Published at the Instruction of the Ministry of Munitions of War
by the Imperial College of Science and Technology.
A MEMOIR ..^-""'
ON
BRITISH RESOURCES
OF
SANDS AND ROCKS USED IN GLASS-MAKING,
, WITH
NOTES ON CERTAIN CRUSHED ROCKS AND
REFRACTORY MATERIALS.
BY
P. G. H. BOSWELL, D.Sc.,
George Herdman Professor of Geology in the University of Liverpool,
formerly of the Imperial College of Science and Technology, London, S.W. 7,
Scientific Adviser (Geological) to the Department of Optical Munitions
and Glassware Supply, Ministry of Munitions of War.
WITH, CHEMICAL ANALYSES BY
H. F. BEARWOOD, M.Sc., Ph.D., and A. A. ELDBJD&E, B.Sc., P.I.C.
SECOND EDITION COMPLETE IN ONE VOLUME.
LONDON :
LONGMANS, GREEN AND CO.,
39 PATERNOSTER ROW, LONDON,
AVENUE & 3OTH STREET, NEW YOBK,
BOMBAY, CALCUTTA, AND MADBA8.
19l8.
1179
First edition, Original Memoir December Wlfi.
Supplementary Memoir November 1917.
Second edition, complete in one Volume May HHR.
PRTN'l'KD BY TATtOIt AND FRANCIS,
nwn T.TON rounr, FLEET STRHBT.
PREFACE TO ORIGINAL MEMOIR.
study of the sands employed' i in the manufacture of
glass has revealed the fact that the veiy exceptional qualities
displayed by the best of them are not merely those due to chemical
composition, but are the outcome of their exact mineralogical
nature, and .even of the size and shape of their constituent grains.
In nearly all kinds of glass there are certain permissible irre-
gularities in both . form and composition of the raw materials
which, allow the employment of. a larger range than had hitherto
been suspected. A search in localities where Glass-Sand has been
worked in the past, and at other " likely " places, has shown that
large supplies are available, and has given, indications of directions
in which further search might be profitably undertaken. The
search cannot be regarded as quite exhaustive indeed, it is still
being prosecuted with vigour, but it has been thought best not
to delay publication, in order to set free as soon as possible the data
already collected. ' -
This work embodies the practical results which flow from a
series of investigations carried on by Dr. Boswell, with the support
of the Imperial College from the beginning and of -the Ministry of
Munitions in its later stages. Large quantities of material have
been accumulating since 1912, every locality described has been
personally studied by the Author, and with the exception of
certain Scottish and Irish sands received by favour o the Assistant
(for Scotland) to the Director of H.M. Q-eological Survey, and of
the Department of Agriculture for Ireland only samples collected
by himself have been subjected to analysis. The chemical analyses
have been made, by kind permission of Professor Baker, in the
Chemical Department of the College. They are the work of
Dr. H. F. Harwood and Mr. A, A. Eldridge, who have devoted
much thought and care to the methods employed. All the
mechanical and microscopic analyses and other work have been
V PREFACE.
carried on in the laboratories of the Geological Department.
Much assistance in indexing and in the preparation of photographs
, has been given by Mr. Or. S. Sweeting.
Our hearty thanks are tendered to many glass-manufacturers
and quarry-owners who have given the Author every facility for
his work, and have freely discussed with him the technique of
glass-making and the economic factors of the industry. We are
also indebted for help on the chemical side, both in the discussion
of results and in the indication of promising lines of enquiry,
to Professor Herbert Jackson, of King's College, London, and
to Dr. Walter Eosenhain, F.E.S., of the National Physical
Laboratory.
As the study of sands and related sediments has become a
matter of pressing national importance, and as this is the first
work published on British resources of these materials, it has
been thought well to go a little outside the obvious scope of the
Memoir in two directions :
(1) The properties of sands are so varied, and the requirements
of the different industries so diverse, that the Author
has entered into some detail both on the best methods
of investigation and on the most convenient modes of ,
expressing the results thus obtained.
(2) At the same time, the properties of sands suitable for
glass-making-are in some cases identical with or allied
^ to those useful for refractory purposes, such as steel-
moulding, fettling of furnaces, and the making of silica
bricks. Reference has been made in passing to proper-
ties of this' nature, and the applicability of the same
modes of enquiry has been indicated.
It should be stated, however, that the sands actually described
in Chapter VI. are only a very small fraction of the total number
examined and analysed. Hosts of others have been "turned
down," either because they were wholly unsuitable or on account
of the possession of properties with which the manufacturer has
not so far been able to deal. As the chemistry of glass-making
advances it is probable that some of these disabilities may dis- .
appear indeed, some of them are all but overcome and then the
large amount of apparently unproductive information obtained and
filed by Dr. Boswell will mid its use.
W. W. WATTS,
Imperial College of Science and Technology.
November 1916.
PREFACE TO THE SUPPLEMENTARY
MEMOIR.
THE reception given "by those interested in glass, whether as
manufacturers or investigators, to the Author's "Memoir oft
British Resources of Sands suitable for Glass-making," published
by the Imperial College at the instance of the Ministry of
Munitions of War, renders it desirable that the information
accumulated up to 1916 should be supplemented by that acquired
since.
Not only has search for suitable quartzose sands been followed
up, but collateral enquiries have been carried out, particularly with
reference to deposits bearing constituents so essential to the Glass
Industry as potash and alumina. It is believed that the survey of
British resources of glass-sand is now fairly exhaustive, and the
Author has again made a point of visiting all the sources of supply
described. A more complete account of crushed rocks and their
possibilities is now furnished, together with a description of the
American glass-sands in more common use,
The work for the "Memoir" received the active support of the
Imperial College, the publication being approved and its cost
guaranteed by the Ministry of Munitions. The supplementary
work detailed in the present publication has been carried out
entirely under the auspices and with the support of the Ministry,
the College setting free as far as possible the services of the Author,
and finding, as before, all necessary laboratory facilities in the
Geological Department.
W. W. WATTS.
Imperial College of Science arid Technology.
November 1917.
AUTHOR'S NOTE.
As the respective Prefaces to the Original Memoir and Supplement
indicate, the greater portion of the information included in this
volume has been the subject-matter of two earlier publications.
It appeared imperative that such information should be, , put
forward as it became available. But the appreciation of the earlier
memoirs by those connected with the industries concerned has
been such as to result in the exhaustion of the first issue and to
necessitate a second edition.
In this volume the original and supplementary publications
have. been combined. A few portions have been re-written and
further information appended, including additional analyses.
Repetition has been avoided as far as possible, but the stress of
the times and the need for rapid re-issue has prevented as exhaustive
a scrutiny as might have been desirable. The Author therefore
begs the reader's indulgence in this respect.
The Department of Optical Munitions and Glass-ware Supply
of the Ministry of Munitions of War has, by its energetic and
prescient measures, done much to place the Glass-making Industry
of the United Kingdom on a sound basis. The scope of manufacture
has been enlarged and the quality of the products much improved
by the co-operation of men of business with men of pure science.
The linking of scientific with industrial elements, to their mutual
benefit and for the good of the Country, both under the conditions
of. actual warfare and of the trade-revival which will follow the
War, is in no small measure due to the far-seeing policy of the
Controller of this Department, A. S. Esslemont, Esq., C.B.E., who
has granted every facility to the Author and freely rendered him
every possible assistance.
The Author desires to record his indebtedness, in general to the
Glass-manufacturers, and in particular to Professor Sir Herbert
Jackson, K.B.E., F.K.S., for the help which has arisen out of many
visits and discussions. Thanks are again due to Dr. H. F. Harwood
AUTHOR S NOTE. Vli
and Mr. A. A. Eldridge, of the Chemical Department of the Imperial
College, who have carried out nearly a hundred complete chemical
analyses and over seventy partial analyses purely for this work.
Ahout one hundred and seventy mechanical analyses and almost as
many mineral analyses have also been made by the Author in
connexion with the investigation. Mr. W. B. Wright, B. A., F. Q-.S.,
of the Q-eological Survey of Ireland, kindly adds a note on some of
the Irish supplies of felspar, communicated by permission of the
Director. Assistance has at all times been freely rendered by
Dr. W. E. S. Turner, M.Sc. and Mr. ,T. H. Davidson, M.Sc.,
of the newly-created Department of Glass Technology in the
University of Sheffield. Prof. C. G. Cullis, D.Sc., of the Imperial
College, has kindly read the proofs and offered many useful
suggestions. The Author is also indebted to Mr. G. S. Sweeting,
who has devoted much time and trouble to checking proofs, and to
assisting with the photomicrographs and index.
At the time of the publication of the original " Memoir " a new
organization, the Society of Glass Technology, had just been in-
augurated. The valuable papers in the Journal of the Society
demonstrate the need which existed for such a Body, and arc-
indicative of the interest now being taken in scientific and technical
questions relating to glass-manufacture. The work of Mr. C. J.
Peddle, M.Sc., Chemist to Messrs. Wood Bros, of Barnslej'-, calls
for special note from the geological point of view, in that he has
shown the possibility of using in the Works even second-grade
British sands for making the best qualities, not excepting even
the optical varieties, of glass.
Finally, the Author gladly takes this opportunity of expressing
his indebtedness to Professor Watts for reading the manuscript and
proofs, both of this and the first edition. The work has benefited
greatly by the valuable suggestions which have been the outcome
of Professor Watts' success in popularizing geology by teaching
and writing, and in promoting the application of geological science
to industry. The plan of the original Memoir was also due in
no small measure to the assistance freely and continually given
by his one-time teacher of geology.
March 1918
TABLE OP CONTENTS.
Page
PREFACE TO ORIGINAL MEMOIR (by Professor W. W. WATTS, Sc.D.,
LL.D., E.R.S., F.G.S.) ................................................... iii
PREFACE TO STJPPLEMBNTABY MEMOIR ....................................... v
ATTTHOR'S NOTE ...................................................................... vi
LIST OF ILLUSTRATIONS ........................................................... r
CHAPTER I. Introductory. Utility of Sands. Grade, etc. Some Uaea
of Sand& in agriculture, as abrasives, for building purposes,
for water-filtration, as refractories and moulding-Bands , for
glass-making ............................................................... 1
CHAPTER II. The Nature of Sands. How Sands are formed. Com-
position, of Sands. Coating of Sand-grains. Association with
organic material. Form of Sand-grains. Size of grains ......... 8
CHAPTBB HI. Methods of Study of Sands. Chemical Composition.
Mineral Composition. Mechanical Composition screening,
elutriation, graphical expression of results .......................... 14
CHAPTER IV. Glass-Manufacture. Literature on Glass-Sands. Raw
materials importance of sand. Colour, eto. of glass. The
process of glass-making ................................................... 33
CHAPTER V. The Requirements of a Good Glass-Band. Characters of
J?ontainebleau Sand general characters, ohemioal composition,
mineral composition, mechanical composition, shape of grains,
economics. Requirements of Glass-Sands. Chemical, mineral,
and mechanical analyses. Angularity of Glass-Sands. The
Ideal Glass-Sand .............................. : ............................. 39
CHAPTER VI. . British Sands etc. Suitable for Glass-making. A. Purely
Siliceous Deposits, (a) Sands Aylesbury, Fairlight (Hast-
ings), Bnlverhyth, Ashurstwood, Lynn, Leighton Buzzard,
Godstone, Eeigate, Aylesf ord, HolHngbourne & Bearsted,
Lancashire, Huttons Ambo, Burythorpe, South Cave, Denford,
Tfl.rl-mn.rt.nTi, Longdown, Fordingbridge, Isle of Wight, Charlton,
Worksop, Alderley Edge. Dune-sands and shore-sands ...... 49
CHAPTER Vll. A. Purely Siliceous Deposits (continued). (6) Crushed
! rooks, treatment. " Sand" from Muokish Mountain, Guiseley,
\.;, Mold, Spital, Caldwell, Kilwinning, Levenseat, Bally-
I castle, Cookstown, Coolkeeragh, Port-a-oloy, Stiperstones,
Appin, Anglesey, Achill I. (Westport Silica), Tinahely, eto... 79
Sections marked thus deal with sands and rooks which are also of value
for. refractory purposes.
I ,
TA.BLE OP CONTENTS. ix
Page-
OHAPTEB Yin. ^British Resources of Glaaa-Sands, etc.' (continued).
B. Deposits containing Alumina and Silica, (a) Sands, clays,
etc. : kaolin from Devon and Cornwall, from Anglesey ; sands
from South Devon, Nprth Devon, Cornwall, Derbyshire, Staf-
fordshire, North Wales 98.
CHAPTBB IX. British Resources of Rocks used, in Qlasa-makvng (Felspars,
etc.). (b) Siliceous rocks bearing Alumina and Potash. Potash-
felspars from Cornwall, Scotland, Ireland ; Meldon rook
(Devon) ; potash-bearing sands 106-
CHAPTBB X. Special Treatment of Sands and Rocks. Colour of Glass-
Sands. Washing, drying, screening, burning. Chemical methods
of treatment. Magnetic methods. Grinding. Crushing strengths. 119 1
CHAPTBB XI. Foreign Glass-Sands : European : Lippe, Fontainbleau,
Belgian, Dutch. American : Ottawa Silica Company, Ottawa,
111. ; Wedron Silica Company, Ottawa, HI. ; Berkshire Glase-
Sand Company, Cheshire, Mass. ; Berkeley Glass-Sand Com-
pany, Berkeley Springs, W. Va. ; Juniata White Sand Company,
Baltimore, ltd. ; Tavern Rock Sand Company, St. Louis 130-
OHAPTBB XIE. Location of British Supplies of Glass-Saiids \ General
Geological considerations : Location in England, Scotland,
Ireland. Distribution of the Glass-making Industry in the
British Isles 14O
CHAPTEB XIII. Economic Coimiderat'ionti. Cost of Foreign Sands.
Economic Factors in working Glass-Sands : workability, treat-
ment, transport. Statistics. General Remarks 147"
TABLE I. British Glass-Sands : Iron-Content 154
TABLE II. Chemical Analyses of British Glass-Sands 155
TABLE HE. Sundry Chemical Analyses of Alumina- and Potash-bearing
Rooks, etc 158.
TABLE IV. Chemical Analyses of Felspar-bearing rocks (Pegmatites) ... 160
TABLE V. Mechanical Analyses of British Glass-Sands 161
TABLE VI. Chemical Analyses of European Glass-Sands 166
TABLE VII. Mechanical Analyses of European Glass-Sands 167
TABLE VIII. Analyses of Danish Glass-Sands , 16S
TABLE IX. A. Analyses of American Glass-Sands 16>
TABLE IX. B. Additional Chemical Analyses of American Glass-Sands . 169-
TABLE IX. C. Additional Mechanical Analyses of American Glass-
Sands 170
INDEX 171
b
. CHAPTER I.
INTEODUCTORY-: USES OF SAITDS..
OF the many mineral resources of Britain none are more abundant
or more varied in quality and use than sands. Their utility, in
the national economy of this country at least, has never "been tully
appreciated. Yet the agriculturist, the builder, the glass-maker,
the metal-founder, and even the housewife, all turn in their need
to the natural sand-resources of the country.
To the man in the street to-day the differences between one sand
and another are neither striking nor important. This attitude has,
of course, not been shared by those who are concerned with the use
of sands in industry, hut it is noteworthy that little or no systematic
investigation of the special properties of British sands of commercial
value has hitherto been attempted.
In many industries the best sand available for the purpose has
been found by a lengthy process of trial and error, but the reason*
for its suitability or the reverse have rarely been systematically
looked into. The inevitable result is that when material of value
for some specific purpose is no longer available serious delay and
inconvenience are caused. Especially has this been the case in
glass-manufacture and in the casting of particular steels, for which
the most suitable -materials in use up to the present were said to be
certain foreign sands with properties peculiar to themselves. The
restriction or stoppage of such imported supplies in war-time, owing
to shortage of ships and labour, has set on foot enquiries as ta.
Avhether suitable sands occur in Britain, and, if so, whether they can
be profitably worked.
Such an enquiry necessitates not only a thorough knowledge of
the sands themselves, their mode of occurrence and properties, but
an investigation into the materials previously in use in each
industry, and an attempt to ascertain the reasons for their special
suitability. Why, for example, should one moulding-sand " burn
on " to the steel poured into a mould and another yield a clean
smooth casting ; or one sand produce a clear, sparkling, white
glass, fit for table-ware or for optical instruments, and another
only a poor green bottle-glass ?
All sands consist, in the main, of silica in the form of broken
grains of crystalline quartz associated with various forms and
proportions of impurities, partly impregnating or coating the
quartz, and partly in the form of grains or dust of other ingre-
dients. When sand is used as a source of silica, as in glass-making,
the most obvious requirement is that it should be as pure as
B
USES OF SAJfDS.
possible and especially free from ingredients which would diminif
the utility or beauty of the finished product. For other purpose
however, the " impurities " themselves may give the sand its speci
value. In certain industries the hardness and shape of the grai:
are more essential than the composition, and the difference betwei
" angular " and " rounded " grains becomes an important matte
Again, the size of the individual grains, and more particular
the relative proportions of material of different sizes in a sarn.pl
has sometimes a bearing on the use of sand : this is spoken oi ;
the " grading " or " grade " of the sand.
In a material xised in such large quantities as sand, suppli
must be cheap. This means that the sand must be abundar
loose, or at least easily disintegrated, and cheaply worked; th
seams or beds must run very evenly in nature and compositio
and must be cleanly marked off from other seams or material
above all, that the market must be easily accessible and carria)
inexpensive and convenient.
The term "sand" to the geologist connotes a limited range
chemical and mineral composition, and a definite grade. Theater
is generally extended to include other minerals than quartz, and
used in commerce for material of varying grades irrespective
composition or angularity. It is also applied to consolidati
sandstones and even to hard siliceous rocks which have be<
crushed for commercial purposes. In this Memoir the most e,
tended commercial application of the term will be taken.
Some Uses of Sands.
Before passing on to discuss the special properties which it
desirable for gkss-sands to possess, it will be well to consid
briefly how desiderata vary in different industries and applicatior
Sands bearing minerals of the rare earths such as monazit
xenotime, thorianite, zircon, etc., are worked for the eleinen
yttrium, zirconium, cerium, thorium, lanthanum, and others, wliw
are used in the manufacture of incandescent mantles and filamen
and _ for refractory paints. Those bearing gems, gold, platirmi
cassiterite, and wolfram are similarly worked for the preckr
materials they contain.
Shore-sands, and others auch as the East Anglian " Crags," ri<
in shell-fragments, form an admirable dressing for the land <
account of the lime that they yield ; this ingredient promot
drainage by^ flocculating the clay of the soil, and helps the pla:
by neutralizing the organic acids naturally produced. Tho val-
of such shell-sands is enhanced when they occur near to agj
cultural country and lime has to be imported from a distanc
It is desirable that all coastal deposits should be investigated .
ihis connexion. Even if the sands are not calcareous they rend
heavy clay soils lighter and more open, breaking them up by t
admixture of coarser grade material, and making the land wannt
more permeable to air, gases, and water, more easily drained, a:
ABEA.S1VES, ETC. O
more amenable to working. Here grade, as well as composition,
is an important factor.
The " Greensands," so-called because they are coloured by the
mineral glauconite which they contain in quantity, have long been
used as fertilizers. The deposits of economic importance in the
United Kingdom are of Cretaceous and Eocene age. Glauconite
is a silicate of iron, aluminium, and potassium ; it decomposes
much more readily than other potash-bearing silicates such as the
felspars, orthoclase and microcliue, and thus liberates the valuable
plant-food, potash. Some greensands are of additional value on
account of their carrying calcium phosphate, an ingredient also of
importance in agriculture. Glauconitic sands have also been used
for softening water.
The use of sand for abrasive purposes depends on the hardness
and toughness of its constituents, and on the " sharpness " of its
grains. Quartz is not only hard, but, as it has no cleavage, it
breaks irregularly and does not easily comminute under wear.
It is employed for grinding marble and other stone, plate-glass,
and metal. It is also used for arming stone-saws, and in the
.sand-blast applied to glass-cutting and etching, the cleaning of
castings, and innumerable other industrial processes. In this work
it soon loses its " sharpness " and requires frequent renewal. In
the old days the housewife used a cheap, fine, sharp sand for
scouring purposes, now she buys scouring-soap consisting largely
of similar tine angular sand bound together with clay, soap, and
gum *. " Silver-sand " is a term used for a fairly pure fine white
sand, used mainly for scouring and for lightening soil. Samples
sold by hardware dealers in London appear, from their mineral
composition, to come from the Lower Greensand.
Large quantities of sand are now consumed in the soap-induslry
for the making of sodium silicate, which is a constituent of some
of the commoner soaps. Not only have pure quartzites and vein-
.quart/ been crushed to yield " sands " for abrasive and other soaps,
but also the relatively impure Glacial sands of Lancashire have
been pressed into service on account of their proximity to the
seat of the manufacture. Sodium silicate (" water-glass ") is also
manufactured for preservative purposes.
In the manufacture of the artificial abrasive, carborundum
(silicon carbide), sand and coke are heated together in an electric
furnace. Carborundum is also used in refractory bricks, as a
.source of silicon in steel-making, and for certain chemical purposes
where its reducing properties are of great value.
Closely allied to abrasives are friction-sands such as those used
to increase the grip of wheels on metal rails. These sands must
be not only hard, tough, and angular, but also dry and of even
:grade so as to slip freely down the feeding-funnel. Similar sands,
which are better if not angular, are used in hour-glasses and
* By on order of the German Government in Aug. 1916, the use of sand
instead of soap for scouring purposes was made compulsory.
4 USES OJ? SANDS.
egg-timers. A well-known geologist, when faced with tl^e enquiry as
to the geological age and characters possessed by these sands, gravely
avoided the issue by pointing out that it was not the custom of
geologists to measure time with hour-glasses !
The practice of sanding floors has almost died out, but the use
of sands for road surfaces and for making road materials is-
increasing rapidly. Angular sands, free from clay, are utilized in
the asphalt industry, the mixture of sand and pitch being of
considerable value for road-dressing. The sands utilized are, as-
far as possible, of local origin ; Lower Greensands from Surrey
and Bedfordshire, and Corallian sand from Oxfordshire, have been
exploited for this purpose.
Considerable quantities of sand are worked for building-purposes.
Most sands are suitable for mixing with lime and water to make
mortar, and usually each district is able to satisfy its own demands.
Shore-sands are, however, avoided on account of the tendency of
mortar made from them to " sweat " owing to the thin films of
deliquescent sea-salts having been left as a' coating on the grains
when the sea-water evaporates. These salts are brought to the
surface by percolating water, and left on evaporation. A similar
effect is observed in the complete breaking up of Chalk fossils
collected from spray -beaten cliffs, unless they have been well soaked
in fresh water before storing. Building-sands should be fairly
angular and not too fine, in order that their grip on the calcareous
matrix may be strong, the mortar becoming . truly a miniature
concrete. Sands used with Portland cement ought not to be
rounded in grain and should previously be washed to ensure
cleanness of surface.
The clays worked for brick-making are often stiff deposits of
almost pure cla}'. As such they can only be used for making flat
tiles and pipes where great strength and adhesion are required. To
reduce shrinkage and cracking during the drying and firing of
bricks, sand is added to the clay and thoroughly mixed with it. A
porous brick of g'ood shape and soundness results. Here, again, the
grade-composition is a leading factor. Manj r of the so-called clays-
in the geological formations of Britain are not true clays, but
contain already a variable admixture 'of sand and are thus really
loams. The G-lacial brick-earths, the Keuper " Marls," and the-
London "Clay" are deposits of this character largely employed
,for brick-making.
Parting-sands, which are usually dry, sharp, fine, quartzose-
sands, are used in metal-casting and in the manufacture of bricks
and pottery. In the case of brick- and tile-making, the sand used
to "dust " the mould exercises considerable influence on the texture
and colour (due usually to oxides of iron) of the surface of the-
article. The ability to withstand weathering and the aesthetic
value thus depend in part upon the sand. The use of sand, as a
substitute for flint when the latter is not procurable in the
making of glasce, has not found much favour in the Potteries.
Sand is used for repairing and lining kilns or " ovens " and for
REFBACTOEY S-AJTDS. 5
dusting tlie floors. In metal-casting, "burnt" moulding-sand
from near the surface of previously-made castings is frequently
and successfully used as a parting-sand.
In connexion with water-supply, sands are of considerable im-
portance for purposes of filtration. In order that there may be a
large proportion of interspace between the grains, the sand should
be fairly coarse and its grains preferably rounded, with as large as
possible a percentage of grains belonging to one grade. Thus the
sand should be free from clay, and of course from organic matter,
while the absence of lime is an additional advantage.
Before the introduction of blotting-paper sand was of service as
an^absorbent f or 'superfluous writing-ink. It is said to be similarly
utilized in modern industrial practice as an absorbent for explosive's
of the mtro-glycerine type, in substitution for such natural siliceous
earths as diatomite and kieselguhr.
The most important commercial uses of sand, namely, those
connected with the property of refractoriness to high temperatures,
have been left until the last. Silica, of which quartz is the com-
monest crystalline form (though other allotropic modifications such
as tridyrnite and cristobalite exist), has to be raised to a very high
temperature (1650 Centigrade) before effective fusion takes place.
Quart/ose sands and sandstones bearing a high percentage of silica
and no fluxes such as alkalies or alkaline earths are therefore in
great demand for the floors, sides, and roofs of kilns and furnaces,
and for the bottoms of soaking-pits. Sands of corresponding
composition are also required for fettling furnaces (that is, re-
coating with silica the baths which hold the molten metal), making
crucibles and fire-bricks, and other similar purposes.
"Silica-bricks," used so largely for furnace-work, gas-ovens, and
similar purposes where very high temperatures must be successfully
withstood, are made from refractory sands. No lime or other
alkaline earths, no alkalies, and very little, if any iron, should be
present. Highly quartzose sands are therefore required, and a
great advantage accrues if such sands possess a " bond " which is
itself refractory. As examples may be quoted the kaolin-bearing
whitish sands of Devon and Cornwall, associated with kaolinized
granite, and the similar deposits of the Mountain Limestone district
of Derbyshire and Staffordshire.
Included in the subject of refractories comes the wide and
difficult problem of moulding- sands. These vaiy according to the
metal which is being cast, the shape of the mould, and their position
with respect to the metal. Thus there are facing- and core-sands
in addition to ordinary moulding-sand, and the range in composi-
tion is from true sands almost entirely composed of quartz to loams
containing no small proportion of clayey bond. The problem of
moulding-sands is too large and controversial to be entered tipon
here, and demands a memoir to itself, but a few points may be
Sections marked thus deal with sands and rocks which are also of value
for refractory purposes.
CHAPTER II.
THE NATURE OP SANDS.
Formation of Sands. Sands and similar deposits are the
result of the gradual breaking down of rocks. The sun's heat,
frost, rain, and gravity are among the geological agencies which
are chiefly engaged in this work of disintegration and attrition.
Fragments of rock, in their continual movement to lower levels,
are reduced in size by wear and tear, and broken up into their
constituent mineral grains. Chemical, as well as mechanical, action
assists in this work. The more easily decomposable minerals rot
away, and the more obstinate are loosened from one another. In
the decay of minerals the more soluble salts are carried off in
solution, while the less soluble yield fine clayey or micaceous
material which may be carried in suspension for long distances.
The disintegration of rocks thus results in the production of
simple individual mineral grains varying considerably in size.
This material is carried downwards towards the sea, and collected
at lower levels. In transit it is winnowed by wind and washed by
water. Most sands and related sediments are either deposited in
water or have been washed down and assorted by water at some
time in their history. The sorting is controlled by the S'VM and
weight of the grains, coarser grains and denser minerals being
.dropped down near to the source of supply. This sorting is never
perfect, and it is not usual to find in geological strata a deposit
made up entirely of material of one size. Nor even do we find,
with very rare exceptions, that one grade sand, silt, or- clay
makes up the whole of a single bed. The manner of transport
and deposition leads in any one deposit to a mixture of grades
which may be valuable or inimical from a commercial standpoint. 1
A tendency generally exists for the collection in basins of
deposit of material which has been brought from many different
sources. Working against this tendency towards the production of
rocks of mixed grades we have the selective transport and depo-
sition due to currents of air and water. Heavier and larger fragments
are dropped first, finer ones are canned farther, and the finest
frequently travel long distances before the velocity of the stream
is so far reduced that they come to rest. A fairly complete.-
natural grouping therefore takes place, gravel, sand, silt, and mud
boing found at successively greater distances from their place of
origin. But this grading by water or air is not a perfect ono ;
the manner of transport varies accordingly as the small particles
Sections marked thus deal with sands and rooks which are also of valuo
for refractory purposes.
iSi LIBRARY )
AND COMPOSITION jGff", SA1TDS. 9 /S
are held in suspension, rolled along the boi
by leaps (saltation), and the final deposition^
variation of direction and velocity of the currents^ 1
upon the precipitating power of dissolved salts.
Sudden arrest of material near to its source, especially where
it has been brought down by torrent-action, results in deposits
consisting of about equal proportions of coarse and fine grades ;
they may be termed " non-graded " (see Fig. 8 and page 32). Such
a case is exemplified by many of the Cretaceous and Tertiary deposits
around the Dartmoor and Cornish granite-masses. Torrential
streams of water poured down the slopes and ravines in past ages,
rolling pebbles and boulders of granite and limestone, fully charged
with grains of quartz, felspar, tourmaline, etc., and milky-white
with china-clay from the decomposed felspar of the granite. The
sudden checking of their velocity when they reached the still waters
of the lakes, the larger sluggish rivers, or the lower ground, caused
the bulk of the transported material to be thrown down higgledy-
piggledy, all grades mixed, frequently as an alluvial fan.
On the other hand, the continual sorting of sediments along the
shore by the action of waves and winds has resulted in the elimination
from shore- and dune-sands of both very coarse and fine material.
The clay and silt particles are carried far away by wind and water,
and the coarse sand and gravel left alone; thus the percentage
of medium-sized sand rises very high, and the deposit is almost
perfectly graded.
Composition of Sands. Usually each grain of sand is an indi-
vidual mineral fragment contributed by the parent rocks which
have undergone denudation. While sands are frequently made up
of a large variety of different minerals, quartz and, to a less extent,
felspar usually constitute more than nine-tenths of their bulk.
The chemical composition of the constituent minerals, their prone-
ness to decay, and the compounds resulting from their partial
or complete decomposition, are all important factors when the
commercial use of the sand is under consideration.
While the grading of sands and the sorting of minerals according
to density are never perfect, a strong tendency exists towards
simplification, which is helped by the proneness to decay of the
less stable minerals. J3y repeated geological action, sorting again
and again, very pure and well-graded sands come to be formed,
and it is noteworthy that ah 1 the best glass-sands occur in the later
geological formations. On the other hand, the ancient Ordovician
and Silurian "sands" are usually ill-sorted and very variable in
composition.
As a rule, sands contain only a small proportion, of the minerals
known as the heavy minerals, which possess a density greater
than 2'8. These, like quartz, have proved themselves sufficiently
stable to withstand decomposition, and their presence is often a
useful indication of the source of the sandy material. Most of
the common rock-forming minerals occur in sediments in more or
10 THE NATTTKE OP SANDS.
less relative abundance. In ordinary sands the proportion of
heavy minerals varies from O02 per cent., or even less, to 4 or 5 per
cent, by weight (the latter quantity in sands of fine or superfine
grade only).
The minerals composing sands may be divided into two groups :
the allothigenous or detrital minerals, derived from older rocks,
and the authigenous minerals, which were formed at the time
the sands were deposited or at some later date. "We are mainly
concerned with the allothigenous minerals. Some of the heavy
detritttl minerals are fixed chemical compounds, others are molecular
mixtures which vary somewhat in their composition, the colour and
optical properties changing- sympathetically with the chemical
constitution. In the latter group are the pyroxenes (augite, etc.),
amphiboles (hornblende, etc.), olivines, epidotes, etc.
The chief heavy minerals occurring in sands are the following:
OXIDES > Anataae, brookite, mtile (TiO a ).
Oassiterite (SnOs) ; corundum (Al a O a ) ; hematite (Fe a O n ) ; limonite
(2Fe.,O., . SH.,0) ; magnetite (Fe-,0,); spinel (oxides of Fe, Cr, Mg r
Al, eto.'); titanoferrite or ilmenite (FeTiO ;1 );
SILICATES : AndaluRite (silicate of Al) ; augite (metasih'oate of Al, Fe r
Mg, Ca, Na, eto.) ; biotito (silicate of Al, H, K, Fe, Mg) ; enstatite
(MgSiO a ) ; epidote (hydrated silicate of Ca, Al, Fe) ; garnet (silicate-
of Mg, Ca, Mn, and Fo, Or, Al) ; glauoonite (ailioa^e of K, Al, Fe) ;
hornblende (metasilicate of, Al, Fa, Mg, Ca, Na, etc.) ; hypersthene
(MgFe)SiO;, ; kyonite (silioate of Al) ; musoovite (silioate of H, K,
Al) ; olivino (orthosilioate of Mg, Fe) j sillimanite (silioate of Al) ;
sphene (CaTiSiOJ ; staurolite (silioate of Fe, Mg, Al) ; topaz (fluo-
silioate of Al) ; tourmaline (boro-ailicate of Al) ; zircon (ZrSiOJ.
Oilier compounds : Apatite (caloium phosphate with calcium, fluoride or
chloride) ; caltrite (CaGO.,) ; monazite (phosphate of Co, La, eto.) - t
pyrite (FeS.J ; pyrrhotite (approximately FeS).
Where older sediments have been broken down to make new
rocks, only the most obstinate detrital minerals, such as iron ores-
(including particularly ihnenite), mtile, zircon, tourmaline and
others, survive, and the proportion by weight is low. When
crystalline rocks of igneous and metamorphic origin are subjected
to denudation, they yield a rich and highly varied assemblage of
minerals. It is noteworthy that most of the heavy minerals
occurring in sediments are of raetnmorphic origin ; as examples
may be quoted, spinels, garnets, rutile, tourmaline, staurolite,
andalusite, sillimanite, sphene, epidote, muscovite, biotite, chlorite,
kyanite, and amphiboles (including common hornblende, glauoo-
phane, actinolite, etc.). Igneous rocks appear to provide an
assemblage of minerals more liable to decomposition. However,
those derived from an area of pneumatolysis are fairly stable, and
include garnets, cassiterite, tourmaline, topaz, andalusite, etc.
Minerals derived from other igneous rocks include zircon, rutile,
anatase, apatite, brookite, white and dark micas, hornblende, and,
less commonly, augite, together with a few others.
The mineral constitution of a sediment varies not only with the-
COATING Ol- 1 SAJTU-aKAUra. 11
parent rocks laid under contribution, but with its distance from
the source of origin, the grade, and the conditions of deposition.
Unless local concentration is produced by wind- or stream-action,
or by the oscillatory effect of currents, the proportion by weight
of the heavy crop will tend to decrease the farther we go afield, and
the variety will be reduced as minerals prone to decay are eliminated.
The exact connexion between mineral composition and grade is
not yet thoroughly understood; it is undoubtedly a close one.
During the process of deposition, other minerals may be formed
through organic agency, among them being glauconite, calcium
phosphate, Hmonite. 'secondary silica, etc.
Finally, we have those minerals (authigenous) which develop
subsequently in sedimentary deposits as a result of alteration of
other minemls ; a few such are iron oxides, secondary silica,
leucoxene, anatase, chlorite, etc.
If the heavy minerals are present in quantity in a sand they
affect its chemical constitution very considerably. Alumina might
be expected to be abundant in a heavy residue, and it is note-
worthy that lime is usually low, the lime-bearing minerals, Avith
the exception of some hornblende, pyroxene, epidote, etc., tending
to decompose. In sands subjected repeatedly to the action of
geological agencies, the latter group of silicates first disappears,
then the ferro-magnesian minerals, and, finally, the aluminous
silicates, when certain iron ores, zircon, rutile, and tourmaline only
survive.
Coating of Sand-grains. On the principle that, chemically,
dirt is only "matter in the wrong place," the detrital minerals
of a sand may be regarded as impurities when we desire to find
a sand pure enough for a particular purpose such as glass-making.
More important, however, are the impurities resulting from decom-
position of these minerals and those introduced either during
deposition of the bed or subsequently by the action of percolating
water. An example of such an impurity is the iron staining in
tints of red, brown, and yellow, so widely met with in rocks.
Oxide of iron (as hematite, Fe.,0.,, or limouite, 2Fe 2 O.,.3H a O),
"Nature's colour-box," acts as a coating to the mineral grains
and at times cements them together into a compact rock. Other
minerals, such as silica itself, clay, fluorspar, barytes, calcite,
dolomite, phosphates, etc., also play a cementing rdle. Certain
unconsolidated sands, while apparent!}' fairly pure and clean, have
a fine dust-like coating of clay or calcareous material deposited
upon the grains.
Association with Organic material. Sometimes organic
material such as plant-remains has the effect, either bj r acting as
a reducing agent or ~by the production of humic acids, of clearing
a sandy deposit of impurities or of rendering them more easily
soluble in percolating water. Some of the purest quartz-sands
known to us, remarkable on account of the freedom or the grains
12
THE MATU11E OP SANDS.
from the slightest ferruginous coating, are associated with carbon-
aceous material ' (see Chapter VI.). The famous glass-sands of
Fontainebleau in France, Lippe in Saxony, Hohenbocka in Prussia,
and Aylesbury in England, are apposite examples. The purity of
Coal-Measure Sandstones is interesting in this connexion, and the
bleaching, to the depth of a few feet, of the yellow and red sands
on our heath-lands is a well-known phenomenon. This question is
considered in more detail on page 140.
Form of Sand -grains. During their progress from the dis-
integrated parent-rock to their final resting-place, mineral grains
suffer continual abrasion. If the habit is needle-like, or the
cleavage good, there is a general tendency for rapid fragmentation
and disappearance. Brittleness and softness help the speedy reduc-
tion in size of grains, but when a soft mineral, such as mica, has a
single perfect cleavage, it may be buoyed up and travel a long way.
The continual battering to which grains carried by water are
subjected results in the wearing down of the sharp edges and
angles, and the sands become suhangular. Prolonged rolling
action produced by currents up and down a shore-line, or repeated
action on the same grains through successive geological cycles, may
gradually round even quartz sand. Pot-hole water-action in a con-
fined space (e. g. under glacier-ice) produces sometimes a beautifully
rounded sand. Much more rapidly, however, are sands rounded
by the action of wind, when the grains are continually rubbed
against one another, or meet other obstacles, with no water present
to act as a cushion or a lubricant to reduce friction. Many
desert-sands consist of grains which have been rounded in this way,
but just as the want of rounding does not imply the absence of
desert-conditions, so also its presence may not necessarily he due
to wind-action. Sand-dunes, so common around the shores of the
British Isles, consist of shore- sands which have been blown up into
mounds by wind-action, hut that action has usually not been
sufficiently prolonged to change the angular or subangular shape of
the grains.
Size of Grains. The sorting effect of water and air upon
sediments has been briefly referred to early in this chapter. It is
necessary to consider systematically the sixes of the grains con-
stituting sediments and their relative proportions by weight. At
the outset it should be repeated that the term " sand " has different
significations to the layman and to the geologist. In the above
remarks '' sand " has been used in its wider commercial sense, and
therefore includes related loose deposits bearing some amount of
clay and other material in their composition. In its stricter geo-
logical use sand is a ' grade " term, that is, one depending
only upon the size of the constituent grains. Although most
sands happen to be made up largely of one mineral quart/, the
real criterion upon which the geologist bases his definition is the
high percentage of grains with average diameter between 1 mm.
SIZE OF GRAINS. 13
and O'l mm. (about 0'04 and 0'004 of an incli). Very coarse
sands may have grains up to 2 mm. diameter, and very fine ones
down to O05 mm., but these, are extreme limits. Pebbles of
diameter over 2 mm. fall into the grade known geologically as
" gravel " (not the commercial term of the building-trades, which
connotes a coarse concrete-making bouldery deposit with a good
deal of sand and fine clayey "bind"). Particles of diameter less
than 0'05 mm. constitute "silts." A further limit exists, and
deposits made up of mineral fragments the diameter of which is
less than 0-01 mm. (0'0004 in.) are true "clays" or "muds."
A useful classification of the size-limits or grades is therefore :
Q. Greater tliau 2 mm. dium. Grnvel (G).
VCS. 1 mm. and loss than 2 mm. Very coavse sand. -->
CS. O'o mm. 1 mm. Coarse sand.
MS. 0-26 mm. 0'6 mm. Medium sand. Sliud -
FS. 0-1 mm. 0-26 mm. Fiiie sand. J" e ^ e
r 0'05 mm. O'l mm. Superfine sand or N ...
\ .,, 1 oilt-
s.-j coarse silt. J Lgj.^
V 0-01 mm. 0'05 mm. Silt. J (a),
c. Leas than O'Ol mm. Clay or mud grade (c).
The letters Gr, S, s, c, etc., denoting the various grades are for
use in this Memoir only as a means of shortening the expression
of the mechanical analyses quoted in later chapters. Thus, a
sand from the Eed Crag at Foxhall, Suffolk, consisting of 11'8 per
cent, by weight of very coarse sand-grade ( > 1 mm. & < 2 mm.
. diam.), 44'1 per cent, of coarse sand-grade (>0'5& <lmm.),
41-5 per cent, of medium sand-grade f>0'25 & <0'5), 2'2 per
cent, of fine sand-grade (>0'1& <0'25), 0'2 per cent, of silt-
grade (>0-01 & <0-1), and O2 per cent, of clay-grade (<0'01>
would be represented thus :
YCS 03 MS FS jj c S
11-8' 44-1' 41-5' 2-2' 0-2;' ; 2 ; 99-6'
where S represents the total sand-grade ( >0'1 mm. diameter).
14 METHODS OF STUDT Of SANDS.
CHAPTER III.
METHODS OF STUDY OF SANDS.
For His proper knowledge of sediments, considering both their
geological interest and economic value, it is desirable that we
should be acquainted with the chemical, mineralogical, and
mechanical compositions of each sample. In the reading of " the
riddle of the sands," each of these three analyses yields interesting
.and valuable data, and for glass-sands in particular the chemical and
mechanical analyses are most important. Although desirable, it
is not so essential for commercial purposes that we should also be
.acquainted with the mineral composition ; the knowledge is, never-
theless, of considerable value in special cases and may give an
indication of the particular treatment required and of the presence
of minerals detrimental to the industry, or may enable the user to
ensure that successive consignments of sand come from the same
quarry or bed.
Chemical Analysis.
Since quartz and felspar usually make up the bulk of a sand;
and aluminous silicates that of a clay, the silica-percentage gener-
ally runs fairly high, reaching in very pure sands and sandstones
9S or 99 per cent. Complete analyses are very desirable, especi-
ally of moulding " sands," but where only fairly pure sands
are investigated, as in connexion with glass-making, it is often
sufficient to estimate silica, iron oxide (as Fe a 3 ), alumina, and
water. Other elements will rarely be present in quantities larger
than "a trace." If they should be, however, it is highly desirable
that even small percentages should be recorded. Their effect in
the actual making of the glass is not known, but .numerous
problems and difficulties have arisen in the processes and have not
jet been explained. Small quantities of foreign substances may
play a greater part than has hitherto been suspected in determining
the character of satisfactory or unsatisfactory glass.
The chemical composition varies according to the amount and
character of the cementing material upon the individual grains,
but more according to the variety and relative abundance of
detrital minerals present. As previously remarked, the heavy
detrital minerals are mostly oxides and silicates, but borates,
fluorides, phosphates, chlorides, etc., also occur. The total silica
estimated in a sand is therefore made up of free silica, that of the
quartz-grains themselves, together wi^h the combined silica of the
other minerals. If it is not desired to carry out a complete
chemical analysis involving fusion with alkaline carbonates, the
iron-content of the sand may be estimated for glass-purposes after
MINERAL ANALYSIS. 15
digesting the sand with hydrofluoric and sulphuric acids in a
platinum basin, as mentioned below.
In carrying out cheinical analyses of glass-sands the following
precautions should be observed. . Silica should be estimated in the;
usual way, being separated by three evaporations with hydro-
chloric .acid with intervening filtrations. The purity of the
weighed silica must in all cases be checked by evaporation with
pure hydrofluoric acid and a drop of sulphuric acid ; if this pre-
caution be omitted the results obtained will invariably be slightly
higher than the true value.
Iron is best determined by a colorimetric method in a separate
sample after solution in hydrofluoric and sulphuric acids. As in
some cases iron-bearing minerals which are only incompletely
attacked by these acids are present, any insoluble residue, especially
if dark coloured, should be filtered oft', ignited, and fused with a
little sodium carbonate or potassium pyrosulphate. The melt is
dissolved in dilute sulphuric acid and added to the main portion.
A blank test with the reagents alone should always be made to
ascertain whether these are free from, traces of iron.
Titanium may be conveniently estimated colorimetricallj- in the
portion used for the determination of the iron. Care must, how-
ever, be taken to ensure the complete expulsion of the hydrofluoric
acid, as even small amounts of this render the colorimetric estima-
tion inaccurate.
No constituents should be estimated by difference, and the
ordinary commercial chemical analyses of sands (which usually
give a total of exactly 100 per cent.) are of little value for glass-
making or refractory purposes.
Mineral Analysis.
Apart from the determination of the actual species present,
the mineral analysis is useful as giving an indication of the
relative amount of heavy detrital minerals and the quantity of
such lighter minerals as quartz and felspar. The earliest method
in use for the purpose of conducting a mineral analysis was that
of "panning," so well known to the miner. Gentle agitation of
the sand beneath water, combined with a slight rotary movement
with a jerking "throw," has the effect of causing the heavier
minerals to segregate at the bottom. The lighter constituents
above, making the bulk of the sand, are washed off carefully in
a gentle water-current. Separation of minerals such as quartz
from gold or cassiterite (tin ore), each of which differs considerably
> from it in density, proves very successful, but for geological in-
vestigation, where it is desired to separate minerals of density a
little below and a little above 2-8, the method by itself is not
suitable. To reduce the bulk of the sediment, and to increase
the relative proportion of heavy constituents in order to obtain a
larger quantity for qualitative examination, panning is adopted.
If carried too far, some of the less dense of the heavy minerals
may be washed away with the lighter.
16
METHODS OF STUDr OF SA.NDS.
Before being analysed inineralogically, a sediment is sifted free
from larger compound grains, and, if necessary, washed clean from
clayey matter. The dried sand or silt is then treated with heavy
liquids to obtain the small crop of minerals the density of which
is greater than 2-8. The proportion of these is usually so small
that examination of the untreated sand only revetls occasional
grains. The densities of quartz and felspar, which make up the
bulk of sands, vary from 2'54 to 2'76, while those of the more
interesting detrital minerals mentioned vary from 2'9 to 4 or
more. Quartz, felspars, and certain other light minerals therefore
float in a liquid of density 2-8, while the heavy minerals sink.
The apparatus required for mineral analysis is very simple. An
ordinary funnel (dropping funnels have been used, but the open
conical form is perhaps preferable) fitted with a ground-glass tap
or rubber- tubing and pinch-clip is all that is required (Figs, 1#, 1 i).
Fig. 1 a.
Fig. II.
\l
Funnels for separating "heavy minerals from sands.
The most suitable heavy liquids in use are brornoform (density
about 2-84) and Thoulet's (Sonstadt's) solution (mercury potassium
iodide in aqueous solution, density from 2*8 to 3 - l, according to
concentration). The heavy liquid is poured into the funnel and
the sediment added, the whole being well stirred at intervals to
permit of the easier settling of the heavy grains. When the
separation is complete (in practice it is probably never perfectly
so) , the light grains form a belt at the top of the liquid, there is
usually an intervening clear portion, and a sediment of heavy
grains occurs below. The latter portion of the sand is tapped off,
MIITEBAL ANALYSIS. ' 17
filtered from heavy liquid, and washed with benzene if bromof orm has
been employed, or distilled water if use has been made of Thoulet's
solution. The light crop is similarly dealt with, the Avashings in
each case being saved and concentrated later over a water-bath or
by distillation. Heavy liquids are thus used many times over.
If necessary, the heavy crop may be further separated for diag-
nostic purposes by magnetic, electromagnetic, electrostatic^ rolling,
and other methods, and by treatment with heavier liquids, such as
inethylene iodide (density 3'3) *.
After some practice, many of the tiny heavy mineral grains may
be recognized by examination with a high-power hand-lens ( x 15
or 20 diameters). Eor permanent use under the microscope they
are mounted in the usual manner in Canada balsam (refractive
index about 1'58), and examined in transmitted and reflected light.
Tor rapid temporary examination it is useful to immerse some of
the residue in such a medium as clove oil (refractive index about
1-53), but then the mount is not permanent. The minerals are
-identified by their shape, crystalline form, cleavage, fracture, en-
closures, alteration, and such optical properties as colour, refractive
index, pleochroism, birefringence, extinction -angle, interference
figure (directions-image), twinning, etc. For these mineral
characters reference must be made to any good book on rock-f orming
minerals. The size of the different mineral grains is measured by
means of eyepiece and stage micrometers.
The heavy detrital minerals usually stand out in relief (owing
to their higher refractive indices) when examined in balsam or
clove oil (see Plate II. figs. 2, 3, and 4). It is also useful to-
examine some of the lighter crop in the same way. Since quartz,
and felspar have refractive indices very near to that of the medium
(clove oil or Canada balsam), the grains if fresh and clean have-
very faint borders in ordinary light (see Plate II. fig. 1). A very
slight ferruginous coating on the grains is then easily detected.
Q-rains of a highly pure glass-sand immersed in clove oil almost
disappear. Felspar is usually turbid with alteration products con-
sisting of micaceous material or clay (kaolinization) .
In certain exceptional cases, where the grading has been well
earned out by natural agencies and a good proportion of heavy
minerals is present, ordinary sifting will separate, to a remarkable-
degree, the coarser light minerals and the finer heavy ones which
required the same strength of wind- or water-current to transport
them. As an example may be quoted the dune-sand from Bal-
gownie Links, near Aberdeen. A mechanical analysis of this
deposit yields : Coarse sand 2 - per cent., medium sand 91-2 per
.cent., fine sand 3'3 per cent., superfine sand or silt 2'9 per cent.,
dust, etc., 0'6 per cent.; total sand-grade (>0'1 mm. diameter)
96'5 per cent. The portion of diameter greater than O25 mm.
