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La découverte d'un gîte de silex dans la zone intertidale, à Montmagny, étend l’aire géographique des sites connus au Québec et témoigne d'activités maritimes commerciales entre cette localité et l'Europe aux siècles derniers. Les silex trouvés comprennent des éléments mixtes, les uns émoussés (galets), prélevés sur des plages, d'autres non usés et fragmentés (concrétions de chert de forme irrégulière ou quelconque), empruntés à des altérites ou ramassés dans des débris de carrière. Leur ressemblance avec les silex de la région de Québec permet de penser qu'ils ont la même origine, soit les formations crayeuses du Crétacé supérieur, de la Manche (Angleterre ou France). Jadis on s'en servait comme lest de bateau.The discovery of a deposit of flints in the intertidal zone, at Montmagny, extends their geographic distribution in Québec, and provides evidence of maritime commercial activities between this locality and Europe during the last centuries. Two types of flints were found. The first are well rounded flints (pebbles) picked up on beaches; the second type includes natural and broken siliceous concretions of irregular shape, collected in quarries or in weathered deposits. Because the flints found at Montmagny are similar to those occurring in the Québec City area, it is likely that they originated from the same source, that is the chalk formations bordering the English Channel (England and France) which belong to upper Cretaceous. In the past, flints were used as ballast in sailing ships

Un gîte de silex européens à Montmagny, côte sud du Saint-Laurent, Québec