152 



THE SAYKE OBSKUV ATORY. 



Applying these corrections to the values of the latitudes given on page 150, we 

 obtain the final results, as follows: 



Final Values of Latitude — All Corrections Applied. 



Weighted Mean Date. 



1 1894 



2 



3 



4 



5 



6 



7 



8 





 10 

 1.1 

 12 

 13 

 14 

 15 

 16 



17 1895 

 18 

 10 

 20 

 21 

 22 

 23 

 24 

 25 



Feb. 4 



Feb. 25 



Mar. 13 



Apl. 



Apl. 



May 10 



June (5 



June 25 



July 10 



Aug. 



Sep. 



Oct. 



Nov. 



Nov. 



Dec. 



9 



25 



18 

 8 



14 

 4 



21 

 4 



!><•<■. 29 



Jan. 

 Jan. 



Mar. 



Apl. 



Apl. 



May 



June 



July 21 



Aug. 12 



18 

 31 

 17 

 15 

 27 

 20 

 13 



I 



No. 



II 



No. 



in 



No. 



IV 



No. 



3.070 



100 



3.199 



31 











3.110 



40 



3.200 



34 











3.197 



71 



3.190 

 3.170 

 3.103 



40 

 49 

 51 















2.989 



48 



8.051 



29 











3.020 



80 



2.985 



42 











2.907 



59 



2.925 



48 















3.028 



59 



8.014 



02 











2.959 



61 



2.878 



71 











2.982 



60 



3.010 



70 



8.098 



57 











3.142 



110 



3.144 



00 











3.181 



66 



3.217 



37 











8.157 



94 



8.208 



89 











3.182 



00 



3.214 



58 















8.194 



57 















3.302 



32 



3.200 



25 











3.200 



72 



3.122 

 3.276 

 8.158 



08 

 53 

 58 







• 









3.029 



91 



3.033 



77 











3.003 



08 



8.044 



44 















2.910 



103 



2.917 



110 











2.908 



78 



2.922 



59 





035 





751 





590 





708 



Mean 



3.137 

 3.155 

 3.190 

 3170 

 3.103 

 3.020 

 2.977 

 2.946 

 3.021 

 2.918 

 2.999 

 8.117 

 8.182 

 3.187 

 8.182 

 3.214 

 8.194 

 3.281 

 3.194 

 8.276 

 8.169 

 3.031 

 3.024 

 2.914 

 2.915 



The folded sheet which follows gives the individual values of the seconds of Latitude, 

 all corrections and reductions having been applied. 



The probable error of a single determination has been derived from these final values, 

 and therefore includes that part due to the adjusted declinations as well as that of obser- 

 vation. 



The results are as follows: 



For Group I r 0".218 from 685 residuals 

 II .212 751 



III .189 590 



IV .193 708 



i 



Mean 



r=0".203 2690 whole uumber of latitude determinations 



