Marble Is A Blank Metamorphic Rock

The standard scientific notation for pressure is expressed in pascals or megapascals 1 pascal is equivalent to 10 bars.

Marble is a blank metamorphic rock. Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism. Metamorphic rocks are formed from other rocks that are changed because of heat or pressure. Metamorphic rock metamorphic rock pressure. Get help with your metamorphic rock homework.

The rocks that make up marble are. The color of marble can range from the purest white to black ranging through the warmer colors in between depending on the other mineral impurities. Metamorphic rock can be marble because marble is a form of metamorphic rock which is composed of coarse crystals from parent limestone or dolostone rocks. 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.

The pressure experienced by a rock during metamorphism is due primarily to the weight of the overlying rocks i e lithostatic pressure and is generally reported in units of bars or kilobars. Although metamorphic rocks typically form deep in the planet s crust they are often exposed on the surface of the earth. Marble is made through the process of pressure and heat added to an existing rock. Access the answers to hundreds of metamorphic rock questions that are explained in a way that s easy for you to understand.

Marble is a metamorphic rock formed when limestone is subjected to high pressure or heat. Marble is commonly used for sculpture and as a building material. Limestone a sedimentary rock will change into the metamorphic rock marble if the right conditions are met. Marble is a metamorphic rock.

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. Like other metamorphic rocks marble has no fossils and any layering that appears in it probably does not correspond to the original bedding of the precursor limestone.