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Ch. 12: Beryl - Garnet

Ch. 12: Beryl - Garnet Page of 311 Ch. 12: Beryl - Garnet Text size:minus plus Restore normal size   Mail page  Print this page
230
PRECIOUS STONES.
and the difference in colour in the various directions may sometimes be seen without the aid of the dichroscope. The green colour of the Emerald is not discharged by strongly heating, hence is not due to organic matter. Before the blowpipe even thin splinters fuse with difficulty, first turning an opaque white.
The specific gravity of Beryl is 2-67 to 2-75. The fracture is conchoidal, and the mineral is distinctly brittle, and
hence must be handled with care. The hardness is 7-1/2 to 8. There is an indistinct cleavage parallel to the basal plane. The streak is white.
In crystalline form it is hexagonal, and the crystals usually sbow a rather slender prismatic habit (Fig. 18), and are often striated vertically by repeated oscillations of different prism faces. The Emerald in particular is very frequently seen to have numerous minute internal cracks and fissures, so that " an Emerald without a flaw " is quite
Ch. 12: Beryl - Garnet Page of 311 Ch. 12: Beryl - Garnet
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