The Andes Mountains in western South America are a result of an oceanic-continental convergence of lithospheric plates. It would occur anywhere that an oceanic plate and a continental plate are moving toward each other.
The three types of convergent plate boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergence occurs when two oceanic plates collide, resulting in the formation of volcanic island arcs. Oceanic-continental convergence happens when an oceanic plate subducts beneath a continental plate, creating volcanic mountain ranges. Continental-continental convergence involves the collision of two continental plates, leading to the formation of large mountain ranges.
Oceanic-Continental Convergence - Andean-Type - the Andes MountainsOceanic-Oceanic Convergence - Aleutian-Type - island arcsContinental-Continental Convergence - the Appalachian Mountains
Continental crust cannot form as a result of oceanic-oceanic convergence. This process typically results in the formation of volcanic island arcs or deep-sea trenches. Continental crust is formed through processes like continental collision and accretion of terranes.
Oceanic-continental convergence (when an oceanic plate meets a continental plate) & oceanic-oceanic convergence (2 oceanic plates) both involve oceanic plates & subduction. Continental-continental convergence (2 continental plates) involves neither.
divergent, transform and convergent divergent plate boundaries move away from each other, convergent plate boundaries move toward each other, and transform plate bounties slide past each other.
The three types of convergent plate boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergence occurs when two oceanic plates collide, resulting in the formation of volcanic island arcs. Oceanic-continental convergence happens when an oceanic plate subducts beneath a continental plate, creating volcanic mountain ranges. Continental-continental convergence involves the collision of two continental plates, leading to the formation of large mountain ranges.
Convergence can occur between oceanic-oceanic, oceanic-continental, and continental-continental plates. This process typically leads to the formation of mountain ranges, deep ocean trenches, and volcanic arcs.
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Its when the oceanic crust and the continental crsut colide together.
Oceanic-Continental Convergence - Andean-Type - the Andes MountainsOceanic-Oceanic Convergence - Aleutian-Type - island arcsContinental-Continental Convergence - the Appalachian Mountains
In oceanic-continental convergence, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This creates a deep ocean trench and can lead to volcanic activity and the formation of mountain ranges on the continental plate. The collision can also cause earthquakes.
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
Continental crust cannot form as a result of oceanic-oceanic convergence. This process typically results in the formation of volcanic island arcs or deep-sea trenches. Continental crust is formed through processes like continental collision and accretion of terranes.
An oceanic-continental convergence typically results in the oceanic plate subducting beneath the continental plate due to its higher density. This can lead to the formation of volcanic mountain ranges on the continental plate, as magma generated by the subducted plate rises to the surface and forms volcanoes. Additionally, intense seismic activity and the potential for tsunamis can also be associated with this type of plate boundary.
Oceanic-continental convergence (when an oceanic plate meets a continental plate) & oceanic-oceanic convergence (2 oceanic plates) both involve oceanic plates & subduction. Continental-continental convergence (2 continental plates) involves neither.
At an oceanic-continental convergence boundary, the oceanic plate is typically subducted beneath the continental plate. This process can lead to the formation of deep oceanic trenches, volcanic arcs on the continental plate, and strong earthquakes due to the intense pressure and friction. Over time, sediment may accumulate on the continental plate as a result of subduction and mountain building.
divergent, transform and convergent divergent plate boundaries move away from each other, convergent plate boundaries move toward each other, and transform plate bounties slide past each other.