Home

Beryl

Beryl is a mineral composed of beryllium aluminum cyclosilicate with the chemical formula Be3Al2Si6O18. It belongs to the orthorhombic crystal system and is known for its hexagonal prismatic crystals and glassy luster. Beryl occurs naturally in a range of colors, including green, blue, yellow, white, and pink, due to trace impurities.

The most well-known varieties of beryl are emerald and aquamarine. Emerald, characterized by its rich green

Beryl deposits are found worldwide, with significant sources in Colombia, Brazil, Pakistan, and Madagascar. The mineral

In addition to its aesthetic appeal as a gemstone, beryl has industrial uses due to its transparency

In mineralogy, beryl is valued for its crystalline structure and varied coloration. It forms under high-temperature

Overall, beryl’s diverse colors, aesthetic qualities, and industrial utility make it a significant mineral in both

color,
derives
its
hue
from
traces
of
chromium
and
vanadium.
Aquamarine,
valued
for
its
pale
blue
to
blue-green
coloration,
contains
iron
impurities.
Other
varieties
include
morganite
(pink
to
peach)
and
heliodor
(yellow
to
gold).
is
typically
associated
with
granite
pegmatites
and
metamorphic
rocks.
and
stability.
Crystals
of
beryl
are
used
as
a
source
of
beryllium,
a
lightweight
metal
with
applications
in
aerospace,
telecommunications,
and
nuclear
industries.
and
high-pressure
conditions
and
is
often
studied
as
a
mineralogical
indicator.
scientific
and
commercial
contexts.
Its
formation
and
occurrence
provide
insights
into
geological
processes
involving
beryllium
and
associated
elements.