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Raro fenômeno de iridescência das nuvens. Esse fenômeno é causado por cristais de gelo que espalham os raios do sol entre as nuvens, de modo que aparecem nas cores do espectro.
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Esse fenômeno ocorre quando uma nuvem está posicionada entre o sol e outras nuvens coloridas durante o pôr do sol. A nuvem bloqueia parcialmente a luz solar, criando uma área sombreada ou uma linha de sombra nas nuvens iluminadas pelo sol, que podem estar tingidas com cores vibrantes devido aos efeitos da luz do fim do dia. Esse contraste entre a área sombreada e as nuvens iluminadas cria um efeito visual impressionante e muitas vezes fotogênico durante o pôr do sol, acrescentando profundidade e
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