GIS Professional Portfolio for William Thoman William M
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Human Health and Vulnerability in the Nyiragongo Volcano Crisis Democratic Republic of Congo 2002
Human Health and Vulnerability in the Nyiragongo Volcano Crisis Democratic Republic of Congo 2002 Final Report to the World Health Organisation Dr Peter J Baxter University of Cambridge Addenbrooke’s Hospital Cambridge, UK Dr Anne Ancia Emergency Co-ordinator World Health Organisation Goma Nyiragongo Volcano with Goma on the shore of Lake Kivu Cover : The main lava flow which shattered Goma and flowed into Lake Kivu Lava flows from the two active volcanoes CONGO RWANDA Sake Munigi Goma Lake Kivu Gisenyi Fig.1. Goma setting and map of area and lava flows HUMAN HEALTH AND VULNERABILITY IN THE NYIRAGONGO VOLCANO CRISIS DEMOCRATIC REPUBLIC OF CONGO, 2002 FINAL REPORT TO THE WORLD HEALTH ORGANISATION Dr Peter J Baxter University of Cambridge Addenbrooke’s Hospital Cambridge, UK Dr Anne Ancia Emergency Co-ordinator World Health Organisation Goma June 2002 1 EXECUTIVE SUMMARY We have undertaken a vulnerability assessment of the Nyiragongo volcano crisis at Goma for the World Health Organisation (WHO), based on an analysis of the impact of the eruption on January 17/18, 2002. According to volcanologists, this eruption was triggered by tectonic spreading of the Kivu rift causing the ground to fracture and allow lava to flow from ground fissures out of the crater lava lake and possibly from a deeper conduit nearer Goma. At the time of writing, scientists are concerned that the continuing high level of seismic activity indi- cates that the tectonic rifting may be gradually continuing. Scientists agree that volcano monitoring and contingency planning are essential for forecasting and responding to fu- ture trends. The relatively small loss of life in the January 2002 eruption (less than 100 deaths in a population of 500,000) was remarkable, and psychological stress was reportedly the main health consequence in the aftermath of the eruption. -
Volcanic Gases and Aerosols Guidelines Introduction
IVHHN Gas Guidelines www.ivhhn.org/gas/guidelines.html Volcanic Gases and Aerosols Guidelines The following pages contain information relating to the health hazards of gases and aerosols typically emitted during volcanic activity. Each section outlines the properties of the emission; its impacts on health; international guidelines for concentrations; and examples of concentrations and effects in volcanic contexts, including casualties. Before looking at the emissions data, we recommend that you read the general introduction to volcanic gases and aerosols first. A glossary to some of the terms used in the explanations and guidelines is also provided at the end of this document. Introduction An introduction to the aims and purpose of the Gas and Aerosol Guidelines is given here, as well as further information on international guideline levels and the units used in the website. A brief review of safety procedures currently implemented by volcanologists and volcano observatories is also provided. General Introduction Gas and aerosol hazards are associated with all volcanic activity, from diffuse soil gas emissions to 2- plinian eruptions. The volcanic emissions of most concern are SO2, HF, sulphate (SO4 ), CO2, HCl and H2S, although, there are other volcanic volatile species that may have human health implications, including mercury and other metals. Since 1900, there have been at least 62 serious volcanic-gas related incidents. Of these, the gas-outburst at Lake Nyos in 1986 was the most disastrous, causing 1746 deaths, >845 injuries and the evacuation of 4430 people. Other volcanic-gas related incidents have been responsible for more than 280 deaths and 1120 injuries, and contributed to the evacuation or ill health of >53,700 people (Witham, in review). -
Annual Report 2011
Annual Report 2011 © RMCA www.africamuseum.be Foreword 2 Foreword The Royal Museum for Central Africa (RMCA) pub- and culture exhibition was extended, while RMCA lishes a beautiful and richly illustrated annual collection pieces were admired in more than 20 report in book form every two years. In intervening major exhibitions held in different parts of the years – such as 2011 – we publish a digital edition globe. Nearly 30,000 children attended our edu- that is available on our website, and for which a cational workshops or school activities, while our hard copy can be produced on demand. Despite colla boration with African communities became its size, the report is not exhaustive. Rather, it more streamlined. We felt a pang of regret at the seeks to provide the most varied overview pos- departure of ‘our’ elephants in 2011. After grac- sible of our many museum-related, educational, ing our museum’s entrance for three years, the scientific, and other activities on the national and 9 pachyderms that formed the work created by international scene. The long governmental crisis South African artist Andries Botha, You can buy my of 2011 notwithstanding, RMCA was highly pro- heart and my soul, left Tervuren Park for good. ductive and remains one of the most important Africa-focused research institutions, particularly 2011 was also a fruitful year in terms of scientific for Central Africa. research. To highlight the multidisciplinary nature that is the strength of our institution, we organ- As with the previous year, the renovation was one ized ‘Science Days’ for the first time. -