* T. Orook, " Tlie Systematic Examination of Loose Detrital Sediments,"'
Appendix to Hatch & Rastall, ' Sedimentary Books,' London, 1913. Wein-
sohenk (translated by Clark), " Petrographio Methods," New York, 1912,.
and other works.
C
jg METHODS OF STUDY OF
(medium and coarse sand) consists of quartz and felspar, while
that of diameter 0'25 to O'l ram. (fine sand) consists almost
entirely of heavy detrital mineral grains, epidote, augite, garnets,
tourmaline, and zircon being conspicuous.
In very pure sands or sandstones, the heavy crop may be less
than O'Ol per cent, in weight, but it sometimes increases to 4 or
5 per cent., as, for example, in some samples of Bagshot Sands,
Inferior Oolite Sands, and others. Usually it is found that the
coarser the sand becomes the smaller is the heavy crop yielded ;
silts and fine sands often cany the highest proportion. Estimation
of the heavy crop of true clays is very difficult to make, as it has
not been possible to obtain a good separation in a heavy liquid of
the very fine material which takes a long time to settle.
Complete mineral analysis may, as a rule, be earned out within
an hour, that time serving also for the identification of all the
important detrital minerals. Mineral analysis is much more rapid
than chemical analysis, and yields general information as to the
chemical compounds present and then; relative abundance. A check
upon the chemical analysis and a knowledge of what elements to
look for are thus obtained. Chemical, mineral, and mechanical
analyses may all be in operation at the same time.
Mechanical Analysis.
A mechanical analysis of a sediment seeks to record the various
sizes of the constituent grains, and the relative proportion by weight
of grains between certain limits of size. These size-limits are
known as " grades," and a useful classification has been given in
Chapter II. on page 13.
The general importance of mechanical analyses in industry is
only being realized very slowly. Agriculturists have long recognized
the value of mechanical soil-analysis ; indeed, the methods of work
were first introduced in this connexion. Mining-engineers subject
their battery-pulps to such analysis in order to determine the effi-
ciency of their machinery, and they use various forms of apparatus
designed to separate pulps into grades*. Water-engineers have
recognized the importance of the knowledge of relative proportions
of certain sizes in coarser sands and gravels in the matter of
water-filtration, and the distribution and movement of underground
waters f. The significance of the method has been realized to
some extent in pottery -work. Not yet, however, have glass-manu-
facturers, metal-founders, brick-makers, and others fully appreciated
the value and importance to themselves of a knowledge of the.
mechanical constitution of the clays, silts, loams, and .sands which *
form their raw materials. ITrequently there has been some realiza-
tion of the value of the investigation^ but crude methods of sifting
* H. Stadler, " Grading Analyses by Elutriation," Trams. Inst. Mitring &
Metall.-rrii. (1912-1913) page 686.
f C. S. Sliebter, "Motions of Underground Waters." Water-Supply and
Irrigation Papers, U.S. Gaol. Surrey, No. 67 (1902); King, U.S. G. S. 19th
.Annual Eeport, 1897-8, page 67.
MECHANICAL ANALYSIS : SCJtEENINtf. 19
rare often deemed sufficient. That the old order of things is
changing is evidenced by the fact that elutriation apparatus has
been set up in a few works as well as in a few scientific institutions
in this country. Some managers of glass-works have recognized that
the grade-analysis of a glass-sand is of as much importance as tne
chemical composition (provided, of course, that the latter does not
fall outside certain limits). Otherwise no scientific investigation
.as to a suitable mechanical composition has been made, experience
being trusted to as a genei-al rule. Usually only sifting through
wire-screens has been adopted by sand-merchants or manufacturers
.and founders.
(a) Screening. Sifting or screening may be resorted to for
^coarse sands, but for fine material the procedure is objectionable
both because of liability to contamination and want of accuracy.
Moreover, very fine grades cannot be separated by sieves, as the
.-apertures cannot be made sufficiently small. Prom a scientific
standpoint the sifting of sediments through wire-screens with
.square or rectangular mesh does not give accurate results, since
grains of various diameters up to the length of the diagonal of the
.aperture pass through. It is the mean and not the major dia-
meter of the grains which determines what shall pass the screen.
Sifting, therefore, does not guarantee sizing. Where sifting is
.adopted, round-holed sieves, with the holes punched out and set in
60 triangular spacing, should be used. It is even then questionable
whether sifting much below 0'5 mm. (about 0-02 inch) is entirely
satisfactory. Smaller holes than 0'5 mm. cannot be punched with-
out difficulty, and O25 mm. (O'Ol inch about) sieves are therefore
wire screens *. The latter mesh is the minimum limit of screening
.adopted by the writer. In these screens and in the smaller " 120
to the inch," supplied by makers, the apertures are square and
tend to become clogged by use. Contamination thus occurs,
-especially if the metal of the screens be iron, which inevitably
rusts in time. All sieves for scientific work should be made of
copper or brass.
Before passing on to a description of the forms of apparatus
used in elutriation, a note is desirable upon the standardization of
.grade-measurements. As in other scientific work, the use of the
metric system units is preferable and simplifies all calculations.
r The grade-sizes adopted in this Memoir are therefore expressed
in millimetres, and may be converted to English units if required
(25'4 mm.. 1 inch). Screens are frequently made according to
English units, 30, 60, 90, etc., meshes to the inch. In the I.M.M.
mesh screens (inch-units) the thickness of the wires is equal to
the diameter of the aperture, hence, for example, a 120-mesh screen
has apertures about 0'004 inch iii diameter (about O'l mm.). In
other screens (30, 60, 90 mesh, etc.) this is not the case, the wires
* Perforated brass or copper screens are now supplied down to O'l mm.
lay Messrs. J. & P. Pool, Ltd., Hayle, Cornwall.
02
20
METHODS OP STUDY OP SANDS.
being of smaller diameter than the apertures. Accurate grading
caunot then be carried out.
A plea must be made for uniformity in the expression ot grade-
sizes, preferably in millimetres. The brass screens in use in this
country for soil-analysis and other grading work, while often made
according to metric units (frequently in Germany) are in nests ot
2 mm., 1 mm., 0'5 mm., and 0'25 mm. diameter holes, the last
being square wire-mesh, and the others punched round holes. In
some of the literature on mechanical analysis of sands, the last
mesh-size or elutriation -size is taken at 0'2 mm. diameter instead
of 0'25 mm. It is then difficult to institute comparison between
analyses. The size 0'25 mm. diameter is adopted here, on account
of the exigencies of the apparatus used.
(b) Elutriation. For determining smaller grades of sand,
screening should give place to elutriation. The process of elutrin-
tion is a classification of particles according to size by means of
upward currents of water. The final velocities attained by small
grains of a particular mineral of known size, when they are allowed
to settle freely in water, have been determined both by calculation
and experiment. The results have proved to be remarkably con-
cordant and indicate that the controlling factor in the settling of
small particles is surface-area, and not density. The free settling
of particles in a liquid is due to gravity, but the velocity attained
is controlled by the viscosity of the liquid. The settling of ^ grains
of diameter up to about 0'2 mm. thus conforms to a law which has
been termed* " the law of viscous resistance." The velocity varies
as the square of the diameter of the particle. The settling of
grains above about O2 mm. diameter is controlled by another law,
that of " eddying resistance,-" where the velocity varies as the
square-root of the diameter. Elutriation, hoAvever, is concerned
only with separation of grains up to about 0'25 mm. diameter ;
above that size, sifting is usually adopted. In elutriation the
assumption is made, and lias been found to be justifiable, that the
final velocity of any grain of known size is approximately that of
the upward current of water which will just keep the grain in
suspension. The process enables us to classify sediments into
grades, if desired, down to a limit of 0'005 mm. (about 0-0002 inch)
diameter.
The velocities of water-currents required for separating [suitable
grade-sizes are as follows :
0'4 mm. diameter,
0-3
0-25
0-2
0-1
0-05
0-01
47
32
25
20
6-7
1-78
0-12
(Temperature 15 C.)
mm. per second.
* Sir Q-. G-. Stokes deduced the law on purely theoretical considerations.
Richards, ' Text-book of Ore-Dressing, ' New York, 1909, p. 264.
21
The viscosity of water decreases rapidly with rise of temperature.
The grading of sands is controlled by this viscosity, and cold water
will therefore cany off larger grains than warm water for any one
head and jet in elutriation. Care must be taken always to elutriate
at approximately the same temperature. The difference in tem-
perature of tap- water in summer and winter is sufficient to alter
appreciably the results obtained in grading a fairly coarse sand.
The two chief forms of elutriators used by the writer in the
investigation of sediments are the Crook pattern and a modification
by Stadler of the Schoene type. The former apparatus *, designed
by Mi-. T. Crook of the Imperial Institute, is simpler to make and
work and enables a mechanical analysis to be made more rapidly
than the Schoene, many grades being separated at once. The
apparatus will be best understood from the sketches. The Crook
elutriator consists (Pig. 2, page 22, & Plate I. fig. 1) essentially of
two cylinders, a lower narrow one A and an upper broad one B.
In order to obtain a constant rate of flow upwards for the water in
these cylinders a small movable reservoir C is used, with an over-
flow funnel and tube D. The reservoir C can be moved up and
down, and a constant head and pressure of water may be obtained
in the apparatus when these vary in the water-taps of the labora-
tory. The vessel B is fitted with a double-holed stopper through
which passes a straight tube E acting as a manometer, and a bent
tube F with a jet at the end. The velocity of the upward current
of water in A and B is regulated by the size of the jet-opening, and
the height of the water-level in C, which may be moved up and
down ; the velocity is indicated by the height to which the water rises
in E. For separation of the sediment into sand-, silt-, and clay-
grades (1 mm. to 0-1 mm., Ol mm. to O'Ol mm., and less than
O01 mm. diameter) the internal areas of cross-section of the cylin-
drical parts of A and B must be closely in the ratio of 1 to 50.
Convenient sizes are found to be 1-4 cm. diameter for A, and
9-8 cm. diameter for B, in which case to obtain the required
upward velocities of the water, of nearly 7 mm. per second in A,
and 0-15 mm. per second in B, the jet F is found to bo about
1 mm. diameter, and must permit an outflow of nearly 100 c.c. in
90 seconds. The outflow is controlled and varied by movement
of C, and when the correct measure is found, the height of the
water-column in E is marked and should be kept constant. The
tube A should be about 30 cm. long with a slight constriction in
the drawn-out bottom end (wliich may also be roughened) to
facilitate the grip of the rubber tube upon it. The vessel B is
about 14 cm. long in the conical part and 12 cm. long in the
cylindrical part. The lower portion of B and the tube A should
be of the same diameter and joined by rubber tubing of the same
internal diameter fitted with a clip. Another clip is used to cut
* T. Crook, Appendix to Hatch & Rastall, * Sedimentary Rocks,' London,
1913, p. 349. Apparatus made by Messrs. A. G-allenkarnp & Co. Ltd., Fiusbury
Square, London, J. Monorieff, Ltd., Perth, and Muller, Oione & Co., 148 High
Holborn, London,
22
METHODS OF STUDY OF SJJS'DS.
off A from C. Other details will commend themselves to the*
user of the apparatus. A weighed quantity of sediment (10 or
20 grammes) sifted to 1 mm., after being suitably treated if clay is
present (boiled with water and deflocculated by the addition of pyro-
gallol or such an alkali as ammonia or Avashing-soda) is introduced
into B. When the clips are released, the upward cm-rents of water
separate the material into grades, the sand-grade from 1 mm. to-
Fit?. 2. Crook's Elutriator.
A. Lower cylinder for sand-grade.
B. Cylinder for silt-grade.
C. Movable reservoir giving head of water.
D. Overflow tube.
E. Pressure-gauge.
F. Outlet tube and jet.
0-1 mm. diameter being buoyed up in A, the silt-grade from 01 to
0-01 mm. diameter being held in suspension in B, and the clay-grade
being earned over by the water through F. The last grade may be
collected in large jars and allowed to settle. The water may then
be decanted off, and the sediment dried and weighed As it is
sometimes necessary, Avith clayey deposits, to keep the apparatus
going tor 12 or more hours, until the separation is complete
(shown by clear water passing over from B), a very large bulk
ELUTETATTON. 23
of water accumulates, and settlement takes much time ; moreover,
the fine clayey material is difficult to deal with. When separation
appears to be complete, the screw-clip between A and B should
be closed a little for a short time before the grades in A and B
are finally clipped off from one another. It is the usual practice,
after drying and weighing the separated grades in A and B 4 to
find the grade of < -01 inin, diameter by difference. The proportion
of material of diameter > 1 mm. may be found by sifting before
elutriation. The grading obtained by this apparatus is there-
fore >1 mm., >O1 and <1 mm., >CK)1 and <0'1 mm., and
< O'Ol mm. As it is often desirable to know the percentages of Hne r
medium, and coarse sand, the dried portion of diameter > - 1 and < 1
mm. may be subjected to sifting through 0*5 and 0-25 mm. sieves.
In the case or time sands, very little material should be found
in B or pass over through F. The height to which a knoAvn
weight of sand is borne up in A during the experiment gives the
observer an idea of the proportion of the coarse, medium, or fine
sand-grades. For example, in the elutriation of Fontainebleau
sand, a seething mass ot grains. 10 cm. high, with a sharp upper
limit and almost clear column of water above, is seen in A. The
sharp upper limit indicates a high percentage of one grade such as
coarse sand, medium sand, etc. An indefinite, hazy border, or the
complete occupation of A denotes a niixture of grades, and the
sand is therefore not of the best for glass-making. Crushed rocks
invariably give the latter result.
The great feature of Crook's apparatus is its simplicity and
rapidity of working. By adjustment other grades than those
>1 mm., >0'1 mm. and <1 mm., >0'01 and <0'1 mm., and
<0'01 mm. can be separated. The Schoene apparatus (or its
modification here described) enables grades between any desired sizes
to be separated, as many as eight or nine grades being obtained if
desired. The apparatus requires much more attention, and, since tbe
grades are separated one at a time, a complete analysis of a sediment
may take a considerable time (sometimes a week of working days).
The Stadler modification of the Schoene apparatus * is repre-
sented simply in Fig. 3, page 24, and Plate I. fig. 2. Essentially
it consists of a cylindrical vessel A about 40 cm. long and 5 cm.
in diameter drawn out and bent round at the bottom, and fitted at
the top with a stoppered funnel B, and outlet tube C. The tube
C divides into the vertical piezometer tube D which registers the
pressure and therefore the velocity of water passing through A,
and a jet E. The tank F gives a fixed head of water; the latter
passes down the tube Gr, controlled by a stop-cock H, into A.
A short length of glass tubing and a clip are attached to the
* H. Stadler, loc. cit. p. 689. Made by Messrs. Griffin & Co., Zingsway,
London. Mr. T. Crook suggested a modification of the Sohoene apparatus,
using jets of varying size, in Roy. Dublin Soo., Eoon. Proo. vol. i. pt. 5 (1904)
p. 267. On elutriators generally, see Keilhack : * Lehrbuob der praktischen
Geologie,' 1908, 2nd ed., Stuttgart, and Edes : ' Clays, their Occurrence,
Properties, and Uses,' 1908, 2nd ed., New York.
METHODS OF STUDY OP SANDS.
lower end of A, which may be fitted with a glass stop-cock. The
tube D is about 100 cm. long and is suitably graduated. A
aeries of jets (best made by the operator and standardized with
the instrument) with holes from 2 mm. diameter down to an
extremely small size (about 0'25 inna.) are fitted in turn at E.
Knowing the internal diameter of A, and measuring the volume
of water outflowing per second from each jet, we can plot curves
and draw up a table showing the jet used and the piezometer
reading for all the velocities of water in A we require.
Fig. 3. Stadler's modification of the Sclioene JSlutriator.
1=-*
F
A. Elutriating; cylinder.
B. Intake funnel for sediment.
C. Outlet tube.
D. Piezometer.
B. Variable jet.
P. Tank to provide fixed head of
water.
G. Connecting tube for water-supply.
H. Screw-tap.
. A weighed quantity of sediment, previously treated as described,
is washed down through B into A, and separated into grades com-
mencing with the finest, by attaching the proper jet E and suitably
adjusting the water-level in D by means of 'the screw-tap H.
To distribute the water-current entering A, shot or mercury may
be placed at the bottom. The grades are thus separated one at a
tune and the procedure is slow, so slow, indeed, as to give time for *
complete settlement of the finest grades as they come over, and
permit decantation and estimation. The grades to be separated will
depend on the nature of the investigation. Mr. H. Stadler, while
at the Royal School of Mines, classified battery-pulps in a series of
grades in a reduction ratio of the weight of a grain of each grade of
four to one. For glass-sands, moulding-sands, and general geological
work, it is more advantageous to adhere to the classification detailed
ELTTTBIATION.
25
above, but the apparatus permits the estimation of certain useful
intermediate grades ( > O01 and < 0'05, > O05 and < 0*1 mm. etc.).
The relative advantages and disadvantages of the two forms of
apparatus cannot be discussed here, but it may be repeated that
for work dealing largely -with deposits which are essentially sands,
Crook's apparatus, combined with careful sifting, is simpler and
more rapid in its action. The wide cylinder B in Crook's elutriator
may be substituted for the cylinder A in the Schoene apparatus,
giving greater accuracy in the separation of the fine grades, while
using the latter apparatus.
As some difficulty has arisen at the present time in getting the
necessary glass-ware blown for such elutriators as that designed by
Crook, it may be of service to give a brief account of the single-
vessel elutriator which can be constructed from wide glass tubing
usually kept in stock. Tubing one and a half, two, or three inches
in diameter is eminently suitable for all but the small grades of
diameter less than 0-05 mm. By changing the head of water,
small differences in velocity may be obtained, but for such variation
as is required for the separation of suitable grades of a sand, the
size of the outlet must be varied by means of jets of differing
apertures.
The single-vessel apparatus is indicated in Fig. 4 (page 26).
Separation of the grades takes place in the tubular vessel A. The
length of the vessel is a matter of importance, and the lower
drawn-out conical portion should be equal in length to the upper
cylindrical part. For two-inch tubes, each should be about 8 inches,
but for the separation of grades in three-inch tubes, 6 inches for
each part is sufficient. It is advisable to have the lower end of the
tube opened out slightly to enable the rubber connexion tubing
to obtain a grip upon it. A constant velocity for any one jet is
obtained by adjusting the height of the vessel B, which gives the
head of water. The vessel A is fitted with a two-holed rubber
stopper, into which are inserted the manometer tube C and the
outlet tube D fitted with the jet E. When the desired velocity of
water passing through A is obtained for any one jet, the height
of the water in C is marked. The area of cross-section of A is
determined accurately, and a number of jets may be standardized to
give the required velocities by measuring the outflow yielded by
each. Small differences in velocity may be adjusted by raising or
lowering B. Approximate sizes of jet-holes and head of water, usirig
the two-inch and three-inch cylinders, are as follows :
2-iiich (51 mm.)
cylinder. \
3-inch (76 mmj
cylinder.
Diameter of grains separated
jet-aperture ...
Head of water
mm.
0-4
7
1880
mm. '
0-2
3
1400
mm. j mm.
0-1 I 0-05
3 2
700 j 400
26
METHODS OF STUDY OP SA1TD3.
As in the Schoene apparatus, described on page 23, successively
coarser grades are run off, one at a time, beginning with the smallest.
The Schoene apparatus differs in having a fixed head of water.
Fig. 4. A single-vessel JForm of Elutriator. x fa.
Water
Inlet.
A. Elutriating Cylinder.
B. Movable reservoir giving
bead of water.
G. Pressure-gauge.
D. Outlet-tube.
E. Jet.
T. Spring- olip.
Usually two or three jets to each cylinder will be found to be-
sufficient. The jets may conveniently be made of glass-tubing,
partially closed in the blow-pipe flame and blunt-nosed. Each is
attached to D by rubber connexion-tubing, close up so that the-
GRADE-SIZES OP BAUDS. 27
glaas parts are touching. Care should be taken that if the rubber
or glass-tubing connecting A and B is replaced by longer or wider
material, the overflow should be remeasured and any necessary
correction of head made. Friction plays a very great part in
retarding the flow of water through tubes, especially when the high
velocities necessary to grade to O3 and o4mm. are obtained. The
tubes connecting A and B are therefore made as wide as possible,
and they should not be changed in length or diameter nor should
rubber be replaced by lengths of glass, without checking all
velocities again. (These remarks apply als,o to the Crook and
Stadler elutriators.)
The accuracy of the ehitriation processes has usually been
checked by examination and measurement of grains from the
separated grades under the microscope. A word of warning is here
necessary. In data relating to mechanical analyses of sediments
(for example, moulding-sands, fire-clays, etc.), the average diameter
of the grains constituting each grade is given. Both geologists
and mining-engineers have found that the average diameter
obtained by microscopic measurement has usually too high a value.
When almost spherical grains of known specific gravity from
any one grade are counted and weighed, the average diameter
may be found by calculation. This value is usually less than
that obtained by microscopic measurement, because the grains
are rarely true spheres. They tend to lie in their "flattest"
position, and thus the minimum diameter is usually not measured.
Particularly is this the case with certain crushed minerals, among
which is quartz. Quartz, although it has no cleavage, tends to
crush into a very flaky form, and elutriation products of this
material, which has been recommended as a glass-sand, always appear,
when examined under the microscope, to be coarser than they
really are (compare, for example, figs. 2 and 6, Plate IV.).
It is an interesting fact that the average diameter of the grains
of a sand is frequently a very small figure which is not at all the
size of grain that appears to the eye to be representative of the
sand. An example will best illustrate the point.
Taking a well-graded, washed sand, such as that from Lynn, of
mechanical composition: >0'25 and < 0'5 mm., 9O8 % ; >O1
and < 0-25, 8-7 % ; > O'Ol and < O'l, 0-2 : / ; < 0-01, 0-3 % ; we
find that the true average diameter (the sum of all the diameters
divided by the number of grains) is OO103 mm. This appears to
be a very low figure, and is due to the fact that even in a tiny
' percentage of a small grade an immense number of grains occur.
(Care must, of course, be taken before elutriating to ensure that
.the sand is dry, or moisture may be* estimated as clay-grade by
difference.) Lynn Sand was chosen as being one of the best-graded
materials. The average diameter of Lippe Sand (see page 131
and Plate III.) similarly worked out at 0'009 mm. If, however,
we multiply the percentage weight of each grade by the average
size of that grade, add together the results and divide by the total
METHODS OF STUDY OF SANDS.
percentage weight (t. e. 100), a method adopted by H. Eies*,
we obtain a result which' is certainly not the average diameter,
but which is a size apparently representative of the sand when
examined and measured under the microscope. In the case of
ihe Lynn Sand above, it works out at 0-285 nrm. The latter
result might be termed the " dominant diameter " ; it has been
called erroneously the average diameter. That it is not the latter
may easily be seen by making a similar calculation upon a sandy
clay.
In connexion with the underground passage of water through
.sands, Hazen desired to find the mean or average-sized grain of
each sample f. This mean size he termed the effective size, and
it was to be such that, if all the grains were of that diameter, the
sand would have the same transmission capacity that it actually
possessed. Hazen adopted screening, and decided that the effective
size should be determined from the mesh of the sieve which allowed
10 per cent, to pass and retained 90 per cent, by weight of the
sand. The variety of sizes present in a sample he indicated by the
uniformity coefficient. To determine this, he found the size of
the sand-grain such that 60 per cent, was of smaller and 40 per
cent, of greater diameter. Then the uniformity coefficient
"tlllS Si Zf 1
= ~~at- ~ - ' Hazen found that 10 per cent, of small grains .
etrective size r
had the same effect on water-flow as 90 per cent, of the larger
grains, provided that the uniformity coefficient was not greater
than 5.
The uniformity coefficient for the majority of British sands here
described (dominant grade == medium sand >0'25 and < 0-5 mm.
diameter) is nearly 2. ,
(c) Graphical Expression of Results. The expression of
mechanical analyses in the form of curves brings out contrasts
and similarities in sediments more graphically than does the use
of space (e. g. " strip " or " butterfly ") diagrams. Similar graphs
have been used for screening-analyses in connexion with water-
supply and pei-colation, in the publications of the United States
Geological Survey, and for analyses of moulding-sands in. those of
the Geological Survey of Denmark. The curves here drawn are to
be regarded as approximations only, serving to visualize the lists of
figures given in the tables of mechanical analyses. Reference
should always be made to the latter. Cumulative percentages by
weight of material above the grade-size (marked horizontally) are
set off vertically as ordinates. For example, in the curve XW '
(Fig. 5) representing a specimen of London Cky, about 17 per
cent, of the sample is of diameter greater than O'l mm. and about
55 per cent, of diameter between O'l and 0-01 mm. ; the ordinate '
at the latter grade-size is therefore 17+55=72 per cent. The
* Trans. Amer. Foundrymen'B ABBOO. 1906, page 63.
f 0. S. Sliohter, " Motions of Underground Waters." Water-Supply and
Irrigation Papers, U.S. Gaol. Survey, No. 67 (1902).
^s*
^? ;
.'.'" ':f /" ^>
EXPHESsroaf. 1 *--Y 29" :*
" l ^- I I H R A R V j '
horizontal scale adopted is proportional to th^tpgarrthms or the- /
diameters quoted, in order to keep the scaltT representing the- V X''^>
^K .^
various grades down to clay within the compass .
The curves are plotted from four or five points,' witfr m
for intermediate points obtained from microscopic examin..
Horizontality in any part of the curve means the absence ofTnt?
grade-size, corresponding to the distance that such horizontality
extends. Verticality in the graph means a considerable percentage
of the grade-size corresponding to the position of the vertical
portion. In the figures for glass-sands and other similar well-
graded sands the verticality is probably greater than represented,
but the absence of information as to percentages of intermediate
grades prevents more accurate plotting. All the curves eventually
turn up at the right-hand eud (in the clay-grade portion) when
the total reaches, as it must do, 100 per cent. The approach to the
upper line may be asymptotic, i. e. the particles may gradually
become smaller and smaller to vanishing point; but it is more
probable that in most sediments a lower limit of size of particle is-
reached, when the curve turns up thus ', Probably solution
eventually causes the disappearance of tiny particles "before they
disintegrate mechanically.
Representing the mechanical composition of a sediment as a
curve (Fig. 5) obtained by plotting cumulative percentages of the-
various grades against the diameter of particles in the grades, we
see that a pure gravel, 100 per cent, of diameter not less than about
2 mm., is represented by the vertical line AB, a pure sand of
medium grade by CD, a pure silt by such a line as EF, and a
pure clay by another vertical line such as G-H beyond. Such ideal
sediments do not seem to be present in nature. The curves TU,
WX, and YZ represent actual British sediments which have been
subjected to mechanical analysis. The curve TU is that of a true
medium sand from. the shore at Kynance Cove, Cornwall, WX is-
a true loam, worked for brick-making, from the London Clay at
Ipswich, and YZ is a true clay of Upper Glacial age from
Hasketon, Suffolk. These three sediments approach very nearly
to the highest perfection to be expected from natural deposits.
With them should be compared the curves indicated in Fig. 6,.
which are of some well-known and successful moulding-sands.
The upper curves, representing the famous "Belgian Red" and
"Cornish Red" (Pliocene Beds, St. Erth, Cornwall) moulding-
sands, etc., are clearly from their position indicative of coarser-
sediments than the other represented, which is the well-known
"Erith" sand from Charlton (Kent), much finer in grain. In spite
of the variation in size of the constituent grains, the proportion
of the grades is constant and causes the curves to be remarkably
sympathetic. The graph of the "Belgian Red" moulding-sand is
seen from the figure to cut across the others, owing to that deposit
containing a greater proportion of clay, apparently, ferruginous
kaolin. ActuaUy it is more nearly the ideal moulding-sand expe.cted
on theoretical grounds, i. e. one with high clay-grade fo. J bJjad T: aflj]l,
1179
30 METHODS OF 8TTJDT OF SANDS.
Fig. 5. Mechanical Analyses of Sediments : Graphical representation.
. Sand . Silt x __Clay
100^
A /*"" U
go
x E
I.
G
1
w.
x/
X
eo
|
^
60
4*
s<5>
1 70-
e|
^
<u
w 3 eo
C
fi
0*
/*'
Z
2 50-
u l
u 1
&
'
Q)
*
c.
4
5 40
v x
e
ra
= 30
?*
0^
//
E
m 1
<>x
jpO
a
y
^v
f
V 20
|
V f
s-jpo
f
1
K
/
<^o^
10
J
D ' F
$$'
B
.T^/
^ vV . VL ^-o
>~ H
2-0
1-0
0-5 0-25 0-1 0-05
> Grade Sizes (diameter in Millimetres}
0-01 mma
Fig. 6.
Analyses of Sands : Moulding- and Glass-Sands
compared.
Sand x '-Silt *---Clay
2-0
l-O
0-5 0-25 0-1 0-05 0-01
'Grade Sizes (diameter /'" Millimetres)
EXPRESSION.
31
Fig. 7. Mechanical Analyses of Sands. An attempt towards
representation of Ideal Q-lass- and Moulding- Sands.
irtn?a. <-- Sand < Silt ---,- .g Clay ---
90 .
^ 80 .
oo
I 70 .
3 60 J
S 50 .
Q_
-^ 40
JO
3
I 30.-
T 20 .
10 .
2-0
i-O
0*5 0-25 0-1 0-03 O-OI.
>Grade-St2es f diameter in Mil/trnetres)
Fig. 8. Mechanical Analyses : Unsorted Deposits.
-Gravel -x:- Sand -- ,->< -.-Silt ><--Clay--
4-0 ,2-0
1-0 0-5 -Q-.25 0-1 0-05
-* Grade Sizes (diameter in Millimetres)
32 METHODS OF STUDY OF SANDS.
with a good quantity of sand-grade (other than fine sand) for
openness and ventilation. The ideal moulding-sand for "greensand
moulding " would he graphed as in Fig. 7, AB, the horizontal part
of the curve passing over the fine sand- and silt-grades. Some of
the Pliocene, Eocene, and Cretaceous Beds fringing the kaolinized
granite-masses of Devon and Cornwall approach very closely to
this ideal. Moreover, the clay-grade is composed largely of kaolin,
the refractory properties of which are excellent. The difficulty to
he solved is that of making the kaolin, which is not a very plastic
clay, into a good "hind."
Fig. 9. Mechanical Analyses : possible variation in true sands.
+ Sand -X Silt -$H<- - Clay-
2-0 1-0 0-5 0-25 0-1 0-05 0-01 mms.
-> Grade 5i7es /diameter in millimetres)
On the other hand, a perfect glass -sand should be all of one
grade, preferably among those sizes not so desirable in a moulding-
sand. In other words, a sand from which glass is to be made
shotdd have all its grains of one size, not greater than Q-5 mm.
or less than O'l mm. diameter. The curve CD (Fig. 7) would
represent such a sand.
With these ideal cases should be compared those of Fig. 8, "
representing such unaorted deposits as those mentioned in
Chapter II. The curves in Fig. 9 show the possible variations
in grade of British sands, and from a comparison of Fig. 9 with
Figs. 10 & 11, page 50 (see also Plate III. figs. 1-5), the special
grading of sands for glass-making will be realized. The badly-
graded products obtained by crushing rocks are indicated in Fig. 12,
page 79 (see also Plate III. fig. 6).
GLASS-MANUFACTURE. 83
CHAPTER IV.
Literature on G-lass- Sands, etc. Comparatively little appears to
have been written upon the important subject of glass-manufacture,
and especially in this country is there a dearth of literature bearing
upon the problem. Only a small amountj too, of the available
literature refers to modem processes and developments. For those
interested in the methods used, and those .who desire to realize
to what extent knowledge of our geological resources may help
the trade, the following works are recommended :
Glass Manufacture (Constable), by Walter Kosenhain, 1908.
Glass (Sir Isaac Pitman & Sons), by P. Maraon. Just published.
The Prinoipleirof Glass-making- (G. Bell & Sons), by Powell and Chance,
1885.
Glass. Articles in ' Enoyolppaadia Britannioa,' llth edition, by Harry
J. Powell and W. Rosenhain.
Jena Glass (MacmiHan & Co.), by Hovestadt ; translated by J. D. and
A. Everett.
Glass-blowing and Glass-working, by Thomas Bolas, 1898.
Abridgments of Patent Specifications of Glass : 10 volumes, 1855-1915.
Glass-blowing, by W. A, Shenstone, 1886.
Glass : Article in Thorpe's Dictionary of Applied Chemistry, 1912.
Le Verro et le Criatal, by J. Hemivaux, 1897.
La Vevrerie an XXme Sieole, by J. Henrivaux, 1911.
Die Glasfabrikation, 2 vols., by E. Dralle and others, 1911.
Die Glasfabrikation, by K. Gerner, 1897.
Die Herstellung grouser Glaskorper, by C. Wetzel, 1900.
Die Glasmduatrie in Jena, by E. Zschimmer, 1909.
Glas : being Part I. of Ghemischo Teohnologie, by B. Miiller, 1911.
Die Glasatzerei, by J. B. Miller, 1910.
Zeitgemasse Herstellung, Bearbeitung, und Verzierung des feineren
Hohlglases, by E. Hbhlbaum, 1910.
Die Bearbeitung 1 des Glases anf dem Blasetisoh, by W. Lermantoff.
Scbmelzen nnd Krystallisieren, by G. Tammann.
Die feuerfesten Tone, by C. Bisohof .
The following catalogues and periodicals may usefully be con-
sulted :
Catalogue of works on glass in the Library of the Society of Glass
Technology.
Catalogue of works on glass in the Library of the English Ceramic
Society.
Catalogue of works on glass in the Public Reference Libraries of
Birmingham, Leeds, and Manchester, 1913.
D
34 GLA-SS-MAJSTUFACTTJEB.
Catalogue of works in the Patent Office Library dealing -with Ceramics
and Glass, 1914.
Spreehsaal Kalendar, annual volumes.
Periodicals :
Die Glaainduatrie.
Spreonsaal.
Glashiitte.
Diamant.
SUlkatB-ZeitBohrift.
Keramisohe Rundsohau.
Tonindustrie Zeitung.
Journal of the Society of Glass Technology.
Transactions of the Optical Society.
English. Ceramio Society.
American Ceramio Society.
References to other scattered papers, etc., and to additional French
and German literature, will be round in the works cited above.
Lists of formulae for various glasses have recently been issued by
the Institute of Chemistry *. Others are supplied confidentially.
On the important question of glass-sands, less still has been
written; indeed, the literature may almost be said to be non-
existent. In veiy few countries do we know the properties,
quantity, and workability of the Band-resources generally, and
little of this knowledge concerns glass-sands.
No thorough discussion of the properties and desiderata of
glass-sands is known to the writer. Scattered notes are to be
found in publications of the Q-eological Surveys of the United
States, Denmark, etc. These are referred to in their appropriate
places hereafter t-
The dearth of literature upon glass-sands in this country is
doubtless due to the fact that before 1914 manufacturers of
glass in the United Kingdom used large quantities of foreign
sands, notably from France, Belgium, and Holland. The use
of such imported sands, frequently to the entire exclusion of
our own resources, was due to two main causes : in the first
place, the sands were generally purer than the obtainable British
sands, and, in the second, the cost was less, particularly when
foreign sands were brought back as ballast on a boat's return
journey. The latter state of afEairs arose because the British
.supplies of sand were frequently situated inland ; thus the cost
of transport by water from abroad was less than that by rail from
one part of the country to another. So little has Britain investi-
gated and relied upon her own resources of sand, that it is not
surprising to find a Q-erman writer upon glass-making declaring
-categorically in 1885 that the English sands were iron-bearing,
while only those of the Isle of Wight were considered worthy of
mention. It is stated that the English obtained glass-sand from
* Proceedings, 1915, Parts ii., iii., & iv.
f Since the above was written, there has appeared a discussion of the
^lass-sands of the U.S.A., by Pettke, Trans. Amer. Cer. Soc. 1917, vol. 19,
page 160.
BAW MATBHIALS.
.35
France, America, and Australia ! * Such statements are hardly
correct; for as far back as 1858 Northampton Sands, Ashdown
and Tunbridge Wells Sands, Aylesbury sands, Aylesford sands,
Lynn sands, Thanet Sands, Bagshot Sands, and others were
.already in use f.
Tscheuschner, the German writer referred to above, mentions that
glass-sands were obtained in France from Maintenon, Fontainebleau,
Nemours, and Champagne ; and in the Q-erman Empire from
Nievelstein in the Rhine Province, Hohenbocka in Prussia, and
Lemgo in Westphalia.
Raw Materials : Importance of Sand. The various kinds of
glass may be regarded as mixed silicates (and, to a smaller extent,
borates) of the alkalies, sodium and potassium, the alkaline earths,
calcium, barium, magnesium, etc., and lead, iron, zinc, and
aluminium.
' Probably the silicates, borates, and oxides are in a state of
mutual solution in one another; but, just in the same way as
much dispute exists among petrologists as to the combinations
into which the various elements enter in a natural molten rock-
magma (of which a natural glass such as obsidian is only a
solidified form), so authorities on the chemistry of glass are by no
means agreed upon tbe actual compounds formed. The geologist
is mainly concerned with the fact that the finished product, glass,
consists of 60 to 75 per cent, of silica, which is contributed
to the raw mixture in the form of a sand.
The " batch 1J or mixture of raw materials such as sand, soda-
.ash CNa.COJ, salt-cake (Na S0 4 ), potash (as K a CO ? or KNO a ),
limestone (CaCO,,), red lead (Pb^OJ, manganese dioxide (MnO a ).
coke or anthracite (C), alumina (A1 2 3 ), boric anhydride (B a 3 ),
barium carbonate, calcium fluoride, etc., according to the kind of
glass required, usually consists of 52 to 65 per cent, by weight
of sand. A small amount of silica is sometimes added in the
form of felspar; but the percentage of silica is increased in the final
product (which, when molten, is termed "metal"), as a result
of the loss of such gases as S0 2> C0 a , etc. The silica-percentages
in some well-known glasses are as follows : Window 53 per cent,,
lead flint 53 per cent., soft soda (chemical laboratory ware, X-ray
tubes, etc.) 54 to 56 per cent., green bottle 57 per cent., miners'
lamps 59 per cent., combustion tubing 60 to 62 per cent., plate
62 per cent., resistance (very like Jena) 63 per cent., soda-lime
(Venetian) 73 -4 per cent., potash-lime (Bohemian), 71'7 per cent.,
1 .and so on, the proportions varying somewhat in actual practice.
In point of bulk, therefore, the sand is the most important
* 'Handbnch der Glasfabrikation,' B. TschenBonner (Weimar, 1885),
page 72. AnalyBes of various glass-Bands are also given in Dralle's ' Die
Glaafabrikation,' and of German glass-sands in the 'Spreohsaal Kalendar'
t 'Mineral Statistics : Mem. Geol. Snrvey (1860, being Part ii. for 1858),
-.page 874.
D a
86 GLASS-MAJSTIFACTUEE.
ingredient, and its properties influence to a large extent the
character of the glass obtained.
As emphasizing the bearing of the sand used upon the qualities
of the glass, an example given by Hovestadt may be quoted.
Thermometer-glass, made in the Thuringian Forest district, owes
its special quality to certain sand found only in the neighbour-
hood of the village of Martinroda. The glass withstands repeated
melting, blowing, and fusing without change ; while ordinary
glass, such as that of windows, becomes rough and dull of surface
even after short exposure to the flame. Other sands are believed
to be unsuitable, especially the pure sand from Brandenburg.
The cause of excellence is attributed to the alumina present,
which forms 8'66 per cent; (page 21, Everett's translation).
The raw materials used in glass-manufacture may be conveniently
grouped, from the geologist's point of view, into two classes :
(a) Bocks and minerals such as native silica (in the form of vein-
quarfci, sands, sandstones, or quartzites), felspar, kaolin, limestone,
anthracite, fluorspar, cryolite, etc., which are used, except perhaps
for washing, in the state in which they aj-e won ; and (b) Chemical
products which have been prepared from naturally-occurring sub-
stances. Among the latter are salt-cake, soda-ash, borax and boric
anhydride, potash, alumina, arsenic, and compounds of lead, barium,
manganese, cobalt, chromium, nickel, zinc, and other metals.
The resources of silica, potash-felspar, and kaolin are referred to
in the following pages. No difficulty exists in obtaining fairly
pure limestone (that from Buxton in Derbyshire is most widely
used) and anthracite. Cryolite is indirectly imported from Green-
land and does not occur in the United Kingdom, nor is it known
to occur in the British Empire ; the resources of fluorspar have
recently been dealt with in a publication by H.M. Q-eological
Survey *.
Of the second group, the minerals from which potash can be
obtained are mentioned hereafter. British resources of alumina
have yet to be described in detail. Those of barium (as barytes
and witherite) and manganese ores have been dealt with by
H.M. Q-eological Survey t- Ores of arsenic and zinc occur in
Great Britain, but the resources have not at present been syste-
matically described. The minerals which yield boron compounds,
cobalt, chromium, and nickel are imported from abroad, and are
used in small quantities only.
Colour etc. of the Glass. Upon the sand depend the trans-
parency, brilliancy, lustre, and hardness of glass. The uniform
density of glass, as will be seen in the sequel, is influenced to no
small extent by the mechanical composition of the sand. In
* Special Eeports on the Mineral Resources of Great Britain, vol. iv.,
Fluorspar; (1916).
f Ibid. vol. i., Tungsten and Manganese Ores ; vol ii., Barytes and
Witherite.
THE PEOCESS OF GLASS-MAKING. 37
order that the finished article may have plenty of "life," and
the sparkle and " water-whiteness " of the best glass, due attention
must be paid to obtaining, and treating suitably, the sand itself.
For optical glass and table-ware ("crystal" and "cut-glass")
only the purest sands can be used.
Where the glass is blown or rolled into thin sheets, as in the
making of laboratory-ware, lamp chimneys, incandescent electric
globes, window-glass, etc., the requirements are not so exacting,
but the sand must still be fairly pure. The light passes through
only a small thickness of glass, which, although possessing a
slight colour when seen in a thick mass (sometimes a faint green
due to the small quantity of iron in the sand, at others a faint
pink due to manganese which has been added in the form Mn(X
as a corrective to the iron), appeal's colourless and has plenty of
life in the attenuated state. The colour may then be observed by
looking at the object " edge-on," that is, through a much greater
thickness of material.
While only the merest trace of iron impurity in the sands is
permitted for optical and cut-glass, less pure sands containing
O'l per cent, of Fe a 3 may be used for plate- and window-glass,
. chemical apparatus, globes, etc.
Small quantities of iron or other impurities are sufficient to
detract from the lustre of table-ware, or to spoil the power of
transmitting light possessed by lenses and prisms of optical glass.
Coloured glasses are prepared in one of two ways, the more
common being that of adding a chemical compound to the batch,
and thus obtaining either a coloured silicate (chromium, for green
glass, cobalt for blue, etc.), or reduction to a very finely-divided
metallic state (copper or gold for ruby gkss). The other method is
known as "flashing," and consists in covering the surface of
colourless glass with a very thin coating of a coloured material
(e. </., copper or gold ruby glass, which is opaque when only ^ inch
thick). In either case, to obtain purity of colour, it is essential
that no amount of impurity such as iron should be present.
The Process of Glass-maJdng. The manner in which the batch
is melted to form the glass has also a bearing on the kind of sand
used and its physical properties. Two different processes are
adopted. The batch may be placed in open or closed " pots," or
crucibles, which stand upon a kind of " false-bottom " in the
furnace. This floor is known as the "siege" (Fr. siege) and
has "ports" or openings in the middle (or in the end and side
walls of the furnaces), by which the heated gas and air enter,
playing around the pots. The pots are arranged around the
periphery of the furnace to facilitate the extraction of the molten
" metal " from them as " gatherings " upon the glass-workers'
iron rods or bio wing- irons. Melting of the batch from the bottom
upwards is ensured as far as possible. For ordinary glass-work,
open pots were used; but for special ware, indeed for most purposes
nowadays, impurities are kept out by using crucibles covered with
38 GLASS-IIAJTUFACTUBE.
a hood, " gatherings " being taken through a mouth-like opening
at the side.
In the tank-furnace, the batch is melted in a long bath or
tank constructed from blocks of highly refractory siliceous sand-
stone. Much larger quantities of material can be dealt with in
this way; for, besides the larger capacity, the process is a con-
tinuous one, the batch being fed in at one end of the furnace
(filling-hole) and the metal being continuously drawn from the
other, and cooler, end of the tank (working-hole). Special and
best quality glasses cannot be made in this manner. The tank is
not covered, and the mixture of burning gas and air, forming
sheets and jets of flame, enters through ports in the side -walls
above the surface of the metal.
When the fusion of the batch is complete, the metal is freed
from bubbles of evolved gases and entangled air by means which
vaiy according to the kind of glass made and the craft of the
glass-maker. This procedure is known as "fining."
The pots are usually made of fire-clay (or of fire-clay mixed
with other highly resistant materials), and are very carefully
prepared. The floors, sides, and crowns of the furnaces are con-
structed from highly refractory silica-bricks and fire-bricks (e. g. t
Dinas, Grlenboig, and Stourbridge bricks, etc.), but frequently both
pots and bricks are partially melted in the intense heat obtained
in the furnace (1500-1600 C.). Most furnaces are now built on
the regenerative, and some on the recuperative, principle, by which
the hot spent gases issuing are utilized to heat the incoming mixture
of gas and air.
For the respective advantages of each kind of furnace, reference
must be made either to books or glass-makers. Briefly, it may be
said that for special glasses, where covering of the metal is essential,
when considerable time is occupied in complete fusion and mixture
of the constituents, when they must be kept together long enough
to combine, and where accurate regulation is required, the pot-
furnace is more suitable. "When large quantities of less pure
glass are required, maximum space and heating are to be utilized,
and. time saved by continuous working (for pot-furnaces must
cool down and be reheated, and pots fail and need renewing) the
tank-furnace is better. The level of the metal is kept fairly con-
stant, and therefore convenient for the withdrawal of gatherings,
in a tank-furnace; while the glass left in the bottom of a pot
frequently becomes "cordy" or "wavy" on blowing, and rarely
is as good, or of the same composition and properties, as that
already used from the pot.
BEQTTIBEMENTB OF A. GOOD GTjASS-SAND. 39
CHAPTER V.
THE REQUIBEMEK-TS OF A. GOOD G-LASS-SAND.
The sand hitherto used in this country for .all the best kinds of
glass-work is that of Upper Oligocene age from Fontainebleau,
near Paris. It is shipped from Rouen and delivered in Britain at a
fairly cheap rate. Since the outbreak of war, manufacturers have
found considerable difficulty in getting it through, owing to shortage
of barges and labour, and the dislocation of trade. Enquiries
were therefore made for suitable substitutes from the geological
formations cropping out in Britain, with the results given later in
this Memoir.
, Characters of Fontainebleau Sand. As a glass-sand, that of
Fontainebleau nearly approaches perfection *. If, therefore, w&
look into its properties in some detail, we may hope to realize the
desiderata of a first-class glass-sand, and know what to look for in
any other deposits exploited for glass-purposes.
(a) General Characters. To the unaided eye, the sand is a
beautiful white, fine, even deposit. With a hand-lens the sand
appears to be composed of water- clear quartz, and only here and
there a few dark grains are to be seen. Unless the sand has been
washed after its arrival at the works (and for all .special glasses
for optical purposes and table-ware it is usually washed carefully),
a little dirt and occasional specks of black coaly matter may be seen.
Such impurities are, of course, adventitious, and obtained from
trucks and barges in course of transit. The grains have no coating
of white clayey matter, as many sands have, their white appearance
being due to the ordinary reflection of light from irregular surf aces
They are almost invisible under the microscope when mounted in
media such as clove oil, Canada balsam, etc., the refractive indices-
of which lie very near to that of quartz (Plate II. fig. 1). The
grains are free from the pale yellowish or brownish coating of iron
oxide so frequently seen in sand.
(b) Chemical Composition. Chemical analyses (see Table VI.)
show that the sand contains 99'65 to 99'97 per cent, of silica, and
therefore must be composed almost entirely of pure quartz. Only
a small quantity of iron oxide is present ; hence glass made from
the sand is practically water-clear (provided, of course, no colouring
compounds are added). The alumina percentage is very low, being
probably accounted for by the rare grain or two of felspar seen,
and by the few heavy minerals present. Lime and magnesia are
practically absent.
* The sand from Lippe, in Saxony, is slightly purer, but Fontainebleau
sand being better known in t^i country, has been selected for description. _j
40
OP A GOOD GLASS-SAND.
SiO,
AL.03
Pe a 3
CaO
Chemical Analysis of Fontainebleau Sand.
1 Derby Glass Works. Barnaley Glass Works.
99-80 per oent.
99-67
0-19
0-002
0-14
MgO .................. none
Loss on ignition ... 0*18
0-13
0-006
traoe
n. d.
0-18
Totals 100-182
100-116 per oent.
(c) Mineral Composition. Fontainebleau sand, like many other
veiy pure quartzose sands, contains less than 0'02 per cent, of heavy
minerals, which is below the average for all sands. In this heavy
crop, of density >2'S, the minerals present are clean and fairly
coarse in grain. They include
magnetite, in irregular black grains ;
zircon, in slender prismatic crystals ;
rutile, an irregular foxy-red grains ;
ilmenite, altering to lencoxene ;
tourmaline, blue and brown, in somewbat rounded prismatic fragments ;
ataurolite, in golden yellow angular grains ;
andalusite, as small clear pleochroio grains ;
mufloovite, in larger flakes ;
kyanite, in almost rectangular well-cleaved fragments ;
limnnite, etc.
