http://earthwise.bgs.ac.uk/index.php?action=history&feed=atom&title=File%3AP916098.jpg 2026-06-30T11:35:07Z Revision history for this page on the wiki MediaWiki 1.42.3 http://earthwise.bgs.ac.uk/index.php?title=File:P916098.jpg&diff=27049&oldid=prev 2016-04-12T17:22:33Z

<p>User created page with UploadWizard</p> <p><b>New page</b></p><div>=={{int:filedesc}}==<br /> {{Information<br /> |description={{|1=Speculative reconstructions of the last ice sheet. a At about the Last Glacial Maximum (LGM): 28?22 ka BP, but when Scottish ice had ceased flowing across Stainmore, and Scandinavian ice had advanced into the central North Sea Basin, forcing ice from the Pennines and Tweed Basin to flow into the Vale of York. b Following a major glacial reorganisation involving ?drawdown? and ?headward scavenging? of the Irish Sea ice stream into the Solway lowlands and Vale of Eden. Exact timing and correlation of events is unknown, but North Sea ice pushed farther into the Teesside lowlands once ice from the Lake District ceased flowing across Stainmore. Subglacial glaciofluvial deposition probably occurred within tunnel valleys in the Durham lowlands prior to the creation of Glacial Lake Wear. c Scottish ice advances into the Solway lowlands following retreat of ice sourced in the Lake District. Multiple readvances affect the Isle of Man and the west Cumbrian coast. Figure 68 in Stone, P, Millward, D, Young, B, Merritt, J W, Clarke, S M, McCormac, M and Lawrence, D J D. 2010. British regional geology: Northern England. Fifth edition. Keyworth, Nottingham: British Geological Survey.}}<br /> |date=2016-04-12 18:19:13<br /> |source=British Geological Survey<br /> |author=British Geological Survey<br /> |permission=<br /> |other versions=<br /> }}<br /> <br /> =={{int:license-header}}==<br /> {{subst:Custom license marker added by UW}}<br /> {{BGS}}<br /> <br /> [[Category:Uploaded with UploadWizard]]</div>

Scotfot