Climatic shifts are known to be capable of effecting fill or clearance of channels and valleys: they can also change channel habit. In addition to the alternation in some near-glacial areas between braiding during maximum cold and meandering during interglacial warmth, the record includes conversions of channel width and meander pattern. On numerous midlatitude streams, existing channels have been much reduced from their earlier dimensions; and on many, but by no means all streams, existing floodplains are contained in the floors of meandering valleys where the wavelength is determined by the plan of the floodplain as opposed to the existing ...(100 of 32811 words)