Almandine

Fe2+3Al2(SiO4)3
IMA status
  • Approved
  • Grandfathered
IMA symbol
Alm
Also known as
  • Adelaide ruby
  • Adelaide-rubin
  • Alabandicus (of Pliny)
  • +8 more

History

The name almandine is a corruption of alabandicus — the term Pliny the Elder applied to a red stone found or worked at Alabanda, an ancient town in Caria, in what is now southwestern Turkey. Alabanda was a Roman-era gem cutting centre, and the name suggests almandine was fashioned into gemstones there.

In antiquity, the deep red almandine was the most prominent of several stones grouped under the Latin word carbunculus — "little coal" — for their glowing colour. Red garnets were the most commonly used gemstones in the Late Antique Roman world and in the Migration Period art of the peoples who succeeded Rome. They were set into gold cells in the cloisonné technique — small compartments of metal each holding one polished stone — a style so closely associated with garnet that it is often simply called garnet cloisonné. The technique runs from Anglo-Saxon England, as at the Sutton Hoo ship burial, to the Black Sea. The trade in raw stones reached far: thousands of gold, silver, and red garnet shipments moved from Tamraparniyan workshops, in what is now Sri Lanka, across the Old World to Rome, Greece, the Middle East, and the Anglo-Saxon north.

Through the medieval period, the gem-quality red almandine continued to be called carbuncle in European lapidaries. The English word descends from the same Latin carbunculus, and it remains the name applied to almandine cut with a domed face — en cabochon — to bring out the colour.

The modern mineral name was fixed in 1546, when the German mineralogist Georgius Agricola — Georg Bauer — published it as almandine in his early mineralogical writings, deriving it directly from Pliny's alabandicus.

Industrial & practical applications

Almandine has two working lives today: one as a gemstone, the other as the dominant raw material of the industrial garnet trade.

As an abrasive

The coarse, opaque varieties of almandine are crushed for use as an abrasive agent. Hard — between 6.5 and 7.5 on the Mohs scale — and angular when broken, the mineral powder cuts metals and other hard materials cleanly. Garnet sand is a good abrasive and a common replacement for silica sand in abrasive blasting operations. The grain shape matters: alluvial grains, rounder from river transport, suit blasting; angular grains broken from hard rock suit waterjet cutting, where the powder is mixed with very high pressure water to slice steel and other materials. Garnet paper, faced with finely sized grains, is favoured by cabinetmakers for finishing bare wood, and garnet sand is also used as a water filtration medium.

The supply base sits with two countries. The largest source today is garnet-rich beach sand on the coasts of India and Australia. These two are the main producers of abrasive garnet.
A third, harder stream comes from the Adirondack Mountains of New York. The open-pit Barton Garnet Mine at Gore Mountain, in Warren County, is a significant source of industrial abrasive. It also yields the world's largest single garnet crystals, commonly 10 to 18 centimetres across.

As a gemstone

Gem-quality almandine — transparent, deep red inclining to purple — is the most abundant of the garnets and the least expensive of the red ones. It is most often faceted for rings. Stones cut en cabochon — with a domed top — are sold as carbuncle, the same trade name the gem has carried since antiquity. Some cabochons show a four-rayed asterism — a star-shaped figure across the dome — when fine needle-shaped inclusions inside the stone are aligned by the crystal's structure.

Where it forms, where it's found

Geological setting

The most common garnet, typically in mica schists and gneisses, from regionally metamorphosed argillaceous sediments and pelites; also in contact metamorphic hornfels. In granites and eclogites; in sedimentary rocks; as a detrital mineral.

Type locality
Alabanda
  1. Çine District
  2. Aydin Province
  3. Turkey

37.5989°, 27.9589°

2,140recorded occurrences
Source · OpenStreetMap

Varieties

Physical

Hardness
123456789107 – 7.5/ 10 MOHS
  1. 1Talc
  2. 2Gypsum
  3. 3Calcite
  4. 4Fluorite
  5. 5Apatite
  6. 6Orthoclase
  7. 7Quartz
  8. 8Topaz
  9. 9Corundum
  10. 10Diamond
Lustre
Vitreous - Resinous
Transparency
Transparent · Translucent
Colour
Deep red · brownish red · red-violet · black

may be sectored

Streak
White
Tenacity
brittle
Cleavage

None

Fracture
Sub-Conchoidal
Density
4.318 g/cm³

Optical

Optical type
Isotropic
Surface relief
Very high
Principal indices
n 1.83
Luminescence
Non-fluorescent
Notes

Anomalously biaxial.

