ランキング (合計) - Ceek.jp Altmetrics

The west coast of Kii Peninsula and Shikoku, western Japan, suffered severe damage from the three Nankaido tsunamis of 1707, 1854 and 1946. There are many old monuments of the 1854 Ansei tsunami along the Kochi coast. Old documents on the Hoei (Oct. 28, 1707) and Ansei (Dec. 24, 1854) tsunamis along the southwest coast of Kochi Prefecture were collected during the present field investigation and illustrated in this paper. Based on the documents, the inundation heights of the 1707 Hoei and 1854 Ansei tsunamis were surveyed by handlevel and compared with those of the 1946 Nankaido tsunami (Dec. 21, 1946). The inundation heights (above M. S. L.) of the 1854 Ansei tsunami along the southwest coast of Kochi averaged 5.5 meters. Those of the 1707 Hoei tsunami averaged 7.7 meters with maximums of 10 meters at places. Although the inundation heights of the 1946 tsunami along the entire Pacific side of Shikoku were nearly uniform, the patterns of height distribution along the west coast of Shikoku for the 1707 and 1854 tsunamis differ significantly from those of the 1946 tsunami. The inundation heights of the 1854 Ansei and 1707 Hoei tsunamis on the western Shikoku coast were 1.5 and 2.1 times respectively, higher than those of the 1946 tsunami. This suggests that the rise times and/or the amount of the slip displacements on the west part of the fault might be different.

2014-05-26 16:05:35
2 + 2 Wikipedia

http://hdl.handle.net/2261/12817

2 0 0 0 OA 7. 和歌山県湯浅・広に遡上した南海道津波の調査 : 1946年南海道および宝永・安政津波について

著者: 羽鳥徳太郎相田勇坂下至功日比谷紀之
出版者: 東京大学地震研究所
雑誌: 東京大学地震研究所彙報 (ISSN:00408972)
巻号頁・発行日: vol.58, no.1, pp.187-206, 1983-07-28

Yuasa and Hiro located on the west side of Kii Peninsula, western Japan, have been hit by many large tsunamis which were generated about every 100 to 150 years. Sources of all these tsunamis were offshore between Wakayama and Shikoku along the Nankai Trough. Traces of the inundated level on many houses in the two towns caused by the 1946 Nankaido tsunami (Dec. 21, 1946) were surveyed, using the automatic level from Oct. 18 to 23, 1982. The behavior of the 1946 tsunami run-up on land was investigated and compared with the two historical tsunamis of Hoei (Oct. 28, 1707) and Ansei (Dec. 24, 1854). The results of the present survey are as follows: (1) At Yuasa, the inundation heights of the 1946 tsunami were 3.0-3.5 meters above M.S.L. Ground about 3.0 meters above M.S.L. was inundated, so that 450 houses were inundated but hardly any were washed away. At Hiro, the sea wall strongly protected the main part of town from the 1946 tsunami (This bank was constructed just after the 1854 Ansei tsunami from Mr. Goryo Hamaguchi's personal funds). However, the tsunami energy concentrated at the head of bay along the Egami River. The inundation heights locally reached 5 meters (above M.S.L.) or more and 22 persons were killed. (2) According to old documents, the inundation area of the 1707 Hoei tsunami elongated along the Yamada, Hiro and Egami Rivers. Forty-one lives were lost at Yuasa and 192 at Hiro. Inundation heights above M.S.L. were estimated 4-5 meters at Yuasa and 5-6 meters at Hiro. (3) By the 1854 Ansei tsunami, 28 lives were lost at Yuasa and 36 at Him. The patterns of damage at Yuasa and Hiro are similar to those of the 1707 Hoei tsunami. There remain even now traces of the inundation level on a few old houses in both towns. Inundation heights above M.S.L. were 4.0-4.7 meters at Yuasa and 5.0 meters in the center of Hiro town. Ground about 4.0 meters above M.S.L. was inundated, 0.7 to 1 meter higher than that during the 1946 Nankaido tsunami.

2014-05-26 16:05:35
2 + 2 Wikipedia

http://hdl.handle.net/2261/12872

2 0 0 0 OA 関東・伊豆東部沿岸における宝永・安政東海津波の挙動

著者: 羽鳥徳太郎
出版者: 東京大学地震研究所
雑誌: 東京大学地震研究所彙報 (ISSN:00408972)
巻号頁・発行日: vol.59, no.4, pp.501-518, 1985-03-30

関東・伊豆東部沿岸を対象に,宝永・安政東海津波における各地の史料・伝承記録を集め,両津波の挙動を調査した.安政津波は,伊豆東部沿岸の集落内に遡上し,津波の高さは3~6mに推定され,半島の付け根付近が高い.また,東京湾では東京・浦安・横浜の河口付近に溢れている.1923年関東地震津波と比べると,相模湾沿岸では津波の高さは下回つたが,外房・九十九里浜では集落に溢れ2倍ほど上回った.宝永津波の高さの分布は,安政津波とほぽ似たパターンを示している,両津波の高さが予想外に大きい要因の一つとして,南海・駿河トラフで発生した津波がエッヂ波のように伊豆東海岸に伝わり,加えて波の屈折効果が作用したものと考える.

2014-05-26 16:05:35
2 + 2 Wikipedia

http://hdl.handle.net/2261/12926

2 0 0 0 OA 九州東部沿岸における歴史津波の現地調査 : 1662年寛文・1769年明和日向灘および1707年宝永・1854年安政南海道津波

著者: 羽鳥徳太郎
出版者: 東京大学地震研究所
雑誌: 東京大学地震研究所彙報 (ISSN:00408972)
巻号頁・発行日: vol.60, no.3, pp.439-459, 1986-02-07

寛文・明和日向灘津波および宝永・安政南海道津波について,史料をもとに大分・宮崎県沿岸各地を現地調査し,津波の高さ,浸水域の広がりを考察した.寛文津波は宮崎平野に広く浸水し,津波の高さは4~5mと推定される.明和津波は大分県沿岸で2~2.5mの波高があり,津波よりむしろ地震災害が上回った.津波マグニチュードは,それぞれm=2と1に格付けできる.両津波の震度・波高分布および地殻変動の記録を近年の日向灘津波と比べると,波源域はいずれも沿岸付近にあったとみなされる.一方,宝永南海道津波は大分・宮崎県沿岸各地の集落に溢れ,津波の高さは3~4.5mに達している.また,熊本・長崎県沿岸にも浸水記録があり,30分程度の長周期波が卓越したことを暗示する.安政南海道津波は宝永津波よりやや小さく,大分・宮崎県沿岸の波高は2~3mと推定される.両津波の規模および震度が1946年南海道津波を上回り,予想以上に九州各地に強い影響を与えていることから,波源域が1946年津波のものより四国の南西沖に伸びていたことを考えさせる.