Archaeoastronomy and ethnoastronomy in the Ryukyu Islands ...
Tsunami recurrence intervals from Holocene …...The Ryukyu subduction zone is locked because: 1....
Transcript of Tsunami recurrence intervals from Holocene …...The Ryukyu subduction zone is locked because: 1....
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Tsunami recurrence intervals from Holocene deposits on Ishigaki and Miyako islands along the Ryukyu
subduction zone
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Masataka Ando1, Masanobu Shishikura2, Yoko, Tu1, Mamoru Nakamura3, Jian-zhi4 Wei and Yasunari Shinjyo3
1: Institute of Earth Sciences, Taiwan 2: Geological Survey and Applied, Geosciences, Japan, 3: Dept. Earth Sciences, Univ. Ryukyus, Japan 4. National Chenggong University, Taiwan
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Coauthors
Masataka Ando1, Masanobu Shishikura2, Yoko, Tu1, Mamoru Nakamura3, Jian-zhi4 Wei and Yasunari Shinjyo3
1: Institute of Earth Sciences, Taiwan 2: Geological Survey and Applied, Geosciences, Japan, 3: Dept. Earth Sciences, Univ. Ryukyus, Japan 4. National Chenggong University, Taiwan
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Highlights • The Ryukyu subduction zone is characterized to
be locked (coupled, seismic) based from the recent geophysical studies, which suggests that large tsunamis will potentially occur along the entire subduction zone.
• Tsunami sediments from past events were studied to establish the recurrence interval, size and location of tsunami sources,
• This is the first study of tsunami deposits in this region.
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Contents 1. Locked or unlocked subduction 2. Ryukyu : Locked subduction zone 3. The 1771 Yaeyama tsunami 4. Excavation of tsunami sediments 5. Summary
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Data from GEONET
GPS , 1997-2006
200 km
1. Locked or unlocked subduction
2003, M8.0
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GPS 1997-2007
1. Locked or unlocked subduction
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The Ryukyu subduction zone is locked because:
1. Intermediate-depth slow-slips (Heki et al. , 2008) 2. The 1771 tsunami source (Nakamura, 2009) 3. Coupled interface from geodetic survey (Nakamura et al., 2010) 4. Very low frequency earthquakes (Ando et al. ,2012) 5. Locked zone from GPS (Hsu et al. 2012)
Focal mechanism: Very low frequency earthquakes
2. Ryukyu: locked subduction
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3. 1771 Yaeyama tsunami
Death rate Causalities/ Population on ishigaki Island = 8,910/17,394 = 51%
92% 98% 32%
27%
7% 3%
25%
4 2%
Population of each of 31 communities
ranging from 500 to 1000 people (Nariyuki-Sho, 1771)
(大波之時各村之形行書 1771)
Wave heights recoded In documents
87%
25%
5% 42%
Death rate, %
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12 m
A tsunami boulder on Shimochi Island
Tsunami boulder
Notch
Up
Down
3. 1771 Yaeyama tsunami
880±70yr BP, 1280±70yr BP
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Nakamura (2009) L=150km, W=30km, Dip=12o, Reverse slip=16m
100 km
Ryukyu trench
3. 1771 Yaeyama tsunami
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Tozato North Tozato South
Arakawa
Nagura
Ishigaki
30m in 1771 5m
in 1771
4. Excavation of tsunami sediments
10 km
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Geoslicer excavation 4. Excavation of tsunami sediments
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Gluing the soil sample to a net sheet 4. Excavation of tsunami sediments
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300 m
10m
10m
Tozato S. excavation site Tsunami height in 1771: 33m
300 m
33m
4. Excavation of tsunami sediments
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Tozato South
Tsunami boulder
Excavation site
4. Excavation of tsunami sediments
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Distance from the coast line: 400m Altitude: 4.5 m
Tozato site
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Shell BC1870-1650
Coral AD420-600
Coral AD690-880
North wall South wall
Cultivated soil
Black soil
Medium sand with rounded pebbles
Tozato South
1771 tsunami boulder
C14 sample
Foraminifera
Coral
Pebble 0 cm
50
100
Before 1771 and after AD 690-880
0 cm
50
100
4. Excavation of tsunami sediments
1. Mixture of materials 2. Reversed C14 dates 3. Deep foraminifera
Tsunami layer
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250m, Lenticulina thalmanni
70m,Quinqueloculina tropicalis
3-4m, Cellanthus craticulatus
80-110m, Spiroloculina henbesti
Continental shelf Continental slope
Foraminifera analysis
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4. Excavation of tsunami sediments
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Modern Seed
AD810-100 Crams
AD1580-1810
AD1550-1800 Shell
AD1660-1950, Wood
Arakawa site 1 C14 sample
Foraminifera
Coral
Pebble
Shell
0 cm
50
100
150
Brown cultivated soil
Dark brown soil
Gray coarse sand with shell and
coral fragments
Gray coarse sand with l large coral
fragments
Tsunami layer
4. Excavation of tsunami sediments
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4. Excavation of tsunami sediments
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Miyako Is.
18m in 1771
>12 m in 1771
50km
Ishigaki Irabu
Irabu 1
Ikema 1
Irabu 1
Irabu 2
Tomori 2
Tomori 1
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Irabu island
A tsunami layer, occurred possibly between 11th C. and 1771
1771 tsunami boulder
50 cm
4. Excavation of tsunami sediments
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100
200
300
Irabu site
2013/2/19 24
AD 550 - 660
AD 160 - 300
AD 120 - 40
BC 2270 – 2110
AD 910 - 1030
AD 1030 - 1170
AD 1060 - 1200
Coarse-grain sand layer
Cultivated soil
Tsunami layer?
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?
AD 2000
1000
0
BC1870-1650
AD420-600
AD690-880
AD1580-1810
AD1550-1800 AD1660-1950
Ishigaki Island
1771 Tsunami
Tsunami
1500
500
AD 1040-1170 AD 1030-1170
1771 Tsunami
Tsunami
Irabu Island
?
Tsunamis
4. Excavation of tsunami sediments
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Ishigaki
Slip rate: 8 cm/y 24 m/300 yrs Only a large tsunami was generated in 1771 from C
8 cm/y
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A B
C
D
Large slip deficit
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5. Summary Western Ryukyu (WR) subduction zone
• Tsunami sediments were found from excavation surveys on the islands.
• Sediments from the 1771 tsunami and a previous event between 8-9th C. and 1771 were identified.
• The WR subduction zone has the potential to generate large tsunamis in the future.
• Further evidence is necessary to identify past tsunamis. 27
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GPS水平運動
Hsu et al. (2012)
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29 Summarized by Goto et al. (2010)
Previous paleotsunami studies on Ryukyus All based on tsunami boulders
Ishigaki Shimochi
Irabu
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C14 Irabu-3, 105cm
BP1310+-30
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Pacific plate
Philippine Sea plate
N. American plate
Eurasian Plate
(Amurian Plate)
Japan
Taiwan
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