
 GEOLEX
Summary of Citation: Cannon
Publication:
Ulrich, E.O., 1911, Revision of the Paleozoic Systems: Geological
Society of America Bulletin, v. 22, p. 281-680
Usage in Publication: Cannon limestone*
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Named
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Appalachian basin
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Limestone
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Summary: Named the Cannon limestone for Cannon Co., TN. Consists of several hundred feet of limestone on the east flank of the Nashville dome. It thins rapidly to the west and finally wedges out in the vicinity of Nashville. Unit overlies the Hermitage formation and underlies the Eden group; it is equivalent in age to the interval spanned by the Bigby, Flanagan, and Perryville limestones, and the Catheys formation. The Cannon is of Middle Ordovician (Trentonian) age.
Summary of Citation: Cannon
Publication:
Milici, R.C. and Smith, J.W., 1969, Stratigraphy of the Chickamauga
Supergroup in its type area, IN Precambrian-Paleozoic
Appalachian problems: Georgia Geological Survey Bulletin,
no. 80, p. 1-35
Usage in Publication: Cannon Limestone
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Areal limits
Revised
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Appalachian basin
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Summary: Geographically extended the Cannon Limestone to northwestern GA and included it in the Nashville Group (middle formation of three). Consists of medium dark gray calcilutite and calcarenite in well defined beds generally 2 to 6 inches thick that contains chert lenses and nodules; It is fossiliferous and contains TETRADIUM, brachiopods, bryozoans, and gastropods. Thickness is 110 to 120 feet. Unit overlies the Hermitage Formation and underlies the Catheys Formation, both of the Nashville Group.
Summary of Citation: Cannon
Publication:
Higgins, M.W., Atkins, R.L., Crawford, T.J., Crawford, R.F.,
III, Brooks, Rebekah and Cook, R.B., Jr., 1988, The structure,
stratigraphy, tectonostratigraphy, and evolution of the
southernmost part of the Appalachian Orogen, Georgia and
Alabama: U.S. Geological Survey Professional Paper, 1475,
173 p., (incl. geologic map, scale 1:500,000), Supersedes
U.S. Geological Survey Open-File Report OF-86-372.
Usage in Publication: Cannon Limestone*
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Dominant Lithology: |
Areal limits
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Appalachian basin
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Summary: The Cannon Limestone of the Nashville Group, as defined by Milici and Smith (1969), is here used in the Chickamauga terrane in GA.
Summary of Citation: Cannon
Publication:
Chowns, T.M., 1989, Stratigraphy of major thrust sheets in the
Valley and Ridge province of Georgia, IN Fritz, W.J., ed.,
Excursions in Georgia geology: Georgia Geological Society
Guidebook, v. 9, no. 1, Joint annual meeting of Geological
Society of America, Southeastern Section, and Georgia Geological
Society, Atlanta, GA, April 6-7, 1989, p. 211-238
Usage in Publication: Cannon Member
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Revised
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Appalachian basin
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Summary: Catheys (Catoosa Co.) and Cannon and Hermitage (Walker Co.) regarded as members of Nashville Formation of Chickamauga Group in this report, following the nomenclature of Carter and Chowns (1986: AL Geol. Soc. Guidebook, 23rd Ann. Field Trip) and Carter and Chowns (in press: Amer. Assoc. Pet. Geol., Studies in Geology).
Summary of Citation: Cannon
Publication:
Clark, S.H.B., Spanski, G.T., Hadley, D.G. and Hofstra, A.H.,
1993, Geology and mineral resource potential of the Chattanooga
1 degrees x 2 degrees quadrangle, Tennessee and North Carolina;
a preliminary assessment: U.S. Geological Survey Bulletin,
2005, 35 p.
Usage in Publication: Cannon Limestone*
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Overview
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Cincinnati arch
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Summary: Nashville Group, consisting of Catheys Formation, Bigby and Cannon Limestones, and Hermitage Formation, is mapped undivided on plate 1. Age of Cannon is Middle Ordovician. Cannon correlates with Bigby.
Summary of Citation: Cannon
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: Cannon Limestone*
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Age modified
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Cincinnati arch
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Summary: Cannon Limestone is Champlainian (Kirkfieldian and Shermanian) in age. Shown undivided with Bigby Limestone.
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