Geological Considerations in Dams Failure Teodora Barbuntoiu A
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Field Trip Report Vajont Valley & Latemar (Italy)
04-06/07/2019 Field trip report Vajont valley & Latemar (Italy) Participants: Baville Paul Bonneau François Caumon Guillaume Clausolles Nicolas Frantz Yves Gouache Corentin Raguenel Margaux Schuh-Senlis Melchior IAMG Student Chapter Nancy RING TEAM - GEORESSOURCES Summary Introduction ............................................................................................................................................. 1 Chronostratigraphy of the field trip ........................................................................................................ 2 1. Vajont Formations (1 Figure 2, 65 – 160 Ma) .............................................................................. 2 2. Calcare del Vajont Formation (2 Figure 2, 160 – 170 Ma)........................................................... 3 3. Ignee Formation (3 Figure 2, 170 – 183 Ma) ............................................................................... 4 4. Soverzene Formation (4 Figure 2, 183 – 200 Ma) ....................................................................... 4 5. Dolomia Principale Formation (5 Figure 2, 200 – 230 Ma) ......................................................... 4 6. Rodella Formation (6 Figure 2, 230 – 247 Ma) ............................................................................ 5 7. Latemar Formation (7 Figure 2, 247 – 250 Ma) .......................................................................... 6 8. Bellerophon Formation (8 Figure 2, 250 – 258 Ma) ................................................................... -
Barren Ridge FEIS-Volume IV Paleo Tech Rpt Final March
March 2011 BARREN RIDGE RENEWABLE TRANSMISSION PROJECT Paleontological Resources Assessment Report PROJECT NUMBER: 115244 PROJECT CONTACT: MIKE STRAND EMAIL: [email protected] PHONE: 714-507-2710 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT Paleontological Resources Assessment Report PREPARED FOR: LOS ANGELES DEPARTMENT OF WATER AND POWER 111 NORTH HOPE STREET LOS ANGELES, CA 90012 PREPARED BY: POWER ENGINEERS, INC. 731 EAST BALL ROAD, SUITE 100 ANAHEIM, CA 92805 DEPARTMENT OF PALEOSERVICES SAN DIEGO NATURAL HISTORY MUSEUM PO BOX 121390 SAN DIEGO, CA 92112 ANA 032-030 (PER-02) LADWP (MARCH 2011) SB 115244 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT TABLE OF CONTENTS 1.0 INTRODUCTION ........................................................................................................................... 1 1.1 STUDY PERSONNEL ....................................................................................................................... 2 1.2 PROJECT DESCRIPTION .................................................................................................................. 2 1.2.1 Construction of New 230 kV Double-Circuit Transmission Line ........................................ 4 1.2.2 Addition of New 230 kV Circuit ......................................................................................... 14 1.2.3 Reconductoring of Existing Transmission Line .................................................................. 14 1.2.4 Construction of New Switching Station ............................................................................. -
31762102033147.Pdf (8.743Mb)
Sedimentology, provenance, and tectonic setting of the Miocene Horse Camp Formation (Member 2), east-central Nevada by Brian Keith Horton A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences Montana State University © Copyright by Brian Keith Horton (1994) Abstract: A study of the sedimentology, compositional trends, and modem tectonic setting of a 1600 m-thick sedimentary succession provides information on the late Cenozoic paleogeography and tectonics of an extensional basin and adjacent orogen in the Basin and Range province of east-central Nevada. Interpretations of depositional environments and reconstructions of paleogeography utilize detailed sedimentologic analyses of