oceanic
The two main types of islands are continental islands, which are formed from the same landmass as a nearby continent, and oceanic islands, which are formed from underwater volcanic activity or coral reefs. Continental islands tend to be larger and closer to continents, while oceanic islands are typically smaller and more isolated.
Oceanic-Oceanic.
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.
The continental islands, Oceanic islands, and the Atolls.
The continental islands, Oceanic islands, and the Atolls.
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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)
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).
The main types of islands are continental islands, which are part of a continental shelf; oceanic islands, which are formed by volcanic activity; and coral islands, which are formed from coral reefs. There are also artificial islands, which are man-made structures typically created for expansion or development purposes.
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.
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
The three different types of convergent plate boundaries are oceanic-continental, oceanic-oceanic, and continental-continental. In an oceanic-continental boundary, the denser oceanic plate subducts beneath the less dense continental plate. In an oceanic-oceanic boundary, one oceanic plate subducts beneath another. In a continental-continental boundary, the plates collide and uplift, forming mountain ranges.