The African Plate is primarily a continental tectonic plate. It includes much of the African continent and extends into the Atlantic Ocean and the Indian ocean. While it contains oceanic crust along its western and eastern boundaries, the main portion of the plate consists of continental crust.
The African plate is both oceanic and continental.
The Arabian Plate is considered a continental plate. It mainly consists of continental crust and is part of the larger African Plate.
When an oceanic plate and a continental plate collide, the oceanic plate is always subducted. Oceanic plates are denser than continental plates, and they have a higher iron content. Since they are denser, oceanic plates always sink below the continental plate in the event of a collision.
The oceanic plate is denser than the continental plate due to its composition of heavier mafic rock. This density difference causes the oceanic plate to sink below the continental plate in a process known as subduction.
In an oceanic-oceanic subduction boundary, one oceanic plate subducts beneath another oceanic plate. This process can result in volcanic island arcs being formed. In an oceanic-continental subduction boundary, an oceanic plate subducts beneath a continental plate. This can lead to the formation of volcanic mountain ranges on the continental plate.
the african plate is continental
The African plate is both oceanic and continental.
The African plate is primarily continental, as it is made up of large landmasses like Africa and parts of the oceanic crust beneath the surrounding oceans.
The Arabian Plate is considered a continental plate. It mainly consists of continental crust and is part of the larger African Plate.
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When an oceanic plate and a continental plate collide, the oceanic plate is always subducted. Oceanic plates are denser than continental plates, and they have a higher iron content. Since they are denser, oceanic plates always sink below the continental plate in the event of a collision.
It is oceanic
The oceanic plate is denser than the continental plate due to its composition of heavier mafic rock. This density difference causes the oceanic plate to sink below the continental plate in a process known as subduction.
Continental plate.
The three types of convergent boundaries are oceanic-oceanic plate boundary (e.g. Japan Trench), oceanic-continental plate boundary (e.g. Andes Mountains), and continental-continental plate boundary (e.g. Himalayas).
In an oceanic-oceanic subduction boundary, one oceanic plate subducts beneath another oceanic plate. This process can result in volcanic island arcs being formed. In an oceanic-continental subduction boundary, an oceanic plate subducts beneath a continental plate. This can lead to the formation of volcanic mountain ranges on the continental plate.
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries