel with the two ends of the valve
for some distance. Hingement, as in pl. i., fig. 2,
One specimen ; Yellow Fullers-earth Clay, Midford.
55. CYTHERIDEA RUGIFERA, sp. n.
Pl. v., figs. 11 a, b, ¢.
Oblong, obliquely rounded in front, rounded and deeply
rimmed behind. Upper and lower margins slightly incurved.
Surface rugulose (not well shown in the figure), with numerous
small, shallow, irregular depressions. A slight curved ridge
rises above and behind the front hinge.
From the base of the Fullers-earth Oolite between N otgrove
and Bourton. In Mr. E. A. Walford’s collection.
56. CYTHERIDEA ACUTIPLICATA, Nn. Sp.
Pl. iv., figs. 7 a, b; 8 a, b, ¢
Obovate, being broader (higher) anteriorly than posteriorly.
* Scabby, as if covered with small oyster shells,
272
Surface marked with sharp longitudinal ridges. There are
two very closely allied forms of this species. In fig. 7 the
anterior margin is thickened and pitted, and the ridges, instead
of occupying the middle of the valve (as in fig. 8), occupy the
posterior half: fig. 7 has also a longer valve, and the dorsal region
differs from that of fig. 8, in not being compressed. Hingement,
as in pl. i, fig. 2.
Two specimens of fig. 7 from the Blue Fullers-earth Clay ;
and one specimen of fig. 8 from the Blue, and one from the
Yellow Fullers-earth Clay of Midford.
57. CYTHERIDEA CRATICULA,* sp. n.
Pl. iv., figs. 9 a, 6, c, and 10 a, J, «.
These two specimens appear to us to belong to one form, fig. 9
being weaker in its details, and narrower in the posterior region
than fig. 10. Taking the latter (fig. 10) as the type, we may
describe it as having an oblong carapace, with an angular posterior
margin. The surface bears several longitudinal ridges, more or
less curved, coarsely reticulate in the interspaces, the meshes
passing up on the sides of the largest ridges, making them
fenestrate. We consider fig. 9 rather as a weak variety, than as
an immature form of fig. 10. Hingement, as in pl. i, fig. 2.
Of fig. 9, one specimen from the Yellow Fullers-earth Clay ;
of fig. 10, two specimens from the Blue Fullers-earth Clay,
Midford.
58. CYTHERIDEA BRADIANA, Jones.
Pl, iv., figs. 11 a, 0, ¢.
Cythere Bradiana, Jones, Quart. Journ. Geol. Soc., vol. xl., 1884,
p. 772, pl. xxxiv., figs. 38 a, b.
* A gridiron
273
We see no reason for separating this form from that figured
under the name of C. Bradiana, from the Richmond boring.
Hingement, like that of pl. i, fig. 2.
This character of ornament, ridges with intermediate rows of
pits, is figured also in Cythere Jurinei, Minster, by G. S. Brady,
Trans. Zool. Soc., vol. v., 1866, p. 372, pl. lix., fig. 1.
Five examples from the Blue Fullers-earth Clay, Midford.
59. CYTHERIDEA FULGURATA, sp. 2.
Pl. iv., figs. 12 a, 6, ©.
Sub-obovate, convex, with straight but oblique dorsal and
ventral margins; rounded and lipped in front, and angular,
broadly lipped, and depressed behind. Surface smooth, and
bearing two longitudinal, slightly curved ridges in the ventral
region, and several minor oblique ridges, irregular, but radiating
from the middle of the dorsal, towards the ventral region.
Hingement, as in pl. i., fig. 2.
Four examples from the Blue Fullers-earth Clay, Midford 5
and two or three examples from the Bradford Clay, Bradford.
60. CYTHERIDEA EXIMIA, sp. 7.
Pl. v., figs. 5 a, 0, c.
Oblong, with obliquely rounded ends; straight dorsal, and
slightly sinuous ventral margin. Both extremities have a
depressed rim. Surface very convex, especially in the posterior
region ; finely punctate, and also pitted with scattered shallow
pits. Edge view, lanceolate. End view, broadly ovate, almost
circular. The hingement is the same as in pl. i, fig. 2.
One specimen ; Yellow Fullers-earth Clay, Midford.
274
61. CYTHERELLA FULLONICA, sp. n.
Pl. i,, figs. 12 a, 6, ¢.
Sub-oblong, compressed, with a faint median sulcus, slightly
incurved on the ventral, and somewhat angular on the dorsal
margin, symmetrically rounded anteriorly; contracted posteriorly.
Surface smooth, muscle-mark unusually distinct, in the ordinary
shallow depression.
This approaches C. pulchra, G. S. Brady (Trans. Zool. Soc.,
vol. v., 1866, p. 361, pl. lvii., fig. 5), in general appearance, but
its ventral incurve is more marked, and the _postero-dorsal
margin has a stronger angle and slope. The dorsal process is
analogous to that seen in C. dromadaria, G. S. Brady ( Challenger
Report, 1880, p. 173, pl. xliii., fig. 6), but is very rare in Cytherella.
C. Leopolitana, Reuss (Denkschr. k. Ak. Wiss., Wien, vol. vii.,
1854, p. 140, pl. xxvii, fig. 4), has projections on both upper and
lower margins.
Four examples from the Blue, and four from the Yellow
Fullers-earth Clay, Midford. We have also seen three similar
valves, but with the dorsal process obsolete or nearly so, in the
small collection of Ostracoda sent to us by Mr. E. A. Walford,
and collected at the base of the Fullers-earth Oolite between
Notgrove and Bourton. ~
62. CYTHERELLA CATENULATA, Sp. 1.
Pl. v., figs. 6 a, b,c.
This Cytherella, of the usual oblong outline, with rounded ends
and slightly incurved ventral region, has an irregularly wavy
surface, very clearly seen in the edge view. The surface is
ornamented with a neatly regular concentric reticulation, the
elongated meshes of which assume a chain-like appearance.
Nine examples from the Blue, and one from the Yellow
Fullers-earth Clay, Midford. We have also received one specimen
from the base of the Fullers-earth Oolite between Notgrove and
Bourton, from Mr. E. A. Walford, F.G.S,
275
TABLE OF THE FOSSIL OSTRACODA FROM THE FULLERS-
EARTH OOLITE AND THE BRADFORD CLAY.
[ Zoologically arranged. |
MIDFORD.
Blue Yellow Base of Bradford
F.E. Clay.
Clay. Clay. Oolite.
1 Bythocypris Winwoodiana, 7. ... wae
2 Macrocypris Horatiana, n. nae x
3 terrz-fullonice, 7.... x
4 Bairdia Juddiana, J. cs
5 trigonalis, J. ... S. ryiyk Ye
x
aie
6 fulloniea, 7.
7 2 spp. . ae
8 Cythere spherulata, 7. wa Naehedes XG
9 2 speciosa, 2. x
10 corrosa, 7. cee aoe cere.
11 oscillum, 7. ae R
12 juglandica, J. var. major, n. es x
13 var. minor, nN, ae ae.
14 Walfordiana. 7. Le Cn es x
15 trapezioides, 7. aa i at x
16 Cythereis fullonica, x. ... EP ae x
17 ———— Walfordiana, n. de — x
18 Cytheridea cequabilis, 2. atk SN a
19 ——_——— punctiputeolata, n. ... Si
20 —— terre-fullonice, n. ... ae ee
21 ——_———- Winwoodiana,n. ... Sof hohe
22 ———-—— coarctata, n. x
23 ———-—— puteolata, n. he Yh eS:
24 ———_——-retorrida, n. re ee
25 ———-—— parallela, ... x
26 —————- sedata, n. ... as See AR To
27 ——_——— eminula, n. x
28 ————— subeminula, z. tee es x
29 —_———- pentagonalis,n. _... oes x
30 ——_———- sugillata, n. a re we
HTT
refecta, 7.
——_—— vulsz, 7.
— Horatiana, 7.
——_—_—— obovata, 7.
——_——- spinigyrata, 7.
spinifastigiata, 7.
—_—_—_——- subtrigona, 7.
—_—__—_—— politula, n.
4 Baka, jal
renoides, 7.
——_—_—— pulvinar, n.
dolabra, 7.
—____—— - transversiplicata, 7.
egregia, 7.
————_ visceralis, 7.
—_—_—— striblita, 7.
ignobilis, ”.
——__—_—_—_ ven trosa ” ...
_—_—__—. pura, 2. ..-
__—___— limaciformis, 7.
—_—
— persica, 2. ...
___—— hbicarinata, 7.
—__—_—— ostreata, 7.
—__—_——-_ rugifera, n.
