“Comment About Tsunamis Occurrence in Northern Caribbean”
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Seismic Philately
Seismic Philately adapted from the 2008 CUREE Calendar introduction by David J. Leeds © 2007 - All Rights Reserved. Stamps shown on front cover (left to right): • Label created by Chicago businessmen to help raise relief for the 1906 San Francisco Earthquake • Stamp commemorating the 1944 San Juan, Argentina Earthquake • Stamp commemorating the 1954 Orleansville, Algeria Earthquake • Stamp commemorating the 1953 Zante, Greece Earthquake • Stamp from 75th Anniversary stamp set commemorating the 1931 Hawkes Bay, New Zealand Earthquake • Stamp depicting a lake formed by a landslide triggered by the 1923 Kanto, Japan Earthquake Consortium of Universities for Research in Earthquake Engineering 1301 South 46th Street, Richmond, CA 94804-4600 tel: 510-665-3529 fax: 510-665-3622 CUREE http://www.curee.org Seismic Philately by David J. Leeds Introduction Philately is simply the collection and the study of postage stamps. Some of the Secretary of the Treasury, and as a last resort, bisected stamps could stamp collectors (philatelists) collect only from their native country, others be used for half their face value. (see March) collect from the stamp-issuing countries around the world. Other philately collections are defined by topic, such as waterfalls, bridges, men with beards, FDC, first day cover, or Covers, are sometimes created to commerate the nudes, maps, flowers, presidents, Americans on foreign stamps, etc. Many first day a new stamp is issued. As part of the presentation, an envelope of the world’s stamps that are related to the topic of earthquakes have been with the new postage stamp is cancelled on the first day of issue. Additional compiled in this publication. -
Ocean Trench
R E S O U R C E L I B R A R Y E N C Y C L O P E D I C E N T RY Ocean trench Ocean trenches are long, narrow depressions on the seafloor. These chasms are the deepest parts of the ocean—and some of the deepest natural spots on Earth. G R A D E S 5 - 12+ S U B J E C T S Earth Science, Geology, Geography, Physical Geography C O N T E N T S 11 Images, 1 Video, 2 Links For the complete encyclopedic entry with media resources, visit: http://www.nationalgeographic.org/encyclopedia/ocean-trench/ Ocean trenches are long, narrow depressions on the seafloor. These chasms are the deepest parts of the ocean—and some of the deepest natural spots on Earth. Ocean trenches are found in every ocean basin on the planet, although the deepest ocean trenches ring the Pacific as part of the so-called “Ring of Fire” that also includes active volcanoes and earthquake zones. Ocean trenches are a result of tectonic activity, which describes the movement of the Earth’s lithosphere. In particular, ocean trenches are a feature of convergent plate boundaries, where two or more tectonic plates meet. At many convergent plate boundaries, dense lithosphere melts or slides beneath less-dense lithosphere in a process called subduction, creating a trench. Ocean trenches occupy the deepest layer of the ocean, the hadalpelagic zone. The intense pressure, lack of sunlight, and frigid temperatures of the hadalpelagic zone make ocean trenches some of the most unique habitats on Earth. -
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information Index Abancay Deflection, 201, 204–206, 223 Allmendinger, R. W., 206 Abant, Turkey, earthquake of 1957 Ms 7.0, 286 allochthonous terranes, 26 Abdrakhmatov, K. Y., 381, 383 Alpine fault, New Zealand, 482, 486, 489–490, 493 Abercrombie, R. E., 461, 464 Alps, 245, 249 Abers, G. A., 475–477 Alquist-Priolo Act, California, 75 Abidin, H. Z., 464 Altay Range, 384–387 Abiz, Iran, fault, 318 Alteriis, G., 251 Acambay graben, Mexico, 182 Altiplano Plateau, 190, 191, 200, 204, 205, 222 Acambay, Mexico, earthquake of 1912 Ms 6.7, 181 Altunel, E., 305, 322 Accra, Ghana, earthquake of 1939 M 6.4, 235 Altyn Tagh fault, 336, 355, 358, 360, 362, 364–366, accreted terrane, 3 378 Acocella, V., 234 Alvarado, P., 210, 214 active fault