Cummingtonite is a monoclinic amphibole that typically forms fibrous or columnar masses in metamorphic environments. It is most easily identified by its characteristic brownish-grey color and its tendency to occur in radiating or bladed habit. It is found in metamorphosed iron-rich deposits and regional metamorphic rocks.
Is this cummingtonite?
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 cummingtonite with a known reference. Cummingtonite 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. Cummingtonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Cummingtonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, gray, greenish-gray, tan.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, columnar, lamellar, or radiating aggregates.
Often confused with
Cummingtonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cummingtonite
Minerals reported to co-occur with cummingtonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- □Mg₂(Mg₅)Si₈O₂₂(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.1-3.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Columnar, Lamellar, Or Radiating Aggregates
- Cleavage
- Perfect in Two Directions At 56 and 124 Degrees
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphosed Iron-rich Rocks, Amphibolites, And Contact Metamorphic Zones
- Typical price
- $10-60 thumbnail, $50-200 cabinet specimen
Where rockhounds find cummingtonite
1 mapped spotsClassic worldwide localities
- Cummington, Massachusetts, USA
- Bod Bodenmais, Bavaria, Germany
- Franklin, New Jersey, USA
- Dalnegorsk, Russia
Field-hunting tip
Look in metamorphosed iron-rich rocks, amphibolites, and contact metamorphic zones country — that is the host setting where cummingtonite typically forms. If you start seeing garnet, hornblende, magnetite in float, you are in the right ground. Field specimens usually show a fibrous, columnar, lamellar, or radiating aggregates habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Wisconsin — start trip planning there.








