The 3 general types are constructive, destructive, and conservative boundaries.
Constructive (divergent) - plates move away from each other, typically creating a rift
Destructive (convergent) - one plate will be subducted, or continental plates collide
Conservative (transform) - plates grind past each other, stalling and slipping
Tensional stress
A compressional bounday is plate boundarys that are being compressed
Cool
they are mainly conservative plate boundaries but can be all but constructive plate boundarys by callum 11
The Phillipine and Pacific plate boundarys are Convergant.A destructive plate boundary.
they occur i think in the plate boundarys.
The Phillipine and Pacific plate boundarys are Convergant.A destructive plate boundary.
Trenches are formed at convergent plate boundaries involving at least one oceanic plate, where the more dense plate subducts under the less dense plate.
Oceanic-Continental Convergence - Andean-Type - the Andes MountainsOceanic-Oceanic Convergence - Aleutian-Type - island arcsContinental-Continental Convergence - the Appalachian Mountains
well mostly along plate boundarys but there can be "hot spots" in the mantle that magma come out of. for ex:hawii is right over a hot spot well mostly along plate boundarys but there can be "hot spots" in the mantle that magma come out of. for ex:hawii is right over a hot spot
Chances Peak, which is part of the Soufrière Hills volcano, is located on the Caribbean plate boundary in the Caribbean region. The volcano is situated at the convergent boundary where the Caribbean plate is being subducted beneath the North American plate.
The Philippines is located at the boundary of several tectonic plates, namely the Eurasian Plate, Philippine Sea Plate, and Pacific Plate. These plate boundaries contribute to the frequent seismic and volcanic activity in the region.