—_____—— acutiplicata, n.
—___—— craticula, 7.
Bradiana, J.
—___—_—— fulgurata, 7.
—————-
—_—_—_——- eximia, %.
Cytherella fullonica,
catenulata, 7.
—_——
trapezoidalis, Terquem
MIDFORD.
Blue Yellow —s
Clay. Clay. Oolite.
vee x
«00 ose x es x
. x
— x
x
. x
x
— = x
ee x
x x
. x
ee x
x
eee — x
2:4 — —
x
eee x
x
x
x
ese x
eee x
wee —= x
o- — x
. x x
ose x x
oe =
ace 1 —_
. . es x
a x x x
eee x x x.
Bradford
Clay.
277
EXPLANATION OF THE PLATES.
N.B. All the Figures are magnified 50 diameters.
Plate i., Figs. 1a, b,c. Cytheridea cequabilis, sp. x.
— » 24,6, c,d. Cytheridea Winwoodiana, sp. n.
i » 34,6, c. Cytheridea coarctata, sp. 2.
” » 4a,b,c. Cytheridea punctiputeolata, sp. x.
S ’, 54a, 6,c. Cytheridea terrz-fullonice, sp. n.
os » 64a,6,c. Cythere spherulata, sp. 7.
of » 74a, 0,¢. Cytheridea puteolata, sp. n.
” » 84a,6,c. Cytheridea retorrida, sp. n.
3 » 94a,0,¢. Cytheridea parallela, sp. n.
- » 10a, 6, c. Cytheridea sedata, sp. n.
+ » lla,6,c. Cytheridea eminula, sp. n.
” » 12a,6,c. Cytherella fullonica, sp. 7.
Plate ii., Figs. 1 a, 6, c. Cytheridea pentagonalis, sp. n.
55 » 2a, 6,c¢. Cytheridea sugillata, sp. n.
a » 38a,b. Cytheridea refecta, sp. n.
en » 4a,6. Cytheridea vulsa, sp. 2.
is » 5a,6,c. Cytheridea Horatiana, sp. n.
rr » 6a,6,c. Cytheridea obovata, sp. n.
&n » 7a, 0,c¢, Cytheridea spinigyrata, sp. n.
5 » 8a,b,c. Cytheridea spinifastigiata, sp. n.
x » 94,6,c. Cytheridea subtrigona. Sp. N.
5 » 10a, b,c. Cythere? speciosa, sp. n.
“ » 1l4a,0,¢,d. Cytheridea Blakeana, Jones.
is » 12a, b,c. Cythere corrosa, sp. n.
Plate iii., Figs. la,6. Cytheridea renoides, sp. n.
os » 2a,b. Cytheridea pulvinar, sp. n.
or » 24,6, c, Cytheridea dolabra, sp. n.
5 » 4a,6,c. Cytheridea transversiplicata, sp. n.
F » 54a,6,c. Cytheridea egregia, sp. n.
os » 6a, 6,c, Cytheridea visceralis, sp. n.
¥ » 74,6, ¢, Cytheridea striblita, sp. n.
“ » 8a,0,c, Cythere oscillum, sp. n.
cf » 94a,6,c. Cytheridea ignobilis, sp. n.
278
fs » 10a,b,c. Cytheridea ventrosa, sp. n.
= » lla,b,c. Cytheridea pura, sp. n.
5s » 12a,6,c. Cytheridea limaciformis, sp. n.
Plate iv., Figs. 1a, b,c. Cytheridea trapezoidalis, Terquem
2 a, b, c, Cythere juglandica, Jones, var. major, nov.
3 a, b, c. Cythere juglandica, Jones, var. minor, nov.
53 Fig. 4 Cytheridea persica, sp. n.
33 Figs. 5 a, b,c, Cytheridea bicarinata, sp. x.
6 a, 6, c. Cytheridea ostreata, sp. n.
7 a,b; and 8a, b,c. Cytheridea acutiplicata, sp. x.
9 a, b,c; and 10 a, 6, c, Cytheridea craticula, sp. n.
11 a, b, c. Cytheridea Bradiana, Jones.
12 a, b, c. Cytheridea fulgurata, sp. 7.
13 a, 6, c. Cythereis fullonica, sp. 7.
Plate v., Figs. 1 a, b, c. Bythocypris Winwoodiana, sp. x.
2a, b, c. Macrocypris Horatiana, sp. 7.
3 a, 6, c. Macrocypris terree-fullonice, sp. n.
4 a, b, c. Bairdia fullonica, sp. x.
5 a, b, c. Cytheridea eximia, sp. n.
6 a, b, c. Cytherella catenulata, sp. n.
7 a, b, c. Cytheridea politula, sp. 7.
8 a, b, c. Cytheridea subeminula, sp. 7.
- » 94a,6,c. Cythere Walfordiana, sp. 7.
10 a, 6, c. Cythere trapezioides, sp. n.
11 a, 6, c. Cytheridea rugifera, sp. n.
12 a, 6, c. Cythereis Walfordiana, sp. n.
”? 499
Landslips and Subsidences. By W. PuMPHREY, Esq.
(Read 16th November, 1887.)
My excuse for taking up your time on the present occasion
must be that having been accidentally very near the scene of the
disaster at Zug, on July 5th, I became considerably interested
in the affair, and possibly am inclined to attach too great
importance to it.
Proc. BathNH.s« Antia.F. Club. Vol VI. No.3 .1888. PII
CD.S&GW. del. Geo West & Sons lith.etimp.
OSTRACODA OF THE FULLERS-EARTH OOLITE.
Proc. BathNH.« Antia.F. Club. Vol VI. No.3 .1888.
1
CD.S&G.W del. Geo West & Sons ith et imp.
OSTRACODA OF THE FULLERS-EARTH OOLITE.
Proc. BathNH.z Antia.F. Club. Vol-VI. No.3 .1888. PIM
C.D.S&GW del . Geo West & Sons lith.et imp.
OSTRACODA OF THE FULLERS-EARTH OOLITE.
Proc. BathNH.« Antia.F. Club. Vol VI. No.3 .1888. PLIV
CD.S&G.W. del Geo West & Sons, lith.et imp
OSTRACODA OF THE FULLERS: EARTH OOLITE.
Proc. BathNH.a Antia.F. Club. Vol VI. No.3 .1888. PLY
CD.S&GW. del.
Geo West & Sons, lith et imp.
OSTRACODA OF THE FULLERS-EARTH OOLITE.
279
Before referring to the event of July it may be well to glance at
the general contour of the surrounding country. The Lake of Zug,
which has an elevation above the sea of 1,388 feet, and a depth of
about 1,300 feet, is at its upper and southern end hemmed in by the
Rigi and the Rossberg, which are separated by the low pass, by
means of which the St. Gothard railway is enabled to avoid some
of the engineering difficulties that the bizarre outline of the Lake
of Lucerne presented. From this low pass and from the northern
slopes of the Rigi, and from the western slopes of the Rossberg a
series of small streams send down their waters to the Lake, but
the quantity is not large. The greater part comes from the
northern slopes of the Rossberg, and after passing through the
Egeri See, takes a northerly direction till it passes the hills that
bound the Lake of Zug on the east, when turning to the west and
then to the south-west it falls into the Lake very near its outlet.
In the latter part of its course it traverses a very level tract of
country, the result apparently of fluvial detritus.
The Rigi and the Rossberg have not contributed largely
towards the filling up the Lake of Zug—the alluvial tract at the
head of the Lake being of small extent. But they have given us
some striking examples of landslips on a large scale. They are
both mainly composed of beds of conglomerate (Nagelfluh)
consisting of calcareous and silicious pebbles cemented together
by a calcareous infiltration, which has bound the whole into a
concrete mass, so firm that very often the compacted pebbles will
break across rather than quit the mass. These beds of conglome-
arate are separated by beds of sand and clay, and anything that
seriously disturbs these beds has a tendency to alter the relation
in which they stand towards each other. Hence changes have
taken place from time to time, and within the last hundred years
two very notable events of this kind have happened. In 1795
there issued from below some of the upper strata of the Rigi, a
vast outflow of mud, which, like a stream of lava, rolled down the
mountain side, spreading ruin and desolation in its course. It is
280
said to have taken fourteen days in reaching the Lake of Lucerne.
This of course gave ample time for escape, and we believe that no
lives were lost, though the destruction of property was very great.
There is also evidence in the piled-up masses of conglomerate
which form what is called the Felsenthor, that at some period of
which we have no record, a berg-fall, similar in kind to that which
we are about to notice took place on the Rigi.
