[Illustration:
_PLATE I_
_Frontispiece_
GEM-STONES]
GEM-STONES
AND THEIR DISTINCTIVE CHARACTERS
BY
G. F. HERBERT SMITH
M.A., D.Sc.
OF THE BRITISH MUSEUM (NATURAL HISTORY)
WITH MANY DIAGRAMS AND THIRTY-TWO PLATES
OF WHICH THREE ARE IN COLOUR
THIRD EDITION
METHUEN & CO. LTD.
36 ESSEX STREET W.C.
LONDON
_First Published_ _March 21st 1910_
_Second Edition_ _June_ _1913_
_Third Edition_ _1919_
PREFACE
In this edition the opportunity has been taken to correct a few
misprints and mistakes that have been discovered in the first, and to
alter slightly one or two paragraphs, but otherwise no change has been
made. G. F. H. S. WANDSWORTH COMMON, S.W.
PREFACE TO THE FIRST EDITION
It has been my endeavour to provide in this book a concise, yet
sufficiently complete, account of the physical characters of the
mineral species which find service in jewellery, and of the methods
available for determining their principal physical constants to enable
a reader, even if previously unacquainted with the subject, to have
at hand all the information requisite for the sure identification of
any cut stone which may be met with. For several reasons I have dealt
somewhat more fully with the branches of science closely connected with
the properties of crystallized matter than has been customary hitherto
in even the most comprehensive books on precious stones. Recent years
have witnessed many changes in the jewellery world. Gem-stones are no
longer entirely drawn from a few well-marked mineral species, which
are, on the whole, easily distinguishable from one another, and it
becomes increasingly difficult for even the most experienced eye to
recognize a cut stone with unerring certainty. So long as the only
confusion lay between precious stones and paste imitations an ordinary
file was the solitary piece of apparatus required by the jeweller, but
now recourse must be had to more discriminative tests, such as the
refractive index or the specific gravity, the determination of which
calls for a little knowledge and skill. Concurrently, a keener interest
is being taken in the scientific aspect of gem-stones by the public at
large, who are attracted to them mainly by æsthetic considerations.
While the treatment has been kept as simple as possible, technical
expressions, where necessary, have not been avoided, but their meanings
have been explained, and it is hoped that their use will not prove
stumbling-blocks to the novice. Unfamiliar words of this kind often
give a forbidding air to a new subject, but they are used merely to
avoid circumlocution, and not, like the incantations of a wizard, to
veil the difficulties in still deeper gloom. For actual practical work
the pages on the refractometer and its use and the method of heavy
liquids for the determination of specific gravities, and the tables of
physical constants at the end of the book, with occasional reference,
in case of doubt, to the descriptions of the several species alone
are required; other methods—such as the prismatic mode of measuring
refractive indices, or the hydrostatic way of finding specific
gravities—which find a place in the ordinary curriculum of a physics
course are described in their special application to gem-stones, but
they are not so suitable for workshop practice. Since the scope of the
book is confined mainly to the stones as they appear on the market,
little has been said about their geological occurrence; the case of
diamond, however, is of exceptional interest and has been more fully
treated. The weights stated for the historical diamonds are those
usually published, and are probably in many instances far from correct,
but they serve to give an idea of the sizes of the stones; the English
carat is the unit used, and the numbers must be increased by about 2½
per cent. if the weights be expressed in metric carats. The prices
quoted for the various species must only be regarded as approximate,
since they may change from year to year, or even day to day, according
to the state of trade and the whim of fashion.
The diagram on Plate II and most of the crystal drawings were made
by me. The remaining drawings are the work of Mr. H. H. Penton. He
likewise prepared the coloured drawings of cut stones which appear
on the three coloured plates, his models, with two exceptions, being
selected from the cut specimens in the Mineral Collection of the
British Museum by permission of the Trustees. Unfortunately, the
difficulties that still beset the reproduction of pictures in colour
have prevented full justice being done to the faithfulness of his
brush. I highly appreciate the interest he took in the work, and the
care and skill with which it was executed. My thanks are due to the
De Beers Consolidated Mines Co. Ltd., and to Sir Henry A. Miers,
F.R.S., Principal of the University of London, for the illustrations
of the Kimberley and Wesselton diamond mines, and of the methods and
apparatus employed in breaking up and concentrating the blue ground;
to Messrs. I. J. Asscher & Co. for the use of the photograph of the
Cullinan diamond; to Mr. J. H. Steward for the loan of the block of the
refractometer; and to Mr. H. W. Atkinson for the illustration of the
diamond-sorting machine. My colleague, Mr. W. Campbell Smith, B.A., has
most kindly read the proof-sheets, and has been of great assistance in
many ways. I hope that, thanks to his invaluable help, the errors in
the book which may have escaped notice will prove few in number and
unimportant in character. To Mr. Edward Hopkins I owe an especial debt
of gratitude for his cheerful readiness to assist me in any way in
his power. He read both the manuscript and the proof-sheets, and the
information with regard to the commercial and practical side of the
subject was very largely supplied by him. He also placed at my service
a large number of photographs, some of which—for instance, those
illustrating the cutting of stones—he had specially taken for me, and
he procured for me the jewellery designs shown on Plates IV and V.
