Revista Del Iiicahgeo
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Fondo De Fomento De Medios De Comunicación Social Regionales, Provinciales Y Comunales
FONDO DE FOMENTO DE MEDIOS DE COMUNICACIÓN SOCIAL REGIONALES, PROVINCIALES Y COMUNALES ACTA DE RECEPCIÓN POSTULACIONES FORMATO PAPEL-LÍNEA CONCURSO 2021 Ministerio Secretaría General de Gobierno Unidad de Fondos Concursables Unidad de Fondos Concursables Fondo de Fomento de Medios de Comunicación Social Regionales, Provinciales y Comunales Concurso 2021 Acta de recepción de postulaciones en Papel y en Línea NUAL D I. Recepción de Proyectos: En las oficinas de la Secretaría Regional Ministerial de Gobierno de la Región del Libertador General Bernardo O’Higgins, ubicada en Plaza Los Héroes Nº 433, comuna de Rancagua, y con la presencia del Sr. Alejandro Álvarez Valenzuela, Secretario Regional Ministerial de Gobierno Región del Libertador General Bernardo O’Higgins, quien actúa como ministro de fe; se indica lo siguiente: II. Recepción de Proyectos en Papel: Se certifica que el día 16 de Abril de 2021 a las 13:00 horas, se recepcionaron los proyectos en formato papel presentados al concurso 2021 del Fondo de Fomento de Medios de Comunicación Social Regionales, Provinciales y Comunales; constatando la cantidad de 0 proyectos. III. Detalle: A continuación, se detallan los proyectos presentados de acuerdo al orden de entrega indicado en la respectiva nómina de registro: NOMBRE RAZÓN SOCIAL/ NOMBRE RUT N° FILIO FANTASÍA DEL NOMBRE PROYECTO COMUNA PER. NATURAL MEDIO MEDIO 1 NO APLICA Unidad de Fondos Concursables | www.fondodemedios.gob.cl Unidad de Fondos Concursables Fondo de Fomento de Medios de Comunicación Social Regionales, Provinciales y Comunales Concurso 2021 Acta de recepción de postulaciones en Papel y en Línea IV. Recepción de Proyectos en Línea: Se certifica que el día 16 de Abril de 2021 a las 23:59 horas, se cerró de forma automática el sistema de postulación en línea, disponible en el sitio web fondos.gob.cl; constatando la cantidad de 60 proyectos, que han sido válidamente presentados de acuerdo al plazo y hora de postulación definidas en las bases que regulan la presente convocatoria. -
Operación Servicios De Transporte Gratuito Plebiscito Nacional 2020, Región De O’Higgins
OPERACIÓN SERVICIOS DE TRANSPORTE GRATUITO PLEBISCITO NACIONAL 2020, REGIÓN DE O’HIGGINS SERVICIOS GRATUITOS QUE OPERARÁN DURANTE EL PLEBISCITO. ZONAS AISLADAS Y SERVICIO ESPECIAL REGIÓN TOTAL GENERAL RURALES MTT ELECCIONES LIBERTADOR GENERAL 52 77 129 BERNARDO O'HIGGINS SERVICIOS ESPECIALES ELECCIONES GRATUITOS HORARIO COMUNA ORIGEN - DESTINO LOCALIDADES - SECTORES HORARIO IDA RETORNO CHÉPICA LA RUDA - CHÉPICA LA RUDA - CHÉPICA 9:00 12:30 ORILLA DE AUQUINCO - ORILLA DE AUQUINCO - LOS RINCONES - CENTRO DE LA ORILLA - CHÉPICA 10:00 13:00 CHÉPICA CHEPICA CHÉPICA LOS AMARILLOS - CHÉPICA LOS AMARILLOS - CHÉPICA 9:00 12:30 PAREDONES DE AUQUINCO - CHÉPICA PAREDONES DE AUQUINCO - CHÉPICA 9:00 - 13:00 12:30 - 15:00 CHÉPICA CHÉPICA LAS PALMAS - CHÉPICA LAS PALMAS - LAS ARAÑAS - CHEPICA 10:00 13:30 CHÉPICA UVA BLANCA - CHÉPICA UVA BLANCA - CHEPICA BAJO - CHEPICA 10:00 13:30 CHÉPICA LA MINA - CHÉPICA LA MINA - CHEPICA BAJO - CHEPICA 10:00 13:30 CHIMBARONGO HUEMUL - CHIMBARONGO HUEMUL 10:00 - 13:00 14:00 - 17:00 CHIMBARONGO QUINTA - CHIMBARONGO QUINTA 10:00 - 13:00 14:00 - 17:00 CODEGUA EL CARMEN - CODEGUA EL CARMEN - CODEGUA 10:00 12:30 CODEGUA TUNCA - CODEGUA TUNCA - CODEGUA 10:00 - 13:30 12:30 - 16:30 CODEGUA CALLEJONES - CODEGUA CALLEJONES - ALDEA AGRICOLA - JACINTO MARQUEZ - CODEGUA 10:00 - 13:30 12:30 - 16:30 LA ESTRELLA ESTERO SECO - LA ESTRELLA ESTERO SECO, QUEBRADA DE LA VIRGEN 10:00 13:00 LAS CABRAS LOS AROMOS - LAS CABRAS LOS AROMOS - LAS CABRAS 10:00 14:00 LOLOL RANGUILI - LOLOL RANGUILI - SANTA TERESA DE QUIAHUE - LOLOL 10:00 13:00 LOLOL -
Deep Carbon Science
