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Emplacement of the St. Narcisse Moraine as a Climatic Event in Eastern Canada

Published online by Cambridge University Press:  20 January 2017

Pierre Lasalle
Affiliation:
Quebec Department of Natural Resources, 1620 Boulevard de l'Entente, Quebec City, Province of Quebec, Canada
J.A. Elson
Affiliation:
Department of Geological Sciences, McGill University, Montreal, Province of Quebec, Canada

Abstract

The length (more than 300 km) and size of the St. Narcisse morainic system suggest that it represents an important glacial event, probably climatically controlled and not related to a surge. Dates on marine material (shells) both from within and external to the moraine suggest that its time of emplacement was roughly 11,000 years ago, well after the beginning of the Champlain Sea Episode, but still possibly correlative with the Valders event of the Lake Michigan area.

Type
Research Article
Copyright
University of Washington

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References

Broecker, W.S., Farrand, W.R., (1963). Radiocarbon age of the Two Creeks forest bed, Wisconsin. Geological Society of America Bulletin 74, 795802.Google Scholar
Denis, R., (1973). Aspects du Quaternaire dans la région au nord de Joliette, P.Q. Le Quaternaire du Québec, 2nd Symposium, ACFAS .Google Scholar
Denis, R., (1974). Late Quaternary Geology and Geomorphology in the Lake Maskinongé Area, Quebec. Univ. Uppsala Dept. Physical GeographyUNGI Rept. 28.Google Scholar
Denis, R., Prichonnet, G., (1973). Aspects du Quaternaire dans la région au nord de Joliette. Le Quaternaire du Québec, 2nd Symposium October 1973 Field Excursion Guidework University of Quebec Montreal.Google Scholar
Elson, J.A., (1962). Pleistocene geology of the St. Lawrence lowlands. Clark, T.H., Guidework, New England Intercollegiate Geological Conference McGill University Montreal.Google Scholar
Gadd, N.R., MacDonald, B.C., Shilts, W.W., (1972a). Deglaciation of Southern Quebec. Geol. Survey CanadaPaper 71-47.CrossRefGoogle Scholar
Gadd, N.R., (1972b). Quaternary Geology and Geomorphology of Southern Quebec; Guidework for Field Excursion A44-C44. 24th International Geological Congress, Montreal, 1972 .Google Scholar
Karrow, P.F., (1957). Pleistocene Geology of the Grondines Map-Area, Quebec. Unpublished Ph.D. thesis University of Illinois.Google Scholar
LaSalle, P., (1966). Late Quaternary vegetation and glacial history in the St. Lawrence lowlands, Canada. Leidse Geologische Mededelingen 38, 91128.Google Scholar
LaSalle, P., Hardy, L., Poulin, P., (1972). An Ice Frontal Position in the Northwest Part of the Parc des Laurentides, and Northeast of Quebec City. Quebec Dept. Nat. ResRep. S-135.Google Scholar
Laverdière, C., Courtemanche, A., (1961). La géomorphologie glaciaire de la région du Mont-Tremblant: Part 2, La région de St-Faustin-St-Jovite. Cahiers de Geographie de Québec 9, 32.Google Scholar
Lowdon, J.A., Blake, W. Jr., (1973). Radiocarbon Dates XIII. Geol. Survey CanadaPaper 73-7.Google Scholar
McDonald, B.C., (1968). Deglaciation and differential postglacial rebound in the Appalachian region of southeastern Quebec. Journal of Geology 76, 664667.Google Scholar
Osborne, F.F., (1951). Parc des Laurentides ice cap and the Quebec Sea. Le naturaliste Canadien 68, 221251.Google Scholar
Parry, J.T., McPherson, J.C., (1964). The St.-Faustin-St.-Narcisse Moraine and the Champlain Sea. Rev. Geog. of Montreal 18, 235248.Google Scholar
Richard, S.H., (1974). Superficial Geology Mapping; Ottawa-Hull Area (Parts of 31 F, G). Geol. Survey Canada 218219Paper 74-1 Part B.Google Scholar
Terasmae, Jaan, (1959). Notes on The Champlain Sea episode in the St. Lawrence Lowlands, Quebec. Science 130, 334336.Google Scholar
Wright, H.E. Jr., (1971). Retreat of the Laurentide Ice sheet from 14,000 to 9,000 years ago. Quaternary Research 1, 316330.Google Scholar