|Appears in Collections:||Biological and Environmental Sciences Book Chapters and Sections|
|Title:||Recessional moraines in nearshore waters, northern Scotland|
|Citation:||Bradwell T & Stoker M (2016) Recessional moraines in nearshore waters, northern Scotland. In: Dowdeswell J, Canals M, Jakobsson M, Todd B, Dowdeswell E & Hogan K (eds.) Atlas of Submarine Glacial Landforms: Modern, Quaternary and Ancient. Geological Society Memoir, 46. London: Geological Society of London, pp. 63-64. http://mem.lyellcollection.org/content/46/1/63; https://doi.org/10.1144/M46.13|
|Series/Report no.:||Geological Society Memoir, 46|
|Abstract:||First paragraph: Suites of relatively small, similar-sized and regularly spaced sediment ridges are commonly found fronting the termini of modern tidewater glaciers in fjords and marine embayments. These ice-flow transverse subaqueous moraine ridges, sometimes referred to as De Geer moraines, record the incremental retreat of the ice front grounding-line over time (De Geer 1889;Lindén & Möller 2005). The distribution and pattern of well-preserved recessional moraines in nearshore waters around Scotland provides insight into the pattern, timing and style of retreat of the last British–Irish Ice Sheet (Bradwellet al.2008a,b;Stokeret al.2009).|
|Rights:||This item has been embargoed for a period. During the embargo please use the Request a Copy feature at the foot of the Repository record to request a copy directly from the author. You can only request a copy if you wish to use this work for your own research or private study. Publisher policy allows this work to be made available in this repository. Published in Atlas of Submarine Glacial Landforms: Modern, Quaternary and Ancient. Geological Society, London, Memoirs, 46, 63-64 by Geological Society of London. The original publication is available at: https://doi.org/10.1144/M46.13|
|BRADWELL_ASGL_2pp_REVISED.pdf||Fulltext - Accepted Version||626.91 kB||Adobe PDF||View/Open|
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