Aradite is an exceptionally rare silicate mineral found in pyrometamorphic complexes where carbonaceous sediments have been baked by high-temperature, low-pressure subterranean combustion. It is typically identified in complex assemblages with other high-temperature calcium silicates. It is named after the city of Arad, Israel, near where it was first described.
Is this aradite?
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 aradite with a known reference. Aradite 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: colorless.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals.
Often confused with
Aradite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside aradite
Minerals reported to co-occur with aradite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaCa₆[(SiO₄)(VO₄)](VO₄)₂F
- Mohs hardness
- 6-7
- Density
- 3.509 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In paralava veins cutting gehlenite-rich pyrometamorphic rock formed by the combustion of organic matter in the sedimentary protolith or methane released by tectonic forces
Where rockhounds find aradite
Classic worldwide localities
- Gurim Anticline, Hatrurim Basin, 5 km SE of Arad, Negev Desert, Israel
Field-hunting tip
Where it forms: In paralava veins cutting gehlenite-rich pyrometamorphic rock formed by the combustion of organic matter in the sedimentary protolith or methane released by tectonic forces. If you start seeing zadovite, gehlenite, pseudowollastonite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.




