Aomoen-Bikini reef is apparent in comparisons of the Bikini station data with other lagoon stations. Data from the Long Period recorders has yet to be examined, Up rush and inundation on Bikini Atoll islands was insignificant except in the Yurochi~Romurikku area, The largest wave of the train approaching this area had a deep water crest height above mean water level of approximately 9 ft. Water crossed the Yurochi-Romurikku causeway and passed to the ocean side of these islands, period associated with] — The short FLATHEAD) waves prevented a major break through of the causeway and limited the water damage to earth works and structures in that area. Eninman-Airukiiji complex. Minor up-rush and cross over occurred in the Energy levels at this point were insufficient to cause any but minor scouring and erosion. of center Enirikku. Water flooded a small seetion No errosion or scouring was apparent. Results of the distant island station are not available at this time, ( ypiED [DUE ie sero ANL RO | ~ 16 - I~