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Title: The chemistry, properties and tests of precious stones

Author: John Mastin

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*** START OF THE PROJECT GUTENBERG EBOOK THE
CHEMISTRY, PROPERTIES AND TESTS OF PRECIOUS STONES ***

THE CHEMISTRY,

PROPERTIES AND TESTS OF
PRECIOUS STONES

BY THE SAME AUTHOR
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ETC. ETC.

THE CHEMISTRY, PROPERTIES

AND TESTS
OF

PRECIOUS STONES.
BY

JOHN MASTIN, M.A. D.Sc. Ph.D. Litt.D.
F.S A.SCOT. F.L.S. F.C.S. F.R.A.S. F.R.M.S. R.B.A.

Author of "Parasites of Insects," "The True Analysis of Milk," "Plate-
Culture and Staining of Amœbæ," etc., etc.
London
E. & F. N. SPON, Limited, 57 HAYMARKET
NEW YORK
SPON & CHAMBERLAIN, 123 LIBERTY STREET
1911

CONTENTS
CHAPTER PAGE
I Introductory 1
II The Origin of Precious Stones 7
III Physical Properties—(A) Crystalline Structure 13
IV " " (B) Cleavage 19
V " " (C) Light 26
VI " " (D) Colour 32
VII " " (E) Hardness 39
VIII " " (F) Specific Gravity 45
IX " " (G) Heat 52
X " " (H) Magnetic and Electric Influences 57
XI The Cutting of Precious Stones 62
XII Imitations, and Some of the Tests of Precious Stones 70
XIII Various Precious Stones 80
XIV " " " (continued) 88
XV " " " " 98

PREFACE
Some little time ago certain London diamond merchants and wholesale
dealers in precious stones made the suggestion to me to write a work on this
section of mineralogy, as there did not appear to be any giving exactly the
information most needed.
Finding there was a call for such a book I have written the present volume
in order to meet this want, and I trust that this handbook will prove useful,
not only to the expert and to those requiring certain technical information,
but also to the general public, whose interest in this entrancing subject may
be simply that of pleasure in the purchase, possession, or collection of
precious stones, or even in the mere examination of them through the plate-
glass of a jeweller's window.
JOHN MASTIN.
Totley Brook,
near Sheffield.

June 1911.

THE CHEMISTRY, PROPERTIES AND TESTS
OF PRECIOUS STONES

CHAPTER I.
INTRODUCTORY.

What constitutes a precious stone is the question which, at the onset, rises in
the mind, and this question, simple as it seems, is one by no means easy to
answer, since what may be considered precious at one time, may cease to be
so at another.
There are, however, certain minerals which possess distinctive features in
their qualities of hardness, colour, transparency, refractability or double
refractability to light-beams, which qualities place them in an entirely
different class to the minerals of a metallic nature. These particular and non-
metallic minerals, therefore, because of their comparative rarity, rise pre-
eminently above other minerals, and become actually "precious."
This is, at the same time, but a comparative term, for it will readily be
understood that in the case of a sudden flooding of the market with one
class of stone, even if it should be one hitherto rare and precious, there
would be an equally sudden drop in the intrinsic value of the jewel to such
an extent as perhaps to wipe it out of the category of precious stones. For
instance, rubies were discovered long before diamonds; then when
diamonds were found these were considered much more valuable till their
abundance made them common, and they became of little account. Rubies
again asserted their position as chief of all precious stones in value, and in
many biblical references rubies are quoted as being the symbol of the very
acme of wealth, such as in Proverbs, chapter iii., verses 13 and 15, where
there are the passages, "happy is the man that findeth wisdom ... she is more
precious than rubies"—and this, notwithstanding the enormous quantity of
them at that time obtained from the ruby mines of Ophir and Nubia, which
were then the chief sources of wealth.
It will also be remembered that Josephus relates how, at the fall of
Jerusalem, the spoil of gold was so great that Syria was inundated with it,
and the value of gold there quickly dropped to one-half; other historians,

also, speaking of this time, record such a glut of gold, silver, and jewels in
Syria, as made them of little value, which state continued for some
considerable period, till the untold wealth became ruthlessly and wastefully
scattered, when the normal values slowly reasserted themselves.
Amongst so many varieties of these precious minerals, it cannot be
otherwise than that there should be important differences in their various
characteristics, though for a stone to have the slightest claim to be classed
as "precious" it must conform to several at least of the following
requirements:—It must withstand the action of light without deterioration of
its beauty, lustre, or substance, and it must be of sufficient hardness to retain
its form, purity and lustre under the actions of warmth, reasonable wear, and
the dust which falls upon it during use; it must not be subject to chemical
change, decomposition, disintegration, or other alteration of its substance
under exposure to atmospheric air; otherwise it is useless for all practical
purposes of adornment or ornamentation.
There are certain other characteristics of these curious minerals which may
be classified briefly, thus:—Some stones owe their beauty to a wonderful
play of colour or fire, due to the action of light, quite apart from the colour
of the stone itself, and of this series the opal may be taken as a type. In
others, this splendid play of colour is altogether absent, the colour being
associated with the stone itself, in its substance, the charm lying entirely in
the superb transparency, the ruby being taken as an example of this class of
stone. Others, again, have not only colour, but transparency and lustre, as in
the coloured diamonds, whilst the commoner well-known diamonds are
extremely rich in transparency and lustre, the play of light alone showing a
considerable amount of brilliancy and beauty of colour, though the stone
itself is clear. Still others are opaque, or semi-opaque, or practically free
from play of light and from lustre, owing their value and beauty entirely to
their richness of colour.
In all cases the value of the stone cannot be appreciated fully till the gem is
separated from its matrix and polished, and in some cases, such as in that of
the diamond, cut in variously shaped facets, on and amongst which the light
rays have power to play; other stones, such as the opal, turquoise and the
like, are cut or ground in flat, dome-shaped, or other form, and then merely
polished. It frequently happens that only a small portion of even a large

stone is of supreme value or purity, the cutter often retaining as his
perquisite the smaller pieces and waste. These, if too small for setting, are
ground into powder and used to cut and polish other stones.
Broadly speaking, the greatest claim which a stone can possess in order to
be classed as precious is its rarity. To this may be added public opinion,
which is led for better or worse by the fashion of the moment. For if the
comparatively common amethyst should chance to be made extraordinarily
conspicuous by some society leader, it would at once step from its humbler
position as semi-precious, and rise to the nobler classification of a truly
precious stone, by reason of the demand created for it, which would, in all
probability, absorb the available stock to rarity; and this despite the more
entrancing beauty of the now rarer stones.
The study of this section of mineralogy is one of intense interest, and by
understanding the nature, environment, chemical composition and the
properties of the stones, possibility of fraud is altogether precluded, and
there is induced in the mind—even of those with whom the study of
precious stones has no part commercially—an intelligent interest in the
sight or association of what might otherwise excite no more than a mere
glance of admiration or curiosity. There is scarcely any form of matter, be it
liquid, solid, or gaseous, but has yielded or is now yielding up its secrets
with more or less freedom to the scientist. By his method of synthesis
(which is the scientific name for putting substances together in order to
form new compounds out of their union) or of analysis (the decomposing of
bodies so as to divide or separate them into substances of less complexity),
particularly the latter, he slowly and surely breaks down the substances
undergoing examination into their various constituents, reducing these still
further till no more reduction is possible, and he arrives at their elements.
From their behaviour during the many and varied processes through which
they have passed he finds out, with unerring accuracy, the exact proportions
of their composition, and, in many cases, the cause of their origin.
It may be thought that, knowing all this, it is strange that man does not
himself manufacture these rare gems, such as the diamond, but so far he has
only succeeded in making a few of microscopic size, altogether useless
except as scientific curiosities. The manner in which these minute gems and

spurious stones are manufactured, and the methods by which they may
readily be distinguished from real, will be dealt with in due course.
The natural stones represent the slow chemical action of water, decay, and
association with, or near, other chemical substances or elements, combined
with the action of millions of years of time, and the unceasing enormous
pressure during that time of thousands, perhaps millions, of tons of earth,
rock, and the like, subjected, for a certain portion at least of that period, to
extremes of heat or cold, all of which determine the nature of the gem. So
that only in the earth itself, under strictly natural conditions, can these rare
substances be found at all in any workable size; therefore they must be
sought after assiduously, with more or less speculative risk.

CHAPTER II.
THE ORIGIN OF PRECIOUS STONES.

Though the origin, formation, composition, characteristics and tests of each
stone will be examined in detail when dealing with the stones seriatim, it is
necessary to enquire into those particulars of origin which are common to
all, in order thoroughly to understand why they differ from other non-
metallic and metallic minerals.
At the very commencement we are faced with a subject on which
mineralogists and geologists are by no means in full agreement, and there
seems just ground for considerable divergence of opinion, according to the
line of argument taken. It is a most remarkable fact that, precious as are
certain stones, they do not (with a few exceptions) contain any of the rarer
metals, such as platinum, gold, etc., or any of their compounds, but are
composed entirely of the common elements and their derivatives, especially
of those elements contained in the upper crust of the earth, and this
notwithstanding the fact that gems are often found deep down in the earth.
This is very significant, and points to the conclusion that these stones were
formed by the slow percolation of water from the surface through the
deeper parts of the earth, carrying with it, in solution or suspension, the
chemical constituents of the earth's upper crust; time and long-continued
pressure, combined with heat or cold, or perhaps both in turn, doing the
rest, as already mentioned.
The moisture falling in dew and rain becomes acidulated with carbonic
acid, CO2 (carbon dioxide), from the combustion and decay of organic
matter, vegetation, and other sources, and this moisture is capable of
dissolving certain calcareous substances, which it takes deep into the earth,
till the time comes when it enters perhaps a division-plane in some rock, or
some such cavity, and is unable to get away. The hollow becomes filled
with water, which is slowly more and more charged with the salts brought
down, till saturated; then super-saturated, so that the salts become
precipitated, or perhaps crystallised out, maybe by the presence of more or

other salts, or by a change in temperature. These crystals then become
packed hard by further supplies and pressure, till eventually, after the lapse
of ages, a natural gem is found, exactly filling the cavity, and is a precious
find in many cases.
If now we try to find its analogy in chemistry, and for a moment consider
the curious behaviour of some well-known salts, under different conditions
of temperature, what is taking place underground ceases to be mysterious
and becomes readily intelligible.
Perhaps the best salt for the purpose, and one easy to obtain for experiment,
is the sulphate of sodium—known also as Glauber's Salt.
It is in large, colourless prisms, which may soon be dissolved in about three
parts of water, so long as the water does not exceed 60° F., and at this
temperature a super-saturated solution may easily be made. But if the water
is heated the salt then becomes more and more insoluble as the temperature
increases, till it is completely insoluble.
If a super-saturated solution of this Glauber's Salt is made in a glass, at
ordinary atmospheric temperature, and into this cold solution, without
heating, is dropped a small crystal of the same salt, there will be caused a
rise in temperature, and the whole will then crystallise out quite suddenly;
the water will be absorbed, and the whole will solidify into a mass which
exactly fits the inner contour of the vessel.
We have now formed what might be a precious stone, and no doubt would
be, if continuous pressure could be applied to it for perhaps a few thousand
years; at any rate, the formation of a natural jewel is not greatly different,
and after being subjected for a period, extending to ages, to the washings of
moisture, the contact of its containing bed (its later matrix), the action of the
changes in the temperature of the earth in its vicinity, it emerges by volcanic
eruption, earthquake, landslip and the like, or is discovered as a rare and
valuable specimen of some simple compound of earth-crust and water, as
simple as Glauber's Salt, or as the pure crystallized carbon.
It is also curious to note that in some cases the stones have not been caused
by aqueous deposit in an already existing hollow, but the aqueous infusion
has acted on a portion of the rock on which it rested, absorbing the rock,

and, as it were, replacing it by its own substance. This is evidenced in cases
where gems have been found encrusted on their matrix, which latter was
being slowly transformed to the character of the jewel encrusted, or
"scabbed" on it.
The character of the matrix is also in a great measure the cause of the
variety of the stone, for it is obvious that the same salt-charged aqueous
solution which undergoes change in and on ironstone would result in an
entirely different product from that resting on or embedded in silica.
Following out the explanation of the aqueous solution, in which the earth-
crust constituents are secreted, we find that the rarer and more precious
metals do not generally enter into the composition of precious stones—
which fact may advisedly be repeated. It is, of course, to be expected that
beryllium will be found in the emerald, since it is under the species beryl,
and zirconium in zircon; but such instances are the exception, and we may
well wonder at the actions of the infinite powers of nature, when we reflect
that the rarest, costliest and most beautiful of all precious stones are the
simplest in their constituents.
Thus we find the diamond standing unique amongst all gems in being
composed of one element only—carbon—being pure crystallised carbon; a
different form from graphite, it is true, but, nevertheless, pure carbon and
nothing else. Therefore, from its chemical, as well as from its commercial
aspect, the diamond stands alone as the most important of gems.
The next in simplicity, whilst being the most costly of all, is the ruby, and
with this may be classed the blue sapphire, seeing that their chemical
constituents are exactly the same, the difference being one of colour only.
These have two elements, oxygen and aluminium, which important
constituents appear also in other stones, but this example is sufficient to
prove their simplicity of origin.
Another unique stone is the turquoise, in that it is the only rare gem
essentially containing a great proportion of water, which renders it easily
liable to destruction, as we shall see later. It is a combination of alumina,
water, and phosphoric acid, and is also unique in being the only known
valuable stone containing a phosphate.

Turning to the silica series, we again find a number of gems with two
elements only, silica—an important constituent of the earth's crust—and
oxygen—an important constituent of atmospheric air. In this group may be
mentioned the opal, amethyst, agate, rock-crystal, and the like, as the best
known examples, whilst oxygen appears also mostly in the form of oxides,
in chrysoberyl, spinel, and the like. This silica group is extremely
interesting, for in it, with the exception of the tourmaline and a few others,
the composition of the gems is very simple, and we find in this group such
stones as the chrysolite, several varieties of topaz, the garnet, emerald, etc.,
etc.
Malachite and similar stones are more ornamental than precious, though
they come in the category of precious stones. These are the carbonate series,
containing much carbonic acid, and, as may be expected, a considerable
proportion of water in their composition, which water can, of course, be
dispelled by the application of heat, but to the destruction of the stone.
From all this will be seen how strong is the theory of aqueous percolation,
for, given time and pressure, water charged with earth-crust constituents
appears to be the origin of the formation of all precious stones; and all the
precious stones known have, when analysed, been found to be almost
exclusively composed of upper-earth-crust constituents; the other
compounds which certain stones contain may, in all cases, be traced to their
matrix, or to their geological or mineralogical situation.
In contradistinction to this, the essentially underground liquids, with time
and pressure, form metallic minerals and mineralise the rocks, instead of
forming gems.
Thus we see that in a different class of minerals—compounds of metals
with the sulphates, such as sulphuric acid and compounds; also those
containing the metallic sulphides; in cases where the metalliferous ores or
the metallic elements enter into composition with the halogens—bromine,
chlorine, fluorine, and iodine—in all these, precious stones are
comparatively common, but the stones of these groups are invariably those
used for decorative or ornamental purposes, and true "gems" are entirely
absent.

It would therefore appear that though metallic minerals, as already
mentioned, are formed by the action of essentially underground chemically-
charged water—combined with ages of time and long-continued pressure,
rocks and earth being transformed into metalliferous ores by the same
means—precious stones (or that portion of them ranking as jewels or gems)
must on the contrary be wholly, or almost wholly, composed of upper-earth-
crust materials, carried deep down by water, and subjected to the action of
the same time and pressure; the simpler the compound, the more perfect and
important the result, as seen in the diamond, the ruby, and the like.

CHAPTER III.
PHYSICAL PROPERTIES.

A—Crystalline Structure.

