Bd. III: 2) CONTRIBUTIONS TO THE GEOLOGY OF THE FALKLAND ISLANDS. 
5 
marked, the bays attain a very characteristic shape: a narrow, riverlike channel 
branching repeatedly towards the interior. On the largest scale we meet this type 
of bay in Port Salvador on the north coast of East Falkland (fig. 2); other typical 
specimens are Many Branch Harbour, Chaffers Gullet, Double Creek and many 
more in West P’alkland. 
'’ilvtuior MiU. 
800 
■tsxtrt- 
Is, 
.Ml ÖUiJL'ML, , 
U rt tcLi n 
Fig. 2. /W Salvador. 
(Copy of the British .Vdmiralty Chart [1115]). 
