The Magazine of Sutton Grammar School Geography
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Information on Natural Disasters Part- I Introduction
Information on Natural Disasters Part- I Introduction Astrology is the one that gave us the word ‘disaster’. Many believe that when the stars and planets are in malevolent position in our natal charts bad events or bad things would happen. Everyone one of us loves to avoid such bad things or disasters. The disaster is the impact of both natural and man-made events that influence our life and environment that surrounds us. Now as a general concept in academic circles, the disaster is a consequence of vulnerability and risk. The time often demands for appropriate reaction to face vulnerability and risk. The vulnerability is more in densely populated areas where if, a bad event strikes leads to greater damage, loss of life and is called as disaster. In other sparely populated area the bad event may only be a risk or hazard. Developing countries suffer the greatest costs when a disaster hits – more than 95 percent of all deaths caused by disasters occur in developing countries, and losses due to natural disasters are 20 times greater as a percentage of GDP in developing countries than in industrialized countries. A disaster can leads to financial, environmental, or human losses. The resulting loss depends on the capacity of the population to support or resist the disaster. The term natural has consequently been disputed because the events simply are not hazards or disasters without human involvement. Types of disasters Any disaster can be classified either as ‘Natural’ or ‘man-made’. The most common natural disasters that are known to the man kind are hailstorms, thunderstorm, very heavy snowfall, very heavy rainfalls, squalls, gale force winds, cyclones, heat and cold waves, earthquakes, volcanic eruptions, floods, and droughts which cause loss to property and life. -
Volcanic Gases
ManuscriptView metadata, citation and similar papers at core.ac.uk brought to you by CORE Click here to download Manuscript: Edmonds_Revised_final.docx provided by Apollo Click here to view linked References 1 Volcanic gases: silent killers 1 2 3 2 Marie Edmonds1, John Grattan2, Sabina Michnowicz3 4 5 6 3 1 University of Cambridge; 2 Aberystwyth University; 3 University College London 7 8 9 4 Abstract 10 11 5 Volcanic gases are insidious and often overlooked hazards. The effects of volcanic gases on life 12 13 6 may be direct, such as asphyxiation, respiratory diseases and skin burns; or indirect, e.g. regional 14 7 famine caused by the cooling that results from the presence of sulfate aerosols injected into the 15 16 8 stratosphere during explosive eruptions. Although accounting for fewer fatalities overall than some 17 18 9 other forms of volcanic hazards, history has shown that volcanic gases are implicated frequently in 1910 small-scale fatal events in diverse volcanic and geothermal regions. In order to mitigate risks due 20 2111 to volcanic gases, we must identify the challenges. The first relates to the difficulty of monitoring 22 2312 and hazard communication: gas concentrations may be elevated over large areas and may change 2413 rapidly with time. Developing alert and early warning systems that will be communicated in a timely 25 2614 fashion to the population is logistically difficult. The second challenge focuses on education and 27 2815 understanding risk. An effective response to warnings requires an educated population and a 2916 balanced weighing of conflicting cultural beliefs or economic interests with risk. -
Source to Surface Model of Monogenetic Volcanism: a Critical Review
Downloaded from http://sp.lyellcollection.org/ by guest on September 28, 2021 Source to surface model of monogenetic volcanism: a critical review I. E. M. SMITH1 &K.NE´ METH2* 1School of Environment, University of Auckland, Auckland, New Zealand 2Volcanic Risk Solutions, Massey University, Palmerston North 4442, New Zealand *Correspondence: [email protected] Abstract: Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas within a wide compositional range from strongly silica undersaturated to saturated and oversatu- rated; less commonly, the spectrum includes more siliceous compositions. Small-scale volcanic systems are commonly monogenetic in the sense that they are represented at the Earth’s surface by fields of small volcanoes, each the product of a temporally restricted eruption of a composition- ally distinct batch of magma, and this is in contrast to polygenetic systems characterized by rela- tively large edifices built by multiple eruptions over longer periods of time involving magmas with diverse origins. Eruption styles of small-scale volcanoes range from pyroclastic to effusive, and are strongly controlled by the relative influence of the characteristics of the magmatic system and the surface environment. Gold Open Access: This article is published under the terms of the CC-BY 3.0 license. Small-scale basaltic magmatic systems characteris- hazards associated with eruptions, and this is tically occur at the Earth’s surface as fields of small particularly true where volcanic fields are in close monogenetic volcanoes. These volcanoes are the proximity to population centres. -
