Liottite
Chemical formula: Na<sub>16</sub>Ca<sub>8</sub>Si<sub>18</sub>Al<sub>18</sub>O<sub>72</sub>(S<sup>6+</sup>O<sub>4</sub>)<sub>5</sub>Cl<sub>4</sub>
A rare mineral from the cancrinite group, forming small, hexagonal crystals with a vitreous luster, found in Vesuvius lavas.
Properties
- Mohs hardness
- 5
- Luster
- Vitreous
- Streak
- White
- Density
- 2.43
- Cleavage
- Imperfect on {1010}
- Fracture
- Uneven to conchoidal
- Transparency
- Transparent to translucent
- Crystal system
- Hexagonal
Diagnostic features
## Identification Liottite can be identified by its characteristic, small, hexagonal crystals with a prismatic habit. Key features include its vitreous luster, occurrence in a specific geological environment (cavities in lavas), and co-occurrence with other minerals from the cancrinite-sodalite group. ## Distinguishing from Similar Minerals It can be confused with other colorless minerals from its group, such as afghanite, cancrinite, or microsommite, which form similar crystals in the same environment. Definitive distinction often requires advanced analytical methods, such as X-ray diffraction (XRD) or chemical analysis (EDS), due to subtle differences in composition and structure. ## Crystal Forms It forms elongated, hexagonal prismatic crystals, terminated by a hexagonal pyramid. Crystals are usually small, reaching at most a few millimeters in length.
Geological environment
## Genesis Liottite is a mineral of volcanic origin. It forms in the late stages of crystallization in cavities (druses and geodes) within phonolitic and tephritic lavas, which are rich in alkalis and poor in silica. It crystallizes from hot, gas-rich volcanic fluids. ## Mineral Associations It most commonly co-occurs with other feldspathoid minerals, such as haüyne, nosean, leucite, and sanidine. It is also accompanied by other rare minerals, such as afghanite, cancrinite, davyn, biotite, and magnetite. ## Localities The most important and classic localities for this mineral are in Italy. These include the type locality in Pitigliano (Tuscany) and the Somma-Vesuvius volcanic complex (Campania), from which many well-formed microcrystals originate. It is also found in the Vico volcanic complex in Lazio. Outside of Italy, its presence has been noted in the Eifel Mountains in Germany.
Rarity
Very rare
For collectors
## Quality Criteria Most valued by collectors are specimens with sharp, well-formed, and transparent crystals that stand out clearly from the matrix rock. The absence of damage and an attractive association with other rare minerals, such as haüyne or afghanite, are important. Due to the small size of the crystals, specimens suitable for microscopic viewing (so-called "micromounts") are standard. ## Popular Localities The most sought-after specimens come from classic Italian localities, especially from the Vesuvius region, which yields the best-formed microcrystals.
Care and storage
## Cleaning Liottite specimens should be cleaned very carefully, using a soft brush to remove dust. Due to its brittleness and potential reactivity, avoid washing in water, and especially avoid using ultrasonics, which could damage the delicate crystals. ## What to Avoid Avoid contact with acids and other chemicals that may react with the mineral's complex composition. The crystals are brittle, so protect them from impacts and scratching. There are no specific recommendations regarding light or temperature, but standard protection against extreme conditions is advisable. ## Storage The safest way to store liottite is to place it in a closed display box, lined with soft material, to prevent mechanical damage. This also protects the specimen from dust and contaminants.