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Djanet Sahara Dunes

Natural wonder Africa

Sahara

The Sahara is a huge, hot desert in Africa. It has sand dunes, rocky plains and tall mountains. Very little rain falls there.

The Sahara fills almost all of northern Africa. Britannica calls it the largest hot desert in the world: about 4,800 kilometers from east to west and about 8.6 million square kilometers in all. Only about a quarter of it is sand dunes; the rest is gravel plains, rocky plateaus and mountains.

The Sahara, from the Arabic word for desert, spans northern Africa from the Atlantic to the Red Sea, about 8.6 million km². It has been arid for at least 2 to 3 million years, perhaps since the Miocene, yet rock art and old lake shores record wetter times. Sand covers only about 25 percent of its surface.

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Photo: Fayeqalnatour, CC BY-SA 4.0, via Wikimedia Commons

Discover the Sahara

The Sahara is a very big desert in Africa.

It is hot and dry. In some places there are hills of sand called dunes. In other places there are rocks, gravel and tall mountains.

The Sahara stretches across almost all of northern Africa, from the Atlantic Ocean in the west to the Red Sea in the east. To the north are the Atlas Mountains and the Mediterranean Sea, and to the south is the Sahel, a strip of semiarid land between the desert and the savannas. The name Sahara comes from the Arabic word for desert.

Britannica calls it the largest hot desert in the world. It is about 4,800 kilometers wide and covers about 8.6 million square kilometers, although its size changes as the desert grows and shrinks over time. Its highest point is Mount Koussi in Chad, 3,415 meters high, and its lowest is Egypt's Qattara Depression, 133 meters below sea level.

Britannica describes the Sahara as the largest hot desert in the world, about 4,800 km (3,000 miles) from east to west and 800 to 1,200 miles from north to south, with an area of some 8,600,000 km² that varies as the desert expands and contracts. It is bordered by the Atlantic, the Atlas Mountains and Mediterranean, the Red Sea and the semiarid Sahel. The name derives from Arabic ṣaḥrāʾ, desert; in Arabic it is Al-Ṣaḥrāʾ al-Kubrā, the Great Desert. Britannica names parts of Morocco, Algeria, Tunisia, Libya, Egypt, Mauritania, Mali, Niger, Chad and Sudan, and describes the territory of Western Sahara, whose political status it calls unresolved, as part of the Sahara.

Its landscapes include seasonally flooded basins (chotts and dayas), large oasis depressions, gravel-covered plains (serirs or regs), rock-strewn plateaus (hammadas), abrupt mountains, and sand sheets, dunes and sand seas (ergs). The highest point is the 3,415 m summit of Mount Koussi in Chad's Tibesti Mountains, and the lowest, 133 m below sea level, lies in Egypt's Qattara Depression.

East to west
about 4,800 km
Area
about 8,600,000 km² (it changes over time)
Highest point
Mount Koussi, 3,415 m (Chad)
Lowest point
Qattara Depression, 133 m below sea level (Egypt)
Djanet Sahara Dunes
Photo: Fayeqalnatour, CC BY-SA 4.0, via Wikimedia Commons

How the Sahara became a desert

The Sahara was not always a desert.

Long ago, there were lakes, and people fished in them. Then the land slowly dried out. Wind blew the sand into big dunes.

Scientists do not all agree on when the Sahara became a desert. Several studies of its rocks point to about 2 to 3 million years ago, but sand dunes about 7 million years old, found in Chad in 2006, suggest it may have been even earlier. Since then, the climate has swung back and forth between drier and wetter times.

During wetter times, there were lakes where people lived, hunted and fished. Ancient paintings and carvings on the Tassili n'Ajjer plateau of Algeria show animals such as hippopotamuses that need water, and the climate changing. Today, high air pressure over the northern Sahara gives it its dry climate. Only about a quarter of the Sahara is covered by sand; wind has piled it into dunes, some nearly 150 meters tall.

