Horomanite is a rare iron nickel sulfide that forms grains. It is a filling space between silicate minerals in lherzolites of a peridotite massif. It was first described from Horoman peridotite massif, Samani-cho, Samani-gun, Hokkaido, Japan.
Is this horomanite?
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 horomanite with a known reference. Horomanite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: brown, yellowish-brown.
- 4Look at form & habitCrystal system: tetragonal. Typical habit: grains.
Often confused with
Horomanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside horomanite
Minerals reported to co-occur with horomanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₆Ni₃S₈
- Mohs hardness
- 3
- Density
- 6.44 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Grains
- Cleavage
- Pronounced
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Filling space between silicate minerals in lherzolites of a peridotite massif
Where rockhounds find horomanite
Classic worldwide localities
- Horoman peridotite massif, Samani-cho, Samani-gun, Hokkaido, Japan
Field-hunting tip
Where it forms: Filling space between silicate minerals in lherzolites of a peridotite massif. If you start seeing bornite, talnakhite, copper in float, you are in the right ground. Typical habit: grains. Train your eye for that shape before scanning the outcrop.







