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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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Caves of the Dickson Spring Basin, Monroe County,exception of Haynes Cave, are all in the headwaters (southern) part of the drainage basin and are complex from a geologic and hydrologic viewpoint. Most of these caves have received little attention in the last forty years because of access limitations.
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Forschungsdesign und empirisches Feldne contact. The result is a patchwork of large underground drainage systems each discharging through a large spring. Analysis of the profiles of active surface streams and abandoned stream beds gives some insight into the developmental history of the karst.
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Innovation und Entrepreneurshipf drainage Systems discharging to two springs 20-km distant from each other with high flows discharge to one and low flows to the other. Drainage patterns have shifted over time as the surface drainage is captured. An estimated age for the entire System is 4.1 million years.
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Zeitoptimales Weihnachtsliedersingen,e limestone. The pattern of passages is typically dendritic with an overall trend sub-parallel to the regional strike. Folding and faulting influence passage orientation in some of the passages, but the perching effect of the underlying shale forces the conduits downward along the local dip.
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