
mineral
Pink halite (rock salt)
Halite (NaCl), likely iron-stained or impurity-colored
AI-generated identification · may be incorrectPale pink, translucent to opaque, with a vitreous to slightly greasy luster and blocky cubic cleavage; Mohs hardness 2–2.5, cubic crystal structure, specific gravity about 2.17. The image alone cannot confirm the identification; calcite or another pale mineral is possible.
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Physical properties
Pale pink, translucent to opaque, with a vitreous to slightly greasy luster and blocky cubic cleavage; Mohs hardness 2–2.5, cubic crystal structure, specific gravity about 2.17. The image alone cannot confirm the identification; calcite or another pale mineral is possible.
Formation & geological history
Halite forms when saline water evaporates in restricted basins, commonly in layered evaporite deposits. Such deposits range from ancient to modern; the specimen’s age and exact locality cannot be determined from the image.
Uses & applications
Halite is used for table salt, chemical production, water softening, and road de-icing; attractive crystals are collected, though this rough piece appears modest.
Geological facts
Halite dissolves readily in water and has perfect cubic cleavage. Pink coloration commonly comes from trace impurities or inclusions.
Field identification & locations
The blocky shape and pale pink color are consistent with halite, but a reliable check is its softness and high water solubility; avoid tasting unidentified specimens. Major deposits occur in evaporite basins worldwide.
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