African River Reaches Atlantic for First Time in Decades
Get the world’s most fascinating discoveries delivered straight to your inbox.
You are now subscribed
Your newsletter sign-up was successful
Want to add more newsletters?
Delivered Daily
Daily Newsletter
Sign up for the latest discoveries, groundbreaking research and fascinating breakthroughs that impact you and the wider world direct to your inbox.
Once a week
Life's Little Mysteries
Feed your curiosity with an exclusive mystery every week, solved with science and delivered direct to your inbox before it's seen anywhere else.
Once a week
How It Works
Sign up to our free science & technology newsletter for your weekly fix of fascinating articles, quick quizzes, amazing images, and more
Delivered daily
Space.com Newsletter
Breaking space news, the latest updates on rocket launches, skywatching events and more!
Once a month
Watch This Space
Sign up to our monthly entertainment newsletter to keep up with all our coverage of the latest sci-fi and space movies, tv shows, games and books.
Once a week
Night Sky This Week
Discover this week's must-see night sky events, moon phases, and stunning astrophotos. Sign up for our skywatching newsletter and explore the universe with us!
Join the club
Get full access to premium articles, exclusive features and a growing list of member rewards.
The Namib Desert stretches along the west coast of Africa, from the Kunene (or Cunene) River in the north to the Orange River in the south. About midway between, a third river, the Kuiseb, stretches toward the Atlantic Ocean.
But the Kuiseb doesn't always make it to this goal. The river is an impermanent one and years have gone by without the river flowing into the ocean.
In 2011, sufficient rainfall propelled the Kuiseb toward the Atlantic Coast for the first time in decades, as is seen in this image taken by NASA's Earth Observing-1 satellite on Feb. 27.
Around Walvis Bay, where the Kuiseb has traditionally drained into the sea, salt works appear as rectangular shapes of orange and brown. Nearby shallow water appears green.
South of the salt works, nature takes over. Irregularly shaped dark patches indicate standing water on the desert surface where water has apparently pooled at the end of the Kuiseb River. In the east, the river's braided channels resemble dark, tangled threads.
The Kuiseb marks a major landscape change in the desert. Bare rocks prevail north of the river, while marching sand dunes predominate to the south. But the ephemeral water body makes only an imperfect boundary.
This image shows numerous sand dunes that have migrated past the Kuiseb and now border on Walvis Bay. By washing out accumulated sand, flash floods on the river generally prevent dunes from migrating past it when flash floods occur.
Get the world’s most fascinating discoveries delivered straight to your inbox.
The cold Benguela Current flowing along the Atlantic Coast prevents much precipitation from moving inland, leaving the Namib Desert parched. Persistently dry conditions allow dunes to continue northward when there is no flowing water in their way.
Human activity also has affected the river's path, according to a NASA statement. A flood in 1963 caused major damage to Walvis Bay, and the subsequent construction of an embankment has blocked the Kuiseb River channel and caused the river to lose direction. Later floods pushed the river into an area of impermanent wetlands, but conditions were too dry to enable the Kuiseb to reach all the way to the Atlantic Ocean until 2011. The pool of water nearest the coast snakes northward to the bay, almost touching the salt works.

