Rosiaite is a very rare lead-antimony oxide mineral originally discovered in the gold-mining district of Rosia Montana, Romania. It typically forms small, distinct yellow crystals associated with other secondary lead minerals and gold-bearing ores.
Is this rosiaite?
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 rosiaite with a known reference. Rosiaite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rosiaite leaves a yellowish-white streak.
- 3Read the lusterHold the specimen under a strong light. Rosiaite typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular to rhombohedral crystals.
Often confused with
Rosiaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside rosiaite
Minerals reported to co-occur with rosiaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbSb₂O₆
- Mohs hardness
- 3-4
- Density
- 4.95 g/cm³
- Colors
- Streak
- Yellowish-white
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular to Rhombohedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Epithermal Gold-silver Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find rosiaite
Classic worldwide localities
- Rosia Montana, Romania
Field-hunting tip
Look in hydrothermal epithermal gold-silver deposits country — that is the host setting where rosiaite typically forms. If you start seeing quartz, pyrite, galena in float, you are in the right ground. Field specimens usually show a tabular to rhombohedral crystals habit, so train your eye for that shape before scanning the outcrop.





