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.
A deep ocean trench typically forms at a subduction zone, which is a convergent plate boundary where one tectonic plate is forced beneath another into the mantle. This process results in the formation of deep trenches in the ocean floor, such as the Mariana Trench in the western Pacific Ocean.
The Aleutian Trench was formed through the process of subduction, where the Pacific Plate is being forced beneath the North American Plate. This creates a deep trench in the ocean floor, and can lead to the formation of volcanic islands along the subduction zone.
Along their colliding (convergent) boundary.
A mountain range or trench can form at a convergent boundary. This is where two tectonic plates collide, causing one plate to be forced under the other (subduction) or where the plates crunch together to form a mountain range.
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.
A deep ocean trench typically forms at a subduction zone, which is a convergent plate boundary where one tectonic plate is forced beneath another into the mantle. This process results in the formation of deep trenches in the ocean floor, such as the Mariana Trench in the western Pacific Ocean.
spreading
A trench or trench system will form when tectonic plates move past each other horizontally along a fault line, causing one plate to be pushed downward. This movement can create deep trenches in the Earth's crust, such as the Mariana Trench in the Pacific Ocean.
No, it would form along a separating (divergent) tectonic plate boundary.
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 Acapulco Trench was formed at a convergent plate boundary where the Cocos Plate is subducting beneath the North American Plate. This subduction process created the trench and is associated with deep-sea trenches, volcanic arcs, and seismic activity.
The Aleutian Trench was formed through the process of subduction, where the Pacific Plate is being forced beneath the North American Plate. This creates a deep trench in the ocean floor, and can lead to the formation of volcanic islands along the subduction zone.
They formed to the west of the trench because that is where the submerged mountain range is. The islands are volcanic due to the water the islands carry under the Mariana plate.
Rebound tendency is when 2 plates from a convergent boundary slide past one another to form a trench
A mountain is an example of a possible result of converging plate boundaries. An actual example of a converging plate boundary would be the Indian-Eurasian Plate Boundarywhich is creating the Himalayan Mountain Range. Other convergent plates can create trenches such as the Mariana Trench, which is the lowest place on the surface of the Earth.
A divergent plate boundary