HOKIZONTAL INTENSITY (7/) 

 (* Value deduced from Vibration Of'y by assuming ]'ali 

 Oljservationß of the East PartA% 1S!}3. 



(39) 



"f M 1 



H^ 0.28844 

 ilcducliou to 1895.0= 950 



„ sPa level = 000_ 



H= 0.28854 

 Observations of the South Party, 1895. 



deduction to 



II-. 



1895.0. 

 sea level- 



0.28947 

 -437 

 000 



11= 0.28943 



26. KAMO. 



Seikaizinzya. (® i^ # JËt) 



DECLINATION (5) 



(^b ;ervation8 of the East Party, 1893 



8 = 5* 30M 



