1 OCEANOGRAPHY the PACIFIC OCEAN by PROF. A. BALSUBRAMANIAN OUTLINE 1.0 Introduction 1.1 Geographic Setting 1.2 Dimension
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Turning the Tide on Trash: Great Lakes
Turning the Tide On Trash A LEARNING GUIDE ON MARINE DEBRIS Turning the Tide On Trash A LEARNING GUIDE ON MARINE DEBRIS Floating marine debris in Hawaii NOAA PIFSC CRED Educators, parents, students, and Unfortunately, the ocean is currently researchers can use Turning the Tide under considerable pressure. The on Trash as they explore the serious seeming vastness of the ocean has impacts that marine debris can have on prompted people to overestimate its wildlife, the environment, our well being, ability to safely absorb our wastes. For and our economy. too long, we have used these waters as a receptacle for our trash and other Covering nearly three-quarters of the wastes. Integrating the following lessons Earth, the ocean is an extraordinary and background chapters into your resource. The ocean supports fishing curriculum can help to teach students industries and coastal economies, that they can be an important part of the provides recreational opportunities, solution. Many of the lessons can also and serves as a nurturing home for a be modified for science fair projects and multitude of marine plants and wildlife. other learning extensions. C ON T EN T S 1 Acknowledgments & History of Turning the Tide on Trash 2 For Educators and Parents: How to Use This Learning Guide UNIT ONE 5 The Definition, Characteristics, and Sources of Marine Debris 17 Lesson One: Coming to Terms with Marine Debris 20 Lesson Two: Trash Traits 23 Lesson Three: A Degrading Experience 30 Lesson Four: Marine Debris – Data Mining 34 Lesson Five: Waste Inventory 38 Lesson -
Continental Shelf the Last Maritime Zone
Continental Shelf The Last Maritime Zone The Last Maritime Zone Published by UNEP/GRID-Arendal Copyright © 2009, UNEP/GRID-Arendal ISBN: 978-82-7701-059-5 Printed by Birkeland Trykkeri AS, Norway Disclaimer Any views expressed in this book are those of the authors and do not necessarily reflect the views or policies of UNEP/GRID-Arendal or contributory organizations. The designations employed and the presentation of material in this book do not imply the expression of any opinion on the part of the organizations concerning the legal status of any country, territory, city or area of its authority, or deline- ation of its frontiers and boundaries, nor do they imply the validity of submissions. All information in this publication is derived from official material that is posted on the website of the UN Division of Ocean Affairs and the Law of the Sea (DOALOS), which acts as the Secretariat to the Com- mission on the Limits of the Continental Shelf (CLCS): www.un.org/ Depts/los/clcs_new/clcs_home.htm. UNEP/GRID-Arendal is an official UNEP centre located in Southern Norway. GRID-Arendal’s mission is to provide environmental informa- tion, communications and capacity building services for information management and assessment. The centre’s core focus is to facili- tate the free access and exchange of information to support decision making to secure a sustainable future. www.grida.no. Continental Shelf The Last Maritime Zone Continental Shelf The Last Maritime Zone Authors and contributors Tina Schoolmeester and Elaine Baker (Editors) Joan Fabres Øystein Halvorsen Øivind Lønne Jean-Nicolas Poussart Riccardo Pravettoni (Cartography) Morten Sørensen Kristina Thygesen Cover illustration Alex Mathers Language editor Harry Forster (Interrelate Grenoble) Special thanks to Yannick Beaudoin Janet Fernandez Skaalvik Lars Kullerud Harald Sund (Geocap AS) Continental Shelf The Last Maritime Zone Foreword During the past decade, many coastal States have been engaged in peacefully establish- ing the limits of their maritime jurisdiction. -
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. -
25. PELAGIC Sedimentsi
^ 25. PELAGIC SEDIMENTSi G. Arrhenius 1. Concept of Pelagic Sedimentation The term pelagic sediment is often rather loosely defined. It is generally applied to marine sediments in which the fraction derived from the continents indicates deposition from a dilute mineral suspension distributed throughout deep-ocean water. It appears logical to base a precise definition of pelagic sediments on some limiting property of this suspension, such as concentration or rate of removal. Further, the property chosen should, if possible, be reflected in the ensuing deposit, so that the criterion in question can be applied to ancient sediments. Extensive measurements of the concentration of particulate matter in sea- water have been carried out by Jerlov (1953); however, these measurements reflect the sum of both the terrigenous mineral sol and particles of organic (biotic) origin. Aluminosilicates form a major part of the inorganic mineral