Isotropy testPPL ↔ XPL diagnostic
PPL intrinsic colour; no change on stage rotation
XPL extinct at every orientation
Single index
n = 1.830

Crystallography

Crystal system
Isometric
Space group
#225
Cell parameters
a = 11.526 Å
Z
8
Morphology

Typically well-formed dodecahedra or trapezohedra, to 1 m; also in rounded grains and massive.

Parting
On (110)
Crystal structure

Chemical composition

Constituent elements
Mass composition breakdown
ElementAtoms At. mass g/mol Mass g/molMass share
8OOxygenOxygen1215.999191.988
38.57%
26FeIronIron355.845167.535
33.66%
14SiSiliconSilicon328.08584.255
16.93%
13AlAluminiumAluminium226.98253.964
10.84%
Total497.742100.00%

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

From IMA formula

Synonyms

  • Adelaide ruby
  • Adelaide-rubin
  • Alabandicus (of Pliny)
  • Alabandine Ruby
  • Alamandine
  • Almandine Garnet
  • Almandit
  • Almandita
  • Almandite
  • Greenlandite (of Klaproth)
  • Oriental Garnet

In other languages

French
Alamandine · almandin · Almandite · Dhanrasite
German
Alabandin · Almandin · Eisen-Tonerdegranat · Eisentongranat
Spanish
almandina · almandines · almandino · almandita
Italian
almandine · almandini · almandino
Japanese
アルマンディン · 鉄礬柘榴石
Chinese
鐵鋁榴石
Traditional Chinese
鐵鋁榴石
Russian
альмандин
Arabic
ألمندين

Classification

Strunz
10th ed.

9.AD.25

  • 9SilicatesClass
  • 9.ANesosilicatesDivision
  • 9.ADNesosilicates without additional anions; cations in [6] and/or greater coordinationGroup
  • 9.AD.25AlmandineSpecies
Dana
8th ed.

51.04.3a.02

  • 51Nesosilicates Insular Sio4 Groups OnlyClass
  • 51.04Insular SiO4 Groups Only with cations in [6] and >[6] coordinationType
  • 51.04.3a— unnamed intermediate level —Group
  • 51.04.3a.02AlmandineSpecies
CIM

16.17.1

  • 16Silicates Containing Aluminum and other MetalsClass
  • 16.17Aluminosilicates of FeGroup
  • 16.17.1AlmandineSpecies

Group, growth & confusion

Often grow together
6 minerals

Literature, links & citation

Citations
  1. 1988Rossman, G.R., Rauch, F., Livi, R., Tombrello, T.A., Shi, C.R., Zhoi, Z.Y. (1988) Nuclear reaction analysis of hydrogen in almandine, pyrope and spessartine garnets. Neues Jahrbuch für Mineralogie Monatshefte: 4: 172-178.
  2. 1991Hofmeister, A.M., Chopelas, A. (1991) Vibrational spectroscopy of end-member silicate garnets. Physics and Chemistry of Minerals, 17 (6). 503-526 doi:10.1007/bf00202230DOI: 10.1007/bf00202230
  3. 1992Armbruster, Thomas, Geiger, Charles A., Lager, George A. (1992) Single-crystal X-ray structure study of synthetic pyrope almandine garnets at 100 and 293 K. American Mineralogist, 77 (5-6) 512-521
  4. 1992Geiger, C.A., Armbruster, Th., Lager, G.A., Jiang, K., Lottermoser, W., Amthauer, G. (1992) A combined temperature dependent 57Fe Mössbauer and single crystal X-ray diffraction study of synthetic almandine: Evidence for the Gol'danskii-Karyagin effect. Physics and Chemistry of Minerals, 19 (2). 121-126 doi:10.1007/bf00198609DOI: 10.1007/bf00198609
  5. 1996Pilati, T., Demartin, F., Gramaccioli, C. M. (1996) Atomic displacement parameters for garnets: a lattice-dynamical evaluation. Acta Crystallographica Section B Structural Science, 52 (2) 239-250 doi:10.1107/s0108768195010925DOI: 10.1107/s0108768195010925
Cite this entry
@misc{mineral2026,
  author    = {Mineral Index editorial board},
  title     = {Almandine — Mineral Index},
  year      = {2026},
  url       = {https://mineralindex.org/minerals/almandine-452},
  note      = {Accessed 2026-05-11}
}