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Washington Division of Geology and Earth Resources Open File Report
l 122 EARTHQUAKES AND SEISMOLOGY - LEGAL ASPECTS OPEN FILE REPORT 92-2 EARTHQUAKES AND Ludwin, R. S.; Malone, S. D.; Crosson, R. EARTHQUAKES AND SEISMOLOGY - LEGAL S.; Qamar, A. I., 1991, Washington SEISMOLOGY - 1946 EVENT ASPECTS eanhquak:es, 1985. Clague, J. J., 1989, Research on eanh- Ludwin, R. S.; Qamar, A. I., 1991, Reeval Perkins, J. B.; Moy, Kenneth, 1989, Llabil quak:e-induced ground failures in south uation of the 19th century Washington ity of local government for earthquake western British Columbia [abstract). and Oregon eanhquake catalog using hazards and losses-A guide to the law Evans, S. G., 1989, The 1946 Mount Colo original accounts-The moderate sized and its impacts in the States of Califor nel Foster rock avalanches and auoci earthquake of May l, 1882 [abstract). nia, Alaska, Utah, and Washington; ated displacement wave, Vancouver Is Final repon. Maley, Richard, 1986, Strong motion accel land, British Columbia. erograph stations in Oregon and Wash Hasegawa, H. S.; Rogers, G. C., 1978, EARTHQUAKES AND ington (April 1986). Appendix C Quantification of the magnitude 7.3, SEISMOLOGY - NETWORKS Malone, S. D., 1991, The HAWK seismic British Columbia earthquake of June 23, AND CATALOGS data acquisition and analysis system 1946. [abstract). Berg, J. W., Jr.; Baker, C. D., 1963, Oregon Hodgson, E. A., 1946, British Columbia eanhquak:es, 1841 through 1958 [ab Milne, W. G., 1953, Seismological investi earthquake, June 23, 1946. gations in British Columbia (abstract). stract). Hodgson, J. H.; Milne, W. G., 1951, Direc Chan, W.W., 1988, Network and array anal Munro, P. S.; Halliday, R. J.; Shannon, W. -
Section 5.4.3: Risk Assessment – Flood
SECTION 5.4.3: RISK ASSESSMENT – FLOOD 5.4.3 FLOOD This section provides a profile and vulnerability assessment for the flood hazard. HAZARD PROFILE This section provides hazard profile information including description, extent, location, previous occurrences and losses and the probability of future occurrences. Description Floods are one of the most common natural hazards in the U.S. They can develop slowly over a period of days or develop quickly, with disastrous effects that can be local (impacting a neighborhood or community) or regional (affecting entire river basins, coastlines and multiple counties or states) (Federal Emergency Management Agency [FEMA], 2006). Most communities in the U.S. have experienced some kind of flooding, after spring rains, heavy thunderstorms, coastal storms, or winter snow thaws (George Washington University, 2001). Floods are the most frequent and costly natural hazards in New York State in terms of human hardship and economic loss, particularly to communities that lie within flood prone areas or flood plains of a major water source. The FEMA definition for flooding is “a general and temporary condition of partial or complete inundation of two or more acres of normally dry land area or of two or more properties from the overflow of inland or tidal waters or the rapid accumulation of runoff of surface waters from any source (FEMA, Date Unknown).” The New York State Disaster Preparedness Commission (NYSDPC) and the National Flood Insurance Program (NFIP) indicates that flooding could originate from one -
Fstate Scientist: Omond Mckillop Solandt and Government Science
fState Scientist: Omond McKillop Solandt and Government Science in War and Hostile Peace, 1939-1956/ Scientifique.de l'Etat: Omond McKillop Solandt et la Science du Gouvernement lors de la Guerre et de la Paix Hostile, 1939-1956 A Thesis Submitted to the Division of Graduate Studies of the Royal Military College of Canada by Jason Sean Ridler, MA Royal Military College of Canada, 2001 BA (Hons.) York University, 1999 In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy August 2008 ©This thesis may be used within the Department of National Defence but copyright for open publication remains the property of the author. Library and Bibliotheque et 1*1 Archives Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-47901-8 Our file Notre reference ISBN: 978-0-494-47901-8 NOTICE: AVIS: The author has granted a non L'auteur a accorde une licence non exclusive exclusive license allowing Library permettant a la Bibliotheque et Archives and Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par Plntemet, prefer, telecommunication or on the Internet, distribuer et vendre des theses partout dans loan, distribute and sell theses le monde, a des fins commerciales ou autres, worldwide, for commercial or non sur support microforme, papier, electronique commercial purposes, in microform, et/ou autres formats. paper, electronic and/or any other formats. -
