Arsenoflorencite-(Ce) is a rare secondary mineral belonging to the florencite group, typically occurring as small rhombohedral crystals. It is primarily identified by its characteristic association with arsenic-rich environments in hydrothermally altered host rocks.
Is this arsenoflorencite-(ce)?
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 arsenoflorencite-(ce) with a known reference. Arsenoflorencite-(Ce) 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. Arsenoflorencite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Arsenoflorencite-(Ce) 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
Arsenoflorencite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside arsenoflorencite-(ce)
Minerals reported to co-occur with arsenoflorencite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CeAsAl₃(PO₄)₂(OH)₆
- Mohs hardness
- 5-6
- Density
- 4.15 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral Crystals
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Tin Deposits and Kaolinized Rhyolite
- Typical price
- $50-300 per specimen
Where rockhounds find arsenoflorencite-(ce)
Classic worldwide localities
- Black Range, New Mexico, USA
- Itambe, Brazil
Field-hunting tip
Look in hydrothermal tin deposits and kaolinized rhyolite country — that is the host setting where arsenoflorencite-(ce) typically forms. If you start seeing quartz, hematite, kaolinite 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.