Before proceeding to the study of precious stones as individual gems,
certain physical properties common to all must be discussed, in order to
bring the gems into separate classes, not only because of some chemical
uniformity, but also because of the unity which exists between their
physical formation and properties.
The first consideration, therefore, may advisedly be that of their crystals,
since their crystalline structure forms a ready means for the classification of
stones, and indeed for that of a multitudinous variety of substances.
It is one of the many marvellous phenomena of nature that mineral, as well
as many vegetable and animal substances, on entering into a state of
solidity, take upon themselves a definite form called a crystal. These
crystals build themselves round an axis or axes with wonderful regularity,
and it has been found, speaking broadly, that the same substance gives the
same crystal, no matter how its character may be altered by colour or other
means. Even when mixed with other crystallisable substances, the resulting
crystals may partake of the two varieties and become a sort of composite,
yet to the physicist they are read like an open book, and when separated by
analysis they at once revert to their original form. On this property the
analyst depends largely for his results, for in such matters as food
adulteration, etc., the microscope unerringly reveals impurities by means of
the crystals alone, apart from other evidences.
It is most curious, too, to note that no matter how large a crystal may be,
when reduced even to small size it will be found that the crystals are still of
the same shape. If this process is taken still further, and the substance is
ground to the finest impalpable powder, as fine as floating dust, when
placed under the microscope each speck, though perhaps invisible to the

naked eye, will be seen a perfect crystal, of the identical shape as that from
which it came, one so large maybe that its planes and angles might have
been measured and defined by rule and compass. This shows how
impossible it is to alter the shape of a crystal. We may dissolve it, pour the
solution into any shaped vessel or mould we desire, recrystallise it and
obtain a solid sphere, triangle, square, or any other form; it is also possible,
in many cases, to squeeze the crystal by pressure into a tablet, or any form
we choose, but in each case we have merely altered the arrangement of the
crystals, so as to produce a differently shaped mass, the crystals themselves
remaining individually as before. Such can be said to be one of the laws of
crystals, and as it is found that every substance has its own form of crystal,
a science, or branch of mineralogy, has arisen, called "crystallography," and
out of the conglomeration of confused forms there have been evolved
certain rules of comparison by which all known crystals may be classed in
certain groups.
This is not so laborious a matter as would appear, for if we take a substance
which crystallises in a cube we find it is possible to draw nine symmetrical
planes, these being called "planes of symmetry," the intersections of one or
more of which planes being called "axes of symmetry." So that in the nine
planes of symmetry of the cube we get three axes, each running through to
the opposite side of the cube. One will be through the centre of a face to the
opposite face; a second will be through the centre of one edge diagonally;
the third will be found in a line running diagonally from one point to its
opposite. On turning the cube on these three axes—as, for example, a long
needle running through a cube of soap—we shall find that four of the six
identical faces of the cube are exposed to view during each revolution of the
cube on the needle or axis.
These faces are not necessarily, or always, planes, or flat, strictly speaking,
but are often more or less curved, according to the shape of the crystal,
taking certain characteristic forms, such as the square, various forms of
triangles, the rectangle, etc., and though the crystals may be a combination
of several forms, all the faces of any particular form are similar.
All the crystals at present known exhibit differences in their planes, axes
and lines of symmetry, and on careful comparison many of them are found
to have some features in common; so that when they are sorted out it is seen

that they are capable of being classified into thirty-three groups. Many of
these groups are analogous, so that on analysing them still further we find
that all the known crystals may be classed in six separate systems according
to their planes of symmetry, and all stones of the same class, no matter what
their variety or complexity may be, show forms of the same group.
Beginning with the highest, we have—(1) the cubic system, with nine
planes of symmetry; (2) the hexagonal, with seven planes; (3) the
tetragonal, with five planes; (4) the rhombic, with three planes; (5) the
monoclinic, with one plane; (6) the triclinic, with no plane of symmetry at
all.
In the first, the cubic—called also the isometric, monometric, or regular—
there are, as we have seen, three axes, all at right angles, all of them being
equal.
The second, the hexagonal system—called also the rhombohedral—is
different from the others in having four axes, three of them equal and in one
plane and all at 120° to each other; the fourth axis is not always equal to
these three. It may be, and often is, longer or shorter. It passes through the
intersecting point of the three others, and is perpendicular or at right angles
to them.
The third of the six systems enumerated above, the tetragonal—or the
quadratic, square prismatic, dimetric, or pyramidal—system has three axes
like the cubic, but, in this case, though they are all at right angles, two only
of them are equal, the third, consequently, unequal. The vertical or principal
axis is often much longer or shorter in this group, but the other two are
always equal and lie in the horizontal plane, at right angles to each other,
and at right angles to the vertical axis.
The fourth system, the rhombic—or orthorhombic, or prismatic, or trimetric
—has, like the tetragonal, three axes; but in this case, none of them are
equal, though the two lateral axes are at right angles to each other, and to
the vertical axis, which may vary in length, more so even than the other
two.
The fifth, the monoclinic—or clinorhombic, monosymmetric, or oblique—
system, has also three axes, all of them unequal. The two lateral axes are at
right angles to each other, but the principal or vertical axis, which passes

through the point of intersection of the two lateral axes, is only at right
angles to one of them.
In the sixth and last system, the triclinic—or anorthic, or asymmetric—the
axes are again three, but in this case, none of them are equal and none at
right angles.
It is difficult to explain these various systems without drawings, and the
foregoing may seem unnecessarily technical. It is, however, essential that
these particulars should be clearly stated in order thoroughly to understand
how stones, especially uncut stones, are classified. These various groups
must also be referred to when dealing with the action of light and other
matters, for in one or other of them most stones are placed, notwithstanding
great differences in hue and character; thus all stones exhibiting the same
crystalline structure as the diamond are placed in the same group. Further,
when the methods of testing come to be dealt with, it will be seen that these
particulars of grouping form a certain means of testing stones and of
distinguishing spurious from real. For if a stone is offered as a real gem (the
true stone being known to lie in the highest or cubic system), it follows that
should examination prove the stone to be in the sixth system, then, no
matter how coloured or cut, no matter how perfect the imitation, the test of
its crystalline structure stamps it readily as false beyond all shadow of
doubt—for as we have seen, no human means have as yet been forthcoming
by which the crystals can be changed in form, only in arrangement, for a
diamond crystal is a diamond crystal, be it in a large mass, like the brightest
and largest gem so far discovered—the great Cullinan diamond—or the
tiniest grain of microscopic diamond-dust, and so on with all precious
stones. So that in future references, to avoid repetition, these groups will be
referred to as group 1, 2, and so on, as detailed here.

CHAPTER IV.
PHYSICAL PROPERTIES.

B—Cleavage.

By cleavage is meant the manner in which minerals separate or split off
with regularity. The difference between a break or fracture and a "cleave," is
that the former may be anywhere throughout the substance of the broken
body, with an extremely remote chance of another fracture being identical
in form, whereas in the latter, when a body is "cleaved," the fractured part is
more readily severed, and usually takes a similar if not an actually identical
form in the divided surface of each piece severed. Thus we find a piece of
wood may be "broken" or "chopped" when fractured across the grain, no
two fractured edges being alike; but, strictly speaking, we only "cleave"
wood when we "split" it with the grain, or, in scientific language, along the
line of cleavage, and then we find many pieces with their divided surfaces
identical. So that when wood is "broken," or "chopped," we obtain pieces of
any width or thickness, with no manner of regularity of fracture, but when
"cleaved," we obtain strips which are often perfectly parallel, that is, of
equal thickness throughout their whole length, and of such uniformity of
surface that it is difficult or even impossible to distinguish one strip from
another. Advantage is taken of these lines of cleavage to procure long and
extremely thin even strips from trees of the willow variety for such trades as
basket-making.
The same effect is seen in house-coal, which may easily be split the way of
the grain (on the lines of cleavage), but is much more difficult and requires
greater force to break across the grain. Rocks also show distinct lines of
cleavage, and are more readily split one way than another, the line of
cleavage or stratum of break being at any angle and not necessarily parallel
to its bed. A striking example of this is seen in slate, which may be split in
plates, or laminæ, with great facility, though this property is the result of the
pressure to which the rock has been for ages subjected, which has caused a

change in the molecules, rather than by "cleavage" as the term is strictly
understood, and as existing in minerals. Mica is also another example of
laminated cleavage, for given care, and a thin, fine knife to divide the
plates, this mineral may be "cleaved" to such remarkably thin sheets as to
be unable to sustain the most delicate touch without shattering.
These are well-known examples of simple cleavage, in one definite
direction, though in many instances there are several forms and directions
of cleavage, but even in these there is generally one part or line in and on
which cleavage will take place much more readily than on the others, these
planes or lines also showing different properties and angular characters,
which, no matter how much fractured, always remain the same. It is this
"cleavage" which causes a crystal to reproduce itself exactly, as explained
in the last chapter, showing its parent form, shape and characteristics with
microscopic perfection, but more and more in miniature as its size is
reduced.
This may clearly be seen by taking a very small quantity of such a
substance as chlorate of potash. If a crystal of this is examined under a
magnifying glass till its crystalline form and structure are familiar, and it is
then placed in a test-tube and gently heated, cleavage will at once be
evident. With a little crackling, the chlorate splits itself into many crystals
along its chief lines of cleavage (called the cleavage planes), every one of
which crystals showing under the microscope the identical form and
characteristics of the larger crystal from which it came.
The cleavage of minerals must, therefore, be considered as a part of their
crystalline structure, since this is caused by cleavage, so that both cleavage
and crystalline structure should be considered together. Thus we see that
given an unchangeable crystal with cleavage planes evident, it is possible
easily to reproduce the same form over and over again by splitting, whereas
by simply breaking, the form of the crystal would be lost; just as a rhomb of
Iceland spar might be sawn or broken across the middle and its form lost,
although this would really be more apparent than real, since it would be an
alteration in the mass and not in the shape of each individual crystal. And
given further cleavage, by time or a sudden breaking down, even the mass,
as mass, would eventually become split into smaller but perfect rhombs.

Much skill is, therefore, required in cutting and fashioning a precious stone,
otherwise the gem may be ruined at the onset, for it will only divide along
its lines of cleavage, and any mistake in deciding upon these, would
"break," not "split" the stone, and destroy the beauty of its crystalline
structure. An example of this was specially seen in the great Cullinan
diamond, the splitting of which was perhaps the most thrilling moment in
the history of precious stones.[A] The value of the enormous crystal was
almost beyond computation, but it had a flaw in the centre, and in order to
cut out this flaw it was necessary to divide the stone into two pieces. The
planes of cleavage were worked out, the diamond was sawn a little, when
the operator, acknowledged to be the greatest living expert, inserted a knife
in the saw-mark, and with the second blow of a steel rod, the marvellous
stone parted precisely as intended, cutting the flaw exactly in two, leaving
half of it on the outside of each divided portion. The slightest
miscalculation would have meant enormous loss, if not ruin, to the stone,
but the greatest feat the world has ever known in the splitting of a priceless
diamond was accomplished successfully by this skilful expert in an
Amsterdam workroom in February, 1908. Some idea of the risk involved
may be gathered from the fact that this stone, the largest ever discovered, in
the rough weighed nearly 3,254 carats, its value being almost anything one
cared to state—incalculable.
[A] The hammer and knife used in cutting the diamond, the two largest pieces of
which are now called "The Stars of Africa," together with a model of the great
uncut stone, are in the Tower of London amongst the Regalia.

These cleavage planes help considerably in the bringing of the stone to
shape, for in a broad sense, a finished cut stone may be said to be in the
form in which its cleavages bring it. Particularly is this seen in the diamond
"brilliant," which plainly evidences the four cleavage planes. These
cleavage planes and their number are a simple means of identification of
precious stones, though those possessing distinct and ready cleavages are
extremely liable to "start" or "split" on these planes by extremes of heat and
cold, accidental blows, sudden shocks and the like.
In stones possessing certain crystalline structure, the cleavage planes are the
readiest, often the only, means of identification, especially when the stones
are chemically coloured to imitate a more valuable stone. In such cases the
cleavage of one stone is often of paramount importance in testing the

cleavage of another, as is seen in the perfection of the cleavage planes of
calcite, which is used in the polariscope.
It sometimes happens, however, that false conditions arise, such as in
substances which are of no form or shape, and are in all respects and
directions without regular structure and show no crystallisation even in the
minutest particles; these are called amorphous. Such a condition sometimes
enters wholly or partially into the crystalline structure, and the mineral loses
its true form, possessing instead the form of crystals, but without a
crystalline structure. It is then called a pseudomorph, which is a term
applied to any mineral which, instead of having the form it should possess,
shows the form of something which has altered its structure completely, and
then disappeared. For instance: very often, in a certain cavity, fluorspar has
existed originally, but, through some chemical means, has been slowly
changed to quartz, so that, as crystals cannot be changed in shape, we find
quartz existing—undeniably quartz—yet possessing the crystals of
fluorspar; therefore the quartz becomes a pseudomorph, the condition being
an example of what is termed pseudomorphism. The actual cause of this
curious chemical change or substitution is not known with certainty, but it is
interesting to note the conditions in which such changes do occur.
It is found that in some cases, the matrix of a certain shaped crystal may,
after the crystal is dissolved or taken away, become filled by some other
and foreign substance, perhaps in liquid form; or a crystalline substance
may become coated or "invested" by another foreign substance, which thus
takes its shape; or actual chemical change takes place by means of an
incoming substance which slowly alters the original substance, so that
eventually each is false and both become pseudomorphs. This curious
change often takes place with precious stones, as well as with other
minerals, and to such an extent that it sometimes becomes difficult to say
what the stone ought really to be called.
Pseudomorphs are, however, comparatively easy of isolation and detection,
being more or less rounded in their crystalline form, instead of having
sharp, well-defined angles and edges; their surfaces also are not good.
These stones are of little value, except in the specially curious examples,
when they become rare more by reason of their curiosity than by their
utility as gems.

Some also show cleavage planes of two or more systems, and others show a
crystalline structure comprised of several systems. Thus calcspar is in the
2nd, or hexagonal, whilst aragonite is in the 4th, the rhombic, system, yet
both are the same substance, viz.:—carbonate of lime. Such a condition is
called dimorphism; those minerals which crystallise in three systems are
said to be trimorphous. Those in a number of systems are polymorphous,
and of these sulphur may be taken as an example, since it possesses thirty or
more modifications of its crystalline structure, though some authorities
eliminate nearly all these, and, since it is most frequently in either the 4th
(rhombic) or the 5th (monoclinic) systems, consider it as an example of
dimorphism, rather than polymorphism.
These varieties of cleavage affect the character, beauty and usefulness of
the stone to a remarkable extent, and at the same time form a means of
ready and certain identification and classification.

CHAPTER V.
PHYSICAL PROPERTIES.

C—Light.

Probably the most important of the many important physical properties
possessed by precious stones are those of light and its effects, for to these
all known gems owe their beauty, if not actual fascination.
When light strikes a cut or polished stone, one or more of the following
effects are observed:—it may be transmitted through the stone, diaphaneity,
as it is called; it may produce single or double refraction, or polarisation; if
reflected, it may produce lustre or colour; or it may produce
phosphorescence; so that light may be (1) transmitted; (2) reflected; or
produce (3) phosphorescence.
(1) Transmission.—In transmitted light we have, as stated above, single or
double refraction, polarisation, and diaphaneity.
To the quality of refraction is due one of the chief charms of certain
precious stones. It is not necessary to explain here what refraction is, for
everyone will be familiar with the refractive property of a light-beam when
passing through a medium denser than atmospheric air. It will be quite
sufficient to say that all the rays are not equal in refractive power in all
substances, so that the middle of the spectrum is generally selected as the
mean for indexing purposes.
It will be seen that the stones in the 1st, or cubic system, show single
refraction, whereas those of all other systems show double refraction; thus,
light, in passing through their substance, is deviated, part of it going one
way, the other portion going in another direction—that is, at a slightly
different angle—so that this property alone will isolate readily all gems
belonging to the 1st system.

A well-known simple experiment in physics shows this clearly. A mark on a
card or paper is viewed through a piece of double-refracting spar (Iceland
spar or clear calcite), when the mark is doubled and two appear. On rotating
this rhomb of spar, one of these marks is seen to revolve round the other,
which remains stationary, the moving mark passing further from the centre
in places. When the spar is cut and used in a certain direction, we see but
one mark, and such a position is called its optical axis.
Polarisation is when certain crystals possessing double refraction have the
power of changing light, giving it the appearance of poles which have
different properties, and the polariscope is an instrument in which are
placed pieces of double-refracting (Iceland) spar, so that all light passing
through will be polarised.
Since only crystals possessing the property of double refraction show
polarisation, it follows that those of the 1st, or cubic system—in which the
diamond stands a prominent example—fail to become polarised, so that
when such a stone is placed in the polariscope and rotated, it fails at every
point to transmit light, which a double-refracting gem allows to pass except
when its optical axis is placed in the axis of the polariscope, but this will be
dealt with more fully when the methods of testing the stones come to be
considered.
Diaphaneity, or the power of transmitting light:—some rather fine trade
distinctions are drawn between the stones in this class, technical distinctions
made specially for purposes of classification, thus:—a "non-diaphanous"
stone is one which is quite opaque, no light of any kind passing through its
substance; a "diaphanous" stone is one which is altogether transparent;
"semi-diaphanous" means one not altogether transparent, and sometimes
called "sub-transparent." A "translucent" stone is one in which, though light
passes through its substance, sight is not possible through it; whilst in a
"sub-translucent" stone, light passes through it, but only in a small degree.
The second physical property of light is seen in those stones which owe
their beauty or value to Reflection: this again may be dependent on Lustre,
or Colour.
Lustre.—This is an important characteristic due to reflection, and of which
there are six varieties:—(α) adamantine (which some authorities, experts

and merchants subdivide as detailed below); (β) pearly; (γ) silky; (δ)
resinous; (ε) vitreous; (ζ) metallic. These may be described:—
(α) Adamantine, or the peculiar lustre of the diamond, so called from the
lustre of adamantine spar, which is a form of corundum (as is emery) with a
diamond-like lustre, the hard powder of which is used in polishing
diamonds. It is almost pure anhydrous alumina (Al2O3) and is, roughly, four
times as heavy as water. The lustre of this is the true "adamantine," or
diamond, brilliancy, and the other and impure divisions of this particular
lustre are: splendent, when objects are reflected perfectly, but of a lower
scale of perfection than the true "adamantine" standard, which is absolutely
flawless. When still lower, and the reflection, though maybe fairly good, is
somewhat "fuzzy," or is confused or out of focus, it is then merely shining;
when still less distinct, and no trace of actual reflection is possible (by
which is meant that no object can be reproduced in any way to define it, as
it could be defined in the reflection from still water or the surface of a
mirror, even though imperfectly) the stone is then said to glint or glisten.
When too low in the scale even to glisten, merely showing a feeble lustre
now and again as the light is reflected from its surface in points which vary
with the angle of light, the stone is then said to be glimmering. Below this,
the definitions of lustre do not go, as such stones are said to be lustreless.
(β) Pearly, as its name implies, is the lustre of a pearl.
(γ) Silky, possessing the sheen of silk, hence its name.
(δ) Resinous, also explanatory in its name; amber and the like come in this
variety.
(ε) Vitreous. This also explains itself, being of the lustre of glass, quartz,
etc.; some experts subdividing this for greater defining accuracy into the
"sub-vitreous" or lower type, for all but perfect specimens.
(ζ) Metallic or Sub-metallic. The former when the lustre is perfect as in
gold; the latter when the stones possess the less true lustre of copper.
Colour.—Colour is an effect entirely dependent upon light, for in the total
absence of light, such as in black darkness, objects are altogether invisible
to the normal human eye. In daylight, also, certain objects reflect so few

vibrations of light, or none, that they appear grey, black, or jet-black; whilst
those which reflect all the rays of which light is composed, and in the same
number of vibrations, appear white. Between these two extremes of none
and all we find a wonderful play and variety of colour, as some gems allow
the red rays only to pass and therefore appear red; others allow the blue rays
only and these appear blue, and so on, through all the shades, combinations
and varieties of the colours of which light is composed, as revealed by the
prism. But this is so important a matter that it demands a chapter to itself.
The third physical property of light, Phosphorescence, is the property
possessed by certain gems and minerals of becoming phosphorescent on
being rubbed, or on having their temperature raised by this or other means.
It is difficult to say exactly whether this is due to the heat, the friction, or to
electricity. Perhaps two or all of these may be the cause, for electricity is
developed in some gems—such as the topaz—by heat, and heat by
electricity, and phosphorescence developed by both.
For example, if we rub together some pulverised fluorspar in the dark, or
raise its temperature by the direct application of heat, such as from a hot or
warm iron, or a heated wire, we at once obtain excellent phosphorescence.
Common quartz, rubbed against a second piece of the same quartz in the
dark, becomes highly phosphorescent. Certain gems, also, when merely
exposed to light—sunlight for preference—then taken into a darkened
room, will glow for a short time. The diamond is one of the best examples
of this kind of phosphorescence, for if exposed to sunlight for a while, then
covered and rapidly taken into black darkness, it will emit a curious
phosphorescent glow for from one to ten seconds; the purer the stone, the
longer, clearer and brighter the result.

