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Shining through openings in clouds particularly stratocumulus [ citation needed ] or between other objects such as mountains, these columns of sunlit scattering particles are separated by darker shadowed volumes. Despite converging toward the light source, the rays are essentially parallel shafts of sunlit and shadowed particles. Their apparent convergence in the sky is a visual illusion from linear perspective. This illusion is the same as railway lines' or long hallways' appearing to converge at a distant vanishing point. The scattering particles that make crepuscular rays visible can be air molecules or particulates. Crepuscular comes from the Latin word "crepusculum", meaning twilight. The rays in some cases may extend across the sky and appear to converge at the antisolar point , the point on the sky sphere directly opposite the sun.