From Crust to Core Carbon plays a fundamental role on Earth. It forms the chemical backbone for all essential organic molecules produced by living organ- isms. Carbon-based fuels supply most of society’s energy, and atmos- pheric carbon dioxide has a huge impact on Earth’s climate. This book provides a complete history of the emergence and development of the new interdisciplinary field of deep carbon science. It traces four cen- turies of history during which the inner workings of the dynamic Earth were discovered, and it documents the extraordinary scientific revolutions that changed our understanding of carbon on Earth for- ever: carbon’s origin in exploding stars; the discovery of the internal heat source driving the Earth’s carbon cycle; and the tectonic revolu- tion. Written with an engaging narrative style and covering the scien- tific endeavors of about 150 pioneers of deep geoscience, this is a fascinating book for students and researchers working in Earth system science and deep carbon research. is a life fellow at St. Edmund’s College, University of Cambridge. For more than 50 years he has passionately engaged in bringing discoveries in astronomy and cosmology to the general public. He is a fellow of the Royal Historical Society, a former vice- president of the Royal Astronomical Society and a fellow of the Geological Society. The International Astronomical Union designated asteroid 4027 as Minor Planet Mitton in recognition of his extensive outreach activity and that of Dr. Jacqueline Mitton. From Crust to Core A Chronicle of Deep Carbon Science University of Cambridge University Printing House, Cambridge CB2 8BS, United Kingdom One Liberty Plaza, 20th Floor, New York, NY 10006, USA 477 Williamstown Road, Port Melbourne, VIC 3207, Australia 314–321, 3rd Floor, Plot 3, Splendor Forum, Jasola District Centre, New Delhi – 110025, India 79 Anson Road, #06–04/06, Singapore 079906 Cambridge University Press is part of the University of Cambridge. -
Supplementary Data
Supplementary data Water sources Places Sites Samples Rivers Vacas, Cuevas, Tupungato and Mendoza 7 42 rivers in Punta de Vacas. Cuevas River in Puente del Inca. Horcones Superior and Horcones rivers at Mt. Aconcagua Confluencia Camp. Ice bodies Horcones Inferior Glacier and Mt. Tolosa 2 34 rock glaciers conglomerate. Groundwaters Vertiente del Inca, La Salada Stream, 6 41 Confluencia Nueva Spring, Confluencia Vieja Spring and geothermal waters of "Copa de Champagne" and "Viejo Túnel", both in "Puente del Inca". Precipitations Collectors at Laguna de Horcones and 2 4 Confluencia Camp, both in the Mt. Aconcagua Park Snow basins Valle Azul, Los Puquios and Santa María 3 33 Table S1 Sampling along the melting period 2013-2014 in Cordillera Principal geological province. Ice body type classification corresponds to the official inventory of glaciers (IANIGLA-ING, 2015a). Sites refers to quantity of sampling sites for each water source Station 2 and MDS HI m3/s Soil MDT °C Air MDT °C DMaxT DMinT °C max-min °C HI Glacier °C streamflow Mean 2.09 7.17 4.90 3.55 0.77 2.72 SD 0.95 3.15 3.35 4.35 3.30 3.02 VC% 45.34 43.90 68.31 122.56 430.53 111.07 Max 4.88 11.60 10.68 11.27 6.41 11.27 Min 0.52 1.35 -3.65 -5.95 -7.28 -5.95 Rock glaciers streamflow MDS Tolosa m3/s Mean 0.02 SD 0.01 VC% 70.80 Max 0.05 Min 0.00 Station 1 Atm Press hPa Air MDT °C DMaxT °C DMinT °C RH% Mean 706.44 11.12 17.82 4.74 37.27 SD 1.55 2.88 3.41 2.66 17.39 VC% 0.22 25.89 19.15 56.17 46.67 Max 710.04 16.57 24.84 11.20 97.60 Min 703.11 2.89 6.25 -0.53 13.60 Station 1 Soil DMT °C Wind Dir.° W mean vel. -
Stratigraphic Distribution and Suggested Evolution of Dendroid Graptolites from the Silurian of Eastern Australia
University of Wollongong Research Online Faculty of Science - Papers (Archive) Faculty of Science, Medicine and Health 1-1-2010 Stratigraphic distribution and suggested evolution of dendroid graptolites from the Silurian of eastern Australia Barrie Rickards University of Cambridge Anthony Wright University of Wollongong, [email protected] Follow this and additional works at: https://ro.uow.edu.au/scipapers Part of the Life Sciences Commons, Physical Sciences and Mathematics Commons, and the Social and Behavioral Sciences Commons Recommended Citation Rickards, Barrie and Wright, Anthony: Stratigraphic distribution and suggested evolution of dendroid graptolites from the Silurian of eastern Australia 2010, 177-190. https://ro.uow.edu.au/scipapers/634 Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Stratigraphic distribution and suggested evolution of dendroid graptolites from the Silurian of eastern Australia Abstract Five evolutionary lineages are proposed for Silurian species of the benthic dendroid graptolite genus Dictyonema, based largely on the exceptional eastern Australian records of the genus, comprising at least 