Koashvite
Chemical formula: Na₆CaTi⁴⁺Si₆O₁₈
Koashvite is a rare sodium, calcium, and titanium silicate, forming transparent, pale yellow crystals, discovered in the Khibiny Massif on the Kola Peninsula.
Properties
- Mohs hardness
- 6
- Luster
- Vitreous
- Streak
- White
- Density
- 2.98
- Fracture
- Conchoidal
- Transparency
- Transparent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Koashvite can be identified by its characteristic pale yellow color, vitreous luster, and mode of occurrence – most often as small, tabular crystals forming radial aggregates. However, a key identifying factor is its unique geological environment – its occurrence in nepheline pegmatites of alkaline massifs. ## Distinguishing from Similar Minerals It can be confused with other rare silicates from the Khibiny and Lovozero massifs, such as lomonosovite or eudialyte, but it differs from them in color, crystal habit, and physical properties. Precise identification requires advanced analytical methods, such as X-ray diffraction (XRD). ## Crystal Forms Koashvite crystals are usually small, with a tabular or short-prismatic habit. They often form radial or stellate aggregates, as well as granular clusters within the host rock.
Geological environment
## Genesis Koashvite is a mineral of magmatic origin, crystallizing in the late stages of the formation of highly differentiated, alkaline intrusions. It forms in nepheline pegmatites and syenites that cut through the Khibiny and Lovozero massifs. ## Mineral Associations This mineral coexists with other rare alkaline minerals. Its paragenesis may include nepheline, microcline, aegirine, eudialyte, lorenzenite, lomonosovite, sodalite, and natrolite. ## Localities Koashvite is an extremely rare mineral, and its occurrence has been confirmed in only two places in the world, both located on the Kola Peninsula in Russia. These are the Khibiny Massif (Mount Koashva – type locality) and the adjacent Lovozero Massif.
Rarity
Very rare
For collectors
## Quality Criteria The most prized specimens by collectors are those with well-formed, sharp crystals creating aesthetic, radial aggregates. The intensity of the pale yellow color and the transparency of the crystals are important. Contrast with darker matrix rock (e.g., with aegirine) also enhances the visual appeal of the specimen. Due to the small size of the crystals, even small but well-formed aggregates are considered valuable. ## Popular Localities The only source of koashvite specimens available on the collector's market is the Kola Peninsula in Russia. The best specimens come from the Koashva quarry in the Khibiny Massif, which is its type locality.
Care and storage
## Cleaning Koashvite specimens should be cleaned very carefully, using a soft brush to remove dust. If necessary, compressed air can be used. Avoid washing in water, especially with detergents, due to the risk of damaging delicate aggregates. ## What to Avoid Avoid contact with acids and other strong chemicals. The mineral is brittle, so it should be protected from impacts and falls. There are no specific recommendations regarding light or temperature exposure, but it is generally advisable to avoid extreme conditions. ## Storage The safest way to store koashvite is to place it in a closed display box, lined with soft foam. This protects the specimen from dust, mechanical damage, and contact with other minerals that could scratch it.