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The Foreign Service Journal, January 1924 (American Consular Bulletin)
AMERICAN Photo Veiga Magellan Monument and Plaza, Punta Arenas, the Southernmost City of the World January, 1924 i^r 11 iii y i ii 11 ii 1111111 ii 11 ii 11111111111111 ii 11111111111111 ii 11 it 1111111 ii 1111 ii 11 ii 11 ii 111 ■ 111111 ii 111 n 11 ii 111111 ill i ii 11111 mi 11 ii 11 ill 11 M 11 iiii THE STANDARD OF VALUE The American Dollar is the Standard of Value all over the World. Regardless of where you are located, you should maintain a banking connection with Washington, D. C. WHY NOT SELECT THE FEDERAL-AM ERIC AN? Foreign Exchange, Letters of Credit, Travelers Checks, Commercial, Savings and Trust Departments, and $14,000,000.00 in assets, assure you of adequate facilities to transact any financial business you may require. Our officers are always glad to advise upon financial matters. FEDERAL-AMERICAN NATIONAL BANK WASHINGTON, D. C. W. T.fGALLIHER, JOHN POOLE, Chairman of the Board President 5iiiiimiiimimimiiimiiiiimiiiiiiiiiiimimiHiiiiiiiMiiiiiiimiiMmimimiiii!imMMimMiiiiiiiimiiiiiiMMiiiiimiiiiiin Press of RansdeU Incorporated Washington, D. C. vmp) •• «• P ox CON sue LLETIN W 1 PUBLISHED MONTHLY BY THE AMERICAN CONSULAR ASSOCIATION VOL. VI. No. I WASHINGTON, D. C. JANUARY, 1924 The United States Tariff Commission Its Work and Functions in Relation to Commerce By JOHN R. TURNER, Chief Economist, United States Tariff Commission [The writer, although a member of the staff of the United States Tariff Commission, personally assumes full responsibility for all the statements contained in this article.] SELF-INTEREST is a guiding motive maxim of public policy that one party to a in all business conduct, in all the pur¬ trade must get cheated, that to the extent suits of wealth. -
Magmatic Evolution of the Nevado Del Ruiz Volcano, Central Cordillera, Colombia Minera1 Chemistry and Geochemistry
Magmatic evolution of the Nevado del Ruiz volcano, Central Cordillera, Colombia Minera1 chemistry and geochemistry N. VATIN-PÉRIGNON “‘, P. GOEMANS “‘, R.A. OLIVER ‘*’ L. BRIQUEU 13),J.C. THOURET 14J,R. SALINAS E. 151,A. MURCIA L. ” Abstract : The Nevado del RU~‘, located 120 km west of Bogota. is one of the currently active andesitic volcanoes that lies north of the Central Cordillera of Colombia at the intersection of two dominant fault systems originating in the Palaeozoïc basement. The pre-volcanic basement is formed by Palaeozoïc gneisses intruded by pre-Cretaceous and Tertiarygranitic batholiths. They are covered by lavas and volcaniclastic rocks from an eroded volcanic chain dissected during the late Pliocene. The geologic history of the Nevado del Ruiz records two periods of building of the compound volcano. The stratigraphie relations and the K-Ar dating indicate that effusive and explosive volcanism began approximately 1 Ma ago with eruption of differentiated andesitic lava andpyroclastic flows and andesitic domes along a regional structural trend. Cataclysmic eruptions opened the second phase of activity. The Upper sequences consist of block-lavas and lava domes ranging from two pyroxene-andesites to rhyodacites. Holocene to recent volcanic eruptions, controled by the intense tectonic activity at the intersection of the Palestina fawlt with the regional fault system, are similar in eruptive style and magma composition to eruptions of the earlier stages of building of the volcano. The youngest volcanic activity is marked by lateral phreatomagmatic eruptions, voluminous debris avalanches. ash flow tuffs and pumice falls related to catastrophic collapse during the historic eruptions including the disastrous eruption of 1985. -
Atacama Pacific Gold Corporation
