The Eye Of The Sahara Looks Like It Can't Possibly Be Natural

The Eye Of The Sahara Looks Like It Can't Possibly Be Natural


July 7, 2025 | Ella Mason

The Eye Of The Sahara Looks Like It Can't Possibly Be Natural


The Sahara's Giant Bullseye Isn't What You Think It Is

At first glance, the Richat Structure looks like the remnants of a lost civilization or a massive impact crater, but it’s entirely natural. Located in the western Sahara Desert of Mauritania, this 40-kilometer-wide geological marvel is often called the “Eye of the Sahara”

The Richat Structure Isn’t A Crater

Originally thought to be the result of a meteorite impact, closer studies in the 1960s ruled that theory out. No shock minerals or deformation consistent with an impact have ever been found. Instead, its dome shape and layered rings are the result of natural erosion over a massive subsurface volcanic intrusion.

File:ISS-42 Richat Structure.jpgNASA, Wikimedia Commons

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It’s Over 100 Million Years Old

The rocks that make up the Richat Structure are ancient, dating from the Late Proterozoic to the Ordovician. The igneous activity beneath it occurred around 94–104 million years ago, during the Cretaceous period. Over millions of years, erosion exposed these layers in a perfect bullseye.

File:ISS-42 Richat Structure, Eye of the Sahara.jpgNASA, Wikimedia Commons

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Volcanic Forces Shaped The Dome

At the core of the Richat Structure is a large body of alkaline igneous rock. Magma from deep within the Earth pushed up and fractured the overlying layers. As the dome lifted and the rock cracked, concentric ring dikes formed and hardened underground.

File:RichatStructure.jpgClemens Schmillen, Wikimedia Commons

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The Rings Are Layers Of Rock Exposed By Erosion

The eye’s layered look is due to alternating hard and soft sedimentary rocks that eroded at different rates. The most erosion-resistant rocks, like quartzite, now stand as ridges forming the striking circular cuestas. 

File:Eye of Africap.jpgDHQ, Wikimedia Commons

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Some Rocks Were Altered By Hydrothermal Fluids

Hot fluids flowed through the dome during and after the volcanic activity, altering many of the rocks. The result is a massive central megabreccia, which is a chaotic mixture of silicified rock fragments. This core alone is 40 meters thick in some places.

File:Mauritania, panorámicas (1997) 03.jpgLBM1948, Wikimedia Commons

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Its Interior Includes Rare Igneous Features

Inside the structure, you’ll find unusual igneous rocks like rhyolites, gabbros, carbonatites, and kimberlites. These formations include lava flows, ring dikes, sills, and even a volcanic plug. The presence of these features helped scientists confirm a deep volcanic origin.

File:Carbonatite.jpgEurico Zimbres Zimbres, Wikimedia Commons

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It Contains Ancient Human Artifacts

Archaeologists have discovered thousands of Acheulean-era stone tools within the Richat Structure. These artifacts are mostly found in the outer ring, near dry riverbeds. Some of them date back hundreds of thousands of years.

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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There Are Burial Mounds And Rock Art

Thousands of stone burial mounds dot the ridges and slopes of the structure. Some nearby rock art depicts warriors, chariots, and animals like elephants and bovids. These suggest the region once supported human life and rich biodiversity during the African Humid Period.

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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The Richat Structure Is A Geological Heritage Site

In 2022, the International Union of Geological Sciences recognized the Richat Structure as one of the world’s 100 most important geological heritage sites. It’s considered a textbook example of a magmatic concentric alkaline complex.

File:Richat Structure ISS030-E-12516.jpgNASA, Wikimedia Commons

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The Sahara Was Once Lush

Between 15,000 and 8,000 years ago, during the African Humid Period, this area was far from a barren wasteland. Seasonal rivers and lakes formed here, leaving behind freshwater fossils in clay and sand deposits. These sediments lie directly over deeply eroded bedrock.

File:Guelb er Richat (Eye Of The Sahara) (14980036258).jpgAmmar Hassan, Wikimedia Commons

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The Structure Has A Local Name

Locals in Mauritania call it Guelb er Richât, or “Tagense,” a word that refers to a circular leather pouch opening used for drawing water. Its rings, seen from above, do resemble the folds of such a pouch.

