Ch. 7: Phenakite and Euclase

Ch. 7: Chrysoberyl Page of 149 Ch. 7: Zircon Text size:minus plus Restore normal size   Mail page  Print this page
       
     
 
ΡΗΕΝAΚΙΤΕ.
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The cymophane, or true cat's-eye, owes its chatoyancy, whether of pale steely whiteness as a flash, or as a line like a silver wire, to the orderly arrangement of an immense number of minute cavities along certain lines causing minute internal striations. The dark yellowish green hue is most prized ; it is usually cut en cabochon. The chrysoberyl occurs in many localities, notably in Brazil and Ceylon, Connecticut, and the Urals. A fine specimen from the Hope collection is in the British Museum.
The chrysoberyl owes its colour chiefly to iron in the form of ferrous oxide ; but traces of chromium and of manganese oxide also occur in it. Its percentage composition is roughly :
Phenakite.
Phenakite is but rarely used as a gem-stone. The colourless transparent variety may, however, be mistaken for a diamond, especially by candlelight, when the prismatic colours, or " fire," of a brilliant-cut specimen are conspicuous. The hardness of this stone lies betweenand 8, while its specific gravity is close upon 3. Crystals of phenakite usually take the form of a low obtuse rhombohedron. This mineral is sometimes perfectly colourless and transparent, but more frequently is rather clouded and milky, or of a straw, sherry, or cinnamon tint. When viewed with a dichroiscope the ordinary image is colourless, the extraordinary image being of a warm yellow or brown, should the specimen ex­amined possess any colour at all.
The best specimens of phenakite known come from the emerald and chrysoberyl mines at Takovaya, eighty-five versts east of Ekaterinburg, Perm, Asiatic Russia : the matrix is a mica-schist ; less important examples are found in Colorado, U.S.A.
In the Mineralogical Gallery of the British Natural History Museum, there are fine specimens of phenakite both in crystals
 
 
 
 
       
Ch. 7: Chrysoberyl Page of 149 Ch. 7: Zircon
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