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Map showing publication footprint
  • Usage in publication:
    • White Tail Ridge Member
  • Modifications:
    • Named
  • Dominant lithology:
    • Sandstone
    • Siltstone
    • Coal
  • AAPG geologic province:
    • Oregon-Washington Coast Ranges province
    • Klamath Mountains province
Publication:

Baldwin, E.M., 1974, Eocene stratigraphy of southwestern Oregon: Oregon Department of Geology and Mineral Industries Bulletin, no. 83, 40 p., (incl. geologic map, scale 1:250,000)


Summary:

Named for White Tail Ridge as lower of two members of Flournoy Formation (new). Makes up White Tail Ridge and Sugar Pine Ridge in Camas Valley quad, Douglas Co, OR. Composed of sandstone, siltstone, and conglomerate. All sandstone formerly mapped as Tyee along Coos and Millacoma Rivers is now assigned to White Tail Ridge member. Coal reported by Theasher (1942) from Melrose and Camas Mountain areas. Is 1500 ft thick along Lookingglass Creek. Is 4000 to 5000 ft along Coos River. Unconformably overlies Lookingglass Formation (new). Underlies Camas Valley Member (new) (Flournoy Formation) or unconformably underlies Tyee Formation. Age is middle Eocene based on stratigraphic position of Flournoy Formation.

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


Map showing publication footprint
  • Usage in publication:
    • White Tail Ridge Member
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Oregon-Washington Coast Ranges province
    • Klamath Mountains province

Map showing publication footprint
  • Usage in publication:
    • White Tail Ridge Member
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Oregon-Washington Coast Ranges province
    • Klamath Mountains province
Publication:

Molenaar, C.M., 1985, Depositional relations of Umpqua and Tyee Formations (Eocene) southwestern Oregon: American Association of Petroleum Geologists Bulletin, v. 69, no. 8, p. 1217-1229. [Available online, with subscription, from AAPG archives: http://www.aapg.org/datasystems or http://search.datapages.com]


Summary:

Olalla Creek Member of Lookingglass Formation and White Tail Ridge Member of Flournoy Formation of Baldwin (1974) are included as second from uppermost member, White Tail Ridge Member, of Umpqua Formation. Baldwin's (1974) Olalla Creek Member is interpreted as more landward facies of White Tail Ridge Member. Overlies Tenmile Member; underlies Camas Valley Member (both of Umpqua Formation). Age is middle Eocene. [members of Umpqua Formation are not adopted in this paper]

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


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