﻿47 



18. ,l/>ril 2.- 



The last I'eeord probaljly refer.s to P3. Origin S. of New ZealiuKl. 



19. Jjjril 25. 



The disturbance probably originated in district D off the W. coast of South America at 22h. 50ra. 

 The large waves would reach the Antipodean region at the times sjiecifiod for the last two stations, 

 respectively 150° and 180° distant. 



