Florencite-(Sm) is a rare rare-earth element phosphate mineral belonging to the beudantite group. It typically occurs as small rhombohedral crystals in hydrothermal deposits and altered metamorphic rocks, and can be visually indistinguishable from other members of the florencite series without analytical testing.
Is this florencite-(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 florencite-(sm) with a known reference. Florencite-(Sm) sits at Mohs 5.5-6, 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: colorless, pale pink, pale yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: rhombohedral crystals.
Often confused with
Florencite-(Sm) vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Luster reads vitreous to greasy on Florencite-(Sm) and greasy to resinous on Florencite-(Ce).

How to tell apart: Luster reads vitreous to greasy on Florencite-(Sm) and greasy to resinous on Florencite-(La).

Often found alongside florencite-(sm)
Minerals reported to co-occur with florencite-(sm). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SmAl₃(PO₄)₂(OH)₆
- Mohs hardness
- 5.5-6
- Density
- 3.60 g/cm³
- Streak
- White
- Luster
- Vitreous to greasy
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral crystals
- Cleavage
- Perfect on {0001}; parting on {112̄0}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In quartz veins cutting quartz meta-conglomerate beds near contacts with Al-enriched metasomatites
Where rockhounds find florencite-(sm)
Classic worldwide localities
- Svodovyi site, Maldynyrd Ridge, Subpolar Urals, Russia
Field-hunting tip
Where it forms: In quartz veins cutting quartz meta-conglomerate beds near contacts with Al-enriched metasomatites. If you start seeing florencite-, xenotime-, quartz in float, you are in the right ground. Typical habit: rhombohedral crystals. Train your eye for that shape before scanning the outcrop.


