KECLAIMING OVERFLOWED LANDS IN MISSISSIPPI. 
17 
(2) Tho approxijnato timo roquirod for tho rivor to fall from a 
maximum to a low stage when no storage exists. 
(3) Tho probable shape of the hydrograph as determdnod from a 
consideraticm of (1) and (2). 
^§f-Hr J^Cir ^et-fir j^i/s- .,60'S91Vl61\ 
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(4) The total run-off for the entire flood period. 
(5) The probable run-off due to rains occurring after the maximum 
stage is reached. 
(6) The amount of run-off which would produce the maximum 
stage as determined by deducting (5) from (4). 
74745°— Bull. 181— IJ 