Miles Poindexter Papers, 1897-1940
Miles Poindexter papers, 1897-1940 Overview of the Collection Creator Poindexter, Miles, 1868-1946 Title Miles Poindexter papers Dates 1897-1940 (inclusive) 1897 1940 Quantity 189.79 cubic feet (442 boxes ) Collection Number 3828 (Accession No. 3828-001) Summary Papers of a Superior Court Judge in Washington State, a Congressman, a United States Senator, and a United States Ambassador to Peru Repository University of Washington Libraries, Special Collections. Special Collections University of Washington Libraries Box 352900 Seattle, WA 98195-2900 Telephone: 206-543-1929 Fax: 206-543-1931 [email protected] Access Restrictions Open to all users. Languages English. Sponsor Funding for encoding this finding aid was partially provided through a grant awarded by the National Endowment for the Humanities Biographical Note Miles Poindexter, attorney, member of Congress from Washington State, and diplomat, was born in 1868 in Tennessee and grew up in Virginia. He attended Washington and Lee University (undergraduate and law school), receiving his law degree in 1891. He moved to Walla Walla, Washington, was admitted to the bar and began his law practice. He entered politics soon after his arrival and ran successfully for County Prosecutor as a Democrat in 1892. Poindexter moved to Spokane in 1897 where he continued the practice of law. He switched to the Republican Party in Spokane, where he received an appointment as deputy prosecuting attorney (1898-1904). In 1904 he was elected Superior Court Judge. Poindexter became identified with progressive causes and it was as a progressive Republican and a supporter of Theodore Roosevelt that he was elected to the House of Representatives in 1908 and to the Senate in 1910. -
Topographic Power Spectra of Cratered Terrains: 10.1002/2014JE004746 Theory and Application to the Moon
JournalofGeophysicalResearch: Planets RESEARCH ARTICLE Topographic power spectra of cratered terrains: 10.1002/2014JE004746 Theory and application to the Moon Key Points: Margaret A. Rosenburg1, Oded Aharonson2, and Re’em Sari3 • Impact cratering produces characteristic variations in the 1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA, 2Department topographic PSD of Earth and Planetary Sciences, Weizmann Institute of Technology, Rehovot, Israel, 3Racah Institute of Physics, Hebrew • The size-frequency distribution and shape of craters control University of Jerusalem, Jerusalem, Israel PSD variations • We investigate the topographic PSD on model terrains and Impact cratering produces characteristic variations in the topographic power spectral density lunar topography Abstract (PSD) of cratered terrains, which are controlled by the size-frequency distribution of craters and the spectral content (shape) of individual features. These variations are investigated here in two parallel Correspondence to: approaches. First, a cratered terrain model, based on Monte Carlo emplacement of craters and benchmarked M. A. Rosenburg, [email protected] by an analytical formulation of the one-dimensional PSD, is employed to generate topographic surfaces at a range of size-frequency power law exponents and shape dependencies. For self-similar craters, the slope of the PSD, , varies inversely with that of the production function, , leveling off to 0 at high (surface Citation: Rosenburg, M. A., O. Aharonson, topography dominated by the smallest craters) and maintaining a roughly constant value ( ∼ 2) at low and R. Sari (2015), Topographic (surface topography dominated by the largest craters). The effects of size-dependent shape parameters power spectra of cratered terrains: and various crater emplacement rules are also considered. -
