5 tept atlered 2pth profile > by The soil > radio3 Site and Measurements of Low Level Radiation Measurements were made at three locations where gamma fandfor cosmic ray dose rates were unusually low in order to study our instrument response as well as for general interest. The results of these measurements are also given in Table V. The first location was an abandoned magnesite mine on The serpentine Red Mountain in Santa Clara County, Calif. 2ur aS soon nan soil, ly in the low a 2stimates 1 data ctright ratory etebt §-— -ing our “ry results 5 “* wall material exhibited almost no detectable gamma activity. Since the overhead cover was 430 feet of rock the dose rate ‘from w mesons was reduced to a negligible amount. A two outside from activity detectable hour spectrum showed the only of the detector itself to be from radon daughters in the air, resulting in a dose rate of less than 0.1 ur/hr. No inherent radioactivity sufficient to affect any of our field measurements waS apparent in any of our instruments. } Directly outside the mine the serpentine material was ‘also very low in natural gamma activity with the only ‘Significant gamma activity coming from deposited fission products. Thus this set of measurements was a useful jaddition to our lake data for our cosmic ray ionization study. =2rg of 5 2 sites [up made ir using The second location was at the open pit asbestos mine near Copperopolis, Calif., where measurements had been taken previously. The site where measurements were made during the trip was only recently excavated and thus was ave completely clear of fission product activity. not otassium the affecting activity of the ossible tive due itself was an excellent near sea level measurement in our cosmic ray ionizationstudy. * 7 for use : The third location was in a deep salt mine near Houston, aoe The major sources of activity in this mine were from pK in the salt and radon daughters in the air. The total dose rate measured was about 0.2 ur/hr. eer te orn The natural almost negligible and again the only significant terrestrial gamma activity was from radon daughters in the air. (See Figure 2) The total terrestrial gamma activity was estimated from the Spectrum to be less than 0.2 ur/hr and thus these data provided iderably, ration serpentine rock

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