Stöfflerite is a rare high-pressure polymorph of calcium-rich feldspar discovered in impact craters. It is typically found as small, microscopic inclusions within impact-melted rocks alongside other shock-metamorphosed minerals. Collectors rarely encounter this mineral as it is primarily significant in planetary science and petrology research.
Is this stöfflerite?
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 stöfflerite with a known reference. Stöfflerite 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. Stöfflerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Stöfflerite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Stöfflerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside stöfflerite
Minerals reported to co-occur with stöfflerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Al₄Si₈O₂₄
- Mohs hardness
- 6
- Density
- 2.75 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Scientific Study, Collector
- Host rock
- Impact Melt Breccia
- Typical price
- n/a (extremely rare specimen, typically in institutional collections)
Where rockhounds find stöfflerite
Classic worldwide localities
- Nördlinger Ries crater, Germany
Field-hunting tip
Look in impact melt breccia country — that is the host setting where stöfflerite typically forms. If you start seeing maskelynite, coesite, stishovite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.




