Lierle Clay Member of Banner Formation named in Adams Co., west-central IL, for Lierle Creek. Unit is composed of massive gray clay with silt and sand. Thickness 3 m. Underlies Loveland or Petersburg Silt, Glasford Formation, or younger deposits.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Banner Formation in the study area includes two members: the informal Casey till member and the overlying Lierle Clay Member. The Lierle is composed of soft, leached clay and silty clay diamicton that commonly becomes finer upward. Mineralogy is dominated by smectite. Interpreted to have been deposited as pedogenically altered colluvium, alluvium, or lacustrine sediment. Locally contains the Yarmouth Soil. Reaches 8.5 ft in thickness east of the Martinsville alternative site, but is less than two ft thick in borings at the site. Overlies bedrock or the Casey till member in the study area and underlies the Smithboro Till Member of the Glasford Formation. Relationship with Martinsville sand is unknown. Age is Pleistocene (Yarmouthian).
Source: GNU records (USGS DDS-6; Reston GNULEX).
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