Bellbergite is an exceptionally rare member of the osumilite group found as tiny prismatic crystals in volcanic rocks. It is primarily known for its type locality at the Bellberg volcano in the Eifel region of Germany. Collectors typically seek it out as a micro-mineral within the vugs of alkaline volcanic ejecta.
Is this bellbergite?
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 bellbergite with a known reference. Bellbergite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: pyramidal.
Often confused with
Bellbergite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bellbergite
Minerals reported to co-occur with bellbergite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (K,Ba,Sr)₂Sr₂Ca₂(Ca,Na)₄(Si,Al)₃₆O₇₂·30H₂O
- Mohs hardness
- ~5
- Density
- 2.20 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Pyramidal
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In leucite tephrite lava at contacts between lava and calcium-rich xenoliths
Where rockhounds find bellbergite
Classic worldwide localities
- Bellerberg volcano, two km north of Mayen, Eifel district, Germany
Field-hunting tip
Where it forms: In leucite tephrite lava at contacts between lava and calcium-rich xenoliths. If you start seeing sanidine, clinopyroxene, pyrrhotite in float, you are in the right ground. Typical habit: pyramidal. Train your eye for that shape before scanning the outcrop.







