This study examines the water-level elevation history of selected flooding and flooded underground mines in the Pittsburgh coal basin of SW Pennsylvania from the time of closure until post-flooding pool-level reequilibration. Mines within this mining district developed pools with nearly steady-state groundwater flow within 10 to 50 years after closure. Equilibrated pool levels within each of the mines were controlled by various combinations of spillage to the surface or other mines, pumpage, and barrier leakage. In a study of flooding in the Clarksville, PA area, field water-level observations, mine geometry, barrier hydraulic conductivity, recharge rates, and late-stage storage gains were parameterized to match known pumping rates and develop a fluid mass balance. Vertical infiltration (recharge and leakage) estimates were developed using a depth-dependent model based on the assumption that most vertical infiltration is focused in areas with <75 m of overburden. A MODFLOW simulation of the nearly steadystate flow conditions was calibrated to hydraulic heads in observation wells and to known pumping rates by varying barrier hydraulic conductivity. The calibrated model suggests significant head-driven leakage between adjacent mines, both horizontally through coal barriers and vertically through interburden into an overlying mine. Calibrated barrier hydraulic conductivities were significantly greater than literature values for other mines at similar depths in the region. This suggests that some barriers may be hydraulically compromised by un-mapped entries, horizontal boreholes, or similar features that act to interconnect mines. These model results suggest that post-mining inter-annual equilibrium conditions are amenable to quantitative description using mine maps, sparse observation-well data, accurately-estimated pumping rates, and depth-dependent vertical infiltration estimates. Results are applicable to planning for postflooding water control schemes, although hydraulic testing may be required to verify model results. iv ACKNOWLEDGEMENTS I would like to express my gratitude to Dr. Joe Donovan whose enduring patience and encouragement allowed me to complete this manuscript. Eberhard Werner and the late Bruce Leavitt provided insight into various aspects of mining and mine hydrology. Information regarding mine operations was provided by Joe Lapkowicz, former mining engineer in Gateway mine. Ken Dufalla, President of the Izaak Walton League of Greene County, shared observations on the location and timing of surface discharges from Clyde and Pitt Gas mines. T. D. Light, J. Hawkins, and two anonymous reviewers provided comments that improved Chapter 3 v