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Root, B.C. (author), Van der Wal, W. (author), Ebbing, J. (author)
journal article 2015
document
Root, B.C. (author), Tarasov, L. (author), Van der Wal, W. (author)
The Barents Sea is subject to ongoing postglacial uplift since the melting of the Weichselian ice sheet that covered it. The regional ice sheet thickness history is not well known because there is only data at the periphery due to the locations of Franz Joseph Land, Svalbard, and Novaya Zemlya surrounding this paleo ice sheet. We show that the...
journal article 2015
document
Root, B.C. (author), Van der Wal, W. (author), Novak, P. (author), Ebbing, J. (author), Vermeersen, L.L.A. (author)
In the central part of Fennoscandia, the crust is currently rising, because of the delayed response of the viscous mantle to melting of the Late Pleistocene ice sheet. This process, called Glacial Isostatic Adjustment (GIA), causes a negative anomaly in the present-day static gravity field as isostatic equilibrium has not been reached yet....
journal article 2015