Megacyclite
Chemical formula: KNa<sub>8</sub>Si<sub>9</sub>O<sub>18</sub>(OH)<sub>9</sub>·19H<sub>2</sub>O
Megacyclite is a very rare, hydrated potassium and sodium silicate, forming colorless, platy crystals with a unique, cyclic structure.
Properties
- Mohs hardness
- 2
- Luster
- Vitreous
- Streak
- White
- Density
- 2.05
- Cleavage
- Perfect on {0001}
- Fracture
- Uneven
- Transparency
- Transparent
- Crystal system
- Trigonal
Diagnostic features
## Identification Identification of megacyclite is practically only possible based on chemical analysis (EDS) and structural analysis (XRD) due to its microscopic size and occurrence in complex parageneses. A helpful feature can be strong, white fluorescence under UV light, but this is not unique to this mineral. ## Distinguishing from similar minerals Megacyclite coexists with other rare sodium silicates, such as grumantite, natrosilite, and rewitzerite. Distinguishing it from these minerals "by eye," even under a microscope, is impossible without advanced analytical techniques. Its platy habit and radial aggregates can be a clue, but not a definitive feature. ## Crystal forms Megacyclite forms thin, platy crystals with a hexagonal outline, often arranged in radial or fan-shaped aggregates.
Geological environment
## Genesis Megacyclite forms under hydrothermal conditions in ultra-alkaline pegmatites of highly differentiated nepheline syenite massifs. It crystallizes in the late stage of crystallization, in voids and fissures, as a result of the interaction of post-magmatic solutions with previously crystallized minerals. ## Mineral associations This mineral coexists with other rare alkaline minerals. In its type locality (Lovozero Massif), it was found in association with aegirine, ussingite, natrosilite, grumantite, rewitzerite, villiaumite, and sphalerite. ## Localities The only confirmed occurrence of megacyclite in the world is its type locality - Mount Alluaiv in the Lovozero Massif, on the Kola Peninsula in Russia.
Rarity
Extremely rare
For collectors
## Quality criteria The quality of megacyclite specimens is assessed solely in the context of micromount collecting. The most highly valued specimens are those that show well-formed, undamaged, radial aggregates of platy crystals, clearly standing out from the host rock. The richness of the association with other rare minerals also increases the value of the specimen. ## Popular localities The only source of megacyclite specimens is the Lovozero Massif on the Kola Peninsula in Russia.
Care and storage
## Cleaning Megacyclite specimens should be cleaned with the utmost care, using only compressed air to remove dust. Any contact with water, even distilled, or other chemicals is absolutely inadvisable due to its solubility. ## What to avoid Avoid contact with water and any liquids that may dissolve or damage the delicate crystals. The mineral is very brittle, so avoid shocks, vibrations, and touching. Protect it from high temperatures and changes in humidity. ## Storage Microscopic specimens (micromounts) should be stored in sealed, airtight boxes to protect them from dust, moisture, and mechanical damage. Display should only be done under a microscope.