Anatomy of a Volcanic Eruption: Case Study: Mt. St. Helens
Anatomy of a Volcanic Eruption: Case Study: Mt. St. Helens Materials Included in this Box: • Teacher Background Information • 3-D models of Mt. St. Helens (before and after eruption) • Examples of stratovolcano rock products: Tuff (pyroclastic flow), pumice, rhyolite/dacite, ash • Sandbox crater formation exercise • Laminated photos/diagrams Teacher Background There are several shapes and types of volcanoes around the world. Some volcanoes occur on the edges of tectonic plates, such as those along the ‘ring of fire’. But there are also volcanoes that occur in the middle of tectonic plates like the Yellowstone volcano and Kilauea volcano in Hawaii. When asked to draw a volcano most people will draw a steeply sided, conical mountain that has a depression (crater) at the top. This image of a 'typical' volcano is called a stratovolcano (a.k.a. composite volcano). While this is the often visualized image of a volcano, there are actually many different shapes volcanoes can be. A volcano's shape is mostly determined by the type of magma/lava that is created underneath it. Stratovolcanoes get their shape because of the thick, sticky (viscous) magma that forms at subduction zones. This magma/lava is layered between ash, pumice, and rock fragments. These layers of ash and magma will build into high elevation, steeply sided, conical shaped mountains and form a 'typical' volcano shape. Stratovolcanoes are also known for their explosive and destructive eruptions. Eruptions can cause clouds of gas, ash, dust, and rock fragments to eject into the atmosphere. These clouds of ash can become so dense and heavy that they quickly fall down the side of the volcanoes as a pyroclastic flow. -
Pyroclastic Flow Hazards
Pyroclastic Flow Hazards Lecture Objectives -definition and characteristics -generation of pyroclastic flows -impacts and hazards What are pyroclastic flows? Pyroclastic flows are high- density mixtures of hot, dry rock fragments and hot gases that move away from the vent that erupted them at high speeds. Generation Mechanisms: -explosive eruption of molten or solid rock fragments, or both. -non-explosive eruption of lava when parts of dome or a thick lava flow collapses down a steep slope. Most pyroclastic flows consist of two parts: a basal flow of coarse fragments that moves along the ground, and a turbulent cloud of ash that rises above the basal flow. Ash may fall from this cloud over a wide area downwind from the pyroclastic flow. Mt. St. Helens Effects of pyroclastic flows A pyroclastic flow will destroy nearly everything in its path. With rock fragments ranging in size from ash to boulders traveling across the ground at speeds typically greater than 80 km per hour, pyroclastic flows knock down, shatter, bury or carry away nearly all objects and structures in their way. The extreme temperatures of rocks and gas inside pyroclastic flows, generally between 200°C and 700°C, can cause combustible material to burn, especially petroleum products, wood, vegetation, and houses. Pyroclastic flows vary considerably in size and speed, but even relatively small flows that move <5 km from a volcano can destroy buildings, forests, and farmland. On the margins of pyroclastic flows, death and serious injury to people and animals may result from burns and inhalation of hot ash and gases. Pyroclastic flows generally follow valleys or other low-lying areas and, depending on the volume of rock debris carried by the flow, they can deposit layers of loose rock fragments to depths ranging from less than one meter to more than 200 m. -
Democratic Republic of the Congo | Mount Nyiragongo Eruption
