Isostasy

Cartoon showing the isostatic vertical motions of the lithosphere (grey) in response to a vertical load (in green)

Isostasy (Greek ísos "equal", stásis "standstill") is the state of gravitational equilibrium between Earth's crust and mantle such that the crust "floats" at an elevation that depends on its thickness and density of underlying roots of the low density of the mountain.

单词	Isostatic theory
释义	Isostatic theory 英语百科 Isostasy Isostasy (Greek ísos "equal", stásis "standstill") is the state of gravitational equilibrium between Earth's crust and mantle such that the crust "floats" at an elevation that depends on its thickness and density of underlying roots of the low density of the mountain.
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Isostatic theory

Isostasy