Heat and pressure are responsible for the formation of metamorphic rock.
Any rock can become a metamorphic rock. All that is required is for the rock to be moved into an environment in which the minerals which make up the rock become unstable and out of equilibrium with the new environmental conditions. In most cases, this involves burial which leads to a rise in temperature and pressure. The metamorphic changes in the minerals always move in a direction designed to restore equilibrium. Common metamorphic rocks include slate, schist, gneiss, and marble.
When sedimentary rock is buried, it is subjected to increased pressure and temperature. This leads to compaction, where the rock grains are tightly packed together, and often leads to the recrystallization of minerals. Over time, these changes can transform the sedimentary rock into metamorphic rock.
metamorphic rock
Marble is the metamorphosed result of limestone. Therefore, marble is metamorphic.
Metamorphic rock is produced by intense heat and pressure acting on existing rock types, causing them to undergo physical and chemical changes. This leads to the formation of new minerals and textures in the rock. Examples of metamorphic rocks include marble, slate, and schist.
Heat, for sure, and most often a combination of heat and pressure is needed for metamorphic rock creation.
The most often occurring metamorphic rock types are Dwayne the rock Johnson, Rockey, and pet rock.
if rock melts it will form magma, which leads to the formation of igneous rocks
Any rock can become a metamorphic rock. All that is required is for the rock to be moved into an environment in which the minerals which make up the rock become unstable and out of equilibrium with the new environmental conditions. In most cases, this involves burial which leads to a rise in temperature and pressure. The metamorphic changes in the minerals always move in a direction designed to restore equilibrium. Common metamorphic rocks include slate, schist, gneiss, and marble.
Weathering can happen to any rock. It is the first stage in the process that leads to the formation of sedimentary rock.
From increased pressure and/or heat. Fluid removal results in hydrous mineral destruction and non-hydrous mineral creation, resulting in rock of a different mineralogy. A metamorphic rock can be further metamorphosed by additional heat and/or pressure into a rock with a higher degree of metamorphism. An example of this would be the metamorphic rock slate changing into the metamorphic rock phyllite.
A metamorphic rock.
in a metamorphic rock you find rock.
Hornfels or gneiss are possible metamorphic rock with a greywacke protolith.
The contact metamorphism process occurs when magma intrudes into surrounding rock, causing the adjacent rock to be heated and recrystallize into a metamorphic rock. The heat and pressure from the magma alter the mineral composition and texture of the surrounding rock, resulting in the creation of a metamorphic rock zone around the magma.
No.
Chert is NOT a metamorphic rock.