tides. ‘The lover gama dose rates observed below the high tide mark would

support this hypothesis.
The water from vells and exposed profiles represents the fresh water

Leng underlying the islands and the ebove data show that they are contanine
ateds These deta are of special interest since these lenses my be
intercedlate systecs for trensferring various nuelides from the soil to

plents.
.

Tho cistern water ani other poteble water supplies of lescer

inportence show varying degrees of contamination depending on such things
as the cleenliness of the reservoir, the watershed areas and the presence or

ebserce of chiclding trees.

The higher levels of activity found in the

ttong of cisterns are to be expected end these data ara included only for
eomarative purposes.

baypsa

1s

“

pimecciecTIT

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