The Lithosphere
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 lithosphere, which includes the Earth's crust and part of the upper mantle, is about 100 km thick. This rigid outer layer is divided into tectonic plates that float on the semi-fluid asthenosphere beneath them.
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 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 layer of the Earth that includes the surface is the crust. It is the outermost solid layer of the Earth, ranging from 5 to 70 km thick beneath the oceans and up to 100 km thick beneath the continents.
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 hard outer layer of the Earth, approximately 100 kilometers thick, is called the lithosphere. It comprises the crust and the uppermost part of the mantle, and is characterized by its solid and rigid structure. The lithosphere plays a crucial role in tectonic processes, as it is divided into tectonic plates that float on the semi-fluid asthenosphere beneath it.
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 lithosphere, which includes the Earth's crust and part of the upper mantle, is about 100 km thick. This rigid outer layer is divided into tectonic plates that float on the semi-fluid asthenosphere beneath them.
100
60-100 km thick
10 cm or 100 mm.
0.1 inch
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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 mantle =)