کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4718949 | 1639150 | 2010 | 6 صفحه PDF | دانلود رایگان |

The 29 September 2009 South Pacific tsunami reached the islands of Futuna and Alofi, 650 km to the west of its origin, between 7 and 7:20 am on 30 September, local time. No warning was issued. We measured run-up heights and inundation distances at 41 sites around the islands. The worst impact (4.5 m run-up; 85 m inundation; 3.8 m flow depth) was observed on Alofi's NW beach. On Futuna, maximum run-ups of 4.4 m on the eastern tip and 4.3 m on the NW tip of the island are associated with maximum inundations of 95 and 72 m, respectively. A flow depth of 2.2 m was inferred on the NE tip. The tsunami arrived as a drawdown of water with the reef exposed well below the lowest tides. It was followed by two positive waves of similar amplitude, ca. 4 min apart. Damage was mainly limited to salt-burnt vegetation and sediments deposited at the coast. There were no casualties, but a significant disaster was avoided because the tsunami arrived in the early morning at close to low tide. This event, together with a small tsunami triggered by a local earthquake in 1993 and an oral legend about a destructive wave, indicate that the hazard is high for the 4500 inhabitants of Futuna who live on the low-lying, narrow coastal strip. The 70 min that the tsunami took to reach the island provided sufficient time for a warning to be issued, but this was not done.
Journal: Marine Geology - Volume 271, Issues 3–4, 15 June 2010, Pages 297–302