front, 408 Álvarez-Marrón, J. M., 219 Adamek, S., 170 Amaziahu, Dead Sea, fault, 297 Adams, J., 52, 66, 71–73, 87, 494 Ambraseys, N. N., 226, 229–231, 234, 259, 264, 275, Adria, 249, 250 277, 286, 288–290, 292, 296, 300, 301, 311, 321, Afar Triangle and triple junction, 226, 227, 231–233, 328, 334, 339, 341, 352, 353 237 Ammon, C. J., 464 Afghan (Helmand) block, 318 Amuri, New Zealand, earthquake of 1888 Mw 7–7.3, 486 Agadir, Morocco, earthquake of 1960 Ms 5.9, 243 Amurian Plate, 389, 399 Age of Enlightenment, 239 Anatolia Plate, 263, 268, 292, 293 Agua Blanca fault, Baja California, 107 Ancash, Peru, earthquake of 1946 M 6.3 to 6.9, 201 Aguilera, J., vii, 79, 138, 189 Ancón fault, Venezuela, 166 Airy, G. -
Kinematic Reconstruction of the Caribbean Region Since the Early Jurassic
Earth-Science Reviews 138 (2014) 102–136 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Kinematic reconstruction of the Caribbean region since the Early Jurassic Lydian M. Boschman a,⁎, Douwe J.J. van Hinsbergen a, Trond H. Torsvik b,c,d, Wim Spakman a,b, James L. Pindell e,f a Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands b Center for Earth Evolution and Dynamics (CEED), University of Oslo, Sem Sælands vei 24, NO-0316 Oslo, Norway c Center for Geodynamics, Geological Survey of Norway (NGU), Leiv Eirikssons vei 39, 7491 Trondheim, Norway d School of Geosciences, University of the Witwatersrand, WITS 2050 Johannesburg, South Africa e Tectonic Analysis Ltd., Chestnut House, Duncton, West Sussex, GU28 OLH, England, UK f School of Earth and Ocean Sciences, Cardiff University, Park Place, Cardiff CF10 3YE, UK article info abstract Article history: The Caribbean oceanic crust was formed west of the North and South American continents, probably from Late Received 4 December 2013 Jurassic through Early Cretaceous time. Its subsequent evolution has resulted from a complex tectonic history Accepted 9 August 2014 governed by the interplay of the North American, South American and (Paleo-)Pacific plates. During its entire Available online 23 August 2014 tectonic evolution, the Caribbean plate was largely surrounded by subduction and transform boundaries, and the oceanic crust has been overlain by the Caribbean Large Igneous Province (CLIP) since ~90 Ma. The consequent Keywords: absence of passive margins and measurable marine magnetic anomalies hampers a quantitative integration into GPlates Apparent Polar Wander Path the global circuit of plate motions. -
Time and Space Distribution of Coseismic Slip of the 2011 Tohoku Earthquake As Inferred from Tsunami Waveform Data Kenji Satake
1 Time and Space Distribution of Coseismic Slip of the 2011 Tohoku Earthquake as 2 Inferred from Tsunami Waveform Data 3 4 Kenji Satake1, Yushiro Fujii2, Tomoya Harada1 and Yuichi Namegaya3 5 6 Electronic Supplement 7 Estimated slip for each subfault at 0.5 min interval 8 http://iisee.kenken.go.jp/staff/fujii/BSSA_Tohoku/BSSA-D-12-00122R1-esupp.html 9 10 11 Corresponding author: Kenji Satake 12 Earthquake Research Institute, University of Tokyo 13 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-0032 Japan 14 [email protected] 15 Revised on July 21, 2012 16 Final version September 26, 2012 17 18 1 19 Abstract A multiple time-window inversion of 53 high-sampling tsunami 20 waveforms on ocean bottom pressure, GPS, coastal wave, and tide gauges shows a 21 temporal and spatial slip distribution during the 2011 Tohoku earthquake. The 22 fault rupture started near the hypocenter and propagated into both deep and 23 shallow parts of the plate interface. Very large, approximately 25 m, slip off Miyagi 24 on the deep part, at a location similar to the previous 869 Jogan earthquake model, 25 was responsible for the initial rise of tsunami waveforms and the recorded tsunami 26 inundation in Sendai and Ishinomaki plains. Huge slip, up to 69 m, occurred on the 27 shallow part near the trench axis 3 min after the rupture initiation. This delayed 28 shallow rupture extended for 400 km with more than 10 m slip, at a location similar 29 to the 1896 Sanriku tsunami earthquake, and was responsible for the peak 30 amplitudes of the tsunami waveforms and the maximum tsunami heights measured 31 on the northern Sanriku coast, 100 km north of the largest slip. -
