Prosperite

Chemical formula: Ca₂Zn²⁺₄(As⁵⁺O₄)₄·H₂O

Prosperite is a rare calcium zinc arsenate, forming colorless or white, prismatic crystals, discovered in the Tsumeb mine in Namibia.

## Characteristics Prosperite is a hydrated calcium zinc arsenate, occurring as small, well-formed crystals. Typical specimens consist of colorless or white, prismatic to acicular crystals, which often form radial or tangled aggregates. Due to its chemical composition and rarity, it is a mineral highly valued mainly by collectors. ## Physical Properties Prosperite crystals exhibit a Mohs hardness of 4.5, making them relatively brittle. They are translucent, with a density of 4.31 g/cm³. The luster is described as vitreous. ## Colors and Varieties This mineral is typically colorless or white. No colored or commercial varieties are distinguished. ## History and Name Prosperite was first described in 1979 based on specimens found in the famous Tsumeb mine in Namibia. Its name honors Prosper J. Williams (1910–1993), a Canadian mineral dealer and collector who provided the first samples for research. ## Uses Prosperite has no industrial application. Its only significance is scientific and collectible.

Properties

Mohs hardness
4.5
Luster
Vitreous
Streak
White
Density
4.31
Transparency
Translucent
Crystal system
Monoclinic

Diagnostic features

## Identification Prosperite can be identified by its characteristic, colorless or white, prismatic crystals, often forming radial aggregates. Its high density and occurrence in association with other Tsumeb arsenates are also important indicators. ## Distinguishing from similar minerals It can be confused with other colorless arsenates or sulfates, such as gypsum or hemimorphite. It is distinguished from them by its higher density, specific crystal form, and occurrence environment. Final confirmation requires advanced chemical analysis. ## Crystal forms Prosperite crystals are elongated, prismatic, often terminated with sharp faces. They usually occur as radial or chaotically arranged aggregates of acicular crystals, growing on the host rock.

Geological environment

## Genesis Prosperite is a secondary mineral, forming in the oxidation zones (gossans) of polymetallic ore deposits rich in arsenic, zinc, and calcium. It forms as a result of the weathering of primary ore minerals. ## Mineral associations This mineral co-occurs with other rare arsenates, especially those characteristic of the Tsumeb deposit. It is most commonly associated with adamite, zincolivenite, tsumcorite, stranskiite, leiteite, and germanite. ## Localities The only confirmed and classic locality of prosperite in the world is the Tsumeb mine (Ongopolo Mine) in the Oshikoto Region of Namibia. This is its type locality, from which all known specimens originate.

Rarity

Very rare

For collectors

## Quality Criteria The most valued prosperite specimens are those with well-formed, sharp, and undamaged crystals, forming aesthetic, radial aggregates on a small rock matrix. Contrast with a darker host rock enhances visual appeal. Crystal size and richness of the aggregate are also important. ## Popular Localities The only source of collectible specimens is the historical type locality - the Tsumeb mine in Namibia. This mine is now closed, which means that new specimens do not appear on the market, and the value of historical samples increases.

Care and storage

## Cleaning Prosperite specimens should be cleaned very carefully, using a soft brush to remove dust. Due to the arsenic content, inhalation of dust should be avoided. After contact with the mineral, it is recommended to wash hands. The use of water is not advisable. ## What to avoid Avoid contact with chemicals, especially acids, which can damage the mineral. Prosperite is brittle, so it must be protected from impacts and scratches. It should not be heated or subjected to ultrasound. ## Storage Specimens are best stored in closed, padded boxes or display cases to protect them from mechanical damage and dust. They should be kept away from minerals that could scratch them.

External references

Sources

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