Żabińskiite is a rare zinc-bearing member of the vesuvianite group, first discovered in the Silesia-Kraków region of Poland. It typically occurs as small, yellowish-brown prismatic crystals within carbonate-hosted zinc-lead ore deposits. Collectors should look for its distinct zinc-dominant composition which differentiates it from the more common calcium-rich vesuvianite.
Is this żabińskiite?
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 żabińskiite with a known reference. Żabińskiite 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: brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: prismatic crystals.
Often confused with
Żabińskiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside żabińskiite
Minerals reported to co-occur with żabińskiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca[Al₀.₅(Ta,Nb)₀.₅](SiO₄)O
- Mohs hardness
- ~5
- Density
- 3.897 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Prismatic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Filling fractures in weakly fractionated parts of anatectic pegmatites in an amphibolite migmatite
Where rockhounds find żabińskiite
Classic worldwide localities
- Olkusz, Poland
Field-hunting tip
Where it forms: Filling fractures in weakly fractionated parts of anatectic pegmatites in an amphibolite migmatite. If you start seeing k-mica, zircon, polycrase- in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.



