Ferro-ferri-obertiite is a rare member of the amphibole supergroup characterized by high iron and sodium content. It typically occurs as small prismatic crystals within alkaline igneous environments and is primarily sought after by advanced mineral collectors and researchers.
Is this ferro-ferri-obertiite?
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 ferro-ferri-obertiite with a known reference. Ferro-ferri-obertiite 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. Ferro-ferri-obertiite leaves a pale green streak.
- 3Read the lusterHold the specimen under a strong light. Ferro-ferri-obertiite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark green, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic, granular.
Often confused with
Ferro-ferri-obertiite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferro-ferri-obertiite
Minerals reported to co-occur with ferro-ferri-obertiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(Na₂)(Fe²⁺₃Fe³⁺₂)(Si₈O₂₂)O₂
- Mohs hardness
- 5-6
- Density
- 3.3-3.4 g/cm³
- Colors
- Streak
- Pale Green
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic, Granular
- Cleavage
- Perfect Prismatic
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find ferro-ferri-obertiite
Classic worldwide localities
- Italy
- Canada
Field-hunting tip
Look in alkaline igneous rocks country — that is the host setting where ferro-ferri-obertiite typically forms. If you start seeing quartz, albite, aegirine in float, you are in the right ground. Field specimens usually show a prismatic, granular habit, so train your eye for that shape before scanning the outcrop.






