Manganolangbeinite

Chemical formula: K₂Mn²⁺₂(S⁶⁺O₄)₃

A rare potassium-manganese sulfate with a characteristic pinkish-red color, belonging to the langbeinite group.

## Characteristics Manganolangbeinite is a sulfate mineral belonging to the langbeinite group. It occurs as granular aggregates or poorly formed, small crystals. Its most characteristic visual feature is its pinkish-red color, which distinguishes it from other fumarolic minerals. ## Physical Properties This mineral is relatively soft, with a Mohs hardness of 2.5-3. It has a density of approximately 3.02 g/cm³, which is an average value. It exhibits a vitreous luster. It is transparent to translucent. ## Colors and Varieties The typical and only recorded color of manganolangbeinite is pinkish-red. No color varieties or commercial varieties are known. ## History and Name The mineral's name refers to its chemical composition - the dominance of manganese (mangano-) and its structural similarity to langbeinite. It was discovered and described in 1924 based on samples from Vesuvius fumaroles. ## Uses Manganolangbeinite has no industrial applications. Its significance is purely scientific and collectible due to its rarity and specific formation environment.

Properties

Mohs hardness
2.5-3
Luster
Vitreous
Density
3.02
Transparency
Transparent to translucent
Crystal system
Isometric

Diagnostic features

## Identification The key diagnostic feature of manganolangbeinite is its unique pinkish-red color combined with its occurrence environment - volcanic fumaroles. Low hardness (2.5-3) and vitreous luster are also helpful in identification. ## Distinguishing from Similar Minerals This mineral can be confused with other pink or red minerals from volcanic zones. Distinguishing it from them often requires chemical analysis (EDS) to confirm the presence of potassium, manganese, and sulfur. Its belonging to the isometric crystal system differentiates it from many other sulfates. ## Crystal Forms Manganolangbeinite primarily forms granular aggregates. Poorly formed, small crystals with a habit typical of the isometric system, such as tetrahedra, are rarely observed.

Geological environment

## Genesis Manganolangbeinite is a mineral of volcanic origin. It forms through the sublimation process from hot gases (exhalations) in fumaroles, where it crystallizes on the walls of fissures and voids in lavas. ## Mineral Associations It co-occurs with other fumarolic minerals, such as hematite, halite, and sylvine. Its presence is closely linked to volcanic activity. ## Localities The most important and classic occurrence (type locality) of manganolangbeinite is the Vesuvius volcanic complex in Campania, Italy. This is the only confirmed and well-documented locality of this mineral in the world.

Rarity

Very rare

For collectors

## Quality Criteria The quality of a manganolangbeinite specimen primarily depends on the intensity and saturation of its pinkish-red color. The most prized specimens are rich, granular coatings covering a significant surface area of the host rock (matrix). The presence of even poorly formed microcrystals significantly increases its collector's value. ## Popular Localities All collector specimens come from a single location in the world - the fumaroles of Vesuvius in Italy. Material from this locality is considered classic and the only one available on the market.

Care and storage

## Cleaning Specimens should be cleaned very carefully, using a soft brush to remove dust. Due to potential water solubility, contact with liquids should be avoided. If wet cleaning is absolutely necessary, use a minimal amount of isopropyl alcohol on a cotton swab and dry the specimen immediately. ## What to Avoid Contact with water, acids, and other chemicals must be strictly avoided. The mineral is sensitive to moisture and can be damaged. It should be protected from high temperatures and sudden temperature changes. ## Storage It is recommended to store specimens in a dry place, preferably in a sealed, lockable display box away from sources of moisture. Placing a desiccant (e.g., silica gel) nearby is a good idea.

External references

Sources

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