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[null,"1.","Record Nr.",null,"UNINA9910735562203321"]
[null,null,"Titolo",null,"Himalaya : Dynamics of a Giant, Current Activity of the Himalayan Range / / edited by Rodolphe Cattin and Jean-Luc Epard"]
[null,null,"Pubbl/distr/stampa",null,"London, England : , : ISTE Ltd and John Wiley & Sons, Inc., , [2023]"]
[{"$nulls":4},"©2023"]
[null,null,"ISBN",null,"1-394-22868-6"]
[{"$nulls":4},"1-394-22866-X"]
[null,null,"Edizione",null,"[First edition.]"]
[null,null,"Descrizione fisica",null,"1 online resource (314 pages)"]
[null,null,"Disciplina",null,"915.49604"]
[null,null,"Soggetti",null,"Himalaya Mountains Region Description and travel"]
[null,null,"Lingua di pubblicazione",null,"Inglese"]
[null,null,"Formato",null,"Materiale a stampa"]
[null,null,null,"Livello bibliografico","Monografia"]
[null,null,null,"Nota di bibliografia","Includes bibliographical references and index."]
[null,null,"Nota di contenuto",null,"Cover -- Title Page -- Copyright Page -- Contents -- Tributes -- Foreword -- Preface. From Research to Education: The Example of the Seismology at School in Nepal Program -- Part 1. Surface Process -- Chapter 1. Orogenesis and Climate -- 1.1. Introduction -- 1.2.Climate inAsia: present and past -- 1.2.1.Present-dayclimate -- 1.2.2.Cenozoic climate evolution -- 1.3. Reconstructing the paleo-elevation of landforms -- 1.4.The contributionof climatemodeling -- 1.4.1. Impact of orogenesis on the atmospheric circulation -- 1.4.2. Impact of orogenesis on the ocean circulation -- 1.4.3. Impact of orogenesis on the chemical composition of the atmosphere -- 1.5.Conclusion -- 1.6.References -- Chapter 2. Eroding the Himalaya: Processes, Evolution, Implications -- 2.1. Introduction -- 2.2.Main process domains in theHimalaya -- 2.2.1.Himalayanrivers -- 2.2.2.The glaciatedHighRange -- 2.2.3. Critical hillslopes -- 2.3. Extreme events and their contribution to denudation -- 2.4. 1-10 ka timescale and climatic oscillations -- 2.5. Impact of long-term tectonic and climatic evolution over several Ma -- 2.6. Out of the Himalaya: sediment transport and storage from the range to the sedimentarybasin -- 2.7.Conclusion -- 2.8.References -- Part 2. Natural Hazards -- Chapter 3. Glaciers and Glacier Lake Outburst Floods in the Himalaya -- 3.1. Introduction -- 3.2.Glaciers andtheir future -- 3.2.1. The present state of glaciers at a regional scale -- 3.2.2. On the interest of monitoring glaciers -- 3.2.3.What will happen to the Himalayan glaciers and Karakoram glaciers? -- 3.3.Glacier lakes -- 3.3.1. Formation and present distribution of glacier lakes in theHimalaya -- 3.3.2. Historic changes of glacier lake "]
[{"$nulls":4},"abundance and size -- 3.3.3.Projectionsof futureglacier lakes -- 3.4. Glacial lake outburst floods and downstream propagation -- 3.4.1.GLOFtriggers."]
[{"$nulls":4},"3.4.2. Dam breach -- 3.4.3.Floodpropagation -- 3.4.4.Earlywarning -- 3.5.Consequences and impact -- 3.6.Role in landscape formation -- 3.7.Conclusion -- 3.8.References -- Chapter 4. Landsliding in the Himalaya: Causes and Consequences -- 4.1. Introduction -- 4.2. Understanding landsliding and their links to the dynamics of theHimalayanrange -- 4.2.1. Preliminary notions on the mechanics of landsliding -- 4.2.2. Seasonal landsliding caused by monsoons and extreme rainfall -- 4.2.3. Landslide induced by earthquakes and other exceptional perturbations -- 4.2.4.Giant and paleo-landslides -- 4.3.LandslideswithinHimalayansociety -- 4.3.1. Hazard cascades and their societal impact -- 4.3.2. Human activities as an additional trigger of landslides -- 4.3.3. Potential for mitigation -- 4.3.4. Climate change and future landsliding -- 4.4.Conclusion -- 4.5.References -- Chapter 5. Himalayan Surface Rupturing Earthquakes -- 5.1. Introduction -- 5.2. The large devastating earthquakes in the Himalaya -- 5.2.1. Historical chronicles and earthquakes -- 5.2.2. Strong instrumental earthquakes -- 5.3. Surface expression of the seismic deformation in the landscape andwithin paleoseismological excavations -- 5.3.1. In the mesoseismal trace of the 1934 earthquake -- 5.3.2. In the mesoseismal trace of the 1714 earthquake in Bhutan -- 5.3.3. In the mesoseismal trace of the 1950 earthquake -- 5.4. Overview of the paleoseismological excavations along theHimalayanarc -- 5.5. Abandoned alluvial terraces, an archive of the paleoearthquakes -- 5.6.Conclusion -- 5.7.References -- Chapter 6. Seismic Coupling and Hazard Assessment of the Himalaya -- 6.1. Introduction -- 6.2. From current ground motion to the buildup of slip deficit at depth -- 6.2.1. Geodetic observations of the interseismic period -- 6.2.2. Inferring coupling along the MHT with a Bayesian analysis."]
