













1.40 SEC" 1 

 1.00 SEC" 1 

 0.70 SEC" 1 



20 

 40 

 60 

 80 





1 VELOCITY 



BOTTOM 

 WATER 



- 



\ 





\ 



\ >^ 











\ 



\ 



s 



V 











\ 



\ 

 \ 

 \ 

 \ 



s. 











\ 



\ 



\ 

 \ 



\ 

 \ 





100 

 120 





\ 









\ 



\ 



s 



\ 



• 











\ 



• 



140 

 160 



\ 













\ 



\ 

 \ 











P-2 



.82 



180 



BASAL 



T V '-5 

 P 



760 V ■ 



s 



= 2530 



1480 1500 1520 1540 1560 1580 



SOUND VELOCITY, V , IN SITU (M/SEC) 

 P 



1600 



Figure 4. In situ sound velocity vs depth in 

 sediment at the Mo hole (Guadalupe Site). Data on 

 basalt from Some rt on e t al . 39 



Following the reasoning and computations discussed 

 in the first section (shallow Bering Sea), some elastic 

 properties of the surficial sediments have been computed; 

 they are included in table 4. 



32 



