Javorieite
Chemical formula: KFe<sup>2+</sup>Cl<sub>3</sub>
Javoryite is an extremely rare potassium iron chloride, forming microscopic, brown crystals in volcanic exhalations.
Properties
- Luster
- Vitreous
- Streak
- Light brown
- Density
- 2.70
- Cleavage
- Perfect on {010}
- Transparency
- Translucent to Opaque
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Amateur identification of javoryite is practically impossible. Key features include its specific occurrence environment (volcanic fumaroles), brown color, and small, bladed crystals. Definitive identification requires advanced analytical methods such as X-ray diffraction (XRD) or chemical microanalysis (EDS). ## Differentiation from Similar Minerals Javoryite can be confused with other rare iron chlorides and oxides found in fumaroles. Differentiation from minerals such as kremersite or eryosfalite requires specialized laboratory equipment. Analysis of associated minerals can be helpful. ## Crystal Forms It forms elongated, bladed or acicular crystals with a rectangular cross-section. These crystals often arrange into small, radial or chaotic aggregates and crusts.
Geological environment
## Genesis Javoryite is a fumarolic mineral. It forms by sublimation from hot volcanic gases (exhalations) at temperatures ranging from 200 to 400°C. It crystallizes directly on the surfaces of volcanic rocks near fumarole vents. ## Mineral Associations This mineral co-occurs with other halides and sulfates formed under similar conditions. It is most commonly associated with sylvite, halite, kremersite, rinneite, and hematite. ## Localities As an extremely rare mineral, javoryite has been confirmed in only a few locations worldwide. The main localities are: - Javorie stratovolcano in central Slovakia (type locality). - Fumaroles of Tolbachik volcano on the Kamchatka Peninsula, Russia.
Rarity
Extremely rare
For collectors
## Quality Criteria Javoryite is a mineral exclusively for micromineral collectors (so-called "micromounts"). The value of a specimen is determined by the richness and abundance of crystals on the rock matrix, their size (although always sub-millimeter dimensions), sharpness of form, and lack of damage. Specimens with well-formed, single crystals or aesthetic aggregates are highly prized. ## Popular Localities The most known and valued specimens come from two main localities: Tolbachik volcano in Kamchatka, which provided rich micromineralogical specimens, and the type locality in Slovakia.
Care and storage
## Cleaning This mineral is hygroscopic and likely water-soluble. **Absolutely avoid contact with water and other liquids.** Cleaning is highly inadvisable. If dust removal is necessary, a soft, dry brush or careful blowing with a photographic air blower can be used. ## What to Avoid Above all, avoid moisture, water vapor, and direct contact with water, which can permanently damage or destroy the specimen. Ultrasonic cleaning and exposure to any chemicals are also not recommended. Store away from heat sources. ## Storage Javoryite specimens must be stored in dry conditions. It is recommended to keep them in tightly sealed containers, such as "perky boxes," preferably with a desiccant (silica gel). Protect from dust and sudden temperature changes.