| i @ 1107 Visual inspection suggests that an appreciable wive washed over Ingsbi, ‘ : closer ialands wern surely inundated, and it is even possible that parts of Kirinian were washed. During @ damage survey on M/ 2, I was foreibly struck :. ‘ by the peculiar shuenee of burned vegetation om Engedi, Ee : charring was very cevere, as in the case of a wooden raft just off shore. ng Bonetholess, no blackened vegetation wes visible on Engebiy the upper brush a Surely the thermal : was scorched, but grass was visibly green at its bese. This seems moet res- | wave action, long after the blast and thermal effects. More direct evidence f 3 was obtained later on during another inspection trip. Project 6.2 had 10 AA _ 4 guns om the east end of Ingebi, just off shore, where the island is unusually e high, about 7 feet, above the lagoon. Mere driftwood wee found lodged in the 2 3 gun mechaniams, scue 7 feet above ground. Also, one gum had been amshed as ’ g from several feet above ground by a large boulder, several feet across; broken parte of this doulier were lying on the gun platforn. 1% seems that only 8 E : ; large wave, greater then 15 fect high, could have yrodeced these effects. On ‘ the fax end of Ingubi, avay from the bomb, gravel was deposited around test { inetalliations, and growad vines were pulled in a way typical of wave action. : The most striking «videnes of wmves cos Rngedi was present on the OCE strue- : ‘+are; oneteetion cf this, faeing the bisat, was made of corrugated iroa, vith 3 the chanséls running horisontally. Deposited on these leéges and plastered on i the wil, wes a mixture of flotecom, sand and fine organic debris, which cer- q tainly looks like wave work. a feet of the top of this 3) foot structure. It would bevery difficult to as- a eribe all. these effects to blast winds Ogle makes a reasopable silternative This material wes deposited to within several BEST AYAILASLE COPY Gu Pate