Oceanic-to-Oceanic plate boundary triggers the formation of active volcanoes as magma rises beneath the surface.
Transform plate boundaries trigger the formation of active volcanoes as magma rises beneath the surface.
Ocean to ocean convergent plate boundaries do not have a chain of composite cone volcanoes. The ocean plate that is more dense will sink beneath the other ocean plate.
Volcanoes.
Seamounts
Convergent oceanic-continental boundary
Pocket of magma beneath the surface
Ocean to ocean convergent plate boundaries do not have a chain of composite cone volcanoes. The ocean plate that is more dense will sink beneath the other ocean plate.
Movement of lithospheric plates at convergent boundaries can result in the subduction of one plate beneath another. This subduction creates conditions for magma to form as the subducting plate melts. The rising magma then reaches the surface, leading to the formation of volcanoes.
Volcanoes.
yes
yes
Seamounts
This kind of boundary is mountainous.
Convergent oceanic-continental boundary
Pocket of magma beneath the surface
The theory of plate tectonics suggests that the Earth's lithosphere (outermost layer) is divided into several large plates that move and interact with each other. When two plates collide, one may be forced beneath the other (subduction) and may melt to form magma. This can lead to the formation of volcanoes on the Earth's surface. Mountains can form when two plates collide, but neither is forced beneath the other, instead, they push against each other and the resulting pressure and folding can uplift the Earth's crust and form mountain ranges. The movement and interactions of these plates over time have shaped the Earth's surface, including the formation of mountains and volcanoes.
Submarine volcanoes can also be called "shield volcano," they are volcanoes that are underwater. There is one volcano that is half underwater and half over-water.That volcano is called "Bora Bora."
Subduction is when one of the plates is forced down beneath the other plate at the convergent boundary.