Gobelinite
Chemical formula: Co²⁺Cu²⁺₄(S⁶⁺O₄)₂(OH)₆·6H₂O
Gobelinite is a very rare hydrated cobalt and copper sulfate, forming characteristic, sky-blue, spherical aggregates.
Properties
- Mohs hardness
- 2.5
- Color
- Pale green, bluish green, greyish green
- Luster
- Vitreous
- Streak
- White (with a pale-green cast)
- Density
- 2.95
- Cleavage
- Perfect on {100}
- Fracture
- Irregular/Uneven
- Transparency
- Transparent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Gobelinite can be identified by its characteristic mode of occurrence – small, spherical aggregates of sky-blue color and radial internal structure. A light blue streak is also a helpful feature. ## Distinguishing from similar minerals It can be confused with other secondary copper sulfates of similar color and form, such as ktenasite, niedermayrite, or serpierite. Differentiation requires advanced analytical methods, such as chemical analysis (EDS/WDS) to confirm the presence and proportions of cobalt and copper, and X-ray diffraction (XRD) to verify the crystal structure. ## Crystal forms It forms spherical or hemispherical aggregates up to 0.5 mm in diameter, composed of radially arranged, thin crystals with a bladed or acicular habit, elongated along the [001] axis.
Geological environment
## Genesis Gobelinite is a secondary mineral, formed in the oxidation (supergene) zones of polymetallic ore deposits. It forms as a result of the weathering of primary minerals containing copper and cobalt, under conditions of low temperature and pressure. ## Mineral associations At its type locality in Germany, it co-occurs with chalcopyrite, tetrahedrite, galena, barite, quartz, niedermayrite, and serpierite. ## Localities The only confirmed locality for gobelinite in the world is its type locality – the former St. Joseph mine (Glücksstern Mine) in GOBELin, Lahnstein, in the Taunus Mountains, Rhineland-Palatinate, Germany.
Rarity
Extremely rare
For collectors
## Quality criteria As a mineral of purely scientific and collector interest, specimens with well-formed, undamaged spherical aggregates, clearly contrasting with the host rock, are most valued. The size of the aggregates and the intensity of the color also affect the specimen's value. Due to their microscopic size, specimens are usually evaluated under magnification.
Care and storage
## Cleaning Due to its extreme rarity, low hardness, and solubility in acids, mechanical or chemical cleaning is absolutely inadvisable. Specimens should be protected from dust and contaminants. ## What to avoid Avoid contact with water, chemicals (especially acids), ultrasound, and sudden temperature changes. The mineral is sensitive to dehydration, so it should not be stored in an overly dry environment or exposed to direct sunlight or strong lighting that could heat it. ## Storage Gobelinite specimens should be stored under stable conditions, preferably in closed, padded collector boxes or special display cases with controlled humidity. They should be protected from vibrations and mechanical damage.