Pumpellyite-(Al) is a sorosilicate mineral typically found in low-grade metamorphic rocks, particularly altered basalts. It is easily identified by its characteristic green color and often appears as fine-grained, radiating, or fibrous aggregates in vesicles and fractures.
Is this pumpellyite-(al)?
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-(al) with a known reference. Pumpellyite-(Al) 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-(Al) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pumpellyite-(Al) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, bluish-green, brownish-green, yellowish-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, radiating, platy aggregates, massive.
Often confused with
Pumpellyite-(Al) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pumpellyite-(al)
Minerals reported to co-occur with pumpellyite-(al). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Al₂Mg(Si₂O₇)(SiO₄)(OH)₂·H₂O
- Mohs hardness
- 5.5
- Density
- 3.18-3.23 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Radiating, Platy Aggregates, Massive
- Cleavage
- Good On {001}
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Metamorphic Basalt, Low-grade Metamorphic Rocks
- Typical price
- $10-50 per specimen depending on size and crystal clarity.
Where rockhounds find pumpellyite-(al)
Classic worldwide localities
- Keweenaw Peninsula, Michigan, USA
- Hokkaido, Japan
- New Caledonia
- Western Alps, Italy
Field-hunting tip
Look in metamorphic basalt, low-grade metamorphic rocks country — that is the host setting where pumpellyite-(al) typically forms. If you start seeing chlorite, quartz, calcite in float, you are in the right ground. Field specimens usually show a fibrous, radiating, platy aggregates, massive habit, so train your eye for that shape before scanning the outcrop.