File:Tea in the Eye of the Sahara (14756513296).jpgMichał Huniewicz, Wikimedia Commons

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The Eye’s Size Is Mind-Blowing

At 40 kilometers in diameter, the Eye of the Sahara could fit the entire city of Paris within it. Its symmetry and scale are best appreciated from space, where it was famously photographed by astronauts aboard the International Space Station.

File:Richat landsat7 big.jpgUSGS/EROS/NASA Landsat, Wikimedia Commons

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It Was Misidentified As Atlantis

Some fringe theorists believe the Eye is the remains of Plato’s Atlantis, citing its circular shape and isolated desert location. However, the structure predates Plato by millions of years, and its geological origin doesn’t match Atlantis’s description.

File:Atlantis Kircher Mundus subterraneus 1678.jpgAthanasius Kircher, Wikimedia Commons

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The “Breathing Earth” Hypothesis Is False

A viral online theory claimed the Richat Structure “breathes” due to seismic activity. This was proven false as any visible pulsation is a time-lapse effect from satellite image processing, not geological movement.

File:Structure de Richat vue par Sentinel 2.jpgEuropean Space Agency / CNES, Wikimedia Commons

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Early Geologists Thought It Was An Impact Site

In the 1940s and 50s, scientists debated whether the structure was caused by an asteroid. Later fieldwork, however, debunked this, finding no signs of impact shock or melted rock. Instead, the evidence pointed to slow, internal geological forces.

File:Museo de la Naturaleza y el Hombre 2019 063.jpgPhotograph by Mike Peel (www.mikepeel.net)., Wikimedia Commons

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Its Rock Layers Dip Outward

The rock strata in the Richat dome tilt outward at angles of 10–20 degrees. This outward dip is another clue supporting the theory of uplift from below, not a collapse from above, as in impact craters.

File:GUELB RICHAT Ombilic (central zone).jpgMichel Jebrak, Wikimedia Commons

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Satellite Mapping Revealed More Hidden Details

Advanced satellite imaging and geophysical surveys helped map the full complexity of the structure. This includes its buried ring dikes and the shape of the magma body that created it. 

File:ISS041-E-81200 - View of Western Sahara.jpgEarth Science and Remote Sensing Unit, Lyndon B. Johnson Space Center, Wikimedia Commons

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The Inner Dome Is Made Of Silica-Rich Breccia

At the center of the structure lies a thick breccia composed of shattered silica-rich rocks. These were cemented together by fluids rich in quartz. The hydrothermal activity that formed this breccia occurred nearly 100 million years ago.

File:Volcanic breccia.jpgJames St. John, Wikimedia Commons

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Carbonatite Dikes Are Found Throughout

Over 30 carbonatite dikes run through the Richat Structure. These dikes are hundreds of meters long and only a few meters wide. They contain unique mineral compositions and solidified without vesicles.

File:Carbonatite breccia (Fen Complex, Ediacaran-Early Cambrian, 523-601 Ma; near Ulefoss, Norway) 2.jpgJames St. John, Wikimedia Commons

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Kimberlite Points To Ancient Volcanic Explosions

In the northern portion of the structure lies a kimberlite plug, which suggests violent volcanic eruptions once occurred here. Kimberlite is also the rock type that often contains diamonds, although no diamonds have been reported at Richat.

File:Kimberlite picture.jpgWoudloper, Wikimedia Commons

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It’s A Magnet For Fringe Theories

In addition to Atlantis, the Eye of the Sahara has been linked to UFOs, ancient megastructures, and even time travel portals by pseudoscientific circles. None of these ideas are supported by geologists or archaeologists.

File:Richat Structure - SRTM.jpgNASA/JPL/NIMA, Wikimedia Commons

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Few Artifacts Are Found In The Center

Although outer areas contain many Acheulean and Aterian tools, the innermost part of the structure is mostly devoid of artifacts. Researchers believe this is due to both environmental conditions and ancient people avoiding the central dome.

File:Acheuleanhandaxes.jpgMatijap, Wikimedia Commons

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Rivers Once Flowed Through Its Rings

Seasonal rivers, or wadis, flowed through the outer rings during wetter periods in prehistory. These rivers left behind gravel beds, fossils, and traces of human life. Today, only the channels remain as dry scars in the landscape.

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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Some Structures May Be Ancient Animal Pens

Satellite imagery has revealed enclosed circular structures on the outskirts of the Richat formation. Archaeologists believe these may have been Neolithic animal enclosures built between 8,000 and 5,000 years ago.

