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22 NCKRI Special Paper No. 1 Figure 11. Variants of hydrostratigraphic position and recharge/discharge relationships for a cave formation in a layered aquifer system. The actual mode of recharge and discharge depends also on the permeability structure within the cave formation, which is not specified. It is assumed to be diffuse in all diagrams but A4. See text for further discussion.
ASCENDING HYPOGENIC SPELEOGENESIS Figure 12. Regionalization of Optymistychna Cave, western Ukraine, a 214+ km long maze, according to its multi-story structures and the reconstruction of recharge-discharge arrangement during the time of its formation. Inset diagrammatically shows the hydrostratigraphy and the stair-case effect of the recharge-discharge offset. The thickness of the gypsum bed (18 m) is exaggerated. From Klimchouk et al. (1995). Figure 13. A = Plan of Wind Cave, Black Hills, South Dakota, USA (courtesy of Wind Cave National Park); B = a diagram illustrating the concept of the uplift origin of the Black Hills maze caves and the staircase effect of recharge-discharge offset. Redrawn from Ford (1989). 23
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