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lithosphere
The lithosphere is the part of the Earth's structure that is approximately 100 km thick. It consists of the crust and the uppermost part of the mantle and is divided into tectonic plates.
the mantle, which contains the lithosphere, asthenosphere and the mesosphere
The crust is the uppermost part of the earth. It is also the coolest and least dense. While the mantle is a warmer and dense. The mantle is made up of the Asthenosphere and the Lithosphere. The lithosphere floats in many plates on top of the taffy-like asthenosphere. The Lithosphere is made up of the upper part of the mantle and the crust.
The asthenosphere is a flowing solid. It's sort of a liquid and a solid.
lithosphere
The thickest part of the lithosphere is typically found beneath continental regions, where the crust can be up to 70 km thick. This thick continental lithosphere is composed of both the crust and the uppermost part of the mantle.
The lithosphere is the part of the Earth's structure that is approximately 100 km thick. It consists of the crust and the uppermost part of the mantle and is divided into tectonic plates.
the mantle, which contains the lithosphere, asthenosphere and the mesosphere
The lithosphere is the part of Earth's structure that is about 100 km thick. It includes the outermost layer of the Earth, including both the crust and the uppermost part of the mantle.
The lithosphere, which includes the crust and upper part of the mantle, is typically around 100 kilometers thick beneath the oceans and up to 200 kilometers thick beneath the continents.
The crust and the lithosphere are the thinnest layers of the Earth. The crust is the outermost layer and can vary in thickness from 5 to 70 km, while the lithosphere, which includes the crust and uppermost solid mantle, is typically around 100 km thick.
There are five basic layers of the Earth, being the crust, upper mantle, inner mantle, outer core, and inner core. Of these, the lithosphere is composed of the crust and upper mantle, and the asthenosphere is part of the mantle, below the lithosphere.
both of them together is 333 kilometers. you can search the Internet for how thick the crust is and subtract that from 333 to get the thickness of the mantle part.
The asthenosphere is approximately 100-200 kilometers thick beneath the Earth's crust. It is a semi-plastic layer of the mantle that lies below the lithosphere and plays a key role in plate tectonics and mantle convection.
The lithosphere includes the Earth's crust and uppermost mantle. Oceanic lithosphere is typically about 50-100 km thick, while continental lithosphere has a range in thickness from about 40 km to perhaps 200 km.
The lithosphere is generally thinner under oceanic crust compared to continental crust. Oceanic lithosphere is typically around 5-10 kilometers thick, while continental lithosphere can be up to 200 kilometers thick. This difference is due to variations in temperature and composition between the two types of crust.