Britannica notes that the Sahara's age is disputed: several studies indicate it became established as a climatic desert about 2 to 3 million years ago, in the late Pliocene to early Pleistocene, while 7-million-year-old dune deposits found in northern Chad in 2006 suggest aridity in the Miocene. Since the Pliocene it has oscillated between drier and more humid conditions. Stable high-pressure cells centered over the Tropic of Cancer cause the dry subtropical climate of the north.

Beneath it lies the African Shield, folded and worn-down Precambrian rock, overlain by flat Paleozoic and Mesozoic layers, including the Nubian sandstones, which hold important aquifers. Volcanic massifs such as the Tibesti and Ahaggar rise in the center. Sand sheets and dunes cover about 25 percent of the surface; pyramidal dunes reach nearly 500 feet and draa ridges are said to reach 1,000 feet. UNESCO's Tassili n'Ajjer rock art, over 15,000 drawings and engravings, records climate change and the loss of water-dependent animals such as the hippopotamus.

Hot days, cold nights

Days in the Sahara can be very hot.

Nights can be cold. Rain hardly ever falls. When a big storm comes, water can rush along dry riverbeds.

Very little rain falls in the Sahara. In the north, about 76 millimeters (3 inches) of rain falls in an average year, and most of that falls in winter. In the south, a little more rain comes in summer, often in thunderstorms.

Temperatures change a lot between day and night. In summer, days can reach about 40 °C and nights drop to about 25 °C, and in the south a high of 50 °C is not unusual. In winter the nights can be cold, and snow sometimes falls on the high plateaus and mountains. Thunderstorms can cause sudden floods, and hot, dusty winds blow sand across the land.

Britannica distinguishes a dry subtropical north, with cold to cool winters, hot summers and two rainfall maxima, from a dry tropical south with mild dry winters and variable summer rains. Average daily swings run from about 20 °C to 5 °C between December and February and from 40 °C to 25 °C between June and August; in the south, highs of 50 °C in late spring and early summer are not unusual. The cold Canary Current keeps a narrow western coastal strip cool and foggy.

Precipitation averages about 76 mm (3 inches) a year in the north and about five inches in the south, highly variable, with occasional snow on northern plateaus and central massifs. Summer thunderstorms can cause flash floods in areas where no rain has fallen. Hot southerly winds carrying dust from the interior are known as the khamsin in Egypt, the ghibli in Libya and the chili in Tunisia; Sudan's shorter, dust-laden haboob winds come mainly in summer and often bring heavy rain. In the southern Sahara winter brings the harmattan, a dry northeasterly wind laden with dust.

Life in the desert

Some plants and animals live in the Sahara.

The fennec fox has giant ears. Camels can walk far across the sand. After rain, little plants grow and flower very fast.

Life is sparse in the Sahara, but it is there. Grasses, shrubs and trees grow in the mountains, in oases and along wadis, dry riverbeds that sometimes flow after rain. Some small plants can sprout within three days of a good rain and make seeds within 10 to 15 days, living almost their whole life in the two or three weeks after a heavy rain.

The fennec fox lives throughout the Sahara. It is the smallest member of the dog family, with the biggest ears for its size, which help it lose heat and hear prey under the sand. Its furry paws grip the sand and protect it from the heat. People have long herded camels, goats and sheep across the desert, and in oases they grow date palms and barley.

Britannica describes Saharan vegetation as generally sparse, concentrated in the highlands, oasis depressions and wadis, with salt-tolerant halophytes in saline basins. Many herbaceous plants are ephemerals that may germinate within three days of adequate rainfall and set seed within 10 to 15 days; relict olive, cypress and mastic trees survive in the massifs, alongside acacias, doum and date palms, oleander and grasses such as Aristida and Panicum. Animals such as the desert snail survive by estivation, a dormancy during extreme stress.

