John Young Buchanan, Popular Science Monthly (1881)
“ By far the greater part of the ocean is, for sounding purposes, practically still water. The surface-currents of any importance are easily recognized, and so also are the under-currents. Just as a physician can, by bringing his experience to bear on the sounds transmitted to him by the stethoscope, divine what is taking place inside the body of his patient, so the experienced seaman can, by observing the behavior of his sounding-line, form a fair diagnosis of what is taking place in the depths of the sea. When the sinker passes into a belt of under-current, the fact is very soon apparent ”
