Show Dr I x James ames E Talmage Tells Tel s i Of Origin of Earthquakes n t j ji a i ylia I Ili T a I ECI CI ri D 1 Li U Ut t 1 ti sI 1518 II 5 I Iv I v 1 r y i l ls s 0 c h S 5 r c o jr t MAP OF EARTHQUAKE HORROR I sketch her the earthquake Ines or of anti and CalAbria T Me have bead h nr many e of the most lWe prior to tINt the t one happened hi the thear ar 1 IJ troU quakes d the In 1 1106 and 0 In lit Titers MV have tiro aMo beep bee The T bott m of Ute the between Ital and Mil h been low M In rather nU mu ft 1 iI S and I le still The 01 dratted lines In lb the map to tak ks In fn the eruct N of Ute We earth In I fd tl the of the LIpari The Th dotted circular a are r to a L aril a lh ter source of DC the earthquakes ot of 1905 and nd The Thc colt no Etna I Is at tIr Ih and ti uvee II ion oI t the radial lh d d f the yea yeal tOO 1901 will wll b I rod In a as a time of week i Detail ot of this thle In the of u I III disaster southern ItalY and th the isle ot of Sicily wen authoritatively re here hR not no 10 uch account a ae have h b EI 1 r the tho tell a taI tab taIr without III n th n r let I i lila 1111 horror horN annals 1 of f that tm on the t un unIt a ars It ap off olt roast of 01 ot of the island I ty nog the th end tr t I of If hont which i tI le ot f On Onh the thO peninsula of I h In III the h severe u k wa 1 1 II I buildings in all the towns I tile area of x but IU as I Is usual with sea Bea Beat by earthquakes at t r I th h after cl of tile lute quake WI wet 1 d than the alt of I I lit own I rite Itself The I 1 e UI a tidal nurr in Ihs Ih dh swept up UI tilt the thet HI t between and I land nd ul the adjacent bison erat out ut from the scene ne of III I lit numbs ot of lives lost And oll the tt iI r th II express f dull ha Iii the count will show number ot Of fatalities Earth th iI c H by fires ll due lue to the of the buildings and amt Ih great rolled In to the work of de 11 tI II f ft It t lIlal that the th dread UI r old u Interest and CLUdy k ss o I t I clI saw nature ot of earth qu k II tn M general Tim The enn eat Is IH to any yin 10 I I II of of r th the artha crust fee 61 of r the kind a are known knowli I tn 11 I ul A Any Y movement lIt of lor 11 St S gain t II r i the h cUlt upon adjoining It I ks III It II a wave waft which Is pr us II a wave 1 of tl with h lIr dr anal extent extant of vibration Ih the depth and or I to I Broadly II III ma may be c classed loJ t In III Use two an follows follow LI I Ii duO due tl to Ii a et f tl rv upon 1 re ren n It g b i Ih known to po Lal is tift d I due to vI nl I to an 1111 t III within a loaIl amail Iud and al n time at ata depth of nul 1111 s L I rant Ih Ih the i tI t x ot Of the first ell t to found u Ih the an earth arth Ik r O ter th 1 nee ut of e hl hi h dt t b r I Is still painfully trash earth nt In III that c Cs se lO was waster ter h of I a Inn of C the coast 01 run UI tI the being traceable for rater tut IiII II a hundred mile ml lr lI a II Its di I I Ih the of the Ibe range an ll nn In of t ty was wa waI sr I Inns I rat r life Ite In rat a nd earthquake e a 01 I not I as a with the OJ dad rl nta in III many other instances ad wic Ar x yr N y S ry I till JAILS JAlES 1 E TI 1 ot of this class claM are ano naturally of and growing mountain ranges A As I le now vet very gen emU undo mountain du not attain their full 1111 growth by a sin 1111 irk gle uplift or fold on the tho contrary they are lit It slow grot at lo In Int t ads U mesa II UI ward producing a fault tault along the plane ot of fracture Such Ii a movement result resulting In ing III hl a vertical ot of but buta a 11 feo few feel thong long miles or of tin the rang generate e before which toe the A beet ot of manmade structures my may fall as a 1 a house ot of card cant III It th the current ot of B a child childs breath Earthquakes ke ot of the second class va A those du due to volcanic are or of 11 of I vol volcanic canic an anu a as all tIe ol 01 are I on relatively small mall islands or r un on the In III of continent sueh fluh earthquakes originate beneath or orIn orIn In 1 lose proximity to the oceans TI 11 If re is es a very ery clue roll I Iti ti bt between earthquakes and volca II s In III the ot of vol Ct fus shocks are 0 of t tre quent urN and many Instances ot of record show a f atlon of Hr earth hacks bock holl the volcano breaks