The light pillar is a vertical beam of light above or below the sun. Usually, only the upper light pillar can be seen. It has about the same width and color as the sun. The upper light pillar is best observed shortly after sunset. It then looks like the light of a strong searchlight rising vertically above the horizon. At sunset, the color is still orange-white. A few minutes after sunset, the pillar becomes increasingly orange-red and fades 20-60 minutes after sunset. When the light pillar is fully developed, its tip can sometimes be seen to be diffusely broadened. This is the
upper tangent arc, whose arms form an acute angle when the sun is low. The height of the light pillar can be well over 30° in ice fog. However, usually only a 5-10° high pillar is observed.
If both the upper and lower light pillars, as well as part of the
parhelic circle are visible, a cross appears in the sky. Such an impressive phenomenon was often regarded in the Middle Ages as a sign from God.
The light pillar is created by the reflection of sunlight on the base surfaces of
rotating plates and on the prism surfaces of rotating columns. However, a prerequisite is that the ice crystals oscillate around their vertical axis. In addition, a light pillar can also be caused by snowflakes. The formation of the pillar is comparable to the path of light created by the setting sun on a shimmering water surface.