Perbøeite-(La)
Chemical formula: (CaLa<sub>3</sub>)(Al<sub>3</sub>Fe<sup>2+</sup>)[Si<sub>2</sub>O<sub>7</sub>][SiO<sub>4</sub>]<sub>3</sub>O(OH)<sub>2</sub>
Perbøeite-(La) is a very rare mineral from the epidote group, characterized by a complex chemical composition with dominant lanthanum.
Properties
- Mohs hardness
- 6-7
- Luster
- Vitreous
- Streak
- Light brown
- Density
- 4.55
- Cleavage
- Good on {001}
- Fracture
- Uneven
- Transparency
- Opaque
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of perbøeite-(La) is impossible without advanced analytical methods. This requires chemical analysis (e.g., electron microprobe - EDS/WDS) to confirm the complex composition with dominant lanthanum, and X-ray diffraction to determine the crystal structure. Visually, it is simply a dark, vitreous grain in the rock. ## Distinguishing from Similar Minerals It can be confused with other minerals from the epidote group, such as allanite, dollaseite, or ferriallanite, as well as other dark rock-forming minerals. Definitive distinction is only possible based on detailed laboratory analyses. ## Crystal Forms It forms poorly developed, subhedral grains, which may occur as small aggregates.
Geological environment
## Genesis Perbøeite-(La) forms as a result of metasomatic processes within nepheline syenites. In its type locality (Mount Eveslogchorr), it occurs in hydrothermal veins cutting foyaite (a variety of nepheline syenite). ## Mineral Associations This mineral is associated with minerals such as microcline, nepheline, aegirine, eudialyte, lorenzenite, lamprophyllite, rinkite, fluorite, as well as other minerals from the epidote group. ## Localities The only confirmed occurrence of perbøeite-(La) in the world is its type locality – Mount Eveslogchorr in the Khibiny Massif on the Kola Peninsula, Russia.
Rarity
Extremely rare
For collectors
## Quality Criteria As a micromineral, perbøeite-(La) is not evaluated according to typical criteria such as color or clarity. Specimens where the mineral grains are as well-formed as possible and clearly visible against the host rock are of the highest value. Crucial are also correct analytical identification and the richness of associated minerals on the sample. ## Popular Localities The only source of specimens is the Khibiny Massif on the Kola Peninsula, Russia.
Care and storage
## Cleaning Specimens of this mineral are typically small grains embedded in rock. Cleaning is not recommended to avoid damaging the delicate crystals and their surroundings. If necessary, compressed air can be used to remove dust. ## What to Avoid Avoid contact with chemicals, acids, and ultrasonic cleaners, which can damage both the mineral itself and the host rock. ## Storage Micromount specimens of perbøeite-(La) should be stored in specialized boxes (so-called micromount boxes), protecting them from dust, moisture, and mechanical damage.