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Home > Art, Film & Photography > Fracture Zones: Mendocino Fracture Zone, Blanco Fracture Zone, Owen Fracture Zone, Diamantina Fracture Zone, Easter Fracture Zone
Fracture Zones: Mendocino Fracture Zone, Blanco Fracture Zone, Owen Fracture Zone, Diamantina Fracture Zone, Easter Fracture Zone

Fracture Zones: Mendocino Fracture Zone, Blanco Fracture Zone, Owen Fracture Zone, Diamantina Fracture Zone, Easter Fracture Zone


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Chapters: Mendocino Fracture Zone, Blanco Fracture Zone, Owen Fracture Zone, Diamantina Fracture Zone, Easter Fracture Zone, Sovanco Fracture Zone, Shackleton Fracture Zone, Panama Fracture Zone. Source: Wikipedia. Pages: 30. Not illustrated. Free updates online. Purchase includes a free trial membership in the publisher's book club where you can select from more than a million books without charge. Excerpt: The Mendocino Fracture Zone is a fracture zone and transform boundary off the coast of Cape Mendocino in far northern California. It runs westward from a triple junction with the San Andreas Fault and the Cascadia subduction zone to the southern end of the Gorda Ridge. It continues on west of its junction with the Gorda Ridge, as an inactive remnant section which extends for several hundred miles. Technically, a fracture zone is not a transform fault, but in the case of the Mendocino, the term has been loosely applied to the active fault segment east of the Gorda Ridge as well as to the true fracture zone segment west of it. Many seismologists refer to the active segment as the Mendocino Fault or Mendocino fault zone. The fault section demarcates the boundary between the northwestward-moving Pacific Plate and the eastward-moving Gorda Plate. The Gorda Plate is subducting beneath the North American Plate just offshore of Cape Mendocino. Where the Mendocino Fault intersects the undersea trench of the subduction zone, it also meets the San Andreas Fault. This seismically active intersection is called a triple junction, and specifically the Mendocino Triple Junction. Robert W. Pease observed in 1965 that the alignment of a transverse tectonic zone extending from Mount Lassen to the Walker Lane at the north end of Honey Lake Fault, suggests it was once the continental terminus of the Mendocino Fault. It forms the boundary of the Modoc Plateau and Columbia Plateau provinces with the Great Basin. Where it meets Honey Lake Faul...More: http: //booksllc.net/?id=301327


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Product Details
  • ISBN-13: 9781157204763
  • Publisher: Books LLC
  • Publisher Imprint: Books LLC
  • Height: 152 mm
  • Sub Title: Mendocino Fracture Zone, Blanco Fracture Zone, Owen Fracture Zone, Diamantina Fracture Zone, Easter Fracture Zone
  • Width: 229 mm
  • ISBN-10: 1157204767
  • Publisher Date: 15 Sep 2010
  • Binding: Paperback
  • Spine Width: 2 mm
  • Weight: 59 gr


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