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, 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.








