Karst geology and hydrogeology of Cape Breton Island, Nova Scotia: an overview
Approximately 23% (2700 km 2 ) of Cape Breton Island consists of a wide variety of glaciated bedrock (meta-carbonates, carbonates, and evaporites) that has the potential for karst development. An additional 1100 km 2 of such strata have been inundated by post-glacial sea-level rise. There have been...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
2014
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Online Access: | http://dx.doi.org/10.1139/cjes-2013-0157 http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2013-0157 http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2013-0157 |