blk Into eruption more vigorous than usual On tho other hand hund after atter a violent arth movement vown volcanoes In the re lIon glun mil may qUIt quiet 01 down to vel very Bantle no C or may a to 10 erupt In III the clan ot of earthquakes earthquake It is often otten pu to In beat with ap p accuracy t the point on the eurac vertically this the locUlI u or place of nt actual origin The Tho subterranean lIn 1 focus le g nellIy called tile the tantrum and the point vertically aho above Itt the ept n trum It If the lw disturbance occur beneath th this acorn poor donI the will be that flow floo In caw cw 1 a huge hu WI will be gen generated by rl and U lub IdeoN of the bottom and this Ihl waft will III 1 outward ul ard front tb the with tout torl upon all hon within Its Ib seen aNn III u power I Much q I t e av e Is III not d r h Its Ill In its l through w hll I lb th n 0 et 1 It I it of mall 11 It If th ho earthquake force I UM hr b tb the arcs Inell ot of aA band I r on th hn har ot of a lit the sea will III I ht lIal and Ind grout t waves will III be a generated ed I Among 11 Ih the swat striking I rs I of n b by yran lIeLl VI the liar 11 I Ic It Tn in J 1115 tb rhy I of f sons d dr T earth oh Shu k raft i it ere t n of III ter largest to In Ih ft city crUe 1 Aft the hl rt tl h had IY wU f II a rat tally Yu t feet d In cud It l d 11 II the that J i shirt 1 h 11 l i Ir ll th At 11 It n te it 01 us 1 so u rn far end of a In 1 he I lit U Jg ury alit n N ot of the WI West ladle ladlee I e S F Ili III Vern lit III I L ii a hour r II IU of Ilia 1111 Aare n Ih the w was by b 1 a a 1 pra a sting till a 11 of io 11 feet A day II Ihs Wu the Ih curet let iii les iF 0 H SIl ut III Iii the k 1 it by Ui HI ea a air In Ih the to In with tb the hIM great will Iw be known later It I that I I Iha h smaller talan islands off n of have bran changed II as Iu III stair t II 1 one ull ii I tl lit Ih the I 0 IS 11 hire 1 01 l us Ii th Iha II lit ut Tiers lal island kar hu Ilia 1541 mull III Ii Ie ve verso and In th Iha II 1 Ii 1 Itt of of III Ihs It I j the loot southern of t the group is IN and andI I this hll bal because ot of Its activity In times hM has given the name vol aJo IIO now applied to all any phenomena ena n ur or the kind Student of the will recall VIrgil allusions to the land Island l then known u as lUna liters In which tyre poet I It Its subterranean caverns as th the workshop 0 of Vulcan the god ot lit fire Dryden trans tran translation lation lallon lit of th the runs as follows Sacred to Vulcan an tale isle talet t there hl lay Betwixt coasts and Hald high on smoking rocks and below I n hollow caves caVeR the Urea or of liana ona gill glow The Cyclops here their heavy ham barn men merre deal Loud And ot of tor tormented steel Are heard around the boiling waters roar And Aud smoky through fuming turrets soar Une Un or the 1 isles 1 of the thelI lI group gawp Iti III t a volcano kang that has hall beets been lb In almost almot continuous eruption for fM maR nutty 0 of years tIU I IIII In III 1788 1781 hn Quiet for 11 s short 1 1100 laud and Immediately after Ida II lIttlon I a violent deru on Ue the adjoining mAin hand IlInd Mount l taw tho larga t volcano In Inthe inthe the Is III reported All as being be beIng Ing In j spasmodic eruption at the tho peas peasant rei ant ent time Ume No violent Is 18 lon hoax hoaxed ed for however as aa th the eat It has hall probably afforded present te re relIt lIt to lh the foree rat t tile the locality It If however lh the relict Is b not later iia wU wll follow or the volcanoes of tie the re glen will increase their activity and wl provide outlets for the Igneous eon en within JE In III the gloat I loer of life incident lent to this most recent fluent ot of mouth Co forces In the 1 nn the horror I Is somewhat mud l Oed ned it If not b by the splendid response to 10 the cry of 01 the survivors National and ot of tate state are aloe forgotten and th the hand of every stun nation is II offering each wh aid lild as It call give Iv Battleships or ar hastening to 10 th the aen of t oft ll C of t mercy bearing ng supplies for the stricken people With cha uc said own great nation I is among the lead Iad era en in III the work ot of TI II a Iret Drel ty good family to which W we belon belong this great t human family ot of ours our JAM E TALMAGE |