CHAPTER VI.
PHYSICAL PROPERTIES.

D—Colour.

Colour is one of the most wonderful effects in nature. It is an attribute of
light and is not a part of the object which appears to be coloured; though all
objects, by their chemical or physical composition, determine the number
and variety of vibrations passed on or returned to the eye, thus fixing their
own individual colours.
We have also seen that if an equal light-beam becomes obstructed in its
passage by some substance which is denser than atmospheric air, it will
become altered in its direction by refraction or reflection, and polarised,
each side or pole having different properties.
Polarised light cannot be made again to pass in a certain direction through
the crystal which has polarised it; nor can it again be reflected at a
particular angle; so that in double-refracting crystals, these two poles, or
polarised beams, are different in colour, some stones being opaque to one
beam but not to the other, whilst some are opaque to both.
This curious phenomenon, with this brief, though somewhat technical
explanation, shows the cause of many of the great charms in precious
stones, for when viewed at one angle they appear of a definite colour, whilst
at another angle they are just as decided in their colour, which is then
entirely different; and as these angles change as the eye glances on various
facets, the stone assumes a marvellous wealth of the most brilliant and
intense colour of kaleidoscopic variety, even in a stone which may itself be
absolutely clear or colourless to ordinary light.
Such an effect is called pleochroism, and crystals which show variations in
their colour when viewed from different angles, or by transmitted light, are
called pleochroic, or pleochromatic—from two Greek words signifying "to

colour more." To aid in the examination of this wonderfully beautiful
property possessed by precious stones, a little instrument has been invented
called the dichroscope, its name showing its Greek derivation, and meaning
—"to see colour twice" (twice, colour, to see). It is often a part of a
polariscope; frequently a part also of the polarising attachment to the
microscope, and is so simple and ingenious as to deserve detailed
explanation.
In a small, brass tube is fixed a double-image prism of calcite or Iceland
spar, which has been achromatised—that is, clear, devoid of colour—and is
therefore capable of transmitting light without showing any prismatic effect,
or allowing the least trace of any except the clear light-beam to pass
through. At one end of this tube there is a tiny square hole, the opposite end
carrying a small convex lens, of such a strength or focus as to show the
square hole in true focus, that is, with perfectly sharp definition, even up to
the corners of the square. On looking through the tube, the square hole is
duplicated, two squares being seen. The colours of a gem are tested by the
stone being put in front of this square, when the two colours are seen quite
distinctly. Not only is this a simple means of judging colour, but it enables a
stone to be classified readily. For if the dichroscope shows two images of
the same colour, then it may possibly be a carbuncle, or a diamond, as the
case may be—for single-refracting stones, of the first or cubic system, show
two images of the same colour. But if these two colours are different, then it
must be a double-refracting stone, and according to the particular colours
seen, so is the stone classified, for each stone has its own identical colour or
colours when viewed through this small but useful instrument.
How clear and distinct are these changes may be viewed without it in
substances strongly dichroic; for instance, if common mica is viewed in one
direction, it is transparent as polished plate-glass, whilst at another angle, it
is totally opaque. Chloride of palladium also is blood-red when viewed
parallel to its axis, and transversely, it is a remarkably bright green. The
beryl also, is sea-green one way and a beautiful blue another; the yellow
chrysoberyl is brown one way and yellow with a greenish cast when viewed
another way. The pink topaz shows rose-colour in one direction and yellow
in another. These are perhaps the most striking examples, and are mostly
self-evident to the naked eye, whilst in other cases, the changes are so
delicate that the instrument must be used to give certainty; some again show

changes of colour as the stone is revolved in the dichroscope, or the
instrument revolved round the stone.
Some stones, such as the opal, split up the light-beams as does a prism, and
show a wonderful exhibition of prismatic colour, which is technically
known as a "play of colour." The descriptive term "opalescence" is self-
suggesting as to its origin, which is the "noble" or "precious" opal; this
radiates brilliant and rapidly changing iridescent reflections of blue, green,
yellow and red, all blending with, and coming out of, a curious silky and
milky whiteness, which is altogether characteristic. The moonstone is
another example of this peculiar feature which is possessed in a more or
less degree by all the stones in the class of pellucid jewels, but no stone or
gem can in any way even rival the curious mixture of opaqueness,
translucency, silkiness, milkiness, fire, and the steadfast changeable and
prismatic brilliance of colour of the precious opal. The other six varieties of
opal are much inferior in their strange mixture of these anomalies of light
and colour. Given in order of value, we have as the second, the "fire" opal
with a red reflection, and, as a rule, that only. The third in value is the
"common" opal, with the colours of green, red, white and yellow, but this is
easily distinguishable from the "noble" or "precious" variety in that the
common opal does not possess that wonderful "play" of colour. The fourth
variety is called the "semi-opal," which is really like the third variety, the
"common," but of a poorer quality and more opaque. The fifth variety in
order of value, is that known as the "hydrophane," which has an interesting
characteristic in becoming transparent when immersed in water, and only
then. The sixth is the "hyalite," which has but a glassy or vitreous lustre,
and is found almost exclusively in the form of globules, or clusters of
globules, somewhat after the form and size of bunches of grapes; hence the
name "botryoidal" is often applied to this variety. The last and commonest
of all the seven varieties of opal is somewhat after the shape of a kidney
(reniform), or other irregular shape, occasionally almost transparent, but
more often somewhat translucent, and very often opaque. This seventh class
is called "menilite," being really an opaline form of quartz, originally found
at Menilmontant, hence its name (Menil, and Greek lithos, stone). It is a
curious blue on the exterior of the stone, brown inside.
History records many magnificent and valuable opals, not the least of which
was that of Nonius, who declined to give it to Mark Antony, choosing exile

rather than part with so rare a jewel, which Pliny describes as being existent
in his day, and of a value which, in present English computation, would
exceed one hundred thousand pounds.
Many other stones possess one or more properties of the opal, and are
therefore considered more or less opalescent. This "play of colour" and
"opalescence," must not be confused with "change of colour." The two first
appear mostly in spots and in brilliant points or flashes of coloured light, or
"fire" as it is termed. This fire is constantly on the move, or "playing,"
whereas "change of colour," though not greatly dissimilar, is when the fire
merely travels over broader surfaces, each colour remaining constant, such
as when directly moving the stone, or turning it, when the broad mass of
coloured light slowly changes, usually to its complementary. Thus in this
class of stone, subject to "change of colour," a green light is usually
followed by its complementary, red, yellow by purple, blue by orange,
green by brown, orange by grey, purple by broken green, with all the
intermediary shades of each.
Thus when the line of sight is altered, or the stone moved, never otherwise,
the colours chase one another over the surface of the gem, and mostly in
broad splashes; but in those gems possessing "play of colour," strictly
speaking, whilst the stone itself remains perfectly still, and the sight is fixed
unwaveringly upon it, the pulsations of the blood in the eyes, with the
natural movements of the eyes and eyelids, even in a fixed, steady glance,
are quite sufficient to create in the stone a display of sparks and splashes of
beautiful fiery light and colour at every tremor.
The term "iridescence" is used when the display of colour is seen on the
surface, rather than coming out of the stone itself. The cause of this is a
natural, or in some cases an accidental, breaking of the surface of the stone
into numerous cobweb-like cracks; these are often of microscopic fineness,
only perceptible under moderately high powers. Nevertheless they are quite
sufficient to interfere with and refract the light rays and to split them up
prismatically. In some inferior stones this same effect is caused or obtained
by the application of a gentle heat, immersion in chemicals, subjection to
"X rays" and other strong electric influence, and in many other ways. As a
result, the stone is very slightly expanded, and as the molecules separate,
there appear on the surface thousands, perhaps millions, of microscopic

fissures running at all angles, so that no matter from what position the stone
may be viewed, a great number of these fissures are certain to split up the
light into prismatic colours causing brilliant iridescence. Similar fissures
may often be seen with the naked eye on glass, especially if scorched or
cooled too rapidly (chilled), and on the surface of clear spar and mica, their
effects being of extreme interest, from a colour point of view, at least.

CHAPTER VII.
PHYSICAL PROPERTIES.

E—Hardness.

Hardness is perhaps one of the most important features in a stone,
especially those of the "gem" series, for no matter how colour, lustre,
general beauty and even rarity may entitle a stone to the designation
"precious," unless it possesses great hardness it cannot be used as a gem or
jewel.
Consequently, the hardness of jewels is a matter of no small importance,
and by dint of indefatigable research, in tests and comparison, all known
precious stones have been classified in various scales or degrees of
hardness. The most popular and reliable table is that of Mohs, in which he
takes talc as the softest of the rarer minerals and classes this as No. 1; from
that he goes by gradual steps to the diamond, the hardest of the stones,
which he calls No. 10, and between these two all other gems are placed.
Here is given a complete list of Mohs's arrangement of stones, according to
their hardness, beginning at No. 1, thus:—

Talc 1
Rock salt 2
Amber 2-1/2
Calcite 3
Malachite 3-1/2
Jet 3-1/2
Fluorspar 4
Apatite 5
Dioptase 5
Kyanite (various) 5-7
Haüynite 5-1/2

Hæmatite 5-1/2
Lapis lazuli 5-1/2
5-1/2-6-
Moldavite (various)
1/2
5-1/2-6-
Rhodonite
1/2
Obsidian 5-1/2
Sphene 5-1/2
5-1/2-6-
Opal (various)
1/2
Nephrite 5-3/4
Chrysolite 6-7
Felspar 6
Adularia 6
Amazon stone 6
Diopside 6
Iron pyrites 6
Labradorite 6
Turquoise 6
Spodumene 6-1/2-7
The Chalcedony group which embraces the Agate, Carnelian,
6-1/2
etc.
Demantoid 6-1/2
Epidote 6-1/2
Idocrase 6-1/2
6-1/2-7-
Garnets (see also "Red Garnets" below)
1/2
Axinite 6-3/4
Jadeite 6-3/4
Quartz, including Rock-crystal,Amethyst, Jasper, Chrysoprase
7
Citrine, etc.
Jade 7
Dichorite (water sapphire) 7-7-1/2
Cordierite 7-1/4
Red Garnets (see also Garnets above) 7-1/4

Tourmaline 7-1/4
Andalusite 7-1/2
Euclase 7-1/2
Staurolite 7-1/2
Zircon 7-1/2
Emerald, Aquamarine, or Beryl 7-3/4
Phenakite 7-3/4
Spinel 8
Topaz 8
Chrysoberyl 8-1/2
The Corundum group embracing the Ruby,Sapphire, etc. 9
Diamond 10

(See also list of stones, arranged in their respective colours, in Chapter XII.)
The method of testing is very simple. A representative selection of the
above stones, each with a sharp edge, is kept for the purpose of scratching
and being scratched, and those usually set apart for tests in the various
groups, are as follows:—

1 Talc
2 Rock-salt, or Gypsum
3 Calcite
4 Fluorspar
5 Apatite
6 Felspar
7 Quartz
8 Topaz
9 Corundum
10 Diamond

The stone under examination may perhaps first be somewhat roughly
classified by its colour, cleavage, and general shape. One of these standard
stones is then gently rubbed across its surface and then others of
increasingly higher degrees, till no scratch is evident under a magnifying
glass. Thus if quartz ceases to scratch it, but a topaz will do so, the degree

of hardness must lie between 7 and 8. Then we reverse the process: the
stone is passed over the standard, and if both quartz and topaz are scratched,
then the stone is at least equal in hardness to the topaz, and its classification
becomes an easy matter.
Instead of stones, some experts use variously-tempered needles of different
qualities and compositions of iron and steel. For instance, a finely-tempered
ordinary steel needle will cut up to No. 6 stones; one made of tool steel, up
to 7; one of manganese steel, to 7-1/2; one made of high-speed tool steel, to
8 and 8-1/2, and so on, according to temper; so that from the scratch which
can be made with the finger-nail on mica, to the hardness of the diamond,
which diamond alone will scratch readily, the stones may be picked out,
classified and tested, with unerring accuracy.
It will thus be seen how impossible it is, even in this one of many tests, for
an expert to be deceived in the purchase of precious stones, except through
gross carelessness—a fault seldom, if ever, met with in the trade. For
example—a piece of rock-crystal, chemically coloured, and cut to represent
a ruby, might appear so like one as to deceive a novice, but the mere
application to its surface of a real ruby, which is hardness 9, or a No. 9
needle, would reveal too deep or powdery a scratch; also its possibility of
being scratched by a topaz or a No. 8 needle, would alone prove it false, for
the corundum group, being harder than No. 8, could not be scratched by it.
So would the expert go down the scale, the tiny scratches becoming fainter
as he descended, because he would be approaching more nearly the
hardness of the stone under test, till he arrived at the felspar, No. 6, which
would be too soft to scratch it, yet the stone would scratch the felspar, but
not zircon or andalusite, 7-1/2, or topaz, 8, so that his tests would at once
classify the stone as a piece of cut and coloured quartz, thus confirming
what he would, at the first sight, have suspected it to be.
The standard stones themselves are much more certain in results than the
needles, which latter, though well selected and tempered, are not altogether
reliable, especially in the more delicate distinctions of picking out the
hardest of certain stones of the same kind, in which cases only the expert
judge can decide with exactness. Accurate in this the expert always is, for
he judges by the sound and depth of his cut, and by the amount and quality

of the powder, often calling the microscope to his aid, so that when the
decision is made finally, there is never the least doubt about it.
Rapidly as these tests can be made, they are extremely reliable, and should
the stone be of great value, it is also subjected to other unerring tests of
extreme severity, any one of which would prove it false, if it chanced to be
so, though some stones are manufactured and coloured so cleverly that to
all but the expert judge and experienced dealer, they would pass well for the
genuine.
In Mohs's list it will be seen that several stones vary considerably, the opal,
for instance, having a degree of hardness from 5-1/2 to 6-1/2 inclusive. All
stones differ slightly, though almost all may be said to fit their position in
the scale; but in the case of the opal, the difference shown is partly due to
the many varieties of the stone, as described in the last chapter.
In applying this test of hardness to a cut gem, it will be noticed that some
parts of the same stone seem to scratch more readily than others, such as on
a facet at the side, which is often softer than those nearest the widest part of
the stone, where the claws, which hold it in its setting, usually come. This
portion is called the "girdle," and it is on these "girdle" facets that the
scratches are generally made. This variation in hardness is mostly caused by
cleavage, these cleavage planes showing a marked, though often but slight,
difference in the scratch, which difference is felt rather than seen. In
addition to the peculiar feel of a cutting scratch, is the sound of it. On a soft
stone being cut by a hard one, little or no sound is heard, but there will form
a plentiful supply of powder, which, on being brushed off, reveals a more or
less deep incision. But as the stones approach one another in hardness, there
will be little powder and a considerable increase in the noise; for the harder
are the stones, cutting and being cut, the louder will be the sound and the
less the powder. An example of this difference is evident in the cutting of
ordinary glass with a "set" or "glazier's" diamond, and with a nail. If the
diamond is held properly, there will be heard a curious sound like a keen,
drawn-out "kiss," the diamond being considerably harder than the material
it cut. An altogether different sound is that produced by the scratching of
glass with a nail. In this case, the relative difference in hardness between
the two is small, so that the glass can only be scratched and not "cut" by the
nail; it is too hard for that, so the noise is much greater and becomes a

screech. Experience, therefore, makes it possible to tell to a trifle, at the first
contact, of what the stone is composed, and in which class it should be
placed, by the mere "feel" of the scratch, the depth of it, the amount and
kind of powder it leaves, and above all, by the sound made, which, even in
the tiniest scratch, is quite characteristic.

