Stishovite is a high-pressure polymorph of silica that forms primarily during meteorite impacts. It is extremely rare in nature and is typically found as microscopic grains embedded within shocked quartz or impact melt rocks.
Is this stishovite?
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 stishovite with a known reference. Stishovite sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Stishovite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Stishovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: microcrystalline aggregates.
Often confused with
Stishovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside stishovite
Minerals reported to co-occur with stishovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SiO₂
- Mohs hardness
- 6.5-7
- Density
- 4.28 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Microcrystalline Aggregates
- Cleavage
- Distinct On {110}
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Impact Craters and Metamorphic Rocks Subjected to Extreme Pressure
- Typical price
- $50-500 depending on specimen size and source
Where rockhounds find stishovite
Classic worldwide localities
- Barringer Crater, USA
- Ries Crater, Germany
- Vredefort Crater, South Africa
- Popigai Crater, Russia
Field-hunting tip
Look in impact craters and metamorphic rocks subjected to extreme pressure country — that is the host setting where stishovite typically forms. If you start seeing coesite, quartz, glass in float, you are in the right ground. Field specimens usually show a microcrystalline aggregates habit, so train your eye for that shape before scanning the outcrop.