TECHNICAL REPORT on the CERRO MARICUNGA GOLD PROJECT Region III CHILE prepared for ATACAMA PACIFIC GOLD CORPORATION 330 Bay Street, Suite 1210, Toronto, Ontario Canada M5H 2S8 October 7, 2011 Prepared By: Michael Easdon, Oregon Reg. Prof. Geologist Alcántara 1128, Depto. 905, Las Condes Santiago, Chile [email protected] TABLE OF CONTENTS 1.0 SUMMARY ........................................................................................................... 1 2.0 INTRODUCTION .................................................................................................. 5 3.0 RELIANCE ON OTHER EXPERTS ...................................................................... 7 4.0 PROPERTY DESCRIPTION AND LOCATION ..................................................... 8 5.0 ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY ............................................................................................... 13 6.0 HISTORY ........................................................................................................... 15 7.0 GEOLOGICAL SETTING AND MINERALIZATION ............................................ 15 7.1 PROPERTY GEOLOGY: ............................................................................. 16 8.0 DEPOSIT TYPE ................................................................................................. 33 9.0 EXPLORATION .................................................................................................. 34 10.0 DRILLING .......................................................................................................... -
Explora Atacama І Hikes
ATACAMA explorations explora Atacama І Hikes T2 Reserva Tatio T4 Cornisas Nights of acclimatization Nights of acclimatization needed: 2 needed: 0 Type: Half day Type: Half day Duration: 1h Duration: 2h 30 min Distance: 2,3 km / 1,4 mi Distance: 6,7 kms / 4,2 mi Max. Altitude: 4.321 m.a.s.l / Max. Altitude: 2.710 m.a.s.l / HIKES 14.176 f.a.s.l 8.891 f.a.s.l Description: This exploration Description: Departing by van, we offers a different way of visiting head toward the Catarpe Valley Our hikes have been designed according the Tatio geysers, a geothermal by an old road. From there, we to different interests and levels of skill. field with over 80 boiling water hike along the ledges of La Sal They vary in length and difficulty so we sources. In this trip there are Mountains, with panoramic views always recommend travelers to talk to their excellent opportunities of studying of the oasis, the Atacama salt flat, guides before choosing an exploration. the highlands fauna, which includes and The, La Sal, and Domeyko Every evening, guides brief travelers vicuñas, flamingos and foxes, Mountains, three mountain ranges on the different explorations, so that among others. We walk through the that shape the region’s geography. they can choose one that best fit their reserve with views of The Mountains By the end of the exploration we interests. Exploration times do not consider and steaming hot water sources. descend through Marte Valley’s sand transportation. Return to the hotel by van. -
Mount Fuji Stromboli Is Located Mount Fuji Is Located in Italy
Stromboli Mount Fuji Stromboli is located Mount Fuji is located in Italy. in Japan. Its highest point is Its highest point is 924m high. Volcanoes Volcanoes 3776m high. The volcano has erupted Fuji last erupted in 1707. throughout the 20th century. This volcano is the highest volcano, it has the highest As long as there are peak in Japan and is historical records, considered one of the three Stromboli has been holy mountains. constantly active. Mount Fuji is an important It is famous for its element in Japanese art. normally small, but regular explosions. At night its eruptions Did You Know...? are visible from far More than 200 000 away so it is known as Did You Know...? Stromboli has an people climb to the the "Lighthouse of the eruption cycle of 20 top of the Mount Mediterranean". to 30 minutes. Fuji every year. Photo courtesy of giopuo, flrnt, island of volcanoes (@flickr.com) - granted under creative commons licence - attribution Photo courtesy of Manish Prabhune, midorisyu (@flickr.com) - granted under creative commons licence - attribution visit twinkl.com visit twinkl.com Ojos del Mauna Loa Mauna Loa is one of five Salado volcanoes that form the Ojos del Salado Island of Hawaii (the US Volcanoes is located on the Volcanoes state) in the Pacific Ocean. Argentina-Chile border. Its highest point is Its highest point is 4170m high. 6893m high. Mauna Loa rises from Nevados Ojos del Salado is the sea floor, and its the world's highest active height from its base to its volcano. summit is 9170m. This is greater than the height of It has two summit peaks of Mount Everest. -
