Wiki User
∙ 15y agoIt is possible to have continental and oceanic crust on the same plate. The only to this exception is with the Pacific plate which exists independently.
Wiki User
∙ 9y agoYes, lithospheric plates can include both continental and oceanic crust. These plates are composed of the rigid outer layer of Earth's surface, which consists of the upper part of the mantle and the crust. Continental crust is less dense and thicker than oceanic crust, but both can form part of lithospheric plates.
Wiki User
∙ 15y agoYes. because the plates create the Lithosphere
Wiki User
∙ 12y agoyes it can. the majority of the plates carry both oceanic and continental crust. especially the north American one
Wiki User
∙ 9y agoYes. Most major plates have both continental and oceanic crust in some measure.
Yes, continental plates are more buoyant than oceanic plates because they are thicker and less dense. Continental plates are made up of less dense material such as granite, while oceanic plates are primarily composed of denser basaltic rock. This difference in density causes continental plates to float higher on the underlying mantle.
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.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
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.
The three categories of convergent boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergent boundaries result in volcanic island arcs. Oceanic-continental convergent boundaries create volcanic mountain ranges. Continental-continental convergent boundaries give rise to large mountain ranges.
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.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
Tectonic plates are also "Continental Crust" and "Oceanic Crust". Also lithospheric plates.
Yes, continental plates are more buoyant than oceanic plates because they are thicker and less dense. Continental plates are made up of less dense material such as granite, while oceanic plates are primarily composed of denser basaltic rock. This difference in density causes continental plates to float higher on the underlying mantle.
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.
Oceanic crust is thinner and more dense will continental crust is thicker and less dense.
Oceanic plates are denser and thinner than continental plates, which causes them to be lower in elevation. The denser oceanic plates are effectively pulled downward by gravity, causing them to sink beneath the less dense continental plates. This difference in density and thickness results in oceanic plates being lower than continental plates.
The lithosphere includes the crust (oceanic and continental) and the uppermost part of the mantle. The lithospheric plates are thinnest at the ocean, varying from between a few kilometers to 100 kilometers in deep-ocean basins. The continental lithosphere, on the other hand, is generally about 100 to 250 kilometers thick. The most important feature of the lithosphere is its divisions into lithospheric plates. These plates move and collide, creating earthquakes, fault lines, etc.
Continental Plates
the oceanic plates are denser than continental plates, therefore, when oceanic plates and continental plates converge, the oceanic will go under the continental plates. But when two oceanic converge either both will rise to form moutains, or both will sink and cause a trench.