Netherlands Antilles: Trade and Integration with CARICOM
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An 1867-Class Tsunami: Potential Devastation in the US Virgin Islands
Watlington, Roy A. (2006) An 1867-class tsunami: potential devastation in the US Virgin Islands. In: Caribbean Tsunami Hazard, (A. Mercado and P. Liu editors, ISBN 981-256-535-3), pp 255-267. AN 1867-CLASS TSUNAMI: POTENTIAL DEVASTATION IN THE US VIRGIN ISLANDS ROY A. WATLINGTON University of the Virgin Islands Abstract This paper describes the potential devastation that might result in the United States Virgin Islands if a tsunami identical to the Virgin Islands tsunami of November 18, 1867 were to occur today. Comparisons are made based on the reported runup in 1867 and also on the changes in population, coastal infrastructure, shipping activity, and in warning and mitigation systems for natural hazards. To find examples and make comparisons to modern demographics and infrastructure, the impacts of recent damaging hurricanes are presented. Recommendations are made on preparing for and mitigating the effects of a local tsunami. Background The 1867 Virgin Islands’ tsunami was initiated by an earthquake along a fault beneath the Virgin Islands Basin. This deep body of water is defined by the islands forming its topographic barriers. St. Thomas, St. John and the British Virgin Islands separate it from the Atlantic; St. Croix separates it from the Caribbean Sea, while Vieques and Culebra define its western boundary. To the east the Basin opens to the Atlantic through the Anegada Passage. It connects to the Caribbean’s Venezuela Basin through the Jungfern Passage and Grappler Channel. Interpretation of historic data and the accounts of witnesses have placed the earthquake’s epicenter at a location approximately equidistant from St. -
A Modified Sverdrup Model of the Atlantic and Caribbean Circulation
MARCH 2002 WAJSOWICZ 973 A Modi®ed Sverdrup Model of the Atlantic and Caribbean Circulation ROXANA C. WAJSOWICZ* Department of Meteorology, University of Maryland at College Park, College Park, Maryland (Manuscript received 9 October 2000, in ®nal form 6 August 2001) ABSTRACT An analytical model of the mean wind-driven circulation of the North Atlantic and Caribbean Sea is constructed based on linear dynamics and assumed existence of a level of no motion above all topography. The circulation around each island is calculated using the island rule, which is extended to describe an arbitrary length chain of overlapping islands. Frictional effects in the intervening straits are included by assuming a linear dependence on strait transport. Asymptotic expansions in the limit of strong and weak friction show that the transport streamfunction on an island boundary is dependent on wind stress over latitudes spanning the whole length of the island chain and spanning just immediately adjacent islands, respectively. The powerfulness of the method in enabling the wind stress bands, which determine a particular strait transport, to be readily identi®ed, is demonstrated by a brief explanation of transport similarities and differences in earlier numerical models forced by various climatological wind stress products. In the absence of frictional effects outside western boundary layers, some weaker strait transports are in the wrong direction (e.g., Santaren Channel) and others are too large (e.g., Old Bahama Channel). Also, there is no western boundary current to the east of Abaco Island. Including frictional effects in the straits enables many of these discrepancies to be resolved. -
Cruise Report W-48 Scientific Activities Undertaken Aboard R/V Westward Woods Hole
Cruise Report W-48 Scientific Activities Undertaken Aboard R/V Westward Woods Hole - St. Thomas 10 October - 21 November 1979 ff/lh Westward (R.Long) • Sea Education Association - Woods Hole, Massachusetts " CRUISE REPORT W-48 Scientific Activities Woods Hole - Antigua - St. Lucia - Bequia - St. Thomas 10 October 1979 - 21 November 1979 R/V Westward Sea Education Association ',,, Woods Hole, Massachusetts .. SHIPBOARD DRAFT .. ----------------------- - ( PREFACE This Cruise Report is written in an attempt to accomplish two objectives. Firstly, and more importantly, it presents a brief outline of the scientific research completed aboard R/V Westward during W-48. Reports of the status of on-going projects and of the traditional academic program are presented. In addition, abstracts from the research projects of each student are included. Secondly, for those of us that participated, it represents the product of