EECL.\IMIXG OVEEFLOWED LANDS IN MISSISSIPPI. 



17 



(2) The approximate time required for the river to fall from a 

 maximum to a low stage when no storage exists. 



(3) The probable shape of the hydrograph as determined from a 

 consideration of (1) and (2). 







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0>loniD50}{ 30000HS NOS'MOVP lllH>iOna AIIQOOZV/^ 



(4) The total run-off for the entii(i flood period. 



(5) Tho probable run-off duo to rains occurring after tho maximum 

 stage is nmoluul. 



(6) The unioiiDt of nui-ofF which would produce tho maximum 

 stage as determined })y deducting (5) fioju (4). 



7474.0'— Hull. 181—1.') 2 



