Late Quaternary glacial history, flow dynamics and sedimentation along the eastern margin of the Antarctic Peninsula Ice Sheet.
(2005)
Journal Article
Evans, J., Pudsey, C., Ó Cofaigh, C., Morris, P., & Domack, E. (2005). Late Quaternary glacial history, flow dynamics and sedimentation along the eastern margin of the Antarctic Peninsula Ice Sheet. Quaternary Science Reviews, 24, 741-774. https://doi.org/10.1016/j.quascirev.2004.10.007
Professor Colm O'Cofaigh's Outputs (4)
Till genesis and glacier motion inferred from sedimentological evidence associated with the surge-type glacier, Bruajokull, Iceland. (2005)
Journal Article
Nelson, A. E., Willis, I. C., & ÓCofaigh, C. (2005). Till genesis and glacier motion inferred from sedimentological evidence associated with the surge-type glacier, Bruajokull, Iceland. Annals of Glaciology, 42, 14-22. https://doi.org/10.3189/172756405781812961
Flow of the West Antarctic Ice Sheet on the continental margin of the Bellingshausen Sea at the Last Glacial Maximum (2005)
Journal Article
Ó Cofaigh, C., Larter, R., Dowdeswell, J., Hillenbrand, C., Pudsey, C., Evans, J., & Morris, P. (2005). Flow of the West Antarctic Ice Sheet on the continental margin of the Bellingshausen Sea at the Last Glacial Maximum. Journal of Geophysical Research, 110, https://doi.org/10.1029/2005jb003619Geophysical data show that during the last glaciation the West Antarctic Ice Sheet (WAIS) drained to the continental shelf edge of the Bellingshausen Sea through a cross-shelf bathymetric trough (Belgica Trough) as a grounded, fast flowing, ice strea... Read More about Flow of the West Antarctic Ice Sheet on the continental margin of the Bellingshausen Sea at the Last Glacial Maximum.
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.2004.10.006Geophysical 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.