A series of volcanic islands that form along a plate boundary is called an island arc. This occurs when one tectonic plate subducts beneath another, leading to magma rising to the surface and forming a chain of volcanic islands. Examples of island arcs include the Japanese archipelago and the Aleutian Islands.
it is on the indo-australian and eurasion plate boundary
The kind of plate boundary that moves apart is a Divergent Plate Boundary
Volcanic island arcs are typically associated with convergent plate boundaries, specifically where an oceanic plate subducts beneath another oceanic plate. This subduction process generates magma, which can rise to the surface, forming a chain of volcanic islands. Examples of volcanic island arcs include the Aleutian Islands in Alaska and the Japanese Archipelago.
A reef or low island.
The 'South Island'. A collision boundary.
Easter Island is located on a convergent plate boundary.
Easter Island is located on a convergent plate boundary.
landforms associated with divergent boundaries are known as island arc orogeny and they lead to formation of islands and volcanoes along with trenches. example would be Japanese island, aleutian island etc.
Its a divergent boundary
convergent boundary.
Easter Island is located on a hot spot, which is not a plate boundary. The hot spot has created a chain of volcanic islands, with Easter Island being one of them.
"Shima" is the Japanese word for island.
A series of volcanic islands that form along a plate boundary is called an island arc. This occurs when one tectonic plate subducts beneath another, leading to magma rising to the surface and forming a chain of volcanic islands. Examples of island arcs include the Japanese archipelago and the Aleutian Islands.
The island is an "island ark" formed at a destructive plate boundary.
'Shima' is "island" in Japanese, though in compound words it can become 'jima.'
Honshu.