Charles F. Fish, Popular Science Monthly (1881)
“ From the fact that the temperature of these wells and that of the mineral springs just east of them is said to be identical, and that they are, like the latter, never affected by surface-drainage, it is claimed that both have a common origin, and those that advocate the theory of sublimation claim that, if the waters are fresh at the site of these fresh-water wells, it is impossible for them to become mineral in their character by the short passage through the rocks that intervene between them and the fault; and hence they insist that the theory of percolation is untenable. ”
