Named Bisher member of West Union formation. Composed predominantly of limestone. Underlain by Crab Orchard clay shale; overlain by Lilley member of West Union formation. Recognized in vicinity of Hillsboro, Highland Co., OH.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Raised in rank to Bisher formation. Originally defined as Bisher member of West Union formation. Herein redefined to include all strata of West Union formation, which is apparently abandoned. Underlain by Alger clay shale; overlain by Lilley dolomite. Occurs over wide area in Highland and Adams Cos., OH. Known to occur in Lewis Co., KY.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Designated Bisher Limestone. Described as light-gray limestone, ranging from finely crystalline to coarse-textured and sandy, dolomitic; highly fossiliferous. Thickness ranges from 20 to 80 ft. Underlain by Crab Orchard Formation; unconformably overlain by Devonian Ohio Shale.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Designated Bisher Dolomite. Described as light-bluish-gray dolomite, medium- to coarse-grained, porous, vuggy, petroliferous; evenly laminated or obscurely or irregularly bedded, locally cross-bedded. Breccia common in lowermost few inches to 1 foot. Fossiliferous. Thickness ranges from 0 to 5 ft. Underlain by Crab Orchard Formation; unconformably overlain by Devonian black shale.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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