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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Stone Tools Span Tens Of Thousands Of Years

Tools from both the Acheulean and Aterian periods have been recovered here. These tools, made from local quartzite, span a timeline of over 100,000 years. Their presence marks the Richat area as a long-standing human habitation zone.

File:Quartzite 1.jpgJames St. John, Wikimedia Commons

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Freshwater Fossils Are Preserved In The Sediment

Lakebed deposits in the outermost ring contain fossils from the time when the Sahara had lakes and grasslands. These include mollusks and other aquatic organisms. Such fossils help scientists date the humid periods in the region.

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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It's A Case Study In Geological Time

The Richat Structure tells a story that spans hundreds of millions of years. From deep magma intrusions to erosion, uplift, and climate shifts, it's a natural record of planetary change. And it’s still teaching scientists today.

The Richat Structure of Mauritania circular feature under clouds, collage. Elements of this image furnished by NASA. - stock photoElen11, Getty Images

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The Eye Is Visible From Space

Astronauts aboard the International Space Station have repeatedly photographed the Richat Structure. Its massive size and perfect concentric shape make it one of the most easily recognizable natural formations on Earth.

Earth Observations, NASA Mission STS-29Space Frontiers, Getty Images

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Early Explorers Thought It Was Man-Made

When early European geologists came across the Richat Structure, its symmetry made them suspect human involvement. The surrounding desert lacked context to explain such an orderly formation. 

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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Its Outer Rings Are Quartzite

Quartzite, a highly resistant rock, forms much of the outer ring system. These harder layers stood up better to erosion, leaving behind raised ridges. Softer rocks between them wore down, carving out the eye-like grooves.

File:Quartzite Sollières.jpgGabriel Haute Maurienne, Wikimedia Commons

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Scientists Call It A “Dome”

Geologists describe the Richat Structure as a "slightly elliptical dome" based on how it bulges upward. Its raised center and surrounding dips resemble a flattened bubble. This doming is caused by the pressure of magma rising from below.

File:모리타니 사하라의눈 (1435).jpegKorea Aerospace Research Institute, Wikimedia Commons

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Some Dikes Stretch Hundreds Of Meters

Within the Richat Structure are carbonatite dikes that can stretch up to 300 meters in length. These intrusions formed as magma pushed through cracks in the rock. They cooled into narrow, hard bands of unique mineral-rich stone.

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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It Hosts One Of The Largest Megabreccia On Earth

The central zone of the structure features an enormous megabreccia. This breccia is thought to have formed from the collapse of rock layers dissolved by hydrothermal fluids. It’s more than 40 meters thick in the center.

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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The Structure Was Mapped Using Gravimetric Tools

To understand what lay beneath the surface, scientists used aeromagnetic and gravimetric mapping. These tools measure tiny changes in Earth's gravity and magnetic field. The results revealed the shape of the giant magma body below the Richat dome.

File:Autograv CG5 P1150838.JPGUser:Sandeep vats, Wikimedia Commons

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The Rings Are Almost Perfectly Concentric

Despite being created by natural forces, the Richat Structure’s rings maintain an astonishingly regular spacing. Each ring marks a different geological layer exposed by erosion. 

File:Richat Ouadane, Mauritânia? Atlântida?.gifAnonymmous-21, Wikimedia Commons

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The Center Contains Rare Silicified Rocks

In the middle of the structure, rocks have been altered by silica-rich fluids, making them incredibly hard. These rocks, including chert and sandstone, show how mineral-laden water changed their composition over time. 

File:ISS001-E-5524 - View of Mauritania.jpgEarth Science and Remote Sensing Unit, Lyndon B. Johnson Space Center, Wikimedia Commons

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The Sahara Was Once A Different World

When the Richat Structure formed, the Sahara was not a desert. During the African Humid Period, it was filled with lakes, rivers, and savannas. 

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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Rock Art Tells Stories Of Lost Cultures

Several locations near the Richat Structure contain ancient rock art. These include images of horse riders, wild animals, and even chariots

Mauritania, surroundings of Guelb El Richat or Guelb Er Richat, nomad campUCG, Getty Images

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Scientists Are Still Studying It

Despite decades of research, the Richat Structure continues to attract new studies. Each year brings new insights into its geology, archaeology, and significance. 

Theodore Monod's Expedition to the patrick chapuis, Getty Images

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