Outputs (6)

Large-scale reorganization and sedimentation of terrestrial ice streams during late Wisconsinan Laurentide Ice Sheet deglaciation (2010)
Journal Article
Ó Cofaigh, C., Evans, D., & Smith, I. (2010). Large-scale reorganization and sedimentation of terrestrial ice streams during late Wisconsinan Laurentide Ice Sheet deglaciation. GSA Bulletin, 122(5-6), 743-756. https://doi.org/10.1130/b26476.1

Glacial geomorphological mapping of Shuttle Radar Topography Mission (SRTM) data from the western Canadian Prairies demonstrates that during the last (late Wisconsinan)deglaciation of the Laurentide Ice Sheet terrestrial ice streams underwent a major... Read More about Large-scale reorganization and sedimentation of terrestrial ice streams during late Wisconsinan Laurentide Ice Sheet deglaciation.

Micromorphological characteristics of glacimarine sediments: implications for distinguishing genetic processes of massive diamicts (2010)
Journal Article
Kilfeather, A., Ó Cofaigh, C., Dowdeswell, J., van der Meer, J., & Evans, D. (2010). Micromorphological characteristics of glacimarine sediments: implications for distinguishing genetic processes of massive diamicts. Geo-Marine Letters, 30(2), 77-97. https://doi.org/10.1007/s00367-009-0160-8

Glacimarine diamicts are produced by diverse processes, and genetic differentiation is often problematic using macro-sedimentological criteria alone. Micromorphology offers a potentially helpful tool in such investigations. Macroscopically massive di... Read More about Micromorphological characteristics of glacimarine sediments: implications for distinguishing genetic processes of massive diamicts.

A major ice drainage pathway of the last British–Irish Ice Sheet: the Tyne Gap, northern England (2010)
Journal Article
Livingstone, S., Ó Cofaigh, C., & Evans, D. (2010). A major ice drainage pathway of the last British–Irish Ice Sheet: the Tyne Gap, northern England. Journal of Quaternary Science, 25(3), 354-370. https://doi.org/10.1002/jqs.1341

The Tyne Gap is a wide pass, situated between the Scottish Southern Uplands and the English Pennines that connects western and eastern England. It was a major ice flow drainage pathway of the last British–Irish Ice Sheet. This study presents new glac... Read More about A major ice drainage pathway of the last British–Irish Ice Sheet: the Tyne Gap, northern England.

Glaciers and Glaciation (2010)
Book
Benn, D., & Evans, D. (2010). Glaciers and Glaciation. (Second). Hodder Education

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and accessible, it has established a reputation as a comprehensive and essential resource. In this new edition, the text, references, and illustrations have b... Read More about Glaciers and Glaciation.

An assessment of fluting and “till esker” formation on the foreland of Sandfellsjökull, Iceland (2010)
Journal Article
Evans, D., Nelson, C., & Webb, C. (2010). An assessment of fluting and “till esker” formation on the foreland of Sandfellsjökull, Iceland. Geomorphology, 114(3), 453-465. https://doi.org/10.1016/j.geomorph.2009.08.016

Intensive sedimentological analysis of tills, parallel-sided flutings, and a conduit fill (till esker) on the recently deglaciated foreland of Sandfellsjökull (a temperate, actively receding piedmont lobe draining the eastern margin of the Mýrdalsjök... Read More about An assessment of fluting and “till esker” formation on the foreland of Sandfellsjökull, Iceland.

Evolution of a debris-charged glacier landsystem, Kvíárjökull, Iceland (2010)
Journal Article
Bennett, G., Evans, D., Carbonneau, P., & Twigg, D. (2010). Evolution of a debris-charged glacier landsystem, Kvíárjökull, Iceland. Journal of Maps, 2010, 40-67. https://doi.org/10.4113/jom.2010.1114

A time-series of 1:12,500 scale maps of the snout and foreland of the Icelandic glacier Kvíárjökull provides a spatial and temporal assessment of landform evolution from a debris-charged glacier snout over a 58 year period between 1945 and 2003. In a... Read More about Evolution of a debris-charged glacier landsystem, Kvíárjökull, Iceland.