Brief Display | Full Display
A. M. McCabe, J. A. G. Cooper, and J. T. Kelley
Relative sea-level changes from NE Ireland during the last glacial termination
Journal of the Geological Society of London (2007), 164(5):1059-1063
Abstract: Index Terms/Descriptors: Latitude & Longitude:
GeoRef, Copyright 2008, American Geological Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States. Reference includes data from The Geological Society, London, London, United Kingdom
Deglacial sea-level records from NE Ireland between 21 and 11 cal. ka bp record marine transgressions and sensitive lithospheric responses to ice loading. The sawtooth sea-level curve contains four intervals characterized by: (1) strong net uplift, subaerial channelling and a global meltwater pulse (21-19 cal. ka bp); (2) ice loading, isostatic depression and high relative sea level (19-17.5 cal. ka bp); (3) ice loading, renewed isostatic depression and high relative sea level for >1000 years (17-14.5 cal. ka bp); (4) catastrophic ice wastage, rapid uplift and lowstand (14.5-13 cal. ka bp). Geophysical models do not capture these fluctuations.
Cenozoic; deglaciation; Europe; ice; Ireland; isostasy; last glacial maximum; loading; lowstands; meltwater; Quaternary; sea-level changes; transgression; uplifts; upper Quaternary; Western Europe
N51°30'00" -
N55°20'00" and
W10°30'00" -
W6°30'00" (Search for maps and images at Alexandria Digital Library)