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U.S. Foreign Assistance to Latin America and the Caribbean: Recent Trends and FY2013 Appropriations
U.S. Foreign Assistance to Latin America and the Caribbean: Recent Trends and FY2013 Appropriations Peter J. Meyer Analyst in Latin American Affairs Mark P. Sullivan Specialist in Latin American Affairs June 26, 2012 Congressional Research Service 7-5700 www.crs.gov R42582 CRS Report for Congress Prepared for Members and Committees of Congress U.S. Foreign Assistance to Latin America and the Caribbean Summary Geographic proximity has forged strong linkages between the United States and the nations of Latin America and the Caribbean, with critical U.S. interests in the region encompassing economic, political, and security concerns. U.S. policymakers have emphasized different strategic interests in the region at different times, from combating Soviet influence during the Cold War to advancing democracy and open markets since the 1990s. Current U.S. policy toward the region is designed to promote economic and social opportunity; ensure citizen security; strengthen effective democratic institutions; and secure a clean energy future. As part of broader efforts to advance these priorities, the United States provides Latin American and Caribbean nations with substantial amounts of foreign assistance. Congress – which authorizes and appropriates aid for the region, and engages in oversight of assistance programs – is currently considering the President’s foreign aid request for FY2013. In recent years, the State Department, Foreign Operations, and Related Programs appropriations measure has been the primary legislative vehicle through which Congress reviews U.S. assistance and influences executive branch policy toward the region. Trends in Assistance Since 1946, the United States has provided over $148 billion (constant 2010 dollars) in assistance to the region. -
Article Is Available Online Initiation, Earth Planet
Solid Earth, 9, 713–733, 2018 https://doi.org/10.5194/se-9-713-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Boninite and boninite-series volcanics in northern Zambales ophiolite: doubly vergent subduction initiation along Philippine Sea plate margins Americus Perez1, Susumu Umino1, Graciano P. Yumul Jr.2, and Osamu Ishizuka3,4 1Division of Natural System, Graduate School of Natural Science and Technology, Kanazawa University, Kakuma-machi, Kanazawa, 920-1192, Japan 2Apex Mining Company Inc., Ortigas Center, Pasig City, 1605, Philippines 3Research Institute of Earthquake and Volcano Geology, Geological Survey of Japan, AIST, Tsukuba Central 7, 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan 4Research and Development Center for Ocean Drilling Science, JAMSTEC, 2-15 Natsushima, Yokosuka, Kanagawa 237-0061, Japan Correspondence: Americus Perez ([email protected], [email protected]) Received: 25 December 2017 – Discussion started: 31 January 2018 Revised: 7 May 2018 – Accepted: 12 May 2018 – Published: 5 June 2018 Abstract. A key component of subduction initiation rock itudes derived from tilt-corrected sites in the Acoje Block suites is boninite, a high-magnesium andesite that is uniquely place the juvenile arc of northern Zambales ophiolite in the predominant in western Pacific forearc terranes and in select western margin of the Philippine Sea plate. In this scenario, Tethyan ophiolites such as Oman and Troodos. We report, for the origin of Philippine Sea plate boninites (IBM and Zam- the first time, the discovery of low-calcium, high-silica boni- bales) would be in a doubly vergent subduction initiation set- nite in the middle Eocene Zambales ophiolite (Luzon Island, ting. -
3D Visualisation Model of the Taupo Volcanic Zone Basement S.A
