NON-CONSERVATIVE PROPERTIES 



195 



STATIONS WS 1070 

 SEA MILES I 



OFFSHORE IOO 



O 



WSIOM 



IOO- 



E 200 



300- 



400 



Fig. 42. Distribution of dissolved oxygen. Section off Sylvia Hill, 25-27 September 1950, survey II. 



Positions of stations are shown in Fig. 2. 



STATIONS 



SEA MILES 

 OFFSHORE I" 



o- 



WSI080 

 I 



WSI078 



I 



VWI077 WSI075 

 ! I 



25 



Fig. 43. Distribution of dissolved oxygen. Section off Walvis Bay, 29 September-3 October 1950, survey II. 



Positions of stations are shown in Fig. 2. 



It was suggested on p. 183 that the water against the edge of the continental shelf at these depths 

 exhibited a southerly movement, and therefore it is interesting to amplify our own results from some 

 stations of the 'Meteor' (Wattenberg, 1933) to the north and south of the region. These are plotted 

 in Fig. 46 and show a still wider contrast between the stations in the north and in the south. The 

 positions of the 'Meteor' stations are shown in Table 10. The two curves from the 'Meteor' stations 



