Perryite is a rare phosphide mineral found exclusively in iron meteorites. It typically occurs as small, bronze-colored metallic grains intergrown with other nickel-iron meteoritic minerals.
Is this perryite?
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 perryite with a known reference. Perryite sits at Mohs 4-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Perryite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Perryite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: bronze, yellow-brown.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: anhedral grains, massive, interstitial.
Often confused with
Perryite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside perryite
Minerals reported to co-occur with perryite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ni,Fe)₈(Si,P)₃
- Mohs hardness
- 4-5
- Density
- 7.05 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Anhedral Grains, Massive, Interstitial
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Iron Meteorites
- Typical price
- Very high, generally only available in meteorite study collections.
Where rockhounds find perryite
Classic worldwide localities
- Perry Station, Tennessee, USA
- Various iron meteorites
Field-hunting tip
Look in iron meteorites country, the host setting where perryite typically forms. If you start seeing kamacite, taenite, schreibersite in float, you are in the right ground. Field specimens usually show a anhedral grains, massive, interstitial habit, so train your eye for that shape before scanning the outcrop.



