From Surf Wiki (app.surf) — the open knowledge base
1946 Nankai earthquake
Magnitude 8.1–8.4 earthquake in Nankaidō, Japan
Magnitude 8.1–8.4 earthquake in Nankaidō, Japan
| Field | Value | |
|---|---|---|
| title | 1946 Nankai earthquake | |
| image | 1946 Nankai Earthquake (12).jpg | |
| local-date | ||
| local-time | 04:19 JST | |
| timestamp | 1946-12-20 19:19:10 | |
| map | 1946 Nankai earthquake intensity.png | |
| map2 | {{Location map | Japan |
| lat | 33.0 | |
| long | 135.6 | |
| mark | Bullseye1.png | |
| marksize | 40 | |
| position | top | |
| width | 260 | |
| float | center | |
| relief | yes}} | |
| anss-url | iscgem898698 | |
| isc-event | 898698 | |
| magnitude | ||
| depth | 30 km | |
| location | ||
| countries affected | Japan | |
| fault | Nankai megathrust | |
| tsunami | Yes | |
| casualties | At least 1362 dead, 2600 injured and 100 missing |
|local-date= |local-time= 04:19 JST |anss-url = iscgem898698 |isc-event = 898698 The 1946 Nankai earthquake (昭和南海地震 Shōwa Nankai jishin) was a great earthquake in Nankaidō, Japan. It occurred on December 21, 1946, at 04:19 JST (December 20, 19:19 UTC). The earthquake measured between 8.1 and 8.4 on the moment magnitude scale, and was felt from Northern Honshū to Kyūshū. It occurred almost two years after the 1944 Tōnankai earthquake, which ruptured the adjacent part of the Nankai megathrust.
Geology
The Nankai Trough is a convergent boundary where the Philippine Sea plate is being subducted beneath the Eurasian plate. Large earthquakes have been recorded along this zone since the 7th century, with a recurrence time of 100 to 200 years.
Earthquake
The 1946 Nankai earthquake was unusual in its seismological perspective, with a rupture zone estimated from long-period geodetic data that was more than twice as large as that derived from shorter period seismic data. In the center of this earthquake rupture zone, scientists used densely deployed ocean bottom seismographs to detect a subducted seamount 13 km thick by 50 km wide at a depth of 10 km. Scientists propose that this seamount might work as a barrier inhibiting brittle seismogenic rupture.
Casualties and damage
The earthquake caused extensive damage, destroying 36,000 homes in southern Honshū alone. The earthquake also caused a huge tsunami that took out another 2,100 homes with its 5 - waves.
References
References
- National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information.. (1972). "Significant Earthquake Information". NOAA National Centers for Environmental Information.
- (13 March 2008). "The 1946 Nankaido earthquake". United States Geological Survey.
- (2000). "Subducted Seamount Imaged in the Rupture Zone of the 1946 Nankaido Earthquake". [[American Association for the Advancement of Science]].
- Kanamori, H.. (1972). "Tectonic implications of the 1944 Tonankai and the 1946 Nankaido earthquakes". [[Elsevier]].
This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.
Ask Mako anything about 1946 Nankai earthquake — get instant answers, deeper analysis, and related topics.
Research with MakoFree with your Surf account
Create a free account to save articles, ask Mako questions, and organize your research.
Sign up freeThis content may have been generated or modified by AI. CloudSurf Software LLC is not responsible for the accuracy, completeness, or reliability of AI-generated content. Always verify important information from primary sources.
Report