| Show QUAKE INSULT IN SALT HE LAKE THREE DISTINCT SHOCKS ARE FELT BUT DAMAGE DONE IS VERY SLIGHT TremP lor causs caus cau s terror among reel real dents man of whom abush for the open when buildings begin to sway and plastering fall from ceilings salt lae tate city three distinct earthquake shocks were felt la in this city sunday morning one of f which was aas of two minute minutes and ten second seconds and of unusual fa nten elty sway lir bull buildings dIngs ani a veri able panic aa 14 the residents when the plastering was shaken from the ceilings of many homes and brie bric a br brae c was scattered scat ered about the floors cala chim neye on several buildings toppled over but aside from tho the scare to tho the residents the property damage was trifling the first shock cam came at 7 28 a m and was of 2 minutes 10 second duration the second at lasting 20 seconds and the third shock lasting 20 second camo came at 1126 too center of tho the disturbance was salt lake take other sections of the state suffered ered but little provo dingham bingham ogden and other cities report almost no damage salt lakes panic while it lasted was widespread hotel guests guest rushed frantically frantl caly from their rooms room und down stairs many being retrained by force from descending fire escapes the few sunday morning occupants of the big down town buildings dashed in terror into the streets blumberh Blum Slum beres bere fl in the residence districts rudely awakened by the first shock hastened hait ened out of doors according to the united opinion of all claiming knowledge of earth earthquakes quaLes there Is in no further danger the earth block Is quiet in a new lodging place dr fred J pack in charge of the at the university of utah lay ebat that the three earthquake shocks traveled from flom the northwest to the southeast and were entirely local in their nature never in the history of the cit city Y or at least since the seismograph was installed says dr pack has there been uch such a distinctly local shock 1 though bough such much shocks have bays been experienced elsewhere ite ito predicts p dicas that other shocks in this section are likely to follow but does not mot believe there Is any danger from the quakes |
