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<br />t <br />~ <br />'. <br /> <br />....."'....""'"'". <br /> <br />1\ <br /> <br />acre-foot.--A volume of water covering I acre to a depth of I foot; <br />43,560 cubic feet. <br />cross section.--A representation of the area between a streambed and <br />an imaginary level string stretched across a stream at right an- <br />gles to the streamflow. The size and shape of the cross section <br />is determined by using surveying instruments to measure distances <br />down to the streambed at various locations along the imaginary <br />s~ring. Floods usually will change the cross-section configura- <br />. tlon unless the streambed is composed of stable material. <br />cub~c foot per second.--A unit of discharge passing a cross section of <br />a stream. Toe unit of discharge represents I cubic foot of water <br />passing a given point in I second and is equivalent to approxi- <br />mately n gallons per second or 450 gallons per minute. <br />discr.arge.--The water flowing past a particular point, such as a point <br />at a cross section. The rate of flow generally is measured in <br />cubic feet per second; the volume of flow, in acre-feet. <br />drainage area.--A land area. usually measured In square miles in a <br />norizontal plane, which collects precipitation and allows the <br />resultant runoff to flow towards the most downstream point In the <br />area.. <br />envelope curve.--A line drawn above plotted points on a graph to <br />enclose the largest floods ever measured in a region; the points <br />show stream discharges for given drainage areas,. Larger floods <br />are possible; if they occur, the envelope curve is moved upward <br />to enclose the new, higher values. <br />f100d plain.--An area that is adjacent to the streambed and is covered <br />with water when the stream overflows its banks during floods. <br />f1ood-prone area map.--A map showing areas along the streambanks which <br />are subject to flooding. Areas expected to be covered by water at <br />least once in any lOa-year period are shown on the Elbert County <br />flood-prone area maps. <br />flood velocity.--Speed with which water moves downstream. A velocity <br />of 10 feet per second (nearly 7 miles per hour) would move an ob~ <br />ject floating in the center of the stream one township (6 miles) <br />farther downstream in less than I hour. <br />floodwater-retarding struature.--A dam placed across a small upstream <br />water course to provide floodwater storage. Earthen dams con- <br />,s t ructed in Elbert County, by the U.S. So i 1 Conservat ion Serv i ce <br />in the 1950's ~ere designed to hold about I inch of runoff from <br />the basin above and to release it gradually through pipes over a <br />period of 2 to 3 days. Excess runoff passes over the emergency <br />spillways at one side of the dams. The structures delay storm- <br />water traveling towards the larger creek ~hannels and help reduce <br />consequent flooding. <br />hundred-year (lOO-year) f1ood.--Peak discharges so large that they may <br />be expected to be equaled or exceeded on the long-term average <br />of about once every lOa years and have a I-percent chance of oc- <br />curring in any given year. The recurrence interval Is an average; <br />no schedule of regularity is implied. <br />runoff.--That part of the precipitation that appears in <br />streams. One inch of runoff is equal to about 27 cubic <br />second of water flowing for one day from each square <br />drainage area above the location considered. <br />stream slope.--The vertical distance a stream drops in traveling a <br />given horizontal distance. When the stream falls more than about <br />50 feet per mile, floodflows are shallow and very fast and may <br />cause considerable channel erosion. As the slope flattens to <br />less than about 50 feet per mile (a I-foot drop about every <br />lOa feet), floodflows become relatively deep and spread out as <br />the water velocity slows. <br />topographic map.--A map that shows surf"<:eceatures of a given area. <br /> <br />surface <br />feet per <br />mi Ie of <br /> <br />", <br />t <br /> <br />! <br /> <br />7 <br />