Ciprianiite is an extremely rare silicate mineral found in the volcanic ejecta of Italy. It typically forms as small, elongated prismatic crystals in cavities and is highly sought after by systematic mineral collectors due to its localized occurrence.
Is this ciprianiite?
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 ciprianiite with a known reference. Ciprianiite sits at Mohs 5-6, 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: pale brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains, tabular.
Often confused with
Ciprianiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ciprianiite
Minerals reported to co-occur with ciprianiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄(ThCa)Al(Be₀.₅□₁.₅)[B₄Si₄O₂₂](OH)₂
- Mohs hardness
- 5-6
- Density
- 3.75-3.85 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral grains, tabular
- Cleavage
- Fair to good on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In miarolitic cavities and voids in alkali-syenitic pyroclastic ejecta
Where rockhounds find ciprianiite
Classic worldwide localities
- Tre Croci, near Vetralla, Viterbo province, Latium, Italy
Field-hunting tip
Where it forms: In miarolitic cavities and voids in alkali-syenitic pyroclastic ejecta. If you start seeing sanidine, plagioclase, feldspathoid in float, you are in the right ground. Typical habit: anhedral grains, tabular. Train your eye for that shape before scanning the outcrop.






