USGS Visual Identifier

GEOLEX

Summary of Citation: Ottosee

Publication:
Ulrich, E.O., 1911, Revision of the Paleozoic Systems: Geological
   Society of America Bulletin, v. 22, p. 281-680
Usage in Publication:
Ottosee shale*

Modifications: Geologic Province: Dominant Lithology:
 Named
 Appalachian basin
 Shale
Limestone

Summary:
Named the Ottosee shale of the Blount group for Ottosee Lake, Chilhowee Park, Knoxville, TN. Consists of mainly shales and thin limestones; in one area it includes an 80 foot thick massive pink marble bed. Unit is 35 to 1200 feet thick. It unconformably overlies the Holston marble in the Knoxville trough and the Tellico sandstone in the Athens trough, and underlies the Lowville formation. The Ottosee is considered the top formation in the Blount group and is of Early Ordovician age.
Summary of Citation: Ottosee

Publication:
Butts, Charles, 1940, Geology of the Appalachian Valley in
   Virginia; Part 1: Virginia Geological Survey Bulletin, no.
   52, 568 p.
Usage in Publication:
Ottosee limestone

Modifications: Geologic Province: Dominant Lithology:
 Revised
 Appalachian basin
 

Summary:
Revised the Ottosee to the Ottosee limestone of the Blount group in VA. Unit overlies the Athens shale, Holston limestone, or the Lenoir limestone and underlies the Lowville-Moccasin limestone of the Black River group. Thickness is 100 to 595 feet. The Ottosee is of Middle Ordovician age.
Summary of Citation: Ottosee

Publication:
Butts, Charles and Gildersleeve, Benjamin, 1948, Geology and
   mineral resources of the Paleozoic area in northwest Georgia:
   Georgia Geological Survey Bulletin, no. 54, 176 p.
Usage in Publication:
Ottosee shale

Modifications: Geologic Province: Dominant Lithology:
 Areal limits
 Appalachian basin
 

Summary:
Geographically extended the Ottosee shale of the Blount group to GA. Unit overlies the Holston marble.
Summary of Citation: Ottosee

Publication:
Neuman, R.B., 1955, Middle Ordovician rocks of the type
   Tellico-Sevier belt, eastern Tennessee, IN Shorter contributions
   to general geology, 1955-57: U.S. Geological Survey Professional
   Paper, 274-F, p. 141-178
Usage in Publication:
Ottosee shale

Modifications: Geologic Province: Dominant Lithology:
 Not used
 Appalachian basin
 

Summary:
The term Ottosee shale is not used in this report. Author believes that the Ottosee shale and Holston formation are time-stratigraphic rather than lithostratigraphic. The Sevier formation is used in place of Ottosee shale.
Summary of Citation: Ottosee

Publication:
Bridge, Josiah, 1956, Stratigraphy of the Mascot-Jefferson City
   zinc district, Tennessee: U.S. Geological Survey Professional
   Paper, 277, 76 p.
Usage in Publication:
Ottosee shale*

Modifications: Geologic Province: Dominant Lithology:
 Revised
 Appalachian basin
 

Summary:
The Ottosee shale is used on the geologic map (not described in report) but is not part of the Blount group. The Blount group is discarded. The Ottosee is included with the Tellico sandstone as a map unit.
Summary of Citation: Ottosee

Publication:
Milici, R.C., 1973, The stratigraphy of Knox County, Tennessee:
   Tennessee Division of Geology Bulletin, no. 70, p. 9-24
Usage in Publication:
Ottosee Shale

Modifications: Geologic Province: Dominant Lithology:
 Revised
 Appalachian basin
 

Summary:
The Ottosee Shale is included in the Chickamauga Group in TN. Consists of fossiliferous shale, siltstone, sandstone, and marble. Shales are brown, brownish-gray, and medium- to dark-gray, and weather yellowish-gray or yellowish-brown. Limestones are coarse and argillaceous. Pinkish marble, similar to the Holston Formation, is scattered throughout the formation. Thickness ranges from 700 to 2000 feet. The Ottosee is of Middle Ordovician age.
Summary of Citation: Ottosee

Publication:
Frey, R.C., 1995, Middle and Upper Ordovician nautiloid cephalopods
   of the Cincinnati arch region of Kentucky, Indiana, and Ohio,
   IN Pojeta, John, Jr., ed., Contributions to the Ordovician
   paleontology of Kentucky and nearby states: U.S. Geological
   Survey Professional Paper, 1066-P, p. P1-P126
Usage in Publication:
Ottosee Shale*

Modifications: Geologic Province: Dominant Lithology:
 Overview
 Appalachian basin
 

Summary:
Tyrone Limestone of north-central TN correlates with Ottosee Shale, Moccasin Limestone, and Eggleston Formation of eastern TN, according to Ross and others (1982).