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Supralateral arcs form when sun light enters horizontally oriented, rod-shaped [[hexagon]]al [[ice crystal]]s through a hexagonal base and exits through one of the [[prism (optics)|prism]] sides. Supralateral arcs occur about once a year.<ref name="meteoros" />
[[File:Icearcs1.jpg|thumb|A faint [[circumzenithal arc]] above
==Confusion with the 46° halo==
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