03959nam 22007095 450 991098613200332120250310115239.09783031665745303166574010.1007/978-3-031-66574-5(CKB)37817223600041(MiAaPQ)EBC31955462(Au-PeEL)EBL31955462(DE-He213)978-3-031-66574-5(EXLCZ)993781722360004120250310d2025 u| 0engur|||||||||||txtrdacontentcrdamediacrrdacarrierDeposits of Volcanic Wet Flows Identifying Deposits of Lahars, Debris Avalanches, and Water Floods in Volcanic Terrain /by Thomas C. Pierson, Lee Siebert, Kevin M. Scott1st ed. 2025.Cham :Springer Nature Switzerland :Imprint: Springer,2025.1 online resource (555 pages)Advances in Volcanology, An Official Book Series of the International Association of Volcanology and Chemistry of the Earth’s Interior,2364-32859783031665738 3031665732 Deposits Emplaced by Volcanic Wet Flows -- Scaling and Timing of Volcanic Wet-Flows in Response to Eruptions -- Criteria for Deposit Identification -- Lahars—Process Overview -- Lahar Deposits—Debris-Flow Type -- Lahar Deposits—Hyperconcentrated-Flow Type -- Volcanic Debris Avalanches—Process Overview -- Volcanic Debris-Avalanche Deposits -- Volcanic Water Floods—Process Overview -- Volcanic Water-Flood Deposits -- Other Deposits Containing Volcanic Rock Particles -- Deposit Identification: Key and Summary Tables -- Annotated Outcrop Photographs: Volcanic Wet-Flow Deposits and Other Unconsolidated Volcanic Deposits -- Index.This book strives to fill in the following gaps. First, there is no comprehensive descriptive treatment of deposits emplaced by lahars, debris avalanches, and muddy floods at volcanoes. Second, until now there has not been a comprehensive effort to describe and differentiate the full range of fragmental deposits on volcanoes—the initially wet volcaniclastic mass-flow and fluid-flow deposits usually studied by geomorphologists and sedimentologists, the initially dry pyroclastic mass-flow, fluid-flow, and tephra-fall deposits studied by volcanologists, and the deposits transported and deformed by flowing glacier ice that are studied by glacial geologists. All these deposits are mainly composed of volcaniclastic particles, are deposited on the flanks of volcanoes, all these deposits are mainly composed of volcanic particles and can closely resemble one another. Third, all these processes have vastly different hazard implications, so a means for reliable identification of past processes from deposits is critical for hazard assessment.Advances in Volcanology, An Official Book Series of the International Association of Volcanology and Chemistry of the Earth’s Interior,2364-3285GeologySedimentologyGeomorphologyMineralogyNatural disastersGeologySedimentologyGeomorphologyMineralogyNatural HazardsGeology.Sedimentology.Geomorphology.Mineralogy.Natural disasters.Geology.Sedimentology.Geomorphology.Mineralogy.Natural Hazards.551.21Pierson Thomas C1390447Siebert Lee1155306Scott Kevin M1790675MiAaPQMiAaPQMiAaPQBOOK9910986132003321Deposits of Volcanic Wet Flows4327406UNINA