Monazite-(Sm) is a very rare rare-earth phosphate mineral belonging to the monazite group. It typically occurs as small crystals in complex pegmatites and is highly prized by collectors for its chemical specificity, despite being mildly radioactive due to thorium impurities.
Is this monazite-(sm)?
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 monazite-(sm) with a known reference. Monazite-(Sm) 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to greasy.
- 4Match the color rangeCompare against the expected color range: yellowish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy, subhedral crystals.
Often confused with
Monazite-(Sm) vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Monazite-(Sm) leaves white, Monazite-(Ce) leaves grayish white; luster reads vitreous to greasy on Monazite-(Sm) and resinous, waxy, vitreous to adamantine on Monazite-(Ce).

How to tell apart: Zircon is the harder of the two (Mohs 7.5 vs. 5-5.5).

Often found alongside monazite-(sm)
Minerals reported to co-occur with monazite-(sm). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SmPO₄
- Mohs hardness
- 5-5.5
- Density
- 5.478 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to greasy
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy, subhedral crystals
- Cleavage
- One good direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- From the inner intermediate zone of a lepidolite-subtype granitic pegmatite
Where rockhounds find monazite-(sm)
Classic worldwide localities
- Annie Claim no. 3, near Greer Lake, near the Winnipeg River, southeastern Manitoba, Canada
- Shimo-ono ilmenite-series granitic pegmatite, Ibaraki, Japan
Field-hunting tip
Where it forms: From the inner intermediate zone of a lepidolite-subtype granitic pegmatite. If you start seeing quartz, albite, lithian muscovite in float, you are in the right ground. Typical habit: platy, subhedral crystals. Train your eye for that shape before scanning the outcrop.





