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Showing 1 to 7 of 7 for “"Glacial geomorphology"”.
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Glacial Geomorphology of southern Alberta, Canada
During deglaciation from the Last Glacial Maximum three terrestrial ice streams within the south western sector of the Laurentide Ice Sheet competed and coalesced in southern Alberta; the High Plains Ice Stream (HPIS), Central Alberta Ice Stream (CAIS) and the east lobe. The ice streams are …
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Glacial Geomorphology of the Eastern Antarctic Peninsula Shelf
During the last glacial maximum, grounded ice from the expanded Antarctic Peninsula Ice Sheet extended across the continental shelf. Grounded and flowing ice carved a distinctive array of glacial geomorphic features into the seafloor, which were gradually exposed as the ice pulled back. The recent …
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Late Quaternary Glacial Geomorphology of the Kearny Creek-South Piney Creek Area, Bighorn Mountains, Wyoming
Made available in DSpace on 2014-12-14T04:57:32Z (GMT). No. of bitstreams: 1 8004130.pdf: 9595700 bytes, checksum: 5ceae210fb5da288403445117b748a7f (MD5) Previous issue date: 1979
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The glacial geomorphology of part of the Western Grampians of Scotland, with especial reference to the limits of the Loch Lomond Advance
… 10,000 and 1 : 25,000. The main forms of mapped glacial evidence comprised moraines, thick till, fluvioglacial landforms, erratics, boulder spreads, ice-moulded bedforms, striae and friction cracks. Outside the glacial limits the main types of mapped periglacial evidence included frost-riven …
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Ice dynamics and glacial history from remote sensing of the Seno Skyring-Seno Otway-Strait of Magellan region, southernmost Patagonia
The glacial geomorphology of southernmost Patagonia records the advance and retreat of the Patagonian ice sheet over a number of glacial cycles. The well-preserved landform assemblages and sediments that have been left behind comprise one of the longest and most complete records of Quaternary …
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Sedimentology and Geomorphology of Glacial Landforms in Southern Sweden
… ice sheet. In particular, processes connected to glacial meltwater drainage are essential to understand ice-sheets behavior in a warming climate. Investigating sediments and geomorphology of drainage systems below ice sheets is complicated; however, formerly glaciated regions are easily …
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Post-glacial rivers: Rates of development, utilization of inherited glacial features, and resulting morphology
Submission original under an indefinite embargo labeled 'Open Access'. The submission was exported from vireo on 2023-09-01 without embargo terms