European Glacial Landscapes 2023
DOI: 10.1016/b978-0-323-91899-2.00008-5
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Northern Central Europe: glacial landforms during deglaciation (18.9–14.9 ka)

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Cited by 4 publications
(2 citation statements)
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“…ka BP, respectively (Hughes et al 2016;Stroeven et al 2016;Clark et al 2022;Esteves et al 2023). In contrast, the southeastern margin of the FIS was initially terrestrial and experienced an overall comparatively slow retreat, although interrupted by several ice-margin standstills and re-advances (Marks et al 2023), before ice marginal retreat accelerated by c. 16 cal. ka BP (Hughes et al 2016;Stroeven et al 2016) through calving in the Baltic Ice Lake that had developed in front of the receding ice sheet (Bj€ orck 1995).…”
Section: Deglaciation and Emergence Of The Fennoscandian Landscapementioning
confidence: 99%
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“…ka BP, respectively (Hughes et al 2016;Stroeven et al 2016;Clark et al 2022;Esteves et al 2023). In contrast, the southeastern margin of the FIS was initially terrestrial and experienced an overall comparatively slow retreat, although interrupted by several ice-margin standstills and re-advances (Marks et al 2023), before ice marginal retreat accelerated by c. 16 cal. ka BP (Hughes et al 2016;Stroeven et al 2016) through calving in the Baltic Ice Lake that had developed in front of the receding ice sheet (Bj€ orck 1995).…”
Section: Deglaciation and Emergence Of The Fennoscandian Landscapementioning
confidence: 99%
“…In contrast, the southeastern margin of the FIS was initially terrestrial and experienced an overall comparatively slow retreat, although interrupted by several ice‐margin standstills and re‐advances (Marks et al . 2023), before ice marginal retreat accelerated by c . 16 cal.…”
Section: Deglaciation and Emergence Of The Fennoscandian Landscapementioning
confidence: 99%