A VISIT to the ANDES of VENEZUELA. A. E. Gunther
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R DEL ES Licardo Archila
'Dr. 'R licardo Archila GEOGRAFIA MEDICO-SANITARIA DEL ES lTADO COJEDES A XII CONFERENCIASANITARIA PANAMERICANA CUADERNOS AMARILLOS PUBLICACIONES DE !A COMlSlON ORGANIZADORA Geografía Médicosanitaria del Estado Cojedes con Especial Referencia al Paludismo Por el doctor RICARDOARCHILA encolaborac~ón con el Dr.MIGUEL NIETO EDLTORIAL GRAFOLIT CARACAS 1946 69 INDICE -BBg. Capítulo 1. Geografía Física .................. 6 Situación geográfica. Orografía.Hidrcgra- fía. Geología. Meteorología. Capitulo 11. GeografíaPolítica y Civil ............ 2% Poblaaión. Etnografía.Régimen Politico. Ciudades. Legislación Sanitaria.Rentas y Gastos Públicos. ServiciosPhblicos y Ser- vicios Médicos Sanitarios.Instrucción PG- blica. Capítulo 111. GeografíaEconómica ................ 88 Producciones Minerales. Agricultura. Gana- 'dería.Explotaciones Vegetales. Industrias. Comercio. Vías de Comunicación. Capítulo IV. GeografíaHumana ................ 117 Aspectos Sociológicos. Ruralización. Sala- rio. Alimentación. Vivienda. Migraciones. Prostitución. Cancubinato. Mendicidad. Re- ligiosidad. Consumo de tóxicos. Delitosde sangre. Educación física. Capítulo V. Demografía ...................... 143 Capítulo VI. Nosografía ...................... 161 Capítulo VII. Paludismo ...................... 172 Datos históricos. Mortalidad. La fauna ana- felina.Prevalencia parasitaria. Pndice es- plénico. Factoresfavorecedores de la en- demia palGdica. Lucha antimalárica. Apéndice .............................. 225 Movimientodemográfico ............ 227 Sistemade riego de San Carlos -
Memorial to Carlos Schubert 1938-1994 THO M a S W
Memorial to Carlos Schubert 1938-1994 THO M A S W. DONNELLY Dept, o f Geological Sciences, State University o f New York, Binghamton, NY 13902-6000 Friends of Carlos Schubert Paetow were shocked and saddened upon hearing of his death in Caracas, Venezuela, on July 22, 1994, following an aneurism and a mesenteric stroke. Carlos, a longtime Fellow of the Geological Society of America, was one of the dominant figures of Venezuelan geology, specializing in his later years in neotectonics and in Quaternary geology. His untimely passing leaves a large void in Latin American—and in Quaternary—geology. His publications were voluminous and spanned a wide range of topics, but dominantly centered in Venezuelan studies. Carlos was bom in Hamburg, Germany, on October 9, 1938, and went to Caracas as an infant. He had a youthful interest in many subjects, but not especially in geology. His decision to pursue this field was the result of parental advice that geology and chemistry were the major fields of the future. Because he was uncom fortable with chemistry, he chose geology. Undoubtedly one of his important inspirations was the German explorer Alexander von Humboldt. Indeed, one of Carlos’s most prized possessions was his German 1815 edition of Humboldt’s Travels. In much of Carlos’s later work we can find a thread linking him to the founder of South American earth science. When he completed his high school studies in Caracas in 1957, he faced the problem that Pérez Jiménez, the president of Venezuela, had closed all Venezuelan universities. Fortunately, Carlos was awarded a scholarship from the Shell Oil Company to attend the University of Arizona, where he received his bachelor’s degree in geology in 1961. -
Agencia Dirección Diferentes Procesos De Recaudación
AGENCIA DIRECCIÓN DIFERENTES PROCESOS DE RECAUDACIÓN LAS MERCEDES AV PPAL LAS MERCEDES CC CADA C/C RÍO DE JANEIRO URB.LAS MERC TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA LA FLORIDA DESINCORPORADA. DESDE 02-05-2002. BM CARTA 25-03-2002 TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA C.C. LIDER LA CALIFORNIA C.C. LIDER ,AV. FRANCISCO DE MIRANDA LA CALIF.NORTE TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA CONCRESA C.C. CONCRESA LOACL 121 PRADOS DEL ESTE TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA PARQUE CENTRAL AV. LECUNA EDIF. TACAGUA NIVEL LECUNA PARQUE CENTRAL TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA