Thickness and extent of the subglacial till layer beneath an Antarctic paleo-ice stream.

Dowdeswell, J.A.; Ó Cofaigh, C.; Pudsey, C.J.

doi:10.1130/g19864.1

All Outputs (5)

Continental slope morphology and sedimentary processes at the mouth of an Antarctic palaeo-ice stream. (2004)
Journal Article
Dowdeswell, J., Ó Cofaigh, C., & Pudsey, C. (2004). Continental slope morphology and sedimentary processes at the mouth of an Antarctic palaeo-ice stream. Marine Geology, 204, 203-214. https://doi.org/10.1016/s0025-3227%2803%2900338-4

Late Quaternary submarine bedforms and ice-sheet flow in Gerlache Strait and on the adjacent continental shelf, Antarctic Peninsula. (2004)
Journal Article
Evans, J., Dowdeswell, J., & Ó Cofaigh, C. (2004). Late Quaternary submarine bedforms and ice-sheet flow in Gerlache Strait and on the adjacent continental shelf, Antarctic Peninsula. Journal of Quaternary Science, 19(4), 397-407. https://doi.org/10.1002/jqs.831

Tunnel Valleys. (2004)
Book Chapter
Ó Cofaigh, C. (2004). Tunnel Valleys. In A. Goudie (Ed.), Encyclopedia of Geomorphology (1074-1075). Routledge

Timing and significance of glacially influenced mass-wasting in the submarine channels of the Greenland Basin (2004)
Journal Article
Ó Cofaigh, C., Dowdeswell, J., Evans, J., Kenyon, N., Taylor, J., Mienert, J., & Wilken, M. (2004). Timing and significance of glacially influenced mass-wasting in the submarine channels of the Greenland Basin. Marine Geology, 207(1-4), 39-54. https://doi.org/10.1016/j.margeo.2004.02.009

The most extensive systems of submarine channels on the continental margins of the Norwegian–Greenland Sea occur in the Greenland Basin (72–75°N). Geophysical records show that these channels are up to 100-m deep, 4-km wide, and extend for about 300... Read More about Timing and significance of glacially influenced mass-wasting in the submarine channels of the Greenland Basin.

Thickness and extent of the subglacial till layer beneath an Antarctic paleo-ice stream. (2004)
Journal Article
Dowdeswell, J., Ó Cofaigh, C., & Pudsey, C. (2004). Thickness and extent of the subglacial till layer beneath an Antarctic paleo-ice stream. Geology, 32(1), 13-16. https://doi.org/10.1130/g19864.1