Abstract. Reconstructing the growth and decay of palaeo-ice sheets
is critical to understanding the relationships between global climate and
sea-level change and to testing numerical ice sheet models. In this study,
we integrate recently acquired high-resolution 2D seismic reflection and
borehole datasets from two wind-farm sites offshore of the Netherlands to
investigate the sedimentary, geomorphological, and glaciotectonic records
left by the Saalian Drenthe substage glaciation, when Scandinavian land ice
reached its southernmost extent in the southern North Sea (ca. 160 ka,
Marine Isotope Stage 6). A complex assemblage of glaciogenic sediments and
glaciotectonic structures is buried in the shallow subsurface. The northern
wind-farm site revealed a set of NE–SW-oriented subglacial meltwater channels
filled with till and glaciofluvial sediments and an E–W-trending composite
ridge with local evidence of intense glaciotectonic deformation that denotes
the maximum limit reached by the ice. Based on the identified glacial
geomorphology, we refine the mapping of the maximum ice sheet extent
offshore, revealing that the ice margin morphology is more complex than
previously envisaged and displaying a lobate shape. Ice retreat left an
unusual paraglacial landscape characterised by the progressive infilling of
topographic depressions carved by ice-driven erosion and a diffuse drainage
network of outwash channels. The net direction of outwash was to the west
and southwest into a nearby glacial basin. We demonstrate the utility of
offshore wind-farm data as records of process–form relationships preserved in
buried landscapes, which can be utilised in refining palaeo-ice sheet
margins and informing longer-term drivers of change in low-relief settings.
Abstract. Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding the relationships between global climate and sea-level change, and to testing numerical ice sheet models. In this study, we integrate recently acquired high-resolution 2D-seismic reflection and borehole datasets from two windfarm sites offshore the Netherlands to investigate the sedimentary, geomorphological and glaciotectonic records left by the Saalian Drenthe substage glaciation, when Scandinavian land ice reached its southernmost extent in the southern North Sea (ca. 160 ka, Marine Isotope Stage 6). A complex assemblage of glaciogenic sediments and glaciotectonic structures are buried in the shallow subsurface. The northern windfarm site revealed a set of NE-SW oriented subglacial meltwater channels filled with till and glaciofluvial sediments and an E-W trending composite ridge with local evidence of intense glaciotectonic deformation that denotes the maximum limit reached by the ice. Based on the identified glacial geomorphology, we refine the mapping of the maximum ice-sheet extent offshore the Netherlands, revealing that the ice margin morphology is more complex than previously envisaged, displaying a lobate shape. Ice retreat left an unusual paraglacial landscape characterised by the progressive infilling of topographic depressions carved during the ice advance and a diffuse drainage network of outwash channels. The net direction of outwash was to the west and southwest into a nearby glacial basin. Antecedent topography influenced subglacial bed conditions, and their impact on ice dynamics during the glaciation and deglaciation stages. We demonstrate the utility of offshore windfarm data in refining palaeo ice margin limits, and the record of processes interactions preserved in buried landscapes to help inform longer-term drivers of change at low relief ice margins.
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