From the chemical composition of these detrital minerals it is
seen that silica is present in some amount, and that small quan-
tities of iron, aluminium, titanium, magnesium, zirconium, and
boron occur. The proportion of heavy minerals in the sand is so
smaJl, however, that even with the large bulk of sand used for the
batch, the aggregate amount of impurities is slight.
(d) Mechanical Composition. The evenness in grain of the
sand (to the eye) has been commented upon, and mechanical
analyses determined in elutriators like those described in Chapter III.
Diams. "I
in mm, J
OS.
>0-5
&<1.
MS.
>0-25
&<0-5.
PS.
>o-i
&<0-25.
B.
>0-01
&<0-1.
c.
<0-01.
s.
Total sand-grade:
>0-1 & <1 mm.
1
2
<o-i %
70-6 %
70-3
26-6 %
28-3
2-8%
0-6
0-0%
0-8
97-2 %
98-6
1. Obtained by the kindness of Mr. Frank Wood, Managing Director of
Messrs. Wood Bros., Glass Manufacturers, Barnsley.
2. Obtained by the kindness of Mr. 8. N. Jenkinson, Managing Director of
the Edinburgh and Leith Gloss Co. Ltd., of Edinburgh.
A suitable method of graphical expression is by means of a
curve, as in Figs. 9, page 32, and 10, page 60. Practically no grains
CHEMICAL COMPOSITION. 41
occur with diameter above O6 mm., and very few are below O'l mm.
diameter (see Plate III. fig. 1).
(e) Shape of Grains. Lastly, as regards shape, Fontainebleau
sand is made up of grains consistently subangular. To what extent
the rapid and even melting of the batch depends upon the shape
of the grains of sand is a disputed question, but it is clear that
such a sand as that of Fontainebleau, the grains of which are all of
similar shape, is preferable to one containing a mixture of angular,
subangular, and rounded fragments.
(f) .Economics. In addition to the recommendation afforded
by chemical purity, evenness of grade, and suitability of size and
shape, Fontainebleau sand can be transported cheaply and con-
veniently to most British glass-making districts. This is due to
the insular position of Britain, and to the fact that the sand can be
directly shipped from Rouen, and without further handling may be
discharged high up the estuaries which notch our industrial areas.
Requirements of Q-lass-Sands.
Up to the present time most manufacturers and writers have
been inclined to emphasize .the importance of chemical analysis, and
to demand a very high standard of purity in the sand. Experi-
mental work earned out since the opening of the war has tended to
indicate that fairly pure British sands can be used with success for
much good flint-glass work, thus tending to destroy the fetish of
"nothing but Fontainebleau." Indeed, a few of the managers
who have studied the technique of their work place the question
of the evenness of grain of their sands on an equality Avith, if not
above, that of very high silica and very low iron-content. In the
manufacture of glass other than that for optical purposes (where
exceedingly pure sands are sometimes required) the mechanical
analysis is of great importance.
1. Chemical Composition. From the chemical point of view,
sands for glass-making should have a very high silica- content, pre-
ferably over 98 per cent., and for the best work over 99 ~5 per cent.*;
they should have a low iron-content, for the best glass-work below
O05 per cent. Iron is always present in the heavy detrital minerals,
as magnetite, limonite, or ilmenite, or in the form of silicates, etc.,
but since the heavy crop in a suitable glass-sand is always less
than 1 per cent., it is not the iron so present which determines
the suitability or otherwise of the sand. Even such a very pure
" sand as that from Fontainebleau contains a proportion of dense
minerals, but its low iron-percentage is due to the absence of any
coating of limonite (hydrated iron oxide) or hematite (Fe a O a ) upon
the quartz-grains. This iron-staining in sands, which is the cause
* See chemical analyses in Tables. In addition to these, Hohenbooka sand
is said to contain 99'71 per cent., and sand from Nievelstein, in the Rhine
Province, QS'Q 1 ? per cent, of silica.
*^ BEQTJIBEMESTTS OF A GOOD UJjASS-SAElJ.
of the rejection of a large number of English samples, usually exists
on the outside of the quartz and felspar grains, but is sometimes-
seen inside, due to subsequent growth of quartz after depositkm of
the pellicle of iron oxide. Inclusions of ferruginous material also
occur in quartz and felspar, having been caught up and enclosed
at the time of their crystallization.
The iron-percentage should therefore always be low, but a small
amount present in the sand need not render it unsuitable, provided
the mechanical analysis is satisfactory, for much good glass-work,
such as lamp chimneys, globes, laboratory -ware, etc. The green
or yellow colour due to iron may be corrected by the addition of
decolorizers (including oxidizing agents or oxygen camel's) such as
manganese dioxide, white arsenic (As a O a ), nickel oxide, selenium,
etc.
Glassy rocks, such as obsidian, tachylyte, etc., which are pro-
duced by the rapid cooling of igneous magmas, similarly owe their
dark green, black, or brown colour to the presence of compounds of
iron, alumina, Urne, etc. Similar "black" or dark green bottle-
glass may obviously be made from impure sands.
In consequence of the demand for a high silica-percentage, the
sands used are almost entirely composed of quartz-grains. The
presence of felspar-grains in a glass-sand is desirable for many
purposes, but, unfortunately, it generally means an increase in iron
and other constituents. The usual method, therefore, of obtaining
the required amount of alumina and alkalies is to add pure felspar,,
alumina, and salts of potassium and sodium to the batch. Sands low
in iron are for the greater part very free from other constituents
also, _ rarely containing, except as' traces, substances other than
alumina. To yield the proportion of alumina required for certain
glasses, a sand consisting of 40 per cent, to 60 per cent, of felspar-
would be required. Such sands, if they are to be free from iron
oxide and certain other substances, are very rare, and indeed could
only result from the denudation of such a rock as a very pure
quartz-porphyry or a pegmatite, with no admixture from any other-
source. In Chapter IV. (page 36) the Thuringian Forest sand,
bearing 3*66 percent, of alumina, was mentioned as being especially
suitable for the making of thermometer-glass.
Calcareous sands are of frequent occurrence, but are to be
avoided. The calcareous material is often sporadic in its distri-
bution. The Fontainebleau deposit is well known to geologists
for the beautiful steep rhombohedral crystals made up completely
o sand-grams, just cemented by calcite into the crystal shape.
The sand used for glass-work is selected free from this calcareous
material, but occasionally the supplies received in Britain contain
a few chalk-cemented balls. These are objected to when found,
but usually all the consignments are similar in their purity and
remarkably true to sample. Other impurities also tend to occur in
calcareous sands ; and lime itself is an undesirable constituent ia
sands used in the manufacture of certain kinds of glass
MINERAL AND MECHANICAL COMPOSITION. 43
2. Mineral Composition. The mineral composition is useful as
giving an indication of the relative amount of heavy detritaL
minerals present in the sand, and the quantity of quartz and
felspar in the lighter crops. Sands with large crops of heavy
minerals can only he used for rough bottle-glass. Indications of :
the presence in quantity of minerals other than quartz are, of
course, yielded by the chemical analysis. Mineral analysis is, how-
ever, a shorter and less tedious process, and like the spectroscopic
examination of sands, reveals the presence of small quantities of
the less common elements. Naturally -panned sands namely, those
in which the heavier minerals have been concentrated as a result of
oscillation produced by currents of wind or water must be avoided,,
even if, as in some cases, they are wlu'te and clean-looking. Iron
minerals frequently make up a considerable bulk of a heavy residue.
Sometimes, by the combined effects of wind-action and screening
by vegetation (as in some of the Irish dune- and beach-sands), a
kind of winnowing action takes place by which they may be purified
locally from heavy minerals. Most of the British sands of this
character are made up of mineral material derived from many
sources, and while yielding interesting mineral assemblages (in-
cluding micas in English, Scotch, and Irish samples, although
Retgers states that these minerals do not occur in Dutch dune-
sands) are, in spite of being washed free from some adherent
limonite and clay, of little use except for green bottle-glass work.
The presence or absence of certain minerals highly objectionable
in glass-making may quickly be noted by mineral analysis. Zircon
crystals ("ZrSiOJ, if present in quantity, are very undesirable on
account of their highly refractory character. They remain un-
digested in the " metal." Titanium minerals such as ilmenite
(FeTiOJ, rubile (TiO.,) and its isorners, anatase and brookite (which
are rarely abundant) are also detrimental to the making of good
glass. Titanium is always an objectionable constituent of the
" metal," and it so happens that ilmenite and rutile, like zircon,
are among the most commonly occurring detrital minerals.
3. Mechanical Composition (see page 21 for description of
apparatus, etc.). Elutriation is carried out on the assumption
that the sediment is composed entirely of quartz, or of minerals of
the same density. Most sediments contain so small a percentage
of heavier or lighter minerals, that the error introduced by them
is less than that due to experimental causes.
Mechanical analyses of glass-sands, including many from abroad
which are successfully used in the trade, indicate that the sand
should have at least 70 per cent., and, if possible, more than
90 per cent., of one grade, and that this grade should be in most
cases medium sand, i. e. with diameter between 0'25 and 0'5 mm.
(O'Ol to 0'02 inch). Although a " medium " sand in t"he geological
sense, it is a fine looking material to the eye. If the true " fine
sand" grade, O'l to 0'25 mm. diameter, forms the bulk of the deposit,
44 REQUIREMENTS OF A. GOOD GLASS-SAITD.
.so much the better, but such sands are not abundant in the British
Isles. A distribution of the bulk of the sand over these two grades
is also not very objectionable, although glass-makers naturally
prefer constancy of size. Grains over 1 ram. diameter in a sand
reduce its value considerably, and it is best that none should have
.a diameter greater than O5 mm. diameter. If the extra expense is
not prohibitive, a pure and fairly well-graded sand may be sifted by
screens to rid it of grains over 0'5 mm. diameter. Of the few sands
used in glass-making, containing the coarse grade, we may mention
ihat from Leighton Buzzard in Bedfordshire (Lower Greensand).
The sand as supplied has been washed, and contains 24'6 per cent
by weight of diameter between 0-5 and 1 mm., and 74 - 3 per cent, of
diameter 0-25 to O5 mm. The latter grade is suitable and its per-
centage is fairly high, but it would be desirable if the other 25 per
cent, were of the next smaller, and not the next larger, grade,
.as in the case of Fontainebleau sand, where the portion >O5inm..
diameter = O'l per cent, or less, >0'25 and <0 - 5 mm. = 7OG per
cent., and >0'1 and <0'25 mm. = 26'6 per cent.
If the " batch " is ground fine before being melted the question
of grade-size in the sand is obviously not of such moment, and
high percentage of silica and low percentage of iron are the
desiderata. Leighton sand was used in this way by one firm making
chemical glass-ware, but it is doubtful whether much advantage
accrues from the grinding except in the case of the best glass-
ware. The extra expense is considerable.
As the Tables indicate, there are many British sands of which
the mechanical analyses are similar to that of Fontainebleau
sand. The regularity of grade of blown -sands in various other
parts of the world has previously been commented upon, and the
same holds true for British dune- and shore-sands. Altbmigh
the evenness of these sands, due to selective transportation and
deposition of material, renders them very suitable for glass-making,
the colour, as previously remarked, shows the presence of too much
iron and heavy mineral residues for the sands to be used for other
than common bottle-glass. Dutch and Belgian sands imported into
this country vary considerably in character. They are uniformly
high in silica (some varieties containing pink quartz) and are
used for other purposes, as well as glass-making, on account of
their refractory properties. The colour and iron-content vary
somewhat, but the grade-analysis, although variable, usually shows
a high percentage (over 90) of the medium-sand grade. These
are good all-round sands, and the nearest .English equivalent in
mechanical composition is the Lower Greensand obtained from
near King's Lynn, in West Norfolk (Sandringharn Sands). Many
qualities of this sand are supplied, and the best has a colour and
low iron-content equal to those of the best Belgian sand, as well as
a high percentage (95 per cent.) of the desirable grade. Further
notes upon the various qualities will be found under the remarks
upon this source of supply.
British sands with a high percentage of the grade of "fine sand"
MECHANICAL COMPOSITION 1 . 45-
include those of the uppermost Thanet Beds from the well-known
Chaiiton pit in Kent, and the Kelloway Beds of Burythorpe, near
Malton, Yorkshire. The fineness of their dominant grade and its.
high percentage (nearly 70 per cent. diam. > O'l and < O25 mm.)
are advantageous.
In the Tables the cumulative percentage of all the sand-grader
( > - 1 and < 1 mm. diameter) is given in a separate column (S)>
This should approximate to 100 per cent, for glass-sands, and
rarely be less than 95 per cent. The grade of diameter > O'Ol mm.
and < O'l is best termed the silt-grade, but actually the coarser- .
material of this grade is a superfine sand. It is theref ore sometimes
desirable to estimate it in two portions : (a) superfine sand of diameter
>0'05 mm., (Z) silt of diameter <0'05 mm. Certain deposits,,
for example, are certainly sands, but contain a high percentage-
of the grade >0'01 and <0'1 mm., the grains composing which
are mostly above 0*05 mm. diameter. Such are the sands of the
Inferior Oolite from Bridport, Midford, Yeovil, the Cotteswolds,
etc., which show a remarkable uniformity of grade over a large
area.
These Inferior Oolite Sands are unfortunately yellow in colour,,
contain much iron oxide, and heavy crops of dense minerals. They
are occasionally calcareous, but clear rapidly to fine white micaceous
sands on warming with dilute acid. Their use for glass purposes
is therefore at present ruled out. Sands of this extremely fine
grade are rare in the British Isles.
Sands to be xisecl for glass-making should not contain much of
the silt-grade. The clay-grade, of diameter < O'Ol mm., certainly
should be absent. The percentages shown in the tables were
estimated by difference (see page 23). The figures in this column,
therefore, include hygroscopic water (some of the samples were
air-dried at first, and all the grades were dried at 100 C. before
weighing), dust accumulated by exposure and during transit of the
sand, the limonitic coating on grains in some cases, and films of
soluble or other salts (e. g. sea-salts in the dune- and shore-sands)..
Probably this grade is practically absent in most cases where it is
recorded as less than 0'5 per cent.
Such sands as those of Triassic age from Wbrksop in Nottingham-
shire, and Spital in Cheshire, actually contain clayey and silty
material (including kaolin). Some of the clayey and dusty matter
coats the grains of quartz and felspar. The Tables indicate that,
although they are fairly clean sands, they are not sufficiently
well-graded to be suitable for the making of other than common
glass.
Mechanical analyses of American and Danish glass-sands are-
appended for comparison (see pages 168, 169, 170).
The use of pot- or tank-furnaces has an important bearing on the-
grade of the sand used for the batch. When a poorly-graded sand,
containing much fine powdery silica, is used in the batch for a
tank-furnace, considerable loss due to "blowing-out" results. The
other constituents such as compounds of the alkalies, which may
46 BEQTJIBBMBNTS OF A GOOD GLASS-SAND.
be in the form of fine powder, melt more rapidly, and so are not
lost*. A con siderably higher temperature must be attained before
silica fuses ; fine material is therefore earned away by the blast of
gas and air before it melts. Not only does a real loss in bulk
thus occur, but the resulting composition of the batch is changed.
When melting takes place in pots, this loss by blowing-out is
obviated. Silica in a fine state of division in a sand is also open to
objection on other grounds. Air-bubbles entangled in the fine
material are introduced into the "metal" from whicli they are re-
moved only with great difficulty. The fine particles melt before the
coarser ones, and the resulting metal sinks to the bottom. The
density of the molten material thus formed is not constant, and
varies as the pot is depleted of its contents. If coarse grains are
present, the batch takes longer to melt, or these remain as undigested
or partly digested lumps in the glass (" seeds '" or " stones "). The
results, therefore, of using non-graded sands are unsatisfactory.
'The value of such a sand as that of Fontainebleau lies in the way
in which the whole of the batch containing it passes smoothly into
the molten condition at almost the same moment. Angularity or
subangularity of the grains may contribute to rapid melting.
No arrangements for stirring the metal exist in most furnaces.
The result of using imperfectly-graded sands is therefore the pro-
duction of "metal" of unequal composition, texture, and density,
with consequent trouble in working. Clayey materials also tend to
cloud the glass, and kaolin itself is highly refractory and formerly
rendered unsuitable a sand containing it.
The statement in an American publication (U. S. G-. S. Bull.
286, p. 454) that sand of diameter less than -fa inch bums out
in the batch, giving less glass, is not borne out by British and
Continental practice, where so much of the sand used is of diameter
less than -^ inch. Sand of 20 to 50-mesh, advocated by American
writers, appears to be coarser than British glass-manufacturers
prefer to use.
4. Angularity of Glass-Sands. The grains composing the
sands in general use for glass -making in Britain are either angular
-or subangular in character. Sands containing rounded grains are
not popular with some glass-manufacturers indeed, angularity is
preferred in England. The most obvious explanation of the pre-
ference for angularity seems to be that the grains fuse more rapidly,
the process beginning at the corners and edges, the surface-area
being greater, volume for volume, than that of rounded grains.
.Some 01 the Belgian sands are highly angular, having a sharp feel.
Rapid melting is desirable and saves much time and trouble ; thus
both furnaces and sands are called upon to contribute towards this
end.
* In many works it is found that n-IWH dust and not silica is carried over
into the flues and chokes them. Careful filling of the batch does much to
prevent the loss of fine material, but rapidity of filling is essential. Damping
-the batch has also been recommended.
VARIATION ACCORDING TO GLASS PRODUCED. 47
Sands composed of rounded grains appear to be successfully used
for glass-making in America (see Plate V. fig. 2) *.
In certain works where table- ware and bottles made of flint-
glass have names and marks etched upon them, by sand-blast action,
the sand used in the blast as the abrasive is the same Fontainebleau,
Belgian, Aylesbury, or Lynn sand as that utilized in making the
glass. Besides its marked angularity (so that its cutting power may
be as great as possible), a sand for etching should be hard and
tough. For common purposes a highly siliceous, i. e. quartzose,
sand is suitable. It must' be perfectly dry and of even grade (not too
coarse), in order that it may pass freely through the funnels, etc.,
and not clog the jets and stencil upon the sudden release of
pressure. If water-vapour is present the adiabatic expansion and
fall of temperature results in its condensation, and clogging takes
place. Some sands used for grinding plate-glass are worked at
Leighton Buzzard ; others have been dredged from the bed of the
River Mersey.
Variation according to the Icinds of G-lass produced.
For the commonest glass (bottle- ware, etc.) the mechanical
analysis is of prime importance. The sand must be well-graded
and composed of suitably-sized grains. Greater latitude in chemical
composition is permissible than with better-class glasses. The
silica-percentage should still be fairly high, but low iron-content is
not so essential: it may vaiy up to 1 per cent, (as Fe 2 OJ. The
presence of small quantities of titanium, aluminium, calcium, and
alkalies is but slightly harmful.
For ah" medium-class glass-ware, including the best bottles,
chemical ware, globes, chimneys, pressed-ware, etc., both chemical
and mechanical analyses are of great importance. High silica-
content (and for much laboratory-ware, etc., high alumina) and
low iron-content are demanded. Other constituents, if present at
all, should be in minimum quantity. Good grading is extremely
desirable, and the size of grain should not fall outside the limits of
0*5 and O'l mm. diameter.
For high-class glass-ware such as optical glass, table-glass (which
is afterwards "cut"), and other special glasses, the chemical
composition is of prime importance, and the mechanical analysis
often, but not always, takes a secondary rank. In the famous
cut-glass table-ware industry of the Stourbridge district, the batch
is not at the present time ground fine, neither do arrangements
exist for stirring the metal ; in consequence the grade, as well as
the chemical composition, must be of a high standard. For the
other ware mentioned, a high percentage of silica (and at times,
alumina) is demanded, and little or no iron should be present.
As the batch is sometimes pulverized and as stirring is occasionally
adopted, the " metal " being allowed to remain molten for a long
* United States Geological Survey, Bull. 285, 1906, page 454. See also
Mineral EesonroeB, ' Sand and Gravel' for 1915 and earlier years.
48 BEQTJIBEMENTS OF A GOOD GLA.SS-SA1TD.
period, crashed rocks and quartz, as well as poorly-graded sands,
might be utilized.
Summary : The Ideal Glass-Sand.
A perfect " sand " in the geological sense, that is one composed
entirely of grains belonging to one grade, which should not be a
coarse one, yields the best material for glass-making, provided that
the chemical composition is suitable. . As a general rule, for all
kinds of glass-work the iron oxide (Fe a O n ) percentage should be
low, always under 1 per cent., the higher limit being permissible
only for glass for the cheapest class of bottles. As already stated,
the sand used for the best varieties of glass, such as optical glass,
best flint- and sheet-glass, best Bohemian glass, " crystal " table-
ware, etc., should contain at the most only a few hundredths
('02 to '08) per cent, of iron oxide. Alumina, magnesia, and
lime may be'present in sands in the form of felspars, ferromaguesian
and lime-bearing minerals, and calcareous cement, but are required
only for certain glasses. These bases are very refractoiy and
lengthen the time taken for melting. Sands free from them are
preferable, both because the bases are required only for refractory
glasses, and then must be added in larger quantities, and because
the presence of minerals containing them in sand usually means
also the presence of a prohibitive quantity of iron. The specific
properties of optical glass are altered by the presence of such
impurities in the sand.
It is found desirable, therefore, to rely upon the sand only as a
source of pure silica, and to add other bases for the purpose of
making the various kinds of gkss desired.
The ideal sand for the best glass-making is one with 100 per
cent, silica and composed of angular grains all of the same size, and
of the grade known as medium or fine sand. Such a perfect sand
has not at present been discovered, but the ideal is approached by
a few sands, including those of Fontainebleau in France (99 - 7
per cent, silica), Lippe in Germany (99-8 per cent, silica), and
Berkeley Springs in the U.S.A. (99-65 per cent, silica). Sands
from Lippe and Berkeley Springs are described in Chapter XT.
BBITISH SANDS SUITABLE FOB GLASS-MAKING. -19
CHAPTEK VI.
BEITISH SANDS SUITABLE FOB G-LASS-MAKIN&.
The Tables of chemical and mechanical analyses on pages 154 to
170 give an indication, in the light of what has heen said before, as
to how far British sands may be used to replace those imported from
abroad. In the first place, there does not appear to exist, anywhere
in the British Isles, a sand so suitable, from all points of view, for
the making of the best kinds of glass, as those from Lippe and
Fontainebleau. The best sands from Aylesbury in Buckinghamshire
and from Fail-light in Sussex are equal to Fontainebleau sand, and the
sands from Huttons Ambo and Burythorpe in Yorkshire, and other
places, are certainly as good as much of the Belgian sand imported.
Lynn sand, at its best, is also equal to much of the Belgian
material, and is superior to some of the Dutch sand. The same-
remarks apply to Grodstone and Reigate sands (Lower Greensand,
Surrey), but the deposits are irregular. A large number of British
sands, especially dune- and shore-sands, are less pure, but are well
suited to the making of common bottle-glass. Mechanical analyses
of some representative examples of these are given in the Tables,
on page 165.
The writer is unable to agree with Dr. W. Kosenhain, who, in
the Cantor Lectures before the lioyal Society of Arts in 1915,
said : " In this respect [_i. e., suitability of sands] glass-makers in
England are unfavourably situated, since there are at present no
very suitable sands available in this country. Whether exhaustive
search might lead to the discovery of a suitable deposit is doubtful,
because a large number of firms have already sought for good
glass-making sands, and find it difficult to supply even the require-
ments for ordinary window (sheet) glass." Necessity, exploration,,
and experience under war-conditions has resulted in the use of
large quantities of British sands for all kinds of glass of better
quality than window-glass. The statement is also an exagge-
ration of the difficulties which existed before 1914.
Analyses and notes upon some important foreign glass-sands are-
given in Chapter XI. for purposes of comparison. A few mechanical
analyses are graphically expressed in the curves of Figs. 10 and 11
(page 50).
No attempt has been made in the following pages to treat
exhaustively British resources of common sands suitable for dark
bottle-making. Such supplies are abundant and ubiquitous, and
can be found at no great distance from the works.
The descriptions are given under the heads : A. Purely siliceous-
50
BRITISH SANDS SUITABLE FOR Q'LA.SB-'MA.TS.TSQ.
Fig. 10. Mechanical Analyses of Glass- Sands : Foreign.
90 .
BO .
I
T 70 4
jBO -
I 50-
a
I 40
JO
| 30
u
t 20
10
./ /./ //"
^p / u ;/
*/ ^//
fe/ /A'
i-o
0-5 0-25
Grade Sizes (diameter in Millimetres}
Fig. 1.1 . Mechanical Analyses of Glass-Sands : British.
90 .
80.
-5,70.
1
60.
I 50.
..I 40 .
1
| 30 .
o
f
1 20 .
10
fil
'
T
1-0
0-5 0-25
Grade Sizes (diameter in Millimetre*)
0-1
AYLESBTTBY SAND. 51
materials, including () sands, (J) crushed rocks; B. Siliceous
deposits caiiying () alumina, and (b~) alumina and potash
A. PUBELY SILICEOUS DEPOSITS
() SANDS.
" Aylesbury " Sand.
Worked by The Aylesbury Sand Company. Manager, Mr. J.
Arnold (Offices, 32 St. Paul's Eoad, Oamden Town, N.W. 1).
Maps. Geological : Old Series, 1-inch, Sheet 46 S.W.
6-inch, Buckinghamshire, Sheet 32 N. W.
Situation. Lot. 51 48' 22", Long. 52' 5" W.
The quarries occur at Stone, three miles west of Aylesbury.
The sand is also exposed in the " Windmill " pit, but is not worked
there to any extent.
Formation . Lower Greensand.
Description. White seams of pure sand, suitable for flint-glass
work, extend to a depth of about eighteen feet. Working is then
stopped by water. Peaty and ferruginous bands occur, and since
the seams of white sand are not very thick (four to six feet) or
persistent, working is rather difficult. It is not easy to ensure that
successive consignments conform to the highest standard of purity
met with, and variability is abhorred by glass-makers. The
whiteness and purity may be connected with the peaty bands.
The colour is good, the best Aylesbury sand being better than
Belgian, and selected samples being equal to Foutainebleau sand.
Washing does not improve the colour of the best sand to any
extent, but a second-quality sand, washed free from limonitic and
clayey pellets (in rotary washing-plant), is also supplied. The
latter sand is pale grey, but reddens slightly on burning, whereas the
former shows little or no change. The chemical composition is as
follows :
Best Washed sand Bulk
Band. as delivered, sample.
SiO 99-80 99-39 98-76 per cent.
AlA 0-32 0-48 0-37
Fe 2 3 0-03 0-02 0-03
CaO' n.d. n.d. 0-17
MgO n.d. n.d. 0-10
Na.,0 n. d. n. d. none
K.6 n.d. n.d. 0-04
Loss on ignition 0'22 0-18 0"33
Totals 100-37 100-02 99-80 per cent.
The evenness of grade is a marked feature, the sand in this
respect very closely resembling Fontainebleau (see Plate III.
figs. 1 & 3). The mechanical composition is as follows :
Sections marked thus deal with sands and rooks which are also of use
refractory materials.
E2
62 BRITISH SANDS SUITABLE FOR GLASS-MAKING.
>0'5 mm., few grains only; >0'25 & <0'5, 78-3 % ; >01 & <0'25, 15'0 % -
>0'01 & <0-1, 6-8 % ; <0-01, 0-9 %. Total sand-grade, >0'1 mm.,
93-3 %.
PCS MS JFS _s_ _o S_ ~j
Ltr.' 78-3' 15-0' 5'8' 0-9 ; 93-3' J
The detritnl mineral suite is very characteristic of the Lower
Greensand throughout England. Heavy minerals are fairly
abundant (0'2 to 0-3 mm. diameter), and the residue consists
almost entirely of coarse, angular kyanite, staurolite, and brown
and blue tourmaline, together with iron ores (magnetite, limonite,
and altered ilmenite), zircon, rutile, etc.
The sands, after being carted to Hartwell Siding near Aylesbury
Station (GK C. Railway), were put on trucks, before the war, at
7s. Qd. per ton. At the time of writing the price is 10s. This is
rather high, and freight charges increase it to about 15s. or 17s. Qd.
by the time it reaches a glass-making district as far distant as
London or Yorkshire.
The estimated quantity available in the area is two million
tons *.
Sands from Fairlight and Hastings.
(1) FAIKLIQHT.
Worked occasionally for sand, Milward Estate (Agent : Mr. G.
E. Barr, 23 Havelock Rd., Hastings).
3fapts. Geological : Old Series, 1-inch, Sheet 5.
6-inch, Sussex, Sheet 58 S.E.
Situation, Lett. 50 52' 30", Long. 38' 36" E.
The pit is situated by the roadside, close to, and immediately to
the south of, Fail-light Church, east of Hastings.
Formation. Ashdown Sands (Wealden).
Description. The bed of snow-white sand occurs at the base of
the Ashdown Sands and immediately above the Fail-light Clays,
of which a splendid succession is exposed in the cliffs below the
Church. G-lass-sands were recorded as having been worked at
Hastings long ago f ; they were doubtless sands like those exposed
in this pit, and in that at Bulverhyth described below. The
association of lignites with the Ashdown and Tunbridge Wells
Sands has been recorded by Topley J and others, and the reducing
action of the vegetable matter probably accounts for the freedom
from ferruginous compounds. Fairlight Church stands towards
the eastern end of a strong sandstone ridge overlooking Hastings.
For two or three miles this ridge has, as its backbone, the white
Ashdown Sands which are mentioned above. In an old quarry
* In eaoli case the estimate of the resources IB by the writer, and is to be
taken as well -within the upper limit.
f Mineral Statistics : Memoir Geol. Survey, 1860, p. 375.
t W. Topley, " The Geology of the Weald," Mem. Geol. Surrey, 1875,
page 395 ; Ashdown Sands, pages 59, 80 ; Tunbridge Wells Sands, pages 78,
85, etc.
FAIRLTQHT AND lIASi'INGS SANDS. 53
about a quarter of a mile west of the Church, a wall of about
twelve feet of white sandstone, not bottomed, is shown over about
a hundred yards of quarry face. Water stands in the quarry.
The deposit is well jointed and bedded and easily workable. Only
three to six feet of valueless overburden occur above the white sands
in the Church pit. The beds jdeld a firm solid face, many of the
joints being superficially dirt-stained. A sample, which is almost
as pure in colour as Fontainebleau sand, burned up slightly pink.
Its chemical composition is as follows :
SiO., 99-47 per cent.
Al,0. t 0-24
Fe~O 3 0-002
CaO 0-29
MgO trace
Loss on ignition 0-20
Total 100-202 per cent.
The high percentage of silica and low percentage of iron are
noteworthy. This sample was not intentionally selected, but
happened to be very low in iron. Another sample from the same
bed contained 0'016 per cent, of iron oxide.
The mechanical analysis shows :
>0-5 mm., none; >0'25 & <0'5, 83'7 % ; >0'1 & <0'25, 16- 1 % ; >0'01 &
<0-1, 0-1 % ; <0-01, 0-1 %. Total sand-gi-ade, >0-1 mm., 99'8 %.
cf incj ,-. A cj
H J? (3 S C B
SS 7 ?' 16 7 !' (FT* (KP OJRT.
Washing would doubtless improve the deposit both chemically
and mechanically.
The mineral composition indicates the presence of a few stable
heavy detrital minerals in very small quantity, the proportion of
density greater than 2 - 8 being only O'Ol per cent. The heavy
residue is rather fine in grain, and the assemblage of minerals
uninteresting. All the readily decomposable compounds have been
eliminated before or since deposition. A little magnetite occurs,
and limonite in small quantity is seen, llmenite is abundant
(0'2 mm. diameter), but practically always altered to leucoxene.
Brown tourmaline (0'15 mm.) is plentiful, and zircon (0-1 mm.),
reddish rutile (O'l mm.), and muscovite (flakes 0*2 mm. diameter)
occur.
The most serious consideration is that of transport. A good
road links the pit to Hastings, the Station (L. B. & S. C. and
S. E. & C. Railways) and quay being four miles distant. The road
is, however, downhill all the way, and motor-traction should be
economically possible. The sand might then be shipped at
Hastings. An alternative suggestion is that of taking the sand
eastwards down to Cliff-End, near Winchelsea, and shipping it
i'rom there. The nearest station to Fairlight is actually Ore
(three miles), but it is badly situated in a hollow with a steep
64 BUIXISH SANDS SUITABLE FOE GLASS-WAKING.
gradient from ,the pit. The proximity of the London market and
the possibility of water-transport to an even greater distance are-
noteworthy.
The available resources are over fifteen million tons.
(2) BULTEEIIYTH, WEST Off HASTINGS.
Worked occasionally for sand, Filsham Estate (Agent : Mr. T.
W. Ellworthy, 81 London Ed., St. Leonards).
JUiaps. Geological: Old Series, 1-inch, Sheet 5.
6-inch, Sussex, Sheet 71 N.W.
Situation. Lot. 50 51' 0", Long. 32' 18" E.
The pit lies by the side of and north of the main road from
St. Leonards to Bexhill. It is situated half a mile west-south-
west of St. Leonards (West Marina) Station (L. B. & S. C.
Bailway).
Formation. Ashdown Sands (Wealden).
Description. The great thickness of overburden (about 3D feet),
consisting of brown sands, silts, and clays, renders doubtful the
profitable working of the few feet of white sands at the base. The
strata dip to the north into the rising ground, so that shallow
excavations farther northward are unlikely to reach the bed.
The ground falls towards the west, and, on the opposite side of the
small lane which runs northward by the western end of the pit, the
glass-sands crop out at the surface. Although they do not appear
to be so pure here, improvement might be seen as they are worked
inwards. The white sand is similar in chemical and mechanical
composition to that at Eairlight described above. The iron-content
is 0'04 per cent., and the grade-analysis is as follows :
>0-5 & <1 mm., 0-8 % ; >0'25 & <0-5, 77'9 % ; >0'1 & <0'25, 20-3 % ;
>0-01 & <0-1, 0-5 % ; <0-01, 0'5 %. Total sand-grade, >(KL mm.,
99-0%.
res MS jrs _a_ _. s ~i
L.O-8' 77-9' 20-3' 0-5' OV 99-0'J
The mineral composition is also similar to that of the sand from
Fairlight, but the heavy crop is distinctly coarser in grain. The
most common rninerals, in order of abundance, are ilmenite, altering
to leucoxene, grey-brown tourmaline (O'l mm. diameter), foxy-red
and, less commonly, yellow rutile (O'l to 0-25 mm.), zircon in
pinkish, purple, brown, and zoned crystals (O'l to 0'25 mm.), and
uruscovite flakes, the average diameter of Avhich is about twee that
of the other grams.
The pit is favourably situated for transport, being at the side of
a main road, and only a quarter of a mile from West St. Leonards
Station (S. E. & C. .Railway). Small quantities of the white sand
have been carted to the station for despatch.
The available resources are under a million tons.
ASHTTRSTWOOD SAMT>. 55
Sand from Ashurstwood, near East Q-rinstead.
Not at present being worked.
Owner. Mr. A. H. Hastie, 66 Lincoln's Inn Fields, W.C. 2.
Maps. Q-eological : Old Series, 1-inch, Sheet 6.
(3-inch, Sussex, Sheet 5 S.W.
Situation. Lat. 61 6' 60", Long. 1' 15" W.
Large excavations at Ashurstwood, particularly in Cherry Garden,
north and north-west of the Church, south-east of East Grinstead,
yield evidence of extensive early working.
formation. Tunbridge Wells Sands (Wealden).
Description. The sand stands up in firm faces and blocks,
sufficiently so to be described as a soft sandstone. The combined
effect of weathering and excavation is to yield picturesque " rocks,"
the creamy-colour of the sand being subdued upon, the weathered
surfaces. A considerable thickness is indicated. Some of the
seams are ferruginous, and washing would doubtless improve
the whole deposit.
Samples of the sand, creamy- white in colour, turn browner on
burning. The chemical composition is as follows :
Si0 2 98-77 per oent.
Al,0 3 0-73
Fe 2 3 0-01
CaO 0-14
MgO trace
Loss on ignition 0'43
Total 100-08 per oent.
The sand is small in grain, and the mechanical analysis
indicates :
>0-5 mm., a few grains only; >0-25 & <0'5, 9-8 % ; >0'1 & < 0-25, 85'5 % - f
>0'01 & <0-1, 2-0 % ; <0-01, 2-7 %. Total sand-grade, >0'1 mm.,
95-3 %.
[-OS MS JTS _s_ o . S "I
|_tr. J 9-8' 85-5' 2-0 1 2-7' 95-3' J
The heavy residue is abundant and fine-grained, amounting to-
O24 per cent. It consists largely of zircon, yellow and foxy-red
rutile, ilmenite, and tourmaline of about 0'05 mm. diameter.
Although the crop is abundant, the mineral assemblage is not
very interesting. Muscovite (flakes O f 5 to 0'6 mm. diam.),
glauconite, and yellow anatase also occur.
The pits are situated about two miles from East Grinstead
Station and a mile and a half from Forest Row (L. B. & S. C.
Railway). There is a good road connecting them. Road- traction
to London, about thirty miles distant, might also be possible.
The available resources are over fifteen million tons.
56 BEITISH SANDS SUITABLE FOB GLASS -MAKING-.
"Lynn." Sand.
(1) Worked by Messrs. Joseph Boam, Ltd. (Offices, Silver
Street, Leicester). (See Plate VI., and also Plate IV. fig. 6.)
Maps. Geological : Old Series, 1-inch, Sheet 66.
6-inch, Norfolk, Sheet 33 S.E.
Situation. Lat. 52 44' to 52 45', Long. 28' to 29' E.
The sand is worked over an extensive area at Middleton and
G-ayton, three miles east of King's Lynn, and numerous scattered
quarries occur.
formation. Sandringharn Sands (Lower Greensand).
Description. The deposit is fairly persistent and thick, so that
large supplies of sand running true to sample can he supplied.
Little variation occurs in successive consignments. The sand is
won for foundry- work, glass-making, building-purposes, etc. The
red sands are used for the last-named purpose and also for the
making of black-bottle glass. In considering the sands suitable for
general glass-making, it is to be noted that the colour of the best
Lynn sand is equal to that of the Belgian, but most of the sand is
rather darker, three qualities, besides a washed and a double-washed
sand being supplied. Rotary washing-plant is employed. The
washed sand has a pale grey to brown colour. The iron-content is
rather higher than that of Aylesbury sand, and on burning there
is a marked change to redder or greyer tints. The chemical
composition of the best sand is as follows :
SiO, 99'23 per cent.
AlA -50
Fe,0' -04
CaO' -11
MgO -02
Loss on ignition . , . '25
Total 100-24 per cent.
Note. A duplicate determination of the silica and also of the alumina
carried out as a control gave the figures 99'20 % and 0'56 % , respectively.
In mechanical composition the sand is seen to be well-graded,
but rather coarser than either Aylesbury or Fontainebleau sand.
The curve representing its composition in Fig. 11, page 50, is there-
fore sympathetic with, but to the left of, those for Aylesbury, etc.,
sands. Typical analyses yield the following results :
>0'5 & < 1 mm., none ; > 0'25 & < 0'5, 94'8 % ; > 0-1 & < 0'25, 4'9 % ;
> 0-01 &<0'1, 0-2 %; <0-01, O'l %. Total sand-grade, >0'l&<lmm.,
99-7 %.
["MS FS _s_ o _S I
|_94-8' 4-9' 0-2' 6 V 1 ; 99'7'J
From the point of view of glass-making, the remarkably good
grading of the sand calls for special note. Although not so low
in iron -content as some other British sands, it is certainly the
LYNN SAND. 57
most even in grain, and for that reason has heen preferred hy
certain glass-manufacturers on account of its rapid melting.
These remarks apply particularly to the sand from the pits near
Middleton Station (G. E. Railway). This sand is washed to remove
clayey and ferruginous matter, and, a new washing-apparatus
(Rikof's pattern) has recently heen installed (see page 122 and
Plate VII.).
The sands "become less pure and more felspathic in the area near
Gayton Road Station (Midland & Q-. N. Joint Railway). They
are worked to a large extent for pale bottle-making, and are also
of considerahle use for furnace-hearths. A chemical analysis of a
sample of one of these sands is as follows :
SiO a 97-34 per cent.
11.03 1-34
Ti<X trace-
Pe 2 a 0-19
CaO 0-09
MgO trace
K.,0 0-37
Na.jO trace
Loss on ignition 0'76
Total 100-09 per cent.
The mechanical analysis of the same sample indicates :
>0-5 & <1 mm., 0-5 % ; >0'25 & <0'5, 95'1 % ; >0'1 & <0'25, 2-7 % ;
>0-01 & <0-1, 0-8 %; <0-01, 0-9 %. Total sand-grade, >0'1 mm.,
98-3 % .
PCS MS FS _s_ o S "1
LO-5' 95-1' 2-7' 0-8' 0-9 ' 98'3'j
Greenish seams of glauconitic material are not uncommon, hut
as the glauconite (silicate of iron, aluminium and potash) is usually
present as a coating to the grains of quartz, washing improves the
sand considerably.
The mineral composition indicates rather more felspar than in
the other Greensand deposits discussed (note A1 2 3 percentage in
chemical .analyses). The heavy detrital mineral assemblage is
similar to that of the Lower Greensand generally, but, in addition,
occasional garnets are found.
The residue is a coarse one, the grains averaging 0'2 mm.
diameter. The sand is extensively used for general glass-work,
including window- and plate-glass, laboratory-ware, incandescent-
lamp globes, chimneys, white and coloured bottles, etc. It has the
great advantage of being cheap.
The prices of the sands put upon the market are as follows :
Brown Sand 3s. Qd. per ton, Unwashed White Sand 3s. 9d. per ton,
Washed Sand 5s. Qd. per ton, Double-washed Sand 6s. per ton,
Specially Selected and Double-washed Sand 8s. per ton, F.O.R. at
Middleton Station (G. E. Railway) or Gayton. Road Station (Mid-
land & G.N. Joint Railway).
T>8 BEITISH BANDS SUITABLE FOE
The washed sand is from the Middleton area, and the unwashed
from near Gayton Eoad Station, but further washing is being
contemplated.
(2) Worked by Messrs. Gay & Wilson (Managing Partner,
Mr. G. W. Smart). ,
Maps. Geological : Old Series, 1-inch, Sheet 65.
6-inch Norfolk, Sheet 33 N.E.
Situation. Lat. 52 46' 0", Long. 29' 0" E.
Formation. Sandringham Sands (Lower Greensand).
Description. The quarries occur immediately north-west of
Bawsey Signal Box, about a mile north-east of Gayton Eoad Station
(M. &G. N. Joint Eailway). The description given above applies
equally well to these deposits, except that the sand is on the whole
rather finer in grain and contains more iron (O16 per cent.). The
results of mechanical analysis are given in the Tables on page 163.
The pits reveal a thirty-foot wall of sand (at times approaching
forty feet where excavations have been made in the floor of the
pits), in places rather regular in quality, capped by Glacial Drift,
which occasionally forms pockets.
The sand is used to a considerable extent in the Yorkshire district
for bottle-making, and also in the manufacture of soap. It is put
on truck at Bawsey siding, Gayton Koad Station, at from 2s. 2d*
to 3s. per ton, a better quality also being selected when desired
and supplied at a correspondingly higher price.
The available resources in the Lynn area are at least three-
hundred million tons.
"Leighton Buzzard" Sand.
Worked by (1) Mr. Joseph Arnold, (2) Mr. George Garside,
(3) Mr.. Gregory Harris.
Maps. Geological : Old Series, 1-inch, Sheet 46 N.W.
6-inch, Bedfordshire, Sheet 28 N.E.
Situation. Lat. 51 56' 15" to 51 57' 10", Lona. 38' 20' '
to 39' 10" W. J
The sand is worked over a large area north and north-east
or Leighton Buzzard. Numerous quarries and old workings occur
(Mile Tree, Shenley Hill, Stone Lane, Chance's Quarry, etc.).
Formation. Lower Greensand.
Description. The deposits are worked for a variety of pur-
poses, glass-making being subordinate.
Both chemical and mechanical compositions vary considerably.
The coarse sands are supplied for water-filtration plant, connrete-
making, grinding, etc. The highly ferruginous sand is used for
building, and most of the pale-coloured medium-grained sands are
worked and washed by a rotary method for foundry purposes, parti-
cularly in connexion with steel-casting. This is on account of the-
LEIGHTON BUZZARD SAND. 59
high silica-percentage, there being very little felspar. For the
greater part the sands are neither so pure and free from iron nor of
so fine a grade as those of Aylesbury ; they are therefore not so well
suited for good glass. They are used for the making of pressed
gkss and laboratory-ware. The iron-staining is patchy in its
occurrence, and the pale sands are thus impersistent. The whitish
sands are again associated with peaty bands.
The chemical composition of some of the samples of glass-sands
is as follows :
(1) (2) (3) (4)
SiO 99-05 99-59 96-77 99-58 per cent.
A1 2 6 3 0-23 0-25 1-77 0-27
Fe a 3 0-14 0-21 0-27 0-03
CaO 0-31 n.d. 0'15 0'22
MgO 0-08 n.d. 0-03 none
KjO none none 0-60 none
Na a O none none 0'02 none
Loss on ignition ... 0-81 0-27 0-63 0-13 '
Totals 100-12 100-32 100-24 100-23 per cent.
(1) Arnold's pita, washed.
(2) unwashed.
(3j a fine grade.
(4) Garaide's pit.
For the most part, the sands are coarse, passing into line quartzose
and cherty gravels. The latter are screened and used for abrasive
purposes, including the grinding of plate-glass. Seams of fine
white and grey sand occur, but are not common.
The whitish and pale yellow sands supplied for glass-making are
rather coarser than manufacturers like. A typical mechanical
analysis is as follows :
> 0-5 & <1 mm., 24-6 % ; >0'25 & <0'5, 74'3 % ; >0'l & <0'25, 1-0 % ;
>0-01 &, < 0-1, less than 0-1 %. Total sand-grade, >0'1& <lmm.,99-9 %.
r_CS_ MB FS _s_ S ~|
|_24-6' 74-3' 1-0' 0-1 ; 99 '9' J
The mineral composition is like that of Lower Greensand deposits
generally. The description of the mineral assemblage of Aylesbury
sand applies here.
The sand is put on boat upon the Grand Junction Canal, or on
truck at Leighton Buzzard, at 6s. per ton (Arnold), and 6s. QcL
per ton (Grarside).
The available resources are at least five hundred million tons.
The Lower Greensand of Plitwick (pit one-third mile north of
the railway station, worked by Mr. Joseph Arnold) is similar, but
less pure. Analyses of this sand are given in the Tables on pages;
156 and 163.
<30 BEITISH SANDS SUITABLE TOE GLASS-MAKING.
Sand from Q-odstone, Surrey.
Worked by Messrs. Goodwyn & Sons, Granville Chambers,
Portman Square, London, W. 1 (owner Sir W. R. Clayton, Bart.).
Maps. Geological : Old Series, 1-inch, Sheet 6.
6-inch, Surrey, Sheet 27 S.E.
Situation.Lat. 51 15' 0", Long. 4' 0" W.
The pit revealing the whitest sand occurs half a mile north-
west of Godstone Church.
Formation. Folkestone Beds (Lower Greensand).
Description. The whitest and best glass-sands occur as irregular
patches in beds more iron- stained. No great supply of standard
material can therefore be guaranteed, an unfortunate fact in view
of its proximity to London and the Thames area. The pit is also
some distance from a railway station. Sand has been sold for glass-
making, but never in quantities of more than 90 tons a week, an
amount hopelessly too small. The bulk of the deposit, consisting
mainly. of the upper beds, is worked for building-purposes, and
some probably reaches London and is sold as silver-sand for soil-
dressing and scouring purposes. The lower beds were used for the
manufacture of glass.
Of the sands suitable for glass-making the colour is white to
faint yellow, at its best almost equal to jihat of Fontainebleau
sand. It changes to faint pink on burning. Washing would
probably improve slightly some of the second-best sand, which
would then serve for white bottle-work. The chemical analysis
yields :
SiCL 99-56 per cent.
ALjO 3 0-26
Fe.,0,, 0-06
Loss on ignition 0'24
Total 100-12 per cent.
From the point of view of glass-making the grade-analysis is
good (Hate III. fig. 4). It is as follows :
>0'5 & <1 mm., 0-6 % ; >0'25 & <0'5, 73-0 % ; >0'1 & <0'25, 25'7 % ;
> 0-01 & < 0-1, 0-2 % ; < O'Ol ,0-5 %. Total sand-grade, >0-1 4<Imm.,
99-3 %.
res MS j?s _s_ o_ _s_ -i
Lo-6' 73-0' 25-7' 0'2' 0-5 ; 99'3' J
_ In mineral composition the sand closely resembles other deposits
of the same age, such as those from Aylesbury, Leighton Buzzard,
Lynn, etc., described. The list of minerals and description there
given hold good for the Godstone deposits.
The price is 6s. 6d. per ton on truck at Caterham Station
(S. E. & G. Railway).
At Oxted and Limpsfleld in Surrey, about two to three miles
east of Godstone, and at other places along the outcrop, the same
salhds (Folkestone Beds, Lower Greensand) are rather coarser in
AND BEICKA.TE SANDS. . 61
character, the mechanical composition (see Table V. on page 163)
resembling that of Leighton Buzzard sand. More iron is present,
and the sands burn redder, but they would be suitable for bottle-
glass work. The mineral composition is again typical of the Lower
Greensand.
Sands of the same age (Lower Greensand), but rather less pure,
occur at Westerham in Kent and at other localities near.
Similar sands occur in the Folkestone Beds (Lower Qreensand)
in Sussex, e. g. near the village of Rogate. The overburden is,
however, great, and the sands frequently contain patches of
calcareous material.
Sand from Reigate, Surrey.
Worked (1) Doods Road Pit : by Mr. A. B. Apted, Doods Road,
Reigate; (2) Park Lane Pit: Agent, Mr. H. Sims, Old Town.
Hall, Reigate.
Maps. Geological : Old Series, 1 inch, Sheet 8.
6-inch, Surrey, Sheet 34 N.E
Situation. Doods Road Pit. Lat. 51 14' 25", Long. 11'
0" W. ; Park Lane Pit. Lat. 51 14' 5' , Long. 12' 45" W.
