Kope Formation
| Kope Formation Stratigraphic range: Late Ordovician (Edenian Stage) |
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Photograph and etched section of hand sample of limestone of Kope Formation. Brachiopods and Bryozoans visible.
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| Type | sedimentary |
| Unit of | Maquoketa Group (in Indiana) |
| Sub-units | Grand Avenue Member, Wesselman Tongue |
| Underlies | Fairview Formation |
| Overlies | Point Pleasant Formation |
| Lithology | |
| Primary | Limestone |
| Other | shale |
| Location | |
| Region | Cincinnati Arch of North America |
| Extent | Kentucky, Ohio, Indiana |
The Kope Formation is one of the three component bedrock formations of the Maquoketa Group that primarily consists of shale (75%) with some limestone (25%) interbedded. In general, it has a bluish-gray color that weathers light gray to yellowish-gray and it occurs in northern Kentucky, southwest Ohio, and southeast Indiana, USA.
Contents
Description
Depositional environment
The depositional environment of the Kope was shallow marine. The central North American continent was a tropical epeiric sea at the time.
Jennette and Pryor (1993) interpret the Kope, along with the Bellevue and Fairview formations, as a progradational succession on a carbonate ramp. The Kope is the most distal facies of the ramp complex.[1]
Notable Exposures
The type section of the Grand Avenue Member is a cliff to the west of Grand Avenue in Cincinnati, Hamilton County, Ohio.[2]
The type section of the Wesselman Tongue of the Kope formation is an east-facing embankment on an unnamed creek that is followed by Wesselman Road in Miami Township, Hamilton County, Ohio. The embankment is 400 ft south of Zion Hill bridge.[2]
Fossils
Brachiopods, trilobites, bryozoans, rugose corals, and echinoderms (including crinoids, asteroids, and edrioasteroids) are all present in the Kope. Due to their mid-continent depositional environment, the fossils are almost free of deformation caused by tectonic activity common in the Appalachian Mountains.
The brachiopods Dalmanella sp., Hebertella sp., Leptaena sp., Petrocrania sp., Philhedra sp., Platystrophia sp., Pseudolingula sp., Rafinesquina sp., Sowerbyella sp., Strophomena sp., Trematis sp., and Zygospira sp. have been recorded from the Cincinnatian Series, which includes the Kope Formation. [3]
The trilobites such as Triarthrus eatoni, Cryptolithus tessellatus, and Proetidella parviusculus have been identified in the Kope, and the Ohio State Fossil, Isotelus maximus, can most likely be found in it.[4]
The bryozoans Ceramophylla sp., Eridotrypa mutabilis, Peronopera vera, Batostoma jamesi, Dekayia aspera, Heterotrypa ulrichi, Parvohallopora sp., and Amplexopora septosa have been found in the Kope.[5]
Among echinoderms, the crinoids Cincinnaticrinus varibrachialis, Ectenocrinus sp., and Iocrinus sp. are present in the Kope. Edrioasteroids and asteroids (starfish), generally rare, are common in overlying formations, and may be present in the Kope.[6]
Age
Relative age dating of the Kope places it in the Late Ordovician period.
Notes
- ↑ Jennette, D.C., and Pryor, W.A., 1993, Cyclic alternation of proximal and distal storm facies; Kope and Fairview Formations (Upper Ordovician), Ohio and Kentucky: Journal of Sedimentary Petrology, v. 63, no. 2, p. 183-203.
- ↑ 2.0 2.1 Ford, J.P., 1967, Cincinnatian geology in southwest Hamilton County, Ohio: American Association of Petroleum Geologists Bulletin, v. 51, no. 6, p. 918-936.
- ↑ Fossils of Ohio, p. 216-18
- ↑ Fossils of Ohio, Fig. 8.1
- ↑ Fossils of Ohio, Fig. 15.1, Fig. 15.2, Fig. 15.3
- ↑ Fossils of Ohio, p. 245-246
References
- Fossils of Ohio, Bulletin 70, Ohio Department of Natural Resources, Division of Geological Survey, Edited by Rodney M. Feldmann and Merrianne Hackathorn, 577 p., 232 plates (some in color), drawings, maps, and tables, 1996 [1]
