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anthophyllite
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anthophyllite

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Anthophyllite is an orthorhombic amphibole mineral: ☐Mg2Mg5Si8O22(OH)2 (☐ is for a vacancy, a point defect in the crystal structure), magnesium iron inosilicate hydroxide. Anthophyllite is polymorphic with cummingtonite. Some forms of anthophyllite are lamellar or fibrous and are classed as asbestos. The name is derived from the Latin word anthophyllum, meaning clove, an allusion to the most common color of the mineral. The Anthophyllite crystal is characterized by its perfect cleavage along directions 126 degrees and 54 degrees.

Key facts

Mineral.name
Anthophyllite
Mineral.category
InosilicatesAmphibole
Mineral.image
Anthophyllite Suède Fond.jpg
Mineral.imagesize
260px
Mineral.formula
☐Mg2Mg5Si8O22(OH)2
Mineral.IMAsymbol
Ath
Mineral.strunz
9.DE.05
Mineral.system
Orthorhombic
Mineral.class
Dipyramidal (mmm)H-M symbol: (2/m 2/m 2/m)
Mineral.symmetry
Pnma
Mineral.unit cell
a = 18.5, b = 17.9c = 5.28 [Å]; Z = 4
Mineral.color
Gray to green, brown, and beige
Mineral.habit
Rarely as distinct crystals. Commonly lamellar or fibrous.
Mineral.cleavage
Perfect on {210}, imperfect on {010}, {100}
Mineral.tenacity
Brittle; elastic when fibrous
Mineral.mohs
5.5 – 6
Mineral.luster
Vitreous, pearly on cleavage
Mineral.refractive
nα=1.598 – 1.674, nβ=1.605 – 1.685, nγ=1.615 – 1.697; indices increase with Fe content

via Wikipedia infobox

Wikidata facts

Image
Anthophyllite Suède Fond.jpg
Show 6 more facts
Nickel-Strunz 9th edition (updated 2009)
9.DE.05
Commons category
Anthophyllite
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
9.DE.05
IMA Mineral Symbol
Ath
chemical formula
☐Mg₂Mg₅Si₈O₂₂(OH)₂
Strunz 8th edition (series ID, updated)
VIII/D.06
Sources (3)

via Wikidata · CC0

~5 min read

Article

4 sections
Contents
  • Occurrence
  • Occurrence in ultramafic rocks
  • Fibrous anthophyllite
  • References

{{Infobox mineral | name = Anthophyllite | category = InosilicatesAmphibole | image = Anthophyllite Suède Fond.jpg | imagesize = 260px | alt = | caption = | formula = ☐Mg2Mg5Si8O22(OH)2 |IMAsymbol=Ath | strunz = 9.DE.05 | system = Orthorhombic | class = Dipyramidal (mmm)H-M symbol: (2/m 2/m 2/m) | symmetry = Pnma | unit cell = a = 18.5, b = 17.9c = 5.28 [Å]; Z = 4 | color = Gray to green, brown, and beige | habit = Rarely as distinct crystals. Commonly lamellar or fibrous. | twinning = | cleavage = Perfect on {210}, imperfect on {010}, {100} | fracture = | tenacity = Brittle; elastic when fibrous | mohs = 5.5 – 6 | luster = Vitreous, pearly on cleavage | refractive = nα=1.598 – 1.674, nβ=1.605 – 1.685, nγ=1.615 – 1.697; indices increase with Fe content | opticalprop = Biaxial (+) | 2V = 57° - 90° | birefringence = δ = 0.017 – 0.023 | pleochroism = | streak = White to gray | gravity = 2.85 – 3.2 | melt = | fusibility = | diagnostic = Characterized by clove brown color, but unless in crystals, difficult to distinguish from other amphiboles without optical and/or X-ray tests | solubility = | diaphaneity = Transparent to translucent | other = | references = }}

Anthophyllite is an orthorhombic amphibole mineral: ☐Mg2Mg5Si8O22(OH)2 (☐ is for a vacancy, a point defect in the crystal structure), magnesium iron inosilicate hydroxide. Anthophyllite is polymorphic with cummingtonite. Some forms of anthophyllite are lamellar or fibrous and are classed as asbestos. The name is derived from the Latin word anthophyllum, meaning clove, an allusion to the most common color of the mineral. The Anthophyllite crystal is characterized by its perfect cleavage along directions 126 degrees and 54 degrees.

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