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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />7 <br /> <br />formed along the shorelines, but most of the river is run type of <br />habitat. Backwaters are found at this time only in the flooded mouths <br />of washes (Walker Hollow, Baser Wash). One small riffle is located <br />near the center of the study area, at the middle station indicated <br />in Figure 1. Other small areas of cobble substrate are located along <br />the shorelines, especially below talus slopes. Over 99% of the river <br />bed is sand. <br />As waters recede in mid-summer, sandbars become exposed and create <br />a more heterogeneous mix of habitat types. Small backwaters become <br />quite common around the sandbars. Silt tends to become deposited in <br />the backwaters, adding to the complexity of substrate types. <br />River banks in the study area are prominent and many are actively <br />eroding. Willow (Salix sp.), salt cedar (Tamarix pentandra), and <br />other shrubs line the banks and large groves of cottonwoods (Populus <br />fremontii) occupy many of the older, more permanent, sandbars. Most of <br />the land surrounding the study area is rolling desert shrub, with some <br />agricultural use, especially between the upper and middle stations <br />(Figure 1). <br /> <br />Biological Characteristics <br /> <br />Literature Review <br />Literature referring to the aquatic biota of the Green River is <br />rare. Material relevant to the Moon lake study area is esrecially <br />scarce. The literature review, therefore, was expanded to include the <br />river from Split Mountain GorQe to Sand Wash. The literature review <br />