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The 1026 Manju tsunami affected the Sea of Japan coast of then
Iwami Province was an old province of Japan in the area that is today the western part of Shimane Prefecture. It was sometimes called . Iwami bordered Aki, Bingo, Izumo, Nagato, and Suō provinces. In the Heian period (794–1192) the capital was at moder ...
on June 16. Considered one of the largest tsunamis in the Sea of Japan, it generated a tsunami with waves of at present-day
Masuda, Shimane is a Cities of Japan, city located in Shimane Prefecture, Japan. , the city had an estimated population of 43,885 in 21,249 households and a population density of 60 persons per km2. The total area of the city is . Geography Masuda is located ...
. Off the coast, an island reportedly sunk because of the waves. More than 1,000 people were killed and 3,000 homes were destroyed. The source of the tsunami has been debated between an earthquake or undersea landslide.


Description

In historical records, locals claimed that a large stone called ''Kuroiwa'' was carried by the tsunami to its present location in Tonda, along
Japan National Route 9 is an important highway in the Kansai and Chūgoku regions. It connects the prefectural capitals of Kyoto, Tottori, Matsue ( Shimane Prefecture), and Yamaguchi. Other significant cities along the route include Yonago, Tottori and Shimo ...
about from
Masuda Station is a passenger railway station located in the city of Masuda, Shimane Prefecture, Japan. It is operated by the West Japan Railway Company (JR West). Lines Masuda Station is served by the JR West San'in Main Line, and is located 514.5 kilomete ...
. The tall stone was allegedly carried from the coast at an elevation of . A subsequent investigation revealed the stone, comprising basalt, originated from the inland mountains, as basalts do not occur at the coast, and was transported downhill by a landslide rather than the reported tsunami. The tsunami reportedly sunk the islands of Kamo, Nabeshima and Kashiwajima, which were then busy settlements. Oral records suggest these features were solid outcrops rather than
sandbar In oceanography, geomorphology, and geoscience, a shoal is a natural submerged ridge, bank, or bar that consists of, or is covered by, sand or other unconsolidated material, and rises from the bed of a body of water close to the surface or ...
s. Kamo Island was located off the coast of Takasu and was long by wide. When the tsunami struck Takatsu and the Masuda River mouth, its waves were about . Subsidence occurred at
Hamada A hamada (, ) is a type of desert landscape consisting of high, largely barren, hard rocky (basalt) plateaus, where most of the sand has been removed by Aeolian processes#Wind erosion, deflation. The majority of the Sahara is hamada. Other e ...
, and there was no record of a tsunami. The waves destroyed the Hitomaro Shrine on Kamo Island and dumped the resident statue of Kakinomoto no Hitomaro in Masuda. In the Toinomawari area of Masuda, the tsunami overwhelmed a sand dune embankment and buried the surrounding land. The waves advanced towards Kamitonoma, flooding Shimotonoma and Nakatonoma along the way. It caused massive devastation to farmland and properties; many people also went missing. Tonomawari Bay became overwhelmed with debris that it was impassable for ships. At the Oko ward of the city, the waves reached the foot of Mount Eboshi, and carried marine life inland. The statue of Kakinomoto no Hitomaro were retrieved and placed in the Matsuzaki Hitomaro Shrine before subsequently relocating to the Kakimoto Shrine in Takatsu. Another temple on Kamo Island, Senpukuji, was reconstructed while Manpukuji was never rebuild. Many other relics such as three statues of
Vaiśravaṇa (Sanskrit: वैश्रवण) or (Pali; , zh, s=多闻天王, t=多聞天王, p=Duōwén Tiānwáng, ) is one of the Four Heavenly Kings, and is considered an important figure in Buddhism. He is the god of warfare and usually portrayed as ...
, a Han dynasty mirror and a pair of
cymbal A cymbal is a common percussion instrument. Often used in pairs, cymbals consist of thin, normally round plates of various alloys. The majority of cymbals are of indefinite pitch, although small disc-shaped cymbals based on ancient designs sou ...
s were recovered. Ruins of an ancient pagoda buried by the tsunami deposit were revealed after a flood in 1729. Near Gōtsu Station, Gōtsu, the tsunami destroyed 1,000 homes while more than 500 temples and homes were damaged. Along the Shioda coast, the tsunami washed away three islets. It travelled up the
Gōnokawa River The is a river that runs through Hiroshima and Shimane prefectures in Japan. It is the largest river in the Chūgoku region. It is also called the Gōgawa River () and, in Hiroshima, the Enokawa River (). The mainstream originates from Mount As ...
and was recorded in Ochi District; the tsunami was also reported as far east as Kuromatsucho.


Tsunami evidence

In 1994, ''
Island Arc Island arcs are long archipelago, chains of active volcanoes with intense earthquake, seismic activity found along convergent boundary, convergent plate tectonics, tectonic plate boundaries. Most island arcs originate on oceanic crust and have re ...
'' published the discovery of a sand layer about beneath the Masuda
coastal plain A coastal plain (also coastal plains, coastal lowland, coastal lowlands) is an area of flat, low-lying land adjacent to a sea coast. A fall line commonly marks the border between a coastal plain and an upland area. Formation Coastal plains can f ...
which could only be explained as the result of a tsunami inundation. This layer comprised mud and medium to fine sand that originated from the sea. These materials, comprising coarse sediment grains and brackish benthic diatoms, were mixed with the
estuary An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime enviro ...
mud under tsunami-like conditions. The absence of bedded grading also suggest these materials had to be quickly transported onto the plain. A piece of wood from the excavated area, above the tsunami layer, was
radiocarbon Carbon-14, C-14, C or radiocarbon, is a radioactive isotope of carbon with an atomic nucleus containing 6 protons and 8 neutrons. Its presence in organic matter is the basis of the radiocarbon dating method pioneered by Willard Libby and coll ...
dated to 930±80 years before present, suggesting the layer may be evidence of the June 16, 1026 event. A water tank experiment suggest the tsunami was triggered by an undersea landslide, and a preserved landslide topography in the Sea of Japan may represent that trigger event. A numerical modelling estimated the mass failure volume at . The historical record does not document any seismic shaking from an earthquake before the tsunami arrived at the coast, however should an earthquake occur, its magnitude would be estimated at 7.8.


See also

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List of earthquakes in Japan This is a list of earthquakes in Japan with either a magnitude greater than or equal to 7.0 or which caused significant damage or casualties. As indicated below, magnitude is measured on the Richter scale (''ML'') or the moment magnitude scale ('' ...
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List of tsunamis This article lists notable tsunamis, which are sorted by the date and location that they occurred. Because of seismic and volcanic activity associated with tectonic plate boundaries along the Pacific Ring of Fire, tsunamis occur most frequentl ...


References

{{earthquakes in Japan 1026 Tsunamis in Japan Earthquakes in Japan History of Shimane Prefecture Masuda, Shimane Gōtsu, Shimane 11th-century disasters 1020s in Japan Landslides in Japan Medieval tsunamis