3D VISUALISATION MODEL OF THE TAUPO VOLCANIC ZONE BASEMENT S.A. Alcaraz 1, M.S. Rattenbury 2, M.D. Rosenberg 1, S. Soengkono 1, G. Bignall 1 and H. van Moerkerk 3 1 GNS Science, Wairakei Research Centre, Private Bag 2000, Taupo 3352, New Zealand 2 GNS Science, PO Box 30-368, Lower Hutt 5040, New Zealand 3 ARANZ Geo Ltd., PO Box 3894, Christchurch 8140, New Zealand [email protected] Keywords: 3D modelling, 3D visualisation, calderas, 2001). The TVZ has been drilled for geothermal and Taupo Volcanic Zone, Torlesse Supergroup, Leapfrog mineral exploration, with recent drilling including Geothermal exploration, production and injection of deep geothermal boreholes. These boreholes are providing new information ABSTRACT on the geology and structure of several TVZ geothermal The Taupo Volcanic Zone (TVZ; ~350 km long, ~60 km systems, including Wairakei-Tauhara (Rosenberg et al., wide) constitutes the southern portion of the active Lau- 2009; Bignall et al., 2010; Alcaraz et al., 2010), Ohaaki Havre-Taupo extensional back arc basin, and formed by (Milicich et al., 2008; Milicich et al., 2010b), Kawerau extension of crust above the Hikurangi subduction zone in (Milicich et al., 2010a; Alcaraz, 2010) and Ngatamariki the central North Island. The fault-controlled depression is (Bignall, 2009). infilled by Quaternary volcanic rock and sediments, with the top of underlying basement greywacke displaced up to In recent years, the New Zealand geothermal community 1-2 km below sea level. has come to consider the potential of untapped, deeper and hotter geothermal resources in the TVZ – i.e. beyond the 1 A geological basement model of top surface of the Torlesse to 3 km depth interval that defines most of the >240°C greywacke in the TVZ is presented. -
EGU2017-16685, 2017 EGU General Assembly 2017 © Author(S) 2017
Geophysical Research Abstracts Vol. 19, EGU2017-16685, 2017 EGU General Assembly 2017 © Author(s) 2017. CC Attribution 3.0 License. From rifting to spreading - seismic structure of the rifted western Mariana extinct arc and the ParceVela back-arc basin Ingo Grevemeyer (1), Shuichi Kodaira (2), Gou Fujie (2), and Narumi Takahashi (2) (1) GEOMAR Helmholtz Centre of Ocean Research, RD4 - Marine Geodynamics, Kiel, Germany ([email protected]), (2) Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan The proto Izu-Ogasawara (Bonin)-Mariana (IBM) Island arc was created when subduction of the Pacific plate be- gan during the Eocene. Today, the Kyushu-Palau Ridge (KPR) at the centre of the Philippine Sea and the western Mariana Ridge (WMR) are considered to be a remnant of the proto IBM Island arc. The KPR and WMR were separated when back-arc spreading began at 30 to 29 Ma in the Shikoku Basin and ParceVela Basin (PVB). Vol- canic activity along the arcs diminished at 27 Ma and there is little evidence of volcanic activity between 23–17 Ma. Arc volcanism was reactivated at ∼15 Ma, when the opening of the Shikoku Basin and PVB ceased. At about 5 Ma the Mariana Basin opened, rifting the WMR from the Mariana arc. Here, we report results from the seismic refraction and wide-angle profile MR101c shot in summer of 2003 by the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) aboard the RV KAIYO during the cruise KY03-06, extending from the PVB across the WMR and terminating just to the east of the WMR. -
Wood Calderas and Geothermal Systems in The
WOOD CALDERAS AND GEOTHERMAL SYSTEMS IN THE TAUPO VOLCANIC ZONE, NEW ZEALAND C Peter Wood Institute of Geological Nuclear Sciences Ltd, Wairakei Research Centre Taupo, New Zealand Key Words: Calderas, Geothermal Systems, Taupo Volcanic Zone. New Zcaland 2. TAUPO VOLCANIC ZONE The Taupo Volcanic Zone Fig. 1) is the consequence of plate subduction beneath the North Island of New Zcaland. ABSTRACT The thin continental crust (-15 km, Stem and Davey, 1987) spreads at rates up to 18 (Darby and Williams, 1991) Silicic calderas and geothermal systems in Taupo Volcanic in active rifting and subsidence. Since c. 1.6 Ma, the Zone (TVZ) of New Zealand are spatially related. Eight calderas, central TVZ has been the most frequently active and productive active since 1.6 Ma, occupy 45% of the Boundaries of region of rhyolitic volcanism on earth (Houghton et al., 1994). calderas arc often speculative, but of 20 geothermal systems producing an estimated 10 - 15 of rhyolite, and considercd, 15 occur on or next to a caldera margin where there is subordinate dacite, andesite and basalt. Debate continues whether enhanced deep permeability: the best examples are at Haroharo TVZ is a migrating andesitic arc and zone of asymmetric crustal where systems occur at the intersection of volcanic lineations and spreading (eg. Stem, or an andesite-dacite arc with bimodal caldera embayments, and at Rotorua. Drillhole evidence supports rhyolite-basalt back arc (eg. Cole, 1990). Whichever is the case, a realignment of caldera margin through the Wairakei- it is a matter of observation that most geothermal fields are geothermal field. Four geothermal systems have no known contained within the area of rhyolite volcanism. -
