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Cave Density of the Greenbrier Limestone Group, West Virginia

Papers in Applied Geography, 2015
The Greenbrier Limestone Group, known in West Virginia as the “Big Lime,” is an extensive, calcium-pure limestone unit of Mississippian Age (350–340 million years). Deposited in a shallow ocean basin during the Carboniferous, the Big Lime is more than 1,000 feet thick in the Greenbrier Valley of West Virginia.
Lee Stocks,, Andrew Shears
exaly   +2 more sources

Terrestrial Fauna in the Greenbrier Karst

2017
The West Virginia cave fauna includes species that leave caves periodically to forage (cave crickets and bats) as well as permanent inhabitants (both species that are limited to caves [troglobionts] and ones that occur elsewhere [troglophiles]). Troglobionts are the best studied, but troglophiles predominate in many caves. Major sources of food for the
David C. Culver, Daniel W. Fong
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Petrology and Paleogeography of Greenbrier Formation

AAPG Bulletin, 1949
ABSTRACT This paper describes the petrology and paleogeography of the Mississippian Greenbrier formation as determined from study of well samples, insoluble residues, heavy minerals, and thin sections. In the Greenbrier formation, clastic limestone beds composed of lime sand, oölites, and quartz sand alternate with beds of fine ...
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The Subterranean Aquatic Fauna of the Greenbrier Karst

2017
The Greenbrier Karst harbors 16 species of stygobionts known from 92 caves, and six of these caves are type localities of ten of the species. The fauna is dominated by crustaceans and especially amphipods of the genus Stygobromus, and they primarily occupy vadose streams and the epikarst, but are notably absent from phreatic waters. Stygobromus spinaus
Daniel W. Fong, David C. Culver
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Hydrology of the Greenbrier Karst

2017
Studies of the karst drainage systems of the Greenbrier limestone in southeastern West Virginia began in the early 1960s and were the first to make extensive use of water-tracing techniques and cave mapping in the USA. The carbonate aquifer is about 400 ft (120 m) thick in the Swago Creek area west of Marlinton (Pocahontas County) increasing to 1000 ft
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The Greenbrier Karst

2017
The segment of the Appalachian karst known as the Greenbrier karst is located in the lower valley of the Greenbrier River in southeastern West Virginia. The karst is developed in the Mississippian Greenbrier Limestone which thickens from 100 to 365 m northeast to southwest.
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A rare case of diffuse penile phytocontact dermatitis caused by common greenbrier

Indian Journal of Skin Allergy, 2023
Penis size has always been a considerable concern to a lot of men. Many men look for ways to increase their penile size, ranging from oral medication, stretch apparatus, injections, and surgery, to traditional methods. Smilax rotundifolia, also known as daun bungkus or common greenbrier in the western hemisphere, is a local herb most found in the West ...
Andrew Yoshihiro Wirya   +2 more
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