Anticrepuscular rays are alternating bright beams and darker shadow bands that appear to converge on the antisolar point — the spot on the horizon directly opposite the sun. They are the very same shafts of sunlight and cloud shadow as ordinary crepuscular rays; in reality the beams are nearly parallel, but perspective makes them seem to meet, just as parallel railway tracks appear to converge at a vanishing point.
Worth knowing
Anticrepuscular rays are always dimmer than the crepuscular rays near the sun, because they rely on light scattered back towards you — and back-scattering is far weaker than the forward-scattering that lights up beams on the sun's side of the sky.
Note
Still unsure it's the same cloud? Our app, Cloud Point— on iOS and Android — reads a photo and returns the likely type with altitude, useful when a formation is fading faster than you can look it up.