The summer of 1808 had been very wet and we may assume
had loosened the intervening beds of clay and sand, or at least
had rendered them so slippery that the superincumbent strata
which rested on them at a considerable angle slid forward, and
the crest of the mountain was precipitated into the valley below.
The mass that fell was about 1,000 feet in length and 100 feet
in thickness and of unknown breadth. Such a mass descending
from a height of between 3,000 and 4,000 feet pressed forward
with irresistible force, bearing down everything that was in its
course, overwhelming villages—filling up about one third of the
Lake of Lowerz and doing untold damage to life and property.
The masses of rock now fill the valley on the eastern side of the
Jlow col on which the village of Goldan stands, and many
of them rest on the slopes of the Rigi about four miles from the
spot whence they began their descent. Though it is now nearly
80 years since the disaster occurred (Sept. 5th, 1808), the crest
of the Rossberg, as seen from the Rigi, appears entirely barren,
and the course of the falling rock is clearly evident all down the
mountain side.
In both these cases the exciting cause appears to have been
the same—an excessive fall of rain rendered the beds of clay
' &c., soft or slippery. In the first case the clay and sand were
squeezed out by the pressure of strata whose angle of inclination
was not sufficient to cause them to slide down ; in the second the
angle of inclination determined the fall of the mass—the sub-
stratum became so altered in its condition as no longer to give
the support that had hitherto sustained the rock in its place.
281.
However disastrous these berg-falls may be they are too
common among the Alps to excite any great attention, except
when of very exceptional extent, as in the case just mentioned ;
but when a large tract of land that looks like solid ground, with
substantial houses built on it and covered with orchards and
gardens sinks down and become part of an adjoining lake we
are more likely to feel and express great surprise. Thus all
Switzerland was taken by surprise when on July 5th of the
present year the telegraph flashed over the whole country, the
intelligence that a portion of the little town of Zug had dis-
appeared below the surface of its lake; the thing seemed utterly
unlikely and the news was received with much incredulity—
nevertheless it was true. The town of Zug is situated at the
north-eastern corner of the lake, at a point where the hills that
have formed the eastern rampart of the lake, continuing onward in
northerly direction leave its shore, which now consists of a dead
level plain. Through this level plain the principal affluent of the
lake finds its way, having in all probability been the agent in pro-
ducing the level plain through which it now flows. Two or three
smaller streams also fall into the lake near Zug. The greater part
of the town lies on the gentle slop of the hills—but a long suburb
extends along that margin of the lake, which I have spoken of as
part of the level alluvial plain. It was in this suburb that the
disaster occured. I have noticed a peculiarity in the Lake of Zug
and possibly some connection may exist between these repeated
subsidences and this peculiarity. The river, Lorze, the principal
feeder of the lake, falls into it at a point not more than a kilometer
and a half (rather under a mile) in a direct line from the place
where the waters of the lake have their outlet.
Whatever may have been the causes, either predisposing or
exciting, the facts are these:—About mid-day, July 5th, some of
the houses that formed part of the suburb I have mentioned sud-
denly sank down, and later in the afternoon other houses, amount-
ing in all to about thirty, were swallowed up, and where but a few
v
282
hours before, stood a substantial hotel—new built and not yet
opened for guests—a street of substantial houses, orchards and
gardens, there was nothing but mud and water, floating wreck.
Though some notice of what might happen was given by cracks
in some of the houses and in the quay that was in course of con-
struction, yet the actual fall was so sudden that about thirty
persons were either drowned or crushed to death in the ruins. I
was staying for a few days at Lucerne, distant about 18 miles, so
accompanied by my brother we went over on the afternoon of the
6th to see for ourselves the extent of the disaster ; but we were
able to see but very little We found the usually quiet town full
of an excited crowd, and all the approaches to the scene guarded
by the Federal soldiers, who would not allow any person to go
near, as it was considered quite unsafe. We were therefore
obliged to return to Lucerne with little definite information ; but
with a knowledge that rumour had not exaggerated the extent of
the disaster.
The Rev. E. Hill, who visited the spot about two weeks after,
when the excitement had calmed down and it was possible to
investigate the causes, &c., read a paper at the meeting of the
British Association, at Manchester, on the subject. He stated
that it had been proved that the first 10 or 12 feet of the soil
consisted of alluvial detritus—and below this there was an
unknown depth of soft oozy stuff. It would seem that the
accumulation of buildings on a soil of this kind had ultimately
produced a state of unstable equilibrium, and anything that
tended either to increase the superincumbent pressure or remove
in ever so slight a degree the support from below would destroy
that equilibrium. It is worth notice that similar calamities have
happened very near the same spot. In 1435 a similiar subsidence
took place accompanied, it is said, by a loss of 160 lives—and
again about 100 years since something very similar occured. In
both these cases there appears to have been some connection with
a sudden reduction of the level of the waters of the lake. It is
283
assumed that the subsidence is due to an outflow towards the
deeper parts of the lake of this oozy substratum—that under
ordinary circumstances the waters of the lake give to this ooze
sufficient support to maintain it in its normal position. But if
by any means that support were withdrawn, or the superin-
cumbent pressure increased, the equilibrium would cease to be
maintained, the oozy matter would be pressed outward and the
upper crust would be broken up. In the present case there had
been no lowering of the level of the water—but a considerable
amount of pile driving had been going on which very possibly
had disturbed the superficial arrangement of the soil below the
surface of the water—and the gradual accumulation of buildings
on the surface had gone on adding from time to time to the
weight that pressed more and more heavily on the soft matter
below. If this be the explanation of the event it comes to very
much the same as in the cases of the Rigi and the Rossberg, viz.,
superincumbent pressure and withdrawal of supports. The moving
bogs of Ireland appear to be phenomena of an analogous kind.
To come still nearer home, we have a series of subsidences
taking place in Cheshire and Worcestershire in consequence of
the abstraction of the salt. In Cheshire these are in some places
altering the face of the country, producing depressions of the
surface, that fill up with water, forming large pools, where only a
few years ago was dry ground. Almost any person who passes along
the railway through Droitwich must have noticed how the retain-
ing walls of the railway are fissured by the sinking of the ground.
Similiar operations have been going on on a large scale in
limestone districts—water charged with carbonic acid, percolating
through beds of limestone, dissolves it, making caverns and
galleries—and these from time to time fall in, forming cliffs and
ravines. The gorge in the cliffs at Cheddar is assigned by many
geologists to this cause.
But at our own doors we have a neat little landslip and we
find it a rather troublesome neighbour. So far as I have been
284
able to ascertain the cause of the movement at Hedgemead is
this—it presents no feature widely different from other landslips
—certain beds of clay are super-saturated with water, they
become softened at their planes of contact, superincumbent
pressure causes them to slide over each other, the upper bed
being the one most liable to move. In the ground of the
Hydropathic Establishment at Limpley Stoke, they have lately
constructed a new tennis lawn, which required that soil should
be cut away from the upper side and transferred to the lower;
in doing this they cut through two thin beds of clay, the support
to these beds being now removed the upper has begun to slide
over the lower, bringing the soil down on to the new level.
What is the remedy for such things? Clearly the first thing
appears to get rid of all superfluous water—and thus to keep the
adjacent beds in a condition to exert as much friction on each
other as possible—and secondly to reduce the superincumbent
pressure.
As regards Hedgemead, we have had long continued warnings—
and if at an unexpected moment some great catastrophe should
happen we cannot plead that we have not had notice. Such an
event is not probable, but there is no saying what might be the
effect of a very wet season and a very stormy time.
Doubtless there are many other forms that landslips and sub-
sidences may take, but these are enough for my present purpose,
which had chiefly reference to the Zug disaster. I see a notice
from Geneva, in last week’s papers, in which it is stated that nearly
the whole of the northern shore of the lake of Zug has become
unsafe, and that it has been deserted by all the inhabitants. It
would be interesting to know how far inland the danger is
supposed to extend. The Railway station is not far away and
may have to be removed.
The plans on the table are copies from one issued at Zurich
directly after the subsidence, and the photos are copies of
photographs of taken on the 6th of July.
285
The Destruction of the two Churches of St. Mary in Bath. By
Austin J. Kine.
(Read December 14th, 1888.)
There were at one time three churches in Bath dedicated to
the Blessed Virgin. One of these was Saint Mary extra muros,
otherwise called St. Mary by the Southgate. This Church is, I
think, intended to be shown on the earliest map of Bath, which
formed the subject of an interesting lecture in this room by Mr.
E. Green. I say intended, because the situation given to it is
almost certainly wrong namely on the north instead of the south
side of the Avon.
I am inclined to think that it was near to the south side of
the Old Bridge, but it must not be confused with the little
Chapel of St. Lawrence built on the centre pier of the bridge.
