Karst landscapes of New South Wales, Australia

Physics

Scientific paper

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Scientific paper

Karst in New South Wales has developed on Proterozoic to Permian limestones, and in Quaternary limestones on Lord Howe Island. Karst features seen today have been controlled by the geotectonic setting of the limestone, its topographic position, climatic regime, and in many areas a history of repeated episodes of karstification extending back at least to Devonian times.

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