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National Geologic Map Database
Geologic Unit: Quincy
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Map showing publication footprint
  • Usage in publication:
    • Quincy diatomite
  • Modifications:
    • Original reference
  • Dominant lithology:
    • Diatomite
  • AAPG geologic province:
    • Eastern Columbia basin
Publication:

Mackin, J.H., 1961, A stratigraphic section in the Yakima Basalt and the Ellensburg Formation in south-central Washington: Washington Division of Mines and Geology Report of Investigations, no. 19, 45 p.


Summary:

Pg. 7-8, 25, 26, 40. Quincy diatomite in Priest Rapids Basalt Member of Yakima Basalt. In vicinity of Columbia River only one of Priest Rapids flows extended north of Frenchman Hills. Throughout western part of Quincy basin this flow rests, not directly on Roza flow (new) but on widespread sheet of diatomite, as much as 20 feet thick, here designated Quincy diatomite. Diatomite bed extends southward across axial part of Frenchman Hills anticline, terminating on its south flank. Age is Miocene.
Named for occurrence in Quincy basin, south-central WA.

Source: US geologic names lexicon (USGS Bull. 1350, p. 607).


Map showing publication footprint
  • Usage in publication:
    • Quincy Diatomite Bed*
  • Modifications:
    • Principal reference
    • Revised
    • Adopted
  • Dominant lithology:
    • Diatomite
  • AAPG geologic province:
    • Eastern Columbia basin
Publication:

Bingham, J.W., and Grolier, M.J., 1966, The Yakima Basalt and Ellensburg Formation of south-central Washington, IN Contributions to stratigraphy, 1965: U.S. Geological Survey Bulletin, 1224-G, p. G1-G15.


Summary:

Pg. G3 (fig. 1), G10. Quincy Diatomite Bed of Priest Rapids Member of Yakima Basalt of Columbia River Group. Diatomite as thick as 35 feet; contains a few lenses of silt and clay. Overlies Roza Member of Yakima Basalt. Age is late Miocene. Adopted by the USGS.
Type area: area of many quarry exposures in southwestern part of Quincy basin near head of Frenchman Springs Coulee [Frenchman Coulee], in S/2 sec. 16, SE/4 sec. 17, NE/4 sec. 20, and N/2 sec. 21, T. 18 N., R. 23 E., [Evergreen Ridge 7.5-min quadrangle, Grant Co., south-central WA].

Source: Publication; Changes in stratigraphic nomenclature, 1966 (USGS Bull. 1254-A, p. A7).


Map showing publication footprint
  • Usage in publication:
    • Quincy Diatomite Bed*†
  • Modifications:
    • Abandoned
Publication:

Swanson, D.A., Wright, T.L., Hooper, P.R., and Bentley, R.D., 1979, Revisions in stratigraphic nomenclature of the Columbia River Basalt Group, IN Contributions to stratigraphy, 1979: U.S. Geological Survey Bulletin, 1457-G, p. G1-G59.


Summary:

Name abandoned for two reasons. First, the diatomite is equivalent to the Squaw Creek Diatomite Bed. Second, its presumed stratigraphic position above the Roza Member [of the Wanapum Basalt of this report] and within the Priests Rapids Member [of the Wanapum Basalt of this report] is incorrect. Squaw Creek thickens westward, becomes sandstone, tuffaceous sandstone, and siltstone, and merges into, or becomes the middle member of the Ellensburg Formation of Miocene age. Name Quincy replaced by Squaw Creek.
[NOTE: The Department of the Interior's Secretarial Order 3404, issued on November 19, 2021, formally identifies the term “squaw” as derogatory. That Order will create a federal Derogatory Geographic Names Task Force, to find replacement names for geographic features in use by federal agencies. We’re awaiting guidance from the Task Force, and will then take the appropriate actions.]

Source: GNU records (USGS DDS-6; Denver 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 ([ ]).