CHAPTER VIII.
PHYSICAL PROPERTIES.

F—Specific Gravity.

The fixing of the specific gravity of a stone also determines its group
position with regard to weight; its colour and other characteristics defining
the actual stone. This is a safe and very common method of proving a stone,
since its specific gravity does not vary more than a point or so in different
specimens of the same stone. There are several ways of arriving at this,
such as by weighing in balances in the usual manner, by displacement, and
by immersion in liquids the specific gravity of which are known. Cork is of
less specific gravity than water, therefore it floats on the surface of that
liquid, whereas iron, being heavier, sinks. So that by changing the liquid to
one lighter than cork, the cork will sink in it as does iron in water; in the
second instance, if we change the liquid to one heavier than iron, the iron
will float on it as does cork on water, and exactly as an ordinary flat-iron
will float on quicksilver, bobbing up and down like a cork in a tumbler of
water. If, therefore, solutions of known but varying densities are
compounded, it is possible to tell almost to exactitude the specific gravity of
any stone dropped into them, by the position they assume. Thus, if we take
a solution of pure methylene iodide, which has a specific gravity of 3.2981,
and into this drop a few stones selected indiscriminately, the effect will be
curious: first, some will sink plump to the bottom like lead; second, some
will fall so far quickly, then remain for a considerable time fairly stationary;
third, some will sink very slowly; fourth, some will be partially immersed,
that is, a portion of their substance being above the surface of the liquid and
a portion covered by it; fifth, some will float on the surface without any
apparent immersion. In the first case, the stones will be much heavier than
3.2981; in the second, the stones will be about 3.50; in the third and fourth
instances, the stones will be about the same specific gravity as the liquid,
whilst in the fifth, they will be much lighter, and thus a rough but tolerably
accurate isolation may be made.

On certain stones being extracted and placed in other liquids of lighter or
denser specific gravity, as the case may be, their proper classification may
easily be arrived at, and if the results are checked by actual weight, in a
specific gravity balance, they will be found to be fairly accurate. The
solution commonly used for the heaviest stones is a mixture of nitrate of
thallium and nitrate of silver. This double nitrate has a specific gravity of
4.7963, therefore such a stone as zircon, which is the heaviest known, will
float in it. For use, the mixture should be slightly warmed till it runs thin
and clear; this is necessary, because at 60° (taking this as ordinary
atmospheric temperature) it is a stiff mass. A lighter liquid is a mixture of
iodide of mercury in iodide of potassium, but this is such an extremely
corrosive and dangerous mixture, that the more common solution is one in
which methylene iodide is saturated with a mixture of iodoform until it
shows a specific gravity of 3.601; and by using the methylene iodide alone,
in its pure state, it having a specific gravity of 3.2981, the stones to that
weight can be isolated, and by diluting this with benzole, its weight can be
brought down to that of the benzole itself, as in the case of Sonstadt's
solution. This solution, in full standard strength, has a specific gravity of
3.1789, but may be weakened by the addition of distilled water in varying
proportions till the weight becomes almost that of water.
Knowing the specific gravity of all stones, and dividing them into six
groups, by taking a series of standard solutions selected from one or other
of the above, and of known specific gravity, we can judge with accuracy if
any stone is what it is supposed to be, and classify it correctly by its mere
floating or sinking when placed in these liquids. Beginning then with the
pure double nitrate of silver and thallium, this will isolate the stones of less
specific gravity than 4.7963, and taking the lighter solutions and
standardising them, we may get seven solutions which will isolate the
stones as follows:—

shows stones which a specific gravity
A 4.7963
the have over
and
B " " " 3.70 4.7963
under
C " " " 3.50 " 3.70
D " " " 3.00 " 3.50

E " " " 2.50 " 3.00
F " " " 2.00 " 2.50
G " " — — under 2.00

Therefore each liquid will isolate the stones in its own group by compelling
them to float on its surface; commencing with the heaviest and giving to the
groups the same letters as the liquids, it is seen that—
Group A.—Isolates gems with a specific gravity of 4.7963 and over 4.70; in
this group is placed zircon, with a specific gravity of from 4.70 to 4.88.
Group B.—Stones whose specific gravity lies between 3.70 and under
4.7963.

Garnets, many varieties. See Group D below.
Almandine 4.11 and occasionally to 4.25
Ruby 4.073 " 4.080
Sapphire 4.049 " 4.060
Corundum 3.90 " 4.16
Cape Ruby 3.861
Demantoid 3.815
Staurolite 3.735
Malachite 3.710and occasionally to 3.996

Group C.—Stones whose specific gravity lies between 3.50 and under 3.70.

Pyrope (average) 3.682
Chrysoberyl 3.689and occasionally to 3.752
Spinel 3.614 " 3.654
Kyanite 3.609 " 3.688
Hessonite 3.603 " 3.651
Diamond 3.502 " 3.564
Topaz 3.500 " 3.520

Group D.—Stones whose specific gravity lies between 3 and under 3.50.

Rhodonite 3.413and occasionally to 3.617

Garnets 3.400 " 4.500
Epidote 3.360 " 3.480
Sphene 3.348and occasionally to 3.420
Idocrase 3.346 " 3.410
Olivine 3.334 " 3.368
Chrysolite 3.316 " 3.528
Jade 3.300 " 3.381
Jadeite 3.299
Axinite 3.295
Dioptase 3.289
Diopside 2.279
Tourmaline (yellow) 3.210
Andalusite 3.204
Apatite 3.190
Tourmaline (Blue and Violet) 3.160
Tourmaline (Green) 3.148
" (Red) 3.100
Spodumene 3.130and occasionally to 3.200
Euclase 3.090
Fluorspar 3.031and occasionally to 3.200
Tourmaline (Colourless) 3.029
Tourmaline (Blush Rose) 3.024
Tourmaline (Black) 3.024and occasionally to 3.300
Nephrite 3.019

Group E.—Stones whose specific gravity lies between 2.50 and under
3.000.

Phenakite 2.965
Turquoise 2.800
Beryl 2.709and occasionally to 2.81
Aquamarine 2.701 " 2.80
Labradorite 2.700
Emerald 2.690
Quartz 2.670

Chrysoprase 2.670
Jasper 2.668
Amethyst 2.661
Hornstone 2.658
Citrine 2.658
Cordierite 2.641
Agate 2.610
Chalcedony 2.598and occasionally to 2.610
Adularia 2.567
Rock-crystal 2.521and occasionally to 2.795

Group F.—Stones whose specific gravity lies between 2.00 and under 2.50.

Haüynite 2.470and occasionally to 2.491
Lapis lazuli 2.461
Moldavite 2.354
Opal 2.160and according to variety to 2.283
" (Fire Opal)2.210(average)

Group G.—Stones whose specific gravity is under 2.00.

Jet 1.348
Amber 1.000

(See also list of stones, arranged in their respective colours, in
Chapter XII.)
In many of these cases the specific gravity varies from .11 to .20, but the
above are the average figures obtained from a number of samples specially
and separately weighed. In some instances this difference may cause a
slight overlapping of the groups, as in group C, where the chrysoberyl may
weigh from 3.689 to 3.752, thus bringing the heavier varieties of the stone
into group B, but in all cases where overlapping occurs, the colour, form,
and the self-evident character of the stone are in themselves sufficient for
classification, the specific gravity proving genuineness. This is especially
appreciated when it is remembered that so far science has been unable
(except in very rare instances of no importance) to manufacture any stone

of the same colour as the genuine and at the same time of the same specific
gravity. Either the colour and characteristics suffer in obtaining the required
weight or density, or if the colour and other properties of an artificial stone
are made closely to resemble the real, then the specific gravity is so greatly
different, either more or less, as at once to stamp the jewel as false. In the
very few exceptions where chemically-made gems even approach the real
in hardness, colour, specific gravity, &c., they cost so much to obtain and
the difficulties of production are so great that they become mere chemical
curiosities, far more costly than the real gems. Further, they are so much
subject to chemical action, and are so susceptible to their surroundings, that
their purity and stability cannot be maintained for long even if kept airtight;
consequently these ultra-perfect "imitations" are of no commercial value
whatever as jewels, even though they may successfully withstand two or
three tests.

CHAPTER IX.
PHYSICAL PROPERTIES.

G—Heat.

Another method of isolating certain stones is by the action of heat-rays.
Remembering our lessons in physics we recall that just as light-rays may be
refracted, absorbed, or reflected, according to the media through which they
are caused to pass, so do heat-rays possess similar properties. Therefore, if
heat-rays are projected through precious stones, or brought to bear on them
in some other manner than by simple projection, they will be refracted,
absorbed, or reflected by the stones in the same manner as if they were
light-rays, and just as certain stones allow light to pass through their
substance, whilst others are opaque, so do some stones offer no resistance to
the passage of heat-rays, but allow them free movement through the
substance, whilst, in other cases, no passage of heat is possible, the stones
being as opaque to heat as to light. Indeed, the properties of light and heat
are in many ways identical, though the test by heat must in all cases give
place to that by light, which latter is by far of the greater importance in the
judging and isolation of precious stones. It will readily be understood that in
the spectrum the outer or extreme light-rays at each side are more or less
bent or diverted, but those nearest the centre are comparatively straight, so
that, as before remarked, these central rays are taken as being the standard
of light-value. This divergence or refraction is greater in some stones than
in others, and to it the diamond, as an example, owes its chief charm. In just
such manner do certain stones refract, absorb, or reflect heat; thus amber,
gypsum, and the like, are practically opaque to heat-rays, in contrast with
those of the nature of fluorspar, rock-salt, &c., which are receptive. Heat
passes through these as easily as does light through a diamond, such stones
being classed as diathermal (to heat through). So that all diathermal stones
are easily permeable by radiant heat, which passes through them exactly as
does light through transparent bodies.

Others, again, are both single and double refracting to heat-rays, and it is
interesting to note the heat-penetrating value as compared with the
refractive indexes of the stone. In the following table will be found the
refractive indexes of a selection of single and double refractive stones, the
figures for "Light" being taken from a standard list. The second column
shows the refractive power of heat, applied to the actual stones, and
consisting of a fine pencil blowpipe-flame, one line (the one twelfth part of
an inch) in length in each case. This list must be taken as approximate, since
in many instances the test has been made on one stone only, without
possibility of obtaining an average; and as stones vary considerably, the
figures may be raised or lowered slightly, or perhaps even changed in class,
because in some stones the least stain or impurity may cause the heat effects
to be altered greatly in their character, and even to become singly or doubly
refracting, opaque or transparent, to heat-rays, according to the nature of the
impurity or to some slight change in the crystalline structure, and so on.

Selection of Singly refracting stones. Indexes of Rays of
Light. Heat.
Fluorspar 1.436 4.10 varies
Opal 1.479 2.10 "
Spinel 1.726 1.00
Almandine 1.764 1.00
Diamond 2.431 6.11 double

Selection of Doubly refracting stones. Indexes of Rays of
Light. Heat.
Quartz 1.545 4.7 single and double
Beryl 1.575 1.0 varies considerably
Topaz 1.635 4.1 " "
Chrysoberyl 1.765 1.1 " "
Ruby 1.949 5.1 single and double

The tourmaline has a light-refractive index of 1.63, with a heat index of
none, being to heat-rays completely opaque.

The refractive index of gypsum is 1.54, but heat none, being opaque.
The refractive index of amber is 1.51, but heat none, being opaque.
In some of the specimens the gypsum showed a heat-penetration index of
0.001, and amber of 0.056, but mostly not within the third point. In all cases
the heat-penetration and refraction were shown by electric recorders. These
figures are the average of those obtained from tests made in some cases on
several stones of the same kind, and also on isolated specimens. Not only
does the power of the stone to conduct heat vary in different stones of the
same kind or variety, as already explained, but there is seen a remarkable
difference in value, according to the spot on which the heat is applied, so
that on one stone there is often seen a conductivity varying between 0.15 to
4.70.
This is owing to the differences of expansion due to the temporary
disturbance of its crystalline structure, brought about by the applied heat.
This will be evident when heat is applied on the axes of the crystal, on their
faces, angles, lines of symmetry, etc., etc., each one of which gives different
results, not only as to value in conductivity, but a result which varies in a
curious degree, out of all proportion to the heat applied. In many cases a
slight diminution in applied heat gives a greater conductivity, whilst in
others a slight rise in the temperature of the heat destroys its conductivity
altogether, and renders the stone quite opaque to heat-rays.
This anomaly is due entirely to the alteration of crystalline structure, which,
in the one case, is so changed by the diminution in heat as to cause the
crystals to be so placed that they become diathermal, or transparent to heat-
rays; whilst, in the other instance, the crystals which so arrange themselves
as to be diathermal are, by a slightly increased temperature, somewhat
displaced, and reflect, or otherwise oppose the direct passage of heat-rays,
which, at the lower temperature, obtained free passage.
Thus certain stones become both opaque and diathermal, and as the heat is
caused to vary, so do they show the complete gamut between the two
extremes of total opacity and complete transparency to heat-rays.
For the purpose under consideration, the temperature of the pencil of heat
applied to the stones in their several portions was kept constant. It will be

seen, therefore, that no great reliance can be placed on the heat test as
applied to precious stones.

CHAPTER X.
PHYSICAL PROPERTIES.

H—Magnetic and Electric Influences.

The word "electricity" is derived from the Greek "elektron," which was the
name for amber, a mineralised resin of extinct pine-trees. It was well-known
to the people of pre-historic times; later to the early Egyptians, and, at a still
later date, we have recorded how Thales—the Greek philosopher, who lived
about the close of the 7th Century b.c., and was one of the "seven wise
men"—discovered the peculiar property which we call "electricity" by
rubbing dry silk on amber.
Many stones are capable of exhibiting the same phenomenon, not only by
friction, as in Thales's experiment, but also under the influence of light,
heat, magnetism, chemical action, pressure, etc., and of holding or retaining
this induced or added power for a long or short period, according to
conditions and environment.
If a small pith ball is suspended from a non-conducting support, it forms a
simple and ready means of testing the electricity in a stone. According to
whether the ball is repelled or attracted, so is the electricity in the stone
made evident, though the electroscope gives the better results. By either of
these methods it will be found that some of the stones are more capable of
giving and receiving charges of electricity than are others; also that some
are charged throughout with one kind only, either positive or negative,
whilst others have both, becoming polarised electrically, having one portion
of their substance negative, the other positive. For instance, amber, as is
well known, produces negative electricity under the influence of friction,
but in almost all cut stones, other than amber, the electricity produced by
the same means is positive, whereas in the uncut stones the electricity is
negative, with the exception of the diamond, in which the electricity is
positive.

