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, 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.







