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<br />to life and p~operty. Wate~ flowing in excess of four feet per <br />second is capable of t~ansporting sediment and causing severe <br />erosion of streambanks and fill around bridge abutments. Where <br />velocities drop below two feet per second, debris and silt deposits <br />can build up, extending the flood damages and creating adverse <br />health conditions. The saturation effects of prolonged flooding <br />can weaken bridge abutments, levees and other embankment works so <br />they fail as the floodwaters recede. <br />Prope~ty damage f~om g~eat floods in developed areas <br />Can be ove~whelming. The entire community suffe~s when streets, <br />b~idges, sewers, and other public utilities are damaged or destroyed. <br />Adding to the phySical haza~ds, a g~eat flood can unleash deadly <br />epidemic diseases, Sanita~y Sewers become p~essure lines, blowing <br />~nhole cove~s to spew raw sewage into the floodwaters; sewage <br />t~eatment plants and feeder lines can be washed out; stockyard waste <br />Can add to the pollution and hazard of an epidemic disease. News~ <br />papers sometime 'report a Hlighter side of the news" in picturing <br />children at play in the mud and standing water left by a receding <br />flood. Unfortunately, the contamination threat to domestic water <br />supplies cannot be illustrated with similar aase. <br /> <br />floodw~ters become isolated and entrapped in overbank areas resulting <br />in depthS greater than thoee n~own on the ~iqh water prOfile". F~ <br />Inter~tate 25 to t~e Mouth of Hospital Canyon, floodwater elevations <br />for future floods may be expected to be greater in the overbank areas <br />than along the ~ainstem because of the obstructive effects of bridge~, <br />freeway aCCess ramps, and roadbed. In past floods, b.-idges "'ere <br />washed out which increased channel conveyance and relieved overbank <br />flooding. The areas i~ediately upstream from the mouth of Meores <br />and Colorado Canyons are subject to severe flooding in case of floods <br />of less magnitude tr4n the Intermediate Regional Flood. The stream <br />channels arc insufficient to car.-y any but the snallest flow. The <br />only major development on these flood plains is the trailer park in <br />Moores Canyon. TheconduitsonfiehersPeakArroyOaooPinonCanyon <br />will not convey floodwatern of Star.dard Project magnitude. Hshers <br />Peak floodwater will leave the channel flowing through buildings and <br />pri~arily do~~ Commercial Street. Floodwater on Pinon Canyon ",ill <br />leave the chanr.elprior to the conduit at Colorado Avenue bccaus" <br />of the ob~tructive effects of the willow Street bridge and insuffi~ <br />cient channel capacity. Floodwaters of Standard Project and Inter~ <br />mediate Region~l ~loods will leave the channel at Willow Street and <br />imnlediately Lelow the Kansas Avenue conduit, respectively. Areal <br />distributi~n for a given flood is non-uniforrr, and paths unprL~ictable. <br />Depths of flow for any given stream location can be estirnated from the <br />high water profiles shown on Plates 16 through 38. Plates 39 through <br />4S show selected cross sections of the streams that are typical of <br />the approximately 145 sections surveyed in the study reaches; all <br />cross section locations dre s'~wn on the profile plates. stream <br /> <br />Flooded Areas and Flood Damage <br />Trinidad Dam will effectively reduce the frequency of <br />flooding ..long the Purgatoire .River in Trinidad from atorms occurring <br />above the dam, but flood events may still inundate the historic flood <br />plains. Should a severe storm occur over the study area, the trib- <br />uta.-ies will sybject mdny areas to flooding, and the Purgatoire <br />floodwaters will increase in intensity while proceeding downstre~~ <br />and c:olleetinCJ frnm thp trihut:u,..". Pl..-rp?, '-'l ~n i"""1< n>'\!, fn,.- <br />the succeeding Plates 3 through 15 which nbow the areas along the <br />Purgatoire River and tributaries that will be flooded by the Stand- <br />ard Project Flood, Ioterm~i~te PegionaL FLood, and the area flooded <br />by the September 1904 flood of record. <br />Floodwater elevations dete~ined in any particular ~rea <br />are not always ir.dicative of the depths actually attained. Often <br /> <br />characteristics d~tPrm'n~ f"-Qm tnP0~,.-~pnic md!,q, ~~,.-f~1 r~~nsr~rhq <br />and valley cross sections were used to compute and define the flood <br />situation. <br /> <br />Velocities, Rates of Pise, and Duration <br />The OCCurrenCe of the Intermediate Regional ~r Stand- <br />ard Project flood would result in the flood characte.-istic$ "ho~~ <br />in Table S. This data .-eflocts the avoraged maxi",,,,,, conditions ~.ith <br /> <br />" <br /> <br />" <br />