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
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