12 



The bathymetric data were used to examine bottom topography and correlate 

 sediment composition information to relative depth within the cell. Precision sound velocity 

 measurements were not collected during the Morris Cove borrow pit survey. However, an 

 appropriate value of 1500 m-s"^ was set in the fathometer for the shallow water survey to 

 provide acceptable depth data. As a result, a small offset (-20 cm) may exist between the 

 depth reported in the profile data and the actual water level over the survey area. 



Monitoring Cruise at the Morris Cove Borrow Pit 



