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.

Hardness
5.5-6
Mohs
Luster
Vitreous
Streak
White
Transparency
Semitransparent

Is this pumpellyite-(fe3+)?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try 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.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: green, brown, black.
  • 5
    Look at form & habit
    Crystal 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.

Common questions

How do you identify pumpellyite-(fe3+)?+
Mohs hardness is 5.5-6. Luster: vitreous. The streak is white. Common colors include green, brown, black.
Where is pumpellyite-(fe3+) found?+
Notable localities include Bulla, Trentino-Alto Adige, Italy.
What rocks look like pumpellyite-(fe3+)?+
Pumpellyite-(Fe3+) is most often confused with Epidote, Prehnite, Actinolite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with pumpellyite-(fe3+)?+
Pumpellyite-(Fe3+) commonly co-occurs with Plagioclase, Hematite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does pumpellyite-(fe3+) form in?+
Where it forms: In altered porphyritic rocks. Working float back to the host body is the standard way to chase a fresh occurrence.
What is pumpellyite-(fe3+) used for?+
Pumpellyite-(Fe3+) is used in collector.

Find pumpellyite-(fe3+) on the map

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