Therasiaite
Chemical formula: (N<sup>3-</sup>H<sub>4</sub>)<sub>3</sub>KNa<sub>2</sub>Fe<sup>2+</sup>Fe<sup>3+</sup>(S<sup>6+</sup>O<sub>4</sub>)<sub>3</sub>Cl<sub>5</sub>
Therasiaite is an extremely rare sulfate-chloride mineral of iron, potassium, sodium, and ammonium, forming microscopic crystals in volcanic exhalations.
Properties
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
Diagnostic features
## Identification Identifying therasiaite in collector conditions is very difficult and relies mainly on the geological context. A key indicator is its occurrence in products of active, high-temperature volcanic fumaroles. The dark reddish-brown color and the form of thin, tabular crystals with a hexagonal outline are characteristic features. However, definitive identification requires advanced analytical methods, such as X-ray diffraction (XRD) and chemical microanalysis (EDS). ## Distinguishing from Similar Minerals Therasiaite can be confused with other darkly colored volcanic sublimation products, such as fine-grained hematite or other complex sulfates. Differentiation based on visual characteristics is practically impossible. Analysis of associated minerals may be helpful, but only laboratory tests provide a definitive determination. ## Crystal Forms The mineral forms very thin, tabular crystals with a hexagonal outline. These crystals often arrange into rosette-like aggregates, fan-shaped clusters, or form thin crusts and coatings on the surface of volcanic rocks.
Geological environment
## Genesis Therasiaite is a fumarolic mineral. It forms through direct sublimation from hot volcanic gases (exhalations) at temperatures of approximately 450-500°C. It crystallizes on the walls of fumarole channels, reacting with the surrounding volcanic rocks. ## Mineral Associations This mineral occurs in association with other rare fumarolic minerals. The most common associations include adranosite-(Fe), adranosite, alunite, hematite, kremersite, letovicite, and sylvine. ## Localities Only two confirmed occurrences of therasiaite are known worldwide. The first is the type locality – the "Arsenatnaya" fumarole on the second cinder cone of Tolbachik volcano (Kamchatka, Russia). The second is the historical locality from which the mineral took its name – fumaroles on Therasia island (Santorini) in Greece.
Rarity
Extremely rare
For collectors
## Quality Criteria Therasiaite is a mineral almost exclusively for "micromount" collections. The value of a specimen is primarily determined by the quality and size of the microcrystals. Specimens with well-formed, sharp, undamaged tabular crystals are most prized. Rich aggregates forming striking clusters and aesthetic associations with other rare fumarolic minerals, especially if they contrast in color, are also highly valued. ## Popular Localities Both known localities – Tolbachik volcano in Kamchatka and Therasia island in Greece – provide material of scientific importance. However, Tolbachik is the source of the best-formed and most commonly found (on a micro scale) therasiaite specimens, as well as many other unique fumarolic minerals, making it more renowned among specialized collectors.
Care and storage
## Cleaning Therasiaite specimens are extremely delicate and potentially water-soluble. They must absolutely not be cleaned with water, steam, or any chemical liquids. The only safe method for dust removal is very gentle blowing with compressed air from a safe distance or using a soft brush. ## What to Avoid Avoid contact with water and moisture, which can dissolve or damage the crystals. The mineral is thermally unstable – as a sublimation product, it can decompose under high temperatures. Protect it from all chemicals, ultrasound, and direct, strong light. ## Storage Specimens should be stored in a dry place, preferably in tightly sealed "micromount" boxes, which protect against dust, moisture, and mechanical damage. Storage at a stable room temperature is crucial for maintaining the mineral's integrity.