British Museum (Natural History) General GuideBritish Museum (Natural History)
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British Museum (Natural History) General Guide
British Museum (Natural History)
British Museum (Natural History) -- Guidebooks; Natural history museums -- England -- London -- Guidebooks
Uraninite, or Pitchblende (10h), consists mainly of Uranium and Oxygen,
but contains traces of Helium and Radium, of which latter it is the
commercial source.
Chrysoberyl (9e) is another precious stone, almost equal in lustre and
hardness to the Sapphire; one variety is a beautiful greenish-yellow;
another, with a peculiar play of light, is the Cat’s-eye; and a third,
green by sunlight, but red by candle- or lamp-light, is known as
Alexandrite.
Corundum (9f), when clear and of the proper colour, is, after the
Diamond, the most precious of stones. When pure, it is colourless, but
with minute traces of colouring ingredient it assumes the richest and
most varied hues; when red it is Ruby, and when blue Sapphire; the
yellow, green, and purple varieties were at one time known respectively
as the Oriental Topaz, Emerald, and Amethyst. The prefix “Oriental”
was at first used to suggest that the stones are not ordinary Topaz,
Emerald, and Amethyst, but other similarly coloured minerals coming
from the East (India, Ceylon, Siam, Pegu, etc.); it was afterwards
understood to suggest only the excellence of their characters. The
Star-stone, another variety of Corundum, when placed in a strong light
shows a six-rayed star.
Hæmatite (11a) is a valuable ore of iron (Iron 70, Oxygen 30, per
cent.).
Cassiterite, or Tin-stone (11f), is the ore of Tin, of which metal it
contains 79 per cent.
Zircon (13b), when clear and without flaws, is one of the precious
stones: one variety with peculiar red tints is the Hyacinth or Jacynth,
while the colourless, yellowish, and dull green phases are termed
Jargoon: the colourless variety, owing to its high refractive and
dispersive power, approaches the Diamond in brilliancy.
Quartz, which is Silica, the oxide of Silicon, is the most common of
Minerals. In its clear and transparent variety it is the Crystal of
the ancients and the Rock-Crystal of modern times; it is the Brazilian
Pebble of spectacle-makers (14c). After the clear come the smoky
varieties, including the Scotch Cairngorm and Occidental Topaz (14g).
Next follows the Amethyst (14g), one of the less valuable, though one
of the most beautiful, of gem stones. The Quartz Cat’s-eye (13f) is a
variety presenting a similar play of light to that of the Chrysoberyl
Cat’s-eye already referred to: the effect is due to enclosed fibres
of an Asbestos-like mineral in the specimens from Ceylon, and to
fibres of Crocidolite in the blue, and of altered Crocidolite in the
brownish-yellow specimens from South Africa.
Jasper (13g) is a coloured mixture of Silica and Clay, distinguished
from ordinary Quartz by its opacity and dull earthy fracture. It is of
various colours, chiefly red, brown, yellow, and green; the colours
being arranged sometimes in a nodular form, as in Egyptian Jasper, at
other times in stripes, as in Riband Jasper.
Public-domain text, read in full here on John Shaqi.
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