Oxystibiomicrolite is a rare antimony calcium tantalum oxide, typically greenish white to white. It was approved as a distinct mineral species in 1938. It was first described from Varuträsk pegmatite, 15 km northwest of Skellefteå, Västerbotten, Sweden.
Is this oxystibiomicrolite?
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 oxystibiomicrolite with a known reference. Oxystibiomicrolite sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Oxystibiomicrolite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Oxystibiomicrolite typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: greenish white, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals.
Often confused with
Oxystibiomicrolite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside oxystibiomicrolite
Minerals reported to co-occur with oxystibiomicrolite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Sb³⁺,Ca)₂Ta₂O₆O
- Mohs hardness
- 5-5.5
- Density
- 5.84-6.22 g/cm³
- Colors
- Streak
- White
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Octahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
Where rockhounds find oxystibiomicrolite
Classic worldwide localities
- Varuträsk pegmatite, Västerbotten, Sweden
Field-hunting tip
Look in granite pegmatites country, the host setting where oxystibiomicrolite typically forms. If you start seeing stibnite, quartz, bismutite in float, you are in the right ground. Field specimens usually show a octahedral crystals habit, so train your eye for that shape before scanning the outcrop.



