Show 4 0 MOVEMENTS orthe EARTH i I 1 L various disturbances to which the land lei la subject shore 11 marks I 1 I 1 awe e lire are to tl I 1 trank I 1 a k v of f I 1 1 c bill A of tit ahr io solid and laced iiii li ii r 1 I i of f ta l ai alir tit littin litin c or ir ellid roond ilia has arii riall rai lize in ill tie ile iiii ILI hn of clearl all 11 aleu ale le on OIL tin tile tiler other we ivl of water ing ai unstable hut but the history lii story of the earth and elie ie more careful of modern times have hav taught in ili that these ideas do not correctly corr cutly rupie sent tile qualities of tile lip laud land I 1 itar goatees of the globed globe 0 I 1 v ac corta M i feil willi one nil aher her tin the vincient shore mar on alic lie continent confine i atud the ile mena of elevation eleva tiou subi subsidence dence that lave been bec observed in historic times confirming their evidence show that the land and the lie ocean tire are continually changing a 0 their level 16 Is to one another nod and it ii lins ii is f further arther been biado nt by b y experiment as well as by a priori reasons reasoning I 1 11 that it is ii not the ocean t that I 1 lot changes but flip land and which till undergoes it e id alternative movements of elevation clestion and depres ion an ali earthquake shook is ia a i phenomenon nuni enon well adopted adapted to destroy the faith of piny an person who feels feel the mhd of lite earth and such lucli by the lie evidence is tile the effect for tile the time on all who ubo experience peri ence these shocks even the light pulsations which sometimes pass of alic united states occasion panic idill iiI excite a momentary impression that everything is falling over or sinking away while the more violent shocks tl that int ore are felt in earthquake infested countries produce indescribable terror and such catastrophes of lisbon and caracas prid and the more recent ones of ischia lilii and the straits of sunda to it a rl that lie alib reason for midi buch terrors is feal and that the continents contin eilLs aloo 0 litt ail not hotl e icalia the general gc LIA V vf of mid el L irth R ll movements the e marit aji b which these phenomena may be most conveniently ate aie vari vario qui uit so f fir 11 19 ts they aliey are now liow considered earthquakes or sudden vic violent alent af the ground 0 round enith tremors or minute move movements mentI which usually sll escape attention by tile hie suii linea of talc ir eulth pill adiong or movements which ire are overlooked on account of the length of their period and earth oscillations or movements a of long period and ili I 1 large arge amplitude like tile shit ting 1 0 of r levels of land masses which attract attention from their geological importance some of the these 0 O a movements ments only sonly decently lecent ly begun to attract attention cution they illey ar are all intimately allae I 1 Y assoni associated abed in their relee rance and t their 1 at oi origin I 1 0 in popular science |