fourteen distinct facies and four facies associations from nine measured stratigraphic sections. Conglomerate compositional data and considerations of modern tectonic setting and local geologic structures provide constraints on the tectonic development of the extensional basin and orogen. Within the Miocene Horse Camp Formation (Member 2), four facies associations are defined by specific combinations of fourteen potential facies and attributed to processes characteristic of particular depositional environments. Subaerial and subaqueous fan-delta environments were characterized by deposition of sediment gravity flows and an absence of fluvial processes. A nearshore lacustrine facies association recorded wave-influenced sedimentation near a lake shoreline. Quiet-water deposition and limited sediment gravity flows characterized an offshore lacustrine environment. Lateral facies variations and stratal thinning and fining trends suggest a sediment source terrane to the south/southeast in the northern Grant Range. Simulated unroofing of this source terrane generated a hypothetical clast composition suite that is similar to actual conglomerate compositional data from Member 2. -
GEOLOGY of the TICK CANYON AREA May 23, 1952
GEOLOGY OF THE TICK CANYON AREA J. Richard Woodcock California Institute of ·rechnology May 23, 1952 Table of Cantents. Abstract •••••••••••••••••••••••••••••••••••••••••••••••••••••••••• 1 Introdttction . • . • . • . • • . • • . • . • . • • • . • . • • • . • . • • • • • • • • . • • • • • . • • • • • • • L. Aknowledgm.ents • • •• • • • ••••••••••• • •• e ••••••••••••••• • •••••••• • ••••••• • • 5 General Geography••••••••••••••••••••••••••••••••••••••••••••••••••••• 6 Statigraphy and Lithology ••••••••••••••••••••••••••••••••••••••••••••• 8 Basement Complex •••••••••••••·••••••••••••••••••••••••••••••••••· 9 Vasq.uez FO:rmation • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • 9 General (Vasquez Formation) ...................................... 19 Tick Canyon Formation .............•.....•..••.•..•............•.. 19 Mint Canyon Formation ............................................ 20 Whonoz Formation ••••••••••••••••••••••••••••••••••••••••••••••••• 20 General (Tick Canyon and Mint Canyon Formations) ................. 21 Structure ............................................................. 22 Geomorphology••••••••••••••••••••••••••••••••••·•••••••••••••••••••••• 2L Drainage • . • • • • • • • • • • . • • • . • • • • • • . • • • . • • • • • • . • • . • • . • • . • • • • • • • • • • • 2 h Relief ........................................................... 24 Geologic History •••••••••••••••••••••••••••••••••••••••••••••••••••••• 26 Illustrations: Figure: 1. Index l~p •••••••••••••••·••••••••••••••••••••••••••••••••••••• -
Live, Virtual and Constructive Identity of the Italian Army Stability Policing
6 1 0 LiveInside the issue 2 r e Live, Virtual and Constructive Identity of the b m Italian Army e c e D Stability Policing: towards new Operational - 4 Capabilities 2 e u s s Technological Innovation and National Security I #Wearejointandcombined 瘀攀爀礀眀栀攀爀攀 愀瀀椀搀氀礀 EDITOR’S NOTE by Col. ITA (A) Gianluigi ARCA CONTENTS NRDC-ITA Commander 攀爀 Lt. Gen. Roberto PERRETTI EDITORIAL BOARD FROM THE STAFF Editor in Chief: Col. ITA (A) Gianluigi ARCA • The eNRF Support Concept Seminar at NRDC-ITA 4 Editors : Lt. Col. ITA (A) Vincenzo SCHETTINI, Maj. GBR (A) Christopher • Stability Policing: towards new Operational Capabilities 6 DAVIES • Public Affairs to become independent branch within HQ! 8 Assistant Editor and Graphic Designer: • NRDC-ITA CIS drives NATO technological innovation! 12 Cpl. ITA (A) Chiara MONTI ...................... • Live, Virtual and Constructive Identity of the Italian Army 14 Assistant in Imagery and Post Production: • Technological Innovation and National Security 20 WO1 ITA (A) Francesco CIVITELLI Photographers: Cpl. ITA (A) Raffaele SAN- SEVERINO, Cpl. ITA (A) Mattia RUSSO Web: WO ITA (A) Italo BOATO SPORT BOARD The everywhere rapidly is the autorized offi- ear reader, cial pubblication of NATO Rapid Deploy- able Corps, Italy. All editorial content of the • Exercise Eagle Triglav 28 this issue marks an im- “ER” issue, in fact, is honoured to everywhere rapidly is prepared , edited and • NRDC-ITA Mountain Military Training on Dolomites 30 Dportant and challenging host an article by Maj. Gen. Mau- approved by the NRDC -ITA Commander, period for NRDC-ITA. The Hea- rizio Boni, who as Ce.Si.Va. -
