Peterchinite

Chemical formula: Zn²⁺₃Zn²⁺₂(OH)₆As⁵⁺[O₃(OH)₃]

Peterchinite is an extremely rare zinc arsenate, forming colorless, hexagonal crystals with a vitreous luster.

## Characteristics Peterchinite is a hydrated zinc arsenate, occurring as small, hexagonal, tabular or prismatic crystals, usually not exceeding 0.2 mm. It also forms rosette aggregates. It is a colorless and transparent mineral with a strong, vitreous luster. ## Physical Properties Peterchinite crystals are too small to precisely determine their hardness, but it is estimated to be around 3 on the Mohs scale. The density calculated based on the chemical formula and unit cell parameters is 4.31 g/cm³. The mineral exhibits perfect cleavage in one plane. ## History and Name The mineral's name honors Peter C. Burns (born 1966), a Canadian mineralogist and crystallographer from the University of Notre Dame in the USA, for his contributions to the mineralogy of uranium and actinides. Peterchinite was approved as a new mineral by the International Mineralogical Association (IMA) in 2017 (IMA2017-091), and its description was published in 2018.

Properties

Mohs hardness
3
Luster
Vitreous
Streak
White
Density
4.31
Cleavage
Perfect on {0001}
Fracture
Uneven
Transparency
Transparent
Crystal system
Monoclinic

Diagnostic features

## Identification Identification of peterchinite is possible only through advanced analytical methods, such as Raman spectroscopy and single-crystal X-ray diffraction (XRD), combined with chemical composition analysis (EDS/WDS). Visual identification in the field or in a collection is impossible due to its small size and lack of characteristic macroscopic features. ## Differentiation from similar minerals Peterchinite can be confused with other secondary, colorless zinc arsenates, such as köttigite or legrandite, which may co-occur in the same environment. Definitive differentiation requires specialized laboratory tests. ## Crystal forms The mineral forms hexagonal, tabular or short prismatic crystals. They often occur as radial or rosette aggregates and clusters.

Geological environment

## Genesis Peterchinite is a secondary mineral, forming in the oxidation zones (gossans) of polymetallic deposits rich in zinc and arsenic. It forms as a result of the weathering of primary ore minerals, such as sphalerite and arsenopyrite, under low temperature and pressure conditions. ## Mineral associations This mineral co-occurs with other rare arsenates, such as o'danielite, prosperite, gartrellite, as well as tenorite, quartz, and hematite. ## Localities The only confirmed locality of peterchinite in the world (type locality) is the historic Tsumeb mine in the Oshikoto region of Namibia. This is one of the most famous mineralogical sites, known for the occurrence of many rare and unique secondary minerals.

Rarity

Extremely rare

For collectors

## Quality criteria As a micromineral, the value of peterchinite is primarily determined by the certainty of the specimen's identification. Samples with well-formed, sharp crystals forming aesthetic, rosette aggregates, set on a contrasting rock matrix, are most highly prized. Due to its colorless nature, the form and transparency of the crystals are key. ## Popular localities All known peterchinite specimens available on the collector's market originate exclusively from the Tsumeb mine in Namibia.

Care and storage

## Cleaning Due to its extreme rarity, small crystal size, and fragility, peterchinite specimens should not be cleaned mechanically or chemically. Any treatment carries the risk of irreversible damage. It is safest to leave the specimen in its original state. ## What to avoid Avoid contact with all chemicals, including acids and bases. The mineral is potentially sensitive to changes in temperature and humidity. It should not be exposed to direct sunlight. ## Storage Peterchinite specimens, as microminerals, should be stored exclusively in specialized "micromount" boxes, protecting them from dust, shocks, and humidity changes. Display is only possible under a microscope.

External references

Sources

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