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Barcona , Columbia County, Oregon, USA
| Lat/Long (Decimal) | 45.86,-123.113 |
|---|---|
| Co-ordinates Derivation | based on nearby landmark |
| Given Location | Oregon, United States |
| Mindat.org Region (for given coordinates) | Columbia County, Oregon, USA |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Barcona (M3856) | Moore E. J. (1976) | Pittsburg Bluff | Middle of formation. The Pittsburg Bluff Formation conformably overlies the Keasey Formation (late Eocene and early Oligocene) and is conformably overlain by the Scappose Formation (late Oligocene and early Miocene). Parts of the formation are lithologically similar and therefore the stratigraphic position of exposures are sometimes uncertain. The estimated thickness for the entire formation is 200 ml the thickest continuous section of the formation is 100 m thick. | sandstone | 33.9 - 28.1 Ma Oligocene |
| Barcona (M3857) | Moore E. J. (1976) | Pittsburg Bluff | Middle of formation. The Pittsburg Bluff Formation conformably overlies the Keasey Formation (late Eocene and early Oligocene) and is conformably overlain by the Scappose Formation (late Oligocene and early Miocene). Parts of the formation are lithologically similar and therefore the stratigraphic position of exposures are sometimes uncertain. The estimated thickness for the entire formation is 200 ml the thickest continuous section of the formation is 100 m thick. | sandstone | 33.9 - 28.1 Ma Oligocene |
Recorded Fossils
References
| Moore E. J. (1976) Oligocene marine mollusks from the Pittsburg Bluff Formation in Oregon, United States Geological Survey Professional Paper 922, 1-66 |
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
