Pg. 4 (table 1); App., p. A10-4 to A10-6. Haven Member of Kewaunee Formation. (Follows the informal usage of L.J. Acomb and others, 1982, GSA Bull., v. 93, p. 289-296; L.J. Acomb, 1978, Univ. Wisconsin MS thesis.) Consists of pinkish-gray, red, and reddish-brown, pebbly, sandy, and clayey silt till. Thickness from 2.4 to 15 m. Occurs in the Lake Michigan Lobe in Wisconsin. Overlies Ozaukee Member (new) and underlies Valders Member, both of the Kewaunee (new). Is equivalent to the Chilton (new) and Kirby Lake (new) Members of the Kewaunee in the Green Bay Lobe. Age is Pleistocene (late Wisconsinan).
Type section: nuclear power plant site in Lake Michigan bluff, in NW/4 NW/4 NE/4 sec. 22, T. 16 N., R. 23 E., Sheboygan North 7.5-min quadrangle, Sheboygan Co., eastern WI. Named from community of Haven [about 1 mi northwest of type section]; name credited to Larry J. Acomb and David M. Mickelson.
[Additional locality information from USGS historical topographic map collection TopoView, USGS GNIS database, accessed on June 9, 2018.]

Source: Publication; US geologic names lexicon (USGS Bull. 1565, p. 126).

Pg. 173-174; Carlson and others, 2011, Wisconsin Geol. Nat. Hist. Survey Bull. 106, p. 9-10. †Haven Member of Kewaunee Formation [abandoned]. Is considered same as Ozaukee Member of Kewaunee Formation.
[See Ozaukee, p. 4 (fig. 2), 7 (fig. 3), 8, 125-126 of Syverson and others, 2011.]

Source: Publication.