The two types of crust may be called continental crust and oceanic crust. They can also be called granitic and basaltic crust respectively.
The South American plate is a major tectonic plate that covers most of the continent of South America. It is primarily composed of continental crust.
A subduction zone is the plate boundary where old and heavy oceanic crust sinks into the mantle. At subduction zones, oceanic crust is forced beneath another tectonic plate, typically a continental plate, due to differences in density. This process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding plate.
The Himalayan mountains were created by the collision of the Indian and Eurasian tectonic plates. The Indian plate collided with the Eurasian plate, causing the crust to buckle and fold, resulting in the formation of the towering Himalayan mountain range.
Mt. Erubus has tectonic plates made up of parts of the lithosphere. These plates grind together or pull apart and this causes volcanoes to erupt.
Seafloor spreading is caused by the movement of tectonic plates away from each other at mid-ocean ridges. As the plates separate, magma rises to the surface, solidifies, and creates new oceanic crust. This process is part of the theory of plate tectonics.
The South American plate is a major tectonic plate that covers most of the continent of South America. It is primarily composed of continental crust.
The tectonic plate under parts of Europe and Asia is a continental crustal plate.
Oceanic crust is usually destroyed by subduction. This occurs when one tectonic plate, typically consisting of denser oceanic crust, is forced beneath another plate, often continental crust. As the oceanic plate subducts into the mantle, it melts and is recycled, leading to geological phenomena such as volcanic activity and the formation of deep ocean trenches.
A subduction zone is the plate boundary where old and heavy oceanic crust sinks into the mantle. At subduction zones, oceanic crust is forced beneath another tectonic plate, typically a continental plate, due to differences in density. This process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding plate.
Transform boundary
Pacific Plate
The Himalayan mountains were created by the collision of the Indian and Eurasian tectonic plates. The Indian plate collided with the Eurasian plate, causing the crust to buckle and fold, resulting in the formation of the towering Himalayan mountain range.
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust.
Mt. Erubus has tectonic plates made up of parts of the lithosphere. These plates grind together or pull apart and this causes volcanoes to erupt.
one talc
Seafloor spreading is caused by the movement of tectonic plates away from each other at mid-ocean ridges. As the plates separate, magma rises to the surface, solidifies, and creates new oceanic crust. This process is part of the theory of plate tectonics.
The Himalayan mountains are fold mountains, formed by the collision of tectonic plates. They are the result of the Indian plate pushing against the Eurasian plate, causing the Earth's crust to fold and uplift. The Himalayas are home to some of the highest peaks in the world, including Mount Everest.