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[MUSIC] Above South America, a weak spot in Earths magnetic field is evolving. Called the South Atlantic Anomaly, this unique region has been expanding for more than a decade. And scientists believe that its beginning to split into two distinct zones. Now, while this anomaly poses little risk to life here on Earth, it does allow scientists to study the complicated mechanisms behind Earths magnetism. Around 1800 miles below the surface, dynamic processes in Earths liquid iron outer core are continuously generating electrical currents. This account for the majority of Earths magnetic field. But unlike a typical bar magnet, with one north and south pole, Earths magnetism isnt all neat and tidy. If we take a look below the anomaly at the boundary separating the core and the mantle, we can see the magnetic variations are much stronger. This picture provides a clear link between the anomaly we see in Earths magnetosphere, its origins deep within Earths interior, and how it is projec