Aravaite is an extremely rare lead-calcium silicate phosphate mineral discovered in the pyrometamorphic rocks of the Hatrurim Basin. It typically occurs as small, colorless, or white platy crystals in association with other rare high-temperature minerals. Because of its locality-specific occurrence, it is highly sought after by advanced mineral collectors specializing in rare species.
Is this aravaite?
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 aravaite with a known reference. Aravaite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Aravaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Aravaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals.
Often confused with
Aravaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside aravaite
Minerals reported to co-occur with aravaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Pb₃(SiO₄)(PO₄)₂(OH)₂
- Mohs hardness
- 3.5
- Density
- 2.84 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Pyrometamorphic Rocks of The Hatrurim Formation
- Typical price
- $100-500 depending on specimen size and rarity
Where rockhounds find aravaite
Classic worldwide localities
- Hatrurim Basin, Israel
Field-hunting tip
Look in pyrometamorphic rocks of the hatrurim formation country — that is the host setting where aravaite typically forms. If you start seeing ettringite, flamite, gehlenite in float, you are in the right ground. Field specimens usually show a platy crystals habit, so train your eye for that shape before scanning the outcrop.




