Meteorology . 



xxin. 





Earthquakes r 



eported in New Zealand durin 



g 1882. 







Place. 



H 



03 



o3 



1-5 



PA 



a 



S3 



CD 

 ft 



o 



S-l 



03 





3 



P 



1-3 



i-s 



CO 



3 

 60 



<! 



CD 



a 



CD 



P< 

 CD 



^4 



CD 

 O 



o 



O 



CD (B 



a -1 



> o 



O CD 



"3 

 o 

 H 



Tauranga . . 





1* 























1 



G-isbome . . 





1* 



















25 







2 



Napier 

 Hawera 





1* 

 1* 



24 



6t 















25* 





1 ' ' 



3 

 2 



Opunake . . 

 Patea 









6t 









24* 













1 

 1 



Marton 





i* 

























1 



Carterton . . 





i" 



















20* 







2 



Wanganui ] 









6t 









24* 



26* 













3 



Wellington j 



Normanby . . 

 Nelson 



9,17 



1*,20 

 21 





6*, 16 



14,15 



6,11 



24,25 







20 



18, 



25* .. 



16 





i* 





6* 

 6* 





















1 



2 



Blenheim . . 









6* 



15 



















2 



Christchurch 



7,io 



i* 



22 



6* 





















5 



Ashburton . . 





l 

























1 



Lincoln 





i 



22 



6" 





















3 



Hokitika . . 





l 











.1 . . 













1 



Oamaru 

















15 













1 



Kumara 

















20* 













1 



Seafield 



















31* 











1 



Kangiora . . 

 Springfield 

 Dunedin . . 











5* 









20 



25 



20 







1 

 1 

 2 



Greymouth 

 Queenstown 





i* 





4* 





















1 



1 



The figures denote the days of the month on which one or more shocks were felt. Those 

 with an asterisk affixed were described as smart, those with a dagger as severe shocks. 

 The remainder were only slight tremors, and no doubt escaped record at most stations, 

 there being no instrumental means employed for their detection. These tables are 

 therefore not reliable so far as indicating the geographical distribution of the shocks. 



