de fish, 2 we do not have y because 42t would not drop off as as much short-lived material prosent. Actually, if we conDare this far enough downstrcan, in spite of the fact that the Plankton wiil bea mest racicactive the most vadioactive forn clese to ths plant, 43 wa so downs troan in tom Bonneville Dam, we are ant to find thet the fish. . . at P-32 are more radioactive than the Plankton forn ' fho turnever or general accumulation of radioactive t5 has been of particular interest ma, terisls on 2 long-term basis ny sorvoir here. haz to us in terns of the Me cNary Dan Resory a strean condition, flushed the naterial out into one of a stagnant environuent, whether this naterial m voir behind tho da So we vere ore Wa changed the ocean, into interested in knowing ht attond +t ing in the in terms of silt copesition. Yio followed this. over a period of a year since the dan was formed, These ara activitics in mid-larvae starti: it is typical, roser- (Indtecatin: in in January where and then we have a drop in February, liarch, April -- auring the flood scason -~ 2 magor build-up during the varm months of the year, These are typical secsonal patteras that we shoved before. Again, last winter a and, rop dovn during the cold months of course, we wore giad to sce that these iavels and the continuing one es beyond this Slide (indicating) nere, virtually are the sam2 as they we during the previcus years, which certainly, for the first yoar at least, indicates that there is