Ferri-mottanaite-(Ce) is a rare boron-bearing sorosilicate mineral belonging to the allanite group. It is primarily found in metamorphic environments and is identified by its distinct chemical composition featuring iron and cerium, usually occurring as small, brownish, prismatic crystals.
Is this ferri-mottanaite-(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 ferri-mottanaite-(ce) with a known reference. Ferri-mottanaite-(Ce) sits at Mohs 6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ferri-mottanaite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ferri-mottanaite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, reddish-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Ferri-mottanaite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferri-mottanaite-(ce)
Minerals reported to co-occur with ferri-mottanaite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCe₄Fe³⁺(Si₂B)O₁₂F(OH)₂
- Mohs hardness
- 6
- Density
- 3.8-4.0 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find ferri-mottanaite-(ce)
Classic worldwide localities
- Malenco Valley, Italy
- Gravelotte, South Africa
Field-hunting tip
Look in metamorphic rocks country — that is the host setting where ferri-mottanaite-(ce) typically forms. If you start seeing quartz, albite, titanite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.







