Axinite-(Fe)

Ca4Fe2+2Al4[B2Si8O30](OH)2
IMA status
  • Approved
  • Grandfathered
IMA symbol
Ax-Fe
Also known as
  • Axiniet-(Fe)
  • Axinitt-(Fe)
  • Feraxinit
  • +4 more

History

The name records a shape. Its crystals grow as thin, wedge-shaped plates with a sharp edge, and an early mineralogist thought they looked like the blade of an axe. So in 1797 the French crystallographer René Just Haüy called the mineral axinite, from the Greek axina — axe — in allusion to that habit.

The name arrived late. For most of the eighteenth century the stone had no settled identity of its own. In 1781 Johann Gottfried Schreiber filed it loosely as a kind of schorl, under the French label Espèce de Schorl. Schorl was an old catch-all term for dark, glassy crystals. Cataloguing crystal forms in 1785, Romé de l'Isle split it by colour into schorl violet and schorl transparent lenticulaire — the lens-shaped transparent schorl. In 1788 the German mineralogist Abraham Gottlob Werner named it Thumerstein, after Thum in Saxony where good crystals were found; the name was later anglicised to thumite.

Other names followed before Haüy's stuck. Jean Claude de la Métherie proposed yanolite in 1792, and Blumenberg called it glasschörl — glassy schorl — in 1799. None survived. Haüy's axinite did, and it became the group name once chemistry revealed that several closely related minerals share the structure.

That chemistry is a calcium-iron-aluminium borosilicate — a silicate built around silicon and oxygen, with boron worked into the framework. The members differ in which metal dominates. In 1909 the American mineralogist Waldemar T. Schaller renamed the iron-rich member ferroaxinite, marking iron's lead in the formula. The modern label came in 2007, when the International Mineralogical Association recoded it with the cation suffix axinite-(Fe).

Industrial & practical applications

Axinite-(Fe) is not an industrial raw material. Although its structure carries boron, no source records it being mined or processed for that element, and it has no role in manufacturing.

Its only practical use is ornamental. When a crystal is transparent and the usual clove-brown colour is clean, a lapidary will sometimes cut it as a gem. The brown-to-violet, plum-blue stones it yields are prized chiefly by collectors and gem enthusiasts, not set in everyday jewellery. The mineral remains a cabinet and gemstone curiosity rather than a commodity.

Where it forms, where it's found

Geological setting

Low to high grade regionally metamorphosed rocks, contact metamorphic rocks, pegmatites.

Type locality
Saint-Christophe-en-Oisans
  1. Grenoble
  2. Isère
  3. Auvergne-Rhône-Alpes
  4. France
237recorded occurrences
Source · OpenStreetMap

Physical

Hardness
123456789106.5 – 7/ 10 MOHS
  1. 1Talc
  2. 2Gypsum
  3. 3Calcite
  4. 4Fluorite
  5. 5Apatite
  6. 6Orthoclase
  7. 7Quartz
  8. 8Topaz
  9. 9Corundum
  10. 10Diamond
Transparency
Transparent · Translucent
Colour
Brown · clove-brown · plum blue · pearl gray
Streak
White
Tenacity
brittle
Cleavage
Distinct/Good

Good on (100) Poor on (001) (110) (011)

Fracture
Irregular/Uneven · Conchoidal
Density
3.25 g/cm³

Optical

Optical type
Biaxial (-) · 2V measured = 69 – 87° · 2V calc = 62 – 82°
Refractive index
1.672 – 1.704
Surface relief
High
Principal indices
nα 1.672 – 1.693 · nβ 1.677 – 1.701 · nγ 1.681 – 1.704
Dispersion
strong
Michel-Lévy diagramhighlighted lineδ = 0.0100
Attainable Michel-Lévy rangeΔ ∈ [0, t·δmax]100 nm1st order
Δ = 0Δmax
Thin-section mosaic70 grains · random 3D orientations
PPLpleochroism per grain
XPLindependent extinctions · rotate the stage
Interference simulatorsingle grain · PPL ↔ XPL
PPLpleochroism only · colour blends on rotation
XPLinterference colour · extinct every 90°
Retardation100 nm
Order1st order
XPL colour

