The western Caribbean area primarily consists of the countries of Mexico, Guatemala, Honduras, Nicaragua, Costa Rica, Panama, Columbia and Venezuela. Mexico, and most of the volcanoes therein are located predominately within the Guerrero Block and includes the Paleogene and Neogene/Quarternary arcs. Guatemala, Honduras and Nicaragua are both located within the Chortis Block whereas the Nicoya Complex flanks Costa Rica on the east by the Limon Basin and on the west. Panama is also part of the Nicoya Basin, flanked on the west and on the east, flanked by the North Panama Fold Belt. Columbia, part of the Guyana Shield and lies basically in the Lianos Basin, Barinas-Apure Basin and the El Baul Swell Basin. Venezuela, also part of the Guyana Shield predominately lies within the Eastern Venezuelan Basin. Both Columbia and Venezuela form the Southern Caribbean Plate Boundary Zone.
Yes, it is actually caused by the subduction of two plates: the Cocos Plate and the Caribbean plate.
Eyjafjallajökull is located on the Mid-Atlantic ridge, which is a divergent plate boundary. It is also over a hot spot.
Destructive and conservative :)
collision plate boundary because they make mountains
What type of eruption does Mt. Shasta have?a composite eruption which is a quiet eruption
A mid-plate volcano, also known as a hot-spot, is an eruption of lava that is NOT on a plate boundary. It occurs right in the middle of a tectonic plate instead of on the boundary of one of them. An example of one is in Hawaii.
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The Philippine plate collided with the Eurasian plate this is called a convergent boundary where the two plates collided and the plate melts and then shoots back up through the volcano causing an eruption
collision plate boundary because they make mountains
it is a hot spot for the boundary because it represents the volcanic eruption
What type of eruption does Mt. Shasta have?a composite eruption which is a quiet eruption
A mid-plate volcano, also known as a hot-spot, is an eruption of lava that is NOT on a plate boundary. It occurs right in the middle of a tectonic plate instead of on the boundary of one of them. An example of one is in Hawaii.
Divergent Boundary Plate BoundaryDivergent Boundary Plate BoundaryDivergent Boundary Plate BoundaryDivergent Boundary Plate BoundaryDivergent Boundary Plate BoundaryvDivergent Boundary Plate BoundaryDivergent Boundary Plate BoundaryDivergent Boundary Plate BoundaryDivergent Boundary Plate BoundaryDivergent Boundary Plate BoundaryDivergent Boundary Plate BoundaryDivergent Boundary Plate Boundary
The Philippine plate collided with the Eurasian plate this is called a convergent boundary where the two plates collided and the plate melts and then shoots back up through the volcano causing an eruption
650 to 1050 Degrees centigrade depending on where the eruption is happening (type of plate boundary).
Calbuco's population is 31,070.
Calbuco was created in 1603-05.
The area of Calbuco is 590.8 square kilometers.
the plate boundary at the mount is a colliding plate boundary
Convergent plate boundary, divergent plate boundary and strike-slip (transform) plate boundary.