16 Volcanoes As Landscape Forms
16 Volcanoes as landscape forms Ordinary, non-volcanic landforms are the results arid environments such as the Atacama Desert or of erosion by wind, water, and ice. Erosion is an the Moon's surface, erosion rates are indeed irreversible process which ultimately reduces immeasurably slow, but in others, such as the even the loftiest mountain range to a flat plain. humid tropics, they can be startlingly fast, even Volcanic landforms by contrast, are the results of by human standards. Catastrophic processes opposing constructive and destructive forces. such as avalanching accomplish in a few Constructive processes operate only while volca moments what it might take millennia to achieve noes arc active. This may be an extremely short otherwise. Whatever their rate, one thing is period-a matter of days or weeks-or rather certain: erosion starts work on a volcano as soon long, with activity continuing intermittently over as it starts growing, even before its lavas cool. tcns ofthousands of years. Paricutin, a common Erosion never ceases. A large volcano may or-garden basaltic scoria cone was born in a experience several phases of rapid construction Mexican cornfield on 20 February 1943. After a in its lifetime, during which the rate of construc year of activity it was 325 m high; when it finally tion exceeds the rate oferosion, but once eruptive simmered into silence in 1952 it w3s410 m high. activity wanes, erosion instantly gains the upper About 2 cubic kilometres of lava and tephra were hand. On a large volcanic massif, erosion may be erupted during its nine years of activity. -
Chile & Easter Island 11
©Lonely Planet Publications Pty Ltd Chile & Easter Island Norte Grande p143 Easter Island Norte Chico (Rapa Nui) p190 p401 Santiago Middle Chile p44 p88 Sur Chico p220 Chiloé p277 Northern Patagonia p297 Southern Patagonia p338 Tierra del Fuego p379 Carolyn McCarthy, Cathy Brown, Mark Johanson, Kevin Raub, Regis St Louis PLAN YOUR TRIP ON THE ROAD Welcome to Chile . 6 SANTIAGO . 44 Cajón del Maipo . 83 Chile Map . .. 8 History . 45 Tres Valles . 86 Chile’s Top 20 . 10 Sights . 45 Activities . 61 MIDDLE CHILE . 88 Need to Know . 20 Courses . 62 Valparaíso & If You Like . 22 Tours . 63 the Central Coast . .. 89 Valparaíso . 89 Month by Month . 25 Festivals & Events . 64 Sleeping . .. 65 Viña Del Mar . 101 Itineraries . 28 Eating . 68 Casablanca Valley Wineries . 106 Chile Outdoors . 33 Drinking & Nightlife . 72 Quintay . 107 Travel with Children . 38 Entertainment . .74 Isla Negra . 108 Shopping . 75 Regions at a Glance . 40 Parque Nacional Around Santiago . 81 la Campana . 108 Maipo Valley Wineries . 81 Aconcagua Valley . 109 Pomaire . 82 Los Andes . 109 BAS VAN DEN HEUVEL/SHUTTERSTOCK © HEUVEL/SHUTTERSTOCK DEN VAN BAS © LARYLITVIN/SHUTTERSTOCK SANTIAGO’S BELLAVISTA PARQUE NACIONAL NEIGHBORHOOD P70 HUERQUEHUE P242 STEVE ALLEN/SHUTTERSTOCK © ALLEN/SHUTTERSTOCK STEVE © STEPHENS/SHUTTERSTOCK LUIS JOSE COLCHAGUA VALLEY P112 IGLESIA SAN FRANCISCO DE CASTRO P289 Contents Portillo . 110 Salto Del Laja . 134 Reserva Nacional Southern Heartland . 111 Los Angeles . 135 Los Flamencos . 158 Colchagua Valley . 112 Parque Nacional El Tatio Geysers . 160 Matanzas . 115 Laguna del Laja . 135 Calama . .. 161 Pichilemu . 115 Angol . 136 Chuquicamata . 163 Curicó . 118 Parque Nacional Antofagasta . .. 163 Nahuelbuta . 137 Parque Nacional South of Antofagasta . -
Laguna Lejía
