Conservación Marina En El Sur De Chile Marine Conservation in Southern Chile
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ISJ-10-1-Hidalgo-Et-Al.Pdf
Island Studies Journal, Vol. 10, No. 1, 2015, pp. 49-70 Affordance of landscapes and economic socio-spatial networks in the Quinchao archipelago, Chile: a contribution to landscape research and island studies. Carlos Hidalgo Universidad de los Lagos, Chile [email protected] Francisco Ther Universidad de los Lagos, Chile [email protected] Gonzalo Saavedra Universidad Austral, Chile [email protected] and Asunción Díaz Universidad de los Lagos, Chile [email protected] ABSTRACT : This article presents research which analyzes landscape transformation, using an interdisciplinary approach embedded in an archipelagic context. The investigation unfolds in Quinchao, a cluster of ten islands of the Quinchao Department, Chiloé archipelago, Región de Los Lagos, Chile. The investigation gathers reflections from such disciplines as anthropology, geography, biology and psychology which share similar reflections on the configuration of landscapes as an affordance or enabled property of the human-in-ecosystem assemblage. Ethnographic interpretations and Social Network Analysis of fieldwork data are used to propose a theoretical framework for the investigation of coastal and marine landscapes in archipelagic contexts. Keywords : archipelago, affordance, Chiloé, dwelling, island studies, landscapes, Quinchao, socio-ecological system © 2015 – Institute of Island Studies, University of Prince Edward Island, Canada Introduction: Global-local intersections and island studies In recent years, some debate has emerged around the idea of ‘archipelagic thinking’ in island studies scholarship. Island studies, or nissology (Baldacchino, 2008; Depraetere, 1991), has advocated an inquiry into islands “on their own terms” (McCall, 1994, p. 6) and, regardless of the rich philosophical and political contributions it has made, debates on the nature of islands and island life, colonialism and other related topics have not quite been able to efficiently address theoretical and methodological challenges that we were warned about by Baldacchino (2008). -
The Crustacea Anomura of Chile
LUNDS UNIVERSITETS ARSSKRIFT. N. F. Avd. 2. Bd 51. Nr 12. KUNGL. FYSIOGRAFISKA SALLSKAPETS HANDLINGAR. N. F. Bd 66. Nr 12. (CONTRIBUTION NO. 158 FROM THE ALLAN HANCOCK FOUNDATION) REPORTS OF THE LUND UNIVERSITY CHILE EXPEDITION 1948—49 20. THE CRUSTACEA ANOMURA OF CHILE BY JANET HAIG ALLAN HANCOCK FOUNDATION, UNIVERSITY OF SOUTHERN CAL1FOBNIA, LOS ANGELES CON RESUMEN EN ESPANOL LUND C. W. K. GLEERUP Read before the Royal Physiographic Society, June 2, 1954. LUND H A K A N OIIL S S O N S BOKTI1Y CK E K 1 19 5 5 Introduction The Crustacea Anomura collected by the Lund University Chile Expedition in 1948—49 form the basis of this report. The Expedition's collections include nearly 1400 specimens of Anomura from Chile, comprising a total of twenty-four species. This is the largest number of species ever taken ha this region by a single expedition. L. H. PLATE'S extensive collections of Crustacea from Chile, which were reported on hi 1902 by LENZ, included twenty anomuran forms. NICOLET (1849) listed twenty-one Anomura from Chile, but not all of these stand today as good species. Although numerous collections have been made and the literature on these crabs is extensive, no account of all the Crustacea of Chile has appeared since the time of NICOLET; furthermore, much of the work on the group is found in obscure or hard-to- obtain publications. It was thought advisable, therefore, to expand the scoj>e of this report to include all the Crustacea Anomura which have been reported from Chile. -
Principales Ríos De Chile. Hidrografía
