Yes. Limestone is the parent rock, or protolith, of marble.
Marble is the metamorphosed result of limestone. Therefore, marble is metamorphic.
Limestone is the parent rock of marble. The word marble can be used to refer to both metamorphosed and unmetamorphosed limestone.
Marble is formed by the metamorphosis of limestone (by heat and pressure). Therefore limestone may be called the parent rock (or more correctly the protolith) of marble.
marble
Limestone doesn't normally have a parent rock. One exception to this may be a detrital limestone, whose parent rock would however also be limestone!
Marble is the metamorphosed result of limestone. Therefore, marble is metamorphic.
Slate and Marble are metamorphic rocks. Slate's parent rock is shale and Marble's parent rock is limestone.
Yes. 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.
By definition a metamorphic rock has undergone recrystallization without melting - that requires a lot of heat and pressure. Marble is a metamorphic rock - it is recrystallized limestone or dolostone.
Slate is a foliated (displaying layers or banding) metamorphic rock, and its parent rock was shale or mudstone. Marble is a non-foliated metamorphic rock (no layers or bands) and its parent rock was limestone.
Limestone is the parent rock of marble. The word marble can be used to refer to both metamorphosed and unmetamorphosed limestone.
Marble is formed by the metamorphosis of limestone (by heat and pressure). Therefore limestone may be called the parent rock (or more correctly the protolith) of marble.
Limestone is the parent of rock of non foliated metamorphic. This is a very old type of rock.
marble
Limestone doesn't normally have a parent rock. One exception to this may be a detrital limestone, whose parent rock would however also be limestone!
Quartzite--sandstone. Marble--limestone. Slate--shale. Gneiss--basalt or granite.
Metamorphism. The heat and pressure can be from depth of burial or from regional metamorphic processes, such as those that would be due to plate collisions Because limestones (the parent rock of marble) are largely made up of one mineral, calcite, and calcite exhibits stability over a wide range of temperatures and pressures, metamorphism of limestone only causes the original calcite crystals to grow larger. Therefore, the limestone can change to marble either by contact metamorphic processes (from proximity to, or contact with, a molten intrusion into a limestone parent rock) or regional processes due to tectonic plate movements, or from depth of burial.