suspension; aluminum is useful as an indicator of these, since this element forms 7 to 9% of the total inorganic component, 2 and can be quantitatively determined at concentration levels down to 3 x lO^i^ (Sackett and Arrhenius, 1962). Measurements of the amount of particulate aluminum in North Pacific deep water indicate an average concentration of 23 [xg/1. of mineral suspensoid, or 10 mg in a vertical sea-water column with a 1 cm^ cross-section at oceanic depth. The mass of mineral particles larger than 0.5 [x constitutes 60%, or less, of the total. From the concentration of the suspensoid and the rate of fallout of terrigenous minerals on the ocean floor, an average passage time (Barth, 1952) of less than 100 years is obtained for the fraction of particles larger than 0.5 [i. -
Appendix 2. the Mystery of Guyot Formation and Sinking
Appendix 2 The Mystery of Guyot Formation and Sinking Origin of Guyots Unknown In 1946, geologist Harry Hess was the first geologist to describe guyots (flat-topped seamount).1 Since then, the number of guyots has become numerous. Resolution Guyot in the Mid-Pacific Mountains that was studied in the 1990s by the Deep Sea Drilling Project2 is a typical guyot. Figure A2.1 shows the silhouette. Ever since Hess’s time, the cause of the flat top has eluded explanation.3 Winterer and Met- Figure A2.1. Silhouette of Resolution Guyot zler maintain: “Since Hess first recognized them in the Mid-Pacific Mountains (drawn by Mrs. Melanie Richard). in 1946, the origin of flat-topped seamounts, or guyots, has remained one of the most persistent problems in marine geology.”4 Since guyots are believed to have been truncated near sea level, there are two suggested subsid- ence mechanisms used to explain why they are now found well below sea level. But some guyots must have become flat well below sea level. Not All Guyots Eroded At Sea Level Many scientists have simply assumed that the flat top of a guyot was eroded at or near sea level.5,6 ‘This has been challenged by a few marine geologists.’7,8 For instance, a number of guyots near the East Pacific Rise have been attributed to the infilling of calderas by small lava flows well below sea level.9,10,11,12 “But, these guyots are small 1 Hess, H.H., 1946. Drowned ancient islands of the Pacific Basin. American Journal of Science 244:772–791. -
Seafloor Mapping of the Continental Slope of the U.S. Atlantic Margin to Study Submarine Landslides That Could Trigger Tsunamis
Seafloor Mapping of the Continental Slope of the U.S. Atlantic Margin to Study Submarine Landslides that Could Trigger Tsunamis An additional Report to the Nuclear Regulatory Commission Job Code Number: N6480 By Atlantic and Gulf of Mexico Tsunami Hazard Assessment Group Seafloor Mapping of the Continental Slope of the U.S. Atlantic Margin to Study Submarine Landslides that Could Trigger Tsunamis An Additional Report to the Nuclear Regulatory Commission By Atlantic and Gulf of Mexico Tsunami Hazard Assessment Group: Uri ten Brink, David Twichell, Jason Chaytor, Bill Danforth, Brian Andrews, and Elizabeth Pendleton U.S. Geological Survey, Woods Hole Coastal and Marine Science Center, Woods Hole, Massachusetts, USA This reports provides additional information to the report Evaluation of Tsunami Sources with Potential to Impact the U.S. Atlantic and Gulf Coasts, submitted to the Nuclear Regulatory Commission on August 22, 2008. October 15, 2010 NOTICE FROM USGS This publication was prepared by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, make any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report, or represent that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. Any views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. -
NPP) A) Global Patterns B) Fate of NPP
OCN 401 Biogeochemical Systems (11.1.11) (Schlesinger: Chapter 9) Oceanic Production, Carbon Regeneration, Sediment Carbon Burial Lecture Outline 1. Net Primary Production (NPP) a) Global Patterns b) Fate of NPP 2. Sediment Diagenesis a) Diagenesis of Organic Matter (OM) b) Biogenic Carbonates Net Primary Production: Global Patterns • Oceanic photosynthesis is ≈ 50% of total photosynthesis on Earth - mostly as phytoplankton (microscopic plants) in surface mixed layer - seaweed accounts for only ≈ 0.1%. • NPP ranges from 130 - 420 gC/m2/yr, lowest in open ocean, highest in coastal zones • Terrestrial forests range from 400-800 gC/m2/yr, while deserts average 80 gC/m2/yr. Net Primary Production: Global Patterns (cont’d.) • O2 distribution is an indirect measure of photosynthesis: CO2 + H2O = CH2O + O2 14 • NPP is usually measured using O2-bottle or C-uptake techniques. 14 • O2 bottle measurements tend to exceed C-uptake rates in the same waters. Net Primary Production: Global Patterns (cont’d.) • Controversy over magnitude of global NPP arises from discrepancies in methods for measuring NPP: estimates range from 27 to 51 x 1015 gC/yr. 14 • O2 bottle measurements tend to exceed C-uptake rates because: - large biomass of picoplankton, only recently observed, which pass through the filters used in the 14C technique. - picoplankton may account for up to 50% of oceanic production. - DOC produced by phytoplankton, a component of NPP, passes through filters. - Problems with contamination of 14C-incubated samples with toxic trace elements depress NPP. Net Primary Production: Global Patterns (cont’d.) Despite disagreement on absolute magnitude of global NPP, there is consensus on the global distribution of NPP. -
