Home > General > Natural History of Washington (U.S. State): Coast Range ARC, Puget Sound Convergence Zone, Armillaria Ostoyae, Hoh Rain Forest
Natural History of Washington (U.S. State): Coast Range ARC, Puget Sound Convergence Zone, Armillaria Ostoyae, Hoh Rain Forest

Natural History of Washington (U.S. State): Coast Range ARC, Puget Sound Convergence Zone, Armillaria Ostoyae, Hoh Rain Forest

          
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About the Book

Purchase includes free access to book updates online and a free trial membership in the publisher's book club where you can select from more than a million books without charge. Chapters: Coast Range Arc, Puget Sound Convergence Zone, Armillaria Ostoyae, Hoh Rain Forest, Golden Gardens Park, British Columbia Mainland Coastal Forests, Hall of Mosses, Arid Lands Ecology Reserve, Omineca Arc, Wenas Creek Mammoth. Excerpt: The Coast Range Arc was a large volcanic arc system, extending from northern Washington through British Columbia and the Alaska Panhandle to southwestern Yukon. The Coast Range Arc lies along the western margin of the North American Plate in the Pacific Northwest of western North America. Although taking its name from the Coast Mountains, this term is a geologic grouping rather than a geographic one, and the Coast Range Arc extended south into the High Cascades of the Cascade Range, past the Fraser River which is the northward limit of the Cascade Range proper. The Coast Range Arc formed as a result of subduction of the Kula and pre-existing Farallon Plates. It is most famous for being the largest granitic outcropping in North America, which then it is usually referred to as the Coast Plutonic Complex or the Coast Mountains Batholith. It is a coast-parallel continential volcanic arc similar to the Andes of South America and the largest continential volcanic arc fossil in the world. Plate tectonics of the Coast Range Arc about 75 million years agoVolcanism in the arc began during the Late Cretaceous period 100 million years ago based on andesitic composition of the Early Cretaceous volcanic sections and their close temporal and spatial association with masses of felsic intrusive igneous rock with phaneritic texture called tonalite. The basement of the Coast Range Arc was likely Early Cretaceous and Late Jurassic intrusions. Stratigraphic and field relations in the arc suggest that the Coast Range Arc was creat... More: http://booksllc.net/?id=19197721


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Product Details
  • ISBN-13: 9781157298267
  • Publisher: Books LLC
  • Publisher Imprint: Books LLC
  • Height: 152 mm
  • No of Pages: 34
  • Series Title: English
  • Weight: 63 gr
  • ISBN-10: 1157298265
  • Publisher Date: 29 May 2010
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Spine Width: 2 mm
  • Width: 229 mm

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