Florencite-(Nd) is a rare phosphate mineral characterized by its neodymium dominance within the florencite group. It typically appears as small, rhombohedral crystals in metamorphic environments and is highly prized by advanced mineral collectors for its chemical specificity.
Is this florencite-(nd)?
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-(nd) with a known reference. Florencite-(Nd) 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: earthy.
- 4Match the color rangeCompare against the expected color range: pink, yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: rhombohedral crystals.
Often confused with
Florencite-(Nd) vs. its common look-alikes, and how to tell them apart in the field.

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

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

How to tell apart: Luster reads earthy on Florencite-(Nd) and vitreous on Gorceixite.
Often found alongside florencite-(nd)
Minerals reported to co-occur with florencite-(nd). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NdAl₃(PO₄)₂(OH)₆
- Mohs hardness
- 5-6
- Density
- 3.5-3.55 g/cm³
- Streak
- White
- Luster
- Earthy
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral crystals
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Lining surfaces of fractures in a weathered chert layer in shale
Where rockhounds find florencite-(nd)
Classic worldwide localities
- Minas Gerais, Brazil
- Ituri Province, Democratic Republic of the Congo
- San Bernardino County, California, USA
Field-hunting tip
Where it forms: Lining surfaces of fractures in a weathered chert layer in shale. If you start seeing churchite-, todorokite, lithiophorite in float, you are in the right ground. Typical habit: rhombohedral crystals. Train your eye for that shape before scanning the outcrop.



