Abstract
Relief features of interest to the geomorphologist are numerous in the Québec City district. Among the more striking are the fault-line scarps at Montmorency Falls and on the island of Orléans and the various Champlain sea terraces among which Goldthwait's « 110-foot » and « Micmac » terraces are particularly well developed. A possible pre-Pleistocene section of the Montmorency river channel bas been suggested but still remains to be definitely established.
Cite
CITATION STYLE
Sabourin, R.-J.-E. (2005). Notes sur la géomorphologie d’une partie de la Côte de Beaupré. Cahiers de Géographie Du Québec, 7(13), 27–36. https://doi.org/10.7202/020417ar
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