Hapkeite is an extremely rare iron silicide mineral first discovered within lunar meteorites. It typically occurs as microscopic inclusions within the fusion crust or regolith of meteorites and is characterized by its distinct metallic luster and cubic structure.
Is this hapkeite?
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 hapkeite with a known reference. Hapkeite sits at Mohs 5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Hapkeite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Hapkeite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, light gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: microscopic grains.
Often confused with
Hapkeite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hapkeite
Minerals reported to co-occur with hapkeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂Si
- Mohs hardness
- 5.5
- Density
- 6.5 g/cm³
- Colors
- Streak
- White
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Microscopic Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Meteorites
- Typical price
- $500-5000+ per microscopic specimen
Where rockhounds find hapkeite
Classic worldwide localities
- Dhofar 280 meteorite (Oman)
- Moon (regolith samples)
Field-hunting tip
Look in meteorites country — that is the host setting where hapkeite typically forms. If you start seeing iron, troilite, kamacite in float, you are in the right ground. Field specimens usually show a microscopic grains habit, so train your eye for that shape before scanning the outcrop.




