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 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.
The four layers of the Earth are the crust, mantle, outer core, and inner core. The crust is the thinnest layer, ranging from about 5-70 km thick, while the mantle is about 2,900 km thick. The outer core is approximately 2,200 km thick, and the inner core is roughly 1,200 km thick.
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 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 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 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 Earth's atmosphere is about 300 miles (480 km) thick.
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.
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.
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it is about 1900 KM thick