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- W2315747954 abstract "Abstract The limestone pavements of the subarctic Nahanni are glaciokarstic forms of pre-Wisconsin age. Despite a harsh climate, annual denudation 11.3 mm!1000 yrs. on bare limestone, and 22.8 mm!1000 yrs. in soil covered areas) is comparable with that in alpine and cold temperate areas. As the pavements evolve they pass through pit-and-tunnel, grike, grike depression, and residual clint stages. The same stages have been identified in other glaciated and non-glaciated pavement and karren karst areas, and in labyrinth karst regions where the equivalent landforms are dolines, karst streets, karst platea, and residual towers. Limestone pavement topography is therefore considered to be micro-scale labyrinth karst." @default.
- W2315747954 created "2016-06-24" @default.
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- W2315747954 date "1981-04-01" @default.
- W2315747954 modified "2023-09-26" @default.
- W2315747954 title "The Limestone Pavements of Nahanni" @default.
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- W2315747954 doi "https://doi.org/10.1080/03736245.1981.10559640" @default.
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