When heated, some stones lose their electricity; others develop it, others
have it reversed, the positive becoming negative and vice versâ; others
again, when heated, become powerfully magnetic and assume strong
polarity. When electricity develops under the influence of heat, or is in any
way connected with a rising or falling of temperature in a body, it is called
"pyro-electricity," from the Greek word "pyros," fire. The phenomenon was
first discovered in the tourmaline, and it is observed, speaking broadly, only
in those minerals which are hemimorphic, that is, where the crystals have
different planes or faces at their two ends, examples of which are seen in
such crystals as those of axinite, boracite, smithsonite, topaz, etc., all of
which are hemimorphic.
Taking the tourmaline as an example of the pyro-electric minerals, we find
that when this is heated to between 50° F. and 300° F. it assumes electric
polarity, becoming electrified positively at one end or pole and negatively at
the opposite pole. If it is suspended on a silken thread from a glass rod or
other non-conducting support in a similar manner to the pith ball, the
tourmaline will be found to have become an excellent magnet. By testing
this continually as it cools there will soon be perceived a point which is of
extreme delicacy of temperature, where the magnetic properties are almost
in abeyance. But as the tourmaline cools yet further, though but a fraction of
a degree, the magnetic properties change; the positive pole becomes the
negative, the negative having changed to the positive.
It is also interesting to note that if the tourmaline is not warmed so high as
to reach a temperature of 50° F., or is heated so strongly as to exceed more
than a few degrees above 300° F., then these magnetic properties do not
appear, as no polarity is present. This polarity, or the presence of positive
and negative electricity in one stone, may be strikingly illustrated in a very
simple manner:—If a little sulphur and red-lead, both in fine powder, are
shaken up together in a paper or similar bag, the moderate friction of
particle against particle electrifies both; one negatively, the other positively.
If, then, a little of this now golden-coloured mixture is gently dusted over
the surface of the tourmaline or other stone possessing electric polarity, a
most interesting change is at once apparent. The red-lead separates itself
from the sulphur and adheres to the negative portion of the stone, whilst the
separated sulphur is at once attracted to the positive end, so that the golden-
coloured mixture becomes slowly transformed into its two separate

components—the brilliant yellow sulphur, and the equally brilliant red-lead.
These particles form in lines and waves around the respective poles in
beautiful symmetry, their positions corresponding with the directions of the
lines of magnetic force, exactly as will iron filings round the two poles of a
magnet.
From this it will clearly be seen how simple a matter it is to isolate the
topaz, tourmaline, and all the pyro-electric stones from the non-pyro-
electric, for science has not as yet been able to give to spurious stones these
same electric properties, however excellent some imitations may be in other
respects. Further, almost all minerals lose their electricity rapidly on
exposure to atmospheric influences, even to dry air; the diamond retains it
somewhat longer than most stones, though the sapphire, topaz, and a few
others retain it almost as long again as the diamond, and these electric
properties are some of the tests which are used in the examination of
precious stones.
Those stones which show electricity on the application of pressure are such
as the fluorspar, calcite, and topaz.
With regard to magnetism, the actual cause of this is not yet known with
certainty. It is, of course, a self-evident fact that the magnetic iron ore,
which is a form of peroxide, commonly known as magnetite, or lodestone,
has the power of attracting a magnet when swinging free, or of being
attracted by a magnet, to account for which many plausible reasons have
been advanced. Perhaps the most reasonable and acceptable of these is that
this material contains molecules which have half their substance positively
and the other half negatively magnetised.
Substances so composed, of which magnets are an example, may be made
the means of magnetising other substances by friction, without they
themselves suffering any loss; but it is not all substances that will respond
to the magnet. For instance, common iron pyrites, FeS2, is unresponsive,
whilst the magnetic pyrites, which varies from 5FeS, Fe2S3, to 6FeS, Fe2S3,
and is a sulphide of iron, is responsive both positively and negatively.
Bismuth and antimony also are inactive, whilst almost all minerals
containing even a small percentage of iron will deflect the magnetic needle,
at least under the influence of heat. So that from the lodestone—the most

powerfully magnetic mineral known—to those minerals possessing no
magnetic action whatever, we have a long, graduated scale, in which many
of the precious stones appear, those containing iron in their composition
being more or less responsive, as already mentioned, and that either in their
normal state, or when heated, and always to an extent depending on the
quantity or percentage of iron they contain.
In this case, also, science has not as yet been able to introduce into an
artificial stone the requisite quantity of iron to bring it the same analytically
as the gem it is supposed to represent, without completely spoiling the
colour. So that the behaviour of a stone in the presence of a magnet, to the
degree to which it should or should not respond, is one of the important
tests of a genuine stone.

CHAPTER XI.
THE CUTTING OF PRECIOUS STONES.

As existing in a state of nature precious stones do not, as a rule, exhibit any
of those beautiful and wonderful properties which cause them to be so
admired and sought after as to become of great intrinsic value, for their
surfaces have become clouded by innumerable fine cuts or abrasions,
because of the thousands of years during which they have been under
pressure, or tumbled about in rivers, or subjected to the incessant friction
caused by surrounding substances. All this occurring above and under
ground has given them an appearance altogether different to that which
follows cutting and polishing. Further, the shape of the stone becomes
altered by the same means, and just as Michael Angelo's figure was already
in the marble, as he facetiously said, and all he had to do was to chip off
what he did not require till he came to it, so is the same process of cutting
and polishing necessary to give to the precious stones their full value, and it
is the manner in which these delicate and difficult operations are performed
that is now under consideration. Just as experience and skill are essential to
the obtaining of a perfect figure from the block of marble, so must the
cutting and polishing of a precious stone call for the greatest dexterity of
which a workman is capable, experience and skill so great as to be found
only in the expert, for in stones of great value even a slight mistake in the
shaping and cutting would probably not only be wasteful of the precious
material, but would utterly spoil its beauty, causing incalculable loss, and
destroying altogether the refrangibility, lustre and colour of the stone, thus
rendering it liable to easy fracture: in every sense converting what would
have been a rare and magnificent jewel to a comparatively valueless
specimen.
One of the chief services rendered by precious stones is that they may be
employed as objects of adornment, therefore, the stone must be cut of such
a shape as will allow of its being set without falling out of its fastening—
not too shallow or thin, to make it unserviceable and liable to fracture, and
in the case of a transparent stone, not too deep for the light to penetrate, or

much colour and beauty will be lost. Again, very few stones are flawless,
and the position in which the flaw or flaws appear will, to a great extent,
regulate the shape of the stones, for there are some positions in which a
slight flaw would be of small detriment, because they would take little or no
reflection, whilst in others, where the reflections go back and forth from
facet to facet throughout the stone, a flaw would be magnified times
without number, and the value of the stone greatly reduced. It is therefore
essential that a flaw should be removed whenever possible, but, when this is
not practicable, the expert will cut the stone into such a shape as will bring
the defect into the least important part of the finished gem, or probably
sacrifice the size and weight of the original stone by cutting it in two or
more pieces of such a shape that the cutting and polishing will obliterate the
defective portions. Such a method was adopted with the great Cullinan
diamond, as described in Chapter IV. From this remarkable diamond a great
number of magnificent stones were obtained, the two chief being the largest
and heaviest at present known. Some idea of the size of the original stone
may be gathered from the fact that the traditional Indian diamond, the
"Great Mogul," is said to have weighed 280 carats. This stone, however, is
lost, and some experts believe that it was divided, part of it forming the
present famous Koh-i-nûr; at any rate, all trace of the Great Mogul ceased
with the looting of Delhi in 1739. The Koh-i-nûr weighs a little over 106
carats; before cutting it weighed a shade over 186; the Cullinan, in the same
state, weighed nearly 3254 carats. This massive diamond was cut into about
200 stones, the largest, now placed in "The Royal Sceptre with the Cross,"
weighing 516-1/2 carats, the second, now placed under the historic ruby in
"The Imperial State Crown," weighing 309-3/16ths carats. These two
diamonds are now called "The Stars of Africa." Both these stones, but
especially the larger, completely overshadow the notorious Koh-i-nûr, and
notwithstanding the flaw which appeared in the original stone, every one of
the resulting pieces, irrespective of weight, is without the slightest blemish
and of the finest colour ever known, for the great South African diamond is
of a quality never even approached by any existing stone, being ideally
perfect.
It requires a somewhat elaborate explanation to make clear the various
styles of cut without illustrations. They are usually divided into two groups,
with curved, and with flat or plane surfaces. Of the first, the curved

surfaces, opaque and translucent stones, such as the moonstone, cat's-eye,
etc., are mostly cut en cabochon, that is, dome-shaped or semi-circular at
the top, flat on the underside, and when the garnet is so cut it is called a
carbuncle. In strongly coloured stones, while the upper surface is semi-
circular like the cabochon, the under surface is more or less deeply concave,
sometimes following the curve of the upper surface, the thickness of the
stone being in that case almost parallel throughout. This is called the
"hollow" cabochon. Other stones are cut so that the upper surface is dome-
shaped like the last two, but the lower is more or less convex, though not so
deep as to make the stone spherical. This is called the "double" cabochon.
A further variety of cutting is known as the goutte de suif, or the "tallow-
drop," which takes the form of a somewhat flattened or long-focus double-
convex lens. The more complicated varieties of cut are those appearing in
the second group, or those with plane surfaces. A very old form is the "rose"
or "rosette"; in this the extreme upper centre, called the "crown," or "star,"
is usually composed of six triangles, the apexes of which are elevated and
joined together, forming one point in the centre. From their bases descend a
further series of triangles, the bases and apexes of which are formed by the
bases and lower angles of the upper series. This lower belt is called the
"teeth," under which the surface or base of the stone is usually flat, but
sometimes partakes of a similar shape to the upper surface, though
somewhat modified in form.
Another variety is called the "table cut," and is used for coloured stones. It
has a flat top or "table" of a square or other shape, the edges of which slope
outwards and form the "bezils" or that extended portion by which the stone
is held in its setting. It will thus be seen that the outside of the stone is of
the same shape as that of the "table," but larger, so that from every portion
of the "table" the surface extends downwards, sloping outwards to the
extreme size of the stone, the underside sloping downwards and inwards to
a small and flat base, the whole, in section, being not unlike the section of a
"pegtop."
A modification of this is known as the "step" cut, sometimes also called the
"trap." Briefly, the difference between this and the last is that whereas the
table has usually one bevel on the upper and lower surfaces, the trap has
one or more steps in the sloping parts, hence its name.

The most common of all, and usually applied only to the diamond, is the
"brilliant" cut. This is somewhat complicated, and requires detailed
description. In section, the shape is substantially that of a pegtop with a flat
"table" top and a small flat base. The widest portion is that on which the
claws, or other form of setting, hold it securely in position. This portion is
called the "girdle," and if we take this as a defining line, that portion which
appears above the setting of this girdle, is called the "crown"; the portion
below the girdle is called the "culasse," or less commonly the "pavilion."
Commencing with the girdle upwards, we have eight "cross facets" in four
pairs, a pair on each side; each pair having their apexes together, meeting on
the four extremities of two lines drawn laterally at right angles through the
stone. It will, therefore, be seen that one side of each triangle coincides with
the girdle, and as their bases do not meet, these spaces are occupied by
eight small triangles, called "skill facets," each of which has, as its base, the
girdle, and the outer of its sides coincides with the base of the adjoining
"cross facet." The two inner sides of each pair of skill facets form the half
of a diamond or lozenge-shaped facet, called a "quoin," of which there are
four. The inner or upper half of each of these four quoins forms the bases of
two triangles, one at each side, making eight in all, which are called "star
facets," and the inner lines of these eight star facets form the boundary of
the top of the stone, called the "table." The inner lines also of the star facets
immediately below the table and those of the cross facets immediately
above the girdle form four "templets," or "bezils." We thus have above the
girdle, thirty-three facets: 8 cross, 8 skill, 4 quoin, 8 star, 1 table, and 4
templets.
Reversing the stone and again commencing at the girdle, we have eight
"skill facets," sometimes called the lower skill facets, the bases of which are
on the girdle, their outer sides forming the bases of eight cross facets, the
apexes of which meet on the extremities of the horizontal line, as in those
above the girdle. If the basal lines of these cross facets, where they join the
sides of the skill facets, are extended to the peak, or narrow end of the
stone, these lines, together with the sides of the cross facets, will form four
five-sided facets, called the "pavilions"; the spaces between these four
pavilions have their ends nearest the girdle formed by the inner sides of the
skill facets, and of these spaces, there will, of course, be four, which also
are five-sided figures, and are called "quoins," so that there are eight five-

sided facets—four large and four narrow—their bases forming a square,
with a small portion of each corner cut away; the bases of the broader
pavilions form the four sides, whilst the bases of the four narrower quoins
cut off the corners of the square, and this flat portion, bounded by the eight
bases, is called the "culet," but more commonly "collet." So that below the
girdle, we find twenty-five facets: 8 cross, 8 skill, 4 pavilion, 4 quoin, and 1
collet.
These, with the 33 of the crown, make 58, which is the usual number of
facets in a brilliant, though this varies with the character, quality, and size of
the diamond. For instance, though this number is considered the best for
normal stones, specially large ones often have more, otherwise there is
danger of their appearing dull, and it requires a vast amount of skill and
experience to decide upon the particular number and size of the facets that
will best display the fire and brilliance of a large stone, for it is obvious that
if, after months of cutting and polishing, it is found that a greater or smaller
number of facets ought to have been allowed, the error cannot be retrieved
without considerable loss, and probable ruin to the stone. In the case of the
Cullinan diamonds, the two largest of which are called the Stars of Africa,
74 facets were cut in the largest portion, while in the next largest the experts
decided to make 66, and, as already pointed out, these stones are, up to the
present time, the most magnificent in fire, beauty and purity ever
discovered.
The positions and angles of the facets, as well as the number, are of
supreme importance, and diamond cutters—even though they have rules
regulating these matters, according to the weight and size of the stone—
must exercise the greatest care and exactitude, for their decision once made
is practically unalterable.

CHAPTER XII.
IMITATIONS, AND SOME OF THE TESTS, OF PRECIOUS
STONES.

We now arrive at the point where it is necessary to discuss the manufacture
and re-formation of precious stones, and also to consider a few of the tests
which may be applied to all stones. These are given here in order to save
needless repetition; the tests which are specially applicable to individual
stones will more properly be found under the description of the stone
referred to, so that the present chapter will be devoted chiefly to
generalities.
With regard to diamonds, the manufacture of these has not as yet been very
successful. As will be seen on reference to Chapter II., on "the Origin of
Precious Stones," it is generally admitted that these beautiful and valuable
minerals are caused by chemically-charged water and occasionally, though
not always, high temperature, but invariably beautified and brought to the
condition in which they are obtained by the action of weight and pressure,
extending unbroken through perhaps ages of time.
In these circumstances, science, though able to give chemical properties and
pressure, cannot, of course, maintain these continuously for "ages,"
therefore the chemist must manufacture the jewels in such manner that he
may soon see the results of his labours, and though real diamonds may be
made, and with comparative ease, from boron in the amorphous or pure
state along with aluminium, fused in a crucible at a high temperature, these
diamonds are but microscopic, nor can a number of them be fused, or in any
other way converted into a large single stone, so that imitation stones, to be
of any service must be made of a good clear glass. The glass for this
purpose is usually composed of 53.70 per cent. of red lead, 38.48 per cent.
of pure quartz in fine powder, preferably water-ground, and 7.82 per cent.
of carbonate of potash, the whole coloured when necessary with metallic
oxides of a similar nature to the constituents of the natural stones imitated.
But for colourless diamonds, the glass requires no such addition to tint it.

From the formula given is made the material known as "strass," or "paste,"
and stones made of it are mostly exhibited under and amongst brilliant
artificial lights. The mere fact that they are sold cheaply is primâ facie proof
that the stones are glass, for it is evident that a diamond, the commercial
value of which might be £50 or more, cannot be purchased for a few
shillings and be genuine. So long as this is understood and the stone is sold
for the few shillings, no harm is done; but to offer it as a genuine stone and
at the price of a genuine stone, would amount to fraud, and be punishable
accordingly. Some of these "paste," or "white stones," as they are called in
the trade, are cut and polished exactly like a diamond, and with such
success as occasionally to deceive all but experts. Such imitations are
costly, though, of course, not approaching the value of the real stones; it
being no uncommon thing for valuable jewels to be duplicated in paste,
whilst the originals are kept in the strong room of a bank or safe-deposit.
In all cases, however, a hard file will abrade the surface of the false stone.
In chapter VII. we found that quartz is in the seventh degree of hardness,
and an ordinary file is but a shade harder than this, so that almost all stones
higher than No. 7 are unaffected by a file unless it is used roughly, so as to
break a sharp edge. In order to prepare artificial diamonds and other stones
for the file and various tests, they are often what is called "converted" into
"doublets" or "triplets." These are made as follows: the body of the glass is
of paste, and on the "table" (see last chapter), and perhaps on the broader
facets, there will be placed a very thin slab of the real stone, attached by
cement. In the case of the diamond, the body is clear, but in the coloured
imitations the paste portion is made somewhat lighter in shade than the real
stone would be, the portion below the girdle being coloured chemically, or
mounted in a coloured backing. Such a stone will, of course, stand most
tests, for the parts usually tested are genuine.
A stone of this nature is called a "doublet," and it is evident that when it is
tested on the underside, it will prove too soft, therefore the "triplet" has
been introduced. This is exactly on the lines of the doublet, except that the
collet and perhaps the pavilions are covered also, so that the girdle, which is
generally encased by the mounting, is the only surface-portion of paste. In
other cases the whole of the crown is genuine, whilst often both the upper
and lower portions are solid and genuine, the saving being effected by using
a paste centre at the girdle, covered by the mounting. Such a stone as this

last mentioned is often difficult to detect without using severe tests and
desperate means, e.g.:—(a) by its crystalline structure (see Chapter III.); (b)
by the cleavage planes (see Chapter IV.); (c) by the polariscope (see
Chapter V.); (d) by the dichroscope (see Chapter VI.); (e) by specific
gravity (see Chapter VIII.); (f) cutting off the mounting, and examining the
girdle; (g) soaking the stone for a minute or so in a mixture said to have
been originally discovered by M. D. Rothschild, and composed of
hydrofluoric acid and ammonia; this will not answer for all stones, but is
safe to use for the diamond and a few others. Should the jewel be glass, it
will be etched, if not completely destroyed, but if genuine, no change will
be apparent; (h) soaking the diamond for a few minutes in warm or cold
water, in alcohol, in chloroform, or in all these in turn, when, if a doublet, or
triplet, it will tumble to pieces where joined together by the cement, which
will have been dissolved. It is, however, seldom necessary to test so far, for
an examination under the microscope, even with low power, is usually
sufficient to detect in the glass the air-bubbles which are almost inseparable
from glass-mixtures, though they do not detract from the physical properties
of the glass. The higher powers of the same instrument will almost always
define the junction and the layer or layers of cement, no matter how delicate
a film may have been used. Any one of these tests is sufficient to isolate a
false stone.
Some of the softer genuine stones may be fused together with splinters,
dust, and cuttings of the same stones, and of this product is formed a larger
stone, which, though manufactured, is essentially perfectly real, possessing
exactly the same properties as a naturally formed stone. Many such stones
are obtained as large as an ordinary pin's head, and are much used
commercially for cluster-work in rings, brooches, for watch-jewels, scarf-
pins, and the like, and are capable of being cut and polished exactly like an
original stone. This is a means of using up to great advantage the lapidary's
dust, and though these products are real stones, perhaps a little more
enriched in colour chemically, they are much cheaper than a natural stone of
the same size and weight.
Some spurious stones have their colour improved by heat, by being tinged
on the outside, by being tinted throughout with a fixed colour and placed in
a clear setting; others, again, have a setting of a different hue, so that the
reflection of this shall give additional colour and fire to the stone. For

instance, glass diamonds are often set with the whole of the portion below
the girdle hidden, this part of the stone being silvered like a mirror. Others
are set open, being held at the girdle only, the portion covered by the setting
being silvered. Other glass imitations, such as the opal, have a tolerably
good representation of the "fiery" opal given to them by the admixture, in
the glass, of a little oxide of tin, which makes it somewhat opalescent, and
in the setting is placed a backing of red, gold, copper, or fiery-coloured
tinsel, whilst the glass itself, at the back, is painted very thinly with a paint
composed of well washed and dried fish-scales, reduced to an impalpable
powder, mixed with a little pure, refined mastic, or other colourless varnish.
This gives a good imitation of phosphorescence, as well as a slight
pearliness, whilst the tinsel, seen through the paint and the curious
milkiness of the glass, gives good "fire."
A knowledge of the colours natural to precious stones and to jewels
generally is of great service in their rough classification for testing, even
though some stones are found in a variety of colours. An alphabetical list of
the most useful is here appended, together with their average specific
gravities and hardness. (See also Chapter VII. on "Hardness," and Chapter
VIII. on "Specific Gravity.")

