Luminescence is a property exhibited by minerals that emit visible
light, usually as a result of irradiation by invisible light. Luminescence
includes both fluorescence, the emmission of light at the same
time as the irradiation, and phosphorescence, the continued emmision
of light after irradiation has ceased. Luminescence is best shown
in a darkened exhibit, using invisible ultraviolet radiation to
demonstrate the property.
As ultraviolet radiation strikes the atoms of luminescent minerals,
the energy causes the electrons to move from their normal orbits
to paths farther out. The return of the displaced electrons to
their normal orbits is accompanied by a release of energy in
the form of light. Thus, a fluorescent mineral will glow while
being irradiated. In a phosphorescent mineral, return of the electrons
is slower, so that a lingering emission of light occurs.
Luminescence is often related to a defect in the minerals crystal
lattice or to the presence of foreign ions. Thus, a typically fluorescent
mineral may also occur in a non-fluorescent form.