25 species. These are: A, the delicatulum lineage with bifurcating ventral autothecal apertural spines; B, the paululum lineage with single ventral apertural spines or processes; C, the elegans lineage with isolated thecal apertures ± processes; D, the sherrardae lineage with dorsal apertural processes; and E, the venustum lineage with simple autothecal apertures. Brief comments are also made on other dendroid genera occurring in Australian strata, namely: Acanthograptus, Koremagraptus, Callograptus, Dendrograptus, Stelechocladia, Thallograptus and Palaeodictyota. Other non-graptoloid benthic hemichordates also listed are the tuboids Galaeograptus, Reticulograptus and Cyclograptus and the rhabdopleuran ?Rhabdopleura. -
Famous Geologist Fact Sheet Your Job Is to Research Information About
Famous Geologist Fact Sheet Your job is to research information about one of the geologists on the list and arrange the information you find into a fact sheet about that person. The fact sheet should only be one side of an 8 ½ x 11 inch paper. Include all of the following information about the scientist. You may turn your project into a wanted poster if you want starting your paper with “Be on the lookout for this man/woman. Wanted for ___________.” You may use bulleted lists where appropriate. A. Give the scientists full name – first, middle, last B. When they were born and when they died (if applicable) C. Where they were born – country, state, city D. Where they grew up if different from where they were born E. Family information – parents, siblings, wife, children F. Where they went to school – elementary, high school, college G. What they did for a job H. What they studied – field of expertise - give a complete description of what they studied I. What they are famous for specifically – include how their contributions affect us now and/or will in the future J. A quote from your scientist if you can find one K. Any other interesting facts about your scientist L. A picture of the scientist – not a cartoon M. A picture pertaining to what they are famous for N. List of important publications by the scientist O. List any awards given and the dates they were given to your scientist for their contributions to science P. Cite your source or sources according to the MLA Style Your grade will be determined by: * Overall presentation, neatness and creativity. -
Geo-Climatic Hazards in the Eastern Subtropical Andes: Distribution, Climate Drivers and Trends Iván Vergara1, Stella M
https://doi.org/10.5194/nhess-2019-381 Preprint. Discussion started: 21 January 2020 c Author(s) 2020. CC BY 4.0 License. Geo-climatic hazards in the eastern subtropical Andes: Distribution, Climate Drivers and Trends Iván Vergara1, Stella M. Moreiras2, 3, Diego Araneo2, 3 and René Garreaud4, 5 1 CONICET-IPATEC, Bariloche, 8400, Argentina 5 2 CONICET-IANIGLA, Mendoza, 5500, Argentina 3 National University of Cuyo, Mendoza, 5502, Argentina 4 University of Chile, Santiago, 8330015, Chile 5 Center for Climate and Resilience Research, Santiago, 8320198, Chile 10 Correspondence to: Iván Vergara ([email protected]) Abstract. Detection and understanding of historical changes in the frequency of geo-climatic hazards (G-CHs) is crucial for the quantification of current hazard and their future projection. Here we focus in the eastern subtropical Andes (32-33° S), using meteorological data and a century-long inventory on 553 G-CHs triggered by rainfall or snowfall. First we analysed their spatio-temporal distributions and the role of climate variability on the year-to-year changes in the number of days with 15 G-CHs. Precipitation is positively correlated with the number of G-CHs across the region and year-round; mean temperature is negatively correlated with snowfall-driven hazards in the western (higher) half of the study region during winter, and with rainfall-driven hazards in the eastern zone during summer. The trends of the G-CHs frequency since the mid-20th century were calculated taking cautions for their non-systematic monitoring. The G-CHs series for the different triggers, zones and seasons were generally stationary. -
Darwin at Puente Del Inca: Observations on the Formation of the Inca's Bridge and Mountain Building