Warner speaks (p. 123) of this Church being a Rectory but it
is clear from the document he cites as his authority that it is the
Church of St. Mary intra muros which was intended.
The words are ‘‘ecclesie beate marie infra portam acquil.”
Leland does not mention this Church on the occasion of his
visit in 1530. Itis probable therefore that it was only an oratory.
The two other Churches dedicated to the Blessed Virgin were
Saint Mary de Stalles or ‘Sancta Maria de Stabulis” more
commonly called Stalls Church and Saint Mary intra muros or
Sancta Maria intra portam Borealem.
And first as to Stalls Church. It has been suggested that the
original name of the Church was “Sancta Maria in Stabulo i
(our Lady of the Stable), and that it was intended to honour the
Blessed Virgin by reference to the stable where Christ was born.
This derivation is ingenious, but I think inaccurate. In the
earliest deeds in our Record room, dated 1218, a district “the
Stalls of Bath” is mentioned, and I am inclined to believe that it
was so called, as being a sort of rough place where temporary
286
booths and sheds were put up. The word used in the convey-
ances as denoting the tenement is “ Selda.”
The Church was situate at what was called “ Bear Corner,”
that is at the junction of Stalls Street with Cheap Street. The
Bear Inn stood of course just opposite at the bottom of what is
now Union Street. The churchyard adjoined, and probably lay
in common with the open space to the west of the Abbey. The
Abbey Church was what its name implied, and was only resorted
to by the citizens on special days. Stalls Church stood, as
regards the Abbey, in the same position and for the same purposes
as did the Church of St. Margaret at Westminster, the Church
which overshadowed it.
Stalls was a Vicarage, the Rectory having been vested in the
Prior and Monks in 1263. To the Vicarage was appendant the
Chapelry of Widcombe. In 1322 the relations between the Vicar
and Rectors were put upon a definite footing, the tithes were
apportioned and it was ordered that the Vicar should be
resident, that there should be a priest at Widcombe, and that
the Rectors should be charged with the repairs of the Chancel.
This Church was the official one of the city, and one of the
aisles was set apart for the Mayor and Corporation, and went
under the name of the Mayor's aisle. The seats in this aisle
were repaired from time to time at the expense of the Chamber.
Numerous gifts and benefactions were made to the Church.
In 1326 Benedict de Stoke gave a pound of wax yearly for a
taper to be lighted on the Feast of the Assumption of the
Blessed Virgin and fourpence for four masses yearly for the
repose of his soul, and charged the necessary annual payments on
a house of his in Stalls Street. In 1403 Sybil Pochon gave her
best veil (manutergium) to Stalls Church, a sum of money to the
Vicar to say masses for her soul and to the image of St.
Catherine de Stalls her best silk robe (unum flamiolum meum
optimum de serico ).
St. Catherine was a favourite saint in Bath. This appears not
287
only from the references to her in the Ruber Codex Bathon at
Longleat, but from the ancient oath taken by apprentices on
taking up their freedom. This rans—
“T schal buxom and obedyent be to the mayr of Bathe
and to al hys successowrys and Y schal mentayne me to
no lordschyp for hynderans of eny burges of Bathe
Nether Y schal nozth plete wyth no burges of Bathe
but on the mayr courte yf hit so be that the mayr wyll
do me ryght or may do ryght Seynt Katern day Y
schall kepe holy day yerely and. Seynt Katern Chapell
and the brigge help to mentayne and to susteyn by my
power. All other custumys and fredumys that Jangit
to the foresayde fredum Y schal well and truly kepe and
mentayne on my behalf selme God and halydom.”
Notwithstanding that the Rectory of Stalls was vested in the
Prior and Monks, the Vicar of Stalls sided with the Citizens in a
memorable dispute with the Monks, temp. Henry V., as to the
‘right: of ringing church bells. The inquisition is set out by
Warner (Appendix xli.) The ancient custom contended for by
the Monks was at this time (1421) distinctly recognized, namely
that none of the City Churches should ring their bells in the
morning before the Abbey bells, nor after the Curfew (ignitigium)
had sounded from the Abbey tower in the evening. Certain
exceptions were allowed ; Christmas, the Epiphany, the feasts of
the dedication of the Churches and of the patron saints of the
Churches and of St. Catherine, St. Nicholas and All Saints. On
other feasts the City Churches were to summon to Matins with
one bell only.
The participation of the Rector of St. Mary intra muros, in this
dispute is the only early recorded fact I have been able to find
concerning this Church. It was a Rectory, and the advowson
was vested in the Prior and Monks. The parish attached to
it must have been a very small one, and it is a little difficult to
conjecture what district it covered. The parish of St. Michael
288
extended to the city walls, and so did the parish of Walcot, and
Stalls parish pressed hard upon the intervening district from the
other side.
The Church was situate just within the Northgate, and across
what is now the junction of Bridge Street with High Street,
It must have been very ancient because we read of its repair by
Fitz Jocelin in 1190. In the reign of Edward VI. the charitable
property annexed to Stalls Church for lights to burn before
statues, anniversary masses and doles, was stated to be £2 16s. 4d.
per annum, and that annexed to St. Mary’s intra muros, to be
£4 Os. 2d. It is clear, however, that these returns were false,
and it is probable that both these Churches had considerable
property belonging to them, much as was proved to be the case
with regard to the Church of St. Michael extra muros.
At the Dissolution the monastic property in Bath was granted
to a speculator, Humphrey Colles. Colles sold to Mathew
Colthurst, and the property descended from him to Edmund
Colthurst. Colthurst thus became possessed of, of course, the
Abbey Church, and the Rectory of St. Mary intra muros, and
St. Mary de Stalls and the advowson of the other parish Churches,
The citizens agreed with Colthurst for the acquisition of
this Church property. The royal licence was required to the
conveyance, and in a “remembrance” to Lord Burleigh the
citizens thus stated their views :—
‘‘ And that whereas there are 3 little Churches decayed
within the said city, that the parishes thereof may be
annexed to the great Church by the assent of the
Ordinary there and that your lordships orators may
have the advowson thereof by grant of the Queen.”
The licence asked for was given on the 21st November, 1572.
It was not, however, for 10 years that the scheme could be
even partially carried out. There were several reasons. In the
first place there was an Incumbent of Stalls, one Henry
Adams. This ecclesiastic had in 1571 been presented by Sir
289
Walter Daveys, to whom Prior Holwaye had granted the “next
presentation.” Adams did not die until 1577, and even then
there was an obstacle in the person of Gilbert Berkley, the Bishop
of the Diocese, whose consent was required. The Bishop died
in 1581, and during the vacancy of the See a Dr. Aubrey was
Vicar Capitular. Aubrey was a pensioner of the Bath munici-
pality, and received some relatively handsome presents for his
complaisance in consenting to the spoliation. The order for
consolidation of the parishes was made in April, 1583. The
order recites that the ‘“‘ruinated church” belonging to the
Priory had been re-edified, except the south aisle, and then orders
that the Church of Stalls and the Chapel of Widcombe should
be annexed “for the increase of Divine worship and the
preaching of the word of God to the said great ruinated Church.
The Abbey Church is then erected into a Parish Church “ to
which as to their Parish Church all and singular the inhabitants
of the said late parishes should be obliged always to come to
and to no other place to hear Divine service and to receive the
Sacraments.” The order permits the use of other Churches
until the repair of the south aisle of the Abbey.
Thus what had been for centuries the parish of St. Mary de
Stalls became the parish of SS. Peter and Paul, the Abbey
having been dedicated to those Saints.
The inhabitants of Widcombe were prompt in the action which
they took. They applied for a, sequestration of the living and
obtained an order to that effect and a Mr. Gaye was appointed
to serve the Chapel. There was consternation amongst the
citizens; and by intriguing and bribing, and probably also by
promises to the men of Widcombe, they got the sequestration
removed.
The parishioners of St. Michael’s exira muwros and St. James
were probably equally active, and to their remonstrances we owe
it that these two city Churches were not desecrated and destroyed.
The little Church of St. Michael intra muros was annexed to St
290
John’s Hospital ; the two Churches of St. Mary were abandoned
to their fate,
We have certain data from which we can approximately fix
the dates of their secularization.
The Church of Stalls was used as the official city Church until
1593, for in that year we find the Chamberlain making a payment
for “twoe mattes for the maior his seate in Stalles Church.”
Probably Stalls Church was soon afterwards given up as a place
of worship for in 1600-1 the partial restoration of the Abbey
Church was finished, and money was expended by the Chamberlain
in fitting that Church with wainscoting and benches. Writing
in 1608 Sir John Harrington says ‘“‘ The tower, the choir and two
aisles are already finished by Mr. Billett, executor of the worthy
Lord Treasurer Burleigh.”