Laguna Lejía Antecedentes Generales del Sistema Salino: Región: Antofagasta Provincia: El Loa Comuna: San Pedro de Atacama UTM 19S HUSO Este: 633.386 UTM 19S HUSO Norte: 7.400.660 Proyección: PSAD 56 Altura: 4.325 m s.n.m Descripción General: Laguna salina andina de color turquesa con costras salinas sulfatadas de escasa difusión y potencia y con paleocostas al norte y este, indicando tamaño mayor de lo actual. Se encuentra adyacente con la cuenca del Salar de Atacama al oeste y la cuenca del Salar de Aguas Calientes Centro 2 ó Pili al este. Su límite norte es el Volcán Lascar. Datos Morfológicos y Climáticos del Sistema Salino: Morfología: Irregular con bordes redondeados. Superficie del Sistema Salino: 1,9 km2 Superficie de la Cuenca: 193 km2 Precipitación: 150 mm/año Evaporación Potencial: 1.500 mm/año Observaciones: Se realizó estudios paleohidrológicos por Grosjean et al. (1995). Potencial Litio: Sin Especificar 1 LEJÍA Datos de Composición Química de Aguas (Año 1978) Tipo de Li K Rb Cs Cl Muestra (ppm) Salmuera 25 985 1,9 < 0,1 8.635 FUENTE: Corporación de Fomento de la Producción (CORFO). 1978. Posibilidades de Litio y Potasio en Depósitos Salinos de la II Región-Chile: Reconocimiento Geológico Preliminar de Salares Andinos y Preandinos. Gobierno Regional II Región y Corporación de Fomento de la Producción (CORFO): 319p. Datos de Composición Química de Aguas (Año 1999) Tipo de Li K Mg Ca Na Cl SO4 As B NO3 Muestra (mg/l) Laguna 26,9 1.180 5.220 533 13.300 9.730 37.800 47,9 213 0,3 FUENTE: Risacher, F.; Alonso, H.; Salazar, C. -
Perdido-No-Atacama (20150812)
Publicidade 00:00 / 00:07 Rádio Go Outside, a trilha da sua aventura. **** Rádio Go Outside, a trilha da sua aventura. **** Rádio Go Outside, a trilha da sua aventura. **** Rádio Go Outside, a trilha da sua aventura. **** Rádio Go Outside, a trilha da sua aventura. **** Notícias Treinamento Equipamentos Guia de Bikes Viagem Fotos Vídeos Revista Eventos Publicidade Notícias 08.08.11 Perdido no Atacama O escalador Maximo Kausch relata uma de suas primeiras aventuras, quando se perdeu no deserto do Vídeos Atacama Patagônia, mon amour As belezas do lugar mais lindo do mundo em um incrível time-lapse Publicidade DUREZA: Dando uma pausa no calor, Maximo bebe uma água na secura Por Maximo Kausch, do Alta Montanha Muitas vezes me perguntam qual é a montanha que mais me marcou. De fato muitas me marcaram. Em algumas, tive acidentes, em outras vi gente morrer, e por isso essas me trouxeram grandes mudanças. Porém o lugar que mais me marcou não foi uma montanha, mas um deserto. O Atacama foi para mim uma daquelas situações que “separam os meninos dos Fotos homens”. Fui para lá com 18 anos, uma época em que eu subestimava tudo o que enfrentava. Queria escalar o mundo e não media limites para isso. Meu sonho de consumo na época não era ter um carro ou roupa de marca. Queria escalar o maior vulcão do mundo. Naquela ocasião, no entanto, eu estava na Bolívia e tinha um “pequeno” acidente geográfico entre o vulcão e eu: o deserto do Atacama. Deste modo me utilizei da minha experiência em atravessar desertos (que era zero) e decidi encarar os milhares de quilômetros que me separavam do destino. -
Contribución Al Conocimiento De La Zona Del Ojos Del Salado (Catamarca)
CONTRIBUCIÓN AL CONOCIMIENTO DE LA ZONA DEL OJOS DEL SALADO (CATAMARCA) A ntecedentes Si consultamos el trabajo de Pedro O. Sánchez 1 los primeros que ievantaron mapas de la zona fueron Alcides D ’Orbigny (1 8 2 6 -3 3 ) ; José Ballivián, mandado por Bolivia (1843) ; Hoogsgaard, por el Perú (1873- 74) ; Amado Pissis, encargado por Chile de estudiar el relieve de la Repú blica desde 1848, quien luego trabajó con Mariano Mugía, boliviano. En 1883, dice Sánchez, Chile mandó levantar una carta a Francisco San R o mán, Santiago Muñoz, Alejandro Chadwick y Abelardo Pizarro, comisión que trabajó con exactitud y sembró la Puna de sugestivos nombres en ho menaje a los científicos que la visitaron: cordilleras D ’Orbigny, Claudio Gay, Domeyko, sierras Gorbea, Barros Arana, monte Pissis, altiplanicie F*hilippi, etc. Alejandro Bertrand, casi en la misma época, se dedicó a la Puna y a sus altas cumbres y publicó Memoria sobre el desierto de A ta- cama y sus regiones limítrofes (1 8 8 4 ). Para su trabajo se valió de cartas anteriores, especialmente las de San Román, Hugo Reck, boliviano, ( 1860- 1863) y la de Brackebusch, mandado por Argentina. El Tnte. de Navio Vicente Montes 1 2 fue encargado por el perito argentino, en el pleito de límites con Chile, de estudiar la región montañosa entre los paralelos 26 y 28 a fin de determinar con precisión qué se debía considerar como cordillera de Los Andes El 29 de abril de 1892 3 con vinieron los peritos en que una comisión mixta iniciaría la demarcación desde el Portezuelo de San Francisco hacia el sur, integrada por Julio Díaz, Luis Dellepiane, Fernando Dousset (Argentina) y Alejandro Bertrand, Aníbal Contreras y Alvaro Donoso (C hile). -
