Thickening of the crust, deposition of sediments, removal of rocks via erosion, or even the emplacement of large ice sheets, can perturb the crust from isostatic equilibrium and cause the surface ...
ISOSTATIC equilibrium ensues only after disturbances have ceased. The strata of mountains must originally have been deposited horizontally. They may be held to have attained to heights much greater ...
Some results have been hidden because they may be inaccessible to you
Show inaccessible results