enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  2. Nojima Fault - Wikipedia

    en.wikipedia.org/wiki/Nojima_Fault

    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] The fault line itself and part of the damage caused by the ...

  3. Nankai megathrust earthquakes - Wikipedia

    en.wikipedia.org/wiki/Nankai_megathrust_earthquakes

    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 subducting Philippine Sea Plate and the overriding Amurian Plate (part of the Eurasian Plate), which dips beneath southwestern ...

  4. Nankai Trough - Wikipedia

    en.wikipedia.org/wiki/Nankai_Trough

    The Nankai Trough (南海トラフ, Nankai Torafu, Southern Sea Trough) is a submarine trough located south of the Nankaidō region of Japan 's island of Honshu, extending approximately 900 km (559 mi) offshore. The underlying fault, the Nankai megathrust, is the source of the devastating Nankai megathrust earthquakes, while the trough itself ...

  5. Wadati–Benioff zone - Wikipedia

    en.wikipedia.org/wiki/Wadati–Benioff_zone

    A primary example of this is located along Japan's largest island of Honshu, where the Wadati–Benioff zone is characterized by two well-defined lines of earthquake foci, with a distance between each line of 30–40 kilometers. [11] A study of the global prevalence of double Benioff zones has found that they are common in subduction zones ...

  6. Cascadia subduction zone - Wikipedia

    en.wikipedia.org/wiki/Cascadia_subduction_zone

    45°N124°W / 45°N 124°W The Cascadia subduction zone is a 960 km (600 mi) fault at a convergent plate boundary, about 100–200 km (70–100 mi) off the Pacific coast, that stretches from northern Vancouver Island in Canada to Northern California in the United States. It is capable of producing 9.0+ magnitude earthquakes and tsunamis ...

  7. Okinawa Plate - Wikipedia

    en.wikipedia.org/wiki/Okinawa_Plate

    Okinawa Plate. The Okinawa Plate, or Okinawa Platelet, is a minor continental tectonic plate in the northern and eastern hemispheres stretching from the northern end of Taiwan to the southern tip of the island of Kyūshū. [ 1 ][ 2 ] The Okinawa Plate hosts typical earthquakes, like the 1911 Kikai Island earthquake, and various types of slow ...

  8. Okhotsk microplate - Wikipedia

    en.wikipedia.org/wiki/Okhotsk_microplate

    Okhotsk microplate. The Okhotsk microplate[ 1 ] is a proposed minor tectonic plate covering the Kamchatka Peninsula, Magadan Oblast, and Sakhalin Island of Russia; Hokkaido, Kantō and Tōhoku regions of Japan; the Sea of Okhotsk, as well as the disputed Kuril Islands. Japan's principal fault system is the zone where the Amurian microplate, the ...

  9. Category:Seismic faults of Japan - Wikipedia

    en.wikipedia.org/wiki/Category:Seismic_faults_of...

    U. Urasoko fault. Categories: Seismic faults by country. Geology of Japan. Seismic faults of Asia. Hidden category: Commons category link is on Wikidata.