Anzaite-(Ce) is a rare cerium iron titanium oxide belonging to the aeschynite group. It is typically found as small, dark, submetallic prismatic crystals within alkaline pegmatite environments, often identified by its distinct chemical composition and specific geological associations.
Is this anzaite-(ce)?
4-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 anzaite-(ce) with a known reference. Anzaite-(Ce) sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: submetallic.
- 3Match the color rangeCompare against the expected color range: grayish black.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Anzaite-(Ce) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside anzaite-(ce)
Minerals reported to co-occur with anzaite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ce₄³⁺Fe²⁺Ti₆O₁₈(OH)₂
- Mohs hardness
- 5-6
- Density
- 5.054 g/cm³
- Colors
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late hydrothermal mineral in altered calcite-amphibole-clinopyroxene silicocarbonatite
Where rockhounds find anzaite-(ce)
Classic worldwide localities
- Afrikanda silicocarbonatite, Kola Peninsula, Russia
Field-hunting tip
Where it forms: A late hydrothermal mineral in altered calcite-amphibole-clinopyroxene silicocarbonatite. If you start seeing titanite, hibschite, clinochlore in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.