Bathymetry of the New Zealand Region
ISSN 2538-1016; 11 NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH BULLETIN 161 BATHYMETRY OF THE NEW ZEALAND REGION by J. W. BRODIE New Zealand Oceanographic Institute Wellington New Zealand Oceanographic Institute Memoir No. 11 1964 This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ Fromispiece: The survey ship HMS Penguin from which many soundings were obtained around the New Zealand coast and in the south-west Pacific in the decade around 1900. (Photograph by courtesy of the Trustees, National Maritime Museum, Greenwich.) This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH BULLETIN 161 BATHYMETRY OF THE NEW ZEALAND REGION by J. W. BRODIE New Zealand Oceanographic Institute Wellington New Zealand Oceanographic Institute Memoir No. 11 1964 Price: 15s. This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ CONTENTS Page No. ABSTRACT 7 INTRODUCTION 7 Sources of Data 7 Compilation of Charts 8 EARLIER BATHYMETRIC INTERPRETATIONS 10 Carte Gen�rale Bathymetrique des Oceans 17 Discussion 19 NAMES OF OCEAN FLOOR FEATURES 22 Synonymy of Existing Names 22 Newly Named Features .. 23 FEATURES ON THE CHARTS 25 Major Morphological Units 25 Offshore Banks and Seamounts 33 STRUCTURAL POSITION OF NEW ZEALAND 35 The New Zealand Plateau 35 Rocks of the New Zealand Plateau 37 Crustal Thickness Beneath the New Zealand Plateau 38 Chatham Province Features 41 The Alpine Fault 41 Minor Irregularities on the Sea Floor 41 SEDIMENTATION IN THE NEW ZEALAND REGION . -
The Taupo Eruption Sequence of AD 232±10 in Aotearoa New
地学雑誌 Journal of Geography(Chigaku Zasshi) 130(1)117141 2021 doi:10.5026/jgeography.130.117 The 100s: Significant Exposures of the World( No. 12) The Taupō Eruption Sequence of AD 232 ± 10 in Aotearoa New Zealand: A Retrospection * * David J. LOWE and Adrian PITTARI [Received 9 June, 2020; Accepted 13 August, 2020] Abstract The Taupō eruption, also known as eruption Y, occurred in late summer to early autumn (typically late March to early April) in AD 232 10 yr at Taupō volcano, an ‘inverse’ caldera volcano underlying Lake Taupō in the central Taupō Volcanic Zone, North Island, Aotearoa New Zealand. The complex rhyolitic eruption, the most powerful eruption globally in the last 5000 years, lasted between several days and several weeks and generated five markedly contrasting pyroclastic fall deposits( units Y1 to Y5) followed by the extremely violent emplacement of a low-aspect-ratio ignimbrite( unit Y6). The fall deposits include three phreatomagmatic units, Y1, Y3, and Y4, the latter two being the products of archetypal phreatoplinian events; and two magmatic units, Y2 and Y5, the latter being the product of an exceptionally powerful plinian (previously described as ‘ultraplinian’) event with an extreme magma discharge rate around 108 to 1010 kg s-1. The pyroclastic fall-generating eruptions were followed by the climactic emplace- ment of the entirely non-welded Taupō ignimbrite( Y6). It was generated by the catastrophic collapse of the 35 to 40-km-high plinian eruption column( Y5) that produced a very-fast-moving (600 to 900 km h-1), hot( up to 500°C) pyroclastic flow( density current) that covered about 20,000 km2 of central North Island over a near-circular area ~160 km in diameter, centred on Lake Taupō, in fewer than about ten to 15 minutes. -
A Submarine Magmatic-Hydrothermal System at Brothers Volcano, Kermadecs
