convergent boundaries are easy to find most of them are found in the ocean. One Famous convergent plate boundary would be the Sunda Double Trench. It is found in the Indian ocean and it reaches a depth of 24,440 feet. It is the deepest trench in the Indian Ocean.
convergent boundaries collide but divergent boundaries move away from each other.
convergent
Trenches are formed at convergent plate boundaries involving at least one oceanic plate, where the more dense plate subducts under the less dense plate.
A reverse fault
A compressional bounday is plate boundarys that are being compressed
Cool
Chances Peak, which is part of the Soufrière Hills volcano, is located on the Caribbean plate boundary in the Caribbean region. The volcano is situated at the convergent boundary where the Caribbean plate is being subducted beneath the North American plate.
Oceanic-Continental Convergence - Andean-Type - the Andes MountainsOceanic-Oceanic Convergence - Aleutian-Type - island arcsContinental-Continental Convergence - the Appalachian Mountains
divergent plate boundary- a boundary where two plates move apart from each other. convergent plate boundary- a boundary where two plates move towards each other so that one plate can sink beneath the other. transform plate boundary- a boundary where one plate slips along side another plate.
Divergent plate boundaries typically produce smaller earthquakes compared to convergent plate boundaries, where tectonic plates collide. At divergent boundaries, tectonic plates move apart, creating new crust, which generally results in less intense seismic activity. In contrast, convergent boundaries often involve subduction, leading to significant stress accumulation and larger earthquakes. Therefore, the largest earthquakes are generally associated with convergent, rather than divergent, plate boundaries.
Tensional stress
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.