GEOS 424/624 Course Description
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Alaska Interagency Operating Plan for Volcanic Ash Episodes
Alaska Interagency Operating Plan for Volcanic Ash Episodes MAY 1, 2008 Cover: A plume of volcanic gas and water vapor rises above the summit crater and growing lava dome at Augustine Volcano in southern Cook Inlet. A mantle of light brown ash discolors the snow on the upper flanks. View is towards the southwest. Photograph taken by C. Read, U.S. Geological Survey, January 24, 2006. Alaska Volcano Observatory database image from http://www.avo.alaska.edu/image.php?id=7051. Alaska Interagency Operating Plan for Volcanic Ash Episodes May 1, 2008 Table of Contents 1.0 Introduction ............................................................................................................... 3 1.1 Integrated Response to Volcanic Ash ....................................................................... 3 1.2 Data Collection and Processing ................................................................................ 4 1.3 Information Management and Coordination .............................................................. 4 1.4 Distribution and Dissemination.................................................................................. 5 2.0 Responsibilities of the Participating Agencies ........................................................... 5 2.1 ALASKA DIVISION OF HOMELAND SECURITY AND EMERGENCY MANAGEMENT (DHS&EM) .............................................................................. 5 2.2 ALASKA VOLCANO OBSERVATORY (AVO)........................................................... 6 2.2.1 Organization..................................................................................................... -
Volcanic Arc of Kamchatka: a Province with High-␦18O Magma Sources and Large-Scale 18O/16O Depletion of the Upper Crust
Geochimica et Cosmochimica Acta, Vol. 68, No. 4, pp. 841–865, 2004 Copyright © 2004 Elsevier Ltd Pergamon Printed in the USA. All rights reserved 0016-7037/04 $30.00 ϩ .00 doi:10.1016/j.gca.2003.07.009 Volcanic arc of Kamchatka: a province with high-␦18O magma sources and large-scale 18O/16O depletion of the upper crust 1, 2 3 1 ILYA N. BINDEMAN, *VERA V. PONOMAREVA, JOHN C. BAILEY, and JOHN W. VALLEY 1Department of Geology and Geophysics, University of Wisconsin, Madison, WI, USA 2Institute of Volcanic Geology and Geochemistry, Petropavlovsk-Kamchatsky, Russia 3Geologisk Institut, University of Copenhagen, Copenhagen, Denmark (Received March 20, 2003; accepted in revised form July 16, 2003) Abstract—We present the results of a regional study of oxygen and Sr-Nd-Pb isotopes of Pleistocene to Recent arc volcanism in the Kamchatka Peninsula and the Kuriles, with emphasis on the largest caldera- forming centers. The ␦18O values of phenocrysts, in combination with numerical crystallization modeling (MELTS) and experimental fractionation factors, are used to derive best estimates of primary values for ␦18O(magma). Magmatic ␦18O values span 3.5‰ and are correlated with whole-rock Sr-Nd-Pb isotopes and major elements. Our data show that Kamchatka is a region of isotopic diversity with high-␦18O basaltic magmas (sampling mantle to lower crustal high-␦18O sources), and low-␦18O silicic volcanism (sampling low-␦18O upper crust). Among one hundred Holocene and Late Pleistocene eruptive units from 23 volcanic centers, one half represents low-␦18O magmas (ϩ4 to 5‰). Most low-␦ 18O magmas are voluminous silicic ignimbrites related to large Ͼ10 km3 caldera-forming eruptions and subsequent intracaldera lavas and domes: Holocene multi-caldera Ksudach volcano, Karymsky and Kurile Lake-Iliinsky calderas, and Late Pleistocene Maly Semyachik, Akademy Nauk, and Uzon calderas. -
The Active Volcanoes of Kamchatka and Paramushir Island, North Kurils in 2007 O
