Show D OF r DIS in t eon tion to the N ti nl 1191 fd delIll of sciences cal gapin IBM li I 1 D 1 ilton titi t iti a 1 calculation ol 01 tl 11 e depal file f lie f n at llo kentei of ui fic li hell ali i ats it at the diblanca di blance of 12 little dow eplow the earth 9 sui face ibe I 1 be ciatu 1 liann I I 1 I 1 n by I 1 1 beit I eit millet of tile at which III I 1 llie tile neapolitan e of or IM 1807 or gina aed wa tle le clist toto ta i pi pl I 1 on tl tie e tl aa that the tile en ell 11 li wave radiates in ill lines aloni ti tie 0 on orl gin ind nil hero beret at diffrient angles of e ner nerg genc e tie mallet found tl it it tt lints dhawn parallel piral p lel to these antl anklow ifopo if wo ejected mould antei act each other at I 1 s mean depth of about fhe file miles tl it a 9 sul lee I 1 lion I 1 0 u sei set ic and omlei oil ei indications the lie mean depth of ll 11 e I 1 loko hami eat eairl tt quake of 1860 w fis As calculated to have bate leen 1 een about 1 miles hile enuch pinkei ol 01 centrum have been a signed to some earthquake the tile accuracy of it e calca lations han to I 1 ien en doubtful caplain buttons new nd of I 1 kill the depth of tho the focal carity at charles ton gives thel afore a most I 1 result but his conclusion til i in I 1 ir lr conj mon with the ob observation obier er of or mallet it earthquakes which I 1 lae ao a verv cicat atea ot of ennoble en nible bible disturbance haic we a also abo a deiy deep facet |