If this book be found by those engaged in the jewellery trade helpful
in their everyday work, and if it wakens in readers generally an
appreciation of the variety of beautiful minerals suitable for gems,
and an interest in the wondrous qualities of crystallized substances, I
shall be more than satisfied.
G. F. H. S.
WANDSWORTH COMMON, S.W.
CONTENTS
CHAP. PAGE
I. INTRODUCTION 1
PART I—SECTION A
THE CHARACTERS OF GEM-STONES
II. CRYSTALLINE FORM 6
III. REFLECTION, REFRACTION, AND DISPERSION 14
IV. MEASUREMENT OF REFRACTIVE INDICES 21
V. LUSTRE AND SHEEN 37
VI. DOUBLE REFRACTION 40
VII. ABSORPTION EFFECTS: COLOUR, DICHROISM,ETC. 53
VIII. SPECIFIC GRAVITY 63
IX. HARDNESS AND CLEAVABILITY 78
X. ELECTRICAL CHARACTERS 82
PART I—SECTION B
THE TECHNOLOGY OF GEM-STONES
XI. UNIT OF WEIGHT 84
XII. FASHIONING OF GEM-STONES 88
XIII. NOMENCLATURE OF PRECIOUS STONES 109
XIV. MANUFACTURED STONES 113
XV. IMITATION STONES 124
PART II—SECTION A
PRECIOUS STONES
XVI. DIAMOND 128
XVII. OCCURRENCE OF DIAMOND 137
XVIII. HISTORICAL DIAMONDS 157
XIX. CORUNDUM (_Sapphire_, _Ruby_) 172
XX. BERYL (_Emerald_, _Aquamarine_, _Morganite_) 184
PART II—SECTION B
SEMI-PRECIOUS STONES
XXI. TOPAZ 197
XXII. SPINEL (_Balas-Ruby_, _Rubicelle_) 203
XXIII. GARNET 207
(_a_) HESSONITE (_Grossular_, _Cinnamon-Stone_,
_Hyacinth_, _Jacinth_) 211
(_b_) PYROPE (‘_Cape-Ruby_’) 212
(_c_) RHODOLITE 214
(_d_) ALMANDINE (_Carbuncle_) 214
(_e_) SPESSARTITE 216
(_f_) ANDRADITE (_Demantoid_, _Topazolite_, ‘_Olivine_’) 216
(_g_) UVAROVITE 218
XXIV. TOURMALINE (_Rubellite_) 219
XXV. PERIDOT 225
XXVI. ZIRCON (_Jargoon_, _Hyacinth_, _Jacinth_) 228
XXVII. CHRYSOBERYL (_Chrysolite_, _Cat’s-Eye_, _Cymophane_,
_Alexandrite_) 233
XXVIII. QUARTZ (_Rock-Crystal_, _Amethyst_, _Citrine_,
_Cairngorm_, _Cat’s-Eye_, _Tiger’s-Eye_) 238
XXIX. CHALCEDONY, AGATE, ETC. 246
XXX. OPAL (_White Opal_, _Black Opal_, _Fire-Opal_) 249
XXXI. FELSPAR (_Moonstone_, _Sunstone_, _Labradorite_,
_Amazon-Stone_) 254
XXXII. TURQUOISE, ODONTOLITE, VARISCITE 257
XXXIII. JADE (NEPHRITE OR GREENSTONE, _Jadeite_) 260
XXXIV. SPODUMENE (_Kunzite_, _Hiddenite_), IOLITE, BENITOITE 265
XXXV. EUCLASE, PHENAKITE, BERYLLONITE 269
XXXVI. ENSTATITE (‘_Green Garnet_’), DIOPSIDE, KYANITE,
ANDALUSITE, IDOCRASE, EPIDOTE, SPHENE, AXINITE,
PREHNITE, APATITE, DIOPTASE 271
XXXVII. CASSITERITE, ANATASE, PYRITES, HEMATITE 281
XXXVIII. OBSIDIAN, MOLDAVITE 283
PART II—SECTION C
ORNAMENTAL STONES
XXXIX. FLUOR, LAPIS LAZULI, SODALITE, VIOLANE, RHODONITE,
AZURITE, MALACHITE, THULITE, MARBLE, APOPHYLLITE,
CHRYSOCOLLA, STEATITE OR SOAPSTONE, MEERSCHAUM,
SERPENTINE 285
PART II—SECTION D
ORGANIC PRODUCTS
XL. PEARL, CORAL, AMBER 291
TABLES
I. CHEMICAL COMPOSITION OF GEM-STONES 300
II. COLOUR OF GEM-STONES 301
III. REFRACTIVE INDICES OF GEM-STONES 302
IV. COLOUR-DISPERSION OF GEM-STONES 303
