A low-relief hill in eastern Ontario, Canada, covered by the easily erodible Queenston Formation and derived sediments — probably the result of Quaternary tectonic uplift

J.L. Wallach, Brian Mahoney
  • Canadian Journal of Earth Sciences, September 2014, Canadian Science Publishing
  • DOI: 10.1139/cjes-2014-0081

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http://dx.doi.org/10.1139/cjes-2014-0081