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Carbonates and Evaporites

, Volume 17, Issue 2, pp 114–115 | Cite as

Karst geomorphology and hydrogeology of the bear rock formation — a remarkable dolostone and gypsum megabreccia in the continuous permafrost zone of northwest Territories, Canada

  • Jim Hamilton
  • Derek Ford
Article

Keywords

Devonian Breccia Subsidence Trough Continuous Permafrost Collapse Sinkhole 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

References

  1. 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
  2. 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

Copyright information

© Springer 2002

Authors and Affiliations

  • Jim Hamilton
    • 1
  • Derek Ford
    • 1
  1. 1.School of Geography and GeologyMcMaster UniversityHamiltonCanada

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