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Marble is a metamorphic rock resulting from regional or at times contact metamorphism of sedimentary carbonate rocks, either limestone or dolostone. This metamorphic process causes a complete recrystallization of the original rock into an interlocking mosaic of calcite and/or dolomite crystals. The temperatures and pressures necessary to form marble usually destroy any fossils and sedimentary textures present in the original rock. Pure white marble is the result of metamorphism of very pure limestones. The characteristic swirls and veins of many colored marble varieties are usually due to various mineral impurities such as clay, silt, sand, iron oxides, or chert which were originally present as grains or layers in the limestone.


An Insight

Mahendra Natural Stone started in the early 2005 as modest enterprises of highly precise fine quality of Natural Stones. Today Mahendra Natural Stone is a trusted name in the world of natural stone with a multi-product range that includes Blocks, Slabs, Tiles, Monuments, Read More

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