The Smithsonian's National Zoo notes that fennec foxes live throughout the Sahara and east to Sinai and Arabia; they have the largest ears relative to body size of any canid, used to shed heat and locate prey under the sand, heavily furred paws, and can go long periods without drinking. People have lived in the Sahara since before recorded history, as nomadic pastoralists herding goats, sheep or camels, oasis farmers growing date palms and barley, and traders on caravan routes.

Photo of Fennec fox
Photo: Anass ERRIHANI, CC BY-SA 4.0, via Wikimedia Commons

Visiting safely

The desert can be very hot, and storms can bring sudden floods.

In one big desert park, visitors always go with a guide. Old rock paintings there are looked after with care. Look at them, but do not touch!

The Sahara can be dangerous for people who are not prepared: very hot days, sudden floods after storms, and winds full of dust. For centuries, people crossed it on caravan routes from oasis to oasis.

In Tassili n'Ajjer, a cultural park and World Heritage Site in Algeria, tourism is strictly controlled, and groups of visitors are always accompanied by an official guide. UNESCO warns that the ancient rock art there can be damaged by the weather and by visitors. So look at the paintings, but never touch them.

The Sahara's hazards are real but well understood: highs near 50 °C in the south, flash floods from summer storms, and dust-laden winds such as the harmattan, khamsin and haboob (Britannica).

At Tassili n'Ajjer, a 72,000 km² plateau in southeastern Algeria inscribed in 1982, UNESCO describes the rock art as vulnerable both to climatic deterioration and to damage caused by visitors. Tourism, which brings income and jobs to local people, is strictly controlled, and groups of visitors are always accompanied by an official guide. On the desert's southern edge, the Great Green Wall initiative, conceived in 2005 and developed with the African Union, plans a 15 km wide belt of drought-resistant native trees across the continent to slow desertification.

Sahara camel calf feeding from her mother
Photo: Garrondo, CC BY-SA 3.0, via Wikimedia Commons

Amazing facts

  • Most of the Sahara is not sand.

    Sand sheets and dunes cover only about a quarter of the Sahara; most of it is gravel plains, rocky plateaus and mountains.

    Britannica estimates sand sheets and dunes at about 25 percent of the Sahara's surface.

  • Some dunes in the Sahara make a booming sound.

    Some desert sands sing or boom, and scientists have not solved exactly why.

    Britannica notes that the singing or booming of desert sands has prompted several hypotheses, such as quartz's piezoelectric property, but remains unsolved.

  • Old rock paintings show hippos in the Sahara!

    Rock art in Tassili n'Ajjer, Algeria, shows hippopotamuses, animals that need lots of water.

    UNESCO notes that Tassili n'Ajjer's rock art depicts water-dependent species like the hippopotamus and species long extinct in the region.

  • Fennec foxes can go a long time without drinking.

    Fennec foxes can go for long periods without drinking water, getting some water from roots, fruits and leaves.

    The National Zoo notes fennec foxes can go long periods without water, eating roots, fruits and leaves that help them hydrate.

Words to know

desert
a place that gets very little rain
dune
a hill of sand piled up by the wind
oasis
a green place in a desert where there is water
wadi
a dry riverbed that fills with water only after rain
Sahel
the strip of dry land between the Sahara and the savannas to the south
desertification
land slowly turning into desert

Discovery challenge

  1. On which continent is the Sahara?

    The Sahara fills most of the north of which continent?

    The Sahara spans which continent, from the Atlantic to the Red Sea?

    • Africa
    • Asia
    • South America
    Show the answer

    Africa

    The Sahara is in Africa.

    It fills almost all of northern Africa.

    It spans northern Africa, from the Atlantic to the Red Sea and from the Mediterranean to the Sahel.

  2. Is most of the Sahara made of sand?

    How much of the Sahara is covered by sand dunes and sand sheets?

    What share of the Sahara's surface does Britannica estimate is sand?

