Continental plate.
either continental or oceanic
Continental plates are thicker than oceanic plates. Continental plates can be up to 70 kilometers thick, while oceanic plates typically range from 5 to 10 kilometers in thickness. This difference in thickness is due to the composition and formation processes of the two types of crust.
Fold mountains.
Oceanic refers to the type of crust that makes up the ocean floor, primarily composed of basalt and denser than continental crust. Continental refers to the landmass crust, which is thicker and primarily made up of lighter rocks such as granite. The differences in density and thickness between oceanic and continental crust significantly influence geological processes, such as plate tectonics and the formation of landforms.
When oceanic and continental plates collide, the oceanic plate is usually forced under the continental plate in a process called subduction. This can result in the formation of mountain ranges on the continental plate and can lead to the creation of volcanic arcs. The collision can also cause earthquakes and tsunamis.
either continental or oceanic
Continental crust is generally thicker than oceanic crust. Continental crust can be up to 70 km thick, while oceanic crust is usually around 5-10 km thick.
oceanic as it is colder; therefore denser
Continental plates are thicker than oceanic plates. Continental plates can be up to 70 kilometers thick, while oceanic plates typically range from 5 to 10 kilometers in thickness. This difference in thickness is due to the composition and formation processes of the two types of crust.
Andean
Fold mountains.
The North American Plate is a combination of continental and oceanic plates. North America itself is continental crust.
The two types of Crust is the Continental Crust and the Oceanic Crust.
Continental crust is typically thicker than oceanic crust. Continental crust can range from around 20 to 70 kilometers thick, whereas oceanic crust is generally much thinner, typically ranging from 5 to 10 kilometers in thickness.
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 refers to the type of crust that makes up the ocean floor, primarily composed of basalt and denser than continental crust. Continental refers to the landmass crust, which is thicker and primarily made up of lighter rocks such as granite. The differences in density and thickness between oceanic and continental crust significantly influence geological processes, such as plate tectonics and the formation of landforms.
A subduction zone is formed when an oceanic plate is pushed under a continental plate, resulting in volcanic activity. Oceanic crust is denser and sinks beneath the less dense continental crust, leading to the formation of volcanic arcs on the overriding plate.