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Dead Camel Thorn trees in the Dead Vlei in the Namib-Naukluft National Park

The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed Camel Thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area. The trees died, as there no longer was enough water to survive. The remaining skeletons of the trees, which are believed to be about 900 years old, are now black because the intense sun has scorched them. The wood does not decompose because it is so dry.
Dead Camel Thorn trees in the Dead Vlei in the Namib-Naukluft National Park