Carbon Dioxide - Wikipedia
5/20/2020 Carbon dioxide - Wikipedia Carbon dioxide Carbon dioxide (chemical formula CO2) is a colorless gas with Carbon dioxide a density about 60% higher than that of dry air. Carbon dioxide consists of a carbon atom covalently double bonded to two oxygen atoms. It occurs naturally in Earth's atmosphere as a trace gas. The current concentration is about 0.04% (412 ppm) by volume, having risen from pre-industrial levels of 280 ppm.[8] Natural sources include volcanoes, hot springs and geysers, and it is freed from carbonate rocks by dissolution in water and acids. Because carbon dioxide is soluble in water, it occurs naturally in groundwater, rivers and lakes, ice caps, glaciers and seawater. It is present in deposits of petroleum and natural gas. Carbon dioxide is odorless at normally encountered concentrations, but at high concentrations, it has a sharp and acidic odor.[1] At such Names concentrations it generates the taste of soda water in the Other names [9] mouth. Carbonic acid gas As the source of available carbon in the carbon cycle, atmospheric Carbonic anhydride carbon dioxide is the primary carbon source for life on Earth and Carbonic oxide its concentration in Earth's pre-industrial atmosphere since late Carbon oxide in the Precambrian has been regulated by photosynthetic organisms and geological phenomena. Plants, algae and Carbon(IV) oxide cyanobacteria use light energy to photosynthesize carbohydrate Dry ice (solid phase) from carbon dioxide and water, with oxygen produced as a waste Identifiers product.[10] CAS Number 124-38-9 (http://ww w.commonchemistr CO2 is produced by all aerobic organisms when they metabolize carbohydrates and lipids to produce energy by respiration.[11] It is y.org/ChemicalDeta returned to water via the gills of fish and to the air via the lungs of il.aspx?ref=124-38- air-breathing land animals, including humans. -
“Virunga Volcanoes Supersite” Abstract
www.earthobservations.org/gsnl.php GSNL Proposal for Permanent Supersite A.1. Proposal Title: “Virunga Volcanoes Supersite” Abstract: The Virunga region is situated between Lake Kivu and Lake Edward in Eastern Africa, on the border of Democratic Republic of the Congo (RDC), Uganda and Rwanda. The Virunga is characterized with very fertile mountainous lands under a tropical climate were live millions of people grouped in cities and villages, and is additionally home for several unique wild animals such as the famous mountain gorillas. On the other hand, the Virunga is located in the western branch of the East African Rift System, and is thus prey to tectonic forces that are presently splitting apart the African plate. The rifting movements yielded the formation of Africa’s great lakes, among which the methane (CH4) and carbon dioxide (CO2)-rich Lake Kivu, and resulted in the highly active volcanoes whose most eruptions are initiated by the rift opening. The inhabitants of Virunga villages and cities (e.g. Goma in RDC and Gisenyi in Rwanda; ~ 1.5 million inhabitants) neighboring Nyiragongo and Nyamulagira active volcanoes and Lake Kivu live in a highly hazardous area. These populations are in fact permanently threatened by lava flows from the two volcanoes, and by a possible explosion of Lake Kivu that could release ~300 3 3 km CO2 and 60 km of CH4 dissolved in its deep waters. Such an explosion of Lake Kivu could be a regional catastrophe as it would affect the ~3 million people living in the catchment of the lake. Goma city and the surroundings have been many times affected by volcanic products. -
Playoff R Ound 1
