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Geology of the Greenbrier Valley

2017
The Greenbrier Karst is located in the Appalachian Highlands in the boundary region between the strongly folded rocks of the valley and ridge province and the gently folded rocks of the Appalachian Plateau. The outcrop of the karstic Greenbrier Limestone occupies portions of Pocahontas, Greenbrier, and Monroe Counties in southeast West Virginia.
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Post-Greenbrier Reflections on Graduate Training in Clinical Neurology

Archives of Neurology, 1967
RECENTLY, some 270 clinical and laboratory neurologists gathered at the Greenbrier Hotel to discuss education in the neurological sciences. Delegates to the conference came from nearly every medical school in the United States and Canada as well as from several special institutes and foreign medical schools.
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Pleistocene Vertebrates from Greenbrier Valley Caves

2017
Every cave has the potential to be a repository of Pleistocene and older bones and past life. The Greenbrier Valley Karst in particular has a rich repository of late Pleistocene faunal remains. Cave entrances lend themselves to be nesting places for birds of prey who deposit the bones of their meals onto cave floors.
E. Ray Garton, Frederick V. Grady
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Petrology and Paleogeology of Greenbrier Limestone: ABSTRACT

AAPG Bulletin, 1948
This paper outlines the petrology and paleogeography of the Greenbrier formation of Mississippian age, as determined from study of well samples, insoluble residues, heavy minerals, and thin sections. In the Greenbrier, clastic limestone beds composed of calcareous sand, oolites, and quartz sand alternate with beds of fine-grained limestone in which ...
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The Exploration History of the Greenbrier Valley Caves

2017
The earliest accounts of caves in the Greenbrier Valley document mining for saltpeter, which occurred in 23 caves at various periods from the late 1700s, through the War of 1812, and the American Civil War. Technical descriptions of the caves began in the late 1940s with the work of William E. Davies.
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The Contact Caves of Central Greenbrier County

2017
Six major cave systems are developed along the eastern border of the basal Hillsdale Limestone (Greenbrier Group) and the underlying Maccrady Shale between the town of Lewisburg and Spring Creek in central Greenbrier County. The total combined surveyed passage is just over 128 km (80 miles).
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Distribution and habitat preferences of eastern hellbenders within the Greenbrier River

Proceedings of the West Virginia Academy of Science, 2018
The eastern hellbender (Cryptobranchus alleganiensis alleganiensis) is experiencing extensive population declines throughout its native range as a result of habitat loss and degradation associated with widespread anthropogenic activity. Consequently, there is a critical need to conserve and expand remaining populations.
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Life history and ecology of the Greenbrier Crayfish Cambarus smilax Loughman, Simon & Welsh, 2011 (Decapoda: Astacoidea: Cambaridae)

Journal of Crustacean Biology, 2022
Zackary A Graham   +2 more
exaly  

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