| Show 40 VOLCANOES AND earthquakes ill atlon lt lon to tile violent efforts binl ill con of tile majority or of the I 1 be V are found aivar or tit nt avast arii l sit lit no vely g rat 1001 t loin tile ili though vol volca mi norf X or of later idler 11 nes tire nrc li mittI to isiom very different from those thoc III winch lo lutille action used train li 0 in ile for or iu lui lante in fit america wo iva have biily 4 on 1 I I 1 the pacific side and ami tile the auden furnish sev sc venil erad mexico central adivi ica evs man vi vi canden andi an tar far hiorth ws us baska no 0 fiad icv i M alf FN V wl M I 1 uc i a 7 41 r 11 birtil OF A VOU VOL ilao mount elias I 1 leits there ire plenty of 0 P volcano esin kirupa 0 pt the active bents nuj and about the red sea 1 l anil and I 1 ahr he caspian iol and ven even c io in tile ilia central clini if there are arc mr front froni critzer the cilc s on tit clr other hand liti ihl are all ol and asia it ill with apeci bieni so MI tile feudi ti aiji to provi prove thit that ahert ol inic ivi nain are apparent the 1 ia i a I had been or now 1 is I beatr at hand there tire about 1 wl ol 01 ca cailles ulles at lit in activity vity four ILI ii campo eleven in fit Ice fanI and jan liml in 10 asit asil ninety three in in C a I 1 axenty rix forty hix in ACL nd the aleutian isar s seven in central Ain erict i and nil the antilles Antil lra in ill south allier lea ica thirty one and twenty four iland s ith volcanic vole anic 4 largely developed eliere may lr ile ciany more resting re volcanoes are open iani or rents rent which sith the melted rock within tha var anil tin the form of voi cancle 3 14 1 4 owing to the i of ol earlic matter As A 3 s it lilli from the opening n billed C tite crater crier the bokano builds ita AS own owl hill and inside tho the crater we flud cones from which team iune issue iu ne These coneS the cone fire are the points of issue of immature ing ina it up pit whole the iglai of aril eption tire much abo usually cicur it couple of days mal e tile aillinn out outbreak break first marike ap bippen petrIt perhaps and the escape of gases arises by daltit clunies H occur new ew are continually in ID pro cm i of fornia fornication tion and ohp alie se violent elloa of kattire grive rim ri M earthquakes to which are tile mot most destructive of iia concu comil ision L tin the slow subsidence end i gradual of tile had I 1 is still going on oil but bill we are frequently startled ly by tile the account of a rupture of the ground round or the ion of it a portion of a city 1 J n re t i earthquake ES the motion of tile the earthquake is yaw ner ally in ili a direct fill line nod arid undulating sometimes what tire termed benned I 1 vertical erlic nl bocas anse find and detroy destroy solidly built cali fils i Mount tini amt have been overturn overturned ed by earthquake shocks and trees have hare been tWILe twisted gl around sometimes the ground i into enor moin lasures tile sea ig liari luto lulo great cruitt waves anil and encroach eit upon tile tin fault laud and when Is lien tile ibe hei hea receded I 1 ibe be re rece celLion dimou of the water n followed ed liy by a more terrible wave sweeping all before it firth I 1 irell lii often occur lar away r frontu volcanoes and without any in N isible c chull LIOU with vOil holmun atile |
