Anatomy of a Catastrophe: Reconstructing the 1936 Rock Fall and Tsunami Event in Lake Lovatnet, Western Norway

Rock falls and landslides plunging into lakes or small reservoirs can result in tsunamis with extreme wave run-ups. The occurrence of these natural hazards in populated areas have encouraged a recent sharp increase of studies that aim to mitigate their impact on human lives and assess infrastructure...

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Main Authors: Nicolas Waldmann, Kristian Vasskog, Guy Simpson, Emmanuel Chapron, Eivind Wilhelm Nagel Støren, Louise Hansen, Jean-Luc Loizeau, Atle Nesje, Daniel Ariztegui
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-05-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.671378/full
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author Nicolas Waldmann
Kristian Vasskog
Kristian Vasskog
Guy Simpson
Emmanuel Chapron
Eivind Wilhelm Nagel Støren
Eivind Wilhelm Nagel Støren
Louise Hansen
Jean-Luc Loizeau
Atle Nesje
Daniel Ariztegui
author_facet Nicolas Waldmann
Kristian Vasskog
Kristian Vasskog
Guy Simpson
Emmanuel Chapron
Eivind Wilhelm Nagel Støren
Eivind Wilhelm Nagel Støren
Louise Hansen
Jean-Luc Loizeau
Atle Nesje
Daniel Ariztegui
author_sort Nicolas Waldmann
collection DOAJ
description Rock falls and landslides plunging into lakes or small reservoirs can result in tsunamis with extreme wave run-ups. The occurrence of these natural hazards in populated areas have encouraged a recent sharp increase of studies that aim to mitigate their impact on human lives and assess infrastructure lost. This paper amalgamates in a novel fashion and at an unprecedented detail in situ historic measurements, geological data and numerical modeling of a rock fall event and associated tsunami wave that occurred in Lake Lovatnet (western Norway) in September 1936. Historical records report an event that released ca. 1 million m3 of rocks and debris from Ramnefjellet Mountain at an altitude of 800 m above Lake Lovatnet. The fragmented material plunged into the lake, causing a tsunami that reached a maximum run-up of 74 m and killed 74 people. In fact, the settlements of Bødal and Nesdal were wiped out as a result of the catastrophic wave. Sediments resulting from the 1936 rock fall and associated tsunami were identified in the subsurface of Lake Lovatnet by shallow geophysical investigations and were retrieved using gravity coring equipment. A set of high resolution physical and geochemical measurements were carried out on the cores with the aim of reproducing a highly detailed reconstruction of this catastrophic event in order to better understand and learn about the processes involved. The cores were retrieved in the northwestern sub-basin of the lake and its chronology was constrained by 210Pb and radiocarbon dating. A specially tailored physically based mathematical model was applied to better understand the tsunami event. Integration of the geophysical record, the sedimentological data and numerical modeling provide a comprehensive background to better understand the effects of such event in a deep fjord-like lacustrine basin and to generate information for better mitigation of similar events elsewhere.
