Levantite is a potassium calcium aluminum phosphate that forms colorless prismatic crystals. It occurs in pyrometamorphic gehlenite-wollastonite hornfels. It was first described from the northern slope of Har Parsa, Negev Desert, near Arad, Israel.
Is this levantite?
4-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 levantite with a known reference. Levantite sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: colorless.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Levantite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside levantite
Minerals reported to co-occur with levantite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KCa₃Al₂(SiO₄)(Si₂O₇)(PO₄)
- Mohs hardness
- 5
- Density
- 2.957 g/cm³
- Colors
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals
- Cleavage
- Good on (100)
- Rarity
- Common
- Uses
- Lapidary, Decorative
- Host rock
- In pyrometamorphic gehlenite-wollastonite hornfels
Where rockhounds find levantite
Classic worldwide localities
- Israel
- Palestine
- Jordan
- Syria
Field-hunting tip
Where it forms: In pyrometamorphic gehlenite-wollastonite hornfels. If you start seeing gehlenite, wollastonite, anorthite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.






