THE LAST FORTY YEARS OF KARST HYDROLOGY STUDIES ON THE CUMBERLAND PLATEAU ESCARPMENT IN TENNESSEE
Straight-line subsurface flow paths documented through tracing studies do not exceed ten miles, but flow paths frequently cross under surface water divides. The limited flow observations that are available at major springs suggest that discharge during floods can be two orders of magnitude greater than baseflow, which is commonly less than 300 liters per minute. Extensive exploration of caves over the past forty years has resulted in a better understanding of geologic controls on hydrogeology. Divergent flow is common in this fluviokarstic terrain, with much of the baseflow that runs off Pennsylvanian clastic rocks sinking into cave streams in Mississippian carbonates while the majority of floodwater remains in surface channels. Major resurgences from cave streams are typically at limestone and chert contacts within the St. Louis limestone or at the contact between the St. Louis and Warsaw formations. Many of these discharges are at least partially submerged in surface streams and are located where access is difficult, complicating hydrology studies. Currently, a collaborative effort between cave explorers and the USGS is leading to a better organized effort to collect hydrology data in Cumberland Plateau escarpment watersheds.