Ocean trenches, volcanic arcs, mountains, uplands, and volcanic islands.
When two tectonic plates collide, it can form various geological features such as mountain ranges, earthquakes, and volcanic activity. The specific features that form depend on the types of plates involved and the specific boundaries at the collision zone.
When two tectonic plates collide, compressional stress occurs. This stress causes the rocks to fold and deform, leading to the formation of mountain ranges, such as the Himalayas. The intense pressure and friction between the plates can also result in earthquakes and volcanic activity.
A convergent plate movement occurs when two tectonic plates collide with each other. This typically happens at subduction zones, where one plate is forced beneath the other due to differences in density. This can create mountains, earthquakes, and volcanic activity.
When two oceanic plates collide, one may be pushed under the other and cause magma from the mantle to rise, forming a volcanoe or volcanoes. When two continential plates collide at a reverse fault tectonic earthquakes occur.
They are called rift volcanoes.
A subduction zone is a convergent boundary where two tectonic plates collide.
The movement or action of the plate determines what type it is. When two plates collide, they are creating a convergent boundary. Therefore you could state that they are convergent (or colliding) tectonic plates.
Overlapping portions of two continents are known as continental plates or tectonic plates. These plates can collide, separate, or slide past each other due to the movement of the Earth's tectonic plates.
convergence
they collide and create earthquake
when two oceanic plates collide they create a deep-ocean trench, at deep-ocean trenches subduction occurs.
Most earthquakes occur at the boundaries of the tectonic plates. Tectonic plates are always in motion, and when two of them collide with one another it causes earthquakes.