Black Marble Stone - Code M103

Supplier Location: Iran
Material Type: Marble
Main Color: Black
Surface Finish: Polished

Reference Price: US$ /

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What Is Marble?

This stone is among the most elegant and luxurious of stones. Marble's beauty will last for generations and is versatile enough for use throughout the home in such places as fireplace surrounds, ornamental furnishings, walls, flooring, and bathrooms. Marble especially stands out in the bath. It can be applied on almost every surface, including vanities, shower walls, tub decks and flooring.

Given that marble is more susceptible to staining by many foods, spilled liquids and other household materials, we do not recommend their use for kitchen countertops. Softer and more porous than granite, marble is more suitable for less-trafficked, formal areas.

Marble Colour Range

Distinctive colours and grain will give unique character and personality to any application in your home. Light, natural tones are most popular however you are not limited to what you see here. Marble is available in a wide range of colours so please feel free to enquire with us.

What Is Marble Composed of?

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. Green coloration is often due to serpentine resulting from originally high magnesium limestone or dolostone with silica impurities. These various impurities have been mobilized and recrystallized by the intense pressure and heat of the metamorphism.

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