NATURAL PHENOMENON - EYE OF THE SAHARA
EYE OF THE SAHARA
Eye of the sahara also known as Richat Structure is prominent circular feature located in the Sahara near Ouadane, west–central Mauritania. The Richat Structure is a deeply eroded, slightly elliptical dome with a diameter of 40 kilometres. The sedimentary rock exposed in this dome ranges in age from Late Proterozoic within the center of the dome to Ordovician sandstone around its edges. The sedimentary rocks comprising this structure dip outward at 10–20°. Differential erosion of resistant layers of quartzite has created high-relief circular cuestas. Its center consists of a siliceous breccia covering an area that is at least 30 kilometres in diameter.
How was the Richat Structure formed? Scientists still have questions about the Eye of the Sahara, but two Canadian geologists have a working theory about its origins. They think that the Eye's formation began more than 100 million years ago, as the supercontinent Pangaea was ripped apart by plate tectonics and what are now Africa and South America were being torn away from each other.
Molten rock pushed up toward the surface but didn't make it all the way, creating a dome of rock layers, like a very large pimple. This also created fault lines circling and crossing the Eye. The molten rock also dissolved limestone near the center of the Eye, which collapsed to form a special type of rock called breccia.
A little after 100 million years ago, the Eye erupted violently. That collapsed the bubble partway, and erosion did the rest of the work to create the Eye of the Sahara that we know today. The rings are made of different types of rock that erode at different speeds. The paler circle near the center of the Eye is volcanic rock created during that explosion. Modern astronauts are fond of the Eye because so much of the Sahara Desert is an unbroken sea of sand. The Eye is one of the few breaks in the monotony, and now it's become a key landmark for them.
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.
How was the Richat Structure found? When the Gemini IV mission, a four-day orbit around Earth, was being prepared in 1965, the astronauts were asked to take photos of Earth's terrain. They were particularly asked to look out for "any large circular features which might be the roots of impact structures," according to the text accompanying a set of photographs published from the mission. Impact craters are geologically important because they tell us about the history of Earth. Also, knowing how many times space rocks have crashed into our planet can help scientists make predictions about the future. And for a while, scientists did think that the Eye of the Sahara was an impact crater. But they didn't find enough melted rocks to make that guess hold water. Current theories suggest a much more complicated story behind this incredible natural formation. The main ring structure of the Eye is the eroded remains of what was once a dome of layers of Earth's crust.
source :
https://en.wikipedia.org/wiki/Richat_Structure
http://www.businessinsider.com/25-of-the-coolest-natural-phenomena-2016-6/?IR=T/#15-giant-snake-orgies-15
http://www.businessinsider.com/the-eye-of-the-sahara-is-still-a-mystery-2016-7/?IR=T
https://www.zmescience.com/science/geology/the-eye-of-the-sahara-05102010/