Mineral (Evaporite)
Halite (Himalayan Pink Salt)
Halite - NaCl (Sodium Chloride)
Hardness: 2.0-2.5 on Mohs scale; Color: Pink, orange, or reddish due to iron oxide impurities; Luster: Vitreous (glass-like); Crystal Structure: Isometric (cubic); Cleavage: Perfect cubic in three directions; Specific Gravity: 2.16.
- Hardness
- 2
- Color
- Pink, orange, or reddish due to iron oxide impurities
- Luster
- Vitreous (glass-like)
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Physical properties
Hardness: 2.0-2.5 on Mohs scale; Color: Pink, orange, or reddish due to iron oxide impurities; Luster: Vitreous (glass-like); Crystal Structure: Isometric (cubic); Cleavage: Perfect cubic in three directions; Specific Gravity: 2.16.
Formation & geological history
Formed through the evaporation of ancient seawater (typically from the Permian period, approx. 250 million years ago) in enclosed basins. The pressure of tectonic plates mountain-building created the dense, dry crystal beds found deep underground.
Uses & applications
Predominantly used as gourmet table salt, spa treatments (salt lamps), livestock lick stones, and as a natural chemical preservative.
Geological facts
Despite being called 'Himalayan', the vast majority of this pink halite is actually mined from the Khewra Salt Mine in the Salt Range of Punjab, Pakistan, roughly 190 miles from the Himalayas themselves.
Field identification & locations
Identify in the field by its distinct cubic habit, salty taste (though avoid tasting unknown minerals), and solubility in water. It is found in massive underground salt domes or dried lake beds. Collectors look for sharp, well-defined cubic edges and deep color saturation.
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