Catalog of Earthquakes, 2000 B.C.–1979, 1981
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USMA the War with Japan.Pt.1 1941-12 1942.08.Pdf
THE COMMAND AND GENERAL STAFF COLLEGE LIBRARY 940.542 U57w 1950 Call Number CGSC Form 154 (Rev) 22 Oct 52 USACGSC—PO-3396—1 Apr 60—5M RCftfRICTED THE WAR WITH JAPAN PART 1 (December 1941 to August 1942) mnn urn mt BY TAG m mmu DEPARTMENT OP MILITARY ART AND ENGINEERING UNITED STATES MILITARY ACADEMY WEST POINT, NEW YORK 195O REQTIUOTHD THE WAR WITH JAPAN PART 1 (December 1941 to August 1942) DEPARTMENT OF MILITARY ART AND ENGINEERING UNITED STATES MILITARY ACADEMY WEST POINT, NEW YORK 195O %\ (\ \! REOTRIOTBD PREFACE This account of the war with Japan has been written for use in the instruction of cadets at the United States Military Academy. It is based for the most part on material furnished by the Historical Division, Department of the Army. Much valuable information has been obtained from the publications of the United States Stra tegic Bombing Survey and the Office of Naval Intelligence. How ever, in acknowledging indebtedness to others it is not desired to place on them the responsibility for any factual errors or for any conclusions drawn. This and other pamphlets on World War II are constantly being revised as additional information becomes available. It will be ap preciated if military personnel who note any apparent errors or dis crepancies, or who have comments or suggestions for the improve ment of the subject matter, will communicate them to: The Professor of Military Art and Engineering U. S. Military Academy West Point, N. Y. August 1947 ARMY-USMA. WEST PDINT. N.Y. 225O 4-3-5O CONTENTS PAGE INTRODUCTION 1 STRATEGIC CONSIDERATIONS 2 JAPANESE WAR PLAN 8 JAPANESE STRATEGIC OFFENSIVE y 10 InitiaLPlaris and Preparations 10 Central Pacific Operations 14 Pearl. -
New Empirical Relationships Among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement
Bulletin of the Seismological Society of America, Vol. 84, No. 4, pp. 974-1002, August 1994 New Empirical Relationships among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement by Donald L. Wells and Kevin J. Coppersmith Abstract Source parameters for historical earthquakes worldwide are com piled to develop a series of empirical relationships among moment magnitude (M), surface rupture length, subsurface rupture length, downdip rupture width, rupture area, and maximum and average displacement per event. The resulting data base is a significant update of previous compilations and includes the ad ditional source parameters of seismic moment, moment magnitude, subsurface rupture length, downdip rupture width, and average surface displacement. Each source parameter is classified as reliable or unreliable, based on our evaluation of the accuracy of individual values. Only the reliable source parameters are used in the final analyses. In comparing source parameters, we note the fol lowing trends: (1) Generally, the length of rupture at the surface is equal to 75% of the subsurface rupture length; however, the ratio of surface rupture length to subsurface rupture length increases with magnitude; (2) the average surface dis placement per event is about one-half the maximum surface displacement per event; and (3) the average subsurface displacement on the fault plane is less than the maximum surface displacement but more than the average surface dis placement. Thus, for most earthquakes in this data base, slip on the fault plane at seismogenic depths is manifested by similar displacements at the surface. Log-linear regressions between earthquake magnitude and surface rupture length, subsurface rupture length, and rupture area are especially well correlated, show ing standard deviations of 0.25 to 0.35 magnitude units. -
Journal Pre-Proof
