NASA scientists discovered a hidden 2.5-billion-year-old internal structure inside the Great Dyke of Zimbabwe using satellite imaging and geophysics mapping.
The Great Dyke is a 550-kilometre-long igneous rock formation located in central Zimbabwe.
It is classified as a lopolith, which is a saucer-shaped igneous intrusion formed from cooled magma.
The structure is believed to be linked to an ancient magma storage zone from the Archaean Eon.
The Great Dyke contains important minerals such as platinum, chromium, nickel, copper, iron, titanium, vanadium, and tin.