Emergency Response Coordination Centre (ERCC) – DG ECHO Daily Map | 04/06/2021 Democratic Republic of the Congo | Mount Nyiragongo eruption CENTRAL SOUTH Nyiragongo volcano • On 2 June, ERCC received a request from DRC to COPERNICUS GRADING PRODUCT AFRICAN SUDAN REPUBLIC 3,470 m activate the EU Civil Protection Mechanism A started erupting on the (UCPM) following to the volcanic eruption in 22nd May 2021 Mount Nyiragongo and the related seismic GDACS activity. UGANDA Red alert • The request consists of food and non-food items, DEMOCRATIC WASH items, shelter, medicines and medical RWANDA REPUBLIC OF KENYA equipment. THE CONGO BURINDI • The European Commission has allocated emergency humanitarian funding of €2 million INDIAN OCEAN for those affected by the eruption. TANZANIA Source: DG ECHO Shaheru ZAMBIA adventive cone MALAWI 2,800 m Vent 1 COPERNICUS GRADING PRODUCT B Vent 2 Destination of population displacement 10,555 North xx Number of displaced people Kivu Source: UN-OCHA as of 31 May Roads A Vent 3 52,650 62,802 53,345 8,747 Rwerere 13,473 4,320 Humanitarian 3,011 situation overview 4,224 Source: UN OCHA as of 25 May, 26 May, 12,669 01 June 31 Fatalities B 232,433 Total displaced 4,758 people 40 1,879 Missing people Nyiragongo Main fault Damage assessment Source: GDACS, Virunga Volcanoes Source: GEM Source: Copernicus EMSR513 Volcanic vent Damaged waste water station Source: UNITAR-UNOSAT Volcanic fissure 1,276 Closed airport Source: UNITAR-UNOSAT ID3300, USGS Airport Destroyed residential Source: UNOCHA Lava flow Latest lava flow detection Urban area buildings 23-30 May as of 1 Jun South Kivu Source: HOTOSM 130 Source: Copernicus EMSR513, UNITAR-UNOSAT ID3300 Rubavu Copernicus grading product Administrative division Lake Possibly damaged Source: Copernicus EMSR513 Goma Country border Kivu residential buildings Destroyed building © European Union, 2021. -
The Science Behind Volcanoes
The Science Behind Volcanoes A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface. Volcanoes are generally found where tectonic plates are diverging or converging. A mid-oceanic ridge, for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by convergent tectonic plates coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust in the interiors of plates, e.g., in the East African Rift, the Wells Gray-Clearwater volcanic field and the Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "Plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so- called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere. -
Case Study Notes
Hazardous Earth: Sakurajima and Nyiragongo Volcano in a Developed Country: Sakurajima, Japan Sakurajima is a composite volcano (also called a stratovolcano) located in southern Japan. The volcano has been extremely active since the 1950s; some years, up to 200 eruptions have taken place! Sakurajima is on a convergent plate boundary, where the Pacific plate subducts beneath the Eurasian plate. (Source:www.flickr.com/photos/kimon/4506849144/) This type of plate boundary causes Sakurajima eruptions to be explosive, producing lots of ash, pyroclastic flows, volcanic bombs and poisonous gases. The lava is andesitic, which has a high gas content and is very viscous (thick). Japan is a developed country, with a GDP of 4.97 trillion USD (2018). Location of Sakurajima (orange icon). h Volcano in a Developing Country: Mount Nyiragongo, DRC Mount Nyiragongo is a composite volcano located in the east of the Democratic Republic of the Congo (DRC). The volcano consists of a huge (2km wide) crater usually filled with a lava lake, and is only 20km away from the city of Goma. Nyiragongo is currently classed as active (2020). (Source: wiki) Nyiragongo is on a divergent plate boundary: the African plate is being pulled apart into the Nubian plate (east) and Somali plate (west), causing lava to rise between. This results in non-explosive eruptions with basaltic lava which has a low viscosity (runny & fast-flowing - up to 37 mph). Location of Nyiragongo (orange icon). This work by PMThttps://bit.ly/pmt-edu-cc Education is licensed under https://bit.ly/pmt-ccCC BY-NC-ND 4.0 https://bit.ly/pmt-cc https://bit.ly/pmt-edu https://bit.ly/pmt-cc Impacts of Volcanoes in Contrasting Areas Impacts in Japan Developed country Primary impacts ● Around 30km3 of ash erupts from the volcano each year, damaging crops and electricity lines. -
Country Travel Risk Summaries