ISSN 0742-0463, Journal of Volcanology and Seismology, 2009, Vol. 3, No. 1, pp. 1–17. © Pleiades Publishing, Ltd., 2009. Original Russian Text © O.A. Girina, S.V. Ushakov, N.A. Malik, A.G. Manevich, D.V. Mel’nikov, A.A. Nuzhdaev, Yu.V. Demyanchuk, L.V. Kotenko, 2009, published in Vul- kanologiya i Seismologiya, 2009, No. 1, pp. 3–20. The Active Volcanoes of Kamchatka and Paramushir Island, North Kurils in 2007 O. A. Girina, S. V. Ushakov, N. A. Malik, A. G. Manevich, D. V. Mel’nikov, A. A. Nuzhdaev, Yu. V. Demyanchuk, and L. V. Kotenko Institute of Volcanology and Seismology of the Far East Division of the Russian Academy of Sciences, 9 Piipa Boulevard, Petropavlovsk-Kamchatskii, 683006 Russia Received March 6, 2008 Abstract—Eight strong eruptions of four Kamchatka volcanoes (Bezymyannyi, Klyuchevskoi, Shiveluch, and Karymskii) and Chikurachki Volcano on Paramushir Island, North Kurils took place in 2007. In addition, an explosive event occurred on Mutnovskii Volcano and increased fumarole activity was recorded on Avacha and Gorelyi volcanoes in Kamchatka and Ebeko Volcano on Paramushir Island, North Kurils. Thanks to close coop- eration with colleagues involved in the Kamchatkan Volcanic Eruption Response Team (KVERT) project from the Elizovo Airport Meteorological Center and volcanic ash advisory centers in Tokyo, Anchorage, and Wash- ington (Tokyo VAAC, Anchorage VAAC, and Washington VAAC), all necessary precautions were taken for flight safety near Kamchatka. DOI: 10.1134/S0742046309010011 INTRODUCTION two months in 2005–2006 the volcano remained rela- tively quiet, up to December 4, 2006. The extrusive– The comprehensive monitoring of active volcanoes explosive eruption of Molodoi (Young) Shiveluch Vol- in Kamchatka and North Kurils is carried out under the cano commenced on that date, with a strong ash ejec- KVERT project [2, 4, 5] in close cooperation with col- tion, and continued during all of 2007. -
Priority Pass Lounge Directory
Content correct as of 24 September 2021 Priority Pass™ Lounge Directory This PDF Lounge Directory details all the lounges in the Priority Pass program – more than 1200 in total, covering over 400 airports around the world. Priority Pass is the world's leading independent lounge program, making membership a must for any frequent traveler. As a Priority Pass member, wherever you travel, you can be sure that you'll experience outstanding standards of comfort and service – a world away from chaotic airport terminals. Do some business. Catch up with calls. Send a few emails. Browse through a favorite magazine. Enjoy refreshments of your choice. Or simply indulge yourself by doing nothing at all. You can use the Priority Pass lounges as detailed in this directory, regardless of your choice of airline, class of ticket or membership in any frequent flyer club. Just be sure to take your Priority Pass membership card with you wherever you travel in order to gain access to participating lounges. Enjoy your visit! For the most up-to-date lounge information and full Priority Pass Conditions of Use, visit our website at prioritypass.com © Priority Pass Ltd 2021. Opening times and availability of facilities may be subject to change. Admittance to the lounges is conditional upon presentation of a valid Priority Pass card only. Page 2 of 473 Content correct as of 24 September 2021 Facility Symbols Air Conditioning Conference Facilities Digital Membership Card Digital Membership Card Unavailable Disabled Access Fax Flight Information Monitor Internet/Dataport Newspapers/Magazines Refreshments (Alcoholic) Refreshments (Soft Drinks) Shower Facilities Telephone Television Wi-fi © Priority Pass Ltd 2021. -
EVENT PASSPORT of the REGION KAMCHATKA Portrait of the Region: a Few Facts
Kamchatka and salmon caviar are virtually inseparable. This gourmet product has long become the brand of the region, along with volcanoes and geysers. The Geyser Valley on Kamchatka is one of the largest in the whole world. It was recognized by nationwide vote as one of the seven wonders of Russia. EVENT PASSPORT OF THE REGION KAMCHATKA Portrait of the Region: A Few Facts Kamchatka is the most remote region from the central part of the country, the area with pristine nature and a very small population. This is the land of volcanoes, geysers and bears. The natural volcano landscape in Kamchatka was included in the UNESCO World Heritage List. FISHING SHOP KAMCHATKA EXHIBITION OF RUSSIA AND INVESTMENT CENTER The fishing industry is the main ● Area: exhibition and congress halls: Largest events link in the economic structure of 600 and 400 m2. at the venue: Kamchatka Krai. In addition to fishing, processing fish, studying fish and fish ● Number of venues: 2 exhibition farming sectors, the local economy and congress halls, a conference ● Kamchatka Forum of Entrepre- includes a number of auxiliary and hall: 80 sq. m, seating 70 people, neurs (November 26–28, 2018). service sectors, as well as institutions 2 meeting rooms. of manufacturing and social ● Total capacity of two