whatever the f*** it is, nobody gives a darn
contact metamorphism, regional metamorphism, dynamic metamorphism
Slate is the rock that forms at the lowest grade of regional metamorphism. With increased metamorphic grade, slate can further transition into phyllite, then schist, and finally gneiss.
Contact metamorphism is the process of forming rocks from the heat of magma intrusion. Regional metamorphism, meanwhile, is the process of forming rocks by pressure and heat at plate boundaries.
The three main types of metamorphism are contact metamorphism, regional metamorphism, and dynamic metamorphism. Contact metamorphism occurs near igneous intrusions, regional metamorphism occurs over large areas due to tectonic forces, and dynamic metamorphism occurs along fault zones due to intense pressure and shearing.
Regional metamorphism would be the product of two plates colliding. The intense pressure and temperature generated during plate collision can create regional metamorphism, which affects a larger area and involves the recrystallization of rocks. Contact metamorphism, on the other hand, is caused by heat from a nearby magma intrusion and affects rocks in a localized area.
whatever the f*** it is, nobody gives a darn
contact metamorphism, regional metamorphism, dynamic metamorphism
contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.
Burial metamorphism differs from regional and contact metamorphism in that it is the result of rocks being buried deeper into the earth's crust through tectonic movements.
contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.
contact metamorphism, regional metamorphism, dynamic metamorphism
Contact metamorphism is the process of forming rocks from the heat of magma intrusion. Regional metamorphism, meanwhile, is the process of forming rocks by pressure and heat at plate boundaries.
contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.
Slate is the rock that forms at the lowest grade of regional metamorphism. With increased metamorphic grade, slate can further transition into phyllite, then schist, and finally gneiss.
Contact metamorphism is the process of forming rocks from the heat of magma intrusion. Regional metamorphism, meanwhile, is the process of forming rocks by pressure and heat at plate boundaries.
Contact metamorphism occurs locally along the edges of intrusions and is characterized by high temperatures but relatively low pressures, resulting in the formation of non-foliated rocks like marble and quartzite. In contrast, regional metamorphism occurs over large areas due to tectonic forces, leading to both high temperatures and pressures that cause the formation of foliated rocks like schist and gneiss.
The three main types of metamorphism are contact metamorphism, regional metamorphism, and dynamic metamorphism. Contact metamorphism occurs near igneous intrusions, regional metamorphism occurs over large areas due to tectonic forces, and dynamic metamorphism occurs along fault zones due to intense pressure and shearing.