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 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Florencite-(Sm) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Florencite-(Sm) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, colorless.
- 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.
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
- 5-6
- Density
- 3.8-4.0 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral Crystals
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins and Metamorphic Rocks
- Typical price
- $50-500 depending on specimen size and locality
Where rockhounds find florencite-(sm)
Classic worldwide localities
- Brazil
- Madagascar
- China
Field-hunting tip
Look in hydrothermal veins and metamorphic rocks country — that is the host setting where florencite-(sm) typically forms. If you start seeing quartz, kaolinite, monazite in float, you are in the right ground. Field specimens usually show a rhombohedral crystals habit, so train your eye for that shape before scanning the outcrop.







