Last edited by Zululmaran
Monday, August 10, 2020 | History

1 edition of Hokkaido Nansei-Oki earthquake July 12, 1993. found in the catalog.

Hokkaido Nansei-Oki earthquake July 12, 1993.

Hokkaido Nansei-Oki earthquake July 12, 1993.

  • 286 Want to read
  • 40 Currently reading

Published by U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Geophysical Data Center in Boulder, CO .
Written in English

    Subjects:
  • Earthquake hazard analysis -- Japan -- Hokkaido Region.,
  • Tsunamis -- Japan -- Hokkaido Region.,
  • Accelerograms.

  • Edition Notes

    Other titlesHokkaido Nansei-oki tsunami July 12, 1993
    ContributionsNational Geophysical Data Center.
    The Physical Object
    Pagination[7] p. :
    ID Numbers
    Open LibraryOL17119299M

    Earthquake Spectra (Chapter in Special Issue on the Hokkaido Nansei Oki Earthquake). Scawthorn, c. “Fire Following Earthquake – The Risk In Vancouver And The Pan Pacific.”. Sedimentary characteristics and depositional processes of onshore tsunami deposits: an example of sedimentation associated with the J Hokkaido-Nansei-oki earthquake (F. Nanayama). Deposits of the Nicaragua Tsunami (B. Higman and J. Bourgeois).

    3 Strong Earthquake and Killer Tsunami Hits Indonesia, June 3, 4 Los Angeles (California) Basin Earthquake, Janu 5 Halmahera Island (Indonesia) Earthquake and Tsunami, Janu 5 Sumatra Island (Indonesia) Earthquake of Febru 5 Hokkaido Nansei-Oki (Japan Sea) Earthquake and Tsunami of J Japan Sea Earthquake, the Hokkaido-Nansei-Oki Earthquake, the Chile Earthquake and the Great East Japan Earthquake were large enough to trigger the warning system for giant tsunamis. With the exception of the tsunami produced by the far off Chile Earthquake, each of these tsunamis resulted in at least people.

    Get free shipping on Tsunami The Underrated Hazard Edition:2nd ISBN from TextbookRush at a great price and get free shipping on orders over $35! In advance of this analysis, we will review the Hokkaido-Nansei-Oki earthquake in the next chapter. 2. The Hokkaido-Nansei-Oki earthquake The variety of focal mechanisms At 17 (GMT) on 12 July , the volume-strain meter at KMU recorded an earthquake measuring magnitude on the Richter scale which occurred offCited by: 3.


Share this book
You might also like
Public building at Richmond, Ky.

Public building at Richmond, Ky.

Albert Schweitzer: an anthology

Albert Schweitzer: an anthology

Trace- and minor-element mineralogy of the microgranite at Ghurayyah, Kingdom of Saudi Arabia

Trace- and minor-element mineralogy of the microgranite at Ghurayyah, Kingdom of Saudi Arabia

Employer sanctions and legalization

Employer sanctions and legalization

Malaysia

Malaysia

Return of Military Dead Buried in France.

Return of Military Dead Buried in France.

archaeological heritage of Jordan.

archaeological heritage of Jordan.

diffusion of new consumer durables and the role of advertising

diffusion of new consumer durables and the role of advertising

Im not hanging noodles on your ears

Im not hanging noodles on your ears

Robin Hood.

Robin Hood.

Living with your eye operation

Living with your eye operation

Getting down to business

Getting down to business

Hokkaido Nansei-Oki earthquake July 12, 1993 Download PDF EPUB FB2

Hokkaido Nansei-Oki earthquake J Boulder, CO: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Geophysical Data Center, [?] (OCoLC) The Hokkaido-Nansei-Oki earthquake on July 12 produced one of the largest tsunamis in Japan's history.

At local time ( UTC), the M s quake rocked the west coast of Hokkaido and the small, offshore island of Okushiri in the Sea of Japan, generating a major minutes, extremely large waves engulfed the Okushiri coastline and the central west coast of Hokkaido.

We present an analysis of the data dependency of surface-wave inversions for source parameters of the 12 July Hokkaido-Nansei-Oki, Japan, earthquake. This dependency is demonstrated by differences between source mechanisms obtained from different data sets, particularly from Rayleigh waves or Love waves, although inversions of various data Cited by: (the hokkaido nansei-oki earthquake and tsunami of ) George Pararas-Carayannis On J a large earthquake off the west coast of Hokkaido and the small offshore island of Okushiri in the Sea of Japan/East Sea, generated a destructive tsunami.

On 12 Julyan earthquake of magnitude occurred with its epicentre ∼ km northwest of Okushiri Island (42°′N, °′E) ().This Hokkaido–Nansei-oki Hokkaido Nansei-Oki earthquake July 12 caused a tsunami that flooded not only Okushiri Island but also the parts of the western side of the Oshima Peninsula in southwestern Hokkaido (), including by: The M w = Hokkaido Nansei-Oki earthquake July 12 earthquake of J was a fortuitous large-scale experiment which allowed the measurement of high-quality runup data and the inference of fairly unambiguous ground deformation contours due to its proximity to seismic instrument arrays in a locale where high-resolution bathymetry and topography data exist.

