HRPP 473 Lumbroso, D.M., Sakamoto, D
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CNRS – INSHS/INS2I * GDR 3359 MoDyS * UMR 3495 MAP École thématique MoDyS 2012 Practical classes data sets Some events and clues ion the history of the city of Fréjus Sources used 3 The city 4 Text 1 History of Fréjus 4 Text 2 The Franks and Arabs in Provence 4 Christianity in Fréjus 5 Text 3 Churches and bishops 5 Text 4 Introduction of Christianity 5 Text 5 Saint Leontius 5 The Episcopal group 6 Text 6 The baptistery 6 Fig 1 A Merovingian Baptistery 6 Text 7 The Cathedral 6 Text 8 The Cloister 7 Collapse of the Malpasset dam 8 Text 9 Malpasset 8 Fig 2 Remains of the Malpasset dam, the day later 8 Text 10 Malpasset Dam 9 2010 floods 10 Text 11 Flood June 2010 10 Text 12 French flash flood toll up to 25 10 Text 13 Flash flood and Debris flood in the Var (France), 15th June 2010 11 Carte de Saint-Raphaël (Var) selon Cassini <http://cassini.ehess.fr/cassini/fr/html/1_navigation.php#> Fiche de données atelier cas concret / L’eau comme ressource École thématique MODYS - CNRS INSHS/INSII GDR 3359 MoDyS UMR 3495 MAP Réseau ISA [JY Blaise I Dudek 09/2012 [email protected]] 2 Fiche de données atelier cas concret / L’eau comme ressource Sources used [1] History of Fréjus http://en.wikipedia.org/wiki/Fr%C3%A9jus [03/10/2012] [2] History of Provence http://en.wikipedia.org/wiki/History_of_Provence [3] Introduction of Christianity http://en.wikipedia.org/wiki/Bishopric_of_Fr%C3%A9jus [4] Saint Leontius http://en.wikipedia.org/wiki/Leontius_of_Fr%C3%A9jus [5] The cathedral in Fréjus http://en.wikipedia.org/wiki/Fr%C3%A9jus_Cathedral [6] Collapse -
9781496222152.Pdf
Empire and Catastrophe France Overseas: Studies in Empire and Decolonization Series editors: A. J. B. Johnston, James D. Le Sueur, and Tyler Stovall Regeneration through Empire: French Pronatalists and Colonial Suspects: Suspicion, Imperial Rule, and Colonial Colonial Settlement in the Third Republic Society in Interwar French West Africa Margaret Cook Andersen Kathleen Keller To Hell and Back: The Life of Samira Bellil Apostle of Empire: The Jesuits and New France Samira Bellil Bronwen McShea Translated by Lucy R. McNair French Mediterraneans: Transnational and Introduction by Alec G. Hargreaves Imperial Histories Colonial Metropolis: The Urban Grounds of Anti- Edited and with an introduction by Patricia M. E. Lorcin Imperialism and Feminism in Interwar Paris and Todd Shepard Jennifer Anne Boittin The Cult of the Modern: Trans-Mediterranean France and Paradise Destroyed: Catastrophe and Citizenship in the the Construction of French Modernity French Caribbean Gavin Murray-Miller Christopher M. Church Cinema in an Age of Terror: North Africa, Victimization, Nomad’s Land: Pastoralism and French Environmental and Colonial History Policy in the Nineteenth-Century Mediterranean World Michael F. O’Riley Andrea E. Duffy Medical Imperialism in French North Africa: Regenerating The French Navy and the Seven Years’ War the Jewish Community of Colonial Tunis Jonathan R. Dull Richard C. Parks I, Nadia, Wife of a Terrorist Making the Voyageur World: Travelers and Traders in the Baya Gacemi North American Fur Trade Transnational Spaces and Identities in the Carolyn Podruchny Francophone World A Workman Is Worthy of His Meat: Food and Edited by Hafid Gafaïti, Patricia M. E. Lorcin, and David Colonialism in Gabon G. -
Malpasset, La Seule Rupture Totale D'un Barrage-Voûte
Malpasset la seule rupture totale d'un Barrage-voûte Pour régulariser l'alimentation en eau des communes du P. DUFFAUT littoral, le département du Var s'est doté d'un barrage au lieudit Malpasset, un barrage-voûte construit en 1952-1954 130, rue de Rennes sur le Reyran, dont le plein remplissage a été différé en 75006 Paris Résumé raison des retards d'une expropriation. Lors de l'automne [email protected] très pluvieux de 1959, l'ouvrage a été ruiné, et le flot liBéré a causé plus de 400 morts et des dégâts considéraBles dans la Basse vallée et la ville de Fréjus. Comme aucun Barrage- voûte n'avait connu de rupture auparavant, et comme la rupture avait manifestement affecté le terrain de fondation, la catastrophe a suscité un ensemBle exceptionnel de calculs et surtout d'essais pour remonter aux causes de la rupture, ce qui a ouvert des chapitres nouveaux dans la connaissance scientifique des massifs rocheux, et permis d'émettre des recommandations pour l'avenir. L'application de la mécanique des roches au génie civil a pris corps dans les années qui ont suivi. Mots-clés : Barrage, mécanique des roches, gneiss, faille, sous-pression, essais sur site. Malpasset, the only total failure of an arch dam In order to regulate the water supply for its coastal communities, the Var department equipped itself with a reservoir dam at Malpasset site. An arch dam was built in 1952- 1954 on the Reyran river. The filling up was delayed due to an Abstract expropriation procedure. During the very rainy autumn 1959, the dam failed and the flow made more than 400 casualties and huge damages along the lower valley and in the Fréjus city. -
