Titlebook: Landslide Tsunamis: Recent Findings and Research Directions; Jean-Pierre Bardet,Fumihiko Imamura,Hugh L. Davies Book 2003 Springer Basel A

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Landslide Tsunamis: Recent Findings and Research Directions,etic opportunities to examine landslide tsunamis. This paper makes recommendations on future research directions, and will hopefully advance scientists’ and engineers’ understanding of these natural hazards and assist planners in mitigating their risks.

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The 1998 Papua New Guinea Earthquake and its Fault Plane Estimated from Relocated Aftershocks,ions near the epicentral area around the Sissano Lagoon carried out by ... (1998). Using three-component seismometers, they carried out observations from August 2 to October 2, 1998 at three sites. Although the network did not record the main shock and immediate aftershocks, the data obtained by tem

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The Aitape 1998 Tsunami: Reconstructing the Event from Interviews and Field Mapping, some estimates as high as 2200; 1000 were seriously injured, and 10,000 survivors were displaced. This paper presents information from interviews with eye-witnesses and from mapping of damage and inundation, and includes new information on the height, shape and timing of the waves; on the possible

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Tectonics and Slumping in the Source Region of the 1998 Papua New Guinea Tsunami from Seismic Refle from a series of seafloor-parallel, coherent reflections that are top-lapped by basin deposits at the foot of the amphitheater to the north. The cross-sectional area of the displaced mass is 2.3 km.. From the bathymetry, the width is approximately 2.5–3 km, yielding a total volume (assuming parabol

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Mitigation Lessons from the July 17, 1998 Papua New Guinea Tsunami,tional recovery funds and the Catholic Diocese. The three Malol villages, two Arop, four Sissano and the Warupu village were permanently abandoned and new villages established inland. Closure of the lagoon and restriction of coastal fishing impacted adjacent villages as well as tsunami survivors. By

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Re-examination of the Source Mechanism of the 1998 Papua New Guinea Earthquake and Tsunami,ide is employed to study the behavior of a landslide-generated tsunami with different size sand depths of the initial slide just outside the lagoon. A landslide model with a volume of 4-8 x 10. m. is selected as the best in order to reproduce the distribution of the measured tsunami runup in the lag

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