Probably the transfer from Stalls to the Abbey was in about
1606, for in that year we read in the Council Book :—
“Agreed upon the 25th march, 1606, by the mayor,
parson and parishioners of Stalls concerning burials in
the great church vault. That any of the degree of a
Knight which shall be buried there shall pay for the
breaking the ground, 20/-, and 6/8 for ringing the
great bell, and others 6/8 for breaking the ground and
2/6 for ringing the bell, and every child 2/- for breaking
the earth.”
The following entry in the Chamberlain’s account in 1609 is.
somewhat obscure :—
“Paid for the Abbey Bell and Stalls ...£20 10 0
Paid for the Clipp of the Bell... oo LO As
but I am inclined to think it refers to the recasting of a bell,
probably the ‘‘Inket” or Inquest Bell formerly in Stalls Church,
and setting it in the Abbey tower.
In 1616 the Corporation took possession of Stalls Churchyard
and granted each other leases at nominal rents ; the site of the
Churchyard can be traced from the block of houses now
standing.
291
From this date we do not hear of Stalls Church being em-
ployed for any ecclesiastical purposes, although the parish
retained for many years its ancient name.
A reference to the valuable collection of Bath maps made by
the late Mr. Russell may here be interesting.
The map of the city erroneously attributed by Wood to Dr.
Jones, dated in 1572, and Speed’s map, issued in 1610, both
show Stalls Church. Gilmore’s map, under date 1694, shows a
blank where a part of the Church stood, and later maps show
the site of the Church. Strachey’s Map of Somerset, published
in 1732, shows the corner where the Church stood by a cross,
and the reference “ St. Mary de Scalys, now dwelling-houses.”
These maps are so manifestly copied from each other, and
contain so many obvious mistakes, that they are not at all reliable
as evidence of dates.
Strachey’s statement as to the conversion of the Church into
dwelling-houses is no doubt correct, for in 1632 we find leases
granted of houses described as “in the Church.” During the
Civil Wars the Church was used as a military prison and hospital.
In 1656 we read in the Council book :—
“Whereas the Tower of the Church of Stalles in this
City is now much fallen into decay and cannot be
repaired. Whether the said tower shall be taken
down so far as the roof of the said Church or so far
as need required or not, the profit to be employed to
the use of the Abbey Church, and the churchwardens
of the said Abbey Church to undertake the care and
oversight thereof.”
This resolution was carried, and three aldermen were elected
to oversee the work and take the churchwardens accounts.
In 1659 the Church itself fell down, for we read :—
“Whereas Stalls Church within the said City is fallen
down, and the materials, by a formal order, appointed
to be employed to and for the use of the Church of St.
292
Peter and Paul within the same City, the question is
who shall be appointed to dispose of the said materials
to the use aforesaid, both to make, sale thereof, and to
employ the money made thereof to the use of the said
Church of St. Peter and Paul.”
It curiously happens that we can trace the exact destination of
the money received from the sale of the materials of this old civic
Church. The sum realized was £100; and in 1663, when the
Citizens were making a present to Charles II., under circum-
stances which 1 have detailed elsewhere,* it was mentioned in the
Council minutes that there was this sum in hand “ belonging to
Stalls Church,” and it was accordingly appropriated to the gift.
And now I return to the Church of St. Mary intra muros.
The last date on which we have evidence of its use for
Ecclesiastical purpose is 1588, and probably its desecration
occurred very shortly afterwards.
But the building was not destroyed. The Grammar School
(founded by Edward VI. out of a portion of the much larger
property formerly devoted to educational purposes), was held in
some rooms over the Westgate. This school was moved into the
nave of St. Mary’s Church, and we can fix the date with
substantial accuracy.
In 1589, we find the Chamberlain paying—
“To Thomas Gardener and Thomas Hibbett, masons, for
byldinge up the chancell at the Schole hous 1/- more
to a Free-mason for making a window in the poining
end 9/-”
From this date then the nave was used as a school, and there
are many quaint and curious records connected with the master
and his teaching. These however relate rather to the history of
the “ Grammar School.”
The tower of St. Mary’s Church was used asa gaol. I have
* “Cavaliers and Round-heads : a Chapter in the History of Bath.”
293
not been able to fix the date at which this user commenced, for
there was, of course, always a gaol for the city, and there is no
record of the change from an older building to this one.
Wood writes :—
“The City Prison so nearly appertaining to her Court of
Justice that structure is the very tower of St. Mary’s
Church . . . but no sooner had Queen Elizabeth
consolidated the Churches of the City into one cure
than they looking upon this house of God no
more as a house of Prayer turned the tower of it into
a den for thieves.”
The gaol in the tower of the Church must not be confused
with the Bridewell or house of correction in the lane of that
name. This was built in 1632, partly by subscriptions, partly
out of the proceeds of a special rate. The entry concerning
this latter is :—
“Whereas Mr. Chambers hath possession of a barn,
stable and backride, which is agreed shall be converted
to a house of correction, what he think fit to give him
freely to quit the possession without any rule £5 to
give him.”
The Church was used for the purposes of the Grammar School
until about 1760, when the present building in Broad Street was
erected. A map of 1750 shows St. Mary’s Church, and refers to
it as St. Mary’s Church now the free school, and another similar
map, published in 1760, contains the same reference to the
Church but shows also the building in Broad Street.
Wood tells us that he completed the design for the Broad
Street schoolhouse in 1742.
The destruction of St. Mary’s Church, was, however, to be
thorough. In 1773 Mr. William Pulteney framed the design of
opening up the Bathwick estate by building what is now
Pulteney Bridge. St. Mary’s Church stood in the way of this
improvement, and he purchased it from the Corporation. No
294
money passed, but certain springs of water on Castle Down were
conveyed to the City, and the family house in Grove Street was
made over for use as a gaol.
We cannot now even accurately fix the spot on which this
ancient Church stood.
A Bath Poll Taz, 2, Richard IT. By HE. Green, F.S.A.
(Read 11th January, 1888).
In my last communication I brought before you the first known
map of our City, endeavouring generally at the same time to work
out its picture from the earliest records; but as those notes
applied entirely to the plan then produced and the surrounding
walls, it remains next to fill the enclosure with a population,—
with the living and moving makers of history. Of our later
times in this respect we know much, but of the early days we
know almost nothing. The documents now offered will it is
hoped,—as a first instalment,—help to throw some light on
several obscure points, such as the number of inhabitants and
their local status, or occupations, or wealth, subjects of no mean
interest, only to be worked out from the class of record here
either quoted or transcribed.
There is also the question ef Christian and Surname ; from
what origin or under what influence did they arise; the extent
to which Surnames had become general and whether derived from
merely personal peculiarities, or from places, or from occupations,
English names derived from places do not imply territorial posses-
sions, as so many hastily assume, but on the contrary, they are
marks simply of residence or a birth of the lowliest, in fact but
for such local designation there was no other name. The early
Law proceedings are full of such instances when the witnesses are
only given as John of this place or of another. The names of
territorial influence, for the most part Norman, were given to,
295
not taken from, the places to which they are attached, and often
in addition to the English name already existing.
The first document which may be noted is of great in-
terest as being the earliest of the class extant as specially
relating to Bath, and although not so full in details as a later one
will well serve the purpose of comparison. It is a Nonz Roll of
the year 1340, 14 Edward III., to be found in our Public Record
Office, relating to a subsidy or tax made for two years for the
good keeping of the Realm and for assisting the King in his wars,
granting in Counties the ninth fleece and the ninth sheaf, and in
Cities and Boroughs the ninth part of all moveable goods and
chattels. It was to be levied by lawful and reasonable
means, the valuation being made by inquisition upon the oath of
the parishioners. Two assessors were appointed for Bath, in this
case they were Adam le Muleward and William Cubboll, who
made a return of the following names and the amount paid by
each for the first of the two years for which the tax lasted :—
Richard le Deyare_... liijs. Thomas Berughogg ... xvjd.
Adam de Doynton ... xijd. Nicholas le Fysshare ... xijd.
Henry le Webbe me vjs. Henry de Sulbury ... lijs.
John Gourlmay 274 ijs. John Payn ... aa liijs.
William le Hoper..._—_ xviijd. John de Heottlegh ... xijd.
Walter le Carpenter ... ijs. William Spray bu iijs.
Isabell de Kary =e liijs. John Baytyn see ijs.
Joan Cooke ... WA ijs. Peter de Lewas 2c lijs.
