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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 part of the Earth that is about 3500 km thick is the mantle. The mantle is located between the Earth's crust and core and is composed of molten rock material that flows slowly over time due to the intense heat and pressure.
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 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 mantle layer of the Earth is approximately 2,900 km thick. It lies between the Earth's crust and core and is composed of solid rock that flows slowly over time due to heat and pressure.
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 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.
60-100 km thick
the lithosphere
The thinnest outermost layer of the Earth is the Earth's crust. It is typically between 5 to 100 km thick and consists of solid rock that forms the Earth's outer shell. Oceanic crust is thinner (5-10 km) compared to continental crust (20-70 km).
The part of the Earth that is about 3500 km thick is the mantle. The mantle is located between the Earth's crust and core and is composed of molten rock material that flows slowly over time due to the intense heat and pressure.
Mantle.
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 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 mantle layer of the Earth is approximately 2,900 km thick. It lies between the Earth's crust and core and is composed of solid rock that flows slowly over time due to heat and pressure.
The thinnest outermost layer of Earth is known as the crust.
A batholith is a pluton exposed across more than 100 square km of Earth's surface. An average batholith is about 10 km thick, but can be up to 20 km thick. A stock is very similar to a batholith, but with less than 100 square km exposed.