Extended from ON, CN into MN part of Rainy Lake area within western extension of Wabigoon subprovince of Superior Province (Lake Superior region). As area is highly deformed, stratigraphic relations cannot be extended for more than a few km along strike. Consists of feldspathic quartz arenite and interbedded polymict conglomerate which have undergone regional metamorphism. Intrusive granites are older and younger than Seine. Is youngest of supracrustal rocks which include in ascending order, Keewatin and Coutchiching Groups. Is part of Late Archean (2.7 Ga) granite-greenstone belt in Rainy Lake area.
Source: GNU records (USGS DDS-6; Denver GNULEX).
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