Article
Bradwell T (2025) Was Scotland covered by an ice sheet during Marine Isotope Stage 4? Insights from the pre-Last Glacial Maximum marine terraces of northwest Scotland. Journal of Quaternary Science.
NSF-GEO-NERC: How important are sea-level feedbacks in stabilizing marine-based ice streams?
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Funded by Natural Environment Research Council.
Collaboration with Durham University, University of California, Santa Barbara, University of Gloucestershire and University of Sheffield.
The overall objective of this proposal is to use the retreat history of the former Minch Ice Stream (Northwest Scotland) to better understand how glaciers and ice streams respond to sea-level changes across a variety of rheological and glaciological settings. Our goal is to better understand the interplay between ice sheets and sea-level change in sensitive marine-based ice streams.
Total award value £31,724.80