Home  

Random  

Nearby  



Log in  



Settings  



Donate  



About Wikipedia  

Disclaimers  



Wikipedia





Neodani Fault





Article  

Talk  



Language  

Watch  

Edit  





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]

Neodani Fault
LocationGifu Prefecture
Coordinates35°37′00N 136°37′11E / 35.61667°N 136.61972°E / 35.61667; 136.61972
CountryJapan
StateGifu Prefecture
Tectonics
Earthquakes1891 Mino-Owari earthquake
Typeleft lateral slip fault
This fault can be seen as a step portion in the center of the photo.
Neodani Fault.

See also

edit

References

edit
  1. ^ "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.
edit


  • t
  • e

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Neodani_Fault&oldid=1193175383"
     



    Last edited on 2 January 2024, at 12:55  





    Languages

     






     

    Wikipedia


    This page was last edited on 2 January 2024, at 12:55 (UTC).

    Content is available under CC BY-SA 4.0 unless otherwise noted.



    Privacy policy

    About Wikipedia

    Disclaimers

    Contact Wikipedia

    Code of Conduct

    Developers

    Statistics

    Cookie statement

    Terms of Use

    Desktop