Adam Knevet aS yjd. William le Porter See lijs.
Thomas le Touker ... vjd. | William Bouche oa) Rade
Robert le Porter emt se John Corteys te iijs.
Ralph le Deyare 3 ijs. Elias Gower... Se xijd.
Nicholas de Deyare ... _iiijd. | John Freman we Xd.
Henry Hurel at XXS, Walter Saundres eek xijd.
Barto de Deyare venta Wiijs: Roger la Tannere_..... ijs.
Adam le Boy ie iijs. Ralph le Taylour EAS vid.
Willliam 4 dieux as ijs. |‘ John de Mersfeld ... iijs.
Richard le Boy ae iijs. | William Gay... .. Xviijd,
Richard le Webbe
Gilbert le Webbe
Richard Shakesho
John Coventree
Adam le Barber
Peter de Marsfeld
Richard Beone
John atte Tame
John RBerughogg
William Hindeman
Nicholas Basse
Ralph atte Tame
William Swayne
John Baron ...
John de Alynton
Walter le Lindraper ...
William Cubboll
John Allyn ...
William de Sarum
John Wodelond
Robert de Natton
John Croknutte
Roger Sutor...
Reginald Nony
John Castell...
John de Durcot
John Tryg
John le Rydelar
John Cole
John Deverel
John Gyvelegh
Robert Pluco
William Orlegh
Thomas Gourlemey
Henry le Mareschal
John atte Brome
ixs.
ijs.
xijd.
lijs.
liljs.
a) ilijs.
xviijd.
ijs.
xijd.
iijs.
lijs.
vjs.
ijs.
liijs.
ijs,
vjd.
296
John de Boldebury xijd.
Thomas Stoke vjd.
William Clement xxd,
John Hoirys... Bes ijs.
Adam Whiteson vjd.
Thomas Fovel : liijs.
Giles de Cheyppenham __ xviijd.
William Symond tie ijs.
Elias la Spicer Se vs.
John de Sambourn ... vs.
Robert le Deyare .. Ljs. vd.
Walter atte Brugge xijd.
Julian de Wyke xijd.
Robert le Deyare . ijs. vjd.
Henry Rossel Hy ijs.
William de Kemyngton iiijs.
Thomas Buryman xijd.
John de Budeston ..... ijs.
EKustach de Button... ijs.
William de Wyke ..... ijs.
John Rolf... AS ijs.
John Nywman af ijs.
John de Farleigh ___.... ijs.
Henry Burel scr xd.
Adam Storch xijd.
Ralph le Hoper iijd.
Nicholas le Chaloner ... xijd.
Agnes le Zork xijd.
Stephen de Pryssheton xijd.
Roger de Roding ... — xijd.
Thomas le Mason _... lis.
Alexander le Deyare xiijs. iiijd.
Richard le Vyngour ... vijs. vjd.
Total ... xiiijli. xs. jd.
297
Thus the substantial men of Bath in 1340 having personalty
warranting taxation numbered 106, and their payment amounting
to £14 10s. 1d. as a ninth, gives the total gross value of the
assessment as £130 10s. 9d.
In a collection of a 20th in 1 Ed. III, the totals only being
returned—Bath produced £8 4s. 7d.; Wells at the same time
paying £10 Os. 6d. As another point of local interest one example
may be given of the entire Hundred of Bath Forum. In 12
Ed. IV. in payment of a 15th and 10th, the return was from :—
Claverton ... a cvs. Wyke Abbatisse xxvijs. viijd.
Hampton ... i iiijlz. Eston es it iiijle.
Aumarle Chamfiour ... iiijlz. xs. Wallecote ... ie eps
Calueston ... ast ijl. Weston = mtr Is.
Northstoke -. Xxxiijs. Lynecombe ... sie lxijs.
Langrigge ... ¥ Sept. Charlcombe... boone , xLViSe
Swayneswyke and Ford a a3 Ixijs._
Ferschford ... xls. xd. Wollegh ... XXVjs. Viijd.
Southstoke ... ay XXXS. Combe af << EES Kile
Analysing the names in the None Roll it will be observed
how many use the de or le—the de being prefixed to names of
places the le to occupations, atte appears only three times. In
some cases the prefix has been either dropped or perhaps never
existed. There are seven bearing the name of le Deyare, but
shown as not necessarily of one family as there are two Roberts.
There are three Webbe, a le Tuker, and le Fisher, and others.
such as Lindraper, Mareschal, Sutor and Spicer, which speak
for themselves ; then there is the name of Swayne so constant in
early Bath deeds.
The taxation of the clerics was distinct, as they claimed to be,
and were taxed separately, and when possible not at all. This
part of the subject being very difficult must be avoided, but an
example which seems fairly clear may be used as well for itself as
also for a further illustration of early name giving. In 1377,
51 Edward III, in a list of the names of all the religious persons .
WwW
298
in the Deanery of Bath, there is found first John Berwykes,
Prior of the Cathedral Church of Bath, and following him come
fifteen brothers, all paying uniformly twelvepence The names of
the brothers are—John Bradlegh, William Tonar, John Brok,
William de Welles, John de Ciceter, Michael de Combe, Nicholas
Vinor, John Kyneton, John Rockbourne, Henry Godeley, John
Preston, John Ploute, Thomas Bampton, Philip de Pekelynch,
Nicholas Huse and John Milverton. Besides these there were
John Astwykes, master of St. John’s Hospital and Brothers Peter
Harding, John Dunstarr, John Briwton and John Wedmor, and
then Edward, without other name, master of the house of St.
Mary Magdalen. The Dean, the Vicars of St. James, St.
Michael, St. Mary, and Stalles, all paid uniformly twelvepence.
The inferior clergy paid fourpence. ;
The modes adopted for taxation in these days are not easily
understood. The plans met with are called fifteenths, and
presently fifteenths and tenths, The fifteenth at first was laid
upon goods only, as granted in 18 Edward I., but later this seems
to have included lands also. Two assessors were appointed for
every County and City, and they in turn appointed a jury of
twelve,—in the Counties a jury in every Hundred,—and these
returned their valuation of every man’s personal estate, and
levied thereon the fifteenth of such value. When the tax fell
upon land also, a valuation was made in 1344, 18 Edward IIL,
of all the cities and towns in England and returned into the
Exchequer, and this became then the fixed guide, the amount due
upon any fifteenth or tenth being always the same, and known
exactly. A Subsidy was another form of taxing. This was laid
upon every individual’s estate either real or personal, and con-
sequently varied in the amount produced. In time these forms
generally became known by the one name of Subsidy. There
was also another plan occasionally met with, the following being
an example for Bath. It is entitled the account of John Natton,
John Gregory and William Cook collectors of a tenth and half a
299
tenth of all moveable goods from the Laity of the City of Bath,
as warranted by Letters Patent dated the fourth of March in the
aforesaid third year. As the year said to be aforesaid is nowhere
given, the date of the document is uncertain, but from internal
indications it is attributed to the third year of Richard II. The
totals only are given, viz. :—
For the 10th ... Per olor eos oO
For the half-a-tenth ... 613 4
Total £20 0 0
It will be noted here that the expression a tenth and half-a-
tenth did not mean a fifteenth, about 64 per cent. or a total
of £8 17s. 94d., as without help it might have done, but it
actually meant 15 per cent. or a total of £20. The gross value
here of the city in 1380 is—£133 6s. 8d., against the same in
1340—£130 10s. 9d. There was yet another plan of taxation
called exactly a Poll Tax. Although a little out of chronological
order, the result of one of the year 1381, 4, Richard II., may
be shortly mentioned. It is entitled—‘‘ A View of the Account
of John Gregory, John Natton and Robert Wattes, collectors
of the Poll Tax of xijd. in the City of Bath on all aged xv.
years, true mendicants excepted.” Payment appears to have
been prompt, as the warrant or order being dated in December,
two-thirds of the assessment were paid at liilary, and the
other third at Pentecost. The totals only are given, and in
this document only the first payment, viz—£9 14s. 8d. for the
two parts of £14 12s.—the Subsidy from two hundred and
ninety-two persons, men and women of the city.
The preceding notes so far will aid towards a comparison with
the next and last example, one for the second year of King
Richard II., the one specially intended for notice, and the one of
the fullest and greatest interest. It is a Subsidy granted on the
accession of Richard in the form of a Poll Tax on the Laity.
The rates were graduated and ranged from ten marks for a Duke
300
down to fourpence for the “general,” not being really mendicants.
