Transform boundary
Convergent boundary
Contact metamorphism is least likely to occur at locations where there is little to no intrusion of magma near the Earth's surface. In areas with minimal igneous activity and no heat source to drive the metamorphic changes, contact metamorphism is less likely to take place. Generally, regions located far away from tectonic plate boundaries or volcanic hotspots are less prone to experiencing contact metamorphism.
When there is directed pressure on a rock, regional metamorphism may occur. This type of metamorphism occurs due to tectonic forces, such as continental collision or subduction, which result in high pressure and temperature conditions that alter the mineralogy and texture of the rock over large areas.
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.
When rocks grind and squeeze past each other due to tectonic forces, dynamic metamorphism can occur. This process can lead to the formation of mylonites, which are fine-grained rocks with a strong foliation formed from the intense deformation.
Dynamic Metamorphism >.<
Dynamic
Convergent boundary
dynamic
Contact metamorphism is least likely to occur at locations where there is little to no intrusion of magma near the Earth's surface. In areas with minimal igneous activity and no heat source to drive the metamorphic changes, contact metamorphism is less likely to take place. Generally, regions located far away from tectonic plate boundaries or volcanic hotspots are less prone to experiencing contact metamorphism.
Metamorphism can occur through contact metamorphism, where rocks are altered by heat from nearby magma; regional metamorphism, where rocks are subjected to high pressure and temperature over a large area; burial metamorphism, where rocks are subjected to increased pressure from being buried deep underground; and dynamic metamorphism, where rocks are deformed under high pressure but low temperature conditions along faults or shear zones.
When there is directed pressure on a rock, regional metamorphism may occur. This type of metamorphism occurs due to tectonic forces, such as continental collision or subduction, which result in high pressure and temperature conditions that alter the mineralogy and texture of the rock over large areas.
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.
When rocks grind and squeeze past each other due to tectonic forces, dynamic metamorphism can occur. This process can lead to the formation of mylonites, which are fine-grained rocks with a strong foliation formed from the intense deformation.
Along fault lines.
dynamic
Yes they do occur under volcanoes