Neodani Fault
根尾谷断層
One of the places locals name first when asked what to see here.
Photos
Photos from Wikimedia Commons — click any image for the photographer and licence.
What this place is
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. The quake was the largest ever recorded in inland Japan.
Background text from Wikipedia (CC BY-SA)
Why it is worth the trip
- A setting that gives you the character of the area in a single visit.
- Scenery and detail that shift with the season, the weather and the time of day.
- Easy to combine with other stops nearby, so it works as the anchor of a half-day plan.
What you can do here
- Take the main viewpoint first, then explore the quieter edges most visitors skip.
- Read the on-site information boards — they usually explain far more than online listings.
- Photograph in the early morning or late afternoon for the best light and fewest people.
- Pair the visit with a nearby café, market or hot spring to round out the trip.
Getting there
We do not have step-by-step transit directions for this spot yet. Open the location on Google Maps for routes from where you are staying.
Good to know before you go
- Check the last admission and last bus/train before you go; rural services stop early.
- Carry cash — smaller sites and rural transport may not accept cards or IC.
- Weekday mornings are consistently the calmest time to visit.
Traveler reviews
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