The Diffusion of Maize to the Southwestern United States and Its Impact
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The Great Basin Landscape Conservation Cooperative
September 2010 The Great Basin Landscape Conservation Cooperative What is a Landscape Conservation The Great Basin Landscape Cooperative? Conservation Cooperative Landscape Conservation Cooperatives (LCCs) are applied science and management partnerships between Interior Department bureaus and others involved in natural resource management and What is the Great Basin LCC? conservation. Secretarial Order No. 3289, issued on Sept. 14, 2009 The Great Basin LCC will be a self-directed partnership. The by Interior Secretary Ken Salazar, calls for the establishment of 21 Great Basin LCC will provide a range of scientific and technical LCCs nationwide to better integrate science and management to support tools for landscape-scale conservation design to a wide address climate change and related issues array of managers. These tools will help managers identify and target biological objectives for native species and habitats in the What will the Great Basin LCC do? face of climate change and other stressors. Open public access to In broad terms, the Great Basin LCC will help link and integrate Great Basin LCC products will promote acceptance and use of Interior’s proposed Climate Science Centers with resource managers the science in regional conservation strategies. This effort is being and science users; will bring additional Interior resources to bear on coordinated with other regional partnerships and will be set up in landscape-scale issues and opportunities; and will help in applying a manner that will facilitate coordination and the identification science and facilitating coordination on a wide range of efforts of needs, capacities and gaps. We will link our efforts to bring to respond to climate change, invasive species, wildfires, human additional science capacity to improve conservation strategies development and other change agents across the Great Basin. -
Machc19-05.4
19th Meeting of the MesoAmerica – Caribbean Sea Hydrographic Commission Regional Capacity Building Update of Brazil on its Regional Project International Hydrographic Organization Organisation Hydrographique Internationale Capacity Building in the Caribbean, South America and Africa - Hydrography Courses Brazil/DHN has been expanding its Capacity Building Project towards other countries in the Amazon region and in the Atlantic Ocean basin. COURSE DESCRIPTION DURATION C-Esp-HN Technician in Hydrography and Navigation (Basic Training) 42 weeks C-Ap-HN Technician in Hydrography and Navigation (IHO Cat. “B”) 35 weeks CAHO Hydrographic Surveyors (IHO Cat. “A”) 50 weeks 2018 – 1 Bolivian Navy Officer (IHO Cat “A”). 2019 – Confirmed: 2 students from Saint Vincent and the Grenadines (IHO Cat “A”). Confirmation in progress: Angola (6), Mozambique (4), Bolivia (1), Colombia (1) and Paraguay (1) (IHO Cat “A” and “B”). 2020 – In the near future, Fluminense Federal University (UFF) and other Brazilian universities and governmental institutions in cooperation with DHN will develop a Hydrography Program and a Nautical Cartography Program. International Hydrographic Organization Organisation Hydrographique Internationale 2 Capacity Building - IHO Sponsored Trainings/Courses Work Program Training/Course Date 2018 Maritime Safety Information (MSI) Training Course 16-18 October 18 participants from 12 different countries Argentina (2) Brazil (6) Bolivia (1) Colombia (1) Ecuador (1) El Salvador (1) Guyana (1) Liberia (1) Paraguay (1) Peru (1) Uruguay (1) -
A Glance at Member Countries of the Mesoamerica Integration and Development Project, (LC/MEX/TS.2019/12), Mexico City, 2019
Thank you for your interest in this ECLAC publication ECLAC Publications Please register if you would like to receive information on our editorial products and activities. When you register, you may specify your particular areas of interest and you will gain access to our products in other formats. www.cepal.org/en/publications ublicaciones www.cepal.org/apps Alicia Bárcena Executive Secretary Mario Cimoli Deputy Executive Secretary Raúl García-Buchaca Deputy Executive Secretary for Administration and Analysis of Programmes Hugo Eduardo Beteta Director ECLAC Subregional Headquarters in Mexico This document was prepared by Leda Peralta Quesada, Associate Economic Affairs Officer, International Trade and Industry Unit, ECLAC Subregional Headquarters in Mexico, under the