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Home > Art, Film & Photography > Landforms of Runion: Headlands of Runion, Lakes of Runion, Mountains of Runion, Rivers of Runion, Volcanoes of Runion
Landforms of Runion: Headlands of Runion, Lakes of Runion, Mountains of Runion, Rivers of Runion, Volcanoes of Runion

Landforms of Runion: Headlands of Runion, Lakes of Runion, Mountains of Runion, Rivers of Runion, Volcanoes of Runion


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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: Headlands of Runion, Lakes of Runion, Mountains of Runion, Rivers of Runion, Volcanoes of Runion, Piton de La Fournaise, Piton Des Neiges, Grand tang, tang de Bois Rouge, Pointe Des Aigrettes, Cape Bernard, Gros Morne, Runion, Rivire Des Marsouins, List of Rivers of Runion, Rivire Des Roches, Rivire Saint-Denis, Rivire de L'est, Rivire Du M¢t, Rivire Des Remparts, Rivire Des Galets, Pointe Des Galets. Excerpt: Piton de la Fournaise - Wikipedia, the free encyclopedia The top part of the volcano is occupied by the Enclos Fouch, a caldera 8 kilometres (5 miles) wide. High cliffs known as remparts form the caldera's rim. The caldera is breached to the southeast into the sea. It is also unstable and in the initial stages of failure and will eventually collapse into the Indian Ocean. Whether it will generate a so called "megatsunami" is controversial. There is evidence on the submerged flanks and abyssal plain of earlier failures. The lower slopes are known as the Grand Brl ("Great Burnt"). Most lava eruptions are confined to the caldera. Inside the caldera is a 400 metre high lava shield known as Dolomieu. Atop the lava shield are Bory Crater (Cratre Bory) and Dolomieu Crater (Cratre Dolomieu), which is by far the wider of the two. Topographic map showing the volcano and surrounding terrain.Many craters and spatter cones can be found inside the caldera and the outer flanks of the volcano. At the beginning of the path that leads to the summit, there lies a noticeable small crater known as formica leo, named for its similar shape to the pitfall built by the antlion. Some of the beaches there are of a greenish colour, because of the olivine sand resulting from picrite basalt lavas. The Grand Brl is formed from solidified lava ... More: http://booksllc.net/?id=962520


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Product Details
  • ISBN-13: 9781158024360
  • Publisher: Books LLC
  • Publisher Imprint: Books LLC
  • Height: 152 mm
  • No of Pages: 46
  • Spine Width: 3 mm
  • Weight: 82 gr
  • ISBN-10: 1158024363
  • Publisher Date: 12 Jun 2010
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Sub Title: Headlands of Runion, Lakes of Runion, Mountains of Runion, Rivers of Runion, Volcanoes of Runion
  • Width: 229 mm


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