2019
DOI: 10.1016/j.earscirev.2019.05.006
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Late Weichselian glacier outburst floods in North-Eastern Poland: Landform evidence and palaeohydraulic significance

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Cited by 45 publications
(33 citation statements)
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“…The lake basin itself is located in the Szeszupa Depression, which was formed as a consequence of dead ice melting in the late glacial (Smolska, 1996). The ice sheet had already retreated from the Szeszupa Depression between 17.9 and 14.4cal ka BP (Dzierżek and Zreda, 2007; Weckwerth et al, 2019) and, according to pollen stratigraphy, lacustrine sedimentation had begun in the Allerød (Kupryjanowicz, M., unpublished data). Lacustrine sedimentation started at sites investigated nearby during the same period, such as Lake Linówek (3 km to the southwest) at ca.…”
Section: Introductionmentioning
confidence: 99%
“…The lake basin itself is located in the Szeszupa Depression, which was formed as a consequence of dead ice melting in the late glacial (Smolska, 1996). The ice sheet had already retreated from the Szeszupa Depression between 17.9 and 14.4cal ka BP (Dzierżek and Zreda, 2007; Weckwerth et al, 2019) and, according to pollen stratigraphy, lacustrine sedimentation had begun in the Allerød (Kupryjanowicz, M., unpublished data). Lacustrine sedimentation started at sites investigated nearby during the same period, such as Lake Linówek (3 km to the southwest) at ca.…”
Section: Introductionmentioning
confidence: 99%
“…Ochyra and Tomaszewicz 1982 ), but was found only at one site near Błaskowizna on 17 July 2017. A very wet mire on thick peat deposits is developed there in a depression, surrounded by parallel, arched and prominent ridges of moraines (glacial curvilineations created by catastrophic megafloods during last glaciation; Weckwerth et al 2019 ). The vegetation represents Pinus - Betula swamp forests, peatbogs and fens, with many relic species (most notable: Eriophorum gracile W. D. J. Koch ex Roth, Baeothryon alpinum T. V. Egorova, Pseudocalliergon trifarium (F. Weber & D. Mohr) Loeske and Scorpidium scorpioides (Hedw.)…”
Section: Methodsmentioning
confidence: 99%
“…If meltwater is stored in an ice dammed lake, it may be released in a catastrophic event which has the potential to scour the topography, erode and transport large volumes of sediments far offshore. Examples include; breaching of the land connection between present-day France and Great Britain, through the English Channel, sculpting large sandur areas in NE Poland and breaching a topographic high in Germany (Gupta et al, 2017;Meinsen et al, 2011;Weckwerth et al, 2019). An even more extreme example can be found between Labrador and Greenland in the Labrador Sea; submarine channels originate at the shelf edge and extend all the way to the abyssal plain in water depths of 3 -4 km.…”
Section: Extreme Scenariosmentioning
confidence: 99%