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Home > Art, Film & Photography > Basins: Depressions (Geology), Drainage Basins, Oceanic Basins, Caldera, Impact Crater, Qattara Depression, Oceanic Trench, Haor
Basins: Depressions (Geology), Drainage Basins, Oceanic Basins, Caldera, Impact Crater, Qattara Depression, Oceanic Trench, Haor

Basins: Depressions (Geology), Drainage Basins, Oceanic Basins, Caldera, Impact Crater, Qattara Depression, Oceanic Trench, Haor


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About the Book

Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Pages: 51. Chapters: Depressions (geology), Drainage basins, Oceanic basins, Caldera, Impact crater, Qattara Depression, Oceanic trench, Haor, List of drainage basins by area, Endorheic basin, Foreland basin, Bodele Depression, Turpan Depression, Subsidence, Kettle, List of places on land with elevations below sea level, Landslip Hill, Drainage system, Beel, L'Atalante basin, Maar, Graben, Laguna Salada, Drainage divide, Blowout, Structural basin, Upemba Depression, Gyeongju Basin, List of watershed topics, Tsushima Basin, Sink, Godzareh depression, Oslo Graben, Arabian Basin, George VI Sound, Bentley Subglacial Trench, Great South Basin, Turan Depression, North Polar Basin, Kalahari Basin, Aleutian Basin, Eurasian Basin, Amerasian Basin, Wharton Basin, Aoukar Depression, Jeanne d'Arc Basin, Nordenskjold Basin, Atlantic-Indian Basin. Excerpt: The oceanic trenches are hemispheric-scale long but narrow topographic depressions of the sea floor. They are also the deepest parts of the ocean floor. Trenches define one of the most important natural boundaries on the Earth's solid surface: the one between two lithospheric plates. There are three types of lithospheric plate boundaries: divergent (where lithosphere and oceanic crust is created at mid-ocean ridges), convergent (where one lithospheric plate sinks beneath another and returns to the mantle), and transform (where two lithospheric plates slide past each other). Trenches are a distinctive morphological feature of plate boundaries. Along convergent plate boundaries, plates move together at rates that vary from a few mm to over ten cm per year. A trench marks the position at which the flexed, subducting slab begins to descend beneath another lithospheric slab. Trenches are generally parallel to a volcanic island arc, and about 200 km (120 mi) from a volcanic arc. Oceanic trenches typicall...


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Product Details
  • ISBN-13: 9781157446569
  • Publisher: Books LLC, Wiki Series
  • Publisher Imprint: Books LLC, Wiki Series
  • Height: 246 mm
  • No of Pages: 52
  • Spine Width: 3 mm
  • Weight: 109 gr
  • ISBN-10: 1157446566
  • Publisher Date: 05 Jul 2011
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Sub Title: Depressions (Geology), Drainage Basins, Oceanic Basins, Caldera, Impact Crater, Qattara Depression, Oceanic Trench, Haor
  • Width: 189 mm


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