Cutta Cutta Cave.
The cave is a strongly joint-controlled linear phreatic system.
It has a complex history of alternating solution and filling with sediments.
The roof in this photo shows a paleokarst fissure fill.
File: C020710.jpg
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Katherine karst area, Daly Basin, NT Cutta Cutta Cave. The cave is a strongly joint-controlled linear phreatic system. It has a complex history of alternating solution and filling with sediments. The roof in this photo shows a paleokarst fissure fill. File: C020710.jpg |
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Katherine karst area, Daly Basin, NT Cutta Cutta Cave. Phreatic spongework in wall. File: C020706.jpg |
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Katherine karst area, Daly Basin, NT Cutta Cutta Cave. Areas of paleokarst fill - red earth. File: C020715.jpg |
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Katherine karst area, Daly Basin, NT Cutta Cutta Cave. Conulite in mud of cave floor. File: C020720x.JPG |