Okavango Delta: From Angola to Kalahari

Each winter, while Botswana bakes under cloudless skies, a vast flood quietly arrives from the north. Fed by distant Angolan rains, the Okavango Delta — a UNESCO World Heritage Site — swells to over 7,000 km² of shimmering channels, lagoons and palm-fringed islands. This seasonal pulse transforms the Kalahari into one of Africa’s richest wildlife habitats, drawing elephants, big cats, and over 400 species of birds to its waters.

Aerial view of the Okavango Delta
Interactive Story

The Pulse of the Okavango

Follow the water's extraordinary 1,200-kilometre journey from the Angolan Highlands to the heart of the Kalahari Desert.

Chapter I

In the Heart of the Kalahari

Deep within southern Africa's vast Kalahari Desert — a sea of sand stretching across a million square kilometres — lies an impossibility. A shimmering jewel of water and life, pulsing with a rhythm that has played out for millennia.

Chapter II

The Source

Every year between October and April, heavy rains drench the Angolan Highlands — a vast plateau of peatlands, source lakes and ancient groundwater reserves rising 1,300 metres above sea level. This is the Okavango's water tower.

The rains collect into countless streams, which merge into two great rivers: the Cuito and the Cubango. Together they carry over 95% of the water that will eventually reach the delta — more than 1,200 kilometres to the south.

Chapter III

Two Rivers, One Destination

The Cuito — slow, steady, fed by deep groundwater — and the Cubango — fast, volatile, driven by surface runoff. Two very different rivers with the same destination.

Their water will take three to four months to complete the journey south, flowing through some of the most remote and pristine wilderness remaining in Africa.

Chapter IV

The Confluence

Near the town of Divundu, where Namibia's Caprivi Strip meets the Angolan border, the Cuito and Cubango finally merge. From this point on, there is only the Okavango — a single river carrying the full force of the Angolan rains south into Botswana.

Chapter V

The Panhandle

The Okavango enters Botswana through a narrow, 100-kilometre channel hemmed between parallel geological faults — the Panhandle. Here the river is still recognisably a river: deep, channelled, flowing purposefully south.

The first pulse of floodwater arrives here in February, swelling the papyrus-lined banks and filling the lagoons that dot the floodplain. The blue areas on the map show open water detected by satellite — watch how they spread as you scroll on.

Chapter VI

The Fan Opens

Then the faults release their grip, and the Okavango does something extraordinary. The land flattens to an almost imperceptible gradient — just 60 metres of elevation change across 250 kilometres — and the river simply dissolves.

It spreads across the Kalahari sand in an immense alluvial fan of channels, lagoons, and islands. By April the transformation is well underway.

From the air, the Okavango reveals its true nature — an endless maze of channels, lagoons, and palm-fringed islands.

Chapter VII

Peak Flood

By July — the middle of Botswana's dry, cool winter — the Okavango Delta reaches its maximum extent. Over 7,200 square kilometres of open water shimmer across what was, just months ago, dry Kalahari scrubland.

This is the great paradox of the Okavango: its flood arrives not in the rainy season, but in the driest months of the year, carried here across a continent by water that fell as rain four months and 1,200 kilometres ago.

Where the water goes, life follows.

Chapter VIII

Life in the Flood

The flood transforms everything. Elephants wade chest-deep between islands. Red lechwe bound through the shallows in sprays of silver. Mokoro — traditional dugout canoes — glide through channels carpeted in water lilies.

This is the Okavango at its most alive: a vast, watery wilderness teeming with hippos, crocodiles, fish eagles, and more than 400 species of birds.

A wilderness explored by mokoro — the way it has been for centuries.

Chapter IX

A River That Never Reaches the Sea

Of all the water that enters the delta, 96% never leaves. It doesn't flow onward to any ocean. Instead, it is drawn slowly back into the sky — evaporated by the fierce Kalahari sun, exhaled by billions of leaves, absorbed into the deep sand.

The Okavango is one of only a handful of rivers on Earth that ends not at a coast, but in a desert. And as the water recedes through October and November, the cycle quietly begins again 1,200 kilometres to the north.

The Cycle Continues

Explore every month of the Okavango's flood cycle with our interactive map — see how the water rises and falls, and discover the best time for your safari.

Explore the Flood Cycle Map Or read: When to visit the Okavango Delta → ↑ Restart the story
Scroll to explore
Flood data: EC JRC/Google (Pekel et al., 2016)