On the Geology of the Western States of North America, 0000, Owen David Dale,

The remarks here submitted will be confined chiefly to that part of the Western States of North America watered by the rivers Ohio, Wabash, Illinois, Rock, Wisconsin, Cumberland and Tennessee, lying between the 35th and 43rd degree of N. latitude and the 81st and 91st of W. longitude. The district includes the states of Illinois, Indiana, Ohio, Kentucky, Tennessee, and the Du Buque and Mineral Point districts of Iowa and Wisconsin. This territory occupies an area of about half a million of square miles, but its geological features are remarkably uniform, belonging, with a few partial exceptions, to the periods of the bituminous coal and carboniferous limestone as found in Europe, and the Silurian rocks as described by Sir R. Murchison; the exceptions are the superficial deposits which occasionally cover up these from view over considerable tracts, and these must either be referred to the age of gigantic mammalia and formations of a much newer date, or belong to a marl and greensand found in the western district of Tennessee, probably a portion of the greensand and other members of the cretaceous group. A general idea of the geological formations of the whole tract may be obtained from the annexed diagram. ... This 250-word extract was created in the absence of an abstract

Preliminary Study of Cave Ecology - with Special Reference to Tennessee Caverns, 1949, Barr Jr. , Thomas C.

Regional Development of Limestone Caves in Middle Tennessee, 1954, Barr Jr. , Thomas C.

Land Snails from the Caves of Kentucky, Tennessee and Alabama, 1964, Hubricht, Leslie

Genesis of the Ordovician zinc deposits in east Tennessee, 1965, Hoagland Alan D. , Hill William T. , Fulweiler Robert E. ,

Zinc occurs in low-iron sphalerite associated with gangue dolomite in dissolution breccias and collapse structures in dolomitized limestone and interbedded fine-grained 'primary' dolomite. These breccias and collapse structures were developed as part of a karst-sinkhole complex formed at depths up to 800 feet below the top of the Knox Dolomite during widespread emergence at the end of Early Ordovician time. Mineralization was completed before the rocks were tilted, and clearly antedates the Appalachian orogeny. Source of hydrothermal solutions is not known

Armadillo Remains From Tennessee and West Virginia Caves, 1966, Guilday, John E.

Extinct Florida Spectacled Bear Tremarctos floridanus (Gidley) from Central Tennessee, 1967, Guilday John E. , Irving David C.

A lower Paleozoic paleoaquifer; the Kingsport Formation and Mascot dolomite of Tennessee and southwest Virginia, 1971, Harris Leonard D. ,

Jaguar (Panthera onca) Remains from Big Bone Cave, Tennessee and East Central North America, 1972, Guilday John E. , Mcginnis Helen

Branchiobdellids (Annelida: Clitellata) from some Eastern North American caves, with descriptions of new species of the Genus Cambarincola., 1973, Holt Perry C.

Branchiobdellids are found as epizoites on crustaceans of the orders Isopoda and Decapoda (cambarine crayfishes) in caves of eastern North America. Species that may be considered as troglobites, since they are not known from epigean waters, appear to be confirmed to truly troglobitic isopods and possibly a few troglobitic crayfishes from Florida and the Tennessee-Kentucky Highland Rim cave belt. The majority of the records of branchiobdellids from caves are of representatives of common epigean forms epizootic un crayfishes. Cross-referenced lists of branchiobdellids, their hosts and cave localities are presented. Some of the new species described are apparently troglobitic or troglophilic, but they present no consistent phylogenetic or geographical pattern and separate origins for them from primitive stocks of the genus Cambarincola are postulated.

Branchiobdellids (Annelida: Clitellata) from some Eastern North American caves, with descriptions of new species of the Genus Cambarincola., 1973, Holt Perry C.

Branchiobdellids are found as epizoites on crustaceans of the orders Isopoda and Decapoda (cambarine crayfishes) in caves of eastern North America. Species that may be considered as troglobites, since they are not known from epigean waters, appear to be confirmed to truly troglobitic isopods and possibly a few troglobitic crayfishes from Florida and the Tennessee-Kentucky Highland Rim cave belt. The majority of the records of branchiobdellids from caves are of representatives of common epigean forms epizootic un crayfishes. Cross-referenced lists of branchiobdellids, their hosts and cave localities are presented. Some of the new species described are apparently troglobitic or troglophilic, but they present no consistent phylogenetic or geographical pattern and separate origins for them from primitive stocks of the genus Cambarincola are postulated.

Typhlichthys subterraneus Girard (Pisces: Amblyopsidae) in the Jackson Plain of Tennessee, 1976, Bechler, David L.

Definitive doline characteristics in the Clarksville Quadrangle, Tennessee, 1976, Kemmerly P. P. ,

Strontium isotopic geochemistry of mississippi valley-type deposits, East Tennessee; implications for age and source of mineralizing brines, 1988, Kesler Stephen E. , Jones Lois M. , Ruiz Joaquin,

Geochemical and petrologic observations on Lechuguilla Cave, New Mexico, 1992, Palmer A. N. , Palmer M. V.