熱海・初島において,1923年関東地震津波について,地震体験者の住民から聞きとり調査を行った.熱海では当時の海岸から約200m,地盤高がT.P.上7m以下の市街地に浸水したことが分った.熱海中心部の海岸では津波の高さは7.0~8.0mと推定される.一方,初島では地盤が隆起して集落内に津波は侵入せず,津波の高さは1.8m程度であった.The Kanto tsunami of Sept, 1, 1923 hit the south Kanto district on the Pacific coast of central Japan. At Atami located in the western part of Sagami Bay, 162 houses were washed away. In this paper, the tsunami behavior at Atami and Hatsushima Island is investigated from the visual observation of inhabitants. The tsunami front ran up 200m into Atami Town and ground about 7.0m above M.S.L. was inundated. The inundation height at the coast seems to be 7.0-8.0m. Hatsushima Island, located 10km southeast of Atami, was uplifted almost uniformly by about 1.8m by the 1923 Kanto e...
The tsunami which was generated off Iturup Island, Kuril Islands, at 14 h 18m(JST), Oct. 13, 1963, w...
Yuasa and Hiro located on the west side of Kii Peninsula, western Japan, have been hit by many large...
A small tsunami was generated by the Urakawa-oki earthquake (M=7.1) near Cape Erimo, southern Hokkai...
1982年12月28日三宅島近海に発生した群発地震で,八丈島八重根検潮所において全振幅40cmの小津波が観測された.しかし,それ以外の伊豆諸島の検潮記録では風浪による顕著な副振動と重なり,津波は検知で...
新史料を加え,1741年渡島沖津波の波高を再検討した.また,北海道渡島沿岸を現地調査し,熊石にある津波地蔵・過去帳を紹介した.津波の高さは渡島沿岸で10m,局地的には15mに達し,津軽で5~6m,佐渡...
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...
海底変動によつて発生する津波の振幅は,海底変動の垂直変位と,変動の速度に依存する.若し変動速度に対する振幅応答の特性が異つた場所があるならば,変動模型を仮定した数値実験の結果と,実際の観測値とを比較す...
The earthquake occurred at 09 : 49, May 16, 1968 at 40.7°N, 143.6°E. The depth of the earthquake was...
For seven tsunamis which reached the coast of Japan, from Iturup, Kamchatka, Aleutian, Alaska and Ch...
There were three major tsunami events that attacked Tohoku region including Minama-Sanriku town in t...
新史料を加え,天保14年(1843年)北海道東部津波の挙動を検討した.浸水被害状況から,津波の高さは厚岸4~5m,白糠3~3.5m,函館0.5m,八戸2.5~3mと推定され,津波マグニチュードはm=2...
The earthquake occurred at 09 : 49, May 16, 1968 at 40.7°N, 143.6°E. The depth of the earthquake was...
1). A great earthquake took place on December 7, 1944, the epicenter of which was announced by the C...
The tsunami caused by the Tonga submarine volcanic eruption that occurred at 13:15 Japan Time (JST) ...
Yuasa and Hiro located on the west side of Kii Peninsula, western Japan, have been hit by many large...
The tsunami which was generated off Iturup Island, Kuril Islands, at 14 h 18m(JST), Oct. 13, 1963, w...
Yuasa and Hiro located on the west side of Kii Peninsula, western Japan, have been hit by many large...
A small tsunami was generated by the Urakawa-oki earthquake (M=7.1) near Cape Erimo, southern Hokkai...
1982年12月28日三宅島近海に発生した群発地震で,八丈島八重根検潮所において全振幅40cmの小津波が観測された.しかし,それ以外の伊豆諸島の検潮記録では風浪による顕著な副振動と重なり,津波は検知で...
新史料を加え,1741年渡島沖津波の波高を再検討した.また,北海道渡島沿岸を現地調査し,熊石にある津波地蔵・過去帳を紹介した.津波の高さは渡島沿岸で10m,局地的には15mに達し,津軽で5~6m,佐渡...
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...
海底変動によつて発生する津波の振幅は,海底変動の垂直変位と,変動の速度に依存する.若し変動速度に対する振幅応答の特性が異つた場所があるならば,変動模型を仮定した数値実験の結果と,実際の観測値とを比較す...
The earthquake occurred at 09 : 49, May 16, 1968 at 40.7°N, 143.6°E. The depth of the earthquake was...
For seven tsunamis which reached the coast of Japan, from Iturup, Kamchatka, Aleutian, Alaska and Ch...
There were three major tsunami events that attacked Tohoku region including Minama-Sanriku town in t...
新史料を加え,天保14年(1843年)北海道東部津波の挙動を検討した.浸水被害状況から,津波の高さは厚岸4~5m,白糠3~3.5m,函館0.5m,八戸2.5~3mと推定され,津波マグニチュードはm=2...
The earthquake occurred at 09 : 49, May 16, 1968 at 40.7°N, 143.6°E. The depth of the earthquake was...
1). A great earthquake took place on December 7, 1944, the epicenter of which was announced by the C...
The tsunami caused by the Tonga submarine volcanic eruption that occurred at 13:15 Japan Time (JST) ...
Yuasa and Hiro located on the west side of Kii Peninsula, western Japan, have been hit by many large...
The tsunami which was generated off Iturup Island, Kuril Islands, at 14 h 18m(JST), Oct. 13, 1963, w...
Yuasa and Hiro located on the west side of Kii Peninsula, western Japan, have been hit by many large...
A small tsunami was generated by the Urakawa-oki earthquake (M=7.1) near Cape Erimo, southern Hokkai...