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A feature of some minerals is fluorescence -- the ability to absorb invisible UV (UltraViolet) light, and to emit the absorbed energy as visible light. While it may sound trivial, it is delightful to observe in reality. In general, the molecules of trace elements\are the source of the fluorescence, such as chromium which causes rubies to fluoresce a deep red, or uranium in hyalite opal which fluoresces a bright green. Some minerals are not consistently fluorescent – kyanite, which often occurs with ruby, typically does not fluoresce, but some specimens fluoresce with the same red as rubies do, indicating the presence of chromium.
Some fluorescent minerals also exhibit phosphorescence, which is the ability to continue to emit visible light after the UV light source is removed. Phosphorescent minerals are much rarer than fluorescent minerals.
Fluorescent mineral fans need UV flashlights to enjoy their specimens. Not being aware of any local sources, I decided to start carrying a small supply of lights for my customers' convenience. My intention is to have a range of LW / 365 NM lights in stock, with SW / 255 NM and MW / 310 NM lights available by order.
Hyalite Opal, Erongo Mountain, Erongo Region, Namibia. Hyalite Opal, aka Opal-AN, from the Erongo Region is highly fluorescent, with some specimens displaying "daylight fluorescence", in which the fluorescence is visible in sunlight. Erongo specimens fluoresce under all UV frequencies, unlike specimens from some other parts of the world.
Willemite, Calcite, Franklinite, Sterling Hill Mine, Ogdensburg NJ. Classic combination from Sterling Hill, of green-fluorescing willemite, red/orange-fluorescing calcite, and non-fluorescent franklinite. The Sterling Hill specimens shown here were self-collected.
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