386 



SUDE No. 7 I 



This is, again, nearby, but the bottom features are considerably 

 different. Here we have white cobbles of Eoceanerage chalk. You 

 can see the direction of transport downslope. Some of the cobble- 

 sized material is glacial erratics: 



Again, the area is relatively steep and irregular. There has been 

 a strong sweep by bottom currents and translocated material in a 

 southwesterly direction through this site. And, again, all of this 

 compounds the difficulty of traversing in a submersible that will 

 only average about 1 mile per hour through relatively flat terrain. 



Next slide, please. 



(Slide No. 8.) 



