Decision Support Tool for Disaster Management in the Case of Strong Earthquakes
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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. -
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. -
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. -
GEOS 424/624 Course Description
COURSE DESCRIPTION GEOS 424/624: INTERNATIONAL VOLCANOLOGICAL FIELD SCHOOL KAMCHATKA TRIP (3 CREDITS) INSTRUCTORS Pavel Izbekov Research Assistant Professor, Geophysical Institute, University of Alaska Fairbanks, Fairbanks AK; email: [email protected]; phone: +1-907-474-5269 Olga Khubaeva Researcher, Institute of Volcanology and Seismology, Petropavlovsk-Kamchatsky, e-mail: [email protected] Dates: August 10-24, 2020 Costs: $2121 or $2883 plus roundtrip airfare to Petropavlovsk-Kamchatsky The field trip to Mutnovsky and Gorely volcanoes in Kamchatka (figure 1) offers a chance to learn about full spectrum of volcanic processes using some of the best examples in the world. This includes ignimbrites of caldera-forming eruptions, lava flows, cinder cones, extrusive domes, and active fumaroles (figure 2). A side trip to the 50 MW Mutnovsky Geothermal Power plant is used as an excellent opportunity to discuss the utilization of geothermal energy. This field trip will be led by Pavel Izbekov and Olga Khubaeva, a field camp Director, acting on behalf of our hosting organization, the Institute of Volcanology and Seismology of Russian Academy of Sciences. PREREQUISITES GEOS 424: Acceptance into the course is contingent upon: (1) A completed application, (2) a reference letter, and (3) permission of the Instructor. GEOS 624: All of the above plus a graduate standing. RESTRICTIONS Students must be in good health, capable of hiking for at least 20 km per day carrying heavy backpacks, and be willing to camp under primitive, remote, and possibly uncomfortable conditions. Basic conversational ability in either English or Russian is required. OBJECTIVES GEOS 424 is a stimulating exploration of physical science in nature, suitable for undergraduate science majors with a zest for adventure and an interest in meeting students from other cultures. -
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 ............................................................................................................................ -
Copper-Containing Agates of the Avacha Bay (Eastern Kamchatka, Russia)
minerals Article Copper-Containing Agates of the Avacha Bay (Eastern Kamchatka, Russia) Galina Palyanova 1,2,* , Evgeny Sidorov 3, Andrey Borovikov 2 and Yurii Seryotkin 1,2 1 Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences, Akademika Koptyuga pr. 3, 630090 Novosibirsk, Russia; [email protected] 2 Department of Geology and Geophysics, Novosibirsk State University, Pirogova str. 2, 630090 Novosibirsk, Russia; [email protected] 3 Institute of Volcanology and Seismology, Far East Branch of Russian Academy of Sciences, Piipa Blvd. 9, 683006 Petropavlovsk-Kamchatsky, Russia; [email protected] * Correspondence: [email protected] Received: 22 October 2020; Accepted: 8 December 2020; Published: 14 December 2020 Abstract: The copper-containing agates of the Avacha Bay (Eastern Kamchatka, Russia) have been investigated in this study. Optical microscopy, scanning electron microscopy, electron microprobe analysis, X-ray powder diffraction, Raman spectroscopy, and fluid inclusions were used to investigate the samples. It was found that copper mineralization in agates is represented by native copper, copper sulphides (chalcocite, djurleite, digenite, anilite, yarrowite, rarely chalcopyrite) and cuprite. In addition to copper minerals, sphalerite and native silver were also found in the agates. Native copper is localized in a siliceous matrix in the form of inclusions usually less than 100 microns in size—rarely up to 1 mm—forming dendrites and crystals of a cubic system. Copper sulphides are found in the interstices of chalcedony often cementing the marginal parts of spherule aggregates of silica. In addition, they fill the micro veins, which occupy a cross-cutting position with respect to the concentric bands of chalcedony. -
More Clout for Russia's Provinces: Kamchatka and the Politics Of
NOT FOR PUBLICATION PHC-20 WITHOUT WRITER'S CONSENT INSTITUTE OF CURRENT WORLD AFFAIRS MORE CLOUTFOR RUSSIA'S PROVINCES KAMCHATKA AND THE POLITICS OF RESOURCE USE ON THE EVE OF ELECTIONS. 1993 October 31, 1993 Petropavlovsk-Kamchatsky Russia Mr. Peter Bird Martin, Executive Director The Institute of Current World Affairs 4 West Wheelock Street Hanover, New Hampshire 03755 Dear Peter, Moscow's Bloody Sunday was a spectacle to send a chill up the spine of any teedom-loving person. Historians may later find justification for the sad events surrounding the burning of the White House, but from here, it looked like a Mafia shootout writ large, and nothing more. The two eternal riddles of Russian politics--chto delat, what is to be done, and kto vinovat, who is to blame--were solved the same brutal way they have been since the time of the Czars. What is to be done?--annihilate the enemy! Who is to blame?--the vanquished! Any optimism I felt about the resolution of the two year stand-off of political dual power--dvoyevlastiye--that has paralyzed Russia since the collapse of the Soviet Union vanished when I saw the violence used to bring it about. The Russian Federation government's greatest contribution to democracy may be that, during its flabby and aimless reign, it has graphically shown the waste and futility of trying to direct all of the activities of the gigantic Russian state from a single center. President Yeltsin vanquished Khasbulatov, Rutskoi, and their followers, but the hardest tasks still lie ahead. Russia has changed in ways few predicted during the first flush of 'democratization' following the attempted August 1991 Coup. -
