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Regional rocks are formed when rocks are compacted tightly through heat and pressure.

Contact rocks are formed when minerals that lie next/by a hot magma pocket are fused together, but *AREN'T MELTED*.

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Compare and contrast contact metamorphism and 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.


Describe how contact metamorphism is different from regional metamorphism?

Contact metamorphism occurs when rocks are subjected to high temperatures and pressures due to being in close proximity to an igneous intrusion, leading to localized changes in mineralogy and texture. In contrast, regional metamorphism affects large areas of rocks over a wide region due to tectonic forces such as mountain building or subduction, resulting in widespread changes in mineralogy and texture. Contact metamorphism is therefore more localized and less intense compared to regional metamorphism.


Compare and contrast contact metamorphism and 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.


How is contact metamorphism different. from regional metamorphism?

contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.


How is contact metamorphism different from regional metamorphic?

contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.


How does Burial metamorphism differ from Regional and Contact 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.


Why are metamorphic rocks formed by contact metamorphism usually not dense or resistant?

Metamorphic rocks formed by contact metamorphism are usually not dense or resistant because they are formed at relatively low pressures and temperatures compared to regional metamorphism. The short duration of the heating process in contact metamorphism does not allow for the recrystallization and reorganization of mineral structures that contribute to denser and more resistant rocks. Additionally, the presence of fluids and gases in contact metamorphism can facilitate alteration and weakening of the original rock material.


How is metamorphism different from regional metamorphism?

contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.


What type of rock is contact and regional?

Contact and regional are terms used to describe two different types of metamorphic rocks. Contact metamorphism occurs when rocks are heated by nearby molten magma, leading to localized changes in mineralogy and texture. Regional metamorphism, on the other hand, involves larger-scale alterations due to high pressure and temperature over broad areas, often associated with tectonic processes like mountain building. Both types of metamorphism result in the formation of metamorphic rocks, which exhibit distinct characteristics from their parent rocks.


On on what basis can metamorphic rocks be identified?

Metamorphic rocks can be identified if the rock is foliated or nonfoliated, foliating type, type of metamorphism (contact/regional), and by probable original rock. :)


Which type of metamorphosis makes non-foliated rocks?

Contact metamorphism does not often produce the foliation caused by regional metamorphism


Where do dynamic contact and regional metamorphism occur?

Dynamic contact metamorphism occurs along tectonic plate boundaries where rocks come into contact with hot magma intrusions, while regional metamorphism occurs over large areas along convergent plate boundaries where high pressure and temperature conditions alter rocks deep within the Earth's crust.