Ronpetersonite

Chemical formula: BaW⁶⁺O₄

Ronpetersonite is an extremely rare mineral from the scheelite group, a barium tungstate, found as microscopic grains in nephelinites.

## Characteristics Ronpetersonite is an extremely rare mineral, approved by the IMA in 2016. It occurs as very small, anhedral (not exhibiting its own faces) grains, not exceeding 20 micrometers in size. Due to the microscopic size of the crystals, its visual characteristics cannot be assessed with the naked eye. Observed in reflected light, it is gray and exhibits weak, internal reflections. ## Physical Properties The hardness of ronpetersonite has been estimated at approximately 4 on the Mohs scale based on analogy with other tungstates. The density calculated from the chemical formula and unit cell parameters is 6.85 g/cm³. This mineral is brittle and characterized by a vitreous luster. ## History and Name The mineral is named in honor of Ronald C. Peterson, a professor of mineralogy at Queen's University in Kingston, Canada, for his contributions to mineralogy and crystallography. It was discovered in samples from the Bellerberg volcano in the Eifel Mountains, Germany, and its description was published in 2017. ## Applications Ronpetersonite has no industrial or commercial applications. Its significance is purely scientific and as a collector's item, as an extremely rare representative of tungstates.

Properties

Mohs hardness
4
Color
colourless
Luster
Vitreous
Streak
white
Density
6.363
Cleavage
neither cleavage nor fracture could be determined
Fracture
Uneven
Transparency
Transparent
Crystal system
Tetragonal

Diagnostic features

## Identification Identification of ronpetersonite is impossible without advanced analytical techniques. It requires the use of an electron microscope with an energy-dispersive spectrometer (EDS/WDS) for chemical composition analysis and X-ray diffraction (XRD) to confirm the crystal structure. In reflected light, it is gray and opaque. ## Distinguishing from Similar Minerals Ronpetersonite is structurally related to scheelite (CaWO₄) and stolzite (PbWO₄). Differentiation from them is based solely on chemical analysis, which shows the dominance of barium. Visually, at the microscopic level, it may be indistinguishable from other fine, gray minerals. ## Crystal Forms To date, it has only been observed in the form of anhedral, rounded grains up to 20 µm in size, occurring as inclusions in other minerals, mainly leucite.

Geological environment

## Genesis Ronpetersonite forms in the late stages of magma crystallization in environments extremely undersaturated in silica and rich in incompatible elements such as barium and tungsten. Its occurrence is associated with alkaline volcanism. ## Mineral Associations This mineral has been found in voids within nephelinite lavas. It co-occurs with minerals such as leucite, nepheline, augite, apatite, magnetite, as well as rarer minerals like baddeleyite, zirconolite, and walstromite. Ronpetersonite grains are most often found as inclusions in leucite crystals. ## Localities The only confirmed locality (type locality) of ronpetersonite in the world is the Bellerberg volcano, part of the Laacher See volcanic complex in the Eifel Mountains, Rhineland-Palatinate, Germany.

Rarity

Extremely rare

For collectors

## Quality Criteria As a microscopic mineral, ronpetersonite is not evaluated based on typical criteria such as color, transparency, or crystal size. The value of a specimen lies in the analytically confirmed presence of the mineral and in the richness and aesthetics of its associated minerals from a given locality. A specimen with a clearly identified (e.g., in an SEM image) and well-displayed ronpetersonite grain will be most desired by specialized micromount collectors. ## Popular Localities The only source of specimens is the type locality - the Bellerberg volcano in Germany. Specimens from there, even without ronpetersonite visible to the naked eye, are valued due to the possibility of its presence and the occurrence of other rare minerals.

Care and storage

## Cleaning Due to its microscopic size and occurrence as inclusions in the host rock, individual grains of ronpetersonite are not isolated or cleaned. The host rock specimen can be gently cleaned with compressed air or, if necessary, a soft brush. ## What to Avoid Avoid contact of the rock with chemicals, especially strong acids and bases, which could damage both ronpetersonite and the surrounding minerals. Ultrasonic cleaners should not be used. ## Storage Specimens containing ronpetersonite should be stored under stable conditions, away from dust and moisture. It is best to keep them in a specialized collector's box (a "micromount box") to protect delicate mineral associations.

External references

Sources

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