It is a process called ridge push.
Volcanoes are located often near trenches because when two tectonic plates collide at a convergent boundary, the denser plate slides under the other plate. As the denser plate bends, a deep depression known as a trench forms. At a trench, one plate moves downward into the mantle. As the plate moves farther downward into Earth's mantle, the rock is subjected to greater heat and pressure. As a result, the plate releases fluids, which causes surrounding rock to melt. This as you know is a volcano.
New crust is formed on the opposite end of the plate as it is pulled away from its neighbor
Subduction.
Ultimately gravity.A2. In a scree or talus, the rocks will fall to eventually come to rest. The driving force is gravity.In a stream, they will be borne easily in steeper streams but in a stream of shallow angle, their movement will be slight. Indeed their only movement may be in a flood. The material will become more worn down as it proceeds downstream. But the force moving the water is still gravity.
An earth plate is a plate you equip to arceus to make its ground type moves.
ridge push
Well rifts do the pushing, but gravity does the downward motion causing the melting.
gravity slab pull
Volcanoes are located often near trenches because when two tectonic plates collide at a convergent boundary, the denser plate slides under the other plate. As the denser plate bends, a deep depression known as a trench forms. At a trench, one plate moves downward into the mantle. As the plate moves farther downward into Earth's mantle, the rock is subjected to greater heat and pressure. As a result, the plate releases fluids, which causes surrounding rock to melt. This as you know is a volcano.
One theory is that gravity pulls the old heavier ocean floor with more force than the newer lighter sea floor.
In theory an earthquake moves enough matter quickly enough to create a gravity wave, but in practice, that gravity wave is much too weak for us to detect at our present level of technology.
New crust is formed on the opposite end of the plate as it is pulled away from its neighbor
Subduction.
A destructive plate boundary.
New crust is formed on the opposite end of the plate as it is pulled away from its neighbor.
The Indo-Australian plate moves Northeast as the Pacific Plate moves around it in a Northwest direction as if rotating.
Heat, pressure, weather, gravity, plate tectonics--all play a part in the rock cycle.