A significant proportion of stream sediment yield in North America com
es from stream channel and bank erosion. One method used for stream st
abilization is the bank installation of timber and stone fish-shelter
structures, but there is little evidence for their potential effective
ness. Nine to nineteen years of precise survey data from Goon Creek, W
isconsin, however, show that fish structures enhance sediment depositi
on along the stream and may retard lateral migration of channels. Such
structures have greater utility for sediment control when streams are
eroding away a high bank and replacing it with a lower bank.