Mascagnite
Chemical formula: (N³⁻H₄)₂S⁶⁺O₄
Mascagnite is a rare, water-soluble ammonium sulfate, forming ephemeral coatings and efflorescences near volcanoes and on mine dumps.
Properties
- Mohs hardness
- 2-2.5
- Luster
- Vitreous, dull
- Streak
- White
- Density
- 1.768
- Cleavage
- On {001}.
- Fracture
- Irregular/Uneven
- Transparency
- Transparent,Translucent,Opaque
- Crystal system
- Orthorhombic
Diagnostic features
## Identification A key diagnostic feature of mascagnite is its immediate and complete solubility in water. The mineral is very soft, light, and often forms characteristic, loose or fibrous efflorescences. Occurrence in the vicinity of volcanic fumaroles or on burning mine dumps is a strong indicator. ## Distinguishing from Similar Minerals It can be confused with other water-soluble sulfates or nitrates, such as epsomite, mirabilite, or salammoniac. It is distinguished from salammoniac (ammonium chloride) by its lack of reaction with nitric acid and silver. Accurate differentiation from other sulfates often requires chemical analysis. ## Crystal Forms Crystals, if well-formed, are usually small, tabular, or short prismatic. However, it most often occurs as granular, powdery, fibrous aggregates, and as coatings and crusts on rocks.
Geological environment
## Genesis Mascagnite is a secondary mineral. It forms mainly through sublimation from volcanic gases near active fumaroles. It also forms as a product of organic matter decomposition (e.g., guano) and on burning coal mine dumps, where ammonia from coal reacts with sulfur oxides. ## Mineral Associations It co-occurs with other fumarolic minerals and products of mine fires, such as native sulfur, salammoniac, sassolite, tschermigite, and boussingaultite. ## Localities The most important localities worldwide include the areas around Vesuvius and Etna in Italy (the type locality is Travale in Tuscany). It also occurs at the Al-Kibrit volcano in Iran, in coal mines in Pennsylvania (USA), on dumps in Kladno (Czech Republic), and in Pecs, Hungary.
Rarity
Rare
For collectors
## Quality Criteria For collectors, specimens with well-formed, transparent crystals are most desirable, which is a great rarity. Rich, abundant coatings and efflorescences on the original matrix rock are also valued. Due to the ephemeral nature of the mineral, it is crucial that the specimen is well-preserved and shows no signs of dissolution. ## Popular Localities Classic and most prized specimens come from Italian volcanoes, especially Vesuvius. Specimens from burning mine dumps in Pennsylvania (USA) or the Czech Republic are also sometimes available on the collector's market.
Care and storage
## Cleaning The mineral is extremely sensitive to water and dissolves immediately in it. **Absolutely no wet cleaning is allowed.** The only permissible method is very gentle dust removal using a soft brush or a stream of compressed air from a distance. ## What to Avoid Avoid contact with water, water vapor, and any moisture. Storage in a humid environment (e.g., a basement) will lead to its dissolution. Protect it from all chemicals and sudden temperature changes. ## Storage Mascagnite specimens require special conditions. They should be stored in tightly sealed, transparent containers (so-called "perky boxes") along with a desiccant (e.g., silica gel). Display should be away from sources of moisture and direct sunlight.