trenches trenches
Plates do not cause volcanoes. Volcanoes generally form at the boundaries between plates. They form at convergent and divergent boundaries.
divergent
dining table plates
Earthquakes can occur at tectonic plate boundaries, such as convergent boundaries where plates collide, divergent boundaries where plates move apart, and transform boundaries where plates slide past each other. The stress from the movement of these plates can cause the crust to fracture and release energy in the form of an earthquake.
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Volcanoes form on tectonic plates at plate boundaries where magma from the Earth's mantle can rise to the surface. This typically occurs at divergent or convergent plate boundaries where there is movement and interaction between the plates, leading to volcanic activity.
Collision boundaries form at tectonic plate boundaries where two plates are either converging, diverging, or sliding past each other. These boundaries are categorized as convergent boundaries, divergent boundaries, and transform boundaries, respectively.
Earthquakes are most likely to occur near tectonic plate boundaries, where tectonic plates interact and cause stress to build up and release in the form of seismic activity. These boundaries include convergent boundaries where plates collide, divergent boundaries where plates separate, and transform boundaries where plates slide past each other.
Some landforms that can form independent of plate boundaries include volcanoes that form over hot spots in the middle of plates, rift valleys that form at divergent boundaries within plates, and dome mountains that form from uplift and erosion processes.
mountains are made when the crust folds, tilts ,and lifts as a result of this meeting of plates.
Mountains usually form on plate boundaries, where two tectonic plates collide and force the ground upward. There are very few volcanic mountains, such as the Hawaiian Islands, that form in the middle of the plates.
Volcanic mountains commonly form along plate boundaries, specifically at subduction zones where oceanic plates sink beneath continental plates or other oceanic plates. They can also form at divergent boundaries where plates move away from each other, allowing magma to rise to the surface and create volcanic activity.