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The Japan Median Tectonic Line is visible in forms of several outcrops and fault saddles in Ina city, Ōshika village, and Iida city in southern Nagano Prefecture. [9] The historic Akiha Kodo pilgrimage route ( Japan National Route 152 ) between Suwa-taisha shrine in central Nagano Prefecture and the Akihasan shrine in Shizuoka Prefecture ...
Nojima Fault (野島断層, Nojima Dansō) is a fault that was responsible for the Great Hanshin earthquake of 1995 (Kobe Quake). [1] It cuts across Awaji Island , Japan and it is a branch of the Japan Median Tectonic Line which runs the length of the southern half of Honshu island. [ 2 ]
To the northeast of the Idosawa Fault complex lies a separate normal fault trace, which was named the Yunodake Fault (also Yunotake) in 2011.Distanced approx. 50 km (30 mi) from the Fukushima Daiichi Nuclear Power Plant, the fault had been dormant for 120,000–130,000 before it ruptured during the magnitude 7.1 M w Fukushima Hamadori earthquake on 11 April 2011. [4]
see Kantō earthquakes: Sagaing Fault: 1500: Myanmar: Dextral: Active: 1839, May 1930, Dec 1930, 1946, 1956, 2012: Salzach-Ennstal-Mariazell-Puchberg Fault System (SEMP) 400 [6] Austria: Sinistral strike-slip: San Andreas Fault System (Banning fault, Mission Creek fault, South Pass fault, San Jacinto fault, Elsinore fault) 1300: California ...
Envisioned focal area of M9.1 Nankai Trough Megathrust Earthquake, by Headquarters for Earthquake Research Promotion, 2013.. Nankai megathrust earthquakes (Japanese: 南海トラフ巨大地震, Hepburn: Nankai Torafu Kyodai Jishin) are great megathrust earthquakes that occur along the Nankai megathrust – the fault under the Nankai Trough – which forms the plate interface between the ...
Japan sits along the “Ring of Fire,” an arc of volcanoes and fault lines in the Pacific Basin. The country has about 1,500 earthquakes each year strong enough to be felt by people.
Pages in category "Seismic faults of Japan" ... Itoigawa-Shizuoka Tectonic Line; J. Japan Median Tectonic Line; N. Nankai Trough; Neodani Fault; Nojima Fault; S ...
These five subdivisions show interesting differences in earthquake behavior: frequency of earthquakes varying on a 90 to 150-year cycle (Mitsui, et al., 2004; Tanioka et al., 2004), similar slip occurrences along the fault segments, the order of subdivision faulting, and finally, different failure features.