supervision of Jorge Mario Martínez Piva, and with contributions from Martha Cordero Sánchez, Olaf de Groot, Elsa Gutiérrez, José Manuel Iraheta, Lauren Juskelis, Julie Lennox, Debora Ley, Jaime Olivares, Juan Pérez Gabriel, Diana Ramírez Soto, Manuel Eugenio Rojas Navarrete, Eugenio Torijano Navarro, Víctor Hugo Ventura Ruiz, officials of ECLAC Mexico, as well as Gabriel Pérez and Ricardo Sánchez, officials of ECLAC Santiago. The comments of the Presidential Commissioners-designate and the Executive Directorate of the Mesoamerica Integration and Development Project are gratefully acknowledged. The views expressed in this document are the sole responsibility of the author and may not be those of the Organization. This document is an unofficial translation of an original that did not undergo formal editorial review. The boundaries and names shown on the maps in this document do not imply official endorsement or acceptance by the United Nations. Explanatory notes: - The dot (.) is used to separate the decimals and the comma (,) to separate the thousands in the text. -
Eocene–Early Miocene Paleotopography of the Sierra Nevada–Great Basin–Nevadaplano Based on Widespread Ash-Flow Tuffs and P
Origin and Evolution of the Sierra Nevada and Walker Lane themed issue Eocene–Early Miocene paleotopography of the Sierra Nevada–Great Basin–Nevadaplano based on widespread ash-fl ow tuffs and paleovalleys Christopher D. Henry1, Nicholas H. Hinz1, James E. Faulds1, Joseph P. Colgan2, David A. John2, Elwood R. Brooks3, Elizabeth J. Cassel4, Larry J. Garside1, David A. Davis1, and Steven B. Castor1 1Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA 2U.S. Geological Survey, Menlo Park, California 94025, USA 3California State University, Hayward, California 94542, USA 4Department of Earth and Environment, Franklin & Marshall College, Lancaster, Pennsylvania 17604, USA ABSTRACT the great volume of erupted tuff and its erup- eruption fl owed similar distances as the mid- tion after ~3 Ma of nearly continuous, major Cenozoic tuffs at average gradients of ~2.5–8 The distribution of Cenozoic ash-fl ow tuffs pyroclastic eruptions near its caldera that m/km. Extrapolated 200–300 km (pre-exten- in the Great Basin and the Sierra Nevada of probably fi lled in nearby topography. sion) from the Pacifi c Ocean to the central eastern California (United States) demon- Distribution of the tuff of Campbell Creek Nevada caldera belt, the lower gradient strates that the region, commonly referred and other ash-fl ow tuffs and continuity of would require elevations of only 0.5 km for to as the Nevadaplano, was an erosional paleovalleys demonstrates that (1) the Basin valley fl oors and 1.5 km for interfl uves. The highland that was drained by major west- and Range–Sierra Nevada structural and great eastward, upvalley fl ow is consistent and east-trending rivers, with a north-south topographic boundary did not exist before with recent stable isotope data that indicate paleodivide through eastern Nevada. -
Great Salt Lake FAQ June 2013 Natural History Museum of Utah
Great Salt Lake FAQ June 2013 Natural History Museum of Utah What is the origin of the Great Salt Lake? o After the Lake Bonneville flood, the Great Basin gradually became warmer and drier. Lake Bonneville began to shrink due to increased evaporation. Today's Great Salt Lake is a large remnant of Lake Bonneville, and occupies the lowest depression in the Great Basin. Who discovered Great Salt Lake? o The Spanish missionary explorers Dominguez and Escalante learned of Great Salt Lake from the Native Americans in 1776, but they never actually saw it. The first white person known to have visited the lake was Jim Bridger in 1825. Other fur trappers, such as Etienne Provost, may have beaten Bridger to its shores, but there is no proof of this. The first scientific examination of the lake was undertaken in 1843 by John C. Fremont; this expedition included the legendary Kit Carson. A cross, carved into a rock near the summit of Fremont Island, reportedly by Carson, can still be seen today. Why is the Great Salt Lake salty? o Much of the salt now contained in the Great Salt Lake was originally in the water of Lake Bonneville. Even though Lake Bonneville was fairly fresh, it contained salt that concentrated as its water evaporated. A small amount of dissolved salts, leached from the soil and rocks, is deposited in Great Salt Lake every year by rivers that flow into the lake. About two million tons of dissolved salts enter the lake each year by this means. Where does the Great Salt Lake get its water, and where does the water go? o Great Salt Lake receives water from four main rivers and numerous small streams (66 percent), direct precipitation into the lake (31 percent), and from ground water (3 percent). -
