convergent
The most common type of land metamorphism is Regional metamorphism. The most common rocks are slates, schists, and gneisses. This occurs within the folds of mountain belts and cratonic areas.
Destructive plate boundaries.
Contact metamorphism
at convergent plate boundries
Convergent plate boundary.
The type of plate boundary that regional metamorphism is associated with convergent plate boundaries. A convergent boundary is also known as a destructive plate boundary due to subduction.
convergent plate boundaries
The most common type of land metamorphism is Regional metamorphism. The most common rocks are slates, schists, and gneisses. This occurs within the folds of mountain belts and cratonic areas.
Destructive plate boundaries.
Contact 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.
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.
at convergent plate boundries
The boundary where a trench can be found is called a convergent plate boundary. It can also be termed a destructive plate boundary in plate tectonics.
transform, divergent, convergent, and hot spots
Regional metamorphism is the creation of metamorphic rock from large geographically significant processes like plate tectonics. Contact metamorphism is the creation of metamorphic rock from the proximity of an existing rock to a heat source provided by a plutonic intrusion.
Convergent plate boundary.