Atacama Desertdriest place on EarthChile geographyMars analograin shadow

Atacama Desert: The World's Driest Non-Polar Landscape

Atacama Desert: The World's Driest Non-Polar Landscape Stretching along the Pacific coast of South America, the Atacama Desert is a vast plateau in northern Chile that holds the title of ...

Atacama Desert: The World's Driest Non-Polar Landscape

Stretching along the Pacific coast of South America, the Atacama Desert is a vast plateau in northern Chile that holds the title of the driest non-polar desert on Earth. Spanning a 1,600-kilometre (1,000-mile) strip of land west of the Andes, this extraordinary region is characterized by extreme aridity and otherworldly landscapes that mirror the surface of Mars.

Covering approximately 105,000 square kilometres—and up to 128,000 square kilometres if the lower slopes of the Andes are included—the Atacama is more than just a barren wasteland. It is a unique intersection of geological forces, astronomical clarity, and resilient biological life.

A flat area of the Atacama Desert between Antofagasta and Taltal
A flat area of the Atacama Desert between Antofagasta and Taltal

Key Facts

  • Location: Northern Chile, between the Andes and the Chilean Coast Range.
  • Climate: The driest non-polar desert globally, with average annual rainfall of about 15 mm (0.6 in).
  • Mars Analog: Used by NASA to test instruments due to soil similarities with the Red Planet.
  • Astronomy: Home to some of the world's most advanced observatories, including ALMA.
  • Unique Weather: Experiences the camanchaca, a dense marine fog that supports specialized life.

Geography and the Science of Aridity

The Atacama's extreme dryness is the result of a phenomenon known as a two-sided rain shadow. The desert is sandwiched between two high mountain chains: the Andes to the east and the Chilean Coast Range to the west. These barriers effectively block moisture from both the Atlantic and Pacific oceans.

This effect is further intensified by the South Pacific anticyclone and the cool, north-flowing Humboldt Current. The result is a landscape where some weather stations have never recorded a single drop of rain. Evidence suggests that the region may have seen no significant rainfall between 1570 and 1971, with hyper-arid conditions persisting since the Miocene epoch.

The lack of humidity, rain, and light pollution together produce a dusty, rocky landscape.[36]
The lack of humidity, rain, and light pollution together produce a dusty, rocky landscape.[36]

The Role of the Camanchaca

Despite the lack of rain, the desert is not entirely devoid of moisture. A thick marine fog called the camanchaca rolls in from the coast. This fog provides the critical hydration necessary for hypolithic algae (organisms living under rocks), lichens, and specialized cacti, such as those in the Copiapoa genus.

Vegetation in Pan de Azúcar National Park on the coast of the Atacama Desert
Vegetation in Pan de Azúcar National Park on the coast of the Atacama Desert

A Terrestrial Mirror to Mars

Because of its extreme dryness and mineral composition, specific regions of the Atacama—particularly around Yungay and María Elena South—are considered Mars analogs. The soil in these areas is so similar to Martian soil that NASA uses the desert to test instruments for future Mars missions.

In 2003, researchers attempted to duplicate the life-detection tests used by the Viking 1 and 2 Mars landers in the Yungay region and found no signs of life, highlighting the region's status as one of the most sterile environments on Earth.

ALMA and the center of the Milky Way[71]
ALMA and the center of the Milky Way[71]

Flora, Fauna, and Rare Phenomena

Life in the Atacama is sparse but highly adapted. While much of the landscape is rocky and dusty, rare rainfall events can trigger the flowering desert phenomenon, where the southern Atacama suddenly erupts in a carpet of blooms.

The fauna is equally specialized, ranging from Andean flamingos in the Salar de Atacama to the Liolaemus nitidus lizard in the southern reaches. Even feral donkeys have found a way to survive in this harsh environment.

Rare rainfall events cause the flowering desert phenomenon in the southern Atacama Desert.
Rare rainfall events cause the flowering desert phenomenon in the southern Atacama Desert.

Andean flamingos in Salar de Atacama
Andean flamingos in Salar de Atacama

Liolaemus nitidus, a lizard native to the southern reaches of the Atacama Desert
Liolaemus nitidus, a lizard native to the southern reaches of the Atacama Desert

Feral donkey in the Atacama desert
Feral donkey in the Atacama desert

Human History and Modern Use

Long before modern borders, the interior of the desert was inhabited by the Atacameño people, who built fortified towns known as pucarás. Later, the region saw the influence of the Inca Empire and the Spanish, who established towns like San Pedro de Atacama.

In more recent history, the desert became a hub for nitrate mining, leaving behind a trail of abandoned mining towns. Today, the region is a center for global industry and science, featuring massive copper mines like Chuquicamata and world-class astronomical facilities.

View of Caspana, a village and Likan Antai settlement in the interior Atacama Desert
View of Caspana, a village and Likan Antai settlement in the interior Atacama Desert

View of Chuquicamata, a large, state-owned copper mine
View of Chuquicamata, a large, state-owned copper mine

View of a forest in Pampa del Tamarugal from Chile Route 5. These forests were once devastated by the demand of firewood associated with saltpeter mining.
View of a forest in Pampa del Tamarugal from Chile Route 5. These forests were once devastated by the demand of firewood associated with saltpeter mining.

A Window to the Universe

The combination of high altitude, low humidity, and minimal light pollution makes the Atacama the premier location for astronomy. The European Southern Observatory (ESO) operates several major sites here:

  • La Silla Observatory
  • Paranal Observatory (home to the Very Large Telescope)
  • Llano de Chajnantor Observatory (hosting the ALMA radio observatory)
  • Cerro Armazones Observatory (site of the future Extremely Large Telescope)

Snow in Paranal Observatory at 2,600 masl[19]
Snow in Paranal Observatory at 2,600 masl[19]

Sports and Adventure

The desert's vast dunes and rugged terrain attract all-terrain sports enthusiasts. It has hosted the Patagonia-Atacama Rally and various editions of the Dakar Rally. Additionally, the region is a popular destination for sandboarding and solar-powered car racing.

Patagonia-Atacama Rally in 2007
Patagonia-Atacama Rally in 2007

Atacama Desert Summary

Overview of the Atacama Desert Region
Feature Details
Total Area 105,000 km² to 128,000 km²
Average Rainfall ~15 mm (0.6 in) per year
Primary Country Chile
Key Ecosystems Deserts and xeric shrublands
Notable Flora Copiapoa cacti, hypolithic algae
Major Industry Copper mining, Astronomy, Tourism

Frequently Asked Questions

Why is the Atacama Desert so dry?

The dryness is caused by a two-sided rain shadow. The Andes Mountains block moisture from the Atlantic, while the Chilean Coast Range blocks moisture from the Pacific. This is reinforced by the cool Humboldt Current and the South Pacific anticyclone.

How does life survive in the Atacama?

Many species rely on the camanchaca, a dense marine fog that provides essential moisture. Some plants, like the Copiapoa cacti, and various lichens and algae have adapted to survive on this fog alone.

Why is the Atacama compared to Mars?

Certain areas, such as Yungay, have soil chemistry and extreme aridity that closely mimic the conditions on Mars. This makes it an ideal location for NASA to test planetary landers and life-detection instruments.

What is the "flowering desert"?

The flowering desert is a rare phenomenon in the southern Atacama where unusual rainfall events trigger the mass germination of seeds, turning the arid landscape into a field of flowers.

Which astronomical observatories are located there?

The region hosts several major facilities, including the ALMA radio observatory at Llano de Chajnantor, the Very Large Telescope at Paranal, and the upcoming Extremely Large Telescope at Cerro Armazones.