Erikjonssonite
Chemical formula: (Pb²⁺₃₂O₂₁)[(V⁵⁺,Si,Mo⁶⁺,As⁵⁺)O₄]₄Cl₉
Erikjonssonite is an extremely rare lead mineral that forms unique, hexagonal crystals of an intense red color.
Properties
- Mohs hardness
- 2.5
- Color
- Orange-red
- Luster
- Adamantine
- Streak
- Light red
- Density
- 7.967
- Cleavage
- (010)
- Fracture
- Irregular/Uneven
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of erikjonssonite is based on its unique characteristics: intense red color, adamantine luster, hexagonal crystal shape, and very high density. The locality of occurrence – the Kombat mine in Namibia – is also key. Final identification requires advanced analytical methods, such as Raman spectroscopy or chemical analysis (EDS). ## Distinguishing from Similar Minerals It can be confused with other rare, red secondary minerals from the oxidation zones of ore deposits, such as some vanadates (e.g., vanadinite) or lead oxides. However, its specific hexagonal crystal form and unique chemical composition distinguish it. Unlike vanadinite, its crystals are usually tabular, not prismatic. ## Crystal Forms Erikjonssonite forms very small, thin, tabular crystals with a hexagonal outline. They occur as single, isolated crystals or small groups on the surface of the host rock.
Geological environment
## Genesis Erikjonssonite is a secondary mineral that formed as a result of low-temperature hydrothermal processes. It forms in the oxidation zones of polymetallic deposits, in this case, a manganese and iron deposit with sulfide mineralization (Cu-Pb-Ag). It likely formed from the reaction of solutions rich in vanadium, chlorine, and other elements with earlier lead minerals. ## Mineral Associations This mineral occurs in association with other rare secondary minerals, such as kombatite, saharaite, asisite, as well as calcite and hematite. It co-occurs on altered, manganese-rich host rock. ## Localities The only confirmed occurrence of erikjonssonite in the world is its type locality – the Kombat mine, in the Otjozondjupa district, Grootfontein region, Namibia. Specimens originate from mine dumps.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of erikjonssonite specimens is primarily assessed based on the size and development of the crystals. The most valued specimens are those with sharp, well-defined, hexagonal crystals of an intense red color. The contrast with the matrix rock and the presence of associated minerals that confirm its origin are also important. Due to the microscopic size of the crystals, their photogenicity under magnification is crucial. ## Popular Localities The only source of specimens is the Kombat mine in Namibia. All specimens available on the collector's market come from this single locality.
Care and storage
## Cleaning Erikjonssonite specimens, due to their extreme delicacy and small size, should generally not be mechanically cleaned. If absolutely necessary, compressed air (from a safe distance) can be used to remove loose dust particles. Contact with water and any chemicals should be avoided. ## What to Avoid Contact with acids and other chemicals that could damage it must be strictly avoided. The mineral is very soft (hardness ~2), so it is susceptible to scratches and mechanical damage. It should be protected from vibrations and impacts. ## Storage It is recommended to store specimens in specialized, sealed "micromount" boxes, which protect them from dust, moisture, and physical damage. Exposure should be away from direct sunlight and heat sources.