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Further hydrogeological investigations of the Mill Creek Kansas Creek area, Northern Tasmania

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Figure

Figure 1. demonstrated MR CR Relationships between karst phenomena and base flow underground drainage routes by water-tracing experiments, The present land tenure in the area is superimposed: = Croeslis Cave State Reserve; SF = State forest; WHA = World He
Table 1. Discharge estimates for streams, 9-12 April 1983 (by velocity head method).
Figure 2. systems. Developed topographic profiles indicating the relative altitudes of components of the karst drainage The extent of negotiable caves discovered and physically explored to date is represented schematically, together with the potential exte
Figure 5. from Catchment of Croesus Cave under very high discharge conditions. Some water this area will also discharge via Mill Creek, Tailender Cave, Lynds Cave and Marakoopa Creek due to flow bifurcations under these conditions

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