Fluorescence

Emission of visible light while a mineral is illuminated by ultraviolet light, caused by activator elements; fluorite, calcite, willemite, scheelite and many amber and opal specimens fluoresce. Short-wave (254 nm) and long-wave (365 nm) UV give different responses.

Sources

Earle, S. (2019). Physical Geology, 2nd ed., Chapter 2: Minerals (CC BY 4.0)
Mindat — Mineralogical glossary (link only)

Cite this article

Stratum Study. "Fluorescence" (Glossary). Stratum Study pack 2026.09, as of 2026-09-16. https://stratum.black/study/glossary/fluorescence. Accessed 2026-09-20.

BibTeX · CSL-JSON

@misc{stratum-fluorescence,
  title        = {Fluorescence},
  author       = {{Stratum Study}},
  howpublished = {\url{https://stratum.black/study/glossary/fluorescence}},
  year         = {2026},
  note         = {Glossary article, Stratum Study pack 2026.09, as of 2026-09-16; sources: stratum. Accessed 2026-09-20.}
}

Citations carry the pack version and the article's as-of date so they resolve to the same text later. The facts themselves belong to the sources listed below; cite those for the science.