Penobsquisite is an extremely rare borate mineral discovered in the potash mines of New Brunswick. It typically appears as small, pale yellow, tabular crystals found within evaporite sequences associated with other borate species.
Is this penobsquisite?
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 penobsquisite with a known reference. Penobsquisite sits at Mohs ~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: vitreous.
- 4Match the color rangeCompare against the expected color range: pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: euhedral crystals.
Often found alongside penobsquisite
Minerals reported to co-occur with penobsquisite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Fe[B₉O₁₃(OH)₆]Cl(H₂O)₂·2H₂O
- Mohs hardness
- ~3
- Density
- 2.26 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Euhedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A very rare residual mineral, obtained by dissolution of halite in a drillcore through a marine evaporite series
Where rockhounds find penobsquisite
Classic worldwide localities
- Penobsquis evaporite deposit, near Sussex, New Brunswick, Canada
Field-hunting tip
Where it forms: A very rare residual mineral, obtained by dissolution of halite in a drillcore through a marine evaporite series. If you start seeing halite, sellaite, fluorite in float, you are in the right ground. Typical habit: euhedral crystals. Train your eye for that shape before scanning the outcrop.