    • All of it
    • About a quarter
    • None of it
    Show the answer

    About a quarter

    No! Only about a quarter is sand. The rest is rock and gravel.

    Only about a quarter is sand; the rest is gravel plains, rocky plateaus and mountains.

    About 25 percent; regs, hammadas, massifs and basins make up the rest.

  3. Which fox with giant ears lives in the Sahara?

    Which small fox uses its huge ears to stay cool in the Sahara?

    Which canid has the largest ears relative to body size and lives throughout the Sahara?

    • Arctic fox
    • Red fox
    • Fennec fox
    Show the answer

    Fennec fox

    The fennec fox has giant ears.

    The fennec fox's ears let heat escape and help it hear prey under the sand.

    The fennec fox, the smallest canid, uses its ears to dispel heat and locate prey.

  4. What did people paint on rocks long ago in the Sahara?

    What does ancient rock art in the Sahara show about the past?

    What does Tassili n'Ajjer's rock art record, according to UNESCO?

    • Snowmen and sleds
    • Animals like hippos, from wetter times
    • Cars and roads
    Show the answer

    Animals like hippos, from wetter times

    They painted animals like hippos.

    The art shows animals that need water, like hippos, from times when the Sahara was wetter.

    Climate change, wildlife migrations and the evolution of human life, including water-dependent species.

  5. In one big Sahara park, who do visitors go with?

    How do visitor groups travel in Tassili n'Ajjer?

    How does UNESCO describe tourism management at Tassili n'Ajjer?

    • They go alone without telling anyone
    • They go with an official guide
    • They take pieces of rock art home
    Show the answer

    They go with an official guide

    They go with an official guide.

    Groups of visitors are always accompanied by an official guide.

    Tourism is strictly controlled, and visitor groups are always accompanied by an official guide.

Nearby places

Experiments to try

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For parents & teachers

What children will learn

  • Locate the Sahara across northern Africa and describe its size and landscapes.
  • Explain what makes the Sahara dry and how it once had wetter periods.
  • Describe how plants, animals and people live in the desert.
  • Discuss why guides and protection matter for visitors and rock art.

Recommended ages: 3 to 17 · About 15 minutes

Talk about it

  • Why do you think most of the Sahara is rock and gravel, not sand?
  • How could a painting of a hippo tell us about a desert's past?
  • What would you need to pack to visit a hot desert safely, and why?

Try at home or in class

  • Use a hair dryer on low over a tray of dry sand (with a grown-up) and watch ripples and small dunes form.
  • Put a damp paper towel and a dry seed in a sealed bag on a sunny windowsill and record how many days the seed takes to sprout.

Key vocabulary: desert, dune, oasis, wadi, Sahel, desertification

Where these facts come from

  1. Wikidata , Wikimedia Foundation (CC0 1.0)
  2. Natural Earth vector data , Natural Earth (NACIS) (Public domain)
  3. Sahara , Encyclopaedia Britannica
  4. Sahara summary , Encyclopaedia Britannica
  5. Western Sahara , Encyclopaedia Britannica
  6. Sahara: Climate , Encyclopaedia Britannica
  7. Sahara: Plant life , Encyclopaedia Britannica
  8. Tassili n'Ajjer , UNESCO World Heritage Centre
  9. Fennec fox , Smithsonian's National Zoo and Conservation Biology Institute
  10. Wikimedia Commons , Wikimedia Foundation (Per file (public domain, CC0, CC BY or CC BY-SA); see each media record)

Checked, not yet human-reviewed. Last updated October 24, 2026. Spotted a mistake? Tell us.

Picture credits
  • Photo: Fayeqalnatour, CC BY-SA 4.0, via Wikimedia Commons · source · license
  • Photo: Anass ERRIHANI, CC BY-SA 4.0, via Wikimedia Commons · source · license
  • Photo: Garrondo, CC BY-SA 3.0, via Wikimedia Commons · source · license