Nosean
Chemical formula: Na<sub>8</sub>(Si<sub>6</sub>Al<sub>6</sub>)O<sub>24</sub>(S<sup>6+</sup>O<sub>4</sub>)·H<sub>2</sub>O
A silicate from the feldspathoid group, most often forming small, hexagonal crystals of gray or bluish color.
Properties
- Mohs hardness
- 5.5-6
- Luster
- Vitreous to greasy
- Streak
- White
- Density
- 2.22-2.40
- Cleavage
- Indistinct on {110}
- Fracture
- Uneven to conchoidal
- Transparency
- Transparent to translucent
- Crystal system
- Cubic
Diagnostic features
## Identification Nosean is most often identified by its occurrence in a specific geological environment – alkaline volcanic rocks, such as phonolites. In granular form, it is difficult to identify without specialized examination. A characteristic feature is its reaction with hydrochloric acid, in which it gels. Under ultraviolet light, it may exhibit reddish-orange or pink fluorescence. ## Distinguishing from Similar Minerals Nosean is very difficult to distinguish from other minerals of the sodalite group (sodalite, haüyne, lazurite) based on visual characteristics. Haüyne is usually more intensely blue. Sodalite can also be blue but has a slightly different chemical composition. Definitive differentiation requires advanced analytical methods, such as chemical analysis (EDS) or X-ray diffraction (XRD). ## Crystal Forms Nosean crystals, though rare, have an isometric habit. Most often, they are rhombic dodecahedra, sometimes cubes, often with modified and rounded faces. It usually occurs as disseminated, rounded grains in the rock.
Geological environment
## Genesis Nosean is a magmatic mineral, crystallizing from lava and magma rich in sodium and other alkaline elements, and simultaneously poor in silica. It forms in the late stages of crystallization in volcanic and subvolcanic rocks, such as phonolites and nephelinites. ## Mineral Associations This mineral often co-occurs with other feldspathoids, such as leucite, nepheline, sodalite, and haüyne. It is also accompanied by sanidine, aegirine, eudialyte, and various minerals from the amphibole and pyroxene groups. ## Localities The most important and classic localities for nosean are in the Eifel volcanic complex in Germany (especially in the area of Lake Laacher See). It also occurs in the Mont-Dore and Cantal massifs in France, on Mount Vesuvius in Italy, in the Canary Islands (Spain), in the Ilimaussaq complex in Greenland, and in Colorado and Arkansas in the USA.
Rarity
Not very common
For collectors
## Quality Criteria The most prized by collectors are specimens with well-formed, sharp-edged crystals of intense, bluish color, set on a contrasting rock matrix. Due to the rarity of large crystals, even small but well-formed specimens are desirable. The presence of rare associated minerals enhances its attractiveness. ## Popular Localities Specimens considered the best in the world come from quarries in the Eifel volcanic region in Germany, especially from the vicinity of Mendig and Maria Laach. These are classic localities from which type specimens for this mineral originate.
Care and storage
## Cleaning Nosean specimens should be cleaned very carefully, using a soft brush to remove dust. For heavier soiling, a damp cloth can be used, but prolonged contact with water should be avoided. Ultrasonic cleaners or steam cleaners are not recommended. ## What to Avoid Nosean is sensitive to acids, which cause its decomposition with the release of hydrogen sulfide (rotten egg smell) and the formation of silica gel. It should be protected from contact with household and laboratory chemicals. Avoid sudden temperature changes and strong impacts. ## Storage Specimens should be stored in a dry place, away from direct sunlight, which, however, does not cause fading in its case. It is best to keep it in separate boxes or on stands to avoid scratching by harder minerals.