• 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

Anthophyllite is a common component of some metamorphic and metasomatic rocks. Its name comes from the Latin word for clove and is an allusion to its typical and distinct clove-brown color. Although it can be differentiated from other amphiboles by its white to brown color, it is often indistinguishable from other amphiboles such as cummingtonite. Cummingtonite and anthophyllite are actually 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.

Anthophyllite is metamorphic and is found in gneisses and schists derived from magnesium rich igneous or dolomitic sedimentary rocks. It also forms from the retrograde metamorphism of other metamorphic minerals and from the metasomatic alteration of olivine and other ultramafic minerals when these minerals are subjected to pressure in the presence of water. Under different conditions (such as more water), serpentine would be the mineral produced from the alteration of olivine.

Like serpentine, some forms of anthophyllite are asbestos-form and can be used as asbestos. Asbestos has many industrial uses despite some health risks and is made of 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 anthophyllite asbestos has its uses such as in refractory cements.

Although individual well formed crystals of anthophyllite are very rare, some aggregate specimens of anthophyllite are striking and can make nice collection pieces. One variety found at Butte, Montana even displays a nice blue schiller effect.


  • Color is usually various shades of brown such as yellow-brown, green-brown or brownish-gray, but also green, off-white or gray.
  • Luster is vitreous to dull or silky in fibrous forms.
  • Transparency: Crystals are translucent to opaque.
  • Crystal System is orthorhombic; 2/m 2/m 2/m.
  • Crystal Habits include prismatic often aggregated crystals and fibrous, asbestos-like masses.
  • Cleavage: is good in two directions at 56 and 124 degree angles forming wedge shapes fragments.
  • Fracture is easy and splintery.
  • Hardness is 5.5 - 6.
  • Specific Gravity is approximately 2.9 - 3.4 (average to slightly above average).
  • Streak is gray.
  • Other Characteristics: Weakly pleochroic and a blue schiller effect is seen in some specimens from Butte, Montana.
  • Associated Minerals are talc, cordierite and phlogopite.
  • Notable Occurrences include Butte, Montana; Delaware County, Pennsylvania; California; Arizona and Franklin County, North Carolina, USA; Ontario, Canada; Greenland; Kongsburg, Norway and Italy.
  • Best Field Indicators are crystal habit, fracture, cleavage, color, streak and hardness.
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ANTHOPHYLLITE specimen ath-1
$ 60.00
Dims: 2.0 x 1.7 x 1.0" (5.1 x 4.3 x 2.5 cm)
Wt: 2.4 oz. (67 g)
Harmanov, Czech Republic
This interesting hand specimen consists of a rounded Anthophyllite "nodule". The nodule consists of a layer of compact, fibrous Anthophyllite that surrounds a core of phlogopite mica. The Anthophyllite layer measures about 0.3" (8 mm) in thickness and is broken open, exposing its fibrous habit. It has a dull gray color and a pearly luster and is essentially opaque. The existing outer surface of the nodule is coated with more phlogopite, but no complete crystals are present.
no photo
ath-1 ($ 60.00)
Harmanov, Czech Republic


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