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.
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.
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 Marianas (or Mariana) Trench is formed by the subduction of the Pacific Plate as it is forced under the smaller Mariana Plate at the bottom of the ocean between Japan and New Guinea.
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 plate boundary.
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The Mariana Trench is a convergent boundary, where two tectonic plates are colliding and one plate is forced beneath the other.
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 on two tectonic plates: The Pacific Plate and the Mariana Plate. The Pacific Plate is beneath the Mariana Plate by subduction.
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.
yes it was, the pacific plate is descending under the Eurasian plate
The Mariana Trench formed at a convergent boundary where the Pacific Plate is being subducted beneath the Mariana Plate. This process creates a deep oceanic trench, which is the deepest part of the world's oceans. The intense geological activity associated with subduction zones also leads to earthquakes and volcanic activity in the surrounding regions.
The Marianas (or Mariana) Trench is formed by the subduction of the Pacific Plate as it is forced under the smaller Mariana Plate at the bottom of the ocean between Japan and New Guinea.
The Mariana Trench is primarily associated with a subduction zone, which is a type of convergent boundary fault. Here, the Pacific Plate is being forced beneath the smaller Mariana Plate, resulting in the trench's formation. This subduction process is responsible for significant geological activity in the region, including earthquakes and volcanic activity.
Oceanic-oceanic convergent lead to the formation of Mariana Trench.