Laserfiche WebLink
~ ::r ~ :: r <br />•x <br />~?. .. • ~, <br />•;~ -. Since all quantities in this equation except for VHouse, Shot X <br />~ ~ .-. . <br />• ~ have been determined by seismic recording, the velocity at the. <br />i <br />.~ -~-'-~~r,~house can be directly calculated (Table 5). For calculations <br />,' , <br />- _. v <br />~^~++~'~"l~+r• based on GOL records it should be observed that the measured <br />!~ <br />.+''~~' •~~~",~, •~ amplitudes are very small and variations may not be representa- <br />~; j~.l <br />~.,~t",~.q.~tive of relative ground motion. None of the estimated velocities <br />n,•t+~for Deer Creek Canyon Quarry shots for the past year have ex- <br />^~~y~9''t~ceeded 0.50 in/sec at the Painter house or rock overhang above <br />_~ .. <br />~-.r <br />,~•~ <br />i ~~ <br />i ;' <br />i\ ~ <br />~__ ®.~ <br />~:. <br />yi 1;~ <br />~• <br />~~~~' <br />~'` ~~ <br />0~~ ~-~ <br />. ~I~ <br />~. `~~- <br />•~ ~ +',~ <br />~,~. ~'~ <br />,Lti ,' <br />o •~aa <br />a .~k ~~. <br />,, <br />24 <br /> <br />MlCROGEOI'HYSlCS <br />