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Raunak Mitra posted an Question
February 10, 2022 • 23:44 pm 30 points
  • IIT JAM
  • Geology (GG)

A 30 km continental crust of density 2.5 gm/cc is in isotactic equilibrium, when it overlies the mantle of density 3.5 gm/cc. a 10 km thick oceanic crust of den

A 30 km continental crust of density 2.5 gm/cc is in isotactic equilibrium, when it overlies the mantle of density 3.5 gm/cc. A 10 km thick oceanic crust of density 3.0 gm/cc under oceans is also in isostatic equilibrium, with reference to the continental crust. The thickness of the water column in the oceans is (in Km)

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