circle circle Score Halftime P1 Round 20 . 19 18 17 16 Room 15 14 13 12 11 10 9 8 Scorer 7 6 Make sure to placescores in thecolumn for the questioncorrect 5 4 3 2 1 ifno change. score ) International Geography Bee: Playoff Round 1 Round Playoff Bee: Geography International include school and For correct placeanswers, running totalnew in student’s for row the corresponding question. For negatives, place running total and Cross Cross out entire column full name Moderator . Student names ( Tournament INSTRUCTIONS: SCORING: it circle circle Score Halftime P1 Round 20 . 19 18 17 16 Room 15 14 13 12 11 10 9 8 Scorer 7 6 Make sure to placescores in thecolumn for the questioncorrect 5 4 3 2 1 ifno change. score ) International Geography Bee: Playoff Round 1 Round Playoff Bee: Geography International include school and For correct placeanswers, running totalnew in student’s for row the corresponding question. For negatives, place running total and Cross Cross out entire column full name Moderator . Student names ( Tournament INSTRUCTIONS: SCORING: it 2018 International Geography Bee US Varsity & Junior Varsity National Championships SEMIFINALS 1. This lake’s primary inflows include the Alamo River and the heavily polluted Rio Nuevo or New River. This body of water’s tourism potential led it to be nicknamed the “New Mediterranean” in the 1950s and Desert Shores is on the western side of this body of water. The southernmost sighting of Ross’ gull, an Arctic bird species, was found on this endorheic lake known for its diverse birdlife. The Whitewater River flows into this body of water as it passes through Riverside County. -
Emergency and Disaster Reports 2014; 1 (4): 3-60 Emergency and Disaster Reports
Emergency and Disaster Reports 2014; 1 (4): 3-60 Emergency and Disaster Reports ISSN 2340-9932 Vol 1, Num 4, 2014 Monographic issue Disasters in North Kivu Province, Democratic Republic of Congo Piia Laitiainen University of Oviedo – Department of Medicine Unit for Research in Emergency and Disaster Emergency and Disaster Reports 2014; 1 (4): 1-47 Letter from the editors The Emergency and Disaster Reports is a journal edited by the Unit for Research in Emergency and Disaster of the Department of Medicine of the University of Oviedo aimed to introduce research papers, monographic reviews and technical reports related to the fields of Medicine and Public Health in the contexts of emergency and disaster. Both situations are events that can deeply affect the health, the economy, the environment and the development of the affected populations. The topics covered by the journal include a wide range of issues related to the different dimensions of the phenomena of emergency and disaster, ranging from the study of the risk factors, patterns of frequency and distribution, characteristics, impacts, prevention, preparedness, mitigation, response, humanitarian aid, standards of intervention, operative research, recovery, rehabilitation, resilience and policies, strategies and actions to address these phenomena from a risk reduction approach. In the last thirty years has been substantial progress in all the above mentioned areas, in part thanks to a better scientific knowledge of the subject. The aim of the journal is to contribute to this progress facilitating the dissemination of the results of research in this field. This issue covers the long-lasting conflict in North Kivu (Democratic Republic of Congo) a small province but with strategic importance due to its location on the border with Rwanda and Uganda. -
Zitierte Sowie Weiterführende Literatur
Zitierte sowie weiterführende Literatur Aeschbach-Hertig W, Kipfer R, Hofer M, Imboden DM, Wieler R, Signer P (1996) Quantifcation of gas fuxes from the sub continental mantle: the example of Laacher See, a maar lake in Germany. Geochim Cosmochim Acta 60:31–41 Ahrens W (1930) Geologisches Wanderbuch durch das Vulkangebiet des Laacher Sees in der Eifel. Enke, Stuttgart Albinus L (2000) Te house of Hades. Studies in ancient Greek eschatology. Aarhus University Press, Aarhus Albricus Philosophus (1742) De deorum imaginibus libellus. Chapter VI: De Plutoe Alighieri D (2001) Die göttliche Komödie. Hölle. Faber und Faber, Leipzig Allan SA (2010) Chemical ecology of tick-host interactions. In: Takken W, Knols BGJ (Hrsg) Ecology and control of vector-borne diseases. Bd 2. Olfac- tion in vector-host interactions. Wageningen Academic, S 327–348 Altunel E, Barka A (1996) Hierapolis’teki arkeosismik hasarların değerlendirilmesi (evaluation of archaeoseismic damages at Hierapolis). Türkiye Jeoloji Bülteni (Geol Bull Turk) 39:56–74 Andreas H (1926) Aus der Pfanzenwelt des Laacher Sees. In: Zepp P (Hrsg) Die Laacher Landschaft – Stimmen zu ihrer Erhaltung. Nat Heim 1:65–81 Anonymus (1869) Erklärendes Wörterbuch der im Bergbau in der Hüttenkunde und in Salinenwerken vorkommenden technischen und in Salinenwerken vor- kommenden technischen Kunstausdrücke und Fremdwörter. Verlag der Falken- berg’schen Buchhandlung, Burgsteinfurt Apollodorus (2008) Götter- und Heldensagen. Deutsch von Christian Gottlob Moser und Dorothea Vollbach. Anaconda, Köln Appoloni S, Lekberg Y, Tercek MT, Zabinski CA, Redecker D (2008) Molecular community analysis of arbuscular mycorrhizal fungi in roots of geothermal soils in yellowstone national park (USA). Microb Ecol 56:649–659 © Springer-Verlag GmbH Deutschland, ein Teil von Springer Nature 2019 191 H. -
United States Department of the Interior Geological Survey
