Observed Performance of Dams During Earthquakes Vol. 3
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Japan's Secretive Death Penalty Policy
Japan’s Secretive Death Penalty Policy: Contours, Origins, Justifications, and Meanings♦ David T. Johnson I. ABSTRACT...................................................................................................62 II. “REIKO IN WONDERLAND” .....................................................................63 A. SECRECY AND SILENCE ..............................................................................70 III. ORIGINS .......................................................................................................76 A. MEIJI BIRTH ...............................................................................................76 B. THE OCCUPATION’S “CENSORED DEMOCRACY” ........................................80 C. POSTWAR ACCELERATION..........................................................................87 IV. JUSTIFICATIONS ........................................................................................97 V. MEANINGS.................................................................................................109 A. SECRECY AND LEGITIMACY......................................................................109 B. SECRECY AND SALIENCE ..........................................................................111 C. SECRECY AND DEMOCRACY.....................................................................117 D. SECRECY AND LAW ..................................................................................119 VI. CONCLUSION.............................................................................................123 -
List of Dams and Reservoirs 1 List of Dams and Reservoirs
List of dams and reservoirs 1 List of dams and reservoirs The following is a list of reservoirs and dams, arranged by continent and country. Africa Cameroon • Edea Dam • Lagdo Dam • Song Loulou Dam Democratic Republic of Congo • Inga Dam Ethiopia Gaborone Dam in Botswana. • Gilgel Gibe I Dam • Gilgel Gibe III Dam • Kessem Dam • Tendaho Irrigation Dam • Tekeze Hydroelectric Dam Egypt • Aswan Dam and Lake Nasser • Aswan Low Dam Inga Dam in DR Congo. Ghana • Akosombo Dam - Lake Volta • Kpong Dam Kenya • Gitaru Reservoir • Kiambere Reservoir • Kindaruma Reservoir Aswan Dam in Egypt. • Masinga Reservoir • Nairobi Dam Lesotho • Katse Dam • Mohale Dam List of dams and reservoirs 2 Mauritius • Eau Bleue Reservoir • La Ferme Reservoir • La Nicolière Reservoir • Mare aux Vacoas • Mare Longue Reservoir • Midlands Dam • Piton du Milieu Reservoir Akosombo Dam in Ghana. • Tamarind Falls Reservoir • Valetta Reservoir Morocco • Aït Ouarda Dam • Allal al Fassi Dam • Al Massira Dam • Al Wahda Dam • Bin el Ouidane Dam • Daourat Dam • Hassan I Dam Katse Dam in Lesotho. • Hassan II Dam • Idriss I Dam • Imfout Dam • Mohamed V Dam • Tanafnit El Borj Dam • Youssef Ibn Tachfin Dam Mozambique • Cahora Bassa Dam • Massingir Dam Bin el Ouidane Dam in Morocco. Nigeria • Asejire Dam, Oyo State • Bakolori Dam, Sokoto State • Challawa Gorge Dam, Kano State • Cham Dam, Gombe State • Dadin Kowa Dam, Gombe State • Goronyo Dam, Sokoto State • Gusau Dam, Zamfara State • Ikere Gorge Dam, Oyo State Gariep Dam in South Africa. • Jibiya Dam, Katsina State • Jebba Dam, Kwara State • Kafin Zaki Dam, Bauchi State • Kainji Dam, Niger State • Kiri Dam, Adamawa State List of dams and reservoirs 3 • Obudu Dam, Cross River State • Oyan Dam, Ogun State • Shiroro Dam, Niger State • Swashi Dam, Niger State • Tiga Dam, Kano State • Zobe Dam, Katsina State Tanzania • Kidatu Kihansi Dam in Tanzania. -
A Review of Geological Records of Large Tsunamis at Vancouver Island, British Columbia, and Implications for Hazard John J
Quaternary Science Reviews 19 (2000) 849}863 A review of geological records of large tsunamis at Vancouver Island, British Columbia, and implications for hazard John J. Clague! " *, Peter T. Bobrowsky#, Ian Hutchinson$ !Depatment of Earth Sciences and Institute for Quaternary Research, Simon Fraser University, Burnaby, BC, Canada V5A 1S6 "Geological Survey of Canada, 101 - 605 Robson St., Vancouver, BC, Canada V6B 5J3 #Geological Survey Branch, P.O. Box 9320, Stn Prov Govt, Victoria, BC, Canada V8W 9N3 $Department of Geography and Institute for Quaternary Research, Simon Fraser University, Burnaby, Canada BC V5A 1S6 Abstract Large tsunamis strike the British Columbia coast