Shocked quartz consists of quartz grains that have been subjected to high-pressure shock waves from meteoritic impacts. Under a microscope, it exhibits characteristic planar deformation features (PDFs) that distinguish it from ordinary quartz. It is primarily found in ejecta blankets and impact melt rocks at identified terrestrial impact craters.
Is this shocked quartz?
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 shocked quartz with a known reference. Shocked Quartz sits at Mohs 7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Shocked Quartz leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Shocked Quartz typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: clear, white, gray, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: massive.
Often confused with
Shocked Quartz vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside shocked quartz
Minerals reported to co-occur with shocked quartz. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SiO₂
- Mohs hardness
- 7
- Density
- 2.65 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Impact Breccia
- Typical price
- $20-200 depending on specimen size and provenance
Where rockhounds find shocked quartz
Classic worldwide localities
- Barringer Crater, USA
- Ries Crater, Germany
- Manicouagan Crater, Canada
- Sudbury Basin, Canada
Field-hunting tip
Look in impact breccia country — that is the host setting where shocked quartz typically forms. If you start seeing coesite, stishovite in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop.





