REPORT OF INVESTIGATIONS No. 42 upper pool at Cherry Lake outlet. The fall between Lakes Louisa and Minnehaha was 0.4 foot during this period. The channel below Cherry Lake has been improved by a canal leading into Lake Lucy and Lake Emma. Palatlakaha Creek follows a more definite channel with steep gradient from Lake Emma to its mouth at Lake Harris. The fall in this reach is about 32 feet in 12 miles. STREAMFLOW Streamflow data. for gaging stations in the Palatlakaha Creek basin during the data-collection phase of the investigation are summarized in table 6. The flow-duration curve for Big Creek near Clermont (station 3), adjusted from the short-term period to the 311/-year period, 1931-62, is shown in figure 15. Long-term records for the Withlacoochee River at Trilby (station 42) were used for the adjustment because discharges at other long-term downstream stations on the Oklawaha River are partly regulated by water-control structures. Streamflow of the headwaters of the Palatlakaha Creek upstream from Lake Louisa is unregulated. Since 1956, the flow below Lake Louisa has been regulated by a water-control structure at the outlet of Cherry Lake. During periods of low rainfall, most of the drainage from the 160-square mile basin above Cherry Lake Outlet is stored in the chain of large lakes and marshes between Lake Louisa and Cherry Lake. Comparison of peak discharges during floods in March 1960 and September 1960 in Big Creek, Little Creek, and the upper Withlacoochee River shows the effect of the interconnections between the Little Creek and the Withlacoochee River basins. The peak discharge for the March 1960 flood in Big Creek at station 3 was 628 cfs. The discharge in Little Creek measured at station 6 near the peak of this flood was 801 cfs. The higher discharge from the smaller drainage area of Little Creek indicates that most of the flow was draining from the Withlacoochee basin into Little Creek through saddles in the drainage divide. The peak discharge during the flood of September 1960 for Big Creek at station 3 was 691 cfs. The concurrent flood peak for Little Creek at station 5 was 400 cfs. The flood peak for Withlacoochee River near Eva (station 36) was 2,160 cfs in March 1960 and 1,290