What Happens When Subduction Stops? AGU Celebrates the Members Who Participated in 2019 Congressional Visits
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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. -
U-Pb LA-ICP-MS GEOCHRONOLOGY
Boletín de Geología Vol. 32, N° 2, julio-diciembre de 2010 U-Pb LA-ICP-MS GEOCHRONOLOGY AND REGIONAL CORRELATION OF MIDDLE JURASSIC INTRUSIVE ROCKS FROM THE GARZON MASSIF, UPPER MAGDALENA VALLEY AND CENTRAL CORDILLERA, SOUTHERN COLOMBIA Camilo Bustamante1, Agustín Cardona1, Germán Bayona2, Andrés Mora3, Víctor Valencia4, George Gehrels5, Jeff Vervoort6 ABSTRACT New U-Pb zircon geochronology from four granitic units sampled along a southeast-northwest transect between the Garzón Massif and the Serranía de las Minas (Central Cordillera), records a Middle Jurassic magmatic activity with two different spatio-temporal domains at ca. 189 Ma and 180-173 Ma. Reconnaissance data suggest that the four granitoids are characterized by mineralogical and geochemical characteristics akin to a continental magmatic arc setting. The new results suggest that the southern Colombian continental margin includes remnants of tectono- magmatic elements formed by the subduction of the Farallon plate under the South American continental margin. This Middle Jurassic arc magmatism is part of the broader Andean scale arc province, and is significant for understanding the tectonic and paleogeographic scenario that characterized the Mesozoic tectonic evolution of the Northern Andes. Key words: U-Pb geochronology, Colombia, Jurassic, Intrusive rocks, Garzón Massif, Central Cordillera. GEOCRONOLOGÍA U-Pb LA-ICP-MS Y CORRELACIÓN REGIONAL DE LAS ROCAS INTRUSIVAS DEL JURÁSICO MEDIO DEL MACIZO DE GARZÓN, VALLE SUPERIOR DEL MAGDALENA Y LA CORDILLERA CENTRAL, SUR DE COLOMBIA RESUMEN Se presentan nuevas edades U-Pb en circones de cuatro unidades graníticas muestreadas a lo largo de una transecta SE-NW entre el Macizo de Garzón y la Serranía de las Minas (Cordillera Central), las cuales registran una actividad magmática en el Jurásico Medio en dos dominios espaciales y temporales diferentes: 189 Ma y 180 a 173 Ma. -
Geologists Suggest Horseshoe Abyssal Plain May Be Start of a Subduction Zone 8 May 2019, by Bob Yirka
Geologists suggest Horseshoe Abyssal Plain may be start of a subduction zone 8 May 2019, by Bob Yirka against one another. Over by the Iberian Peninsula, the opposite appears to be happening—the African and Eurasian plates are pulling apart as the former creeps east toward the Americas. Duarte noted that back in 2012, other researchers conducting seismic wave tests found what appeared to be a dense mass of unknown material beneath the epicenter of the 1969 quake. Some in the field suggested it could be the start of a subduction zone. Then, last year, another team conducted high-resolution imaging of the area and also found evidence of the mass, confirming that it truly existed. Other research has shown that the area just above the mass experiences routine tiny earthquakes. Duarte suggests the evidence to date indicates that the bottom of the plate is peeling away. This could happen, he explained, due to serpentinization in which water percolates through plate fractures and reacts with material beneath the surface, resulting A composite image of the Western hemisphere of the in the formation of soft green minerals. The soft Earth. Credit: NASA mineral layer, he suggests, is peeling away. And if that is the case, then it is likely the area is in the process of creating a subduction zone. He reports that he and his team members built models of their A team of geologists led by João Duarte gave a ideas and that they confirmed what he suspected. presentation at this past month's European The earthquakes were the result of the process of Geosciences Union meeting that included a birthing a new subduction zone. -
Working Group I Contribution to the Ipcc Fifth Assessment Report Climate Change 2013: the Physical Science Basis
