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Marble is metamorphosed limestone, composed of fairly pure calcite (a crystalline form of calcium carbonate, Ca C O3). It is extensively used for sculpture, as an building material, and in many other applications.
Faux marble or faux marbling is a wall painting technique that imitates the color patterns of real marble (not to be confused with paper marbling). Marble dust can be combined with cement or synthetic resins to make reconstituted or cultured marble .
Places named after the stone include Marble Hill, Manhattan, New York and the town of Marble, Minnesota. The Elgin Marbles are marble sculptures taken from the ParthenonThe Parthenon ( Greek: Παρθενων, the Temple of Athena the Virgin is the most famous surviving building of Ancient Greece and one of the most famous buildings in the world. The building has stood atop the Acropolis of to BritainThe United Kingdom of Great Britain and Northern Ireland is a state in Western Europe, usually known simply as the United Kingdom the UK Britain or less accurately as Great Britain . The UK was formed by a series of Acts of Union which united the formerly by the Earl of ElginThomas Bruce, 7th Earl of Elgin and 11th Earl of Kincardine ( July 20, 1766 November 14, 1841) was a British nobleman and diplomat, notorious for the removal of marble sculptures from the Parthenon in Athens popularly known as the Elgin Marbles. Elgin was.
Marble is a metamorphic rockMetamorphic rock is the result of the transformation of a pre-existing rock type, the protolith in a process called metamorphism (which means "change in form", derived from the Greek words meta, "change", and morphe, "form"), through which the protolith i resulting from regional or at times contact metamorphism of sedimentaryshale overlaid by limestone. Cumberland Plateau, Tennessee. Sedimentary rock is one of the three main rock groups (along with igneous and metamorphic rocks) and is formed in three main ways—by the deposition of the weathered remains of other rocks (known carbonate rocks, either limestone or dolostoneDolostone is a sedimentary rock that contains a high percentage of the mineral dolomite. It is usually referred to as dolomite rock. publications it was referred to as magnesian limestone. Typically, dolostone and impure limestone occur together, along wi. 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.