Gem-Stones and Their Distinctive CharactersSmith, George Frederick Herbert
Science
Gem-Stones and Their Distinctive Characters
Smith, George Frederick Herbert
Precious stones
Serpentine has been largely used for decorative purposes, as well
as for cameos and intaglios, and formed most of the famous ‘verde
antique.’ Being the result of the decomposition of other silicates
it varies enormously in appearance and characters, but the most
attractive stones are a rich oil-green in colour and resemble jade. The
composition approximates to the formula H_{4}Mg_{3}Si_{2}O_{9}, but it
invariably contains other elements. The hardness varies from 2½ to 4
on Mohs’s scale, according to the minerals contained in the stone; the
specific gravity is about 2·60 and the refractivity 1·570.
The beautiful rose-red stone, thulite, makes a handsome decorative
stone. It has nearly the same composition as epidote (p. 275), and like
it has strong dichroism, the principal colours being yellow, light
rose, and deep rose. The colour is due to manganese. Its refractive
index is about 1·70, specific gravity 3·12, and hardness 6 to 6½ on
Mohs’s scale; it possesses an easy cleavage. Fine specimens come from
Telemark, Norway, and it is therefore called after the old name for
Norway, Thule.
Marble is a massive calcite, carbonate of lime, with the formula
CaCO_{3}. When pure it is white, but it is usually streaked with other
substances which impart a pleasing variety to its appearance. It is
always readily recognized by the immediate effervescence set up when
touched with a drop of acid. Calcite is highly doubly refractive (cf.
p. 40), the extraordinary index being 1·486, and ordinary 1·658, a
difference of 0·172; the specific gravity is 2·71, and hardness 3 on
Mohs’s scale. Lumachelle, or fire-marble, is a limestone containing
shells from which a brilliant, fire-like chatoyancy is emitted
when light is reflected at the proper angle. It sometimes resembles
opal-matrix, but is easily distinguished by its lower hardness and by
its effervescent action with acid. Choice specimens come from Bleiberg
in Carinthia, and from Astrakhan.
Apophyllite has not many characters to commend it, being at the best
faintly pinkish in colour, and always imperfectly transparent. It is
a hydrous silicate of potassium and calcium with the complex formula
(H,K)_{2}Ca(SiO_{3})_{2}.H_{2}O. Its refractivity is about 1·535,
specific gravity 2·5, and hardness 4½ on Mohs’s scale; it possesses
an easy cleavage. It occurs in the form of tetragonal crystals at
Andreasberg in the Harz Mountains, and in the Syhadree Mountains,
Bombay, India.
PART II—SECTION D
ORGANIC PRODUCTS
CHAPTER XL
PEARL, CORAL, AMBER
Public-domain text, read in full here on John Shaqi.
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