description Cuvelai-Etosha Basin Overview
The Cuvelai-Etosha Basin is an inland drainage system extending across southern Angola and northern Namibia. Seasonal water flows through shallow channels, locally called oshanas and omirambas, rather than through a permanent river network, creating temporary wetlands during the rainy season. The system drains toward Etosha Pan, a broad saline depression in northern Namibia that is usually dry but can become partially flooded and attract large numbers of waterbirds.
help Cuvelai-Etosha Basin FAQ
Where is the Cuvelai-Etosha Basin?
The Cuvelai-Etosha Basin extends across southern Angola and northern Namibia. It is an inland drainage system rather than a basin that reaches the sea through a permanent river.
What are oshanas in the Cuvelai-Etosha Basin?
Oshanas are shallow seasonal channels that carry water through parts of the basin. Along with omirambas, they create temporary wetlands after seasonal rains.
Does the Cuvelai-Etosha Basin have a permanent river network?
No. Seasonal water moves through shallow channels such as oshanas and omirambas instead of a permanent river system.
Why does the Cuvelai-Etosha Basin flood seasonally?
Rainfall creates temporary flows through the basin's shallow channels and low-lying areas. These flows form seasonal wetlands across southern Angola and northern Namibia.
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