Langhofite

Chemical formula: Pb²⁺₂(OH)[W⁶⁺O₄(OH)]

Langhofite is a very rare, secondary lead tungstate mineral, forming microscopic, colorless to white tabular crystals.

## Characteristics Langhofite is a hydrated lead tungstate, occurring as extremely small, tabular or platy crystals, rarely exceeding 0.2 mm in length. They typically form rosette-like or radial aggregates. Individual crystals are colorless to white and transparent, exhibiting a vitreous or slightly pearly luster on cleavage surfaces. ## Physical Properties Due to the microscopic size of the crystals, most physical properties, such as hardness or density, have not been precisely determined. The density calculated based on the chemical formula and unit cell parameters is 7.45 g/cm³. The mineral exhibits perfect cleavage in one direction. ## Colors and Varieties The mineral is colorless to white. No varieties have been distinguished. ## History and Name Langhofite was discovered in the dumps of the historic Clara Mine in the Black Forest (Germany) and described in 2011 by Werner Krause, Heinz-Jürgen Bernhardt, Heralt Effenberger, and Norbert Brandstätter. The name honors Jochen Langhof (born 1971), a Swedish mineral collector who found the first samples of this mineral and specializes in the mineralogy of Långban and the Clara Mine.

Properties

Mohs hardness
2.5
Color
colourless to white
Luster
Vitreous, Pearly
Streak
white
Density
7.95
Cleavage
{010} and {100} cleavages
Fracture
Irregular/Uneven,Splintery
Transparency
Transparent
Crystal system
Triclinic

Diagnostic features

## Identification Identification of langhofite is possible only through advanced analytical methods, such as Raman spectroscopy or X-ray diffraction (XRD), due to its microscopic size and occurrence. Visually, it is characterized by tiny, colorless, tabular crystals forming rosette-like aggregates on the matrix rock. ## Distinguishing from Similar Minerals It can be confused with other secondary, colorless lead or tungsten minerals, such as hydrocerussite, raspberrite, or stolzite, which may co-occur in the same environment. Reliable differentiation from these minerals requires specialized chemical and structural analysis. ## Crystal Forms Crystals are very small, thin, and tabular, with a hexagonal outline. They often form radial or rosette-like clusters and aggregates.

Geological environment

## Genesis Langhofite is a secondary mineral, formed in the oxidation zones of polymetallic deposits. In its type locality (Clara Mine), it forms as a result of the weathering of tungsten minerals (mainly scheelite) in the presence of lead-rich solutions, originating from the oxidation of galena. ## Mineral Associations This mineral co-occurs with other secondary lead and tungsten minerals. In the Clara Mine, it was found in association with cerussite, mimetite, stolzite, raspberrite, as well as quartz and barite. ## Localities The only confirmed locality of langhofite in the world is the dumps of the Clara Mine, Rankach, Oberwolfach, Black Forest, Baden-Württemberg, Germany. This is its type locality.

Rarity

Extremely rare

For collectors

## Quality Criteria As a microscopic mineral, langhofite is primarily valued for its confirmed presence on a specimen. The most highly rated specimens are those where well-formed, though still microscopic, rosette-like crystal aggregates are visible, clearly standing out from the matrix rock. The abundance of these aggregates on the matrix and association with other rare secondary minerals increase the collecting and scientific value of the specimen.

Care and storage

## Cleaning Specimens with langhofite should be handled with utmost care due to their extreme rarity and microscopic size. Cleaning is not recommended, as mechanical methods (brushes, ultrasonics) will irreversibly damage the delicate crystals. Dust can only be removed using a gentle stream of compressed air. ## What to Avoid Avoid contact with all chemicals, including acids and bases, which may react with the mineral. Also avoid ultrasonic cleaners, high temperatures, and sudden changes in pressure. ## Storage Specimens should be stored under stable conditions in sealed "micromount" containers to protect them from dust, mechanical damage, and contamination. Due to the lead content, it is recommended to wash hands after contact with the specimen.

External references

Sources

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