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6 <br />Five river habitat types were arbitrarily named and described be- <br />cause measurement of physical characteristics such as velocity, depth, <br />width, or height of fall rarely was possible. These types are: <br />CATARACT Broken water - gradient or force of current <br />over or around an obstruction eliminates <br />standing waves (Figure 2). <br />RAPIDS Broken water - generally with regular <br />cresting, standing waves caused by chan- <br />nel constriction, submerged or protruding <br />obstructions, or gradient (Figure 3). <br />RUN Smooth surface - current flows in center <br />of stream and/or eddies compose less than <br />one-third of stream width (Figure 4). <br />RIFFLE Surface broken - water depth is "shallow" <br />(Figure 5). <br />POOL Smooth surface - main current flows to <br />one side of center and/or eddies compose <br />more than one-third of stream width <br />(Figure 6). <br />Location and length of each type was marked on a map. The percen- <br />tage of each type was derived by dividing the total length of each type <br />by the stream length. <br />Data on water chemistry were derived from Wiltzius (1966) and Mor- <br />gan (1959). <br />BIOLOGICAL DATA <br />Biological data consist of fish species identification, distribu- <br />O <br />tion, age and condition determination, aquatic plant samples, and aqua- <br />tic insect samples. <br />Fish samples were collected with: 1) variable mesh gill-nets, 2) <br />electro-fishing units, 3) set lines, 4) rod and reel, and 5) seines. <br />o <br />Gill-nets were 125 feet by 6 feet and were divided into five sec- <br />tions of one inch, one and one quarter inch, one and one-half inch, one <br />and three-quarters inch, two inch square mesh. The nets were set in