our efforts and contains a record of other events that were an important part of the trip, in particular the activities during port stops. Once again, lowe special thanks to Abby Ames, who was in charge of the shipboard laboratory, and upon whom I was able to depend through out the cruise. Her effectiveness and perseverance under the difficult working conditions at sea, and her cheerful attitude and enthusiasm were greatly appreciated by us all. Rob Nawojchik, who participated as an Assistant Scientist, added a new field of interest to the cruise with his vast knowledge of ichthyology. The energy with which he pursued his interest and his enthusiasm for the subject, set an example for us all. Two visiting scholars participated in different legs of this cruise. -
595 VERIFICATION of an ARCHAIC AGE OCCUPATION on BARBADOS, SOUTHERN LESSER ANTILLES Scott M Fitzpatrick Some of the More Central
RADIOCARBON, Vol 53, Nr 4, 2011, p 595–604 © 2011 by the Arizona Board of Regents on behalf of the University of Arizona VERIFICATION OF AN ARCHAIC AGE OCCUPATION ON BARBADOS, SOUTHERN LESSER ANTILLES Scott M Fitzpatrick Department of Sociology and Anthropology, NC State University, Raleigh, North Carolina, USA. Email: [email protected]. ABSTRACT. The Caribbean Archaic Age (about 3000–500 BC) is thought to represent the earliest migration of humans from South America into the Lesser Antilles. However, there is a conspicuous absence of these early sites on islands south of the Guadeloupe Passage. To date, only a single radiocarbon date derived from a Queen conch (Strombus [Eustrombus] gigas) shell at the Heywoods site on Barbados was indicative of an Archaic occupation in the southern Antilles apart from a scatter- ing of poorly reported (and mostly undated) sites. Given a number of issues associated with reliance on a single date to estab- lish a cultural horizon, along with other problems derived from possible carbonate cement contamination and dating marine shells of a longer-lived species such as Queen conch, 2 additional samples were taken from the same unit and context at Hey- woods to confirm whether the site is truly representative of an occupation during the Archaic Age. Results from a Queen conch shell adze in Context 7 dated to 2530–2200 BC (2 ) and overlaps with the only other Archaic date from the site dating to 2320–1750 cal BC, while a juvenile specimen of the same species from Context 8 at 3280–2940 BC (2 ) indicates that Barbados may have been settled even earlier. -
By W. G. D'arcy Issued by the SMITHSONIAN INSTITUTION
ATOLL RESEARCH BULLETIN No. 139 THE ISLAND OF ANEGADA AND ITS k'LORA by W. G. D'Arcy Issued by THE SMITHSONIAN INSTITUTION Washington, D. C., U. S. A. February 16, 1971 THE ISLAND OF ANEGADA AND ITS nORA The island of Anegada in the British Virgin Islands is of interest because of its isolated location in relation to the Antillean island arc, its unusual topography amongst the Virgin Islands, and also the fact that it has received very little scientific attention. It now seems destined to join the list of islands which have succumbed to modern "development". This checklist combines past published reports with the writer's own collections and attempts to correct the nomenclature formerly applied to this flora. THE ISLAND Anegada is the northeasternmost of the British Virgin Islands and of the entire West Indian arc for that matter, vying with the rocky lighthouse, Sombrero, well to the southeast, as the closest Antillean approach to Europe. Its geographic coordinates are 18'45'N and 64°20'W, and it encompasses 14.987 square miles (Klumb and Robbins 1960) or about 33 square km. In shape it is a rather lumpy crescent with its long axis running approximately west by north and east by south. The nearest land, Virgin Gorda, some thirteen miles (ca 22 km) to the south and slightly west, is a prominent feature on the horizon (Fig. I), as is the mass of the other Virgins--Tortola, Camanoe and Jost Van Dyke-- further to the southwest. To the north and east there is no land for a long way. -
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) ............................................... -
Map of National and International River Basin Districts Version 29 October 2012
