In pure form marble consists of calcium carbonate calcite and is sparkling white.
Marble black rock.
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Marble takes a high polish.
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Impurities produce pale gray brown or variegated colored rock.
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Black marble also occurs.
It can also be found in various european countries including england czech republic and bohemia.
It can be cut and inlaid with other decorative stones and minerals using a.
Marble is commonly used for sculpture and as a building material.
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When it is formed from a limestone with very few impurities it will be white in color.
Marble that contains impurities such as clay minerals iron oxides or bituminous material can be bluish gray pink yellow or black in color.
Black and gray colours result from the presence of fine scales of graphite.
Bands of calc silicate rock may alternate with bands of marble or form nodules and patches sometimes producing interesting decorative effects but these rocks are particularly difficult to finish because of the great difference in hardness between the silicates and.
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This mineral is also being collected by some people.
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.
Ashford black marble is a very fine grained sedimentary rock and is not a true marble in the geological sense.
Marble is usually a light colored rock.
Bolivia and china are two of the countries with the most amount of cassiterite deposits.
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