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Home > Art, Film & Photography > Cinder Cones of Canada: Tseax Cone, Nazko Cone, Itcha Range, Atlin Volcanic Field, Kostal Cone, Volcano Mountain, Nahta Cone
Cinder Cones of Canada: Tseax Cone, Nazko Cone, Itcha Range, Atlin Volcanic Field, Kostal Cone, Volcano Mountain, Nahta Cone

Cinder Cones of Canada: Tseax Cone, Nazko Cone, Itcha Range, Atlin Volcanic Field, Kostal Cone, Volcano Mountain, Nahta Cone


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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: 100. Not illustrated. Chapters: Tseax Cone, Nazko Cone, Itcha Range, Atlin Volcanic Field, Kostal Cone, Volcano Mountain, Nahta Cone, Iskut-Unuk River Cones, Ibex Mountain, Opal Cone, Alligator Lake Volcanic Complex, Cinder Cone, Kitasu Hill, Cocoa Crater, Satah Mountain, Eve Cone, Cracker Creek Cone, Williams Cone, Gabrielse Cone, Volcanic Creek Cone, Cinder Mountain, Dragon Cone, Coffee Crater, Sidas Cone, Desolation Lava Field, Buck Hill, Big Timothy Mountain, Machmell River Cone, Pointed Stick Cone, Storm Cone, Sleet Cone, Cinder Cliff, Moraine Cone, Ridge Cone, Twin Cone, Cache Hill, Camp Hill, Triplex Cone, Kana Cone, the Saucer, Ne Ch'e Ddhawa. Excerpt: Tseax Cone - Volcanic rock erupted from the Tseax ConeThe Tseax Cone has been the site of some of the youngest volcanic eruptions in Canada. It has been active at least twice in the past few hundred years and other remnants of lava flows exist in the area. It is 290 m (951 ft) in diameter at its base and rests on the remnants of an earlier and somewhat larger, dissected, 460 m (1,509 ft) diameter cone. The volcano is made of volcanic bombs and cinders with a crater at its summit where a churning lava lake ponded and overflowed its rim during the 18th century. Volcanism at the Tseax Cone is caused by the rifting of the Earth's crust where two parts of the North American Plate are breaking apart. The cause of this rifting is the result of the Pacific Plate sliding northward along the Queen Charlotte Fault, on its way to the Aleutian Trench. The lava emitted in eruptions at the Tseax Cone is fluid. Its lavas are made of basalt, a common grey to black or dark brown extrusive volcanic rock low in silica content (the lava is mafic) that is usually fine-grained due to rapid cooling of lava on the Earth's surface. Phoehoe is found at the volcano, which have a smooth, billowy, undu...


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Product Details
  • ISBN-13: 9781155521909
  • Publisher: Books LLC
  • Publisher Imprint: Books LLC
  • Height: 229 mm
  • No of Pages: 102
  • Spine Width: 6 mm
  • Weight: 159 gr
  • ISBN-10: 1155521900
  • Publisher Date: 15 Sep 2010
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Sub Title: Tseax Cone, Nazko Cone, Itcha Range, Atlin Volcanic Field, Kostal Cone, Volcano Mountain, Nahta Cone
  • Width: 152 mm


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