Mössbauerite
Chemical formula: Fe<sup>3+</sup><sub>6</sub>O<sub>4</sub>(OH)<sub>8</sub>(CO<sub>3</sub>)·3H<sub>2</sub>O
Mössbauerite is a rare mineral from the hydrotalcite group, forming hexagonal, platy crystals of reddish-brown color with a pearly luster.
Properties
- Mohs hardness
- <2
- Luster
- Pearly
- Streak
- Red-brown
- Density
- 3.05
- Cleavage
- Perfect on {0001}
- Fracture
- Micaceous
- Transparency
- Translucent
- Crystal system
- Trigonal
Diagnostic features
## Identification Identification of mössbauerite is possible almost exclusively using advanced analytical methods, such as Mössbauer spectroscopy (as per its name), X-ray diffraction (XRD), and electron microprobe chemical analysis (EDS/WDS). Visually, in the field or in a collection, it is practically impossible to unequivocally identify. Characteristic, though not unique, are reddish-brown, rosette-like aggregates of fine, hexagonal plates. ## Distinguishing from Similar Minerals It can be confused with other minerals from the hydrotalcite group, such as fougèrite or trænkneryt, as well as other secondary iron minerals with a similar appearance, e.g., goethite or hematite in earthy forms. Certain differentiation requires specialized laboratory tests. ## Crystal Forms Crystals have the form of thin, hexagonal plates. They typically form rosette-like, spherical, or spherulitic aggregates, as well as coatings and efflorescences.
Geological environment
## Genesis Mössbauerite is a secondary mineral, forming as a result of low-temperature hydrothermal processes or weathering. At the type locality (Panzhihua mine), it was found in calcite veins cutting through a titanomagnetite deposit. ## Mineral Associations It co-occurs with minerals such as calcite, aragonite, goethite, magnetite, pyrite, and minerals from the phlogopite group. ## Localities The only confirmed and described occurrence of this mineral is the Panzhihua iron mine in Sichuan Province, China.
Rarity
Very rare
For collectors
## Quality Criteria As a "micromount" type mineral, the quality of a specimen is primarily determined by the abundance and good formation of microscopic aggregates on the rock matrix. The most desirable specimens are those with distinct, well-formed rosettes, contrasting with a light background (e.g., white calcite). The certainty of identification, preferably analytically confirmed, is also important. ## Popular Localities The only source of specimens is the type locality – the Panzhihua mine in China.
Care and storage
## Cleaning Due to the extreme delicacy and small size of the crystals, mechanical cleaning is not recommended and can lead to the destruction of the specimen. Contact with water should be avoided, as it can affect the mineral's hydrated structure. ## What to Avoid All chemicals, especially acids, which will easily dissolve it, should be avoided. The mineral is very soft and sensitive to any mechanical damage, including scratches and abrasion. It should be protected from high temperatures and direct sunlight. ## Storage Mössbauerite specimens should be stored exclusively in specialized, sealed "micromount" boxes, which protect them from dust, moisture, and physical damage. Store in stable room conditions.