170 Revista de la Asociación Geológica Argentina 64 (1): 170- 179 (2009) DARWIN AT PUENTE DEL INCA: OBSERVATIONS ON THE FORMATION OF THE INCA'S BRIDGE AND MOUNTAIN BUILDING Victor A. RAMOS Laboratorio de Tectónica Andina, FCEN, Universidad de Buenos Aires - CONICET. Email: [email protected] ABSTRACT The analyses of the observations of Charles Darwin at Puente del Inca, during his second journey across the High Andes drew attention on two different aspects of the geological characteristics of this classic area. Most of his descriptions on the characteristics and the origin of the natural bridge were not published, mainly due to his poor impression of Puente del Inca. However, the application of the uniformitarian principles shows that it was formed as an ice bridge associated with snow and debris avalanches later on cemented by the minerals precipitated by the adjacent hot-water springs. Darwin's observations on the complex structural section at Puente del Inca, together with his findings of shallow water marine fossil mollusks in the thick stratigraphic column of the area interfingered with volcanic rocks, led him to speculate on several geological processes. Based on his geological observations, Darwin argued on the mountain uplift, the subsidence of the marine bottom, the epi- sodic lateral growth of the cordillera, and their association with earthquakes and volcanic activity, which was an important advance in the uniformitarian hypothesis of mountain uplift proposed by Charles Lyell. Darwin was able to recognize the epi- sodic nature of mountain uplift, and based on these premises he concluded that the Andes were still undergoing uplift. -
Catalog of Paleontological Type Specimens in the Geological Museum, University of Minnesota
MINNESOTA GEOLOGICAL SURVEY INFORMA TION CIRCULAR 33 CATALOG OF PALEONTOLOGICAL TYPE SPECIMENS IN THE GEOLOGICAL MUSEUM, UNIVERSITY OF MINNESOTA UNIVERSITY OF MINNESOTA Minnesota Geological Survey Priscilla C. Grew, Director Information Circular 33 CATALOG OF PALEONTOLOGICAL TYPE SPECIMENS IN THE GEOLOGICAL MUSEUM, UNIVERSITY OF MINNESOTA By William F. Rice University of Minnesota St. Paul, 1990 ISSN 0544-3105 The University of Minnesota is committed to the policy that all persons shall ha ve equal access to its programs, facilities, and employment without regard to race, religion, color, sex, national origin, handicap, age, veteran status, or sexual orientation. CONTENTS Page FOREWORD, by Robert E. Sloan ...................................................... v INTRODUCTION ............................................................................. 1 ORGANIZATION OF THE CATALOG ........................................... 1 PRIMARY PALEONTOLOGICAL TYPES .................................... 3 PHYLUM ANNELIDA ...................................................................... 4 PHYLUM ARTHROPODA Class Merostomata ..................................................................... 15 Subclass Ostracoda ..................................................................... 16 Class Trilobita ........................................................................... 35 PHYLUM BRACHiOPODA ........................................................... 39 PHYLUM BRYOZOA .................................................................... 45 -
Relatos Desde El Litoral: La Represión Dictatorial En Pichilemu 1973-1977
Universidad de Chile Facultad de Filosofía y Humanidades Seminario de grado: Procesos políticos de postmemorias autoritarias. Chile en la segunda mitad del siglo XX. Relatos desde el litoral: La represión dictatorial en Pichilemu 1973-1977. Un acercamiento a la verdad Informe para optar al Grado de Licenciada presentado por: Álvaro Cabrera Monsalve Profesora guía: Azun Candina Polomer Santiago de Chile 2018 Agradecimientos Agradecer en primera instancia a la Universidad de Chile y al Departamento de Historia por brindar en estos cuatro años espacios de crecimiento, no solo intelectual, sino que personal. A mis compañeros de generación, que de alguna manera u otra fueron parte de esta historia. En segundo lugar, a la profesora Azun Candina, que fue parte de 3 de los 4 años que tuve en la Universidad, por su paciencia, conocimiento y organización durante este proceso que nos permitió abordar de la mejor manera este viaje llamado tesis. A la profesora Carla Peñaloza, por su trabajo constante por la recuperación de la memoria y su ayuda brindada en este proceso. A mi madre Pilar Monsalve y a mi padre Iván Cabrera por su inmenso cariño, su enorme paciencia y entrega. A mis hermanas Natalia y Sofía, mis compañeras de vida. A mis amigas y amigos que me mantienen con los pies en la tierra en momentos difíciles. A Maya, Luna y Hugo. Agradecer el aporte desinteresado de Eugenio Gonzáles, Omar Rubio, Luis Castro, Rafael Moraga, Roberto Becerra y Bernabé Pavéz. Sin ellos, nada de esto habría sido posible. A mis abuelas Eliana y Gladys A mis abuelos José Miguel y Jorge 1 Índice Introducción ……………………………………………………………………….......... -