WORKING GROUP I CONTRIBUTION TO THE IPCC FIFTH ASSESSMENT REPORT CLIMATE CHANGE 2013: THE PHYSICAL SCIENCE BASIS Final Draft Underlying Scientific-Technical Assessment A report accepted by Working Group I of the IPCC but not approved in detail. Note: The final draft Report, dated 7 June 2013, of the Working Group I contribution to the IPCC 5th Assessment Report "Climate Change 2013: The Physical Science Basis" was accepted but not approved in detail by the 12th Session of Working Group I and the 36th Session of the IPCC on 26 September 2013 in Stockholm, Sweden. It consists of the full scientific and technical assessment undertaken by Working Group I. The Report has to be read in conjunction with the document entitled “Climate Change 2013: The Physical Science Basis. Working Group I Contribution to the IPCC 5th Assessment Report - Changes to the underlying Scientific/Technical Assessment” to ensure consistency with the approved Summary for Policymakers (IPCC-XXVI/Doc.4) and presented to the Panel at its 36th Session. This document lists the changes necessary to ensure consistency between the full Report and the Summary for Policymakers, which was approved line-by-line by Working Group I and accepted by the Panel at the above- mentioned Sessions. Before publication the Report will undergo final copyediting as well as any error correction as necessary, consistent with the IPCC Protocol for Addressing Possible Errors. Publication of the Report is foreseen in January 2014. Disclaimer: The designations employed and the presentation of material on maps do not imply the expression of any opinion whatsoever on the part of the Intergovernmental Panel on Climate Change concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
Opening Session
1.0 OPENING 1.1 Opening Remarks and Administrative Arrangements Pempkowiak, Burkill, Urban 1.1.1 Memorials for Scientists Involved With SCOR. p. 1-1 1.2 Approval of the Agenda—Additions or modifications to the agenda may be suggested prior to approval of the final version, p. 1-5 Burkill 1.3 Report of the SCOR President—The President will briefly review activities since the SCOR General Meeting in September 2014, p. 1-5 Burkill 1.4 Report of SCOR Executive Director, p. 1-6 Urban 1.5 Appointment of an ad hoc Finance Committee, p. 1-8 Burkill 1.6 2016 SCOR Elections for SCOR Officers, p. 1-8 Fennel 1-1 1.0 OPENING 1.1 Opening Remarks and Administrative Arrangements Pempkowiak, Burkill, Urban 1.1.1 Memorials for Scientists Involved With SCOR Burkill John Knauss John Knauss was a participant in the first International Indian Ocean Expedition. From www.legacy.com: John A. Knauss, the noted oceanographer whose research and advocacy helped raised alarms about the delicate state of the world’s oceans, died Nov. 19, according to The Associated Press. He was 90. After obtaining his bachelor's degree in meteorology from the Massachusetts Institute of Technology in 1946, where he studied as part of the United States Navy’s V-12 program, Knauss earned a master's degree in physics from the University of Michigan and a doctorate in oceanography from the Scripps Institution of Oceanography. His work quickly become pivotal to the nascent national debate on the environment and water quality, and his pioneering work as a member of the influential Stratton Commission on the report "Our Nation and the Sea: A Plan for National Action" led to the creation of the National Oceanic and Atmospheric Administration (NOAA) and the formation of the Coastal Zone Management Act. -
Aeromagnetic Patterns in Southern Uruguay
Aeromagnetic patterns in Southern Uruguay: Precambrian-Mesozoic dyke swarms and Mesozoic rifting structural and tectonic evolution Pablo Demarco, Henri Masquelin, Claudia Prezzi, Tahar Aifa, Rossana Muzio, Judith Loureiro, Elena Peel, Nestor Campal, Leda Sánchez Bettucci To cite this version: Pablo Demarco, Henri Masquelin, Claudia Prezzi, Tahar Aifa, Rossana Muzio, et al.. Aeromagnetic patterns in Southern Uruguay: Precambrian-Mesozoic dyke swarms and Mesozoic rifting structural and tectonic evolution. Tectonophysics, Elsevier, 2020, 789, pp.228373. 10.1016/j.tecto.2020.228373. insu-02878330 HAL Id: insu-02878330 https://hal-insu.archives-ouvertes.fr/insu-02878330 Submitted on 23 Jun 2020 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. Aeromagnetic patterns in Southern Uruguay: Precambrian-Mesozoic dyke swarms and Mesozoic rifting structural and tectonic evolution Pablo Demarco, Henri Masquelin, Claudia Prezzi, Tahar Aifa, Rossana Muzio, Judith Loureiro, Elena Peel, Nestor Campal, Leda Sánchez Bettucci To cite this version: Pablo Demarco, Henri Masquelin, Claudia Prezzi, Tahar Aifa, Rossana Muzio, et al.. Aeromag- netic patterns in Southern Uruguay: Precambrian-Mesozoic dyke swarms and Mesozoic rifting struc- tural and tectonic evolution. Tectonophysics, Elsevier, In press, 10.1016/j.tecto.2020.228373. -
Cumulated Bibliography of Biographies of Ocean Scientists Deborah Day, Scripps Institution of Oceanography Archives Revised December 3, 2001
