White Tail Ridge Formation

White Tail Ridge Formation
Stratigraphic range: Early Eocene
TypeFormation
Unit ofUmpqua Group
Sub-unitsBerry Creek Member
Remote Member
Coquille River Member
Rasler Creek tongue
UnderliesTyee Formation
OverliesTenmile Formation
AreaSouthwestern Oregon
ThicknessUp to several thousand feet
Lithology
PrimarySandstone, conglomerate, Siltstone
OtherMudstone, Coal
Location
Coordinates43°13′48″N 123°06′00″W / 43.2299°N 123.1000°W / 43.2299; -123.1000
RegionDouglas County, Oregon
CountryUnited States
ExtentSouthern Oregon Coast Range and Umpqua Basin
Type section
Named forWhite Tail Ridge, Douglas County
Named byIn-Soo Ryu and Alan R. Niem
Year defined1992

The White Tail Ridge Formation is a geologic formation in Oregon. It preserves fossils dating back to the Paleogene period. The formation records fluvial, deltaic, and shallow-marine deposits along the margin of an Eocene basin of southwestern Oregon. Conglomeratic intervals contain clasts derived from volcanic, plutonic, metamorphic, and sedimentary source terranes associated with tectonic uplift in the Klamath Mountains and adjacent regions.[1]

The formation preserves marine invertebrate fossils, plant material, and carbonaceous deposits indicative of warm, humid Paleogene environments. It is regionally overlain by the Tyee Formation and overlies older lower Eocene strata including the Tenmile Formation.[2]

See also

References

  1. ↑ Ryu, In-Soo; Niem, Alan R. (1992). Geology, geochemistry, and petroleum potential of the Tertiary Cenozoic rocks in the southern Tyee Basin, southwestern Oregon (PDF) (Report). Open-File Report. Portland, Oregon: Oregon Department of Geology and Mineral Industries. Archived from the original (PDF) on 2024-07-07.
  2. ↑ Wells, Ray E.; Bukry, David; Friedman, Richard; Pyle, Donald (2000). Geologic map and database of the Roseburg 30' × 60' quadrangle, Douglas and Coos Counties, Oregon (PDF) (Report). Open-File Report. United States Geological Survey. Archived from the original (PDF) on 2017-01-09.