Wildenauerite
Chemical formula: Zn<sup>2+</sup>(Fe<sup>3+</sup><sub>0.5</sub>Mn<sup>2+</sup><sub>0.5</sub>)<sub>2</sub>Mn<sup>2+</sup>Fe<sup>3+</sup>(PO<sub>4</sub>)<sub>3</sub>(OH)<sub>3</sub>(H<sub>2</sub>O)<sub>8</sub>
Wildenauerite is a very rare, hydrated zinc, iron, and manganese phosphate, forming unique, dark green to black, bladed crystals.
Properties
- Mohs hardness
- 3
- Luster
- Vitreous
- Streak
- Pale green
- Density
- 2.86
- Cleavage
- Good on {010}
- Fracture
- Uneven
- Transparency
- Translucent
- Crystal system
- Triclinic
Diagnostic features
## Identification Wildenauerite is identified by its characteristic form - tiny, bladed or acicular crystals forming radial aggregates. Key features also include its dark green to black color, vitreous luster, and co-occurrence with quartz and other phosphates in a specific geological environment. ## Distinguishing from Similar Minerals It can be confused with other dark, acicular minerals from the strunzite group or other phosphates. Final distinction from minerals such as strunzite or laueite requires advanced analytical methods, such as Raman spectroscopy or chemical analysis (EDS), due to subtle differences in composition and structure. ## Crystal Forms Crystals are elongated and flattened (bladed) along the [001] axis and may exhibit striations. They usually form radial, stellate, or haphazardly tangled aggregates. They also occur as single crystals embedded in rock cavities, most often in quartz.
Geological environment
## Genesis Wildenauerite is a secondary mineral that crystallizes under low-temperature hydrothermal alteration conditions. It forms in cavities and fissures within quartz-siderite veins that cut through Devonian sandstones and shales. Its formation is a result of the alteration of earlier minerals in the presence of phosphorus-rich solutions. ## Mineral Associations This mineral occurs in association with quartz, siderite, hematite, goethite, as well as other rare phosphates such as strengite, cacoxenite, beraunite, strunzite, and laueite. ## Localities The only confirmed occurrence of wildenauerite in the world is its type locality - the historic Christian mine in Wildenau, in the Siegerland region, North Rhine-Westphalia, Germany.
Rarity
Very rare
For collectors
## Quality Criteria The most prized wildenauerite specimens are those with well-formed, sharply terminated crystals forming aesthetic, radial aggregates. The contrast with a light quartz background significantly enhances the visual appeal of the specimen. Due to the microscopic nature of the mineral, the size of aggregates and individual crystals is also important, although they rarely exceed a millimeter. ## Popular Localities The only source of specimens is the Christian mine in Wildenau, Germany. Material from this locality is extremely rare and sought after by specialized collectors of systematic minerals and microminerals.
Care and storage
## Cleaning Specimens should be cleaned very carefully, using a soft brush to remove dust. Due to the brittleness and small size of the crystals, wet cleaning and ultrasonic cleaners should be avoided. ## What to Avoid Avoid contact with all chemicals, acids, and detergents. The crystals are brittle and susceptible to mechanical damage, so they should be protected from impacts and scratches. The specimen should not be heated or exposed to sudden temperature changes. ## Storage Wildenauerite specimens, as microminerals, are best stored in specialized "micromount" boxes, which protect them from dust and mechanical damage. Avoid exposure to direct sunlight, although there is no evidence of fading.