Inderborite is a rare hydrated calcium magnesium borate mineral typically found in evaporite basins. Collectors should look for its characteristic prismatic, often colorless to white crystals that usually form within salt lake deposits or salt domes.
Is this inderborite?
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 inderborite with a known reference. Inderborite 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, radial aggregates.
Often confused with
Inderborite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside inderborite
Minerals reported to co-occur with inderborite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaMg[B₃O₃(OH)₅]₂·6H₂O
- Mohs hardness
- 3.5
- Density
- 1.93-2.00 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, radial aggregates
- Cleavage
- On {100}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- With other borates in the caprock of a salt diapir (Inder deposit, Kazakhstan); in lacustrine borate deposits (Sarıkaya, Turkey)
Where rockhounds find inderborite
Classic worldwide localities
- Furnace Creek district, Death Valley, Inyo Co., California, USA
- Der borate deposit, Kazakhstan
- Sarıkaya, near Kirka, Eskiçehir Province, Turkey
- Günevi mine, Bigadiç borate district, Balıkesir Province, Turkey
- Santa Rosa mine, Sijes district, Salta Province, Argentina
Field-hunting tip
Where it forms: With other borates in the caprock of a salt diapir (Inder deposit, Kazakhstan); in lacustrine borate deposits (Sarıkaya, Turkey). If you start seeing inyoite, colemanite, ulexite in float, you are in the right ground. Typical habit: prismatic crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.






