Viscosity and Finite Strength of the Mantle as Determined from Water and Ice Loads
Some recent examples of transient Earth loads (Lake Bonneville, Utah; Glacier Bay, Alaska; northeast Greenland) indicate that both the viscosity and finite strength of the mantle are lower than is commonly presumed. A time constant (1/ e ) of 4000 years is estimated for Lake Bonneville, and of 1000...
| Published in: | Geophysical Journal of the Royal Astronomical Society |
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| Main Author: | |
| Format: | Text |
| Language: | English |
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Oxford University Press
1967
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| Online Access: | http://gji.oxfordjournals.org/cgi/content/short/14/1-4/261 https://doi.org/10.1111/j.1365-246X.1967.tb06243.x |
| Summary: | Some recent examples of transient Earth loads (Lake Bonneville, Utah; Glacier Bay, Alaska; northeast Greenland) indicate that both the viscosity and finite strength of the mantle are lower than is commonly presumed. A time constant (1/ e ) of 4000 years is estimated for Lake Bonneville, and of 1000 years for northeast Greenland. A strain rate of 10−14 is typical. These figures imply viscosities in a homogeneous half space ranging from 1020 to 1021 poises. An upper limit of finite strength is set by Lake Bonneville at a few times 106 dyn/cm2. If mountain ranges like the Sierra Nevada or Himalaya are regarded as dynamically supported rather than static systems, this low value is not incompatible with other geologic observations. |
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