Hoanib

The Hoanib is one of the 12 ephemeral seasonal rivers in the west of Namibia, where it was the border between northern Damaraland and Kaokoland. Its length is 270 km. With the low population density, the oasis character of the river valley and the relatively high wildlife population of Hoanib, together with the Hoarusib its valley is one of the last true wilderness areas in Namibia, one of the last settlements of desert elephants and shows strong wind and water eroded and weathered stone deposits (up to 10 m height). Inflows of Hoanib are Ombonde, Ganamub, Mudorib and Tsuxab.

Hydrology

The Hoanib's catchment area of 17,200 km ² extends from the west coast to Ojiovasando and the black peaks of the interior. It also includes the resource-rich region Sesfontein, Warmquelle and the Khowarib Gorge. The highest point of the watershed is at 1800 m. The rainfall in the catchment area is sporadic and vary from 0 mm / yr in the west to 325 mm in the north east of the catchment. The proportion of area with less than 100 mm / yr is 71%. In only 12% of the catchment area is the annual rainfall over 300 mm. The Hoanib flows only every few years from heavy rainfall in the hinterland of the catchment area, but then the flood wave can be several meters high and last for several days. Not always, but more often in recent years, the water reaches the mouth in the Atlantic. A large part of the water seeps into and contributes to a large dense subsurface aquifer, from the exits at various points in the river bed, so that even in dry years there is groundwater. Surrounding groundwater forms efflorescence used by many antelope as salt licks. During dry periods Hoanib desert elephant foot dig deep holes to reach the near-surface groundwater.