Avon Marbles

Sector 4, Noida, Uttar Pradesh

Marble is a metamorphic rock resulting from regional or rarely 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, aragonite and/or dolomite crystals. The temperatures and pressures necessary to form marble usually destroy any fossils and sedimentary textures present in the original rock. Marble has long been highly valued for its beauty & strength; Marbles are suitable for both interior and exterior applications.

A marble is a metamorphic rock formed by alteration of limestone or dolomite, often irregularly colored by impurities and used especially in architecture and sculpture. Marble tiles are suitable for bathrooms, entryways and fireplaces, living & dining areas. Marble floor tiles are also used for both interior and exterior flooring applications. Some of the different colors of marble are white, red, black, mottled and banded, gray, pink, and green.

Marble has been valued for thousands of years for its rich palette of beautiful colors and appearance and is perfect, pretty much anywhere in the house.

Marbles 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 1800F. 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 dolomite marbles are of pure white color. Variations of whiteness of pure marbles are due to the mixture of foreign substances. Such impurities form bands, streaks and clouds. Black and grayish shades are due to graphite; pinks, reds are mainly due to the presence of manganese oxides or hematite.