Sillimanite is an index mineral for high temperature and variable pressure metamorphism.
Slate is a low-grade metamorphic rock.
It is a medium-grade metamorphic rock with a preponderance of the platy mineral graphite.
Gneiss is usually considered a high grade metamorphic rock (although there are some weird exceptions).
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.
Metamorphic rocks are classified as being foliated or being non-foliated. Foliated metamorphic rocks have visible banding or sheet-like layering. Slate, phyllite, gneiss, and schist are foliated metamorphic rocks. Non-foliated metamorphic rocks do not display banding or layering. Marble and quartzite are non-foliated metamorphic rocks. Metamorphic rocks can also be classified as either regional metamorphic rocks or contact metamorphic rocks, depending on their method of formation.
Slate is a low-grade metamorphic rock.
Slate is a low-grade metamorphic rock.
It is a medium-grade metamorphic rock with a preponderance of the platy mineral graphite.
Garnet is a mineral most often found in high grade metamorphic rock.
Gneiss is usually considered a high grade metamorphic rock (although there are some weird exceptions).
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.
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Metamorphic rock can undergo a series of changes called degrees of metamorphism, from low-grade to high-grade.
It is schist.
Metamorphic rocks are classified as being foliated or being non-foliated. Foliated metamorphic rocks have visible banding or sheet-like layering. Slate, phyllite, gneiss, and schist are foliated metamorphic rocks. Non-foliated metamorphic rocks do not display banding or layering. Marble and quartzite are non-foliated metamorphic rocks. Metamorphic rocks can also be classified as either regional metamorphic rocks or contact metamorphic rocks, depending on their method of formation.
Slate. Slate is a low grade metamorphic rock derived from shale or mudstone.
Most schists are derived from phyllite, a lower grade metamorphic rock.