contact metamorphism, regional metamorphism, dynamic metamorphism
It is called contact metamorphism.
Contact metamorphism occurs next to an intrusion of molten magma. This type of metamorphism happens when hot magma comes into contact with existing rock, causing the rock to undergo changes in mineralogy and texture due to the heat and pressure.
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.
Burial metamorphism.
contact metamorphism, regional metamorphism, dynamic metamorphism
is level 3. or grades 1-3
Shale undergoes low-grade metamorphism to form slate, then phyllite, schist, and finally gneiss as metamorphic grade increases. This sequence is a result of increasing temperature and pressure conditions during metamorphism, leading to the formation of different minerals and textures in the rock. The progression from shale to gneiss represents a range of metamorphic grades and the increasing intensity of metamorphic processes.
The four types of metamorphism are contact metamorphism, regional metamorphism, dynamic metamorphism, and hydrothermal metamorphism. Contact metamorphism occurs near igneous intrusions, regional metamorphism happens over large areas due to tectonic forces, dynamic metamorphism occurs along fault zones, and hydrothermal metamorphism involves hot, circulating fluids altering rocks.
Grades 3, 5, 7 and 9.
The main types of rock metamorphism are contact metamorphism, regional metamorphism, and dynamic metamorphism. Contact metamorphism occurs when rocks are altered by heat and pressure from nearby magma. Regional metamorphism happens on a larger scale due to tectonic forces and deep burial. Dynamic metamorphism results from intense pressure along fault lines.
contact metamorphism, regional metamorphism, dynamic metamorphism
It is called contact metamorphism.
There is no grade of metamorphism beyond gneiss. Higher grades of metamorphism mean higher temperature and pressure. Beyond the conditions that form gneiss, temperatures are high enough to melt rock, at which point the resulting rock will be igneous rather than metamorphic.
Dynamic Metamorphism >.<
Regional Metamorphism
contact metamorphism is what happens when something is really hot. regional metamorphism on the other hand involves much larger packages of rocks.