Principales Ríos de Chile. Hidrografía. La hidrografía de Chile es distinta a lo largo del país, esto se debe a los distintos climas y relieves de cada zona: Norte Grande: De aquí se puede destacar el Río Loa que es el río más largo de Chile mide 440 Km. de largo. Norte Chico: La mayoría de los ríos de esta zona desembocan en el mar, es decir son exorreicos, provienen de la nieve de la zona andina. Río Elquí. Río Limarí Zona Central: En esta zona los ríos desembocan en el mar aunque a medida que se acercan al mar aumentan su caudal, especialmente en los meses de verano, ya que al subir la temperatura se derrite la nieve y se distribuye en ríos. En invierno también aumentan su caudal considerablemente pero esto se debe a las precipitaciones El río más destacable de esta zona es el río Biobío cuyo caudal medio es de 899m3 Zona Sur: en la zona sur los ríos son más pluviales que nivales, es decir que provienen de la nieve. Son menos torrentosos debido a que no tienen tanta pendiente como más al norte, por lo que son más navegables. Se pueden destacar grandes lagos y ríos como el río Valdivia. Aquí se puede observar una persona navegando en canoa por el río Valdivia Río Valdivia Zona Oceánica: En esta zona del país las precipitaciones provocan los cursos de agua, por lo que se le denominan intermitentes. Zona Austral y Antártica de Chile: Los ríos de esta zona son de gran caudal, son originados por los deshielos de las nieves, nacen de la vertiente oriental de los andes. -
Lahuén Ñadi ‡ 114 ‡ Monumentos Naturales De Chile
09.- ‡ Lahuén Ñadi ‡ 114 ‡ Monumentos Naturales de Chile Helecho película (hymenophyllum pectinatum). Lahuén Ñadi ‡ 115 Natural Monument (NM) Declaration Date: January 10, 2000. Fecha de creación como Monumento Natural (MN): 10 de enero del año 2000. Location: Region X of The Lakes, Llanquihue Province, Puerto Montt County. Ubicación: X Región de los Lagos, provincia de Llanquihue, comuna de Puerto Montt. Surface area: 200 hectares1. Superficie: 200 hectáreas1. Motive for conservation: It is a small relic of an old-growth forest, representative of the temperate rainforests that Motivo de conservación: Es un pequeño bosque relicto, covered the entirety of the intermediate depression of Chile representativo de los bosques húmedos templados de la prior to the European colonization period, particularly zona sur de Chile que cubrían la depresión intermedia de la the German colonization that took place during the 19th región antes de la colonización europea, particularmente century. The forest contains alerce trees that are over 1,800 alemana, durante el siglo XIX. Destacan los alerces, algunos years old. Old-growth alerce trees are nearly extinct, con hasta 1.800 años de edad. Esta especie casi se extinguió, but continue to exist in protected areas like this. y hoy sólo sobrevive gracias a áreas protegidas como ésta. 1 www.conaf.cl Reviewed July 3, 2012. 1 www.conaf.cl Revisado 3-7-2012 116 ‡ Monumentos Naturales de Chile Lahuén Ñadi ‡ 117 118 ‡ Monumentos Naturales de Chile Dosel de alerces. Name origin: The name derives from the indigenous Mapudungún Origen del nombre: Proviene del mapudungún, lengua language, spoken by the Huilliche people who used to inhabit utilizada por los huilliches que habitaban la zona. -
Geology of the Caspiche Porphyry Gold-Copper Deposit, Maricunga Belt, Northern Chile*
©2013 Society of Economic Geologists, Inc. Economic Geology, v. 108, pp. 585–604 Geology of the Caspiche Porphyry Gold-Copper Deposit, Maricunga Belt, Northern Chile* RICHARD H. SILLITOE,1,† JUSTIN TOLMAN,2,** AND GLEN VAN KERKVOORT3,*** 1 27 West Hill Park, Highgate Village, London N6 6ND, England 2 Exeter Resource Corporation, Suite 1660 - 999 W. Hastings St., Vancouver, BC V6C 2W2, Canada 3 Exeter Resource Corporation, Suite 701, 121 Walker St., North Sydney, NSW 2060, Australia Abstract The Caspiche porphyry gold-copper deposit, part of the Maricunga gold-silver-copper belt of northern Chile, was discovered in 2007 beneath postmineral cover by the third company to explore the property over a 21-year period. This company, Exeter Resource Corporation, has announced a proven and probable mineral reserve of 1,091 million tonnes (Mt) averaging 0.55 g/t Au, all but 124 Mt of which also contain 0.23% Cu, for a total of 19.3 Moz of contained gold and 2.1 Mt of copper. The deposit was formed in the latest Oligocene (~25 Ma) during the first of two volcanic and corre- sponding metallogenic epochs that define the Maricunga belt. The gold-copper mineralization is centered on a composite diorite to quartz diorite porphyry stock, within which five outward-younging phases are rou- tinely distinguished. The centrally located, early diorite porphyry (phase 1) hosts the highest-grade ore, av- eraging ~1 g/t Au and 0.4% Cu. The subsequent porphyry phases are quartz dioritic in composition and char- acterized by progressively lower gold and copper tenors. Stock emplacement was both pre- and postdated by the generation of large-volume, andesite-dominated breccias, with tuffaceous matrices, which are be- lieved to be shallow portions of diatremes. -
