Ahrensite is a rare high-pressure mineral of the spinel group, discovered primarily in shocked Martian meteorites. It forms as a result of the transformation of olivine under the extreme temperatures and pressures experienced during cosmic impact events.
Is this ahrensite?
3-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 ahrensite with a known reference. Ahrensite sits at Mohs 8, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: bluish green.
- 3Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals.
Often confused with
Ahrensite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ahrensite
Minerals reported to co-occur with ahrensite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂SiO₄
- Mohs hardness
- 8
- Density
- 4.26 g/cm³
- Colors
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Octahedral crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- From the transformation of fayalite-rich rims of olivine megacrysts or Fe-rich microphenocrysts in contact with shock melt pockets in an olivine-phyric shergottite meteorite [TL]
Where rockhounds find ahrensite
Classic worldwide localities
- Tissint meteorite
- Zagami meteorite
Field-hunting tip
Where it forms: From the transformation of fayalite-rich rims of olivine megacrysts or Fe-rich microphenocrysts in contact with shock melt pockets in an olivine-phyric shergottite meteorite [TL]. If you start seeing bridgmanite, ringwoodite, wüstite in float, you are in the right ground. Typical habit: octahedral crystals. Train your eye for that shape before scanning the outcrop.









