John Milne,
Quarterly Journal of the Geological Society of London
(1877)
“ If we take a map of Northern Europe on which are indicated the general direction of ice-markings, any inference which can be drawn from such directions, which all point more or less at right angles to the sea-coast, is as favourable to the view that they were produced by coast-ice acting on a rising area as it is to the fact that they point out the direction in which the great ice-sheets travelled. ”
