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, 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.




