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  • Usage in publication:
    • Cold Spring Gneiss
  • Modifications:
    • Named
  • Dominant lithology:
    • Gneiss
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Crowley, W.P., 1976, The geology of the crystalline rocks near Baltimore and its bearing on the evolution of the eastern Maryland Piedmont: Maryland Geological Survey Report of Investigations, no. 27, 40 p.


Summary:

Named for Cold Spring Park, Baltimore City, Baltimore Co., east-central MD. Consists of biotite-muscovite-quartz-feldspar gneiss or schistose gneiss. Intrudes Hollofield Layered Ultramafite and Mount Washington Amphibolite (Baltimore Mafic Complex), and Druid Hill Amphibolite Member of James Run Formation. Age is Ordovician(?) or Silurian(?).

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 ([ ]).

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