Name Spring Brook shale member of Ludlowville formation credited to G.A. Cooper (unpub. thesis). Unit described as shale and impure limestone. Thickness about 20 ft. Overlies Ledyard shale member and underlies Eighteenmile Creek member. Cooper (1930) includes strata of both Spring Brook and Eighteenmile Creek in Wanakah shale member. Age is Middle Devonian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Spring Brook and Eighteenmile Creek Members of Ludlowville Formation reduced in rank in this report to submembers of Wanakah Member of Ludlowville Formation in keeping with nomenclature presented here for Ledyard Member of Ludlowville. Spring Brook overlies Mt. Vernon bed of Pond Spring interval of Elma Submember of Ledyard Member.
["Submember" not recognized as a formal stratigraphic rank term (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005). Considered informal until formally published. The rank or lithologic term should not be capitalized.]
Source: GNU records (USGS DDS-6; Reston GNULEX).
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