Sedimentology of a debris-rich, perhumid valley glacier margin in the Rakaia Valley, South Island,New Zealand
(2012)
Journal Article
Hyatt, O., Shulmeister, J., Evans, D., Thackray, G., & Rieser, U. (2012). Sedimentology of a debris-rich, perhumid valley glacier margin in the Rakaia Valley, South Island,New Zealand. Journal of Quaternary Science, 27(7), 699-712. https://doi.org/10.1002/jqs.2556
Outputs (10)
Dartmoor’s overlooked glacial legacy. (2012)
Journal Article
Evans, D., Harrison, S., Vieli, A., & Anderson, E. (2012). Dartmoor’s overlooked glacial legacy. Geology Today, 28(6), 224-229. https://doi.org/10.1111/j.1365-2451.2012.00855.x
Glacier retreat and landform production on an overdeepened glacier foreland: the debris-charged glacial landsystem at Kvíárjökull, Iceland. (2012)
Journal Article
Bennett, G., & Evans, D. (2012). Glacier retreat and landform production on an overdeepened glacier foreland: the debris-charged glacial landsystem at Kvíárjökull, Iceland. Earth Surface Processes and Landforms, 37(15), 1584-1602. https://doi.org/10.1002/esp.3259
The subglacial and ice-marginal signature of the North Sea Lobe of the British–Irish Ice Sheet during the Last Glacial Maximum at Upgang, North Yorkshire, UK. (2012)
Journal Article
Roberts, D., Evans, D., Lodwick, J., & Cox, N. (2012). British–Irish Ice Sheet during the Last Glacial Maximum at Upgang, North Yorkshire, UK. Proceedings of the Geologists' Association, https://doi.org/10.1016/j.pgeola.2012.08.009
Glaciodynamics of the central sector of the last British–Irish Ice Sheet in Northern England. (2012)
Journal Article
Livingstone, S., Evans, D., Ó Cofaigh, C., Davies, B., Merritt, J., Huddart, D., …Yorke, L. (2012). Glaciodynamics of the central sector of the last British–Irish Ice Sheet in Northern England. Earth-Science Reviews, 111, 25-55. https://doi.org/10.1016/j.earscirev.2011.12.006
Hørbyebreen polythermal glacial landsystem, Svalbard. (2012)
Journal Article
Evans, D., Strzeleckia, M., Milledge, D., & Orton, C. (2012). Hørbyebreen polythermal glacial landsystem, Svalbard. Journal of Maps, 2012, 1-11
Stratigraphic architecture and sedimentology of a Late Pleistocene subaqueous moraine complex, southwest Ireland. (2012)
Journal Article
Evans, D., Hiemstra, J., & O´ Cofaigh, C. (2012). Stratigraphic architecture and sedimentology of a Late Pleistocene subaqueous moraine complex, southwest Ireland. Journal of Quaternary Science, 27, 51-63. https://doi.org/10.1002/jqs.1513
Till stratigraphy and sedimentology at the margins of terrestrially terminating ice streams: case study of the western Canadian prairies and high plains. (2012)
Journal Article
Evans, D., Hiemstra, J., Boston, C., Leighton, I., Ó Cofaigh, C., & Rea, B. (2012). Till stratigraphy and sedimentology at the margins of terrestrially terminating ice streams: case study of the western Canadian prairies and high plains. Quaternary Science Reviews, 46, 80-125. https://doi.org/10.1016/j.quascirev.2012.04.028Complex glacigenic sediment sequences arranged in large arcuate assemblages and demarcating the lobate termini of fast ice flow corridors in western Canada represent the terrestrial equivalents of the trough-mouth fans of the marine palaeo-ice stream... Read More about Till stratigraphy and sedimentology at the margins of terrestrially terminating ice streams: case study of the western Canadian prairies and high plains..
Late Pleistocene chronostratigraphy and ice sheet limits, southern Ireland. (2012)
Journal Article
Ó Cofaigh, C., Telfer, M., Bailey, R., & Evans, D. (2012). Late Pleistocene chronostratigraphy and ice sheet limits, southern Ireland. Quaternary Science Reviews, 44, 160-179. https://doi.org/10.1016/j.quascirev.2010.01.011
The glaciation of Dartmoor: the southernmost independent Pleistocene icecap in the British Isles (2012)
Journal Article
Evans, D., Harrison, S., Vieli, A., & Anderson, E. (2012). The glaciation of Dartmoor: the southernmost independent Pleistocene icecap in the British Isles. Quaternary Science Reviews, 45, 31-53. https://doi.org/10.1016/j.quascirev.2012.04.019The granite uplands of Dartmoor have traditionally been considered to be relict permafrost and periglacial landscapes that lay beyond the limits of Quaternary glaciations but a variety of landform evidence indicates that a plateau icefield existed on... Read More about The glaciation of Dartmoor: the southernmost independent Pleistocene icecap in the British Isles.