Jarosite

21 in the gallery

Jarosite is a hydrous potassium iron sulfate mineral that forms in acid-sulfate environments, typically as earthy to ferruginous aggregates and sometimes as well-formed crystals. It commonly occurs in oxidized zones of sulfide deposits and mine dumps, where cloudy brown to yellow-brown masses reflect its iron- and sulfate-rich chemistry. Crystallography ranges from granular masses to plate-like or prismatic habits, and it often exhibits a dull to resinous luster. Notable specimens come from a variety of localities, including classic deposits in the United States, Spain, Mexico, Bolivia, and Greece, making it a familiar sight in many mineral collections.

Formula
KFe3+3(SO4)2(OH)6
Rarity
Common
Stability
Stable
Collector interest
Moderate Interest

Where Jarosite is found

About Jarosite

Collectors prize jarosite for its distinctive color and its visibility in oxidized zones, as well as its association with late-stage, secondary mineral parageneses. While individual crystals may be modest in size, aggregates can be striking in appearance, especially when contrasted with quartz or goethite in a matrix. As a mineral that signals a specific geochemical milieu, jarosite provides context for the oxidation history of a deposit and often accompanies other iron sulfates, making it a practical and aesthetically engaging addition to a cabinet or display. Its presence across several well-documented localities helps collectors track provenance and diversify specimen suites.