42 FLORIDA GEOLOGICAL SURVEY cfs and the peak flow on the same day was 24,800 cfs-over 2% times greater. The flow-duration curve for Pine Barren Creek given in figure 15 shows the percent of time a specified discharge has been equaled or exceeded. For example, the mean daily flows at the gaging station were CHANNEL DISTANCE ABOVE SOUTH, IN MILES Figure 24. Channel-bottom profile of Pine Barren Creek. greater than 67 cfs (43 mgd) for 98 percent of the time. If an industry needs a water supply of 43 mgd, a deficiency 2 percent of the time might be tolerated if it were uniformly distributed, with only a few days of deficient flow in any continuous period. A deficient flow of 2 percent of the time, on the other hand, could prove disastrous if it came in a con- tinuous period of several months duration. The data given in figure 25 are helpful in determining probability of length of periods of deficient flow. The lowest average flow for a specified period can be determined from the lower curve in figure 25. -00 -- -- ,r -- -- -- -/- - ,I. _. ___ I __ - S ___ S Spe.g5ophic map. 2) ' -f rr---- 0o 2 4 10 12 14 as t 20 22 24 26 i