Known as the “Eye of the Sahara," the Richat Structure in northwestern Mauritania is a circular geologic feature thought to be caused by an uplifted dome—geologists would classify it as a domed anticline—that has been eroded to expose the originally flat rock layers.
Information
Taken in
Space
Author
NASA
Description
Known as the “Eye of the Sahara," the Richat Structure in northwestern Mauritania is a circular geologic feature thought to be caused by an uplifted dome—geologists would classify it as a domed anticline—that has been eroded to expose the originally flat rock layers.