Product DescriptionMarbles are formed from limestone or dolomite that has undergone enough heat and pressure to get metamorphosized into a crystalline structure. This metamorphosis takes place when the weight of overlying material, pressure from crystal collisions and heat from the earth's core generate temperatures in excess of 1800?F. It has an interlocking or mosaic texture composed of crystalline grain of calcite, dolomite or both. Texture of marble depends on the form, size and uniformity of grains. The chemical constituents of marble determine the color of the marble. Generally calcite and
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