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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. -
Historical Archaeology in the French Caribbean: an Introduction to a Special Volume of the Journal of Caribbean Archaeology
Journal of Caribbean Archaeology Copyright 2004 ISSN 1524-4776 HISTORICAL ARCHAEOLOGY IN THE FRENCH CARIBBEAN: AN INTRODUCTION TO A SPECIAL VOLUME OF THE JOURNAL OF CARIBBEAN ARCHAEOLOGY Kenneth G. Kelly Department of Anthropology University of South Carolina Columbia SC 29208, USA [email protected] _______________________________________________________ The Caribbean region has seen a projects too numerous to mention, throughout tremendous growth in historical archaeology the Caribbean, with only a few areas excepted over the past 40 years. From important, (for an example of the coverage, see the although isolated beginnings in Jamaica, at papers in Farnsworth 2001 and Haviser 1999). Port Royal and Spanish Town and Montpelier (Mayes 1972; Mathewson 1972, 1973; Not only have nearly all islands of the Higman 1974, 1998), in Barbados at Newton Caribbean been the focus of at least some Cemetery (Handler and Lange 1978), and historical archaeology, but also the types of elsewhere in the Caribbean, the field has historical archaeological research have been expanded at a phenomenal rate. The late diverse. Thus, studies of both industry and 1970s and the early 1980s saw the initiation of labor have been conducted on sugar, coffee several important long-term studies, including and cotton plantations in the Greater and Norman Barka’s island-wide focus on rural Lesser Antilles. Military fortifications have and urban life in the Dutch territory of St. been documented and explored in many areas. Eustatius (Barka 1996), Kathleen Deagan’s Urban residential and commercial sites have multi-year project at Puerto Real and the been investigated, and ethnic minorities neighboring site of En Bas Saline in Haïti within the dominant class, such as Jewish and (Deagan 1995), Douglas Armstrong’s work at Irish populations, have been the focus of Drax Hall, Jamaica (Armstrong 1985, 1990), research programs. -
By the Becreu^ 01 Uio Luterior NFS Form 10-900 USDI/NPS NRHP Registration Form (Rev
NATIONAL HISTORIC LANDMARK NOMINATION NFS Form 10-900 USDI/NPS NRHP Registration Form (Rev. 8-86) 0MB No. 1024-0018 FORT FREDERIK (U.S. VIRGIN ISLANDS) Page 1 United States Department of the Interior, National Park Service____________________________ National Register of Historic Places Registration Form l^NAMEOF PROPERTY Historic Name: FORT FREDERIK (U.S. VIRGIN ISLANDS) Other Name/Site Number: FREDERIKSFORT 2. LOCATION Street & Number: S. of jet. of Mahogany Rd. and Rt. 631, N end of Frederiksted Not for publication:N/A City/Town: Frederiksted Vicinity :N/A State: US Virgin Islands County: St. Croix Code: 010 Zip Code:QQ840 3. CLASSIFICATION Ownership of Property Category of Property Private: __ Building(s): X Public-local: __ District: __ Public-State: X Site: __ Public-Federal: Structure: __ Object: __ Number of Resources within Property Contributing Noncontributing 2 __ buildings 1 sites 1 __ structures _ objects 1 Total Number of Contributing Resources Previously Listed in the National Register :_2 Name of related multiple property listing: N/A tfed a by the becreu^ 01 uio luterior NFS Form 10-900 USDI/NPS NRHP Registration Form (Rev. 8-86) OMB No. 1024-0018 FORT FREDERIK (U.S. VIRGIN ISLANDS) Page 2 United States Department of the Interior, National Park Service _______________________________National Register of Historic Places Registration Form 4. STATE/FEDERAL AGENCY CERTIFICATION As the designated authority under the National Historic Preservation Act of 1966, as amended, I hereby certify that this __ nomination __ request for determination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 CFR Part 60. -
Historical and Contemporary Use of Natural Stones in the French West Indies
Article Historical and Contemporary Use of Natural Stones in the French West Indies. Conservation Aspects and Practices Yves Mazabraud * Géosciences Montpellier, Université des Antilles, Université de Montpellier, CNRS, Morne Ferret, BP517, 97178 Les Abymes, France; [email protected]; Tel.: +590-590-21-36-15 Received: 20 June 2019; Accepted: 19 August 2019; Published: 22 August 2019 Abstract: The French West Indies (F.W.I.), in the Eastern Caribbean, are part of a biodiversity hotspot and an archipelago of very rich geology. In this specific natural environment, the abundance or the lack of various natural resources has influenced society since the pre-Columbian era. The limited size of the islands and the growth of their economy demand a clear assessment of both the natural geoheritage and the historical heritage. This paper presents a brief review of the variety of the natural stone architectural heritage of the F.W.I. and of the available geomaterials. Some conservation issues and threats are evidenced, with particular emphasis on Guadeloupe. Some social practices are also evoked, with the long-term goal of studying the reciprocal influence of local geology and society on conservation aspects. Finally, this paper argues that unawareness is one of the main obstacles for the conservation of the geoheritage and the natural stone architectural heritage in the F.W.I. Keywords: building stones; Guadeloupe; Martinique; French West Indies; eastern Caribbean; cultural heritage; geological heritage; historical and Archaeological sites 1. Introduction In 2002, the law for a Democracy of Proximity [1] was voted by the French parliament. It stated that the State takes care of the conception, the animation, and the evaluation of the Natural Heritage. -
