They do if at least one of the plates is oceanic. If they are both continental, then a mountain range will form.
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 boundaries
No. Sea floor trenches are found at convergent boundaries. divergen boundaries form mid-ocean ridges.
trenches
Convergent plate boundaries
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 boundaries
No. Sea floor trenches are found at convergent boundaries. divergen boundaries form mid-ocean ridges.
trenches
Subduction zones, trenches and volcanic islands: the boundary that is oceanic. Trenches and volcanic islands: an oceanic-continental boundary. Folded mountain ranges: a continental and continental collision.
Convergent plate boundaries
Convergent boundaries form when two tectonic plates move toward each other and collide. This collision can result in the creation of mountain ranges, deep ocean trenches, and volcanic activity. Subduction zones, where one plate is forced beneath the other, are a common feature of convergent boundaries.
The locations of mountains, trenches, and volcanoes are primarily influenced by plate tectonics. Mountains form at convergent plate boundaries where plates collide and create uplift. Trenches are formed at subduction zones where one plate is forced beneath another. Volcanoes can occur at convergent boundaries, divergent boundaries, and hot spots where magma rises to the surface.
Three things that can form at convergent plate boundaries are mountain ranges, deep ocean trenches, and volcanic arcs.
The process that occurs at convergent boundaries is called subduction. This is when one tectonic plate moves under another, creating deep ocean trenches and often leading to volcanic activity and earthquakes.
There are three types of convergent boundaries: Oceanic, continental, and continental-oceanic convergent boundaries. Continental-continental convergent boundaries form mountain ranges. Continental-oceanic boundaries result in subduction zones and the recycling of lithosphere. The continental side of the boundary may form a mountain range. Oceanic-oceanic form deep oceanic trenches and sometimes volcanoes.
Compression stress is found at convergent boundaries, where two tectonic plates are moving towards each other. This stress can result in the formation of mountains, deep ocean trenches, and volcanic arcs.