Smirnovskite is a rare radioactive phosphate-silicate mineral typically found as resinous, yellow to brown massive aggregates. It is primarily identified through its association with specific pegmatite environments and its significant thorium content.
Is this smirnovskite?
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 smirnovskite with a known reference. Smirnovskite sits at Mohs 4-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Smirnovskite leaves a yellowish-white streak.
- 3Read the lusterHold the specimen under a strong light. Smirnovskite typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, aggregates.
Often confused with
Smirnovskite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside smirnovskite
Minerals reported to co-occur with smirnovskite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Th,Ca,Ce)₂(P,Si)O₄(OH,F)·nH₂O
- Mohs hardness
- 4-5
- Density
- 4.8-5.0 g/cm³
- Streak
- Yellowish-white
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find smirnovskite
Classic worldwide localities
- Eastern Siberia, Russia
- Transbaikalia, Russia
Field-hunting tip
Look in granite pegmatites country, the host setting where smirnovskite typically forms. If you start seeing quartz, feldspar, mica in float, you are in the right ground. Field specimens usually show a massive, aggregates habit, so train your eye for that shape before scanning the outcrop.





