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?
4-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.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: yellowish white.
- 4Look at form & habitCrystal system: cubic. Typical habit: microscopic crystals.
Often confused with
Hapkeite vs. its common look-alikes, and how to tell them apart in the field.
All properties
- Chemical formula
- Fe₂Si
- Mohs hardness
- 5.5
- Density
- 6.83 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Microscopic crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a highland regolith breccia clast in the lunar meteorite Dhofar 280, formed by impact-induced, vapor-phase deposition under extreme reducing conditions in lunar soil
Where rockhounds find hapkeite
Classic worldwide localities
- Lunar meteorite Dhofar 280 collected in Dhofar Province (Al Janubiyah Province), Oman
Field-hunting tip
Where it forms: In a highland regolith breccia clast in the lunar meteorite Dhofar 280, formed by impact-induced, vapor-phase deposition under extreme reducing conditions in lunar soil. If you start seeing fesi, vitrified plagioclase, feni in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.


