A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6

During the last (MIS 2) and older glaciations of the North Sea, a North Sea Lobe (NSL) of the British-Irish Ice Sheet flowed onshore and terminated on the lowlands of eastern England, constructing inset sequences of either substantial ice-marginal deposits and tills or only a thin till veneer, indic...

Full description

Bibliographic Details
Published in:Proceedings of the Geologists' Association
Main Authors: Evans, David J.A., Roberts, David H., Bateman, Mark D., Ely, Jeremy, Medialdea, Alicia, Burke, Matthew J., Chiverrell, Richard C., Clark, Chris D., Fabel, Derek
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2019
Subjects:
Online Access:http://eprints.gla.ac.uk/221640/
http://eprints.gla.ac.uk/221640/1/221640.pdf
id ftuglasgow:oai:eprints.gla.ac.uk:221640
record_format openpolar
spelling ftuglasgow:oai:eprints.gla.ac.uk:221640 2023-05-15T16:41:13+02:00 A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6 Evans, David J.A. Roberts, David H. Bateman, Mark D. Ely, Jeremy Medialdea, Alicia Burke, Matthew J. Chiverrell, Richard C. Clark, Chris D. Fabel, Derek 2019-10 text http://eprints.gla.ac.uk/221640/ http://eprints.gla.ac.uk/221640/1/221640.pdf en eng Elsevier http://eprints.gla.ac.uk/221640/1/221640.pdf Evans, D. J.A., Roberts, D. H., Bateman, M. D., Ely, J., Medialdea, A., Burke, M. J., Chiverrell, R. C., Clark, C. D. and Fabel, D. <http://eprints.gla.ac.uk/view/author/5585.html> (2019) A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6. Proceedings of the Geologists’ Association <http://eprints.gla.ac.uk/view/journal_volume/Proceedings_of_the_Geologists==2019_Association.html>, 130(5), pp. 523-540. (doi:10.1016/j.pgeola.2018.10.004 <http://dx.doi.org/10.1016/j.pgeola.2018.10.004>) cc_by_nc_nd_4 CC-BY-NC-ND Articles PeerReviewed 2019 ftuglasgow https://doi.org/10.1016/j.pgeola.2018.10.004 2020-08-27T22:10:18Z During the last (MIS 2) and older glaciations of the North Sea, a North Sea Lobe (NSL) of the British-Irish Ice Sheet flowed onshore and terminated on the lowlands of eastern England, constructing inset sequences of either substantial ice-marginal deposits and tills or only a thin till veneer, indicative of complex and highly dynamic glaciological behaviour. The glaciation limit represented by the Marsh Tills and the Stickney and Horkstow Moraines in Lincolnshire is regarded as the maximum margin of the NSL during MIS 2 and was attained at ∼19.5 ka as determined by OSL dating of overridden lake sediments at Welton le Wold. A later ice marginal position is recorded by the Hogsthorpe-Killingholme Moraine belt, within which ice-walled lake plains indicate large scale ice stagnation rapidly followed ice advance at ∼18.4 ka based on dates from supraglacial lake deposits. The NSL advanced onshore in North Norfolk slightly earlier constructing a moraine ridge at Garrett Hill at ∼21.5ka. In addition to the large ice-dammed lakes in the Humber and Wash lowlands, we propose that an extensive Glacial Lake Lymn was dammed in the southern Lincolnshire Wolds by the NSL ice margin at the Stickney Moraine. Previous proposals that older glacier limits might be recorded in the region, lying between MIS 2 and MIS 12 deposits, are verified by our OSL dates on the Stiffkey moraine, which lies immediately outside the Garrett Hill moraine and appears to be of MIS 6 age. Article in Journal/Newspaper Ice Sheet University of Glasgow: Enlighten - Publications Glacial Lake ENVELOPE(-129.463,-129.463,58.259,58.259) Moraine Ridge ENVELOPE(168.050,168.050,-72.300,-72.300) Proceedings of the Geologists' Association 130 5 523 540
institution Open Polar
collection University of Glasgow: Enlighten - Publications
op_collection_id ftuglasgow
language English
