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The mantle. It's the "sandwich filling" between the crust and the core.
isostatic equilibrium
lithosphere
The mantle is that part of the Earth between the crust and the outer core. It's upper boundary is at the base of the crust at a depth below the surface which can vary between 7 and 35 km. It extends all the way to the Earth's outer core at a depth of around 2890 km.the Earths mantle is located between the crust and outer core of the Earth. it is the thickest layer.
The hot spots in the oceanic crust are caused by upwellings of hotter material (known as mantle plumes) in the mantle below the crust.
The crust is above the mantle and the mantle is below the crust
Isostatic equilibrium is the balance between Earth's crust and the layer of mantle it floats on. The denser the crust is, the more it sinks into the mantle. Equilibrium is achieved when the crust floats at a certain level in the mantle.
Mantle Is The Below Layer Of The Crust In Earth.
The Earth's mantle is below the crust. The layers of the Earth form concentric spheres. Below the mantle is the core.
The mantle. It's the "sandwich filling" between the crust and the core.
isostatic equilibrium
the mantle
lithosphere
15 kilo meters is the distance between the crust and the mantle
Just below the crust we find the mantle.
The interior of the Earth, similar to the other terrestrial planets, is chemically divided into layers. The mantle is a highly viscous layer between the crust and the outer core. As such, the core (split into the solid inner and liquid outer layers) is below the mantle.
The hard, rocky upper mantle to which it is attached.