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Specie:
Beryl
Chemical composition: Beryllium
Aluminum Silicate
Chemical Formula :
BE3 AL2 SI6 O18
Hardness (Moh's Scale)
7.5-8.0-
Fracture: Conchoidal vitreous
Cleavage: Imperfect |
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Luster:
Vitreous, in polished surfaces
Specific Gravity: 2.67-2.71
Crystal System: First order
hexagonal prism, tabular habit, flat well
terminated surfaces common, etching and
growth marks.
Optic sign and character:
U(-)
Pleochroism Varies according
to body color in intensities from weak to
distinct varies according to body color
in intensities from weak to distinct |
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Red
fluorescence in emeralds
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Refractive
index: 1.569- 1.575 Varies with
origin and locality
Birefringence .06
Chemical elements responsible for
color: Chromium, Vanadium, Iron
Fluorescence: UV (Short wave):
variable, from inert to very pale reddish
pink
UV (Long wave): variable,
from inert to medium reddish pink to red
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Absorption
Spectra: Typical chromium with
doublet in deep red at about 680-685nm line
at 635-640 wide absorption band in yellow.
Varies slightly with origin.
Phenomena: Chatoyance Rare
, "Trapiche Star" fix six ray
star (Colombian Emerald)
Thermal conductivity: Medium
low
Reaction to heat: May cause
fracturing or breakage
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Reaction
to chemicals: Resistant to all
acids except hydrofluoric acid
Electric conductivity:
Beryl in general are nonconductors
Modes of formation: Hydrothermal
and in Pegmatite
Main producers: Colombia,
Brazil, Zambia, Pakistan, Afghanistan, Madagascar
and Russia
Oldest source of emeralds: Egypt
(Not presently under production)
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Cutting
Style: The ideal cut depends on
the shape and color distribution of the
rough material. The ideal cutting style
used is the rectangular or square step cut
known as "Emerald Cut." Other
cutting styles suit Emeralds. It is common
to find Emeralds in oval shape, pear shape
and cabochon. The cushion shape, marquee
and round shape cuts are less common. |
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