Campostriniite

Cabinet No. 40

Campostriniite

Chemical formula: (Bi<sup>3+</sup><sub>2.5</sub>Na<sub>0.5</sub>)(N<sup>3-</sup>H<sub>4</sub>)<sub>2</sub>Na<sub>2</sub>(S<sup>6+</sup>O<sub>4</sub>)<sub>6</sub>·H<sub>2</sub>O

Campostriniite is an extremely rare bismuth, sodium, and ammonium sulfate, forming colorless, prismatic crystals known only from one locality in the world.

Description

## Characteristics Campostriniite is a complex, hydrated sulfate of bismuth, sodium, and the ammonium group. It forms very small, colorless, and transparent crystals with a pseudohexagonal prismatic habit, reaching a maximum length of 0.2 mm. They typically occur as small, radial or chaotic aggregates within rock cavities. Due to their size, campostriniite specimens fall within the domain of micromineralogy. ## Physical Properties The crystals exhibit a vitreous luster. They are completely transparent. Mohs hardness and density have not yet been determined due to the small size and rarity of the research material. ## Colors and Varieties This mineral is colorless. No colored or commercial varieties have been identified. ## History and Name Campostriniite was recognized as a new mineral species by the International Mineralogical Association (IMA) in 2017 (IMA number 2017-018). Its name honors Italo Campostrini (born 1957), an Italian collector and expert in minerals from the Apuan Alps region, who found the first specimens. The scientific description of the mineral was published in 2018 in the "Mineralogical Magazine" journal. ## Applications As a mineral of microscopic size and extreme rarity, campostriniite has no industrial applications. It is solely of scientific interest and is an object of interest for specialized micromineral collectors.

Diagnostic features

## Identification Amateur identification of campostriniite is practically impossible. It requires advanced analytical methods, such as X-ray diffraction (XRD) and chemical microanalysis (EDS). Visual features that may only suggest its presence are small, colorless, prismatic crystals with a vitreous luster in association with other bismuth minerals. ## Differentiation from Similar Minerals In its occurrence environment, it may be confused with other colorless sulfates, such as gypsum, which often accompanies it. However, campostriniite is distinguished by its pseudohexagonal crystal form and unique chemical composition. Its association with bismuth minerals is a key diagnostic clue. ## Crystal Forms This mineral forms elongated, prismatic crystals with a pseudohexagonal outline. They occur as single, isolated needles or, more commonly, as small, radial aggregates.

Geological environment

## Genesis Campostriniite is a secondary (supergene) mineral. It formed as a result of weathering processes of primary ore minerals under low temperature and pressure conditions. It crystallizes in small cavities (druses) within quartz veins cutting Paleozoic phyllites. ## Mineral Associations At the type locality, campostriniite coexists with minerals such as native bismuth, bismuthinite, joséite-B, and gypsum. ## Localities The only confirmed occurrence of this mineral in the world is its type locality: a quarry in the Fornovolasco area (Fabbriche di Vergemoli), in the province of Lucca, Tuscany, Italy.

Rarity

Extremely rare

Collector aspects

## Quality Criteria For such a rare micromineral, the main criterion of value is its mere presence on a piece of host rock. Specimens with well-formed, sharp, and transparent crystals are more highly valued. The richness of the specimen (number of crystals or aggregates) and aesthetic arrangement on the matrix also increase its attractiveness. Co-occurrence with other rare bismuth minerals is also of great importance. ## Popular Localities Specimens come exclusively from the type locality in Italy, making them extremely difficult to acquire.

Care and storage

## Cleaning Specimens should only be cleaned dry, using compressed air from a safe distance or a very soft brush. Any contact with water and other liquids should be avoided, as it may be soluble as a sulfate. ## What to Avoid Contact with water, chemicals, ultrasound, and sudden temperature changes must be strictly avoided. The crystals are extremely small and fragile, susceptible to mechanical damage. ## Storage It is recommended to store specimens in specialized, sealed "micromount" boxes that protect against dust, moisture, and physical damage. Avoid exposure to direct sunlight and keep away from sources of vibration.