The Mariana Trench is a convergent plate boundary.
yes it was, the pacific plate is descending under the Eurasian plate
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 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.
In this region, where the western subducting edge of the Pacific plate plunges beneath the Philippine plate, is found the most volcanically active convergent plate boundary on Earth.
Convergent plate boundary.
The Mariana Islands are associated with a convergent plate boundary, specifically a subduction zone where the Pacific Plate is being subducted beneath the Mariana Plate. This process has led to the formation of the Mariana Trench, the deepest part of the world's oceans, and volcanic activity in the region that created the islands.
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).
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Convergent boundary Convergent boundary
convergent plate boundary and the pacific plate