A salt glacier is a flow of salt (typically halite) that is created when a rising diapir in a salt dome breaches the surface, much like toothpaste from a tube. Gravity causes the salt to flow like glaciers into adjacent valleys. The resulting tongue-shaped bodies can extend for kilometers, with repeating bow-shaped ridges separated by crevasse-like gullies and with steep sides and fronts. Clays may be brought up with the salt, turning it dark.

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