Show U IUS E ERUPTION ND EA TH Scientists Unwilling to Advance Arguments Tending to Con Connect Connect neot the Two SHOCK DUE TO SLIPPING ROCK of O IJ I I tig An 1 Abundant nt Through i oI California Washington 1 The Cation of ot O the thc lu tn Ian Ban Fran Fan rl cO to tho of ot t J thc ut unions d nl ls In IU this city lI today tola Xon ne Of ot f them s u Milling to tu ml ull anre ance flY any nn would lend lendt lell t to conn t OlO 1110 with the th olli other r In 11 fact th of ot the tho geological golo 1111 sur Mur WI far that heio van no III whatever them A OPINION ro c H II of f geol i y of t tho tI I IUt 1111 11 The I Frap en dl me meto due die to 10 thc th II of ot the Iho e to t to tu con cn oi 11 t th earth cu rth Thy They have Ii a vi C m 11 hl Whatever to tin tho eruption rulon cf ol U u Tin rhe rii I lor r ut of the t ti en t h hm u h m lit Iut I a ii I molten In Iii tin t IP I E Ion on ot OC Ih hut but If It you yiu 11 n no go godOwn dOwn a 1 of o Ii M 4 nr or II 70 it 71 I I PI the th rOd rock sire Ir practically In i H I 1 lit traIn rr tam the Hie pi 1 ensure on flu 01 toT top ot 01 I lm The net iut like u a I liquid they float to 10 t to foH nut BulL when yon rOi nI mine ii I me neat 1 I 11 er fr the Ih tiro siro r hard bird I brittle brt It le the t m i m of 11 n n ui I pint part of 01 the t e crust oun t along ulong the Jim of or n nI orfa fault fa t will Von 01 ohI the I attended tho the luck In mu 11 Han HUl Trail cl fo Tho rho ho old it anti take tuk It io I n A hole I t IA i a body hud and IK IN II In Ina tl a R state t tc of or 0 constantly I hen dip down there hun hll to hI I ne an In of ot the tho Ilk the tie lp up P ot of Ice Ico on ona of or the a rIver u 1 I lt o toCk block blo k to each other Thin la m evident evidently b ly what hat has haA II Just ju t haill on t ti Pa Pacific Il coart mOl IUKA an ProC W NV Ills 11 Moore 1011 chief of ot the thetta neather tta her bureau hureau ICI It II 11 hl hil pIn on thai thit thero Ihl no flO 10 relationship between the th eruption or of Ve e c ful s und imd the thc San Sai co disturb disturbance ance R VI m i Vi Director Wolcott olot of or the lurvey une aid ald all that when iuen the tho nen of ot fan Francisco Frand cn disturbance dl reached bis gk Ih th tilA very 1 naturally aroe ar ot re HS us lS to lu whether there might not nol be he tome pome ore connection between them thuei and the t eruption hut but bo he do rt dc that them li fui I not nut the least huAI I at 01 any 11 connection between hH the Iho thet t two IwO o The Thc Vesuvius Y he hn added li I 3 i purely volcanic hut but the P al co If I h much like bike that of or S f In II 1886 that In is I It I occurred In lit II u II district that Is Ismor moro mor or 01 J 9 faulted and II Ban Sau Ial s A In region that has hag hUI been heen visited IId by h hockl most mOlt of tiC lt them WH vre very vet cr minute being hell I only nb on 01 the thc el but the roe rec erds of 20 O years show Hios hol ninny of 01 shocks cach year al nt at Sun Sil The of or geologically recent faulting ate ore extremely ec t reu through out the tho greater part of Call Cali California fornia forni and an especially the Iho western wc tern see sec section tion ton ti n In thc th count coast range ranc curl It IH I mob ably toly that most moM If It not till all 11 of nl tho the earth earthquakes earthquakes earthquakes quakes which visit It that region are arc the moi mol or los I of ot extensive move along ulong fault planes HOME KOMU OMi London Lonion April Apri 19 The calamity which hit ht ha befallen belal n th thu people of 01 San Cisco cIco tCO In Ilu Interest nit nil al other In the thc newspapers here this morning All 1 hl tho the papers publish h long Ions irnI M descrIbIng the thc terri tern M tm He l of ot the earthquake te together d of the tha th city Its It I beauty Ho tc and Interviews with San Ian Fran residents In London In fact tact anything an calculated to bring homo home to th the reader n a realization of ot the impendent lu nature of or the tM disaster Fol Fo FollowIng lowIng losing tn 80 soon HOOD upon the eruption of ot Ml sit Vesuvius unit tho the earthquake hokR on the Island of or Formosa the thc Is II I debated whether Is II any an connection between these vents ernt Few Fr hOVe have flu yet ot Ct pressed un an opinion on the subject PROP JOHN JOI MILNE lLE Prof Irot John Milne 1 I 1 t whose who o seismic ob Db n ut at on the thc Isle of 01 Wight r u ii 1 disturbance ut lit lt IM tO I I la afternoon h tinie U es th the opinion that the Ihn earth arth qu kc had no connection whatever the eruption n THINKS TIrs VESUVIUS THE TI CAUSE CAUSEE CE E W superintendent Ku of tho the Greenwich observatory on al the contrary I that In all probability It was wa ni IS a n con of 01 tho activity of or ort oft tt t t ulus WhOsO Wh A eruption a a f severe wave 0 movement through hp the Ihl t of ot lie earth Iril Ho lie Jo considers ronAld rs however how r that there theio thelo IB Is I not tent Int reason I to 10 connect these with Wih displays or of solar activity JIM aM comments on the tho th comparatIve lly Ity II of or earthquakes In lii 11 tho the United States jr lIson ut another lc export valuable re ro record cord but could no ho connection u I the e Ve eU lu und anti UI San Fran two CIlO All thi 1 the tho morning print pint editorials the deeply sympathizing with wIh 1 p people ople the victims of or the tho f amity The Thc Standard Mya MI Wt s e 4 nie well wel convinced that there thera 11 I not bo h lacking In Iii II thin luau land so Imp hup fly rily 1 removed from frol these sudden an nn Impulse to succor our al citizens en In I n a distress d |