When plates are different densitys and collide to make volcanoes.
subducting
The Aleutian Islands are located at a convergent boundary, where the Pacific Plate is subducting beneath the North American Plate. This geological process creates volcanic activity and leads to the formation of the islands. The ongoing convergence results in significant earthquakes and volcanic eruptions in the region.
Convergence Boundary.
Convergence Boundary.
Yes, subducting plate boundaries are a type of convergent plate boundary where one tectonic plate moves under another plate. Convergent plate boundaries, in general, are locations where two tectonic plates move towards each other. Subduction is a specific mechanism of convergence.
A subducting ocean plate is a tectonic plate that is moving beneath another plate at a convergent boundary. As it moves, the subducting plate is forced down into the Earth's mantle, creating a subduction zone. This process can lead to volcanic activity, earthquakes, and the formation of deep ocean trenches.
Convergence plate boundary between the Eurasian Plate and the Indian Plate.
Reventador volcano is located on the South American Plate boundary where the Nazca Plate is subducting beneath it. This type of plate boundary is known as a convergent boundary.
non boundary mountains
A Convergence Boundary.
An oceanic-continental convergence typically results in the oceanic plate subducting beneath the continental plate due to its higher density. This can lead to the formation of volcanic mountain ranges on the continental plate, as magma generated by the subducted plate rises to the surface and forms volcanoes. Additionally, intense seismic activity and the potential for tsunamis can also be associated with this type of plate boundary.
It is not on a plate boundary. Therefore it may be on hotspot.