Bentorite is a very rare member of the ettringite group typically found as small, delicate, pinkish-violet prismatic crystals. It is primarily known from its type locality in the Hatrurim Basin of Israel, occurring in high-temperature metamorphic environments. Due to its softness and high water content, specimens should be handled with care and stored in a low-humidity environment.
Is this bentorite?
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 bentorite with a known reference. Bentorite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: very pale violet.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: violet, light violet.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals.
Often confused with
Bentorite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Bentorite leaves very pale violet, Ettringite leaves white.

How to tell apart: Thaumasite is the harder of the two (Mohs 3.5 vs. 2); streak differs, so Bentorite leaves very pale violet, Thaumasite leaves white.
Often found alongside bentorite
Minerals reported to co-occur with bentorite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₆Cr₂(SO₄)₃(OH)₁₂·26H₂O
- Mohs hardness
- 2
- Density
- 2.025 g/cm³
- Colors
- Streak
- Very pale violet
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic crystals
- Cleavage
- {1010}, perfect; {0001}, distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In low-temperature hydrothermal veins in black calcite–spurrite marble
Where rockhounds find bentorite
1 mapped spotsClassic worldwide localities
- Marble quarry in the Hatrurim Formation, near the Arad-Sodom road, Negev Desert, Israel (type locality)
Field-hunting tip
Where it forms: In low-temperature hydrothermal veins in black calcite–spurrite marble. If you start seeing calcite, thaumasite, truscottite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah. Start trip planning there.





