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<br />4 <br /> <br />All sites were slightly larger in channel area and width in 1986. <br />The channel area for all alluvial sites increased from 3,336 acres <br />in 1978 to 3,413 acres in 1986, an increase of 2.3 percent. An increase <br />of 77 acres in 41.8 river-miles equates to 1.8 acres per river-mile. <br />The channel area for nonalluvial sites changed from 2,275 acres in <br />1978 to 2,319 acres in 1986, a net increase of 1.9 percent. An increase <br />of 44 acres in 27.4 miles equates to 1.6 acres per river-mile. The <br />net change in average channel width from 1978 to 1986 ranged from a <br />gain of 30 feet for river-miles 142 to 131 to a gain of 7 feet for <br />river-miles 128.3 to 117. Average channel width for alluvial sites <br />changed from 659 feet in 1978 to 674 feet in 1986, a net increase of <br />2.3 percent. The average channel width for nona1luvial areas increased <br />from 684 feet in 1978 to 697 feet in 1986, a net increase of 1.9 percent. <br />The total river area increased by 120 acres (+2.1 percent) and channel <br />width increased from 669 to 683 feet (+2.1 percent). <br /> <br />The slight increase in channel width indicated by the 1986 data may <br />be attributed to flood incidents in the early 1980's. Increases in <br />alluvial sites channel width were slightly smaller than width increases <br />in nonalluvial areas. <br /> <br />Figure 2 graphs the channel width from 1963 to 1986. Although the <br />average river channel width decreased significantly from 1963 to 1974, <br />it is not of the same magnitude reported by Andrews (1986), which was <br />90 feet in this segment of the Green River. The slight river width <br />increase between 1978 and 1986 probably demonstrates the Green River's <br />response to flood episodes in 1983 and 1984. The very slight changes <br />in channel width from 1974 to 1978 indicate that the Green River channel <br />width is stabilizing from Split Mountain to Willow Creek. <br /> <br />It was observed that of the 357 acres of channel area lost between <br />1963 and 1974, 154 acres (43 percent) were related to increases in <br />number of islands, island size, and the loss of side channels previously <br />associated with islands that have increased in size to the point that <br />they have become part of the channel bank. In table 3, old islands <br />are islands that are now part of the channel bank, and old channels <br />are side channels that have been filled and are not part of the bank. <br />In general, the number of islands and their acreages increased from <br />1963 to 1974 when old islands and old side channels were included in <br />the calculations. The acreage of islands increased only slightly from <br />1974 to 1978. There was a relatively small decrease in island acreage <br />from 1978 to 1986, again reflecting the flooding which occurred in <br />1983 and 1984. Figure 3 illustrates the changes in vegetated islands <br />per river-mile. The largest change occurred from 1963 to 1974, as <br />expected (+12 percent), leveled off from 1974 to 1978, and decreased <br />slightly from 1978 to 1986. The increase in island acreages was approxi- <br />mately twice as large in nonalluvial areas than in alluvial areas. <br />Andrews (1986) also reported that the most significant process narrowing <br />the channel in this segment of the Green River occurred where a side <br />channel filled with bed material and the midchannel bar had become <br />attached to the bank. <br />