An ocean trench does not become a volcanic island, however volcanic islands often form near ocean trenches.
If an ocean trench is located west of volcanic islands, you can assume that there is a continental shelf nearby. You can also assume that the trench is at least 7000Êm deep.
The definition of the word island arc is " a curved chain of volcanic islands located at a tectonic plate margin, typically with a deep ocean trench on the convex side."
The chain of volcanic islands that form parallel to a deep ocean trench is known as an island arc. These arcs are created by the subduction of one tectonic plate beneath another, leading to melting of the mantle and formation of magma that rises to the surface. Common examples include the Aleutian Islands in Alaska and the Japanese archipelago. Island arcs are characterized by their volcanic activity and often have a curved shape.
A Volcanic Island is an island that was made from volcanoes erupting from the ocean floor.
The Mariana Trench is located south of Japan and east of China, in the northern Pacific Ocean, near the island of Guam.
volcanic island arcs
A seamount is an underwater mountain formed by volcanic activity, while a volcanic island is a landmass that rises above the ocean's surface due to volcanic eruptions. Seamounts can eventually grow to become volcanic islands if the volcanic activity continues and brings the seamount above the water level.
it is a string of islands formed above a deep ocean trench
It depends on the type of crust involved. If both plates carry oceanic crust, an ocean trench is formed along with a volcanic island are on the overriding plate. If one plate carries oceanic crust and the other continental, you will get an ocean trench, a continental volcanic arc, and a mountain range. If both plates carry continental crust, then a mountain range is formed.
Hawaii is a volcanic island, formed by volcanic activity millions of years ago. It is part of a volcanic island chain in the Pacific Ocean.
When an oceanic to oceanic happens, two oceanic plates converge and one of the plates subducts into a trench. The subducted plate sinks down into the mantle and begins to melt. Molten rock from the plate rises toward the surface and forms a chain of volcanic islands, also called a volcanic island arc, behind the trench in the ocean.
First of all there are different kinds of sea mounts, in reference to your question it would have to be a volcanic sea mount to begin with. It would become a volcanic island by continuing to erupt until it broke the surface of the ocean. Some excellent examples of volcanic sea mounts that became volcanic islands are the Hawaiian Islands