Map of National and International River Basin Districts Version 29 October 2012 -30° W -20° W -10° W 0° 10° E 20° E 30° E 40° E 50° E 60° E Azores (PT) k ar FI nm in Teno, F RU Atlantic Ocean NO NO Naatamojoki, s 0 100 m FI Paatsjoki ro km T T or T R ne o i r ve n Madeira (PT) r i Madeira (PT) FI o K e m i j o k i WHITE n j SEA o RU k FI d i n a l Atlantic Ocean 60° N d r Bothnian Bay NORWEGIAN o 0 100 N SE Oulujoki SEA km NO FI a Canaries (ES) i Canaries (ES) N g 1. La Palma n a l 2. El Hierro NO h 1 7 Moere NO e t 4 60° N d 3. La Gomera A o A K 5 n G and r o B u K V u o k s i 4. Tenerife e B c k 6 h l o e f y 2 3 Romsdal f o i m r Bothnian t p m o FI 5. Gran Canaria E h T o e f i n a j l F o 6. Fuertaventura Atlantic Sea i a e f a i k g n n i RU l n o j l - 7. Lanzarote 0 100 Ocean o a C Sogn u S S k n km e e i- d and G a a Glomma SE - O Fjordane Guadeloupe (FR) NO d Guadeloupe (FR) NO lan in f F Hordaland f o ul Caribbean age West G ass C E Sea e P Bay t Aland a up k North West s lo a t de a Islands ua r g Baltic Estonia EE E G I r e s t e t t o 0 100 g Agder a EE n km a i T K k Gauja a Rogaland ak r S d LV er n Martinique (FR) Scotland ag K LV D RU Martinique (FR) k a a South LV RU N S V tt e LV a e Baltic Neagh g n u a SE t Lielupe g t a a North Bann BALTIC LT v Caribbean A NORTH SEA LT BY a Western IE Jutland SEA LT Sea Solway and N LT L Swieza UK UK North- Funen e Tweet d Zealand m 0 10 North s umbria RU u Western IE e Bornholm Jarft a km IE IE Vidaa-Krusaa ly n W RU T n Eastern o a o g PL Eastern h DK Schlei/Trave e s 50° N n -
Seattle 2015
Peripheries and Boundaries SEATTLE 2015 48th Annual Conference on Historical and Underwater Archaeology January 6-11, 2015 Seattle, Washington CONFERENCE ABSTRACTS (Our conference logo, "Peripheries and Boundaries," by Coast Salish artist lessLIE) TABLE OF CONTENTS Page 01 – Symposium Abstracts Page 13 – General Sessions Page 16 – Forum/Panel Abstracts Page 24 – Paper and Poster Abstracts (All listings include room and session time information) SYMPOSIUM ABSTRACTS [SYM-01] The Multicultural Caribbean and Its Overlooked Histories Chairs: Shea Henry (Simon Fraser University), Alexis K Ohman (College of William and Mary) Discussants: Krysta Ryzewski (Wayne State University) Many recent historical archaeological investigations in the Caribbean have explored the peoples and cultures that have been largely overlooked. The historical era of the Caribbean has seen the decline and introduction of various different and opposing cultures. Because of this, the cultural landscape of the Caribbean today is one of the most diverse in the world. However, some of these cultures have been more extensively explored archaeologically than others. A few of the areas of study that have begun to receive more attention in recent years are contact era interaction, indentured labor populations, historical environment and landscape, re-excavation of colonial sites with new discoveries and interpretations, and other aspects of daily life in the colonial Caribbean. This symposium seeks to explore new areas of overlooked peoples, cultures, and activities that have -
Search Bullet No
SEARCH BULLET NO. 236 ashineon, D.C., U.S.A. November 1979 I Poior t Md,tiniq"Q - CARI88EAN g o i 5r LvuajJ =& 8' SEA v'"i'"r? aJ,bdd-,D The White Horra , VENEZUELA - Jort Vai Gwat rcbw '& .; ",& THE VIRGIN ISLANDS Scale of Mlles III I d I bog Rod Heights In Feet SOME ASPECTS OF THE ECOLOGY OF REEFS SURROUNDING ANEGADA, BRITISH VIRGIIY ISLANDS 1. 2. by R.P. Dunne and B.E. Brown Introductory Description Anegada is a most unique island from many aspects. Northernmost of the American and British Virgin Islands and easternmost of the Greater Antilles, it is a flat limestone island, 17 km long and 4 km wide with a total area of about 14.94 square miles (9,567 acres 54 sq km), It is set aside from the other British Virgin Islands, being some 19 km from Virgin Gorda, its closest neighbour. It lies in distinct contrast to the volcanic and mountainous landscapes of the Virgin Group, with a maximum elevation of only 8 metres, To the north and east (windward side) the island is edged by extensive reefs beyond which stretches the Atlantic Ocean. On the leeward side, a shallow sea (2 to 8 m) separates Anegada from the main Virgin Island Group. His tory Schmburgk (1832) is the earliest authority on the island, having visited it in 1831 when he completed a most extensive survey. He writes: 'Of its history little is known; there is no likelihood that it was settled early. Ere Labat, the only early writer who speaks of the Lesser West India islands, observes, that aborigines used it as an occasional rendezvous, where they procured great quantities of conchs (~trombusgigas); and large piles of these shells are still to be seen at the east end of the island, but nowhere else ; which seems to prove decidedly that it was not permanently accupied, but merely resorted to from time to time. -