Aconcagua Expedition Trip Notes 2021/22
ACONCAGUA 6,962M / 22,841FT 2021/22 EXPEDITION TRIP NOTES ACONCAGUA EXPEDITION NOTES 2021/22 EXPEDITION DETAILS Dates: November 29 to December 18, 2021 January 3–22, 2022 Duration: 20 days Departure: ex Mendoza, Argentina Price: US$6,350 per person A successful team prepares to descend the mountain. Photo: Suze Kelly Aconcagua, the “Sentinel of Stone”, is the highest peak outside of the Himalayas. Located in western Argentina, the heart of the Central Andes, it is South America’s highest peak and one of the much sought after Seven Summits. An ascent of this eminent Andean Peak is ideal for on the only available summit day. Our climbing those wishing to experience high altitude expedition route traverses over the mountain making best use mountaineering and is often undertaken as a preparation of the time available and allowing for a faster exit climb for the big mountains of the Himalayas. via the shorter Horcones Valley, whilst giving us the opportunity to appreciate the relative remoteness of The Adventure Consultants Aconcagua expedition the Vacas Valley on the approach. provides the very best opportunity for you to climb this lofty mountain in an environment that Unlike most of the operators on Aconcagua, we provide is properly managed to give you the best chance a client focused expedition that is geared towards to succeed in safety and relative comfort. You will giving you the maximum opportunity of succeeding benefit from our many years of experience on this on this peak. Our success rate is an indication of the and other high mountains across the globe and our emphasis we place on your well-being and a successful highly qualified guides will offer you an experience outcome for you. -
Long-Term Landscape Evolution, Genesis, Distribution and Age
GONDWANA PALEOLANDSCAPES: LONG-TERM LANDSCAPE EVOLUTION, GENESIS, DISTRIBUTION AND AGE Jorge RABASSA 1,2 (1) Laboratorio de Cuaternario y Geomorfología, CADIC-CONICET, Bernardo Houssay 200, 9410. Tierra del Fuego, Argentina. E-mail: [email protected] (2) Universidad Nacional de la Patagonia - San Juan Bosco, Sede Ushuaia. “Let the landscape teach me” Lester C. King, personal letter to Charles Higgins, 1958. “While the geologist may often be in error, the Earth is never wrong” Lester C. King, 1967. Introduction The Concepts of Gondwana Paleolandscapes and Long-Term Landscape Evolution: Previous Works Gondwana Paleolandscapes: Basic Scientific Concepts Related The Evolution of the Gondwana Cratonic Areas During the Mesozoic Mesozoic and Paleogene Climates Granite Deep Weathering Passive-Margin Geomorphology Duricrusts: Ferricretes, Silcretes, Calcretes A Brief and Preliminary Review of Gondwana Landscapes and Other Ancient Paleolandscapes in the Southern Hemisphere and Other Parts of the World Discussion and Conclusions Acknowledgements Bibliographic References ABSTRACT – The concept of “Gondwana Landscape” was defined by Fairbridge (1968) as an “ancestral landscape” composed of “series of once-planed remnants” that “record traces of older planation” episodes, during the “late Mesozoic (locally Jurassic or Cretaceous)”. This has been called the “Gondwana cyclic land surface” in the continents of the southern hemisphere, occurring extensively in Australia, Southern Africa and the cratonic areas of South America. Remnants of these surfaces are found also in India, in the northern hemisphere and it is assumed they have been preserved in Eastern Antarctica, underneath the Antarctic ice sheet which covers that region with an average thickness of 3,000 meters. These paleolandscapes were generated when the former Gondwana super-continent was still in place and similar tectonic conditions in its drifted fragments have allowed their preservation.