Akrochordite

Chemical formula: Mn<sup>2+</sup>Mn<sup>2+</sup><sub>2</sub>Mn<sup>2+</sup><sub>2</sub>(As<sup>5+</sup>O<sub>4</sub>)<sub>2</sub>(OH)<sub>4</sub>(H<sub>2</sub>O)<sub>4</sub>

Akrochordite is a rare, hydrated manganese arsenate, forming characteristic aggregates in the form of warts or spherulites.

## Characteristics Akrochordite, with the chemical formula (Mn,Mg)₅(AsO₄)₂(OH)₄·4H₂O, is a mineral that forms small, spherical aggregates or botryoidal clusters resembling warts in appearance. Individual spherulites rarely exceed a few millimeters in diameter and consist of tiny, radially arranged crystals. Specimens typically have a waxy or vitreous luster. ## Physical Properties This mineral is relatively soft, with a Mohs hardness of 3.5. Its density is approximately 3.19 g/cm³. It is characterized by a vitreous luster, transitioning to greasy, and is translucent. ## Colors and Varieties Akrochordite occurs in shades from yellowish-brown and reddish-brown to brown. Colorless forms are rarer. No commercial names or color varieties are distinguished. ## History and Name The mineral's name comes from the Greek word *akrochordon* (ἀκροχορδών), meaning "wart," which directly refers to the typical form of its aggregates. It was first described in 1922 by Gustav Flink based on specimens found in the historic Långban mine in Värmland, Sweden. ## Uses Due to its rarity and small crystal size, akrochordite has no industrial applications. It is solely an object of scientific and collector interest.

Properties

Mohs hardness
3.5
Luster
Vitreous to greasy
Streak
White
Density
3.19
Cleavage
Good on {010}
Fracture
Uneven
Transparency
Translucent
Crystal system
Monoclinic

Diagnostic features

## Identification The key diagnostic feature of akrochordite is its unique form as small, spherical or "wart-like" aggregates. The place of origin (Långban, Sterling Hill) and co-occurrence with other manganese minerals are also important. ## Distinguishing from Similar Minerals It can be confused with other arsenates or carbonates with a similar botryoidal structure, such as allactite, sarkinite, or kutnohorite, which occur in the same localities. Certain differentiation often requires hardness analysis, reaction with acids, or advanced research methods, but the characteristic "wart-like" appearance is a strong indicator. ## Crystal Forms Akrochordite almost always occurs in the form of spherical, botryoidal, or reniform aggregates. Single, well-formed crystals are extremely rare and appear as small, tabular forms.

Geological environment

## Genesis It is a rare secondary mineral, formed in iron and manganese ore deposits that have undergone metamorphic processes. It is most commonly found in vugs and fissures within hausmannite-dolomite skarns. ## Mineral Associations Akrochordite often co-occurs with minerals such as hausmannite, baryte, brandtite, sarkinite, allactite, pyrochroite, and calcite. ## Localities The most important and historically first locality is the Långban mine in the Värmland region of Sweden, which is its type locality. The second significant occurrence is Sterling Hill in Ogdensburg, New Jersey, USA. Specimens from other locations are practically unheard of.

Rarity

Very rare

For collectors

## Quality Criteria The most highly valued specimens are those with well-formed, clearly separated spherical aggregates of an intense, reddish-brown color. Placement on a contrasting rock matrix, as well as the presence of other rare minerals, especially from Långban or Sterling Hill, adds significant value. ## Popular Localities Collector specimens come almost exclusively from two classic localities: Långban in Sweden and Sterling Hill in the USA. Swedish specimens are historically most important, while American ones can be somewhat larger.

Care and storage

## Cleaning Akrochordite specimens should be cleaned very carefully, using only a soft brush and distilled water. Ultrasonic cleaners should be avoided, as they can damage delicate aggregates. ## What to Avoid The mineral is sensitive to acids and strong chemicals. As a hydrated mineral, it is also susceptible to damage from high temperatures, which can lead to dehydration and structural degradation. Prolonged exposure to direct sunlight should be avoided. ## Storage It is recommended to store specimens in stable conditions, in separate, padded boxes, to prevent abrasion and mechanical damage. It should not be stored in contact with harder minerals.

External references

Sources

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