Schirmerite, pronounced /ʃɪərməraɪt/, is a rare mineral discovered in 1972 in the Tintic mining district, Utah, USA. The word is spelled as it sounds and is derived from the name of Swedish mineralogist Erik Johan Schirmer. It appears as a dull grey mineral that may have a reddish tint and is composed of silver, antimony, sulfur, and arsenic. Schirmerite is a relatively soft mineral and one of the many rare minerals found in the Tintic mining district.
Schirmerite is a rare mineral that belongs to the selenide mineral group. It is named after the German mineralogist Reinhard Schirmer, a professor at the Mining Academy of Freiberg. It was first discovered in 1922 in Jistebnice, Czech Republic. The mineral typically occurs as an accessory mineral in hydrothermal silver-rich deposits.
Schirmerite has a distinctive metallic to opaque gray color and is known for its high luster. It often occurs in elongated prismatic or acicular crystal formations. The mineral has a high density and is relatively brittle in nature.
Chemically, schirmerite is classified as a silver selenide mineral with the chemical formula AgTeSe₂. It is closely related to other minerals in the selenide group, such as naumannite and klockmannite. These minerals often occur together in mineral deposits and can exhibit similar physical and chemical properties.
Schirmerite is considered a minor ore of silver due to its silver content. It is not widely used in industrial applications; however, it is highly sought after by mineral collectors and enthusiasts due to its rarity. Some specimens of schirmerite may exhibit interesting crystal formations or associations with other minerals, making them valuable for collectors.
In summary, schirmerite is a rare silver selenide mineral with high luster and distinctive gray color. It occurs as an accessory mineral in hydrothermal silver-rich deposits and is prized by mineral collectors for its rarity and aesthetic appeal.