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  4. Occurrence of 1?ka-old corals on an uplifted reef terrace in west Luzon, Philippines: Implications for a prehistoric extreme wave event in the South China Sea region
 
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Occurrence of 1?ka-old corals on an uplifted reef terrace in west Luzon, Philippines: Implications for a prehistoric extreme wave event in the South China Sea region

Journal
Geoscience Letters
Journal Volume
4
Journal Issue
1
Date Issued
2017
Author(s)
Ramos, N.T.
Maxwell, K.V.
Tsutsumi, H.
Chou, Y.-C.
Duan, F.
CHUAN-CHOU SHEN  
Satake, K.
DOI
10.1186/s40562-017-0078-3
URI
https://scholars.lib.ntu.edu.tw/handle/123456789/492997
URL
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85019183789&doi=10.1186%2fs40562-017-0078-3&partnerID=40&md5=5ea1dd37b3e3deb3efc6698d11b77ec7
Abstract
Recent 230Th dating of fossil corals in west Luzon has provided new insights on the emergence of late Quaternary marine terraces that fringe west Luzon Island facing the Manila Trench. Apart from regional sea level changes, accumulated uplift from aseismic and seismic processes may have influenced the emergence of sea level indicators such as coral terraces and notches. Varied elevations of middle-to-late Holocene coral terraces along the west Luzon coasts reveal the differential uplift that is probably associated with the movement of local onland faults or upper-plate structures across the Manila Trench forearc basin. In Badoc Island, offshore west of Luzon mainland, we found notably young fossil corals, dated at 945.1 ± 4.6 years BP and 903.1 ± 3.9 years BP, on top of a ~5-m-high reef platform. To constrain the mechanism of emergence or emplacement of these fossil corals, we use field geomorphic data and wave inundation models to constrain an extreme wave event that affected west Luzon about 1000 years ago. Our preliminary tectonic and tsunami models show that a megathrust rupture will likely lead to subsidence of a large part of the west Luzon coast, while permanent coastal uplift is attributed to an offshore upper-plate rupture in the northern Manila Trench forearc region. The modeled source fault ruptures and tsunami lead to a maximum wave height of more than 3 m and inundation distance as far as 2 km along the coasts of western and northern Luzon. While emplacement of coral boulders by an unusually strong typhoon is also likely, modeled storm surge heights along west Luzon do not exceed 2 m even with Typhoon Haiyan characteristics. Whether tsunami or unusually strong typhoon, the occurrence of a prehistoric extreme wave event in west Luzon remains an important issue in future studies of coastal hazards in the South China Sea region. © 2017, The Author(s).
Subjects
230Th dating; Coastal hazards; Coral terraces and boulders; Philippines; Prehistoric extreme wave event; South China Sea region
SDGs

[SDGs]SDG11

[SDGs]SDG14

Other Subjects
coral reef; extreme event; fault zone; fossil record; future prospect; reef formation; terrace; tropical cyclone event; uplift; Luzon; Manila Trench; Pacific Ocean; Philippines; South China Sea
Type
other

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