EDIF. ATRIUM, AV. TAMANACO CON AV. VENEZUELA Y SOROCAIMA, URB. EL ROSAL, ESTADO MIRANDA, EL ROSAL MUNICIPIO CHACAO, PARROQUIA CHACAO TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA GUARENAS C.C.TRPICHITO,LOCALES 52 AL 59 ,URB. TRAPICHITO TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA CHUAO C. BANAVEN E/ERNESTO BLOHN Y LA ESTANCIA , CHUAO TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA BELLO MONTE AV.PPAL. DE BELO MONTE C/SORBONA EDIF. TORRE FINANCIERA TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA EL BOSQUE AV. EL BOSQUE C/FRANCISCO DE MIRANDA C.C. UNICO ,CHACAITO TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA LA URBINA EDIF. QUINSA,E/CALLES 8 Y 9 ,LA URBINA TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA LOS TEQUES EDIF. DON CHICHI ,AV. BERMUDEZ C/ARISMENDI TODAS LAS FORMAS DE IMPUESTO (ISLR - IVA) EXCEPTO ADUANA LA GUAIRA EDIF. -
Venezuela Location Geography Food
Venezuela Location Venezuela, officially the Republic of Venezuela, is a republic (1995 est. pop. 21,005,000), 352,143 sq mi. (912,050 sq. km), in the northern part of South America. With the Caribbean Sea in the north, Venezuela has a coastline of 1,750 long. It is bordered on the south by Brazil, on the west and southwest by Colombia, and on the east by Guyana. Dependencies include Margarita Island, Tortuga Island, and many smaller island groups in the Caribbean. Caracas is the capital and also the largest city in Venezuela. Geography Venezuela, a third larger than Texas, occupies most of the northern coast of South America on the Caribbean Sea. Mountain systems break Venezuela into four distinct areas: (1) the Maracaibo lowlands; (2) the mountainous region in the north and northwest; (3) the Orinoco basin, with the llanos (vast grass-covered plains) on its northern border and great forest areas in the south and southeast, and (4) the Guiana Highlands, south of the Orinoco, accounting for nearly half the national territory. Food The food in Venezuela is generally easy and flavorful. Caracas, the capital of Venezuela, claims to have a greater variety of restaurants than any other South American city, and it would certainly be a pleasure to try and prove it, even if you failed. Venezuelan cooking has European, indigenous, and African roots – a heterodox cuisine formed over the centuries by immigrants. Some of the native dishes include: Page 1 of 7 - Pabellon - stewed and shredded meat accompanied by rice, black beans, and baban -Hallaca - a traditional Christmas dish. -
FRESH-WATER SHRIMPS (CRUSTACEA, DECAPODA, NATANTIA) of the ORINOCO BASIN and the VENEZUELAN GUAYANA Gilberto Rodriguez the Guaya
JOURNAL OF CRUSTACEAN BIOLOGY, 2(3): 378-391, 1982 FRESH-WATER SHRIMPS (CRUSTACEA, DECAPODA, NATANTIA) OF THE ORINOCO BASIN AND THE VENEZUELAN GUAYANA Gilberto Rodriguez ABSTRACT Shrimps of the families Sergestidae and Palaemonidae collected in the Orinoco basin, the upper Cuyuni River, and the upper and lower Rio Negro, are dealt with in this paper. New records and comments are given for Acetes paraguayensis, Macrobrachium amazonicum, M. brasiliense, M. jelskii, M. nattered, M. surinamicum, and Palaemonetes carteri. Two new palaemonids are described: Macrobrachium cortezi, a form related to M. nattereri, from several localities in the Orinoco River and upper Rio Negro, and M. aracamuni, from an altitude of 680 m in the Cerro Aracamuni in the drainage area of the upper Rio Negro. Another previously undescribed species of Macrobrachium is recorded but not named due to the lack of mature males. The Guayana highland is an ancient land mass extending from the Amazon River to the Atlantic coast of South America and includes the Guianas and parts of Venezuela and Brazil. The Venezuelan Guayana comprises 41,300 km2 of territory, mostly above 400 m that separate the Orinoco from the Amazon basin and forms a formidable barrier to the dispersion of the fresh-water fauna of the lowlands. The hydrology of the zone is defined by the Orinoco River that bounds the area to the west and north and its tributaries that generally flow north or northwesterly. A smaller portion to the east is drained by the Cuyuni River. The Orinoco and the Amazon basins are connected through the Brazo Casiquiare, while the inundated savannah of Rupununi allows intermittent connections be tween the Branco and the Esequibo Rivers (Lowe-McConnell, 1964). -
