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 — that is 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.



