Peretaite

A variety of Minerals

What is Peretaite?

Peretaite is a sulfate of antimony and calcium. The mineral, Ca(SbO)4(SO4)2(OH)2 (2(H2O)), was named Peretaite for its locality. It was first discovered in an antimony-bearing vein at Pereta, Tuscany, Italy.

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North ZoneCentral RidgeSouth Basin

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Key Characteristics

Characteristics of Peretaite

The mineral peretaite has transparent crystals that are colorless. It has a vitreous luster and perfect {100} cleavage. The density of peretaite was determined by a heavy-liquid method, crystals tend to float in a Clerici solution, which has a density of 4.0 g/cm, therefore the density is 3.8 g/cm.

Formation of Peretaite

Peretaite occurs in only small quantities, as aggregates of tabular crystals. The crystals are found in the geodes of a deeply silicified limestone. It also occurs in the cavities of columnar stibnite. Other associated minerals are stibnite, quartz, calcite, pyrite, valentinite, kermesite, sulfur, and gypsum. Peretaite can often be red from the inclusion of valentinite. The mineral was formed by the action of sulfuric acid on the stibnite; peretaite is closer to the boundary of the country rock limestone, which is the source of the calcium in peretaite.

Quick Facts

Physical Properties

Color
Colourless
Hardness (Mohs)
3.5 - 4
Density
4.06 g/cm³

Chemical Properties

Chemical Formula
Ca(SbO)4(SO4)2(OH)2 · 2H2O
Elements
Ca, H, O, S, Sb
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