“Ro obtada ton aet icee “ates < measurements,
(«
tae sani Zoy debris from time Arsy
‘s 1ecessarvy tc +. >etract ‘he component due te background
pricr to the #207.
to ve 0.025 ar Ur,
This seasuremes’ ms not reported.
Tt is sseunsd here
‘.0. the same as measured ot Alamo ead Caliente is
December, 1962.
The dose rate contours reporte: ‘vy Lareom et al from aircraft mencurements,
and the surface neasurements sade ‘y Lt. Wade and kis moniters cre generelt
esnstotent.
Both indicste areas waere the deposition level me egprextuste
ly 2 times that noted in the Cams - cekley - Sayderville aren.) Beth
indicate some high Levels of fallout om U. 3. Rewke 49 Betunen Buoheene end
Straveerry Lake, and tate Road {5 between Duchecse and Tabomia. ‘The high
levels vetween Pruitiand and Stravberry Lake and Thistle and Stravberty Lak
are not emnetiy iadiceted by the coctours as shown.
Tats might be ane te «
ineorrect location of the 1 zr ‘hr-et-2h-wour conteur fram the hot spot just
east of Fruitland.
Although scattered light precipitation is reperted in the bs eget even ah:
July 1%, 15, and 16, the readily available date (36) suggest that, geet of
the fallout ceeurred largely without precipitation op with very little
preeightation -
Lareon’s éxta (Figure 21,
-1cate that the locations at vhteh milk samples
cere taken (ames, Oak)+
-ad Snyderville) lie om the edge ef the hot apot
area, and heve 24 nour ¢.-«rnal game dose rates of lees than 0.2 ar/tr.
The only surface messurements vnich indicate am ro value ot Kame, Onkley,
and Snyderville are those wade ~y the army moniters on their route passing
thru Kamas ‘Figure 23),
From Figure 23 it is seen that the net dose rate (i.e. substracting 0.085