G.D. McKeever was a resident of Swago, West Virginia, who was involved in the study of caves and karst hydrology in the Greenbrier Valley. He co-authored a paper with William B. White in 1992 titled "The Caves and Karst Hydrology of Southern Pocahontas County and the Upper Greenbrier River Valley, West Virginia" which was published in the book Caves and Karst of the Greenbrier Valley in West Virginia.
Sure, here is a summary of the book "The Caves and Karst Hydrology of Southern Pocahontas County and the Upper Greenbrier River Valley, West Virginia" by Gary D. Storrick, published in 1992. This is the tenth volume of the West Virginia Speleological Survey's Bulletin Series. The book contains a comprehensive overview of the caves and karst hydrology of southern Pocahontas County and the upper Greenbrier River Valley.
Storrick begins by discussing the stratigraphy of the Greenbrier Group, which is the main rock formation in the study area. The Greenbrier Group is a thick sequence of limestones, dolomites, and shales that was deposited in a warm, shallow sea during the Devonian Period. The limestones and dolomites are the most soluble rocks in the Greenbrier Group, and they are the ones that have been dissolved to form caves.
Next, Storrick discusses the development of caves and karst hydrology. Karst is a type of landscape that is characterized by sinkholes, springs, and caves. It is formed by the dissolution of soluble rocks, such as limestone and dolomite. The dissolution of these rocks creates a network of underground passages that can transport water over long distances.
Storrick then discusses the limestone springs in southern Pocahontas County. These springs are an important source of water for both human and natural communities. Storrick describes the location, flow characteristics, and water quality of these springs.
Finally, Storrick discusses the spelean fauna of southern Pocahontas County. The spelean fauna is the community of animals that live in caves. Storrick describes the various species of spelean fauna that have been found in the study area, and he discusses the threats to these species.
The book is well-illustrated with maps, photographs, and diagrams. It is a valuable resource for anyone interested in the caves and karst hydrology of southern Pocahontas County and the upper Greenbrier River Valley.
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