Annual Report 2013.Pdf
ATOMIC HERITAGE FOUNDATION Preserving & Interpreting Manhattan Project History & Legacy preserving history ANNUAL REPORT 2013 WHY WE SHOULD PRESERVE THE MANHATTAN PROJECT “The factories and bombs that Manhattan Project scientists, engineers, and workers built were physical objects that depended for their operation on physics, chemistry, metallurgy, and other nat- ural sciences, but their social reality - their meaning, if you will - was human, social, political....We preserve what we value of the physical past because it specifically embodies our social past....When we lose parts of our physical past, we lose parts of our common social past as well.” “The new knowledge of nuclear energy has undoubtedly limited national sovereignty and scaled down the destructiveness of war. If that’s not a good enough reason to work for and contribute to the Manhattan Project’s historic preservation, what would be? It’s certainly good enough for me.” ~Richard Rhodes, “Why We Should Preserve the Manhattan Project,” Bulletin of the Atomic Scientists, May/June 2006 Photographs clockwise from top: J. Robert Oppenheimer, General Leslie R. Groves pinning an award on Enrico Fermi, Leona Woods Marshall, the Alpha Racetrack at the Y-12 Plant, and the Bethe House on Bathtub Row. Front cover: A Bruggeman Ranch property. Back cover: Bronze statues by Susanne Vertel of J. Robert Oppenheimer and General Leslie Groves at Los Alamos. Table of Contents BOARD MEMBERS & ADVISORY COMMITTEE........3 Cindy Kelly, Dorothy and Clay Per- Letter from the President..........................................4 -
On R.E Size Effect Measurements Fermi
V "" ON R.E SIZE EFFECT MEASUREMENTS FERMI SURFACE IN INDIUM D.G.deGROOT V-' VRIJE UNIVERSITEIT TE AMSTERDAM ON R.F. SIZE EFFECT MEASUREMENTS AND THE FERMI SURFACE IN INDIUM ACADEMISCH PROEFSCHRIFT TER VERKRIJGING VAN DE GRAAD VAN DOCTOR IN DE WISKUNDE EN NATUURWETENSCHAPPEN AAN DE VRIJE UNIVERSITEIT TE AMSTERDAM, OP GEZAG VAN DE RECTOR MAGNIFICUS MR.I.A.DIEPENHORST, HOOGLERAAR IN DE FACULTEIT DER RECHTSGELEERDHEID, IN HET OPENBAAR TE VERDEDIGEN OP DONDERDAG 2 MEI 1974 TE 13.30 UUR IN HET HOOFDGEBOUW DER UNIVERSITEIT, DE BOELELAAN 1105 DOOR DIRK GEERT DE GROOT. GEBOREN TE EINDHOVEN *hk r r PROMOTOR: DR. A. LODDER COREFERENT: DR. J.H.P. VAN WEEREN This investigation was part of the research program of the "Stichting voor Fundamenteel Onderzoek der Materie (F.O.M.)", which is financially supported by the "Nederlandse Organisatie voor Zuiver Wetenschappelijk Onderzoek (Z.W.O.)". STELLINGEN 1. Het is gewenst in de berekening van de laag freguente ruis in de verzadigingsstroom in avalanche diodes naast de schrootruis in de injectiestroom andere ruiscomponenten te betrekken. 2. Bij het onderzoek van anomalieen in de transmissie van electromagnetische golven door metaalkristallen vormt de ondergrond in de transmissie in vele gevallen een niet te scheiden component van het signaal. 3. De benaming O.P.W. berekening voor een pseudopotentiaal interpolatie schema, waarbij de Fouriercomponenten van de pseudopotentiaal als aan te passsen parameters worden ge- hanteerd, wekt ten onrechte de indruk dat de gebruikte golffuncties orthogonaal staan op de atomaire pit golf- functies. 4. Het is gewenst dat de Nederlandse regering een prejudiciele beschikking uitlokt, die tot gevolg zal hebben dat dienst- merken onder de beschermende werking van de Eenvormige Beneluxwet op de Warenmerken worden gebracht. -
University of Cincinnati
