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talia cave1-770Talia Cave in South Australia has formed along a joint in the basement 1550 million year old Mesoproterozoic sandstone. The red sandstone is capped by 20 m of Pleistocene dune calcarenite that form the walls and roof. Waves break over rocks seaward of the cave mouth and surge up the gully (above figure) to dissipate on a boulder beach at the rear of the 50 m long cave (below figure). This photo was taken October 2010 by Andrew D. Short, Coastal Studies Unit, School of Geosciences, University of Sydney, Sydney NSW 2006, Australia, This email address is being protected from spambots. You need JavaScript enabled to view it.

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