Refining the Late Quaternary Tephrochronology for Southern
Quaternary Science Reviews 218 (2019) 137e156 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Refining the Late Quaternary tephrochronology for southern South America using the Laguna Potrok Aike sedimentary record * Rebecca E. Smith a, , Victoria C. Smith a, Karen Fontijn b, c, A. Catalina Gebhardt d, Stefan Wastegård e, Bernd Zolitschka f, Christian Ohlendorf f, Charles Stern g, Christoph Mayr h, i a Research Laboratory for Archaeology and the History of Art, 1 South Parks Road, University of Oxford, OX1 3TG, UK b Department of Earth Sciences, University of Oxford, OX1 3AN, UK c Department of Geosciences, Environment and Society, Universite Libre de Bruxelles, Belgium d Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Alten Hafen 26, D-27568, Bremerhaven, Germany e Department of Physical Geography, Stockholm University, SE-10691 Stockholm, Sweden f University of Bremen, Institute of Geography, Geomorphology and Polar Research (GEOPOLAR), Celsiusstr. 2, D-28359, Bremen, Germany g Department of Geological Sciences, University of Colorado, Boulder, CO, 80309-0399, USA h Institute of Geography, Friedrich-Alexander-Universitat€ Erlangen-Nürnberg, Wetterkreuz 15, 91058 Erlangen, Germany i Department of Earth and Environmental Sciences & GeoBio-Center, Ludwig-Maximilians-Universitat€ München, Richard-Wagner-Str. 10, 80333 München, Germany article info abstract Article history: This paper presents a detailed record of volcanism extending back to ~80 kyr BP for southern South Received 12 March 2019 America using the sediments of Laguna Potrok Aike (ICDP expedition 5022; Potrok Aike Maar Lake Received in revised form Sediment Archive Drilling Project - PASADO). Our analysis of tephra includes the morphology of glass, the 29 May 2019 mineral componentry, the abundance of glass-shards, lithics and minerals, and the composition of glass- Accepted 2 June 2019 shards in relation to the stratigraphy. -
Balance De Gestión Integral Año 2019 Ministerio De Obras Públicas Dirección De Vialidad
Balance de Gestión Integral Año 2019 Ministerio de Obras Públicas Dirección de Vialidad Pag. 1 Índice 1 Presentación Cuenta Pública del Ministro del ramo 3 2 Resumen Ejecutivo Servicio 6 3 Resultados de la Gestión año 2019 7 3.1 Resultados asociados al Programa de Gobierno, mensajes presidenciales y otros aspectos relevantes para el jefe de servicio 3.2 Resultados de los Productos Estrategicos y aspectos relevantes para la Ciudadania 4 Desafíos para el período de Gobierno 13 Anexo 1 Identifcación de la Institución 20 Anexo 2 Recursos Humanos Anexo 3 Recursos Financieros Anexo 4 Indicadores de Desempeño año 2017 - 2019 25 Anexo 5 Compromisos de Gobierno 2018 - 2022 28 Anexo 6 Evaluaciones 29 Anexo 7 Cumplimiento de Sistemas de Incentivos Institucionales 2019 30 Anexo 8 Cumplimiento Convenio de Desempeño Colectivo 2018 - 2022 32 Anexo 9 Resultados en la Implementación de medidas de Género 2018 - 2022 36 Anexo 10 Proyectos de Ley en tramitación en el Congreso Nacional 2019 / Leyes Promulgadas durante 2019 37 Anexo 11 Premios y Reconocimientos 38 Pag. 2 1 Presentación Cuenta Pública del Ministro del ramo Ministerio Ministerio de Obras Públicas En línea con el mandato entregado por el Presidente Sebastián Piñera y nuestros objetivos estratégicos institucionales -que son mejorar la calidad de vida de las personas a través de conectividad, buena infraestructura pública y acceso a los recursos hídricos-, el Ministerio de Obras Públicas ejecutó durante el año 2019 un presupuesto de un billón 761 mil millones de pesos en diversas obras a lo largo