Karst geomorphology and hydrogeology of the bear rock formation — a remarkable dolostone and gypsum megabreccia in the continuous permafrost zone of northwest Territories, Canada
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KeywordsDevonian Breccia Subsidence Trough Continuous Permafrost Collapse Sinkhole
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- HAMILTON, J.P., 1995, Karst geomorphology and hydrogeology of the northeastern Mackenzie Mountains, District of Mackenzie, N.W.T., Canada. Ph.D. thesis, McMaster University, 532 p.Google Scholar
- MEIJER DREES, N.C., 1993, The Devonian succession in the subsurface of the Great Slave and Great Bear Plains, Northwest Territories:Geological Survey of Canada Bulletin, no. 393.Google Scholar
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