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Image Caption: In This distant view of the Aurora Australis or Southern Lights (location unknown), a spiked and sinuous band of red and green airglow above the Earth Limb is highlighted by moonglow. Auroral activity is due to exitation of atomic oxygen in the upper atmosphere by radiation from the van Allen Radiation Belts and is most common above the 65 degree north and south latitude range during the spring and fall of the year.