Beryl
Encyclopedia

Silicates · Sourced PROFILE

Beryl

Be₃Al₂Si₆O₁₈

A ring silicate mineral family that includes emerald and aquamarine.

AT A GLANCE

Formula
Be₃Al₂Si₆O₁₈
Crystal system
Hexagonal
Space group
P6/mcc
Mohs hardness
7.5
Density
2.63–2.97 g/cm³
Optical character
Uniaxial (−)

CRYSTALLOGRAPHY

Crystal form & structure

Usually hexagonal prisms, sometimes tabular; crystals may be vertically striated, etched, or exceptionally large in pegmatites.

HAND-SAMPLE PROPERTIES

Physical properties

Cleavage
Imperfect basal cleavage
Fracture
Conchoidal to uneven
Tenacity
Brittle
Streak
White
Luster
Vitreous to resinous
Transparency
Transparent to translucent
Observed colours
Colourless, green, blue, yellow, pink, red, or white

LIGHT & OPTICS

Optical properties

Optical class
Uniaxial (−)
Refractive index
nω about 1.568–1.602; nε about 1.564–1.595
Fluorescence & electrical behaviour
Usually weak or inert; response varies with colour centres and impurities.

GEOLOGICAL SETTING

Formation

Commonly crystallizes in granitic pegmatites and some metamorphic environments.

MINERAL COMPANY

Common associations

Quartz, feldspars, muscovite, lepidolite, spodumene, tourmaline, topaz, and cassiterite

FIELD NOTES

How to identify it

Recognise hexagonal prisms, hardness 7.5–8, relatively low density, and imperfect basal cleavage. Emerald and aquamarine are coloured beryl, sharing the same ring-silicate framework.

NAME & HISTORY

Where the name comes from

From ancient Greek beryllos, a name for precious blue-green stones.

SCIENTIFIC SOURCE

Handbook of Mineralogy — Beryl

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

Open reference PDF

PROVENANCE

Documented occurrences

Pamir orogen

Kukurt pegmatite field, Eastern Pamir · Beryl is documented as a common accessory mineral in the Dorozhny miarolitic granitic pegmatite. The public record remains at regional precision and is not collecting guidance.

Sourced · Region precisionBadakhshanite-(Y), a new mineral species from a granite miarolitic pegmatite in Eastern Pamir (Pautov et al., 2020)