Zoisite
Zoisite is a calcium aluminium hydroxy sorosilicate belonging to the epidote group ofminerals. Its chemical formula is Ca2Al3(SiO4)(Si2O7)O(OH). Zoisite is named after theSlovene scientist Baron Sigmund Zois von Edelstein (Žiga Zois), who realized that this was an unknown mineral when it was brought to him by the mineral dealer Simon Prešern, who had discovered it in the Saualpe mountains (Svinška planina) of Carinthia in 1805. Zoisite was first known as saualpite, after its type locality. Zoisite occurs as prismatic, orthorhombic (2/m 2/m 2/m) crystals or in massive form, being found in metamorphic and pegmatitic rock. Zoisite may be blue to violet, green, brown, pink, yellow, gray, or colorless. It has a vitreous luster and a conchoidal to uneven fracture. When euhedral, zoisite crystals are striated parallel to the principal axis (c-axis). Also parallel to the principal axis is one direction of perfect cleavage. Zoisite is somewhat higher than 6 inhardness and its specific gravity is between 3.10 - 3.38, depending on the variety. Zoisite streaks white and is said to be brittle. Clinozoisite is a more common monoclinic polymorph of zoisite. Transparent material is fashioned into gemstones while translucent-to-opaque material is usually carved. A metamorphic rock known as anyolite consists of green zoisite with blacktschermakite and ruby crystals.[4][5] Sources of zoisite include Tanzania (tanzanite), Kenya (anyolite), Norway (thulite),Switzerland, Austria, India, Pakistan, and Washington in the USA. |
Sunday, July 19, 2009
Zoisite
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