The smaller pit, in Park Lane, is situated about one-third of a
mile south-west of the Castle, and the larger, Doods Eoad Pit,
occurs by the northern side of the railway half -way between Reigate
and Reclhill.
Formation. Folkestone Beds (Lower Greensand).
Description. The Reigate sand is similar in age and character-
to that at Godstone, but the purer parts are of greater extent.
The iron-staining is distributed in patches, but is never so serious
as to prevent the sand being worked for second-quality glass
(sheet-glass, pressed ware, laboratory- ware, etc.). Topley, in the
"Geology of the Weald," stated (page 141) that Reigate sand was
used for glass-making. The best seams of sand are equal in colour
to Fontainebleau sand. The presence of calcareous material in
places will probably necessitate washing. The chemical analysis-
is as follows :
SiO a 98-93 per cent.
A1 2 6 3 0-67
Fe 3 3 0-02
CaO trace
MgO none
KaO n.d.
Ma^O n.d.
Loss on ignition 0-28
Total 99-90 per cent.
The mechanical analysis indicates : * -
>0-5 & <1 mm., 2-7 % ; >0'25 & <0-5, 79 % ; >0'1 & <0'25, 14'5 % - f
>0-01 & <0-1, 1-8 % ; <0-01, 2-0 %. Total sand-grade, >0-1 mm.,
96-2 %.
PCS MS^ FS j_ o^ JL1
l_2'7' 79-0' 14-5' 1-8 2-6 ; 96-2'J
62 BEITISH SANDS SUITABLE FOE GIA SB-MAKING.
The grading is rather variable, a gradual passage from coarse to
fine sands being frequently observed. The mineral composition is
typical of the Lower Green sand. The sands should be worked
with care, both from the point of view of grade and of iron-content.
That the available resources here are very great is indicated by the
abundance of caves throughout the Keigate area. Large quantities
of cream-coloured sand have been removed from these excavations.
Doods Eoad Pit shows a 40-foot face of sand.
From the Doods Road Pit, selected fine silver sand is put on
truck at Redhill Station at Qs. per ton (unwashed).
The available resources in the area are over one hundred million
tons.
Sand from Aylesford, Kent.
Worked by Mr. Silas Wagon, Aylesford.
Maps. Q-eological : Old Series, 1-inch, Sheet 6.
6-inch, Kent, Sheet 31 S.W.
Situation. Lat. 51 18' 25", Long. 29' 0" E.
The pit exhibiting the whitest sand lies immediately north-east
of Aylesford Church. The Nickle pit, a quarter of a mile west of
the church, contains rather yellower sand (worked by the Nicopits
Sand Company, Ltd.).
Formation. Folkestone Beds (Lower Greensand).
Description. Whitish sands with a northerly dip are covered
in one part of the pit by the red ferruginous sandstone known as
carstone. About twelve feet of the sand are worked, but the
floor of the pit was covered with water at the time of writing.
White chalky matter is often present. The general characters
Are similar to those of the other Greensand deposits described.
The colour is pale grey to cream, but the sand burns up pink.
The chemical analysis of the best sand is as follows :
SiO,, 99-06 per cent.
A1 2 6., 0-56
Fe 2 3 0-04
CaO 0-17
MgO trace
K,0 0-26
Na a O 0-11
Loss on ignition -22
Total 100-42 per cent.
The grading is good, a mechanical analysis being as follows :
>0-5 & <1 mm., few grains only ; >0-25 & <0'5, 88-7 % ; >0'1 & <0-25,
16'0 % ; >0-01 & <0-1, 0-3 % ; <0-01, none. Total sand-grade,
>0-1 & <1 mm., 99-7 %.
es MS JFS a_ s -i
fa? 83-7' 16-0' 0-3 : 99-7' J
SAND FBOM HOLLINGBOITBNE AND BEAE8TED. 63
The mineral composition is that o the Lower G-reensand
generally, tourmaline, staurolite, and kyanite being large and
conspicuous in the heavy mineral crop.
The sand is supplied on ship upon the Medway at Aylesford at
8s. per ton, and on truck at Aylesford Station (S. E. & C. Rail-
way) at 9s. Qd. It is used for bottle-making at Queenborough,
but would be of service for better glass.
The available resources are about five million tons.
Sand from Hollingbourne and Bearsted.
Not at present being worked.
Maps. Geological : Old Series, 1-inch, Sheet 6.
6-inch, Kent, 43 N.W.
Situation. Lat. 51 16' 0", Long. 35' 30" E.
The chief excavations, in the form of caves, lie nearly half a mile
east-south-east of Bearsted Church, and one mile south-east of the
railway station.
Formation. Lower Greensancl (Folkestone Beds).
Description. Sands were stated to have been worked formerly
at Bearsted, Hollingboume, and Aylesford*, for making the
commoner kinds of glass, "about 1000 tons being annually shipped."
The caves at present existing at the first two localities testify to
the extent of the former working. The sands are similar in
diameter to those of the same age at Aylesford, Godstone, and
Keigate, the caves being very similar to those of the last-named
place. The sand is cream-coloured, turning after ignition to a
browner tint. A chemical analysis yielded the following result :
SiO, 99-25 per cent.
A1 2 0, 0-31
Fe 2 3 0-04
CaO 0-09
MgO none
LOBS on ignition 0-31
Total 100-00 per cent.
Alkalies absent.
A mechanical analysis yielded the following figures :
>0-5 mm., none; >0-25 & <0'5, 94' 6 % j >0'1 & <0'25, 4'2 % ; >0'01 &
<0'1, 0-8 % ; <0-0], 0-4 %. Total sand-grade, >0'1 mm., 98'8 %.
PMS PS B_ e . S "I
I_94-6' 4-2' 0-8' 0-4' 98'8'J
The mineral composition is similar to that of the Lower G-reen-
sand generally (see pages 50,54-59), the percentage of heavy detrital
* Mineral Statistics : Mem. Geol. Snrv. I860, p. 374.
64 BRITISH HANDS SUITABLE FOB GLASS-MAKING.
minerals of density greater than 2'8 being 0'026. Large kyanite
(0 - 4 mm. diameter), staurolite, and tourmaline grains (0'2 mm.)
are abundant; ilmenite, zircon, rutile, and linaonite (O'l mm.)
are common, and flakes of muscovite mica (O'G mm.) are also
present.
The sand requires to be carted one mile by road to the nearest
station, Hollingbourne (S.E. & C. Railway) ; Bearstead Station is
about two miles away by road.
The available resources in this district are over twenty million
tons.
Lancashire Sand.
Worked by a considerable number of glass-manufacturers and
sand-merchants.
Maps. Geological : Old Series, 1-inch, Sheet 89 S.W.
6-inoh, Lancashire, Sheets 92 N.E., S.E. ; 100 N.E.,
S.E. ; 101 N.W., S.W.
Situation Lett. 53 28' to 53 33', Long. 2 44' to 2 50' W.
The pits and excavations are situated in the belt of country
running south-east to north-west from St. Helens to Onnskirk.
Formation. Glacial Sands.
Description. The sands are worked extensively for the making
of bottles and window-glass (at and near St. Helens), also in
connexion with the soap-industry. The deposits occur at Crank,
Rookery, Kainford, Kings Moss, Upholland, Skelmersdale, etc.*,
north-west of St. Helens, and are used locally, so that no great
amount of transport takes place. Skehnersdale, the farthest distant,
is about nine miles from St. Helens. The sands are brown,
frequently dark brown, in colour, and are very peaty. They occur
in a series of hollows now drained by the small streams which flow
south-eastwards to St. Helens and Warrington, and so into the
Mersey. In late Glacial or post-Glacial times, these hollows were
doubtless badly drained, and became filled with vegetation which has
yielded the present peaty material. The abundance of place-names
containing " Moss " is very significant. The decomposition of the
vegetable matter has had a reducing effect on the ferric oxide in
the sands, and in many cases, by the action of the acid peaty waters,
has dissolved the iron out. The sands are worked to the drainage-
level, usually a depth of about four feet only, and the turned-over
knd is again devoted to agriculture. The sands are washed at the
various localities where they are won, and it is interesting to see
in operation all styles of washing, from the most primitive to the
latest and most effective. In the former case, the sands are washed
by being run into shallow troughs and boxes let into the ground,
where the material is kept in motion by shovelling. Paddle-
methods of washing are also used, as well as modern rotary,
dredging, and worm appliances. Vegetable matter is screened off,
* The Shirdley Hill sands of the Geological Survey Memoir, " The Superficial
Geology of S.W. Lanos." 1877.
LANCASHIRE AND HFTTONS AHO SANDS.
and the water after washing is coffee-coloured with -peaty and
dissolved ferruginous compounds.
Mechanical analyses of washed and unwashed samples from
Rainford are as follows :
OS.
>0-5 &
<1 mm.
MS.
>0-25&
<0-5.
FS.
>o-i&
<0-25.
a.
>0'01 &
<0-1.
0.
<0-01
mm.
S.
Total sand-grade :
>0'1 mm.
Unwashed ...
WaBhed
3-3%
1-3
83-0 %
84'5
11-7%
18-1
0-9%
0-2
M%
0-9
98-0%
98'9
The material is thus fairly well-graded and of suitable size in
grain.
Although the sand is of a medium brown colour even after
washing, the iron-content is low. The following are chemical
analyses of Kainford Sands :
Washed.
SiO 96-59
3 1-72
3 0-03
OaO 0-19
MgO 0-08
K a O 1-05
Na.,0 0-05
Loss on ignition 0*43
Unwashed.
Fe tt O a 0-05 percent.
Total 100-14 per cent.
Duplicate determination, K a O, I'Ol % ; Na 2 0, 0-08 % .
The available resources are over a hundred million tons.
Sand from Buttons Ambo, near Malton, Yorks.
Worked by The High Silica Sands Company, Commercial
Street, Norton, Malton.
Maps. Geological : New Series, 1-inch, Sheet 63.
Old 93N.E.
6-inch, Yorkshire, Sheet 141 N.E.
Situation. Lat. 54 5' 50", Long. 51' 40" W.
Greyish and pale yellow sands occur at Sleights and Hutton
Bank, and the working is in process of development.
Formation. Upper Estuarine Series (Lower Oolites).
Description. The sections at present exposed show in the lower
part ten to seventeen feet of cream-coloured sands with a small
admixture of kaolin. Black specks of ilmenite are in places rather
abundant. The sand is improved by washing, which removes
calcareous and aluminous material also. The kaolin may be' an
advantage in the making of certain glasses, and for other purposes
66 BEITISH SATTDS SUITABLE FOR GLASS-MAKING.
it is easily removed if desired. Unwashed, this deposit serves
excellently for bottle-glass making and for lining the hearth-
bottoms of steel furnaces. (See Plate IV. figs. 1 & 2.) One seam
of the sand is extremely pure, but most will have to be washed.
The sand reddens slightly on burning.
A chemical analysis of a washed sample is as follows :
SiO a ..................... 99-04 per cent.
A1A ................. 0-84
Fe.O.j .................. 0-03
CaO ..................... 0-10
MgO .................. 0-18
Loss on ignition ...... 0'19
Total ......... 100-38 per cent.
Before being washed, the sand contains 0-13 per cent, of iron oxide.
The mechanical analysis indicates :
>0-5 & <1 mm., 1-4 % ; >0'25 & <0'5, 84'9 % ; >0'1 & <0'25, 75 % :
>0-01 & <0-1, 4-1 % ; <0-01, 2-1 %. Total sand-grade, >0'1 &
<1 mm., 93-8 %.
PCS MB ES _a_ _o JJ_ -I
Ll'4' 84 ; 9' 7-5' 4-1' 2'1 ; 93-8-J
The upper part of the sections reveals beds, twelve feet in thick-
ness, of yellow and brown clayey sands with greyish carbonaceous
layers. Much more " bind " occurs in these beds, and the deposit
is of great value for refractory purposes such as steel-casting.
The chemical analysis of the latter refractory sand is as follows :
SiO, ........................ 83-8 per cent.
^AiA ........................ 9-2
Fe 2 3 ..................... 1-6
CaO ........................ 0-6
MgO ........................ trace
LOBS on ignition ......... 4*7
Total 99-9 percent.
Anal. : S. Hewitt.
The sand is quartzose, felspar being much less abundant than in
the Kelloway Beds. In mineral composition the sand does not
exhibit a rich variety of minerals, the heavy residue being coarse
(averaging O2 mm. diameter). Very little magnetite is present,
but ilmenite is abundant. Limonite and leucoxene occur. Large
red garnets are common, and also tourmaline, staurolite, deep red
rutile, and zircon. Grains of serpentine are occasionally seen.
The workings have now been considerably developed, a seventy-
yard face having been opened up. A siding from the N. E.
Kailway, between Castle Howard and Ehrtfcons Ambo, has been
built. It is hoped that the sand will be delivered at Knottingley
and other places in the Yorkshire area at 7*. to 9s. per ton. It is
put on truck at Huttons Ambo at 3s. 3d. per ton.
The estimated resources are one million tons.
BimYTHOJtPE SAND. 67
Sand from Burythorpe, near Malton, Yorks.
Working given up some years ago.
Maps. Geological : New Series, 1-inch, Sheet 63.
Old 93N.E.
6-inch, Yorkshire, Sheet 42 N.W.
Situation. Lat. 54 4' 40", Long. 48' 40" W.
Whitish sands are exposed in several pits, the chief of which
lies near the Fox Cover, and three-quarters of a mile north-west
of Burythorpe Church.
Formation. Kelloway Beds of the Jurassic.
Description. As in the case of the countiy around Leighton
Buzzard, Middleton and Gayton, Q-odstone, etc., the sand supports
only a poor heath flora by means of which its fairly extensive
outcrop is vaguely defined. Some years ago it was worked for
glass-sand, but the Avorldng was given up; it may be re-exploited
shortly.
The sand possesses a slight brown tint, due to irou -staining, but
the best quality is nearly white (cream-coloured). The tint
becomes slightly browner on burning, but the original colour,
which lies between those of Fontainebleau and Belgian sands, is
not improved to any extent by washing, although calcareous
material is removed.
The chemical composition is as follows :
Pox Cover Burythorpe
Pit. Pork.
SiO, 96-79 96-70 per cent.
Al.,6, 1-63 1-49
TiO,' n.d. 0-35
Fe.d, 0-22 0-07
Cab' n.d. 0-12
MgO ' n.d. 0-07
K. 2 n.d. 0-84
Na.,0 n.d. 0-08
LOBS on ignition 0-60 0*56
Totals 99-24 100-28 per bent.
The dominant grade of the sand is smaller than that of foreign
and also other British glass-sands, but this is an advantage,
for the deposit is well-graded (see Plate III. fig. 5).
In the mechanical composition the grade-percentages are :
>0'5 & <1 mm., few grainn only; >0-25 & <0'5, 39-2 % ; >0'1 &
59-0 % ; >0'0i & <0-1, I'O % ; <0'01, 0'8 %. Total sand-grade, >0'l'
&<1 mm., 98-2 %.
rCS MS FS s o S
l_tr.' 39-2' 59-6' 1-0' 0'8 ; "98 1 !
The grains mostly consist of subangular clean quartz, but grains
of turbid felspar are not uncommon. The heavy residue is abundant
and consists of much fine-grained dark material (average diameter
68 BBTT1SU SANDS SUITABLE l'0il G-LASS-MAKIKG-.
O'l mm.). In character it most resembles the mineral assemblage
of the Inferior Oolite, which is remarkably similar all over its
outcrop across England, from the Dorset coast to Yorkshire.
Abundant magnetite and ihnenite occur, and colourless to pale
brown and pink angular garnet grains (O12 mm. diameter) make up
most of the residue. Kutile is extremely plentiful and zircon is
common (both about Ol mm. or less diam.). Staurolite and grey-
brown tourmaline grains occur. Muscovite is present, but the
diameter of the flakes (0'12 mm; diameter) is not much larger than
that of the average for the rest of the grains.
The question of transport to the nearest railway station, Malton
(almost 5 miles), the high railway freights, and also the distance to
the nearest port are serious considerations. The great glass-making
area of Yorkshire is, however, near at hand.
Some trial-borings and a trial-hole have recently been put down
a short distance away in Burythorpe Park by the owner, B. JB.
Colton JFox, Esq. The best of the sand brought to the surface
looks very promising, and subject to an improvement in the
economic conditions specified above, development of the area may
be expected. (For analyses, see Tables, pages 156, 162.)
The available resources in the area amount to three million
tons.
Less pure sands in the Kelloway Beds are worked at South Cave,
near the station (by Messrs. T. H. Lyon and Partner, of Norton,
Malton). They are of service for white bottle-glass and much
other ware. Similar sands occur at Newbald. At Sancton, near
by, white micaceous sands are found in the Estuarine Series.
Sand from Denford, Northamptonshire.
Worked by the Ebbw Vale Steel, Iron & Coal Company, Ltd.,
Irthlingborough.
Maps. Geological : Old Series, 1-inch, Sheet 52 N.W.
6-inch, Northamptonshire, Sheet 33 N.W.
Situation. Lett. 52 22' 20", Long. 33' 45" W.
The pits, which have really been opened for the purpose of
exploiting the Northamptonshire Ironstone below the sand, occur
nearly one mile west-south-west of Denford Church.
Formation. Estuarine Series (Inferior Oolite).
Description. Sands occur at the same geological horizon near
by at Corby, Wansford, Apethorpe, Blatherwyke, etc., and were
mentioned as having been worked for glass-making about 1860.
Unfortunately, the variability and limitation in quantity which
detracted from the value of these affect also the Denford deposits.
It might be possible to get a good average quality by washing,
but the sand is too fine in grain to be easily washed without
considerable loss (see page 122).
The sand is cream-coloured and burns up pink. A chemical
analysis of an average sample is as follows :
DENFOBD AND LONGBOWS' SANDS. 69
Si0 2 98-19 per cent.
Al,0 3 1-23
Fe,0 3 0-06
CaO 0-15
MgO none
LOSB on ignition 0'46
Total 100-09 per oent.
The effect of washing would be to remove certain ferruginous
pellets that occur, and to reduce appreciably the iron-percentage,
which is already low.
The sand is veiy fine in grain and is well-graded, a mechanical
analysis indicating :
>0-5 mm., none; >0>25 & <0'5, 2-9 % ; >0'1 & <0-25, 92-3 % j >0'01 &
<0-1, 3-0 % ; >0-01, 1-8 %. Total sand-grade, >0'1 mm., 95'2 %.
[-MS F8 a o S "I
|_2-9' 92-3' 3-0' 1-8 : 95'2'J
The sand carried an abundant and dark residue of heavy detrital
minerals, the portion of density greater than 2'8 being 0'38 per cent.
The residue is dark as a result of the preponderance of ilmenite,
.and the mineral assemblage resembles that of the Inferior Oolite
generally in its outcrop across England. The following is a list of
the common mineral species in order of abundance : Ilmenite and
iron ores, garnets, zircon, red rutile, kyanite, tourmaline, glauconite,
.staurolite, muscovite, and yellow anatase.
The available resources, owing to the variability of the beds, are
probably small.
Sands of similar age ("Inferior Oolite), but less pure, occur at
Tadmarton, about four miles west-south-west of Banbury. The pit
is situated half a mile east of Tadmarton Church (Lai. 52 2' 12",
.Long. 1 25' 5" W.), and is worked by Mr. H. H. Salmon. About
.sixteen feet of rather variable sands containing peaty layers may
be seen. Some of the bands are more iron-stained, rendering the
profitable working of the pit for glass-sands, in view also of
the location, improbable. The sand is coarse] 1 than that from
Denford (see Table of Mechanical Analyses, page 162), but the
mineral composition is similar, large pink and brown garnets, large
staurolite, grey-brown tourmaline, abundant ilmenite and iron ores,
.zircon, and red rutile being characteristic.
Sand from Longdown, near Southampton.
Worked by Messrs. Sandell Bros., 79 High Street, Southampton.
Maps. G-eological: New Series, 1-inch, Sheet 315.
Old 11.
6-inch, Hampshire, Sheet 72 N.E.
Situation. Lat. 50 52' 30", Long. 1 29' 10" W.
BEITISH SANDS SUITABLE FOB GLASS-MAKINCK
The pits are worked a little to the south-east of the hamlet of
Longdown in the New Forest, and are situated about four miles
west-south-west of Southampton West Railway Station (L. &
S. W. Kailway).
Formation. Barton Sand (Upper Bagshot Beds).
Description. Sand from Longdown, situated upon land in
the New Forest belonging to the Crown, was mentioned as
having been worked for glass-making, and sent to the north of
England, as early as 1858*. It is said to have been nearly
as white as the Isle of Wight sand, and to have cost Qd. per
cubic yard. Assuming a cubic yard to contain 30 cwts., we-
should now consider this price exceedingly low.
Two sets of pits are at present being worked. At the western end
may be seen a fifteen-foot section of fine-grained, cream-coloured
sand, containing yellowish patches and streaks which are more-
plentiful near the top. The overburden is very small. At the
eastern end of the excavation red and yellow sands form a thicker
topping, and the white sand is less constant. The latter is worked
down to ground-water level.
If the sand were washed the iron-content and grading would
doubtless be much improved, but the washing-plant at present on
the market is not well suited to the rather fine grain of the sand.
Inevitable loss of fine sand would result. Washing improves the
colour slightly, and samples of the sand on ignition become a
rather darker brown. The chemical composition indicates :
SiO, 95'41 per cent.
Al.,0., 2-35
Fe 2 On 0-09
CaO! 0-26
MgO 0-18
K a O 1-33
Na.^0 trace
Loss on ignition 0'50
Total 100-12 per cent.
After being washed the sand contains 0-06 per cent, of iron oxide-
(asFeA)-
The deposit is fine-grained, mechanical analyses being as
follows :
MS.
FS.
B.
0.
S.
>0-25&
>0-1&
>0-01 &
<0-01
Total sand-grade :
<0'5mm.
<0-25.
<0-1.
mm.
>0-1 mm.
Western end . . .
8-9%
84-6 %
3'8 %
27%
93-5 %
Eastern and , . .
5-9
91-2
1-5
1-4
97-1
* Mineral Statistics : Mem. Gteol. Survey, 1860, p. 374.
SAND. 71
The heavy minerals of density greater tban 2'8 constitute
0-08 per cent, of the whole. Large flakes (0'4 mm. diameter) of
a greenish nmscovite are very abundant. Brown tourmaline
(O'l mm.), kyanite (0'2 mm.), iron ores, including ilmenite
(altered to leucoxene), magnetite and liinonite, are plentiful.
Zircon and rutile in small grains about 0'05 mm. in diameter
occur commonly, and the presence of epidote and green hornblende
(O'l mm.) was also noted.
The sand is carted by road about two miles to Lyndhurst Eoad
Station (L. & S. W. Railway), where it is put F.O.R. at Qs. per
ton. Two miles' cartage eastwards will also bring the sand to a
small quay on Southampton Water owned by Messrs. Sandell Bros.,
the water-freight to the London area being about 2s. Qd. and to
Bristol 3s. per ton before the war. The sand is at present being
supplied to the Bristol area (railway-freight about 10s. per ton) for
bottle-making, but it is sufficiently good for better quality glass.
The sand occupies several square miles of wooded country, and
the available resources are certainly not under four million tons.
Sand from near Fordingbridge, Hants.
Working being undertaken by Mr. A. J. Terrill, Eosebank,
Fordingbridge ; Lybum Estate, owned by Cecil Lee, Esq.
Maps. Geological, 1-inch. New Series, Sheet 315.
6-inch, Wiltshire, Sheet 77 S.E.
Situation. Lat. 50 57' 30", Long. 1 39' 30" W.
The locality is actually across the county boundary in Wiltshire,
but Fordingbridge is the nearest town.
The pits occur near "No Man's Land" about five miles east-
north-east of Fordingbridge, and nine miles south-east of Salisbury.
Formation. Bagshot Sand.
Description. Wide stretches of sandy heath occur in this area.
For the greater part the sands have been bleached white, or are
coloured grey by an admixture of peaty material. So far as the
small excavations enable the observer to judge, a bed of pale grey
sand at least six or seven feet thick (the greatest depth yet proven),
and probably much thicker, extends over a considerable area.
The sand is pale brown in colour and becomes grey on ignition.
The chemical analysis of a bulk sample as collected is as
follows :
SiO a 99-28 per cent
AL,0., 0-17
TiO a '. 0-07
Pe..0 a 0-02
Cab: , 0-11
MgO none
K.jO none
Na 2 none
Loss on ignition 0'27
Total 99-92 per cent.
74 BRITISH SANDS SUITABLE FOll Q-LABS-MATCINO.
The chemical analysis is as follows :---
SiO, 95-21 per cent.
ALP, 2-43
Fe^O'a 0-42
CaO 0-19
MgO none
K.,0 0-89
Na,0 0-19
Loss on ignition . . . 0'88
Total 100-21 per cent.
The mechanical analysis indicates that the grade of " fine sand "
is dominant, as in the Burythorpe deposit :
>0-5 & <1 mm., none; >0'25 & <0'5, 16-2 % ; >OvL & <0-25, 79'6 % ;
>0-01 & <0-1, 3-1 %; <0-01, 1-1 %. Total sand-grade, >0'1 &
<1 mm., 95-8 %.
TMS JF3_ _B_ _c S -I
Ll6'2' 79-6' 3-1' 1-1 ' 95'8'J
In mineral composition the sand resembles the Thanet Beds
generally along the southern outcrop, the detrital minerals being
fairly abundant, and occurring in angular grains. Ilmenite
(altering to leucoxene) and limonite (O2 mm. diam.), zircon
(O'l.rnm.) and rutile (0 - 2 mm.) abound, and tourmaline (0'2 mm.),
staurolite, ? andalusite, and flakes of muscovite (0'2 mm. diam.) are
also found.
Bail and river are near, and the sand is supplied at about 3*. Qd.
to 5s. per ton at the pit (Is. 6rf. and upwards per " foot ").
The available resources of glass-sands are over two hundred
thousand tons.
Thanet Sand near Rochester is similarly worked for the bottle-
industry at Queenborough, Higham, etc.
Sand from Worksop.
Worked by Messrs. Jas. Turner & Son, Ltd., Kiveton Park,
near Sheffield, and at Worksop.
Maps. Geological : Old Series, 1-inch, Sheet 82 N.E.
6-inch, Nottinghamshire, Sheet 8 S.W.
Situation. Lot. 53 18' 48", Long. 1 7' 64" W.
The quarry, in which the sand suitable for glass-making is.
exposed, lies about one-third of a mile west of Worksop Station
(Q-. C. Eailway).
formation. Lower Bunter.
Description. The excavations being made for Messrs. Turner's
new glass-works, which are in course of erection, have revealed
an excellent section of Permian marls. The marls are purple and
green in bands, and the basal Bunter Sands rest upon their wavy
upper surface. Fifteen feet of pale-coloured sands are seen, of
WOKJCSOP SAJfJ). 75
which the lowest seven or eight feet are worked for glass-making.
In places these sands have a pale greenish appearance, and certainly
appear to have a better colour where they occur below ground-
water level. This may be due to solution of ferric compounds
by algal or bacterial action. It is proposed to treat this bed by
tank-washing, but at present the sand is being shipped to the
Tyneside glass-works just as it is quarried. The uppermost few
feet of the pale sands contain ferruginous streaks and patches,
lied sand, strongly current-bedded and rather coarse in grain,
forms the upper part of the section, fifteen to twenty feet high. It
is worked as an " open " moulding-sand and for building-purposes.
The glass-sand is pale brown in colour and darkens on heating.
A washed sample analysed by Mi-. J. H. Davidson, M.Sc., of the
Department of Glass Technology in the University of Sheffield,
gave the following result :
SiO., 95-10 per cent.
ALA 2- 32
TiO.> trace
Fe,6., 0-51
OaO! 0-22
MgO 0-24
Loss on ignition 0-54
Alkalies, by difference . 1'07
Total 100-00 per cent.
An average sample of unwashed sand (as sent to the North of
England) collected by the writer contained only O10 per cent,
of ferric oxide.
The mechanical analysis is as follows :
>l mm., 2-0 % ; >0-5 & <1 mm., 6'6 % ; >0'25 & <0-5, 58'65 % ; >0'1 &
< 0-25, 26-15%; >0-01 &<0-1,4'5 %; <0-01, 2'1%. Total Hand-grade,
>0-1 mm., 93-4%.
rvcs cs MS PS_ _B _o_. s I
L 2-0 ' 6-6' 58-65' 26 ; 15' 4-5* 2-1 ' 93'4' J
The percentage of alumina in the sand is an advantage for bottle-
making, as it strengthens the glass. The alumina is present partly
as felspar, and partly as its decomposition product kaolin. Much
of the latter washes' out of the sand, and its presence is indicated
by the high clay-grade in the mechanical analysis.
L In mineral composition the deposit resembles many other Bunter
Sands. Ilmenite is abundant but very much altered to leucoxene.
Yellow-brown and grey tourmaline in highly rounded grains are
very abundant. Pink garnets (0-2 mm.), angular staurolite, and
apatite also occur. Zircon and red rutile (O'lxO'03 mm.) are
plentiful.
The quarry lies by the side of the G. C. Railway from Sheffield
to Ketford (via Worksop), and the Chesterfield Canal, which has,
hoAvever, fallen into disrepair, especially in the adjacent Norton
76 BRITISH SAjSDS SUITABLE FOB GLASS-MAKING-.
Tunnel. The sand is supplied F.O.R. at Worksop (unwashed) at
3s. Qd. per ton. It could be put on boat on the canal for about
4s. Qd. per ton.
The available resources are over six million tons.
At Alderley Edge, Cheshire, occur large tips of sand which
have accumulated from the copper and lead mines (6-inch Map,
Cheshire, 28 S.W. Lot. 53 17' 40", Long. 2 18' 15 <( ). The
Keuper Waterstones are impregnated at this locality with galena
(lead sulphide) and malachite (copper carbonate). The sandstones
were formerly mined, and after being crushed were treated with
acid to dissolve the metalliferous ores. The resulting sand was
washed to recover as much as possible of the metallic salts, and
has thus accumulated as waste material.
The acid treatment has doubtless removed part of the iron oxide,
but about 0'12 per cent, remained in a sample tested. The sand is
pale brown and becomes greyer after ignition. It is markedly
felspathic. The alumina present in the felspar would add to the
value of the sand for bottle-making, when the iron-content would
certainly not be too high for pale bottles.
In consequence of the washing, the grading is fairly good, as the
following analysis indicates :
>0'5 & <1 mm., 2-4%; >0'25 & <0'5, 76'9%; >0vl & <0'25, 17'2%;
>0-01&<0-l,l-6%; <0-01,1'9%. Total sand-grade, >0'1 mm.,96'5%.
PCS MS FS a o S ."I
l_2 T 4' 76-9' 17-2' 1-6' 1-9 J 96 : 5j
Unfortunately the deposits are not situated upon a coalfield or a
bottle-making area, and it is doubtful whether it would pay to
move the sand as far as either the Manchester or Yorkshire districts.
The mines are situated about one and a half miles south-east of
Alderley Edge Station (L. & N. W. Railway), the road being u
good one and downhill. ,
Dune-Sands and Shore-Sands.
Although some of these sands, the analyses of which are given
in the Tables (pages 157, 165), have been used for bottle-glass, no
blown-sand or shore-deposit from the British Isles pure enough
(with the exception of that from the Isle of Jura) and in sufficient
quantity for the making of flint or better-class glass lias yet been
seen by the writer. The constituents of these sands have usually a
very mixed origin ; but if local derivation from, decomposing pure
sandstones or quartzites can be ensured, suitable sands may be found.
Usually, in dune- and shore-sands, current-action tends to defeat
this object. Nevertheless, the dune- and shore-sands of the
United Kingdom (especially those bordering the Archaean areas of
Scotland and Ireland) ought to be more thoroughly investigated
than they have been. The colour of such sands varies from pale
iDUJS'E-SAJSDS A5TD SHOJtE-SAlTDS. 77
grey and brown to deeper tints, and usually darkens considerably
on burning. Too much iron is present, and the heavy mineral
crop is frequently large. Commercial electromagnetic separation
will hardly clean the sands sufficiently. They are of little use
except for "black" glass-work when the industry is located close
at hand.
The purest shore-sand met with is that occurring on the western
shores of the Isle of Jura, and derived from the Dalradian
quartzites forming the greater part of the island. This sand is
said to have been formerly worked for glass, but it is of limited
extent and, although very white-looking, contains O07 per cent,
of iron oxide.
The beach-sand from the Isle of Eig'g is also of fairly good
quality, and consists of very clean and colourless angular quartz,
mixed with a considerable quantity of dark kaolinized felspar, but
it yields a large crop of heavy minerals derived from neighbouring-
igneous masses (augite, olivine, epidote, garnet, zircon, etc.).
Similar sands from near Dublin (Sandymotuit Strand) have
been used in the dark-bottle industry of that city.
Additional shore- and dune-sands from Ireland have, also been
examined in view of the needs of the bottle-industry *. Samples of
blown sands .from Button (Kilbarrick) near Dublin, Washing Bay,
Coalisland (on Lough Neagh), Ballycastle (Co. Antrim), etc.,
have been examined and analysed, with the results given oi>
page 165.
GK H. Kinahan. in his account of the economic geology of Ire-
land f, mentions the occurrence at Ballycastle of a white sand suitable
for glass-making, stating that it occurs as Drift. It lies upon and
is presumably derived, at any rate in part, from the Carboniferous
Sandstone. The sand worked for the old Ballycastle Glass-works,
(up to 1820) was blown-sand from the dunes, not a very pure
material, and the glass made was a rough thick green bottle-glass
only-
Specimens of a shore-sand from Maghera, Ardara, Co. Donegal,
have been forwarded by the Officer in Charge of the Coastguard
Station, who says that the quantity available is unlimited. The
sand is unfortunately somewhat shelly and rich in heavy detrital
minerals. The iron -percentage (Fe a 3 ) is 0'7 per cent. A similar
but slightly less pure sand has been obtained from Sandflelds,
Ardara. Mechanical analyses of these sands will be found in the
Tables.
Besides those sands analyses of which are given later (see
pages 167, 165), samples from the following localities (sent by the
courtesy of Sir Bertram Windle, F.R.S., President of University
* Prof. Gilbert Morgan issued a report on Irish Glass-sands shortly after
the outbreak of war. This statement mentioned, besides Muckish Mountain
Sand, deposits which might bo worked for bottle -making', and whioh occurred
at Sutton near Dublin, Bosslare, Silver Strand (Wicklow), Ardara (Co. Done-
gal), and Washing Bay (Lough Neagh).
f Journal Royal Geol. Soo. Ireland, vol. viii. (1887).
78 BRITISH SAtfDS SUITABLE FOR GLASS -
College, Cork) have been examined : Castlefreke (Cork), Clay-
castle (Youghal), Glenbeigh (Keny), Kilkee (Kerry), and Rush-
mere (Tramore).
Information regarding other sands investigated will be found in
the Tables or, incidentally, in the remarks below. Sandstones and
quartzites naturally disintegrated or crushed to produce "glass-
sands " are discussed in Chapter VII.
CRUSHED BOOKS. 79
CHAPTER VII.
A. PURELY SILICEOUS DISPOSES (continued}.
(6) CRUSHED BOCKS.
Many crushed quartzose rocks have been placed upon the market
as proposed substitutes for glass-sands. At the outset, it may
be said that they have never found much favour with British
Fig. 12. Mechanical Analyses of Glass- Sands : Crushed RocTcs, etc.
100%-t m
10 -
,
-
'0 0-5 O-Z5 0-1 mms.
> Grade Sizes (diameter in Mil I i metres)
manufacturers, although such materials appear to be exten-
sively used abroad. The great evil of rock-crushing lies in the
quantity of dust, which is waste material, produced. Mining
engineers are still endeavouring to devise a machine that will grind
or crush rocks to a fine even grade without producing slime.
So far as glass-making materials go, the remarks regarding the
un suitability of sand not of even grade apply still more empha-
tically here. Several pure sandstones and quartzites, of various
geological ages from pre- Cambrian to Coal Measures, occur in the
British Isles, and a few have been crushed and exploited. Mechanical
analyses of the products are given in the Tables. Sifting is usually
carried out at the quarries, and so those coarse grades which are
objectionable are eliminated. Large quantities of fine grades and
80 CRUSHED EOCKS.
t
dust are, however, produced, and, in order to yield an effective
sand, these ought to be washed away with water-currents of
strength calculated as above from elutriation data. It is frequently
necessary to remove electromagnetically the iron particles derived
from the crushing-plant. The cost of quarrying, crushing, and
sifting has generally been too great to permit of washing also,
and the price of the unwashed material is often prohibitively high,
even in the neighbourhood where it is produced. Much more is
the cost increased by the usual heavy freights, so that there is
little likelihood of such materials replacing glass-sands to any
extent for ordinary work in this country. High-content of silica,
and alumina also if that is desired, low iron, and general purity
and angularity are their chief recommendations. Difficulties
occur in the use of these crushed rocks. Often it does not pay
to wash them, and consequently loss results from the burning
out of the fine grade, and unevenness in the " metal" is caused by
irregular melting. The fine material carries with it air-bubbles,
from which the "metal" is cleared with great difficxilty. As in the
case of crushed quartz-crystals themselves, it is also objected by
many glass-manufacturers that the "metal" produced from' the
crushed material tends to be "cordy" or "wavy" and to remain
" sticky " too long upon cooling, which also takes a longer time
than is desirable. Whether this is the result of the mixture of
fine grades, of the presence of two allotropic low temperature forms
of quartz, differing crystallographically, one possibly as a cement,
of the different hydration of the silica acting as matrix, or of the
presence of certain inclusions in the quartz, is not known. Greater
heat, or more prolonged melting of the batch, appears to be re-
quired when crushed rocks are used *. It is noteworthy that the
sand obtained from Muckish Mountain, Co. Donegal, Ireland, is a
naturally disintegrated pure pre- Cambrian quartzite. It is often
difficult to draw the line between a true sand and such a disinte-
grated sandstone or quartzite. The mechanical analyses on page 82
indicate, however, that it has been well-graded, probably a result
of percolating waters for a long period, helped by the fact that the
original sandstone was also well-graded, and most of the cement
has since been removed. It contains rather too much coarse
material, but this is very friable, and can be rubbed down in the
fingers, compound-grains thus breaking up. The analyses (see
also Fig. 12) should be compared with those of Guiseley material
(which was supplied sifted to 40 -mesh), Port-a-cloy Silica,
Westport Silica, etc. Even after washing and sifting, the residual
rock-particles are distributed over several grades and the mixture
is still unsatisfactory.
Among decomposed or crushed sandstones and quartzites ex-
amined were the following :
* On the behaviour of the forms of silica, see Fenner, Ainer. Journ. Science,
vol. 36 (1913) p. 331, and Jonrn. Wash. Acad. So. TO]. 2 (1912) p. 471 ; Wright
& Larson, Amer. Journ. Science, vol. 27 (1909) p. 421, and others.
MUCE:ISH MOUNTAIN SANDSTONE. 81
Muckish Mountain Sand, Co. Donegal.
Worlced by Messrs. Arkwright & Rapaport, 22 Bank Buildings,
Kingsway, W.C. 2.
Maps. Geological: Old Series (Ireland), 1-inch, Sheet 10.
6-inch, Donegal, Sheet 34.
Situation. Lat. 55 6' 20", Long. 7 59' 50" W.
The sand lies on the top and upper slopes of a hill (Muckish
Mountain) of quartzite about four miles from the sea, and about
thirty- three miles east of north of Donegal. It consists of scree
material resulting from the decomposition of the quartzite.
.Formation. Pre- Cambrian (Dalradian) .
Description. Trial- workings are being carried out to ascertain
the extent of the sand. Many pits and trenches, including one
driven twenty feet into the hillside, have now been made, and a
considerable area of rock cleared of grass, peat, and rubble. The
amount of sand still appears to be small, but the excavations have
proved the existence of several beds of considerable extent,
consisting of soft white sandstone a result of the partial disinte-
gration of the quartzite. All the chemical analyses of Muckish
Mountain material reveal the presence of a small quantity of lime
(CaO), so that it is possible that the sandstone was once cal-
careous, perhaps bearing a calcareous cement, and that the calcium
carbonate has been leached out as a result of the weathering
agencies and acid peaty waters. The rock is seen in all stages of
decomposition, from hard flinty quartzite to a friable sandstone
which can be broken up in the fingers. The quantity of actual
unconsolidated sand present is very limited.
As the seams of soft rock occur immediately below the flat top
of the mountain, over two thousand feet above sea-level, it is
probable that much of the soft rock will be reduced to sand in the
process of running it down the shoots to the foot, However,
a certain amount of the material will not be broken up in this way
and will require crushing. (See Plate IV. figs. 3 & 4, which show
the manner of cementation of the grains.) Owing to the softness
of the cement, this will not be a difficult or expensive matter.
Screening is also necessitated, since the crushed and decomposed
products contain coarse compound grains which remain as "stones"
in the glass made from the rock. Washing is desirable to assist
the grading by clearing the sand of fine dusty silica, etc., and to
reduce the iron-content of the browner varieties. The available
water-supply is small, especially in the summer.
The chemical analyses, of some samples of the rock recently
collected are as follows :
Bulk sample, mixed from all the trenches.
SiO., .................. 99-55 per cent.
Fe,0, ............... 0-02
CaO ' ................. 0-20
Mg-0 ............... trace
Loss on ignition ... 0-16
Total ......... 100*10 per cent,
Iron-content.
Trench 1 0-028 per cent.
2 0-022
3 0-009
CRUSHED ROCKS.
The brown colour of many specimens is due to staining by peaty
waters and is not detrimental. One such brown variety contained
only 0*029 per cent, of iron oxide (Fe a O s ).
Mechanical analyses of the same samples are as follows :
vos.
OS.
MS.
FS.
s. c.
S.
>1
>0-5&
>0'25&
>0'1&
>0'01&
<0-01
Total sd.-gr, :
mm.
<1 mm.
<0'5.
<0'25.
<o-i.
mm.
>0'1 mm.
Trench 1 ...
2-5%
72-3 %
19'9 %
3-0 %
1'8 %
95-2%
2 ...
2-0 %
14-7
73-9
7-9
0-5
1-0
98'5
2a...
9-8*
73-1
15-8
0-8
0-5
98-7
3 ...
2-5
13-6
75'4
7-5
1-0
o-o
99-0
A fine seam .
0-3*
36-7
58-3
3-2
1-5
95'3
* Compound grains.
The rock contains a very small proportion of heavy detrital
minerals, little else but zircon being present. The sand was used
by the Irish Department of Agriculture in the reproduction of
Waterford Glass for the Cork Exhibition in 1902. Good glass has
also been made from it in the London, Birmingham, and Yorkshire
.areas.
The price at which this material is to be supplied has not yet
been fixed. Should it not be low enough to enable the sand to
replace foreign supplies in England, we may still be assured, in the
Muckish Mountain deposit, of a large supply of material of excellent
quality, sufficiently good for the making or the best optical glass.
The nearest port is Ballyness, six miles from the foot of the hill.
The Donegal Eailway runs about a mile from the foot, and the
port of Dunfanaghy is six miles distant.
Crushed Sandstone from Guiseley, near Leeds.
Worked by The Guiseley Ganister Company.
Maps. Geological : Old Series, 1-inch, Sheet 92 S.E.
6-inch, Yorkshire, Sheet 202 N.W.
Situation. Lat. 53 52' 5", Long. 1 44' W.
The quarry lies one mile west-south-west of Guiseley.
Formation. Coal Measures.
Description. The purity and high silica-content of certain
sandstones of Coal Measure age are well-known and the rocks on
that account are prized. The Guiseley rock is much shattered, and
is washed at the quarries, being supplied at present to the steel
industry. It is proposed to crush and sift the rock for glass-making.
The sifted product is free from coarse grains, but naturally is spaced
over several grades, and contains objectionable fine material. The
cost of washing, to rid the sand of' the latter, is somewhat pro-
hibitive, the price without washing varying from 15s. to 17s. per ton
even in the neighbouring Yorkshire glass-making area. However,
AXD MOLD SANDSTO2O3S. 83
certain glass-manufacturers are trying the sand. It is white,
bears only a small quantity of iron, and does not darken on burning.
The chemical analysis of the crushed rock is as follows :
SIC., ........................ 97<45 per cent.
Fe,0 3 ........................ 0-09
Cab ........................ 0-13
MgO ........................ trace
Loss on ignition ......... 0'78
Total 100-21 per cent.
An un crushed sample of rock yields the following analysis :
Si0 2 98-93 per cent.
AU). } : 0-60
Fe^O 3 0-03
CaO 0-24
MgO none
Loss on ignition 0-29
Total 100-09 per cent.
The greater amount of iron in the crushed sample is therefore
presumably due to additional impurity obtained from the crushers.
The mechanical composition, after sifting to 40-meshj is :
>0-5 & <1 mm., 0-1 % ; >0-25 & <05, 40-1 % ; >0'1 & <0-25,
44-3 % ; >0'01 & <0-1, 9-2 % ; <0-01 mm., 6'3 %. Total sand-
grade, >0-1 mm., 84'5 %.
? j?. s A j
l' 40-1' 44-3' 9-2' 6*3 ; 84-5'
The mineral composition indicates the presence of very rare
felspar, a colourless flake of garnet (?), anatase growing on ilmenite,
abundant small red-brown rutile, zircon, limonite, leucoxene, etc.
Sandstone from Mold, Flintshire.
Worked by The Mineral Milling Company, Mold.
Maps. 1-inch Geological, Sheet 79 S.E.
6-inch Flintshire, Sheet 13 N.W.
Situation. Lat. 58 10' 20", Long. 3 11' 12" W.
The mine occurs at Waen, immediately north of the Smithy,
one hundred and fifty yards north of Trinity Church and about two
miles west of Mold.
.Format ion . Carboniferous Limestone.
Description. The bed of white sandstone is about twenty- three
feet thick and occurs below a bed of Carboniferous Limestone,
which in the shaft is about twenty-two feet thick. Impure
limestone also occurs below the sandstone. At present the rock is
84 CRUSHED HOCKS.
mined and brought up the shaft, but a drift is being run eastwards
from the surface down to the working. The sandstone is of good
colour \\ith little or no iron-staining. It is constant in quality and
grade, and is soft and easily crushed. After ignition, the colour
remains unchanged. The unwashed product contains only 0-024 per
cent, of iron oxide. The washed product has the following chemical
composition :
SiO, 98-97 per cent.
Al,6 a * 46
TiO, 0-04
Fe 2 s 0-02
CaO 0-10
MgO 0-07
K 2 0-08
Na^O none
Loss on ignition 0*34
Total 100-08 per cent.
The crushed material is fairly well-graded, as the following
result of a mechanical analysis indicates :
>0-5mm.&<lmm. 5 9'2 % ; >0'25 & <O5, 78'1 % ; >01 & <0'25, 10'5 % ;
>0-01 & <0'1, 0-9 % ; H)1, 1-3 %. Total sand-grade, >0-1 mm.,
97-8%.
? 5! JL S JL _2_ J? .1
2' 78-1' 10'5' 0-9' 1-3' 97*8 J
Washing improves it by removing the fine dusty material.
The heavy detrital minerals form a very small percentage of the
whole (0-01 per cent.). The assemblage includes only the stable
commonly-occurring detrital minerals, such as magnetite in well-
shaped crystals, ilmenite altering to leucoxene, and with crystals of
anatase growing upon it, tourmaline in bluish, greenish, and brown
grains (all O'l to 0'2 mm. diameter), together with tiny zircons
and rutiles (0-05 mm. diameter). The sandstone also contains-
decomposed felspar.
The material is utilized in the manufacture of abrasive soaps,
but should also be of much value for glass-manufacture and for
refractory purposes.
Two miles of good road connect the mines to Mold Station
(L. & N. W. Railway), where it is put uncrushed F.O.R. at
17s. 6^. per ton. The crushed product can be similarly supplied
at about 20s. to 22s. per ton.
The available resources are over ten million tons.
The deposits of sandstone at Pant du and Minera are similar in
character to that described above, but are on the whole less pure.
The highly siliceous ^ sand " from Mow Cop in Cheshire is of the
same character and is worked for pottery purposes (see pages 155
and 161).
SPITAL SANDSTONE. 85
The pulverized material obtained from the cutting and dressing
of sandstones of Millstone Grit age at Eowsley, in Derbyshire, is
used for the making of common bottle-glass in Derby.
"SpitalSand."
Worked by Mr. H. A. Walker, 13 Imperial Buildings, Exchange
Street East, Liverpool.
Maps. Geological: Old Series, 1-inch, Sheet 79 N.E.
6-inch, Cheshire, Sheet 13 S.E.
Situation. Lat. 53 21' 5 ', Long. 3 1' 45" W.
The quarry is situated at Higher Bebington, near Spital, half a
mile south-south-west of the Church, and over one mile west-south-
west of Bebington Railway Station.
Formation. Keuper Waterstones.
Description. About thirty to forty feet of creamy-white, soft
sandstone are exposed in a large quarry, showing strong faulting on
the western side. Like many of the Keuper deposits, the sandstone
is felspathic, much of the orthoclase felspar having decomposed to
kaolin -like material. The sandstone, which is easily crushed,
therefore yields a poorly-graded deposit. Washing would effect a
considerable improvement in the sand, so far as glass-making is
concerned.
In its present state it is used for making pale bottles (Dublin,
Belfast, etc.), and as a refractory material in the iron, steel, and
copper industries.
Although the grains are coated in part with white clayey matter,
the sand, which is about equal in colour to that of Lynn, darkens
on burning. The chemical composition is as follows :
SiO a 94-60 per cent.
Al.,0., 2-99
Fe"0 3 0-06
CaO 0-20
MgO 0-14
K 2 1-44
Na 2 none
Loss on ignition O65
Total 100-08 per cent.
Another sample, after being washed, showed an iron-content of
0-09 per cent.
Although the clayey matter is objectionable, there is little doubt
that the alumina present strengthens considerably the bottle-glass
made from the sand.
