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National Geologic Map Database
Map showing publication footprint
  • Usage in publication:
    • Port Refugio Formation*
  • Modifications:
    • Named
    • Biostratigraphic dating
  • Dominant lithology:
    • Graywacke
    • Conglomerate
    • Siltstone
    • Shale
    • Basalt
  • AAPG geologic province:
    • Alaska Southeastern region
Publication:

Eberlein, G.D., and Churkin, Michael, Jr., 1970, Paleozoic stratigraphy in the northwest coastal area of Prince of Wales Island, southeastern Alaska: U.S. Geological Survey Bulletin, 1284, 67 p., (incl. geologic map, scale 1:125,000)


Summary:

Named for exposures at type locality at Port Refugio on northeast side of Suemez Island and includes west shore of Ulloa Channel from Port Refugio to Adrian Cove, AK. Composed of interbedded graywacke, siltstone, shale, conglomerate, pillow basalt, breccia, and aquagene tuff. Thickness is uncertain due to tight folding, but is estimated at several thousand ft as suggested by lateral extent along Ulloa Channel. Conformably overlies or is intercalated with Wadleigh Limestone (new). Underlies Peratrovich Formation in Shelikof Islands area. Assigned Late Devonian age based on stratigraphic relations and biostratigraphic dating of brachiopods associated with branching vascular plants and SPIRIFER DISJUNCTUS.

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


Map showing publication footprint
  • Usage in publication:
    • Port Refugio Formation*
  • Modifications:
    • Biostratigraphic dating
  • AAPG geologic province:
    • Alaska Southeastern region
Publication:

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 ([ ]).