Edtollite
Chemical formula: K₂NaCu²⁺₅Fe³⁺O₂(As⁵⁺O₄)₄
Edtollite is a rare copper, iron, sodium, and potassium arsenate, forming small, tabular crystals of a dark green color and vitreous luster.
Properties
- Color
- Brown–black to black
- Luster
- Vitreous
- Streak
- Green
- Density
- 4.26
- Cleavage
- Perfect on {001}
- Fracture
- Brittle
- Transparency
- Transparent to Translucent
- Crystal system
- Triclinic
Diagnostic features
## Identification Field identification of edtollite is impossible. Identification requires advanced laboratory methods, such as chemical analysis (EDS) and X-ray diffraction (XRD). In a collection, it can be preliminarily identified based on its characteristic appearance (dark green, tabular crystals in aggregates) and, most importantly, its locality – it occurs exclusively in the fumaroles of Tolbachik volcano. ## Distinguishing from Similar Minerals It can be confused with other green copper arsenates found in the same environment, such as lammerite, eriostranite, or popovite. Definitive distinction is only possible through chemical and crystallographic analysis. ## Crystal Forms Edtollite forms thin, tabular or bladed crystals, elongated along one of the axes. These crystals often combine into radial, stellate, or rosette-like aggregates.
Geological environment
## Genesis Edtollite is a mineral of volcanic origin, formed by sublimation from volcanic gases in high-temperature fumaroles. It crystallizes in exhalation zones, where hot gases rich in arsenic, copper, and other elements react with the surrounding rocks. ## Mineral Associations This mineral occurs in association with other rare arsenates and sulfates formed under similar conditions. It co-occurs with tenorite, hematite, aphthitalite, langbeinite, sanidine, eriostranite, lammerite, popovite, arsmirandite, and others. ## Localities The only confirmed occurrence of edtollite in the world is its type locality: the Yadovitaya fumarole on the Second Scoria Cone of the North Breach of the Great Fissure Eruption of Tolbachik volcano in Kamchatka, Russia.
Rarity
Very rare
For collectors
## Quality Criteria The quality of an edtollite specimen primarily depends on the richness and size of the crystal aggregates on the matrix. The most prized specimens are those with clearly formed, rosette-like clusters of dark green crystals, contrasting well with the host rock. Due to the microscopic nature of the mineral, even small but well-formed aggregates are considered valuable. ## Popular Localities The only source of edtollite specimens is Tolbachik volcano in Kamchatka. Material from this locality is extremely difficult to obtain due to its remote and dangerous location, making every specimen a valuable acquisition for specialized collectors.
Care and storage
## Cleaning Due to its extreme rarity, small size, and brittleness of crystals, mechanical cleaning is not recommended. Specimens should be protected from dust in sealed containers. ## What to Avoid Avoid contact with chemicals, especially acids, which can damage the mineral. Ultrasonic and steam cleaning should also be avoided. The mineral is stable under normal conditions but should be protected from extreme temperatures. ## Storage Edtollite specimens, typically microscopic crystals on matrix, should be stored in specialized "micromount" boxes to prevent mechanical damage and dust accumulation. Vibrations and shocks should be avoided.