The mechanical analysis is as follows :
>0-5 & <1 mm., 0-7% ; >0-25 & <0'5, 81-7% ; >0-1 & <0-25, 13-6%
>0'01 & <0-1, 1-4%; <0-01, 2-6%. Total sand-grade, > 0-1 mm.,
96-0%.
r^ -? - . . s - ~i
|_0-7' 81-7' I3 7 6 5 1-4' 2-6 ; 96-6 J
86 CRUSHED HOCKS.
The microscopic examination of the rock indicates that the
heavy minerals are remarkably well-rounded, but that the variety
among the commonly-occurring minerals is not great. A. little
magnetite is found, but ihnenite (0-2 mm. in diameter) is much
more abundant, fellow-brown, highly rounded grains of tour-
maline are veiy plentiful (0'2 to 0*3 mm.), and characteristic deep
blue and purplish grains occur. Tiny zircons and rutiles (0*1 mm. ) ,
and yellow to colourless anatase crystals (0*1 mm.) also are seen.
The heavy detrital residue amounts to 0'06 per cent..
The crushing strength, tested on 3-inch cubes (average of four
tests) is 1450 Ibs. per square inch.
The price is 7*. W. per ton F. O.E. at Spital Station (L. &N.W.
& G.W. Joint Railway), and 9s. 6d. F.O.B. at Birkenhead.
The available resources are over twenty million tons.
Sand from Caldwell, tf.B.
Worked ly The Caldwell Sand Company Ltd., per Mr. Wm. F.
Pirrit, 96 Eenfielcl St., Glasgow.
Maps. Geological, 1-inch, Sheet 22.
6-inch, Renfrewshire, Sheets 15 N.E. and 16 N.W.
Situation, Lot. 55 46' 15", Long. 4 29' 0" to 20" W.
Several quarries occur on the south-east side of the Barrhead
Eoad, nearly a mile north-east of Caldwell Station (Glasgow &
South Western Railway). The quarry at present being worked is
the most westerly of them-.
Formation. Carboniferous Limestone Series.
Description. The quarry exhibits about twenty to thirty feet
of soft decomposed sandstone of variable colour, from cream to red-
brown. The strata dip north- westwards towards the road, and
shale is revealed in the bottom of the quarry, underlying the
sandstone. Pebbly seams occur, and in parts the sandstone is coarse
and not well-graded.
On ignition the sand darkens slightly to a brown tint. The
chemical analysis of an unwashed sample of the best material
available for glass-making is as follows :
SiO 2 , 93-74 per cent.
A1 2 3 4-11
EeoO'a 0-04
CaO 0-27
MgO 0-12
K,0 0-46
Na.jO 0*03
Loss on ignition 1-37
Total 100-14 per cent.
Another washed and screened sample contained 0-08 per cent,
of iron oxide.
The mechanical analyses of washed and unwashed samples
(collected at different times) are as follows :
CALBWELL AND KILWHTNTNG SANDSTONES.
87
i
OS.
MS.
FS.
s.
c.
S.
>0-5 &
<1 mm.
>0'25&
<0'5.
>0-1 &
<0-25.
>0-01 &
<0-1.
M)1
mm.
Total sand-
grade :
>0'1 mm.
Unwashed ...
5'5 %
82-9%
5-8%
1-1 %
4-7%
94-2 %
Wasted
21-0
69'4
8-9
0-5
0-2
99-3
The mineral analysis indicates the abundance o large pink and
colourless garnets (O5 mm. diameter) with good crystal form,
uruscovite flakes (0*4 mm.), grey tourmaline (0*1 mm.), limoiiite,
ilmenite, abundant zircon and red rutile, and, rarely, epidote. The
heavy mineral crop constitutes 0'08 per cent, of the sand.
The material is crushed in a pan -mill, washed in rotary apparatus,
and screened before being supplied to the G-lasgow steel-area.
Some of the other quarries were formerly worked for glass-sand,
but at present the output is taken entirely for refractory purposes.
The prepared material costs 10s. per ton F.O.R. at Caldwell
Station (Glasgow & South Western Railway).
The available resources are over two million tons.
Sand from Zilwinning, N.B.
Not at present being worked.
Maps. G-eological, 1-inch, Sheet 22.
6 -inch, Ayrshire, Sheet 11 S.JE.
Situation. Lat. 55 39' 33", Long. 4 44' 45" W.
The outcrops of white sandstone occur close to the south-western
end of Ashgrove Loch, near to Lochcraigs Farm, about a mile and a
half west-north-west of Kil winning Station. A less pure sandstone
of slightly different age crops out by the roadside near Bankend
Farm, north-east of the Loch.
Formation. Carboniferous Limestone Series.
Description. A considerable area of rough ground and crags
overlooking the southern end of the Loch is occupied by the
outcrop of a bed of white sandstone which is apparently over
twenty feet thick. The sandstone is white and breaks down easily
in the fingers. It looks decidedly promising for glass-making and
refractory purposes, and after being washed yields a well-graded
and pure sand, which becomes greyer on ignition.
The chemical composition of an unwashed sample is as follows :
SiO.> 98-85 per cent.
Al.,6 3 0-53
Ti6 2 ! 0-06
Fe O 3 0-02
OaO 0-11
MgO . 0-06
K 2 O trace
Na.,0 none
Loss on ignition O f 38
Total 100-01 per cent.
88
CBUSHED BOOKS.
The iron-content of another washed sample is OO28 per cent.
Some of the material is fine in grain and rather well-graded
(sample J). Other samples collected were much coarser. Mechanical
analyses are as follows :
VOS.
OS.
MS.
FS.
S.
0.
s.
>1 mm.
>0-5 &
<1 Tnnn.
>0-25 &
<0-5.
>o-i&
<0-25.
>o-oi &
<0'1.
<0-01
mm.
Total Band-
grade:
>0'1 mm.
Unwashed (a) .
13-5 %
30-0 %
54-6 %
1'1%
0-2%
0-6%
99-2 %
Washed (6) ...
0-5
92-5
5-5
0-5
1-0
98-5
[(a) and (Z>) were different, samples of sand.]
A mineralogical analysis shows the presence of ilrnenite and
leucoxene, limonite, muscovite (flakes Q'5 mm. diameter), brown
tourmaline (0*3 mm.), sillimanite, red. rutile, and zircon (O'l mm.)
among the heavy crop of minerals, which amounts to O02 per cent,
of the whole. The heavy residue of the sample examined was
rather coarse in grain.
Difficulties may arise over transport. The nearest station is
Kilwinning, hut to reach it half a mile of rough farm-track and a
quarter of a mile of fairly good road have to he traversed.
The available resources appeal 1 to he not less than half a million
tons.
Sand from Levenseat, K.B.
Worked by Messrs. J. & T. Thornton, Levenseat Quarries.
Maps. Geological : 1-inch, Sheet 31.
6-inch, Edinburgh, Sheet 10 S.E.
Situation. Lat. 55 48' 30" to 45", Long. 3 41' 40" W.
The sandstone is being worked in several quarries, about one and
a half miles east-south-east to south-east of Fauldhouse Station,
and one mile south-east of Crofthead Station (Caledonian Railway).
.The chief quarry is the most southerly and lies on higher ground
about three-quarters of a mile south of Levenseat Hamlet.
Formation. Millstone Grit.
Description. The best face of sandstone is that revealed in the
quarry on the higher ground, where a thirty -foot wall of the deposit,
practically free from overburden, is to be seen. In the lower
quarries several feet of Drift occur above the bed, and shale is met
with about four feet below the floor of the pit. In all, the workable
sandstone bed is probably about eighty feet thick and covers a wide
area. The stone, yellowish to brown in colour, has decomposed
until it breaks down readily into sand when rubbed in the fingers
or on being dropped into water. On ignition it darkens to a red-
brown tint. Much of the yellow 'or brown staining washes away
freely from the grains of quartz, clayey matter is removed from
LEVENSEAT SANDSTONE.
89
tlie decomposed felspar, and a well-graded cream-coloured sand is
yielded. On ignition the washed product becomes slightly darker.
The chemical analysis of a washed sample is as follows :
SiO a 99-46 per cent.
ALO. 0-16
TiO, 0-04
Fe 2 a 0-03
OaO 0-13
MgO none
K 2 none
Na 2 none
Loss on ignition 0*19
Total 100-01 per cent.
Before being washed, a sample of the sand was found to contain
0'07 per cent, of ferric oxide.
The result of washing is also to improve the grading veiy con-
siderably indeed, a well-graded material is produced :
OS.
MS.
FS.
s.
c.
S.
>0-5 &
>0-25 &
XML &
>0-01 &
<0-01
Total sand-
<1 mm.
<0-5.
<0'25.
<0-1.
mm.
>0-1 mm.
Unwashed ...
3-7%
88-5 %
6-0%
0-2%
1'6%
98-2 %
Washed
a few
94-3
5-5
0-1
0-1
99-8
grains.
The mineral composition of the sand calls for little note and the
heavy crop amounts to only 0-09 per cent. The most commonly-
occurring heavy detrital minerals are ilmenite altering to leucoxene,
zircon, rutile, and brown and grey tourmaline. The heavy residue
is fine-grained, the average diameter being O'l mm.
In its unwashed state, the sandstone, after having been crashed
in a pan-mill and screened, is sent to the Edinburgh district for the
making of green bottles, floats, etc. The alumina present adds
considerably to the tensile strength of the glass. Arrangements
have now been made, it is satisfactory to add, by Mr. Hugh Reid
of Motherwell, to wash the sand in tank-washers. The washed
product should be of high quality, and, as the above analysis
indicates, of great value in the steel industry for furnace purposes.
The unwashed crushed material is put F.O.R. at Crofthead
Station at 9s. a ton.
The available resources are probably over fifteen million tons.
Other Carboniferous Sandstones of the Midland Valley of Scot-
land have been worked extensively for building-stone. Among
these are the rocks from Cowle and Plean, two localities near
Stirling, Kingacavil, near Linlithgow, Grlenboig, and Hailes near
90 CRUSHED BOOKS.
Edinburgh. Most of these are soft greyish-white or pale brown
sandstones, with occasional carbonaceous layers.
The sandstone of Corallian age which is associated with coal and
oil-shale ("parrot") at Erora is greyish- white, and is fine and
regular in grain. The best exposure is in Clyneleish Quarry, half
a mile north-west of Brora, but although the rock is fairly soft, it
could not be crushed and transported to a glass-making area at
other than a prohibitive price. A certain amount of sand, the
result of decomposition of the rock, is also to be found. The
material is not pure enough for the making of good gkss-ware,
the iron-content (as Fe 2 s ) being 0-12 per cent., but it might
serve for refractory purposes.
Sand from Ballycastle, Co. Antrim.
Not at present being worked : Ballycastle Estate ; Agent,
Capt. S. J. Lyle, M.C.
Maps. 1-inch Geological, Sheet 8.
6-inch, Co. Antrim, Sheet 5:
Situation. Lat. 55 12' 50", Long. 6 11' to 6 13' W.
The exposures of cream-coloured sandstone occur in the cliff-
sections, east of Ballycastle, from "White Mine to Gobb, a distance
of about a mile.
Fwrnation. Lower Carboniferous Sandstone.
Description. About sixty feet of whitiah sandstone occur above
the Main Coal of the Ballycastle Coalfield. In the upper portion
shale bands occur, and the best sandstone material is the "post"
which forms the roof of the Main Coal. The sandstone crops out
along the shore and is visible in the cliffs at White' Mine, where it
is seemingly purest and best-graded, Griffin Mine, Gobb, and other
places. Much lateral variation in particular sandstone beds is to
be observed. The Main Coal is at present worked by Messrs,
Heckie, Aiton & Kerr (Ballycastle Colliery). In view of the
proximity of fuel, availability of machinery, and abundant water-
supply, it should be possible to work and treat this sandstone
economically. The rock is soft and easily crushed. It would
also need washing and screening. '
The sand, which is cream-coloured, becomes browner after
ignition. The chemical composition is as follows :
Si0.j 98-57 per oent.
ALO 9 0-52
TiO 0-05
Pe a O a 0-02
OaO 0-20
MgO 0-05
Z a O 0-06
Na.,0 0-05
Loss on ignition 0*42
Total 99-94 per cent.
BALLYCASTLE AND COOKSTOWN SANDSTONES.
The mechanical composition of a crushed sample is :
91
OS.
MS.
FS.
s.
0.
S.
>0'5&
<1 mm.
>0-25<fc
<0'5.
>0-1 &
<0-25.
>0-01 &
<0-1.
<0-01
TTlm.
Total sand-
grade :
. >0-1 mm.
Unwashed ...
3-3%
82-8 %
12-0%
1-1%
0-8%
98-1 %
Washed
5-3
87-3
6-5
0-6
0-3
99-1
In mineral composition, the sandstone resembles other Coal-
Measure Sandstones of the north of Ireland. The heavy residue,
forming O03 per cent, of the sand, is coarse in grain, and consists
chiefly of the stable and common minerals, zircon, rutile, limonite
(all about - 2 mm. in diameter), muscovifce (O4 mm.), and
anatase.
The railway facilities are not good (the Ballycastle Railway
links Ballycastle to Ballynioney on the Midland, N. C. I., Railway),
but a pier and a jetty are also close at hand. '
Messrs. Heckie, Aiton & Ken* propose to work the deposit at
White Mine, and the British Silica & Minerals Company Ltd.
that at Gobb. The material, being a high-silica sand, is ot value
as a refractory material (for furnace-linings, etc.) as well as glass-
making.
The available resources are undoubtedly large.
Sand from Cookstovni, Co. Tyrone.
Worked by Richard duff, Esq., Kildress House, Cookstown.
Maps. 1-inch Geological, Sheet 26.
6-inch, Co. Tyrone, Sheet 29.
Situation. Lat. 54 38' 40", Long. 6 47' 0" W.
The pit is situated in the townland of Lower Kildress about
half a mile east of Kildress House.
formation. Calciferous Sandstone (Upper Group).
Description. About thirty feet of soft sandstones are exposed in
the pit which is by the side of the small stream known as the
Ballinderry River. The upper portion is stained red and brown, in
part as a result of the percolation of peaty waters and in part by
oxide of iron. Ferruginous bands, often wedge-shaped, also occur
lower down, but the iron oxide is not present in large quantity,
and washing frees the quartz-grains easily from the pink pellicles.
Some six or seven feet of pure white sandstones are seen. The
sandstone is thoroughly decomposed and washing in water serves to
disintegrate it. Screening, however, must be adopted to free the
product from quartz-pebbles and harder sandstone pellets.
The red sands darken in colour on ignition, and the cream-
coloured sand becomes greyer.
92
CHTTSHED HOCKS.
The chemical composition is as follows :
SiO a 96-97 per cent.
Al,0 3 1-61
Fe a 3 0-04
GaO 0-20
MgO 0-11
K a O 0-15
Na a O 0-03
Loss on ignition 0'72
Total 99-83 per cent.
- The iron -content of a washed sample of reel sand is O04 per cent.,
and of the cream-coloured sand, P 02 per cent.
Much clayey material (kaolin) is present a result of the
decomposition of felspar. After "being washed, the sand is well-
graded, as the following mechanical analyses indicate : '
vcs.
OS. ! MS.
FS.
B.
c.
S.
>1 mm.
>0-5 &
<1 mm.
>0-25 &
<0-5.
>0-1 &
<0-25.
>o-oi &
<0-1.
<o-oi
mm.
Total sand-
grade-.
>0-1 mm.
Unwashed.
1-8%
9-7%
80-6 %
4-2%
0-8%
S'4%
96-8 %
Washed ...
2-0
8-1
79-0
10-1
0-8
,0-5
99-2
,
i
The heavy mineral residue (0-03 per cent.) is fine in grain and
consists mainly of zircons (0'05 mm. diameter). Other minerals
noted were yellow rutile, anatase growing on ilmenite, and brown
and blue tourmaline.
At the present time the mixed and unwashed sand is sold for
bottle-making in Belfast at about 20s. per ton, which represents a
cost of 14s. tid. per ton at Cookstown Station. From the quarry
to the station three miles of road-transport are necessary. If the
* white sandstone were washed and screened, the material would
serve for the making of glass of much better quality. Water-power
and an abundant water-supply are available.
The resources are difficult to estimate, but are considerable.
The liability of the rocks to vary laterally introduces difficulty in
computation.
Sand from Coolieeragh, Londonderry.
On the eastern side of the Foyle, and north-east of Coolkeeragh
House, five miles north of Londonderry, a small excavation has been
opened by Mr. John Bums, the owner of the estate. Soft white
and pale-reddish sandstones are visible, apparently of about the
same age and very similar in appearance to those at Cookstown,
etc. (Upper Calciferous Sandstone). ,The same rock occurs also at
White Castle on the shores of the Foyle, but is much less accessible.
BOOKS PEOM COOLKEEBAGH AND POBT-A-CLOT.
93
The Coolkeeragh rock breaks down very easily, disintegrating when
placed in water. In its present state it serves for bottle-making,
but if washed and screened would be useful for better-class glass-
making. On ignition it becomes greyer, and the chemical com-
position of an unwashed sample is as follows :
SiO., 84-96 per cent.
Al a Oj 8-59
TiO s 0-18
Fe-jO,, 0-18
CaO 0-34
MgO 0-31
Z a O 4-54
Na a O .., 0-08
Loss on ignition 1-54
Total 100-72 per cent.
Another sample collected by the writer contained 0-13 per cent,
of feme oxide, while the content of a washed sample was 0-075
per cent.
Washing removes also the kaolin yielded by the decomposing
felspar, and results in the production of a well-graded sand, as the
following mechanical analyses indicate :
VCS.
OS.
MS.
FS.
B.
c.
S.
>1 mm.
>0-5 &
<1 mm-
>0-25 &
<0-5.
>0-1 &
<0-25.
>o-oi &
<0-1.
<0-01
mui.
| Total Band-
grade :
>0-1 mm.
Unwashed ...
M%
75-9%
7-5 %
3-0 %
6-5%
90-5%
Washed
M%
2-7
90-4
4-6
0-5
0-7
98-8
The mineral assemblage is like that of other sandstones of
similar age in northern Ireland (Cookstown, Ballycastle, etc.), the
commonly-occurring heavy minerals (which form 0'05 per cent, of
the sand) being muscovite and chlorite (flakes 0'6 mm. diameter),
brown tourmaline, small irregular and angular garnets (O'l mm.),
small zircons and rutiles, leucoxene, and plentiful anatase, in yellow
tablets or growing upon ilmenite.
The deposit is favourably situated for transport. The Midland
Kailway (Londonderry to Coleraine and Belfast) is only a few
yards distant, and the deposit is close to the Eiver Foyle.
Further exploration is desirable before the resources can be
estimated.
" Port-a-cloy Silica."
This material is apparently a decomposed or crushed quartz-mica
schist (Dalradian), and is to be worked by the China-Clay, Felspar,
96
CHUSHED BOOKS.
A compact and good quality quartzite is worked by Messrs. Win.
Wild & Sons in extensive quarries 011 Holynead Mountain, Anglesey.
It is crushed and used for the making of silica-bricks, and for
" gannister " for lining Bessemer converters, etc. In places it is
very pure, but joint-planes stained with ferruginous matter spoil it
for use in glass-making. The quartzite is of pre- Cambrian age
and frequently exhibits a foliated structure. It is traversed by
abundant quartz-veins. The chemical composition of a typical
sample of rock is as follows :
SiO g 99-32 per cent.
Al/) 3 0-19
Ti0 2 0-03
Fe 4 3 0-02
Cat) 0-12
MgO 0-08
KjO none
Na 2 none
LOBS on ignition T. 0'21
Total 99-97 per cent.
A similar quartzite, but less pure, has been worked at Forth.
Wen, near Amlwch, Anglesey.
The vein-quartz from Slieve More, Achill Island was formerly
crushed and supplied by the Irish Industrial Minerals Company,
Westport.
The chemical composition of a sample of the crushed rock supplied
(quality No. 3) is as follows :
SiO., 99-20 percent.
AijO;, 0-24
Fe a 3 0-04
CaO 0-09
MgO trace
Loss on ignition 0*23
, Total 99-80 per cent.
The uncrushed roek contains 99-51 per cent. SiO a and OOG4 per
cent. Fe a 9 . Some of the iron seems to have been introduced as a
result of crushing the material (see page 128).
The flaky form of the crushed product is seen in Plate IV.fig. 5.
Mechanical analyses of numbered samples supplied are as
follows :
OS.
MS.
PS.
s.
c.
S.
Quality.
>0-5 &
<lmm.
>0-25 &
<0-5.
>0'1 &
<0-25.
>0-01 &
<0-1.'
<0-01
mm.
Total sand-grade :
>0-1 mm.
....
0-3 %
0-7%
99-0%
0-3 %
1 ....
fewgrs.
3-5
1-8
94-7
3-5
la ....
2-0%
17-9
36-5
43-6
19-9
2 ....
0-2%
9-0
53-5
23-5
13-8
62-7
3 ....
1-0
85-5
11-6
0-4
1-5
98-1
4 ....
54-9
42-9
0-5
0-2
1-5
98-3
QTTAETZITBS AJTD TEDT-QTrAETZ. 97
Examination of the samples for heavy detrital minerals by means
of bromoform reveals the fact that, in the crushed material of
quality 3 as supplied, a large part of the crop of density greater
than 2'8 (O'l per cent.) consisted of rust-reddened metallic iron
easily attracted by a bar-magnet. Most of the remainder of
the residue consists of flakes of a greenish biaxial mica (O3 mm.
diameter) containing plates and dendritic growths of hematite.
Before the war, the No. 2 material fetched 27s. to 30s. per ton
for use in the making of abrasive soaps.
A foliated micaceous quartzite has also been worked at
Kildownet in the south of Achill Island.
At White Bock, about four miles north-west of Tinahely, Co.
Wicklow, a knob of vein-quartz occurs associated with quartz-mica
schists. The mass forms a prominent feature on the landscape, and
is at least a hundred yards long by fifty yards wide. Quarrying
indicates that it is more than thirty feet deep. The rock quarried
is a pure white vein-quartz of good quality. It is carted to Tinahely
Station by road, and thence delivered on the quays at Arklow or
Dublin. The cost at Arklow of the uncrushed rock is about 6s. Qd.
per ton, and at Tinahely Station about 4s. Qd. Crushed, rolled, and
screened material (1 inch to -fa inch) can be delivered into an
English port at from 28s. to 50s. per ton. Larger-sized material.
could be similarly delivered at about 25s. per ton.
The quartz is said to contain 99'50 per cent, of silica. The quarry
is worked by Mr. E. Page, "Woodenbridge, Co. Wicklow.
Similar vein-quartz has been supplied from near Ynyslas Station,
Cardiganshire. The crushed product is far from well-graded, and
its cost is prohibitive for glass-making.
Veins of quartz are of wide distribution among the older rocks
of the west and north of Ireland, Wales, and Scotland. They are
not often sufficiently thick or persistent to be of economic value.
Samples have been collected from Anglesey, the Lleyn Peninsula,,
Bardsey Island, and other localities.
98
CHAPTER VIII.
BBITISH RESOURCES OP GLASS-SANDS, ETC. (continued?).
B. DEPOSITS CA&RYIN& ALUMINA AND SILICA.
Alumina commonly occurs in sands and rocks used for glass-
making in the form of the mineral felspar or the decomposition
product, kaolin (china-clay), which results largely from the
.alteration of felspar. Certain rocks as, for example, those of the
Triassic and Carboniferous Systems are rich in decomposed felspars
.and contain a certain amount of clayey material. This renders their
crushed products poorly-graded, but the small proportion of alumina
present may actually be an advantage, as in the case of bottle-
making, where strength and toughness are required in the glass.
Unfortunately, most British sands bearing a high proportion of
.alumina contain also much iron, and are useless for the manufacture
of glass-ware other than common bottles.
A prejudice against alumina in sands for bottle-making was
formerly met with, but it is now slowly dying out. In rare cases
Alumina is even added to the batch for bottle-making. Dr. W. E. S.
Turner, of the Department of Grlass Technology in the University
of Sheffield, is of the opinion that, far from having a tendency to
cause devitrification, alumina if in moderate amount has just
the opposite properties and will prevent glass from devitrifying.
Experiments have shown that when alumina is added to a window-
.glass batch, the glass which is produced does not undergo devitri-
fication when heated in a blow-pipe flame. If the amount of
-alumina is high, it is possible for a clouded glass to be produced,
-as when felspar itself is used. According to the investigations of
Singer *, it is possible to add to a glass-batch containing alumina
more sand and more lime, and to reduce in proportion the amount
of alkali, thereby cheapening the cost of production.
Of the sands and rocks described or mentioned in the foregoing
pages, those from Sandymount Strand (Dublin), Parsley Hay and
Brassington (see below), Charltou, South Cave, Huttons Ambo,
and Leyenseat, carry appreciable, and sometimes large, quantities
of alumina f.
The sand from Sandymount Strand is used in the Dubh'n black-
bottle industry. To give greater "body" to the glass, broken
lumps of Bridgwater or other homogeneous brick are added to the
bajxih. The brick is red and is highly ferruginous, as the following
analysis indicates :
* F. Singer, 'Die Keramische Rundachau,' yol. v. 1915, "TJeber den
Einfluss von Tonerde anf die Sohmelzbarkeit von GHasern."
t See note on page 34 ref erring to sand from Martinroda used for ther-
mometer-glasB.
DEPOSITS .CABBYING ALTJimTA AJO) SILICA. 99
Analysis of Bridgwater Brick.
SiO, ..................... 58-20 per oent.
AlA ..................... 16-42
TiO' ..................... 1-29
Fe 3 3 ..................... 6-74
FeO ........................ 0-13
CaO ..................... 7-37
MgO ..................... 3-02
K a O ........................ 3-65
Nft.,0 ..................... 0-93
C0 2 ........................ 0-13
P.,0, ..................... 0-07
MiiO ..................... 0-08
LOBS on ignition ......... 2-50
1 [HjO flJid carbonaceous
matter.] ' -
Total ......... 100-53 per oent.
The addition of the brick increases the depth of colour of the
"bottles, and undoubtedly strengthens them by toughening the
glass a result of the addition of the 16 per cent, of alumina.
"This is a distinct advantage where the bottles have shoulders and
.are required to stand considerable pressure from contained gases.
In the St. Helens district a baked clay is added to the batch for
the same purpose. A partial analysis of such a baked clay from
.Messrs. Nuttall's works is as follows :
SiO., ..................... 63-99 per cent
AlA ..................... 15-17
TiO a ..................... 0-65
Fe,0 3 ..................... 6-13
Total ......... 85-94 per cent.
" Spital sand " is used for bottlfc-raaking, and contains almost
:3 per cent, of alumina. The sand from Worksop is similar in
mineral composition and might well be more extensively used in
the bottle industry of Yorkshire, which is located close at
hand.
Eaglescliffe " sand," mentioned in Chapter X., is a chemically-
treated rock of the same age. The iron-content has been very
much reduced (see analyses), but the alumina, forming 3'51 pe*r
cent., has been retained. The Stiper Quartzite and the Appin
Qtiartzite are felspathic, and in consequence contain about 2 per
cent, each of alumina. The Port-a-cloy rock has already been
described (page 93) and, contains, before washing, 12'66 per cent.
of alumina. A washed material from it contains still -23 per
cent, of iron oxide (Fe.,0 a ) and 11'57 per cent, of alumina.
Kaolin-bearing sands ancl crushed rocks cannot be washed to
reduce the iron-content without loss also of the alumina (see,
-for example, the analyses of Huttons Ambo sands on page 65 :
before washing, 8'68 .per cent. Al.jO n , 1'28 per cent. Fe a 3 ; after
-washing, 0-84 per cent. Al a 3 , 0'03 per cent. Fe,0 3 ).
ir 2
100 -DEPOSITS CAERYINa ALUMINA. AND SILICA.
In addition to the a"bove, the following alumina-bearing sands*
and rocks may be mentioned :
(fl) SANDS, CLATS, ETC.
Kaolin, as prepared in Cornwall and Devon from the altered and
decomposed granite, is used in glass-making where resistant or
tough glasses are required. It is added to the batch in the usual
way, but since it is a refractory body, greater heat is required to
get it into solution than is usually required in glass-making.
Moreover^ aggregates of the mineral sometimes form and are
difficult to melt up. They tend to remain as "stones." Any
natural sandy deposit therefore which is low in iron-content and
rich in kaolin, and has its sand-grains coated evenly by the latter,
is of considerable value for particular glasses such as those used for
chemical and pharmaceutical purposes (laboratory apparatus, com-
bustion tubing, thermometers, ampoules, etc.). Such materials
cannot, of course, be well-graded.
The kaolin resources of England have been carefully described
in detail by J. Allen Howe, in a Memoir of the Geological
Survey, " A Handbook to the Collection of Kaolin, China-Clay
and China-Stone in the Museum of Practical Geology " (1914).
Since the production of the Handbook, fresh but smaller resources .
have been discovered at Holyhead Mountain, Anglesey (worked by
W. Wild & Sons Ltd., Brassfounders, Liverpool St., Sheffield), and
Port-a-cloy, Co. Mayo (The China- Clay & Felspar Company Ltd.,.
Dublin), as well as a few other localities.
In the preparation of china-clay (of theoretical composition-
Alp., . 2Si0 4 . 2H 2 0), great care is taken to eliminate all micas, etc.,
partly because of their coarseness and partly because of the alkalies
and alkaline eai-ths in their composition which render the clay
less refractory. For glass-inanufacture the small quantity of
alkalies in the settlings known commercially as "micas" is not
objectionable and may even be advantageous. An analysis of
" coarse micas " mechanically separated at the Standardised China-
Clay Company's Works at Eoche, Cornwall, is as follows :
SiO., 48-18 per cent.
. AlA 36-14
Ti0 2 ' : 0-15
Pe,0 3 0-98
Cat) 0-13
MgO 0-28
K,0 2-12
Na.,0 0-23
* Loss on ignition H'98
Total 100-14 per cent.
The tips of rejected coarse material from the kaolin workings in-
Devon and Cornwall contain high silica and .fairly high alumina- -
content. The tourmaline could be extracted by electromagnetic-
SANDS. 101
means, and the alumina, is mostly present as micas, kaolin, and
partially decomposed felspar. The deposits are poorly graded, con-
taining much coarse quartz and felspar. It is a pity the material
cannot be made use, of ; sands with a good proportion of alumina
.are desirable for certain glass-work, and a market is badly needed for
the rejectamenta from the kaolin-works. The material is utilized
for the making of refractory bricks.
Refractory Sands, etc., of Devonshire.
^The deposits occur in two well-marked basins, south and north
of Dartmoor respectively. The basin of Bovey has long beeii
known and has frequently been described and discussed*. Kaolin-
bearing sands and fireclays, associated with lignites, have been
worked on a large scale at Heathfield, and also near Newton'
Abbot. For the greater part, 'the sands bear too much tourmaline
(boro-silicate of aluminium and iron) to be of use for glass-making,
-and the electromagnetic separation of the mineral would prove too
expensive. The deposits are of considerable value for refractory
purposes.
The second basin occurs north of Hatherleigh and south of
Tomngton, in North Devon, and has not yet been described in
detail. In recent years, large open-cast workings and mines have
been made in order to obtain the peaty clays and clayey sands for
the making of fire-bricks and for pottery purposes. The material
is kaolin-bearing and undoubtedly derived from the Dartmoor
Granite. A chemical analysis . .of , .Torrington sand is given in the
Table on pige 157.
Sands, etc., from St. Agnes, Cornwall.
Sands of white to yellowish colour, felspathic and kaolin-bearing,
occur in association with refractory clays near St. Agnes Beacon,
Cornwall. The deposits, which occur on the 400 ft. platform, are
believed to be of Pliocene age. They have been used as refractory
materials, but are of limited extent and thickness. The principal
pits are close to Beacon Cottage, one mile west-south- Avest of the
Church and half a mile north of the Beacon (west and west-north-
west of the Church). The best whitish sand occurs below red
sand and " candle " clays. The material can be shipped from
Trevanaunce Cove or Chapel Combe near by, or carted to St. Agnes
Station (two miles). The resources of the area would very soon be
exhausted.
Kaolin from Anglesey. ^
On Holyhead Mountain, Anglesey, several dykes occur in the
pre-Cambrian quartzite (see page 96). They have a north-south
strike J and vary in width from about twenty feet to a very small
* See, for example, Mem. Geol. STLTV., "The Geology of the Country
around Newton Abbot" (Sheet 339), 1913.
102 DEPOSITS CARHTI>'Q ALUMINA AJU? SILICA.
amount. It is difficult to say what the original rock of these dykes;
has "been. In places, the clay now tilling them is somewhat sandy,
hut in others the clayey material is so pure as to discounfcenance-
the suggestion that they were originally rnicrogranite. The
presence of- quartz- veins in the adjacent rock, and at times the-
abundance of limonitic matter in the ctykes, together with plentiful
evidence of alteration of the quartzite walls of the veins and dykes,
suggests hydrothennal action and that the dyke'-niaterials in their
present form may he secondaiy in origin. The dykes at present
being worked occur in Messrs. Wm. Wild & Sons' quarry, where
the clay has heen used as a hinder for the broken quartette in-
making " gannister " for lining steel-converters. A very good
grade kaolin has been washed out of the material from another
of these dykea. The chemical composition of a sample of the raw
material, which is a clayey sand, is as follows :
SiO, 94-90 per cent.
Al.,0., 2-31
Ti0 ' 0-45
FeCf 0-48
Fe 3 0., 015 .
CaO.' 0-13
MgO 0-12
K.0 0-74
Na a O 0-02'
MnO tnwe
Loss on ignition 0'68
- Total 99'98 per oent.
The alumina-content of this sample is surprisingly low. It
probably cannot be taken as typical.
The Refractory Sands of Derbyshire and Staffordshire.
The irregular accumulations of sands and clays which occur in
hollows in the surface of the Carboniferous Limestone district of
Derbyshire and Staffordshire are well-known on account of their
highly refractory character. They have been mentioned by Greo. Maw,
J. Allen Howe, Dr. A. Strahan, and others, but no systematic account
of them seems to have been written. At present they are utilized
for the making of high-class silica-bricks, when variability in
iron-content, up to several per cent., is not detrimental. Selected
deposits of white to cream-coloured sand or clayey sand might be-
of considerable value for glass-making, but the* available resources
are very limited and it will be difficult to keep to sample.
Tflese kaolin -beaiing sands are free from alkalies, lime, etc.,
and at times cany very little iron oxide. They are worked at
Carsington Pastures, near Harborough Bocks, at Longcliffe, Low
Moor, Friden, Blake Moor, Parsley Hay and Alsop en le Dale in
Derbyshire, and also at Eibden in Staffordshire. The hollows,
are clean-sided, with fresh limestone walls, steep and sometimes.
SANDS FROM DERBYSHIRE AND STAJETOJIDSHIRE.
overhanging. The limestone displays no evidence of ordinary
weathering. Signs of stratification are visible in the material
filling the hollows ; the association is not turbulent as described,
but appears to yield evidence of a definite order related to the;
succession of the Triassic sediments, which at one time were con-
tinuous over the whole district. Bunter Sandstone, the Pebble-bed,
Keuper Marls, and black shale probably belonging to the Bhsetic,
have foundered into the hollows. The oldest deposits occur nearest
the walls of the basin. The various sediments have suffered a
curious alteration, characterized by the production of kaolin
material and the almost complete elimination of alkalies and alkaline
earths. The appearance of the workings, especially of the white
deposits of the central and deeper portions of the basins, is strikingly
similar to that of the china-clay pits of Devon and Cornwall. One
area at least reproduced the conditions of the Bovey deposits indeed,
Geo. Maw noted the similarity long ago, lignites, pipe-clays, and
refractory sands indicating the filling up of a swampy hollow ^with
vegetation and kaolin-mud at a time when the bulk of the Triassic
rocks had been removed, but when foundering was still hi progress.
Chemical analyses of some of the purest of these deposits are :
Parsley Hay. Brassington. Ne-wnaven.
SiO
. 74-64
18-04
TiO ""
, n.d.
Pe.,0, ,
0-05
CaO ,
a-19
MgO
none
E Q
. n. d.
Na a O
. n.d.
Loss on ignition . , .
. 7-24
Totals
100-06
90-40
6-56
n. d.
0-18
0-16
trace
n. d.
n. d.
2-48
99-78
98-17 per cent.
a- 71
0-42
0-025
0-11
0'07
0-09
0-02
0-41
100-025 per cent.
The composition of the Parsley Hay material corresponds to a
mixture of about 53 per cent, of pure silica sand, and 45 per cent,
pure kaolin (of composition A1 2 S . 2SiO a . 2H a O).
Mechanical analyses of some of the deposits, whieh are neces-
sarily not well-graded, since they are clayey sands, are :
OS.
MS.
IB.
8.
0.
S.
>0-5 &
>0-25 &
>0-1&
>o-oi &
<o-oi
Total sand-grade;
<1 mm.
<0-5.
<0-25.
<o-i.
mm.
>0-1 mm.
Parsley Hay ...
0-3%
20-2 %
35-7%
18-5 %
80-8 %i
56-2 %
rassington ...
1-5
71-4
11-8
os. 2 ' 1 fs.
13-2
84-7
>0-05.
<0'05.
Bibden
4-6
43-6
23-8
0-6
10-5
16-9
72-0
Newkaven
0-2
49-9
30-4
l-o
10-9
7-6
&0-5
Longoliffe
2-2
58-6
23-7
0-7
5-2
9-6
84-5
Oaraington ...
2-0
68-7
11-0
0-8
4-1
18-4
76-7
104 DEPOSITS CULRBYING ALUMINA A3TD SILICA.
' The mineral assemblages of certain of the deposits include well-
Tounded grains of heavy minerals. Among the species noted were
anatase, apatite, cassiterite, epidote, rutile, spinel, staurolite, and
zircon.
Deposits in North Wales.
Similar materials, but more siliceous and apparently derived
also from Millstone Grit or Carboniferous sandstones which
have long since been worn away, occur in the surface of the
Carboniferous Limestone areas of Flintshire (Haliyn, Rhes y cae,
Pant du, etc.), Denbighshire (near Llandudno and Afoergele), and
Carnarvonshire (Conway, etc.). Analyses of some of these
deposits are given in the Tables on pages 157 and 164. With the
possible exception of Abergele, they are of small extent and for the
most part not now worked.
In the recent quarrying of the limestone at Kinmel Park Camp,
near Abergele, a fair amount of this material seems to have been
exposed. The quarry, however, has since been partly filled in, and
little can be seen except clayey matter which is reminiscent of the
Derbyshire deposits and may be derived from the Trias. Indications
.are seen all over the area of similar deposits and of likely hollows,
.and explorations might reveal supplies of . valuable refractory
materials. The white sand from Abergele (Kinmel Park) forwarded
to the writer by Mr. E. D. Griffith of Bethesda, is rather sugary in
character, containing many compound grains. It may have been
derived from the Millstone Grit, and is much less aluminous than
most of the other deposits mentioned. Its chemical composition
is :
Si0 3 99-35 per oent.
ALA 0-54
Fe 2 3 0-04
loss on ignition .- 0'36
Total 100-29 per cent
Alkalies and alkaline earths not determined ; probably absent.
It is of a good white colour and does not change on ignition.
The mechanical analysis indicates that treatment by washing and
screening would improve it :
>1 mm., 2-6 % j >0'5 & <1 mm., 8'8 % ; >0-25 & <0'5, 77'7 % ; >0-1 &
<0-25, 8-6 % ; >0-01 A <0'1, 2'3 % ; <0'01, none. Total sand-grade,
> 0-1 mm., 97-7%.
BCS OS _MS_ FS ' _s_ _c_ S ."I
6 ' 8-6' 77-7' 8-8' 2-3' O'O ' 97'7 J
The detrital mineral residue is very small in amount (O'Ol
per cent.) and shows the presence of minute zircons and rutiles
SANDS FEOM MtJETH WALES. 105
(0'02 to 0'05 mm. in diameter), ihnenite and limonite, anatase, and
muscovite flakes (0'4 mm. diameter).
Without further exploratory work, no opinion can be given as to
the available resources. In any case, the material has no great
areal extent; it merely occupies hollows and cracks in the
Carboniferous Limestone.
106 SILICEOUS HOCKS BEABIN-G ALUMINA AND POTASH.
OHAPTEK IX.
BEITISH RESOURCES or BOCKS USED IN GLASS-MAKING
(FELSPABS, ETC.).
SILICEOUS BOCKS BEABLN& ALUMINA AND POTASII.
Although large quantities of rocks rich in alumina and silica
occur in the British Isles, few contain little or no ferruginous
material. The otherwise pure felsites and rhyolites are open to
this objection. The chief rocks, therefore, which may be of value
to the glftss-manufacturer are pegmatites, aplites, rniorogranites,
and modified granites free from iron-bearing minerals. Some
likely-looking rocks were analysed and yielded the following
results :
(1) (2) (3)
SiO, 80-12 82-88 78-84 per cent.
ALA 10-68 9-39 10-50
0-14
0-26
0-33
0-20
0-07
8-65
0-41
0-03
0-02
0-57
0-10
trace
none
n. d,
0-23
TiO a
-0-09
0-15
,PeO
0-49
0-56
Ee
0-06
0*22
Oab'
1-01
0-09
MgO
0-63
0-20
K a O
1-42
1-88
Na a O
3-44
3-98
BaO
0-01
trace
MnO
0-05
0-01
H 3 0+
0-80
0-48
H 2 0-
00,
0-28
1-20
0-13
01.., trace
P a O B
trace
none
ZrO 2
0-03
0-02
S
0-09
none
100-40
99-99
Leas f or S , . , ,
0-03
'
100-35 per cent.
08
Total 100-87 100-27 per cent.
(1) Granophyre from Brandy Gill (Carrook Pell Syndicate Co.).
(2) Pelsite from Wioklow, H. 5.
(3) Tramore (Waterford), C 2.
Other partial analyses are given in Table III. page 168. These-
analyses are given as fairly typical examples of what may be
expected, so far as glass-making is concerned, in rooks of this,
character. The iron-content is too high for good glass-making.
The best and most accessible British rocks of this kind
(pegmatites, aplites, etc.) are mentioned below. They generally
occur as dykes, that is, more or less narrow parallel-sided sheets of
rock intruded into other rocks, usually standing almost vertically..
The outcrop of such rocks at the surface is rarely more than
CORNISH FELSPARS. 107"
a hundred yards wide, and is often only a few feet, but it may
be of considerable length, and the rock may extend to a great
depth.
The pegmatites consist mainly of quartz and felspar crystallized
together. The felspar may contain potash, soda, and lime. Those-
rocks which bear potash are most in demand by the potter and
glass-manufacturer, and have therefore been investigated more-
fully.
Felspar is chiefly used in the glass- industry of this country in-
the manufacture el chemical ware, being imported for the purpose-
from Norway and Sweden. Owing to the fact that felspar is-
usually delivered in the form of either pegmatite or graphic granite,,
the exact composition of the rock is always liable to vary in
successive consignments. The use of kaolin (china-clay) is open
to the same objection, but to a smaller degree. For the best
qualities including optical glass, where, however, the requirements-
of raw materials other than sand are relatively small in amount, it
is found advisable to add the soda, potash, lime and alumina, in a
form of purity and in the required proportions. For second-grade-
glass-ware, the use of felspar is a convenient and cheap means of
adding both potash and alumina. Care must be taken, of course, to-
ensure that the iron-content of the felspar-rock is low (as it is
in many British pegmatites). Little use is made of felspar at the-
present time in the bottle-trade. As already mentioned, the
requisite alumina-content is obtained in rough work by the addition,
to the batch of brick, baked clay, or even raw ball-clay. For flint-
glass bottles, pale bottles, etc., where strengthening and toughening 1
are required, china-clay is sometimes used. British felspars, if
properly worked, should be cheaper to procure than foreign material,
and might be used with advantage much more extensively.
Potash. Felspars.
The chief potash-bearing felspars which occur in Great Britain'
(but not in Ireland) have already been dealt with in one of the-
Special Eesources Memoirs of H.M. Geological Survey*, recently
issued. One at least of .those described, besides others not mentioned,
are at present being worked.
The following account includes notes on Koche felspar additional
to those published.
Felspar from the old quarry of Tresayes, near Koche r
Cornwall.
The following description of the deposit is given in the Memoir
of the Geological Survey upon Bodmin and St. Austell, 1909-
(pages 61, 62) :
" At Tresayes Downs there is a wide extremely coarse pegmatite
vein in the Killas a few yards from the margin of the granite. It
* " Special Reports on the Mineral Besouroea of Great Britain. Yol. T.
Potash. Felspar, etc." Mem. Geol. Survey, 1916.
108 SILICEOUS HOCKS BEAHING ALUMINA. AND POTASH.
consists mainly of enormous orthoclase crystals, 'roughly parallel
and arranged vertically, some of which are graphically intergrown
with quartz. Some quartz occurs interstitially, frequently asso-
ciated with tourmaline and a little fluorspar. There is also a little
pale mica. The vein has a north and south direction nearly
parallel with the margin of the granite at this pkce, and is nearly
50 yards in width. The vein was formerly worked for felspar for
use in glass-making, but the work was abandoned about 1880."
Some half-a-dozen trial holes have recently been put down and
the rock proved over an area one hundred yards long by fifty yards
wide. At the time of the writer's visit, the pegmatite was visible
in the old quarry to a depth of about ten feet, the bottom being
occupied by water. The pegmatite is rather iron-stained along
joint-planes and contains crystals of tourmaline. For glass and
pottery purposes, the felspar is hand-picked. The best means of
transport is down the small valley to Carbis siding. A mineral line
already extends almost up to the quarry, which at the time of
writing has once more been opened up. Good-quality felspar is
being extracted.
The f ollowing are analyses of Roche felspar :
(1) ' (2) - (3) (4)
SiO, 65-00 65-33 62*98 64-21 per cent.
AljO., 19-00 19-16 18-92 19-66
Pe^Oa 0-50 0'50 1-18 0-18
CaO 1-57 1-68 0-75 0'35
MgO tr. tr. 0-36 0-07
K 2 10-87 10-37 11-68 12-35
Na,0 2-40 2-40 4-18 2-79
H 2 0-83 0-50 0-30 0-73
Totals... 99-67 99'94 100-35 100-34 per cent.
(1) & (2) J. A. Phillips, Phil. Mag. Feb. 1871.
(3) W. Orossley, 281 Dunstan's HU, E.G.
(4) Dr. H. P. Harwood. Analysed -with especial regard to gla.BH.Tna.1rmg
requirements. No titanium or barium was present.
'The quantity of iron in (3) may be due to included tourmaline
crystals.
The chemical analysis (4) corresponds to the 'following approxi-
mate mineral composition (percentage weights by calculation) :
Potash-felspar 73'18 per cent.
Albite (soda-felspar) 28-67
96-85
Remainder (mainly quartz) . . . 3-49
Total 100-34 per cent .
Other dykes of pegmatite are now being opened up at Kemick,
near Trevisco, and on Trelavour Downs. Chemical and mineral
analyses of these deposits will be found in Table IV., page 160,
SCOTTISH FELSPABS. 109
Felspar from Pegmatites occurring in Scotland.
A fairly full account of the most accessible pegmatite veins in
Scotland has been given in the memoir cited*. The veins at three
localities (1) between Lochs Laxford and Inchard, (2) between
Durness and Eriboll, and (3) at Overscaig, Loch Shin, are described
in detail with accompanying sketch-maps for the first and second
localities. The veins at the first two places occur in the Lewisian
G-neiss in the extreme north-west of Scotland, where the working
conditions and questions of transport leave much to be desired.
The Overscaig pegmatite occurs in the Moine Schists and is also
difficult to work from rail or boat. The estimated resources
from the most accessible veins at the first locality mentioned are
not less than 190,000 tons. At the second locality, not less than
twelve million tons of pegmatite are available.
A chemical analysis of the rock from the third locality is given
as follows :
Si0.j 72-94 per oent.
ALfl, 14-26
TiO a 0-06
FeA 0-21
FeO 0-22
(CoNi)O nt.f<L
OaO 0-23
MgO 0-08
E 2 7-42
Na a O 3-49
Li 2 trace
BaO 0-25
H.,Oatl05C 0-05
H a O above 105 C. ... 0-17
P a O, 0-49
MnO 0-11
FeS. nt.fd.
C0 a " 0-06
Total 100-04 per oent.
E. G. Eadley (Anal.).
Calculation from this analysis gives (percentages by weight) :
Miorocline 43-96
Albite 29-61
Felspar 73-57
Minor Constituents . . . 2*38
Quartz 24-09 by difference.
Total 100-04 per cent.
Chemical analyses carried out by Dr. Harwood, with especial
reference to the requirements of the glass-industry, of samples of
* " Special Reports on the Mineral Besourees of Great Britain. Vol. v.
Potash Felspar, etc." Mem. Geol. Survey, 1916.
110 SILICEOUS BOCKS JBEAltlira ALUMINA AND POTASH.
Scottish pegmatites collected by the writer may be added for
comparison :
(1) (2) (3)
Bi0. 2 69-05 71-53 70-36 per cent.
Al,O 3 16-84 15-33 15-97
Ti6 2 none trace none
IV> 3 0-07 0-05 0-08
CaO 0-21 0-28 0'12
MgO 0-06 0-15 0-08
Z a O 10-08 10-43 10-42
Na,0 2-83 1-91 2-19
BaO 0-12 0-60 0'53
Loss on ignition 0-42 0-21 0*29
Totals 99-68 100-49 100-04 per cent.
(1) From the exposure on the shore of Loch Shin, a little more than
600 yards south-east from Overscaig Farm.
(2) From a vein 300 yards north of Badcall Pier, about a mile north-west
from Laxford Bridge, Sutherlandshire.
(3) From a thick belt of veins on the north-west slope of Beinn Oeannabeinne ,
near Durness, close to locality A of the sketch-map in the Beport on
Potash-Felspar by H.M. Geological Survey.
The approximate mineral composition of each sample calculated
from these analyses is :
(1) '(2) (3)
Potash felspar 59'71 61-80 61-74 per cent.
