Chiavennite is a rare beryllium-bearing zeolite mineral that typically forms prismatic, radiating crystal sprays. It is most commonly identified in hydrothermal veins or cavities within alkaline igneous rocks and is highly sought after by mineral collectors specializing in rare species.
Is this chiavennite?
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 chiavennite with a known reference. Chiavennite sits at Mohs ~3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white to pale ocher.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to pearly.
- 4Match the color rangeCompare against the expected color range: yellow, orange, red orange.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, radial aggregates.
Often confused with
Chiavennite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chiavennite
Minerals reported to co-occur with chiavennite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaMnBe₂(Si₅O₁₃)(OH)₂·2H₂O
- Mohs hardness
- ~3
- Density
- 2.56-2.64 g/cm³
- Colors
- Streak
- White to pale ocher
- Luster
- Vitreous to pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic crystals, radial aggregates
- Cleavage
- Good to perfect on {100}, {010}, and {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Coating beryl in late-stage pegmatites (Tanno, Italy); in vugs in syenite pegmatites (Norway)
Where rockhounds find chiavennite
Classic worldwide localities
- Tanno, Chiavenna, Lombardy, Italy
- Heia and Vevja larvikite quarries, near Larvik, Tvedalen district, Norway
- Blåfjell, Langangen, and in the Saga larvikite quarry, Porsgrunn, Langesundsfjord, Norway
- Bakkane, Brunlanes, Norway
- Utö Island, Sweden
Field-hunting tip
Where it forms: Coating beryl in late-stage pegmatites (Tanno, Italy); in vugs in syenite pegmatites (Norway). If you start seeing beryl, bavenite, analcime in float, you are in the right ground. Typical habit: prismatic crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.








