the top part of the boundary it creates the the deep ocean trench along with the edge of a continent......:D
convergent
The Mariana Trench was formed along a convergent boundary where two tectonic plates are colliding. More specifically, it was created by the subduction of the Pacific Plate beneath the smaller Mariana Plate in a process known as plate tectonics.
The boundary between the Indo-Australian Plate and the Pacific Plate is mainly a divergent boundary in the region of the East Pacific Rise and a transform boundary along the Tonga Trench and the Alpine Fault in New Zealand. Additionally, there are some regions of convergence near New Zealand and the New Hebrides Trench.
The type of plate boundary along the Peru-Chili trench is the convergent type which is acting between the Nazca plate and the South American plate Md. Rafiqul Islam, PhD Assistant Professor Dept. of Petroleum & Mining Engineering Shahjalal University of Science & Technology Sylhet-3114, Bangladesh
Guatemala City is located approximately 75 miles (120 kilometers) away from the closest plate boundary, which is the subduction zone along the Middle America Trench where the Cocos Plate is subducting beneath the Caribbean Plate.
convergent
trench
If a deep ocean trench is located adjacent to a continent, active volcanoes would likely be found on the continent's edge or along the tectonic plate boundary. These volcanoes are often associated with subduction zones where one tectonic plate is being pulled beneath another, leading to magma generation and volcanic activity.
The Mariana Trench was formed along a convergent boundary where two tectonic plates are colliding. More specifically, it was created by the subduction of the Pacific Plate beneath the smaller Mariana Plate in a process known as plate tectonics.
The boundary between the Indo-Australian Plate and the Pacific Plate is mainly a divergent boundary in the region of the East Pacific Rise and a transform boundary along the Tonga Trench and the Alpine Fault in New Zealand. Additionally, there are some regions of convergence near New Zealand and the New Hebrides Trench.
The Aleutian Trench is located in the Pacific Ocean, stretching along the southern coastline of Alaska and the Aleutian Islands. It marks the boundary where the Pacific Plate is subducting beneath the North American Plate.
Subduction happens along plate boundaries which pushes up magma which then creates volcanoes.
The type of plate boundary along the Peru-Chili trench is the convergent type which is acting between the Nazca plate and the South American plate Md. Rafiqul Islam, PhD Assistant Professor Dept. of Petroleum & Mining Engineering Shahjalal University of Science & Technology Sylhet-3114, Bangladesh
A collisional plate boundary along which one lithospheric plate overrides another and produces a deep-sea trench, a volcanic arc, and seismicity.
Guatemala City is located approximately 75 miles (120 kilometers) away from the closest plate boundary, which is the subduction zone along the Middle America Trench where the Cocos Plate is subducting beneath the Caribbean Plate.
Hekla volcano is located along a divergent plate boundary in Iceland, where the North American and Eurasian plates are moving apart. This movement creates rift zones where volcanic activity is common, including Hekla.
Along the southern coast of Alaska is the Aleutian Trench.