Giuseppettite is a rare tectosilicate mineral belonging to the cancrinite group, primarily found within the volcanic ejecta of the Colli Albani region in Italy. Collectors should look for its distinctive hexagonal prismatic habit within cavities of alkaline volcanic rocks, often requiring micro-analysis for definitive identification.
Is this giuseppettite?
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 giuseppettite with a known reference. Giuseppettite sits at Mohs 6-7, 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: light violet blue.
- 5Look at form & habitCrystal system: trigonal. Typical habit: anhedral grains.
Often confused with
Giuseppettite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside giuseppettite
Minerals reported to co-occur with giuseppettite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,K,Ca)₈(Si,Al)₁₂O₂₄(SO₄,Cl,OH)₂
- Mohs hardness
- 6-7
- Density
- 2.35 g/cm³
- Colors
- Light violet blue
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As veinlets in a block of sanidinite volcanic ejecta
Where rockhounds find giuseppettite
Classic worldwide localities
- Sacrofano, in the Biachella Valley, Lazio, Italy
Field-hunting tip
Where it forms: As veinlets in a block of sanidinite volcanic ejecta. If you start seeing potassic feldspar, nepheline, häuyne in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.




