| Opal
is a poorly crystalline or amorphous
hydrous silica that is compact and
vitreous and most commonly translucent
white to colourless. Precious opal
reflects light with a play of brilliant
colours across the visible spectrum,
red being the most valued. Opal
forms by precipitation from silica-bearing
solutions near the Earth's surface.
Electron microscopy has shown that
many opals are composed of spheres
of tens to a few thousand angstroms
in size that are arranged in either
hexagonal or cubic close packing.
The spheres are composed of hydrous
silica that may be either almost
cristobalite-like, tridymite-like,
mixtures of both, or random and
nondiffracting. The specific gravity
and refractive index are lower than
those of pure silica minerals. The
play of colours in precious opal
arises from the diffraction of light
from submicroscopic layers of regularly
oriented silica spheres. When heated,
opal may lose as much as 20 percent
of its weight of water, fracture,
and then crystallize to one of the
silica minerals described above.
|
| Gemological
Information |
| Color
: |
White,
green, blue, black, red, orange, violet,
pink, grey, yellow. |
| Refractive
Index: |
1.44-1.46 |
| Chemical
Composition: |
SIO2nH2O |
| Hardness: |
5.5
- 6.0 |
| Density: |
2.65
- 3.00 |
| Crystal
Group: |
Amorphous |
| Ocurrence: |
Czechoslovakia,
Mexico, Honduras, Australia, Brazil,
Tanzania. |
| Opal
usually contains 4 to 9 percent
water, but lower and much higher
values have been observed. The contents
of alumina, ferric oxide, and alkalis
are variable but may amount to several
percent in light-coloured opals
and more if pigmenting minerals
are also present. Precious opal
has been synthesized. Opaline silica
is a friable hydrous silica found
near hot springs and geysers.
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