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Green auroras arch over a cracked frozen lake at dusk, their reflection mirrored on the ice next to conifer silhouettes.
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Aurora Borealis Over Frozen Lake at Dusk

This aurora is formed when charged solar particles collide with oxygen in Earth's upper atmosphere, typical of high latitude winter nights. The still frozen lake acts as a near perfect mirror, doubling the visual effect of the shifting light ribbons in the sky.

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