Show geological CHANGES AT SALT mr G a ac coi dint to science riven to the of silt like oil alio piola bailit s do tie slow and baill con of the i in ho jasm I 1 alons it fiat turis alie earths crust on onu side being and tilted into dountain noun tain altitude dy in up that es completion ami distortion in alio rock ams until alio llio can no lo conr nr ba lorna ind mutt ie riv lad is a flippin blip pin ot one wall of alio ciuro on the oilier lai to ind tins is felt a an lien e a lone period winch tue n g sed anili a shock canned in owen a billiy alonar alie etstein bi e of the deaia in 1872 when a nip five to twenty act liike in 1 doity mits ony as product J scalp thirty or forty beit hiah n known along alie foot offin vas th south ot bill lake an cirp ofin il ir origin nave en found it alio ot ann ofalie gasn 11 chedie of lien for motion is not known ant it must le alicy still so little worn way V they aio arch and ol 01 modem 13 pi lafity aiom ikes foi ayes to toine a ions lime is i foi tl P accumulation of strain to bauo i slipping of one wall of the liucc on the oter condei cly mi hen ali y old and vorn doivo ali beak b eak ap str ean now bo almost ind in on tl quake inac be dt an tinn cic it balt inke for continuous a iri the fault chip alons the be ot the no il nt near the city ho arm si lines to emigration cinon they have not been found ind lie i of then is that i cay loep lia eap td ine thur lot leneal in hi penol tl baith train h is 1 aci nci cosine some di it ft ill arc fr action lift the a few ket and re e or calo the ci tairo pho of often s valk ame |