Byströmite is a rare magnesium antimonate mineral that typically forms as small, prismatic, transparent yellow crystals. It is most commonly found in association with antimony ore bodies and is a prized target for advanced mineral collectors.
Is this byströmite?
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 byströmite with a known reference. Byströmite sits at Mohs ~7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale gray.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: blue.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: prismatic crystals.
Often confused with
Byströmite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside byströmite
Minerals reported to co-occur with byströmite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgSb₂O₆
- Mohs hardness
- ~7
- Density
- 5.5 g/cm³
- Colors
- Streak
- Pale gray
- Luster
- Adamantine
- Transparency
- Transparent to translucent
- Crystal system
- Tetragonal
- Crystal habit
- Prismatic crystals
- Cleavage
- Distinct on {110}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In quartz veins in an oxidized antimony deposit
Where rockhounds find byströmite
Classic worldwide localities
- La Fortuna and San Jose mines, El Antimonio, 27 km southwest of Agua Prieta, Sonora, Mexico
Field-hunting tip
Where it forms: In quartz veins in an oxidized antimony deposit. If you start seeing stibiconite, quartz in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.


