Abstract
An accurate picture of relative sea-level (RSL) change is a prerequisite for understanding the Quaternary history of Ireland. Consequently, sea-level research has been a prominent feature of Irish Quaternary science since its foundations in the 19th century. Over the intervening years, the methods used to study past RSL have evolved, although many of the fundamental challenges associated with its precise reconstruction remain. Ireland’s RSL history is complex and highly variable in space and over time. The quest to better understand the multiple, interacting processes driving these changes is a work in progress. This chapter provides a synopsis of RSL change around the coast of Ireland, with particular reference to recently published work and areas of current debate. It reviews the information obtained from the study of raised shorelines, focussing on the evidence for ‘pre-glacial’ sea levels. It then examines the general patterns of RSL change since the Last Glacial Maximum as inferred from geological data and geophysical modelling. The chapter concludes by briefly discussing the timing and significance of RSL maxima and minima around the Irish coast along with their implications for Ireland’s physical connection to Britain and Europe.
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Acknowledgments
Thanks to Glenn Milne, Joseph Kuchar and Sarah Bradley for supplying data and comments on the glacial rebound modelling. We are grateful to colleagues for supplying pre-prints of material that was unpublished at the time of writing. We are grateful to Helen Roe for her helpful comments on this chapter.
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Edwards, R., Craven, K. (2017). Relative Sea-Level Change Around the Irish Coast. In: Coxon, P., McCarron, S., Mitchell, F. (eds) Advances in Irish Quaternary Studies. Atlantis Advances in Quaternary Science , vol 1. Atlantis Press, Paris. https://doi.org/10.2991/978-94-6239-219-9_7
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