usually it is mountains
All boundaries produce seismic activity, however convergent and transform boundaries have the most activity.
Earthquakes and volcanoes are hazards typically associated with convergent boundaries where tectonic plates collide. Mountains can also form at convergent boundaries due to the collision of plates. Trenches are associated with subduction zones at convergent boundaries where one plate is forced beneath another. Mudslides are not directly related to convergent boundaries.
convergent
Convergent boundaries occur continuously along tectonic plate boundaries. The most recent significant convergent boundary activity can be observed today along subduction zones, such as the Pacific Ring of Fire, where one plate is being forced beneath another. This ongoing process results in seismic and volcanic activity.
Earthquakes are produced at all types of plate boundaries: convergent boundaries, where plates collide; divergent boundaries, where plates separate; and transform boundaries, where plates slide past each other. The release of stress along these boundaries can result in seismic activity.
The two types of convergent boundaries are oceanic-continental and continental-continental. At oceanic-continental convergent boundaries, an oceanic plate subducts beneath a continental plate, leading to volcanic activity and the formation of mountain ranges. In contrast, at continental-continental convergent boundaries, two continental plates collide, resulting in the uplift of mountain ranges without significant subduction. These interactions are responsible for significant geological features and seismic activity.
Convergent boundaries are where two tectonic plates hit each other. This can cause earthquakes, but can also create mountains.
hot spots and convergent boundaries
Yes, volcanism is found at both convergent and divergent boundaries of tectonic plates. At convergent boundaries, subduction zones can result in the formation of volcanoes due to the melting of subducted crust. At divergent boundaries, magma rises to the surface to create new crust, leading to volcanic activity as seen in mid-ocean ridges.
An example of convergent plate boundaries on earth is the Himalayas. :)
convergent boundaries collide but divergent boundaries move away from each other.
Convergent boundaries, where tectonic plates collide, can cause volcanic activity due to the subduction of one plate beneath another. This process can lead to the formation of volcanic island arcs, such as Japan or the Aleutian Islands.