Ferchromide is an extremely rare iron-chromium alloy typically found as microscopic inclusions within chromite grains in ophiolitic rocks. Due to its metallic nature and rarity, it is almost exclusively a micro-mineral for advanced collectors and researchers studying geological mantle processes.
Is this ferchromide?
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 ferchromide with a known reference. Ferchromide 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. Ferchromide leaves a gray streak.
- 3Read the lusterHold the specimen under a strong light. Ferchromide typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: grains.
Often confused with
Ferchromide vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferchromide
Minerals reported to co-occur with ferchromide. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CrFe
- Mohs hardness
- 5-6
- Density
- 6.5-7.0 g/cm³
- Colors
- Streak
- Gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ophiolite Complexes
- Typical price
- $50-500 depending on specimen size and rarity
Where rockhounds find ferchromide
Classic worldwide localities
- Oman
- Russia
Field-hunting tip
Look in ophiolite complexes country — that is the host setting where ferchromide typically forms. If you start seeing chromite, olivine, serpentine in float, you are in the right ground. Field specimens usually show a grains habit, so train your eye for that shape before scanning the outcrop.