COUNTRY RISK SUMMARIES Powered by FocusPoint International, Inc. Report for Week Ending September 19, 2021 Latest Updates: Afghanistan, Burkina Faso, Cameroon, India, Israel, Mali, Mexico, Myanmar, Nigeria, Pakistan, Philippines, Russia, Saudi Arabia, Somalia, South Sudan, Sudan, Syria, Turkey, Ukraine and Yemen. ▪ Afghanistan: On September 14, thousands held a protest in Kandahar during afternoon hours local time to denounce a Taliban decision to evict residents in Firqa area. No further details were immediately available. ▪ Burkina Faso: On September 13, at least four people were killed and several others ijured after suspected Islamist militants ambushed a gendarme patrol escorting mining workers between Sakoani and Matiacoali in Est Region. Several gendarmes were missing following the attack. ▪ Cameroon: On September 14, at least seven soldiers were killed in clashes with separatist fighters in kikaikelaki, Northwest region. Another two soldiers were killed in an ambush in Chounghi on September 11. ▪ India: On September 16, at least six people were killed, including one each in Kendrapara and Subarnapur districts, and around 20,522 others evacuated, while 7,500 houses were damaged across Odisha state over the last three days, due to floods triggered by heavy rainfall. Disaster teams were sent to Balasore, Bhadrak and Kendrapara districts. Further floods were expected along the Mahanadi River and its tributaries. ▪ Israel: On September 13, at least two people were injured after being stabbed near Jerusalem Central Bus Station during afternoon hours local time. No further details were immediately available, but the assailant was shot dead by security forces. ▪ Mali: On September 13, at least five government soldiers and three Islamist militants were killed in clashes near Manidje in Kolongo commune, Macina cercle, Segou region, during morning hours local time. -
Recent Activity at Nyiragongo and Lava-Lake Occurrences
RECENT ACTIVITY AT NYIRAGONGO AND LAVA-LAKE OCCURRENCES HAROUN TAZIEFF TAZIEFF, HAROUN, 1985: Recent Activity at Nyiragongo and lava-lake occurrences. Bull. Geol. Soc. Finland 57, Part 1—2, 11—19. The behaviour of Nyiragongo, before and after its outbreak on January 10th, 1977, as compared with the behaviour of the other two volcanoes containing sub- permanent lava-lakes nowadays, Erta'Ale and Mount Erebus, suggests that the considerable convection necessary to feed such a lake with fresh magma can exist only if wide open fractures intersect at a given spot, thus creating a channel broad enough to allow such a convection. In contrast to Halemaumau, whose lava-lake vanished during the Kilauea eruption in 1924 and has still not reappeared, and Nyamlagira, whose lava-lake was drained out during its long (from 1938 to 1940) eruption, Mount Nyiragongo has resumed this exceptional type of activity a mere five years after its own lake was tapped off. The proposed hypothesis is that the January 1977 outbreak was a »passive» one whereas the 1924 and 1938 eruptions were »ac- tive». By active, we mean those which are due to a specific magma eruptivity, that is to say, vesiculation of the gaseous phase previously dissolved in the silicated melt. The outbreak on 10th January 1977 was passive in that both the lava-lake end the underlying magma were flowing out of the volcanic cone when the cone cracked not under its own magma pressure, which in fact had not yet reached vesicular eruptive maturity, but under the subjacent parental magma, pushing up both the Nyiragongo and Nyamlagira volcanoes from beneath. -
Preliminary Volcano-Hazard Assessment for Augustine Volcano, Alaska
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Preliminary Volcano-Hazard Assessment for Augustine Volcano, Alaska by Christopher F. Waythomas and Richard B. Waitt Open-File Report 98-106 This report is preliminary and subject to revision as new data become available. Any use of trade, product or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey Alaska Volcano Observatory Anchorage, Alaska 1998 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Thomas J. Casadevall, Acting Director For additional information: Copies of this report may be purchased from: U.S. Geological Survey U.S. Geological Survey Alaska Volcano Observatory Branch of Information Services 4200 University Drive Box 25286 Anchorage, AK 99508 Denver, CO 80225-0286 CONTENTS Summary of hazards at Augustine Volcano....................................... 1 Introduction ............................................................... 3 Purposeandscope ...................................................... 3 Physical setting of Augustine Volcano ...................................... 4 Relation to previous studies on Augustine hazards ............................. 5 Prehistoric eruptive history ................................................... 5 Historical eruptions ......................................................... 8 Hazardous phenomena at Augustine Volcano ..................................... 8 Volcanic hazards ....................................................... 12 Volcanicashclouds