Rock Identifier
Potash (Sylvite/Potassium Feldspar) (Potassium chloride (KCl) or Orthoclase (KAlSi3O8)) — mineral
mineral

Potash (Sylvite/Potassium Feldspar)

Potassium chloride (KCl) or Orthoclase (KAlSi3O8)

Hardness: 2-6 depending on exact mineral type; Color: reddish-pink to orange; Luster: vitreous (glassy); Crystal structure: cubic or monoclinic; Cleavage: excellent in two directions

Hardness
2-6 depending on exact mineral type
Color
reddish-pink to orange
Luster
vitreous (glassy)
Identified More mineral
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Physical properties

Hardness: 2-6 depending on exact mineral type; Color: reddish-pink to orange; Luster: vitreous (glassy); Crystal structure: cubic or monoclinic; Cleavage: excellent in two directions

Formation & geological history

Commonly formed in evaporite deposits from ancient seas (if Sylvite) or as a major constituent of igneous rocks like granite (if Feldspar).

Uses & applications

Primarily used in agriculture as fertilizer (potash), glassmaking, ceramics, and occasionally as a display mineral for collectors.

Geological facts

The name 'Potash' comes from 'pot ash', referring to the historical method of plant ashes soaked in water in a pot. It is a vital nutrient for plant growth.

Field identification & locations

Identify by the pink/orange color and distinctive step-like cleavage planes. Common in areas with ancient salt beds like Saskatchewan, Canada, or Permian basins in New Mexico/Texas.