EECLAIMIISTG OVEEFLOWED LANDS 11^ MISSISSIPPI. 



13 



run-off would have been for the same period had there been no rain 

 after May 20. This lower curve was obtained by platting a portion 

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practically no ruirifull equal to th(i period May 24 to July 17, a point 

 of beginning on this hydrograph being taken where the discharge 

 equaled that of May 24. The area between the upper and lower 

 curves represents the total amount of run-off due to the period of 