Married couples paid at a single rate. The Roll here transcribed
consists of three consecutive membranes duly indented, and by
good fortune the counter indenture or duplicate also exists, or, on
account of the decay of the ink, without such duplicate the
names could not have been read. The business of deciphering
has been certainly most troublesome and fatiguing, and not-
withstanding often examination and every care it is more than
possible that some names may bear a different reading. The
occupations however, perhaps the chief point, will be found
correct. The document is not only of extreme interest as giving
full names of persons and their occupations, but it also by a
happy chance gives the names of the streets in which they lived,
so that we have presumably a complete Directory for the city in the
year 1379. It will be seen that the Mayor begins, an early
notice of one, perhaps the earliest actually named.
CITY OF “BATH.
Indenture made the fourth day of June, in the second year of
King Richard the Second after the conquest, between John
Gregory, John Natton and Robert Compe, assessors of the
Subsidy of (iiij.) pence, for the lord the King on the one part, and
Robert Wattes, Richard Ford, John Swayne and John Cherde,
collectors of the same on the other part, from all the men and
women of the age of xvj. years, true mendicants excepted.
John Natton, Maior, — (xs).
SOWTHEYATE STRET.
John Balle... see tanner eee aca.) elles
William Webbe ice laborar a -oo, adli@e
William Zawoher 5 laborar sie sao, pallga.
Felicia Launder aie filator wee Pep en ibiye ts
Walter Thesher Bs laborar ae - iif.
John Growe ... sae laborar ath Lee as
John Bowby ... sed laborar a .. lj.
John Hosteler oe laborar_.... . liijd.
John Coxler ...
William Y — dene
Philip Bryan...
Stephen Growe
Robert Baker
John Fanna ...
Elen Sims
John Fletcher
John Feyror ...
Harri Wreg ..
BYNBURI
Richard Port ...
Richard Legge
Jobn Beyon ...
Andrew Trotebosse
Robert Schoylocke
Richard Farley
John Nappeford
William Redheffed
William Bedistone
301
laborar
’ Jaborar
folator
(ilegible)
(illegible)
(illegible)
(illegible)
laborar
laborar
laborar
Total :—xixs. viijd.
STRETE.
cissor des
laborar
laborar
laborar
laborar
laborar
laboror
laborar
laborar
Total :—iijs. ijd.
BY YE BATHE STRETE.
John Popp
Robert Porch
John Taylor ...
Alan Cissor
Robert Waterman
John Warbey
John Eston
John Mulwerton
John Pochon ...
Richard Lockyer
John Porke
John Howard a
Walter Hasilwod ode
laborar
laborar
laborar
laborar
laborar
laborar
laborar Fcc
laborar Ae .
laborar
laborar ede
laborar ade
laborar ea ase
laborar add
Total :—iiijs. iiijd.
302
STALLE STRETE,
John Lacockes sb carnifex
Thomas Norhorne me carnifex
Agnes Porter ... ie filator
John Norhamton Sao laborar
John Tame ... sp artificer
Roger Chepman wee pedeler
Christiana Caunton... filator
Robert Cauersam ae pedeler
John Monemewye ras laborar
Walter Wek . faber
John, serviens ‘ the said Walter
Roger Gewe ... ane skynner
Philip, serviens to the said Roger
John Stone ... A laborar
John Streyle ... ace soutor
laborar
cissor
Richard Swetys ace cissor
John Fyssher See artificer
John Seymour : faber
Jobn, serviens to the ied John
Joan Forester aes filator
Richard Andrewe ae laborar
Thomas Porter ae laborar
John Teyntyghulle ... laborar
Herri Touker eet folator
John Panter ... at laborar
Edward Hopere ot laborar
William Parson eck laborar
John Mytteford eee skynner
Alice Pigeley ... wee braciator
Joan, serviens to the said Alice
William Carpenter... laborar
William, serviens to the said William
William Hulle .. mit cissor
William Rolphe Ase folator
303
John Castell ... ae laborar
John Druhed... aoe artificer
Morgery, serviens to the said John
Thomas Durant ibe laborar
Richard Baysse aie cissor
John Scottfisher Pas (nil)
John Hawkyn as cissor
Agnes, serviens to the said John Scottfisher
Thomas Bedull oe braciator
Agnes, serviens to the said Thomas
John Fadur ... aa folator
Roger Vookes ie laborar
John Mycham ae laborar
Nicholas Burynton _... artificer
John Bobichon as: braciator
John, serviens to the said John
William Caulestocke ... laborar
Robert Pistor... ae artificer
Nicholas, serviens to the said Robert
Richard Bedulle Se textor
William, serviens to the said Richard
Herri Jolifphe Be braciator
William Payne a laborar
Richard Chepman wad pedeler
John Cherd ... a laborar
Richard Browne ons laborar
William Cooke ... Dpety marchant
John, serviens to the said William
Matilda, serviens to the said William
Agnes, daughter of the said William
John Schete ... ay pedeler
William Chaumberleyn laborar
Roger, serviens to the Prior of Bath
William, serviens to John Brocke Bee
Richard Cooke, serviens to the Prior of Bath
Nicholas, serviens to the said Prior
Thomas, serviens to the said Prior
Walter Palfreyman ... (nil)
iijs. iii
304
Thomas Plomer, jun ... (nil) see wee liijd.
Richard, serviens to the baker of the Prior of Bath ... 1iijd.
John Waderleder Ye Jaborar’* \" <:. co alee
Total: ; —xliijs. iiijd.
WESTYATE STRETE.
John Morekek ts laborar... a. ilijd.
Richard Bromilbe iss laburar—.... ..- iliijd.
John Sarne ... se textor oes feo Pas
John Homfrey ress laborar_—.... ws. iiijd.
Christiana Homfrey ... filator ee .. iliijd.
John Goffe... shes laborar ee w» Liijd.
Thomas Mountwalle ... (nil) | see .. iiijd.
Thomas, serviens to John Cerne sys ws, ay
Robert Greywod ass laborar a w. iiijd.
John Atteberwe os laborar ae wes . UNG
Nicholas Speragroue ... sutor ef vse, eee
Herri V yuour ae sutor ee .. xijd.
John Freyne ... a laborar oy oe MR
John Baytn ... ais laborar ie we. Llijd.
Stephen Corior bk laborar aa .. iiijd.
Thomas Payerd ac laborar ace ... iliijd.
Walter Deyher ae laborar pe ... iiijd.
Walter Souter ia laborar 7 aco MULL
Total :—ixs.
SOWTER STRET.
Richard Vitull Ls pedeler Bis .. xijd.
William Hedeman ~ laborar an ... iiijd.
John Chaperwe BAe pedeler +e ous Kl
John Clacton... 5c faber ne ae XG
Thomas Swayne fos hosteler... OA ijs.
Robert Coppe ow »., pedeller .. son, KAJ
Agnes Carter ... as filator Ss w. iiijd.
John Barbor ... Ree artificer ... w= Vd.
Robert Brent ar hosteler: <.. . Asm ede
Joan Lokyngton ots filator ie ... liijd.
Walter Mirkely ee laborar as ... iiijd.
Margery Sowthstok ... braciator ... a Xa
305
John Bregwater ae laborar
Geoffrey Nynnan Re laborar
Edithe, serviens to the said Goeffery
John Donne ... one cissor
Robert Waccus a pety marchant
Thomas Berwehog fee laborar
Robert Cherchward ... pedeler
Thomas. Poffe ai laborar
Alice, serviens to Robert Cherchward
Peter Heneley ate artificer
Robert Spyrelackes.... soutor
Thomas Brockword ... pedeler
John Keynshym gi laborar
William Cropp wes laborar
Joan Swayne oe filator
Nicholas Swayne oe laborar
Alice, serviens to Richard Vitull
John, serviens to Robert Waccus
Joan, serviens to the said Robert
William Bath ae laborar
John, servaunt to Thomas Swayne
John, servaunt to John Barbor
Thomas, servaunt to Hugh Coteler
Walter, servaunt to the said John Clacton ...
Aylmer Flemyng 2 artificer
John Tybowode ae laborar
NORYATE STREET.
Stephen Brigman = laborar
John Compe ... aie pety marchant
Xpine Loffe ... ae filator
John Carnyfex acy carnifex
William Chestburie ... laborar
Herri Aurifaber aie (nil)
Roger Skynner see artificer
Stephen Dernned a cissor
Thomas Carewyle oii soutor
Total :—xxvs.
iiijd.
liijd.
liijd.
xijd.
ijs.
liijd.
ijs.
liijd.
iiijd.
vjd.
xijd.
vjd.
iiijd.
iiijd.
iiijd.
liijd.
liijd.
liijd.
iiijd.
liijd.
liijd.
iiijd.
iiijd.
liijd.
vjd.
liijd.
iiijd.
vs.
iiijd.
vjd.
iiijd.
xijd.
vjd.
yjd.
xijd.
