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fluorescent minerals



Glowing Geology



Photos and text by Chad Arment, 2024



Calcite



What is Fluorescence?



Fluorescence is one form of ‘cold’ emission of light (luminescence), rather than from the heated state of incandescence. Fluorescence occurs through the excitation of atoms, molecules, or physical structure (lattices) through the addition of energy in the form of electromagnetic radiation (here, that would be ultraviolet light). The fluorescent emission is a lower energy state (a longer wavelength) than the absorbed light. Fluorescent rocks usually have activators, or trace minerals, that interact with their own atoms, allowing fluorescence to occur. Willemite, for example, uses manganese as an activator. A few minerals are self-activating, and do not require the addition of other elements.



Chalcedony (?)



Where can you find fluorescent rocks?



Fluorescent rocks can be found all over the world. In order to look for them, you will need an ultraviolet light. UV lights used to be bulky and expensive, but now you can acquire LED flashlights with appropriate filters in shortwave, midwave, and longwave emission from rockhound dealers. Visit some online fluorescent rock forums for brand reviews. Most of the rocks I am photographing here are shown under shortwave light. (The sodalite is shown under longwave light.) A few rocks are known to glow different colors under longwave and shortwave lights. There are many fluorescent rock dealers online, but if you are just starting a collection, I would recommend sticking to inexpensive material.


Be aware that you should never shine a UV light into eyes, and limit exposure to skin. (Basically, just point the flashlight at the rocks; make sure kids are carefully supervised.)



Yellow Calcite



Elk Creek, South Dakota



Differences



A mineral's ability to fluoresce varies from location to location, as it depends greatly on mineral composition. Too much of an activator may quench fluorescence, while the presence of other trace elements may alter coloration. Fluorite in one location may glow blue, in another location it may glow cream (or yellow, white, green, red, etc.), or it may not glow at all. (And, of course, fluorite under natural light may be found in a wide range of colors, making it a prized focus of many collections.)



Fluorite and Celestite



Clay Center, Ohio



Further reading



Modreski, Peter J., and Regina Aumente-Modreski. Fluorescent minerals: A review. Rocks & Minerals 71(1): 14-22.


Schneider, Stuart. 2010. Collecting Fluorescent Minerals. 2nd ed. Atglen, PA: Schiffer Publishing.



Tabular Calcite



Chihuahua, Mexico



Chalcedony



Safford, Arizona



Botryoidal Fluorite



Cañon City, Fremont Co., Colorado



Fluorite on Amethyst



Unaweep Canyon, Colorado


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