bluish
light occasionally plays upon it. Werner called it " Diamond Spar." It
is said that some crystals found near St. Gothard, exhibit two colours,
and that some of these are in dolomite, but mere commonly they are
found in mass. Some in Styria have grown in with the granite, and so
firmly that it is difficult, if not impossible, to remove them without
damage. The crystals may be from the size of a pea to that of a hazel
nut, of a greenish-blue or duck's-neck violet. Some pieces display
several colours. In Bohemia they are found embedded in pebbly masses of
hercinite. In Rhodes, Sweden, and the Urals, they may also be found
with tourmaline in schist, with platinum and magnetic iron ore. In
Ceylon, China, and India, they are found in beautiful green crystals,
possessing characteristic stri pes, with black hornblende.
Pleonaste.
This
mineral received the name of ceylanite from Rome d' L'Isle, who
analyzed it with a number of others brought from Ceylon, Haiiy, seeing
its crystal was like that of the spinel, desired to give it a special
position in the system of minerals, and named it pleenaste, which signifies superfluity. Further investigation shewed that it was in reality a black variety of the spinel.
The specific gravity of, this stone rises from 3'5 to 3'8- It
consists principally of alumina, and about 10 per cent of protoxide af
iron. Its in-i*sibility before the blow-pipe, and its formation with
borax into an iron-coloured glass, are the surest indications of
pleonaste. Acids have but little influence upon it. It is found in
Russia and' other cold climates, but it is also found in Ceylon, as
well as in the dolomite region in Ratan.
Spinel,
in consequence of its lustre, colour, and hardness, is used for
personal ornament, and for objects of luxury; but it is only when the
crystals are fine and large that they are considered gems. In cutting,
it receives the same form as the ruby.
Spinal ruby for balas ruby varies in value according to its cut and colour.
In the inventury of the French Crown Jewels, in the year 1791, we find the following :—