Ferro-ferri-hornblende is a member of the complex amphibole group, typically appearing as dark, elongated prismatic crystals. It is primarily found in metamorphic environments and certain igneous intrusions, identified by its distinct cleavage angles. Collectors typically identify this mineral through X-ray diffraction or electron microprobe analysis due to its similarity to other hornblende species.
Is this ferro-ferri-hornblende?
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 ferro-ferri-hornblende with a known reference. Ferro-ferri-hornblende 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: vitreous.
- 3Match the color rangeCompare against the expected color range: dark green.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, fibrous, columnar, or massive.
Often confused with
Ferro-ferri-hornblende vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ferro-ferri-hornblende
Minerals reported to co-occur with ferro-ferri-hornblende. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Fe²⁺₄Fe³⁺(Si₇Al)O₂₂(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.362 g/cm³
- Colors
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, fibrous, columnar, or massive
- Cleavage
- Perfect on {110}
- Rarity
- Uncommon
- Uses
- Collector, Scientific research
- Host rock
- In a contact metamorphic rock (skarn)
Where rockhounds find ferro-ferri-hornblende
Classic worldwide localities
- Traversella iron mine, Val Chiusella, Ivrea, Piemonte, Italy
Field-hunting tip
Where it forms: In a contact metamorphic rock (skarn). If you start seeing tremolite, hastingsite, magnesio-hastingsite in float, you are in the right ground. Typical habit: prismatic crystals, fibrous, columnar, or massive. Train your eye for that shape before scanning the outcrop.