White or Colourless Stones.

Hardness. Specific Gravity.
(See Chapter VII.) (See Chapter VIII.)
Beryl 7-3/4 2.709-2.81
Corundum 9 3.90-4.16
Diamond 10 3.502-3.564
Jade 7 3.300-3.381
Opal 5-1/2-6-1/2 2.160-2.283
Phenakite 7-3/4 2.965
Quartz 7 2.670
Rock-crystal7 2.521-2.795
Sapphire 9 4.049-4.060
Spinel 8 3.614-3.654
Topaz 8 3.500-3.520
Tourmaline 7-1/4 3.029
Zircon 7-1/2 4.700-4.880

Yellow Stones.

Specific
Hardness.
Gravity.
(See Chapter (See Chapter
VII.) VIII.)
Amber 2-1/2 1.000
Beryl 7-3/4 2.709-2.810
Chrysoberyl 8-1/2 3.689-3.752
Chrysolite 6-7 3.316-3.528
Corundum (the yellow variety
known as "Oriental Topaz" [not "Topaz"], 9 3.90-4.16
see below)
Diamond 10 3.502-3.564
Garnets (various) 6-1/2-7-1/2 3.4-4.5
Hyacinth (a form of Zircon) 7-1/2 4.7-4.88
Quartz (Citrine) 7 2.658
Sapphire 9 4.049-4.060

Spinel 8 3.614-3.654
Topaz (for "Oriental Topaz," see above) 8 3.500-3.520
Tourmaline 7-1/4 3.210

Brown and Flame-Coloured Stones.

Hardness. Specific Gravity.
(See Chapter (See Chapter
VII.) VIII.)
Andalusite 7-1/2 3.204
Diamond 10 3.502-3.564
Garnets (various) 6-1/2-7-1/2 3.40-4.50
Hyacinth (a form of Zircon), see
7-1/2 4.70-4.88
below
Quartz (smoke coloured) 7 2.670
Tourmaline 7-1/4 3.100
Zircon (Hyacinth) 7-1/2 4.70-4.88

Red and Rose-Coloured Stones.

Hardness. Specific Gravity.
(See Chapter VII.) (See Chapter VIII.)
Carnelian (a variety of Chalcedony) 6-1/2 2.598-2.610
Diamond 10 3.502-3.564
Deep Red Garnet 7-1/4 3.40-4.50
Jasper 7 2.668
Opal (the "Fire Opal") 5-1/2-6-1/2 2.21
(average)
Ruby 9 4.073-4.080
Rhodonite 5-1/2-6-1/2 3.413-3.617
Sapphire 9 4.049-4.060
Spinel Ruby 8 3.614-3.654
Topaz 8 3.500-3.520

Tourmaline 7-1/4 3.024
Zircon 7-1/2 4.70-4.88

Pink Stones.

Hardness. Specific Gravity.
(See Chapter VII.) (See Chapter VIII.)
Beryl 7-3/4 2.709-2.810
Diamond 10 3.502-3.564
Ruby 9 4.073-4.080
Spinel 8 3.614-3.654
Topaz ("burnt" or "pinked"),
8 3.500-3.520
see Chapter XIV., page 92
Tourmaline 7-1/4 3.024

Blue Stones.

Hardness. Specific Gravity.
(See Chapter VII.) (See Chapter VIII.)
Beryl 7-3/4 2.709-2.810
Diamond 10 3.502-3.564
Dichorite (Water Sapphire)7-7-1/2 4.049-4.060
Disthene (Kyanite) 5-7 3.609-3.688
Iolite (Cordierite) 7-1/4 2.641
Lapis lazuli 5-1/2 2.461
Sapphire 9 4.049-4.060
Topaz 8 3.500-3.520
Tourmaline 7-1/4 3.160
Turquoise 6 2.800

Green Stones.

Hardness. Specific Gravity.

(See Chapter VII.) (See Chapter VIII.)
Aquamarine 7-3/4 2.701-2.800
Chrysoberyl 8-1/2 3.689-3.752
Chrysolite 6-7 3.316-3.528
Chrysoprase (Quartz) 7 2.670
Diamond 10 3.502-3.564
Dioptase 5 3.289
Emerald and Oriental Emerald 7-3/4 2.690
Euclase 7-1/2 3.090
Garnet (see also Red Garnet) 6-1/2-7-1/2 3.400-4.500
Heliotrope (Chalcedony) 6-1/2 2.598-2.610
Hiddenite (a variety of Spodumene) 6-1/2-7 3.130-3.200
Jade 7 3.300-3.381
Jadeite 7 3.299
Malachite 3-1/2 3.710-3.996
Peridot (a variety of Chrysolite) 6-7 3.316-3.528
Plasma (a variety of Chalcedony) 6-1/2 2.598-2.610
Quartz 7 2.670
Sapphire 9 4.049-4.060
Topaz 8 3.500-3.520
Tourmaline 7-1/4 3.148

Violet Stones.

Hardness. Specific Gravity.
(See Chapter VII.) (See Chapter VIII.)
Amethyst 7 2.661
Diamond 10 3.502-3.564
Quartz (Amethyst) 7 2.670
Sapphire 9 4.049-4.060
Spinel 8 3.614-3.654
Tourmaline 7-1/4 3.160

Chatoyant Stones.

These stones are easily recognisable by their play of colour. (See Chapter
XIV.)

Black Stones.

Hardness. Specific Gravity.
(See Chapter VII.) (See Chapter VIII.)
Diamond 10 3.502-3.564
Garnet 6-1/2-7-1/2 3.400-4.500
Jet 3-1/2 1.348
Onyx (a variety
6-1/2 2.598-2.610
of Chalcedony)
Quartz 7 2.670
Tourmaline (not unlike
7-1/4 3.024-3.300
Black Resin in appearance)

CHAPTER XIII.
VARIOUS PRECIOUS STONES.

The Diamond.

To recapitulate certain of the facts respecting the diamond.—This
wonderful gem has the distinction amongst precious stones of being unique;
though many are composed of two, three, or but a small number of
elements, the diamond is the only stone known consisting of one element,
and absolutely nothing else—pure crystallised carbon. Its hardness is
proverbial; not only is it untouched by the action of a hard file, but it
occasionally refuses to split when struck with finely tempered steel, which
it often causes to break. Such was the case with the South African diamond,
for when the knife that was to break it was struck smartly with a steel bar,
the first blow broke the blade without affecting the diamond, yet a piece of
bort, or diamond dust, splinters, or defective diamonds (all these being
called bort), may readily be pulverised in a hard steel mortar with a hard
steel pestle.
The diamond is the hardest stone known; it is also the only stone known
which is really combustible. It is of true adamantine lustre, classed by
experts as midway between the truly metallic and the purely resinous. In
refractive power and dispersion of the coloured rays of light, called its fire,
it stands pre-eminent. It possesses a considerable variety of colour; that
regarded as the most perfect and rare is the blue-white colour. Most
commonly, however, the colours are clear, with steely-blue casts, pale and
neutral-colour yellow, whilst amongst the most expensive and rare are those
of green, pale pink, red, and any other variety with strong and decided
colour. Although these stones are sold by the carat, there can be no hard and
fast rule laid down as to the value of a carat, for this depends on the size,
quality, and the purity of the stone. The larger the stone the greater the value
per carat, and prices have been known to range from 25l. per carat for a

small stone to 500l. per carat for a large one, whereas the exceptionally
large stones possess a value almost beyond estimation.
It often happens that some stones—particularly those from South Africa and
Brazil—are tinted when uncut, probably by reason of the action upon them
of their matrix, especially if ironstone, or with rolling for ages amongst
ironstone in river-beds, which gives them a slight metallic appearance; in
each case the cause is suggested by the fact that these tinted stones are
usually found in such places, and that the tinting is very thin and on the
surface only, so that the cutting and shaping of the stone gets below it to the
perfectly clear diamond.
From Pliny and other historians we gather that at various periods
considerable superstition has existed with regard to diamonds, such as that
if one is powdered it becomes poisonous to a remarkable degree; that gifts
of diamonds between lovers—married and unmarried—produce and seal
affection; hence the popularity of diamonds in betrothal rings. Pretty as is
this conceit, there is no doubt about the fact that the gift of diamonds to the
object of one's affections does usually produce a feeling of pleasure to both
parties, from which it would appear that there is some ground for the belief.

Corundum.

This mineral is a species of crystal, or crystalline alumina—an almost pure
anhydrous alumina, Al2O3—in many varieties, both of shape and colour.
The chief stone is the ruby, considered, when large, to be of even more
importance and value than the diamond. There are many other red stones in
this group; sapphires, also, are a species of corundum, both the blue and the
colourless varieties, as are also the aquamarine, the emerald, the amethyst,
the topaz, and others, all of widely differing colour, as well as the star-
shaped, or "aster" ruby, called the "ruby" cat's-eye. All these vary more in
colour than in their chemical properties. Still another variety, greyish-black
and generally associated with hæmatite iron ore, is called emery, and, when
ground in different degrees of fineness, is so well known by its general use
as a polishing medium as to need no description. It should, however, be
mentioned that amongst the more coarsely ground emery it is no uncommon
thing to find minute sapphires, taking sapphires in their broad, commercial

meaning, as signifying any variety of corundum, except the red and the
emery. The surfaces of crystals of corundum are often clouded or dull,
whilst its classification of lustre is vitreous. It is double refracting and has
no cleavage. It is found in China, India, Burma, Ceylon, South Africa,
America, and in many other places, having a wide distribution.

The Ruby.

In the dichroscope the ruby shows two images, one square of a violet red,
the second square being a truer and a paler red. It may be subjected to
strong heat, when it changes its colour to a sooty or dirty slate, this varying
with the locality in which the stone is found, and the manner in which the
heat is applied. But as it cools it becomes paler and greener, till it slowly
enrichens; the green first becomes broken, then warmer, redder, and finally
assumes its original beautiful blood red. This method of heating is
sometimes used as a test, but it is a test which often means the complete
ruin of a stone which is not genuine. Another characteristic which, in the
eyes of the expert, invariably isolates a real from an artificial ruby is its
curious mild brilliance, which as yet has not been reproduced by any
scientific method in paste or any other material, but perhaps the safest test
of all is the crystalline structure, which identical structure appears in no
other stone, though it is possible, by heating alumina coloured with oxide of
iron and perhaps also a trace of oxide of chromium to a very high
temperature for a considerable time, and then cooling very slowly, to obtain
a ruby which is nearly the same in its structure as the real gem; its specific
gravity and hardness may perhaps be to standard, and when properly cut, its
brilliance would deceive all but an expert. And as in some real rubies there
are found slight hollows corresponding or analogous to the bubbles found in
melted glass, it becomes a matter of great difficulty to distinguish the real
from the imitation by such tests as hardness, specific gravity, dichroism,
and the like, so that in such a case, short of risking the ruin of the stone,
ordinary persons are unable to apply any convincing tests. Therefore, only
the expert can decide, by his appreciation of the delicate shade of difference
in the light of a true ruby and that of an excellent imitation, and by the
distribution of the colour, which—however experienced the chemist may
be, or with what care the colouring matter may have been incorporated in
the mass—has been found impossible of distribution throughout the body of

an artificial stone so perfectly and in the same manner and direction as
nature herself distributes it in the genuine. This alone, even in the closest
imitations, is clear to the eye of the expert, though not to the untrained eye,
unless the stone is palpably spurious. To one who is accustomed to the
examination of precious stones, however perfect the imitation, it is but
necessary to place it beside or amongst one or more real ones for the false
to be almost instantly identified, and that with certainty.

The Sapphire.

The Sapphire is not so easy to imitate, as its hardness exceeds that of the
ruby, and imitations containing its known constituents, or of glass, are
invariably softer than the natural stone. As before remarked, almost any
form of corundum other than red is, broadly, called sapphire, but giving
them their strictly correct designations, we have the olivine corundum,
called "chrysolite" (oriental), which is harder than the ordinary or "noble"
chrysolite, sometimes called the "peridot." The various yellow varieties of
corundum take the name of the "oriental topaz," which, like most, if not all,
the corundum varieties, is harder than the gem which bears the same name,
minus the prefix "oriental." Then we have the "amethyst" sapphire, which
varies from a red to a blue purple, being richer in colour than the ordinary
amethyst, which is a form of violet-coloured quartz, but the corundum
variety, which, like its companions, is called the "oriental" amethyst, is both
rarer and more precious. A very rare and extremely beautiful green variety
is called the oriental emerald. The oriental jacinth, or hyacinth, is a brown-
red corundum, which is more stable than the ordinary hyacinth, this latter
being a form of zircon; it changes colour on exposure to light, which colour
is not restored by subsequent retention in darkness.
The blue sapphire is of all shades of blue, from cornflower blue to the very
palest tints of this colour, all the gradations from light to dark purple blues,
and, in fact, so many shades of tone and colour that they become almost as
numerous as the stones. These stones are usually found in similar situations
to those which produce the ruby, and often along with them. The lighter
colours are usually called females, or feminine stones, whilst the darker
ones are called masculine stones. Some of these dark ones are so deep as to
be almost black, when they are called "ink" sapphires, and if inclining to

blue, "indigo" sapphires, in contradistinction to which the palest of the
stones are called "water" sapphires. The colouring matter is not always
even, but is often spread over the substance of the stone in scabs or
"splotches," which rather favours imitation, and, where this unevenness
occurs, it may be necessary to cut or divide the stone, or so to arrange the
form of it that the finished stone shall be equally blue throughout.
In some cases, however, the sapphire may owe its beauty to the presence of
two, three or more colours in separate strata appearing in one stone; such as
a portion being a green-blue, another a cornflower blue, another perfectly
colourless, another a pale sky blue, another yellow, each perfectly distinct,
the stone being cut so as to show each colour in its full perfection.
This stone, the sapphire, is hardness No. 9 (see "Hardness" table), and
therefore ranks next to the diamond, which makes it a matter of great
difficulty to obtain an imitation which is of the same specific gravity and of
the same degree of hardness, though this has been done. Such stones are
purchasable, but though sold as imitations at comparatively low price, and
the buyer may consider them just as good as the real gem, to the
experienced eye they are readily detectable.
By heating a sapphire its blue colour slowly fades, to complete transparency
in many cases, or at any rate to so pale a tint as to pass for a transparent
stone. Valuable as is the sapphire, the diamond is more so, and it follows
that if one of these clear or "cleared" sapphires is cut in the "rose" or
"brilliant" form—which forms are reserved almost exclusively for the
diamond—such a stone would pass very well as a diamond, and many so
cut are sold by unscrupulous people as the more valuable stone, which fraud
an expert would, of course, detect.
Sapphires are mentioned by Pliny, and figure largely in the ancient history
of China, Egypt, Rome, etc. The Greeks dedicated the sapphire specially to
Jupiter, and many of the stones were cut to represent the god; it also figured
as one of the chief stones worn by the Jewish High Priest on the breast-
plate. Some stones have curious rays of variegated colour, due to their
crystalline formation, taking the shape of a star; these are called
"asteriated," or "cat's eye" sapphires. Others have curious flashes of light,
technically called a "play" of light (as described in Chapter VI. on

"Colour"), together with a curious blue opalescence; these are the "girasol."
Another interesting variety of this blue sapphire is one known as
"chatoyant"; this has a rapidly changing lustre, which seems to undulate
between a green-yellow and a luminous blue, with a phosphorescent glow,
or fire, something like that seen in the eyes of a cat in the dark, or the
steady, burning glow observed when the cat is fascinating a bird—hence its
name. This is not the same variety as the "asteriated," or "cat's eye" or "lynx
eye" mentioned above.