Crystallography

Crystal system
Triclinic
Space group
#2
Cell parameters
a = 7.1437(4) Å · b = 9.1898(6) Å · c = 8.9529(4) Å
Cell angles
α = 91.857(6) ° · β = 98.188(5) ° · γ = 77.349(4) °
Ratio a:b:c
1 : 1.286 : 1.253
Z
2
Morphology

Flattened, axe head shaped, granular, massive

Crystal structure

Chemical composition

Constituent elements
Mass composition breakdown
ElementAtoms At. mass g/mol Mass g/molMass share
8OOxygenOxygen3215.999511.968
44.90%
14SiSiliconSilicon828.085224.680
19.70%
20CaCalciumCalcium440.078160.312
14.06%
26FeIronIron255.845111.690
9.79%
13AlAluminiumAluminium426.982107.928
9.47%
5BBoronBoron210.81021.620
1.90%
1HHydrogenHydrogen21.0082.016
0.18%
Total1140.214100.00%

Mass share = atoms × atomic mass ÷ molar mass × 100

From IMA formula

Synonyms

  • Axiniet-(Fe)
  • Axinitt-(Fe)
  • Feraxinit
  • Feraxinita
  • Feraxinite
  • Feroaksinito
  • Ferro-axinite

In other languages

German
Axinit-(Fe)
Spanish
Axinita- · Axinita-(Fe)
Italian
Axinite- · Axinite-(Fe) · Ferroaxinite
Chinese
铁斧石

Classification

Strunz
10th ed.

9.BD.20

  • 9SilicatesClass
  • 9.BSorosilicatesDivision
  • 9.BDSi2O7 groups, with additional anions; cations in tetrahedral [4] and greater coordinationGroup
  • 9.BD.20Axinite-(Fe)Species
Dana
8th ed.

56.02.02.01

  • 56Sorosilicates Si2o7 Groups, with Additional O, Oh, F and H2oClass
  • 56.02Si2O7 Groups and O, OH, F, and H2O with cations in [4] and/or >[4] coordinationType
  • 56.02.02Axinite groupGroup
  • 56.02.02.01Axinite-(Fe)Species
CIM

17.5.47

  • 17Silicates Containing other AnionsClass
  • 17.5BorosilicatesGroup
  • 17.5.47Axinite-(Fe)Species

Group, growth & confusion

In the same group
3 members

Literature, links & citation

Citations
  1. 1796Haüy, René Just (1796) Extrait du Traité Élémentaire de Minéralogie que le C.en Haüy s'occupe de rédiger. Journal des mines, 5 (28). 249-334
  2. 1906Anderson, C. (1906) Mineralogical notes. No. III. Axinite, petterdite, crocoite, and datolite. Records of the Australian Museum, 6. 133-144 doi:10.3853/j.0067-1975.6.1906.998 DOI: 10.3853/j.0067-1975.6.1906.998
  3. 1909Dana, Edward S., Ford, William E. (1909) A System of Mineralogy - Second Appendix to the Sixth Edition of Dana's System of Mineralogy. John Wiley & Sons.
  4. 1980Pringle, Ian J., Kawachi, Yosuke (1980) Axinite mineral group in low-grade regionally metamorphosed rocks in southern New Zealand. American Mineralogist, 65 (11-12) 1119-1129
  5. 1981Swinnea, J. Steven, Steinfink, Hugo, Miron, L. E. Rendon-Diaz, Vega, and S. Enciso de la (1981) The crystal structure of a Mexican axinite. American Mineralogist, 66 (3-4) 428-431
Cite this entry
@misc{mineral2026,
  author    = {Mineral Index editorial board},
  title     = {Axinite-(Fe) — Mineral Index},
  year      = {2026},
  url       = {https://mineralindex.org/minerals/axinite-fe-1459},
  note      = {Accessed 2026-05-11}
}