1362 EDWARD D. LYNTON 
HORIZONTAL INTENSITY 
78 
2 erFy | les 
oye r 
FREEHAND MAJOR VECTORS. MON 
CURVES, ABOVE 
TERN 
ee 
ISOLA MINOR FEATURE - 
‘QUE TO FAULT eS) 
LINES OF FORCE > ys ie 
: GRAWITE “A. 
FAULT i. 
SECTION 
SEPARATION OF 
MAJOR AND MINOR MAGNETIC EFFECTS 

FIG. 5 
ported by the results of the drilling of The Texas Company’s Eastwood 
No. 1, 3 miles east of the town of Hueneme, which entered basalt at 
1,915 feet. As this assumption was proved correct, it follows that the 
80 
