Turtmannite
Chemical formula: Mn<sup>2+</sup><sub>25</sub>O<sub>5</sub>(V<sup>5+</sup>O<sub>4</sub>)<sub>3</sub>(SiO<sub>4</sub>)<sub>3</sub>(OH)<sub>20</sub>
An extremely rare mineral from the silicate and vanadate group, forming tabular crystals of a reddish-brown color.
Properties
- Mohs hardness
- 3
- Luster
- Vitreous to Submetallic
- Streak
- Red-brown
- Density
- 3.65
- Cleavage
- Perfect on {001}
- Fracture
- Uneven
- Transparency
- Translucent to Opaque
- Crystal system
- Triclinic
Diagnostic features
## Identification Key diagnostic features of turtmannite include its characteristic habit of reddish-brown, tabular rosettes, low hardness, and perfect cleavage. The luster, described as vitreous to submetallic, is also helpful. However, the most important indicator is its origin from a very limited number of localities and its co-occurrence with other manganese minerals. ## Differentiation from Similar Minerals Turtmannite can be confused with other rare, reddish-brown manganese minerals with a lamellar habit. Visually, it may resemble some microscopic forms of hematite or pyrophanite, but it differs from them in crystal habit and occurrence environment. Positive identification is almost exclusively possible using advanced analytical methods, such as X-ray diffraction (XRD) or chemical microanalysis (EDS). ## Crystal Forms Crystals are very small, thin-tabular, with a hexagonal outline. They most often form fan-shaped or rosetted aggregates, less frequently occurring as single, dispersed lamellae on the rock matrix.
Geological environment
## Genesis Turtmannite is a mineral of metamorphic origin. It forms in manganese ore deposits that have undergone metamorphism under amphibolite facies conditions. It occurs in quartz-rich lenses and rock layers within these deposits. ## Mineral Associations This mineral occurs in association with other manganese minerals. The most common associations include braunite, tephroite, rhodonite, spessartine, quartz, as well as other rare manganese vanadates and silicates, such as parsettensite or piemontite. ## Localities It is an extremely rare mineral, known from only a few locations worldwide. The most important and type locality is Pipji-Alp in the Turtmanntal valley in Switzerland. It has also been reported in the nearby Fianel mine in the Val Ferrera valley in Graubünden, also in Switzerland.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of turtmannite specimens, which are almost exclusively micromounts, is assessed based on several criteria. Specimens with well-formed, sharp crystals forming aesthetic rosettes or fans are most highly valued. The intensity and saturation of the reddish-brown color are important. The attractiveness is also enhanced by the contrasting placement of aggregates on a light quartz matrix and the presence of other rare associated minerals. ## Popular Localities The vast majority of the best and most sought-after specimens come from the type locality – Pipji-Alp in the Turtmanntal valley in Switzerland. This is a classic locality for collectors specializing in rare minerals and micromounts.
Care and storage
## Cleaning Turtmannite specimens are extremely delicate and should be handled with the utmost care. For dust removal, it is best to use canned compressed air, applied from a safe distance. Any mechanical cleaning, including with brushes, should be avoided. Washing in water is not recommended, and if absolutely necessary, only distilled water should be used, and the specimen allowed to air dry naturally. ## What to Avoid Ultrasonic cleaners, which would destroy the brittle crystals, must be absolutely avoided. The mineral is sensitive to all chemicals, including acids and bases. It should be protected from impacts and abrasions due to its low hardness and perfect cleavage. ## Storage Turtmannite should be stored in specialized micromount boxes that protect it from dust, shocks, and contact with other specimens. It is not sensitive to light, but exposure should occur under stable humidity and temperature conditions.