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.
Volcanic arcs form at plate subduction zones. Island arcs are volcanic islands that form over "hot spots" in the Earth's mantle. Because the islands are moving with the oceanic plate, they eventually are removed from the hot spot, forming a chain of islands in the direction of the plate movement.
The American islands that are actually an underwater chain of volcanoes are the Hawaiian Islands. These islands were formed by volcanic activity from the Hawaiian-Emperor seamount chain. The islands of Hawaii, Maui, Oahu, Kauai, and others are all part of this volcanic chain.
A volcanic island arc is formed when an oceanic tectonic plate subducts beneath another oceanic plate. This subduction process leads to the melting of the subducted plate, resulting in magma that rises to the surface and creates volcanic islands. These islands typically form in a curved chain, parallel to the trench created by the subduction zone. Over time, repeated volcanic activity can build up a significant landmass above sea level.
Hawaii.
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 Aleutian Islands.
japan
Aleutian Islands
A chain of 14 large volcanic islands and 55 smaller ones form the Aleutian Islands.
If it is a single island, it is simply known as a volcanic island! If however it is a chain or string of separate islands then it may be a volcanic island arc (these form parallel to trenches at subduction zones) or a volcanic island chain (these form where a mantle plume creates a hotspot and may be in the centre of a tectonic plate. A good example would be the Hawaiian island chain). They can also form a cluster of islands (an archipelago) such as the Canary Islands (again formed by hotspot volcanism) in the Atlantic of the coast of Morocco.
An island arc is a curved chain of volcanic islands that typically forms along convergent tectonic plate boundaries, where an oceanic plate subducts beneath another oceanic plate. These arcs are characterized by volcanic activity, often resulting in the formation of stratovolcanoes, and are usually found parallel to the trench created by the subduction process. The islands often exhibit steep topography and are associated with earthquakes due to the tectonic activity in the region. Common examples include the Aleutian Islands and the Japanese Archipelago.
The Aletian Islands.