Plunge pool height of fall, the volume of water, the resistance of the rock below the pool and other factors. The impacting and swirling water, sometimes carrying rocks within it, abrades the riverbed into a basin, which often features rough and irregular sides. Plunge pools can remain long after the waterfall has ceased flow or the stream has been diverted. Several examples of former plunge pools exist at Dry Falls in the Channeled Scablands of eastern Washington. Plunge pools are fluvial features of erosion which occur in the youthful stage of river development, characterized by steeper gradients and faster water flows. Where
Big Chute Marine Railway again made to build three locks at Big Chute, to be part of a new section of canal which would take boats from Big Chute and rejoin the existing waterway downstream from the Little Chute, avoiding the fast water in the Little Chute. However because of the post-war recession the scheme was put on hold once more, although remains of the beginning of the dams required to maintain the water levels can still be found in the surrounding forest. In 1923, the original railway at Big Chute was replaced, as the size and number of boats had increased, with the