an average of once every several hundred years. Some of the tsunamis, including one from Alaska in 1964, are the result of distant great earthquakes. Most, however, are triggered by earthquakes at the Cascadia subduction zone, which extends along the Paci"c coast from Vancouver Island to northern California. Evidence of these tsunamis has been found in tidal marshes and low-elevation coastal lakes on western Vancouver Island. The tsunamis deposited sheets of sand and gravel now preserved in sequences of peat and mud. These sheets commonly contain marine fossils, and they thin and "ne landward, consistent with deposition by landward surges of water. They occur in low-energy settings where other possible depositional processes, such as stream #ooding and storm surges, can be ruled out. The most recent large tsunami generated by an earthquake at the Cascadia subduction zone has been dated in Washington and Japan to AD 1700. The spatial distribution of the deposits of the 1700 tsunami, together with theoretical numerical modelling, indicate wave run-ups of up to 5 m asl along the outer coast of Vancouver Island and up to 15}20 m asl at the heads of some inlets. -
Potamopyrgus Antipodarum (Gray, 1843) (Gastropoda, Tateidae) in Chile, and a Summary of Its Distribution in the Country
16 3 NOTES ON GEOGRAPHIC DISTRIBUTION Check List 16 (3): 621–626 https://doi.org/10.15560/16.3.621 Range extension of the invasive Potamopyrgus antipodarum (Gray, 1843) (Gastropoda, Tateidae) in Chile, and a summary of its distribution in the country Gonzalo A. Collado1, 2, Carmen G. Fuentealba1 1 Departamento de Ciencias Básicas, Facultad de Ciencias, Universidad del Bío-Bío, Avenida Andrés Bello 720, Chillán, 3800708, Chile. 2 Grupo de Biodiversidad y Cambio Global, Universidad del Bío-Bío, Avenida Andrés Bello 720, Chillán, 3800708, Chile. Corresponding author: Gonzalo A. Collado, [email protected] Abstract The New Zealand mudsnail Potamopyrgus antipodarum (Gray, 1843) has been considered as one of the most invasive mollusks worldwide and recently was listed among the 50 most damaging species in Europe. In the present paper, we report for the first time the presence ofP. antipodarum in the Maule river basin, Chile. The identity of the species was based on anatomical microdissections, scanning electron microscopy comparisons, and DNA barcode analysis. This finding constitutes the southernmost record of the species until now in this country and SouthAmerica. Keywords Alien species, DNA barcode, cryptic species, invasive mollusks, Maule River, range distribution. Academic editor: Rodrigo Brincalepe Salvador | Received 05 February 2020 | Accepted 23 March 2020 | Published 22 May 2020 Citation: Collado GA, Fuentealba CG (2020) Range extension of the invasive Potamopyrgus antipodarum (Gray, 1843) (Gastropoda, Tateidae) in Chile, and a summary of its distribution in the country. Check List 16 (3): 621–626. https://doi.org/10.15560/16.3.621 Introduction the 50 most damaging species in Europe (Nentwig et al. -
Status of Monitored Major Dams
Ambuklao Dam Magat Dam STATUS OF Bokod, Benguet Binga Dam MONITORED Ramon, Isabela Cagayan Pantabangan Dam River Basin MAJOR DAMS Itogon, Benguet San Roque Dam Pantabangan, Nueva Ecija Angat Dam CLIMATE FORUM 22 September 2021 San Manuel, Pangasinan Agno Ipo Dam River Basin San Lorenzo, Norzagaray Bulacan Presented by: Pampanga River Basin Caliraya Dam Sheila S. Schneider Hydro-Meteorology Division San Mateo, Norzagaray Bulacan Pasig Laguna River Basin Lamesa Dam Lumban, Laguna Greater Lagro, Q.C. JB FLOOD FORECASTING 215 205 195 185 175 165 155 2021 2020 2019 NHWL Low Water Level Rule Curve RWL 201.55 NHWL 210.00 24-HR Deviation 0.29 Rule Curve 185.11 +15.99 m RWL BASIN AVE. RR JULY = 615 MM BASIN AVE. RR = 524 MM AUG = 387 MM +7.86 m RWL Philippine Atmospheric, Geophysical and Astronomical Services Administration 85 80 75 70 65 RWL 78.30 NHWL 80.15 24-HR Deviation 0.01 Rule Curve Philippine Atmospheric, Geophysical and Astronomical Services Administration 280 260 240 220 RWL 265.94 NHWL 280.00 24-HR Deviation 0.31 Rule Curve 263.93 +35.00 m RWL BASIN AVE. RR JULY = 546 MM AUG = 500 MM BASIN AVE. RR = 253 MM +3.94 m RWL Philippine Atmospheric, Geophysical and Astronomical Services Administration 230 210 190 170 RWL 201.22 NHWL 218.50 24-HR Deviation 0.07 Rule Curve 215.04 Philippine Atmospheric, Geophysical and Astronomical Services Administration +15.00 m RWL BASIN AVE. RR JULY = 247 MM AUG = 270 MM BASIN AVE. RR = 175 MM +7.22 m RWL Philippine Atmospheric, Geophysical and Astronomical Services Administration 200 190 180 170 160 150 RWL 185.83 NHWL 190.00 24-HR Deviation -0.12 Rule Curve 184.95 Philippine Atmospheric, Geophysical and Astronomical Services Administration +16.00 m RWL BASIN AVE. -
