Regional metamorphism occurs due to the change in pressure and temperature over a large region of the crust. It is the result of high pressure and elevated temperatures that are associated with deep burial in an organic belt.
Very low grade regional metamorphism.
Contact metamorphism does not cause profound compaction, which is the reduction in size of the spaces between mineral particles due to increases in pressure. Regional metamorphism causes compaction and possibly recrystallization, increasing the density of the rock.
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
regional metamorphism occurs over a large area while local metamorphism occurs over a small area.
contact metamorphism, regional metamorphism, dynamic metamorphism
Very low grade regional metamorphism.
Contact metamorphism does not cause profound compaction, which is the reduction in size of the spaces between mineral particles due to increases in pressure. Regional metamorphism causes compaction and possibly recrystallization, increasing the density of the rock.
Regional Metamorphism
contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.
contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.
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
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.
regional metamorphism occurs over a large area while local metamorphism occurs over a small area.
Regional 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.