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Geologic Unit: Astoria
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  • Usage in publication:
    • Astoria sandstones
  • Modifications:
    • Original reference
  • AAPG geologic province:
    • Oregon-Washington Coast Ranges province
Publication:

Dall, W.H., and Harris, G.D., 1892, Correlation papers; Neocene: U.S. Geological Survey Bulletin, 84, 349 p.


Summary:

Pg. 223-227. Astoria sandstones. Series of sandstones on both sides of river above Astoria, though beds developed on north or right bank. The sandstone are granular, brittle, or friable, sometimes very compact and hard, usually brownish. Included in Astoria group. Dana regards the sandstones more recent than the shales, and this is strengthened by fact that fissures in the shales are filled with sand resembling that of which the sandstones are composed. Present in northwestern Oregon and southwestern Washington. Age is Miocene. [See also under †Astoria group.]
Named from Astoria, Clatsop Co., northwestern OR.

Source: US geologic names lexicons (USGS Bull. 896, p. 85; USGS Bull. 1200, p. 157-158).


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 ([ ]).