Outputs (175)

Sedimentation during MIS 3 at the eastern margins of the Glacial Lake Humber basin, England (2018)
Journal Article
Evans, D. J., Roberts, D. H., Bateman, M. D., Medialdea, A., Ely, J., Moreton, S. G., …Fabel, D. (2018). Sedimentation during MIS 3 at the eastern margins of the Glacial Lake Humber basin, England. Journal of Quaternary Science, 38(3), 871-891. https://doi.org/10.1002/jqs.3066

The stratigraphic sequence at North Cave, on the eastern margins of the Lake Humber basin, records the deposition of a fluvioperiglacial fan (LFs 1–4), with early sedimentation (LF1) dating to Marine Isotope Stage (MIS) 3 (optically stimulated lumine... Read More about Sedimentation during MIS 3 at the eastern margins of the Glacial Lake Humber basin, England.

Glacial geomorphology of Teesdale, northern Pennines, England: Implications for upland styles of ice stream operation and deglaciation in the British-Irish Ice Sheet (2018)
Journal Article
Evans, D. J., Dinnage, M., & Roberts, D. H. (2018). Glacial geomorphology of Teesdale, northern Pennines, England: Implications for upland styles of ice stream operation and deglaciation in the British-Irish Ice Sheet. Proceedings of the Geologists' Association, 129(6), 697-735. https://doi.org/10.1016/j.pgeola.2018.05.001

The glacial geomorphology of Teesdale and the North Pennines uplands is analysed in order to decipher: a) the operation of easterly flowing palaeo-ice streams in the British-Irish Ice Sheet; and b) the style of regional deglaciation. Six landform cat... Read More about Glacial geomorphology of Teesdale, northern Pennines, England: Implications for upland styles of ice stream operation and deglaciation in the British-Irish Ice Sheet.

Lack of evidence for a substantial sea-level fluctuation within the Last Interglacial (2018)
Journal Article
Barlow, N., McClymont, E., Whitehouse, P., Stokes, C., Jamieson, S., Woodroffe, S., …Sanchez-Montes, M. (2018). Lack of evidence for a substantial sea-level fluctuation within the Last Interglacial. Nature Geoscience, 11, 627-634. https://doi.org/10.1038/s41561-018-0195-4

During the Last Interglacial, global mean sea level reached approximately 6 to 9 m above the present level. This period of high sea level may have been punctuated by a fall of more than 4 m, but a cause for such a widespread sea-level fall has been e... Read More about Lack of evidence for a substantial sea-level fluctuation within the Last Interglacial.

Glacial geomorphological mapping: A review of approaches and frameworks for best practice (2018)
Journal Article
Chandler, B. M., Lovell, H., Boston, C. M., Lukas, S., Barr, I. D., Benediktsson, Í. Ö., …Stroeven, A. P. (2018). Glacial geomorphological mapping: A review of approaches and frameworks for best practice. Earth-Science Reviews, 185, 806-846. https://doi.org/10.1016/j.earscirev.2018.07.015

Geomorphological mapping is a well-established method for examining earth surface processes and landscape evolution in a range of environmental contexts. In glacial research, it provides crucial data for a wide range of process-oriented studies and p... Read More about Glacial geomorphological mapping: A review of approaches and frameworks for best practice.

Ice margin oscillations during deglaciation of the northern Irish Sea Basin (2018)
Journal Article
Chiverrell, R., Smedley, R., Small, D., Ballantyne, C., Burke, M., Callard, S., …Wilson, P. (2018). Ice margin oscillations during deglaciation of the northern Irish Sea Basin. Journal of Quaternary Science, 33(7), 739-762. https://doi.org/10.1002/jqs.3057

We present a new chronology to constrain ice‐margin retreat in the northern Irish Sea Basin. Estimates on the timing of ice thinning derived from surface exposure ages for boulders from the summits of the Isle of Man and south‐west Cumbria suggest th... Read More about Ice margin oscillations during deglaciation of the northern Irish Sea Basin.