CHAPTER XIV.
VARIOUS PRECIOUS STONES—continued.

The Chrysoberyl.

There are certain stones and other minerals which, owing to their
possession of numerous microscopically fine cavities, of a globular or
tubular shape, have the appearance of "rays" or "stars," and these are called
"asteriated." Several of such stones have been discussed already in the last
chapter, and in addition to these star-like rays, some of the stones have,
running through their substance, one or more streaks, perhaps of asbestos or
calcite, some being perfectly clear, whilst others are opalescent. When these
streaks pass across the star-like radiations they give the stone the
appearance of an eye, the rays forming the iris, the clear, opalescent, or
black streak closely resembling the slit in a cat's eye, and when these stones
are cut en cabochon, that is, dome-shaped (see Chapter XI. on "Cutting"),
there is nothing to deflect the light beams back and forth from facet to facet,
as in a diamond, so that the light, acting directly on these radiations or
masses of globular cavities and on the streak, causes the former to glow like
living fire, and the streak appears to vibrate, palpitate, expand, and contract,
exactly like the slit in the eye of a cat.
There are a considerable number of superstitions in connection with these
cat's-eye stones, many people regarding them as mascots, or with disfavour,
according to their colour. When possessing the favourite hue or "fire" of the
wearer, such as the fire of the opal for those born in October, of the ruby for
those born in July, etc., these stones are considered to bring nothing but
good luck; to ward off accident, danger, and sudden death; to be a charm
against being bitten by animals, and to be a protection from poison, the
"evil eye," etc. They figured largely, along with other valuable jewels, in the
worship of the ancient Egyptians, and have been found in some of the
tombs in Egypt. They also appeared on the "systrum," which was a sacred
instrument used by the ancient Egyptians in the performance of their

religious rites, particularly in their sacrifices to the goddess Isis. This,
therefore, may be considered one of their sacred stones, whilst there is some
analogy between the cat's-eye stones and the sacred cat of the Egyptians
which recurs so often in their hieroglyphics; it is well known that our
domestic cat is not descended from the wild cat, but from the celebrated cat
of Egypt, where history records its being "domesticated" at least thirteen
centuries B.C. From there it was taken throughout Europe, where it
appeared at least a century B.C., and was kept as a pet in the homes of the
wealthy, though certain writers, speaking of the "mouse-hunters" of the old
Romans and Greeks, state that these creatures were not the Egyptian cat,
but a carniverous, long-bodied animal, after the shape of a weasel, called
"marten," of the species the "beech" or "common" marten (mustela foina),
found also in Britain to-day. It is also interesting to note that the various
superstitions existing with regard to the different varieties and colours of
cats also exist in an identical manner with the corresponding colours of the
minerals known as "cat's eye."
Several varieties of cat's-eye have already been described. Another
important variety is that of the chrysoberyl called "cymophane." This is
composed of glucina, which is glucinum oxide, or beryllia, BeO, of which
there is 19.8 per cent., and alumina, or aluminium oxide, Al2O3, of which
there is 80.2 per cent. It has, therefore, the chemical formula, BeO,Al2O3.
This stone shows positive electricity when rubbed, and, unlike the sapphires
described in the last chapter, which lose their colour when heated, this
variety of chrysoberyl shows no change in colour, and any electricity given
to it, either by friction or heat, is retained for a long time. When heated in
the blowpipe alone it remains unaltered, that is, it is not fusible, and even
with microcosmic salt it requires a considerably long and fierce heat before
it yields and fuses, and acids do not act upon it. It crystallises in the 4th
(rhombic) system, and its lustre is vitreous.
The cymophane shows a number of varieties, quite as many as the
chrysoberyl, of which it is itself a variety, and these go through the gamut
of greens, from a pale white green to the stronger green of asparagus, and
through both the grey and yellow greens to dark. It is found in Ceylon,
Moravia, the Ural Mountains, Brazil, North America, and elsewhere. The
cat's-eye of this is very similar to the quartz cat's-eye, but a comparison will

make the difference so clear that they could never be mistaken, apart from
the fact that the quartz has a specific gravity considerably lower than the
chrysoberyl cat's-eye, which latter is the true cat's-eye, and the one usually
understood when allusion is made to the stone without any distinguishing
prefix, such as the ruby, sapphire, quartz, etc., cat's eye. It should, however,
be mentioned that this stone is referred to when the names Ceylonese and
Oriental cat's-eye are given, which names are used in the trade as well as
the simple appellation, "cat's eye." One peculiarity of some of these stones
is that the "fire" or "glow" is usually altered in colour by the colour of the
light under which it is seen, the change of colour being generally the
complementary. Thus, a stone which in one light shows red, in another will
be green; the "eye" showing blue in one light will become orange in
another; whilst the yellow of another stone may show a decided purple or
amethyst in a different light.
A good test for this, and indeed most precious stones, is that they conduct
heat more quickly than does glass, and with such rapidity that on breathing
upon a stone the warmth is conducted instantly, so that, though the stone is
dimmed the dimness vanishes at once, whereas with glass the film of
moisture fades but slowly in comparison.

The Topaz.

The name topaz is derived from the Greek topazos, which is the name of a
small island situated in the Gulf of Arabia, from whence the Romans
obtained a mineral which they called topazos and topazion, which mineral
to-day is termed chrysolite. The mineral topaz is found in Cornwall and in
the British Isles generally; also in Siberia, India, South America and many
other localities, some of the finest stones coming from Saxony, Bohemia,
and Brazil, especially the last-named. The cleavage is perfect and parallel to
the basal plane. It crystallises in the 4th (rhombic) system; in lustre it is
vitreous; it is transparent, or ranging from that to translucent; the streak is
white or colourless. Its colour varies very much—some stones are straw-
colour, some are grey, white, blue, green, and orange. A very favourite
colour is the pink, but in most cases this colour is not natural to the stone,
but is the result of "burning," or "pinking" as the process is called
technically, which process is to raise the temperature of a yellow stone till

the yellow tint turns to a pink of the colour desired. The topaz is harder than
quartz, as will be seen on reference to the "Hardness" table, and is
composed of a silicate of aluminium, fluorine taking the place of some of
the oxygen. Its composition averages 16.25 per cent. of silica, 55.75 per
cent. of alumina, or oxide of aluminium, and fluoride of silicium, 28 per
cent. Its formula is [Al(F,OH)]2 SiO4, or (AlF)2SiO4. From this it will be
understood that the fluorine will be evolved when the stone is fused. It is,
however, very difficult to fuse, and alone it is infusible under the blowpipe,
but with microcosmic salt it fuses and evolves fluorine, and the glass of the
tube in the open end of which the stone is fixed is bitten with the gas.
Such experiments with the topaz are highly interesting, and if we take a
little of the powdered stone and mix with it a small portion of the
microcosmic salt, we may apply the usual test for analysing and proving
aluminium, thus: a strongly brilliant mass is seen when hot, and if we
moisten the powder with nitrate of cobalt and heat again, this time in the
inner flame, the mass becomes blue. Other phenomena are seen during the
influence of heat. Some stones, as stated, become pink on heating, but if the
heating is continued too long, or too strongly, the stone is decoloured.
Others, again, suffer no change, and this has led to a slight difference of
opinion amongst chemists as to whether the colour is due to inorganic or
organic matter. Heating also produces electricity, and the stone, and even
splinters of it, will give out a curious phosphorescent light, which is
sometimes yellow, sometimes blue, or green. Friction or pressure produces
strong electrification; thus the stones may be electrified by shaking a few
together in a bag, or by the tumbling of the powdered stone-grains over
each other as they roll down a short inclined plane. The stones are usually
found in the primitive rocks, varying somewhat in different localities in
their colour; many of the Brazilian stones, when cut as diamonds, are not
unlike them.
In testing, besides those qualities already enumerated, the crystalline
structure is specially perfect and unmistakable. It is doubly refractive,
whereas spinel and the diamond, which two it closely resembles, are singly
refractive. Topaz is readily electrified, and, if perfect at terminals, becomes
polarised; also the commercial solution of violets, of which a drop only
need be taken for test, is turned green by adding to it a few grains of topaz
dust, or of a little splinter crushed to fine powder.

The Beryl.

The beryl is a compound of silicates of beryllia and alumina, with the
formula 3BeOSiO2 + Al2O3,3SiO2, or 3BeO,Al2O3,6SiO2. It differs very
little indeed from the emerald, with the exception of its colour. In the
ordinary varieties this is somewhat poor, being mostly blue, or a dirty or a
greenish yellow; the better kinds, however, possess magnificent colour and
variety, such as in the aquamarine, emerald, etc. The cleavage is parallel to
the basal plane. Its lustre is sometimes resinous, sometimes vitreous, and it
crystallises in the 2nd (hexagonal) system. It occurs in somewhat long,
hexagonal prisms, with smooth, truncated planes, and is often found in
granite and the silt brought down by rivers from granite, gneiss, and similar
rocks. It is found in Great Britain and in many parts of Europe, Asia, and
America, in crystals of all sizes, from small to the weight of several tons.
The common kinds are too opaque and colourless to be used as gems and
are somewhat difficult of fusion under the blowpipe, on the application of
which heat some stones lose their colour altogether, others partly; others,
which before heating were somewhat transparent, become clouded and
opaque; others suffer no change in colour, whilst some are improved. In
almost every case a slight fusion is seen on the sharp edges of fractures,
which become smooth, lose their sharpness, and have the appearance of
partly fused glass. The hardness varies from 7-1/4 to 8, the crystals being
very brittle, breaking with a fracture of great unevenness. The better
varieties are transparent, varying from that to translucent, and are called the
"noble" beryls. Transparent beryl crystals are used by fortune-tellers as
"gazing stones," in which they claim to see visions of future events.

The Emerald.

Considering the particular emerald which is a variety of beryl—although
the name emerald in the trade is applied somewhat loosely to any stone
which is of the same colour, or approaching the colour of the beryl variety
—this emerald only differs chemically from the beryl, just described, in
possessing an addition of oxide of chromium. In shape, crystallisation,
fracture and hardness, it is the same, and often contains, in addition to the
chromium, the further addition of traces of carbonate of lime, magnesia,

and occasionally faint traces of hornblende and mica, which evidently result
from its intimate association with the granite rock and gneiss, amongst
which it is mostly found, the latter rocks being of a slaty nature, in layers or
plates, and, like granite, containing mica, pyrites, felspar, quartz, etc.
Emeralds have been known from very early times, and are supposed to have
been found first in the mines of ancient Egypt. They were considered
amongst the rarest and the most costly of gems, and it was the custom,
when conferring lavish honour, to engrave or model emeralds for
presentation purposes. Thus we find Pliny describes Ptolemy giving
Lucullus, on his landing at Alexandria, an emerald on which was engraved
his portrait. Pliny also relates how the short-sighted Nero watched the fights
of gladiators through an eye-glass made of an emerald, and in ancient times,
in Rome, Greece, and Egypt, eye-glasses made of emeralds were much
valued. Many of these, as well as engraved and carved emeralds, have been
discovered in ruins and tombs of those periods.
The copper emerald is rare; it is a hydrous form of copper silicate, CuOSiO2
+ H2O, of a beautiful emerald green, varying from transparent to
translucent. It exhibits double refraction, and is a crystallised mineral,
brittle, and showing a green streak. This is less hard than the real emerald,
is heavier, deeper in colour, and is usually found in crystals, in cavities of a
particular kind of limestone which exists at Altyn-Tübe, a hill in the Altai
Mountains, in the Urals, and in North and Central America.

The Tourmaline.

The tourmaline is a most complex substance; almost every stone obtained
has a different composition, some varying but slightly, with mere traces of
certain constituents which other stones possess in a perceptible degree.
Consequently, it is not possible to give the chemical formula, which might,
and possibly would, be found but seldom, even in analyses of many
specimens. It will therefore be sufficient to state the average composition,
which is:—ferrous oxide, manganous oxide, potash, lime, boracic acid,
magnesia, soda, lithia, and water. These form, roughly speaking, 25 per
cent. of the bulk, the remainder being oxide of silicon and oxide of

aluminium in about equal parts. It crystallises in the 2nd (hexagonal)
system, with difficult cleavage and vitreous lustre.
It will naturally be expected that a substance of such complexity and variety
of composition must necessarily have a corresponding variety of colour;
thus we find in this, as in the corundum, a wonderful range of tints. The
common is the black, which is not used as a gem. Next come the colourless
specimens, which are not often cut and polished, whereas all the transparent
and coloured varieties are in great demand. To describe adequately their
characteristics with relation to light would alone require the space of a
complete volume, and the reader is referred to the many excellent works on
physics (optics) which are obtainable. This stone is doubly refracting,
exhibiting extremely strong dichroism, especially in the blue and the green
varieties. It polarises light, and when viewed with the dichroscope shows a
remarkable variety of twin colours. It will be remembered that in Hogarth's
"Rake's Progress," the youth is too engrossed in the changing wonders of a
tourmaline to notice the entrance of the officers come to arrest him.

CHAPTER XV.
VARIOUS PRECIOUS STONES—continued.

Zircon.

Zircon appears to have been first discovered by Klaproth in 1789, in the
form of an earth, and six years later he found that the stone hyacinth
contained a similar substance, both having the formula, ZrSiO4, and both
having as their colouring agent ferric oxide. There are several methods of
obtaining the metallic element, zirconium; it is however with the silicate of
zirconium that we have to deal at the moment. This is called zircon, ZrSiO4,
or hyacinth when transparent or red, but when smoke-coloured, or
colourless, it is the jargoon, or jarcon, and is found in silt and alluvial soils,
limestone, gneiss, and various forms of schist, in India, Australia, the Urals,
and certain parts of America. It is often combined with and found in
juxtaposition to gold and certain varieties of precious stones. The lines of
cleavage are parallel to the sides of the prism, and the crystals have an
adamantine, or diamond lustre, varying from the completely opaque to the
transparent. In some varieties the oxide of uranium is also present in traces.
It crystallises in the 3rd (tetragonal) system, with indistinct cleavage. Its
specific gravity varies from 4.70 to 4.88, according to the specimen and the
locality.
This stone, like some of the others described, has a very wide range of
colour, going through reds, browns, greens, yellows, oranges, whites, greys,
blues from light to indigo, notwithstanding which it is somewhat difficult to
imitate scientifically, though its composition of 33 per cent. of silica with
67 per cent. of zirconia (the oxide of zirconium), is practically all it
contains, apart from the colouring matter, such as the metallic oxides of
iron, uranium, etc. Its hardness is 7-1/2, consequently it is untouched by a
file, and so far, if one or perhaps two of the three qualities of colour,
hardness, and specific gravity, are obtained in a chemically made zircon, the
third is wanting. Under the blowpipe, zircons are infusible, but the coloured

stones when heated strongly become heavier, and as they are contracting,
their colour fades, sometimes entirely, which changes are permanent, so that
as they possess the adamantine lustre, they are occasionally cut like a
diamond, and used as such, though their deficiency in fire and hardness, and
their high specific gravity, make them readily distinguishable from the
diamond.
On exposure to light the coloured zircon becomes more or less decoloured;
especially is this so in sunlight, for when the direct rays of the sun fall upon
it, the colours fade, and for a moment or two occasional phosphorescence
follows, as is the case when the stone is warmed or heated in a dark room.
The stone appears to be very susceptible to brilliant light-rays, and in
certain specimens which were split for testing, one half of each being kept
excluded from light for purposes of comparison, it was found that sunshine
affected them most; then brilliant acetylene gas, which was more effective
still when tinted yellow by being passed through yellow glass. The electric
arc was not so effective, but the electric light of the mercury-vapour lamp,
though causing little change at the first, after a few hours' exposure rapidly
bleached certain of the colours, whilst having no effect on others. Coal gas
with incandescent fibre mantle was slightly effective, whilst the coal-gas,
burned direct through an ordinary burner, affected very few of the colours,
even after twenty-four hours' exposure at a distance of three feet. In all
these cases, though the colours were slightly improved by the stones being
kept for a time in the dark, they failed to recover their original strength,
showing permanent loss of colour.

The Silicates.

