This document discusses fluorescent minerals, which are minerals that temporarily absorb light and re-emit light of a different wavelength, causing a color change. Fluorescence is caused by certain impurities in minerals called activators, such as metals like tungsten, molybdenum, and rare earth elements. About 15% of known minerals fluoresce. Common fluorescent minerals mentioned include calcite, tourmaline, topaz, and diamonds. Ultraviolet light is needed to see fluorescence, and different types of UV wavelengths cause different color changes in minerals.