New geomorphic evidence for a multi‐stage proglacial lake associated with the former British–Irish Ice Sheet in the Vale of Pickering, Yorkshire, UK

Abstract

Former proglacial lakes provide insight into the temporal and spatial evolution of past ice sheet dynamics and the glaciohydrological systems associated with them. Glacial Lake Pickering was a proglacial lake in North Yorkshire impounded by the British-Irish Ice Sheet. However, geomorphic evidence for its existence and extent is weak and contested. This paper presents, for the first time, systematic mapping of geomorphic features from high-resolution (50 cm to 5 m) digital terrain model data and undertakes palaeogeographical reconstructions to establish Palaeolake Pickering's extent and levels. Results show only weak evidence for a 70-m lake. This and the fact that the present landscape configuration is unable to impound such a large lake suggests that it either did not exist or is much older and that considerable landscape erosion has since taken place. There is good geomorphological evidence to support lake levels between 45 and 20 m. The new palaeogeographical reconstructions show these lake levels were initially controlled by the balance between the North Sea and the Vale of York Lobes of the British-Irish Ice Sheet with lower and later levels impounded by the Filey moraine. A multi-stage Palaeolake Pickering with various extents and levels possibly spanning more than one glacial period has implications for other British-Irish Ice Sheet palaeolake extents reconstructed only from undifferentiated lacustrine sediments and their maximal elevation. The existence of an extensive multi-phase proglacial Palaeolake Pickering along with other similar ones in Eastern England would have impacted mass loss and frontal dynamics via subaqueous melting and iceberg calving, potentially playing a role in controlling the dynamic behaviour of the North Sea Lobe.

Pleistocene river diversions caused by large landslides in the western Pyrenees (Oria River drainage basin, N Spain)

“…The elevation of the highest fan delta preserved is constrained (limited) by the lowest elevation of the original river basin divide at the site of the new divide. As the latter is progressively eroded, other fan deltas can develop at lower elevations, the earlier ones being variably preserved, dissected or even dug out (Eddey et al, 2022; Link et al, 2014).…”