Lun'okite
Chemical formula: MgMn<sup>2+</sup>Al(PO<sub>4</sub>)<sub>2</sub>(OH)·4H<sub>2</sub>O
Lun'okite is a very rare, hydrated magnesium, manganese, and aluminum phosphate, forming tiny, bladed crystals of white or yellowish color.
Properties
- Mohs hardness
- 3
- Luster
- Vitreous
- Streak
- White
- Density
- 2.49
- Cleavage
- Perfect on {010}
- Fracture
- Uneven
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Identification of lun'okite under amateur conditions is practically impossible. It requires advanced analytical methods, such as X-ray diffraction (XRD) and chemical analysis (EDS/WDS). Visually, it can be suspected based on the characteristic form of tiny, bladed crystals forming radial aggregates in the specific geological environment of granitic pegmatites. ## Differentiation from Similar Minerals It can be confused with other rare, secondary phosphates found in pegmatites, such as wardite, eosphorite, or strengite. Differentiation requires specialized laboratory studies, as visual characteristics (color, habit) often overlap. ## Crystal Forms Lun'okite forms elongated, bladed or acicular crystals, often flattened. These crystals usually occur as radial or chaotically tangled aggregates, as well as thin coatings.
Geological environment
## Genesis Lun'okite is a secondary mineral, forming in hydrothermal alteration zones within granitic pegmatites. It forms as a result of the alteration of earlier phosphate minerals, such as lithiophilite, in the presence of magnesium- and aluminum-rich solutions. ## Mineral Associations This mineral co-occurs with other phosphates and pegmatite minerals. At its type locality, it was found in association with lithiophilite, eosphorite, strengite, wardite, quartz, microcline, and albite. ## Localities The only confirmed and described occurrence of lun'okite in the world is its type locality – a pegmatite vein near the Lun'ok River, in the Vayvis-gora massif on the Kola Peninsula, Murmansk Oblast, Russia.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of a lun'okite specimen is primarily assessed based on the richness and visibility of crystal aggregates on the rock matrix. Since the crystals are microscopic, specimens with clearly formed, radial crystal groups are most desirable. Color contrast with the substrate and association with other rare phosphates also increase collecting value. ## Popular Localities The only source of lun'okite specimens is its type locality on the Kola Peninsula in Russia. All materials available on the collector's market originate from this single location.
Care and storage
## Cleaning Specimens containing lun'okite should be handled with utmost care. Cleaning should be limited to very gently removing dust with a soft brush or a photographic air blower. Contact with water should be avoided, as it can damage delicate crystals or associated minerals. ## What to Avoid Ultrasonic cleaners, all chemical agents, acids, and detergents should be absolutely avoided. The mineral is soft and brittle, making it very susceptible to mechanical damage. It should be protected from high temperatures, which can lead to dehydration and structural destruction. ## Storage Lun'okite specimens, due to their microscopic nature and fragility, should be stored in stable conditions, preferably in sealed "micromount" boxes that protect against dust, shocks, and sudden changes in humidity. Exposure to direct sunlight should be avoided.