- Also called "Eye Sahara",the Richat Structure is a huge geological structure found in the Sahara in Mauritania, near the town and Adan. The curved. Guelb er Richat (arabisch قلب الريشات, DMG Qalb ar-Rīšāt), deutsch auch Richat-Struktur, umschrieben mit Auge Afrikas, Bull's eye oder Auge der Sahara,. The Richat Structure. A circular feature in the Sahara desert that is ~30 miles wide. Not an impact crater nor a volcano. MeteoritenkraterGeheimnisvolle.
Eye Of Sahara Dateiverwendung
Guelb er Richat (arabisch قلب الريشات, DMG Qalb ar-Rīšāt), deutsch auch Richat-Struktur, umschrieben mit Auge Afrikas, Bull's eye oder Auge der Sahara,. Datei:ISS Richat Structure, Eye of the lyst.nu aus Wikipedia, der freien Enzyklopädie. Zur Navigation springen Zur Suche springen. Datei; Dateiversionen. The Richat Structure in the Sahara desert of Mauritania via Chaudron Will 50 Watts. The Richat Structure, also known as the Eye of the Sahara and Guelb er Richat, is a prominent circular feature in the Sahara desert near Ouadane, west–central. The Richat Structure. A circular feature in the Sahara desert that is ~30 miles wide. Not an impact crater nor a volcano. MeteoritenkraterGeheimnisvolle. - The Eye of the Sahara This spectacular landform, also called The Richat Structure, in the Sahara desert is so huge with a diameter of 30 miles that. Guelb er Richat (Eye of Africa) in der Sahara. Das Satellitenbild des Monats Juni zeigt ein Echtfarbenbild des „Guelb er Richat“ oder auch „Eye.
- The Eye of the Sahara This spectacular landform, also called The Richat Structure, in the Sahara desert is so huge with a diameter of 30 miles that. Eye of Sahara: Stockfotos und Bilder bei imago images lizenzieren, sofort downloaden und nutzen. Datei:ISS Richat Structure, Eye of the lyst.nu aus Wikipedia, der freien Enzyklopädie. Zur Navigation springen Zur Suche springen. Datei; Dateiversionen.
However, it is possible to visit the dry, sandy desert that the Eye of the Sahara calls home—but it's not a luxurious trip. Travelers must first gain access to a Mauritanian visa and find a local sponsor.
Once admitted, tourists are advised to make local travel arrangements. Some entrepreneurs offer airplane rides or hot air balloon trips over the Eye, giving visitors a bird's-eye view.
The Eye is located near the town of Oudane, which is a car ride away from the structure, and there is even a hotel inside the Eye.
However, because the Eye is located in a sparsely inhabited region of the desert with very little water or rainfall, it is not under much threat from humans.
That leaves the Eye open to the vagaries of nature. The ongoing effects of erosion threaten the landscape, just as they do other places on the planet.
Desert winds may well bring more dunes to the region, particularly as climate change causes increased desertification in the area. It's quite possible that, in the distant future, the Eye of the Sahara will be inundated with sand and dust.
Future travelers may find only a windswept desert burying one of the most striking geological features on the planet.
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The Future of the Eye The eye of the Sahara lures both geologists and tourists. Traces of Pangaea The primitive rocks in the eye of the Sahara have proffered investigators with data about its foundation.
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However, since these sites were first discovered by Theodore Monod in ,  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. Poupeau, and M. Comptes Rendus, vol. Fudali, and W.