the lithoseshere
the mantle is a hot ocean of lava basically and on it floats a series of tectonic plates, on the surface of the plates is the crust. there is your answer hope it helps.
Many volcanos occur along tectonic boundaries, whether they are convergent (pushing together) or divergent (pulling apart). These boundaries typically occur between continental and oceanic plates or between two oceanic plates. Some volcanos however are created by hot spots where molten magma from the mantle of the Earth pushes through the crust, these hot spots can form islands such as the Hawaiian Islands.
The middle layer of earth that is MANTLE. It has the tectonic plates floating on it.
asthenosphere
Depends on the type of tectonic plate. If it is two continental plates, usually a mountain range will be formed and the plates will 'lock' together due to their thickness. The Indian sub-continent colliding with the eurasian plate is one example. If an oceanic plate is subducting under a continental plate an island arc can be formed or mountain range such as Japan and the Andies mountains respectively. This type is also where volcanoes will be commonly found unlike the collision of two continental plates, due to the magma formed from the subduction of the oceanic plate. If two oceanic plates collide, usually form an oceanic mountain range and lock together similar to the continental plates.
That would be the lithosphere which is split into tectonic plates.
Oceanic plates, continental plates, and microplates are all examples of tectonic plates that make up the Earth's lithosphere. These plates move around due to the heat-driven convection currents in the Earth's mantle, causing phenomena like earthquakes, volcanoes, and mountain-building.
Oceanic plates are denser and thinner, found beneath the oceans, while continental plates are thicker and less dense, making up the Earth's landmasses. These two types of tectonic plates interact at boundaries, influencing processes like earthquakes and volcanic eruptions.
Lithosphere is categorized into two sections. They are crust and upper most mantle. Crust includes continental and oceanic crust and technology.
Continental plates are tectonic plates. They are tectonic plates upon which continents rest, and they move as do all tectonic plates. Basically, there is no difference, other than the fact that oceanic plates are another type of tectonic plate.
The two types of tectonic plates are continental and oceanic.
There are two kinds of plates- continental lithosphere and oceanic lithosphere. There are many types of plate boundaries, like convergent, divergent, transform, and more. Continental lithosphere is granite and oceanic is basalt.
The two types of tectonic plates are continental and oceanic.
Tectonic plates are also "Continental Crust" and "Oceanic Crust". Also lithospheric plates.
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The lithosphere is composed of oceanic or continental crust and the uppermost part of the mantle. It is divided into tectonic plates that float on the semi-fluid asthenosphere and interact with each other to create geological features like earthquakes and mountain ranges.
Tectonic plates consist of both continental and oceanic crust. The Earth's lithosphere is divided into several large and small plates that constantly move and interact with each other. Some plates are predominantly made up of continental crust, while others are mostly composed of oceanic crust.