Weichselian upper pleniglacial aeolian and ice‐cored morphology in the southern Netherlands (Noord‐Brabant, groote peel)

• Published in: Permafrost and Periglacial Processes
• Main Authors: Kasse, K., Bohncke, S.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1992
• Subjects: ice core; Permafrost and Periglacial Processes
• Online Access: http://dx.doi.org/10.1002/ppp.3430030407; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030407; https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030407

Abstract The morphology of the Weichselian Late Pleniglacial land surface in the Groote Peel nature reserve (southern Netherlands) is characterized by numerous circular to oval depressions. The depressions are up to 90 m wide and 3 m deep. Some are surrounded by low (50–100 cm) ridges. Two depressions were selected for detailed study. One, of aeolian origin, is shallow (less than 1 m), the underlying sedimentary units are undisturbed and the ridge surrounding it consists of horizontally bedded aeolian sand. The second, formed by the melting of an ice core, is deeper (3 m) and dissects older units. The ice lens probably formed during the Weichselian Late Pleniglacial. Ice segregation was favoured by a low topographic gradient, impermeable beds in the subsoil and poor drainage. After partial decay of the ice core, a remnant survived during the cold, arid conditions of the Beuningen deflation phase. Final melting of the ice core occurred after deposition of Late Pleniglacial aeolian coversand, at the onset of the Late Glacial climatic amelioration. Palynological analysis indicates that infilling of the ice‐core depression started in the Late Glacial Older Dryas and possibly even during Oldest Dryas.