Continental plates are primarily characterized by their thickness, typically ranging from 30 to 70 kilometers, which makes them less dense than oceanic plates. They are composed mainly of granitic rocks, giving them a lighter composition compared to the basaltic rocks of oceanic plates. Additionally, continental plates are older than oceanic plates, with some parts being billions of years old, and they play a crucial role in the formation of mountain ranges and the occurrence of earthquakes.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
The Antarctic Plate is primarily an oceanic plate, as it includes the seafloor of the Southern Ocean surrounding Antarctica. However, it also contains a significant continental portion, which is the landmass of the Antarctic continent itself. This combination makes the Antarctic Plate unique, as it encompasses both oceanic and continental characteristics.
Oceanic-continental plate boundary: where an oceanic plate and a continental plate collide, causing the oceanic plate to subduct beneath the continental plate. Oceanic-oceanic plate boundary: occurs when two oceanic plates collide, with one plate usually subducting beneath the other. Continental-continental plate boundary: where two continental plates collide, leading to the formation of mountain ranges through intense compression and uplifting of the crust.
The Arabian Plate is considered a continental plate. It mainly consists of continental crust and is part of the larger African Plate.
The Oceanic plate is subducted under the Continental plate because oceanic crust is much more dense than continental crust. The average density of the oceanic crust is 3g/cm^3 while the average density of continental crust is 2.7g/cm^3.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
The Antarctic Plate is mostly a continental plate, as it is made up of continental crust beneath the ice. However, in the region where it interacts with the surrounding oceanic plates, it can also have some oceanic characteristics.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
The Antarctic Plate is primarily an oceanic plate, as it includes the seafloor of the Southern Ocean surrounding Antarctica. However, it also contains a significant continental portion, which is the landmass of the Antarctic continent itself. This combination makes the Antarctic Plate unique, as it encompasses both oceanic and continental characteristics.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
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).
Oceanic-continental plate boundary: where an oceanic plate and a continental plate collide, causing the oceanic plate to subduct beneath the continental plate. Oceanic-oceanic plate boundary: occurs when two oceanic plates collide, with one plate usually subducting beneath the other. Continental-continental plate boundary: where two continental plates collide, leading to the formation of mountain ranges through intense compression and uplifting of the crust.
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
The Arabian Plate is considered a continental plate. It mainly consists of continental crust and is part of the larger African Plate.
the african plate is continental
The Oceanic plate is subducted under the Continental plate because oceanic crust is much more dense than continental crust. The average density of the oceanic crust is 3g/cm^3 while the average density of continental crust is 2.7g/cm^3.