Location

St. Louis, Missouri

Presentation Date

02 Apr 1995

Abstract

A powerful earthquake was caused in the northern region of the Awajishima Island, Japan, on 16 January 1995, and many human lives, structures and facilities suffered fatal damage from the seismic motions in the Hanshin' (Osaka-Kobe) region. The epicenter was located 20 kilometers below the ground surface and the seismic magnitude was 7.2 on Japan Meteorological scale. The aftershocks have been observed in a slender zone oriented to the northeast and stretching to a northern limit on the west-east trending Arima-Takatsuki fault line, which is analogous to the geological area accompanied with the tectonic collapse (Fig. 1).

Department(s)

Civil, Architectural and Environmental Engineering

Meeting Name

3rd International Conference on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics

Publisher

University of Missouri--Rolla

Document Version

Final Version

Rights

© 1995 University of Missouri--Rolla, All rights reserved.

Creative Commons Licensing

Creative Commons License
This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License.

Document Type

Article - Conference proceedings

File Type

text

Language

English

Share

COinS
 
Apr 2nd, 12:00 AM Apr 7th, 12:00 AM

Distribution of Structural Damage in Nishinomiya City and the Eastward Suffered from the Great Hanshin (Hyogoken Nanbu) Earthquake of January 16, 1995

St. Louis, Missouri

A powerful earthquake was caused in the northern region of the Awajishima Island, Japan, on 16 January 1995, and many human lives, structures and facilities suffered fatal damage from the seismic motions in the Hanshin' (Osaka-Kobe) region. The epicenter was located 20 kilometers below the ground surface and the seismic magnitude was 7.2 on Japan Meteorological scale. The aftershocks have been observed in a slender zone oriented to the northeast and stretching to a northern limit on the west-east trending Arima-Takatsuki fault line, which is analogous to the geological area accompanied with the tectonic collapse (Fig. 1).