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<br />3 <br /> <br />CHAPTER 2 <br />CHANNEL NARROWING OF THE GREEN RIVER NEAR GREEN <br />RIVER, UTAH: HISTORY AND RATES OF NARROWING1 <br /> <br />INTRODUCTION <br />~he adjustment of landforms to changes in the magnitude and frequency <br />of their formative processes and to changes in vegetation is of long-standing <br />geomorphic interest. Twentieth-century climatic change, nonnative vegetation <br />invasion, and construction of large dams have altered the character and <br />function of riverine ecosystems in the semiarid western United States. Habitat <br />availability at critical life stages of endemic endangered fish, the quality of river <br />recreation, and the magnitude of sediment transfer to downstream reaches <br />have also been altered. The Colorado River system has been greatly affected <br />by each of these climatic, biotic, and anthropogenic changes. In an era when <br />dam operations are being revised to mitigate and improve downstream river <br />environments, it is essential that we understand the magnitude of twentieth- <br />century channel change and the relative roles of climate, vegetation, and dam <br />construction in causing those changes. <br />This study concerns adjustment of the Green River near Green River, <br />Utah (Fig. 1). This reach has been known to geologists since John Wesley <br /> <br />1Coauthored by Tyler M. Allred and John C. Schmidt <br />