California North Coast Offshore Wind Studies
California North Coast Offshore Wind Studies Overview of Geological Hazards This report was prepared by Mark A. Hemphill-Haley, Eileen Hemphill-Haley, and Wyeth Wunderlich of the Humboldt State University Department of Geology. It is part of the California North Coast Offshore Wind Studies collection, edited by Mark Severy, Zachary Alva, Gregory Chapman, Maia Cheli, Tanya Garcia, Christina Ortega, Nicole Salas, Amin Younes, James Zoellick, & Arne Jacobson, and published by the Schatz Energy Research Center in September 2020. The series is available online at schatzcenter.org/wind/ Schatz Energy Research Center Humboldt State University Arcata, CA 95521 | (707) 826-4345 California North Coast Offshore Wind Studies Disclaimer This study was prepared under contract with Humboldt State University Sponsored Programs Foundation with financial support from the Department of Defense, Office of Economic Adjustment. The content reflects the views of the Humboldt State University Sponsored Programs Foundation and does not necessarily reflect the views of the Department of Defense, Office of Economic Adjustment. This report was created under Grant Agreement Number: OPR19100 About the Schatz Energy Research Center The Schatz Energy Research Center at Humboldt State University advances clean and renewable energy. Our projects aim to reduce climate change and pollution while increasing energy access and resilience. Our work is collaborative and multidisciplinary, and we are grateful to the many partners who together make our efforts possible. Learn more about our work at schatzcenter.org Rights and Permissions The material in this work is subject to copyright. Please cite as follows: Hemphill-Haley, M.A., Hemphill-Haley, E. and Wunderlich, W. (2020). -
Significant Aspects of Geotechnical and Seismic Engineering and Management of Bridges and Structures in the U.S
SIGNIFICANT ASPECTS OF GEOTECHNICAL AND SEISMIC ENGINEERING AND MANAGEMENT OF BRIDGES AND STRUCTURES IN THE U.S. M. Myint Lwin1 Abstract It is important to integrate the knowledge and experience of geotechnical and seismic engineering and management of bridges to make sound decisions to reduce earthquake damages to highways, bridges and structures. Research continues to play important roles in developing modern bridge seismic design criteria, detailing practices and seismic retrofit strategies for reducing structural damages and casualties. Bridge management systems can be used effectively to incorporate seismic assessment data for prioritizing seismic retrofit needs. Introduction Major earthquakes, such as the 1964 Alaska Earthquake, Anchorage, Alaska; the 1989 Loma Prieta Earthquake, California; the 1994 Northridge Earthquake, California; the 1995 Kobe Earthquake, Japan; and so on, have taken thousands of lives, caused billions of dollars in damages, and incurred other indirect costs as a result of damage to bridges and structures, highways, and other public facilities. It is necessary to integrate the knowledge and experience in geotechnical and seismic engineering, and the management of bridges and structures, and other public facilities to mitigate seismic hazards. The important seismic hazards are strong ground shaking, ground failures (such as, liquefaction, lateral spread, differential settlement, landslides), soil-structure interaction, and other indirect effects caused by ground shaking and failures, such as, tsunamis, seiches, floods and fires. The engineers and code writers must take these seismic hazards into account in developing earthquake-resistant design, construction and management. Seismologic and Geologic Aspect of Earthquakes When an earthquake occurs, seismic waves traveled from the source to the earth’s surface through body waves and surface waves. -
New Populations of Two Threatened Species of Alsodes (Anura
