Rhönite is a relatively rare member of the aenigmatite group typically found in silica-undersaturated alkalic volcanic rocks. It forms dark, brownish-black tabular or prismatic crystals and is primarily a curiosity for advanced mineral collectors studying volcanic paragenesis.
Is this rhönite?
5-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 rhönite with a known reference. Rhönite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rhönite leaves a brownish grey streak.
- 3Read the lusterHold the specimen under a strong light. Rhönite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: black, brown, dark brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, granular aggregates, prismatic.
Often confused with
Rhönite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rhönite
Minerals reported to co-occur with rhönite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Na,Mg,Fe²⁺,Fe³⁺,Ti,Al)₈(Si,Al)₆O₂₀
- Mohs hardness
- 5.5-6
- Density
- 3.5-3.6 g/cm³
- Colors
- Streak
- Brownish Grey
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Granular Aggregates, Prismatic
- Cleavage
- Good in Two Directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkalic Igneous Rocks, Basaltic Lavas
- Typical price
- $20-150 per specimen depending on size and crystal quality
Where rockhounds find rhönite
Classic worldwide localities
- Rhön Mountains, Germany
- Etna, Italy
- Kaiserstuhl, Germany
- Cape Verde
- Hocheifel, Germany
Field-hunting tip
Look in alkalic igneous rocks, basaltic lavas country, the host setting where rhönite typically forms. If you start seeing nepheline, olivine, augite in float, you are in the right ground. Field specimens usually show a tabular crystals, granular aggregates, prismatic habit, so train your eye for that shape before scanning the outcrop.






