
Mineral
Pink Himalayan Salt (Halite)
Halite - NaCl (Sodium Chloride) with trace Iron Oxide and Magnesium
Hardness: 2.5 on Mohs scale; Color: Pink, orange, or reddish-brown due to trace minerals; Luster: Vitreous (glassy); Crystal Structure: Isometric/Cubic; Cleavage: Perfect cubic; Specific Gravity: 2.16
- Hardness
- 2
- Color
- Pink, orange, or reddish-brown due to trace minerals
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 2.5 on Mohs scale; Color: Pink, orange, or reddish-brown due to trace minerals; Luster: Vitreous (glassy); Crystal Structure: Isometric/Cubic; Cleavage: Perfect cubic; Specific Gravity: 2.16
Formation & geological history
Formed through the evaporation of ancient landlocked prehistoric seas (primarily the Tethys Ocean) during the Precambrian to Permian periods (roughly 200-800 million years ago) followed by tectonic compression.
Uses & applications
Used in culinary applications (table salt), interior design (salt lamps), spa treatments (halotherapy), and as decorative ornaments for collectors.
Geological facts
Most authentic Himalayan salt comes from the Salt Range in Pakistan, specifically the Khewra Salt Mine. The pink hue is caused by iron oxide (rust) and other mineral impurities trapped in the crystal lattice.
Field identification & locations
Identify in the field by its distinct salty taste (though not recommended for unknown specimens), cubic cleavage, and solubility in water. It will feel 'greasy' in humid conditions as it absorbs moisture from the air.
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