• Chemistry: (Mg, Fe)7Si8O22(OH)2 , Magnesium Iron Silicate Hydroxide.
  • Class: Silicates
  • Subclass: Inosilicates
  • Group: Amphibole
  • Uses: Are limited to some asbestos uses and as mineral specimens.
  • Specimens

Cummingtonite is the name of a series as well as the name of a mineral. The mineral cummingtonite, is basically the middle member of the Cummingtonite Series, which include the minerals grunerite and magnesiocummingtonite. All three minerals' formulae are essentially the same: (Mg, Fe)7Si8O22(OH)2. However the percentage of magnesium to iron varies in the series and determines the mineral whereas, little else does. In grunerite, the iron rich member, the ratio of Mg/(Mg +Fe) equals 0.00 to 0.29; but in magnesiocummingtonite, as the name implies it is magnesium rich, the ratio equals 0.70 to 1.00. Cummingtonite by default has a ratio of 0.30 to 0.69, the majority of the middle and as can be expected is the most common member of the series.

Cummingtonite shares its formula with another mineral called anthophyllite. Cummingtonite and anthophyllite are polymorphs, a situation where two minerals share the same chemistry but have different structures (poly=many, morphs=shapes). Diamond and graphite are the most famous examples of polymorphism. In the case of anthophyllite and cummingtonite, anthophyllite is orthorhombic and cummingtonite is monoclinic. The two minerals can have similar distinctive brown colors and are hard to differentiate from each other, although cummingtonite is typically darker and slightly denser. Despite their distinctive brown color, the two are often indistinguishable from other amphiboles without optical or X-ray tests.

Cummingtonite is a common component of some regional metamorphic rocks. If more intense metamorphism were to occur, the minerals hypersthene, enstatite or olivine are produced at the expense of cummingtonite. Retrograde metamorphism can conversely restore cummingtonite as well as other iron-magnesium amphiboles.

One form of cummingtonite (a variety called "amosite") is asbestos-form and can be used as asbestos. Asbestos has many industrial uses despite some health risks and is made from different minerals, all with a fibrous habit. Serpentine and tremolite asbestos are considered the better varieties due to their greater flexibility and tensile strength, but cummingtonite asbestos has its uses and is being mined for this reason in South Africa.


  • Color is a dark grayish or greenish-brown and dark green.
  • Luster is silky to vitreous.
  • Transparency: Crystals are translucent to opaque.
  • Crystal System is monoclinic; 2/m.
  • Crystal Habits include fibrous, lamellar and radiating masses. Twinning is common and is either simple or lamellar.
  • Cleavage: is good in two directions at 56 and 124 degree angles.
  • Fracture is splintery.
  • Hardness is 5 - 6.
  • Specific Gravity is approximately 3.1 - 3.6 (average to slightly above average).
  • Streak is white.
  • Other Characteristics: Non-pleochroic.
  • Associated Minerals are hematite, hornblende, actinolite and anthophyllite.
  • Notable Occurrences include Cummington (hence the name), Hampshire County, Massachusetts; Homestake gold mine, Lawrence County, South Dakota and La Paz County, Arizona, USA; Scotland; South Africa and Sweden.
  • Best Field Indicators are crystal habit, fracture, cleavage, color, density and hardness.
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CUMMINGTONITE specimen cum-1
$ 60.00
Dims:1.9x1.3x1.1" (4.8x3.2x2.7 cm)
Wt: 1.7oz. (49g)
West Chesterfield, Massachusetts, U.S.A.
The host rock of this specimen is nearly covered completely with brown, fibrous, radiating crystals of cummingtonite. These crystals are opaque, or nearly so, and exhibit silky luster. Also present are tiny crystals of an unidentified black mineral. I believe these to be crystals of one of the manganese oxide minerals. There is no appreciable damage to this specimen.
no photo
cum-1 ($ 60.00)
West Chesterfield, Massachusetts, U.S.A.


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