APPENDIX 



The data included in the appendix are not necessary to the 

 main arguments of the papero They represent valuable field data that 

 are worthy of recordo 



Table 15, — Averagei/ vertical position of isotherms 

 on stations 1 through 1 , Smith Cruise 5p 

 in the vicinity of Canton Island, All 

 depths are in feet„ 



1/, 



Three to six 900-foot bathytheiiuograms were taken at each station. 



2/, 



Top 01' thermoclins is the point of major change of temperature 



with depth. When the change was not wall defined selection was 



somewhat arbitraryo Generally this occurred near the Equatoro 



3/t 



emperatures taken with bucket thermometer 



41 



