Nearly circular bands, called
auroral ovals, surround both poles of our planet.
While the cause of
the auroral oval emissions is reasonably well understood, the origin of the theta aurora was unclear until now.
Alaska is one of the most celebrated places to visit the Aurora Borealis, mainly because its geographic location lies directly beneath
the auroral oval.
Earth's full North Polar
auroral oval, in an image taken in ultraviolet light by the U.S. Polar spacecraft over northern Canada, April 6, 1996.