The oceanic plate is forced to sink beneath the continental plate as it is denser. This is subduction. From here, a further series of events unfolds (if you are still interested)...
The volcanoes formed are explosive because the lava is very viscous as it has a high silica content. This is because of the sediment which was also subducted with the crustal rock. When the magma pushes up, it often cools quickly within the cone of the volcano, forming a plug. When the pressure of the magma is too great, the volcano explodes, like the spectacular eruption at Mt. St. Helens in September 1980.
With this collision, you will also find many earthquakes occurring as friction occurs between the plates.
when two plates collide they form trenches.
Continental-continental, Oceanic-oceanic and Oceanic-continental convergent boundaries.
divergence of continental crust create rift zones e.g.east african rift valley.firstly,divergence will create updoming of the area.after that step faulting will take place and that will result in narrow linear sea formation like red sea.finally separation of land and ocean ridge will occur.
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
Newton's Third Law is closely related to Conservation of Momentum. When objects collide, whether the collision is elastic or not, momentum is conserved. (An elastic collision is one in which mechanical energy is conserved. In an elastic collision, after the collision, the objects go away at the same relative speed at which they approached before the collision.)
Andes - continental oceanic aleutians - oceanic oceanic North American cordillera - arc continent Appalachians - continental continental
very very high mountains, e.g. India and Asia making Himalayas.
The definition of ocean continental collision means the continental crust and the ocean's crust collide with one another. A subduction is formed when the collision occurs.
During a continental-continental collision, two landmasses converge and eventually collide, leading to the formation of very large mountain ranges. The collision can cause intense deformation of Earth's crust, resulting in the uplift and folding of rocks. Earthquakes and volcanic activity may also be triggered as a result of the collision.
Yes, continental-continental collisions can lead to the formation of mountain ranges through the process of crustal uplift and folding. The intense pressure and deformation generated during the collision cause the Earth's crust to fold, creating large-scale mountain systems like the Himalayas.
The definition of ocean continental collision means the continental crust and the ocean's crust collide with one another. A subduction is formed when the collision occurs.
The collision and joining of crustal fragments to a continent is called continental accretion.
The collision between the Indian Plate and the Eurasian Plate that led to the formation of the Himalayas is a geographic example of a continental collision. This collision continues to uplift the Himalayas, creating some of the world's tallest mountains.
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Collision...
Two continental plates colliding can cause the formation of mountain ranges through a process called continental collision. The intense pressure and friction between the plates push the crust upwards, resulting in the formation of large fold mountains such as the Himalayas. This collision can also trigger earthquakes and volcanic activity along the plate boundaries.
Some examples of mountain ranges created by continental-continental convergence are the Himalayas (resulting from the collision of the Indian and Eurasian plates) and the Alps (formed by the collision of African and Eurasian plates).