Triboluminescence is a flash of light produced when a material is subjected to friction, impact or breakage. The phenomenon
is also known as fractoluminescence and mechanoluminescence. Triboluminescence is common in minerals. About 50%
of crystalline materials are thought to exhibit the property. It is also observed in many noncrystalline materials .
How to Demonstrate Triboluminescence
**** Safety glasses recommended ****
A very easy way to observe triboluminescence is to get two milky quartz pebbles that are large enough to easily hold and rub
together with a bit of force. Take them into a darkened room and stand in the dark for a few minutes to allow your eyes
to adjust to the darkness. You don't need total darkness but the less light the better.
Hold one piece of quartz in your left hand and the other piece in your right hand. Firmly press an edge of one piece of
quartz against the other and while holding firm pressure, quickly drag it across the surface in a motion similar to what you
would use to strike a large match. Don't be wimpy. Hold firm pressure while you quickly drag one pebble across the surface
of the other. If you do this properly and if you have pieces of quartz that are triboluminescent, you will see a brief flash of
light that penetrates deeply into the translucent quartz.
Experiment with different speeds, different amounts of pressure and directions of drag to maximize the flash of light. Some specimens
will also produce small amounts of light if you bang them together or rub them against one another. You can also experiment with
different minerals to see if they are triboluminescent.
You will probably find many minerals that exhibit the property.
Triboluminescence in Minerals
Triboluminescence is present in quartz; however, the strength of the phenomenon varies from specimen to specimen. Triboluminescence is well
known in sphalerite, fluorite, calcite, muscovite, and many feldspar minerals. Some specimens of common opal produce a bright orange flash.
Test a few specimens yourself. Don't forget to wear safety glasses and be aware that this test will scratch your specimens. You will probably
discover lots of specimens of various minerals that are triboluminescent. We have found that the flash of light is brightest when we use specimens that are transparent or very
translucent. These specimens allow the light to penetrate deeply, making the flash easier to observe.
For years we have observed flashes of light while cutting lapidary rough on a rock saw or shaping it on a diamond wheel. We originally thought
this light was incandescence (an emission of light from a hot object), but now we think that at least some of that light was triboluminescence.
Triboluminescence is not a good property to use for mineral identification. Some specimens of a mineral might exhibit the property and
other specimens will not.
Why is Light Produced?
The phenomenon of triboluminescence is poorly understood. Some researchers believe that scratching or hitting materials together
provides an input of energy that excites electrons within the materials. When the electrons fall from their excited state, a flash
of light is produced . Others believe that triboluminescence is similar to lightning
and caused by an electrical current generated by force applied to the materials. The electrical current travels through the material
causing molecules of gas trapped within the crystal to glow .
The flashes of light produced by triboluminescent minerals is usually white or orange, but other colors are possible. We may not see all of
the light that is produced because some of it could have wavelengths that are outside of the visible spectrum of humans .
Wint O Green Lifesavers?
**** Safety glasses recommended ****
An interesting material that exhibits a blue triboluminescence is Wint O Green Lifesavers. If you crush them with a pair of pliers in a dark
room you should see some nice blue flashes of light. The crystalline sugar in the candy is thought to be the source of the triboluminescence and
the methyl salicylate (wintergreen flavoring) produces a blue fluorescence . Many other types of hard sugar candy exhibit triboluminescence.
Practical Uses for Triboluminescence
Triboluminescent materials can be used to detect structural damage. If triboluminescent materials are embedded in a composite, they will generate
light if the composite begins to experience structural failure. A sensor will detect the light and report that failure has occurred.
This monitoring can detect failure in its early stages because many composite materials begin to fracture at the microscopic level far in
advance of complete failure.
These methods are expensive to implement and can only be used in equipment where detecting early-stage failure can result in high-value savings.
Component parts of spacecraft, aircraft, naval vessels, buildings, dams, bridges and other critical structures are where these methods might
be used .
Wall Maps - World maps, United States maps, continent maps, maps of individual states.
Tumbled Stones are rocks that have been rounded, smoothed and polished in a rock tumbler.
Hand Lens A 10-power folding magnifier in a metal case. A frequently used lab and field tool.
Iris Agate produces surprising colors when light passes through its thin bands.
Olivine is a rock-forming mineral found in the crust, the mantle, and in some meteorites.
Methane Hydrate deposits contain more fuel value than all other fossil fuels combined.
Aventurine is translucent quartz with tiny reflective inclusions that produce aventurescence.
Helium is a byproduct of the natural gas industry. Its most important use is in MRI.
YouTube video demonstration of triboluminescence. We use two pieces of milky quartz to produce a few flashes of light. You can easily find other minerals that exhibit triboluminescence. About 50% of all crystalline substances exhibit the property . Safety glasses recommended if you do the demonstration yourself.