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Deux blocs de dolomie à stromatolites trouvés sur les rivages du Saint-Laurent estuarien témoignent vraisemblablement d'un déplacement glaciaire excédant 500 km, la source la plus probable étant la région des lacs Mistassini-Albanel, au NO. Si c'est effectivement le cas, ces erratiques fournissent un indice supplémentaire à l'hypothèse d'un écoulement glaciaire du NO vers le SE, dans l'axe des lacs Mistassini-Albanel — Québec-Tadoussac, au cours du Wisconsinien.Two stromatolitic dolomite boulders found along the middle St. Lawrence Estuary shorelines have been most likely transported by glacier ice over 500 km, the nearest and most probable source being the Lake Mistassini-Albanel area to the NW. If the two boulders really originated from that area, their occurrence along the St. Lawrence Estuary shorelines provides an additional evidence for a glacial flow from the NW to the SE during the Wisconsinan

Blocs de dolomie à stromatolites sur les rives de l’estuaire du Saint-Laurent, Québec