Rock Identifier
Pink halite (rock salt) (Halite (NaCl), likely iron-stained or impurity-colored) — mineral
mineral

Pink halite (rock salt)

Halite (NaCl), likely iron-stained or impurity-colored

AI-generated identification · may be incorrect

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.

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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.