enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  2. List of fault zones - Wikipedia

    en.wikipedia.org/wiki/List_of_fault_zones

    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, United States. Dextral strike-slip.

  3. 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 ...

  4. 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 ...

  5. 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 ...

  6. 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 ...

  7. Fault (geology) - Wikipedia

    en.wikipedia.org/wiki/Fault_(geology)

    A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. [3] [4] A fault zone is a cluster of parallel faults.

  8. Okhotsk microplate - Wikipedia

    en.wikipedia.org/wiki/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 Eastern edge of the ...

  9. Ring of Fire - Wikipedia

    en.wikipedia.org/wiki/Ring_of_Fire

    Diagram of the geological process of subduction. The Ring of Fire (also known as the Pacific Ring of Fire, the Rim of Fire, the Girdle of Fire or the Circum-Pacific belt) [ note 1 ] is a tectonic belt of volcanoes and earthquakes. It is about 40,000 km (25,000 mi) long [ 1 ] and up to about 500 km (310 mi) wide, [ 2 ] and surrounds most of the ...