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<br /> <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />floodwater in a common ponding area, The <br />principal areas of flooding along Pine Ridge <br />Gulch comprise ponding areas at the Highway <br />40 and Highway 13-789 crossings. A large <br />sheet flow area would extend from the <br />Highway 13-789 crossing southerly to the <br />flood plain of the Yampa River, The principal <br />areas of lOa-year flooding on Cedar Mountain <br />Gulch comprise sheet floll- west of the stream <br />in the vicinity of the upper crossing of <br />Highway 355, and overbank flow to the east at <br />the 101l'er crossing of Highway 355, A ponding <br />area would occur at the upstream side of <br />Highway 40, and sheet flow that commingles <br />with Pine Ridge Gulch sheet flow would occur <br />downstream from Highway 40, <br /> <br />In general. the 500-year flood would follow <br />the same patterns as the lOa-year flood, but <br />inundation would extend farther from the <br />stream channels and be substantially deeper <br />in some locations. On Fortification Creek, 500- <br />year flood flows would break out to the east <br />upstream from the Highway 40 crossing to <br />inundate historically' flooded areas around <br />and easterly of the fairgrounds, Five-hundred <br />year sheet flow flooding in the central section <br />of the city would extend in a widening fan <br />shape from the vicinity of 10th Street on the <br />north to the railroad on the south. and from <br />Ranny Street on the west to the creek on the <br />east, Approximately 45 city blocks north of <br />Victory Way would be subject to sheet flow <br />flooding, <br /> <br />In total, the lOa-year flood would inundate <br />approximately 11,800 acres, of which 10,150 <br /> <br />FLOOD DAMAGES <br /> <br />A 100- or 500-year flood in the Craig area <br />would cause substantial residential, commer- <br />cial, and industrial damage, Agricultural <br />losses would also be significant and would <br />occur primarily in the bottom lands along the <br />Yampa River where crops and livestock <br />would be destroyed; farm and ranch improve' <br />ments, especially irrigation systems, would be <br />damaged; and substantial costs would be <br />incurred to restore crop and pasture lands <br />covered with silt and debris or damaged by <br />erosion, Residential losses would include <br />damage to foundations, exterior and interior <br />.walls, floors, furnishings, and appliances <br />(especially appliances and heating systems in <br /> <br />acres are agricultural. 325 acres are residen- <br />tial, 200 acres are commercial-industrial, <br />1,100 acres are streamway, and 25 acres are <br />rights-of-way, It should be noted that all of the <br />flooded areas shown on Plates 2-27 may not be <br />inundated at the same time because flood <br />producing conditions in the various tributary <br />watersheds would not necessarily occur con- <br />currently. Shallow flooding (generally less, <br />than 6 inches deep) may occur beyond the <br />flooded areas shown. The depth of flow in the <br />channels and adjacent flooded areas along the <br />streams and stream ways under study can be <br />determined from the water surface profiles <br />shown on Plates 28-44, <br /> <br />The flooded areas shown on Plates 2~27 <br />reflect unobstructed channel flow. Ice jams <br />could alter the patterns shown, especially <br />along Fortification Creek. Therefore. the <br />possibility of ice jams aggravating the flood <br />situation should be given consideration in <br />using this report. Areas historically flooded <br />due to ice jams are generally described and <br />illustrated in the newspaper articles and <br />photographs covering the 1921 and 1947 <br />floods (pages 7-12 and cover photographs), It <br />must be pointed out, however, that significant <br />changes in the alignment of Fortification <br />Creek have been made since 1947 and its <br />carrying capacity has increased, that changes <br />in streets and highways have been made, and <br />localized changes in topography have <br />occurred, Therefore, any future flooding <br />resulting from ice jams would not necessarily <br />affect areas identical to those inundated from <br />this type of flooding in the past. <br /> <br />basements subject to filling with floodwater), <br />Outside improvements such as lawns and <br />gardens would be damaged by deposits of <br />sand and silt. Commercial losses would <br />include structural and equipment damage; <br />temporary loss of business; loss of inventory <br />stored on lower floors and in basements; and <br />the costs of cleanup, repair, and restoration. <br />Railroad track, embankment, and industrial <br />sidings would be subject to damage from <br />inundation, and streambanks would be <br />eroded. Access to various areas could be cut <br />off for periods ranging from a few hours to a <br />few days. <br /> <br />25 <br />