The tall craggy cliffs of the Drakensberg Mountains, with late season snow still slightly visible and high altitude clouds forming a V-shape
The tall craggy cliffs of the Drakensberg Mountains, with late season snow still slightly visible and high altitude clouds forming a V-shape in the Background. These iconic cliffs and peaks of the Drakensberg Mountains formed due to the combination of the Jurassic period large flood basalt during the break-up of the Gondwana Supercontinent and erosion from the later uplift of the African Continent. The Drakensberg Park were declared a Unesco World Heritage site in 2000 to protect the natural habitats, but also due to its cultural significant since it has the largest concentration of rock paintings in Sub Sahara Africa.
Size: 3456px × 5184px
Location: Drakensberg Mountains, South Africa
Photo credit: © Marieke Peche / Alamy / Afripics
License: Royalty Free
Model Released: No
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