Proceedings 26th NZ Geothermal Workshop 2004 A SUBMARINE MAGMATIC-HYDROTHERMAL SYSTEM AT BROTHERS VOLCANO, KERMADECS A. G. REYES, C.E.J. DE RONDE, AND C. W. R. SOONG Institute of Geological and Nuclear sciences, Lower Hutt, New Zealand SUMMARY –Secondary minerals in dredge samples from the Brothers Volcano include silicates, silica polymorphs; Na-Al, Ca, Ba and Ba-Sr sulphates; Fe, Cu, Zn, As and Pb sulphides; Fe and Mn oxide/oxyhydroxides and native S. The variety and range of mineral compositions indicate deposition in different parts of a submarine hydrothermal system characterised by differences in temperature (ambient seawater to >300oC), fluid compositions, degree of magmatic-hydrothermal water-rock interaction and degree of seawater influence. Secondary minerals originate from a partly exhumed waning hydrothermal system/s (NW caldera); the main upflow of a relatively well-established active magmatic-hydrothermal system on the seafloor where sulphide-rich chimneys are extant (SE caldera) and a nascent magmatic- hydrothermal system where crack zones localise upwelling acid waters from depth (cone). 1. INTRODUCTION possibly two more) of 13 volcanoes (Massoth et al, 2003). The unusually high concentrations of Active seafloor hydrothermal venting and CO2, sulphur gases and Fe in the seafloor vent sulphide deposits were first reported in two discharges are believed to be hybrid mixtures of southern Kermadec frontal arc caldera volcanoes, hydrothermal and magmatic fluids (Massoth et al, Brothers and Rumble II (West), of the Kermadec- 2003). Of the seven hydrothermally active Havre arc-back arc system (Fig. 1) by Wright et al volcanoes, the Brothers volcano is the most (1998). In 1999 a systematic reconnaissance for active, (de Ronde et al, 2003) having two separate submarine hydrothermal activity in the southern vent sites including high-temperature black Kermadec arc found hydrothermal chemical smoker venting (Stoffers et al, 1999). -
The Transatlantic Cocaine Market
Vienna International Centre, PO Box 500, 1400 Vienna, Austria Tel.: (+43-1) 26060-0, Fax: (+43-1) 26060-5866, www.unodc.org The Transatlantic Cocaine Market Research Paper United Nations publication FOR UNITED NATIONS USE ONLY ISBN ???-??-?-??????-? ISSN ????-???? Sales No. T.08.XI.7 Printed in Austria ST/NAR.3/2007/1 (E/NA) job no.—Date—copies April 2011 ACKNOWLEDGEMENTS This report was prepared by the Studies and Threat Analysis Section in collaboration with the Regional Office in Senegal and the Integrated Programme and Oversight Branch of UNODC. The following staff members contributed to this document: Studies and Threat Analysis Section: Thibault Le Pichon, Thomas Pietschmann, Ted Leggett, Raggie Johansen Regional Office in Senegal: Alexandre Schmidt, David Izadifar Integrated Programme and Oversight Branch: Aisser Al-Hafedh, Olivier Inizan Strategic Planning Unit: Gautam Babbar DISCLAIMER This report has not been formally edited. The designations employed and the presentation of material in this report do not imply the expression of any opinion whatsoever on the part of UNODC concerning the legal status of any country, territory or city or its authorities, or concerning the delimitation of its frontiers and boundaries. The contents of this report do not necessarily reflect the views of the Member States. The Transatlantic Cocaine Market Key findings....................................................................................................................... 2 Key data / estimates ......................................................................................................... -
Chile: Earthquake GLIDE EQ-2010-000034-CHL 27 February 2010
Information bulletin n° 1 Chile: Earthquake GLIDE EQ-2010-000034-CHL 27 February 2010 This bulletin is being issued for information only, and reflects the current situation and details available. The Chilean Red Cross (CRC) has determined that external assistance is not required at this time; however, as the situation is assessed, there may be a need for funding or other assistance from donors once more information is available on the impact of the disaster. <click here to view the map of the affected area, or here for detailed contact information> On 27 February 2010 at about 3:35 a.m. local time, an earthquake of magnitude 8.8 occurred in the moderately populated region of Bio-Bio in central Chile. The earthquake struck 90 kilometres north-east of the city