Difference between revisions of "Benitoite"

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(Spectrum)
(Cause of Color)
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[[Image:Benitoite absorption spectra.jpg|left|thumb|500px|Transmission Spectrum: <br />The more saturated the blue, the higher the peak in the 400-500 nm range]]<br clear="left" />
 
[[Image:Benitoite absorption spectra.jpg|left|thumb|500px|Transmission Spectrum: <br />The more saturated the blue, the higher the peak in the 400-500 nm range]]<br clear="left" />
  
==Cause of Color==
+
=Cause of Color=
 
The origin of color in benitoite has not been definitively established. <br />
 
The origin of color in benitoite has not been definitively established. <br />
 
Proposed ideas include: <br />
 
Proposed ideas include: <br />
 
Fe2+ - Ti4+ or the Fe2+ - Fe3+ intervalance charge transfer. <br />
 
Fe2+ - Ti4+ or the Fe2+ - Fe3+ intervalance charge transfer. <br />
 
While most benitoite is colorless when viewed down the c-axis, there is a very small number (3) of exceedingly rare stones (now cut into gemstones) which are pink in this direction.
 
While most benitoite is colorless when viewed down the c-axis, there is a very small number (3) of exceedingly rare stones (now cut into gemstones) which are pink in this direction.
 +
 
==The Benitoite Gem Mine ==
 
==The Benitoite Gem Mine ==
  

Revision as of 09:48, 18 March 2012

Benitoite
Chemical composition BaTiSi3O9
Crystal system Trigonal
Habit Bipyramids
Cleavage None
Fracture Conchoidal
Hardness 6.5
Optic nature Uniaxial +
Refractive index 1.75-1.80
Birefringence 0.047
Dispersion High, 0.046
Specific gravity 3.65
Lustre Bright vitreous
Pleochroism Strong

Beniotite is a very rare mineral that was discovered in 1907 in San Benito County in California. It has never been found elsewhere. It was originally mistaken for sapphire. Benitoite is very highly dispersive (the ability to take white light and disperse it into various components of the spectrum) with an adamantine luster when polished.
Benitoite is associated with other rare minerals such as black-red neptunite, snow white natrolite and brown-yellow joaquinite. Since the only source of this rare combination occurs at San Benito County, California, it has been designated the California state gemstone. Crystals, and cut stones, tend to be small and quite expensive!

Photo Courtesy of: Rob Lavinsky
Photo Courtesy of: Barbra Voltaire

Spectrum

4mm faceted benitoites: Colorless to Dark Blue
Photo Courtesy of: Barbra Voltaire

Transmission Spectrum:
The more saturated the blue, the higher the peak in the 400-500 nm range

Cause of Color

The origin of color in benitoite has not been definitively established.
Proposed ideas include:
Fe2+ - Ti4+ or the Fe2+ - Fe3+ intervalance charge transfer.
While most benitoite is colorless when viewed down the c-axis, there is a very small number (3) of exceedingly rare stones (now cut into gemstones) which are pink in this direction.

The Benitoite Gem Mine

The Early Days: An Interview with Ed Swoboda and Peter Bancroft
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