Attempts were made to apply an analytical groundwater flow model (MINEFLO) to a reclaimed surface coal mine spoil in West Virginia, U.S.A., that exhibited characteristics of both a conventional porous medium and pseudokarst flow. The model utilizes the method of analytic elements to derive a steady-state solution to the ground water flow equation for a single aquifer. Two simulations were performed, using hydrologic features and parameter values determined from field observations, slug withdrawal tests (1989) and slug injection tests (1990). Simulated heads at base-flow conditions for 1989 were about 12% different ihan measured values, with a root-mean-square (RMS) en-or of 0.82 m. A similar simulation for I 990 produced a somewhat better match, with an average head difference of less than 10% (RMS e1Tor of0.66 m). However, in both cases, the simulated flow rate at the toe-of-spoil seep was over 75% less than the measured rate. This suggested that the hydraulic conductivity values obtained from the slug tests may have underestimated the overall hydraulic conductivity of the aquifer materials, perhaps because of the influence ofpseudokarst and/or fracture flow mechanisms. It was concluded that the model could predict (within 10%) the base-flow water levels at a spoil site where recharge is known to occur primarily from adjacent unmined strata. The use of the model's only transient feature (pumping well) at the study site is doubtful due to the large RMS en-or in the steady-state simulation.