PLAN of part of the Course -oft. he GAN GE S , to explain the nature of the steep and shelving Banks, &r. 
Thilos. Trans. Vol.LtXXl .Tab . P ^ U ■ 
J\.A. Steep Bants corroded by die Current, the fragments 
of which are depofitBd,and form the Banks 13. B. 
C . A Sand Bank accumulating to an dfland .'This once 
joind (o D. till updated by a Breach of the River. 
E. An Island formed k inhabited.. This also was a Sand 
Bank thrown up round die Point F. 
G. An Ip and ateunuda/i/uj in the midp of the Channel. 
Ii . The line ■ of die Jb-oru/ejl Current. 
■ fp L 
fp-t: M 
Pubna . / t 
