Namansilite
Chemical formula: NaMn³⁺Si₂O₆
Namansilite is a rare, dark red sodium manganese silicate from the clinopyroxene group, discovered in Russia at the end of the 20th century.
Properties
- Mohs hardness
- 6-7
- Luster
- Vitreous
- Streak
- Brownish violet
- Density
- 3.51
- Cleavage
- {110}
- Fracture
- Uneven
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Helpful features for identifying namansilite include its characteristic brownish-red or purplish-red color, relatively high hardness (6-7), and brownish-purple streak. It occurs in a specific geological environment, which is also an important clue. ## Distinguishing from Similar Minerals Namansilite can be confused with other manganese pyroxenes or pyroxenoids, such as rhodonite. However, rhodonite is usually pink, has a lower hardness (5.5-6.5), and perfect cleavage in two directions. Accurate identification often requires advanced analytical methods, such as X-ray diffraction (XRD). ## Crystal Forms Namansilite most commonly forms granular, fibrous, or radial aggregates. Well-formed, prismatic crystals typical of monoclinic pyroxenes are rarely observed.
Geological environment
## Genesis Namansilite is a mineral formed as a result of metamorphic processes acting on manganese-rich sedimentary deposits. It forms under conditions of high pressure and relatively low temperature, in rocks such as quartzite. ## Mineral Associations This mineral co-occurs with other manganese minerals. In its type locality, it was found in association with quartz, piemontite, alurgite (a manganese-rich variety of muscovite), braunite, and hematite. ## Localities The most important and well-documented occurrences of namansilite are in Russia, in the Khabarovsk Krai, within the Ir-Nimi manganese deposit (Dzhavodi and Zaoblachnyi areas), which is its type locality. Beyond Russia, its occurrence has also been reported in the Cerchiara mine in Italy and in Ehime Prefecture, Japan.
Rarity
Very rare
For collectors
## Quality Criteria The most prized specimens by collectors are those with well-formed, even if small, transparent crystals of intense, purplish-red color. Contrastive placement on a light rock matrix, for example on quartz, also enhances its attractiveness. Due to its rarity, even rich granular or fibrous aggregates are sought after. ## Popular Localities By far the most desirable specimens come from the type locality in Russia (Ir-Nimi deposit), where the best-formed crystals originate. Specimens from other, few localities are also valuable from a collector's perspective due to their rarity.
Care and storage
## Cleaning Namansilite specimens should be cleaned very carefully, using a soft brush to remove dust. If necessary, distilled water can be used, and then the specimen should be thoroughly dried. Ultrasonic cleaners should be avoided, as they can damage aggregates. ## What to Avoid The mineral should be protected from contact with strong acids and other aggressive chemicals. Due to its chemical composition, prolonged exposure to moisture is not recommended. Sudden temperature changes should also be avoided. ## Storage Collectible namansilite specimens are best stored in stable conditions, in closed display boxes or cabinets, away from direct sunlight and dust. It is advisable to isolate it from harder minerals to prevent scratching.