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The Owasco is a thin distinct silty unit. It has sharp distinct boundaries at its top and base. It is flaggy, locally fossiliferous and is displays cross bedding in some locations. The upper contact maybe a diastem, rather than an erosional disconformity. This unit is fairly thin only 1-2' thick in outcrops. It thickens westward.[2]
Fossils
The brachiopodAIlanella tullius is one of the fossils the Owasco is noted for.
Jaycox
The Jaycox Formation is a geologic formation in New York. It preserves fossils dating back to the Devonian period.
The basial Jaycox contains the Hills Gulch bed, a fossiliferous bed with corals and shells, as well as megaburrows at its basial contact. The Hills Gulch is a calcareous siltstone.[3]
Spafford
Wanakah
Centerfield Limestone
The Centerfield Limestone is a geologic formation in New York, and Pennsylvania. It dates back to the Devonianperiod. It is the lowest member of the Ludlowville Formation and it overlies the Skaneateles Formation.[4][5] The Peppermill Gulf bed is included within the Centerfield Lime. The unit was named by Smith (1930)
Gantz, Hundred-foot sand, Fifty-foot sand, Thirty-foot sand, Nineveh-Snee, Gordon Stray, Fourth Sand, Fifth Sand, Bayard Sand, Elizabeth Sand, Sweet Richard,
Chadakoin Formation, First Warren
Bradford Group
Upper Warren, Lower Warren, Speechely Stray, Speechely, Balltown A, Balltown B, Balltown C, Sheffield, First Bradford, Second Bradford, Third Bradford, Kane