Evaluación Paleosísmica Del Segmento San Felipe De La
Boletín de Geología ISSN: 0120-0283 [email protected] Universidad Industrial de Santander Colombia Audemard M., Franck A. EVALUACIÓN PALEOSÍSMICA DEL SEGMENTO SAN FELIPE DE LA FALLA DE BOCONÓ (VENEZUELA NOROCCIDENTAL): ¿RESPONSABLE DEL TERREMOTO DEL 26 DE MARZO DE 1812? Boletín de Geología, vol. 38, núm. 1, enero-abril, 2016, pp. 125-149 Universidad Industrial de Santander Bucaramanga, Colombia Disponible en: http://www.redalyc.org/articulo.oa?id=349643441011 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Boletín de Geología ISSN: 0120-0283 Vol. 38, N° 1, enero-abril de 2016 URL: boletindegeologia.uis.edu.co EVALUACIÓN PALEOSÍSMICA DEL SEGMENTO SAN FELIPE DE LA FALLA DE BOCONÓ (VENEZUELA NOROCCIDENTAL): ¿RESPONSABLE DEL TERREMOTO DEL 26 DE MARZO DE 1812? Franck A. Audemard M. 1, 2 DOI: http://dx.doi.org/10.18273/revbol.v38n1-2016007 Forma de citar: Audemard, F.A. 2016. Evaluación paleosísmica del segmento San Felipe de la Falla de Boconó (Venezuela noroccidental): ¿responsable del terremoto del 26 de marzo de 1812?. Boletín de Geología, 38 (1): 125-149. RESUMEN La Falla de Boconó (FB), estructura mayor de la frontera transpresiva entre las placas Caribe y Suramérica, presenta claras evidencias geomórficas diagnósticas de transcurrencia dextral cuaternaria en su sector más -
The Question of the Legal Regularization of Urban Barrios in Venezuela
The Question of the Legal Regularization of Urban Barrios in Venezuela Teolinda Bolívar Barreto, Teresa Ontiveros and Julio de Freitas Taylor © 2000 Lincoln Institute of Land Policy Lincoln Institute of Land Policy Working Paper The findings and conclusions of this paper are not subject to detailed review and do not necessarily reflect the official views and policies of the Lincoln Institute of Land Policy. Please do not photocopy without permission of the Institute. Contact the Institute directly with all questions or requests for permission. ([email protected]) _ Lincoln Institute Product Code: WP07TB1 Abstract This article records the work pursued in the wake of an enlightening conference in October 1998 in Barquisimeto, Venezuela. Bidding farewell to a Brazilian researcher after the congress, it occurred to us to seek answers to a key question regarding the legal regularization of the urban barrios in Venezuela: Why has it not taken place? Among the answers found by interviewing social actors who participate in the production of barrios were the existence, acceptance, and reproduction of legally precarious but stable possession. Certain evident causes serve to obscure other causes that may be key to understanding this question (Parts Two and Three). About the Authors Teolinda Bolívar is a professor in the Faculty of Architecture and Urban Studies (Facultad de Arquitectura y Urbanismo - FAU) at the Universidad Central de Venezuela (UCV). She is the coordinator of the research group The Production of Urban Barrios (La Producción de los Barrios Urbanos) at the FAU-UCV School of Architecture. She got her doctorate in Urban Studies at Paris XII. -
The Venezuelan Hydrocarbon Habitat, Part 1: Tectonics, Structure, Palaeogeography and Source Rocks
Journal of Petroleum Geology, vo1.23(1), January 2000, pp 5-53. 5 THE VENEZUELAN HYDROCARBON HABITAT, PART 1: TECTONICS, STRUCTURE, PALAEOGEOGRAPHY AND SOURCE ROCKS K. H. James* Venezuela forms part of an important hydrocarbon province, defined by the presence of prolific Cretaceous source rocks, which extends across northern South America. By early 1997, the country had produced 53 billion barrels of oil. Reserves are estimated to total 73 billion barrels of oil and 146 TCF of gas with 250 billion barrels recoverable in the Heavy Oil Belt. Most reserves are located within the intermontane Maracaibo and foreland Barinas-Apure and Eastern Venezuela BasinxThey correspond to more than 1.5 trillion BOE originally in place. The province S hydrocarbon history began with a