The Mariana Trench is a convergent plate boundary.
The Mariana Trench is a convergent boundary, where two tectonic plates are colliding and one plate is forced beneath the other.
Mariana Trench
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 located at a convergent plate boundary where the Pacific Plate is subducting beneath the smaller Mariana Plate. This subduction zone is one of the deepest parts of the Earth's oceans, where the oceanic crust is being forced down into the mantle.
Examples of convergent boundaries include the Himalayan mountain range (where the Indian Plate is colliding with the Eurasian Plate), the Andes mountain range (where the South American Plate is subducting under the Nazca Plate), and the Mariana Trench (where the Pacific Plate is subducting beneath the Mariana Plate).
The Mariana Trench is a convergent plate boundary.
The Mariana Trench is a convergent boundary, where two tectonic plates are colliding and one plate is forced beneath the other.
convergent
Mariana trench
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.
Mariana Trench
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.
Oceanic-oceanic convergent lead to the formation of Mariana Trench.
The Mariana Trench is the deepest part of the world's oceans, located in the western Pacific Ocean. It is associated with tectonic plates because it is formed at a subduction zone, where one tectonic plate is being forced beneath another. This process creates the extreme depths and unique geologic features found in the Mariana Trench.
yes it was, the pacific plate is descending under the Eurasian plate
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 located at a convergent plate boundary where the Pacific Plate is subducting beneath the smaller Mariana Plate. This subduction zone is one of the deepest parts of the Earth's oceans, where the oceanic crust is being forced down into the mantle.