{ 
P. E. Chase on Magnetic Inclination. 171 
e 
that may possibly become valuable in the course of future re- 
pie . oth 
ee 
? . . . . . . 
If we suppose their specific magnetisms to be inversely pro- 
portioned to the disturbance of their specific gravities, we have, 
assuming the specific magnetism of iron as the unit, 
t * 4318 > 307 2 
a value which is intermediate between those given by MM. 
_ Becquerel (giz) and Pliicker (s$7)!” This result would be 
I know of no physicist who has given so lucid a theoretical 
explanation of the various magnetic perturbations, as the illus- 
trious Fullerian Professor, and as his hypotheses appear to me 
still more satisfactory when viewed in connection with the gravi- 
ced. . 
dences of the identity of helices and magnets (2239); the exist- 
2578); the dence of the magnetic motions of 
£919); the probable dependenc | 
fluids upon their mass and density (2768, 2769, 2781, 2863) ; the 
gee.) Ts on : * enn : 2 
-o bh iar vasay Fave pis se to the Te of benno for iron, in 
®“ Artizan,” to. t on the dil 
sabe ary - 981). According to these data, the 
of oxygen would be between 3}, and cg eee 
