BECLAIMIFG OVEEFLOWED LANDS IN MISSISSIPPI. 



9 



removed from the sm^face of the ground instead of being allowed to 

 accumulate over the bottoms as storage. In order to ascertain this 

 increased rate of run-off it is necessary to make a careful study of 







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■> !»^ Vj V > ^ '<N 1-- V *o <N V V 'o '^ '-^ V ^ '^ '^ 

 0>i 90/090^ 70000HS N09>iOVr nlH>^^^IO AIIQOOZVJ, 



- ft 



rainfall and run-ofi' couditioiis on tlio Pearl Iliver for the maximum 

 storms and flood conditions recorded. 



The rMinfull records of the TIniled Stattw W<Milher Bim^au for sta- 

 tions on the J-*earl Iliver watershed show tliat tlio two greatest pro- 

 tracted and general rain-s occurring since 1898 were in March, 1902, 