Subduction Initiation May Depend on a Tectonic Plate's History 22 June 2021, by David Shultz
Subduction initiation may depend on a tectonic plate's history 22 June 2021, by David Shultz geological history makes it an ideal location to study how subduction starts. The team's seismic structural analysis showed that subduction zone initiation begins along existing weaknesses in Earth's crust and relies on differences in lithospheric density. The conditions necessary for the subduction zone's formation began about 45 million years ago, when the Australian and Pacific plates started to pull apart from each other. During that period, extensional forces led to seafloor spreading and the creation of new high-density oceanic lithosphere in the south. However, in the north, the thick and buoyant continental crust of Zealandia was merely stretched and slightly thinned. Over the next several million years, the plates rotated, and strike- The Puysegur Trench follows the natural curvature of slip deformation moved the high-density oceanic New Zealand’s South Island, extending southwest from lithosphere from the south to the north, where it the island’s southern tip. Credit: NASA slammed into low-density continental lithosphere, allowing subduction to begin. Subduction zones are cornerstone components of The researchers contend that the differences in plate tectonics, with one plate sliding beneath lithospheric density combined with existing another back into Earth's mantle. But the very weaknesses along the strike-slip boundary from the beginning of this process—subduction previous tectonic phases facilitated subduction initiation—remains somewhat mysterious to initiation. The team concludes that strike-slip might scientists because most of the geological record of be a key driver of subduction zone initiation subduction is buried and overwritten by the because of its ability to efficiently bring together extreme forces at play. -
Marine Snow Storms: Assessing the Environmental Risks of Ocean Fertilization
University of Wollongong Research Online Faculty of Law - Papers (Archive) Faculty of Business and Law 1-1-2009 Marine snow storms: Assessing the environmental risks of ocean fertilization Robin M. Warner University of Wollongong, [email protected] Follow this and additional works at: https://ro.uow.edu.au/lawpapers Part of the Law Commons Recommended Citation Warner, Robin M.: Marine snow storms: Assessing the environmental risks of ocean fertilization 2009, 426-436. https://ro.uow.edu.au/lawpapers/192 Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Marine snow storms: Assessing the environmental risks of ocean fertilization Abstract The threats posed by climate change to the global environment have fostered heightened scientific interest in marine geo-engineering schemes designed to boost the capacity of the oceans to absorb atmospheric carbon dioxide. This is the primary goal of a process known as ocean fertilization which seeks to increase the production of organic material in the surface ocean in order to promote further draw down of photosynthesized carbon to the deep ocean. This article describes the process of ocean fertilization, its objectives and potential impacts on the marine environment and some examples of ocean fertilization experiments. It analyses the applicability of international law principles on marine environmental protection to this process and the regulatory gaps and ambiguities in the existing international law framework for such activities. Finally it examines the emerging regulatory for legitimate scientific experiments involving ocean fertilization being developed by the London Convention and London Protocol Scientific Groups and its potential implications for the proponents of ocean fertilization trials. -
Geophysical Structure of the Southern Alps Orogen, South Island, New Zealand