The Polyphased Tectonic Evolution of the Anegada Passage in the Northern Lesser Antilles Subduction Zone Muriel Laurencin, Boris Marcaillou, D
The polyphased tectonic evolution of the Anegada Passage in the northern Lesser Antilles subduction zone Muriel Laurencin, Boris Marcaillou, D. Graindorge, F. Klingelhoefer, Serge Lallemand, M. Laigle, Jean-Frederic Lebrun To cite this version: Muriel Laurencin, Boris Marcaillou, D. Graindorge, F. Klingelhoefer, Serge Lallemand, et al.. The polyphased tectonic evolution of the Anegada Passage in the northern Lesser Antilles subduction zone. Tectonics, American Geophysical Union (AGU), 2017, 36 (5), pp.945-961. 10.1002/2017TC004511. hal-01690623 HAL Id: hal-01690623 https://hal.archives-ouvertes.fr/hal-01690623 Submitted on 23 Jan 2018 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. PUBLICATIONS Tectonics RESEARCH ARTICLE The polyphased tectonic evolution of the Anegada Passage 10.1002/2017TC004511 in the northern Lesser Antilles subduction zone Key Points: M. Laurencin1 , B. Marcaillou2 , D. Graindorge1, F. Klingelhoefer3, S. Lallemand4, M. Laigle2, • New bathymetric and seismic data 5 highlight the deformation pattern of and J.-F. Lebrun the northern -
Annotated Supplement to the Commander's Handbook On
ANNOTATED SUPPLEMENT TO THE COMMANDER’S HANDBOOK ON THE LAW OF NAVAL OPERATIONS NEWPORT, RI 1997 15 NOV 1997 INTRODUCTORY NOTE The Commander’s Handbook on the Law of Naval Operations (NWP 1-14M/MCWP S-2.1/ COMDTPUB P5800.1), formerly NWP 9 (Rev. A)/FMFM l-10, was promulgated to U.S. Navy, U.S. Marine Corps, and U.S. Coast Guard activities in October 1995. The Com- mander’s Handbook contains no reference to sources of authority for statements of relevant law. This approach was deliberately taken for ease of reading by its intended audience-the operational commander and his staff. This Annotated Supplement to the Handbook has been prepared by the Oceans Law and Policy Department, Center for Naval Warfare Studies, Naval War College to support the academic and research programs within the College. Although prepared with the assistance of cognizant offices of the General Counsel of the Department of Defense, the Judge Advocate General of the Navy, The Judge Advocate General of the Army, The Judge Advocate General of the Air Force, the Staff Judge Advo- cate to the Commandant of the Marine Corps, the Chief Counsel of the Coast Guard, the Chairman, Joint Chiefs of Staff and the Unified Combatant Commands, the annotations in this Annotated Supplement are not to be construed as representing official policy or positions of the Department of the Navy or the U.S. Governrnent. The text of the Commander’s Handbook is set forth verbatim. Annotations appear as footnotes numbered consecutively within each Chapter. Supplementary Annexes, Figures and Tables are prefixed by the letter “A” and incorporated into each Chapter. -
(Coryphaena Hippurus) in the Northeastern Caribbean
Fisheries Research 175 (2016) 24–34 Contents lists available at ScienceDirect Fisheries Research journal homepage: www.elsevier.com/locate/fishres Movement dynamics of dolphinfish (Coryphaena hippurus) in the northeastern Caribbean Sea: Evidence of seasonal re-entry into domestic and international fisheries throughout the western central Atlantic a,b,∗ a b Wessley Merten , Richard Appeldoorn , Donald Hammond a Department of Marine Sciences, University of Puerto Rico, Mayagüez, PO Box 9000, Mayagüez, PR 00681, United States b Cooperative Science Services LLC, Dolphinfish Research Program, 961 Anchor Road, Charleston, SC 29412, United States a r t i c l e i n f o a b s t r a c t Article history: Distinct spatial variation and fisheries exchange routes for dolphinfish (Coryphaena hippurus) were Received 1 February 2015 resolved relative to the northeastern Caribbean Sea and U.S. east coast using conventional (n = 742; Received in revised form 26 May 2015 mean ± SD cm FL: 70.5 ± 15.2 cm FL) and pop-up satellite archival tags (n = 7; 117.6 ± 11.7 cm FL) Accepted 18 October 2015 from 2008 to 2014. All dolphinfish released in the northeastern Caribbean Sea moved westward ◦ ◦ (274.42 ± 21.06 ), but slower in the tropical Atlantic than Caribbean Sea, with a maximum straight- Keywords: line distance recorded between San Juan, Puerto Rico, and Charleston, South Carolina (1917.49 km); an Dolphinfish 180-day geolocation track was obtained connecting the South Atlantic Bight to the northern limits of Fisheries management Migration the Mona Passage. Two recaptures occurred within the Mona Passage from San Juan, Puerto Rico, and Mark-recapture St.