Look at this strange feather-like iridescent cloud photographed in the sky of Warwick, Australia on March 28, 2016.
The rainbow cirrus cloud also known as “feather clouds” or “mares tails” really looks like a feather floating in the evening sky.
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Cloud iridescence is the occurrence of colors in a cloud. It is a fairly uncommon phenomenon, most often observed in altocumulus, cirrocumulus, lenticular clouds and cirrus clouds.
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Iridescence is generally produced near the sun. Iridescent clouds are a diffraction phenomenon caused by small water droplets or small ice crystals individually scattering light. Larger ice crystals produce halos.
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If parts of clouds have small droplets or crystals of similar size, their cumulative effect is seen as colors. The cloud must be optically thin, so that most rays encounter only a single droplet. Iridescence is therefore mostly seen at cloud edges or in semi-transparent clouds, and newly forming clouds produce the brightest and most colorful iridescence.
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In our case, the feather-like cirrus cloud photographed by Kerri Trusz, commonly found of altitudes of 20,000 feet (6,455 m) or higher, was most probably composed of hexagonal ice crystals.