| Show earthquakes frequently TI I 1 os e strictly local in ili nature have been recorded anthe on the ge rlaph upon so KO many mamo lial er t out clit occasions that lint tile lie pepo voile to look alp ilp aicia tw tile r U as a place of 0 pel disturbance the aliu quake ia A londay dIV night was fw cording to id the bel ment by a shifting or oc UK tit praza filliat piano north or tile ain city Ws linvs it 11 differ elit theory aeu wr att liuio ilav he in ill inesti orr ama acabi se others ot liers have beell made by kell li nt lit the th sam arii Illo graph the hie hourn liotis N fa and i p lit in tini is is based upon sound alad huion evidence lir C when lian one sees tile figur ft f T it soled shoe in ill tit alitt 44 leading bradin arillo 1 alio inn heinn adma dma ww olle is ally led to till alir collell ision that ir wn cn hits been mailing ra side it certainly harv burat it mistake or r some Kf olo d qa 4 dent and not liot it fault eliat produced tit aliu m record of nr lit last it Al oliday 1 the is always air ur ailing 11 ins order it il is hard d to believe 11 ts SS it 1 IL A 1 ill D I 1 F it 11 S G K 1 bmw be deceived liy by it a mm mere tion of the or of araz mid and strain to it a huge bvrke ir cement it if wis we havo failed ofir theory clear wf we addiw n m cavy will doimi stud etil ns t arnd e r 41 ill in neology geology ii bic ma ch roni elv |
