Petedunnite is a rare zinc-rich pyroxene typically found in the famous ore deposits of Franklin, New Jersey. It is usually identified by its characteristic green color and granular habit within a complex mineral assemblage of zinc ores.
Is this petedunnite?
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 petedunnite with a known reference. Petedunnite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Petedunnite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Petedunnite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark green, yellow-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular, massive.
Often confused with
Petedunnite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Streak differs, so Petedunnite leaves white, Hedenbergite leaves white to pale green; luster reads vitreous on Petedunnite and vitreous to resinous on Hedenbergite.

How to tell apart: Streak differs, so Petedunnite leaves white, Augite leaves grayish white.
Often found alongside petedunnite
Minerals reported to co-occur with petedunnite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaZnSi₂O₆
- Mohs hardness
- 5-6
- Density
- 3.8-3.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular, Massive
- Cleavage
- Good in Two Directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Zinc Ore Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find petedunnite
Classic worldwide localities
- Franklin, New Jersey, USA
Field-hunting tip
Look in metamorphic zinc ore deposits country, the host setting where petedunnite typically forms. If you start seeing willemite, franklinite, zincite in float, you are in the right ground. Field specimens usually show a granular, massive habit, so train your eye for that shape before scanning the outcrop.