Zoosyst. Evol. 94 (2) 2018, 349–358 | DOI 10.3897/zse.94.25189 New populations of two threatened species of Alsodes (Anura, Alsodidae) reveal the scarce biogeographic knowledge of the genus in the Andes of central Chile Claudio Correa1,*, Paulo Zepeda2, Nicolás Lagos3, Hugo Salinas4, R. Eduardo Palma2, Dayana Vásquez2,* 1 Departamento de Zoología, Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, Barrio Universitario S/N, Concepción, Chile 2 Departamento de Ecología, Facultad de Ciencias Biológicas, Pontificia Universidad Católica de Chile, Alameda 340, Santiago, Chile 3 Alianza Gato Andino, Jenner 152, B° La Quinta, Segunda Sección Villa Carlos Paz, Córdoba, Argentina 4 Ecodiversidad Consultores, Riñihue 1022, Puente Alto, Santiago, Chile http://zoobank.org/D9185A98-A5A3-4B0B-9010-E81BC732E6FA Corresponding author: Claudio Correa ([email protected]) Abstract Received 21 March 2018 High Andean environments of central Chile (32°–38°S) are inhabited by several endemic Accepted 1 June 2018 species of the genus Alsodes. Two of them, A. pehuenche and A. hugoi, have geographic Published 17 July 2018 distributions restricted to their type locality and surroundings. The Chilean government classifies A. pehuenche as Critically Endangered (like the IUCN) and A. hugoi as Vul- Academic editor: nerable. In this study we report 16 new localities of Alsodes, corresponding to first order Peter Bartsch streams, located in the Andes of Chile between 35°58’ and 36°32’S (1800–2470 m). In some of these sites, adults and juveniles morphologically similar to A. pehuenche and Key Words A. hugoi were observed, as well as specimens of Alsodes that could not be identified by their external morphology. -
Schinus Molle L.) to CONTROL RICE WEEVIL (Sitophilus Oryzae L.
154RESEARCH CHILEAN J. AGRIC. RES. - VOL. 69 - Nº 2 - 2009 BIOLOGICAL ACTIVITY OF ESSENTIAL OILS FROM LEAVES AND FRUITS OF PEPPER TREE (Schinus molle L.) TO CONTROL RICE WEEVIL (Sitophilus oryzae L.) 1 1 1* Verónica Benzi , Natalia Stefanazzi , and Adriana A. Ferrero ABSTRACT Rice weevil (Sitophilus oryzae L.) is a primary insect pest of stored grain. The development of resistance resulted in the application of synthetic insecticides. In recent years many plant essential oils have provided potential alternatives to currently used insect control agents. The Brazilian pepper tree (Schinus molle L. var. areira (L.) DC.�����������������) (Anacardiaceae) has different biological properties such as insecticidal activity. In this study, repellent, fumigant activity, nutritional indices, and feeding deterrent action were evaluated on S. oryzae adults. Filter paper impregnation was used to test fumigant toxicity, whereas treated whole wheat was used to evaluate repellent activity and a flour disk bioassay was done to evaluate feeding deterrent action and nutritional index alteration. Leaf essential oils showed repellent effects at both concentrations (0.04 and 0.4% w/w), while fruit essential oils lacked repellent activity. Both plant oils altered nutritional indices. Fruit essential oils had a strong feeding deterrent action (62%) while leaves had a slight effect (40.6%). With respect to fumigant activity, neither of the essential oils was found to be toxic. Key words: Schinus molle, Sitophilus oryzae, repellency, fumigant toxicity, nutritional indices, feeding deterrence. INTRODUCTION Resistance and toxicity problems of the synthetic insecticides have resulted in the necessity of finding Harvest grains are basic human food products (Padín more effective and healthier alternatives. -
Post-Evaluation Report for ODA Loan Projects 1999
PHILIPPINESPHILIPPINES Flood Forecasting and Warning System for Dam Operation Project (II) Report Date: October 1998 Field Survey: Not implemented 1 Project Summary and JBIC's Cooperation Flood Forecasting and Warning System for MYANMAR LAOS CHINA Dam Operation Project aims to contribute to THAILAND PHILIPPINES PACIFIC� VIETNAM MANILA mitigation of flood damage on human life and CAMBODIA OCEAN assets, and stabilize the lives of residents in SOUTH� the downstream reaches of the dams in the CHINA� SEA Philippines, a country that, due to its MALAYSIA geographic location, suffers serious flood SINGAPORE damage from typhoons, etc. every year. Under this project, the flood forecasting and INDONESIA� warning system was constructed at 5 major INDIAN OCEAN dams (Angat, Pantabangan, Binga, Cagayan River Ambuklao and Magat) on Luson Island, Luzon Island where are the most populated and ④� :Project industrialized parts of the Philippines. Of the five dams listed above, the dams at Angat and Pantabangan were covered by the “Flood Forecasting and Warning System for Ambuklao