Itinerary (Preliminary)
Metals, Minerals, and Society Keystone, Colorado, USA September 22-25, 2018 SEG 2018 Field Trip Itinerary (Preliminary) FT01 - Central and South Kamchatka Mining Districts, Far East of Russia www.seg2018.org/field-trips.html#1 Date: September 13-19, 2018 Location: Departing from and returning to Petropavlovsk-Kamchatsky, Russia Leader: Daria S. Bukhanova Included: Accommodation, Food, Transport Not Included: Flights/Airfare Kamchatka Peninsula is located in the northeastern section of the Pacific Ring of Fire. There are 31 active volcanoes and more than 150 groups of hot springs, countless boiling mud cauldrons, fumaroles, and other forms of volcanic activity. This is a geologically dynamic area with highly prospective mining districts for the discovery of Cu-Au-Mo porphyry, Au- Ag epithermal deposits. The field trip will provide the opportunity to visit the Central Kamchatka mining district with the Shanuch Ni-Cu-Co Mine and Kirganik Cu-Au porphyry deposit (a greenfields exploration project). The trip also includes a visit to the South Kamchatka mining district, which is surrounded by active volcanoes and hydrothermal systems. It hosts the Mutnovskoe and Rodnikovoe Au-Ag low-sulfidation deposits, Mutnovsky and Gorely active volcanoes (a crater visit is included), the Mutnovsky Geothermal Power Plant, and several groups of hot springs (Dachniy, Vilyuchinskie and Verkhne Paratunskie). Participants must have warm and waterproof field clothing. The temperature in mid-September typically ranges from +10° to –5°C. Transportation from Petropavlovsk-Kamchatsky city to the mining districts will be by truck and locally by all-terrain vehicles. Most foreign nationals are required to have an entry visa to Russia (excluding most South American and CIS countries). -
Kamchatka Summer Trips 2019
Kamchatka Summer Trips 2019 KAMCHATKA TRAVEL COMPANY Tel: (4152) 20-10-10, 42-70-71 Mobile: +7-914-786-11-16 Fax: (4152) 42-77-41 E-mail: [email protected] Skype: sedova.ira www.kamchatintour.ru http://www.facebook.com/ VisitKamchatka https://vk.com/kamchatintour Welcome to Kamchatka! Kamchatka is called the Edge of Russia, every morning In the work of our company we pay special attention to of our unbounded Motherland begins here. the concepts of ecological tourism. We only organize such kind of activities that do not harm the unique Kamchatka Have you ever heard of Kamchatka? Have you ever had nature. We organize only „catch-and-realease“ fishing a chance to look into the crater of an active volcano or to tours and hunting with a camera trips. Some of the most TRIPS SUMMER KAMCHATKA watch a bear fishing for salmon? These and many other popular destinations among our foreign guests are flower adventurous trips can be done with the Tourist Company watching, animal and bird viewing tours. The culture „Kamchatintour“. of local Kamchatka natives, Itelmens, Koryaks, Evens, The „Kamchatintour“ tourist company can be fairly Aleutians and Chukchis are also of great interest. called a veteran of Kamchatka tourism. Our company has Amazing landscapes, volcanoes, geysers and hot springs been working since May 1990. make a great impression upon Kamchatka guests. Today dozens of specialists are engaged in work during the high season: guides and interpreters, Kamchatka is the land of unique drivers and delivery men, cooks, porters, conductors, doctors, consulting scientists, and many others. -
2000 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory by Christina A
2000 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory by Christina A. Neal, Robert G. McGimsey, and Olga Chubarova Open-File Report 2004-1034 U.S. Department of the Interior U.S. Geological Survey 2000 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory By Christina A. Neal1, Robert G. McGimsey1,and Olga Chubarova2 1Alaska Volcano Observatory, 4200 University Dr., Anchorage, AK 99508-4664 2Kamchatka Volcanic eruptions Response Team, Institute of Volcanic Geology and Geochemistry, Piip Blvd, 9 Petropavlovsk-Kamchatsky, 683006, Russia AVO is a cooperative program of the U.S. Geological Survey, University of Alaska Fairbanks Geophysical Institute, and the Alaska Division of Geological and Geophysical Surveys. AVO is funded by the U.S. Geological Survey Volcano Hazards Program and the State of Alaska Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 2004-1034 U.S. Department of the Interior U.S. Geological Survey TABLE OF CONTENTS Introduction . 1 Volcanic Activity, Northeast To Southwest Along Aleutian Arc. 4 Wrangell Volcano . 4 Snowy Mountain . 5 Chiginagak Volcano . 10 Shishaldin Volcano. .11 Volcanic Activity, Kamchatka Peninsula, And The Northern Kurile Islands, Russia . 13 Sheveluch Volcano . 15 Klyuchevskoy Volcano . 17 Bezymianny Volcano . 19 Karymsky Volcano . 20 Mutnovsky . 21 References. 23 Acknowledgments . 25 Figures 1a. Location of historically active volcanoes in Alaska. 2 1b. Map showing those volcanoes monitored with a seismic network . 3 2. Location map showing Snowy Mountain .