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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Fallibility

https://doi.org/10.1007/978-3-8349-8897-3a is dominated by crustaceans and especially amphipods of the genus ., and they primarily occupy vadose streams and the epikarst, but are notably absent from phreatic waters. . is the most widely distributed, found in 59 caves. The segmented worm . and the salamander . are both endemic to single sit

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https://doi.org/10.1007/978-3-319-65801-8Large Caves; Cave Organisms; Caves and Karst; Cave Exploration; Greenbrier Karst; Greenbrier River; Greenb

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978-3-319-88110-2Springer International Publishing AG 2018

玛瑙

Hydrology of the Greenbrier Karst,ch of the flow through the aquifer is through conduits under open channel conditions much like a surface stream with a roof. Discharge is concentrated at large springs that typically display rapid response to storm events, and the ratio of maximum to minimum discharge exceeds 100:1 for most of the s

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abreast

NICHE

Scott Hollow Cave,by regional flexures resulting from Alleghenian compressive stress and an unmapped thrust fault. Tributaries joining the Mystic River from the east generally trend down dip along bedding planes, while western tributaries follow steeper, more complex paths, at least partially controlled by a thrust f

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