The Whitesburg Formation is a dark limestone with interbedded shales geologic formation in Tennessee and Virginia.[1] It preserves fossils dating back to the Ordovician period.
Whitesburg Formation | |
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Stratigraphic range: Ordovician | |
Type | Formation |
Sub-units | Fetzer member |
Lithology | |
Primary | limestone |
Other | shale |
Location | |
Region | ![]() ![]() |
Country | ![]() |
Type section | |
Named for | Whitesburg, Tennessee |
Named by | E.O. Ulrich [1] |
History
editThe Whitesburg Formation was formally proposed in 1930, though E.O. Ulrich had used the name prior to the formal proposal.[1] The Whitesburg formation was later downgraded to the Whitesburg limestone, and was considered a basal member of the Blockhouse Shale.[2] The Whitesburg Formation was then elevated back to formation status with the Fetzer member assigned as the basal member.[3] The Fetzer is not considered to be a continuous body of rock, and exists in the Whitesburg formation as lenses.
See also
editReferences
edit- ^ a b c Ulrich, E. O. (1930). "Ordovician trilobites of the family Telephidae and concerned stratigraphic correlations". U.S National Museum Proceedings. 76: 2. Retrieved 29 June 2018.
- ^ Nueman, Robert B. (1955). "Middle Ordovician rocks of the type Tellico-Sevier belt, eastern Tennessee" (PDF). U.S. Geological Survey Shorter contributions to general geology. 274-F: 149–150. Retrieved 29 June 2018.
- ^ Walker, Kenneth R.; Steinhauff, D. M.; Roberson, K. E. (1992). "Uppermost Knox Group, the Knox unconformity, the Middle Ordovician transition from shallow shelf to deeper basin at Dandridge, Tennessee". Paleosols, paleoweathering surfaces, and sequence boundaries. 21: 13–18.
- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.