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 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 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 mantle is the part of the Earth's layers that is approximately 2300 km thick. It lies between the crust and the outer core and is composed of solid rock that flows over long periods of time, causing tectonic plate movement.
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 Earth's layers vary in thickness. The crust is thinnest under the oceans, around 5-10 km thick, and thicker under continents, around 20-70 km thick. The mantle extends from the crust to about 2,900 km below the surface, while the outer core is about 2,300 km thick and the inner core is about 1,200 km thick.
Combined the inner and outer cores are 3500 km thick.
The Core of Mars http:/en.wikipedia.org/wiki/Mars#Geology
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.
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.
1200 km thick
60-100 km thick
The Earth's atmosphere is about 300 miles (480 km) thick.
The mantle is the part of the Earth's layers that is approximately 2300 km thick. It lies between the crust and the outer core and is composed of solid rock that flows over long periods of time, causing tectonic plate movement.
The thickness of Earth's layers varies: the crust is between 5-70 km thick, the mantle is about 2,900 km thick, the outer core is about 2,300 km thick, and the inner core is about 1,200 km thick.
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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.