The chief of these are the garnets, crystallising in the cubic system, and
anhydrous. The garnet is usually in the form of a rhombic dodecahedron, or
as a trisoctahedron (called also sometimes an icosatetrahedron), or a
mixture of the two, though the stones appear in other cubic forms. In
hardness they vary from 6-1/2 to 8-1/2. They average from 40 to about 42
per cent. of silica, the other ingredients being in fairly constant and definite
proportions. They are vitreous and resinous in their lustre and of great
variety of colour, chiefly amongst reds, purples, violets, greens, yellows and
blacks, according to the colouring matter present in their mass. There are

many varieties which are named in accordance with one or more of their
constituents, the best known being: (A) The iron-alumina garnet, having the
formula 6FeO, 3SiO2 + 2Al2O3, 3SiO2. This is the "precious" garnet, or
almandine, sometimes called the "Oriental" garnet; these stones are found
in Great Britain, India, and South America, and are deep red and
transparent, of vitreous lustre. They get up well, but certain varieties are so
subject to defects in their substance, brought about by pressure, volcanic
action, and other causes, some of which are not yet known, that their quality
often becomes much depreciated in consequence. This inferior variety of
the iron-alumina garnet is called the "common" garnet, and has little lustre,
being sometimes opaque. The perfect qualities, or almandine, as described
above, are favourite stones with jewellers, who mount great quantities of
them.
The second variety is the (B) lime-iron garnet, formula, 6CaO,3SiO2 +
2Fe2O3,3SiO2. The chief of this class is the melanite, sometimes dull, yet
often vitreous; it is mostly found in volcanic rocks, such as tuff; this variety
is very popular with jewellers for mourning ornaments, for as it is a
beautiful velvet-black in colour and quite opaque, it is pre-eminent for this
purpose, being considerably less brittle than jet, though heavier. Another
variety is the "topazolite," both yellow and green. The "aplome" is greenish-
yellow, yellowish-green, brown, and usually opaque. A further form of
lime-iron garnet is the "pyreneite," first found in the Pyrenees Mountains,
hence its name.
The (C) lime-chrome garnets—6CaO,3SiO2 + 2Cr2O3, 3SiO2—the chief of
which is "uwarowite." This is of a magnificent emerald green colour,
translucent at edges and of a vitreous lustre. When heated on the borax bead
it gives an equally beautiful green, which is, however, rather more inclined
to chrome than emerald. This is an extremely rare stone in fine colour,
though cloudy and imperfect specimens are often met with, but seldom are
large stones found without flaws and of the pure colour, which rivals that of
the emerald in beauty.
The fourth variety (D) is the lime-alumina garnet, its formula being—
6CaO,3SiO2 + 2Al2O3,3SiO2. Like the others, it has a number of sub-
varieties, the chief being the "cinnamon stone," which is one of great beauty

and value when perfect. This stone is almost always transparent when pure,
which property is usually taken as one of the tests of its value, for the
slightest admixture or presence of other substances cloud it, probably to
opacity, in accordance with the quantity of impurity existent. This variety is
composed of the oxides of aluminium and silicon with lime. In colour it
ranges from a beautiful yellowish-orange deepening towards the red to a
pure and beautiful red.
"Romanzovite" is another beautiful variety, the colour of which ranges
through browns to black. Another important variety is the "succinite,"
which gets up well and is a favourite with jewellers because of its beautiful,
amber-like colour, without possessing any of the drawbacks of amber.
(E) The magnesia-alumina garnet—6MgO,3SiO2 + 2Al2O3,3SiO2—is
somewhat rare, the most frequently found being of a strong crimson colour
and transparent. This variety is called "pyrope," the deeper and richer tints
being designated "carbuncle," from the Latin carbunculus, a little coal,
because when this beautiful variety of the "noble" garnet is held up between
the eyes and the sun, it is no longer a deep, blood-red, but has exactly the
appearance of a small piece of live or glowing coal, the scarlet portion of its
colour-mixture being particularly evident. The ancient Greeks called it
anthrax, which name is sometimes used in medicine to-day with reference
to the severe boil-like inflammation which, from its burning and redness, is
called a carbuncle, though it is more usual to apply the word "anthrax" to
the malignant cattle-disease which is occasionally passed on to man by
means of wool, hair, blood-clots, etc., etc., and almost always ends fatally.
A great deal of mystery and superstition has always existed in connexion
with this stone—the invisibility of the bearer of the egg-carbuncle laid by a
goldfinch, for instance.
(F) The manganese-alumina garnet—6MnO,3SiO2 + 2Al{2}O3,3SiO2—is
usually found in a crystalline or granular form, and mostly in granite and in
the interstices of the plates, or laminæ, of rocks called schist. One variety of
this, which is a deep hyacinth in colour, though often of a brown-tinted red,
is called "spessartine," or "spessartite," from the district in which it is
chiefly found, though its distribution is a fairly wide one.

The Lapis-Lazuli.

The lapis-lazuli, sometimes called "azure stone," is almost always blue,
though often containing streaks of white and gold colour, the latter of which
are due to the presence of minute specks or veins of iron pyrites, the former
and colourless streaks being due to free lime, calcite, and other substances
which have become more or less blended with the blue colour of the stone.
It has a vitreous lustre, crystallises in the 1st, or cubic system, and is a
complex substance, varying considerably in its ingredients in accordance
with the locality in which it is found, its matrix, and the general geological
formation of the surrounding substances, which may, by the penetration of
moisture, be brought to bear upon the stone, thus influencing to a great
extent its chemical composition. So that we find the stone composed of
about a quarter of its substance of alumina, or oxide of aluminium, silica to
the extent of almost half, the remainder being lime, soda, sulphur, and
occasionally traces of copper and iron. It is mostly found in granite and
certain crystalline limestone rocks, in fairly large masses. It is of great
antiquity, figuring extensively in ancient Egyptian history, both in its form
as a stone and ground up into a pigment for the decoration of sacred and
royal vessels and appointments. When so ground, it forms the stable and
magnificent colour, genuine ultramarine, which is the finest and purest blue
on the artist's palette, but owing to its extremely high price its use is not in
very great demand, especially as many excellent chemical substitutes of
equal permanence are obtainable at little cost.

The Turquoise.

The turquoise is a pseudomorph (see Chapter IV., "Cleavage.") In colour it
is blue or greenish-blue, sometimes opaque, varying between that and
feeble translucency, though it should be said that in all forms, even those
considered opaque, a thin cutting of the stone appears almost transparent, so
that the usual classing of it among the opaque stones must be done with this
reservation. In composition it contains about 20 per cent. of water, about a
third of its substance being phosphoric acid, or phosphorus-pentoxide;
sometimes nearly half of it is alumina, with small quantities of iron in the
form of variously coloured oxides, with oxide of manganese. The great
proportion of water, which it seems to take up during formation, is mostly
obtained in the cavities of weathered and moisture-decomposing rocks. Its
average formula may be said to be Al2O3P2O5 + 5H2O, and sometimes

Al2O3 FeOP2O5 + 5H2O. It must therefore follow that when the stone is
heated, this water will separate and be given off in steam, which is found to
be the case. The water comes off rapidly, the colour of the stone altering
meanwhile from its blue or blue-green to brown. If the heat is continued
sufficiently long, this brown will deepen to black, while the flame is turned
green. This is one of the tests for turquoise, but as the stone is destroyed in
the process, the experiment should be made on a splinter from it.
This stone is of very ancient origin, and many old turquoise deposits, now
empty, have been discovered in various places. History records a
magnificent turquoise being offered in Russia for about £800 a few
centuries ago, which is a very high price for these comparatively common
stones.
Owing to the presence of phosphorus in bones, it is not uncommon to find,
in certain caves which have been the resort of wild animals, or into which
animals have fallen, that bones in time become subjected to the oozing and
moisture of their surroundings; alumina, as well as the oxides of copper,
manganese and iron, are often washed across and over these bones lying on
the cave floor, so that in time, this silt acts on the substance of the bones,
forming a variety of turquoise of exactly the same composition as that just
described, and of the same colour. So that around the bones there eventually
appears a beautiful turquoise casing; the bone centre is also coloured like its
casing, though not entirely losing its bony characteristics, so that it really
forms a kind of ossified turquoise, surrounded by real turquoise, and this is
called the "bone turquoise" or "odontolite."

INDEX
Adamantine lustre, 28
glimmering, 29
glinting, or glistening, 29
lustreless, 29
shining, 29
splendent, 29

Agate, 11

Almandine, 101

Amethyst, 11
oriental, 85
sapphire, 85

Amorphous stones and their characteristics, 23

Analysis, 5

Aplome, 101

Asters, or asteriated stones, 82, 87-91

Azure-stone, 103

Beryl, 10, 94
colours of, in dichroscope, 34

Beryllium, 10

Bezils, 66

Black stones, list of, 79

Blue sapphire, composition of the, 10
stones, list of, 77

Bone-turquoise, 106

Break, as opposed to cleavage, 19

Brilliant-cut stones, 66

Brown stones, list of, 76

Building up of crystals, 13

Burnt, or pinked topaz, 92

Cabochon-cut stones, 64
(the double), 65
(the hollow), 65

Carbonate series, 11

Carbuncle, 102, 103

Cat of Egypt, 89

Cat's eye stones, 82, 87-91
list of (see "Chatoyant Stones"), 78

Ceylonese cat's eye (see "Cat's eye")

Change of colour (not to be confused with "Play of colour" and
"Opalescence," which see; see also "Fire"), 36

Characteristics of precious stones, 1, 3

Chatoyant stones, list of, 78

Chemical illustration of formation of precious stones, 8

Chloride of palladium in dichroscope, 34

Chrysoberyl, 88

Chrysolite, 11
ordinary, or "noble", 85
oriental, 85

Cinnamon stone, 102

Claims of precious stones, 4

Cleavage affecting tests, 43
and "cleavage" as opposed to "break", 19, 22

Colour, 26, 28, 30, 32

Colourless stones, list of, 75

Colours and characteristics of the various opals, 35, 36
of precious stones, list of, 75-79

Common garnet, 101
opal, 35

Composite crystals, 13

Composition of paste, or strass, for imitation stones, 71

Composition of precious stones, 7

Converted stones, 72

Corundum, 82

Crown portion of stones, 65, 66

Crystalline structure, physical properties, of 13

Crystallography, 14

Crystals, axes of symmetry, 15
groups of, 15, 16
planes of symmetry, 15
systems of, 16
(1) Cubic—isometric, monometric, regular, 16
(2) Hexagonal—rhombohedral, 16
(3) Tetragonal—quadratic, square prismatic, dimetric, pyramidal, 16
(4) Rhombic—orthorhombic, prismatic, trimetric, 16
(5) Monoclinic—clinorhombic, monosymmetric, oblique, 16, 17
(6) Triclinic—anorthic, asymmetric, 16, 17
treatment of, 14

Culasse portion of stones, 66

Cullinan diamond (see also "Stars of Africa"), 22, 64, 68, 80

Cutting of precious stones, 3, 4, 62

Cymophane, 90

Definition of a precious stone, 1

Diamond, characteristics of the, 80
composition of the, 10
(sapphire), 86
unique, 10

(zircon), 99

Diaphaneity, 26, 28

Diaphanous stones, 28

Dichroscope, 33
how to make a, 33
how to use a, 34

Dimorphism in precious stones, 25

Double cabochon-cut stones, 65
refraction (see "Refraction")

Doublets, 72

Electric and magnetic influences, 57
experiments with precious stones and pithball and electroscope, 57
experiments with tourmaline, 58, 59

Emerald, 10, 11, 95, 96
oriental, 85

En cabochon-cut stones, 64

Experiments to show electric polarity, 58, 59

Facets in stones, description of the, 67, 68

Feminine stones, 85

Fire in stones (see also "Change of Colour," "Opalescence," and "Play of
Colour"), 36, 37

Fire opal, 35

Flame-coloured stones, list of, 76

Flaws, 63

Formation of precious stones, 5, 8
chemical illustration of, 8, 9

Garnet, 11, 100

Garnets
(A) iron-alumina (called also almandine and precious or oriental garnet),
101
sub-variety, common garnet, 101
(B) lime-iron, 101
sub-variety aplome, 101
melanite, 101
pyreneite, 101
topazolite, 101
(C) lime-chrome, 101, 102
sub-variety uwarowite, 101, 102
(D) lime-alumina, 102
sub-variety cinnamon stone, 102
romanzovite, 102
succinite, 102
(E) magnesia-alumina, 102, 103
sub-variety carbuncle, or anthrax, 102, 103
noble, 103
pyrope, 102
(F) manganese-alumina, 103
sub-variety spessartine, or spessartite, 103

Girdle portion of a stone, 66

Glimmering, in lustre, definition of, 29

Glinting, or glistening in lustre, definition of, 29

Goutte de suif-cut stones, 65

Great Mogul diamond, 64

Green stones, list of, 78

Groups of crystals (see "Crystals")

Hardness, physical properties of, 39
table of, 39, 40, 41

Heat indexes, 54
physical properties of, 52

Hollow-cabochon, 65

Hyacinth, ordinary (a form of zircon), 85, 98
oriental, 85

Hyalite (opal), 35

Hydrophane (opal), 35

Imitations and tests of precious stones, 70

Indigo sapphires, 86

Ink sapphires, 85

Iridescence, and cause of, 37, 38

Iron-alumina garnets, 101

Jacinth, oriental, 85

Jarcon, or jargoon, 98

Koh-i-nûr, 64

Lapis-lazuli, 103

Light, physical properties of, 26

Lime-alumina garnets, 102
cinnamon stone, 102
romanzovite, 102
succinite, 102

Lime-chrome garnets, 101, 102
uwarowite, 101, 102

Lime-iron garnets, 101
aplome, 101
pyreneite, 101
topazolite, 101

List of stones according to colour, 75-79
hardness, 39-41
specific gravity, 48-50

Lustre, 26, 28

Lustreless, definition of, 29

Lynx-eye stones, 87

Magnesia-alumina garnets, 102, 103
carbuncle, or anthrax, 102
noble, 103
pyrope, 102

Magnetic and electric influences, 57-61

Malachite, 11

Manganese-alumina garnets, 103
spessartine, or spessartite, 103

Masculine stones, 85

Melanite, 101

Menilite (opal), 36

Metallic-lustre stones, 28, 29

Mohs's table of hardness, 39-41

Noble garnet, 103
or precious opal, 35

Non-diaphanous stones, 28

Odontolite, 106

Olivine corundum (see "Chrysolite"), 85

Opal, 11
varieties of, 35, 36

Opalescence (not to be confused with "Change of Colour" and "Play of
Colour," which see; see also "Fire"), 36, 37

Oriental amethyst, 85
cat's eye (see "Cat's eye")
emerald, 85
garnet, 101
topaz, 85

Origin of precious stones, 7

Paste, or strass, for imitation stones, composition of, 71

Pavilion portion of cut stones, 66

Pearly-lustre stones, 28, 29

Peridot (see "Noble Chrysolite"), 85

Pink-coloured stones, list of (see also Red), 77

Pinked topaz, 92

Phosphorescence, 26, 30

Physical properties:—
A.—Crystalline structure, 13
B.—Cleavage, 19
C.—Light, 26
D.—Colour, 32
E.—Hardness, 39
F.—Specific gravity, 45
G.—Heat, 52
H.—Magnetic and electric influences, 57

Play of colour (not to be confused with "Change of Colour" and

"Opalescence," which see; see also "Fire"), 36, 37

Pleochroism, 33

Polarisation, electric, 58, 59
of light, 26, 27

Polariscope, 27, 28

Polishing precious stones, 3, 4

Polymorphism in precious stones, 25

Precious, or noble opal, 35

Pseudomorphism in precious stones, 23, 24

Pyreneite, 101

Pyro-electricity, development and behaviour of, 58-60

Pyrope, 102

Qualities of precious stones, 1, 3

Red and rose-coloured stones, list of (see also Pink), 76, 77

Reflection of light, 26, 28

Refraction of heat, 52-55
light, 26, 27

Reproduction of crystalline form, 20, 21

Resinous lustre stones, 28, 29

Rock-crystal, 11

Romanzovite, 102

Rose-coloured stones (see Red, above), 76, 77

Rose, or rosette-cut stones, 65

Rothschild's testing solution, 73

Ruby, characteristics of, 83
composition of, 10

Sapphire, amethyst, 85
and its varieties, 84, 85
cleared, 86
diamonds, 87
indigo, 86
ink, 85
the blue, composition of, 10, 85
water, 86

Semi-diaphanous stones, 28

Shining, in lustre, definition of, 29

Silica group, composition of the, 11

Silicates, 100

Silky-lustre stones, 28, 29

Single-refraction (see "Refraction")

South African diamond (see "Cullinan Diamond")

Specific gravity, 45

Splendent, in lustre, definition of, 29

Splitting of the Cullinan diamond, 22

Star-portion of stones, 65

Stars of Africa (see also "Cullinan Diamond"), 22, 64, 68

Starting or splitting of stones on cleavage planes, 23

Step-cut stones, 66

Stones arranged according to colour, 75-79
hardness, 39-41
specific gravity, 48-50

Strass for imitation stones, composition of, 71

Sub-metallic in lustre, definition of, 29

Sub-translucent stones, 28

Sub-transparent stones, 28

Succinite, 102

Synthesis, 5

Systems of crystals (see "Crystals")

Table-cut stones, 65

Tallow drops, 65

Teeth of stone, 65

Testing by crystalline structure, 17
hardness, 40, 43
with needles, 41
gems by dichroscope, 33, 34
solution (Rothschild's), 73

Tests of precious stones (general), 70

Topaz, 11, 91
colours of, in dichroscope, 34
oriental, 85

Topazolite, 101

Tourmaline, 96, 97
electric experiments with, 58, 59

Translucent stones, 28

Transmission of heat, 52-56
light, 26

Transparent stones, 28

Trap-cut stones, 66

Tri-morphism in precious stones, 25

Triplets, 72

Turquoise, 104
(bone), 106
composition of the, 11
odontolite, 106

Uwarowite, 101, 102

Violet stones, list of, 78

Vitreous-lustre stones, 28, 29

Water-sapphires, 86

White (paste) stones, 71
stones, list of, 75

Yellow stones, list of, 76
topaz, 92

Zircon, 10, 98
diamonds, 99

Zirconium, 10

LONDON: PRINTED BY WILLIAM CLOWES AND SONS, LIMITED,
GREAT WINDMILL STREET, W., AND DUKE STREET, STAMFORD
STREET, S. E.

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