of Concepción, the capital of Bio-Bio, and there have been many aftershocks. A tsunami alert has been generated in Chile and most of all countries on the Pacific Coast. At least 100 people have been killed and many affected after the huge earthquake struck the Chilean coast and caused buildings to collapse in the capital, Santiago. The Pacific Tsunami Warning Centre informed that sea level readings indicate a tsunami was generated. The Situation The 8.8 magnitude earthquake that hit the coast of Chile has killed at least 100 people, flattening buildings and triggering a tsunami. This has been the country’s largest earthquake for 25 years. A tsunami warning has been extended across the Pacific rim, including most of Central and South America and as far as Australia and Antarctica. -
Chapter 36D. South Pacific Ocean
Chapter 36D. South Pacific Ocean Contributors: Karen Evans (lead author), Nic Bax (convener), Patricio Bernal (Lead member), Marilú Bouchon Corrales, Martin Cryer, Günter Försterra, Carlos F. Gaymer, Vreni Häussermann, and Jake Rice (Co-Lead member and Editor Part VI Biodiversity) 1. Introduction The Pacific Ocean is the Earth’s largest ocean, covering one-third of the world’s surface. This huge expanse of ocean supports the most extensive and diverse coral reefs in the world (Burke et al., 2011), the largest commercial fishery (FAO, 2014), the most and deepest oceanic trenches (General Bathymetric Chart of the Oceans, available at www.gebco.net), the largest upwelling system (Spalding et al., 2012), the healthiest and, in some cases, largest remaining populations of many globally rare and threatened species, including marine mammals, seabirds and marine reptiles (Tittensor et al., 2010). The South Pacific Ocean surrounds and is bordered by 23 countries and territories (for the purpose of this chapter, countries west of Papua New Guinea are not considered to be part of the South Pacific), which range in size from small atolls (e.g., Nauru) to continents (South America, Australia). Associated populations of each of the countries and territories range from less than 10,000 (Tokelau, Nauru, Tuvalu) to nearly 30.5 million (Peru; Population Estimates and Projections, World Bank Group, accessed at http://data.worldbank.org/data-catalog/population-projection-tables, August 2014). Most of the tropical and sub-tropical western and central South Pacific Ocean is contained within exclusive economic zones (EEZs), whereas vast expanses of temperate waters are associated with high seas areas (Figure 1). -
Evaluating the Environmental Impacts of Fracking in New Zealand: an Interim Report
1 Evaluating the environmental impacts of fracking in New Zealand: An interim report November 2012 2 Acknowledgements The Parliamentary Commissioner for the Environment would like to express her gratitude to those who assisted with the research and preparation of this report, with special thanks to her staff who worked so tirelessly to bring it to completion. Photography Cover: Coal seam gas fracking in Ohai, Southland. Photo courtesy of Dr Murry Cave. This document may be copied provided that the source is acknowledged. This report and other publications by the Parliamentary Commissioner for the Environment are available at: www.pce.parliament.nz 3 Contents Contents 3 Overview 5 3 1 Introduction 9 1.1 The purpose of this report 11 1.2 What is fracking? 12 1.3 Structure of the report 15 1.4 What the report does not cover 15 2 From conventional oil and gas to fracking 17 2.1 The early days 18 2.2 The rise of fracking 20 2.3 Fracking controversy 21 3 New Zealand history of gas and oil 23 3.1 Early discoveries of oil and gas in New Zealand 23 3.2 Natural gas and 'Think Big' 25 3.3 Unconventionals and the prospect of oil 26 3.4 Fracking in New Zealand 27 3.5 What worries people about fracking? 28 4 Environmental issues associated with fracking 31 4.1 Choosing where to drill 32 4.2 Establishing the well site 34 4.3 Drilling and constructing the well 35 4.4 Fracking the well 38 4.5 Flowback and transitioning into production 45 4.6 Handling the waste 46 4.7 Ending production and abandoning the well 48 4.8 Summary 49 5 The role of public agencies