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- W2181300923 abstract "Rapid coastal erosion along a peninsula forming the seaward shoreline of Tuktoyaktuk has resulted in ongoing control measures since the mid-1970's. While wave-generated erosion is significant along this section of the Beaufort Sea coastline, subsidence resulting from thawing of massive ice beneath nearshore sediments is also suggested as a major contributory cause of recession. This study presents the thermal and physical condition of subsurface sediments within the nearshore zone, where permafrost and massive ice was documented in 1974. Observations from six boreholes drilled in March 1994 indicate that alteration in subsurface thermal and ground ice regimes over the last 20 years has been significant. Thawing of ground ice likely resulted in nearshore subsidence in excess of 3 m. This subsidence may create a sediment demand, supplied by the shoreface, that results in ongoing erosion. This study illustrates the importance of linking thermal and mechanical aspects when assessing coastal instability in this environment." @default.
- W2181300923 created "2016-06-24" @default.
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- W2181300923 date "1998-01-01" @default.
- W2181300923 modified "2023-09-23" @default.
- W2181300923 title "COASTAL PERMAFROST INVESTIGATIONS ALONG A RAPIDLY ERODING SHORELINE, TUKTOYAKTUK, N.W.T" @default.
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