The Afromontane grasslands of the Drakensberg mountains with a common sugarbush in the foreground
The Afromontane grasslands of the Drakensberg mountains with a common sugarbush in the foreground. 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.
Size: 5184px × 3456px
Location: Royal Natal National Park, Drakensberg Mountains, South Africa
Photo credit: © Marieke Peche / Alamy / Afripics
License: Royalty Free
Model Released: No
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