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                | CALCITE is a carbonate of lime (CaCo3). It 
                crystallizes in rhombohedron class. It is also known by the name 
                calc-spar. It is white in colour but is also found in various 
                shades like pink, brown etc., depending upon the impurities 
                present. It is identified easily from other lime minerals by its 
                well defined rhombohdral cleavage and hardness 3 of Moh's scale. 
                Its composition is identical to that of limestone but the latter 
                occurs as sedimentary beds. There is another mineral, aragonite, 
                of the same chemical composition. It crystallizes in 
                orthorhombic system. It is, however, an unstable mineral, found 
                mainly associated with gypsum beds and the tests of 
                reef-building corals. It is not found in the same large quantity 
                as that of calcite. |  
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                    | Hardness | 3 (only on the basal pinacoidal faces, calcite 
                    has a hardness of less than 2.5 and can be scratched by a 
                    fingernail). |  
                    | Associated Minerals | Numerous but include these classic associations: Fluorite, 
                    quartz, barite, sphalerite, galena, celestite, sulfur, gold, 
                    copper, emerald, apatite, biotite, zeolites, several metal 
                    sulfides, other carbonates, and borates and many other. |  
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			Chemical/Typical composition | CaO56.03 % CO243.97 %
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			Colour | Extremely variable but generally white or colorless or with 
                    light shades of yellow, orange, blue, pink, red, brown, 
                    green, black and gray. Occasionally iridescent. |  
                    | Characteristics | Refractive indices of 1.49 and 1.66 causing a 
                    significant double refraction effect (when a clear crystal 
                    is placed on a single line, two lines can then be observed), 
                    effervesces easily with dilute acids and may be fluorescent, 
                    phosphorescent, thermoluminescence and triboluminescent. |  
                    | Luster | Vitreous to resinous to dull in massive forms. |  
                    | Field Indicators | Crystal habit, reaction to acid, abundance, 
                    hardness, double refraction and especially cleavage. |  |  
                | Industrial ApplicationsCalcite in pulverized form finds use mostly as filler in rubber 
                and textile goods. A considerable quantity is also used in the 
                ceramics industry for the preparation of glazes. Super white 
                quality of calcite in powder form (-300 mesh) is used in the 
                manufacture of paint and distemper. Calcite is now insecticides. 
                It is also used in the manufacture of cement, calcium carbide, 
                metal polish and sometimes also as a fluxing agent. The 
                transparent and clear crystals are used in the optical industry, 
                for the manufacture of nicol prism. Principal characteristics 
                which make iceland-spar of special value for use in optical 
                instruments are its very high birefringence, high degree of 
                purity, perfect crystalline structure and transparency. The 
                mineral must be in pieces at least 25mm. long, 12mm. thick, 
                colourless, transparent and free from cloudy inclusions, 
                cavities, and foreign substances.
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