The Motion of a Viscous Fluid Under a Surface Load¶
Haskell, N. A. (1935). The Motion of a Viscous Fluid Under a Surface Load. Physics.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Isostasy
- All are consistent with a viscoelastic Earth model whose upper-mantle effective viscosity is on the order of 10²¹ Pa·s — the parameter that sets how slowly the rebound proceeds
This sourceThe classic inference of a mantle viscosity of order 1e21 Pa s from post-glacial rebound, obtained from a uniform viscous half-space model, so the value is a depth-averaged mantle viscosity rather than an upper-mantle one.
Supported in partVerified against the source
- All are consistent with a viscoelastic Earth model whose upper-mantle effective viscosity is on the order of 10²¹ Pa·s — the parameter that sets how slowly the rebound proceeds
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Registry ID ref:2def69ff111d · see in the full table