Ternesite
Chemical formula: Ca<sub>5</sub>(SiO<sub>4</sub>)<sub>2</sub>(S<sup>6+</sup>O<sub>4</sub>)
Ternesite is a rare calcium silicate-sulfate, forming colorless or pale blue crystals in high-temperature metamorphic rocks.
Properties
- Mohs hardness
- 5
- Luster
- Vitreous
- Streak
- White
- Density
- 2.96
- Cleavage
- Good on {010}
- Fracture
- Uneven
- Transparency
- Transparent to Translucent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Field identification of ternesite is practically impossible due to its rarity and small crystal size. A key indicator is its specific occurrence environment – high-temperature contact metamorphic zones. Definitive identification requires advanced analytical methods, such as X-ray diffraction (XRD) or chemical microanalysis (EDS). ## Distinguishing from Similar Minerals Ternesite can be confused with other colorless minerals occurring in the same paragenesis, such as larnite, spurrite, or some zeolites. Distinguishing it based on visual characteristics is very difficult. It differs from them in chemical composition (simultaneous presence of silicate and sulfate groups) and crystallographic parameters. ## Crystal Forms Ternesite crystallizes in the orthorhombic system. It forms small, tabular or prismatic crystals, often aggregated into small, radial or granular masses. It usually occurs as single, well-formed crystals grown in small rock cavities.
Geological environment
## Genesis Ternesite is a mineral characteristic of contact metamorphism and pyrometamorphism conditions, which are characterized by very high temperatures and low pressures. It forms as a result of the thermal alteration of carbonate rocks, often within limestone xenoliths entrained by volcanic lava. ## Mineral Associations This mineral coexists with other rare high-temperature minerals, such as larnite, spurrite, mayenite, brownmillerite, gehlenite, wollastonite, and diopside. ## Localities The most important ternesite localities in the world are few. The type locality is the Mayen region in the Eifel Mountains, Germany. It is also known from the Hatrurim Formation in Israel, from Jebel Nafusah in Libya, and from several other locations with similar geology worldwide.
Rarity
Very rare
For collectors
## Quality Criteria The collector's value of ternesite specimens primarily depends on the quality and size of the crystals. Specimens with well-formed, transparent crystals that clearly stand out from the matrix rock are most highly prized. Association with other rare minerals is also of great importance, increasing the scientific and aesthetic value of the entire specimen. ## Popular Localities Specimens from the type locality in the Eifel region of Germany are considered classic and most sought after by collectors. They serve as the standard for this mineral.
Care and storage
## Cleaning Ternesite specimens, due to their small size and fragility, should be cleaned very carefully. It is recommended to use a soft brush to remove dust or gentle rinsing in distilled water. Ultrasonic cleaners should be avoided, as they can cause crystal fracturing. ## What to Avoid The mineral is sensitive to acids, which can damage it. Rapid temperature changes and exposure to strong impacts or pressure should also be avoided. ## Storage The best way to store ternesite is to place it in a sealable "micromount" box, which protects delicate crystals from dust, moisture, and mechanical damage. A label with the name and location is crucial for preserving the scientific value of the specimen.