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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.

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rdf:type
rdfs:label
  • 네오다니 단층 (ko)
  • 根尾谷断層 (ja)
  • Neodani Fault (en)
  • 根尾谷斷層 (zh)
rdfs:comment
  • 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. (en)
  • 네오다니 단층(根尾谷断層)은 일본 기후현 모토스시 (구 네오촌)을 지나는 길이 30 km의 활단층이다. 의 일부인 의 두 단층 중 하나이다. 네오촌 미즈토리 지구의 단층은 일본 국가지정천연기념물로 지정되어 있다. 향후 지진 발생 확률이 거의 없는 Z급 단층으로 지정되어 있다. (ko)
  • 根尾谷断層（ねおだにだんそう）は、岐阜県本巣市根尾地域を中心とする活断層である。市内の水鳥（みどり）地区の断層崖は国指定の特別天然記念物に指定されている。1891年に起きた濃尾地震の地震断層であり、日本最大の地震断層である。地質学的にも貴重である。 (ja)
  • 根尾谷斷層（日语：根尾谷断層（ねおだにだんそう））是一条位于日本岐阜縣本巢市的活断层。日本地質百選。1891年濃尾地震的地震斷層。 (zh)
name
  • Neodani Fault (en)
geo:lat
geo:long
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Neodani_Fault_Relief_Map_(Marked),_SRTM-1.gif
  • http://commons.wikimedia.org/wiki/Special:FilePath/Neodani_fault.jpg
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country
  • Japan (en)
location
  • Gifu Prefecture (en)
state
  • Gifu Prefecture (en)
type
  • left lateral slip fault (en)
georss:point
  • 35.61666666666667 136.6197222222222
has abstract
  • 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. (en)
  • 네오다니 단층(根尾谷断層)은 일본 기후현 모토스시 (구 네오촌)을 지나는 길이 30 km의 활단층이다. 의 일부인 의 두 단층 중 하나이다. 네오촌 미즈토리 지구의 단층은 일본 국가지정천연기념물로 지정되어 있다. 향후 지진 발생 확률이 거의 없는 Z급 단층으로 지정되어 있다. (ko)
  • 根尾谷断層（ねおだにだんそう）は、岐阜県本巣市根尾地域を中心とする活断層である。市内の水鳥（みどり）地区の断層崖は国指定の特別天然記念物に指定されている。1891年に起きた濃尾地震の地震断層であり、日本最大の地震断層である。地質学的にも貴重である。 (ja)
  • 根尾谷斷層（日语：根尾谷断層（ねおだにだんそう））是一条位于日本岐阜縣本巢市的活断层。日本地質百選。1891年濃尾地震的地震斷層。 (zh)
earthquakes
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  • POINT(136.61972045898 35.616664886475)
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