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY NATURAL HAZARDS ASSOCIATED WITH LAKE KIVU AND ADJOINING AREAS OF THE BIRUNGA VOLCANIC FIELD, RWANDA AND ZAIRE, CENTRAL AFRICA FINAL REPORT By Michele L. Tuttle1 , John P. Lockwood2 , and William C. Evans3 U.S. Geological Survey Denver, Colorado, 2Volcano, Hawaii, 3Menlo Park, California Open File Report 90-691 1990 with partial funding from the Office of Foreign Disaster Assistance of the U.S. Agency for International Development This report is preliminary and has not been edited or reviewed for conformity with Geological Survey standards or nomenclature. Use of brand names in this report does not imply endorsement by the U.S. Geological Survey. TABLE OF CONTENTS Executive Summary .............................................. 1 Introduction ................................................... 2 Regional Geography and Geologic History................... 2 Background................................................ 2 Locations Studied and Sampled.................................. 3 Lakes and Springs ......................................... 3 Mazuku (Terrestrial Gas Vents) ............................ 3 Volcanic Rock and Charcoal................................ 4 Water and Gas Geochemistry ..................................... 4 Results................................................... 4 Water Temperature ................................... 4 Water Chemistry ..................................... 5 Gas Chemistry ....................................... 6 Implications of Lake Kivu -
Lake-Level Rise in the Late Pleistocene and Active Subaquatic Volcanism Since the Holocene in Lake Kivu, East African Rift
Geomorphology 221 (2014) 274–285 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Lake-level rise in the late Pleistocene and active subaquatic volcanism since the Holocene in Lake Kivu, East African Rift Kelly Ann Ross a,b,⁎, Benoît Smets c,d,e,MarcDeBatistf, Michael Hilbe a,b,g, Martin Schmid a, Flavio S. Anselmetti g a Department of Surface Waters Research and Management, Eawag: Swiss Federal Institute of Aquatic Science and Technology, Switzerland b Institute of Biogeochemistry and Pollutant Dynamics, ETH: Swiss Federal Institute of Technology, Switzerland c European Center for Geodynamics and Seismology, Luxembourg d Department of Geography, Vrije Universiteit Brussel, Belgium e Department of Earth Sciences, Royal Museum for Central Africa, Belgium f Renard Centre of Marine Geology, Department of Geology and Soil Science, Ghent University, Belgium g Institute of Geological Sciences and Oeschger Centre for Climate Change Research, University of Bern, Switzerland article info abstract Article history: The history of Lake Kivu is strongly linked to the activity of the Virunga volcanoes. Subaerial and subaquatic Received 25 July 2013 volcanoes, in addition to lake-level changes, shape the subaquatic morphologic and structural features in Lake Received in revised form 23 April 2014 Kivu's Main Basin. Previous studies revealed that volcanic eruptions blocked the former outlet of the lake to Accepted 11 May 2014 the north in the late Pleistocene, leading to a substantial rise in the lake level and subsequently the present- Available online 2 June 2014 day thermohaline stratification. Additional studies have speculated that volcanic and seismic activities threaten to trigger a catastrophic release of the large amount of gases dissolved in the lake. -
2018 IGB Canadian Championships – Finals
2018 International Geography Bee Canadian National Championships FINALS 1. This lake’s primary inflows include the Alamo River and the heavily polluted Rio Nuevo or New River. This body of water’s tourism potential led it to be nicknamed the “New Mediterranean” in the 1950s and Desert Shores is on the western side of this body of water. The southernmost sighting of Ross’ gull, an Arctic bird species, was found on this endorheic lake known for its diverse birdlife. The Whitewater River flows into this body of water as it passes through Riverside County. Formed accidentally after the flooding of the Colorado River, this body of water marks boundaries of the Coachella Valley and the Imperial Valley. For the point, name this lake that is the largest entirely in California. ANSWER: Salton Sea 2. This company’s Astro 430 was built specifically to track dogs. Garry Burrell and Min Kao co-founded this company headquartered in Lenexa, Kansas. Though not Fitbit, this company sells a wristwatch that monitors sleep and physical movement known as the Vivofit. Along with Asus, this company designed a hands-free version of its main technology known as Nuvifone. Originally named ProNav, this company’s StreetPilot was one of its first products used in automobiles. For the point, name this company known for its GPS technology. ANSWER: Garmin 3. This city’s Zarechnaya metro station is allegedly haunted by the ghosts of laborers who died while working on it. The Fedorovsky Embankment is home to many walking tours in this city that is served by Strigino International Airport.