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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

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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Creative #:
156412955
License type:
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.
Photographer:
Danita Delimont
Collection:
Gallo Images
Max file size:
5,616 x 3,744 px (18.72 x 12.48 in) - 300 dpi - 8.39 MB
Release info:
No release, but release may not be required.More information

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Aurora Light Wapusk National Park Manitoba Canada Stock Photo 156412955Abstract,Aurora Borealis,Beauty In Nature,Canada,Color Image,Day,Dramatic Sky,Green Color,Horizontal,Light,Manitoba,Natural Phenomenon,Nature,Night,No People,Outdoors,Photography,Scenics,Sky,Star,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