2024
DOI: 10.1007/978-3-031-45762-3_39
|View full text |Cite
|
Sign up to set email alerts
|

Unique Landscape Originated by Cataclysmic Glacial Floods at the Weichselian Glaciation Decline in North-Eastern Poland

Piotr Weckwerth,
Wojciech Wysota
Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

0
5
0

Year Published

2024
2024
2024
2024

Publication Types

Select...
1
1

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(5 citation statements)
references
References 62 publications
0
5
0
Order By: Relevance
“…Th e origin of selected fragments of outwash plains in NW Poland was linked to glacial lake-outburst floods (GLOFs), based on morphometry investigations (Szafraniec 2008(Szafraniec , 2010a(Szafraniec , b, 2013. In the case of NE Poland, largescale subaqueous bedforms were identified, which developed in a proglacial setting and unambiguously indicate the occurrence of extreme high meltwater discharges as catastrophic glacial lake-outburst floods (GLOFs) and prove that the proglacial area was significantly and rapidly transformed during NE Poland's deglaciation (Weckwerth et al 2019(Weckwerth et al , 2020Weckwerth and Wysota 2024).…”
Section: Introductionmentioning
confidence: 91%
See 4 more Smart Citations
“…Th e origin of selected fragments of outwash plains in NW Poland was linked to glacial lake-outburst floods (GLOFs), based on morphometry investigations (Szafraniec 2008(Szafraniec , 2010a(Szafraniec , b, 2013. In the case of NE Poland, largescale subaqueous bedforms were identified, which developed in a proglacial setting and unambiguously indicate the occurrence of extreme high meltwater discharges as catastrophic glacial lake-outburst floods (GLOFs) and prove that the proglacial area was significantly and rapidly transformed during NE Poland's deglaciation (Weckwerth et al 2019(Weckwerth et al , 2020Weckwerth and Wysota 2024).…”
Section: Introductionmentioning
confidence: 91%
“…This region lies at the front of the former SIS margin from the Pomeranian Phase of the Weichselian glaciation (Weckwerth and Wysota 2024). Thus, the border between this basin and the Western and Eastern Suwałki Lakelands is well-defined in morphology and in terms of the extent of glaciofluvial sediments, because these lakelands comprise flat or undulating till plains (Ber 1972(Ber , 1974Bogacki 1976Bogacki , 1980Weckwerth et al 2019;Weckwerth and Wysota 2024).…”
Section: Regional Settingmentioning
confidence: 99%
See 3 more Smart Citations