Space-Geodetic Constraints on Glacial Isostatic Adjustment in Fennoscandia

Milne. (2001). Space-Geodetic Constraints on Glacial Isostatic Adjustment in Fennoscandia.

Type

Unclassified

Intellectual base

Unclassified

Year

2001

DOI

10.1126/science.1057022

Link

https://doi.org/10.1126/science.1057022

Cited by

1 citation across 1 artifact.

Domain-specific

• Isostasy
  • The ice melted roughly 10,000 years ago, but the land is still rising, fastest in the Gulf of Bothnia at on the order of 10 mm/yr, because the underlying mantle has been flowing viscously ever since to restore the column balance that the lost ice load left unmet

Verification

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Registry ID ref:4c270b2547f1 · see in the full table