V. CHARACTER OF THE REFRACTION OF GEM-STONES 303
VI. DICHROISM OF GEM-STONES 304
VII. SPECIFIC GRAVITIES OF GEM-STONES 305
VIII. DEGREES OF HARDNESS OF GEM-STONES 305
IX. DATA 306
INDEX 307
LIST OF PLATES
PAGE
I. GEM-STONES (in colour) _Frontispiece_
II. REFRACTIVE INDEX DIAGRAM 36
III. INTERFERENCE FIGURES 48
IV. JEWELLERY DESIGNS 62
V. JEWELLERY DESIGNS 88
VI. APPLIANCES USED FOR POLISHING DIAMONDS 102
VII. POLISHING DIAMONDS 103
VIII. SLITTING AND POLISHING COLOURED STONES 104
IX. FACETING MACHINE 105
X. LAPIDARY’S WORKSHOP AND OFFICE IN ENGLAND 106
XI. LAPIDARY’S WORKSHOP IN RUSSIA 107
XII. FRENCH FAMILY CUTTING STONES 108
XIII. INDIAN LAPIDARY 109
XIV. BLOWPIPE USED FOR THE MANUFACTURE OF RUBIES
AND SAPPHIRES 118
XV. KIMBERLEY MINE, 1871 140
XVI. KIMBERLEY MINE, 1872 141
XVII. KIMBERLEY MINE, 1874 142
XVIII. KIMBERLEY MINE, 1881 143
XIX. KIMBERLEY MINE AT THE PRESENT DAY 144
XX. WESSELTON (open) MINE 145
XXI. LOADING THE BLUE GROUND ON THE FLOORS, AND PLOUGHING IT
OVER 146
XXII. WASHING-MACHINES FOR CONCENTRATING THE BLUE GROUND 147
XXIII. DIAMOND-SORTING MACHINES 148
XXIV. KAFIRS PICKING OUT DIAMONDS 149
XXV. CULLINAN DIAMOND (natural size) 168
XXVI. LARGE AQUAMARINE CRYSTAL (one-sixth natural size),
FOUND AT MARAMBAYA, MINAS GERAES, BRAZIL 196
XXVII. GEM-STONES (in colour) 226
XXVIII. OPAL MINES, WHITE CLIFFS, NEW SOUTH WALES 252
XXIX. GEM-STONES (in colour) 256
XXX. NATIVES DRILLING PEARLS 294
XXXI. METAL FIGURES OF BUDDHA INSERTED IN A PEARL-OYSTER 296
XXXII. SECTIONS OF CULTURE PEARL 297
GEM-STONES
CHAPTER I
INTRODUCTION
Beauty, durability, and rarity: such are the three cardinal virtues
of a perfect gem-stone. Stones lacking any of them cannot aspire to
a high place in the ranks of precious stones, although it does not
necessarily follow that they are of no use for ornamental purposes. The
case of pearl, which, though not properly included among gem-stones,
being directly produced by living agency, yet holds an honoured place
in jewellery, constitutes to some extent an exception, since its
incontestable beauty atones for its comparative want of durability.
That a gem-stone should be a delight to the eye is a truism that need
not be laboured; for such is its whole _raison d’être_. The members
of the Mineral Kingdom that find service in jewellery may be divided
into three groups, according as they are transparent, translucent,
or opaque. Of these the first, which is by far the largest and the
most important, may itself be further sub-divided into two sections:
stones which are devoid of colour, and stones which are tinted. Among
the former, diamond reigns supreme, since it alone possesses that
marvellous ‘fire,’ oscillating with every movement from heavenly blue
to glowing red, which is so highly esteemed and so much besought.
