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Neodani Fault (根尾谷断層,
Neodani Dansō) is a left
lateral slip
fault in
central ****an, Gifu Prefecture,
which ruptured causing the 1891 Mino–Owari earthquake...
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October 28, 1891 8.0 ML 7,273 1891 Mino–Owari
earthquake 濃尾地震 Nōbi
Jishin Neodani Fault June 20, 1894 6.6 ML 31 1894
Tokyo earthquake 明治東京地震 Meiji-Tokyo...
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accretionary complexes of Jur****ic
period or younger.
Urasoko fault ****ozu
Fault Neodani Fault Nojima Fault Hida
orogenic belt (Hida
Mountains and Ryōhaku Mountains)...
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Nukumi segment ran 20 km (12 mi) with a
maximum offset of 3 m (9.8 ft). The
Neodani and
Umehara faults had
rupture lengths of 35 km (22 mi) and 25 km (16 mi)...
- The
declination is
called the Nōbi Tilt (濃尾傾動運動 Nōbi Keidō Undō). The
Neodani Fault running through the
central part of the Nōbi
Plain was the cause...
-
photographs of the
Neodani Fault when he
investigated the 1891 Mino–Owari earthquake.
Kotoite (小藤石) 1891 Mino–Owari
earthquake (
Neodani Fault) 367日誕生日大事典...
- Honshū, ****an
Subduction zone
Active see
Nankai megathrust earthquakes Neodani Fault ****an Oblique-slip
Active 1891 Mino–Owari (M8.0) New
Madrid Fault...
- 85″E / 36.1477000°N 137.6246806°E / 36.1477000; 137.6246806
Neodani Fault (根尾谷断層,
neodani dansō) — — 3.5 Gifu MotosuMotosu, Gifu 35°37′1.62″N 136°37′14...
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Ikoma City, Nara Enshō-ji:
Great Nobi
Earthquake (Enshoji
Temple in
ruins at
Neodani Kinbara)
Archived 2011-07-22 at the
Wayback Machine, Gifu Prefecture...
- ISBN 0-231-04940-4 Enshō-ji, Gifu Prefecture:
Great Nobi
Earthquake (Enshoji
Temple in
ruins at
Neodani Kinbara)
Archived 2011-07-22 at the
Wayback Machine...