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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 /> <br />Within the study reacnes, the Lake Fork has an average gradient of 0.6% <br />and an average channel widt~ Of EO feet. Normal water depths are 2.5 feet. <br />Henson CreeK, v;lth;n Its S:UGj reacn, "as an average gradient of 1.2%, average <br />width of 50 feet and average depth of 2 feet (during normal flows). Stream <br />sub-strate consists of large boulders, cobbles and bedrock. Streamside <br />vegetation consists of cottonwoods, willows and similar brush along both <br />streams. <br />Obstructions to floodflows within the study reach include both natural <br />obstructions such as vegetation growth, fallen trees, ice jams, etc. and <br />man-made obstructions such as bridges, buildings, fences and roadways. These <br />obstructions have a tendency to increase flood elevations upstream of the <br />obstructions and increase velocity downstream of the obstruction. <br />The stream valley above the Lake Fork study reach is essentially similar <br />to the study reach description (except it has a narrower flood plain). Lake <br />San Cristobal, a natural lake approximately 3.5 miles above Lake City, has a <br />dampening effect on potential floods such as those occurring from high intensity, <br />short duration rainfall. For long duration spring snowmelt and combination <br />rainfall, however, the effect of the lake on peak floodflows is minimal. <br />The stream valley above the Henson Creek study reach is very narrow and <br />steep. Trees and brush grow out over the channel in many areas along this <br />tight valley. High waters could carry great amounts of debris through the <br />study reach and accentuate the flood elevations. <br />The historical use of the floodplain has been for range, wildlife and <br />resort activities. Land adjacent to the streams is privately owned. These <br />areas have good plant cover and support meadow vegetation, willows and <br />cottonwood. Small areas within the floodplain are flooded annually and support <br />little or no vegetation. The growth of Lake City in recent years has forced <br />greater development in the flood plain. With this increased encroachment of <br />development in the flood plain, the flood hazard to the community is increased <br />and will continue in the future unless adequate measures are adopted to keep <br />the development outside the flood hazard areas. <br /> <br />I Il- 5 <br />