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<br />FLOOO FREQUENCY-ELEVATION AND DISCHARGE DATA II
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<br />on
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<br />Stationing
<br />from Mouth
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<br />Ident i fi cat ion
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<br />Stream Bed
<br />Elevation
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<br />Existing ConditionsA;b~ /:1,77
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<br />Crest-Elevation Feet (Metres) National Geodetic Vertical
<br />Datum, and Peak Discharge c.f.s. (c.m.s.)
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<br />n : Feet (Metres)
<br />
<br />Feet (Metres)
<br />N.G.V.D.
<br />
<br />IO-Year
<br />Flood
<br />
<br />50-Yea r
<br />Flood
<br />
<br />, 100-Year
<br />, Flood
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<br />SOO-Year
<br />Flood
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<br />75.;7>~,-~: ;~0cJ(), () /010.3 / '>"ll-)C) _:l
<br />/'/() / / ,.50 /j (}(J /650
<br />70 {];L. 9 7/, U:5'- /' 700.5:7 "'J ' ;/-
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<br />770 //50 /300 /650
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<br />/0/I<Q~J ,/'::0/0" . . / /0/ ,
<br />770 //5'0 /...700 /6.50
<br />70//.2 '/ -/ / 'g . /. 'L ;-J;:;;:'/.6
<br />/'10 ,-:_ ~ ,A..:1(': ,";-
<br />770 //5'0 /300 ,/~.1--.)
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<br />"'/~71""] .7.50 .?
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<br />/':;,j~? 76 "F-' 76 :S.);_~- ,";'35:7
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<br />770 //.5CJ /Z90 /0-:5CJ
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<br />.<5" r 70
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<br />3;70
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<br />ood elevations pertain to the primary channel and usually remain constant in a lateral direction across the flood
<br />ain. However, flood elevations in the outer portions of a cross section may differ from the primary channel due to
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