Abstract
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). The Hole is the northernmost of the contact caves and drains north to Spring Creek. Ludington, McClung, Maxwelton Sink, Benedict, and Wades caves drain southwest to Davis Spring. These caves are developed in the lower section of the Hillsdale Limestone with many passages entrenched by vadose erosion by up to 12 m (40 ft) into the shale. Recharge is mostly from small surface streams that flow westward on the Maccrady Shale and sink at the contact with the 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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References
Balfour, W.M. 1973. The origin of contact passages developed at the contact between the Greenbrier Series and The Maccrady Series, Greenbrier County. West Virginia. Region Record 3 (1): 14–17.
Gams, I. 1965. Types of accelerated corrosion. In Problems of the speleological research, ed. O. Štelcl, 133–139. Prague: Czechoslovak Academy of Sciences.
Heller, S.A. 1980. A hydrogeologic study of the Greenbrier limestone karst of central Greenbrier County, West Virginia, 421pp. PhD Thesis, West Virginia University.
Mihevc, A. 1994. Contact karst of the Brkini hills. Acta Carsologica 23: 100–109.
Palmer, A.N. 1974. Geologic influence upon cave–passage orientation in Ludington Cave, Greenbrier County, West Virginia. In Proceedings of the fourth conference on Karst geology and hydrology, ed. H.W. Rauch, and E. Werner, 33–40. Morgantown, WV: West Virginia Geologic and Economic Survey, Morgantown.
Pasquarell, G.C., and D.G. Boyer. 1995. Agricultural impacts on bacterial water quality in Karst groundwater. Journal Environmental Quality 24: 959–969.
Price, P.H., and E.T. Heck. 1939. Greenbrier County, 846. Morgantown, WV: West Virginia Geologic and Economic Survey County Report.
Rutherford, J.M. 1967. Initial explorations of the contact caves of the Great Savannah (abs.). National Speleological Society Bulletin 29 (3): 111.
Wells, D., J.J. Renton, and R.L. Perkins. 1967. Normal faulting in the Caldwell-Lewisburg area of Greenbrier County, West Virginia. West Virginia Academy of Science Proceedings 1966 (38): 155–158.
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Balfour, W.M. (2018). The Contact Caves of Central Greenbrier County. In: White, W. (eds) Caves and Karst of the Greenbrier Valley in West Virginia. Cave and Karst Systems of the World. Springer, Cham. https://doi.org/10.1007/978-3-319-65801-8_11
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DOI: https://doi.org/10.1007/978-3-319-65801-8_11
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