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is primarily cobble/rubble in flowing areas and silt/sand <br />in slower moving sections. Water temperatures may exceed <br />20 C throughout this reach. Peak discharges during this <br />study exceeded those recorded since 1970 (Figure 3). High <br />flows approached but barely exceeded 4000 cfs until 195.3 <br />when discharge at the Below Meeker. U. S. Geological <br />Survey lUSGS) gage station exceeded 6000 cfs. <br />7 <br />