halls and ● Architectural exposition, exhibition infrastructure. The most important meeting rooms: up to 500 people. “Your Home 2018.” of those are ship repair, construction, transport, storage and transshipment ● Distance to the city’s historic ● Kamchatka Business Strategy and of fish products. downtown area: 11 km. Management Cup. LEADING ECONOMY SECTORS Fishing Minerals and Energy Tourism Agriculture and fish other natural farming Resources PLANNING BRIGHTEST WEATHER IN A VISIT IMPRESSIONS PETROPAVLOVSK- Visit the unique Kronotsky Nature KAMCHATSKY Accessibility Reserve—the caldera of Uzon Volcano and one of seven wonders of Russia, Elizovo Airport is the main arrival the Valley of Geysers. -
Airport Lounge List
Dreamfolks Membership Programme: Airport Lounge List Last updated on 21th Jan, 2021 S.No Country City Region Airport Name Lounge Name Terminal United Arab Middle International 1 Dubai Dubai International Marhaba Lounge Emirates East Departure Terminal 3 United Arab Middle International 2 Dubai Dubai International Marhaba lounge Emirates East Departure Terminal 1 United Arab Middle International 3 Dubai Dubai International Marhaba Lounge (T2) Emirates East Departure Terminal 2 South 4 Singapore Singapore Singapore Changi International SATS Premier Lounge (T2) Terminal 2 East Asia South 5 Singapore Singapore Singapore Changi International SATS Premier Lounge Terminal 3 East Asia South Miracle First Class 6 Thailand Bangkok Bangkok Suvarnabhumi International International East Asia Lounge(Concourse A - Level 3) International United Arab Middle Miracle First Class 7 Dubai Dubai International Airport-DXB Departure Terminal 3 Emirates East Lounge(Concourse A - Level 3) Concourse B Middle Miracle First Class 8 Qatar Doha Doha Hamad International International East Lounge(Concourse A - Level 3) South Miracle First Class International 9 Thailand Bangkok Suvarnabhumi International Airport East Asia Lounge(Concourse A - Level 3) Departures International South Miracle First Class 10 Sri Lanka Colombo Bandaranaike International Airport Departure Main East Asia Lounge(Concourse A - Level 3) Terminal South Miracle First Class 11 Thailand Bangkok Bangkok Don Mueang International Terminal 1 East Asia Lounge(Concourse A - Level 3) South Miracle First Class -
Water-Methane Geothermal Reservoirs in a South-West Foothills of Koryaksky Volcano, Kamchatka
PROCEEDINGS, 46th Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 15-17, 2021 SGP-TR-218 Water-Methane Geothermal Reservoirs in a South-West Foothills of Koryaksky Volcano, Kamchatka Alexey Kiryukhin1, Pavel Voronin1, Nikita Zhuravlev1, Galina Kopylova2 1 - Institute of Volcanology & Seismology FEB RAS, Piip 9, Petropavlovsk-Kamchatsky, Russia, 683006, 2 - Kamchatka Branch of the Geophysical Survey of the Russian Academy of Sciences (KB GS RAS) [email protected] Keywords: Geothermal, Kamchatka, Magma, Fracking, Production, Faults, Reservoirs, Volcanoes ABSTRACT The Ketkinsky geothermal reservoirs appears to be the product of magma and water injection from the Koryaksky volcano. Actual thermal supply may be carried out by magma injections in the form of sills in the depth range of -6 to -3 km abs. from the SW sector of the Koryaksky volcano. Water supply according to the isotopic composition of water is mixed: it is carried out through the structure of the Koryaksky volcano from above 2 km abs. and at the expense magmatic fluids. The system of the identified productive faults and magma fracking system is geometrically conjugated through some of the existing faults. Well E1 located above of the magma- hydrothermal connection above mentioned demonstrates water level change sensitivity to magma fracking events of Koryaksky volcano 2008-2009. Thus, Ketkinsky geothermal field appears to be the product of magma and water injection from the Koryaksky volcano. 1. INTRODUCTION The Avachinsko-Koryaksky volcanogenic basin with an area of 2530 km2 includes 5 quaternary volcanoes (2 of which Avachinsky (2750 m abs) and Koryaksky (3456 m abs) are active), sub-basins of volcanogenic-sedimentary Neogene-Quaternary deposits up to 1.4 km thick (Fig. -
Kamchatka Oblast Pressure Are Common
