to 



-2 



1 1 



1 



1 1 1 1 1 1 



1 1 1 1 1 1 1 



1 1 



1 



_^\^ 



"^ 



"tT ^ 



80 Uaves TO 1 - 



Sol Id 



_ 



— ^\^ 





A ^ 



80 Uaves T03 - 



Dashed 



— 



— 





A 







" 



- 











- 



— 





^\^ ^ — ^ 



o^ - ^ 





— 



— 











— 



1 1 



1 1 







1 l\ 1 1 1 ^ ~1 



\| ~|^ 



t^ 



-4 



2 4 G 



RANGE - (ft) 



10 12 14 



1 



_l 



1 1 1 1 



1 1 1 1 1 



1 



1 1 1 1 1 



1 1 



_ 





^^J 



"'^^v — ~ ^ 







370 Waves TO 1 



- Sol id 



— 







"\.l ~^ 



\. 





370 Ulaves T03 



- Dashed 



- 



% ° 



— 



^^^" 



"^ 









~ 



^^^^c^^ 



^^^ \ 









- 



' 



— 



^"~^^^ 



^^~^- - _ \ 









— 



> 



LU 









\^ 





^\^ x^ 



^ 



— 



-2 



1 



1 1 1 1 



1 1 1 1 1 



V. 



1 1 1 1 1 



-^1 1 



-^^^ 



RANGE ^- (ft) 



10 12 



1G 



1 



_i , 



1 1 1 



1 



1 1 1 1 1 



1 



1 1 1 1 1 1 



1 l_ 





---^' 



— ^ ^ 



^ 







1650 -P Waves TO 1 - 



So lid ~ 







\^^ 





- 





1G50 -P Waves T03 - 



Dashed— 











^v^ 



























~ 



^ 



-Sc^ 



\ 







- 





- 







^C^^^"^^^^^ 





^^^^^ 



- 



1 



- 







^\^ 



\ 



\ ^^Sv 



- 





— 







^\^^ 





~\ \. 



- 





— 







^\,^ 





^ ^^ 



""^^-v^_ — 



2 



1 



1 1 1 



1 



1 1 1 1 1 



>\ 



1 1 1 1 ~1 \l 



1 1 



2 4 G 8 10 12 14 



RANGE - (ft) 



Figure 24. Reduced sediment comparison, TOl versus T03 



69 



