The Northern Lights

The Auroral Oval is a giant ribbon of energy 124 miles (200 km) in diameter and 124 to 186 miles (200 to 300 km) high. It encircles the magnetic north pole and creates a corona of light known as the Aurora Borealis.

The bright dancing lights of the aurora are actually collisions between electrically charged particles from the sun that enter the earth’s atmosphere. The lights are seen above the magnetic poles of the northern and southern hemispheres. They are known as ‘Aurora borealis’ in the north and ‘Aurora australis’ in the south..
Auroral displays appear in many colours although pale green and pink are the most common. Shades of red, yellow, green, blue, and violet have been reported. The lights appear in many forms from patches or scattered clouds of light to streamers, arcs, rippling curtains or shooting rays that light up the sky with an eerie glow.

On a clear night in the fall, the Northern Lights can be viewed from the Lodge dancing magically across the sky.