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it is on the indo-australian and eurasion plate boundary
Yellowstone is situated within a tectonic plate, not at a plate boundary! Volcanic activity is thought to be as a result of a mantle plume, much like the volcanism that created the Hawaiian Island chain.
White Island Volcano is located on a convergent plate boundary where the Pacific Plate subducts beneath the Australian Plate. This subduction process generates magma that fuels volcanic activity on the island.
Mount Tambora was formed by a convergent plate boundary. It is located on the Indonesian island of Sumbawa, where the Australian Plate converges with the Sunda Plate, causing subduction and volcanic activity in the region.
Surtsey (part of an island group off SW Iceland) is on constructive plate boundaries, which means the two plates move away from each other and magma rises to the surface. This is how a volcano like Surtsey is formed.
Eldfell is located on a divergent plate boundary, specifically along the Mid-Atlantic Ridge on the island of Heimaey in Iceland.
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.
it is on the indo-australian and eurasion plate boundary
Yellowstone is situated within a tectonic plate, not at a plate boundary! Volcanic activity is thought to be as a result of a mantle plume, much like the volcanism that created the Hawaiian Island chain.
White Island Volcano is located on a convergent plate boundary where the Pacific Plate subducts beneath the Australian Plate. This subduction process generates magma that fuels volcanic activity on the island.
Mount Tambora was formed by a convergent plate boundary. It is located on the Indonesian island of Sumbawa, where the Australian Plate converges with the Sunda Plate, causing subduction and volcanic activity in the region.
Surtsey (part of an island group off SW Iceland) is on constructive plate boundaries, which means the two plates move away from each other and magma rises to the surface. This is how a volcano like Surtsey is formed.
Easter Island is located on a convergent plate boundary.
The Mid-Atlantic Ridge (MAR) is a mid-ocean ridge, a divergent tectonic plate boundary located along the floor of the Atlantic Ocean, and part of thelongest mountain range in the world. It separates the Eurasian Plate and North American Plate in the North Atlantic, and the African Plate from the South American Plate in the South Atlantic. The Ridge extends from a junction with the Gakkel Ridge (Mid-Arctic Ridge) northeast of Greenland southward to theBouvet Triple Junction in the South Atlantic. Although the Mid-Atlantic Ridge is mostly an underwater feature, portions of it have enough elevation to extend above sea level. The section of the ridge which includes the island of Iceland is also known as the Reykjanes Ridge. The average spreading rate for the ridge is about 2.5 cm per year.[1]en.wikipedia.org/wiki/Mid-Atlantic_Ridge
Easter Island is located on a convergent plate boundary.
In plate tectonics, a Divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other. These areas can form on the end of continents but eventually form ocean basins. Divergent boundaries within continents initially produce rifts which produce rift valleys. Therefore, most active divergent plate boundaries are between oceanic platesand are often called mid-oceanic ridges. Divergent boundaries also form volcanic islands which occur when the plates move apart to produce gaps which molten lava rises to fill. Thus creating a shield volcano which would eventually build up to become a volcanic island.
The 'South Island'. A collision boundary.