lineatlon appear to differ from those south of the llneatlon. 

 This suggests further that the fault separates areas of dif- 

 ferent geologic character. The fault appears to be a strike- 

 slip fault. However, the direction and amount of movement 

 along this fault are difficult to determine. 



From the contour charts, it appears probable that the 

 major magnetic feature extends beyond the limits of the sur- 

 vey area. If projected to the northeast, this lineatlon would 

 pass through the Kalohl and Pallolo channels south of the 

 Island of Molokai. The feature Is most pronounced to the west 

 and may extend for some distance in that direction. 



