Incorporation of Variable Bed Friction into Titan2D Mass-Flow Model : Application to Little Tahoma Peak Avalanches (Washington)

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• Articoli dello stesso fascicolo (disponibili singolarmente)

  • Introduction
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  • Seismic Recordings of Ice and Debris Avalanches of Iliamma Volcano (Alaska)
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  • The June 2001 Rainfall-Induced Landslides and Associated Lahars at Aso Volcano (Southwestern Japan)
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  • Late Pleistocene Deposits Associated with a Southern Flank Collapse of the Nevado del Huila Volcanic Complex (Colombia)
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  • Substrata Influence in the Transport and Emplacement Mechanism of the Ollagüe Debris Avalanche (Northern Chile)
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  • Geology and Stability of the Southern Flank of Irazu Volcano (Costa Rica)
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  • Character, Stratigraphy and Magnitude of Historical Lahars of Cotopaxi Volcano (Ecuador)
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  • A Pleistocene Stacked Succession of Volcaniclastic Mass Flows in Central Colombia
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  • Morphological Evolution of La Concepción Valley by Huge Mass Movements on Plateau Edges in the Eastern Part of the Mexican Volcanic Belt (Xalapa, Veracruz, Mexico)
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  • Tsunami-Induced Conglomerates and Debris-Flow Deposits on the Western Coast of Gran Canaria (Canary Islands)
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  • Palaeohydraulic Analysis of the 1953 Tangiwai Lahar ; New Zealand's Worst Volcanic Disaster
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  • Incorporation of Variable Bed Friction into Titan2D Mass-Flow Model
  • Volcanic Risk and Evolution of the Territorial System in the Volcanic Areas of Campania
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• Informazioni

  Codice DOI: 10.1400/19102

  ISSN: 1724-0425

  Permalink: http://digital.casalini.it/10.1400/19102