The nonfoliated metamorphic equivalent of limestone is marble.
Marble is the metamorphic equivalent of which rock.
Some characteristics of metamorphic rocks to look for.
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.
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.
Foliated metamorphic rocks appear layered.
Marble is a metamorphic rock formed from limestone.
Although metamorphic rocks typically form deep in the planet s crust they are often exposed on the surface of the earth.
Marble is a metamorphic rock formed when limestone is subjected to high pressure or heat.
Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism.
They are invariably bright and lustrous.
Mineral alignment in a metamorphic rock usually gives the rock a foliated texture.
Slate is another common metamorphic rock that forms from shale.
Marble is commonly used for sculpture and as a building material.
Sandstone is a sedimentary rock formed from sand.
Coarse grained metamorphic rocks may show crystals that grew larger during metamorphism.
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Marble is the metamorphic equivalent of limestone.
In geology metasedimentary rock is a type of metamorphic rock such a rock was first formed through the deposition and solidification of sediment then the rock was buried underneath subsequent rock and was subjected to high pressures and temperatures causing the rock to recrystallize the overall composition of a metasedimentary rock can be used to identify the original sedimentary rock even.