
Sundogs are formed by reflection or refraction of sunlight by ice crystals found within cirrus or cirrostratus clouds. These are the thin wispy clouds you sometimes see in the sky that seem to go for miles. Sundogs normally occur, but not always, when the sun is low in the sky, like at sunrise and sunset. The ice crystals within the clouds act as prisms breaking up the light into the different wavelengths producing the spectrum of colors. When the light hits the prism-shaped ice crystals, the white light is slowed down causing it to separate into the different colors. This process is called dispersion. If you want to learn more, here is a great site that goes into all the physics behind sundogs. The link at the bottom of this sites page explains how they are formed.
I didn't have my camera with me, but I pulled a few images from Wikipedia. I have seen only one sundog before. This was my sister's first.