Burst of a Dam 2 December 1959 Malpasset (Var) France
French Ministry for Sustainable Development - DGPR / SRT / BARPI N° 29490 Burst of a dam Dam (failure) Design 2 December 1959 Insufficient preliminary studies Malpasset (Var) Geology France Checks Acceptance THE FACILITIES INVOLVED The site: In order to meet the local water demand, a dam was built on the REYRAN river downstream to the confluence with the BUEME river at Malpasset to the north of Fréjus (mileage point 16.625 of C.D.37). The dam was supposed to regulate the rate of flow of the raging river and store 50 million m 3 of water for agriculture (vegetable crop and floriculture), domestic use, as well as for use in the booming tourism sector. The Reyran river is almost dry in summers but regularly causes floods in the region during the heavy autumn and end of winter downpours. Several successive projects were carried out on the structure between 1865 (a project running at 300 m downstream the Malpasset dam / 25 m high holding 5.6 million m 3) and the project that started on 1 st April 1952 and ended in October 1954 (60 m high / 50 million m 3 of water). The site and the height of the structure varied during the projects. All geological studies forecasted optimal conditions of performance. The compensating reservoir was studied by geologists from the science department in Marseille who confirmed its excellent water tightness. However, the storage site was heavily debated upon right from the initial studies. Geologists observed a fault as early as 1946 and underlined the importance of carefully leakproofing the structure including rendering the foundation ground impervious. -
Barrage De Malpasset (Var) Pierre Duffaut
Cinquantenaire de la rupture des fondations et du barrage de Malpasset (Var) Pierre Duffaut To cite this version: Pierre Duffaut. Cinquantenaire de la rupture des fondations et du barrage de Malpasset (Var). Travaux du Comité français d’Histoire de la Géologie, Comité français d’Histoire de la Géologie, 2009, 3ème série (tome 23), pp.201-224. hal-00913866 HAL Id: hal-00913866 https://hal.archives-ouvertes.fr/hal-00913866 Submitted on 4 Dec 2013 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. TRAVAUX DU COMITÉ FRANÇAIS D’HISTOIRE DE LA GÉOLOGIE (COFRHIGÉO) TROISIÈME SÉRIE, t. XXIII, 2009, n° 9 (séance du 9 décembre 2009) Pierre DUFFAUT Cinquantenaire de la rupture des fondations et du barrage de Malpasset (Var) Résumé. Pour régulariser l’alimentation en eau des communes du littoral, le département du Var s’est doté d’un barrage sur le Reyran au lieudit Malpasset, un barrage voûte construit en 1952-1954, dont le plein remplissage a été différé en raison du retard d’une expropriation. Lors de l’automne très pluvieux de 1959, l’ouvrage a été ruiné et le flot libéré a causé plus de 400 morts et des dégâts considérables dans la basse vallée et la ville de Fréjus. -
Deposits Related to the Failure of the Malpasset Dam in 1959 an Analogue for Hyperpycnal Deposits from Jökulhlaups
Marine Geology 260 (2009) 81–89 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Deposits related to the failure of the Malpasset Dam in 1959 An analogue for hyperpycnal deposits from jökulhlaups T. Mulder a,⁎, S. Zaragosi a, J.-M. Jouanneau a, G. Bellaiche b, S. Guérinaud a, J. Querneau a a Université de bordeaux, UMR 5805 EPOC, avenue des facultés, F-33405 Talence cedex b Hameau de la Corne d′Or, 12 Boulevard Corne d′Or, 06230 Villefranche-sur-Mer, France article info abstract Article history: Sediment cores collected in the Gulf of Fréjus (SE France) contain submarine deposits related to the failure of Received 25 July 2008 the Malpasset Dam in 1959. These deposits constitute a dark, sandy terrigeneous layer of 10–40 cm thickness Received in revised form 3 February 2009 lying above an erosion surface. The deposits are composed of ungraded, non-bioturbated sands and silts Accepted 4 February 2009 displaying no apparent sedimentary structure, but rich in organic matter and rock or shell fragments. During the event, this layer prograded onto the inner continental shelf and froze rapidly. These hyperconcentrated Keywords: flow deposits are related to an unsteady inertia flow generated by a surge-like flood and bedload-dominated flood fl fl freezing hyperpycnal ow. Rapid freezing on ow sides generated lateral, coarse-grained, levee-shape deposits. The inertia flow deposits related to the failure of the Malpasset Dam are drastically different from classical suspended-load- jökulhlaup dominated hyperpycnites deposited by a steady, flood-generated, hyperpycnal flow. However, they are Malpasset Dam break comparable with present-day deposits on a volcanic, ice-covered margin (Icelandic jökulhlaups), with surge-flow ancient deposits resulting from the pulsating output of subglacial lakes during a deglaciation, or with Martian SE France landforms resulting from sporadic ice–melt events during early Martian times.