Asimowite is a rare high-pressure silicate mineral identified almost exclusively in shocked meteorites. It typically occurs as microscopic inclusions within the vein material of meteorite specimens and requires specialized laboratory equipment for positive identification.
Is this asimowite?
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 asimowite with a known reference. Asimowite sits at Mohs 6, 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: blue, pale blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral to subhedral inclusions.
Often confused with
Asimowite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside asimowite
Minerals reported to co-occur with asimowite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂SiO₄
- Mohs hardness
- 6
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral to subhedral inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- shocked chondritic meteorites
Where rockhounds find asimowite
Classic worldwide localities
- Tenham meteorite
Field-hunting tip
Where it forms: shocked chondritic meteorites. If you start seeing ringwoodite, majorite, bridgmanite in float, you are in the right ground. Typical habit: anhedral to subhedral inclusions. Train your eye for that shape before scanning the outcrop.




