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Outputs (8)

Till deposition by glacier submarginal, incremental thickening (2005)
Journal Article
Evans, D., & Hiemstra, J. (2005). Till deposition by glacier submarginal, incremental thickening. Earth Surface Processes and Landforms, 30(13), 1633-1662. https://doi.org/10.1002/esp.1224

Macro- and micro-scale sedimentological analyses of recently deposited tills and complex push/squeeze moraines on the forelands of Icelandic glaciers and in a stacked till sequence at the former Younger Dryas margin of the Loch Lomond glacier lobe in... Read More about Till deposition by glacier submarginal, incremental thickening.

The Glacier-marginal landsystems of Iceland. (2005)
Book Chapter
Evans, D. (2005). The Glacier-marginal landsystems of Iceland. In C. Caseldine, A. Russell, J. Hardardottir, & O. Knudsen (Eds.), Iceland - Modern Processes and Past Environments (93-126). Elsevier

The last British Ice Sheet: A review of the evidence utilised in the compilation of the Glacial Map of Britain (2005)
Journal Article
Evans, D., Clark, C., & Mitchell, W. (2005). The last British Ice Sheet: A review of the evidence utilised in the compilation of the Glacial Map of Britain. Earth-Science Reviews, 70(3-4), 253-312. https://doi.org/10.1016/j.earscirev.2005.01.001

This paper reviews the evidence presently available (as at December 2003) for the compilation of the Glacial Map of Britain (see [Clark C.D., Evans D.J.A., Khatwa A., Bradwell T., Jordan C.J., Marsh S.H., Mitchell W.A., Bateman, M.D. , 2004. Map and... Read More about The last British Ice Sheet: A review of the evidence utilised in the compilation of the Glacial Map of Britain.

Flow dynamics and till genesis associated with a marine-based Antarctic palaeo-ice stream (2005)
Journal Article
Ó Cofaigh, C., Dowdeswell, J., Allen, C., Hiemstra, J., Pudsey, C., Evans, J., & Evans, D. (2005). Flow dynamics and till genesis associated with a marine-based Antarctic palaeo-ice stream. Quaternary Science Reviews, 24(5-6), 709-740. https://doi.org/10.1016/j.quascirev.2004.10.006

Geophysical and geological data indicate that during the last glacial cycle a palaeo-ice stream drained the Antarctic Peninsula Ice Sheet (APIS) through Marguerite Bay to the edge of the continental shelf via a bathymetric trough (Marguerite Trough).... Read More about Flow dynamics and till genesis associated with a marine-based Antarctic palaeo-ice stream.