Flurlite
Chemical formula: Zn<sup>2+</sup>Zn<sup>2+</sup><sub>3</sub>Fe<sup>3+</sup>(PO<sub>4</sub>)<sub>3</sub>(OH)<sub>2</sub>(H<sub>2</sub>O)<sub>7</sub>·2H<sub>2</sub>O
Flurlite is a very rare, hydrated zinc iron phosphate, forming aggregates of microscopic, platy crystals of a yellowish-brown color.
Properties
- Mohs hardness
- 2
- Luster
- Vitreous
- Streak
- Light yellow
- Density
- 2.82
- Cleavage
- Perfect on {010}
- Fracture
- Uneven
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of flurlite is based on its characteristic form – radial aggregates of small, platy, yellowish-brown crystals. The key factors are its occurrence locality (Silberberg mine) and co-occurrence with other secondary zinc phosphates. ## Distinguishing from Similar Minerals It can be confused with other secondary phosphate minerals of similar appearance, such as schoonerite or phosphophyllite. Reliable differentiation is almost exclusively possible using advanced analytical methods, such as Raman spectroscopy or X-ray diffraction (XRD). ## Crystal Forms Flurlite forms thin, platy crystals, elongated along [001] and flattened parallel to {010}. These crystals combine into radial, rosette-like, or spherulitic aggregates.
Geological environment
## Genesis Flurlite is a secondary mineral that forms in the oxidation zone of ore deposits, in this case, as a result of the weathering of sphalerite and pyrite. It crystallizes in vugs and on rock surfaces in an environment rich in phosphorus, zinc, and iron. ## Mineral Associations This mineral occurs in association with other rare phosphates, such as phosphophyllite, schoonerite, plimerite, as well as with quartz, pyrite, and sphalerite. ## Localities The only confirmed locality for flurlite in the world (type locality) is the historic Silberberg mine, located near Bodenmais in the Bavarian Forest, Germany.
Rarity
Extremely rare
For collectors
## Quality Criteria The most prized flurlite specimens are those with rich, well-formed, radial aggregates of intense, yellowish-brown color, contrasting with a light host rock. Due to the microscopic size of the crystals, the aesthetics of the entire aggregate are crucial. The presence of rare associated minerals also increases the value of the specimen. ## Popular Localities The only source of specimens is the type locality – the Silberberg mine in Germany. Material from this location is extremely rare and sought after by specialized collectors.
Care and storage
## Cleaning Due to its extreme delicacy and reactivity, cleaning with water or any chemical agents is not recommended. The safest method for dust removal is to use a soft brush or carefully blow air from a safe distance. ## What to Avoid Contact with water, acids, detergents, and other chemicals must be strictly avoided. The mineral is sensitive to changes in temperature and humidity. It should not be heated or exposed to direct sunlight, which can cause dehydration and disintegration. ## Storage Flurlite specimens should be stored under stable conditions, preferably in a sealed, closed "micromount" box, away from dust, humidity, and temperature fluctuations. Due to its fragility, any vibrations and shocks should be avoided.