Meteorology. xlv. 
Eartmquakes reported in New ZraLanp during 1883. 
x H ss : 
E p » A 3 
Place. z È aj a s 9189: 3 E : 
s a 2 a Q 51% Q 2 E 
28.3 1418/35/8 27|2/$/5| 3 5 
5 Fu 5 iqials |] 5 [4jan|¡oO|24/ A m 
aupo sa DAS ds Es A. qe is t 
Gisborne ee oe .. LJ LJ ee . .. 15+ ee .. .. LE ] 
atea va Dus sa s mila Pai i Du. [owl ge 1 
Wanganui = é sa ` .. è “pi ta | + Sa 1 3 
Wellington | .. | 5,14 | 21,28 te A ee ee 11 
Blenheim ..|. n Z vi sd BO bis pu 1 
iko oe LE 5* ee .. 24* LI ee . .. .. 3 
Christchurch | .. > de é #04 24 ; Sl rie e a ei 
Hokitika jovi is ys se | atiis we veda es 18 
Westport ..| .. dn A vous Ts oe Seo a 2 [eae T 
talea A 14 vi ii UST T a ee ea Pee RAR ) 
Balclutha ..| .. e x d 1. da FECE Es 18* 
nedin . a a x a 18 
Greymouth ; 22 . è È .. È 18* } 
Queenstown ` . Se 18* | 
Invercargill v x es uud. Dus en e dia be koat | 
Bluff e: up ia sa poa dos =» Ce ead ee bee 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. 
