Marble is a metamorphic rock composed of recrystallized carbonate minerals most commonly calcite or dolomite marble is typically not foliated although there are exceptions in geology the term marble refers to metamorphosed limestone but its use in stonemasonry more broadly encompasses unmetamorphosed limestone.
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Descriptions contain sizing and source information for each stone.
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By studying a material s grain color and texture you can easily identify the presence of one of the minerals below be sure to examine your sample on a clean surface and pay close attention to the material s luster and hardness.
Look for a black streak and a strong attraction to a magnet.
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Marble is commonly used for sculpture and as a building material.
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Marble is usually a light colored rock.
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Dimension stones have also left deep imprints on the architectural heritage of the country.
When it is formed from a limestone with very few impurities it will be white in color.
Innumerable temples forts and palaces of ancient indian civilisation have been carved out of locally available stones.
Magnetite or lodestone is a common accessory mineral in coarse grained igneous rocks and metamorphic rocks.
Green and greenish rocks get their color from minerals that contain iron or chromium and sometimes manganese.
Crystals are common with striated faces shaped in octahedrons or dodecahedrons.
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Marble that contains impurities such as clay minerals iron oxides or bituminous material can be bluish gray pink yellow or black in color.
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