The Nazca Plate and the South American Plate are colliding. Because oceanic plates like the Nazca are more dense than continental plates, they are forced below the continental plate and subduct, or flow downward into the mantle at varying degrees of descent from the area of collision!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
Mount hoot is formed by the Juan de Fuca Plate subducting under the North American Plate.
It was formed from the volcanism created by a subducting oceanic plate at a convergent plate boundary.
The Pacific Ring of Fire was formed due to the subduction of the Nazca Plate beneath the South American Plate, the Cocos Plate beneath the Caribbean Plate, the Pacific and Juan de Fuca Plate beneath the North American Plate, the Pacific Plate and Philippines Plate beneath the Eurasian Plate, the Indo-Australian Plate beneath the Eurasian Plate, and the Pacific Plate beneath the Indo-Australian Plate. This all occurs around the Pacific Ocean.
This was because part of the northward-moving African Plate is subducting beneath the Eurasian Plate. Trapped lava forms bubbles of gas as it gets near the surface. Pressure is released by coming to the surface. It bursts out as lava. Then layers build up to form the cone shape. There you go!
sand rocks :)
trenches
trenches
It was formed by the subduction of the Pacific Plate beneath the north American plate.
Mount hoot is formed by the Juan de Fuca Plate subducting under the North American Plate.
The Benioff Zone is formed when a piece of oceanic crust is being subducted into the mantle. This line of earthquakes follow the angle of the subducting plate as it slides beneath the continental crust.
It was formed from the volcanism created by a subducting oceanic plate at a convergent plate boundary.
The Pacific Ring of Fire was formed due to the subduction of the Nazca Plate beneath the South American Plate, the Cocos Plate beneath the Caribbean Plate, the Pacific and Juan de Fuca Plate beneath the North American Plate, the Pacific Plate and Philippines Plate beneath the Eurasian Plate, the Indo-Australian Plate beneath the Eurasian Plate, and the Pacific Plate beneath the Indo-Australian Plate. This all occurs around the Pacific Ocean.
A series of volcanic islands formed by an older oceanic plate subducting under a newer oceanic plate.
This was because part of the northward-moving African Plate is subducting beneath the Eurasian Plate. Trapped lava forms bubbles of gas as it gets near the surface. Pressure is released by coming to the surface. It bursts out as lava. Then layers build up to form the cone shape. There you go!
It appears to be continuous because it is a cycle. Old plate is subducted, but new plates are formed.
The Eurasian and Australian plates. Krakatau was formed by the Australian plate subducting under the Eurasian plate.
These gases are formed by chemical reactions at high temperature and pressure.