Stenhuggarite

Chemical formula: CaFe<sup>3+</sup>Sb<sup>3+</sup>As<sup>3+</sup><sub>2</sub>O<sub>7</sub>

Stenhuggarite is a very rare calcium iron arsenate-antimonate, forming tiny, dark red to black crystals with a metallic luster.

## Characteristics Stenhuggarite is an extremely rare mineral from the arsenate and antimonate group. It occurs as very small, tabular or prismatic crystals, rarely exceeding 1 mm in size. It usually forms granular aggregates or appears as single, overgrown crystals. Its appearance is inconspicuous, and identification requires advanced analytical methods. ## Physical Properties Crystals exhibit a metallic to submetallic luster. The mineral is opaque and quite brittle. Its Mohs hardness is approximately 4, and its density is high, approximately 5.55 g/cm³. ## Colors and Varieties Stenhuggarite ranges in color from dark red, through reddish-brown, to black. The streak is characteristically reddish-brown. No varieties of this mineral have been distinguished. ## History and Name The mineral was discovered in the historic Långban mine in Sweden, known for the occurrence of many rare and unique minerals. It was described in 1966 by P.B. Moore. The name "stenhuggarite" comes from the Swedish word "stenhuggare," meaning "stonecutter," and was given in honor of all the anonymous stonecutters and miners whose work contributed to the mineralogical discoveries in Långban.

Properties

Mohs hardness
4
Luster
Metallic, Sub-Metallic
Streak
Red-brown
Density
5.55
Cleavage
Good on {001}
Fracture
Uneven
Transparency
Opaque
Crystal system
Tetragonal

Diagnostic features

## Identification Amateur identification of stenhuggarite is practically impossible. The mineral is distinguished by its reddish-brown streak, metallic luster, and high density. It occurs as very fine, black or dark red crystals. Definitive identification requires specialized analyses, such as X-ray diffraction (XRD) and chemical analysis (EDS/WDS). ## Distinguishing from Similar Minerals It can be confused with other rare, dark minerals from Långban, such as magnussonite or hematophanite. Differentiation is based on chemical composition analysis (presence of calcium, iron, antimony, and arsenic in specific proportions) and crystallographic data. ## Crystal Forms It forms very small, tabular crystals with a square or octagonal cross-section, often flattened. It also occurs as granular aggregates and irregular grains embedded in the host rock.

Geological environment

## Genesis Stenhuggarite forms as a result of metamorphic processes in iron and manganese ore deposits. Its occurrence is associated with skarns and metamorphosed carbonate rocks. It forms under specific physicochemical conditions, which explains its extreme rarity. ## Mineral Associations This mineral co-occurs with other rare minerals from the Långban deposit, such as calcite, hausmannite, magnussonite, tegengrenite, hematophanite, berzeliite, and iron oxides. ## Localities The only confirmed locality of stenhuggarite in the world is its type locality – the Långban mine in Filipstad Municipality, Värmland region, Sweden. This is one of the most famous mineralogical sites in the world.

Rarity

Extremely rare

For collectors

## Quality Criteria The quality of a stenhuggarite specimen primarily depends on the presence of well-formed, even microscopic, crystals. The most valued specimens are those where crystals are clearly visible, have a defined shape, and contrast with the rock matrix. Due to its extreme rarity, every authentic specimen, even in the form of small grains, has great scientific and collector value. ## Popular Localities All known and valued specimens come exclusively from one place in the world: the Långban mine in Sweden. Specimens from this locality are unique and represent a classic for advanced collectors specializing in rare or systematic minerals.

Care and storage

## Cleaning Stenhuggarite specimens are usually very small and embedded in a rock matrix. Due to their brittleness and rarity, mechanical cleaning by amateurs is not recommended. If necessary, compressed air can be used to remove dust. Contact with water and chemicals should be avoided. ## What to Avoid All acids and strong bases, which can damage the mineral, must be strictly avoided. It is sensitive to shocks and impacts, so it should be handled with great care. It should not be heated or subjected to ultrasound. ## Storage Specimens should be stored in stable conditions, away from moisture and chemical contaminants. It is best to keep them in a sealed "micromount" box, which protects against dust and mechanical damage.

External references

Sources

Read more