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<br />i <br /> <br /> <br />RESTORATION OF REGULATED RIVERS <br /> <br />401 <br /> <br />High <br /> <br />Channel Substratum Composition <br /> <br /> <br />Sand & Silt <br /> <br />~ <br /> <br />High <br /> <br />Water Temperature <br /> <br /> <br /> <br /> <br />Low <br />High <br /> <br />Minimum <br /> <br />.. <br /> <br />Native Biodiversity <br /> <br />] <br />~ <br />j <br /> <br /> <br />Low <br /> <br />Headwater <br />Stream <br /> <br />Headwater <br />Transition <br /> <br />Montane <br />Floodplain <br /> <br />Montane <br />Transition <br /> <br />Piedmont <br />Valley <br />Floodplain <br /> <br />Piedmont <br />Transition <br /> <br />Coastal <br />Floodplain <br /> <br />Estuary <br /> <br />s <br /> <br /> <br />lsition (see <br />s were pre. <br />ctober and <br />large (mid. <br />en the flow <br />urvey data, <br /> <br />at create <br />minated, <br />d or lost <br /> <br />Figure 5, Conceptualized continuum of a large river after regulation by a high volume, high head storage dam in the montane transition <br />(compare with Figure 2), Tributaries downstream from the dam are assumed to be unregulated. Vertical bars on the plot of maximum <br />temperature represent the annual range of annual maximum temperature across all habitats at any point in the river continuum, Num. <br />bers indicate stream order. The figure is not drawn to scale; transition reaches are often much longer than inferred <br /> <br />