( l-u ) 



T A 1> 1. K U. 

 Kcv^nlls for iho oiMTociion o\' Ocvumüu'^ \aluo tor tho oastorn loim-i- 



tiuio of Si. no!u>-l\oniuon. obtained from ocouliaiioiis. usini;- 

 disapiHwraiu'OS and roapjuwranoos indisiincily. 



• Tbese ooeultatioiis have beeu calculated aft<?r Be«;>iu.'j iuc;hod. The luodincation of this 

 method, to which I referred in the tbotnote of p. 605 of my previous paper, may be fouud, as I 

 perceive :Uters\-a.n.ls_, in CHAvrKXET, 1 u. 556, iu § 344. it consists iu this that the coordinates .r, v, :, 

 ^, n and ^ are nor computed from hour to hour but only tor the iustaut of tho ocoultation. the 

 Greenwich time of which is found by means of au assumed 'value of the loncitiide- 

 The diöerences between these results and those af^er mv method \ve.r«: 



It appears that all the differences remain below one second of time. 



