TABLE B-1 



II I Horizontal Kinetic 

 I energy (dynes/sec) 



"^ I speed (cm/sec) 



Furthermore, when this energy is broken down into the tidal and residual compon- 

 ents, "crse random motion is actually greater than that due to tidal forces. Al- 

 tnough tne lower percentage of tidal flow would reduce the potential for predic- 

 tion of currents, the lower absolute value of the currents is well below any 

 threshold values for erosion of sediment. 



~ha 10% hignest speed measured during this sampling period was 13.6 cm/sec, 

 also below threshold erosion velocities. Wave action should have minimal effect 



