A convergent plate boundary.
The Mariana Trench is a convergent boundary, specifically a subduction zone, where the Pacific Plate is being subducted beneath the Mariana Plate. This results in the trench being the deepest part of Earth's ocean.
The Mariana Trench is a convergent boundary, where two tectonic plates are colliding and one plate is forced beneath the other.
Mid-Atlantic Trench
A convergent plate boundary causes a trench to form. This occurs when two tectonic plates collide, with one plate sinking beneath the other due to its greater density. This process creates a deep trench in the Earth's crust.
The boundary between the Philippines and Pacific plates is a convergent boundary, specifically a subduction zone where the denser oceanic Philippines Plate is being pushed beneath the lighter Pacific Plate. This subduction process is responsible for the formation of the Philippine Trench and associated volcanic activity in the region.
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A convergent plate boundary creates a deep ocean trench along the edge of a continent. In this boundary type, an oceanic plate is forced beneath a continental plate, leading to the formation of the trench due to subduction.
The Mariana Trench is a convergent boundary, specifically a subduction zone, where the Pacific Plate is being subducted beneath the Mariana Plate. This results in the trench being the deepest part of Earth's ocean.
The Mariana Trench is a convergent boundary, where two tectonic plates are colliding and one plate is forced beneath the other.
Mid-Atlantic Trench
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.
A convergent plate boundary causes a trench to form. This occurs when two tectonic plates collide, with one plate sinking beneath the other due to its greater density. This process creates a deep trench in the Earth's crust.
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
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.
Near the Aleutian Trench, you would expect to find a convergent boundary. This type of boundary occurs where an oceanic plate is subducting beneath another oceanic plate or a continental plate. The subduction process leads to the formation of deep ocean trenches and volcanic arcs, characteristic of the Aleutian Islands, which are a result of the associated volcanic activity.
A Transform Fault ZoneIn the textbook Earth Science and the Environment (4th Edition) by Thompson and Turk. Located on page 163, it shows that Tonga has a Convergent Boundary. A convergent boundary is where two lithospheic plates collide head on.
"subduction"