Günterblassite is a rare phyllosilicate mineral discovered in the volcanic regions of the Eifel mountains in Germany. It typically forms thin, platy, pseudo-hexagonal crystals within the cavities of phonolitic rocks, often requiring magnification for clear identification.
Is this günterblassite?
4-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch günterblassite with a known reference. Günterblassite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Match the color rangeCompare against the expected color range: colorless, pale yellow, brown.
- 4Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, pseudo-hexagonal aggregates.
Often found alongside günterblassite
Minerals reported to co-occur with günterblassite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (K,Ca,Ba,Na,□)₃Fe[(Si,Al)₁₃O₂₅(OH,O)₄]·7H₂O
- Mohs hardness
- 4
- Density
- 2.18 g/cm³
- Streak
- White
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy crystals, pseudo-hexagonal aggregates
- Cleavage
- Perfect on (001), less perfect on (100) and (010)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Encrusts the walls of miaroles in alkali basalt
Where rockhounds find günterblassite
Classic worldwide localities
- Mount Rother Kopf, near Gerolstein, Rheinland-Pfalz, Germany
Field-hunting tip
Where it forms: Encrusts the walls of miaroles in alkali basalt. If you start seeing nepheline, leucite, augite in float, you are in the right ground. Typical habit: platy crystals, pseudo-hexagonal aggregates. Train your eye for that shape before scanning the outcrop.






