oceanic
The two different types of islands are oceanic and continental
Subduction zones, trenches and volcanic islands: the boundary that is oceanic. Trenches and volcanic islands: an oceanic-continental boundary. Folded mountain ranges: a continental and continental collision.
oceanic- continental boundary
Oceanic-Oceanic.
The continental islands, Oceanic islands, and the Atolls.
The continental islands, Oceanic islands, and the Atolls.
at an oceanic to continental convergent boundary trenches and volcanic mountains can form. at an oceanic to oceanic convergent boundary trenches and volcanic islands can form. at a continental to continental convergent boundary fold mountains can form
A convergent boundry, when an oceanic plate and a continental plate collide.
Oceanic-Continental, Oceanic-Oceanic, and Continental-Continental.
When two crustal plates are in the process of collision they deform, the results of which vary:continental-continental, large mountain building (e.g. asia-india building the himalayas)oceanic-oceanic, island arc building with volcanic islands (e.g. the Japanese islands)oceanic-continental, subduction of oceanic plate under continental plate with inland volcanoes (e.g. volcanoes in Washington, Oregon, and northern California)
Oceanice oceanic has a trench, which is usually the deepest part of the ocean. It also has a volcanic island. That is how Islands are found in the center of oceans. oceanic convergent has similar features but do not have islands but instead volcanic arc on the continents.
Some Islands are parts of continents (high points in the continental shelf) eg The British Isles. Some Islands are parts of continents that have become detached during continental drift (eg Seychelles or Madagascar) Some Islands are unrelated to continents and result from oceanic plate processes (eg Hawaii). Some Islands are a result of the interaction between continental and oceanic plates (eg some of the Caribbean Islands, Japan and Cyprus).