Thomas Codrington, Quarterly Journal of the Geological Society of London (1870)
“ The streams ending in chines present no unusual features until they come within a short distance of the coast, when they begin to fall more and more rapidly through a ravine, which has been cut out in the bottom of a valley corresponding in level and cross section, and continuous with that in which the stream flows before it enters the ravine. The increased rate of fall towards the sea is opposed to the general tendency of streams to fall less as they near their outfall, and it seems to point to a somewhat sudden change in the conditions under which the streams flowed. ”
