— 230 — 
Applying this difference = 2.'4, we find the following 
deviations from the normal for D. 
M. civil T. AD M. civil T. AD 
of Grw. May 15th—May 13th of Grw. May 18th— May 13th 
4^ 15" a 0.34 6^45" a 0.76 
30 0.61 10 0. 76 
45 0. 61 15 0. 34 
5 0 0.51 30 — 0,09 
15 0.43 45 — 0. 40 
30 0. 42 sU — 0. 89 
45 0. 10 15 0 18 
6 0 0.41 30 1,89 
15 0. 59 45 SE MN 
30 0. 69 y. weg YO 
The curve which represents these deviations is to be found 
in the plate above the corresponding curve for Buitenzorg 
1871, but in a reversed position with regard to the latter curve, 
having easterly deviations downward, westerly upward. 
The resemblance of the two curves is obvious; exactly as 
in the case of the Buitenzorg-curve, a secundary maximum 
is reached at the time about totality, but the next minimum 
occurs at Karang-Sago one hour later than at Buitenzorg. 
The range from maximum to minimum being 0.'7, is the 
same for both curves. 
Horizontal Intensity. 
According to what has been said above, we may associate 
the large wave from 4^"— 7^ m. e. T. of Greenwich with the 
eclipse. ; 
It is easy to draw a curve parallel to the normal which 
might have been the course of the curve in case no eclipse 
should have occurred. It is represented in the plate by a 
dotted line, and the deviation of the real curve from the 
assumed undisturbed line, consists in an increase, in maximo 
9 7, chiefly during the first half of the eclipse, followed by 
IEE E N eg 
