Along Seneca Lake, near Lodi, in Seneca Co., NY, the Lodi Limestone Member of the Genesee Formation consists of large discoidal limestone nodules intercalated in a bed of dark-gray fossiliferous calcareous siltstone overlying the Geneseo Shale Member. Nodules come together in places to form a lumpy bed of black argillaceous limestone about 6 in. thick. Fauna of the Lodi is distinctive and has been identified in outcrop as far west as eastern Erie Co. Unit increases in thickness to the southwest of Seneca Lake. Used locally for correlation in Allegany and Steuben Cos.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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