The Melville Moraine: sea-level change and response of the western margin of the Foxe Ice Dome, Melville Peninsula, Northwest Territories
Marine-limit elevations and radiocarbon dates from Melville Peninsula suggest rapid deglaciation of Committee Bay about 9100 years ago when sea level was 235 m higher than present. During deglaciation, an extensive prominent moraine with both terrestrial and glaciomarine segments developed along the...
Published in: | Canadian Journal of Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1990
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Online Access: | http://dx.doi.org/10.1139/e90-129 http://www.nrcresearchpress.com/doi/pdf/10.1139/e90-129 |