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 “ 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