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National Geologic Map Database
Geologic Unit: Wallkill
Map showing publication footprint
  • Usage in publication:
    • Wallkill blue limestone*
  • Modifications:
    • Named
  • Dominant lithology:
    • Limestone
  • AAPG geologic province:
    • Appalachian basin
Publication:

Wolff, J.E., and Brooks, A.H., 1898, The age of the Franklin white limestone of Sussex County, New Jersey, IN Walcott, C.D., Eighteenth annual report of the United States Geological Survey to the Secretary of the Interior, 1896-1897; Part II, Papers chiefly of a theoretical nature: U.S. Geological Survey Annual Report, 18, pt. 2, p. 425-457.


Summary:

Name Wallkill blue limestone introduced for a generally blue limestone, fine-grained, homogeneous, becoming arenaceous or shaly as it merges into underlying Hardistonville [Hardyston] quartzite. One belt of it occupies Wallkill Valley south of Franklin Furnace.

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


Map showing publication footprint
  • Usage in publication:
    • Wallkill limestone†
  • Modifications:
    • Abandoned
  • AAPG geologic province:
    • Appalachian basin
Publication:

Kummel, H.B., 1901, Report on Portland cement industry: New Jersey Geological Survey Report of Progress, 1900, p. 9-101.


Summary:

The term Kittatinny limestone is preferable for this unit as it is not well exposed along Wallkill River, and it is preeminently the great limestone formation of the Kittatinny Valley.

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


Map showing publication footprint
  • Usage in publication:
    • Wallkill Member
  • Modifications:
    • Reinstated
  • Dominant lithology:
    • Dolomite
  • AAPG geologic province:
    • Appalachian basin
Publication:

Markewicz, F.J., and Dalton, Richard, 1977, Stratigraphy and applied geology of the lower Paleozoic carbonates in northwestern New Jersey, IN Guidebook for the 42nd annual field conference of Pennsylvania geologists: Field Conference of Pennsylvania Geologists, no. 42, p. 10-12.


Summary:

Wallkill limestone, named for valley north of Hamburg village is here reinstated as Wallkill Member of Leithsville Formation. Described as dark gray dolomite, 400 to 500 ft thick at type section. Underlies Limeport Member of Allentown Formation; overlies Hamburg Member of Leithsville. Age is [Middle] Cambrian.

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


Map showing publication footprint
  • Usage in publication:
    • Wallkill Member
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Appalachian basin
Publication:

Dalton, Richard, 1989, Stratigraphy of the "Kittatinny Limestone", IN Grossman, I.G., ed., Paleozoic geology of the Kittatinny Valley and southwest Highlands area, New Jersey; field guide and proceedings: Geological Association of New Jersey Annual Field Conference, 6th annual meeting, October 20-21, 1989, v. 6, p. 59-94.


Summary:

Upper part of Leithsville is referred to as Wallkill Member in NJ, but it is poorly to rarely exposed. It consists of dark-gray, patchy dolomite and overlies the Hamburg Member on the east side of the Wallkill Valley, north of Hamburg. Underlies the Limeport Member of the Allentown Formation. Thickness ranges from 350 to 500 ft. It is estimated that the Leithsville in NJ varies from 500 to 800 ft thick. Author assigns an Early Cambrian age to the Leithsville, based on the discovery of the index fossil HYOLITHELLUS MICANS by Markewicz (1964, unpublished).

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


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

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

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).