Oceanic plates are young and made of basalt and recent sediments.
Continental plates are old and contain continental crust made of old rocks and they are usually considerably thicker than the oceanic plates
Most plates are a combination of both oceanic and continental crust. The Pacific Plate and the Eurasian Plates are the biggest plates.
Oceanic is heavier but thinner.
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oceanic plates
Convergence between oceanic plate and one continental plate. Convergence between two oceanic plates.
A convergent boundary between two continental plates causes both plates to crumple to form fold mountains e.g. the HimalayasA convergent boundary between a continental and an oceanic causes one to rise above the other. Granite is less dense than basalt, so the continental plate rises above the oceanic plate. This also forms mountains, like the Andes.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
oceanic plate
Oceanic.
Convergence between oceanic plate and one continental plate. Convergence between two oceanic plates.
The oceanic plate usually subsides after colliding with a continental plate.
When two plates meet each other thats called a Convergent boundary. They include areas where an oceanic plate slides below a continential plate.
Continential drift is a large landform of our continents.
It is oceanic
A subduction zone occurs at convergent plate margins where an oceanic plate is going underneath a continental plate or a less dense oceanic plate. A mid-ocean ridge is a divergent plate boundary on the ocean floor with a mountain range and a rift running through the center of it. Sea floor spreading also occurs at mid ocean ridges.
A convergent boundary between two continental plates causes both plates to crumple to form fold mountains e.g. the HimalayasA convergent boundary between a continental and an oceanic causes one to rise above the other. Granite is less dense than basalt, so the continental plate rises above the oceanic plate. This also forms mountains, like the Andes.
The oceanic crust consists of heavier rock, mostly Basalt, so that if a oceanic plate collides with a continental plate the oceanic plate will be forced down below the continental plate, forming island arcs.continental plates are thicker than oceanic plates.
The oceanic crust consists of heavier rock, mostly Basalt, so that if a oceanic plate collides with a continental plate the oceanic plate will be forced down below the continental plate, forming island arcs.continental plates are thicker than oceanic plates.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.