Public (O) | ||
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Session Sub-category | Public | |
Session ID | O-09 | |
Title | Mechanism of the 2024 Noto Peninsula Earthquake and its disaster | |
Short Title | 2024 Noto Peninsula Earthquake | |
Main Convener | Name | Takashi Azuma |
Affiliation | National Institute of Advanced Industrial Science and Technology | |
Co-Convener 1 | Name | Dan Matsumoto |
Affiliation | National Institute of Advanced Industrial Science and Technology | |
Co-Convener 2 | Name | Atsuko Nonomura |
Affiliation | Kagawa University | |
Co-Convener 3 | Name | Kazuo Tamura |
Affiliation | ||
Session Language |
J |
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Scope |
We believe the Earth is stable, but sometimes it causes huge disasters to human life. The Noto-Hanto Earthquake (M 7.6) and tsunami occurred in the evening on the first day of the new year in 2024 when people had a peaceful time with their families. Houses, buildings, and constructions were destroyed and damaged by strong grand motions, tsunamis, slope failures, and liquefactions. Electric power and water supply were shut down for a long time. These situations made rescue and support operations difficult. In this session, we discuss the mechanism of the 2024 Noto-Hanto Earthquake and its disasters, as well as how earth science would contribute to earthquake disaster mitigation. |
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Presentation Format | Oral and Poster presentation |
Time | Presentation No | Title | Presenter |
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Oral Presentation May 25 PM1 | |||
13:55 - 14:15 | O09-01 | Overview of damage to buildings in the 2024 Noto Peninsula Earthquake | Kazuo Tamura |
14:15 - 14:35 | O09-02 | Investigation of Tsunami Damage and Occurrence Mechanisms in the 2024 Noto Peninsula Earthquake | Taro Arikawa |
14:35 - 14:55 | O09-03 | Coseismic landslides in the 2024 Noto Peninsula Earthquake | Yuki Matsushi |
14:55 - 15:15 | O09-04 | Strong ground motions and site amplifications in relation to the structural damage ratios during the 2024 Noto Hanto earthquake | Hiroshi Kawase |
Oral Presentation May 25 PM2 | |||
15:30 - 15:50 | O09-05 | Earthquake activity in the Noto Peninsula during 2020-2024 deduced from geodetic observations | Takuya NISHIMURA |
15:50 - 16:10 | O09-06 | Relationship between the uplift caused by the 2024 Noto Peninsula earthquake and past coseismic uplifts | Masanobu Shishikura |
16:10 - 16:30 | O09-07 | Submarine active faults around the northern part of Noto Peninsula | Takahiko Inoue |
16:30 - 16:50 | O09-08 | Event deposits recorded in the coastal lowlands of the Ishikawa and Toyama areas | Atsushi Urabe |