By Newell and Zhou / Sources: Ministry of Natural Resources, 2002; ESRI, 2002. KORYAKIA UST-KAMCHATSKY Krutoberegovo Klyuchi Ust-Kamchatsk ! ! Maiskoe Anavgai Kozyrevsk Esso Krapivnaya Atlasovo ALEUTSKY C o m m BYSTRINSKY MILKOVSKY a n d e r I s l a Dolinovka n d s Kurilskoe Lake Krutogorovsky Kirganik Milkovo Sharomy SOBOLEVSKY Sobolevo Kirovsky ELIZOVSKY N Ganaly A Malki Koryaki E Elizovo Dalny !. C Paratunka P! Apacha PETROPAVLOVSK-KAMCHATSKY O Ust-Bolsheretsk UST-BOLSHERETSKY C Bolsheretsk I F I Map 10.1 C A Kamchatka Oblast Ozernovsky P 70,800 sq. km ¯ km 100 Russian Far East KAMCHATKA 340 Ⅲ THE RUSSIAN FAR EAST Newell, J. 2004. The Russian Far East: A Reference Guide for Conservation and Development. McKinleyville, CA: Daniel & Daniel. 466 pages CHAPTER 10 Kamchatka Oblast Location Kamchatka Oblast makes up the southern portion of the Kamchatka peninsula, which is located in northeastern rfe. It is washed by the Pacifi c Ocean and Bering Strait to the east and the Sea of Okhotsk to the west. To the north, the oblast borders the Koryak Autonomous Okrug, which covers the northern section of the peninsula. Kamchatka also includes the Komandorskie (Commander) Islands within its administrative territory. Size 70,800 sq. km (17.2 million ha). Climate The infl uence of the Pacifi c Ocean and the Sea of Okhotsk makes Kamchatka’s climate milder than continental parts of the rfe. In general, winters are long with heavy snows, and summers are short, cool, and rainy. Heavy fog and sudden changes in atmospheric pressure are common. Annual precipitation is 50–100 cm, with average temperatures ranging from –11°c in February to 14°c in July.1 Geography and ecology Located on the Pacifi c Rim of Fire, Kamchatka has 29 active volcanoes, 186 geysers, countless boiling mud cauldrons, steam vents, fumaroles, and other forms of volcanic ac- tivity. -
Doc.7383-EN Aeronautical Information Services Provided By
Doc 7383/102 AERONAUTICAL INFORMATION SERVICES PROVIDED BY STATES SERVICES D’INFORMATION AÉRONAUTIQUE ASSURÉS PAR LES ÉTATS SERVICIOS DE INFORMACIÓN AERONÁUTICA SUMINISTRADOS POR LOS ESTADOS АЭРОНАВИГАЦИОННОЕ ИНФОРМАЦИОННОЕ ОБСЛУЖИВАНИЕ, ПРЕДОСТАВЛЯЕМОЕ ГОСУДАРСТВАМИ Edition No. 102 / Édition no 102 / Edición núm. 102 / Издание № 102 June – Juin – Junio – Июнь 2014 INTERNATIONAL CIVIL AVIATION ORGANIZATION ORGANISATION DE L’AVIATION CIVILE INTERNATIONALE ORGANIZACIÓN DE AVIACIÓN CIVIL INTERNACIONAL МЕЖДУНАРОДНАЯ ОРГАНИЗАЦИЯ ГРАЖДАНСКОЙ АВИАЦИИ Suzanne Doc 7383/102 AERONAUTICAL INFORMATION SERVICES PROVIDED BY STATES SERVICES D’INFORMATION AÉRONAUTIQUE ASSURÉS PAR LES ÉTATS SERVICIOS DE INFORMACIÓN AERONÁUTICA SUMINISTRADOS POR LOS ESTADOS АЭРОНАВИГАЦИОННОЕ ИНФОРМАЦИОННОЕ ОБСЛУЖИВАНИЕ, ПРЕДОСТАВЛЯЕМОЕ ГОСУДАРСТВАМИ Edition No. 102 / Édition no 102 / Edición núm. 102 / Издание № 102 June – Juin – Junio – Июнь 2014 INTERNATIONAL CIVIL AVIATION ORGANIZATION ORGANISATION DE L’AVIATION CIVILE INTERNATIONALE ORGANIZACIÓN DE AVIACIÓN CIVIL INTERNACIONAL МЕЖДУНАРОДНАЯ ОРГАНИЗАЦИЯ ГРАЖДАНСКОЙ АВИАЦИИ The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of ICAO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. Les appellations employées dans cette publication et la présentation des données qui y figurent n’impliquent de la part de l’OACI aucune prise de position quant au statut juridique des pays, territoires, villes ou zones, ou de leurs autorités, ni quant au tracé de leurs frontières ou limites. Las denominaciones empleadas en esta publicación y la forma en que aparecen presentados los datos que contiene no implican, de parte de la OACI, juicio alguno sobre la condición jurídica de ninguno de los países, territorios, ciudades o áreas, o de sus autoridades, ni respecto de la delimitación de sus fronteras o límites. -
The Geography of Kamchatka
Global and Planetary Change 134 (2015) 3–9 Contents lists available at ScienceDirect Global and Planetary Change journal homepage: www.elsevier.com/locate/gloplacha The geography of Kamchatka Vivienne Jones a,⁎, Olga Solomina b a ECRC, Department of Geography, University College London, Pearson Building, London WC1E 6BT, UK b Russian Academy of Sciences, Institute of Geography RAS, Staromonetny-29, Moscow 119017, Russia article info abstract Article history: This paper briefly reviews the physical and human geography of the Kamchatka region and summarises previous Received 9 February 2015 research on Holocene climate dynamics. We provide context for the rest of the Special Issue of the Journal Global Received in revised form 2 June 2015 and Planetary Change entitled ‘Holocene climate change in Kamchatka’, the primary focus of which is the use of Accepted 4 June 2015 lake sediment records for palaeoclimatic inferences. In this paper