sedimentary

Himalayan Pink Salt

Halite (NaCl) with trace impurities of iron oxide

AI-generated identification · may be incorrect

Hardness: 2.0-2.5 on Mohs scale; Color: Pink, orange, or reddish-white; Luster: Vitreous; Crystal structure: Cubic; Cleavage: Perfect cubic; Solubility: Highly soluble in water

Hardness: 2
Color: Pink, orange, or reddish-white
Luster: Vitreous

Identified July 7, 2026More sedimentary →

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Physical properties

Hardness: 2.0-2.5 on Mohs scale; Color: Pink, orange, or reddish-white; Luster: Vitreous; Crystal structure: Cubic; Cleavage: Perfect cubic; Solubility: Highly soluble in water

Formation & geological history

Formed by the evaporation of ancient seas during the Precambrian or early Paleozoic eras, approximately 250 to 500 million years ago. Found in deep underground mines in the Punjab region of Pakistan.

Uses & applications

Culinary use (gourmet salt), home decor (salt lamps), spa/wellness treatments (halotherapy), and as mineral licks for livestock.

Geological facts

The pink hue is caused by infinitesimal amounts of iron oxide (rust). Despite the name, most Himalayan salt is mined in the Khewra Salt Mine in Pakistan, nearly 300 kilometers from the actual Himalayas.

Field identification & locations

Identified by its distinctive salty taste, cubic cleavage, and low hardness (can be scratched by a fingernail). It will 'sweat' or dissolve slightly in humid environments.