Cadvanite
Chemical formula: Cd(V⁵⁺O₃)₂
Cadvanite is a very rare cadmium vanadate mineral, forming microscopic, acicular yellow crystals.
Properties
- Mohs hardness
- 2.5-3
- Color
- brownish-yellow
- Luster
- Vitreous to silky
- Streak
- pale yellow
- Density
- 4.210
- Cleavage
- two cleavages, possibly [100] and [001].
- Fracture
- Splintery
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Cadvanite identification is based on its characteristic form – tiny, acicular crystals forming radial aggregates – and its intense yellow color. Identification is practically only possible under a stereoscopic microscope. Final confirmation requires advanced analytical methods, such as EDS spectroscopy or X-ray diffraction (XRD), due to its co-occurrence with other rare vanadates. ## Distinguishing from Similar Minerals Cadvanite can be confused with other secondary yellow vanadium minerals, such as carnotite, tyuyamunite, or pascoite. "Eyeball" differentiation is practically impossible. Key factors are the occurrence location (mineral associations) and chemical analysis confirming the presence of cadmium as the main cation. ## Crystal Forms Cadvanite forms elongated, acicular or bladed crystals, often flattened. They usually occur as radial or stellate aggregates, as well as single, scattered needles on the rock surface.
Geological environment
## Genesis Cadvanite is a secondary mineral, forming in the oxidation zones of uranium-vanadium deposits in sedimentary rocks (sandstones). Its crystallization occurs as a result of weathering processes of primary ore minerals under conditions of low temperatures and pressures. ## Mineral Associations This mineral occurs in association with other rare vanadates. In its type locality (Burro Canyons, Colorado), it was found in association with metarossite, pascoite, sherwoodite, as well as montroseite and other vanadium oxides. ## Localities The only confirmed and described occurrence of cadvanite in the world is its type locality – the uranium mine in the Burro Canyons area, San Miguel County, Colorado, USA.
Rarity
Extremely rare
For collectors
## Quality Criteria Due to its extreme rarity and microscopic size, any authenticated cadvanite specimen is valuable to specialized collectors of rare minerals (so-called "micromounters"). The most highly prized specimens are those with rich, well-formed, radial aggregates of intense color, clearly contrasting with the host rock. Aesthetic association with other rare minerals is also important. ## Popular Localities The only source of cadvanite specimens is its type locality in Colorado, USA. Material from this location is extremely difficult to obtain and appears on the collector's market sporadically.
Care and storage
## Cleaning Cadvanite specimens are extremely delicate and small, therefore they should not be cleaned mechanically or chemically. Any attempts at cleaning risk irreversible damage to the microscopic crystals. If dust removal is necessary, it can be done very carefully with a soft brush or by blowing air from a safe distance. ## What to Avoid Contact with water, chemicals, ultrasound, and sudden temperature changes must be strictly avoided. The crystals are brittle and sensitive to vibrations and shocks. ## Storage Cadvanite specimens should be stored exclusively in specialized, sealed "micromount" boxes that protect them from dust, mechanical damage, and humidity. They should not be exposed to direct sunlight.