The physiography of the river Nile and is basin . - 5 S X S M. %;?? S3- n ifi G — 170 — of the water near tlie jiiiictioii was passing down with a velocity nearlythe same as that of the Blue Nile water. It is very doubtful if at anytime water flows from the Blue Kile np the White Nile channel, butthroughout as has been stated to be the case July and August, butthis point is discussed in detail by Mr. J. I. Craig in Chapter \, too, that the Sobat flood-supply nuist be estimated at lessthan 1500 cubic metres per second, and that of the Bahr el Zaraf, Bahrel Jebel and Bahr el Ghazal com
The physiography of the river Nile and is basin . - 5 S X S M. %;?? S3- n ifi G — 170 — of the water near tlie jiiiictioii was passing down with a velocity nearlythe same as that of the Blue Nile water. It is very doubtful if at anytime water flows from the Blue Kile np the White Nile channel, butthroughout as has been stated to be the case July and August, butthis point is discussed in detail by Mr. J. I. Craig in Chapter \, too, that the Sobat flood-supply nuist be estimated at lessthan 1500 cubic metres per second, and that of the Bahr el Zaraf, Bahrel Jebel and Bahr el Ghazal combined at less than 500 cubic metres persecond,- the maxinuun discharge cannot reach 200O cuijic metres persecond under the present conditions, when the amount of flooding inthe Taufikia-Kliartouin reach, ami the amount of water wdiicli themarshes lining its banks must absorb, is taken into account; aho thedischarjiesfor 1902 and 1003 show that the maximum dischar<ce of theWhite Nile takes i)lace in Deceml)Cr when the floods are subsiiling,after th
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Keywords: ., bookcentury1900, bookdecade1900, booksubjectwatersupply, bookyear
