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- W1528717265 abstract "This chapter discusses the results of work carried out in East-Central Ireland between 1993 and 1999. The area studied is situated on the northeastern margin of the Irish central lowlands and covers 4000 km 2 , including Northwestern County Dublin and all of County Meath, as well as the southern extreme of County Cavan and parts of Counties Louth and Westmeath. The study focused on the sedimentology of key features across the study area, generally in gravel pits. The sediment-landform assemblages provided a striking record of glaciation and deglaciation. The glacial sediments are dominated by drumlinised lodgement tills and the deglacial sediments are composed of glaciofluvial sandar, subaerial, and subaquatic fans, deltas, eskers, and moraines comprised of melt-out and flow tills. These seem to reflect a continuous retreat of ice across the area at between 19,000 and 16,000 years BP with associated ponding and development of broad glaciofluvial systems." @default.
- W1528717265 created "2016-06-24" @default.
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- W1528717265 date "2004-01-01" @default.
- W1528717265 modified "2023-09-25" @default.
- W1528717265 title "Evidence for several ice marginal positions in east central Ireland, and their relationship to the Drumlin Readvance Theory" @default.
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- W1528717265 doi "https://doi.org/10.1016/s1571-0866(04)80069-1" @default.
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