Professor Colm O'Cofaigh's Outputs (6)

Sedimentary evidence for deforming bed conditions associated with a grounded Irish Sea glacier, southern Ireland. (2001)
Journal Article
Ó Cofaigh, C., & Evans, D. (2001). Sedimentary evidence for deforming bed conditions associated with a grounded Irish Sea glacier, southern Ireland. Journal of Quaternary Science, 16(5), 435-454. https://doi.org/10.1002/jqs.631

Late Quaternary iceberg rafting along the Antarctic Peninsula continental rise and in the Weddell and Scotia seas. (2001)
Journal Article
Ó Cofaigh, C., Dowdeswell, J., & Pudsey, C. (2001). Late Quaternary iceberg rafting along the Antarctic Peninsula continental rise and in the Weddell and Scotia seas. Quaternary Research, 56, 308-321. https://doi.org/10.1006/qres.2001.2267

Workshop explores debris transported by icebergs and paleoenvironmental implications. (2001)
Journal Article
Dowdeswell, J., Ó Cofaigh, C., Andrews, J., & Scourse, J. (2001). Workshop explores debris transported by icebergs and paleoenvironmental implications

Laminated sediments in glacimarine environments: diagnostic criteria for their interpretation. (2001)
Journal Article
Ó Cofaigh, C., & Dowdeswell, J. (2001). Laminated sediments in glacimarine environments: diagnostic criteria for their interpretation. Quaternary Science Reviews, 20, 1411-1436. https://doi.org/10.1016/s0277-3791%2800%2900177-3

Holocene glacimarine sedimentation, inner Scoresby Sund, East Greenland: the influence of fast-flowing ice-sheet outlet glaciers. (2001)
Journal Article
Ó Cofaigh, C., Dowdeswell, J., & Grobe, H. (2001). Holocene glacimarine sedimentation, inner Scoresby Sund, East Greenland: the influence of fast-flowing ice-sheet outlet glaciers. Marine Geology, 175, 103-129. https://doi.org/10.1016/s0025-3227%2801%2900117-7

Deforming bed conditions associated with a major ice stream of the last British ice sheet (2001)
Journal Article
Ó Cofaigh, C., & Evans, D. (2001). Deforming bed conditions associated with a major ice stream of the last British ice sheet. Geology, 29(9), 795-798. https://doi.org/10.1130/0091-7613%282001%29029%3C0795%3Adbcawa%3E2.0.co%3B2

The Irish Sea ice stream was the largest ice stream to drain the last British ice sheet, and around the margins of the Celtic Sea it deposited a shelly diamict facies that has been variously interpreted as subglacial till or distal glacial marine mud... Read More about Deforming bed conditions associated with a major ice stream of the last British ice sheet.