Book Review of “The Story of Vaiont Told by the Geologist Who Discovered the Landslide”
Nat. Hazards Earth Syst. Sci., 11, 485–486, 2011 www.nat-hazards-earth-syst-sci.net/11/485/2011/ Natural Hazards doi:10.5194/nhess-11-485-2011 and Earth © Author(s) 2011. CC Attribution 3.0 License. System Sciences Book Review of “The Story of Vaiont Told by the Geologist Who Discovered the Landslide” F. Guzzetti1 and G. Lollino2 1Istituto di Ricerca per la Protezione Idrogeologica, Consiglio Nazionale delle Ricerche, via Madonna Alta 126, 06128 Perugia, Italy 2Istituto di Ricerca per la Protezione Idrogeologica, Consiglio Nazionale delle Ricerche, Strada delle Cacce 73, 10135 Torino, Italy THE STORY OF VAIONT TOLD BY THE GEOL- jont landslide in August 1959, four years before the catas- OGIST WHO DISCOVERED THE LANDSLIDE, BY: trophic failure. Semenza performed a systematic, large-scale E. SEMENDA, K-FLASH PUBLISHER, FERRARA, 205 geological and geomorphological investigation of the area, PAGES, PRICE: 28.00 C, ISBN 978-88-89288-02-3 and specifically of the site affected by the landslide before the On 9 October 1963, at 10:39 p.m. local time, between 240 slope failed catastrophically. During his fieldwork, Semenza and 300 million cubic meters of sedimentary rocks detached was able to identify and document a number of geological from Mount Toc, in Veneto, northern Italy, and slid into the and morphological features that he correctly interpreted as Vajont Lake. The falling rock mass acted like a huge piston, evidence of the presence of a very large, ancient landslide pushing the water of the lake against Casso and Erto, two deposit. The geomorphological information and geological small villages on the slope in front of the slope that failed, data collected by Semenza remain a brilliant example of a and then over an artificial dam 210 m high. -
Expecting Disaster: the 1963 Landslide of the Vajont Dam
Expecting Disaster: The 1963 Landslide of the Vajont Dam Wilko Graf von Hardenberg On October 9, 1963, at 10:39 pm 260 million cubic meters of rock broke off from the top of Monte Toc, on the border between Veneto and Friuli Venezia Giulia. It fell into the reservoir of the Vajont Dam, producing an enormous wave of at least 50 million cubic meters of water. The dam, completed in 1959 and one of the biggest in the world at the time, did not suffer any serious damage. However, flooding destroyed several villages in the valley and killed almost 2,000 people. A third of the population of Longarone, the largest village downstream of the dam, perished. The town of Longarone, Italy, before the landslide, 1963. The town of Longarone after the dam was overtopped by a giant wave. Unknown photographer, 1963. Courtesy of Vajont Survivor’s Committee. Unknown photographer, 1963. Click here to view image source. Courtesy of the Vajont Survivor’s Committee. Click here to view image source. This work is licensed under a Creative Commons Public Domain Mark 1.0 License . This work is licensed under a Creative Commons Public Domain Mark 1.0 License . Though the dam incorporated the latest technical expertise, it had been built without due consideration of geological reports, possible tectonic problems, local knowledge of the territory and Monte Toc’s connate instability. Source URL: http://www.environmentandsociety.org/node/3401 Print date: 04 March 2020 11:07:46 Hardenberg, Wilko Graf von. "Expecting Disaster: The 1963 Landslide of the Vajont Dam." Arcadia ( 2011), no. -
Masculinity and Political Authority 241 7.1 Introduction 241
