alunitas

Alunitas is a term used in some languages to refer to alunite minerals, a group of hydrated aluminum sulfate minerals. The two principal endmembers are potassium-bearing alunite, with the chemical formula KAl3(SO4)2(OH)6, and sodium-bearing natroalunite, NaAl3(SO4)2(OH)6. They commonly occur together as solid solutions in hydrothermal alteration zones. Minor substitutions by other cations such as iron or calcium are also recorded, but potassium or sodium typically dominate the X site.

Structure and appearance

Alunitas crystallize in forms that are commonly tabular, prismatic, or crust-like. Color ranges from colorless and white to pink, violet, red, or brown; the luster is vitreous to resinous. Mohs hardness is around 5, and specific gravity is about 2.8–3.4.

Formation and geological setting

They form by hydrothermal alteration of aluminum- and potassium-rich rocks, especially feldspars, in acidic sulfate-rich fluids. They are common in potassic alteration zones adjacent to granitic or volcanic rocks and can fill veins, voids, and cataclastic spaces. Associated minerals include quartz, goethite, jarosite, and other sulfates.

Distribution and notable localities

Alunitas occur worldwide. Notable deposits are found in parts of the western United States, Europe such as Italy and Romania, and areas in South America including Peru. The natroalunite variety is common in sodium-rich alteration zones and can be associated with other sodium sulfates.

Uses and significance

Historically, alunite was mined as a source of alum for tanning and dyeing. Today it is mainly of mineral-collecting interest and as a potential source of alumina or potash in some altered systems, though it is not a major ore. Its scientific value lies in understanding hydrothermal processes and alteration histories.

Etymology

The name alunite derives from alum, reflecting its relation to alum compounds; the term alunitas reflects linguistic variation in naming.