Geology
The park consists of the two major valley systems of the Kidepo and Narus Rivers. The valley floors lie between 3,000 feet (910 m) and 4,000 feet (1,200 m) AMSL.
Kanangarok (also spelled Kananorok or Kanatarok) is a tepid hot spring in the extreme north of the Park, beside the South Sudanese boundary. This spring is the most permanent source of water in the park. The soil in the park is clayey. In the Kidepo Valley black chalky clay and sandy-clay loam predominate, while the Narus Valley has freer-draining red clays and loams.
Read more about this topic: Kidepo Valley National Park