UNIVERSITY OF CINCINNATI Date:__7/30/07_________________ I, __ MUNISH GUPTA_____________________________________, hereby submit this work as part of the requirements for the degree of: DOCTORATE OF PHILOSOPHY (Ph.D) in: MATERIALS SCIENCE AND ENGINEERING It is entitled: LOW-PRESSURE AND ATMOSPHERIC PRESSURE PLASMA POLYMERIZED SILICA-LIKE FILMS AS PRIMERS FOR ADHESIVE BONDING OF ALUMINUM This work and its defense approved by: Chair: __Dr. F. JAMES BOERIO ___ ______ __Dr. GREGORY BEAUCAGE __ ___ __ __Dr. RODNEY ROSEMAN _____ ___ __Dr. JUDE IROH _ _____________ _______________________________ LOW-PRESSURE AND ATMOSPHERIC PRESSURE PLASMA POLYMERIZED SILICA-LIKE FILMS AS PRIMERS FOR ADHESIVE BONDING OF ALUMINUM A dissertation submitted to the Division of Research and Advanced Studies of the University of Cincinnati in partial fulfillment of the requirements for the degree of DOCTORATE OF PHILOSOPHY (Ph.D) in the Department of Chemical and Material Engineering of the College of Engineering 2007 by Munish Gupta M.S., University of Cincinnati, 2005 B.E., Punjab Technical University, India, 2000 Committee Chair: Dr. F. James Boerio i ABSTRACT Plasma processes, including plasma etching and plasma polymerization, were investigated for the pretreatment of aluminum prior to structural adhesive bonding. Since native oxides of aluminum are unstable in the presence of moisture at elevated temperature, surface engineering processes must usually be applied to aluminum prior to adhesive bonding to produce oxides that are stable. Plasma processes are attractive for surface engineering since they take place in the gas phase and do not produce effluents that are difficult to dispose off. Reactive species that are generated in plasmas have relatively short lifetimes and form inert products. -
Geologic Map of the Victoria Quadrangle (H02), Mercury
H01 - Borealis Geologic Map of the Victoria Quadrangle (H02), Mercury 60° Geologic Units Borea 65° Smooth plains material 1 1 2 3 4 1,5 sp H05 - Hokusai H04 - Raditladi H03 - Shakespeare H02 - Victoria Smooth and sparsely cratered planar surfaces confined to pools found within crater materials. Galluzzi V. , Guzzetta L. , Ferranti L. , Di Achille G. , Rothery D. A. , Palumbo P. 30° Apollonia Liguria Caduceata Aurora Smooth plains material–northern spn Smooth and sparsely cratered planar surfaces confined to the high-northern latitudes. 1 INAF, Istituto di Astrofisica e Planetologia Spaziali, Rome, Italy; 22.5° Intermediate plains material 2 H10 - Derain H09 - Eminescu H08 - Tolstoj H07 - Beethoven H06 - Kuiper imp DiSTAR, Università degli Studi di Napoli "Federico II", Naples, Italy; 0° Pieria Solitudo Criophori Phoethontas Solitudo Lycaonis Tricrena Smooth undulating to planar surfaces, more densely cratered than the smooth plains. 3 INAF, Osservatorio Astronomico di Teramo, Teramo, Italy; -22.5° Intercrater plains material 4 72° 144° 216° 288° icp 2 Department of Physical Sciences, The Open University, Milton Keynes, UK; ° Rough or gently rolling, densely cratered surfaces, encompassing also distal crater materials. 70 60 H14 - Debussy H13 - Neruda H12 - Michelangelo H11 - Discovery ° 5 3 270° 300° 330° 0° 30° spn Dipartimento di Scienze e Tecnologie, Università degli Studi di Napoli "Parthenope", Naples, Italy. Cyllene Solitudo Persephones Solitudo Promethei Solitudo Hermae -30° Trismegisti -65° 90° 270° Crater Materials icp H15 - Bach Australia Crater material–well preserved cfs -60° c3 180° Fresh craters with a sharp rim, textured ejecta blanket and pristine or sparsely cratered floor. 2 1:3,000,000 ° c2 80° 350 Crater material–degraded c2 spn M c3 Degraded craters with a subdued rim and a moderately cratered smooth to hummocky floor. -
Art-Related Archival Materials in the Chicago Area
ART-RELATED ARCHIVAL MATERIALS IN THE CHICAGO AREA Betty Blum Archives of American Art American Art-Portrait Gallery Building Smithsonian Institution 8th and G Streets, N.W. Washington, D.C. 20560 1991 TRUSTEES Chairman Emeritus Richard A. Manoogian Mrs. Otto L. Spaeth Mrs. Meyer P. Potamkin Mrs. Richard Roob President Mrs. John N. Rosekrans, Jr. Richard J. Schwartz Alan E. Schwartz A. Alfred Taubman Vice-Presidents John Wilmerding Mrs. Keith S. Wellin R. Frederick Woolworth Mrs. Robert F. Shapiro Max N. Berry HONORARY TRUSTEES Dr. Irving R. Burton Treasurer Howard W. Lipman Mrs. Abbott K. Schlain Russell Lynes Mrs. William L. Richards Secretary to the Board Mrs. Dana M. Raymond FOUNDING TRUSTEES Lawrence A. Fleischman honorary Officers Edgar P. Richardson (deceased) Mrs. Francis de Marneffe Mrs. Edsel B. Ford (deceased) Miss Julienne M. Michel EX-OFFICIO TRUSTEES Members Robert McCormick Adams Tom L. Freudenheim Charles Blitzer Marc J. Pachter Eli Broad Gerald E. Buck ARCHIVES STAFF Ms. Gabriella de Ferrari Gilbert S. Edelson Richard J. Wattenmaker, Director Mrs. Ahmet M. Ertegun Susan Hamilton, Deputy Director Mrs. Arthur A. Feder James B. Byers, Assistant Director for Miles Q. Fiterman Archival Programs Mrs. Daniel Fraad Elizabeth S. Kirwin, Southeast Regional Mrs. Eugenio Garza Laguera Collector Hugh Halff, Jr. Arthur J. Breton, Curator of Manuscripts John K. Howat Judith E. Throm, Reference Archivist Dr. Helen Jessup Robert F. Brown, New England Regional Mrs. Dwight M. Kendall Center Gilbert H. Kinney Judith A. Gustafson, Midwest -
