A transform plate boundary
Mount Adatara is associated with a convergent plate boundary, as are all of Japan's volcanoes.
Vesuvius is associated with a convergent boundary between the African Plate and the Eurasian Plate.
Kilauea is not associated with a plate boundary, it and the other Hawaiian volcanoes are the result of a hot spot.
Mountain formation is a feature associated with a continental plate boundary, where the collision of two continental plates results in the uplift of the Earth's crust, creating mountain ranges such as the Himalayas.
The plate boundary between the Nazca Plate and the South American Plate does produce volcanoes, earthquakes, and tsunamis. Hurricanes have nothing to do with plate boundaries.
The type of boundary associated with Icelandic volcanoes is the constructive plate boundary, where two plates slowly move apart and magma seeps up through the gap.
Mount Adatara is associated with a convergent plate boundary, as are all of Japan's volcanoes.
Vesuvius is associated with a convergent boundary between the African Plate and the Eurasian Plate.
No. A volcano is not a plate boundary. Most volcanoes on land are associated with convergent boundaries, but many are associated with divergent boundaries and others with hot spots.
Kilauea is not associated with a plate boundary, it and the other Hawaiian volcanoes are the result of a hot spot.
Mountain formation is a feature associated with a continental plate boundary, where the collision of two continental plates results in the uplift of the Earth's crust, creating mountain ranges such as the Himalayas.
Most volcanoes of any type, including cinder cones, are found at plate boundaries, but some are associated with hot spots.
The Transform plate boundary commonly forms a chain of volcanoes - Professer Humifiken
convergent oceanic oceanic
The plate boundary between the Nazca Plate and the South American Plate does produce volcanoes, earthquakes, and tsunamis. Hurricanes have nothing to do with plate boundaries.
Such volcanoes are hot spot volcanoes.
Volcanoes on continents can develop at path convergent and divergent boundaries. They can occur where an oceanic plate subducts under a continental plate, producing a volcanic arc such as in the Cascade Range. Volcanoes can also occur in areas of rifting, such as Africa's Great Rift Valley, a developing divergent boundary. Where two oceanic plates converge volcanoes can develop underwater and eventually form volcanic islands. Volcanoes can also develop away from a plate boundary over a hot spot.