Fluorescents
WHAT IS IT?
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Fluorescent minerals emit light when exposed to light or another form of electromagnetic radiation.
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The emitted light has a longer wavelength (lower frequency) than the absorbed radiation.
(The emitted light photons have a lower energy than those that are absorbed) - There are over 500 types of fluorescent minerals.
- Common fluorescent minerals include fluorite, calcite, opal, selenite, sodalite, and chalcedony.
WHAT IS LUMINESCENCE, PHOTOLUMINESCENCE, PHOSPHORESCENCE, FLUORESCENCE?
- Luminescence is the ability of a substance to emit light. The source are numerous, a few chemical reactions, radioactivity & light absorption.
- Photoluminescence is a form of luminescence that is activated by the absorption of electromagnetic radiation.
- Fluorescent minerals are actually photoluminescent
- There are two types of photoluminescence: Phosphorescence & Fluorescence
- Phosphorescence is characterized by the continued emission of light after the source radiation has been removed.
The lifetime of these emissions is from tens of nanoseconds to seconds. - Like phosphorescent materials, fluorescent materials also continue to emit light after the source radiation is removed,
but they do so for a shorter period of time - from femtoseconds to tens of nanoseconds.
HOW IS ULTRAVIOLET LIGHT CLASSIFIED?
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Fluorescent mineral collectors are interested in specimens that emit visible light when exposed to invisible
ultraviolet light due to the resulting magnificent visual effects. - Fluorescent minerals often glow with different colors dependent on the wavelength of the ultraviolet light that
they are exposed to. - There three wavelength bands that are commonly used to classify the ultraviolet light source type:
TYPE OF UV WAVELENTH CLASSIFICATION WAVELENGTH IN NANOMETERS (nm)
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UV-A long wave (LW) 315 - 400
UV-B medium wave (MW) 280 - 315
UV-C short wave (SW) 100 - 280
WHERE ARE FLuoreScent MINERALS FOUND?
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The most famous fluorescent mineral location is northwest New Jersey
(the mines at Franklin & the Sterling Hill mine).
This area has been named "the fluorescent capital of the world".
The minerals from this region produce the most spectacular displays. - There are over 300 different fluorescent minerals that have been mined in the vicinity of Franklin, New Jersey.
- The rarest fluorescent mineral is Benitoite which was only mined at a single location along the San Benito River in California.
That mine has been closed since 2006. Benitoite is the state gem of California. - There are common fluorescent minerals such as calcite & fluorite that are found around the world.
WHAT TYPES ARE THERE?
- There are too many types to list here.
Please refer to the following links for detailed information:
http://webmin.mindat.org/determin/luminescence.php#.YVNiFMjYrrc
https://www.uvminerals.org/minerals/common-fluorescent-minerals/
https://www.uvminerals.org/minerals/gallery/
https://geology.com/articles/fluorescent-minerals/
https://franklinmineralmuseum.com/about/fluorescent-minerals/
https://www.naturesrainbows.com/major-locality-mines-of-new-jersey
https://www.sterlinghillminingmuseum.org/minerals-of-sterling-hill-and-franklin
WHAT IS IT USED FOR?
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Collecting
- Various industrial uses (example: fluorite is used as a flux, for glass & enamel making, and by the chemicals industry)