Durham E-Theses The political uses of identity an enthnography of the northern league Fernandes, Vasco Sérgio Costa How to cite: Fernandes, Vasco Sérgio Costa (2009) The political uses of identity an enthnography of the northern league, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/2080/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk University of Durham The Political Uses of Identity: An Ethnography of the Northern The copyright of this thesis rests with the author or the university to which it was League submitted. No quotation from it, or information derived from it may be published without the prior written consent of the author or university, and any information derived from it should be acknowledged. By Vasco Sergio Costa Fernandes Department of Anthropology April 2009 Thesis submitted in accordance with the requirement for the Degree of Doctor of Philosophy Supervisors: Dr Paul Sant Cassia Dr Peter Collins 2 1 MAY 2009 Abstract This is a thesis about the Northern League {Lega Nord), a regionalist and nationalist party that rose to prominence during the last three decades in the north of Italy Throughout this period the Northern League developed from a peripheral and protest movement, into an important government force. -
Induced Earthquakes
Department of Political Science Bachelor in Politics, Philosophy and Economics Chair in Population Environment and Sustainability THE EFFECTS OF HUMAN ACTIVITIES ON THE EARTH: INDUCED EARTHQUAKES SUPERVISOR Prof. Marcello di Paola CANDIDATE Chiara Ghesini 076572 ACADEMIC YEAR 2016/201 1 INDEX Introduction 3 1.1 Reservoir- Induced Seismicity 5 1.2 Zipingpu Dam 1.3 Vajont Dam 2.0 Underground Open-Pit Mining 9 3.0 Geothermal Energy 11 4.0 Nuclear Activity 13 4.1 Nuclear Events 5.0 Underground Waste Water Injection and Massive Extraction 17 5.1 Praga Oklahoma Earthquake 6.0 State Institutions 21 6.1 Federal Institutions 6.1.2 Environmental Protection Agency 6.1.3 Bureau of Land Management 6.1.4 U.S. Forest Service 6.1.5 United States Geological Survey 6.2 Castor Project 7.0 Considerations 30 Conclusion 32 Bibliography 33 2 Introduction Earthquakes have always been considered natural events in our societies, causing hundreds of victims every year around the entire world. Nowadays the things are changing, due to the increased request of natural sources and the continuous growth of world’s population, more energy and more resources are being required. Our epoch can be perfectly defined with the term “Anthropocene”, referring to the influence that human activities have on our planet, basing the evidence on continuous atmospheric, hydrologic, geologic and biospheric alterations. Starting in the 1950s, this process is damaging the earth with a trend that, if not reversed, is going to leave future generations in a hopeless situation. Having been born in this time period we are used to take many of the utilities we have for granted, not knowing that we obtain them through activities like gas storage, mining and underground water extraction. -
Monografia Che Tenete in Mano
RDM_SantaGiustina_book.indd 1 11/09/19 08:10 Parte Due Content Part Two Santa Giustina Parte Uno 11 Chi siamo Part One About Us RDM Group 12 La nostra Storia Our History 14 La nostra Vision Our Vision 16 I nostri Valori Our Values 18 Together we shape the Future Together we shape the Future Parte Tre 20 Struttura operativa del Gruppo Part Three Group Operations Framework Our People 22 Dove siamo Where we are 24 Modello di Business Business Model 26 I nostri prodotti Our Products 2 RDM_SantaGiustina_book.indd 2 11/09/19 08:10 Parte Due 31 Santa Giustina e RDM Group Content Part Two Santa Giustina and RDM Group Santa Giustina 32 Highlight Highlights 38 Storia dello stabilimento History of the Mill 42 Gli Stakeholder di Santa Giustina The Stakeholders of Santa Giustina 44 I clienti di Santa Giustina The customers of Santa Giustina 46 La sostenibilità per Santa Giustina Sustainability for Santa Giustina Chi siamo About Us 48 Le foto di ieri Yesterday’s Photographs La nostra Storia Our History 80 Le foto di oggi Today’s Photographs La nostra Vision Our Vision 100 I prodotti di Santa Giustina The Products of Santa Giustina I nostri Valori Our Values 108 Certificazioni Certifications Together we shape the Future Together we shape the Future Parte Tre 112 Massimo Marcer Struttura operativa del Gruppo Part Three 116 Gianluca Scaglioni Group Operations Framework Our People 120 Francesco Canal 124 Diana Callegari Dove siamo 128 Dino Dal Pan Where we are 132 Giancarlo De Min Modello di Business 136 Fabrizia Casagrande Business Model 138 Paolo Brugnera Muraro 140 Emilio Dal Zot I nostri prodotti Our Products 142 Fin che ‘l pope gira 3 RDM_SantaGiustina_book.indd 3 11/09/19 08:10 LETTERA DEL CEO Gentili, si dice che gli anniversari vadano sempre festeggiati, penso però che alcuni meritino davvero un’attenzione speciale. -