broad passive margin over which the sea transgressed throughout much ofthe Cretaceous. Limestones and shales followed basal sands and included rich source rocks. Convergence between the distal part of the area and the Caribbean Plate created an active margin that migrated southwards, so that flysch and wildflysch followed the transgressive facies. The process culminated in Lute Cretaceous to Middle Eocene orogeny with the emplacement of southward-vergent nappes and the development of northward-deepeningforedeeps. Flysch and wildflysch formed in the north while important deltaic - paralic reservoir sands accumulated in the south. Major phases of hydrocarbon generationfrom Jurassic-Cretaceoussource rocks occurred across the entire margin of northern South America during the orogeny. They are recorded by Jurassic - Middle Cretaceous graphitic marbles, schists and quartzites (metamorphosed, organic limestones and shales and oil-bearing sandstones) in the Coastal and Northern Ranges of Venezuela and Trinidad. -
Tetonic Inheritance and Structural Styles in the Merida
Third ISAG, St Malo (France), 17-19/9/1996 TECTONIC INHERITANCE AND STRUCTURAL STYLES IN THE MERIDA ANDES (WESTERN VENEZUELA). Bernard COLLETTA( l ) , Franqois ROURE( l) Bruno DE TONI(~),Daniel LOLTREIRO(~)Herminio PASSALACQUA(~)~~~Yves GOU(~). (I hnstitut Franqais du PCtrole, BP3 1 1, 92506 Rueil-Malmaison, France (2)~ntevep,Apartado 76343, Caracas 1070-A, Venezuela (3)~eicipFranlab, 92506 Rueil-Malmaison, France KEY WORDS: Venezuela, Merida Andes, tectonic inversion, crustal scale balanced sections INTRODUCTION Unlike the adjacent Caribbean and Central Andean orogens, the Merida Andes (Fig. 1) do not relate to direct interactions between the South American craton and either arc terranes or oceanic domains, but represent only minor intraplate readjustements between the Eastern Cordillera in the south and the South Caribbean transform margin in the north.Although no deep seismic profiling has yet been attempted across the Venezuelan Andes, a large set of conventional seismic reflection profiles has been recorded by the petroleum industry in the Maracaibo and Barinas-Apure basins, respectively along the North and South Andean foothills. In addition, isolated refraction and magnetotelluric data are available. However, only the gravimetric coverage is really complete, thus providing a relatively coherent image of the basement architecture. STRUCTURE OF THE SOUTH ANDEAN FLANK The Barinas-Apure basin extends from the Andean foothills in the northwest to the Guyana shield in the southeast, thus encompassing most of the drainage area of the Rio Apure, a tributary of the Orinoco River. Southwards, it connects directly with the Llanos basin in Colombia. The Barinas basin hardly compares with a flexural basin. It is largely dominated by either north- or south-verging basement- involved structures. -
Late Quaternary Deglacial History of the Mérida Andes, Venezuela
JOURNAL OF QUATERNARY SCIENCE (in press) Copyright ß 2007 John Wiley & Sons, Ltd. Published online in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/jqs.1109 Correspondence the terminal and lateral moraines of the El Caballo and Reply: Late Quaternary deglacial La Mucuchache glaciers. A chemically untreated organic history of the Me´rida Andes, sample from 1.5 m above the base of the section yielded a conventional age of 22 750 cal. yr BP (19 000 14C yr BP), Venezuela: response whereas a peat sample immediately below the top of the section yielded an age of 19 960 cal. yr BP (16 500 14C yr BP). to comment We recognise that other workers (e.g. Mahaney et al., 2001, 2004; Dirszowsky et al., 2005) have re-analysed the Pedregal fan complex. For example, the sedimentology was described in detail by Dirszowsky et al. (2005). However, the chronology in We welcome the opportunity to respond to Mahaney et al.’s these papers is questionable and not useful for constraining the critique of our article on the deglacial history of the LGM. All of the recently published dates are on refractory Venezuelan Andes (Stansell et al., 2005). The source of our organic matter isolated using a cellulose extraction technique disagreement appears to stem primarily from differences in which concentrates refractory carbon, resulting in ages research strategies and methodology. Our work in the between 47 000 and 60 000 14C yr BP. These ages include mul- Venezuelan Andes employs lake sediment archives that record tiple reversals and are at the very edge of interpretability as continuous sedimentary sequences and can be dated using finite radiocarbon ages; nonetheless, the authors have inter- accelerator mass spectrometry (AMS) radiocarbon dating of preted them as valid ages. -