Journal Pre-proof From Historical Seismology to seismogenic source models, 20 years on: Excerpts from the Italian experience Gianluca Valensise, Paola Vannoli, Pierfrancesco Burrato, Umberto Fracassi PII: S0040-1951(19)30296-3 DOI: https://doi.org/10.1016/j.tecto.2019.228189 Reference: TECTO 228189 To appear in: Tectonophysics Received date: 1 April 2019 Revised date: 20 July 2019 Accepted date: 5 September 2019 Please cite this article as: G. Valensise, P. Vannoli, P. Burrato, et al., From Historical Seismology to seismogenic source models, 20 years on: Excerpts from the Italian experience, Tectonophysics(2019), https://doi.org/10.1016/j.tecto.2019.228189 This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. Please note that, during the production process, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. © 2019 Published by Elsevier. Journal Pre-proof From Historical Seismology to seismogenic source models, 20 years on: excerpts from the Italian experience Gianluca Valensise, Paola Vannoli, Pierfrancesco Burrato & Umberto Fracassi Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy Contents 1. Introduction 1.1. Why Historical Seismology 1.2. A brief history of Historical Seismology 1.3. Representing and exploiting Historical Seismology data 2. -
Checklist of Fish and Invertebrates Listed in the CITES Appendices
JOINTS NATURE \=^ CONSERVATION COMMITTEE Checklist of fish and mvertebrates Usted in the CITES appendices JNCC REPORT (SSN0963-«OStl JOINT NATURE CONSERVATION COMMITTEE Report distribution Report Number: No. 238 Contract Number/JNCC project number: F7 1-12-332 Date received: 9 June 1995 Report tide: Checklist of fish and invertebrates listed in the CITES appendices Contract tide: Revised Checklists of CITES species database Contractor: World Conservation Monitoring Centre 219 Huntingdon Road, Cambridge, CB3 ODL Comments: A further fish and invertebrate edition in the Checklist series begun by NCC in 1979, revised and brought up to date with current CITES listings Restrictions: Distribution: JNCC report collection 2 copies Nature Conservancy Council for England, HQ, Library 1 copy Scottish Natural Heritage, HQ, Library 1 copy Countryside Council for Wales, HQ, Library 1 copy A T Smail, Copyright Libraries Agent, 100 Euston Road, London, NWl 2HQ 5 copies British Library, Legal Deposit Office, Boston Spa, Wetherby, West Yorkshire, LS23 7BQ 1 copy Chadwick-Healey Ltd, Cambridge Place, Cambridge, CB2 INR 1 copy BIOSIS UK, Garforth House, 54 Michlegate, York, YOl ILF 1 copy CITES Management and Scientific Authorities of EC Member States total 30 copies CITES Authorities, UK Dependencies total 13 copies CITES Secretariat 5 copies CITES Animals Committee chairman 1 copy European Commission DG Xl/D/2 1 copy World Conservation Monitoring Centre 20 copies TRAFFIC International 5 copies Animal Quarantine Station, Heathrow 1 copy Department of the Environment (GWD) 5 copies Foreign & Commonwealth Office (ESED) 1 copy HM Customs & Excise 3 copies M Bradley Taylor (ACPO) 1 copy ^\(\\ Joint Nature Conservation Committee Report No. -
Bridges Across Oceans: Initial Impact Assessment of the Philippines Nautical Highway System and Lessons for Southeast Asia
Bridges across Oceans Initial Impact Assessment of the Philippines Nautical Highway System and Lessons for Southeast Asia April 2010 0 2010 Asian Development Bank All rights reserved. Published 2010. Printed in the Philippines ISBN 978-971-561-896-0 Publication Stock No. RPT101731 Cataloging-In-Publication Data Bridges across Oceans: Initial Impact Assessment of the Philippines Nautical Highway System and Lessons for Southeast Asia. Mandaluyong City, Philippines: Asian Development Bank, 2010. 1. Transport Infrastructure. 2. Southeast Asia. I. Asian Development Bank. The views expressed in this book are those of the authors and do not necessarily reflect the views and policies of the Asian Development Bank (ADB) or its Board of Governors or the governments they represent. ADB does not guarantee the accuracy of the data included in this publication and accepts no responsibility for any consequence of their use. By making any designation of or reference to a particular territory or geographic area, or by using the term “country” in this document, ADB does not intend to make any judgments as to the legal or other status of any territory or area. ADB encourages printing or copying information exclusively for personal and noncommercial use with proper acknowledgment of ADB. Users are restricted from reselling, redistributing, or creating derivative works for commercial purposes without the express, written consent of ADB. Note: In this report, “$” refers to US dollars. 6 ADB Avenue, Mandaluyong City 1550 Metro Manila, Philippines Tel +63 2 632 -