A fault plane model and a finite element hydrodynamic model are applied to the simulation of the Hokkaido Nansei-Oki tsunami of J The joint performance of the models is assessed based on the overall ability to reproduce observed tsunami waveforms and to preserve mass and energy during tsunami by:   See the damage caused by a Japan tsunami that occurred in The Okushiri tsunami was generated by the Hokkaido-Nansei-Oki earthquake.

The video is. Key words: Tsunamis, Hokkaido Nansei-Oki earthquake, Okushiri Island. Introduction The Hokkaido Nansei-Oki (southwest off Hokkaido) earthquake of J generated devastating tsunamis that caused significant damage in Japan, particularly on Okushiri Island.

The earthquake began on July 12 at 17 local time at latitude 42 47' North, ° 12' E at a depth recorded during the Hokkaido-nansei-oki earthquake are generally EERI SPECIAL EARTHQUAKE REPORT -AUGUST TSUNAMI locations --on the beach, in wrecked automobiles, and in.

The Southwest Hokkaido Earthquake of Magnitude 7. 9 (J 17 JST) caused serious tsunami disasters in the southwestern part of Hokkaido, particularly on Okushiri Island (a tiny island off the southwest coast of Hokkaido with a population of about 4, at the time of earthquake).

The M Hokkaido Nansei-Oki earthquake that occurred on 12 July, at local time, produced a devastating tsunami wave that quickly hit Okushiri Island [1,2,3,4,5,6] (see Figure 1a–f).Approximately 4 min after the mainshock, a tsunami that was reported to be approximately 10 m high struck and swept away much of the urban area of the island’s Aonae by: 1.

The fault geometry and slip distribution of the Hokkaido Nansei-oki, Japan, earthquake of J are estimated using seismic wave, tsunami, and geodetic data. K ikuchi, M. (), Source Process of the Hokkaido-Nansei-Oki Earthquake of J Inferred from Teleseismic Body Wave Inversion, Abst.

of SSJ Meeting 2, 28 Google ScholarCited by: The Hokkaido-Nansei-Oki, Japan, earthquake (Mw = ) occurred at GMT on 12 Julyvery close to Okushiri Island, southwest of Hokkaido, Japan. The earth- quake, subsequent tsunamis, landslides, and fires resulted in deaths and 42 missing people.

As this earthquake oc. Both the Japan Sea Earthquake Tsunami and the Hokkaido Nansei-Oki Earthquake Tsunami were surveyed very accurately and in details. The latter was used as the data for an international bench mark test, in which many modelers competed to show the superiority of their numerical by: Four years after the 12 July Hokkaido–Nansei-oki earthquake tsunami, the sedimentary characteristics and facies of the onshore tsunami deposits were examined by the peel and oriented-lunch box sampling methods at Taisei, in an estuary area of the Usubetsu River.

The Southwest Hokkaido Earthquake of Magnitude 7. 9 (J 17 JST) caused serious tsunami disasters in the southwestern part of Hokkaido, particularly on Okushiri Island (a tiny island off the southwest coast of Hokkaido with a population of about 4, at the time of earthquake).

Four years after the 12 July Hokkaido–Nansei-oki earthquake tsunami, the sedimentary characteristics and facies of the onshore tsunami deposits were Author: Futoshi Nanayama. In a half year period oftwo large earthquakes, Kushiro­ oki on January 15 and Hokkaido Nansei-oki on J occurred in Japan causing much damage.

These earthquakes also damaged such agricultural facilities as farm roads, irrigation and drainage canals and pipelines. This paper describes the damageAuthor: S.

Tani. During the Hokkaido-Nansei-Oki Earthquake(M=) of Jthe south-western part of the high-land area of Mt. Komagatake (Fig. 1) suffered liquefaction damage causing differential settlements in 44 wooden houses in Akaigawa-area in Mori Town as reported by the local municipal office.

Similar damages were also found in the.The tsunami caused by the Hokkaido Nansei-Oki Earthquake (M=) on J brought severe damages over wide area along the Japan sea. The topical points of the Hokkaido Nansei-Oki Earthquake tsunami are: (1) This tsunami was generated at a location where earthquakes have not been observed before.(2) The runup of this tsunami records maximum height in the recent years.(3) Effects of Author: Toshifumi Mikami, Hidenori Shibaki, Chiaki Goto.The Kobe Earthquake.

The " Hokkaido Nansei-Oki " Earthquake of J in the Sea of Japan/East Sea. The "Nihonkai-chubu" Earthquake of 26 May in the Sea of Japan. The Earthquake of 20 April in the Ryukyu Islands. MEXICO.