1. Presentación. 2.Fundamentación
1 UNIVERSIDAD VERACRUZANA INSTITUTO DE INVESTIGACIONES HISTORICO-SOCIALES INTRODUCCION A MESOMERICA Y NUEVOS DESCUBRIMIENTOS PROFR. DR. PEDRO JIMENEZ LARA I.I.H-S 1. Presentación. El presente curso pretende ofrecer una visión de los elementos y períodos culturales que identifican al México Antiguo. Las regiones son: oasisamérica, aridoamérica y mesoamérica Los horizontes que la componen son: arqueolítico, cenolítico inferior, cenolítico superior, protoneolítico, oasisamérica, aridoamérica, mesoamérica y los primeros contactos en el s. XVI: Planteamiento que se hace de esta manera para una mejor comprensión del curso y entender la evolución de los grupos asentados en territorio mexicano. 2.Fundamentación. Las área culturales del México Antiguo no solo se reduce a Mesoamérica como el período de máximo florecimiento que le antecedió a la conquista. En otros tiempos, antes de conocerse esta macroárea cultural, llegaron diversos grupos de cazadores-recolectores nómadas. El proceso evolutivo de estos grupos fue largo y lento, permitiendo avanzar e ir tocando diferentes niveles de desarrollo y los conocimientos necesarios para el cultivo y domesticación de las plantas como uno de los descubrimientos mas importantes durante esta fase que cambio el curso de la historia. Otra de las regiones es la llamada Oasisamérica localizada al sw de E.U. y norte de México, compuesta por grupos sedentarios agrícolas pero con una complejidad similar a la Mesoamericana. El área denominada mesoamérica, espacio donde interactuaron y se desarrollaron diversos grupos culturales, fue la “…sede de la mas alta civilización de la América precolombina. (Niederbeger, 11, 1996), se desarrollo en la mayor parte del territorio mexicano. Mesoamérica, definida así por Kirchhoff en 1943, es punto de referencia no solo para estudiosos del período prehispánico, en el convergen diversos especialistas amparados en diferentes corrientes ideológicas y enfoques: antropólogos, geógrafos prehistoriadores, historiadores, sociólogos, arquitectos, biólogos, sociólogos, por mencionar a algunos. -
The Americas and Oceania Ben06937.Ch21 538-563.Qxd 8/9/07 3:36 PM Page 539
ben06937.Ch21_538-563.qxd 8/9/07 3:36 PM Page 538 Worlds Apart: 21 The Americas and Oceania ben06937.Ch21_538-563.qxd 8/9/07 3:36 PM Page 539 States and Empires in Mesoamerica States and Empires in South America and North America The Coming of the Incas The Toltecs and the Mexica Inca Society and Religion Mexica Society Mexica Religion The Societies of Oceania Peoples and Societies of the North The Nomadic Foragers of Australia The Development of Pacific Island Societies In November 1519 a small Spanish army entered Tenochtitlan, capital city of the Aztec empire. The Spanish forces came in search of gold, and they had heard many reports about the wealth of the Aztec empire. Yet none of those reports prepared them adequately for what they saw. Years after the conquest of the Aztec empire, Bernal Díaz del Castillo, a soldier in the Span- ish army, described Tenochtitlan at its high point. The city itself sat in the water of Lake Tex- coco, connected to the surrounding land by three broad causeways, and as in Venice, canals allowed canoes to navigate to all parts of the city. The imperial palace included many large rooms and apartments. Its armory, well stocked with swords, lances, knives, bows, arrows, slings, armor, and shields, attracted Bernal Díaz’s professional attention. The aviary of Tenochti- tlan included eagles, hawks, parrots, and smaller birds in its collection, and jaguars, mountain lions, wolves, foxes, and rattlesnakes were noteworthy residents of the zoo. To Bernal Díaz the two most impressive sights were the markets and the temples of Te- nochtitlan. -
Texto Completo (Pdf)
