APPENDIX B.
RADIO-ACTIVE MINERALS.
Those natural mineral substances which possess marked radio-active
properties have been found to contain either uranium or thorium,
one of these elements being always present in sufficient proportion
readily to permit its chemical separation and identification by the
ordinary analytical methods[1].
A large number of uranium and thorium minerals are known at the present time, but they are for the most part found very sparingly, and some of them have been observed to occur only in a single locality. The chief commercial sources of uranium are uraninite, gummite, and carnotite, while thorium is obtained almost exclusively from monazite.
Rutherford and Soddy (Phil. Mag. 65, 561 (1903)), were the first to call attention to the important fact that the relations between the various radio-active substances and the other elements could best be determined from the study of the natural minerals in which these bodies occur, since these minerals represent mixtures of extreme antiquity, which have remained more or less undisturbed for almost countless ages. In dealing with these matters, however, it is highly important that we bring to our aid the data furnished by geology and mineralogy, from which it is often possible to determine the relative ages of the different substances with at least a rough degree of approximation. Thus, for example, if a certain mineral occurs as a primary constituent of a rock of remote geological period, it can safely be assumed that its age is greater than that of a similar or different mineral occurring in a later formation. It is, moreover, quite evident that those minerals which are obviously produced by the decomposition and alteration of the primary minerals, through the action of percolating water and other agencies acting from the surface down-*
- ↑ An apparent exception has been observed by Danne in the case of certain lead minerals which occur under peculiar conditions at d'Issy-l'Évêque, France. See p. 465.
