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National Geologic Map Database
Map showing publication footprint
  • Usage in publication:
    • Cobleskill Limestone
  • Modifications:
    • Revised
    • Areal extent
  • AAPG geologic province:
    • Appalachian basin
Publication:

Heyman, Louis, 1977, Tully (Middle Devonian) to Queenston (Upper Ordovician) correlations in the subsurface of western Pennsylvania: Pennsylvania Geological Survey Mineral Resource Report, 4th series, no. 73.


Summary:

Cobleskill Limestone extended into Warren Co., northwestern PA where it is assigned to Bass islands Group. Underlies Bois Blanc Formation (Lower Devonian); overlies Bertie Dolomite of Bass Islands Group (Upper Silurian). Age is Late Silurian.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Cobleskill Formation
  • Modifications:
    • Revised
  • Dominant lithology:
    • Limestone
    • Dolostone
  • AAPG geologic province:
    • Appalachian basin
Publication:

Ciurca, S.J., Jr., 1990, Eurypterid biofacies of the Silurian-Devonian evaporite sequence; Niagara Peninsula, Ontario, Canada, and New York, IN Lash, G.G., ed., Western New York and Ontario; field trip guidebook: New York State Geological Association Guidebook, 62nd annual meeting, Fredonia, NY, no. 62, p. Sat/Sun D1-D30.


Summary:

Bertie Group redefined. Author includes the Akron-Cobleskill interval and the newly named Moran Corner Waterlime in his revised Bertie Group. Term Rondout Formation or Group is restricted to its type area in southeastern NY. In this report, Bertie Group in western NY is subdivided into (ascending) Fort Hill Waterlime, Oatka Formation, Fiddlers Green Formation, Scajaquada Formation, Williamsville Formation, Cobleskill Formation, and Moran Corner Waterlime. Akron-Cobleskill sequence described as poorly fossiliferous, massive mottled dolostone. No eurypterids are known from the Cobleskill of western NY and the Niagara Peninsula, CAN, but as eastward facies changes occur, eurypterid-bearing limestone and dolostone are encountered.

Source: GNU records (USGS DDS-6; Reston GNULEX).


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