| Name: Calcite |
Origin of name: from Latin calcx, or calcis, meaning lime or limestone |
Chemical composition: CaCO3 |
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Calcite is the most common mineral in the Earth's crust, after quartz. It occurs as rhombohedral and scalenohedral crystals, in many different combinations, but also as massive or compact rocks - chalk, limestone and marble.
Clear rhombs of calcite, known as "Iceland Spar", demonstrate a property known as double refraction; objects viewed through the crystal show two images (as shown in this picture). This is because light travels through the calcite crystal at different speeds in different directions. |
Crystal system: trigonal/hexagonal |
| Class: Carbonates |
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| Hardness: 3 |
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| Cleavage: perfect |
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| Colour: white, colourless, grey, red, brown, green or black |
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| Specific gravity: 2.71 |