Name: |
calcite |
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Class: |
Carbonates |
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Chemistry: |
CaCO3 calcium carbonate |
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Color(s): |
white, yellow, pink, red, brown, green, clear, etc. |
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Hardness: |
3 |
SpecGrav: |
2.6 - 2.8 |
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Fracture: |
conchoidal |
Cleavage: |
perfect |
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Crystal: |
hexagonal (rhombohedral, prismatic, and virtually all other shapes in the hexagonal system and many combinations.) It can easily be cleaved to form perfect rhombohedrons. |
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Envronment: |
typical sedimentary mineral formed by precipitation through evaporation. Under high carbon dioxide pressure it is stable through most phases of metamorphosis, when the pressure is reduced it may dissociate into a variety of complex calcium silicates. It has been found in lava flows, and is often associated with hydrothermal veins. A very abundant mineral. |
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Association: |
quartz, mica, dolomite, ore minerals, sulfides, analcime |
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Locals: |
| Alps | France | Germany | Ireland | England | Canada | Russia | China | Mexico | Mo., Co. Tn., USA | (just about everywhere) |
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Misc: |
soluble in cold HCl with loss of CO2 , fluorescence under UV light several colors depending on local, high double refraction. |
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