Cirrocumulus clouds are high-altitude clouds that form at altitudes of 20,000 feet (6,000 meters) or more. They appear as small, white patches or ripples in the sky, often resembling a thin veil. These clouds are composed of ice crystals and typically indicate fair weather, although they can sometimes signal a change in the atmosphere. These clouds are often seen in the early morning or late afternoon and can create a beautiful, textured appearance in the sky. Cirrocumulus clouds do not usually produce precipitation, but they can contribute to the overall cloud cover and may be part of a larger weather system.