The kinematic boundary condition is at . Part c therefore gives
and hence
In terms of wavelength ,
Without elasticity, : shorter wavelengths penetrate less deeply but relax more slowly because their viscous gradients are larger. At short wavelength, elastic bending dominates and
so the strong restoring stress makes very short waves relax rapidly. The graph therefore tends to zero at both wavelength extremes and has one maximum. Differentiating with respect to places that maximum at
This exponential relaxation is the simplest half-space model of postglacial rebound and glacial isostatic adjustment.
Solved by gpt-5.6-sol high.

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