Submarginal debris transport and till formation in active temperate glacier systems: The southeast Iceland type locality (2018)
Journal Article
Evans, D. J., Roberts, D. H., Hiemstra, J. F., Nye, K. M., Wright, H., & Steer, A. (2018). Submarginal debris transport and till formation in active temperate glacier systems: The southeast Iceland type locality. Quaternary Science Reviews, 195, 72-108. https://doi.org/10.1016/j.quascirev.2018.07.002

Exhaustive sedimentological analysis of freshly exposed subglacial surfaces and moraines in southern Iceland provides diagnostic sedimentological signatures of: a) debris transport pathways through active temperate glacier snouts; and b) till product... Read More about Submarginal debris transport and till formation in active temperate glacier systems: The southeast Iceland type locality.

The Glacial Geomorphology of the Ice Cap Piedmont Lobe Landsystem of East Mýrdalsjökull, Iceland (2018)
Journal Article
Evans, D., Ewertowski, M., Orton, C., & Graham, D. (2018). The Glacial Geomorphology of the Ice Cap Piedmont Lobe Landsystem of East Mýrdalsjökull, Iceland. Geosciences, 8(6), Article 194. https://doi.org/10.3390/geosciences8060194

A surficial geology and geomorphology map of the forelands of the Sandfellsjökull and Oldufellsjökull piedmont lobes of the east Mýrdalsjökull ice cap is used to characterise the historical and modern landscape imprint in a glacial landsystems contex... Read More about The Glacial Geomorphology of the Ice Cap Piedmont Lobe Landsystem of East Mýrdalsjökull, Iceland.

Trough geometry was a greater influence than climate-ocean forcing in regulating retreat of the marine-based Irish-Sea Ice Stream (2018)
Journal Article
Small, D., Smedley, R., Chiverrell, R., Scourse, J., Ó Cofaigh, C., Duller, G., …Clark, C. (2018). Trough geometry was a greater influence than climate-ocean forcing in regulating retreat of the marine-based Irish-Sea Ice Stream. GSA Bulletin, 130(11-12), 1981-1999. https://doi.org/10.1130/b31852.1

Marine terminating ice streams are a major component of contemporary ice sheets and are likely to have a fundamental influence on their future evolution and concomitant contribution to sea-level rise. To accurately predict this evolution requires tha... Read More about Trough geometry was a greater influence than climate-ocean forcing in regulating retreat of the marine-based Irish-Sea Ice Stream.

Bedrock mega-grooves in glaciated terrain: a review (2018)
Journal Article
Newton, M., Evans, D., Roberts, D., & Stokes, C. (2018). Bedrock mega-grooves in glaciated terrain: a review. Earth-Science Reviews, 185, 57-79. https://doi.org/10.1016/j.earscirev.2018.03.007

Bedrock mega-grooves are assemblages of straight and parallel troughs eroded in bedrock, typically over 1000 m in length; most sites occur within the limits of the Last Glacial Maximum, both on- and off-shore. In this paper, we review the current und... Read More about Bedrock mega-grooves in glaciated terrain: a review.

Geomorphology and till architecture of terrestrial palaeo-ice streams of the southwest Laurentide Ice Sheet: a borehole stratigraphic approach (2018)
Journal Article
Norris, S., Evans, D., & O Cofaigh, C. (2018). Geomorphology and till architecture of terrestrial palaeo-ice streams of the southwest Laurentide Ice Sheet: a borehole stratigraphic approach. Quaternary Science Reviews, 186, 186-214. https://doi.org/10.1016/j.quascirev.2017.12.018

A multidimensional study, utilising geomorphological mapping and the analysis of regional borehole stratigraphy, is employed to elucidate the regional till architecture of terrestrial palaeo-ice streams relating to the Late Wisconsinan southwest Laur... Read More about Geomorphology and till architecture of terrestrial palaeo-ice streams of the southwest Laurentide Ice Sheet: a borehole stratigraphic approach.