Albite (soda-felspar) 24-01 16'20 18-58
83-72 78-00 80-32
Quartz and other constituents... 15'96* 22-49* 19-72* by difference.
Totals 99-68 100-49 100-04 per cent.
The following note t as to the composition of the Scottish
pegmatite veins is of importance to glass-manufacturers :
" The pegmatite material consists predominantly of quartz and
felspar. Iron -bearing minerals, such as .biotite and hornblende,
are present, but generally constitute less than 1 or 2 per cent., and
though the proportion may sometimes reach 5 per cent., it is only
in certain infrequent bands. Where the pegmatites are un crushed,
these ferromagueskn minerals (which tend to be associated with
the plagioclase felspars) could be hand-picked from the quarried
material."
, [Such iron-bearing minerals as biotite and hornblende are very
undesirable in felspars used for glass-making. The iron-percentage
in the analysis quoted above (FeO+Fe 3 3 , 0;43 per cent.) is too
high for good glass-making.
f - * The content of barium felspar (celsian) in 1, 2, and 8 is 0-48 %, 2-42 /
mid. 2-14 % respectively. The remaining minor constituents are small in
amount.
f "Special Reports on the Mineral Eesouroes of Great Britain. Vol. v.
Potash Felspar, etc." Mem. Geol. Survey, 1916, p. 9.
IRISH FELSPARS. Ill
The average mineral composition of the pegmatites is said to
be : quartz 24-8, and f elspai 1 75'2 per cent. Figures in particular
analyses vary between the extremes : quartz 17*65, and felspar
82'35 per cent. ; quartz 39'0, and felspar 61'0 per cent.
The average value for the potash-percentage in the Sutherland
felspar is stated by H.M. Geological Survey to be 12-81, which
agrees closely with that of felspar from other localities. The
potash-content of the pegmatites would, thus amount to about
9'2 'per cent., which is in accord with the results of the analyses
made by the Survey.
For the following notes, published by permission of the Director
of the Geological Survey of Ireland, on the Belleek felspar, the
writer is indebted to Mr. W. B. Wright, B.A., F.G.S :
The Pegmatite Deposits of Belleek, Co. Fermanagh.
" The felspar deposits of Belleek, the presence of which in the
district was one of the inducements which led to the establishment
of the Belleek Pottery, occur in the area of gneissose rocks to the
north of Belleek and Caatlecalclwell. They are not, however,
exploited at the present time, because the requirements of the
Pottery are so small that it would not pay anyone to mine for the
purpose of supplying this demand alone, as long as materials can
be obtained from Norway at prices which are reasonable. The
Manager of the pottery states that from his point of view there is
little to choose between the native felspar and that which is now
imported.
" The felspar occurs as the main constituent of pegmatite dykes,
which are found traversing the gneissose rocks. It is, to a varying
extent, graphically intergrown with quartz, and in some places
penetrated by coarser veins of quartz. White mica also occurs
here and there as an impurity.
" The following are the localities (as far as they could be ascer-
tained by local enquiry extending over two days) in which attempts
have been made in the past to test the extent and quality of the
felspar-bearing veins.
" (1) Townland of Derryrona Glebe, north of Lough Scolban,
and three and a half miles E.N.E. of Belleek. The pit is now
filled tip, but the vein is reported by a local farmer to have been
four feet wide. There is a heap of felspar containing about three
tons beside the pit. It is graphically intergrown with quartz. in
the proportion of say one part of quartz to three or four parts of
felspar. The felspar crystals are sometimes as much as 18 inches
square.
" (2) Townland of Scardans Lower, two miles north of Castle-
caldwell. The vein appears to bo about 4 feet wide and the shaft
that has been sunk in it is reported to be about 30 feet deep. The
felspar got out here is not so pink as elsewhere. The crystals are
up to a foot in length. There is, if anything, less graphically
112 SILICEOUS BOCKS BEABIKG ALUMINA AND POTASH.
intergrown quartz than at Lough Scolban. The vein is said to
have a definite wall and to part easily from it.
"In this townland there are several other localities where felspar
can be seen exposed at the surface, or where the local farmers state
that explorations have been carried out in the past.
" (3) Townland of Larkhill, in the bog to the north of Croagh
More, a vein has been opened up in this locality running N. 35 E.,
and dipping N.W. at 50 or 60 degrees. It appeal's to be 4 or 5
feet thick and was excavated to a depth of about 20 feet at the
N.E. end. There is a heap of about 20 tons at one side. It
varies greatly in quality and in its quartz content, which seems to
be somewhat greater than at localities (1) and (2).
" There have been some other minor openings in the same
townland.
" (4) On the moorland between Loughs TTnshin and Columb-
kille, about a quarter of a mile S.W. of Lough Unshin and two
and a half miles north of Belleek there is a nine-foot vein of
pegmatite running "W. 35 N. and traceable for about 50 yards.
Only surface quarrying has been done on this vein. It varies a
good deal in quality. In some places it contains a fair amount
of quartz and mica, but in others it is almost entirely composed of
large felspar crystals with minute graphic intergrowth of quartz.
"The localities numbered (1) to (4) are, as regards size and
content of the veins, the best which are at present known in the
district. Veins up to two feet in thickness occur in many places,
as for example at Grarvary, near Castlecaldwell, where several
openings have been made. These, however, are hardly worth
considering until it is known that the larger veins could be made
to pay.
"As regards the continuity, laterally and in depth, of these
veins or dykes of pegmatite, it is impossible to make any confident
statement, as the country in which they occur is so much obscured
by drift and bog. Smaller veins in better exposed ground are seen
to be fairly continuous for considerable distances but vary much
in width. There ought to be about the same ease or difficulty in
following them as there is in following an ordinary lode, and they
have about the same chance of maintaining their width.
" From the nature of the rocks and the reports regarding the
shafts already sunk, it is not anticipated that any difficulty would
arise from water in the mines. A certain amount of felspar could
undoubtedly be got out by surface quarrying, but in the end
mining would have to be resorted to.
" The following are distances from the railway :
" Locality (1). 1 mile from Castlecaldwell Station.
(2) & (3). Lmile from rail, 2 miles from Castlecald-
well Station.
(4). 2 miles from Belleek Station.
" The railway freight for coal from Londonderry to Belleek is
IBISH FELSPAB.8.
113
4s. 6d. a ton. The harbour at Ballyshannon is difficult of navi-
gation."
Chemical analyses of the Belleek Pegmatite (by Dr. H. F. Har-
wood and Mr. A. A. Eldridge) are as follows :
Locality (1)
SiO, 73-18
AlA 14-58
TiO. 2 , none
Fe.,0 3 0-06
CaO 0-22
MgO 0-08
K 2 10-48
Na a O 1-52
BaO trace
Loss on ignition 0-27
(2)
(3)
(4)
73-07
65-74
70-96 per cent.
14-71
18-36
15-53
none
none
none
0-05
0-06
0-27
0-22
0-21
0-28
0-05
0-13
0-07
10-14
13-08
10-95
1-60
2-07
1-55
0-02
0-03
0-16
0-46
0-25
0-48
Totals 100-39 100-32 99'93 100-25 per cent.
The approximate mineral composition of each sample calculated
from these analyses is :
(1) (2) (3) (4)
60-07 77-49 64-90 per cent.
13-57 17-56 13-15
Potash felspar ..................... 62-10
Albite (soda-felspar) ............ 12'89
74-99
Quartz and minor constituents 25"40
73-64
26-68
95-05
4-88
78-05
22-20
Totals ............ 100-39 100-32 99-93 100-25 per cent-
A few other workable veins of pegmatite were also visited in
this area by the writer. A chemical analysis of rock from Garvary
Wood is given in Table IV. page 160. At a very conservative-
estimate many thousands of tons occur. On the whole, these Irish
deposits are more easy of access than the Scottish and seem to have
less quartz intergrown with the felspar ; their soda-content is also
less. Occasionally stringers of ferromagnesian minerals are met
with, as in the Scottish pegmatites, but hand-picking will generally
remove these.
At Ballymanns, near Aughrim (Co..Wicklow), felspar was said
locally to have been worked and used in glass-making or pottery
work. Prof. Grenville A. J. Cole, F.B.S., Director of the Geological
Survey of Ireland, has kindly examined G. H. Kinahan's field-maps
for the writer, and finds upon them dykes (running from north-
east to south-west) of quartz-felspar rook at Ballymanus. Working,
except for the granite, has been given up for a long time.
In point of bulk the Scottish deposits stand first, but their
relative inaccessibility reduces the value of the large resources
present. The Cornish pegmatites are very limited in quantity, and
are liable to contain tourmaline. The chief iron-bearing mineral in
the pre- Cambrian pegmatites is biotite. Other occurrences of
114 SILICEOUS ROCKS BEAMING ALUMINA AND POTASH.
felspars in Argyllshire, Co. Donegal (Fintown, Dooey, Glenties, and
Q-weebarra), and Co. Mayo (Belmullet, Ems Head, Doolough, etc.)
have heen visited and their workability is being considered. They
will shortly be described in detail* ; in the meantime, chemical and
mineral analyses are given in Table IV. page 160.
For comparison with the analyses of English, Scotch, and Irish
felspars, may be quoted that of one of the Swedish felspars
imported in large quantities for glass-making and pottery
purposes t-
SMX ........................ 65-78 per cent.
19-01
TiOj ..................... none
Ee.,0, ..................... 0-23
CaO.' ....................... 0-27
MgO .................... 0-28
K 2 ........................ 11-01
Na 2 ..................... 2-21
Loss on ignition ......... 0-36
Total 99-10 per cent.
The Scandinavian felspar at present in use at the Belleek Pottery
"has the following composition (H. F. H. & A. A. E.) :
Si0 9 65-60 per cent.
AlA 19-05
TiO a none
Fe 2 3 0-02
CaO 0-26
MgO trace
K a O 12-12
Na a O 3-08
Loss on ignition 0-28
Total 100-41 per cent.
Analyses of " Mixed Stone " and " Purple Stone " are also
given :
Mixed Stone. Purple Stone.
SiO a 72-15 70-31 per cent.
ALO 3 16-28 16-62
TiO 2 0-20 0-17
Fe 2 O, 1-45 FeO 1-50
MgO 0-20 0-08
CaO 1'65 1-50
K a O 5-01 5-69
Na a O 1-50 2-62
LOBS on ignition ... 1'15 1-25
Totals 99-59 99-74 per cent.
* An account is being published by the writer in the Trans. Soo. of Glass
Technology, vol. ii. (1918). Dr. A. Campbell has recently dealt with further
Scottish resources in a paper before the Edinburgh Geological Society
(Jan. 1918). Additional supplies have since been discovered and will shortly
be described.
t Trans. Ceramic Soo. vol. rii. (1912-13) p. 65.
MELDON HOCK. , 115
With these may be compared the analyses made by Dr. H. F.
Harwood of china-stone from the West of England China Stone
A Clay Company Ltd., St. Austell :
SiO a 75-23 per cent.
Al.,0., 14-27
Fe,0 3 0-08
Cab 1-64
MgO 0-20
K.0 4-35
Na.,0 ' 2-81
Loas on ignition 1-44
Total 100-02 per oent.
Duplicate determination of SiO.,, 75-19 per cent.
This rock is crushed and ground to a fine powder in the works
at Par, and is sent to the Potteries. The analyses are quoted as
indicating that china-stone and related material, if they can be
secured free from, or with a low percentage of, iron oxide, may be
of considerable value to the glass-trade as sources of alumina and
silica, and at times also of potash.
The British resources of china-stone have been fully dealt with
in the Memoir quoted above (" A Handbook to the Collection of
Kaolin, China-clay, and China-stone in the Museum of Practical
Geology," Mem. Geol. Survey, 1914).
The following rock is of a similar character :- -
Meldon Rock and "Sand." ("Devonshire Hard Purple
Stone.")
Worked by the Meldon Valleys Co., c/o Messrs. Fox, Eoy, &
Company Ltd., Plymouth.
Maps. Geological : Old Series, 1-inch, Sheet 25.
6-inch, Devon, Sheet 76 S.E.
Situation. Lat. 50 43' 0", Long. 4 1' 50" W.
The quarries occur about half a mile east-north-east of Meldon
Church and near the viaduct of the L. & S.W. Railway, about
four miles south-west of Okehampton.
Formation. Aplite dyke intrusive into Culm Shales (Carboni-
ferous).
Description. The rock occurs as a broad dyke running roughly
parallel with the edge of the Dartmoor Granite, and separated
from it by an outcrop of Carboniferous (Culm) Shales about sixty
feet or more broad. The rock is a fine-grained aplite, varying
1 in colour from grey to pale purple. One band runs very true to
sample, and the good conditions of quarrying, the water-power
present, and proximity of the L. & S.W. Railway, permit profitable
working and crushing. Water-power and therefore electric-power
being available, it is possible that at some later date, if the market
permits it, washing, screening, and also electromagnetic treatment
will be instituted to grade the product and free it from some of
nts iron.
i2
116 ' SILICEOUS BOCKS BEABING ALUMINA AND POTASH.
A chemical analysis of the rock is as follows :
Si0 2 71-07 per cent.
AU> 3 16-79
TiOj 0-06
Fe a O, 0-27
CaO 0-87
MgO 0-05
K 2 3-83
Na. 2 4-92
01 trace
Loss on ignition 1-87
Total 99-73 per cent.
Duplicate determination of Si0 2 gave 70-98 per cent., and of K^O,
3-81 per cent.
The iron-content of a sample of the crushed hut untreated
product is 0-15 per cent. FeO (Fe a O a absent).
The mechanical analysis of the crushed product is as follows,
tut it should be mentioned that no attempt has yet heen made
commercially to grade the " sand."
>2 mm., 24-6 % ; >1 mm. & <2 mm., 18-5 % ; >0'5 & <1 mm., lO'l % ;
>0'25 & <0'5, 20-2 % ; >0'1 & <0'25, 12'5 % ; >0'01 & <0-I, 8'2 % ;
<0-01, 5-9 %. Total sand-grade, >0'1 mm,, 85-9 %.
F VCS OS_ MS _FS _s ^ G&S -i
L24-6' 18-5' 10-1' 20-2' 12-5 ' 8-2 ' 5-9 ; 85'9 J
The mineral assemblage in the rock is a full and interesting one.
Apart from the minerals occasionally occurring in veins, etc.
(axinite, green tourmaline, lithionite, fluor-spar, etc.), separation
with bromoform enabled the following to he identified : greenish
and pale yellowish tourmaline, purple to colourless fluor, topaz,
ilmenite, zircon in very small grains, muscovite, etc.
The crushing strength is 24,100 Ibs. per square inch.
,.- The rock may be valuable for the alumina it contains and also
for the proportion of potash. For hottle-glass, the addition of
limestone and alkali only is required. The rock is at present
worked for pottery purposes, the crushed material "being supplied
at 15s. per ton. The freight to Staffordshire is now about 19s.
per ton ; before the war it was about lls. The available resources
are very considerable.
/
Potash-bearing Sands.
Very few of the minerals which occur in sands or racks carry
potash. The felspars have already been mentioned. Muscovite,
or potash-mica, rarely occurs in quantity in Britain. As a partial
decomposition product of felspar (of which the final stage is repre-
sented by the formation of kaolin), it occurs in the "micas" of
the china-clay works (see page 100 for analysis, etc.). The amount
of f erruginous impurity in these " micas " almost prohibits their
use for glass-making. The only other potash-bearing mineral of
G-LAUCONITIC SANDS.
117
anything like common occurrence is glauconite, which is a silicate of
iron, aluminium, and potassium. It lias been used as a fertilizer
because of its potash-content, and it is also of service for softening
water. The mineral varies in colour from olive and deep bluish-
green to such pale tints as to be practically colourless. It does not
Appear to have a fixed chemical constitution indeed, the term
probably includes a number of minerals of similar composition, but
with varying quantities of iron, potash, soda, etc. Being an iron-
bearing material, it cannot be utilized directly in glass-manu-
facture. Chemical analyses of some samples of glauconite are as
follows :
(1)
SiO, 49-42
Al a 3 10-23
Pe a 3 16-01
PeO 3-00
MgO 3-78
CaO 0-31
K a O 7-91
Na-O 0-26
H.,6 8-08
P,0<
Totals 99-00
(2)
50-42
4-79
19-90
5-96
2-28
3-21
7-87
0-21
5-28
tr.
99-92
(3)
46-91 per cent.
7-04
23-06
2*64
4-40
2-95
7-31
0-91
4-71
99-93 per cent.
(1) Borne.
(2) A Continental Q-lauoonite.
(3) Channel Islands.
Some highly glauconitic deep green Br
following composition :
(1)
SiC^ 60-61
itish sands have the
(2)
44-76 per cent.
5-02
0-45
9-21
2-05
14-56
2-20
4-40
0-09
0-02
.. 3-24
.. 2-48
.. 10-64
.. 0-07
. trace
ALO n
9-73
H 2 0+ .
H,0- .
C6 a ....
MnO ....
01
TiO 2
0-70
Pe,,0,
9-67
PeO
0-45
CaO
1-22
MeO
1-89
K,O
2-98
Na a O
0-83
P.O.
0-13
BaO
. trace
ices on ignition 12*38
Totals: 100-09
99-79 per cent.
(1) Prom the Thanet Beds at Bramford, near Ipswich.
{2) Prom the Upper Greensand, Coffin Glen, Belfast.
118 SILICEOUS HOCK8 BEA.BING ALUMIXTA AND L'OTASII.
The potash-content of other British glauconites will be found
in the Table on page 169.
It may be possible in the future to utilize glauconite as a source
of potash, but no British deposits yet found cany sufficient of that
compound. A satisfactory chemical process must first be devised
and made commercial. Although the potash-percentage is lower
than in potash-felspar, the supplies of glauconite are large and
widely distributed.
Numerous processes have been worked out for extracting the
potash from felspar. A summary of some of these is given in the
" Special Reports on the Mineral Resources of Great Britain. Vol. v.
Potash-Felspar, etc." an account similar to that in the Mineral
Resources .Reports of the United States Geological Survey. "Refer-
ence may also be made to " The World's Supply of Potash," BulL
Imperial Institute, 1915. A modification of earlier processes lias
been suggested by E. A. Ashcroft (lust. Mining & Motall. Doc.
1917). One of the most promising and interesting of rc-cout
processes is that suggested by Frasser, Holland, and Miller (Journ.
Indust. &Bngin. Chemistry, vol. ix. No. 10, page 985, Oct. 1917) j
it aims at producing aluminium sulphate, with potash us a. by-
product.
The results on British felspars of procedure patented by Mr. J.
Rhodin were given in the ' Journal of the Board of Agriculture '
for February 1917 (Br. Pat. 13,448 of 1914, 21,097 of 1911, and
16,780 of 1899).
TBEATMEHT OF SANDS AND BOOKS. 119
CBCAPTER X.
SPECIAL TREATMENT or SANDS AND ROOKS.
Sands, like many other natural products, can be improved by
washing. If the process is carried out effectively, a third-quality
sand may be brought up to the rank of second-quality, but it does
not produce, in the case of most British samples, a first-quality
glass-sand. Moreover, the question of extra expense due to washing
(and sometimes drying also) and consequent additional handling
and movement, is here an important factor, since very large quantities
of second- and third-rate sands are used for making glass for lamp-
chimneys, electric -light globes, flint-glass bottles, window-glass,
commoner table-ware, etc., individual firms each using as much a
three hundred tons of sand a week.
Colour of Glass-Sands Although in the field a considerable
number of sands appear by comparison to be white, it is remark-
able how very few are snow-wliite. The colour is frequently a good
indication of the relative freedom of the sand from oxide of iron.
The best English sands are locally white, but usually grey, cream-
coloured, or faintly yellow or brown. To realize the true colom 1 ,.
samples may be placed upon white paper or compared with Fon-
tainebleau sand. Small quantities may also be mounted in clovo
oil and examined under the microscope, when the faint yellow,
brown, or grey pellicles of ferruginous material are easily visible.
A dark colour is not necessarily an indication of much iron ;
organic matter, which may subsequently be burnt out, produces
this effect. A pink colour may be due to pink quartz and not to
iron oxide. Similarly, glass itself may be water- white and brilliant,
and yet contain no small percentage of iron.
(a) WasJiing. Hematite-coated grains (like those in Permian
and Triassic deposits) cannot be cleaned without very great
difficulty, eveii where the coating is thin and the sand pale-coloured.
In the case of sand-grains having a thin pellicle of liraonite,
mere washing by water may improve the quality considerably.
Seeond-ckss sands from the Lower Greensand of Aylesbury,
Leighton Buzzard, and King's Lynn have been improved and
made suitable for flint-glass work in this way, but the results are
not even then so good as the best of the Aylesbury or Lynn sands
actually found in the quarries. The best sands are not improved
in the matter of iron-percentage by washing, but the adoption of
washing does obviate to a considerable extent the trouble or careful
selection, and enables variable sands to be profitably exploited.
120 TBEATMENT OF SANDS AITO BOOKS.
Apart fi-oin the question of the increased cost of washing, which is
considerable (at least 6d. per ton, but reaching at times, with the
extra handling, as much as 2s. 6d. per ton), the expense of drying
has also to be taken into account.
The coating of sea-salts around the grains of dune- and shore-
sands does not appear to be objectionable for glass-making (as it
is when such sands are used for concrete or for building-purposes),
similar salts being added in the batch. The sands have the advantage
of being well-graded (see Table V., page 165) as a result of repeated
sorting by wind and water, but since their colour is not good and
they often contain abundant shell-fragments, it is clear that repeated
washing will not produce purity without the intervention of living
organisms and percolation of water (c/!, for example, the patchiness
of colour in the red sands of the Permian and Trias due to reduction
around organic remains).
The value and importance of washing must be strongly empha-
sized. It is satisfactory to note that the producers of sand are now
becoming alive, under war-conditions, to the improvement thus
affected in sands and the correspondingly enhanced market value.
Sands for refractory purposes, as well as glass-making, are now
being washed in many instances by the producers. Although the
process is frequently earned out at the sand- quarries, water is not
always available in the quantities desirable. It will often pay
glass-manufacturers to wash or re- wash their sand at the works, as
dirt, dust, etc., are usually picked up during transit. The effect
of washing is two-fold. It removes much adherent iron oxide,
calcareous material, etc., and also clay, silt, and fine sandy matter
which are undesirable in a glass-sand. A comparison of analyses
of glass-sands before and after washing is of considerable value.
Improvement will be noted in both grading and chemical
composition. (See Tables on next page.)
In this connexion, as indicating the material washed out of a
glass-sand, it is of interest to quote the following analysis from the
remarks upon American Glass-sands in Bulletin 285 of the United
States Geological Survey (page 461) :
Analysis of a Slime from washings of a sand from Ottawa, 111.
Si0 2 87-21 per cent.
Fe 2 a 0-52
CaO none
MgO none
Na.,0 ' 20
Total 95-43 per cent.
Bflmainder mainly water.
This analysis indicates that besides ferruginous and clayey
matter, much fine silica had also been removed from the sand.
WASHING OF BANDS.
121
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OS 't
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rt2i
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OS iH
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g 1
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Untreated.
Washed.
-0
-?
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ri ^
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fl .
Untreated.
Washed.
Untreated.
Double washed.
r
o
ShirdleyHill...
i> ,, ...
Port-a-cloy . . .
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o
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1 =
122 TREATMENT OP SANDS AND EOCZS.
A method of washing sand adopted abroad is on the principle of
acid-scrubbers, the sand being arranged upon tiers of platforms
above one another and washed by distributed descending sprays of
water.
Various methods, including tank-washing, have been adopted in
this country, but some form of rotary process is most commonly
used.
In some cases the sand is washed twice over to ensure better
cleansing. It is often an advantage, especially when washing is.
adopted in order to cleanse a sand from iron oxide, to have the-
cylinder much longer than it usually is. Care should be taken
to ensure that rotary washing-plant is suited to the grade of the
sand. If the latter is too fine for the apparatus, much loss will
result owing to the carrying off of fine sand in the stream of dirty
water.
The most efficient machine for washing sand at present in use in
this country is, in the writer's experience, that devised by Mr. 0.
Bikof of 159 Pentonville "Rd., London, N. 1. A short description
may be of use to sand-merchants and gl^ss-manufacturers.
The Washing and Screening Machine (Eikof's Patent) is
illustrated in Plato VII. and Fig. 13, and is so designed that it will,
with small modifications to suit particular cases, wash any material
from coarse gravel to fine sand. By an automatic feeding device
the material is delivered into the slightly inclined revolving
washing cylinder, the feeding being continuous and uniform so that
all the materials are subjected to an equal amount of washing.
The machine can therefore be run at maximum output without
incurring the risk of temporarily overtaxing its capacity, which
might happen in the case of manual feeding.
The length of the washing cylinder is fixed in accordance with
the time required by the water for removing the binding materials
and for separating the particles from each other. The cylinder is
divided into sections or compartments so arranged that while the
washing water overflows from a cleaner compartment into one-
containing dirtier material, and is finally discharged at the higher
end of the cylinder, the material travels in the opposite direction
and is automatically propelled over the partitions, each time
into a compartment containing cleaner water. Eventually the
materials are delivered into cylindrical screens, the number and
fineness of which depend on the grades into which the said
materials are to be divided. The screens are arranged concen-
trically, the innermost cylinder having the largest holes. The
holes in the outermost cylinder determine the largest grains of the
finest sand. Water-sprays between the screens facilitate the
screening and subject the particles to a final cleansing. The water
is led away with the sand into a special sediment separator, which
constitutes a novelty in sand-washing machines and is necessary
for securing clean, drained, sand (Fig. 13). This contrivance is
most simple in construction as well as in working. It consists
of a steel cone fixed at its larger end on to a wide flange centred
BIKOP'S WASHING MACHINE.
123-
on an almost horizontal slowly revolving shaft. On the outside
of this cone are numerous vanes or blades forming pockets-
for receiving the washed sand and the cleansing water. The
pockets are so arranged that the top edge of each is level when
reaching the horizontal plane containing the cone axis, and in this*
position it cuts off the supply of water and sand, which then goes into
the next pocket. The contents, which during the filling are most
vigorously agitated, become calm after the supply has ceased, and
Fig. 13. Cone-attacliment to JtiJcofs Washing Machine,
fw cleansing and draining Sand.
the sand settles quickly in the lower portion of -the pocket near the
flange, the water with the silt in suspension being gradually tilted
off: at the smaller end of the cone as the latter revolves and the larger
end of the pocket is elevated over the top of the cone. When
farther advanced, the sand is discharged at the other side of the
cone, and the empty pocket proceeds on its way to receive a new
charge. >
The efficiency of the machine is dependent on its being worked
at the proper speed and with a water-supply suiting the nature of
the materials under treatment. Once carefully studied, however,
124 TREATMENT OP SANDS ATST) ROCKS.
and properly adjusted, the machine works automatically and with
excellent results.
- The arrangement described above for draining the sand renders
the question of drying it a much less serious matter. Air-drying
is usually effective and sufficient. The users of .sand naturally
prefer it to be delivered in a dry condition, but methods of artificial
drying are frequently too expensive for the sand-merchant to
undertake. The transport of perfectly dry sand is also at times a
troublesome matter.
Other devices are employed to hasten the drying by draining off
the water, and sometimes the process is carried out in large ovens
(two tons at a time), but systematic drying- plant like that used
in America has not yet been introduced. Drying is carried out in
the Mississippi valley and other places by the use of tier dryers,
rotary methods, or steam coils. Small quantities of dry sand are
frequently required in this country during the winter, for use as
parting-sand in facing moulds for brick-making, etc. In this case
a small oven is built of bricks, a fire lighted within it, and the sand
heaped over and around the oven.
(b) Screening, etc. In the matter of the improvement of the
grade of a sand, screening may be combined with washing without
much difficulty, and clayey and silty materials may be washed out
by suitably controlled streams of water. If an elutriator is set up
in the works' laboratory, analysis of the sand or crushed rock will
give an indication of the velocity of the stream of water which will
cany off all grades below that desired. For certain gksses it is not
too expensive to treat local sands on a large scale in water-currents
adjusted to this determined velocity. The process, in addition,
will clean the sand of dirt and possibly some iron oxide. A velocity
of 3 - 5 mm. per sec. (42 feet per hour) is the theoretical velocity
which will carry away all particles (which can move freely) of
diameter less than '075 mm. The use of a greater velocity than
this will be necessary on account of the friction of sluices, etc. and
the bulk of sand treated. An air-blast may be used, as it is occa-
sionally in engineering practice or for filtration purposes, to clear
a sand of fine material. Such a blast of about l - 5 metres per second
(about 4'9 feet per second) will carry off all particles of diameter
less than O'l mm.
The importance of screening sands and crushed rocks to free
them from coarse grains and fragments which Avould remain
as undigested " seeds " or " stones " in the glass, has already
been emphasized. It is frequently of value to fine-screen n
glass-sand also. Mr. C. J. Peddle, chemist to Messrs. Wood Bros.
Q-lass-Works of Bamsley, lias demonstrated the improvement in
the properties of glass-melts made from sands sifted to 80-mesh
ft)'22 mm.), the portion passing the screens being rejected. The
reason for this is threefold. Clay and silt are removed as by
washing. The surface 1 -area of grains increases relatively as they
decrease in diameter. The grains composing the line grades of a
SCREENING AND BURNING OF SANDS.
125
sand therefore tend to carry a relatively greater proportion of
ferruginous and clayey coatings. In the third place, the pro-
portion of heavy detrital , minerals in a sand (including the
objectionable zircon, rutile, and iron-bearing minerals) rises with
decrease in grade-size. The following figures* illustrate this,
point :
Heavy Minerals in Q-lass-Sanfa.
Variation with grade of percentage of crop having a density
greater than 2'8.
Grade-size in mm.
0-025-0-05.
0-05-0-1.
0-1-0-2. 0-2-0-4.
Pork Lane Reigtvte
407 %
253
302
870
700
356
098 %
191
050
230
060
098
014 %
024 f
008
Ashurstwood
1-26 %
Longdown
Denford
Jarvis Brook, Crowborough . .
Dry-screening may be adopted to improve the grade and iron-
content of certain sands, where the coating of the quartz-grains,
consists of the valuable kaolin and not feme oxide,
(c) Burning. The better-class sands are undoubtedly improved
by ignition. Water, often an objectionable constituent, is driven
ofE. Organic substances are burnt out, and an improvement in
whiteness results. Impurities which have been introduced during
transit, e.g., dirt and coal (when the sand is brought back by
coal-barges as ballast) are eliminated. For very special work, such
as optical glass or the finest crystal ware, it is advisable to wash
and burn even a very pure sand like that from Fontainebleau.
Burning, therefore, cleans a sand if it has been darkened by in-
cluded peaty matter, but if the discoloration is due to staining by iron
in a slight degree, the sand becomes a darker grey, brown, pink,
or red colour, the usual change being that from the hydrated oxide,
limonite, to the anhydrous oxide, hematite. The effect of burning
thus yields in most cases a rough indication of the amount of iron
present as staining, that in the heavy minerals, as already stated,
usually being of little importance. If the burning is earned on
* These are a selection from the results of a lengthy series of experiments
which were carried out by my friend, Mr. Y. C. Tiling, M.A., P.G.S., of the-
Eoyal School of Mines (Imperial College of Science and Technology), and
which he kindly permits me to quote.
f The heavy crop in the grade >0-4 mm. diameter amounted to less than.
0-001 per cent.
126 THEATilENT OF SA2O)S AXD DOCKS.
under standard conditions, the temperature being; recorded by means
of a pyrometer, and the increase in colour compared with the tint
of known standard materials, an approximate id^a of the amount
of iron and organic matter present may be obtained. Most of the
British deposits under consideration darken on heating, as do also
the Belgian glass-sands so extensively used in this country. The
latter are almost white, but attain a slightly pinker colour, while
Dutch sand becomes greyer. Of the few British deposits which,
like Fontainebleau sand, show no change on heating, the following
may be mentioned : the best quality sand from Aylesbury and
selected Godstone and lieigate sands (Lower Greensancl), sand
from Muckish Mountain, Co. Donegal, and a sand from Abergele,
North Wales (the last two contain ferruginous patches which
darken considerably). Pure white sandstones, such as the Coal-
Meaeure Sandstone from Ghiiseley, near Leeds, also show no change
-of colour on heating.
Many glacial sands appear to be light-coloured and fairly pure,
but on examination are usually found to contain limonite pellets
(often representing decomposed iron -bearing minerals). They burn
up to a much darker colour.
(d) Qliemieal Methods. Other processes for the purification of
sand from iron are too costly if any great quantity of the sand ia
required in industry *. Acids only partiallv clean the sands, even
with application of heat. Hydrochloric acid has been used in this
way, but the solution of iron oxide is never complete. By raising
,a mixture of a sand with about 2J per cent, of common salt to a
red heat, and afterwards lixiviating with water, complete purifica-
tion from iron is obtained t- Treatment with sodium hydrosulphide
is said to yield the same result at lower temperatures. Nitre-cake
has been successfully used on a small scale for dissolving out
ferruginous and other compounds from sands. It consists of a
mixture of acid and neutral sodium sulphates, its bleaching
properties depending upon the unrecovered free sulphuric acid
present. Nitre-cake has also been recommended for use in glass-
making as a partial substitute for potash. A by-product from
explosive works, it was obtainable before the outbreak of war for
the mere carrying away from the tips, or for a nominal price of
I/- per ton. Since 1914 the demand for it has largely increased,
-owing to the unrecovered acid present, and the price is now
. about 17/- per ton at the works.
As an example of what can be done in the way of cleansing
sand, the following analyses may be quoted. A yellow-brown
* The largest glass-making firms each use 100,000 to 150,000 tons of sand
. a year.
t Patent No. 8495 (1914) by J. G. A. Rhodin, "Improved Means for and
Process of Bleaching Sand." The same idea was suggested in Bassett's
patent for the extraction of potash from felspar, U.S. 1913 (see Potash Salts,
U.S. G. S. Mineral Resources, 1913).
CHEMICAL AND MAGNETIC METHODS.
127
impure Triassic sandstone from EaglesclifPe was treated with
nitre-cake, and yielded a clean white sand :
Before treatment : Fe.,0., 0-20 per cent.
After treatment : Fe^OJ, (a) 0-03, (i) 0-048, (c) 0-045 per cent.
Analysis of treated sand.
SiO., 93-59 per cent.
A1,O 3 3-51
Fe" 2 3 0-03
CaO 0-16
MgO * 0-14
K.,o 0-94
Na^O 0-83
LOBS on ignition 0'66
Total 99-86 per cent.
This white sand does not change colour on burning.
The amount of alumina in this material is noteworthy. The
product having been well screened and washed, several different-
sized sands can be supplied. The products are well-graded, as the
following mechanical analyses indicate :
| OS.
MS.
FS.
S.
c.
S.
, i >0-5 &
Sample. |<lmm
i
>0-25 &
<0-5.
>0-1 &
<0-25.
>0-01 &
<0-1.
<o-oi
mm.
Total
sand-grade :
>0-1 mm.
i ! o-i %
15-3 %
82-7 %
1'5 %
0-4 %
98-1 %
2 i ...
94-7
4-2
1-1
94-7
i
Material of rather coarser grade than this will also be available.
Sodium carbonate (washing soda) may also be employed for
cleansing purposes, as the following figures of a sand from Leighton
Buzzard indicate :
Before treatment, Fe a O.,, 0'04 per cent. ; after treatment, 0-015 per cent.
These methods are usually too costly except where pure sand is
required for very special work, such as optical glass.
(e) Magnetic Methods. Endeavours to remove objectionable
heavy minerals from a sand are not, as a rule, paying propositions.
Electromagnetic methods have, however, been applied in glass-works
in the United States of America to the freeing of an otherwise
suitable sand from such iron ores as magnetite. . Separators have
only been employed where high -class gkss is made, and it is
claimed that the colour and brilliancy are improved as a result
of the treatment of the sand. Other iron-bearing minerals
(including silicates, etc.) less permeable to electromagnetic action
can at the same time be removed.
If hard rocks, such as well-cemented sandstones and quartzites,
12S TKEATMKS'T OF SA2TDS AND BOOKS.
art- crushed for glass-purposes (see below), magnetic separation
must be resorted to in order to free the product from frag-
ments of iron or steel obtained from the rolls or jaws of the
crushing-plant. The process is similar to that employed in the
{reparation of raw materials for the manufacture of pottery, .It
has not been found necessary to apply this treatment to sand
t btained from soft grits and sandstones.
As an example illustrating the necessity of electromagnetic
treatment of the product obtained by crushing a rock, the folio wing-
may be mentioned :
West of England China Stone & Clay Company.
China-stone crushed at Far, Cornwall:
Product before electromagnetic treatment : Iron estimated as Pe a 3 , 0-12 \>. c.
after ,. 0-08 p. o.
About one c\rt. of iron is abstracted Weekly from about fifty tons
of the crushed rock.
(For analysis of this china-stone, see page 120.)
The amount of ferruginous matter introduced by crushing rooks
may be gauged from the following figures :
Iron-content estimated as I"e 2 s .
Westport Silica (vein-quartz from Adhill I.) :
before crashing, 0'004 per cent, ; omened product, 0-04 per cent.
Meldon Valley rock (aplite) :
before crushing, 0'15 per cent. ; crushed product, 0-27 per cent.
Griadingor Milling. Onlj for the best glasses for optical
Sa" V^^' * ,?* ^ ^-grind the sand to 1 line
rt L 5 T^IF and moi>e re S nIar and ^a melting
W ^ T i\\ * the 6X P ense is ^siderable. The process
has been adopted in the making of laboratory glass-ware but t i s
doubtful Aether any great advantage accrues. 5 The procedur s
eco r ic
the rock breaks down, of the chie rn^? ?J Pr T Ure
mended as sources of si^a and al^' ^ ^ been rccom -
mcidentally for refractoj ^^^oses " ^ 5S ^^S, and
CRUSHING STRENGTHS. 129
The crushing strength of pegmatites is very similar to, but
perhaps rather less than, that of granites, which varies from ahout
12,000 to 38,000 Ibs. per square inch. An average figure is perhaps
18,000 Ibs. per square inch.
Sandstones vaiy very much in their crushing strengths according-
to the degree of their consolidation and character of the matrix.
A moderately soft sandstone from Plean, N.B., has a crushing-
strength of 953 Ibs. per square inch, while a finely-cemented
quartzite may have a crushing strength of over 30,000 Ibs. per
square inch. Some sandstones used as building-stones give way at
less than 3000 Ibs. per square inch. Others withstand successfully
a pressure of 16,000 Ibs. per square inch.
The average crushing strengths of some of the rocks which
have been crushed and put on the market as glass-sands or refractory
materials are given in the following table. The tests were earned
out in the Laboratories of the City and Guilds (Engineering)
College (Imperial College of Science and Technology), with the
kind co-operation of Prof E. F. D. Witchell, cubes of 2*5 ins. side-
being used, except where otherwise stated .-
Spital Sandstone 1,450 Ibs. per square inch (3-inoh cubes)
MeldonBook 24,100 (3-inoh cubes).
Stiper Qimrtzite 32,000
Appin Quartzite 32,200
Holyhead Quartzite... 30,600
180 FOBEIGN GLASS-SANDS.
CHAPTER XI.
FOREIGN GLASS-SANDS.
A discussion of suitable British glass-sands would not be
complete without comparative notes upon some widely-used Con-
tinental and American examples. Notes upon a few well-known
foreign glass-sands are therefore appended.
EUROPEAN SANDS.
Lippe Sand.
This sand was imported into Britain before the war for the
making of silica- ware and certain special varieties of glass ; but
its use was not extensive. Two different samples of this famous
glass-sand from DOrentrup, Saxony, were supplied to the writer
through the kindness of Dr. Walter Rosenhain, F.R.S., Director
of the Metallurgical Department, National Physical Laboratory,
Teddington, and were subjected to analysis and examination.
The sand occurs in deposits of Miocene age, and is associated
with rafts of braunkohle*. In this connexion it may also be
noted that the valuable glass-sand of Hohenbocka in Prussia,
occurring in Miocene strafe, is also associated with carbonaceous
layers f.
Both samples of Lippe sand are beautifully white, of better
colour even than that from Fontainebleau. The better sample is
finer in grain and remarkably even, while the second is rather
coarser. The chemical analyses are as follows :
I. H.
SiO a 99-88 per cent. 99-73 per oent.
A1 2 3 0-18 0-20
Fe a 3 J n.d. n.d.
Loss on ignition . . . 0*21 0-23
Totals 100-27 per oent. 100-16 per oent.
* Jahresb. nieders&onB, geol. Yer, 1910, p. 185 ; and Zeitsohr. deutsoh.
.geol. Geaellsoh. Band xl., 1888, p. 310.
f K. Keilhaok, Jahrb. K.-prenss. geol. Landesanat. 1908, Band "rix. pt. ii.
p. 214.
J Separate estimation of iron gave : I. 0-02 per oent., II. 0-03 per cent.
Analyst ; B. Spencer. These values are probably too high.
LIPPB SAJrt). 131
It is said that, such is the remarkable constancy of chemical
purity, the sand is guaranteed when sold to contain 99 '98 per
cent, of silica.
The mechanical analysis of the finer and better sample is :
>0-S & <1 mm., one or two grains; >0-25 & <0'5, 78'6 % ; >0-1 &
<0-25, 19-9 % ; >0'01 & <0'1, 0'4 % ; <0'01, 1-1 % *. Total eand-
grade: >0'1 &,<! mm., 98'5 %.
PCS NS FS _s_ _c S "I
L tr.' 78-6' 19-9' 0-4' 1-1 5 98-5 'J
Measurement under the microscope shows that the average dia-
meter of the grains is O3 mm. (or perhaps slightly less). They
are composed, with the exception of the tew detrital minerals, of
colourless clean quartz and a very little felspar, subangular to
angular in shape. The mechanical analysis (if the second
sample is :
>0'5 & <1 mm., 10-2 % ; >0'25 & <0'5, 85'8 % ; >0'1 & <0-25, 1-4 % ;
>0-01 & <0'1, 1-0 %j <0-01, 1-6 % *. Total sand-grade: >0'1 &
<1 mm., 97-4 %.
PCS MS FS ^_ _c _S -1
LlO'2' 85-8' 1-4' I'O' 1-6 J 97 : 4'J
The grains, which are subangular, are similar under the micro-
scope, but are for the most part nearly 0'5 mm. in diameter.
The heavy residue of minerals was small in each case (less than
O'Ol per cent, by weight), but, as is often the case, was greater in
the finer sand than in the coarser.
The former yielded a pretty residue consisting of abundant zircon
and red-brown rutile, rather rounded, and averaging 0*12 mm.
diameter, together with large Icyanite fragments up to 0'7 mm.
long, and coai-se staurolite and tourmaline grains. The stiiurolite
is deep golden-brown in colour, of diameter 0'2 to 3 mm. The
tourmaline occurs in grains up to 0'3 mm. diameter, of brown,
greyish, greenish blue, and deep blue colour. Magnetite, ilmenite,
leucoxene (0'2 to O3 mm. diameter), and limonite occur. Small
.and non-pleochroic dusky grains of andalusite occur less com-
monly, and chlorite also was seen.
The second sample yielded a rather coarser residue, consisting of
.abundant pleochroic andalusite (0'3 mm. diarn.), krge, yellow,
grey-brown, and greenish tourmaline (O3 mm. diam.), deep green
hornblende (0'2 mm. long), and ilmenite. Staurolite and zircon
occurred in small grains 0'05 mm. long. Chalcedony wa,s also
seen in the sand.
* Hygroscopic water included.
K2
132
TOBEIGN GLASS-SANDS.
Fontainefcleau Sand.
The sand, of Upper Oligocene (Stampian) age and associated
with lignites *, occurs in considerable quantities at Fontainebleau,
near Paris. . ...
The- mechanical and chemical composition are given in the
Tables, and the general properties are discussed in Chapter V.
The sand costs upon delivery at British works from 12s. to 39s.
per ton (rising to 50s. and 60s. through war-difficulties), according
to distance brought on mil, an average price being 17s. The cost
lias, of course, increased owing to the war ; and for some time after
the outbreak of war, as well as again at the time of writing, diffi-
culties existed, due to shortage of labour and ships, in getting it
through to England and Scotland.
Belgian Sand.
The sands cost, upon delivery in this country, from 4s. to 1G.
per ton. They often arrive as balkst, packing for bottles, etc.
Large quantities were sent from the Campine.
Some of the sands are shipped from Rotterdam, and the unequal
qualify since the outbreak of war leads to the suspicion that some
of those now being supplied may be inferior Dutch sands. Much
variability in tint and slight differences in mechanical composition
occur (see Tables, pages 166, 167, and Fig. 10, page 50). The sands
may he almost white, a very pale grey, or a marked pale pink, in
part due to the presence of pink quartz. Their iron-content is
slightly greater than that of Fontainebleau sand, and they burn to
a rather darker pink shade. Washing does not improve the colour
noticeably.
One sample from Barnsley Glass-works, which was analysed,
proved to have the following chemical composition :
Si0 2 99'38 per cent.
ALfl n 0-30
Fe.,0., 0-02
Losa on ignition 0'28
Total 99-93 per cent.
Mechanical analyses show the following grade-proportions :
-
CS.
>0-5 &
<1 mm.
MS.
>0'25 &
<0-5.
FS.
>0-1 &
<0-25.
s.
>0-01 &
<0-1.
0.
<0-01.
S.
Total sand-grade :
>0-1 & <1 mm.
Knottingley
Glass-works.
Barnsley Glass-
works
9-6%
<0-1
83-3 %
99-3
5-9%
0-3
1-2%
fl-4.
0-0%
A.A
98-8 %
yy G
TVT * liS^" 1 . 3 * k Fenme de Fontainebleau," Bull. Serv. Carte g<5ol. France,
No. 122, vol. xuc. (1909) p. 9 ; and numerous other references.
BELGIAN AND DUTCH .GLASS-SAJfDS.
133
Quartz, somewhat rounded to subangular, makes up the bulk o
the sand, but cleavage-flakes of felspar are to be seen. The heavy
residue is small, and of the type which in Britain characterizes the
Pliocene deposits. Among the coarse dense grains are kyanite,
andalusite, staurolite, rutile, yellow-brown tourmaline,, iron ores,
etc.
Dutch Sand.
The prices of Dutch sand have varied considerably in pre-war
and present times, the range being from 9s. to 28s. per ton.
Only a few samples have been analysed. They had a slight
grey or brown colour, some darker than Belgian sand, and differed
to some extent in grade-percentage (see Tables, pages 166, 167, and
Fig. 10, page 50). Occasionally the sand is white and equal in
quality to that from Fontainebleau.
The chemical analyses of two samples are as follows :
Al,0.,
Pe.,0'., .
CaO '
MgO
LOBS on ignition
Knottingley
Glass-works.
99-23 per cent.
0-50
0-02
n.d.
n.d.
0'22
Edinburgh & Leith
Glass-works.
99-63 per cent.
0-35
0-03
0-08
trace
0-19
Totals 99-97 per cent
100-28 per cent.
The grading composition is indicated by the following results of
mechanical analyses :
OS.
MS.
PS.
B.
c.
s.
>0'5&
>0-25 &
>o-i &
>o-oi &
<fO-l
Total sand-grade :
<1 mm.
<0-5.
<0'25.
<o-i.
'
>0-1 mm.
Knottingley
Glass-works.
0-7%
68-0 %
30-8 %
0-5 %
o-o %
99-5 %
York Glass-
works
0-4
93-5
4-8
1-3
o-o
98-7
The heavy crop is a rich and abundant one, consisting of well-
rounded grains 0'15 to 0-2 mm. diameter. The minerals present,
besides quartz and felspar, include purple and brown tourmaline,
epidote, staurolite, kyanite, red gamet, green hornblende, scircor,
andalusite, muscovite, ilmenite and leucoxene, magnetite, limonite,
etc.
134 FOREIGN GLASS-SANDS.
AMERICAN HIGH-GRADE GLASS-SANDS *.
For the samples of sands upon which the following descriptions-
are based, the writer is indebted to Dr. G. Otis Smith, the Director
of the United States Geological Survey.
The beauty and high quality of the best American glassware
have long been known to those concerned with the industry in
Britain. It may therefore be of interest to give a brief description
of the best glass-sands produced in the United States. The
samples were collected by Mr. Ralph W. Stone, whose valuable
accounts of the American glass-sands and their treatment have
been of great use to British workers. For additional information,
therefore, reference should be made to his descriptions of some of
the sands in Bulletins 285 and 815 of the United States Geological
Survey and to the Annual Reports on Mineral Resources (e. g.,
1911-15). The following notes are based upon examination of
the samples supplied, but the accompanying letters from the
sand-merchants have given information as to the treatment to-
which the materials have been subjected.
It will be observed that the crushing, screening, washing, and
drying of the sands are more carefully and thoroughly carried out
across the water than here. British glass - manufacturers will
doubtless note this with interest, and endeavour to impress the
fact upon the sand-merchant at home. We should remember,
however, that the American quarrying and treatment are earned
out upon a large scale and that greater facilities for transport appear
to exist in the United States than in this country.
For comparison with British deposits, it is interesting to note
that the glass-sands are obtained by the treatment of friable sand-
stones, all of which are of considerable geological age. They
range from Cambrian quartzite to Carboniferous sandstone.
Similar materials have been recommended from these islands,
and the writer has dealt elsewhere with such resources. It is.
interesting to note, however, that all the best West European
glass-sands, including many of those from the British Isles, come
from geological deposits of Tertiary age, /. e., are comparatively
recent in formation.
The fact that practically no compound grains are present in
these American glass-sands points to friability of material and
care in treatment. All are highly quartzose and none very
aluminous in character. The alkalies have not been estimated,
since in most cases they are either absent or exceedingly small in
amount f. The mineral-content in all the sands is small, and the-
few detrital minerals are mostly of the common, very stable, type.
The iron-content throughout is remarkably uniform, and low,
* This aooonnt is reprinted with slight modifications from the ' Trans-
actions of the Sooiety of Glass Technology, 1 vol. i. (1917) p. 147, by permission
of the Council of the Sooiety.
t All the analyses have been made upon the treated samples aa received.
