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 — 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 — 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 — that is 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.