Brochure Route-Of-Parks EN.Pdf
ROUTE OF PARKS OF CHILEAN PATAGONIA The Route of Parks of Chilean Patagonia is one of the last wild places on earth. The Route’s 17 National Parks span the entire south of Chile, from Puerto Montt all the way down to Cape Horn. Aside from offering travelers what is perhaps the world’s most scenic journey, the Route has also helped revitalize more than 60 local communities through conservation-centered tourism. This 1,740-mile Route spans a full third of Chile. Its ecological value is underscored by the number of endemic species and the rich biodiversity of its temperate rainforests, sub-Antarctic climates, wetlands, towering massifs, icefields, and its spectacular fjord system–the largest in the world. The Route’s pristine ecosystems, largely untouched by human intervention, capture three times more carbon per acre than the Amazon. They’re also home to endangered species like the Huemul (South Andean Deer) and Darwin’s Frog. The Route of Parks is born of a vision of conservation that seeks to balance the protection of the natural world with human economic development. This vision emphasizes the importance of conserving and restoring complete ecosystems, which are sources of pride, prosperity, and belonging for the people who live in and near them. It’s a unique opportunity to reverse the extinction crisis and climate chaos currently ravaging our planet–and to provide a hopeful, harmonious model of a different way forward. 1 ALERCE ANDINO National Park This park, declared a National Biosphere Reserve of Temperate Rainforests, features 97,000 acres of evergreen rainforest. -
Baseline Study on Marine Debris and Municipal Waste Management in Chiloé-Corcovado, Southern Chile
BASELINE STUDY ON MARINE DEBRIS AND MUNICIPAL WASTE MANAGEMENT IN CHILOÉ-CORCOVADO, SOUTHERN CHILE Master Thesis Master of Sciences in Regional Development Planning and Management SPRING HORSTMANN, Johannes VALDIVIA, CHILE July 2007 DECLARATION OF THE AUTHOR BASELINE STUDY ON MARINE DEBRIS AND MUNICIPAL WASTE MANAGEMENT IN CHILOÉ-CORCOVADO, SOUTHERN CHILE by HORSTMANN, Johannes This thesis was submitted to the Faculty of Economic and Administrative Sciences in partial compliance of the requirements to obtain the academic degree “Master of Sciences in Regional Development Planning and Management” jointly offered by University Austral de Chile in Valdivia and the Faculty of Spatial Planning, University of Dortmund/Germany, in the 2-years post-graduate study programme “Spatial Planning for Regions in Growing Economies (SPRING)”. The author declares to have elaborated the present research solely by his own efforts and means. All information taken from external sources is marked accordingly. ------------------------------ Johannes Horstmann Valdivia, Chile 02-July-2007 ii MASTER THESIS APPROVAL REPORT The Thesis Assessment Committee communicates to the Graduate School Director of the Faculty of Economic and Administrative Sciences that the Master Thesis presented by the candidate HORSTMANN, Johannes has been approved in the Thesis defense examination taken on 10th of July 2007, as a requirement to opt for M.Sc. Regional Development Planning and Management Degree. Sponsor Professor _________________________ Professor Rodrigo Hucke-Gaete Assessment Committee ________________________ Professor Manfred Max-Neef ________________________ Dr. Christoph Kohlmeyer _________________________ Ing. Maria Luisa Keim Knabe iii ACKNOLEDGEMENTS “Gracias a la vida, que me ha dado tanto…” I want to express my love and gratefulness to my parents who gave life to me and my sisters. -
Antecedentes Históricos Del Conflicto Territorial En El Sur De Chile
