‘7
Considering
the atoll as a whole,
an
‘est sertes,
and the three successive
tne evidence from Figure 2 suggests that the 1956
8 curntributed not mure than 1/100 as much radioactivity as
tie orig?nil 1754 fallout,
uni the 195@ sertes, not more than
27,5. 28 nwuch as trie 1956 serios.
Ps ko CGulcladed un.t t..e northern part of Rongelap Atoll
rene ied a heavier Calicut from che March 1,
Cia tie couthern part.
Slicnt
rope
1954 detonation at
In contrast,
the relatively
Callout Prom luver detonitions affected the southern
Tnoun tae northern parts of the atoll,
as is evidenced by
tae hisier levels of rudto.ctivity at Rongelap Island than at
3
ae a ce el