The aurora borealis, or northern lights, illuminates the sky over
Stockholm on April 6, 2000. The red and yellow-green colors of
this auroral display are due to oxygen gas hovering at two
different altitudes. Oxygen in the atmosphere more than 150 miles
above the surface of the Earth glows red when exposed to
fast-moving particles from the magnetosphere, while oxygen closer
in appears yellow-green or green, the brightest and most common
auroral hues.