Paracutin is in the trans-Mexican volcanic belt formed by the riviera and cocos plates subducting under the north American plate
The Transversal Plate east west across a 700 mile line that extends across southern Mexico.
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North American Plate
Paricutin is in a zone of many active volcanoes caused by plate subduction under Mexico
Its a Convergent Boundary
hotspot volcanoes are formed away from the edge of plate boundaries. Plate boundary volcanoes are near a plate boundary
A divergent plate boundary.
is formed at a divergent plate boundary
They are formed by the continental contienal plates
A convergent boundary is formed when a plate is pushed into another by the process of subduction.
It was formed from the volcanism created by a subducting oceanic plate at a convergent plate boundary.
The boundary that is formed is called a Tranform Boundary
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.
Divergent boundary is formed
Convergent boundary
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.
hotspot volcanoes are formed away from the edge of plate boundaries. Plate boundary volcanoes are near a plate boundary
It is not on a plate boundary but in the middle of a plate. Kilauea has formed over a hot spot.
convergent plate boundary
A constructive plate boundary, as it pushes land upwards (which formed the mountains)
Mount Everest was formed by a convergent or collision boundary.
It is not on a plate boundary but in the middle of a plate. Kilauea has formed over a hot spot.