The 2013–2018 Matese and Beneventano Seismic Sequences (Central–Southern Apennines): New Constraints on the Hypocentral Depth Determination
geosciences Article The 2013–2018 Matese and Beneventano Seismic Sequences (Central–Southern Apennines): New Constraints on the Hypocentral Depth Determination Brando Trionfera 1, Alberto Frepoli 2,*, Gaetano De Luca 2, Pasquale De Gori 2 and Carlo Doglioni 1,2 1 Dipartimento Scienze della Terra, Università La Sapienza, 00185 Roma, Italy; [email protected] (B.T.); [email protected] (C.D.) 2 Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Nazionale Terremoti, 00185 Roma, Italy; [email protected] (G.D.L.); [email protected] (P.D.G.) * Correspondence: [email protected] Received: 19 November 2019; Accepted: 24 December 2019; Published: 30 December 2019 Abstract: The Matese and Beneventano areas coincide with the transition from the central to the southern Apennines and are characterized by both SW- and NE-dipping normal faulting seismogenic structures, responsible for the large historical earthquakes. We studied the Matese and Beneventano seismicity by means of high-precision locations of earthquakes spanning from 29 December 2013 to 4 September 2018. Events were located by using all of the available data from temporary and permanent stations in the area and a 1D computed velocity model, inverting the dataset with the Velest code. For events M > 2.8 we used P- and S-waves arrival times of the strong motion stations located in the study area. A constant value of 1.83 for Vp/Vs was computed with a modified Wadati method. The dataset consists of 2378 earthquakes, 18,715 P- and 12,295 S-wave arrival times. We computed 55 new fault plane solutions. The mechanisms show predominantly normal fault movements, with T-axis trends oriented NE–SW. -
What Works and Does Not Work in the Science and Social Science Of
What Works and Does not Work in the Science and Social Science of Earthquake Vulnerability? Report of an International Workshop held in the Department of Earth Sciences, University of Oxford on 28 th and 29 th January, 2011. Philip England1, John Holmes, James Jackson & Barry Parsons This Workshop, supported by Shell, Chun Wo Development Holdings (Hong Kong), and the National Centre for Earth Observation, was held in response to NERC’s Action Plan: Increasing resilience through improved hazard forecasting and take-up of scientific advice in earthquake-prone and volcanic regions. Over fifty scientists, social scientists, and engineers attended the Workshop, bringing exten- sive experience of earthquake risk from Greece, India, Italy, Iran, Pakistan, Turkey, and the USA. The list of the international participants is given in Appendix B, and electronic versions of their presentations can be found on the Workshop website. The participants considered earthquake resilience in a global context, but were also aware of the constraints (Rees) associated with NERC’s Programme in Increasing Resilience to Natural Hazards, particularly the limited budget and time frame. Their discussion therefore was also conditioned by the following questions: (i) Which areas in UK science can make the greatest impact in increasing resilience and reducing uncertainty about risk? (ii) What practical outcomes can be achieved within the financial and temporal constraints of this programme? The following recommendations arose from the two days of discussion: - The overwhelming priority, when considering resilience to earthquakes, is the risk to human life in the developing world. (Section 1) - The greatest risk to human life from earthquakes lies not at plate boundaries, but in the conti- nental interiors, where growing populations are exposed to earthquake risk from distributed networks of faults that are poorly characterized. -
Ferrara Di Ferrara
