This uplift locally created rugged mountains reduced by erosion to their present state largely during the Pennslyvanian & Permian Periods. Extensive weathering produced the tors of the Charon Gardens region and the "river" of boulders that descends the west slope of Mount Scott. Likewise, weathering produced the bowling-ball sized boulders in the Permian Post Oak Conglomerate locally found in and around the mountains. In addition to outcrops of the conglomerate, the boulders are preserved in the distinctive rock buildings of Medicine Park. As the Permian progressed, river sediments buried the Wichita Mountains, preserving them from further weathering. Recent geological erosion has removed these sediments, excavating these once buried fossil landforms.