Zinc-olivenite

Chemical formula: Cu₂+Zn₂+As₅+O₄(OH)

Zinc-olivenite is a rare arsenate mineral, the zinc analogue of olivenite, characterized by its green color and vitreous luster.

## Characteristics Zinc-olivenite is a zinc and copper arsenate, typically forming small, acicular or prismatic crystals, often occurring in radial or fibrous aggregates. Its color ranges from light green to dark green, sometimes with a yellowish tint. Zinc-olivenite specimens are usually small, but their intense color and characteristic forms make them prized by collectors. ## Physical Properties The Mohs hardness of zinc-olivenite is 3 to 4, making it a relatively soft mineral. It has a vitreous luster, and its fracture is uneven to conchoidal. It is transparent to translucent. The density of zinc-olivenite is approximately 4.2-4.3 g/cm³. ## Colors and Varieties Zinc-olivenite occurs mainly in shades of green, from light green, through apple-green, to dark green, sometimes with a yellowish admixture. No specific commercial varieties are distinguished, and its color depends on the proportion of copper and zinc in the structure and the presence of other trace elements. ## History and Name The name zinc-olivenite comes from its chemical composition, indicating the presence of zinc, and its similarity to olivenite, with which it forms an isomorphic series. The mineral was described relatively recently, and its identification was associated with studies of minerals from the oxidation zone of zinc and copper deposits. ## Applications Zinc-olivenite has no industrial applications due to its rarity and small occurrences. It is exclusively a collector's mineral, valued for its aesthetics and rarity.

Properties

Mohs hardness: 3-4
Luster: Szklisty
Streak: Jasnozielona do białawej
Density: 4.2-4.3
Cleavage: Dobra wg {010}
Fracture: Nierówny do muszlowego
Transparency: Przezroczysty do przeświecającego
Crystal system: Jednoskośny

Diagnostic features

## Identification Zinc-olivenite can be identified by its characteristic green color, vitreous luster, and typical acicular or prismatic crystal forms. It often occurs in radial aggregates. Its hardness (3-4 on the Mohs scale) is also a diagnostic feature. ## Distinguishing from Similar Minerals Zinc-olivenite is very similar to olivenite, with which it forms an isomorphic series. Distinguishing these two minerals usually requires chemical analysis, as they are almost identical visually. It can also be confused with some varieties of malachite; however, malachite usually has lower hardness and a characteristic fibrous structure, often with banded coloration. ## Crystal Forms Zinc-olivenite typically forms small, elongated crystals with an acicular or prismatic habit. They often occur in radial aggregates, forming attractive, hedgehog-like aggregates. More isometric crystals are less common.

Geological environment

## Genesis Zinc-olivenite forms in the oxidation zones of polymetallic deposits, especially those rich in zinc and copper. It forms as a result of weathering processes of primary sulfide minerals, where arsenate-rich solutions react with zinc and copper-bearing minerals. ## Mineral Associations Zinc-olivenite often co-occurs with other secondary minerals of the oxidation zone, such as azurite, malachite, hemimorphite, smithsonite, cerussite, as well as olivenite and other copper and zinc arsenates. It can also occur with quartz and limonite. ## Localities Known localities of zinc-olivenite include mines in Tsumeb, Namibia, where some of the best specimens have been found. It also occurs in some mines in Europe, such as the Clara mine in Germany, and in the United States and Mexico.

Rarity

Rare

For collectors

## Quality Criteria The most prized zinc-olivenite specimens are those with intense, vivid green color, well-formed, distinct crystals, and attractive radial aggregates. Larger crystal sizes and the absence of mechanical damage also increase collectible value. Specimens with aesthetic associations with other minerals are also highly valued. ## Popular Localities The Tsumeb mine in Namibia is historically the most important source of high-quality zinc-olivenite specimens. Specimens from this locality are particularly sought after due to their aesthetics and crystal size. Other localities, although less frequently providing specimens of such high quality, are also valued by collectors.

Care and storage

## Cleaning Zinc-olivenite is a relatively soft mineral, so it requires gentle cleaning. It is best to use a soft brush and lukewarm water. Distilled water can also be used to avoid hard water deposits. Avoid vigorous rubbing, which could scratch the mineral's surface. ## What to Avoid Avoid contact of zinc-olivenite with acids and strong bases, which can damage its structure. High temperatures and sudden temperature changes can also be harmful. Prolonged exposure to direct sunlight can lead to color fading. The mineral is sensitive to impacts and abrasion. ## Storage Zinc-olivenite should be stored in a dry place, away from direct sunlight and heat sources. It is best to place it in a closed display case or a box lined with soft material to protect it from dust and mechanical damage. Due to its softness, avoid storing it with harder minerals.

Sources

IMA Mineral List (CNMNC)