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 pacfic plate and n. American plate are moving away from each other, under the sea the point at which they meet is the subduction zone
convergent
Convergent
spreading
The chain of islands is formed by volcanic action along a fissure between Japan and Alaska. The fissure leis in "The Aleutian Trench" as seen in the diagram below in "Related links".
trench- valleys that form on the ocean floor where two plates come together, the deepest place in the ocean
aleutian trench
The Aleutian Trench is a tectonic plate boundary that is between the Aleutian Islands and Alaska. It is over 2000 miles in length.
No, the Marianas trench is.
Aleutian trench
Along the southern coast of Alaska is the Aleutian Trench.
It is about 20 million years old.
Subduction usually occurs in trenches, for example the Marriana's Trench or the Aleutian trench! Hope that Helps!
The Aleutian Islands were formed by the collision of tectonic plates. The islands lie along the boundary where the Pacific Plate is being pushed beneath the North American Plate in a process known as subduction. This tectonic activity has led to the creation of a chain of volcanic islands.
oceanic side of the Aleutian trench
Oceanic side of the Aleutian trench.
The latitude near the 180W longitude line intersects with the Aleutian Trench is ~50.5 degrees North.See related links for more information.Another answerThe approximate latitude is 52 degrees north and 172 degrees east. not west however it has different coordinates depending on what you want.
Convergent boundary Convergent boundary