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An aurora, or polar aurora, is a glow in the sky, seen often in a ring-shaped region around the magnetic poles ("auroral zone") and occasionally further equatorward. The name comes from an older one, "aurora borealis," Latin for "northern dawn," given because an aurora near the northern horizon (its usual location when seen in most of Europe) looks like the glow of the sky preceding sunrise. Also known as "northern lights," although it occurs both north and south of the equator.

An aurora, or polar aurora, is a glow in the sky, seen often in a ring-shaped region around the [[magnetic pole]]s ("auroral zone") and occasionally further equatorward. The name comes from an older one, "aurora borealis," [[Latin]] for "northern dawn," given because an aurora near the northern [[horizon]] (its usual location when seen in most of [[Europe]]) looks like the glow of the sky preceding [[sunrise]]. Also known as "northern lights," although it occurs both north and south of the [[equator]].

The aurora is generally caused by fast electrons from space, guided earthward by magnetic field lines, and its light comes from collisions between such electrons and the atoms of the upper atmosphere, typically 100 km (60 miles) above ground.

The aurora is generally caused by fast [[electron]]s from space, guided earthward by magnetic field lines, and its light comes from collisions between such electrons and the [[atom]]s of the upper [[atmosphere]], typically 100 km (60 miles) above ground.

[[Category:Physics]]

[[Category:Physics]]