Stanfieldite is a rare phosphate mineral primarily known for its occurrence in stony-iron meteorites like pallasites. It typically forms as small, microscopic inclusions within the silicate and metallic phases of these extraterrestrial rocks.
Is this stanfieldite?
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 stanfieldite with a known reference. Stanfieldite sits at Mohs 4.5-5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow brown, reddish yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains.
Often confused with
Stanfieldite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside stanfieldite
Minerals reported to co-occur with stanfieldite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄Mg₅(PO₄)₆
- Mohs hardness
- 4.5-5
- Density
- 3.15 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- A rare component of some meteorites
Where rockhounds find stanfieldite
Classic worldwide localities
- Estherville mesosiderite meteorite, and the pallasite meteorites Albin, Finmarken, Imilac, Newport, Mount Vernon, Santa Rosalia, and Zaisho
Field-hunting tip
Where it forms: A rare component of some meteorites. If you start seeing olivine, whitlockite, farringtonite in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.