Dam Dam Operation Project (FFWS) (I)”. This Binga Dam project continued from that project, covering ⑧� the remaining three dams at Binga, Ambuklao ⑦� and Magat. The ODA loan covers the entire Magat Dam foreign currency portion of the project. ②� 2 Agno River ⑥� Pantabangan Dam Evaluation Results Angat Dam Pan pang River ①� ⑤� (1) Project Implementation Pasig River ⑨� (i) Project Scope Manila Bicol River There were no changes in the project ③� scope, and the project was implemented as planned. ◯ Flood Forecasting and Warning System � (ii) Implementation Schedule for Luzon Island Flood Forecasting and Warning System L/A NO. Executing Agency The completion of this project was 49 ①�Pan pang River� (Grant)� PAGASA� months (approximately 4 years) behind � (ABC system)� PAGASA� ②�Agno River� PH-P18� � schedule compared to the original plan. -
How to Survive Earthquakes and Tsunamis in Oregon
Living on Shaky Ground How to survive earthquakes and tsunamis in Oregon Copyright 2018, Oregon Office of Emergency Management with help from the Oregon Department of Geology and Mineral Industries. Originally adapted from Humboldt Earthquake Education Center at Humboldt State University. Reproduction by permission only. Disclaimer: This document is intended to promote earthquake and tsunami readiness. It is based on the best currently available scientific, engineering, and sociological research. Following its suggestions, however, does not guarantee the safety of an individual or of a structure. Contributors • Michael Murphy, Coos County • Patence Winningham, City of Eugene • Justin Ross, Multnomah County • Cynthia Valdivia, Washington County • Bonny Cushman, City of Portland • Barbara Ayers, Hood River County • Curtis Peetz, American Red Cross • John Bowles, Morrow County • Virginia Demaris, Lincoln County • Terri Eubanks, City of Ashland • Althea Rizzo, Oregon Office of Emergency Management • Paula Negele, Oregon Office of Emergency Management ii Oregon Office of Emergency Management Introduction You can prepare for the What do I do? next quake or tsunami an earthquake you should: During Some people think it is not worth preparing for • If you are indoors, DROP and take COVER an earthquake or a tsunami because whether you under a sturdy table or other furniture. HOLD survive or not is up to chance. NOT SO! ON to it and stay put until the shaking stops. Most Oregon buildings will survive even a large • Stay clear of items that can fall and injure you, earthquake, and so will you, especially if you such as windows, fireplaces and heavy furniture. follow the simple guidelines in this handbook • Stay inside. -
The 1964 Prince William Sound Earthquake Subduction Zone Steven C
Adv. Geophys. ms. Last saved: 2/12/2003 6:lO:OO PM 1 Crustal Deformation in Southcentral Alaska: The 1964 Prince William Sound Earthquake Subduction Zone Steven C. Cohen Geodynamics Branch, Goddard Space Flight Center, Greenbelt, MD 2077 1 email: Steven.C.Cohen @ .nasa.gov; phone: 301-6 14-6466 Jeffrey T. Freymueller Geophysical Institute, University of Alaska, Fairbanks, AK 99775 Outline: 1. Introduction 2. Tectonic, Geologic, and Seismologic Setting 3. Observed Crustal Motion 3.1 Coseismic Crustal Motion 3.2 Preseismic and Interseismic (pre-1964) Crustal Motion 3.3 Postseismic and Interseismic (post-1964) Crustal Motion 4. Models of Southcentral Alaska Preseismic and Postseismic Crustal Deformation 5. Conclusions 6. References Adv. Geophys. ms. Last saved: a1 a2003 6:lO:OO PM 2 1. Introduction The M, = 9.2 Prince William Sound (PWS) that struck southcentral Alaska on March 28, 1964, is one of the important earthquakes in history. The importance of this Great Alaska Earthquake lies more in its scientific than societal impact. While the human losses in the PWS earthquake were certainly tragic, the sociological impact of the earthquake was less than that of is earthquakes that have struck heavily populated locales. By contrast Earth science, particularly tectonophysics, seismology, and geodesy, has benefited enormously from studies of this massive earthquake. The early 1960s was a particularly important time for both seismology and tectonophysics. Seismic instrumentation and analysis techniques were undergoing considerable modernization. For example, the VELA UNIFORM program for nuclear test detection resulted in the deployment of the World Wide Standard Seismographic Network in the late 1950s and early 1960s (Lay and Wallace, 1995).