Revisiting the Paleo Elbe Valley: Reconstruction of the Holocene, Sedimentary Development on Basis of High-Resolution Grain Size Data and Shallow Seismics

The Paleo Elbe Valley is the most prominent subsurface structure in the southern North Sea. During the Weichselian (marine isotope stage (MIS) 2), the valley traversed the exposed sea floor and drained the southern margin of the Scandinavian ice sheet. Today the valley is filled with up to 16 m thic...

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Bibliographic Details
Main Authors: Svenja Papenmeier, H. Christian Hass
Format: Article
Language:English
Published: MDPI AG 2020-12-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/10/12/505