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metamorphicregional metamorphism
suduction or sea floor spreading
contact metamorphism, regional metamorphism, dynamic metamorphism
The most common type of land metamorphism is Regional metamorphism. The most common rocks are slates, schists, and gneisses. This occurs within the folds of mountain belts and cratonic areas.
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Contact = Close to a hot spot Dynamic = Along a transform boundary Impact = Near a crater Regional = At deep subduction areas
Contact - Close to a hot spot Dynamic - Along a transform boundary Impact - Near a crater Regional - At deep subduction areas
It forms deep inside the Earth's surface
Contact metamorphism occurs locally, next to igneous intrusions and along fractures that were in contact with hydrothermal fluids. Regional metamorphism occurs over very large areas, such as deep within the cores of rising mountain ranges, and generally occurs with the folding of rock layers. Both result in the formation of metamorphic rocks.
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Deep underground from heat and pressure.
metamorphicregional metamorphism
metamorphicregional metamorphism
Most metamorphism takes place deep underground, where high heat and pressure change the rocks, since both increase with depth.
Regional metamorphism takes place in large areas around plate boundaries.
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