2. Geophysics and the Structure of the Lesser Antilles Forearc1
2. GEOPHYSICS AND THE STRUCTURE OF THE LESSER ANTILLES FOREARC1 G. K. Westbrook, Department of Geological Sciences, University of Durham and A. Mascle and B. Biju-Duval, Institut Français du Pétrole2 ABSTRACT The Barbados Ridge complex lies east of the Lesser Antilles volcanic arc along the eastern margin of the Caribbean Plate. The complex dates in part from the Eocene, and elements of the arc system have been dated as Late Cretaceous and Late Jurassic, although most of the volcanic rocks date from the Tertiary, particularly the latter part. It is probable that the arc system was moved a considerable distance eastward with respect to North and South America during the Tertiary. The accretionary complex can be divided into zones running parallel to the arc, starting with a zone of initial accre- tion at the front of the complex where sediment is stripped from the ocean floor and the rate of deformation is greatest. This zone passes into one of stabilization where the deformation rate is generally lower, although there are localized zones of more active tectonics where the generally mildly deformed overlying blanket of sediment is significant dis- turbed. Supracomplex sedimentary basins that are locally very thick are developed in the southern part of the complex. The Barbados Ridge Uplift containing the island of Barbados lies at the western edge of the complex; between it and the volcanic arc lies a large forearc basin comprising the Tobago Trough and Lesser Antilles Trough. There are major longitudinal variations in the complex that are broadly related to the northward decrease in sedi- ment thickness away from terrigenous sources in South America and that are locally controlled by ridges in the oceanic igneous crust passing beneath the complex. -
Two New Species of Dyscinetus from the West Indies and South America (Coleoptera: Scarabaeidae: Dynastinae)
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Papers in Entomology Museum, University of Nebraska State February 1986 TWO NEW SPECIES OF DYSCINETUS FROM THE WEST INDIES AND SOUTH AMERICA (COLEOPTERA: SCARABAEIDAE: DYNASTINAE) Brett C. Ratcliffe University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/entomologypapers Part of the Entomology Commons Ratcliffe, Brett C., "TWO NEW SPECIES OF DYSCINETUS FROM THE WEST INDIES AND SOUTH AMERICA (COLEOPTERA: SCARABAEIDAE: DYNASTINAE)" (1986). Papers in Entomology. 72. https://digitalcommons.unl.edu/entomologypapers/72 This Article is brought to you for free and open access by the Museum, University of Nebraska State at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in Entomology by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. The ColeopteristsBulletin, 40(1):75-80. 1986. TWO NEW SPECIES OF DYSCZNETUS FROM THE WEST INDIES AND SOUTH AMERICA (COLEOPTERA: SCARABAEIDAE: DYNASTINAE) Systematics Research Collections, W436 Nebraska Hall University of Nebraska, Lincoln, NE 68588-05 14 U.S.A. Dyscinetus imitator is described as new from Grand Cayman Island, West Indies, and D. ornaticaudus is described as new from Colombia. The New World genus Dyscinetus Harold was last revised by Endrodi (1 966) wherein he listed 13 valid species. Since that time, Chalumeau (1 982) described one additional species. Great reliance is placed on the form of the parameres of the male genitalia to distinguish Dyscinetus species. This is necessary because the body form and external sculpturing are often so similar between certain taxa that reliable separation based on these characters in impossible. -
Caribbean Markets for US Wood Products
,~~~~United States Department of i_/ Agriculture Caribbean Markets Forest Service Southern Forest for U.S. Wood Experiment Station New Orleans, Products Louisiana Research Paper SO-225 July 1986 Harold W. Wisdom, James E. Granskog, and Keith A. Blatner Mexico I SUMMARY The West Indies and the continental countries bordering the Caribbean Sea constitute a significant market for U.S. wood products. In 1983, wood product exports to the region totaled almost $157 million. The Caribbean Basin primar- ily is a market for softwood products, with pine lumber being the most promi- nent item. The flow of exports to the region is dominated by (1) overseas shipments from southern ports to the West Indies and (2) overland shipments from the Southwestern United States to Mexico. CONTENTS INTRODUCTION ................................................. 1 THE CARIBBEAN BASIN .......................................... 1 Forests .......................................................... 1 Mexico ........................................................ 2 Central America ............................................... 2 South Rim ..................................................... 3 West Indies .................................................... 3 Wood Production and Trade ....................................... 3 U.S. WOOD EXPORTS ............................................. 4 Roundwood ...................................................... 5 Logs ........................................................... 5 Poles ......................................................... -
