Pumpellyite-(Mg) is a sorosilicate mineral frequently found as a secondary mineral in altered igneous rocks. It is most recognized for its distinct radiating or fibrous habit in shades of green and blue-green, often forming within veins or amygdules.
Is this pumpellyite-(mg)?
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-(mg) with a known reference. Pumpellyite-(Mg) sits at Mohs 5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pumpellyite-(Mg) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pumpellyite-(Mg) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, blue-green, brown, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, radiating, or acicular crystals; also massive.
Often confused with
Pumpellyite-(Mg) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pumpellyite-(mg)
Minerals reported to co-occur with pumpellyite-(mg). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂MgAl₂(SiO₄)(Si₂O₇)(OH)₂·H₂O
- Mohs hardness
- 5.5
- Density
- 3.1-3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Radiating, Or Acicular Crystals; Also Massive
- Cleavage
- Poor
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Low-grade Metamorphic Rocks, Particularly Metabasalt and Glaucophane Schist
- Typical price
- $10-50 thumbnail
Where rockhounds find pumpellyite-(mg)
Classic worldwide localities
- Keweenaw Peninsula, USA
- New Caledonia
- Val Malenco, Italy
- Japan
Field-hunting tip
Look in low-grade metamorphic rocks, particularly metabasalt and glaucophane schist country — that is the host setting where pumpellyite-(mg) typically forms. If you start seeing epidote, prehnite, quartz in float, you are in the right ground. Field specimens usually show a fibrous, radiating, or acicular crystals; also massive habit, so train your eye for that shape before scanning the outcrop.






