The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals.
Black marble rock.
Marble is a rock resulting from metamorphism of sedimentary carbonate rocks most commonly limestone or dolomite rock.
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Ashford black marble is the name given to a dark limestone quarried from mines near ashford in the water in derbyshire england.
Impurities produce pale gray brown or variegated colored rock.
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Metamorphism causes variable recrystallization of the original carbonate mineral grains.
Marble is usually a light colored rock.
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In pure form marble consists of calcium carbonate calcite and is sparkling white.
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Marble is a metamorphic stone formed by subjecting limestone to heat or pressure.
Once cut turned and polished its shiny black surface is highly decorative.
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Ashford black marble is a very fine grained sedimentary rock and is not a true marble in the geological sense.
When it is formed from a limestone with very few impurities it will be white in color.
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Black limestones containing bituminous matter which commonly emit a fetid odour when struck are widely used.
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The well known petit granit of belgium is a black marble containing crinoid stem plates derived from fossil echinoderms invertebrate marine animals.
Marble that contains impurities such as clay minerals iron oxides or bituminous material can be bluish gray pink yellow or black in color.