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Map showing publication footprint
  • Usage in publication:
    • Rancocas formation
  • Modifications:
    • Named
  • Dominant lithology:
    • Greensand
    • Sand
  • AAPG geologic province:
    • Atlantic Coast basin
Publication:

Clark, W.B., 1894, Cretaceous and Tertiary geology: New Jersey Geological Survey Report of Progress, 1893, p. 329-355., See also "Origin and classification of the greensands of New Jersey," Jour. Geol., v. 2, p. 161-177, 1894


Summary:

Rancocas formation named for exposures along Rancocas Creek in Burlington Co., NJ. Composed largely of greensand, although much more highly glauconitic in lower than in upper half. Lower half largely a pure greensand, but in some parts of State it becomes very argillaceous toward base, forming the so-called "chocolate marl." Is Middle Marl bed of previous reports. Thickness 45 ft. Underlies Manasquan formation and overlies Redbank formation.

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


Map showing publication footprint
  • Usage in publication:
    • Rancocas Group*
  • Modifications:
    • Revised
    • Age modified
  • AAPG geologic province:
    • Atlantic Coast basin
Publication:

Owens, J.P., and Minard, J.P., 1962, Pre-Quaternary geology of the Columbus quadrangle, New Jersey: U.S. Geological Survey Geologic Quadrangle Map, GQ-160, 1 sheet, scale 1:24,000 [http://ngmdb.usgs.gov/Prodesc/proddesc_610.htm]


Summary:

Rancocas Group in NJ expanded to include the Eocene Manasquan Formation. Group now subdivided into (ascending) Hornerstown, Vincentown, and Manasquan Formations. Age of Rancocas, therefore, is modified to Paleocene and Eocene. Underlies Miocene(?) Kirkwood Formation and overlies Upper Cretaceous Red Bank Formation of Monmouth Group.

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


Map showing publication footprint
  • Usage in publication:
    • Rancocas Group
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Atlantic Coast basin
Publication:

Gallagher, W.B., 1993, The Cretaceous/Tertiary mass extinction event in the northern Atlantic Coastal Plain: The Mosasaur, Journal of the Delaware Valley Paleontological Society, v. 5, p. 75-129.


Summary:

Report offers excellent overview of the Hornerstown and Vincentown Formations, which compose the Rancocas Group as used here. Discussion includes age, lithology, thickness, fauna, and areal extent. Unit overlies the Monmouth Group and underlies the Shark River Formation. The K/T boundary occurs in the basal portion of the Hornerstown. The age of the Rancocas, therefore, is Late Cretaceous and Paleocene.

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


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For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

Asterisk (*) indicates published by U.S. Geological Survey authors.

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