Grunerite is a cummingtonite-subgroup amphibole known for its association with iron-rich metamorphic rocks. It often presents in fibrous or radiating columnar masses and is most famous for its fibrous variety, amosite, historically used as a commercial form of asbestos.
Is this grunerite?
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 grunerite with a known reference. Grunerite 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. Grunerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Grunerite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, greenish-brown, gray, dark green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, columnar, or massive aggregates.
Often confused with
Grunerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside grunerite
Minerals reported to co-occur with grunerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₇Si₈O₂₂(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.4-3.6 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Columnar, Or Massive Aggregates
- Cleavage
- Perfect in Two Directions
- Rarity
- Common
- Uses
- Collector, Scientific Study
- Host rock
- Metamorphosed Iron Formations
- Typical price
- $10-100 depending on specimen size and quality
Where rockhounds find grunerite
Classic worldwide localities
- Ontario, Canada
- Minnesota, USA
- France
- Japan
- Switzerland
Field-hunting tip
Look in metamorphosed iron formations country — that is the host setting where grunerite typically forms. If you start seeing magnetite, quartz, hematite in float, you are in the right ground. Field specimens usually show a fibrous, columnar, or massive aggregates habit, so train your eye for that shape before scanning the outcrop.







