The most important factor when determining the types of boundaries that form when two lithospheric plates collide is the relative motion between the plates. Depending on whether the plates are moving towards each other, away from each other, or past each other, different types of boundaries like convergent, divergent, or transform boundaries will form.
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A convergent boundary is formed when two lithospheric plates collide. One plate is forced beneath the other in a process known as subduction. This collision often leads to the formation of mountain ranges or volcanic activity.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
Continental Plates
oceanic and continental
The most important factor when determining the types of boundaries that form when two lithospheric plates collide is the relative motion between the plates. Depending on whether the plates are moving towards each other, away from each other, or past each other, different types of boundaries like convergent, divergent, or transform boundaries will form.
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The lithospheric plates consist of the crust and the uppermost part of the mantle. The crust can be further divided into the continental crust and the oceanic crust.
subduction boundary eruption
When two lithospheric plates move apart, a divergent boundary is formed. This process results in the creation of new oceanic crust as magma rises to fill the gap between the plates, forming a mid-ocean ridge.
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These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
The two types of tectonic plates are continental and oceanic.
A convergent boundary is formed when two lithospheric plates collide. One plate is forced beneath the other in a process known as subduction. This collision often leads to the formation of mountain ranges or volcanic activity.
A transform boundary is formed when two crustal lithospheric plates slide past each other horizontally in opposite directions. The movement at these boundaries is typically characterized by frequent earthquakes due to the friction between the two plates as they slide. An example of a transform boundary is the San Andreas Fault in California.