Reedmergnerite is a rare boron-bearing member of the feldspar group, structurally similar to albite but with boron substituting for aluminum. It is most famous for its occurrences as small, transparent crystals within the oil shales of the Green River Formation in Utah. Collectors typically look for it in micro-mounts or small specimens from alkaline environments.
Is this reedmergnerite?
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 reedmergnerite with a known reference. Reedmergnerite sits at Mohs 6-7, 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, beige yellow, orange.
- 5Look at form & habitCrystal system: triclinic. Typical habit: prismatic crystals, blocky.
Often confused with
Reedmergnerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside reedmergnerite
Minerals reported to co-occur with reedmergnerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaBSi₃O₈
- Mohs hardness
- 6-7
- Density
- 2.70-2.78 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Prismatic crystals, blocky
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As authigenic crystals along bedding laminations, in brown dolomitic rock and black oil shale from well cuttings (Duchesne Co., Utah, USA)
Where rockhounds find reedmergnerite
Classic worldwide localities
- Joseph Smith #1 well, near Duchesne, Duchesne Co., Utah, USA
- Wind Mountain, Otero Co., New Mexico, USA
- Dara-i-Pioz massif, Alai Range, Tien Shan, Tajikistan
- Lovozero massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: As authigenic crystals along bedding laminations, in brown dolomitic rock and black oil shale from well cuttings (Duchesne Co., Utah, USA). If you start seeing eitelite, shortite, nahcolite in float, you are in the right ground. Typical habit: prismatic crystals, blocky. Train your eye for that shape before scanning the outcrop.








