Hanauerite
Chemical formula: Ag<sup>1+</sup>Hg<sup>2+</sup>S<sup>2-</sup>I<sup>1-</sup>
Hanauerite is a very rare silver and mercury sulfide and iodide, forming microscopic, black crystals with a metallic luster.
Properties
- Luster
- Metallic
- Streak
- Black
- Density
- 7.19
- Cleavage
- Perfect on {100}
- Transparency
- Opaque
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Identification of hanauerite is possible only through advanced laboratory methods, such as scanning electron microscopy with chemical analysis (EDS/WDS) and X-ray diffraction (XRD). Under collecting conditions, without specialized equipment, identification is impossible. Characteristic features include its chemical composition (Ag, Hg, S, I), black color, metallic luster, and co-occurrence with other rare mercury and silver minerals. ## Differentiation from Similar Minerals It can be confused with other fine, black minerals with a metallic luster, such as acanthite, cinnabar (metacinnabar variety), or other sulfides. Definitive differentiation requires chemical analysis, which will show the simultaneous presence of silver, mercury, sulfur, and iodine – a unique combination for hanauerite. ## Crystal Forms Hanauerite forms very small, thin, tabular or platy crystals, often grouped into small aggregates. These crystals do not exceed 100 micrometers in length and a few micrometers in thickness.
Geological environment
## Genesis Hanauerite forms as a result of low-temperature hydrothermal processes. It occurs in calcite-quartz veins cutting meta-volcanic rocks (specifically metarhyolites). Its formation is associated with the activity of solutions rich in silver, mercury, sulfur, and iodine. ## Mineral Associations This mineral occurs in association with other, often rare, minerals. In the type locality, its co-occurrence has been noted with calcite, quartz, cinnabar, native mercury, acanthite, pyrargyrite, miargyrite, polybasite, sphalerite, pyrite, chalcopyrite, galena, hematite, and undetermined minerals from the chlorine group and manganese oxides. ## Localities The only confirmed locality of hanauerite in the world is its type locality: the historical mines in the Rotfuchs area, near Weitental, municipality of Bruck an der Mur in Styria, Austria.
Rarity
Extremely rare
For collectors
## Quality Criteria As a microscopic mineral, the main criterion for value for collectors is the quality and richness of the host specimen. The most desirable samples are those on which well-formed, though tiny, hanauerite crystals, analytically identified, are visible. The aesthetics of the rock matrix and the presence of other rare associated minerals are also of great importance. Due to their size, specimens are evaluated under a microscope. ## Popular Localities The only source of hanauerite specimens is its type locality in Austria (Rotfuchs area, Bruck an der Mur, Styria). Material from this location is extremely difficult to obtain and represents a great rarity on the collector's market.
Care and storage
## Cleaning Due to their microscopic size and fragility, hanauerite specimens should not be cleaned mechanically or chemically. The safest method is to remove dust using compressed air from a safe distance. ## What to Avoid Avoid contact with any chemicals, acids, and detergents. It should not be subjected to ultrasound. Specimens should be protected from high temperatures and sudden temperature changes. As a mercury-containing mineral, situations leading to its pulverization and inhalation should be avoided. ## Storage Hanauerite specimens, usually found on a rock matrix, should be stored in stable conditions, in closed, padded "micromount" boxes to protect them from mechanical damage and dust. It is recommended to store them in a dry place, away from direct sunlight.