Part of greenstone-granite terrane of northern MN in the Lake Superior region. Consists of (decreasing abundance): 1) graywacke member--mostly graywacke with felsic-intermediate pyroclastic rocks; 2) felsic volcaniclastic member--partly reworked dacitic tuff and agglomerate; 3) mixed volcaniclastic member--felsic-intermediate tuff breccia; and 4) basaltic lavas. Exceeds 3000 m in thickness. Overlies Ely Greenstone and underlies Newton Lake Formation in western part of Vermilion district. Generalized geologic map, geologic evolution chart. Is Precambrian W in age.
Source: GNU records (USGS DDS-6; Denver GNULEX).
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