Is Marble Sedimentary Rock

Marble is a rock resulting from metamorphism of sedimentary carbonate rocks most commonly limestone or dolomite rock. It was a sedimentary rock before it was metamorphosed. In its pure form marble is a white stone with a crystalline and sugary appearance consisting of calcium carbonate caco 3 usually marble contains other minerals including quartz graphite pyrite and iron oxides these minerals can give marble a pink brown gray green or variegated coloration.

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Any limestone pure or impure can recrystallize as a marble.

Is marble sedimentary rock.

Sedimentation is the collective name for processes that cause these particles to settle in place. The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals. The particles that form a sedimentary rock are called sediment. Sedimentary rock rock formed at or near the earth s surface by the accumulation and lithification of sediment or by the precipitation from solution at normal surface temperatures.

Marble is a metamorphic rock formed when limestone is subjected to high pressure or heat. Sedimentary rocks are types of rock that are formed by the accumulation or deposition of small particles and subsequent cementation of mineral or organic particles on the floor of oceans or other bodies of water at the earth s surface. All that is required is some combination of high temperature and high pressure enough time for the recrystallization to take pl. Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism.

Metamorphism causes variable recrystallization of the original carbonate mineral grains. It is composed primarily of the mineral calcite caco 3 and usually contains other minerals such as clay minerals micas quartz pyrite iron oxides and graphite under the conditions of metamorphism the calcite in the limestone recrystallizes to form a rock that is. Sedimentary rocks are the most common rocks exposed on the earth s surface but are only a minor constituent of the entire crust.

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