Paleogeography of the Caribbean Region: Implications for Cenozoic Biogeography
PALEOGEOGRAPHY OF THE CARIBBEAN REGION: IMPLICATIONS FOR CENOZOIC BIOGEOGRAPHY MANUEL A. ITURRALDE-VINENT Research Associate, Department of Mammalogy American Museum of Natural History Curator, Geology and Paleontology Group Museo Nacional de Historia Natural Obispo #61, Plaza de Armas, CH-10100, Cuba R.D.E. MA~PHEE Chairman and Curator, Department of Mammalogy American Museum of Natural History BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY Number 238, 95 pages, 22 figures, 2 appendices Issued April 28, 1999 Price: $10.60 a copy Copyright O American Museum of Natural History 1999 ISSN 0003-0090 CONTENTS Abstract ....................................................................... 3 Resumen ....................................................................... 4 Resumo ........................................................................ 5 Introduction .................................................................... 6 Acknowledgments ............................................................ 8 Abbreviations ................................................................ 9 Statement of Problem and Methods ............................................... 9 Paleogeography of the Caribbean Region: Evidence and Analysis .................. 18 Early Middle Jurassic to Late Eocene Paleogeography .......................... 18 Latest Eocene to Middle Miocene Paleogeography .............................. 27 Eocene-Oligocene Transition (35±33 Ma) .................................... 27 Late Oligocene (27±25 Ma) ............................................... -
Viscosity from Newton to Modern Non-Equilibrium Statistical Mechanics
Viscosity from Newton to Modern Non-equilibrium Statistical Mechanics S´ebastien Viscardy Belgian Institute for Space Aeronomy, 3, Avenue Circulaire, B-1180 Brussels, Belgium Abstract In the second half of the 19th century, the kinetic theory of gases has probably raised one of the most impassioned de- bates in the history of science. The so-called reversibility paradox around which intense polemics occurred reveals the apparent incompatibility between the microscopic and macroscopic levels. While classical mechanics describes the motionof bodies such as atoms and moleculesby means of time reversible equations, thermodynamics emphasizes the irreversible character of macroscopic phenomena such as viscosity. Aiming at reconciling both levels of description, Boltzmann proposed a probabilistic explanation. Nevertheless, such an interpretation has not totally convinced gen- erations of physicists, so that this question has constantly animated the scientific community since his seminal work. In this context, an important breakthrough in dynamical systems theory has shown that the hypothesis of microscopic chaos played a key role and provided a dynamical interpretation of the emergence of irreversibility. Using viscosity as a leading concept, we sketch the historical development of the concepts related to this fundamental issue up to recent advances. Following the analysis of the Liouville equation introducing the concept of Pollicott-Ruelle resonances, two successful approaches — the escape-rate formalism and the hydrodynamic-mode method — establish remarkable relationships between transport processes and chaotic properties of the underlying Hamiltonian dynamics. Keywords: statistical mechanics, viscosity, reversibility paradox, chaos, dynamical systems theory Contents 1 Introduction 2 2 Irreversibility 3 2.1 Mechanics. Energyconservationand reversibility . ........................ 3 2.2 Thermodynamics.