an additional perspective from ongoing tree Available online 6 June 2015 ring, ice core and borehole temperature reconstructions illustrates that the Kamchatka region is rich in paleocli- fi Keywords: matic proxies. The period of the last 200 years is suf ciently covered by the proxy information, including recon- fl Volcanism structions with annual resolution. In this period the tree-rings, ice cores, boreholes, and glacier uctuations Flora recorded a 1 °C warming and a general glacier retreat, i.e. the transition from the Little Ice Age climate to the mod- Fauna ern one. Although the proxies have different resolution, accuracy and seasonality in general they demonstrate a Climate coherent picture of environmental changes in the last two centuries. -
UNDP Kamchatka Final Evaluation 2011.Pdf
Final Evaluation United Nations Development Progrramme - Global Environment Facility Project Demonstrating Biodiversity Conservation in Four Prootected Areas of Russia’s Kamchatka Krai. Phase 2. August 2011 Implementing Agency: United Nations Development Programme Executinng Agency: Ministrry of Natural Resources, Russian Federation Operational Programme: 4. Mountain Ecosystems Strategic Priority: 1. Catalyzingn Sustainability of Protected Areas GEF Prooject ID 2235 UNDP PIMS ID 3346 Michael R Appleton Adviser, Consultant, Trainer: Conservation, Protected Areas, Sustainable Management [email protected] Contents Acknowledgements ........................................................................................................................................... 3 1 Executive summary ................................................................................................................................... 4 1.1 Brief description of the project ........................................................................................................... 4 1.2 Context and purpose of the evaluation ............................................................................................... 4 1.3 Main conclusions, recommendations and lessons learned ................................................................. 5 2 Introduction ............................................................................................................................................... 7 2.1 Project background ............................................................................................................................ -
Decision Support Tool for Disaster Management in the Case of Strong Earthquakes
2020/8/25 Decision Support Tool for Disaster Management in the Case of Strong Earthquakes Decision Support Tool for Disaster Management in the Case of Strong Earthquakes Chen Yong*, Chen Q.F.*, Frolova N.**, Larionov V.***, Nikolaev A.**, Pejcoch J.****, Suchshev S.*****, A.N. Ugarov***** * China Seismological Burea, 100036, Beijing, China, e-mail: [email protected] ** Seismological Center of IGE, Russian Academy of Sciences, Nikoloyamskaya str. 51, Moscow 109004, Russia, e-mail: [email protected] *** All Russian Scientific Research Institute on Civil Defense and Emergency Problems, Davydkovskaya str. 7, Moscow 121352, Russia, e-mail: [email protected] **** T-SOFT s.r.o., Novodvorska 1010/14, 142 01 PRAHA, Czech Republic, e-mail: [email protected] ***** Extreme Situations Research Center, Yunykh Lenintsev str, Moscow, Russia, e-mail: [email protected] Abstract The paper provides a description of the Web Based Decision Support Tool "WaveLet" for expected damage and loss assessment, as well as for the identification of effective response measures to strong earthquakes. This System takes advantages of GIS "Extremum", "GloSeisRisk" and "EIG/GEM Infobook". The "WaveLet" System development is supported by the World Agency on Planetary Monitoring and Earthquake Risk Reduction. Keywords: Web based decision support tool; possible damage extent; seismic and complex risk; expected social and economic losses due to strong earthquakes; effective response measures; geographical information system 1. Introduction Strong earthquakes and secondary processes result in catastrophic human suffering, loss of property and other negative consequences. Over 1.6 million people have died in earthquakes during the 20th century. Analysis of natural emergencies including earthquakes occurring all over the world during the last 5 years show that these types of emergencies are growing at an average rate of about 5% per year.