The geomorphology and permafrost conditions of Garry Island, N.W.T. ...
Garry Island, approximately 11 kilometres (7 miles) long and 0.8 to 3.2 kilometres (0.5 to 3.2 miles) wide, is located at about latitude 69° 28'N and longitude 135° 42'W in the southern part of the Beaufort Sea. The stratigraphy consists mainly of unconsolidated sands, silts, clays and sto...
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| Format: | Text |
| Language: | English |
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University of British Columbia
2011
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| Online Access: | https://dx.doi.org/10.14288/1.0102152 https://doi.library.ubc.ca/10.14288/1.0102152 |
| Summary: | Garry Island, approximately 11 kilometres (7 miles) long and 0.8 to 3.2 kilometres (0.5 to 3.2 miles) wide, is located at about latitude 69° 28'N and longitude 135° 42'W in the southern part of the Beaufort Sea. The stratigraphy consists mainly of unconsolidated sands, silts, clays and stony clays which have been intensively deformed by the thrusting action of glacier-ice moving from the south. The deformed sediments are locally overlain by undisturbed sands and gravels containing marine fossils dated at >42,000 years. The absence of any evidence of glacial till on top of the sands suggests that Garry Island lay beyond the northwestern limits of the Laurentide ice sheet during the late-Wisconsin glaciation. Elevated strand-lines, which may be of great antiquity and occur at approximately 7.5 metre (25 feet) intervals to an altitude of almost 46 metres (150 feet), indicate the extent of Pleistocene fluctuations of sea level and the drowning of a pre-existing topography. The development of tundra polygons, ... |
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