Show ERUPTION AND EARTH Scientists Unwilling to Advance Arguments Tending to Con Cone Connect neot the Two SHOCK DUE TO SLIPPING ROCK of Iti Ft tilt An rl lit h I nut Hit Cul n Arh Ahll K 1 The relation o ot tile the In Hun uti uli Fran to the of or Vesuvius e formed forme 1 the subject of o t lon among llon tM In 10 this city c today lodd None of Ot them va willing to 10 ad advance 11 ai vance nc any an argument which would tend tent to connect one un with wih the Ih other In fad fact tac the of or the tho geological sur survey vey v t that there then WOK sas no relation shIp whatever between them HAVES lA ns OPINION fi C Ht 1 fl or of Ir ery of the geological survey Urve mild OCI TM Th San 81 Francisco disturbances dl OP ai due to 10 the tho Ile of or the surface rocks to o l to chained lon eonS Inside the tl th earth They Th lw have havo nn ni ni niI dlton I I whatever to 10 the II eruption ru P t Ion of et Vesuvius The Interior of the In IR I In Ia a I tute except In ta 11 tho the re rc reelon IC Ion glen of the th hut but If ir I you 11 tt BO go O down o n R of or M I 0 or ti I 70 iO miles the tho rocks rock f are practically In to 11 ft A 1 null state from th Ihl immense lr on n top of or thio They oct like u a I liquid and they float oal to In EI to U changed nut Hut when you 01 near nar nearer narPI er r the surface urtie where th thi strata are III hard PI and brittle the clipping of ut f a IL I port part Jar of r the crust the line or ora o o oa a mutt fault will gIve you ou JUKI jURl tho the ih t attended thu attack In 11 Hen Han HOI Frau The Tho old oh earth take tako It I UI n a ahot aa whole a hot hole Is I a n very ver er uneasy body bod tint and Inel In Is In to ton Ina a n Mate of nt If constantly con toll changing When the th foundations dip down clown has hs to 10 be I nn on adjustment of nr r the tho th e like the Ih breaking up or of Ice on ona onn ona a n river rl r 11 and n a readjustment l a of o the Ih bock blocks to 10 euth other ThIs Thil la Is II evident evidently ly h I what hat has Mi Just happened on 01 the Pa Pacific Je rOlt WOK PiOt A fIrM Vur II IIII Moore chief of or o the tho weather r bureau burell declared It I nc nf nu his hlA opinion pInIOn that there was wn 11 no 10 relationship between the eruption of ot Ve Vesuvius VeI I and tho the San Francisco CO In e DIRECTOR DUCOR Director Wolcott Volcott of or the survey saId aId that when tho ho 1011 of or the th thian San ian Francisco reached his fan office the question ery very naturally as es to 10 whether there thero might not be some ome connection I between them and Ild the recent Vesuvius eruption but he de tic declared re dared that there In Is not the least probability ability of any 01 an connection between bel the tho thelo two lo The he eruption lie he h IMd is 15 a fl purely pUr I volcanic but bUI the San ion Francisco Franeisco Francsco IH Is much like that of or Charleston S H 0 f In that In t Is II It II occurred In iii n a district that IH Is Ismore more 1011 or yr lusH less faulted und Bun tUI Is s In that has been visited I by I earthquake l shocks hocks hockl although mont of oC o oIhem them were vere very ery er minute being recorded d donl only on 01 the but bul the rec record I ord of ot 20 years al hol many of o theo shock each ench yau nt at lt San Sun Francisco The evidence of 01 geologically recent faulting Are arc tl extremely abundant through thru h out tho greater part of r Call till and especially the western ter sec tec section lec lion tion In the coast range mid and It IH Is 1 ably that most 1081 Ir If not nt nil 11 of or o the Ihl earth curth earthquakes quakes s which visit that region re lon are Irr tho th result more ur or 1 f of extensive I move ulong fault plane oMi I London Londen April 19 The calamity which ha has befallen tim tho people POlle of or Sun San Fran Frand d rl co ro In Intel Interest est all 11 other topics M In the here this morning All 1 II the papers publish long 1011 describing the tern tile hie effects or of the earthquake together with wih descriptions d of or the city cly It its beauty helu etc ele and Interviews with wih San Ian Fran rc In Ix In tact fact anything calculated to bring brinK home homo to the Hie English reader a realization of oC the stupendous nature n lUI of or the disaster Fol Following FollowIng lowing so o soon KOon upon tipon tho hl eruption of or orI Ml Mt I Vesuvius c and uund Ind tho earthquake Iho kH on In the Island of Formosa the ue lon In is II debated whether Is I any connection between these tent Few scientists have as ni yet et pr an opinion on en 11 the subject PROF JOHN MILNE Prof John Milne lIIne WhOM hosn seismic ob Y it at II on nn the Isle ilo of or Wight recorded re orre n a 1 disturbance at II 1 3 Wednesday nel I afternoon lI l h time tl the tita opinion that lIt Ih earth earthquake quake had no connection whatever WIth the volcanic eruption THINKS TUB 11 K V 81 of the Greenwich observatory on the tho contrary considers that In Iu all 11 probability It I Wil raa 1 a rt consequence of oC the tho activity of or Ml I Vesuvius whose eruption started Marled u a I savere wave 10 movement through time the crust ruH of o lImo Iho earth Ho lie Io however that Ihal there th II Is not reason connect to 10 these cata wih displays of or solar activity I and mi tin tho Iho comparative nor ril Ity Imy I of In lii the ihn Dr of ur another expert obtained valuable re ro reford ortis ford but mit could suggest no connection 11 the th Vesuvius Ve and San Fran Isen nc All 1 the tho morning newspapers leW print deeply Mep sympathizing with lh tha tho people Ind nd tl victims of or the calamity Tho Tha Standard says la 0 o ore are well el convinced that there m 1 not be lacking In this land so tO hap hop I rily Jl removed from these the c sudden lel ties In distress an Impulse to 10 succor our OUI citizens |