Chrysothallite
Chemical formula: K<sub>6</sub>Cu<sup>2+</sup><sub>6</sub>Tl<sup>3+</sup>Cl<sub>17</sub>(OH)<sub>4</sub>·H<sub>2</sub>O
Chrysochalcite is an extremely rare potassium, copper, and thallium halide, forming golden-yellow, platy crystals, known exclusively from the fumaroles of Tolbachik volcano.
Properties
- Luster
- Vitreous
- Streak
- Yellow
- Density
- 3.86
- Cleavage
- Perfect on {001}
- Transparency
- Transparent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Diagnostic features of chrysochalcite include its characteristic golden-yellow color, platy form of microscopic crystals, and specific occurrence environment – products of volcanic exhalations. Final identification is only possible using advanced analytical methods, such as X-ray microanalysis (EDS) and X-ray diffraction (XRD). ## Distinguishing from Similar Minerals Several other yellow fumarolic minerals occur at the same locality. Chrysochalcite can be distinguished based on specific mineral associations and precise chemical analysis, which will show the presence of potassium, copper, and thallium in characteristic proportions. ## Crystal Forms Chrysochalcite forms thin, platy crystals, flattened parallel to {001}. These crystals combine into fan-shaped, radial, or chaotic aggregates and form thin coatings and crusts.
Geological environment
## Genesis Chrysochalcite is a mineral of volcanic origin. It forms by sublimation from hot gases (exhalations) in active fumaroles. It crystallizes at temperatures from 250 to 450°C directly on the surface of volcanic rocks. ## Mineral Associations This mineral co-occurs with other rare halides and oxides formed under similar conditions. The most common associated minerals include tenorite, belloite, eriochalcite, avdoninite, as well as hematite and halite. ## Localities The only confirmed locality of chrysochalcite in the world is its type locality – Arsenatnaya fumarole on the second cinder cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of specimens of this micromineral is primarily assessed based on the abundance of chrysochalcite on the rock matrix. Samples with well-formed, distinct crystals forming aesthetic aggregates are more highly valued. The presence of rare associated minerals on the same specimen is also of great importance. ## Popular Localities The only source of chrysochalcite specimens is Tolbachik volcano in Kamchatka. All samples available on the collector's market come from this single locality.
Care and storage
## Cleaning Chrysochalcite specimens should not be wet cleaned. Any contact with water or other liquids can lead to damage or dissolution. Only very careful, mechanical removal of dust with a soft brush or a low-pressure stream of compressed air is permissible. ## What to Avoid The mineral contains thallium – a highly toxic element. Avoid inhaling dust and direct skin contact. Wash hands thoroughly after each contact with the specimen. Chrysochalcite is likely unstable in humid environments and sensitive to temperature changes. It should be protected from all chemicals. ## Storage Due to its toxicity and delicacy, chrysochalcite specimens must be stored in tightly sealed, dry containers, such as "micromount" boxes or membrane boxes. The container should be clearly labeled with information about the mineral's toxicity. Store away from moisture and heat sources.