LA FRONTERA CULTURAL MESO-ARIDOAMERICANA: CONSTRUCCIÓN DE IMAGINARIOS NACIONALISTAS EN LA HISTORIA MEXICANA MESO-ARIDOAMERICAN CULTURAL FRONTIER: CONSTRUCTION OF NATIONALIST IMAGINARIES IN MEXICAN HISTORY Adriana Gómez Aíza PhD en Análisis de Discurso por la Universidad de Essex. Profesora investigadora adscrita al Área Académica de Historia y Antropología, Instituto de Ciencias Sociales y Humanidades, Universidad Autónoma del Estado de Hidalgo. [email protected] Sergio Sánchez Vázquez Doctor en Antropología por la Escuela Nacional de Antropología e Historia. Profesor investigador adscrito al Área Académica de Historia y Antropología, Instituto de Ciencias Sociales y Humanidades, Universidad Autónoma del Estado de Hidalgo. [email protected] Nota. Una primera versión de este trabajo se presentó en la Memoria del VI Congreso de la Gran Chichimeca: 1-13. Instituto de Investigaciones Humanísticas, UASLP. México. 2007 Resumen La noción de frontera valida ciertas interpretaciones sobre la historia de una nación: lugar donde se nace y comparte con los demás una identidad, un modo de entenderse a sí mismo en relación con otros, con los que pertenecen a ese entorno y los que son ajenos o viven más allá de los confines que los dividen y separan. Aquí se discute la pertinencia de aplicar el término frontera cultural a la presunta división regional entre grupos sedentarios agrícolas mesoamericanos y grupos chichimecas seminómadas de los desiertos del actual norte de México. Para ello se aborda el papel jugado por Mesoamérica y la Gran Chichimeca en la conformación de imaginarios étnicos y nacionalistas, especialmente el nahua-centrismo impuesto por la conquista española, y la reivindicación del pasado prehispánico como constitutivo de la historia de México, enfatizando el contraste entre la reivindicación oficial del mestizaje a partir de la derrota militar de Tenochtitlán y la exégesis chicana que invoca su pasado en Aztlán, tierra mítica de origen de los mexicanos. -
Central Basin and Range Ecoregion
Status and Trends of Land Change in the Western United States—1973 to 2000 Edited by Benjamin M. Sleeter, Tamara S. Wilson, and William Acevedo U.S. Geological Survey Professional Paper 1794–A, 2012 Chapter 20 Central Basin and Range Ecoregion By Christopher E. Soulard This chapter has been modified from original material Wasatch and Uinta Mountains Ecoregion, on the north by the published in Soulard (2006), entitled “Land-cover trends of Northern Basin and Range and the Snake River Basin Ecore- the Central Basin and Range Ecoregion” (U.S. Geological gions, and on the south by the Mojave Basin and Range and Survey Scientific Investigations Report 2006–5288). the Colorado Plateaus Ecoregions (fig. 1). Most of the Central Basin and Range Ecoregion is located in Nevada (65.4 percent) and Utah (25.1 percent), but small segments are also located Ecoregion Description in Idaho (5.6 percent), California (3.7 percent), and Oregon (0.2 percent). Basin-and-range topography characterizes the The Central Basin and Range Ecoregion (Omernik, 1987; Central Basin and Range Ecoregion: wide desert valleys are U.S. Environmental Protection Agency, 1997) encompasses bordered by parallel mountain ranges generally oriented north- approximately 343,169 km² (132,498 mi2) of land bordered on south. There are more than 33 peaks within the Central Basin the west by the Sierra Nevada Ecoregion, on the east by the and Range Ecoregion that have summits higher than 3,000 m 120° 118° 116° 114° 112° EXPLANATION 42° Land-use/land-cover class Northern Basin ECSF Snake River Basin Water Forest and Range Developed Grassland/Shrubland Transitional Agriculture Mining Wetland MRK Barren Ice/Snow Ecoregion boundary 40° WB Sample block (10 x 10 km) 0 50 100 150 MILES 0 50 100 150 KILOMETERS WUM OREGON IDAHO bo um ld 38° H t R iver Ogden Sparks Reno 80 Sierra Truckee River Lockwood GREAT Tooele Nevada Salt Carson River Lake Walker RiverBASIN City Walker Lake SIERRA NEVADA CCV Mojave DESERT UTAH Basin and Range Colorado NEVADA 36° SCCCOW Plateaus SCM ANMP CALIFORNIA Figure 1. -
1 Sierra Front-Northwestern Great Basin Resource Advisory Council
Sierra Front-Northwestern Great Basin Resource Advisory Council Meeting Minutes March 5, 2019 ATTENDANCE BLM Jon Raby, Nevada State Director (By phone) Ester McCullough, Winnemucca District Manager Colleen Dulin, Carson City District Manager Heather O’Hanlan, Winnemucca Public Affairs Specialist Lisa Ross, Carson City Public Affairs Specialist and RAC Coordinator RAC Members: (Name, Employer, Representing, Notes) Matthew Gingerich, NV Energy, Transportation and Rights-of-Way (ROWs), RAC Chair Tim Dufurrena, Livestock Permittee, Grazing, returning RAC member Ben Veach, Civil Engineer, Environmental, transferred from Forest Service RAC Robert Jones, NDOW, State Agency Kyle Snyder, Ormat, Energy & Mineral Ron Kyle, (retired Forest Service), Public at Large Ken Tipton, Humboldt County Commissioner, Recreation Paul Scott, Sprint, ROWs John Ugalde, Livestock