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Page 13 of 23
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Functions & Conditions - Evaluating the Physical Features

 

Amount of fine materials on the channel bottom

Figure 2-15
A thick layer of fine sediments on the stream bottom may be symptomatic of a sediment/water imbalance in the system.

A properly functioning stream should, generally, be able to move fine sediments through the system. The presence of fine sediments (silts, clays and decomposing organic material) on the channel bottom (see Figure 2-15) may be an indication that not enough water is running through the system or that there is too much sediment entering the stream. This is especially the case when sediments remain in place through one or more high flow events. Fine sediments cover fish spawning areas as well as change the composition of macro-invertebrates (bugs) in the stream, which also affects fish populations.