| Show TWO RINDS OF QUAKES It Si IH 11 In lets Get Are Arp rl nf of anti and Ruled with special reference to Ie time the th Ort Great fault belt plane In anti Its It relations to tn ll formed the Ih theme them of or sits fin I dolts by hy Dr Or J 1 Pac Pak k of oC time the nl 11 of Ir the Ihl Itah toh So Ho Society o ebdy of or Engineers I lint 1111 night Dr Ur Pack Paek In part pan P rt said There are lire two kinds of distinct earthquake the t and the he vol volcanic 01 canic The Tho earthquakes are a thone with which we ire 0 In this rrt i of or the tho country countr have to contend In the kind where lo slip eUI I Hie tim disturbance In is felt r lt with equal se Itt severity verity Int In many distant Parts part At AI Ban Sari In 1110 the tIm great dl dIsaster ister wan wn Allied by It blocks block of slipping upon each Ih other In ins a R hurl direction rise horizontal lvis 10 20 feet and the vertical displacement was va but tut tutu butU u few f Inches Th The great ut fault plane ex tX x tends front from 11 on thus south to to Col al inton on the north In III traversing tills this It II Nephi 11 IU Fork Provo ruin cuts m r Nfl 1111 the mouth of or the th Cottonwood i lo to the buck back of ur Fort Douglas I ern Dry Ur behind thin the toner on all the thu th hill bill tile tho Ih Warm Spring HecKH s lint Hat thence north to The Ph on May MI 23 2 wn caused by u et sill of o the surface or of about of tin 11 moth Inch In of ti tha Ih future I would stimuli Willi Buy Sti that wo We are arc very vory or 11 ft t e p TIme The h WR ia Ritch arc zil n no iii vv very leery Ir old and when they IhlY have hiatt ha o n od to 10 grow amine we see 11 have no more inUre If hi anything should happen f II so that the time fault would b h luau us II sorest nn imme 30 fett feI there would Omit not b be a it house lug lag In the tit town teflon I do tin not believe hull how or that Ihal We ItO arO arb In lii any of or a 4 disaster lor |