Rusakovite
Chemical formula: (Fe<sup>3+</sup>,Al)<sub>5</sub>(V<sup>5+</sup>O<sub>4</sub>)<sub>2</sub>(OH)<sub>9</sub>·3H<sub>2</sub>O
Rusakovite is a rare iron and aluminum vanadate, forming small, spherical aggregates with a characteristic yellowish-brown color.
Properties
- Mohs hardness
- 1
- Luster
- Dull
- Streak
- Yellow-brown
- Density
- 3.45
- Cleavage
- None
- Fracture
- Earthy
- Transparency
- Opaque
- Crystal system
- Tetragonal
Diagnostic features
## Identification Key diagnostic features include its occurrence as small, radial spheres, characteristic yellowish-brown color, dull luster, and extreme softness. Its association with other vanadates in sedimentary rocks is also an important indicator. ## Differentiation from Similar Minerals Rusakovite can be confused with other secondary vanadium minerals, such as carnotite or tyuyamunite, which, however, usually have a brighter, yellow color and often exhibit fluorescence under UV light, which rusakovite does not. It can also be mistaken for other earthy iron oxides (e.g., goethite), but chemical tests will reveal the presence of vanadium. ## Crystal Forms This mineral does not form well-developed crystals. It occurs exclusively as spherulitic (globular) aggregates with a radial internal structure and as earthy coatings and masses.
Geological environment
## Genesis Rusakovite is a secondary mineral, forming in the oxidation zones of vanadium deposits. Its formation is associated with the weathering of primary vanadium-bearing minerals under strongly oxidizing conditions, in the presence of iron and aluminum. It is most commonly found in sedimentary carbonate-siliceous rocks. ## Mineral Associations This mineral co-occurs with other vanadium minerals, such as hewettite, pascoite, satpaevite, as well as gypsum, calcite, and clay minerals. ## Localities The most important and typical occurrence of rusakovite is the Kurumsak vanadium deposit in the Karatau Range in southern Kazakhstan. This is the only confirmed and well-documented locality for this mineral worldwide.
Rarity
Extremely rare
For collectors
## Quality Criteria The most desirable specimens for collectors are those with well-formed, distinct spherules (globules) of an intense, yellowish-brown color, contrasting with the rock matrix. The size of the aggregates and their abundance on the specimen's surface significantly increase its value. Due to its rarity, even small but distinct masses are prized. ## Popular Localities The only source of collector specimens is the historical type locality – the Kurumsak deposit in Kazakhstan.
Care and storage
## Cleaning Due to its extreme brittleness and softness, mechanical cleaning is not recommended. If absolutely necessary, compressed air can be used from a distance to blow off loose dust. Contact with water should be avoided, as it can affect the mineral's hydrated structure. ## What to Avoid All chemicals, especially acids, which will easily dissolve it, should be avoided. The mineral is very soft, so it must be protected from any touch, abrasion, or vibrations. Changes in humidity and temperature should be avoided. ## Storage Rusakovite specimens should be stored in stable conditions, in closed "micromount" boxes, to protect them from mechanical damage and dust. They should not be exposed to direct sunlight or moisture.