/'.! ' 



m.y. 



Mowed iii 



inn.l- 



■ Monte '■ 



itru in Kurupe 

 ■ml. near I.al, 

 in Nurtli A 

 IX In lli'- pa pel ■ hi ' rth- 



quaki proved that the major- 



ity pasw (1 aim t-le which 



• ith 

 11 the 



•nl mid center of 

 land, giving rise to the mors 



tland, which some- 

 ictirred almost daily for 



rcle, which, pawing 



izai- 

 iro. in Ne« Zealand, to the evei active 

 in (lie ('ape \ I 



and, 

 ig the north 

 I south counties of 

 near Uornliolen 

 where ft laU number of ■Nairn. 

 if the numb) 



while 



\ i 



■iml chiefly along I'm 



continental bell which mn- paral- 

 kppalachians, and 

 livity in I' 



igraphy ol that 

 chain, and still giving 

 ! 

 Ha. ill. .in. < '.linn 

 which like Com] 



! 



this 

 mtinued -m on thi 



iting 



2 i- the mate of 

 v i 



at the equator, trending north 

 - .. 1 trends north 

 STo. S mark* the vi 

 lifornia, ol the Sierra Nevada 

 and ol Alaska, as well .-i- the eartb- 

 lalifornia. 

 portion »' ioh paasea through 

 America, ol th ircle conatitu- 



ling the Asiatic eastern trend and 



ing the bell of lim 

 in Kumtchatka, Japan, <£c. In North 

 ica it Follows bain 



of lakes from • - Man- 



and tin- center of the continent 

 Superior ; thence the 

 belt he eai thquake region in 



n ■ i ili Madrid and other portion 

 tbr Mi-- illey disturbed in 



1811-12 in ili- W • -■ I udii - ii . 

 belw< - Domingo, In 



South America il 



bich was desolate d al abon 

 period N Madrid, 



- nth Amei i. a t" ili- 

 portion u ! Brazil. I he mate 



to Al stern continental I 



and iruporlani seismic bell 



which, ail. i- its circuil from vol 

 .linn) ami from th 

 •i|.h aved ishi - with ilie 



itOI ill. I" 1 l.-.U.i i 



:ii our Y- 



gion .in! running in arly | 

 the earth's n 



