Garnet group
Encyclopedia

Silicates — garnet group · Sourced PROFILE

Garnet group

X₃Y₂(SiO₄)₃

A family of cubic silicates sharing one structure but spanning several compositions and many gemstone colours.

AT A GLANCE

Formula
X₃Y₂(SiO₄)₃
Crystal system
Cubic
Space group
Ia̅3d (representative garnet structure)
Mohs hardness
6.5–7.5
Density
Common gem garnets roughly 3.5–4.3 g/cm³ depending on species
Optical character
Isotropic

CRYSTALLOGRAPHY

Crystal form & structure

Typically dodecahedral or trapezohedral crystals; also granular or massive. This group profile uses almandine as a representative reference.

HAND-SAMPLE PROPERTIES

Physical properties

Cleavage
None
Fracture
Conchoidal to uneven
Tenacity
Brittle
Streak
White
Luster
Vitreous to resinous
Transparency
Transparent to opaque
Observed colours
Red, orange, yellow, green, purple, brown, black or colourless

LIGHT & OPTICS

Optical properties

Optical class
Isotropic
Refractive index
n commonly about 1.73–1.89 across the group
Fluorescence & electrical behaviour
Usually inert to variable; fluorescence is not a group-level diagnostic.

GEOLOGICAL SETTING

Formation

Common in metamorphic rocks and also present in igneous rocks, skarns, and sediment derived from garnet-bearing sources.

MINERAL COMPANY

Common associations

Micas, quartz, feldspars, kyanite, sillimanite, pyroxenes, amphiboles and calcite depending on species and setting

FIELD NOTES

How to identify it

Equant dodecahedral habit, absent cleavage, relatively high hardness and density are useful clues; refractive index and chemistry are needed to identify the garnet species.

NAME & HISTORY

Where the name comes from

From Latin granatus, grain-like, referring to rounded crystals resembling seeds.

SCIENTIFIC SOURCE

Handbook of Mineralogy — Almandine (representative garnet species)

External reference; factual profile paraphrased and attributed. Copyright remains with the publisher.

Open reference PDF

PROVENANCE

Documented occurrences

South Pamir

Sokhcharv valley, Rushan district, Western Pamir · Pinkish almandine forms well-shaped single and clustered crystals, mostly 1 mm to 1 cm and up to about 7 cm, in garnet-bearing schist horizons. The record stays at regional precision.

Sourced · Region precisionMineralogy of garnet-containing horizons, Sokhcharv valley, Western Pamir (Vatanbekov, Zhou, Yogibekov, Gurminjova, 2020)