[{"$nulls":4},"6.2.3. Interseismic couplingdistribution -- 6.2.4.Discussion -- 6.3.Seismic potentialof theMHT -- 6.3.1.Conservationof the seismicmoment -- 6.3.2. Magnitude-frequency distribution in the Himalaya -- 6.3.3. Including the physics of fault slip in seismic hazard -- 6.3.4.Seismic potential of theMHT -- 6.4. Seismic hazard in the Himalaya -- 6.4.1. Ground motion prediction equations and Vs30 -- 6.4.2.Modelingscenario events -- 6.4.3. Probabilistic seismic hazard assessment -- 6.4.4. From hazard to risk -- 6.5.Conclusion -- 6.6.References -- Part 3. Focus -- Chapter 7. Recent and Present Deformation of the Western Himalaya -- 7.1. Introduction -- 7.2.Structural styles and tectonic prismmodel -- 7.2.1.Themainstructural zones -- 7.2.2. The Himalaya in the west of the syntax -- 7.2.3. The Himalaya of the Jammu-Kashmir area -- 7.2.4. A structural evolution in agreement with the tectonic prismmodel -- 7.3. Out-of-sequence deformation in the western Himalayan syntax -- 7.3.1. Quaternary out-of-sequence activity of the NW Himalayan thrusts -- 7.3.2. Out-of-sequence seismological and paleoseismological activity in theNWHimalaya -- 7.4. Deformation associated with a ductile décollement, not always aseismic -- 7.4.1. Seismic coupling assessment along the MHT -- 7.4.2. Occurrence of ruptures on asperities -- 7.4.3. Transition between thin-skin and thick-skin tectonics -- 7.5.Conclusion -- 7.6.References -- Chapter 8. The 2015 April 25 Gorkha Earthquake -- 8.1. Introduction -- 8.2. The mainshock and its effects on the ground -- 8.2.1. Overview description of the mainshock -- 8.2.2. Ground motion and deformation -- 8.3. Investigatingthe seismic source at depth -- 8.4.Aftershockactivity andpost-seismic relaxation -- 8.4.1. Early aftershocks and the "]
[{"$nulls":4},"occurrence of the Kodari earthquake -- 8.4.2. Seismicity monitored by denser, dedicated temporary networks."]
[{"$nulls":4},"8.4.3. Post-seismic relaxation monitored by geodetic and seismological networks -- 8.5. A more earthquake-informed and earthquake-resilient local community in the aftermath of the earthquake -- 8.6.Conclusion -- 8.7.References -- Chapter 9. Crustal Fluids in the Nepal Himalaya and Sensitivity to the Earthquake Cycle -- 9.1. Introduction -- 9.2. Overview of thermal springs geochemistry in Nepal -- 9.3. Overview of gaseous emission zones in Nepal -- 9.4.Spatial organizationof crustalfluid release -- 9.5. Temporal variations of crustal fluid release: a tectonic control -- 9.6.Conclusion -- 9.7.References -- Conclusion -- List of Authors -- Index -- Summaries of other volumes -- EULA."]
[null,null,null,"Sommario/riassunto","The Himalaya is well known as the largest and highest mountain belt on Earth. Advances in geoscience over the past few decades have revealed a complex picture of the dynamics of this giant, opening up questions about the initial stages of Himalayan building, lateral variations in its structures, variations in tectonic forcing, tectonic-climate coupling and assessments of the natural hazards affecting this area. In this three-volume book, we present the current knowledge on the building and present-day behavior of the Himalayan range. The objective is not to be exhaustive, but to provide some key elements used by researchers to unravel the many processes acting in the Himalayan dynamics. Mountain environments are at the forefront of climate change with glacier retreat, landslides, flash floods and water availability. Understanding the delicate balance that controls the dynamics of the Himalayan giant is now, more than ever, a major challenge for the scientific community."]