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GEMSTONES
COLOURLESS
STONES
CS1
RED
STONES
RD1
Dark red
RD2 Pinkish red
RD3
Orangy red
RD4 Slightly purplish red
RD5 Purplish red
PINK STONES
PK1 Lilac pink
PK2 Pink and orangy pink
PK3 Brownish and purplish pink
ORANGE
STONES
OR1
These are the first sections to be uploaded and additional gems will be
inserted in them as we proceed |
Diffraction Spectra
of yellow, brown and
green
Chrysoberyl

Colour Properties
of yellow,
brown and green Chrysoberyl
|
Colour |
Pale greenish yellow to shades of green, greenish brown and brown.
|
|
Cause of colour |
Iron; Small traces of chromium may contribute to some green stones |
|
Optical Character |
Biaxial positive |
|
Pleochroism |
Often just two shades of body colour detected; α - darker; γ -
paler |
|
Colour change |
No, but some green stones may appear a more brownish green in
tungsten light. |
|
Spectrum; no polar, calibration in nm. |
Main band due to iron centred at 444nm.easily resolved in yellows
but more difficult in browns and may cut off in dark greens at
450.Weaker lines may be seen in darker browns at 485 and 505. |
|
Ordinary ray |
Not applicable |
|
Extraordinary ray |
Not applicable |
|
Alpha ray |
444 band and others are stronger and broader in this direction |
|
Beta ray |
Untested - awaiting a suitable single crystal for observation. |
|
Gamma ray |
444 band narrower. Weak Cr. line at 680 in some green stones
|
|
Emission lines |
No |
|
Database reference |
None yet |
|
Notes |
Some greens may also show a very weak line at 680 due to Cr. and
absorb strongly in the deep blue to almost mask the 440 iron band.
No definite colour change is seen but these stones may appear red
under crossed colour filters. - In my opinion these are not
Alexandrite |
Copyright John S.
Harris
2000-2010 |
SPECTRA OF PRINCIPAL
COMMERCIAL GEMSTONES
ALEXANDRITE
ALMANDINE GARNET
DIAMOND
EMERALD
GREEN JADEITE
PERIDOT
RUBY
SAPPHIRE
RED SPINEL
GREEN & BLUE SPINEL
SYN. BLUE SPINEL
& Co. GLASS
SYN. COLOUR
CHANGE CORUNDUM
ZIRCON (High type)
ZIRCON (Low type)
Other pages are under construction
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