convergent oceanic oceanic
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.
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.
The two boundaries responsible for the volcanoes along the Cascade Range are the subduction zone between the Juan de Fuca Plate and the North American Plate, causing the Cascade Volcanic Arc, and the boundary between the Pacific Plate and the Juan de Fuca Plate, triggering the formation of the Juan de Fuca Ridge.
The two major plate boundaries that cause volcanoes to exist along the Cascade Range in the Pacific Northwest are the convergent boundary between the Juan de Fuca Plate and the North American Plate, and the divergent boundary where the Juan de Fuca Plate is being subducted beneath the North American Plate. These tectonic processes lead to magma generation and volcanic activity in the region.
The Cascade Mountains are primarily located along the boundary between the Juan de Fuca Plate and the North American Plate. This boundary is a convergent plate boundary, where the Juan de Fuca Plate is subducting beneath the North American Plate, leading to the formation of the Cascade Range through volcanic activity.
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.
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.
The two boundaries responsible for the volcanoes along the Cascade Range are the subduction zone between the Juan de Fuca Plate and the North American Plate, causing the Cascade Volcanic Arc, and the boundary between the Pacific Plate and the Juan de Fuca Plate, triggering the formation of the Juan de Fuca Ridge.
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.
The two major plate boundaries that cause volcanoes to exist along the Cascade Range in the Pacific Northwest are the convergent boundary between the Juan de Fuca Plate and the North American Plate, and the divergent boundary where the Juan de Fuca Plate is being subducted beneath the North American Plate. These tectonic processes lead to magma generation and volcanic activity in the region.
Kilauea is not associated with a plate boundary, it and the other Hawaiian volcanoes are the result of a hot spot.
I have a strong feeling it is cascade range.
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.