The wave crests were estimated to be 500-600 m apart (observations by Dickson Dalle). (1998): An American Anthropologist in Melanesia.
“The book itself is a tribute to the ones lost and memorial to those who responded and helped.“It is a model from which lessons can be drawn, and I encourage us to have a copy of this book,” Prof Davies said.
The sunken reefs are at depths of 460 m and 82 m, respectively. In G. Herbenstreit (ed.
It is now recognised that such events can be very dangerous, as the earthquake may be too small to be felt on land, or detected by the The earthquake consisted of a main shock and several aftershocks that were felt in several towns in the area around the epicenter. Since the beginnings of written history in this region, the Aitape tsunami is exceeded in impact by only the 1888 tsunami, triggered by the collapse of Ritter Island volcano (Everingham, 1977).The tsunami happened at a time when the nation was ill prepared.
In addition, there is a newly-recorded oil seep offshore from Lemieng (Fig. In 1998, a tsunami killed nearly 3,000 people along the coast of Papua New Guinea, west of Aitape. Before the tsunami, about 12,000 people lived in the coastal villages west of Aitape, from Malol to Sissano (Fig. In this sector the wave fronts moved from east to west along the coast; all structures were destroyed, and 20-40 percent of the population was killed. A callophylum tree on the coast of Tumleo Island. People went to the beach to investigate the unusual noise and observed that the sea was 'boiling' or bubbling, and had receded by 50 m or so, exposing the nearshore sea bed.
The second of the three waves rose to a height of 10-15 m above sea level after it had crossed the shoreline and caused most damage. More could have been learned with a concerted program of enquiry. Subsidence at the former site of Warapu village is permitting erosion of the Warapu peninsula at the mouth of the Sissano Lagoon. 4) observers estimated that the waves arrived "about 5 minutes" after the aftershocks.People who saw the broken wave approach the mouth of the lagoon described it as a dirty mass of broken water filled with dark sand, logs and other debris. Transactions of the Royal Society (in press).Tanioka, Y.
1), including the great church that had stood since 1926. However, precise information is not easily obtained, because people in the villages generally do not concern themselves with knowing the time to the minute but, rather, take the time from the sun.
Berlin: Dietrich Reimer Pegler, G., Das, S., and Woodhouse, J.H.
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aitape tsunami 1998