Pumpellyite-(Fe3+) typically occurs as radiating sprays or fibrous masses within low-grade metamorphic environments. It is often identified by its characteristic deep green color and habit in amygdaloidal basalts, where it frequently forms alongside native copper or other secondary minerals.
Is this pumpellyite-(fe3+)?
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 pumpellyite-(fe3+) with a known reference. Pumpellyite-(Fe3+) sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: green, brown, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, radiating, or massive aggregates.
Often confused with
Pumpellyite-(Fe3+) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pumpellyite-(fe3+)
Minerals reported to co-occur with pumpellyite-(fe3+). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Fe³⁺Al₂(SiO₄)(Si₂O₇)(OH)₂·H₂O
- Mohs hardness
- 5.5-6
- Density
- 3.25 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, radiating, or massive aggregates
- Cleavage
- Distinct in one direction
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- In altered porphyritic rocks
Where rockhounds find pumpellyite-(fe3+)
Classic worldwide localities
- Bulla, Trentino-Alto Adige, Italy
Field-hunting tip
Where it forms: In altered porphyritic rocks. If you start seeing plagioclase, hematite in float, you are in the right ground. Typical habit: fibrous, radiating, or massive aggregates. Train your eye for that shape before scanning the outcrop.





