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The Richat Structure contains more than 32 carbonatite dykes which are 1 to 4 meters wide and meters long. According to researchers, the carbonatite rocks in the Richat Structure date back to million years ago.

In the northern part of the Giant Eye, scientists have found kimberlitic plug that is believed to be 99 million years old. Aside from rocks, hydrothermal features are also part of the Giant Eye in the Sahara desert.

When it was first discovered, the Giant Eye of Africa was considered an asteroid impact structure. The reasoning behind the theory is that the high degree of circularity could be a result of an asteroid impact.

However, nowadays, scientists argue that the feature it is symmetrical and deeply eroded geological dome.

A recent study argues that the carbonates in the Richat Structure were created by hydrothermal waters with low temperature.

However, no matter what people believe, every scientist out there is certainly in one thing: the Giant Eye of Africa needs protection and requires a deeper and more analytical research of its origin.

Modern astronauts are fond of the Eye because so much of the Sahara Desert is an unbroken sea of sand. NASA explained:. The Richat Structure in the Sahara Desert of Mauritania is easily visible from space because it is nearly 50 kilometers across.

The possibility that the Richat Structure was formed by a volcanic eruption also seems improbable because of the lack of a dome of igneous or volcanic rock.

Rather, the layered sedimentary rock of the Richat structure is now thought by many to have been caused by uplifted rock sculpted by erosion.

The above image was captured last year by the orbiting Landsat 7 satellite. Why the Richat Structure is nearly circular remains a mystery.

Some people believe that the Eye of the Sahara is actually the remains of the city of Atlantis, which Plato described as concentric rings of water and land.

But if you ask us, the geological history this formation reveals is way more interesting. Join our mailing list to receive the latest news and updates from our team.

October 7, Popular Popular. Now Week Month. Arcturians Aliens — Watchers and Earth Protectors? Ancient Times. Enuma Elish — Creation of the World and of Mankind.

Nikola Tesla. They include the extensive hydrothermal alteration of rhyolites and gabbros and a central megabreccia created by hydrothermal dissolution and collapse.

The breccia consists of fragments of white to dark gray cherty material, quartz -rich sandstone, diagenetic cherty nodules, and stromatolitic limestone and is intensively silicified.

The hydrothermal alteration, which created this breccia, has been dated to have occurred about The Richat Structure is regarded by geologists as a highly symmetrical and deeply eroded geologic dome.

Richard-Molard considered it to be the result of a laccolithic thrust. After extensive field and laboratory studies in the s, no credible evidence has been found for shock metamorphism or any type of deformation indicative of a hypervelocity extraterrestrial impact.

Work on dating the structure was done in the s. The circular distribution of ridges and valleys is explained as the formation of cuestas by the differential erosion of alternating hard and soft rock layers uplifted as a dome by an underlying alkaline igneous complex of Cretaceous age.

A multianalytical study on the Richat megabreccias concluded that carbonates within the silica-rich megabreccias were created by low-temperature hydrothermal waters, and that the structure requires special protection and further investigation of its origin.

The Richat Structure is the location of exceptional accumulations of Acheulean artifacts. Pre-Acheulean stone tools also have been found in the same areas.

These sites are associated with rubbly, chaotic outcrops of quartzite that provided the raw material needed for the manufacture of these artifacts.

The most important Acheulean sites and their associated outcrops are found along the north-west of the outer ring, from which Wadi Akerdil heads east and Wadi Bamouere to the west.

Sparse and widely scattered Neolithic spear points and other artifacts have also been found. However, since these sites were first discovered by Theodore Monod in , [15] mapping of artifacts within the area of the Richat Structure have found them to be generally absent in its innermost depressions.

So far, neither recognizable midden deposits nor manmade structures have been recognized and reported from the Richat Structure.

This is interpreted as indicating that area of the Richat Structure was used for only short-term hunting and stone tool manufacturing.

The local, apparent wealth of surface artifacts is the result of the concentration and mixing by deflation over multiple glacial - interglacial cycles.

Artifacts are found, typically redeposited, deflated, or both, in Late Pleistocene to early Holocene gravelly mud , muddy gravel , clayey sand , and silty sand.

These sediments are often cemented into either concretionary masses or beds by calcrete. Ridges typically consist of deeply weathered bedrock representing truncated Cenozoic paleosols that formed under tropical environments.

The Pleistocene to Middle Holocene sediments occur along wadis as thin, meter- to less than meter-thick accumulations in the interior annular depressions to 3—4 meters 9.

The gravelly deposits consist of mixture of slope scree, debris flow , and fluviatile or even torrential flow deposits.

The finer grained, sandy deposits consist of eolian and playa lake deposits. The latter contain well-preserved, freshwater fossils.

Numerous, concordant radiocarbon dates, indicate that the bulk of these sediments accumulated between 15, and 8, BP during the African humid period.

These deposits lie directly upon deeply eroded and weathered bedrock. From Wikipedia, the free encyclopedia. Richat Structure Inner ring of the Richat Structure.

Circular geological feature in the Sahara desert. Business Insider. Retrieved 3 October Fabre, J.

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