Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism.
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Some kinds of metamorphic rocks granite gneiss and biotite schist are two examples are strongly banded or foliated.
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Non foliated metamorphic rocks such as hornfels marble quartzite and novaculite do not have a layered or banded appearance.
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Foliated means the parallel arrangement of certain mineral grains that gives the rock a striped appearance.
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Common metamorphic rocks include phyllite schist gneiss quartzite and marble.
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The preexisting rocks may be igneous sedimentary or other metamorphic rocks.
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Like other metamorphic rocks marble has no fossils and any layering that appears in it probably does not correspond to the original bedding of the precursor limestone.
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It is composed primarily of the mineral calcite caco 3 and usually contains other minerals such as clay minerals micas quartz pyrite iron oxides and graphite under the conditions of metamorphism the calcite in the limestone recrystallizes to form a rock that is.
Foliated metamorphic rocks such as gneiss phyllite schist and slate have a layered or banded appearance that is produced by exposure to heat and directed pressure.