
mineral
Pink halite (rock salt)
Halite (NaCl), likely colored by trace impurities
AI-generated identification · may be incorrectSoft (Mohs 2–2.5), pale pink to white, vitreous to dull luster, cubic crystal structure and perfect cubic cleavage; commonly translucent. The specimen’s rough, granular appearance is consistent with halite, though an image alone cannot confirm the identification.
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Physical properties
Soft (Mohs 2–2.5), pale pink to white, vitreous to dull luster, cubic crystal structure and perfect cubic cleavage; commonly translucent. The specimen’s rough, granular appearance is consistent with halite, though an image alone cannot confirm the identification.
Formation & geological history
Forms when saline water evaporates in arid basins or restricted seas, commonly in sedimentary evaporite layers. Deposits range from ancient to actively forming today.
Uses & applications
Used as a source of salt and in chemical production; attractive pink specimens are collected and sometimes displayed, but are generally not used as gemstones.
Geological facts
Pink coloration can result from trace minerals or microscopic inclusions; halite dissolves readily in water and tastes salty, but tasting unknown specimens is not recommended.
Field identification & locations
Look for cubic cleavage, low hardness, and rapid dissolution; common sources include evaporite deposits and salt lakes such as the Himalaya-region deposits. Keep dry to prevent deterioration.
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