306
Robert Waspour ne artificer
John Wyche ... ee laborar
Philip Bichewe a artificer
Thomas Saundrus 1a pedeler
Sewale Fraunces Sc artificer
John Kynt... ies braciator
William Cissor ele laborar
Thomas Hopere oes laborar
Alice, servaunt to Sewale Frauncis
Robert Bentley mae pedeler
William Aurifaber es (nil)
Vylbo, servauut to the said William
Richard de Forde it artificer
Margery, servaunt to the said Richard
Xpine Bynald sek filator
Edmund Teylerd ae laborar
William Peyntor ses artificer
Jokn Heyward me artificer
Robert, servaunt to the said John
Walter Meynard T laborar
John Benet ... ek artificer
Henry Barbor =e laborar
Hugh Coteler ae artificer
John Colurbre bie laborar
John Gowher sve laborar
William Cherward ... artificer
Thomas, servaunt to John Compe
John, servaunt to William Chestiburie
Henry, famulus to the said William
John, famulus to Stephen Derned
Agnes, servaunt to Philip Bichewe
Jobn Wyte ... oe faber
Richard, servaunt to the said John
Total :—xx
BRADE STRET.
Thomas Saltford wi laborar
William Deyher be laborar
iijs. itijd.
ijs.
liijd.
xijd.
vjd.
ijs.
xijd.
liijd
iiijd.
liijd.
xijd.
xijd.
liijd.
vs.
liijd.
liijd.
iiijd.
vjd.
xijd.
iiijd.
liijd.
vjd.
liijd.
vjd.
liijd.
iiijd.
xijd.
iiijd.
liijd.
iiijd.
liijd.
liijd.
vjd.
liijd.
iiijd.
iiijd.
307
Deodonay (Belde) cor soutor
Margery, serviens to the said Deudonay
Richard Carter ahi folator
Richard Hoper a3 artificer
John Broun ae laborar
Walter Webbe ane artificer
Laurence, famulus to the said Walter
Robert, famulus to the said Walter
Joan, serviens to the said Walter
Iwan Glover ... see laborar
John Gregorye oy (ntl)
John, famulus to the said John
Tsolda, serviens to the said John
Alice, serviens to the said John
John Lacy... ode laborar
Agnes, serviens to the said John
Alexander, famulus to John Natton
Morgery, serviens to the said John
John Garrard its laborar c
Walter, serviens to:the said John Gregory ..
Thomas Plomer ees artificer
John Fadur ... 2 artificer
Herri Workman eft laborar
Joan Wysdom oes filator
Richard Folator ef (nil)
Stephen, famulus to the said Richard
Richard, famulus to the said Peter Cissor
Philip Follator fu (nil)
John, famulus to the said Philip
John Wysdome see laborar
William Burrell aes laborar
Isack Irysse itp artificer
John, famulus to the said Isack
Peter Cissor ... vs (nil)
John Banestre ov laborar
Herre Kente ... ore laborar
John Salpe ... tr laborar
William Kymton de laborar
308
John Duke ... S36 laborar
John, son of John Brown dee
Thomas Kymton sas artificer
John Honybrige si textor
William Rowse ive artificer
John Faber ... ae (nil)
Henry Colnette wes laborar
Total :—xxviijs. ijd.
WALCOTE STRET.
William Deyher on artificer ...
Agnes, serviens to the said William
Thomas Barbor Se artificer
William, famulus to the said Thomas
Roger, famulus to the said Thomas
Robert, famulus to the said Thomas
Thomas Webbe (nil) See
John, serviens to the said Thomas...
John Smalcombe es artificer
John Cornewalle ae: follator
Richard Balleard as artificer :
Ralph Scerfhe... me laborar Ses
John Harneham Ae laborar
John, famulus to Richard Ballard ... te
Willliam Momeray .... laborar ...
John Gregory... oe webbe artificer
William Teylour see artificer ...
William Workman ote laborar eee
Robert Heyward aos laborar
Alexander Workman ... laborar
William Seaker re laborar
Hugh Teyler ... mee laborar
William Hanykok 200 laborar
William Reding ai laborar ane
Thomas Parchimennor ... laborar ork
Roger Glover ai artificer
Robert Parchimennor ... artificer
Roger, famulus to the said Robert ese
William Bekyngton ... laborar
iiijd.
iiijd.
vjd.
ijs.
vid.
vjd.
liijd.
vjd.
iiijd.
ijs.
vjd.
liijd.
liijd.
vjd.
iiijd.
vid.
vjd.
vjd.
iiijd.
liijd.
iiijd.
iiijd.
vjd.
vid.
ilijd.
liijd.
iiijd.
liijd.
liijd.
liijd.
iiijd.
ilijd.
xijd.
vjd.
iiijd.
iiijd.
309
William Tyborde bo: laborar
Peter, famulus to the said Roger Glover
Roger, famulus to the said Roger
William, famulus to the said Roger
John Colingborne =. laborar
John Busseswayne_... laborar
Robert Cissor oes (nil)
Henry Cissor Fe (nil)
Richard Pochon ses pedeler
Thomas, son of the said Richard
Robert Bolle ae pedeler
Herri Wolley din laborar
Richard Cluherd ots pedeler
Margery, servaunt to the said Richard
Herri Tonker
“ \v
va <
es ' x © 4
#, a ‘ue hae © 5
a tf " . ved
LP
ae a ;
Ol
>
ity : )
af j 4 * .#
eee,
| i
bene | bt
fe
ree cays 7.4
yp 4
Ph “
‘ “4
ef eile nb bets Wigs. O) iste vt “tt a hte? ii intel
Mata) - lage wWnewees de i Sl
Yo “4 hn 4 ' a =
.
The Honorary Trexsurer in account with “The Bath Natural History and Antiquarian Field Club”
for the Year ending February 18th, 1889.
SSS :///[——” mm”_—, —O—
Dr.
Balance from last year’s Account
2
92 Subscriptions, at 10/- (four arrears from 1887) 46
1
5 Entrances, at 5/- ... ses
One Subscription Unpaid
eee eee
£49 15 8
Also Deposit in Post Office Savings Bank of £40, with Interest
to 19th March, 1888, £1 15s.—Total £41 15s.
‘15th February, 1889,
Examined and found correct,
Cr.
Donation to the Literary and Scientific Institution
Gratuities—Librarian, 10/-; Assistant ditto, 7/6 ;
Porter, 2/6
Ditto at Printer’s for Addressing Cards, &e, ...
Ditto at Excursions #0
Donation to the Broome Botanical Fund wae
Lithographing Professor R. Jones’s Drawings
Messrs. Lewis, viz. :—
Printing Proceedings & Postage of do. 22 0
Cards, Circulars, &c.
Postage, viz. :—Honorary Secretary
a3 i Treasurer
a at Institution
Balance in hand SIE ee
5
5 11 10
£s. d.
40 0
10 0
0 5 0
015 6
Ll:
13 5 6
27 12 3
015 8
109
£49 15 8
ee
J. T. CHANDLER, Treasurer.
( Bd TALON;
\ JAMES HERDMAN.
re, i
seach
Se
DAT AI
ut
H
y
;
Hh
4
_
~
ere
7
TAKEN IN ‘THE NeeHBouRHOOD OF Bias
‘Liwur. Cot. De ee Poe Ent 8.
“4 ~~ ' a.
- :
‘g CFR
a .
Pere oe Se + t
~ ee *.
. « y |
A
—_ ’ ¥
TS PT ed er ey
PATA rar
tela ta tata ip
ri
er hid
TAinfelelatel ate lala '
at , PEAT ETE
i
Biel Fatal
ny Ny igs HEIDI ATT AAT aty
rrteidp int did dt tril f
MTS APATAT AT AT AT error et aiierer
TE
An ly
—
Loclhen entien’!
hag ogy ogy es
ss
+."
tis iA e erry
areas Ue ete
HH ER
i eal ieiniucie t
irdy si Hip tif oi era tgs tyr
j ir seicick: { fey ie.
—
at
ten
—_
j fJ j
ese eseieinie
Sis fei
141
545 fy tt
Apspsy, 1 i /
Say
Ay Ay, i a
uf
if
ify? Af it
Lisih Aff iff; iy ats ig uy
i seeseiidedi sits!
J leple pigs Spe bis
Jali dist Peal ayiy
ips (iil tipgtt
Wi, f (i ete
Bide tity pipes
itty
7 Aft ie
“Sigi
Perens
By dy i he
SIS Te ie
Sig hyde ty