Permittee, Dispersed Recreation Pat Irwin, Public at Large (By phone) Jeanne Herman, Washoe County Commissioner, Elected Official (By phone) Non- RAC Members Present: Donovan Walker, Winnemucca District Fire Managing Officer David Kampwerth, Humboldt River Field Office Manager Mark Hall, Black Rock Field Office Manager James (Andy) Boerigter, Black Rock Field Office Assistant Field Manager Derek Messmer, Winnemucca District Fire Fuels Manager Garrett Swisher, Black Rock Field Office Wild Horse and Burro Specialist CALL TO ORDER 8:03 a.m. PUBLIC COMMENTS • Greg Hendricks, former WHB RAC member, shared information regarding Virginia Range fertility control program. They are finishing up the first year of this program and have applied fertility control to approximately 3,000 wild horses. This is the biggest fertility control program in the world. There is be a mini-documentary filming about the project at Patagonia Outlet Store in Reno on March 12, 2020, 7:00 pm. -
Ongoing Paleoclimatic Studies in the Northern Great Basin," Reno, Nevada, May 1993
CIRC. 1119 U.S. GEOLOGICAL SURVEY CIRCULAR 1119 Proceedings of the Workshop "Ongoing Paleoclimatic Studies in the Northern Great Basin," Reno, Nevada, May 1993 Proceedings of the Workshop "Ongoing Paleoclimatic Studies in the Northern Great Basin," Reno, Nevada, May 1993 Edited by Larry V. Benson U.S. GEOLOGICAL SURVEY CIRCULAR· 1119 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Government U.S. GOVERNMENT PRINTING OFFICE: 1996 Free on application to the U.S. Geological Survey Information Services Box 25286 Federal Center Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Workshop "Ongoing Paleoclimatic Studies in the Northern Great Basin" (1993: Reno, Nev.) Proceedings of the Workshop "Ongoing Paleoclimatic Studies in the Northern Great Basin," Reno, Nevada, May 1993/ edited by Larry V. Benson. p. em.- (U.S. Geological Survey circular; 1119) Includes index. 1. Paleoclimatology-Great Basin-congresses. 2. Great Basin-climate-Congresses. I. Benson, Larry V. II. Title. Ill. Series QC884.W67 1993 96-29329 551.6979-dc20 CIP PREFACE The workshop "'Ongoing Paleoclimatic Studies in the Northern Great Basin" was jointly sponsored by the U.S. Geological Smvey (USGS), the University ofNevada-Reno (UNR), and the Quaternary Sciences Center (QSC) of the Desert Research Institute, Reno, Nevada. W. Berry Lyons, chairman of the Hydrology Program (UNR), and Dale Ritter, head of the QSC, chaired the presentations. On May 16, Joseph Smoot, of the USGS, led a field trip along the Truckee River Canyon downstream from Wadsworth, Nevada. -
Reconstructing the History of Mesoamerican Populations Through the Study of the Mitochondrial DNA Control Region
Reconstructing the History of Mesoamerican Populations through the Study of the Mitochondrial DNA Control Region Amaya Gorostiza1,2,Vı´ctor Acunha-Alonzo3,Lucı´a Regalado-Liu1, Sergio Tirado1, Julio Granados4, David Sa´mano5,He´ctor Rangel-Villalobos6, Antonio Gonza´ lez-Martı´n1* 1 Department of Zoology and Physical Anthropology, Faculty of Biology, Complutense University of Madrid, Madrid, Spain, 2 Laboratorio de Identificacio´n Gene´tica, GENOMICA S.A.U. Grupo Zeltia, Madrid, Spain, 3 Laboratorio de Gene´tica Molecular, Escuela Nacional de Antropologı´a e Historia, Mexico City, Mexico, 4 Divisio´nde Immunogene´tica, Departamento de Trasplantes, Instituto Nacional de Ciencias Me´dicas y Nutricio´n Salvador Zubiran, Mexico City, Mexico, 5 Academia de Cultura Cientı´fica – Humanı´stica, Universidad Auto´noma del Estado de Me´xico, Mexico City, Mexico, 6 Instituto de Investigacio´n en Gene´tica Molecular, Centro Universitario de la Cie´naga, Universidad de Guadalajara, Ocotlan, Mexico Abstract The study of genetic information can reveal a reconstruction of human population’s history. We sequenced the entire mtDNA control region (positions 16.024 to 576 following Cambridge Reference Sequence, CRS) of 605 individuals from seven Mesoamerican indigenous groups and one Aridoamerican from the Greater Southwest previously defined, all of them in present Mexico. Samples were collected directly from the indigenous populations, the application of an individual survey made it possible to remove related or with other origins samples. Diversity indices and demographic estimates were calculated. Also AMOVAs were calculated according to different criteria. An MDS plot, based on FST distances, was also built. We carried out the construction of individual networks for the four Amerindian haplogroups detected.