continental slope
When tectonic plates collide and the direction of the forces is primarily perpendicular, the plates push up forming a mountain. The Himalayan Mountains are formed by the collision of two plates and are still growing. The summit of Mount Everest is, in fact, marine limestone.
sinks
A subduction zone is formed when two tectonic plates collide and one plate is forced beneath the other into the Earth's mantle. This process creates deep ocean trenches, volcanic arcs, and seismic activity.
A convergent boundary is formed when plates collide. At this type of boundary, the denser plate sinks beneath the less dense plate in a process known as subduction. This collision often results in the formation of mountain ranges, volcanoes, and deep ocean trenches.
It depends on the type of crust involved. If both plates carry oceanic crust, an ocean trench is formed along with a volcanic island are on the overriding plate. If one plate carries oceanic crust and the other continental, you will get an ocean trench, a continental volcanic arc, and a mountain range. If both plates carry continental crust, then a mountain range is formed.
volcanoes in an island arc
When plates collide it is called a convergent boundary.newtest3
When tectonic plates collide and the direction of the forces is primarily perpendicular, the plates push up forming a mountain. The Himalayan Mountains are formed by the collision of two plates and are still growing. The summit of Mount Everest is, in fact, marine limestone.
sinks
when two oceanic plates collide they create a deep-ocean trench, at deep-ocean trenches subduction occurs.
sinks
sinks
A subduction zone is formed when two tectonic plates collide and one plate is forced beneath the other into the Earth's mantle. This process creates deep ocean trenches, volcanic arcs, and seismic activity.
Mid - ocean ridges
Mid - ocean ridges
That is called subduction.
When tectonic plates collide and the direction of the forces is primarily perpendicular, the plates push up forming a mountain. The Himalayan Mountains are formed by the collision of two plates and are still growing. The summit of Mount Everest is, in fact, marine limestone.