I I 71-15,061 CAMERON, Christopher Paul, 1940- PALEOMAGNETISM of SHEMYA and ADAK ISLANDS, ALEUTIAN ISLANDS, ALASKA. University O
Paleomagnetism Of Shemya And Adak Islands, Aleutian Islands, Alaska Item Type Thesis Authors Cameron, Christopher Paul Download date 23/09/2021 14:56:00 Link to Item http://hdl.handle.net/11122/9194 I I 71-15,061 CAMERON, Christopher Paul, 1940- PALEOMAGNETISM OF SHEMYA AND ADAK ISLANDS, ALEUTIAN ISLANDS, ALASKA. University of Alaska, Ph.D., 1970 Geology University Microfilms, A XEROX Company, Ann Arbor, Michigan tutc nTCCTDTATTOM MAC HTTM MTPROFIT.MFD F.VAPTT.Y AS RF.OF.TVF.D Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. PALE01IAGNETISM OF SHEMYA AMD ADAK ISLAUDS, ALEUTIAN ISLANDS, ALASKA A DISSERTATION Presented to the Faculty of the University of Alaska in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY by Christopher P/" Cameron B. S. College, Alaska May, 1970 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. PALEOilAGNETISM OF SHEMYA AND ADAK ISLANDS, ALEUTIAN ISLANDS, ALASKA APPROVED: f t l ‘y l .V" ■i. n ■ ■< < ; N w 1 T *W -C ltc-JL It / _ _ ____ /vx... , ~ ~ 7 YdSV Chairman APPPvOVED: dai£ 3 / 3 0 / 7 0 Dean of the College of Earth Sciences and Mineral Industry Vice President for Research and Advanced Study Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ABSTRACT Paleomagnetic results are presented for Tertiary and Quaternary volcanic rocks from Shemya and Adak Islands, Aleutian Islands, Alaska. The specimens were collected and measured using standard paleomagnetic methods. Alternating field demagnetization techniques were applied to test the stability of the remanence and to remove unwanted secondary components of magnetization. -
Virginia B. Sisson
Virginia B. Sisson Education: Ph.D., Princeton University, 1985, Dissertation: Contact Metamorphism and Fluid Evolution Associated with the Ponder pluton, Coast Plutonic Complex, British Columbia, Canada M.A., Princeton University, 1981 A.B., Bryn Mawr College cum laude with honors in geology, 1979 Research Interests and Skills: Field oriented petrotectonic studies in Alaska and Guatemala on convergent margins, triple junction interactions, granite emplacement, subduction zone metamorphism and exhumation processes, and jadeitite formation. Have also done field work in Venezuela, British Columbia, India, Malaysia, Norway, California, Washington, Montana, Nevada, Maine, Pennsylvania, and Myanmar Fluid inclusion studies and boron geochemistry of metamorphic rocks Languages Spanish and French at a basic level. Employment: 2008 - present Research Associate Professor, Director Geology Field Course, Co-Director Learning Center, Department of Earth and Atmospheric Sciences, University of Houston 2001 - present Research Associate, American Natural History Museum 2003 - present Research Associate, Department of Geology, University of Utah 2001 - 2004 Research Scientist, Department of Earth Science, Rice University 2001 - 2003 Research Associate Professor, Department of Geology, University of Utah 1999 - 2001 Clinical Assistant Professor, Department of Geology and Geophysics, Rice University 1999 - 2001 Advisor for Encyclopedia Britannica on Rocks and Minerals 1992 - 1999 Assistant Professor, Department of Geology and Geophysics, Rice University -
The Caribbean-North America-Cocos Triple Junction and the Dynamics of the Polochic-Motagua Fault Systems
