I'/iitos. Tnms. Vnl. f-V.Y7.T.ili. tV p H4 . 
A A. Steep Banks corroded by Che Current, the fragments 
of which are depojited.and term the Banks B.B, 
C . si Sand Bank accumulating to an [/land. This once 
Joind to D. till insulated by a Breach of the River. 
E. An Island formed fc inhabited. This also was a Sand 
Rank thrown up round die Point F. 
G. An Ifland accumulating iti the midjlofthe Channel . 
H. The line of the Jirongeft Current. 
Pubna 
.Miles. 
Sujanagur 
1 ^ A Gulf occasioned by the force of the (hr rent t 
from die oppofite side striking against the Banff 
die origin of a future Branch Jir iking out from 
die Ganges . In a Course of time, the first Reach 
becomes Retrograde to the Course oC the River. 
( See Mote page gji as at K&: L . 
Level doping the height of the Wet Seafon . 
300 Yards. 
jcvcl in the dryeft part o f t he Year. 
PLAN of part of the Course of the CrAN GE 8 , to explain the nature of the strep and shelving Ban Us, fi'r. 
SECTION of a Branch of the IrA JNTG E S , as a farfbrr r.vp/a nation of rhe f rep and ft/ ch/ing Bvn/cs. 
.'MB. This is e.raetly Jimifetr to rhe Section op the winding parts tgthr (rouges itpip, except in the article tgioidth. 