Antecedentes históricos del conflicto territorial en el sur de Chile Al momento de la Independencia de Chile, el pueblo mapuche gozaba de autonomía territorial al sur del río Biobío, frontera que había sido establecida tras sucesivas negociaciones con la Corona española durante la Colonia. Esta situación no se alteró mayormente, sino hasta el comienzo de la segunda mitad del siglo XIX. Primero por la ocupación no violenta de inmigrantes chilenos, y luego por la invasión militar del territorio por parte el Ejército chileno. Una vez conquistado el territorio, el Gobierno comenzó el proceso de radicación (1883-1929), que consistía en determinar las tierras que estaban ocupadas por indígenas y otorgarles títulos de merced, para luego disponer del restante. Este es el origen de lo que hoy se conoce como las “tierras antiguas”. En forma paralela a la radicación, se dio el fenómeno de la usurpación de tierras, mediante el cual, personas no mapuche, e incluso el propio Estado, se fueron apropiando por medios ilegítimos de tierras contenidas en los títulos de merced. Este es el origen de las llamadas “tierras usurpadas”. Con la Reforma Agraria, particularmente bajo el gobierno de Salvador Allende, los mapuches lograron recuperar buena parte de las tierras reivindicadas. Sin embargo, la dictadura militar retrotrajo la situación a su estado anterior. Este es el origen de las “tierras de la Reforma Agraria”. Por otro lado, el gobierno militar fomentó intensa y directamente la industria forestal, con el resultado de su concentración en la zona mapuche. Su ubicación y efectos ecosistémicos, constituye el principal foco del conflicto territorial en la actualidad. -
Cnidaria, Hydrozoa: Latitudinal Distribution of Hydroids Along the Fjords Region of Southern Chile, with Notes on the World Distribution of Some Species
Check List 3(4): 308–320, 2007. ISSN: 1809-127X NOTES ON GEOGRAPHIC DISTRIBUTION Cnidaria, Hydrozoa: latitudinal distribution of hydroids along the fjords region of southern Chile, with notes on the world distribution of some species. Horia R. Galea 1 Verena Häussermann 1, 2 Günter Försterra 1, 2 1 Huinay Scientific Field Station. Casilla 462. Puerto Montt, Chile. E-mail: [email protected] 2 Universidad Austral de Chile, Campus Isla Teja. Avenida Inés de Haverbeck 9, 11 y 13. Casilla 467. Valdivia, Chile. The coast of continental Chile extends over and Cape Horn. Viviani (1979) and Pickard almost 4,200 km and covers a large part of the (1971) subdivided the Magellanic Province into southeast Pacific. While the coastline between three regions: the Northern Patagonian Zone, from Arica (18°20' S) and Chiloé Island (ca. 41°30' S) Puerto Montt to the Peninsula Taitao (ca. 46°–47° is more or less straight, the region between Puerto S), the Central Patagonian Zone to the Straits of Montt (ca. 41°30' S) and Cape Horn (ca. 56° S) is Magellan (ca. 52°–53° S), and the Southern highly structured and presents a large number of Patagonian Zone south of the Straits of Magellan. islands, channels and fjords. This extension is A recent study, including a wide set of formed by two parallel mountain ranges, the high invertebrates from the intertidal to 100 m depth Andes on Chile’s eastern border, and the coastal (Lancellotti and Vasquez 1999), negates the mountains along its western edge which, in the widely assumed faunal break at 42° S, and area of Puerto Montt, drop into the ocean with proposes a Transitional Temperate Region between their summits, forming the western channels and 35° and 48° S, where a gradual but important islands, while the Andes mountain range change in the species composition occurs. -
Finding More Missing Pieces of a Puzzle in a Maze
FINDING MORE MISSING PIECES OF A PUZZLE IN A MAZE continuing the benthic exploration of channels and fjords in Southern Chilean Patagonia As an intricate system of fjords, labyrinth of channels and islands, each exemplifying different stages of glacial action and associated successional periglacial ecosystems, the Chilean fjord region offers extremely diversified benthic communities which, despite being unique worldwide, have been among the least studied so far. This region is threatened by different anthropogenic effects, such as global warming, the huge salmon farming industry planning to move into currently unprotected fjords, or illegal fishing of protected shellfish species such as ʻlocosʼ (Concholepas concholepas). In order to protect benthic fauna and monitor future changes in biodiversity distribution, it is essential to create accurate faunistic inventories. This is why we initiated a series of scientific expeditions, beginning in 2005. The first one lead us to the Guaitecas Archipelago, south of Grand Chiloé Island. The second took us to the fjords Tempano and