The Caribbean-North America-Cocos Triple Junction and the dynamics of the Polochic-Motagua fault systems: Pull-up and zipper models Christine Authemayou, Gilles Brocard, C. Teyssier, T. Simon-Labric, A. Guttierrez, E. N. Chiquin, S. Moran To cite this version: Christine Authemayou, Gilles Brocard, C. Teyssier, T. Simon-Labric, A. Guttierrez, et al.. The Caribbean-North America-Cocos Triple Junction and the dynamics of the Polochic-Motagua fault systems: Pull-up and zipper models. Tectonics, American Geophysical Union (AGU), 2011, 30, pp.TC3010. 10.1029/2010TC002814. insu-00609533 HAL Id: insu-00609533 https://hal-insu.archives-ouvertes.fr/insu-00609533 Submitted on 19 Jan 2012 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. TECTONICS, VOL. 30, TC3010, doi:10.1029/2010TC002814, 2011 The Caribbean–North America–Cocos Triple Junction and the dynamics of the Polochic–Motagua fault systems: Pull‐up and zipper models C. Authemayou,1,2 G. Brocard,1,3 C. Teyssier,1,4 T. Simon‐Labric,1,5 A. Guttiérrez,6 E. N. Chiquín,6 and S. Morán6 Received 13 October 2010; revised 4 March 2011; accepted 28 March 2011; published 25 June 2011. -
Present Day Plate Boundary Deformation in the Caribbean and Crustal Deformation on Southern Haiti Steeve Symithe Purdue University
Purdue University Purdue e-Pubs Open Access Dissertations Theses and Dissertations 4-2016 Present day plate boundary deformation in the Caribbean and crustal deformation on southern Haiti Steeve Symithe Purdue University Follow this and additional works at: https://docs.lib.purdue.edu/open_access_dissertations Part of the Caribbean Languages and Societies Commons, Geology Commons, and the Geophysics and Seismology Commons Recommended Citation Symithe, Steeve, "Present day plate boundary deformation in the Caribbean and crustal deformation on southern Haiti" (2016). Open Access Dissertations. 715. https://docs.lib.purdue.edu/open_access_dissertations/715 This document has been made available through Purdue e-Pubs, a service of the Purdue University Libraries. Please contact [email protected] for additional information. Graduate School Form 30 Updated ¡ ¢¡£ ¢¡¤ ¥ PURDUE UNIVERSITY GRADUATE SCHOOL Thesis/Dissertation Acceptance This is to certify that the thesis/dissertation prepared By Steeve Symithe Entitled Present Day Plate Boundary Deformation in The Caribbean and Crustal Deformation On Southern Haiti. For the degree of Doctor of Philosophy Is approved by the final examining committee: Christopher L. Andronicos Chair Andrew M. Freed Julie L. Elliott Ayhan Irfanoglu To the best of my knowledge and as understood by the student in the Thesis/Dissertation Agreement, Publication Delay, and Certification Disclaimer (Graduate School Form 32), this thesis/dissertation adheres to the provisions of Purdue University’s “Policy of Integrity in Research” and the use of copyright material. Andrew M. Freed Approved by Major Professor(s): Indrajeet Chaubey 04/21/2016 Approved by: Head of the Departmental Graduate Program Date PRESENT DAY PLATE BOUNDARY DEFORMATION IN THE CARIBBEAN AND CRUSTAL DEFORMATION ON SOUTHERN HAITI A Dissertation Submitted to the Faculty of Purdue University by Steeve J. -
ABSTRACT a Preliminary Natural Hazards Vulnerability Assessment
1 ABSTRACT A Preliminary Natural Hazards Vulnerability Assessment of the Norman Manley International Airport and its Access Route Kevin Patrick Douglas M.Sc. in Disaster Management The University of the West Indies 2011 The issue of disaster risk reduction through proper assessment of vulnerability has emerged as a pillar of disaster management, a paradigm shift from simply responding to disasters after they have occurred. The assessment of vulnerability is important for countries desiring to maintain sustainable economies, as disasters have the potential to disrupt their economic growth and the lives of thousands of people. This study is a preliminary assessment of the hazard vulnerabilities the Norman Manley International Airport (NMIA) in Kingston Jamaica and its Access Route, as these play an important developmental role in the Jamaican society. The Research involves an analysis of the hazard history of the area along with the location and structural vulnerabilities of critical facilities. Finally, the mitigation measures in place for the identified hazards are assessed and recommendations made to increase the resilience of the facility. The findings of the research show that the NMIA and its access route are mostly vulnerable to earthquakes, hurricanes with flooding from storm surges, wind damage and sea level rise based 2 on their location and structure. The major mitigation measures involved the raising of the Access Route from Harbour View Roundabout to the NMIA and implementation of structural protective barriers as well as various engineering design specifications of the NMIA facility. Also, the implementation of structural mitigation measures may be of limited success, if hazard strikes exceed the magnitude which they are designed to withstand. -
