mantle
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 lower mantle is approximately 2,900 kilometers thick and extends from a depth of around 660 kilometers to 2,900 kilometers beneath the Earth's surface. It is composed mainly of solid rock that exhibits solid-state flow over geological timescales.
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 thickest part of the Earth's crust is typically found beneath mountain ranges, where tectonic plates collide and push the crust upward, creating a thicker layer of rock. This thicker crust is known as continental crust and can be up to 70 km (43 miles) thick in places like the Himalayas.
The thickest part of the crust is generally found beneath mountain ranges and can reach up to around 45 miles thick, with the average thickness being around 25 miles. However, the thickness can vary significantly depending on the location and geological setting.
The crust is around five miles deep under the oceans and twenty five miles thick underneath the continents.
The earth's crust is the thinnest layer.the crust wich is the outermost layer on the earth on which we live
mantle
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
The layer of Earth that is between 3 to 30 miles thick is the mantle. It lies beneath the crust and extends to about 1,800 miles deep. The upper part of the mantle is involved in tectonic activity and is partially molten, allowing for the movement of tectonic plates. The mantle is composed of silicate rocks rich in magnesium and iron.
The part that is dry land is about 25 miles thick.
The lower mantle is approximately 2,900 kilometers thick and extends from a depth of around 660 kilometers to 2,900 kilometers beneath the Earth's surface. It is composed mainly of solid rock that exhibits solid-state flow over geological timescales.
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 thickest part of the Earth's crust is typically found beneath mountain ranges, where tectonic plates collide and push the crust upward, creating a thicker layer of rock. This thicker crust is known as continental crust and can be up to 70 km (43 miles) thick in places like the Himalayas.
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.
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