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Titlebook: Caves and Karst of the Greenbrier Valley in West Virginia; William B. White Book 2018 Springer International Publishing AG 2018 Large Cave

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發(fā)表于 2025-3-21 18:08:35 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Caves and Karst of the Greenbrier Valley in West Virginia
編輯William B. White
視頻videohttp://file.papertrans.cn/223/222682/222682.mp4
概述Presents detailed descriptions of some of the largest caves in eastern United States.Explores the aquatic fauna, terrestrial fauna, and fossil remains found in these caves.Provides a comprehensive geo
叢書名稱Cave and Karst Systems of the World
圖書封面Titlebook: Caves and Karst of the Greenbrier Valley in West Virginia;  William B. White Book 2018 Springer International Publishing AG 2018 Large Cave
描述The focus of this book is on the more than 2000 caves of the Greenbrier Valley of West Virginia of which the 14 with lengths greater than 10 km have an aggregate length of 639 km. The major caves form the core part of sub-basins which drain to big springs and ultimately to the Greenbrier River. Individual chapters of this book describe each of the major caves and its associated drainage basin. The caves are formed in the Mississippian Greenbrier Limestone in a setting of undulating gentle folds. Fractures, lineaments and confining layers within the limestone are the main controlling factors. The caves underlie an extensive sinkhole plain which may relate to a major erosion surface. The caves are habitat for both aquatic and terrestrial organisms which are cataloged and described as are the paleontological remains found in some of the caves. The sinkhole plain of the Greenbrier karst and the underlying complex of cave systems are the end result of at least a ten million year history oflandscape evolution which can be traced through the evolving sequence of cave passages and which is described in this book..
出版日期Book 2018
關(guān)鍵詞Large Caves; Cave Organisms; Caves and Karst; Cave Exploration; Greenbrier Karst; Greenbrier River; Greenb
版次1
doihttps://doi.org/10.1007/978-3-319-65801-8
isbn_softcover978-3-319-88110-2
isbn_ebook978-3-319-65801-8Series ISSN 2364-4591 Series E-ISSN 2364-4605
issn_series 2364-4591
copyrightSpringer International Publishing AG 2018
The information of publication is updating

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Entscheidungsverhalten im Feld,bsurface either east to Stamping Creek springs or southwest to Locust Spring. However, few parts of the underground are accessible to observation. The caves of the Little Levels are of intermediate size, one to two miles, and many carry active streams which allow some interpretation of the eastern and western edges, but not the central portion.
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The Swago Creek Basin,epresented by Barnes Pit, Tub Cave, and the Carpenters-Swago System. The Carpenter-Swago System has 3.1 miles of surveyed passage, and it is strongly controlled by a N60°E fracture system. Extensive stream tracing in the basin reveals details of drainage pattern which is strongly controlled by the shaly Taggard Formation.
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