Aerinite
Chemical formula: (Ca,Na)<sub>6</sub>(Fe<sup>3+</sup>,Fe<sup>2+</sup>,Mg,Al)<sub>4</sub>(Al,Mg)<sub>6</sub>Si<sub>12</sub>O<sub>36</sub>(OH)<sub>12</sub>(CO<sub>3</sub>)·12H<sub>2</sub>O
Aerinite is a silicate mineral, valued for its characteristic, intense blue coloration and fibrous habit.
Properties
- Mohs hardness
- 3
- Luster
- Waxy
- Streak
- Light blue
- Density
- 2.47 - 2.51
- Cleavage
- None
- Fracture
- Uneven
- Transparency
- Translucent to opaque
- Crystal system
- Trigonal
Diagnostic features
## Identification The most important diagnostic feature of aerinite is its intensely blue color combined with low hardness (approximately 3 on the Mohs scale) and fibrous or compact structure. Its light blue streak is also characteristic. It occurs in a specific geological environment – in altered basic rocks. ## Distinguishing from Similar Minerals Aerinite is sometimes confused with other blue minerals: - **Azurite**: It is harder (3.5-4) and reacts vigorously with hydrochloric acid, effervescing. Aerinite does not exhibit such a reaction. - **Lazulite**: It is significantly harder (5-5.5). - **Chrysocolla**: Usually has a more greenish hue and often occurs in botryoidal or mammillary forms. ## Crystal Forms Aerinite most often forms microcrystalline, fibrous aggregates that fill fissures and voids in the host rock. It can occur as coatings, veins, or compact, massive forms. Well-formed crystals are extremely rare and appear as needles.
Geological environment
## Genesis Aerinite is a secondary mineral, forming under conditions of low-temperature metamorphism or hydrothermal processes. It forms as a result of the alteration of basic igneous rocks, such as basalts, andesites, or dolerites. It fills veins, fissures, and gas vesicles within them. ## Mineral Associations It often co-occurs with minerals such as prehnite, scolecite, calcite, and also with iron sulfides – pyrite and marcasite. ## Localities The most important and well-known aerinite localities worldwide are in Spain, in the Aragonese Pyrenees (Huesca province, e.g., near Estopiñán del Castillo) and in Andalusia. It is also known from occurrences in France (Saint-Pandelon).
Rarity
Not very common
For collectors
## Quality Criteria The most highly valued aerinite specimens are characterized by a deep, uniform, saturated blue color. The size and form of the aggregate are also important – thick veins of the mineral cutting through the host rock or massive fragments with a pure color are attractive. The contrast with white host rock or co-occurring minerals (e.g., white scolecite) enhances the visual appeal of the specimen. ## Popular Localities The localities in Spain, especially in the municipality of Estopiñán del Castillo in Huesca province, are considered classic and yield the best quality specimens. Specimens from this region are the benchmark for aerinite and command the highest prices in the collector's market.
Care and storage
## Cleaning Aerinite specimens should be cleaned very carefully due to their low hardness. It is best to use a soft brush to remove dust. If necessary, it can be rinsed with distilled water and then thoroughly dried with a soft cloth. ## What to Avoid Aerinite is susceptible to scratches, so contact with harder minerals should be avoided. It should be protected from acids and strong chemicals. Ultrasonic cleaners and steam cleaners are not recommended. ## Storage It is recommended to store aerinite specimens in separate, padded boxes or display cases to prevent abrasions and mechanical damage. It should be protected from dust and direct, prolonged exposure to sunlight, although it is not particularly sensitive to fading.