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, 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.



