oceanic and continental
There are two types of lithosphere: the oceanic lithosphere and the continental lithosphere. The oceanic lithosphere exists in the ocean basins while the continental lithosphere exists in the continental crust.
The two types of lithospheric crust are continental crust, which is thicker and less dense than oceanic crust, and oceanic crust, which is thinner and more dense than continental crust.
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.
Continental Plates
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subduction boundary eruption
Pangaea was a supercontinent that existed about 335 million years ago, formed by the movement of lithospheric plates. As Pangaea broke apart, the lithospheric plates moved to their current positions, resulting in the Earth's current continents and ocean basins. This movement also influenced the distribution of different types of lithospheric rocks around the world.
i believe it is the crust and upper mantle...
1. Tectonic (lithospheric) cycle. 2. Rock cycle. 3. Mineral (minerological) cycle.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
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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.