Cumulated Bibliography of Biographies of Ocean Scientists Deborah Day, Scripps Institution of Oceanography Archives Revised December 3, 2001. Preface This bibliography attempts to list all substantial autobiographies, biographies, festschrifts and obituaries of prominent oceanographers, marine biologists, fisheries scientists, and other scientists who worked in the marine environment published in journals and books after 1922, the publication date of Herdman’s Founders of Oceanography. The bibliography does not include newspaper obituaries, government documents, or citations to brief entries in general biographical sources. Items are listed alphabetically by author, and then chronologically by date of publication under a legend that includes the full name of the individual, his/her date of birth in European style(day, month in roman numeral, year), followed by his/her place of birth, then his date of death and place of death. Entries are in author-editor style following the Chicago Manual of Style (Chicago and London: University of Chicago Press, 14th ed., 1993). Citations are annotated to list the language if it is not obvious from the text. Annotations will also indicate if the citation includes a list of the scientist’s papers, if there is a relationship between the author of the citation and the scientist, or if the citation is written for a particular audience. This bibliography of biographies of scientists of the sea is based on Jacqueline Carpine-Lancre’s bibliography of biographies first published annually beginning with issue 4 of the History of Oceanography Newsletter (September 1992). It was supplemented by a bibliography maintained by Eric L. Mills and citations in the biographical files of the Archives of the Scripps Institution of Oceanography, UCSD. -
Martian Crater Morphology
ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter. -
Bierknes Memorial Lecture Richard J
Bierknes Memorial Lecture Richard J. Reed1 The Development and Status of Modern Weather Prediction2 Abstract or writings. Despite his many accomplishments and honors, Bjerknes was a modest man. I trust that he The progress made in weather prediction since national would approve of our decision to focus attention in this weather services began issuing forecasts is traced and assessed. Specific contributions of J. Bjerknes to this program are lecture on the subject to which he devoted much of his pointed out. Lessons learned from the historical record con- life's work rather than on his personal achievements cerning factors and conditions responsible for the important alone. advances are considered, and a limited evaluation is then During the period under consideration, weather fore- made of the increase in forecast skill that resulted from these advances. Finally, some comments are offered on the future casting was transformed from a practical art to a partly prospects of weather prediction. quantitative science. Thus it will be convenient in the discussion that follows to divide the period into three eras: a first extending from 1860 to 1920 in which fore- 1. Introduction cast practice was based almost entirely on human ex- We gather tonight to celebrate the memory of Jacob perience and skill, a second extending from 1920 to 1950 Bjerknes, one of the towering figures in the history of in which physical concepts received increasing emphasis, meteorology. In a long and distinguished career that and finally the modern era in which physical-numerical spanned a period of more than 50 years, Bjerknes made methods have been introduced and become firmly es- monumental contributions to our knowledge and under- tablished. -
A NEW EYE on COASTS Celebrating 2 Award-Winning Years of Eos Magazine and Eos.Org
VOL. 98 NO. 1 JAN 2017 Antarctic Trek for Space Weather Partnering Academia and the Military Earth & Space Science News Whisker-like New Mineral Discovered A NEW EYE ON COASTS Celebrating 2 Award-Winning Years of Eos Magazine and Eos.org Nearly 1 Million Online Readers An International Readership Spanning 196 Countries Multiple Awards from Association TRENDS and Association Media & Publishing VOL. 97 NO. 23 1 DEC 2016 VOL. 96 NO. 4 1 MAR 2015 VOL. 96 NO. 13 15 JUL 2015 Earth & Space Science News Earth & Space Science News HowHowHow Ready ReadyReady is Isis Los Los Angeles Angeles LEARNING Sonar Data forfor thethe NextNext “ GEOSCIENCE from the Water Column “Big OneOne”? Tracking Global ? BY DOING Landslide Hazards ”? Students Launch High-Altitude Balloons Monitoring Colombia’s GEOSCIENCE Slumbering Volcanoes Seismic Hazard Assessment Lab Simulates Science Fares Well in U.S. Solar Eruptions Gender Parity Proposed Federal Budget Magnetic Islands Caterpillar-Like Motion in Space of the Greenland Ice Sheet New for 2017: You’ll receive Eos magazine once a month, and now you’ll enjoy More Content: More features, news, and Research Spotlights More Depth: Special issues on important and emerging topics The satisfaction of a reduced carbon footprint And, as always, you can read articles free online as soon as they are published on Eos.org or by adding Eos.org to mobile apps like SmartNews and Flipboard. Earth & Space Science News Contents JANUARY 2017 PROJECT UPDATE VOLUME 98, ISSUE 1 14 Space Weather from a Southern Point of View A recently completed instrument array monitors geospace from the Antarctic end of Earth’s magnetic field lines. -
Kadiworking Paper Finalcorrected
ACADEMY OF EUROPEAN LAW EUI Working Papers AEL 2009/10 ACADEMY OF EUROPEAN LAW CHALLENGING THE EU COUNTER-TERRORISM MEASURES THROUGH THE COURTS edited by Marise Cremona, Francesco Francioni and Sara Poli EUROPEAN UNIVERSITY INSTITUTE , FLORENCE ACADEMY OF EUROPEAN LAW ROBERT SCHUMAN CENTRE FOR ADVANCED STUDIES Challenging the EU Counter-terrorism Measures through the Courts EDITED BY MARISE CREMONA , FRANCESCO FRANCIONI AND SARA POLI EUI W orking Paper AEL 2009/10 This text may be downloaded for personal research purposes only. Any additional reproduction for other purposes, whether in hard copy or electronically, requires the consent of the author(s), editor(s). If cited or quoted, reference should be made to the full name of the author(s), editor(s), the title, the working paper or other series, the year, and the publisher. The author(s)/editor(s) should inform the Academy of European Law if the paper is to be published elsewhere, and should also assume responsibility for any consequent obligation(s). ISSN 1831-4066 © 2009 Marise Cremona, Francesco Francioni and Sara Poli (editors) Printed in Italy European University Institute Badia Fiesolana I – 50014 San Domenico di Fiesole (FI) Italy www.eui.eu cadmus.eui.eu Abstract This collection of papers examines the implications of the European Court of Justice’s approach to UN-related counter-terrorism measures against individuals (so-called ‘smart sanctions’), as expressed by its ruling in Case C-402/05P Kadi v Council and Commission , in which it annulled an EC act implementing a UN Security Council resolution. The impact of this seminal judgment on the EC legal order, on its relationship with the UN Charter, and on the case-law of the European Court of Human rights is the theme of this collection. -
DMAAC – February 1973
LUNAR TOPOGRAPHIC ORTHOPHOTOMAP (LTO) AND LUNAR ORTHOPHOTMAP (LO) SERIES (Published by DMATC) Lunar Topographic Orthophotmaps and Lunar Orthophotomaps Scale: 1:250,000 Projection: Transverse Mercator Sheet Size: 25.5”x 26.5” The Lunar Topographic Orthophotmaps and Lunar Orthophotomaps Series are the first comprehensive and continuous mapping to be accomplished from Apollo Mission 15-17 mapping photographs. This series is also the first major effort to apply recent advances in orthophotography to lunar mapping. Presently developed maps of this series were designed to support initial lunar scientific investigations primarily employing results of Apollo Mission 15-17 data. Individual maps of this series cover 4 degrees of lunar latitude and 5 degrees of lunar longitude consisting of 1/16 of the area of a 1:1,000,000 scale Lunar Astronautical Chart (LAC) (Section 4.2.1). Their apha-numeric identification (example – LTO38B1) consists of the designator LTO for topographic orthophoto editions or LO for orthophoto editions followed by the LAC number in which they fall, followed by an A, B, C or D designator defining the pertinent LAC quadrant and a 1, 2, 3, or 4 designator defining the specific sub-quadrant actually covered. The following designation (250) identifies the sheets as being at 1:250,000 scale. The LTO editions display 100-meter contours, 50-meter supplemental contours and spot elevations in a red overprint to the base, which is lithographed in black and white. LO editions are identical except that all relief information is omitted and selenographic graticule is restricted to border ticks, presenting an umencumbered view of lunar features imaged by the photographic base.