Active Structures in the Barbados Accretionary Wedge of the Lesser Antilles Subduction: Implications for Slip Partitioning
EGU2020-10732 https://doi.org/10.5194/egusphere-egu2020-10732 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Main active structures in the Barbados accretionary wedge of the Lesser Antilles Subduction: implications for slip partitioning Gaëlle Bénâtre1, Nathalie Feuillet1, Hélène Carton1, Eric Jacques1, and Thibaud Pichot2 1Université de Paris, Institut de Physique du Globe de Paris, CNRS UMR7154, Paris, F-75005, France ([email protected]) 2Beicip-Franlab, Rueil-Malmaison, France At the Lesser Antilles Subduction Zone (LASZ), the American plates subduct under the Caribbean plate at a slow rate of ~2 cm/yr. No major subduction megathrust earthquakes have occurred in the area since the 1839 and 1843 historical events, and the LASZ is typically considered weakly coupled. At the front of the LASZ, the Barbados accretionary wedge (BAW) is one of the largest accretionary wedges in the world. The width of the BAW decreases northward, owing to the increasing distance to the sediment source (Orinoco river) and the presence of several aseismic oceanic ridges, in particular the Tiburon ridge, that stops sediment progression. Marine geophysical studies conducted to date over the northern part of the BAW (Guadeloupe-Martinique sector) have mostly focused on resolving the geometry of the backstop. However, the structure of the wedge and the mechanical behavior of the subduction interface remain poorly known. Our study aims to describe the geometry of the BAW by a detailed morpho-tectonic analysis in order to place constraints on present and past dynamic interactions between the subducting and overriding plates. -
Creolization on the Move in Francophone Caribbean Literature
Georgia State University ScholarWorks @ Georgia State University World Languages and Cultures Faculty Publications Department of World Languages and Cultures 1-2015 Creolization on the Move in Francophone Caribbean Literature Gladys M. Francis Georgia State University, [email protected] Follow this and additional works at: https://scholarworks.gsu.edu/mcl_facpub Part of the Other Languages, Societies, and Cultures Commons Recommended Citation Francis, Gladys M. "Creolization on the Move in Francophone Caribbean Literature." The Oxford Diasporas Programme. Oxford: The University of Oxford (2015): 1-15. http://www.migration.ox.ac.uk/odp/pdfs/ Francis,%20G,%202015%20Creolization%20on%20the%20Move-1.pdf This Working Paper is brought to you for free and open access by the Department of World Languages and Cultures at ScholarWorks @ Georgia State University. It has been accepted for inclusion in World Languages and Cultures Faculty Publications by an authorized administrator of ScholarWorks @ Georgia State University. For more information, please contact [email protected]. Working Papers Paper 01, January 2015 Creolization on the Move in Francophone Caribbean Literature Dr Gladys M. Francis This paper is published as part of the Oxford Diasporas Programme (www.migration.ox.ac.uk/odp). The Oxford Diasporas Programme (ODP) is funded by the Leverhulme Trust. ODP does not have an institutional view and does not aim to present one. The views expressed in this document are those of its independent author. Abstract In this paper I explore the particular use of dance and music observed in the writings of Maryse Condé, Ina Césaire, and Gerty Dambury. I examine how their use of orality, oral literature, and the body in movement create complex levels of textuality, meaning, and reading. -
THE LIMITS of SELF-DETERMINATION in OCEANIA Author(S): Terence Wesley-Smith Source: Social and Economic Studies, Vol
THE LIMITS OF SELF-DETERMINATION IN OCEANIA Author(s): Terence Wesley-Smith Source: Social and Economic Studies, Vol. 56, No. 1/2, The Caribbean and Pacific in a New World Order (March/June 2007), pp. 182-208 Published by: Sir Arthur Lewis Institute of Social and Economic Studies, University of the West Indies Stable URL: http://www.jstor.org/stable/27866500 . Accessed: 11/10/2013 20:07 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. University of the West Indies and Sir Arthur Lewis Institute of Social and Economic Studies are collaborating with JSTOR to digitize, preserve and extend access to Social and Economic Studies. http://www.jstor.org This content downloaded from 133.30.14.128 on Fri, 11 Oct 2013 20:07:57 PM All use subject to JSTOR Terms and Conditions Social and Economic Studies 56:1&2 (2007): 182-208 ISSN:0037-7651 THE LIMITS OF SELF-DETERMINATION IN OCEANIA Terence Wesley-Smith* ABSTRACT This article surveys processes of decolonization and political development inOceania in recent decades and examines why the optimism of the early a years of self government has given way to persistent discourse of crisis, state failure and collapse in some parts of the region. -
Colonisation of the Antilles by South American Fauna: Giant Sunken Islands As a Passageway?
