Marble Original Rock

Metamorphism causes variable recrystallization of the original carbonate mineral grains.

Marble original rock.

Marble granular limestone or dolomite i e rock composed of calcium magnesium carbonate that has been recrystallized under the influence of heat pressure and aqueous solutions. In bhedaghat of jabalpur district in the state of madhya pradesh the river has carved the soft marble creating a beautiful gorge of about 8 km in length it is a popular indian tourist destination the local marble is mined and carved into various figures and transported all over india. Petrographically marbles are massive rather than thin layered and consist of a. Marble is a metamorphic rock resulting from regional or at times contact metamorphism of sedimentary carbonate rocks either limestone or dolostone.

Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism. 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 resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals. This metamorphic process causes a complete recrystallization of the original rock into an interlocking mosaic of calcite and or dolomite crystals.

Marble is a metamorphic rock formed when limestone is subjected to high pressure or heat. 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.