El Poblamiento Prehispánico De La Cordillera Andina De Mérida-Venezuela Boletín Antropológico, Vol
Boletín Antropológico ISSN: 1325-2610 [email protected] Universidad de los Andes Venezuela Gordones Rojas, Gladys; Meneses Pacheco, Lino El poblamiento prehispánico de la Cordillera Andina de Mérida-Venezuela Boletín Antropológico, vol. 22, núm. 60, enero-abril, 2004, pp. 37-71 Universidad de los Andes Mérida, Venezuela Disponible en: http://www.redalyc.org/articulo.oa?id=71206002 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Boletín Antropológico. Año 22, Nº 60, Enero-Abril 2004, ISSN: 1325-2610. Universidad de Los Andes. Mérida. Gladys Gordones y Lino Meneses. El poblamiento prehispánico de la Cordillera ... pp. 37-71. El poblamiento prehispánico de la Cordillera Andina de Mérida-Venezuela1 Gladys Gordones Rojas2 Lino Meneses Pacheco3 Resumen: En el artículo se exponen las propuestas que elaboraron en distintas épocas diversos/as intelectuales venezolanos/as en torno al origen étnico de los antiguos habitantes de la cordillera andina de Mérida-Venezuela para proponer, a partir de las evidencias arqueológicas y de los toponímicos y antroponímicos presentes en los documentos de los siglos XVI y XVII, un nuevo modelo que explique el poblamiento y el origen étnico de los habitantes prehispánicos de Los Andes merideños. Palabras Claves: Arqueología, Cordillera andina de Mérida, toponímicos, antroponímicos Abstract: The article presents the propositions that venezuelan intellectuals of different times have elaborated concerning the ethnic origin of the ancient people of the Andes Cordillera of Merida, Venezuela. -
Andean Venezuelan
Venezuelan Andean Spanish Intonation Venezuelan Andean Spanish Intonation* Lluïsa Astruca, Elsa Morab and Simon Rewc The Open University and The University of Cambridgea Universidad de Los Andesb The University of Cambridgec 1. Introduction Lying in western Venezuela, the state of Mérida is traversed by the eastern branch of the northern Andes and has an area of 11,300 km2, which corresponds to approximately 1.2% of the national territory. The main economic activities of the region are agriculture and tourism. The city of Mérida itself has 300,000 inhabitants (2001 census) and constitutes a national cultural and university centre. The Universidad de Los Andes is a major source of employment in the region, specifically in the areas of teaching, research and services. The structure of this chapter is as follows. Section 1 first offers an overview of past intonational research in Venezuelan Spanish and especially in Venezuelan Andean Spanish and then describes the methodological procedure used in the present study. Section 2 presents an inventory of pitch accents and boundary tones found in the Mérida dialect. Section 3 analyses the basic intonation contours found in the Mérida corpus. Finally, Section 4 summarises the nuclear patterns in the different sentence types. The study of intonation does not have a long history in Venezuela and, furthermore, the rather scant research has been mostly oriented towards dialectology. The first study of the intonation of Venezuelan Spanish was published in the phonetics section of El habla de Caracas (Mosonyi 1971). A decade later, Obregón (1981) carried out a dialectal study in which he analysed the distribution of certain characteristic patterns (which he called construcciones entonativas) and which led him to propose a division into five dialectal areas: Mérida and Táchira (southwest), Maracaibo (northwest), Nueva Esparta and Sucre (east), Apure and Guárico (south) and the rest of the country (centre).