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National Geologic Map Database
Geologic Unit: Alloway
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Map showing publication footprint
  • Usage in publication:
    • Alloway clay
  • Modifications:
    • Named
  • Dominant lithology:
    • Clay
  • AAPG geologic province:
    • Atlantic Coast basin
Publication:

Kummel, H.B., and Knapp, G.N., 1904, The stratigraphy of the New Jersey clays: New Jersey Geological Survey Final Report, no. 6, p. 117-209.


Summary:

Alloway clay, part of Kirkwood formation, is described as a continuous bed of clay without sand beds of sufficient extent to show in outcrop. Usually light brown, although some parts are white, yellow, and black. Thickness ranges from 0 to 80 ft. Underlies Shiloh marl and overlies a thin bed of micaceous white talc-like clayey sand near Woodstown and towards Ewan Mills. Continuous from near Swans Mill, south of Mullica Hill, Gloucester Co., to a point 2 mi south of Alloway, Salem Co. Isolated outcrops have been seen as far south as Stow Creek Township, Cumberland Co., NJ.

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


Map showing publication footprint
  • Usage in publication:
    • Alloway Clay Member
  • Modifications:
    • Revised
    • Overview
    • Areal extent
  • AAPG geologic province:
    • Atlantic Coast basin
Publication:

Isphording, W.C., and Lodding, William, 1969, Facies changes in sediments of Miocene age in New Jersey, IN Subitzky, Seymour, ed., Geology of selected areas in New Jersey and eastern Pennsylvania and guidebook of excursions: Rutgers University Press [Field Trip Guidebook], Geological Society of America, [82nd] annual meeting, Atlantic City, NJ, p. 7-13.


Summary:

Alloway Clay Member of Kirkwood consists of silty clay and is limited in outcrop to Gloucester, Salem, and Cumberland Cos., southern NJ. At its northern limit it merges with the lower portion of the Grenloch Sand Member and loses its identity. It apparently contains the Shiloh Marl beds and the here informally established "Cohansey quartzite-sandstone lithofacies" (formerly known as the "Cohansey quartzite").

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


Map showing publication footprint
  • Usage in publication:
    • Alloway Clay Member*
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Atlantic Coast basin
Publication:

Nemickas, Bronius, and Carswell, L.D., 1976, Stratigraphic and hydrologic relationship of the Piney Point aquifer and the Alloway Clay Member of the Kirkwood Formation in New Jersey: U.S. Geological Survey Journal of Research, v. 4, no. 1, p. 1-7.


Summary:

Alloway clay of Kummel and Knapp (1904) adopted as Alloway Clay Member of Kirkwood Formation as used by Isphording (1970). Unit is basal member of Kirkwood; probably underlies Shiloh Marl Member. Overlies Piney Point aquifer. Occurs Cumberland, Atlantic, Gloucester, and Camden Cos., NJ. Age is middle Miocene.

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


Map showing publication footprint
  • Usage in publication:
    • Alloway Clay Member*
  • Modifications:
    • Revised
    • Areal extent
  • AAPG geologic province:
    • Atlantic Coast basin
Publication:

Gibson, T.G., 1982, Depositional framework and paleoenvironments of Miocene strata from North Carolina to Maryland, IN Scott, T.M., and Upchurch, S.B., eds., Miocene of the southeastern United States; proceedings of a symposium: Florida Geological Survey Special Publication, Tallahassee, FL, December 4-5, 1980, no. 25, p. 1-22.


Summary:

In northeastern MD and central DE, Alloway Clay Member reassigned from Calvert Formation of Chesapeake Group to Kirkwood Formation, here geographically extended from NJ and PA into northeastern MD and central DE.

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


Map showing publication footprint
  • Usage in publication:
    • Alloway Clay Member
  • Modifications:
    • Revised
    • Areal extent
  • AAPG geologic province:
    • Atlantic Coast basin
Publication:

Gibson, T.G., 1983, Stratigraphy of Miocene through lower Pleistocene strata of the United States central Atlantic Coastal Plain, IN Ray, C.E., ed., Geology and paleontology of the Lee Creek Mine, North Carolina, I: Smithsonian Contributions to Paleobiology, no. 53, p. 35-80.


Summary:

Advance copy (1978). Alloway Clay Member of Calvert Formation. Tentatively extended into Maryland and Delaware as a member of Calvert Formation. Overlies Fairhaven Member. Interfingers with Plum Point Marl Member. (Alloway Clay Member of Calvert Formation not adopted by the USGS; see Gibson, 1982, Florida Geol. Survey Spec. Pub., no. 25.)

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


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