SANDS FHOH OTTAWA, ILLINOIS. 185
namely, about O02 per cent. In some of the sands, such as those
from the St. Peter's sandstone, the very pure appearance of the sand
would lead the observer to expect a smaller percentage even than
this. When the heavy minerals are examined, the reason is clear.
In these cases, the iron-percentage is due to the authigenous pyrite
(FeS a ) present. Most of the sands show no change of colour on
ignition.
Sufficient material could not be spared for the purpose of working
out the mineral composition of each sand exhaustively.
Sand from the Ottawa Silica Company, Ottawa, Illinois.
The sand is produced by crushing the very friable St. Peter's
sandstone of Carboniferous age ; the Company state that it lias
been washed twice, steam-dried, and screened. It is slightly
greyish in colour, and consists of beautifully rounded grains, a
few of which are spherical, most being spheroidal. The surfaces
are in many cases roughened and etched. A few large grains
occur.
The chemical analysis quoted by the Company is :
Si0 2 99-82 per cent.
Al a O a andFe a O, ... 0-05
CaOandMgO 0-13
Total 100-00 per cent.
and that by Dr. Harwood and Mr. Eldridge :
Si0 2 99-48 per cent.
ALO., 0-16
Ie 2 3 0-02
CaO 0-11
MgO 0-05
Loss on ignition . . . 0-13
Total 99-95 per oent.
The mechanical analysis is as follows :
>1 mm., 0-5 %; > 0-5 & <1 mm., 21-6 %; > 0-25 & < 0-5, 75'6 %; > O'X
& < 0-25, 1-3 %; > 0-01 & < 0-1, 0-3%; < O'Ol, 0>7 %. Total sand-
grade, >0-1 mm., 99'0 %.
rvos cs[ MS FS _s_ _o_ _s -i
L.0-5' 21-6' 75-6' 1-3' 0-3* 0-7 '' 99'0'J
The heavy detrital minerals are small in quantity (O02 per
cent.) and of little interest. Many are well-rounded, blue and
brown tourmaline, zircon, and large garnets (0'2 mm. diameter)
being notable. Pyrite with excellent crystal form is abundant,
and is undoubtedly authigenous, that is, has been produced since
the deposition of the sandstone. It has suffered no abrasion. Its
136 POBEIGN GLASS-SANDS.
presence probably accounts for the 0-02 per cent, of Fe a 3 indi-
cated in the analysis, an amount larger than the appearance of
the sand would lead us to expect.
Sand from the Wedron Silica Company, Ottawa, Illinois.
This sand is of the same age as the kst, and is stated by the
Company to be washed twice, thoroughly dried, and screened. It
is a beautifully white, clean sand, composed of perfectly rounded
grains (Plate V. fig. 2). The description of the Ottawa Silica
Oompany's sand applies to this sand also.
Dr. Harwood's chemical analysis is as follows :
SiQ, 99-58 per cent.
Al/) a 0-12
Pe 3 3 0-02
CaO' 0-13
MgO trace
Loss on ignition O'l 7
Total 100-02 per cent.
The mechanical analysis indicates :
> 0-5 & < 1 nun., 6-1 %; > 0-25 & < Q'5, 88'4 %; > O'l & < 0-25, 5vL %;
>0-01 & < 0-1, 0-2 %j < 0-01, 0-2 %. Total Band-grade, >0'1 mm.,
99-6 %.
TOS MS FS _s_ _c_ S "I
|_6-r 88-4' 5-1' 0-2' 0-2 ; 99'6j
The heavy detrital minerals, as before, are highly rounded,
averaging - 12 mm. diameter. The pyrite, which is again abun-
dant, is clearly not detrital.
Sand from the Berkshire Glass-Sand Company, Cheshire,
Mass.
The sand is produced from a crushed Cambrian quartzite. The
Company state that it is washed three times and passed through
a 40-mesh brass wire-screen. An average sample of the sand
taken from the quarry (and therefore unwashed) by Mr. H. C.
Demming, who was investigating silica-sands for filtration-plant,
had a composition as follows :
Silica 99-28 per cent.
ATninrnii. 0'49
Iron oxide 0-34
Lime 0-12
Magnesia 0-003
Phosphorus oxide 0-0047
Sodinm and Potassium oxides ... 0-38
Sulphur 0-0096
Organic matter and loss 0-17
Total 100-7973 per cent.
CHESHIRE AND BEBEELEY SPRINGS SANDS. 137
Dr. Harwood's analysis of the washed sample supplied is :
Si0 2 99-00 per cent.
AljO., 0-30
Fe 2 0, 0-03
OaO 0-15
MgO none
Loss on ignition . . . 0-21
Total 99-69 per cent.
A mechanical analysis gave the following information :
>0-5 mm., none ; >0-25 & <0-5, 76-6 % ; >0-1 & <0'25, 21'3 % j >CH)1 &
<0-1, 0-3 % ; <0-01, 1-8 %. Total sand-grade, >0'1 mm., 97-9 %.
T MS FS so S
[_76-6' 21-3' 0-5' 1-8 ; 97'9'
The sand is rather fine-grained, sugary to the touch, and fairly
angular. The detrital mineral assemblage is greater in amount
(0'04 per cent.) and more interesting than that of the Illinois
sands. Much limonitic matter occurs, and rnuscovite mica,
chlorite, green hornblende, tourmaline, and zircon are also present.
The sand is widely used for the finest cut-glass.
Sand from the Berkeley Glass-Sand Company, Berkeley
Springs, W. Va.
This sand is the well-known high-grade deposit from Berkeley
Springs, used so largely for table-glass and the best ware. . It is
produced by crushing the Oriskany sandstone of Silurian age.
After being crushed, it is sent through a wet screen, then
steam-dried, and, finally, once more screened. It is kept in concrete
storage-bins of about 1500 tons capacity, the daily production being
about 400 tons.
The chemical analysis indicates (H. F. H. and A. A. E.) :
SiO, 99-65 per cent.
Al 2 6 a 0-11
Pe a O a 0-02
CaO 0-12
MgO trace
* Loss on ignition 0-23
Total 100-13 per cent.
The mechanical composition is as follows :
>0-5 & < 1 mm., 1-5 %; > 0-25 & < 0-5, 97'1 %; > 0-1 & < 0-25, 0-8 %
>0-01 & < 0-1, 0-2 %; <0-01, 0-4 %. Total sand-grade, >0-1 mm.,
99-4 %.
PCS MS FS _s_ c 3 "I
Ll-5' 97-1' 0-8' 0-2' 0-4 ; 99:4 J
The sand is pure white and consists of somewhat irregular
grains (Plate V. fig. 1). The detrital mineral percentage is
small (O'Ol per cent.), and is of the usual type.
138 TOJiEIGIT GLASS-SANDS.
Sand from the Jtmiata White Sand Company, Hanover St.*
Baltimore, Maryland.
The quany of the Juniata Sand Company is at Mapleton, Pa.,
and is also in the Oriskany sandstone. The rock is crushed, and
is said to go through five washings and three screenings.
Dr. Harwood's analysis is as follows :
SiO 99-33 per cent.
A1 2 6 3 0-16
Fe-jO, 0-02
CaO 0-15
MgO 0-11
Loss on ignition . . . 0-20
Total 99-97 per cent.
The mechanical analysis yields the following information as to
grades :
>1 mm., 1-6 % ; > 0-5 & < 1 mm., 11'2 % ; >0'25 & < 0'5, 85-7 % ; > O'l
& < 0-25, 0-4 % ; > 0-01 & < 0-1, 0-1 %;< 0-01, 1-0 %. Total sand-
grade, >0-1 mm., 98-9 %.
pTCS CS MS FS _B_ jo_ S ~]
L 1-6 ' 11-2' 85-7' (P4 1 <Fl' 1/0 ' 98-9J
The sand is subangular, a few spherical grains only being seen.
The detrital mineral percentage is small (0'02per cent.), consisting
largely of zircon, tourmaline (blue, green, and brown), ilmenite
and leucoxene (O2 mm. diameter), rutile, and blue anatase.
Sand from the Tavern Rock Sand Company, St. Louis.
This glass-sand is produced by crushing the friable St. Peter's-
sandstone of Carboniferous age. The Company do not wash any
sand, but crush, dry, and screen once. The quarries are at Pacific
Mo.
Dr. Harwood's analysis is as follows :
SiO a 99-08 per cent
A1 2 0, 0-23
Fe.,0., 0-02
CaO 0-21
MgO 0-05
Loss on ignition ... 0-35
Total 99-89 per cent
The composition as given by the Company is :
99-97 per cent
0-OS
i *_*' "ww
CaO
Total 100-00 per cent.
BALTIMOBE, ST. LOUIS (u.SA.) AND COLONIAL SANDS, 139"
For an unwashed sand, the silica-content is very high and the-
iron-percentage very low.
The mechanical analysis is :
>1 mm., a few oomponnd grains ; >0'5 & <1 mm., 2'7 %; >0'25 & <0'5,
90-1 % ; >0-1 & <0-25, 6-1 %; ><H)1 & < 0-1, 0'5 %; <0'01, 0'6 %,.
Total sand-grade, >0'1 mm., 98'9 %.
KCS OS MS IPS _B o^ _S_-|
r. ' 2-7' 90-1' 6-1' : 5' 0-6 ; 98'9'J
The sand is fairly well rounded, but not very clean. The
percentage of detrital minerals is low (O'Ol per cent.) and the suite
consists chiefly of zircon, tourmaline, ilmenite, and leucoxene
(O'o mm. diameter).
COLONIAL GLASS-SANDS.
Chemical and Mechanical Analyses of several glass-sands, from
India and Australia are given in the Tables on pages 154, 157, and
165. Of these, the Jubbulpore sand is that used in the well-known
Allahabad Glass-worls, while for the remainder of the samples the
writer is indebted to the respective Directors of the Geological
Surveys of India and Victoria. There is little doubt that the
Colonies can supply their own needs in this direction ; the sands
examined by the writer have all been of good quality.
140 LOCATION OF BEITISH GLASS-SANDS.
CHAPTER XII.
LOCATION OP BRITISH SUPPLIES OF GLASS-SANDS.
General Geological Considerations.
With the view of realizing the geological conditions under which
glass-sands occur, it is instructive to draw attention to several
salient facts, in order the better to search for suitable supplies.
The association of pure white sands with carbonaceous matter has
frequently been mentioned in this Memoir. Indeed, it may be said
that every example of the better-class glass-sands in Europe indicates
that the deposit is associated with vegetable matter. Lippe sand
occurs with rafts of braunkohle. Hohenbocka sand is associated
with carbonaceous layers ; Fontainebleau sand with lignites ; and
Aylesbury and Leighton sands with peaty layers. Some of our
purest sandstones occur in the Coal Measures, and, of second-rate
sands, the Heaclon Hill and Bagshot Sands of the Isle of "Wight
(Alum Bay, WhiteclifE Bay, etc.), Dorset, and elsewhere are inter-
bedded with lignites ; while the white beds of the Northampton
Sands (Inferior Oolite) and the Estuarine Series in Yorkshire are
found in deposits carrying plant-remains. The well-known Brora
coal in the Jurassic of north-east Scotland is associated with white
sandstones. The purest Ashdown Sands (Wealden) often carry
plant-remains. The glacial sands of Lancashire, used for the
making of window-glass, owe their low percentage of iron to the
association with peaty material.
The bleaching of red and yellow sands for a few feet in depth on
heaths and by the action of peat are other examples of this pheno-
menon. The explanation appears to lie in the reducing action of the
vegetable matter. Ferric compounds are reduced to the ferrous
state, and are often carried off in solution by percolating water.
Sometimes, however, they remain and are revealed by the return
of the red colour on burning.
Estuarine or lagoon conditions favour the formation of white
sands and sandstones. In our search for glass-sands, particularly
in the Colonies, we have therefore a valuable indication of the kind
of strata in which to look (that is, beds containing coal, lignites,
peaty matter, etc.) and the conditions under which we may expect
deposition of the required material to have occurred. Simplicity of
composition and perfection of grading are more likely to be found
in deposits of late geological age, as exemplified by the occurrence
of glass-sands in Western Europe. It is very improbable that any
new and large British supplies of first-class glass-sands will be
revealed ; but, in addition to the extension of supplies now being
GENERAL GEOLOGICAL CONSIDERATIONS.
141
exploited, deposits .of small extent, at present unknown, probably
occur in many cases in proximity to, or along the outcrops of,
strata previously worked.
Location of 'British Supplies of G-lass-Sands.
(a) England. Considered stratigraphically (that is, according
to geological age), the chief localities for English supplies, with
their corresponding geological horizons, may be detailed as
follows :
Recent (blown & shore) Sands.
Glacial.
Deposits of Doubtful Age (pre-GHaoial).
Upper Eocene.
Lower Eocene.
Lower Oretaoeous.
Middle Oolites.
Lower Oolites.
Upper Trias.
Lower Trias.
Carboniferous.
Headon Hill Sands.
Barton Sands.
Thanet Beds.
Lower Greenaand.
Tunbridge Wells Sands.
Ashdown Sands.
Kelloway Beds.
Upper Estuorine Beds.
Lower Estuarine Beds.
Keuper Waterstones.
Lower Bunter Sands.
Coal Measures.
Carboniferous Limestone,
Lower Ordovioian. Arenig.
Passim.
Crank, Roinford, etc, (Lanes).
Parsley Hay (Derbyshire).
Brassington (Derbyshire).
Low Moor (Derbyshire).
Eibden (Staffs).
Abergele (Denbighshire).
Ehes y oae (Flintshire), etc.
Alrnn Bay, I. of Wight, etc.
Fordingbridge (Hants).
Longdown, New Forest.
Charlton (Kent).
Rochester (Kent).
Aylesbury (Bucks).
Aylesford (Kent).
Blackgang Chine (I. of W.).
Godstone (Surrey).
Hollingbonrne & Bearsted
(Kent).
Leighton Buzzard (Beds).
Lynn (Norfolk).
Oxted (Surrey).
Eeigate (Surrey).
Ashurat wood ' (Sussex) .
Fairlight (Sussex).
Bulverhyth (Sussex).
Burythorpe (Yorks).
South Cave (Yorks).
Huttons Ambo (Yorks).
Corby, etc. (Northants).
Denford (Northants).
Spital (Cheshire).
Alderley Edge (Cheshire),
Workaop (Notts)
Guiseley (Yorks).
Mold (Flintshire).
Minera (Denbighshire).
Stiperstones (Shropshire).
Most of these localities and geological horizons are marked upon
the map, Plate VIII. The outcrop of each formation is shown, in
order that the direction of the possible extension of glass-sand
resources may be indicated. Take, for example, the deposit known
as the Lower Greensand, from which so many of our best glass-sands
142 LOCATION OF BRITISH GLASS-SANDS.
.are obtained. The bed is worked for glass-making at Lynn, Leighton
Buzzard, Aylesbury, and Aylesford; it was formerly worked at
Keigate, Godstone, Hollingbourne, and in the Isle of Wight.
Many of these localities are marked upon the map, and will be
seen to ba distributed over the outcrop of the bed. The area
marked by the outcrop is therefore that over which extension of
the supplies may be expected, and which should be explored for the
purpose. Another important horizon is that of the Inferior Oolite
(and in Yorkshire, of the Middle Oolites also). The beds are
frequently variable in this series of deposits, but investigation
of the outcrop will doubtless reveal extensions or new deposits of
the glass-sands.
The Tunbridge Wells Sands and the Ashdown Sands of the
Wealden area yield important supplies of pure sand-: The resources
have not been properly explored, and are certainly great. Unfor-
tunately, the localities where they are at present worked are not
well situated, for transport.
The Triassic System rarely yields sands pure enough for glass-
making, and when such are found the best glass- ware which can
be made from them is the class of work exemplified by pale bottles.
The Bunter Sands of Worksop, the Keuper Sandstone of Spital,
Cheshire, and possibly the similar rock at Alderley Edge, are
deposits of this character, the first two being fortunately situated
near to coalfields.
We may classify these localities broadly according to the kind
-of glass for which the sand may be used. Obviously the limits
will not be easy to define, and moreover, as mentioned in the
Preface, and also on page 151, with the advance of chemical
research upon glass, the latitude permitted in the composition of
sands for certain glasses is increasing.
The shore- and dune-sands occurring around our coasts are never
sufficiently pure for making other than common bottle-glass. The
Glacial Sand from Eainford, Crank, and Shirclley Hill in Lancashire
is used (after washing) for the making of window-glass and for
bottles. The Eocene sands mentioned from the Hampshire Basin
have at present been used only for better-class bottle-making, but,
-especially if they are washed, would be of value for such better
qualities as lighting-glass, laboratory-ware, etc. The Thanet Sands
from Kent are utilized for bottle-making only. Highly siliceous
sands, but less pure and more indurated than those from the Lower
Greensand occur in the Upper Greensand over a wide area from
the Isle of Wight to Wiltshire and Kent. Of the Lower Greensand
deposits, Ayles bury sand can be used for the manufacture of optical
glass, table-glass, chemical and pharmaceutical apparatus, and
many other varieties. Leighton and Lynn sands are successfully
employed for lighting-glass of all descriptions (electric-globes,
chimneys, etc.), for laboratory- ware, flint-bottles, pressed- ware, etc.
Aylesford sand at present goes only to bottle-making areas, but
like the sand from Reigate, could be successfully used for better
kinds of gkss. The Tunbridge Wells Sands and Ashdown Sands
UTILIZATION OF PARTTOULAK SANDS. 143
mentioned as occumng in Sussex, are not at present worked for glass
purposes, but as their analyses indicate (see pages 5254) they will
be of service for much good glass-ware, if economic considerations
permit their exploitation.
The English Jurassic strata are very variable, and it is possible
"that sands of great purity not known to us at present may turn up,
but their thickness and extent must be limited. The Corallian Beds
often contain claye}' or calcareous sands, and the Portland Sands
are too grey or brown and impure for glass -making.
The Kelloway Beds of Burythorpe and South Cave in Yorkshire
are of great value for the bottle industry of that county, and with
washing could be utilized for window-glass, lighting-glass, etc.
The Estuarine Sands from Huttons Ainbo, when washed, are
suitable for the manufacture of all qualities of glass, even up to
certain optical varieties. Unwashed, they would serve for bottle-
making, when the alumina they contain would be of much value
on account of its strengthening properties.
The Inferior Oolite " Sands " of the western area (Dorset Coast,
Bridport, Yeovil, Midford, Wotton, Cotteswolds, Cheltenham, etc.)
are too ferruginous and are occasionally calcareous. In the North-
ampton Sands and Estuarine Series, beds of whitish sand occur, but
are usually calcareous and never very pure. The detrital mineral
percentage is also high. Sands are said to have been worked for
glass-making about 1860 from Wansford, Apethorpe, Blatherwyke,
Burleigh, Gas wick, etc.; but the glass cannot have been of good
quality. Analyses of sands from Corby, Denford, etc.. will be
found in the Tables. The Estuarine Sands of the Midlands are
difficult to work owing to their variability, and are rather fine in
grain. Their suitability may be determined from their analyses
(pages 69, 156, and 162).
The Triassic sands are usually only of value for bottle-making,
when their alumina-content is a distinct advantage. They are
not sufficiently well-graded, nor are they very pure. "Washing
may improve the Spital sand sufficiently to render it pf value for
better-class glass.
The Lower Permian Yellow Sands are often incoherent, but are
too deeply iron -stained and calcareous all along their outcrop to be
of service.
The Carboniferous Period was one in which very pure sandstones
were laid down, the association with much organic matter being
here noteworthy. The decomposition of pure sandstones (e. gr., in
Ireland, near Glasgow, in Yorkshire, etc.) has given suitable sands,
and some very good examples have been found. Such rocks are
often crushed and washed before being put upon the market. In
some pale-coloured sandstones the cement is barytes (often derived
from Permian deposits above), when crushing hardly pays. Nothing
suitable seems to occur, nor would it be expected, in Devonian
strata.
Incoherent glass-sands are not to be expected from Archtean and
Palaeozoic rocks. Very pure quartzites occur, but the objections
144 LOCATTO^ OP BBITISH GLASS-SANDS.
to crushed, rocks (see page 80) and the question of expense almost
rule them out. Where veiy pure rocks have rotted in situ and
been exposed to washing by rain, etc., glass-sands may be pro-
duced. The whitish Cambrian quarbzites of the Midlands are not
sufficiently pure. Other Cambrian sandstones are less pure still,
and the same objection applies to Ordovician and Silurian Rocks.
The high alumina-bearing deposits of Derbyshire and Stafford-
shire (Parsley Hay, Newhaven, LongclifEe, Eibden, etc.) are of
very great value for refractory purposes, and so far as glass-
making goes, may be of importance for resistance-glasses such
as those required in the making of thermometers, ampoules,
combustion-tubing, etc., as well as for certain varieties of optical
gkss.
(b) Scotland. The Scottish deposits fall into two well-marked
groups. In the first group, and of little importance, are the dune-
and shore-sands worked for bottle-making. Those from Jura and
Islay are pure enough for better quality glass. In the second
group are the white, grey, or pale brown, soft and decomposed
sandstones of the Carboniferous System, which have been crushed
and treated to provide " sands " for refractory purposes and glass-
making. Such are the deposits belonging to the Millstone Grit,
Carboniferous Limestone Series, and Calciferous Sandstone Series
from Caldwell, Glenboig, Hailes, Kolwinning, Kongscavil, Levenseat,
and Plean. Of these, the best are the Levenseat, Caldwell, and
Kihvinning materials. The deposits are at present utilized for
low-grade glass-work only.
Many of the pre- Cambrian quartzites (e. g. Jura, Islay, Appin,
Killiecrankie, etc.) seem to be pure enough to crush as sources
of silica for glass-making and furnace purposes. The expense
involved in the crushing and subsequent treatment is, however,
prohibitive.
It is possible, though unlikely, that the pale-grey sandstone of
Brora (Middle Oolites) will be worked for glass-purposes, although
a low-grade fuel is close at hand.
The glass-sand resources of Scotland (and also of Ireland) are
thus much more limited than those of England. This is due to a
geological fact that of the absence or small development of those
stratigraphical horizons such as the Inferior Oolite, Lower Green -
sand, Eocene, Miocene, and Oligocene, which carry the best
glass-sands of "Western Europe.
(c) Ireland. The Irish supplies, in the same way, fall into two
well-defined classes. Shore- and dune-sands, usually suitable for
bottle-glass only, occur at Arda/ra (Co. Donegal), Ballycastle (Co.
Antrim), Coalisland (Lough Neagh), the shores of the river Foyle,
Millisle (Co. Down), Portrush (Co. Antrim), Rosslare (Co. Wick-
low), Saudymount Strand near Dublin, Silver Strand near Wick-
low), Sutton near Dublin, and other localities. The more valuable
DISTBIBUT1ON OF THE GLASS-MAKING INDUSTET. 145
" sands " are obtained from the decomposition or crushing of pre-
Oambrian rocks from Muckish Mountain (Co. Donegal), Westport
(actually from Acliill Island), Port-a-cloy (Co. Mayo), Tinanely
(Co. Wicklow), and other places, and of the sandstones of Carboni-
ferous age from Ballycastle, Cookstown, and Coolkeeragh.
The best Irish material is undoubtedly that from Muckish
Mountain, Co. Donegal. If the rock, which has already been
described as a partially decomposed quartzite, is *properly treated
by crushing, screening, washing, and drying, much of it will be of
service for the best optical glass and table-ware; the material
generally will be of use for all qualities of glass.
The old Irish glass-industry, carried on at Ballycastle, Limerick,
Cork, and Waterford among other places, was dependent upon
sands from Alum Bay (Isle of Wight), Lynn, and Eeigate.
Distribution of the Glass-making Industry in the
British Isles.
The Maps (Plates IX. & X.) show the localization of the chief
British glass-making areas *, and also indicate the localities
where glass-sands are worked, the ports into which foreign sands
are brought, and the coalfields. It is noteworthy that, with the
exception of the London district, in which almost everything is
bought, manufactured, or sold, the glass-making areas are situated
upon, or veiy close to, the coalfields. The industry consumes a
large quantity of fuel either directly as coal, or indirectly as
producer gas, etc., made from it. About a ton and a quarter of
fuel are consumed for each ton of finished glass produced in tank-
furnaces, and the consumption is greater in pot-furnaces. To yield
a ton of finished glass about a ton and a third of raw materials are
required. Coal, as is well known, is much more bulky and trouble-
some to move than the same weight of such raw materials as
sand, hence the location of the manufacture.
A general statement only is possible regarding the distribution
of the various kinds of glass-manufacture.
Optical glass is made in the Birmingham and Derby areas.
Table and decorative ware is manufactured in the Stourbridge
area near Birmingham, and in Manchester. London, Glasgow,
Wan-in gton, and Tutbury also contribute a certain amount. The
Stourbridge area (including Brierley Hill, Dudley, Walsall, etc.)
has long been famous for its beautiful "crystal" ware, both on
account of the quality of the glabs and the artistic character of the
work.
Scientific and technical glass is made in Edinburgh and Perth
as well as the following localities notable for laboratory and
* The writer was able to make this analysis as a result of visits to most
of the glass-works in the United Kingdom, and by using freely the excellent
card-catalogue of British Glass-Manufacturers, compiled by the Board of
Trade.
146 LOCATION OP BHITISH GLASS-SANDS,
medical apparatus: London, Leeds, Birmingham, Bamsley, Man-
chester, Dudley, and St. Helens. Gauge-glasses have been manu-
factured at St. Helens, Manchester, Birmingham, and Perth.
The manufacture of electric bulbs, etc. is now being earned on
near and far, but possibly the following may be considered the
chief areas : Stourbridge, Birmingham, Tutbury, Knottingley,
Barnsley, Leeds, London, and Tyneside.
For lighting-glass generally, the districts including London,
Manchester, Glasgow, Stourbridge, and Birmingham are note-
worthy, but the industry is carried on in many other towns.
For pressed-ware, Glasgow, Gateshead, Manchester, Warrington,
and Sunderland should be mentioned. Ship- and lamp-lenses are
made in the same areas.
The plate-glass industry is practically confined to the St. Helens
and Birmingham areas. Sheet-glass (window-glass, stained glass,
etc.), is made at St. Helens, Birmingham, and Oldbury, and staining
is earned on at Edinburgh.
In the matter of the total amount of raw materials used and fuel
consumed, the bottle-making branch of the industry is of course by
far the most important. It would be laborious to enumerate the
places at which bottles are made ; the manufacture is ubiquitous, and
only the chief localities can be mentioned. The South Yorkshire
area is, of course, the district par excellence for this work. The
bottle-industry of Tyneside has declined considerably. Medical
bottles are made in the London, Yorkshire, Gateshead, Manchester,
and St. Helens ^areas. Flint-glass bottles are produced in the same
districts, and for ordinary pale and dark bottles the following
localities also must be added : the districts of Sunderland, Edin-
burgh, and the Firth of Forth, Bristol, Newport (Mon.), Queen-
borough, Dublin, and Belfast.
Finally, as we should expect in a city winch manufactures
everything from a pin to a steam, engine, " egg-boilers " and time-
glasses, as well as the largest and most beautiful glass objects,
have their birth in Birmingham.
From what has been stated above concerning the kinds of glass
for which various British sands tire suitable, and the location of
both these sands and the corresponding glass-making areas, an
idea may be obtained of the transport required. To assist the
reader, the most important canals and navigable river-systems have
ben inserted on the Maps (Plates IX. & X.) together with tho
chief railway connexions. Transport by cnnal, sea, or rail, and
the very variable freightage iiites on diffeiimt railways will, however,
prevent comparison of the cost of moving any individual supply into
any particular manufacturing area. Nevertheless, the maps aro
given for what they are worth.
ECONOMIC CONSIDERATIONS. 147
CHAPTEK XIII.
ECONOMIC CONSIDEKATIONS. G-ENEEAL
i
In the development of the national resources of iu\v materials for
glass-making, questions of the cost of working, suitable treatment,
and transport play a most important part.
The margin of profit upon sands is small. This and the fact
that our large export coal-trade to the Continent enabled foreign
sands to be brought back very cheaply as ballast have been mainly
responsible for the small development of home resources of sands
and allied rocks, and for the lack of investigation into them. The
glass-manufacturer hitherto has not experimented to any great
extent with British sands, and is thus not generally acquainted
with their potentialities. Moreover, before 1914 it was by no
means certain that the best British sands actually reached the
manufacturer. Owing to lack of systematic working, want of
proper treatment and careful transport, British materials sent to
the glass-making areas have to overcome the prejudice which they
previously caused. This state of affairs is now rapidly being
remedied, since the cutting off of a considerable proportion of foreign
supplies of sand, due to the shortage of labour and shipping caused
by the war, has necessitated the systematic surveying and exploita-
tion of British mineral resources.
"When brought as ballast or packing for bottles, Belgian and
Dutch sands could formerly be delivered in our East Coast estuaries
at from 4s. to 5s. per ton. Fontainebleau sand was similarly
delivered (although it was not usually brought as ballast) at 10s.
per ton. These prices were doubled or trebled by the time the sand
reached inland glass-making districts, the railway freights on sands
being high. Even then the prices were below those of British sands,
since the cost of production of the latter was, as a rule, greater.
The prices at which sands etc. can be supplied are, of course, liable
to fluctuation according to the state of the labour market, cost of
fuel, etc. The figures quoted in the foregoing chapters therefore
vary within small limits.
Since the outbreak of war, partly owing to the greater demand
for British materials and partly as a result of certain facilities
having been granted which permit cheaper working, British
sands are being delivered at a price which will enable them to
compete successfully with foreign supplies. This improvement has
been effected and a systematic development made possible by the
high cost of foreign sands at the time of writing. Fontainebleau
148 ECONOMIC CCXN'SIDEBATIOB'B.
sand costs from 20s. to 60s. per ton, and Belgian and Dutch
sands 17s. to 28s. per ton, when procurable at all, according to the
position of the glass-making area. Even when prices return to
the normal level it will be possible for sand-merchants to exploit
their deposits if the demand is sufficient and if railway and canal
facilities are given. Some British sands have for many years been
carried as balkst from one part of the coast to another.
High class glass-sands, like the sand from Fontainebleau, have
frequently been used in this country in what might be termed
a wasteful manner for common glass-manufacture. In certain
maritime areas the sand can be obtained as cheaply as a less pure
one, and is therefore used. In other areas, rather than have
two different sands in use in the same glass-house, entailing
possibih'ty of confusion (which is perhaps unnecessarily feared),
the manufacturer uses the same sand for crystal table-ware and
also for commoner glass.
As a result of the importation of foreign sands, many British
supplies which were formerly worked have been abandoned. Giass-
sand appears to have fallen very considerably in price during the
last fifty years, for, in 1858, Aylesbury sand fetched 26s. per
ton at Aylesbury. In comparison with the present prices of
British glass-sands given in the previous chapter, it may be
stated that the average price in the United States of America
is 4s. per ton.
Each of the economic factors will be considered in turn.
Workability. In recommending sources of sand suitable for
glass-making (or, for that matter, any other industry) due con-
sideration must be given to the very important question of work-
ability. Since the margin of profit on sands and gravels is low,
attention must be paid to many factors other than those concerned
with the actual properties of the sand. Of the latter, the high
silica and low iron-content, low heavy-mineral percentage, absence
of harmful minerals, the even grade (medium or fine sand), and
possibly the shape, are the chief points to be considered. High
content of alumina and potash are at times valuable.
In the field occurrence of the sand, due regard must be paid to
the regularity of the deposit, the quantity available, the location
with respect to supplies of fuel and markets, and to transporting
routes, whether by road, rail, canal, or sea. The accessibility of the
deposits on hills, near bogs and marshes, on river-bottoms (from
which they are dredged), or in sea-cliffs as well as the conditions
of quarrying (workable depth below ground-level, position of water-
table, direction of drainage, thickness of overburden, etc.), and the
state of the local labour market have to be considered.
Treatment. The cost of washing sands is usually about 6d., or
perhaps rather more, jper ton. The additional handling and moving
consequent upon washing, drying, or treating magnetically a sand or
149
crushed rock, raise the cost considerably. Little washing is done
in England, and where it is carried on, ordinary draining and air-
drying are generally considered sufficient. The question is, of
course, one of cost ; hut washed deposits ought to be dried before
being put on rail or on board ship, for carriage should not be paid
upon water. Sands have the power of retaining a considerable
quantity of water, and their hygroscopic nature should be clearly
recognized. When crushing, washing, and drying are earned on,
the proximity and price of fuel supplies and the available water-
supply are important factors. If the crushing, screening, etc., of
pure sandstones and quartzites ever becomes a paying proposition
in this country, a considerable quantity of raw materials will be
found to occur in the older rocks, especially in Scotland and Ireland.
At present, for all but the best glass-ware, most of these are
ruled out. If a rock which has to be crushed is to be worked
successfully, it must be exceedingly good in chemical composition,
and fairly accessible.
Such rocks are at times of value for the alumina or the alumina
and potash, as well as the silica, which they contain. If they are
very hard, subsequent electromagnetic treatment is necessary, after
crushing, to free the sand from particles of steel, etc., derived from
the crushers. The cost of electromagnetic separation is Qd. or
more per ton, according to local conditions.
Where sandstones and quartzites are disintegrating under atmo-
spheric conditions, working may be carried out profitably, for the
crushing, washing, and drying are done by natural meins for
the exploiter, and the deposit often needs screening only. If such
deposits or other glass-sands are situated at a suitable elevation
and water-power is available, the use of monitors to wash down
the sand may be found advantageous. Gravity will then assist
in transport, and the washing may well improve the quality of
the product, both as regards mechanical composition and iron-
content.
The enormous glass-industry of the Middle Mississippi Basin is
supplied by crushing the St. Peter's Sandstone, which crops out in
the States of Minnesota, Wisconsin, Iowa, Illinois, Missouri,
Arkansas, etc. It is blasted, crushed, screened, washed, and dried.
The well-known Oriskany sandstone of West Virginia (Berkeley
Springs, etc.) is similarly treated (see Chapter XI.). Certain pure
quartzites are, it is said, now being crushed and treated in Sweden
to provide the sand for the manufacture of the well-known
laboratory glass. Before 1914, Fontainebleau and Lippe sands were
imported for the purpose.
Transport. Carriage by road is expensive, and aerial transit,
even for short distances and when aided by gravity, does not
always appear to be satisfactory, besides being frequently costly.
Railway freights upon sand (as well as upon the finished article,
glass) should be reduced so as to permit the transportation of
English glass-sand over any distance. Glass-sands, being purer,
150 ECOITOMIO
are unfortunately at present subject to a more expensive rate than
ordinary sands. Canal -transport should replace rail -transport
wherever possible in developing British sand-resources, and must
be further revived and reorganized for this purpose, as too few of
our deposits are situated near the sea or large rivers (see Plate IX.).
There is urgent need for the improvement, repairing, and widening
of canals. With a decrease in the cost of transport, it may well
be that the sand-merchant will find it possible to treat and
improve his sand (perhaps to dry as well as wash and screen it)
before delivery, and thus more successfully compete with foreign
supplies. Co-operation between users and producers ought to lead
to increased demand, and therefore to more extensive and cheaper
exploitation.
. The levying of greater import duties upon foreign sands may not
be desirable, but it may have to be considered. If British sands are
to be exploited to any large extent, the question of the necessity
for a revision of freights, leading to standardization and reduction
is urgent. It should be noted that certain Continental supplies
of glass-sand are larger, more regular and persistent, and in part
purer than deposits in our own country,
Statistics. The available figures relating to the imports and
exports of sands are of the most meagre character. In the Home
Office Returns of Minerals, etc. *, it is stated that the Production
of Gravel and Sand in 1913 was 2,409,152 tons of value 184,818,
and in 1914 was 2,498,872 tons of value 215,351. The value
was therefore about 1*. 6d. to Is. 8d. per ton. The production of
sandstone in 1913 was 3,977,303 tons of value 1,143,431, and
in 1914 was 3,464,528 tons of value 1,057,096. The value was
therefore about 5s. 9d. to 6. per ton. In 1915 the output of sand
and gravel was 2,350,267 tons of value 213,373 (Is. lOd. per ton),
and of sandstone, 2,520,856 tons of value 758,325 (6s. per ton).
No separate figures exist to indicate even what proportion of the
total was occupied by sand, much less to show what was the
separate production of building-sands, glass-sands, moulding-sands,
soap-making sands, filtration-sands, abrasive-sands, etc.
For the following figures dealing with imports and exports of
sands, the writer is indebted to the Comptroller- Q-eneral of the
Department of Commercial Intelligence of the Board of Trade. The
total value of the exports of Earth and Sand of British production
during the five years 1911 to 1915 was as follows :
1911 .38,884
1912 23,912
1913 23,470
1914 15,773
1915.... 10,655
* Home Office : Mines & Quarries General Eeport : Part 1H., Output for
1915 (1917), -and previous issues.
GKENEBAL BEMABKS.
151
STATEMENT showing the Imports and Ke-exports of SAND into
and from the United Kingdom in the years 1911-1916.
Total
Imports.
of which
Belgium.
from:
France.
Total
Be-exports.
1911
Tons
Tons
223,095
85,322
228,822
89,338
197,670
68,623
197,187
68,712
25,554
15,377
27,582
18,399
7
15
8
27
1912
1913
Tons
273,352
103,095
233,754
79,085
35,157
20,724
1
2
1914
Tons
195,860
80,643
150,945
54,165
33,523
19,173
1915
Tons
102,103
65,433
35,043
20,239
33,662
24,815
537
741
With the exception of a little special moulding-sand and fumace-
sand, this imported material may be taken to be sand for glass-
making purposes. The figures tell their own story of war-conditions.
General Remarks. As a result of the chemical investigation
which has been going forward while this geological enquiry has
been in hand, it has been found that a lower standard of purity
than that hitherto admitted may be permissible in glass-sands.
Owing to the paucity of chemists and works' laboratories in the
glass-trade generally, little check has been kept upon other raw
materials, and these have frequently been found to be impure. It
should be possible to obtain the latter in a high degree of purity,
and if any latitude is permitted, it should certainly be in the sand,
where freedom from iron and casual impurities is more difficult to
ensure than in manufactured chemical products. The sand has
often been suspected, while the manganese dioxide, red lead, lime-
stone, or even felspar, have been responsible for the^ iron. On the
other hand, by varying the composition of the glass, less pure sands
may be used to produce excellent ware, of water- whiteness and great
brilliancy. The limit of iron oxide in sands for certain optical
glasses may, according to Professor Sir Herbert Jackson, even
reach 0'04 per cent.
The cost of chemical treatment of sand may also not be
prohibitive when the manufacture of optical glass is under con-
sideration.
While there are deposits in this country equal in quality to
Eontainebleau sand, they do not appear to equal that deposit
in ' extent and maintenance of sample. Our very pure and well-
graded sands are of limited extent, bxit we possess large supplies of
sand suitable for flint-glasses, soda-glasses, laboratory- ware, lamp-
chimneys, globes, bottles, etc. Suitable sands for black and green
bottle-work are common enough, and are widely distributed. The
152 .ECONOMIC) CONSIDB!RA.TIO]!fB.
price paid for sands for common glass in many British areas is far
nigher than it need be.
Q-ood crystal -ware has been made from Aylesbury sand, and
the application of this and other sands to best glass-work is steadily
growing. Selected samples might well be tried for certain optical
glasses *. For such glass the variation in cost of sand is small
compared witb the considerable cost of production. It has been
said that the whole world's trade in optical glass would not yield a
stockbroker's profit. Before the war the production of optical
glass probably did not amount to more than a. few tons a year.
The price of the sand is therefore not such an acute question,
and a highly desirable sand will be obtained at any reasonable price,
even where transport is expensive.
Early in this Memoir it was pointed out that sands suitable for
glass-making (and therefore carrying a high percentage of silica,
or silica and alumina) were of great value to the steel-founder
for furnace-bottoms, soaking-pits, moulding- sands, silica-bricks,
crucible-making, etc. We must note that the price paid for
such sands by steel manufacturers and founders is usually well in
advance of, and sometimes double as much as, that which the gla.ss-
maker is prepared to pay. Freedom from iron oxide or a very low
percentage of it is not essential to the steel-maker ; it is therefore
desirable that the best silica-sands should, if possible, be retained
for glass-making. Many deposits exist which are of great use as
refi'actories, but are quite unsuitable for glass-making.
Glass-manuf acturers have been very fortunate in being able to
obtain from abroad large and constant supplies of their essential
raw material, pure sand, at a comparatively low price. The con-
stancy in grade and chemical composition has enabled them to go
forward with very little alteration of batch, and with no apparent
need for investigation and analysis. The future cannot be ignored.
It must be understood that foreign deposits, in particular those
of Fontainebleau, are not inexhaustible, nor is it likely that they
will always arrive in this country so cheaply or so true to sample
in consignment after consignment as they did before 1914. The
output of Fontainebleau sand might at any time be restricted for
domestic reasons, or a tariff might be put upon it. It therefore
behoves glass-manufacturers to investigate the properties of their-,
glass-sands and the questions of suitability or unsuitability of
British supplies. More skilled chemists must be employed .in the
works to investigate not only the finished products and the neces-
sary mixtures for special glasses, but also the chemical and
mechanical composition of their raw materials, including sand.
The discussion of the uses and nature of sands, and of the methods
* While this Memoir has been, in the press, excellent optical glass has
actually been manufactured from a number of British sands, many less pure
than Ayleabury Baud.
CONCLUDING fiEMAEKS, 168
of study, together with the requirements of good glass-sands, have
been expanded in this Memoir with the view of aiding glass-manu-
facturers to investigate sands for themselves. Chemical analysis
is familiar to all. Mechanical analysis can he carried out with
very little apparatus, which is also such as can generally be blown
in the works. Mineral analysis indicates the presence or absence
of certain objectionable minerals in glass-making, and will enable
the manufacturer to determine, within certain limits, whether his
successive consignments come from the same bed or quarry. The
last method of work, for example, is sufficient to prove at the
present time whether the consignments of sand, which may well
vary slightly in chemical or mechanical constitution, are the same
Belgian or Dutch sand as that hitherto obtained.
Our Colonial resources of sand, particularly with reference to
moulding (or, perhaps, refractories generally) and glass-making,
ought to be thoroughly investigated. If it becomes desirable that,
for certain special glasses, such as the valuable and important
optical glass, the Empire should become self-supporting, it is
highly probable that sands of sufficient purity and of suitable grade
will be found in the Colonies, and may be shipped home, possibly
as ballast. Such sands occur, among other places, in India, British
Guiana, South Africa, and Victoria. The pulps obtained by crushing
quartz-rock for extracting gold are often very pure ; they accu-
mulate in large quantities, but the remoteness of their location
possibly rules them out. A ' revival of interest has recently
taken place in Indian glass-making. The Tertiary deposits of
Northern India are of similar age and character to those of
Western Europe, which contain such excellent glass-sands. India
may, therefore, well be self -supporting in the matter of glass-ware,
and, if desired, may provide the necessary pure sands for British
pptical glass-making. This is one case among many, but it serves to
emphasize the desirability of further investigation and of closer union
in industrial and scientific questions between the Colonies and the
Mother country.
M.
154
STATISTICS.
TABLE I. BKITISH Q-L ASS-SANDS : IBON- CONTENT.
"With a few exceptions, complete analyses -were not made of the sands
mentioned below.
Percentage weights, as Fe a O s .
Page
Page
81
Pre-Gambrian :
MTirik]R'h MoTiTitflrin, Trench 1 ..
028
90
Jurassic :
Brora
12
: 81
81
2..
3-
022
009
65
65
Huttons Ambo, unwashed
washed
13
03
81
96
Bulk sample
Westporfc, unoruHhed
02
004
Weald&n
96
crushed, No. 3
04
"RnTliin
Ofl
93
Port-a-cloy (a)
1-82
52
Pairlight, old pit
02
93
(6)
09
52
"htiroh pit (hnlk)
02
93
(c)
23
52
,1 9 , another
023
Carboniferous :
52
54
selected..
Btdverhyth
002
04
86
Caldwell, washed and screened .
08
55
AshurHtwood (a)
01
91
Idookstown, red sand
04
55
(b)
015
91
washed
02
92
Goolk'OWB'gli j TiTvwftBJ 1 I'd , - .
13
Lower Qreensand
92
075
58
Leighton Buzzard, unwashed
14
89
Glenboig, N.B
27
58
washed , ...
09
82
(^niRftley, TinoTTi^herl
03
56
Tiynn (Boara), imwashed
19
82
09
56
,, ,, double washed
04
Londonderry
11
56
(Gay & Wilson)
16
115
Meldon rook, A ^
Fe a 8
03,
Eocene :
PeO ;
71
PoTfJingbTldg^, A ,
03
[
26 |
71
B
02
115
Tt -f
FeO !
69
Longdown, unwashed
09
15 !
69
06
83
Mold, unwashed ' . .
024
83
020'
115
Par china-stone, uncruahed
08
102
Doubtful age :
Edbden
38
9> ornahed
Permian :
Pontefraot, treated
09
Glacial :
71
washed
68
Trias:
64
Tfraipfnrd, irnw-nlied , . . . ...,.,,.,.
05
76
.Alderley TMge ., ,
12
64
,, washed
03
127
TJagleRoliffe, irntrefttfld , . . .
20
127
127
treated (coarse) . . .
(fine)
03 \
048 |
77
8hor0-8aiids :
^TdaTft, Mftghflrft
70
84
Spitftl, unwashed , ,. .
06
fflnTin.lri1ty , , , , ,
1-23
84
74
washed (another sample)
Worksop, unwashed
09 i
51 i
139
India, 21/186
08
74
,', washed (anaLJ.H.D.)
19 '
139
Z/624
24
These sands are also of value for refractory purposes.
155
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BRIT. RES,
Pz. II.
: ig. 1. Quartz (faint and^clear) and fel-
spar (turbid) In a good glas8 T 8and.
X40.
ig. 2.--Heavy mineral residue from a
British glass-sand: kyanite, stauro-
lite, tourmaline, ilmenite,/etc.
Epidote and a crystal
of Tourmaline (dart).
Fig. 3. Zircon and Rutile: harmful
minerals in glass-sands.
Photomicrographs of M{
Kyanite.
40.
Staurolite.
lS;.4v- Heavy minerals from Sands.
itted light).
RES. Q-LASS-SANDS, PL. Ill
Ftg. 1. Fontafnebleau Sand.
FFg 2 LippeSand.
f fr
..J
>,
cc
Ffg. 3. -Aylesbury Sand.
&*?('* --'"' ; i /^'
"^' ; S "'' V, .:'-.''.'
Fig. 4. Godstone Sand,
' -" i V -. -'
. i . -^ .if. 1 1 ,.,
" ''
Fig. 5. Burythorpe Sand.
Fig. 6. Crushed pock : Guiseley.
Photomicrographs of Glass-Sands (reflected light).
[All figures magnified 20 diameters,]
SETT. RES. Q- LASS- SANDS, PL. IV
*-
FTg. 1. Huttons Ambo Sand,
before being washed.
Fig. 2. Huttons Ambo Sand,
after being washed.
Fig. 3. Muckish Mountain Quartzite Fig. 4." Muckish Mountain Quartzite ;
ordinary light. crossed nicols. Same field as Fig. 3.
Fig. 5. Crushed Vein-Quartz,
Achill Island (Quality 3).
Fig. 6. Sand from King's
Photomicrographs of Glass-Sands (reflected light);*/ -
[All figures magnified 21 diameters.] - i / i " _1
SUIT. RES. GLASS-SANDS, PL. V.
X 21.
Fig. 1. Sand from Berkeley Springs, West Virginia, U.S.A.
r
Fig. 2;^ Sand from Ottawa, Illinois (Wedron Silica Company),
U.S.A.
Photomicrographs of American Glass-Sands
(reflected light).
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SKIT.
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Rikof's Machine for the Washing of Sands.
(Tha draimjg-oone shown in Kg. 18, p. 128, is partly obscured by the staging
and is marked by a white dross.)
Plate Yl
SKETCH-MAP SHOWING THE OUTCROPS OF THE GEOLOGICAL
FORMATIONS IN WHICH GLASS-SANDS OCCUR, AND ALONG
WHICH THE EXTENSION OF SUPPLIES MAY BE EXPECTED.
By Professor P.G.H.BOSWELL
ENGLAND & WALES
Bagahot Beds. etc. Oolite Somfc
Qreenaonrf [>^^S| Tnewaic Sonrfs
fl*o/s Sands for commm bottJe-gltus are not included.
PlateX
SKETCH-MAP SHOWING THE LOCATION OF THE CHIEF IRISH RESOURCES OF
GLASS- SANDS IN RELATION TO THE GLASS-MAKING AREAS,
COALFIELDS. RAILWAYS, AND INTERNAL WATERWAYS.
By Professor P. G.H. BOSWELL.
Glw-jnaking anas.
i!iO CoaJFiettte.
Gbw-sand producin.
The depth of colour in tht gktM- making or&ta yields tut indication of the
'. the greafoet depth of coJour reprettntiny
fia.ilna.ys in red.
Canals Waterways it
nd produced the palest colour
INDEX.
Note. Descriptions of particular Glass-Sands, etc. occur on pages
marked in black figures.
Aberdeen, 17, 165.
Abergele (Denbighshire), 79, 104,
126, 141, 157, 164.
Abrasive Sands, 3, 47, 59, 84, 97.
Absorbent Sands, 5.
Accuracy of Elutriation, 27.
Achffl Island (Co. Mayo), 96, 128,
145. See also Westport.
Acid Treatment of Sands, 126.
Agriculture, Irish Department of, 82.
.Agriculture, Sands used in, 2.
Air-blast, 124.
Alderley Edge (Cheshire), 76, 141,
142, 154, 162.
Allahabad Glass Works, 189, 157.
AUothigenous minerals, 10.
Alaop en le Dale (Derbyshire), 102.
Alum Bay, Isle of Wight, 72, 14,0,
141, 145, 156, 163.