THE CONTINENTAL DRIFT CONTROVERSY Volume IV: Evolution Into Plate Tectonics
Comp. by: Kkavitha Stage: Proof Chapter No.: FrontMatter Title Name: FRANKEL_Vol-4 Page Number: 0 Date:20/1/12 Time:17:17:28 THE CONTINENTAL DRIFT CONTROVERSY Volume IV: Evolution into Plate Tectonics Resolution of the sixty-year debate over continental drift, culminating in the triumph of plate tectonics, changed the very fabric of Earth Science. Plate tectonics can be considered alongside the theories of evolution in the life sciences and of quantum mechanics in physics in terms of its fundamental importance to our scientific under- standing of the world. This four-volume treatise on The Continental Drift Controversy is the first complete history of the origin, debate and gradual acceptance of this revolutionary explanation of the structure and motion of the Earth’s outer surface. Based on extensive interviews, archival papers, and original works, Frankel weaves together the lives and work of the scientists involved, producing an accessible narrative for scientists and non-scientists alike. Explanations of the curious magnetic anomalies on the seafloor and discovery and explanation of transform faults in the ocean crust in the mid-sixties led to the rapid acceptance of seafloor spreading. The birth of plate tectonics followed soon after with the geometrification of geology. Finally it was understood that the Earth’s surface is divided into a small number of nearly rigid plates, most of which contain continental and oceanic parts, and whose relative motions are describable in terms of Euler’s fixed point theorem. Although plate tectonics did not explain the cause or dynamic mechanism of drifting continents, it provided a convincing kinematic explanation that continues to inspire geodynamic research to the present day. -
Jamaica Country Document on Disaster Risk Reduction, 2014
Jamaica Country Document on Disaster Risk Reduction, 2014 Prepared by: Disaster Risk Reduction Centre (DRRC) University of the West Indies December 5, 2014 Jamaica Country Document on Disaster Risk Reduction, 2014 December 2014 Office of Disaster Preparedness and Emergency Management (ODPEM) National coordination: Office of Disaster Preparedness and Emergency Management (ODPEM) Mr. Richard Thompson, Director General (acting) Ms. Michelle Edwards, Senior Director Preparedness and Emergency Operations Ms. Anna Tucker, Disaster Risk Management Specialist Regional coordination: United Nations Office for Disaster Risk Reduction Alexc ia Cooke & Sandra Amlang Authors: Disaster Risk Reduction Centre (DRRC) University of West of Indies Dr. Barbara Carby Mr. Dorlan Burrell Mrs. Cleonie Samuels-Williams Proof Readers Dr. Barbara Carby Mr. Craig Williams Cover page design : Maria Camila García Ruiz This document covers humanitarian aid activities implemented with the financial assistance of the European Union. The views expressed herein should not be taken, in any way, to reflect the official opinion of the European Union, and the Europe an Commission is not responsible for any use that may be made of the information it contains. ECHO U&ISDR European Commission's Humanitarian Aid and United Nations Office for Disaster Risk Civil Protection department Reduction Regional office for the Caribbean Regional office for the Americas Santo Domingo, República Dominicana Ciudad del Saber (Clayton) , Panamá Email: [email protected] Email: [email protected] URL: http://ec.europa.eu/echo/ URL: http://www.eird.org/ http://www.dipecholac.net/ http://www.unisdr.org/americas ii Table of Contents Pages i. List of Figures vi-vii ii. List of Tables vii-viii iii.