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 — that is 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.