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spelling doaj.art-dfb39e0b37f74635a71de3c7cd21b6112022-12-21T23:30:11ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-05-01910.3389/feart.2021.671378671378Anatomy of a Catastrophe: Reconstructing the 1936 Rock Fall and Tsunami Event in Lake Lovatnet, Western NorwayNicolas Waldmann0Kristian Vasskog1Kristian Vasskog2Guy Simpson3Emmanuel Chapron4Eivind Wilhelm Nagel Støren5Eivind Wilhelm Nagel Støren6Louise Hansen7Jean-Luc Loizeau8Atle Nesje9Daniel Ariztegui10Dr. Moses Strauss Department of Marine Geosciences, Charney School of Marine Sciences, University of Haifa, Haifa, IsraelDepartment of Geography, University of Bergen, Bergen, NorwayBjerknes Center for Climate Research, University of Bergen, Bergen, NorwayDepartment of Earth Sciences, University of Geneva, Geneva, SwitzerlandLaboratory Geographie De l’Environnement (GEODE), University of Toulouse Jean Jaurès, Toulouse, FranceBjerknes Center for Climate Research, University of Bergen, Bergen, NorwayDepartment of Earth Science, University of Bergen, Bergen, NorwayGeological Survey of Norway, Trondheim, NorwayDepartment F.-A. Forel for Environmental and Aquatic Science, University of Geneva, Geneva, SwitzerlandDepartment of Earth Science, University of Bergen, Bergen, NorwayDepartment of Earth Sciences, University of Geneva, Geneva, SwitzerlandRock falls and landslides plunging into lakes or small reservoirs can result in tsunamis with extreme wave run-ups. The occurrence of these natural hazards in populated areas have encouraged a recent sharp increase of studies that aim to mitigate their impact on human lives and assess infrastructure lost. This paper amalgamates in a novel fashion and at an unprecedented detail in situ historic measurements, geological data and numerical modeling of a rock fall event and associated tsunami wave that occurred in Lake Lovatnet (western Norway) in September 1936. Historical records report an event that released ca. 1 million m3 of rocks and debris from Ramnefjellet Mountain at an altitude of 800 m above Lake Lovatnet. The fragmented material plunged into the lake, causing a tsunami that reached a maximum run-up of 74 m and killed 74 people. In fact, the settlements of Bødal and Nesdal were wiped out as a result of the catastrophic wave. Sediments resulting from the 1936 rock fall and associated tsunami were identified in the subsurface of Lake Lovatnet by shallow geophysical investigations and were retrieved using gravity coring equipment. A set of high resolution physical and geochemical measurements were carried out on the cores with the aim of reproducing a highly detailed reconstruction of this catastrophic event in order to better understand and learn about the processes involved. The cores were retrieved in the northwestern sub-basin of the lake and its chronology was constrained by 210Pb and radiocarbon dating. A specially tailored physically based mathematical model was applied to better understand the tsunami event. Integration of the geophysical record, the sedimentological data and numerical modeling provide a comprehensive background to better understand the effects of such event in a deep fjord-like lacustrine basin and to generate information for better mitigation of similar events elsewhere.https://www.frontiersin.org/articles/10.3389/feart.2021.671378/fullmass transport depositsgeohazardnumerical modelingtsunami depositlacustrine sedimentsshallow geophysics
spellingShingle Nicolas Waldmann
Kristian Vasskog
Kristian Vasskog
Guy Simpson
Emmanuel Chapron
Eivind Wilhelm Nagel Støren
Eivind Wilhelm Nagel Støren
Louise Hansen
Jean-Luc Loizeau
Atle Nesje
Daniel Ariztegui
Anatomy of a Catastrophe: Reconstructing the 1936 Rock Fall and Tsunami Event in Lake Lovatnet, Western Norway
Frontiers in Earth Science
mass transport deposits
geohazard
numerical modeling
tsunami deposit
lacustrine sediments
shallow geophysics
title Anatomy of a Catastrophe: Reconstructing the 1936 Rock Fall and Tsunami Event in Lake Lovatnet, Western Norway
title_full Anatomy of a Catastrophe: Reconstructing the 1936 Rock Fall and Tsunami Event in Lake Lovatnet, Western Norway
title_fullStr Anatomy of a Catastrophe: Reconstructing the 1936 Rock Fall and Tsunami Event in Lake Lovatnet, Western Norway
title_full_unstemmed Anatomy of a Catastrophe: Reconstructing the 1936 Rock Fall and Tsunami Event in Lake Lovatnet, Western Norway
title_short Anatomy of a Catastrophe: Reconstructing the 1936 Rock Fall and Tsunami Event in Lake Lovatnet, Western Norway
title_sort anatomy of a catastrophe reconstructing the 1936 rock fall and tsunami event in lake lovatnet western norway
topic mass transport deposits
geohazard
numerical modeling
tsunami deposit
lacustrine sediments
shallow geophysics
url https://www.frontiersin.org/articles/10.3389/feart.2021.671378/full
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