Regional Geophysics chapter 15/04/2007 1 GEOPHYSICAL STRUCTURE OF THE SOUTHERN ALPS OROGEN, SOUTH ISLAND, NEW ZEALAND. F J Davey1, D Eberhart-Phillips2, M D Kohler3, S Bannister1, G Caldwell1, S Henrys1, M Scherwath4, T Stern5, and H van Avendonk6 1GNS Science, Gracefield, Lower Hutt, New Zealand, [email protected] 2GNS Science, Dunedin, New Zealand 3Center for Embedded Networked Sensing, University of California, Los Angeles, California, USA 4Leibniz-Institute of Marine Sciences, IFM-GEOMAR, Kiel, Germany 5School of Earth Sciences, Victoria University of Wellington, Wellington, New Zealand 6Institute of Geophysics, University of Texas, Austin, Texas, USA ABSTRACT The central part of the South Island of New Zealand is a product of the transpressive continental collision of the Pacific and Australian plates during the past 5 million years, prior to which the plate boundary was largely transcurrent for over 10 My. Subduction occurs at the north (west dipping) and south (east dipping) of South Island. The deformation is largely accommodated by the ramping up of the Pacific plate over the Australian plate and near-symmetric mantle shortening. The initial asymmetric crustal deformation may be the result of an initial difference in lithospheric strength or an inherited suture resulting from earlier plate motions. Delamination of the Pacific plate occurs resulting in the uplift and exposure of mid- crustal rocks at the plate boundary fault (Alpine fault) to form a foreland mountain chain. In addition, an asymmetric crustal root (additional 8 - 17 km) is formed, with an underlying mantle downwarp. The crustal root, which thickens southwards, comprises the delaminated lower crust and a thickened overlying middle crust. -
Active Continental Margin
Encyclopedia of Marine Geosciences DOI 10.1007/978-94-007-6644-0_102-2 # Springer Science+Business Media Dordrecht 2014 Active Continental Margin Serge Lallemand* Géosciences Montpellier, University of Montpellier, Montpellier, France Synonyms Convergent boundary; Convergent margin; Destructive margin; Ocean-continent subduction; Oceanic subduction zone; Subduction zone Definition An active continental margin refers to the submerged edge of a continent overriding an oceanic lithosphere at a convergent plate boundary by opposition with a passive continental margin which is the remaining scar at the edge of a continent following continental break-up. The term “active” stresses the importance of the tectonic activity (seismicity, volcanism, mountain building) associated with plate convergence along that boundary. Today, people typically refer to a “subduction zone” rather than an “active margin.” Generalities Active continental margins, i.e., when an oceanic plate subducts beneath a continent, represent about two-thirds of the modern convergent margins. Their cumulated length has been estimated to 45,000 km (Lallemand et al., 2005). Most of them are located in the circum-Pacific (Japan, Kurils, Aleutians, and North, Middle, and South America), Southeast Asia (Ryukyus, Philippines, New Guinea), Indian Ocean (Java, Sumatra, Andaman, Makran), Mediterranean region (Aegea, Cala- bria), or Antilles. They are generally “active” over tens (Tonga, Mariana) or hundreds (Japan, South America) of millions of years. This longevity has consequences on their internal structure, especially in terms of continental growth by tectonic accretion of oceanic terranes, or by arc magmatism, but also sometimes in terms of continental consumption by tectonic erosion. Morphology A continental margin generally extends from the coast down to the abyssal plain (see Fig. -
Mapping the Canyon
Deep East 2001— Grades 9-12 Focus: Bathymetry of Hudson Canyon Mapping the Canyon FOCUS Part III: Bathymetry of Hudson Canyon ❒ Library Books GRADE LEVEL AUDIO/VISUAL EQUIPMENT 9 - 12 Overhead Projector FOCUS QUESTION TEACHING TIME What are the differences between bathymetric Two 45-minute periods maps and topographic maps? SEATING ARRANGEMENT LEARNING OBJECTIVES Cooperative groups of two to four Students will be able to compare and contrast a topographic map to a bathymetric map. MAXIMUM NUMBER OF STUDENTS 30 Students will investigate the various ways in which bathymetric maps are made. KEY WORDS Topography Students will learn how to interpret a bathymet- Bathymetry ric map. Map Multibeam sonar ADAPTATIONS FOR DEAF STUDENTS Canyon None required Contour lines SONAR MATERIALS Side-scan sonar Part I: GLORIA ❒ 1 Hudson Canyon Bathymetry map trans- Echo sounder parency ❒ 1 local topographic map BACKGROUND INFORMATION ❒ 1 USGS Fact Sheet on Sea Floor Mapping A map is a flat representation of all or part of Earth’s surface drawn to a specific scale Part II: (Tarbuck & Lutgens, 1999). Topographic maps show elevation of landforms above sea level, ❒ 1 local topographic map per group and bathymetric maps show depths of land- ❒ 1 Hudson Canyon Bathymetry map per group forms below sea level. The topographic eleva- ❒ 1 Hudson Canyon Bathymetry map trans- tions and the bathymetric depths are shown parency ❒ with contour lines. A contour line is a line on a Contour Analysis Worksheet map representing a corresponding imaginary 59 Deep East 2001— Grades 9-12 Focus: Bathymetry of Hudson Canyon line on the ground that has the same elevation sonar is the multibeam sonar.