NATIONAL PRESS RELEASE – PARIS – 18 MAY 2021 Colonisation of the Antilles by South American fauna: giant sunken islands as a passageway? Fossils of land animals from South America have been found in the Antilles. The appearance/disappearance of archipelagos is due to tectonic plate movements and glacial- interglacial cycles. Archipelagos have emerged and sunk in a cyclic manner for millions of years, favouring the displacement of the Antilles. Fossils of land animals from South America have been found in the Antilles, but how did these animals get there? According to scientists from the CNRS, l’Université des Antilles, l’Université de Montpellier and d’Université Côte d’Azur, land emerged in this region and then disappeared beneath the waves for millions of years, explaining how some species were able to migrate to the Antilles. This study will be published in June 2021 issue in Earth-Science Reviews. Fossils of land animals from the Antilles, including mammals and amphibians, have their closest relatives in South America. The crossing of the Caribbean Sea from South America was therefore possible, but how? As swimming across the continent must be ruled out, given that several hundred kilometres separate the South American continent from the Antilles, the dispersal of this fauna has been attributed either to natural rafts coming out of the continent's flooded rivers, or to the existence of land bridges that are now submerged. A scientific project involving geologists, palaeontologists and geophysicists1 is now solving some of the mysteries related to these terrestrial species in the Antilles. The researchers have reconstructed the geography of the northern Lesser Antilles over the last 40 million years and have shown that the movements of the tectonic plates at the junction between the Lesser Antilles, the Greater Antilles and the Aves Ridge (an underwater mountain), have several times given birth to archipelagos and islands quite close to each other, which were then swallowed up in the course of time. -
Latin America and the Caribbean in the World Economy
2014 Latin America and the Caribbean in the World Economy Regional integration and value chains in a challenging external environment 2014 Alicia Bárcena Executive Secretary Antonio Prado Deputy Executive Secretary Osvaldo Rosales Chief, Division of International Trade and Integration Ricardo Pérez Chief, Publications and Web Services Division Latin America and the Caribbean in the World Economy is the annual report prepared by the Division of International Trade and Integration of ECLAC. The ECLAC subregional headquarters for the Caribbean, the ECLAC subregional headquarters in Mexico and the Latin American and Caribbean Institute for Economic and Social Planning (ILPES) assisted with the preparation of this year’s edition. The production of the report was overseen by Osvaldo Rosales, Chief of the Division of International Trade and Integration. Keiji Inoue, Senior Economic Affairs Officer of the Division, was responsible for its technical coordination. The following staff members of the Commission assisted in the preparation and drafting of the chapters: José Elías Durán, Sebastián Herreros, Sheldon McLean, Nanno Mulder and Dayna Zaclicever. The authors are grateful for contributions made to the work by Sebastián Castresana, Carlos D’Elía, Myriam Echeverría, Alfonso Finot, Tania García-Millán, René Hernández, Antoine Le Squeren, Jorge Mario Martínez, José Carlos Mattos, Javier Meneses, Yoshimichi Murakami, Nahuel Oddone, Ramón Padilla and Gustavo Zanabria. Notes The following symbols have been used in the tables in this publication: • Three dots (…) indicate that data are not available or are not separately reported. • A dash (-) indicates that the amount is nil or negligible. • A comma (,) is used to indicate decimals. • The word “dollars” refers to United States dollars, unless otherwise specified.