Donowensite
Chemical formula: Ca(H₂O)₃Fe³⁺₂(V⁵⁺₂O₇)₂
Donowensite is an extremely rare, orange-brown iron and calcium vanadate, forming microscopic, bladed crystals.
Properties
- Mohs hardness
- 3
- Color
- Yellow
- Luster
- Vitreous
- Streak
- Orange
- Density
- 2.97
- Cleavage
- on {001}; also very good on {100} and {010}
- Fracture
- Splintery
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
Diagnostic features
## Identification Identification of donowensite is practically possible only through advanced analytical methods, such as Raman spectroscopy or chemical analysis using an electron microprobe (EDS/WDS). Visually, under high magnification, characteristic orange-brown, bladed crystals forming rosette-like aggregates can be observed. ## Distinguishing from Similar Minerals It can be confused with other secondary vanadium minerals of similar color and habit, such as carnotite, tyuyamunite, or pascoite. Definitive distinction requires specialized chemical analysis to confirm the unique composition of donowensite. ## Crystal Forms Donowensite forms very small, thin, bladed crystals, elongated in one direction. These crystals often combine into radial or rosette-like aggregates, and also form thin coatings on the rock.
Geological environment
## Genesis Donowensite is a secondary mineral, formed in the oxidation zone of uranium-vanadium deposits. It forms as a result of weathering processes of primary vanadium minerals in a calcium-rich environment. It occurs in vugs and on fracture surfaces in sandstones. ## Mineral Associations This mineral co-occurs with other secondary vanadate minerals, such as carnotite, tyuyamunite, pascoite, as well as gypsum and montmorillonite. ## Localities The only confirmed locality of donowensite in the world (type locality) is the Packrat Mine, located in the Gateway area, Mesa County, Colorado, USA.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of a donowensite specimen primarily depends on the richness and development of its microscopic crystals. Specimens with clearly formed, rosette-like aggregates of intense, orange-brown color, contrasting well with the host rock, are most valued. The absence of damage to the delicate crystals is also important. ## Popular Localities The only source of donowensite specimens is its type locality – the Packrat Mine in Colorado, USA. All specimens available on the collector's market originate from this single location.
Care and storage
## Cleaning Due to the extreme fragility and microscopic size of the crystals, mechanical cleaning is highly inadvisable. Specimens should be protected from dust by storing them in sealed containers. If cleaning is absolutely necessary, compressed air can be used from a very long distance and at low pressure. ## What to Avoid Avoid contact with water, chemicals, ultrasound, and all forms of mechanical cleaning (brushes, cloths). The crystals are extremely brittle and easily damaged or detached from the substrate. Rapid temperature changes should also be avoided. ## Storage Donowensite specimens should be stored exclusively in specialized "micromount" boxes that protect them from physical damage and dust. Vibrations and shocks should be avoided.