Neodani Fault
Left lateral split fault in Gifu Prefecture, Japan
35°37′00″N 136°37′11″E / 35.61667°N 136.61972°E / 35.61667; 136.61972![](http://upload.wikimedia.org/wikipedia/commons/thumb/c/c0/Neodani_Fault_Relief_Map_%28Marked%29%2C_SRTM-1.gif/220px-Neodani_Fault_Relief_Map_%28Marked%29%2C_SRTM-1.gif)
Neodani Fault (根尾谷断層, Neodani Dansō) is a left lateral slip fault in central Japan, Gifu Prefecture, which ruptured causing the 1891 Mino–Owari earthquake (otherwise known as the Nōbi earthquake) in 1891. It caused a 6m vertical offset and 8m left lateral offset, and ruptured over 80 km.[1] The quake was the largest ever recorded in inland Japan.[citation needed]
See also
References
- ^ "Long-Term Seismic Behavior of a Fault Involved in a Multiple-Fault Rupture: Insights from Tectonic Geomorphology along the Neodani Fault, Central Japan" (PDF). Archived from the original (PDF) on 23 Jul 2011. Retrieved 19 May 2021.
External links
![](http://upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/30px-Commons-logo.svg.png)
Wikimedia Commons has media related to Neodani Fault.
- Seismic Faults Observation & Experience House
- Long-Term Seismic Behavior of a Fault Involved in a Multiple-Fault Rupture: Insights from Tectonic Geomorphology along the Neodani Fault, Central Japan
- v
- t
- e