Correction: Corrigendum: Glacial isostatic uplift of the European Alps | Zendy

Jürgen Mey | Zendy; Dirk Scherler | Zendy; Andrew D. Wickert | Zendy; David L. Egholm | Zendy; Magdala Tesauro | Zendy; Taylor Schildgen | Zendy; Manfred R. Strecker | Zendy

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Correction: Corrigendum: Glacial isostatic uplift of the European Alps

Author(s) -

Jürgen Mey,

Dirk Scherler,

Andrew D. Wickert,

David L. Egholm,

Magdala Tesauro,

Taylor Schildgen,

Manfred R. Strecker

Publication year - 2017

Publication title -

nature communications

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 5.559

H-Index - 365

ISSN - 2041-1723

DOI - 10.1038/ncomms16138

Subject(s) - deglaciation , younger dryas , post glacial rebound , glacier , glacial period , geology , physical geography , last glacial maximum , geomorphology , geography

Nature Communications 7: Article number:13382 (2016); Published 10 November 2016; Updated 14 July 2017 In an earlier publication, Norton and Hampel proposed post-glacial uplift promoted the re-advance of glaciers at the onset of the Younger Dryas by enlarging their accumulation areas, and estimated a maximum present-day uplift rate due to deglaciation of ∼0.

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