Berzelianite
Chemical formula: Cu₂-xSe (x ≈ 0.12)
Berzelianite is a rare copper selenide with a metallic luster, which quickly develops a blue-gray patina.
Properties
- Mohs hardness
- 2
- Luster
- Metallic, when fresh.
- Streak
- Shiny
- Density
- 6.71
- Cleavage
- None
- Fracture
- Irregular/Uneven
- Transparency
- Opaque
- Crystal system
- Isometric
Diagnostic features
## Identification The key diagnostic feature of berzelianite is its silvery-white color on a fresh fracture, which very quickly becomes covered with a characteristic, blue-gray, dull or iridescent patina. It is very soft (hardness 2) and heavy. It produces a shiny streak. ## Distinguishing from Similar Minerals Berzelianite is sometimes confused with other selenides, such as eucairite or umangite. Eucairite (AgCuSe) is usually more creamy-white. Umangite (Cu₃Se₂) has a characteristic violet-red color. It is distinguished from similar sulfides (e.g., chalcocite) by its faster tarnishing and specific patina color. ## Crystal Forms Berzelianite crystallizes in the isometric system, but very rarely forms well-developed crystals. It is most commonly found in the form of granular aggregates, massive compact forms, and as dendrites (plant-like forms) embedded in calcite or other minerals.
Geological environment
## Genesis Berzelianite is a hydrothermal mineral. It forms at low to medium temperatures in ore veins where selenium-rich solutions are present. It usually occurs in paragenesis with other selenides. ## Mineral Associations It often co-occurs with other, also rare, selenides such as eucairite, clausthalite, tiemannite, umangite, and klockmannite. It is also accompanied by calcite, barite, and copper sulfides. ## Localities Key localities for this mineral worldwide include the type locality – the Skrikerum mine in Sweden; Lehrbach and Zorge in the Harz Mountains (Germany); Příbram (Czech Republic); Mendoza (Argentina); the La Cacheuta mine in Sierra de Cacheuta (Argentina); and the Lake Athabasca region in Saskatchewan (Canada).
Rarity
Rare
For collectors
## Quality Criteria The most prized specimens by collectors are those with well-formed, distinct dendrites, especially those embedded in contrasting white calcite. Rich, massive accumulations of berzelianite are also highly valued. The size of the aggregates and the intensity of the natural patina also influence the attractiveness of a specimen. ## Popular Localities Specimens from the historical localities in the Harz Mountains in Germany and from the Swedish Skrikerum mine are considered classic and most desirable. Dendritic specimens from Argentina also enjoy great popularity in the collector's market.
Care and storage
## Cleaning Berzelianite specimens should generally not be cleaned to avoid removing the natural, often diagnostic, patina. If cleaning is absolutely necessary, only compressed air should be used to remove dust. Water and any chemical agents should be avoided. ## What to Avoid The mineral is very soft and susceptible to scratching. Contact with harder minerals should be avoided. Chemicals, especially acids, can damage it. Prolonged exposure to humid air accelerates the oxidation process and surface discoloration. ## Storage It is recommended to store specimens in closed, dry containers or display cases to limit contact with air and moisture, which will slow down the patination process. It should be protected from dust and mechanical damage, preferably by isolating it from other minerals.