Aouelloul Crater
Inchiri
Aouelloul Crater is a well-preserved meteorite impact crater located in the Inchiri region of Mauritania. Measuring approximately 390 meters in diameter, it was formed by the impact of a meteorite estimated to have struck the Earth around 3.1 million years ago during the Pliocene epoch. The crater is characterized by a raised rim and a relatively flat floor, typical of simple impact craters. It is one of the few recognized impact structures in Africa and provides valuable geological insights into impact processes and planetary science. The site is notable for fragments of meteorite material found in and around the crater, which have been studied extensively by scientists. Its remote desert location adds to its intrigue, attracting researchers and adventurous travelers interested in natural history and geology.
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Consejo: The best time to visit Aouelloul Crater is during the cooler months to avoid extreme desert heat. Visitors should prepare for remote travel conditions, as the site is located in a sparsely populated desert area with limited facilities. It is advisable to arrange guided tours or local transportation in advance. There are no entrance fees, but visitors should carry sufficient water, sun protection, and supplies. Purchasing tickets or permits is generally not required, but checking local conditions before travel is recommended.
Datos interesantes
- •Aouelloul Crater is one of the few confirmed meteorite impact craters in Africa.
- •Meteorite fragments found at the site have been used to study the composition of iron meteorites.
- •The crater dates back to the Pliocene epoch, about 3.1 million years ago.
- •Its well-preserved state is due to the arid desert climate minimizing erosion.
Historia
The Aouelloul Crater was formed approximately 3.1 million years ago by the impact of an iron meteorite during the Pliocene epoch.
It was first scientifically described in the mid-20th century when meteorite fragments were recovered from the site.
Over the decades, it has been an important location for studying impact craters and meteorite composition.
The crater's preservation is attributed to the arid desert environment, which limits erosion and weathering processes.