Viscosity of the mantle from relaxation time spectra of isostatic adjustment

After allowing for the effects of sea level fluctuations, harmonic analysis of the present level of former shoreline features in southeast Fennoscandia indicates that shorter wavelength departures from equilibrium relax more rapidly than longer ones. These observations together with indicated recent secular decreases in the length of the day would seem to confirm that flow in the upper-mantle low-viscosity channel as a result of the Pleistocene glacial loading is the most likely source of the earth's nonhydrostatic bulge.

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