Named the Ironwood formation for Ironwood, Gogebic Co., MI. Consists of cherty iron-bearing carbonates, ferruginous slates and cherts, jaspilites, ore bodies, and actinolite-magnetite schists. Unit is 850 feet thick. It overlies the Palms formation and underlies the Tyler slate. The Ironwood is of Precambrian age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Divided the Ironwood formation into five members (ascending): Plymouth ferruginous chert, Yale, Norrie ferruginous chert, Pence ferruginous slate, and Anvil ferruginous chert.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Changed name to Ironwood iron-formation. Age is pre-Cambrian (middle Huronian).
Source: Modified from US geologic names lexicon (USGS Bull. 896, p. 1026).
Pg. 2845 (fig. 2, stratigraphic chart compiled from Leith and others, 1935; James, 1958; Gair and Thaden, 1968). Ironwood Iron-Formation of Menominee Group of Marquette Range Supergroup (new; replaces †Animikie series of James, 1958, south of Lake Superior, in Michigan and Wisconsin). Present in Gogebic Range, northwestern Michigan. Overlies Palms Quartzite of Menominee Group. Upper boundary is marked by an unconformity. Age is middle Precambrian.
Source: Publication.
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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