What is the difference between regional contact and dynamic metamorphism?
Regional metamorphism usually produces foliated rocks such as gneiss and schist. Dynamic Metamorphism also occurs because of mountain-building. These huge forces of heat and pressure cause the rocks to be bent, folded, crushed, flattened, and sheared.
What is the difference between regional and contact metamorphism include a simple sketch showing the difference?
0:033:14Contace & Regional Metamorphism – YouTubeYouTubeStart of suggested clipEnd of suggested clipThe first type is called contact metamorphism. And the second is called regional metamorphism. SoMoreThe first type is called contact metamorphism. And the second is called regional metamorphism. So let's talk a little bit about the difference between these two.
What are the 2 types of metamorphism?
There are two major kinds of metamorphism: regional and contact. Regional metamorphism. Most metamorphic rocks are the result of regional metamorphism (also called dynamothermal metamorphism). These rocks were typically exposed to tectonic forces and associated high pressures and temperatures.
What is contact metamorphism?
Contact metamorphism. This is metamorphism produced by intrusion of magma. Heat and fluids from the crystallizing magma cause chemical and mineralogical changes in the rocks being intruded.
What is meant by regional metamorphism?
( rē′jə-nəl ) A type of metamorphism in which the mineralogy and texture of rocks are changed over a wide area by deep burial and heating associated with the large-scale forces of plate tectonics.
What is regional metamorphic rock?
Regional metamorphic rocks occur where rocks are altered by high temperatures and / or high pressures usually deep within the Earth. Regional metamorphism can affect large volumes of the crust and typically happens at convergent plate boundaries, beneath new mountain ranges.
What are contact metamorphic rocks?
Contact metamorphic rocks form when rocks are heated to high temperatures, usually through contact with an igneous intrusion at a relatively low pressure. The effects of contact metamorphism usually only extend for a short distance from the cooling igneous rock that is providing the heat.