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Kango Caves
WI_za178.jpg Kyzylsu Valley  |  Gypsum karst and landslideThumbnails

The cave system formed by dissolution of Precambrian limestone of the Swartberg Mountains. It was discovered in 1780 and has since become a popular tourist cave.

Keywords
cave, karst processes
Created
Friday 12 November 2004 by Martin Mergili in Africa / South Africa (851 visits)