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National Geologic Map Database
Geologic Unit: Hellam
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Map showing publication footprint
  • Usage in publication:
    • Hellam conglomerate member*
  • Modifications:
    • Named
  • Dominant lithology:
    • Conglomerate
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Stose, G.W., and Jonas, A.I., 1922, The lower Paleozoic section in southeastern Pennsylvania: Washington Academy of Sciences Journal, v. 12, no. 5, p. 358-366.


Summary:

Hellam conglomerate member of the Chickies quartzite named and accepted for USGS usage in PA. Is basal member of Chickies quartzite [and is also basal member of the "Hellam" quartzite, a name used by Frazer (1886) for the Chickies. Lesley (1892) says that Chiques sandstone is not only the oldest name for this formation but is the locality of its finest exposure.] Rests unconformably on Precambrian schist or greenstone and aporhyolite. Age is Early Cambrian.

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


Map showing publication footprint
  • Usage in publication:
    • Hellam Member*
  • Modifications:
    • Revised
    • Age modified
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Higgins, M.W., 1972, Age, origin, regional relations, and nomenclature of the Glenarm series, central Appalachian Piedmont; a reinterpretation: Geological Society of America Bulletin, v. 83, no. 4, p. 989-1026.


Summary:

Redefined Hellam Member of Chickies Formation. Age changed to latest Precambrian.

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


Map showing publication footprint
  • Usage in publication:
    • Hellam Member*
  • Modifications:
    • Age modified
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Lyttle, P.T., and Epstein, J.B., 1987, Bedrock geologic map of the Newark 2 degrees quadrangle, New York, New Jersey, and Pennsylvania: U.S. Geological Survey Miscellaneous Investigations Series Map, I-1715, 2 sheets, scale 1:250,000 [http://ngmdb.usgs.gov/Prodesc/proddesc_9892.htm]


Summary:

Hellam Member of the Chickies Quartzite is in lower part of the Chickies. Consists of coarse-grained, gray, tourmaline-bearing quartzite, arkose-pebble conglomerate, and interbeds of black slate and biotite schist. Rests unconformably and abruptly on a wide variety of Proterozoic gneisses. Age is Early Cambrian.

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.

"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 ([ ]).