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<br />DRAINAGE: BASIN <br /> <br />i\part of the surf"ce of tr.1l "ilrth thilt isocclJpied by a drairla'Je <br /> <br />Sy.'ltlOffi '"hich consists of <br /> <br />surfdc" <br /> <br />stream, <br /> <br />its tributiuies, arld <br /> <br />, <br /> <br />impounded surface ."iJters and lakes. <br /> <br />EOLIAN <br /> <br />A term 2lpplied to deposits arranged by <br /> <br />", <br /> <br />wind, <br /> <br />such <br /> <br />" <br /> <br />", <br /> <br />sands and other loose materials along shores. <br /> <br />FLOOD <br /> <br />An overflow on lands not rlormally covered by water and that are <br /> <br />used or usable by man. <br /> <br />FloodS have two essential characteristics; the <br /> <br />irlundationof land is temporary; and <br /> <br />", <br /> <br />land <br /> <br />is adjacent <br /> <br />" <br /> <br />ood <br /> <br />inundated <br /> <br />by overflow <br /> <br />from <br /> <br />a river or stream or an ocean, lake, or <br /> <br />other body of stilmlin'l waton. <br /> <br />Normally a flood is considered <br /> <br />as any <br /> <br />temporary <br /> <br />rise in str"ilm[1uw or stilge, but not the ponding of surf,;"e <br /> <br />w~tQr, that results in significa~t adverse effects <br /> <br />, 0 <br /> <br />the vi"inity. <br /> <br />Adverse <br /> <br />effects may <br /> <br />include <br /> <br />damay"s <br /> <br />fror;1 <br /> <br />overflow of land areas, <br /> <br />t",",PO ~ dry bacb-lat..,~ cffectlJ in IJc....c~" ;1:"1d <br /> <br />lec,,1 <br /> <br />dr.:;J.naga ch"nn"ls, <br /> <br />creiltion of <br /> <br />uns;1nitilry conditions or other lmf<lvorJ.ble situations by <br /> <br />deposition of materials in stream channels during <br /> <br />flood <br /> <br />re"..ssions, <br /> <br />u,"" <br /> <br />"f ground <br /> <br />water coincid..nt with increased streamflow, and other <br /> <br />problems. <br /> <br />Fl.OOD, Hll-YEAR <br /> <br />A typo of <br /> <br />flood, <br /> <br />including <br /> <br />,", <br /> <br />'..ater <br /> <br />Sur [ace elevation and <br /> <br />t<e"it"ri.'ll <br /> <br />"ccup~ t ion ttll' reof, ...1'. ic,~ can be ex pected to occur ,1t any <br /> <br />t line in a Cj i V.HI ara" hilsed upon recorded hi ~to r icnl pr ec i pi tation and <br /> <br />other <br /> <br />valid data, but with <In average statistical arle percent chance <br /> <br />" <br /> <br />I <br />II <br />" <br /> <br />of being equ.'Ill..<'l or ..xceeded during ilny one year. The term <br /> <br />i:; usc.d <br /> <br />interchangeably with a one percent <br /> <br />flood or rntermediate Regional <br /> <br />F'lood. <br /> <br />(S..e<1efinition for tntermediate Regional Flood.) <br /> <br />I <br />I <br />, <br /> <br />,LOODCRE:ST <br /> <br />The maximum state or eleViltion reached by the waters of <br /> <br />, <br /> <br />flood <br /> <br />ilt a given location. <br /> <br />Fl.OOD FREQiJE:NCY <br /> <br />(See ProbabilitY.l <br /> <br />The "verage recurrence interval of specific <br /> <br />disch,uges or water stages which COluse flooding. <br /> <br />FLOOD PEAK <br /> <br />The maximum <br /> <br />instantaneous dischan.le of <br /> <br />flood <br /> <br />at a given <br /> <br />, <br /> <br />location. <br /> <br />It usuOllly occurs at or near the time of the flood crest. <br /> <br />FLOODPLAIN <br /> <br />'h, <br /> <br />in and <br /> <br />adjacent to <br /> <br />are" <br /> <br />a stream, <br /> <br />whiCh Is subject to <br /> <br />fl<'l<'lo1ic,<; a" th~ r'""..,lt .,! th" ':l<",ur~enc(! ':l: ;l l~'t-l'c'::~ ~lood 011.0 which <br /> <br />is thus So ad\lers.. to past, current, or <br /> <br />foreseeOlble construction or <br /> <br />land <br /> <br />use <br /> <br />as to constitute a significant haZily(l tn puhlic health and <br /> <br />sOlfetyor to property. <br /> <br />FL00~ PRC'f E.~ <br /> <br />^ grilph showing the relationship of water <br /> <br />surface elevation <br /> <br />" <br /> <br />location, the latter generally expressed as distance above mouth for a <br /> <br />stream of water flowin'] in <lit o!l"n "hannel. <br /> <br />It is <)enerally drawn to <br /> <br />show surface elevation for the crest of a specific flood, but may be <br /> <br />pr~par"d for conditions at a given t1me or stage. <br /> <br />24 <br />