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Aurora light, Wapusk National Park, Manitoba, Canada : Stock Photo
An aurora plural: aurorae or auroras; from the Latin word aurora, dawn is a natural light display in the sky particularly in the high latitude Arctic and Antarctic regions, caused by the collision of energetic charged particles with atoms in the high altitude atmosphere thermosphere. The charged particles originate in the magnetosphere and solar wind and, on Earth, are directed by the Earth's magnetic field into the atmosphere

Aurora light, Wapusk National Park, Manitoba, Canada

Credit: 
Danita Delimont
Caption:
An aurora plural: aurorae or auroras; from the Latin word aurora, dawn is a natural light display in the sky particularly in the high latitude Arctic and Antarctic regions, caused by the collision of energetic charged particles with atoms in the high altitude atmosphere thermosphere. The charged particles originate in the magnetosphere and solar wind and, on Earth, are directed by the Earth's magnetic field into the atmosphere
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156412957
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No release, but release may not be required.More information
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Rights-managedRights-managed products are licensed with restrictions on usage, such as limitations on size, placement, duration of use and geographic distribution. You will be asked to submit information concerning your intended use of the product, which will determine the scope of usage rights granted.
Collection:
Gallo Images
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5,616 x 3,744 px (18.72 x 12.48 in) - 300 dpi - 8.18 MB

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Aurora Light Wapusk National Park Manitoba Canada Stock Photo 156412957Aurora Borealis,Beauty In Nature,Canada,Color Image,Day,Forest,Green Color,Horizontal,Light - Natural Phenomenon,Manitoba,Natural Phenomenon,Nature,Night,No People,Outdoors,Photography,Scenics,Silhouette,Sky,Star,Tree,Wapusk National ParkPhotographer Collection: Gallo Images An aurora plural: aurorae or auroras; from the Latin word aurora, dawn is a natural light display in the sky particularly in the high latitude Arctic and Antarctic regions, caused by the collision of energetic charged particles with atoms in the high altitude atmosphere thermosphere. The charged particles originate in the magnetosphere and solar wind and, on Earth, are directed by the Earth's magnetic field into the atmosphere