description During the last (MIS 2) and older glaciations of the North Sea, a North Sea Lobe (NSL) of the British-Irish Ice Sheet flowed onshore and terminated on the lowlands of eastern England, constructing inset sequences of either substantial ice-marginal deposits and tills or only a thin till veneer, indicative of complex and highly dynamic glaciological behaviour. The glaciation limit represented by the Marsh Tills and the Stickney and Horkstow Moraines in Lincolnshire is regarded as the maximum margin of the NSL during MIS 2 and was attained at ∼19.5 ka as determined by OSL dating of overridden lake sediments at Welton le Wold. A later ice marginal position is recorded by the Hogsthorpe-Killingholme Moraine belt, within which ice-walled lake plains indicate large scale ice stagnation rapidly followed ice advance at ∼18.4 ka based on dates from supraglacial lake deposits. The NSL advanced onshore in North Norfolk slightly earlier constructing a moraine ridge at Garrett Hill at ∼21.5ka. In addition to the large ice-dammed lakes in the Humber and Wash lowlands, we propose that an extensive Glacial Lake Lymn was dammed in the southern Lincolnshire Wolds by the NSL ice margin at the Stickney Moraine. Previous proposals that older glacier limits might be recorded in the region, lying between MIS 2 and MIS 12 deposits, are verified by our OSL dates on the Stiffkey moraine, which lies immediately outside the Garrett Hill moraine and appears to be of MIS 6 age.
format Article in Journal/Newspaper
author Evans, David J.A.
Roberts, David H.
Bateman, Mark D.
Ely, Jeremy
Medialdea, Alicia
Burke, Matthew J.
Chiverrell, Richard C.
Clark, Chris D.
Fabel, Derek
spellingShingle Evans, David J.A.
Roberts, David H.
Bateman, Mark D.
Ely, Jeremy
Medialdea, Alicia
Burke, Matthew J.
Chiverrell, Richard C.
Clark, Chris D.
Fabel, Derek
A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6
author_facet Evans, David J.A.
Roberts, David H.
Bateman, Mark D.
Ely, Jeremy
Medialdea, Alicia
Burke, Matthew J.
Chiverrell, Richard C.
Clark, Chris D.
Fabel, Derek
author_sort Evans, David J.A.
title A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6
title_short A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6
title_full A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6
title_fullStr A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6
title_full_unstemmed A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6
title_sort chronology for north sea lobe advance and recession on the lincolnshire and norfolk coasts during mis 2 and 6
publisher Elsevier
publishDate 2019
url http://eprints.gla.ac.uk/221640/
http://eprints.gla.ac.uk/221640/1/221640.pdf
long_lat ENVELOPE(-129.463,-129.463,58.259,58.259)
ENVELOPE(168.050,168.050,-72.300,-72.300)
geographic Glacial Lake
Moraine Ridge
geographic_facet Glacial Lake
Moraine Ridge
genre Ice Sheet
genre_facet Ice Sheet
op_relation http://eprints.gla.ac.uk/221640/1/221640.pdf
Evans, D. J.A., Roberts, D. H., Bateman, M. D., Ely, J., Medialdea, A., Burke, M. J., Chiverrell, R. C., Clark, C. D. and Fabel, D. <http://eprints.gla.ac.uk/view/author/5585.html> (2019) A chronology for North Sea Lobe advance and recession on the Lincolnshire and Norfolk coasts during MIS 2 and 6. Proceedings of the Geologists’ Association <http://eprints.gla.ac.uk/view/journal_volume/Proceedings_of_the_Geologists==2019_Association.html>, 130(5), pp. 523-540. (doi:10.1016/j.pgeola.2018.10.004 <http://dx.doi.org/10.1016/j.pgeola.2018.10.004>)
op_rights cc_by_nc_nd_4
op_rightsnorm CC-BY-NC-ND
op_doi https://doi.org/10.1016/j.pgeola.2018.10.004
container_title Proceedings of the Geologists' Association
container_volume 130
container_issue 5
container_start_page 523
op_container_end_page 540
_version_ 1766031658320920576