Adaptive Finite Volume Methods with Well-Balanced Riemann Solvers For
INTERNATIONAL JOURNAL FOR NUMERICAL METHODS IN FLUIDS Int. J. Numer. Meth. Fluids (2010) Published online in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/fld.2298 Adaptive finite volume methods with well-balanced Riemann solvers for modeling floods in rugged terrain: Application to the Malpasset dam-break flood (France, 1959)‡ D. L. George∗,† Cascades Volcano Observatory, U.S. Geological Survey, 1300 SE Cardinal Ct., Bldg. 10, Vancouver, WA 98683, U.S.A. SUMMARY The simulation of advancing flood waves over rugged topography, by solving the shallow-water equations with well-balanced high-resolution finite volume methods and block-structured dynamic adaptive mesh refinement (AMR), is described and validated in this paper. The efficiency of block-structured AMR makes large-scale problems tractable, and allows the use of accurate and stable methods developed for solving general hyperbolic problems on quadrilateral grids. Features indicative of flooding in rugged terrain, such as advancing wet–dry fronts and non-stationary steady states due to balanced source terms from variable topography, present unique challenges and require modifications such as special Riemann solvers. A well- balanced Riemann solver for inundation and general (non-stationary) flow over topography is tested in this context. The difficulties of modeling floods in rugged terrain, and the rationale for and efficacy of using AMR and well-balanced methods, are presented. The algorithms are validated by simulating the Malpasset dam-break flood (France, 1959), which has served as a benchmark problem previously. Historical field data, laboratory model data and other numerical simulation results (computed on static fitted meshes) are shown for comparison. -
WARD's Natural Science Establishment, Inc
MANUAL FOR WARD'S COLLECTION OF CLASSIC NORTH AMERICAN ROCKS 45 E 7217 Ward's is indebted to Dr. E. William Heinrich, Professor of Mineralogy, The University of Michigan, for the classification ofthe rocks in the new col ledion, for the descriptions of Thin Sedions and for editorial assistance in the preparation of the manual that accompanies the colledion. Since the geology of the region in which the rock is found and other relevant data in the literature may be of considerable interest, brief references to pertinent literature is provided for each rock. A bibliography of petrologic literature is also provided. WARD'S Natural Science Establishment, Inc. Copyright1970;Aev.1990 Printed in U.SA WARD'S COLLECTION OF CLASSIC NORTH AMERICAN ROCKS BIBLIOGRAPHY Allen, J.B. and ~harsley: NEPHELINE-SYENITE AND PHONOLITE Alling, H.L.: INTERPRETATIVE PETROGRAPHY OF THE IGNEOUS ROCKS Barth, T.F.W.: THEORETICAL PETROLOGY Daly, R.A.: IGNEOUS ROCKS AND THE DEPTHS OF THE EARTH Dana, E.S.: DANA'S TEXTBOOK OF MINERALOGY, 4th Ed. Revised by W.E. Ford Fairbairn, H.W.: STRUCTURAL PETROLOGY OF DEFORMED ROCKS Grout, F.F.: PETROLOGY AND PETROGRAPHY Harker, A.: PETROLOGY FOR STUDENTS Hatch, F.H. and Rastall, R.H.: PETROLOGY OF THE SEDIMENTARY ROCKS Heinrich, W.E.: MICROSCOPIC PETROGRAPHY THE GEOLOGY OF CARBONATITES Hess, H.H. and Poldervaart, A.: BASALTS, Vols. 1 and 2 Holmes, Arthur: PETROGRAPHIC METHODS AND CALCULATIONS Iddings, J.P.: ROCK MINERALS IGNEOUS ROCKS, Vols. I, II Johannsen, Albert: MANUAL OF PETROGRAPHIC METHODS A DESCRIPTIVE PETROGRAPHY OF THE IGNEOUS ROCKS Vol. I Introduction, Textures, Classifications and Glossary Vol.