Gl | ’ « * Bere on tho averasto. activity a «| - a 7 ne In other worcs, whieh dis apravontly moving im st “44a dhe op ans - “4 “ fas tnozss is aw! this ~ as tho current Stroama, 4% 4 “4 i viceosnrone oO A ee Some a war oo 4 we 8 te t. ast Lon eye wyen Be nag G2 it at losst- has made the tuzgn into the Javanese curroat, but Gl . it has not yat reonened the United Svat. DR. DIORA roy . « . : Shank you very mush, he Those tg , a two poesentarioenas ara now Goen for cdiscevssacn, BX. LEVDBSNG: DR. HARLEY: Was there any inddcaticn of the cepth? fo an semoewhat ef a srade avsut that. Covdencat thet ws had, With this ov almest any acscsuntiag Gandrmmont, our acccuatensers Were very nich, dust env standard Coviation to counting alene may have been as hich es 2550. terns of large numbers of those (indicating). FF am spoaking in If you take a Jong proltilo andaverare tint cut, you roaline that thet coos not do much and you will got a fadriy nice falloff with a logosriphic cetivity, aad you got scovt of a tail, and this is cowa at a vory low activity where you would get one of those averages Wnich is quite deiinite. In other words, I belicsve there is semo activity betwvoon the thermocline and boloy tho osdduary mised laver, rathor lew and only twice 660 meters, It is Gid wo mako moasurenents mucn below Below 6609 meters covn--and thove are several cascs of several bottles--the activity was newtliciblic, but 600 maters was d3finitely below ths thernocline. FROU THE FLOOR: wouldn't bo below th ££ contft know the Pacizic very well, Y rmanent tharmeslina, ft