Müllerite
Chemical formula: Pb<sup>2+</sup><sub>2</sub>Fe<sup>3+</sup>(Te<sup>6+</sup>O<sub>6</sub>)Cl
Müllerite is an extremely rare lead iron tellurate, distinguished by its unique chemical composition and occurrence as microscopic crystals.
Properties
- Mohs hardness
- 3
- Luster
- Sub-Metallic to Vitreous
- Streak
- Light brown
- Density
- 7.47
- Cleavage
- Perfect on {001}
- Fracture
- Uneven
- Transparency
- Opaque
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of müllerite is possible almost exclusively using advanced analytical methods, such as energy-dispersive spectroscopy (EDS/EDX) to confirm its unique chemical composition (Pb, Fe, Te, Cl). Visually, at the occurrence site, it can be suspected based on its dark brown color, submetallic luster, and co-occurrence with other rare tellurates. ## Distinguishing from Similar Minerals In its environment, it can be confused with other dark, fine-grained secondary minerals. Differentiation from similar tellurates, such as backite or schieffelinite, requires chemical analysis. Its characteristic composition is a key diagnostic feature. ## Crystal Forms Müllerite forms very small, thin, tabular or bladed crystals, often flattened. They usually occur as small, radial or irregular aggregates on the surface of the host rock.
Geological environment
## Genesis Müllerite is a secondary mineral that forms in the oxidation zones (gossans) of hydrothermal ore deposits rich in tellurium. It forms under desert conditions as a result of the weathering of primary sulfides and tellurides. ## Mineral Associations This mineral occurs in association with other rare secondary minerals, especially tellurates and tellurites. It most commonly co-occurs with quartz, schieffelinite, backite, cerussite, anglesite, jarosite, and hematite. ## Localities The only confirmed locality of müllerite in the world (type locality) is the dumps of the St. Joe mine (Joe Mine) in the Tombstone mining district, Cochise County, Arizona, USA.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of a müllerite specimen is primarily assessed based on the richness and size of the crystal aggregates. Most valued are specimens with clearly formed, though still microscopic, rosettes or radial crystal clusters, well-separated from the host rock. A contrasting quartz matrix enhances visual appeal. Purity is not a key criterion, as the mineral is opaque. ## Popular Localities The only source of müllerite specimens is its type locality – the St. Joe mine in Tombstone, Arizona. All specimens available on the collector's market originate from this single location.
Care and storage
## Cleaning Müllerite specimens, being microminerals, generally do not require cleaning. If absolutely necessary, compressed air (from a safe distance) can be used to remove dust. Avoid contact with water and any chemicals. ## What to Avoid Avoid ultrasonic cleaners, acids, solvents, and sudden temperature changes. The mineral is brittle, so protect it from shocks and impacts. Due to the presence of lead, avoid inhaling dust and wash hands after contact with the specimen. ## Storage Specimens should be stored in specialized micromount boxes to protect them from mechanical damage and dust. Store in a dry place, away from direct sunlight.