﻿74 



95. June 21. 



There is also a record from Cordova at 7 16 '8, but as the duration is 8 hours, it suggests a tremor 

 storm. If it is assumed that the shock originated a few minutes before 7.43, and at no great distance from 

 Christchurch, the times of arrival for P3, as noted at the other stations, approximate to what would be 

 expected. It is, however, difficult to understand why records were not obtained at stations lying between 

 New Zealand and its antipodes. 



96. June 25. 



A disturbance was also noted at Strassburg at 13.24 by a Eebeur-Ehlert pendulum, and at 14.22 by a 

 Milne pendulum. In Taschkent there was a record at 13 27-7.* The time interval for M between the 

 "Discovery" and the English station lies between 71 and about 96 minutes. If the shock originated in 

 the Antarctic region, we should expect the interval to have been about 90 minutes (sec Nos. 91 and 95). 



Local 



origin. 



• This is in tlic Strassburg register for June, but not in the 'Russian Bulletin,' April to June, 1903. For June 24 in 

 the ' Bulletin ' there is a shock, recorded at Irknt.sk 13.6, Tasc-hkent 13 -5, Tiilis 13.8, which may correspond with a 

 record for Mauritius 13.49 with a maximum at 14.4. 