Other stones, such as ‘fired’ zircon, white sapphire, white topaz, and
rock-crystal, may dazzle with brilliancy of light reflected from the
surface or emitted from the interior, but none of them, like diamond,
glow with mysterious gleams. No hint of colour, save perhaps a trace
of the blue of steel, can be tolerated in stones of this category;
above all is a touch of the jaundice hue of yellow abhorred. It taxes
all the skill of the lapidary to assure that the disposition of the
facets be such as to reveal the full splendour of the stone. A coloured
stone, on the other hand, depends for its attractiveness more upon its
intrinsic hue than upon the manner of its cutting. The tint must not be
too light or too dark in shade: a stone that has barely any colour has
little interest, and one which is too dark appears almost opaque and
black. The lapidary can to some extent remedy these defects by cutting
the former deep and the latter shallow. In certain curious stones—for
instance tourmaline—the transparency, and in others—such as ruby,
sapphire, and one of the recent additions to the gem world, kunzite—the
colour, varies considerably in different directions. The colours that
are most admired—the fiery red of ruby, the royal blue of sapphire,
the verdant green of emerald, and the golden yellow of topaz—are pure
tints, and the absorption spectra corresponding to them are on the
whole continuous and often restricted. They therefore retain the purity
of their colour even in artificial light, though certain sapphires
transmit a relatively larger amount of red, and consequently turn
purple at night. Of the small group of translucent stones which pass
light, but are not clear enough to be seen through, the most important
is opal. It and certain others of the group owe their merit to the
same optical effect as that characterizing soap-bubbles, tarnished
steel, and so forth, and not to any intrinsic coloration. Another
set of stones—moonstone and the star-stones—reflect light from the
interior more or less regularly, but not in such a way as to produce
a play of colour. The last group, which comprises opaque stones, has
a single representative among ordinary gem-stones, namely, turquoise.
In this case light is scattered and reflected from layers immediately
contiguous to the surface, and the colour is due to the resulting
absorption. The apparent darkness of a deep-coloured stone follows from
a different cause: the light passing into the stone is wholly absorbed
within it, and, since none is emitted, the stone appears black. The
claims of turquoise are maintained by the blue variety; there is little
demand for stones of a greenish tinge.
It is evidently desirable that any stones used in jewellery should be
able to resist the mechanical and chemical actions of everyday life. No
one is anxious to replace jewels every few years, and the most valuable
stones are expected to endure for all time. The mechanical abrasion
is caused by the minute grains of sand that are contained in ordinary
dust, and gem-stones should be at least as hard as they—a condition
fulfilled by all the principal species with the exception of opal,
turquoise, peridot, and demantoid. Since the beauty of the first named
does not depend on the brilliancy of its polish, scratches on the
surface are not of much importance; further, all four are only slightly
softer than sand. It may be noted that the softness of paste stones,
apart from any objections that may be felt to the use of imitations,
renders them unsuitable for jewellery purposes. The only stones that
are likely to be chemically affected in the course of wear are those
which are in the slightest degree porous. It is hazardous to immerse
turquoises in liquids, even in water, lest the bluish green colour be
oxidized to the despised yellowish hue. The risk of damage to opals,
moonstones, and star-stones by the penetration of dirt or grease into
the interior of the stones is less, but is not wholly negligible.
Similar remarks apply with even greater force to pearls. Their charm,
which is due to a peculiar surface-play of light, might be destroyed by
contamination with grease, ink, or similar matter; they are, moreover,
soft. For both reasons their use in rings is much to be deprecated.
Nothing can be more unsightly than the dingy appearance of a pearl ring
after a few years’ wear.
It cannot be gainsaid that mankind prefers the rare to the beautiful,
and what is within reach of all is lightly esteemed. It is for this
reason that garnet and moonstone lie under a cloud. Purchasers can
readily be found for a ‘Cape-ruby’ or an ‘olivine,’ but not for a
garnet; garnets are so common, is the usual remark. Nevertheless,
the stones mentioned are really garnets. If science succeeded in
manufacturing diamonds at the cost of shillings instead of the pounds
that are now asked for Nature’s products—not that such a prospect is at
all probable or even feasible—we might expect them to vanish entirely
from fashionable jewellery.
A careful study of the showcases of the most extensive jewellery
establishment brings to light the fact that, despite the apparent
profusion, the number of different species represented is restricted.
Diamond, ruby, emerald, sapphire, pearl, opal, turquoise, topaz,
amethyst are all that are ordinarily asked for. Yet, as later pages
will show, there are many others worthy of consideration; two among
them—peridot and tourmaline—are, indeed, slowly becoming known. For
the first five of the stones mentioned above, the demand is relatively
steady, and varies absolutely only with the purchasing power of the
world; but a lesser known stone may suddenly spring into prominence
owing to the caprice of fashion or the preference of some great lady
or leader of fashion. Not many years ago, for instance, violet was the
favourite colour for ladies’ dresses, and consequently amethysts were
much worn to match, but with the change of fashion they speedily sank
to their former obscurity. Another stone may perhaps figure at some
royal wedding; for a brief while it becomes the vogue, and afterwards
is seldom seen.
Except that diamond, ruby, emerald, and sapphire, and, we should add,
pearl, may indisputably be considered to occupy the first rank, it is
impossible to form the gem-stones in any strict order. Every generation
sees some change. The value of a stone is after all merely what it will
fetch in the open market, and its artistic merits may be a matter of
opinion. The familiar aphorism, _de gustibus non est disputandum_, is a
warning not to enlarge upon this point.
PART I—SECTION A
THE CHARACTERS OF GEM-STONES