PROVINCIA COMUNE DI FERRARA DI FERRARA Visit Ferraraand its province United Nations Ferrara, City of Educational, Scientific and the Renaissance Cultural Organization and its Po Delta Parco Urbano G. Bassani Via R. Bacchelli A short history 2 Viale Orlando Furioso Living the city 3 A year of events CIMITERO The bicycle, queen of the roads DELLA CERTOSA Shopping and markets Cuisine Via Arianuova Viale Po Corso Ercole I d’Este ITINERARIES IN TOWN 6 CIMITERO EBRAICO THE MEDIAEVAL Parco Corso Porta Po CENTRE Via Ariosto Massari Piazzale C.so B. Rossetti Via Borso Stazione Via d.Corso Vigne Porta Mare ITINERARIES IN TOWN 20 Viale Cavour THE RENAISSANCE ADDITION Corso Ercole I d’Este Via Garibaldi ITINERARIES IN TOWN 32 RENAISSANCE Corso Giovecca RESIDENCES Piazza AND CHURCHES Trento e Trieste V. Mazzini ITINERARIES IN TOWN 40 Parco Darsena di San Paolo Pareschi WHERE THE RIVER Piazza Travaglio ONCE FLOWED Punta della ITINERARIES IN TOWN 46 Giovecca THE WALLS Via Cammello Po di Volano Via XX Settembre Via Bologna Porta VISIT THE PROVINCE 50 San Pietro Useful information 69 Chiesa di San Giorgio READER’S GUIDE Route indications Along with the Pedestrian Roadsigns sited in the Historic Centre, this booklet will guide the visitor through the most important areas of the The “MUSEO DI QUALITÀ“ city. is recognised by the Regional Emilia-Romagna The five themed routes are identified with different colour schemes. “Istituto per i Beni Artistici Culturali e Naturali” Please, check the opening hours and temporary closings on the The starting point for all these routes is the Tourist Information official Museums and Monuments schedule distributed by Office at the Estense Castle. -
Geochemical Monitoring of the 2012 Po Valley Seismic Sequence: a Review and Update
CHEMGE-18183; No of Pages 16 Chemical Geology xxx (2016) xxx–xxx Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Geochemical monitoring of the 2012 Po Valley seismic sequence: A review and update G. Martinelli a,⁎,A.Dadomob, F. Italiano c,R.Petrinid,F.F.Slejkoe a ARPAE Environmental Protection Agency, Emilia Romagna Region, 42100 Reggio Emilia, Italy b Geoinvest Srl, Piacenza, Italy c INGV Istituto Nazionale Geofisica Vulcanologia, Palermo, Italy d University of Pisa, Dept. Earth Sciences, Pisa, Italy e University of Trieste, Dept. Mathematics and Geosciences, Trieste, Italy article info abstract Article history: A seismic swarm characterized by a Ml = 5.9 mainshock occurred in the Po Valley, northern Italy, in 2012. The Received 15 July 2016 area has been studied for active compressional tectonics since the beginning of the twentieth century. A variety Received in revised form 24 November 2016 of geophysical and geochemical parameters have been utilized with the purpose of identifying possible precur- Accepted 2 December 2016 sory signals. This paper considers groundwater level data and geochemical data both in groundwaters and in Available online xxxx gases. All considered parameters have led to the conclusion that possible long and medium precursory trends have been identified in geofluids. No short-term precursors have been clearly identified. Hydrogeological and Keywords: Earthquake precursor geochemical monitoring could be more effectively utilized in a different geological context, and seismic hazard Earthquake effect reduction procedures could benefitfromgeofluid monitoring. Geofluid monitoring © 2016 Elsevier B.V. All rights reserved. Geochemical monitoring Emilia earthquake Po Valley 1. Introduction 2. -
Kodiak ___+. 10 +. 12 +. 01 +. 03 +. 11
MAY 1939 MONTHLY WEATHER REVIEW 153 TABLE1.-Averages, departures, and edremes of atmospheric prea- 124'24' W. A strong oceanic anticyclone was pressing awe at aea level, North Paci$c Ocean, May 1030, at selected at the time close upon the California coast. stations Typhoon.-Subjoined is an account by the Reverend Depar- Bernard F. Doucette, S. J., Weather Bureau, Manila, :wefrom EIighest Date Lowest Date P. I., of the typhoon of April 29 to May 9, 1939, in waters normal of the Far East. Mail reports from ships caught in this Inchu Inch Jnchea Inchea typhoon indicate its greatest intensity to have occurred on Point Barrow_________ 29.89 -0.10 30.22 12 29.64 5 the 8th. The British steamship LacMan, noted by Father Dutch Harbor ________ 29.94 +. 10 30.44 8 29.36 17 St. Paul. _______-_--__28.96 +. 12 30.40 8 29.30 17 Doucette as ha.ving a south wind of force 9, in 31' N., Kodiak _______________ 29.83 -. 01 30.30 1 29.54 n 29.93 -. 06 30.33 10 29.12 28 136' E., at 1 p. m. of that date, ran into the full force of 30.07 +. 06 30.32 7 29.73 29 the storm shortly after 3. p. m. with a north gale of hur- 30.00 +. 01 30.23 19 29.78 29 29.85 .OO 29.50 16,20,21 29.80 4,8,24,29,31 ricane intensity. The lowest known barometer in con- 30.04 -. 01 30.15 13 29.88 9 nection with the typhoon was 29.06, read on board the 30.00 +. -
