From Wikipedia, the free encyclopedia
Aurora est lux in caelo naturaliter splendens, quoddam modo aurorae similis, qui circum undique in regionibus polaribus, etsi interdum apud latitudines humiles, saepius videri potest. Causa est concursus energeticorum particulorum oneratorum in fluxu venti solaris adlatorum cum atomis in atmosphaera altitudinum altiorum circa campum magneticum.
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Vicimedia Communia plura habent quae ad auroras boreales et australes spectant. |
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