Akasakaite-(Ce)
Chemical formula: CaCe<sup>3+</sup>(Al<sub>2</sub>Mn<sup>2+</sup>)(Si<sub>2</sub>O<sub>7</sub>)(SiO<sub>4</sub>)O(OH)
Akasakaite-(Ce) is an extremely rare mineral of the epidote group, a complex cerium, calcium, aluminum, and manganese silicate, occurring as dark brown grains.
Properties
- Mohs hardness
- 6
- Luster
- Vitreous
- Streak
- Light brown
- Density
- 4.11
- Cleavage
- Good on {001}
- Transparency
- Translucent to Opaque
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of Akasakaite-(Ce) based on visual characteristics is impossible. Due to its occurrence as fine, black grains, it requires advanced analytical techniques. Definitive identification is only possible through chemical analysis (e.g., using an electron microprobe - EDS/WDS) to confirm its unique composition, especially the presence and proportions of cerium, manganese, and aluminum. ## Distinguishing from similar minerals This mineral can be confused with other dark epidote-group minerals, such as allanite-(Ce), or with other rare manganese silicates. Certain differentiation from these requires specialized chemical and crystallographic analysis. ## Crystal forms Akasakaite-(Ce) forms exclusively irregular, anhedral grains up to 0.5 mm in size. Its occurrence as well-formed crystals has not yet been observed.
Geological environment
## Genesis This mineral forms under conditions of contact metamorphism. Its genesis is associated with high-temperature, low-pressure skarns that developed in Paleozoic limestones within metamorphosed manganese ore deposits. ## Mineral associations At the type locality, Akasakaite-(Ce) coexists with minerals such as celsian, anandite, cymrite, hedyphane, johannsenite, rhodonite, calcite, and quartz. ## Localities The only confirmed occurrence of this mineral in the world is its type locality – the Fuka mine, located in Bitchu-cho, Takahashi City, Okayama Prefecture on Honshu Island, Japan.
Rarity
Extremely rare
For collectors
## Quality criteria As a microscopic mineral, the collector's value of Akasakaite-(Ce) is determined by the certainty of its identification. The most valuable specimens are those where the mineral grains are clearly visible, as large as possible, and associated with other rare minerals from that locality. The richness of the aggregate and the aesthetics of the host specimen also enhance its attractiveness. ## Popular localities The only source of specimens is the Fuka mine in Japan. Material from this locality is highly prized by collectors specializing in rare minerals and microminerals.
Care and storage
## Cleaning Specimens of this mineral are typically microscopic grains on a host rock. Cleaning is not recommended and is usually not possible without specialized equipment. If dust removal is necessary, a photographic air blower can be used. ## What to avoid Avoid contact with chemicals, especially strong acids. Specimens should not be cleaned in ultrasonic cleaners. Protect them from shocks and mechanical damage. ## Storage The safest storage method is to place the specimen in a specialized micromount box, which protects it from dust, moisture, and physical damage.