Halurgite is a rare magnesium borate mineral typically found in evaporite deposits associated with salt domes. It is most recognized for its tabular habit and perfect cleavage, often appearing as colorless to white crystalline masses within saline environments.
Is this halurgite?
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 halurgite with a known reference. Halurgite sits at Mohs 2.5-3, 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: subvitreous.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular to prismatic crystals, often as fibrous aggregates.
Often confused with
Halurgite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Boracite is the harder of the two (Mohs 7-7.5 vs. 2.5-3); luster reads subvitreous on Halurgite and vitreous to adamantine on Boracite.

How to tell apart: Preobrazhenskite is the harder of the two (Mohs 4.5-5 vs. 2.5-3); luster reads subvitreous on Halurgite and pearly on Preobrazhenskite.
Often found alongside halurgite
Minerals reported to co-occur with halurgite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₄[B₈O₁₃(OH)₂]₂·7H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.19 g/cm³
- Colors
- Streak
- White
- Luster
- Subvitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular to prismatic crystals, often as fibrous aggregates
- Cleavage
- Perfect on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Of rare occurrence in interstices and vugs in a rock salt diapir
Where rockhounds find halurgite
Classic worldwide localities
- Chelkar salt dome, Ak-saı̆ Valley, Uralsk district, Kazakhstan
Field-hunting tip
Where it forms: Of rare occurrence in interstices and vugs in a rock salt diapir. If you start seeing boracite, kaliborite, pinnoite in float, you are in the right ground. Typical habit: tabular to prismatic crystals, often as fibrous aggregates. Train your eye for that shape before scanning the outcrop.





