ABSTRACT

River cave is the finest of many very active stream-sink caves (Waltham & Smart, 1975), but all routes drop quickly to sumps, where the long phreatic passages beyond remain unexplored. Scattered through the karst are a number of collapse dolines and impressive open shafts 100-200 m deep, but none leads into long cave systems. Fragments of abandoned phreatic trunk caves survive within the karst (Figure 1); many passages are more than 20 m high and wide, and are liberally decorated with secondary calcite deposits. Also notable among the many caves on the island (Fincham, 1997) are Jackson’s Bay Caves, with 3300 m of large and beautiful water passages beneath a dry region of low-lying, cactus-covered karst near the south coast.