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<br />GLOSSARY OF TERMS <br /> <br />which the elevation Is measured. <br /> <br />"004 <br /> <br />IlsadLoss <br /> <br /> An overflow "0 lands ~, normally covered by water and <br />thataro used or usable 'f man. Floods have two essential character- <br />istics: T", inundation of land ;, temporary; '"' '", land Isadjacont <br /> <br />to and inundated by overflow from a rivoror stream or an ocoan, lake, <br />Or othor body of standing water. <br />Normally a "flocd" is considered I>S any to/l'lpora,.y rise in <br />stream flow 0,. stage, that results In significant adverso effects In <br />the vicinIty. Adverse effects may InClude damages from overflow of <br />land areas, temporary backwater effects in sewers and local drainage <br />channels, creation of unsanitary condItions or other unfavorable <br />situatIons by deposition of materials In stream channelS during flood <br />recessIons, rise of ground water coincident wIth increased stream flow, <br />and other problems. <br /> <br />The etfect of obstructions, such as na,.row bridge openings <br />orbulldlngsthatllmittheareatnroughwnichwate,.musttIOlO,raising <br />the surface of the water upstroam from the obstruction. <br /> <br />Intermediate Regional Flood <br />A flood having an average frequency of occurrence In the <br />order of once in 100 yegrs although the flood may occur in any year. <br />It Is based On st~tlstical analyses of stream flow records av~ilable <br />for thG watershed and analyses of rainfall and runoff characteristics <br />in the "general region of the watershed." <br /> <br />Left Bank <br /> <br />The bank on the left side of a river, stream or water <br />course, looking downstream. <br /> <br />FloodPlain <br /> <br />The relatively flat area or low landS adjoining th~ chan- <br />nelofariver, streilmor watercourse or ocean, lake,orotherbody <br />Of standing water, which has been or may be covered by flood water. <br /> <br />Low Steel (orUnderclearance) <br /> <br />See "underclearance." <br /> <br />, loo~ Prof I Ie <br /> <br />RIght9ank <br /> <br />A graph showing the relationship of water surface elevation <br />fo loclltion. the latter generally ex::>ressed as dIstance ilbovemouth <br />fora stream of water flowing in an open channel. ItlSgen",rally <br />drawn to show surface elevation for the crest of a specific flood, <br />but may be prepared tor condItions at a given tlm~ or stage. <br /> <br />The bank on the right side of a river, stream, or wate,. <br />course, looking downstream. <br /> <br />Flood Stage <br /> <br />Standard Project Flood <br />The flood that may be expected trom the most severe com- <br />bination of meteorological and hydrological conditions that is con- <br />sidered reasonably characteristic of the geograrhlcal area In whiCh the <br />drainage basin Is located, excluding extremely rare combInatIons. Peak <br />discharges for these floods are generally about 40 percent to 60 percent <br />of the Prob~ttle MaxImum Floods for the sa~ basins. Such floods, as <br /> <br />The stage or elevation at whiCh overflow on the natural <br />banks 0+ " stroam or body of "ater begins In the roach or arail in <br /> <br />21 <br /> <br />22 <br />