BeackibG OW MidWETOK SURVEY
~2-
DEAFT
the reacing was C.G me/pyr at 3 feet aleve the surface.
On the Tip
of the crater (above the creter iv the ‘erow-out portion) the value
was up te DomPser at 2 feet
the Teter G: Jenmee
tformerdy Enueebi, sice of (Tho ana EASY on
gperatiad VerkhkoOSe, 2252, and Vv -RAY on Creration SANDSTONE, 1048),
hee ye
oe
CHER
FeV
Che
wpe.
SEYVGR
‘
a...
PO USS
fF
ms
TP cal
.
GY
et
gt
«
Alek
tote
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o
.
ok
Pre SO be Py ote oe ee,
6
TOP
eo
eee
,
oe
ua
vee at
Meads,
rile wba ts
:
Peer
irar,
(PE
228
>
moot
Pant
Dope
dd
Lyte
were
Que
rs a
oe dy
aT
-
'
.
va
ete
POUL oT
“ire tefard to
were
ete
Lay}.
pre Crean-up tian caiis for moving juto co> area about Aucust
25, US7i. ave start clearine avay the brush in early September.
Thers ty)
je
7
fat cmoy] BE caltbrabien sheets
dortne the Srd week
we
s
of Sepce er, then cortlinue with the clean-up.
The next phase of
clecr-un fn ocreniysation for the experiment will be scranina the coral
overcuree Gown ta the water surface on the islanc, where in most
nlaces this is 4 1/2 to 3 feet below the present surface.
If there
fs anv ton soit this wilt ba separated and pulled to one side.
The
coral sand wil] be pulled over to the jaaoon side to enlarge the
island.
The area on the west end of the istand is cantaminated with
berylldum and fs nosted.
xperiment.
The area will not be disturbed during this