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

Author： Wallach J.L.   Mahoney Brian  

Publisher： NRC Research Press

ISSN： 1480-3313

Source： Canadian Journal of Earth Sciences, Vol.51, Iss.9, 2014-01, pp. : 862-876

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