Bernardo, including adjacent channels down to 49°S (see GME3, pp. 18–21). Enriched by our 2005 experience, we embarked in 2006 for another adventurous boat trip further south to 52°S. Our international team (seven in total) started Sample sorting through the night. gathering in Punta Arenas at the beginning of March, end of headed north through the channels along Puerto Eden as the austral summer. Some arrived directly from the Huinay well as around Isla Wellington to explore the exposed coast. Scientific Field Station, others from Germany and Belgium. We planned 2 dives/day, leaving about 9 hours of A 3 hour bus trip lead us to Puerto Natales, our departure navigation/day for the two week expedition. -
Alacalufe Oct.2018 Ok.Fh11
GLACIERS IN THE CHILEAN PATAGONIA... A DREAMING DESTINATION CHILE SPECIAL CRUISE ON BOARD M/V SKORPIOS III NOMADS OF PATAGONIA ROUTE PUERTO MONTT • PUERTO NATALES 7 NIGHTS / 8 DAYS Skorpios offers you the unique experience of a Special Cruise on board M/V Skorpios III through the Northern and Southern Icefields, sailing through fjords and channels, getting to know remote fishermen villages such as Puerto Aguirre and Puerto Edén, enjoying the Quitralco Hotsprings and visiting Bernardo, Pío XI, Amalia, El Brujo and Bernal Glaciers. From USD 3,000 Rate per passenger • Athens deck • Double occupancy SET SAIL: SUNDAY 06 - DISEMBARKATION SUNDAY 13 OCTOBER 2019 INFORMATIONS AND RESERVATIONS, PLEASE CALL Itinerary Places Rates Images Augusto Leguía Norte 118, Las Condes, Santiago, Chile • E-mail: [email protected] - www.skorpios.cl NOMADS OF PATAGONIA ROUTE, A SPECIAL CRUISE ON OCTOBER 2019, M/V SKORPIOS III NAVIGATION PROGRAM SATURDAY OCTOBER 5, 2019. Optional additional night in M/V Skorpios III previous to TRACK OF NAVIGATION the sailing. (Additional costs). Check-in from 18:00hrs onwards. Additional night includes accommodation in the booked cabin, dinner and breakfast-buffet (sail day). SUNDAY OCTOBER 6, 2019 12:00hrs. Set sail from Puerto Montt, through Tenglo Channel, Llanquihue Archipelago, sight of Calbuco village and crossing of Ancud Gulf. 17:00hrs. Navigation Chiloé Archipelago, Mechuque, Chauques, Caguache, Tranqui islands. Crossing of Corcovado Gulf. MONDAY OCTOBER 7, 2019 07:00hrs. Sailing through Moraleda Channel. 08:30hrs. Arrival to Puerto Aguirre Village in the Guaitecas Archipelago, visit to this picturesque fishermen village. 10:30hrs. Sailing through Ferronave, Pilcomayo, Paso Casma and Canal Costa channels, arriving at Quitralco Fjord at 15:00hrs. -
RESEÑA DE LA VEGETACIÓN DE CHILE SERVICIO AGRÍCOLA Y GANADERO División De Protección De Los Recursos Naturales Renovables Subdepto
RESEÑA DE LA VEGETACIÓN DE CHILE SERVICIO AGRÍCOLA Y GANADERO División de Protección de los Recursos Naturales Renovables Subdepto. de Vida Silvestre Autor: Miguel Angel Trivelli Jolly Zona Norte: Vista de un sector de la región altiplánica de la Región de Tarapacá. Zona Norte: Vista de un sector, próximo a la zona costera de la Región de Atacama, con matorrales pequeños y herbáceas (añañucas). Zona Central: Vista de la región de la vegetación esclerófila, en un sector de la Región Metropolitana. Zona Sur: Vista de los bosques que integran las pluviselvas del sur de Chile. 1 INTRODUCCIÓN El presente trabajo tiene como objetivo, contribuir al conocimiento general de la vegetación chilena y de cómo ésta se distribuye en nuestro territorio. La información que se entrega está basada en numerosos trabajos científicos, como también, en el conocimiento generado por el autor. Cabe destacar, que los sistemas de clasificación de la vegetación chilena son diversos y dependen de los distintos autores. Al respecto, cabe mencionar las clasificaciones de Schmithüsen (1956), Veblen y Schlegel (1982) y Gajardo (1994). Por esta razón, no es de extrañarse que existan diferencias en cómo se clasifica la vegetación chilena, sin que esto quiera decir que existan errores en cada una de ellas, sino que corresponden a diferentes puntos de vista. El contenido del presente documento está basado en los autores anteriormente descritos, procurando resumir la información, sobre la vegetación chilena, en un documento que sea de fácil entendimiento y comprensión por todo lector que tenga la inquietud por aprender acerca de una parte importante de nuestros ecosistemas y recursos naturales.