Alumina-bearing Books, 14, 36, 42,
89, 98, 99, 106, 127, 143, 158.
AlnmiTiti., used in Glass-manufacture,
107.
American Glass-Sands, 34, 45, 48,
120, 134, 135, 136, 137, 138, 169,
170.
Amlwch, Anglesey, 96.
Ammonia, Use of in Elutriation, 22.
Analyses of raw materials, 152.
Anglesey, 96, 155.
Angularity of Sands 2, 8, 12, 46.
Antrim Co., Sands from, 77, 90,
165.
Apethorpe (Northants), 68, 148.
Aplite, 106, 115, 129, 159.
Apparatus required for Analysis,
16, 21.
Appin (Argyllshire), 95, 99, 129, 144,
155
Apted, A. B., 61.
Archasan Rooks, 76, 143. See also
Pre-Oambrian.
Ardara, Maghera (Co. Donegal), 77,
144, 154, 165.
Arenig deposits, 141.
Argyllshire, Quartzite from, 95, 99,
129, 144, 155.
Argyllshire, Pegmatites from, 114.
Arkansas, U.S.A., 149.
Arklow (Co. Wioklow), 97.
Arkwrig-ht find Eapaport, 81.
Arnold, Joseph, 51, 58, 156.
Arsenic, Use of, 36, 42.
Ashcroft, E. A., Process for extrac-
tion of Potash, 118.
Ashdown Sands, 35, 52, 54, 140, 141,
142, 156, 162, 163.
Ashford (Kent), 162.
Ashgrove Loch (Kilwinning), 87.
Ashurstwood (Sussez), 55, 141, 154,
156, 162.
Aughrim (Co. Wioklow), 113.
Australia, Sands from, 139, 153,
157.
Authigenous minerals, 10, 117, 135.
Average Diameter of Grains, 27.
Aylesbury (Bucks), 12, 35, 47, 49, 50,
51, 56, 119, 126, 140, 141, 142,
148, 152, 156, 163.
Ayleaford (Kent), 35, 62, 141, 142,
156, 163.
Ayrshire, Sand from, 87.
BadcallPier (Sutherlandshire), 110.
Bagshot Sand, 18, 35, 69, 71, 72, 73,
140, 141, 154, 157, 163, 164.
Baked Clay added to batch, 99,
108.
Balgownie Links (Aberdeen), 17.
172
INDEZ,
BaUinderry E. (Cookstown), 91.
Ballyoastle (Co. Antrim), 77, 90, 144,
145, 155, 161, 165.
Ballymanus (Go. Wicklow), 113.
Ballymoney (Co. Antrim), 91.
BallynesB (Oo. Donegal), 82.
BallyphetriBli (Tiree), 165. ;
'Ballyshannon (Co. Donegal), US.
Baltimore, U.S.A., 138, 169, 170.
Bank-end Farm, Kilwinning, 87.
Banbnry, 69.
Bardaey Island (CarnarronBliire),
Vein-quartz from, 97.
Barium Felspar (Celsian), 110.
Bamsley Glass- Works, 40, 124, 132,
146, 166, 167.
Barton Sands, 70, 141
Barytes, Cementing Sandstone, 36,
143.
"Batch" for Glass-making, 35.
Bawsey Siding, near Lynn, 58.
Bawtry (Yorkshire), 154.
Bearsted (Kent), 63, 141, 156, 163.
Bebington (Cheshire), 85.
Bedfordshire, Sands from, 4, 44, 58,
141. See also Leighton Buzzard.
Beinn Ceannaheinne, Dumess, 110.
Belfast, Bottle-making at, 85, 92,
146.
Belfast Lough, 157.
Belfast, CoUin Glen, 117, 159.
"Belgian Bed" Moulding - Sand, 29,
30.
Belgian Glass-Sands, 34, 44, 46, 49,
50, 51, 56, 67, 126, 132, 147, 153,
166, 167, 168.
Belleek (Co. Fermanagh), 111, 112,
113, 114, 160.
Belleek Pottery, 111, 114, 160.
Belmnllet (Co. Mayo), 114, 160.
Berkeley Sand Co. ("W. Va.), 137,
169, 170.
Berkeley Springs (W. Vs.), 48, 137,
149, 169, 170.
Berkshire Sand Co., Cheshire, Mass.,
136, 169, 170.
Bexhill (Sussex), 54, 154, 162.
Birkenhead, 86.
Birmingham, Glass-making at, 82,
145, 146.
Birmingham Public Library, 33.
Birmingham Moulding-Sand, 30.
Bisohof, C., 33.
"Blaokfoot" Moulding-Sand, 73.
Blaokgang Chine (Isle of Wight), 141,
168.
Blackheath (OldhaTen) Beds, 164.
Blake Moor (Derbyshire), 102.
Blatherwyke (Northants), '68, 143.
" Blowing-out" of fine material, 45.
Blown-Sands, 17, 32, 44, 77, 141,
165.
Blyth (Northumberland), 165.
Boam, Joseph Ltd., 56, 154, 163.
Bodmin (Cornwall), 107.
Bohemian Glass, 35, 48.
Solas, T., 38.
Bottle-Glass, 35, 42, 43, 48, 56, 64 r
66, 68, 73, 75, 76, 85, 89, 92, 99 r
116, 142, 143, 146.
Bovey Beds, 31, 101, 103.
Brandenburg, Sand from, 36.
Bramford (Suffolk), Glauoonite from,,
117, 159. '
Brandy Gill, Granophyre from, 106,
158.
Brasaington (Derbyshire), 98, 103,
157, 164.
Braunkohle associated with Glass-
Sands, 130, 140.
Briok added to batch, 98.
Brick-making, Sands for, 4, 29.
Bridgwater Brick added to batch, 98,
158.
Bridport (Dorset), 45, 148.
Brierley Hill (Staffs), Glass-making-
at, 145.
Bristol, Glass-making at, 71, 146.
British Guiana, Sands from, 153.
British Sands suitable for Glass-
making, 49.
British Silica and Minerals Co. Ltd.,,
91.
Brockenhurst (Hants), 73, 163.
Bromley (Kent), 32, 164.
Bromoform, Use of, in separating-
minerals, 16.
Brora, N.B., 90, 144, 154.
Buckinghamshire, Sands from, 49, 51,
141, 156, 163.
Building-Sand, 4, 56, 58, 60.
Bulverhyth (Sussex), 52, 54, 141 r
154, 162.
Bunter Sands, 74, 103, 141, 142, 154,
162.
Burleigh (Northants), 143.
Burning of Sands, 125.
Burns, J., 92.
Burythorpe (Yorkshire), 32, 45, 49 r
67, 68, 141, 156, 162.
Burton (Derbyshire), limestone from,
36.
Calcareous Sands, 2, 42.
Caloiferoua Sandstone, 91, 144, 145,
154, 155, 161.
Caloite in Sands, 42. .
CaldweU, N.B., 86, 144, 154, 155,
161. :
INDEX.
173
Caldwell Sand Co. Ltd., 86.
Callovian Sand, 32. See also Bury-
thorpe.
Comas, Eigg, 77, 165.
Cambrian Books, 134, 136, 14,4, 169,
170.
Campine (Belgium), Sand from, 132.
Canal-transport, 146, 150.
" Candle Clays," 101.
Cantor Lectures on Optioal Gloss,
49.
Carbonaceous matter associated with
Sands, 11, 51, 52, 90, 101, 103,
130, 140.
Carboniferous Limestone, 5, 83, 104,
141.
Carboniferous Limestone, Hollows in
surface, 102, 104.
Carboniferous Limestone Series
(Scotland), 86, 87. ,
Carboniferous Sandstones, 77, 82, 83,
84, 86, 87, 88, 89, 90, 91, 104,
134, 135, 143, 144, 145, 154, 155,
161.
Carboniferous System, alumina-
bearing Sands from, 98.
Carborundum, Sands for making,
3.
Cardiganshire, Rooks from, 97, 164.
Carnarvonshire, Hooks from, 97.
Carsington Pastures (Derbyshire),
103, 164.
CastlecaldweU (Co. Fermanagh), 111.
Castiefreke (Cork), 78.
Castle Howard (Yorkshire), 66.
Caswiok (Northants), 143.
Caterham (Surrey), 60.
Celsion (Barium Felspar), 110.
Cement, Sands for, 4.
Cements of Sandstones, 11.
Ceramic Society (American), 34.
Ceramic Society (English), 83, 34.
Champagne, Sands from, 35.
Chance's Quarry (Leighton Buzzard),
58.
Channel Islands, GHauoonite from,
117.
Chapel Combe (Cornwall), 101.
Charlton (Kent), 29, 45, 50, 73, 98,
141, 156, 164.
Cheltenham, 143.
Chemical Analyses, 121, 154, 155,
156, 166, 168, 169.
Chemical Composition of Glass-Sands,
41.
Chemical research on Glass, 142,
151.
Chemical Ware, 35, 100, 145.
Cherry Garden (Ashuretwood), 55.
Cheshire, Mass., 136, 169, 170.
Cheshire, Sands from, 45, 84, 141,
142. See also Spital.
Chesterfield Canal, 75.
China-clay, 9, 98, 100, 101, 107.
Ohina-olay, Felspar and Silioa Co.,
Ltd., 93.
China-stone, 114, 115, 128, 154,
159.
Classification of Grades, 13.
Clayoastie, Toughol, 78.
Clay grade, 9, 11, 100, 124.
Cliff-End, Winohelsea, 53.
Clonakilty (Co. Cork), 154.
Cluff, R., 91.
Clyneleish Quarry, Brora, 90.
Coalisland, L. Neagh, 77. 144, 165.
Coal-Measure Sandstones, 12, 79, 82,
91, 140, 141, 155, 161.
" Coarse Micas," 100, 159.
Coating on Sand-grains, 11, 17.
Colcerrow (Cornwall), 159.
Cole, Prof. G. A. J., 113.
Coleroine, 93.
Collin Glen, near Belfast, Glauoonite
from, 117, 159.
Colonial Sands, 139, 140, 153, 157,
165.
Colouring of Gloss, 37.
Colour of Glass-Sands, 119.
ColumbHQe (Co. Donegal), 113, 160.
Combustion-tnbing, 35.
Composition of Sands, 1, 9.
Concrete, Sands for, 4, 58.
Connemara Quartzite, 155.
Continental Glass-Sands, 89, 130, 147,
149, 150, 160, 166, 167.
Continental Glauconites, 117.
Conway, 104.
Cookstown (Co. Tyrone), 91, 145,
154, 155, 161.
Coolkeeragh (Co. Londonderry), 92,
121, 145, 154, 155, 161.
Oorallian Sands, 4, 90, 143.
Gorby (Northants), 68, 141, 162.
" Oordy" Glass, Cause of, 38.
Core-Sands, 5.
Cork Co., Sands from, 78, 145.
Cork Exhibition (1902), 82.
" Cornish Red" Moulding-Sand, 29.
Cornwall, Rocks from, 5, 9, 29, 32,
100, 101, 107, 113, 154, 159, 160.
Cost of foreign Sands, 147.
Cotteswold Sands, 32, 45, 143.
Cowie, N.B., 89. -
Crank (Lanes), 64, 141, 142.
Greeohbarrow (Dorset), 73.
Cretaceous Deposits, 3, 4, 9, 81, 141.
(See also Greensanda and Weolden.)
Croagh More (Co. Fermanagh), 112.
Crofthead, N.B., 88.
174
INDEX.
Crook's Elntriator, 21, 22, 25.
Crook, T., on Sands, 17.
Crucible-making, Sands for, 5.
Crushing of Rooks, 48, 79, 128.
Crushing Strengths, 86, 95, 128,
129.
Cryolite, 86.
"Crystal" Ware, 37, 48, 128, 145,
152.
Culbin (Nairn), 165.
Culm Shalea (Carboniferous), 115.
Curracloe, Eoaalare, 77, 165.
"Cut-glass," 37, 47, 48, 128, 137,
145, 152.
Daliadian Books, 77, 81, 98, 95.
Danish Glass-Sands, 34, 45, 168.
Dartmoor, Alumina - bearing Sands
near, 9, 101.
Dartmoor Granite, 9, 101, 115.
Davidson, J~. H., 75, 94.
Decolorisers of Glass, 37, 42.
Decorative "Ware, 145.
Denbighshire, Sandstone from, 104,
141, 164.
Denford (Northants), 68, 141, 143,
156, 162.
Denmark Geological Surrey. 28, 34,
168.
Deposition of Sands, 8.
Deposits carrying Alumina and
Silica, 98.
Deposits in North Wales, 104.
Derby Glass-works, 40, 85, 145, 166,
167.
Derbyshire, Sands and Books from,
5, 36, 85, 102, 141, 144, 157,
164.
Derrylogan (Co. Donegal), 113.
160.
Derryrona (Co. Fermanagh), 111
160.
Desert-Sands, 12.
Detrital Minerals, 10, 43.
Devon, Kaolin from, 100.
Devon, Refractory Sands from, 5, 32
101.
Devon, Aplite from, 115, 159, 161.
Devonian Rocks, 143.
" Devonshire Hard Purple Stone "
115.
Diatomite, 5.
Dinas bricks, 38.
Distribution of Glass - making in
British Islea, 145.
Dog-Trap Gully, Victoria (Australia),
139, 157, 165.
' Dominant Diameter," 28.
Donegal, Pegmatites from, 114, 160.
Donegal, Rocks from, 77, 81, 112,
113, 154, 155, 160, 161, 165.
Dooey (Co. Donegal), 114.
Doolough (Co. Mayo), 114, 160.
Dorentrup (Saxony), 130.
Dorset, Sands from, 45, 68, 73, 140,
143.
Down, Co., Sands from, 165.
Downie, W. Maoalpine, 95.
Downton (Hants), 72.
Dralle, R., 33, 35.
Drift-sand, 77 See also Glacial
Deposits.
Drying of Sands, 120, 124.
Dry-screening of Sands, 125.
Dublin, Glass-making at, 77, 85,
146.
Dublin Co., Sand from, 77, 165.
Dudley, Glass-making at, 145, 146.
Dune-Sands, 9, 17, 43, 44, 49, 76,
142, 144.
Dunfanaghy (Co. Donegal), 82.
Dumess (Sutherlandshire), 109, 110,
160.
Dutch Glass-Sands, 44, 49, 50, 126,
133, 147, 158, 166, 167.
Eaglesoliffe "Sand," 99, 127," 154 r
156, 162.
East Anglian Sands, 2.
East Grinstead (Sussex), 55.
East Hoathly, 162.
East Mills, Fordingbridge, 72.
East Wickham (Kent), 164.
Ebbw Vale Steel Co., 68.
Economic Considerations, 41, 147.
Edinburgh, Glass-making at, 89, 145,
146.
Edinburgh and Leith Glass- Works,
40, 133, 166, 167.
" Effective size " of Sands, 28.
Egg-timers or " egg-boilers," Sands-
for, 4, 146.
Eigg, KB., 77, 16B.
Electric Globes, 37, 42, 142, 146.
Electromagnetic treatment of Sands,
etc., 17, 80, 128, 149.
EUworthy, T. W., 54.
Elntriation, 20, 43.
Elutmtors, 21.
English Glass-Sands, 43, 141. .
English Ceramic Society, 33, 34.
Eocene Deposits, 3, 29, 31, 45, 69 r
71, 72, 73, 141, 142, 154, 156.
163.
Eriboll (Sutherlandshire), 109.
Erith Moulding-Sand, 29, 30, 73.
Ends Head (Co. Mayo), 114, 160.
Estuarine Series, 68, 140, 141, 143.
INDEX.
175
Etching of Glass, 47.
Etruria (Staffs), 160.
European Glass-Sands, 39, 130, 132,
133, 134, 153, 166, 167, 168.
Everett, J. D. and A., 33, 36.
Examination of Sands under the
microscope, 17.
Exportation of Sands, 73, 150.
Extraction of Potash from Silicates,
118.
Facing-Sands, 5.
Fsen0 (Denmark), 168.
FairHght (Sussex), 49, 52, 54, 141,
154, 156, 163.
Fauldhouse, N.B., 88.
Felsites, 106, 158.
Felspar, 9, 17, 35, 36,42, 43, 56,106,
107.
Felspar - bearing Books, 107, 108,
109, 110, 111, 112, 113, 114,
160.
Felspar used in Glass-making, 106,
Fenner, On behaviour of Silica, 80.
Fermanagh, Bocks from Co., Ill, 112,
113, 160.
Fertilizing, Sands for, 3, 117, 159.
Fettke, On American Glass-Sands,
34.
Fettling Furnaces with Sands, 5, 7.
Filtration-Sands, 5, 58, 95, 136.
" Fining " of glass, 38, 128.
Fintown (Co. Donegal), 114.
Fire-bricks, 38.
Fire-bricks, Sands for, 5.
Fire-clay, 38.
Firth of Forth, Glass-making near,
146.
" Flashing," 37.
Flint-glass, 7, 35, 48, 142, 146.
Flintshire, Sandstone from, 83, 104,
141, 164.
Flitwiok (Bedfordshire), 59, 156,
163.
Fluorspar, 36.
Folkestone, 159.
Folkestone Beds, 60, 61, 62, 63, 156,
103.
Fontainebleau Sand, 12, 32, 35, 39,
40, 42, 44, 46, 47, 48, 50, 53, 56,
60, 61, 67, 126, 132, 140, 147, 149,
151, 152, 166, 167.
Fordingbridge (Hants), 71, 141, 154,
157.
Foreign Glass- Sands, 34, 50, 130,
166, 167, 169, 170.
Forest Row (Sussex), 55.
Form of Sand-grains, 12.
Formation of Sands, 8.
Formulsa in Glass-making, 34.
Foundry-Sand, 5, 56, 58.
Fox, E. B. Colton, 68.
Fox Cover Pit, Borythorpe, 67.
Foxhall (Suffolk), 13, 32.
Fox Boy and Co. Ltd. (Meldon Book),
115.
Foyle, Biver, Sand from, 92, 144.
France, Sand from. See Fontaine-
bleau.
Frazer and others, Extraction of
Potash from Felspar, 118.
Friction- Sands, 3.
Friden (Derbyshire), 102.
Fuel, Consumption of, in Glass-
making, 145, 146.
Furnace-Sands, 5, 56, 66, 91, 144.
Furnaces for Glass-making, 37, 38.
" Gannister," 82, 95, 96, 102.
Garside, G., 58, 156, 163.
Garvary Wood (Co. Fermanagh), 112,
160.
Gateshead, Glass-making at, 146.
Gauge-glasses, 146.
Gay and Wilson, 58, 154, 163.
Gayton (Norfolk), 56.
Geological Survey of Denmark, 28,
34, 168.
Geological Survey of Great Britain,
35, 100, 101, 109, 110, 115, 118,
160.
Geological Survey of ludia, 139,
157.
Geological Survey of Ireland, 111,
113.
Geological Survey, TT.S.A,, 28, 34, 46,
47, 118, 134, 169.
German Glass-Sands, 35, 49, 130,
166, 167, 168.
Gerner B., 33.
Gilbert, E., 73.
Glacial Deposits, 3, 4, 29, 58, 64,
126, 140, 141, 142, 154, 157, 165.
Glasgow, Glass- making at, 145,
146.
Glasgow, Sandstones from, 86, 87,
143.
Glass-making, Distribution of, 145.
Glass-manufacture, Process of, 33.
Glass-Sand, Ideal, 31, 48.
Glass Technology, Department of
University, Sheffield, 75, 94.
Glass Technology, Society of, 33, 34,
134.
Glauoonitio Sands, 3, 57, 117, 118,
159.
Glaze, Sands used for, 4.
Glenbeigh (Kerry), 78.
IBDEX.
Olenboig, N.B., 38, 89, 144, 154 t
181.
Glenties (Co. Donegal), 114.
Gobb, Ballyoastle, 90.
Oodatone (Surrey), 49,50, 60, 61, 63,
67, 126, 141, 142, 156, 163.
Goodwyn and Sons, 60.
Orade-aizes, 13.
Grading of Sands, 2, 8, 43.
Granham'e Moor Quarries, Pontea-
bury, 95.
Granite, 5, 100, 106, 108, 115, 129,
159.
Granophyre, 106, 158.
Graphical expression of Mechanical
Analyses, 28.
Gravel, 9, 13.
Great Haldon Bolls (Devon), 31.
Oreensands, 3, 4, 57, 117, 118, 159.
See also tipper Greensand and
Lower Greensand.
Grejs Dal (Denmark), 168.
Grejs Mjzflle (Denmark), 168.
Griffin Mine, BallycastLe, 90.
Grinding of Glass, 47, 59.
Grinding of Glass-Sands, 47.
Gniaeley (Yorkshire), 79, 80, 82, 141,
154, 155.
Gniseley Gannister Co., 82.
Oweebarra (Co. Donegal), 114, 160.
Hailes, KB., 89, 144.
Halkyn Monntain (Flintshire), 104.
Hampshire, Sands from, 69, 71, 72,
73, 141, 142, 154, 156, 157, 163,
164.
Harborongh Books (Derbyshire),
102.
Harris, Gregory, 58, 163.
Hartiepool (Durham),, 165.
Hartwell siding, near Ayleabury, 52.
Hasketon (Suffolk), 29, 30.
Hastie, A. H., 55.
Hastings Sands, 52, 54, 141. See
also Ashdown and Tnnbridge Wells
Sands.
Hatherleigh (Devon), 101.
Hazen on Grade-size, 28.
Headon Hill Sands, 72, 140, 141, 156,
163, 164.
Heathfield (Devon), 101.
Heavy Liquids, 16.
Heavy Minerals in Sands, 9, 10, 16,
125.
Heokie, Alton and Kerr (Ballyoastle),
90.
Hematite coating Sand-grains, 11, 41,
119, 125.
Henrivanx, J., 33.
TTigha. (Kent), Glass-making- at,
74.
Higher Bebington (Cheshire), 85.
High Peak (Derbyshire), 102, 157,
164.
High Silica Sands Co., 65.
Hohenbocka (Prussia), 12, 35, 41,
130, 140.
Hohlbanm, R., 33.
Holland, Sands from, 34.
Hollingbonrne (Kent), 63, 141, 142,
156, 163.
Holyhead Monntain (Anglesey), 96,
100,101,129,155.
Horn-glasses, Sands for, 3.
Hovestadt on Jena Glass, 33, 36.
Howe, J. Allen, 100, 102.
Huttons Ambo (Yorkshire), 49, 65,
98, 99, 121, 143, 154, 156, 162.
Hvidbjerg (Denmark), 168.
Hydrochloric acid for cleaning
Sands, 126.
Ideal Glass-Sand, 31, 48.
Ideal Moulding-Sand, 31.
Ignition of Sands, 125.
LUing, V. 0., 125.
Illinois, U.S.A., 135, 136, 149, 169,
170.
Djnenite in Sands, 43, 65.
Importance of Sand in Glass-making,
35, 45.
Importation of Sands, 34, 147, 150,
151.
Impurities in Sands, 11, 151.
Inohard, Loch (Sutherlandshire),
109.
Inchnadamff (Sutherlandshire), 155.
Indian Sands, 139, 153, 154, 157,
165.
Inferior Oolite, 18, 45, 65, 68, 69,
140, 141, 142, 143, 156, 162.
Institute of Chemical Glass-formula,
34.
Institute of Chemistry, 34.
Institution of Mining and Metallurgy ;
Screens, 19.
Iowa, U.S.A., 149.
Ipswich, 29, 30.
Ireland, Pegmatites from, 111, 112,
113, 160.
Ireland, Sands from, 43, 77, 90, 91,
92, 93, 97, 134, 144, 155, 157, 158,
159, 161, 165.
Irish Glass Industry, Ancient, 145.
Irish Industrial Minerals Co. Ltd.,
96.
Iron-bearing Minerals, 10, 110,
113.
INDEX.
177
Iron, Impurity due to crushing, 83,
96.
Iron, Impurity in Glass, 87.
Iron, Impurity in reagents, 15.
Iron oxide in Sands, 10, 11, 14, 87,
119, 151, 154.
Iron-percentage in Glass-sands, 41,
42, 48.
Islay, N.B., 95, 144, 165.
Isle of Eigg, 77.
Isle of Jura, 76, 77, 95, 144, 157,
165.
Isle of Wight Sands, 34, 70, 72, 73,
140, 141, 142, 145, 156, 163,
164.
Jaokson, Sir Herbert, 151.
Jena Glass, 33, 35.
Jenkinson, S. N., 40.
Jet-holes, Size of, for Elutriators,
25.
Jubbulpore, India, 139, 157, 165.
Juniata White Sand Co., Baltimore,
Md., 138, 169, 170.
Jura, N.B., 76, 77, 95, 144, 157,
165.
Jurassic Deposits, 65, 67, 68, 140,
143, 154, 156.
Kaolin, 36, 100, 116.
Kaolin-bearing Sands, 5, 9, 32, 46,
85, 93, 94.
Keilhaok K., on Elutriation, 23.
KeUoway Beds, 32, 45, 50, 66, 67, 68,
141, 143-, 156,. 162.
Kent, Sands from, 29, 32, 45, 62, 63,
73, 74, 141, 142, 156, 163, 164.
Ken-fallen (Argyllshire), 95.
Kerniok (Cornwall), 108, 160.
Kerry Co., Sanda from, 78.
Keuper Marls, 4, 103.
Keuper Sandstone, 76, 85, 141, 142,
156, 162.
Kieselguhr, 5.
Kilbarriok, Sutton (Dublin), 77.
Kildownet (Aohill Island), 97.
Kilkee (Kerry), 78.
Killieorankie, N.B,, 144.
KUwinning, N.B., 87, 144, 155,
161.
Kinahan, G. H., 77, 113.
Kingsoavil, N.B., 89, 144.
King's Lynn (see Lynn).
Kings Moss (Lanos), 64.
Klondike, Mo., 169.
Knottingley Glass -Works, 132, 133,
166, 167.
Kynance Cove (Cornwall), 29, 30.
Laboratory-ware, 35, 87, 42, 57, 59,
61, 100, 142, 145.
Laggas Bay, Islay, 165.
Laig Bay, Eigg, 77, 165.
Lancashire Sands, 3, 64, 121, 140,
141, 142, 157, 165.
Twit-hill (Co. Fermanagh), 112.
Larson, On Behaviour of Silica, 80.
Laxf ord Looh (Sutherlandshire), 109,
110, 160.
Leavening (Yorkshire), 162.
Lee, Cecil, 71.
Leeds, Glass-making at, 146.
Leeds Public Library, 33.
Leighton Buzzard (Bedfordshire), 44,
47, 50, 58, 61, 67, 119, 121, 127,
140, 141, 154, 156, 163.
Lemgo (Westphalia), 35.
Lenses, 146.
Lermantoff, W., 33.
Levenseat, N.B., 88, 98, 144, 155,
161.
Lewisian Gneiss, 109.
Lighting Glass, 37, 42, 57, 119, 142,
146.
Lignites associated with Glass-Sands,
52, 132, 140.
Limerick, 145.
Limestone in Glass-making', 36.
Limonite coating on Sand-grains, 11,
41, 45, 119, 125.
, Limpafield (Surrey), 60.
LinlithgowBhire, Sand from, 89.
Lincolnshire, Sand from, 165.
Lippe Sand, 12, 27, 48, 49, 50, 130,
140, 149, 166, 167.
Literature on Glass-Sands, 33.
Little Haldon Hills (Devon), 31.
Llandudno, 104.
Lleyn Peninsula, Vein-quartz from,
97.
Location of British Glass-Sands,
140.
Loohoraigs Farm, Kilwinning, 87.
London, Glass-making in, 52, 54, 60,
73, 82, 145, 146.
London Basin, Sands of, 73.
London Clay, 4, 29.
Londonderry, 92, 112, 154.
Longoliffe (Derbyshire), 103, 144,
164.
Longdown (Hants), 69, 141, 154,
157.
Lower Estuarine Sands, 162. See
also Corby.
Lower Greensand, 3, 4, 49, 50, 51,
58, 58, 59, 60, 61, 62, 63, 119,
126, 141, 142, 144, 154, 156, 163.
Lower Kildress, Oookstown, 91.
Lower Oolites, 65, 68, 141.
178
INDEX.
Low Moor (Derbyshire), 102, 141.
Luxullian (Cornwall), 160.
Lyle, Capt. S. J., 90.
Lymington (Hants), 73, 164.
Lynn (Norfolk), 27, 30, 35, 44, 47,
49, 50, 56, 67, 141, 142, 145, 154,
156, 163.
Lyon, T. H., and Partner, 68.
MacriliaiiiBh Bay (Argyllshire), 165.
Maghera, Ardara (Oo. Donegal), 77,
154, 165.
Magnetic separation, 17, 97.
Magnetic treatment of Sands, 17, 80,
127, 128, 148.
Maiden Bradley (Wilts), 159.
Maintenon (Prance), 35.
Malton (Yorkshire), 45, 50, 65, 67.
Manchester, Glass-making at, 76,
145, 146, 167.
Manchester Pnblic Library, 33.
Manganese dioxide, Use of, for de-
colorising, 37, 42.
Marson, P., 33.
Martinroda (Saxony), 36.
Maryland, "U.S.A., Sand from, 138,
169, 170.
Massachusetts, Sand from, 136, 169,
170.
Maw, George, 102.
Mayo, Books from, 93, 96, 114,
160.
Mechanical Analyses, 18, 121, 161,
167,168,169,170.
' Mechanical Composition of Glass-
Sands, 43.
Medical apparatus, 146.
Medway, E., 63.
Meldon Eock, 115, 128, 129, 154,
159, 161.
Memoirs, Geological Survey of Great
Britain, 35, 36, 52, 61, 68, 64,
70.
Mersey, E., 47, 64.
" Metal " in Glass-making, 35.
Methods of investigating sands, 14.
Mica in Sands, 12, 43, 68, 101.
Micaceous Sands, 68, 71.
" Micas " of China-clay works, 100,
116, 159.
Miorocline, 3, 109.
Miorogranite, 106.
Microscopic examination of Sands,
17.
Middleton (Norfolk), 56.
Middle Oolites, 141, 142, 144.
Midford (Somersetshire). 45, 143.
Midland Valley of Scotland, 89.
Mile Tree (Leighton Buzzard), 58.
Miller, J. B., 33.
MiUisle (Co. Down), 144, 165.
Millstone Grit, 85, 88, 104, 144.
Minera (Denbighshire), 84, 141, 161.
Mineral Analyses, 15.
Mineral Composition of Sands, 10,
43.
Mineral Impurities in Glass-Sands,
43.
Mineral Milling Co., Mold, 83.
Miner's Lamps, Glass for, 35.
Minnesota, "U.S.A., 149.
Miocene Deposits, 81, 101, 130, 144,
157.
Mississippi Basin, Glass-sands of,
124, 149.
Missouri, U.S.A., 149.
" Mixed Stone " for Pottery work,
114.
Moine Schists, 109.
Mold (Flintshire), 83, 141, 154, 155,
161.
Monazite-bearing Sands, 2.
Monorieff, J. Ltd., for Elutriators,
21.
Montana, Sands from, 188, 169, 170.
Montrose, 32, 165.
Morgan, Prof. Gilbert, 77.
Mortar, Sands for, 4.
Moulding-Sands, 5, 29, 31, 73, 75.
Mow Cop (Cheshire), 84, 155, 161.
Muckish Mountain (Co. Donegal),
77, 79, 81, 126, 145, 154, 155,
161.
Mud-grade, 13.
Muller, B., 33.
Muscovite Mica, 116.
Nature of Sands, 8.
Neagh, Lough, 77, 165.
Nemours (France), 35.
Newbald (Yorkshire), 68.
New Forest (Hants), 70.
Newhaven (Derbyshire), 103, 144,
157, 164.
Newport (Mon.), Glass-making at,
146.
Newton Abbot (Devon), 101.
Nioopits Sand Co. Ltd., 62.
Nievelstein (Ehine Province), 35,.
41.
Nitre-cake for bleaching Sand, 126.
" No Man's Land," 71.
Non-graded Deposits, 9, 31.
Non-graded Materials, 79, 80.
Norfolk, Sands from, 27, 30, 35, 44,
49, 56, 58, 60, 67, 85, 141, 142,
145, 154, 156, 163.
Northamptonshire Ironstone, 68.
INDEX.
17&
Northampton Sands, 35, 143.
Northamptonshire, Sands from, 68,
141, 143.
North Wales, Sands from, 104.
Norton Tunnel, 75.
Norway, Felspar from, 107, 111.
Nottinghamshire, Sands from, 45,
74, 76, 99, 141, 142, 154, 162.
Obsidian, 42.
Okehampton (Devon), 115.
Oldbury, Glass-makhig at, 146.
Oldhaven (Blackheath) Beds, 32.
Old Irish Glass, 145.
Oligooene Strata, 39, 144.
Oolites, 141.
Optical Glass, 37, 47, 48, 82, 128,
145, 151, 152, 153.
Optical Society, Trans., 34.
Ordovioian Rocks, 95, 141, 144, 155.
Organic matter in Sands, 5, 11, 119.
Origin of Sanda, 8.
Oriskany Sandstone (U.S.A.), 137,
138, 149.
Orthoolane, 3.
Ottawa, Illinois, 120, 135, 13C, 169,
170.
Ottawa Silica Co., HliiioiH, 135.
OverHcaig (Suthorlandehire), 109,
160.
Oxfordshire, Sands from, 4.
Oxted (Surrey), 60, 141, 163.
Pacific, Mo., 138.
Page, E,, Woodenbridge (Co. Wick-
low), 97.
PaltBOZoio Books, 143.
' Panning " of Sands, 15.
Pant dn (near Mold), 84, 104.
Par (Cornwall), 115, 128, 154, 159.
Paris, Sand from near, 39.
" PaiTot," 90.
Parsley Hay (Derbyshire), 98, 102,
103, 141, 144, 157.
Parting-Sands, 4.
Patent Office Library, 33, 34.
Patent Specifications on Glass, 33.
Pirrit, W. P., 86.
Pittsburg Plate Glass Co., Montana,
169.
Peaty matter in Sands, 51, 64, 69, 71,
140.
Pebble-bed, Bunter, 103.
Peddle, C. J., 121, 124.
Pegmatites, 42. 107, 108, 109, 110,
111, 112, 113, 114, 129, 160.
Periodicals on Glass-making, 34.
Permian Marls, 74.
Permian Sands, 119, 143, 154.
Perth, Glass-making at, 145, 146.
'Pharmaceutical Glass, 100, 142.
Plate Glass, 47, 57, 146.
Plean, N.B., 88, 89, 129, 144, 161.
Pliocene Deposits, 29, 31, 101, 138.
Pontefraot, 154.
Pontesbury (Salop), 95, 155.
Pool and Co. Ltd., for Screens, 19.
Port-a-oloy (Co. Mayo), 79, 80, 93,
99, 100, 121, 145, 154, 155, 161.
Porth Wen, 96.
Portland Cement, Sands for, 4.
Portland Sands, 143.
Portrush (Co. Antrim), 144, 165.
Potash extraction from Silicate a,
118.
Potash Felspars, 86, 42, 107.
Potash - bearing Books, 106, 158,
160.
Potash-bearing Sands, 3, 116.
Pot-furnaces, 37, 45, 145.
Potteries, 4, 114, 160.
Powell, H. J., 83.
Pre-Cambrian Pegmatites, 109.
Pre-Oambrian Books, 79, 81, 93, 95,
96, 101, 109, 113, 144, 154, 155,
161.
Precautions in Chemical Analyses,
15.
Pre-Glaoial Deposits of doubtful age,
141.
Pressed-ware, 59, 61, 142, 146.
Process of Glass-making, 37.
Producer-gas in Glass-making, 37,
145.
Production of Sand, 150.
Profit on Glass-Sands, 148.
Prussia, Sands from, 12, 35.
Pulps from Gold-bearing Books, 24,
153.
" Purple Stone " for Pottery-work,
114, 115.
Pyrite in Glass-Sands, 135.
Pyrogallol, Use of in Elutriation, 22.
Quartz, 1, 3, 5, 9, 12, 14, 16, 27, 36,
41, 43, 47. See also Vein-quartz.
Quartzites, 36, 77, 79, 81, 93, 94, 95,
96, 143, 145, 155.
Quartz-Porphyry, 42.
Queenborough, Glass-making at, 74,
146.
Badley, E. G., Analyst, 109.
Bainford (Lanes), 64, 121, 141, 154,
157, 165.
Bapaport, Arkwright and, 81.
CHECKED 2000
IgQ
INDEX.
Raw Materials for Glass-making, 35.
Recent Sands, 77, 141, 164, 157,
169.
Recuperative Furnaces, 38.
Bed Crag Sands, 13.
Redhffl (Surrey), 61, 62.
Refractory Clays, 101.
"Refractory Minerals, 43.
Refractory Sands, 3, 5, 51, 52, 55, 56,
58, 60, 61, 62, 63, 65, 73, 74, 81,
82, 83, 84, 85, 86, 88, 90, 91, 95,
101, 102, 120, 128, 152, 154, 155,
156, 161-167.
"Regenerative Furnaces, 38.
Reid, Hugh, 89.
Reigate (Surrey), 49, 61, 63, 126,
141, 142, 145, 156, 163.
Renfrewshire, Sand from, 86.
Requirements of Glass-Sands, 39.
Resistance Glasses, 35, 36, 48.
Retgers on Dune-sands, 43.
Rhffltic Shales, 103.
Rhes y oae (Flintshire), 104, 141,
164.
Rhine Province, Sands from, 35, 41.
Rhodin, J.Q-.A., Patent for Bleaching-
aands, 126.
Rhodin, J. G-. A., Patents for Extrac-
tion of Potash, 118.
Ribden (Staffs), 102, 141, 144, 154,
164.
Ries, H., On Clays, 23.
Ries, H., On Sands, 28.
Rikofs Washing Machine, 57, 122.
Road-dressing, Sands for, 4.
Roche (Cornwall), Felspar from, 107,
160.
Roche, " Micas " from, 100, 159.
Rochester (Kent), 74, 141.
Rogate (Sussex), 61, 163.
Rome, Glauconite from, 117,
Rookery (Lanes), 64.
Rosenhain, Dr. W., 33, 49, 130.
Rosslare (Co. Wicklow), 77, 144,
165.
Rouen, 39.
Rounded Sand-grains, 27, 135, 136.
Rounding of Grains, 2, 12.
Rowsley (Derbyshire), 85.
"Ruby" Glass, 87.
Ruahmere (Waterford), 78.
Rutile, 10, 43, 94.
St. Agnes (Cornwall), Refractory
Sands from, 101.
St. Erth (Cornwall), 29.
St. George's Hill (Surrey), 73, 164.
St. Helens, Glass-making at, 64, 99;
146.
St. Ives (Cornwall), 165. ,
St. Keverne (Cornwall), 31.
St. Leonards (Sussex), 54.
St. Louis (TLSA.), 138, 169, 170.
St. Peter's SandstonS (TT.S.A.), 135,
138, 149.
Salisbury, 71.
Salmon, H. H., 69.
Sancton (Yorkshire), 68.
Sand-blast, 47.
Sand-dunes, 12.
Sandell Bros., 69.
Sandfields, Ardara (Co. Donegal), 77,
165.
Sand-grade, 13.
" Sand-paper," 7.
Sandringham Sands, 44, 56, 58.
Sands for Abrasive purposes, 3, 47,
59, 84, 97.
Sands for Absorbent purposes, 5.
Sands for Agricultural purposes, 2.
Sands for Brick-making, 4, 29.
Sands for Building purposes, 4, 56,
58, 60.
Sands for Crucible-making, 5.
Sands for Filtration, 5, 58, 95, 136.
Sands for Fire-bricks, 5.
Sands for making Carborundum, 8
Sands for making 1 Cement, 4.
Sands for making Concrete, 4, 58.
Sands for Mortar, 4.
Sands for Refractory purposes, 5.
Sands for Silica-bricks, 5, 36, 96.
Sands for Silicate of Soda (' "Water-
glass"), 3.
Sands for Soap-making, 3.
Sandstone, 36.
Sandstones, Crushing strength of,
129.
Sandymonnt Strand (Dublin), 77, 98,
144, 157, 165.
Saxony, Sands from, 12.
Scandinavian Felspars, 111, 114,
160.
Scardans Lower (Co. Fermanagh),
111, 160.
Sohoene Elutriator, 21, 26.
Scientific Glass, 145. See also La-
boratory-ware.
Soolban, Lough (Co. Fermanagh),
. 111.
Scotland, Glass-sands from, 43, 144.
Scotland, Pegmatites from, 109, 110,
160.
Scouring-sand, 3, 61.
Screening of Sands, 19, 122, 123,
124, 161.
Sonnthorpe (Linos), 165.
Secondary Minerals, 11.
" Seeds " in Glass, Cause of, 46.
INDEX.
181
Selenium in Glass, 42.
Shape of Grains, 41, 46.
Sheet-Glass, 48, 49, 61, 146.
Sheffield, Sand from works, 1H7.
Sheffield, Sand from near, 74, 75.
Sheffield University, Department of
Glasa Technology, 75, 94.
Shell Sands, 2.
Shenley Hill (Leighton Buzzard), 58.
Shenatono, W. A., 38.
Shin, Looh (Sutherlandshire), 109.
Shirdley Hill (Lanos), 64, 121, 142.
Shore-Sands, 2, 9, 29, 43, 44, 49, 76,
77, 141, 142, 144, 154, 157, 165.
Shropshire, Quartzite from, 95, 155.
Sieves, Use of, 19.
Silioa-brioks, Sands for, 5, 38, 96.
Silica, Estimation of, 15.
Silicate of Soda, Sands for, 3
Silica-ware, 130.
Silt-grade, 9, 13, 12-4.
Silurian Rooks, 144.
Silver-sand, 3, 60.
Silver Strand (Co. Wioklow), 77,
144, 165.
Sims, H., 61.
Singer, F., On Use of Alumina, 98.
Single-vessel Elutriator, 25.
Size of Grains, 12.
Skelmersdale (Lanes), 64.
Sliohter, G. S., On Grading, 18, 28.
Slieve More (Aohill Island), 96.
Slime from washing Glass - Sands,
120.
Smart, G. W., 58.
Smith, Dr. G. Otis, 134.
Soaking Pits, Sands for, 5, 7.
Soap-making Sands, 3,
Society of Glass Technology, 33, 34,
134.
Soda-ash, 35.
Soda-glass, 35.
Sodium Carbonate for cleaning Sand,
127.
Sodium Carbonate, Use of in Elutri-
ation, 22.
Sodium Hydrosulphide for Bleaching
Sands, 126.
Sonstodt's Solution, 16.
Sorting of Sands, 12.
South Africa, Sands from, 153.
Southampton, G9.
South Cave (Yorkshire), 68, 98, 141,
143, 156, 162.
Spital (Cheshire), 45, 85, 99, 129,
141, 142, 143, 154, 156, 162.
Spreohsaol, 34.
Spreohsaal Kalendar, 34, 85.
Stadler, H., On Elutriation, 18, 21,
23.
Staffordshire, Freight to, from Mel^
don, 116.
Staffordshire, Sands from, 5, 102,
141, 144, 164.
Stained-glass, 146.
Statistics dealing with Sands, 150.
Steenberg,N., On Danish Sands, 168.
Staling (Denmark), 168.
Stiperatones (Salop), 95, 99, 129,
141, 155.
Stirling, N.B., 89.
Stoborough (Dorset), 73, 164.
Stone, near Aylesbury, 51.
Stone, Balph W., 134.
Stonefield (Co. Mayo), 94.
Stone Lone (Leighton Buzzard), 58.
" Stones " in Glass, Cause of, 46.
Stourbridge Fire-bricks, 38.
Stourbridge, Glass-making at, 47 r
145, 146.
Strahan, Dr. A., 102.
Sudbury (Suffolk), 159.
Suffolk, Sands from, 13, 29, 159.
Sunderland, Glass-making at, 146.
Superfine Sand, 13, 45.
Surrey, Sands from, 4, 49, 60, 61,
141.
Sussex, Sands from, 49, 52, 54, 61,
141, 143.
Sutherlandsliiro, Rocks from, 109,
155, 160.
Button (Co. Dublin), 77, 144, 165.
Svendborg (Denmark), 168.
" Sweating " of Mortar due to Sand,
4.
Sweden, Felspars from, 114.
Sweden, Glass- Sands of, 149.
Table-glass, 47, 48, 142, 145.
Tables, 121, 125, 154-170.
Taohylyte, 42.
Tadmarton (Oxfordshire), 69, 162.
Talargooh (Flintshire), 98, 164.
Tammann, G., 33.
Tank-furnaces, 38, 45, 145.
Tank-washing, 64, 89.
Tavern Rook Sand Co., St. Louis,
138, 169, 170. .
Technical Glass, 145.
Temperature Effect on Elutriation,
21.
Tertiary Deposits, 9, 72, 73, 134,
153, 156, 163, 168.
Terrill, A. J., 71.
ThanetBeds, 35, 45, 50, 73, 74, 117,.
141, 142, 156, 159, 164.
Thermometer-glass, 36, 42.
Thorianite in Sands, 2.
Thornton, J. & T., 88.
182
INDEX.
Thorpe, T., 33.
Thoulet's Solution, 16.
Thuringian Forest-sand, 36, 42.
Time-glasses, 4, 146.
Tinahely (Go. Wicklow), 97, 145.
Tiree, N.B., 165.
Titanium-bearing Minerals, -13.
Titanium in Sands, 15, 94.
Topley, W., On Wealden Sands, 52,
61.
Torrington (Devon), 101, 157.
Tramore (Waterford), 78, 106, 158.
Transmission Capacity of Sand, 28..
Transport of Sands, 146, 149.
Treatment of Sands and Eocks, 76,
80, 119, 134, 148.
Trelavour (Cornwall), 108, 160.
Tresayes (Cornwall), 107, 160.
Trevanaunce Cove (Cornwall), 101.
Trevisoo (Cornwall), 108, 160. .
Triassio Books, 45, 74, 84, 98, 103,
' 104, 119, 120, 127, 141, 142, 143,
154, 156, 162.
Tridymite, 5.
Tscheuschner, E., On Glass-Sands,
.35.
Tunbridge Wells Sands, 35, 52, 55,
141, 142, 156, 162, 163.
Turner and Sons, James, 74.
Turner, Dr. W. E. S., 98.
Tutbury, Glass-making at, 145, 146.
Twelve Pins (Co. Galway), 155.
Tyneside, Glass-making at, 146.
Tyrone Co., Sand from, 91. fr'ee also
Cookstown.
Tyrsbaek (Denmark), 168.
Uniformity Coefficient in Sands, 28.
United States Geological Survey, 28,
34, 46, 47, 118, 120, 184, 169.
Unshin, Lough (Co. Donegal), 112.
Upholland (Lanes), 64.
Upper Estnarine Series, 65.
Upper Glacial Deposits, 29.
Upper Greensand, 117, 118, 142,
159.
Uses of Sands, 1.
Utica (Illinois), 169.
Variation in Glass-Sands, 47.
Vegetable Matter associated with
Sands, 5, 11, 75, 119.
Vein-Quartz, 36, 96, 97, 128.
Vejle Dal (Denmark), 168.
Vejle Fjord (Denmark), 168.
Velocities of Water and Air-currents
for separating Sands, 20, 124.
Venetifin Glass, 35.
Victoria (Australia), Sand from, 139,
153, 157, 165.
Waen (Flintshire), 83.
Wagon, S., 62.
Walker, H. A., 85.
Walsall, Glass-making at, 145.
Wansford (Northants), 68, 143.
Wareham (Dorset), 73.
Warrington, 64, 145.
Washing, Apparatus for, 57, 89, 122.
Washing Bay, Coalisland, L. Neagh,
77, 165.
Washing- of Sands, 57, 58, 64, 89,
119, 148.
Washing-soda, Use of in Emtriation,
22.
Waterford Glass, 82, 145.
Waterfoid, Eocks from, 78, 106,
158.
" Water-glass," Sands for, 3.
Water-supply, Sands used for, 5.
Wealden Deposits, 85, 52, 54, 55,
140, 141, 142, 154, 156, 162.
Wedgwood's Pottery, 160.
Wedron Silica Co., Ottawa, Illinois,
136, 169, 170.
Weinsohenk on Petrographio me-
thods, 17.
Westerham (Kent), 61.
Western Europe, Glass-sands of, 3.9,
130-133, 144, 153, 166, 167.
Westphalia, Sands from, 35.
" Westport Silica," 80, 96, 128, 145,
154. 155, 161.
West Virginia, U.S.A., 137, 149, 169,
170.
Wetzel, C., 33.
Werford, Sands from, 77, 165.
Weybridge (Surrey), 73.
White Castle (Londonderry), 92.
Whiteoliff Bay (Isle of Wight), 72,
73, 140, 141, 164.
White Mine (Ballycastle), 90.
White Book, Tinahely, 97.
Wioklow, Felsite from, 106, 158.
Wioklow Co., Sands from, 77, 97,
165.
Wild & Sons, William, 96.
Wilson, Sir Spenoer Maryon, 73.
Wiltshire, Sands from, 71, 142.
Winohelsea (Sussex), 53.
Windle, Sir Bertram, 77.
Window-glass, 35, 36, 37, 49, 57, 64,
140, 142, 146.
Wisconsin, U.S.A., 149.
Witchell, Prof. E. T. D., 129.
Wood, W. Frank, 40.
Workability of Sands, 148.
INDEX.
183
Worksop (Notts), 45, 74, 76, 99, 141,
14,2, 154, 162.
Wotton (Ootteswolds), 32, 143.
Wright, On Behaviour of Silica, 80.
Wright, W. B., 111.
Xonotime in Sands, 2.
Yorkshire, Glass-making in, 52, 68,
76, 82, 99, 146.
Yorkshire, Glass-Sands from, 32, 45,
49, 65, 67, 68, 82, 98, 99, 121, 140,
141, 142, 143, 156, 162.
Youghal, 78.
Yeovil (Somerset), 45, 143.
Ynyalas (Cardiganshire), 97, 164.
York Glass-Works, 133, 167.
Zsohimmer, B., 33.
Zircon, 2, 10, 43.
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