Chromferide is an extremely rare iron-chromium alloy first discovered in the Khatyrka meteorite. It occurs as microscopic grains within extraterrestrial rock and is significant for its unique composition and discovery in a quasicrystal-bearing meteorite.
Is this chromferide?
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 chromferide with a known reference. Chromferide sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: gray white.
- 5Look at form & habitCrystal system: cubic. Typical habit: grains.
Often confused with
Chromferide vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chromferide
Minerals reported to co-occur with chromferide. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₁.₅Cr₀.₂
- Mohs hardness
- 4
- Density
- 6.69 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Research, Collector
- Host rock
- In quartz veins within brecciated amphibolites and schist
Where rockhounds find chromferide
Classic worldwide localities
- Southern Ural Mountains, Russia (type locality)
Field-hunting tip
Where it forms: In quartz veins within brecciated amphibolites and schist. If you start seeing iron, copper, bismuth in float, you are in the right ground. Typical habit: grains. Train your eye for that shape before scanning the outcrop.