Philippines 13
©Lonely Planet Publications Pty Ltd Philippines North Luzon p119 Manila #_ Around Manila p101 p52 Southeast Mindoro Luzon p198 p171 Cebu & Boracay & Eastern Western Visayas Palawan Visayas p283 p383 p217 Mindanao p348 Paul Harding, Greg Bloom, Celeste Brash, Michael Grosberg, Iain Stewart PLAN YOUR TRIP ON THE ROAD Welcome MANILA . 52 Subic Bay & Olongapo . 115 to the Philippines . 6 Mt Pinatubo Region . 117 The Philippines Map . 8 AROUND MANILA . 101 The Philippines’ Top 15 . 10 NORTH LUZON . 119 Need to Know . 18 Corregidor . 103 Zambales Coast . 122 First Time Philippines . 20 South of Manila . 103 Tagaytay & Lake Taal . 103 Southern What’s New . 22 Zambales Coast . 122 Taal . 107 If You Like . 23 Iba & Botolan . 123 Batangas . 108 Month by Month . 25 North of Iba . 124 Anilao . 109 Itineraries . 28 Lingayen Gulf . 124 Mt Banahaw . 110 Diving in the Bolinao & Patar Beach . 124 Pagsanjan . 110 Philippines . 33 Hundred Islands Outdoor Activities . 39 Lucban . 111 National Park . 124 Eat & Drink Lucena . 112 San Juan (La Union) . 125 Like a Local . .. 44 North of Manila . 112 Ilocos . 127 Regions at a Glance . 49 Angeles & Clark Airport . 113 Vigan . 127 ALENA OZEROVA/SHUTTERSTOCK © OZEROVA/SHUTTERSTOCK ALENA © SHANTI HESSE/SHUTTERSTOCK EL NIDO P401 TOM COCKREM/GETTY IMAGES © IMAGES COCKREM/GETTY TOM STREET FOOD, PUERTO PRINCESA P385 Contents Laoag . 132 San Jose . 164 Mt Isarog Pagudpud & Around . 134 Northern Sierra Madre National Park . 177 The Cordillera . 135 Natural Park . 164 Caramoan Peninsula . 177 Baguio . 137 Tuguegarao . 165 Tabaco . 180 Kabayan . 144 Santa Ana . 166 Legazpi . 180 Mt Pulag National Park . 146 Batanes Islands . 166 Around Legazpi . -
Areal Distribution of Ground Effects Induced by Strong Earthquakes in the Southern Apennines (Italy)
AREAL DISTRIBUTION OF GROUND EFFECTS INDUCED BY STRONG EARTHQUAKES IN THE SOUTHERN APENNINES (ITALY) S. PORFIDO1, E. ESPOSITO1,E.VITTORI2, G. TRANFAGLIA3, A.M. MICHETTI4, M. BLUMETTI5, L. FERRELI2, L. GUERRIERI2 and L. SERVA2 1Istituto di Ricerca Geomare Sud - C.N.R., Via A. Vespucci, 9, 80142, Napoli, Italy E-mail: porfi[email protected] 2ANPA – Agenzia Nazionale per la Protezione dell’Ambiente, Via Vitaliano Brancati, 48, 00144, Rome, Italy 3Servizio Idrografico e Mareografico, Via Marchese Campodisola 21, 80133 Napoli, Italy 4Dipartimento di Scienze CC.FF.MM, Universitá dell’Insubria, Via Lucini, 3, 22100, Como, Italy 5Dipartimento Servizi Tecnici Nazionali - Servizio Sismico, Via Curtatone, 3, 00185, Rome, Italy (Received 2 January 2002; Accepted 17 June 2002) Abstract. Moderate to strong crustal earthquakes are generally accompanied by a distinctive pattern of coseismic geological phenomena, ranging from surface faulting to ground cracks, landslides, liquefaction/compaction, which leave a permanent mark in the landscape. Therefore, the repetition of surface faulting earthquakes over a geologic time interval determines a characteristic morphology closely related to seismic potential. To support this statement, the areal distribution and dimensions of effects of recent historical earthquakes in the Southern Apennines are being investigated in detail. This paper presents results concerning the 26 July 1805 earthquake in the Molise region, (I =X MCS, M = 6.8), and the 23 November 1980 earthquake in the Campania and Basilicata regions (I =XMSK,Ms = 6.9). Landslide data are also compared with two other historical earthquakes in the same region with similar macroseismic intensity. The number of significant effects (either ground deformation or hydrological anomalies) versus their minimum distance from the causative fault have been statistically analyzed, finding characteristic relationships.