Abstract
This work is the beginning1 of a systematic investigation of the absorption spectra of solids, particularly single crystals of the ions of the rare earths, over a range of temperatures. We expected that the ions of the rare earths in the solid state would exhibit line absorption spectra because their magnetic moments agreed quantitatively with theories2 which had been successful in elucidating the line spectra of gases. The latter definitely established that only the 44 electronic shell is incompletely filled and extrapolation of the energies from x-ray data led to the conclusion that the energy necessary to remove a 44 electron might possibly be measured through quartz.