The North European Plain

Woronko, Barbara; Dąbski, Maciej

doi:10.1007/978-3-031-14895-8_12

Cited by 1 publication

(1 citation statement)

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“…But how can we explain the occurrence of similar landforms in an aseismic area with a stable bedrock and lacking salt domes? The features identified by us are in an area that was covered by permafrost during the Vistulian glaciation (Woronko & Dąbski, 2022). The aim of the research was to determine the origin and evolution of the surface cracks in a different geological setting compared to northern Germany during the Late Glacial and Holocene.…”

Section: Introductionmentioning

confidence: 99%

Origin and post‐glacial evolution of surface cracks: A case study from the area of the Last Glaciation, north‐eastern Poland

Karasiewicz,

Hrynowiecka,

Weckwerth

et al. 2023

Earth Surf Processes Landf

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The analysis of LiDAR‐based digital elevation models revealed the existence of groups of longitudinal fractures in the ground in northern Poland at the limit of the ice sheet's extent during its last maximum. Our research on the closed elongated depressions (CEDs) of the Jedwabno test field (Szuć site, north‐east Poland) focuses on explaining their origins and their post‐glacial history. This region was covered by an ice sheet and glacitectonically active during the Vistulian, and at least some surface fractures are possible witnesses to this activity. Using geomorphological mapping, sedimentological and geophysical research, we assumed it was related that the origin of these features here is associated with groundwater migration at the end of the Vistulian glaciation or later when groundwater flow intensified due to a rapid climate warming that caused permafrost to melt. The thawing of permafrost caused to transition from continuous permafrost to discontinuous, which in turn created groundwater flow that was probably responsible for the development of the surface cracks (fractures). Radiocarbon, palaeobiological (pollen, Cladocera) and geochemical studies allowed for an estimation of the formation time of these unique surface cracks in the Older Dryas. Prevailing conditions were also reconstructed for the later dynamic changes of the end of the Late Vistulian glaciation and in the Late Holocene until the Subatlantic Period (Megalayan stage). The surface cracks with steep slopes, despite their small area, are extraordinary sedimentation traps that have, in a special way, retained an almost complete record of the environmental and climate changes of the Late Glacial. There are sedimentological gaps in the Holocene, especially after the Preboreal (old part of the Greenlandian Stage), caused by changes in water levels, aeolian processes and human activity.

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Section: Introductionmentioning

confidence: 99%