2000 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory by Christina A
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Confirmed Soc Reports List 2015-2016
Confirmed State of Conservation Reports for natural and mixed World Heritage sites 2015 - 2016 Nr Region Country Site Natural or Additional information mixed site 1 LAC Argentina Iguazu National Park Natural 2 APA Australia Tasmanian Wilderness Mixed 3 EURNA Belarus / Poland Bialowieza Forest Natural 4 LAC Belize Belize Barrier Reef Reserve System Natural World Heritage in Danger 5 AFR Botswana Okavango Delta Natural 6 LAC Brazil Iguaçu National Park Natural 7 LAC Brazil Cerrado Protected Areas: Chapada dos Veadeiros and Natural Emas National Parks 8 EURNA Bulgaria Pirin National Park Natural 9 AFR Cameroon Dja Faunal Reserve Natural 10 EURNA Canada Gros Morne National Park Natural 11 AFR Central African Republic Manovo-Gounda St Floris National Park Natural World Heritage in Danger 12 LAC Costa Rica / Panama Talamanca Range-La Amistad Reserves / La Amistad Natural National Park 13 AFR Côte d'Ivoire Comoé National Park Natural World Heritage in Danger 14 AFR Côte d'Ivoire / Guinea Mount Nimba Strict Nature Reserve Natural World Heritage in Danger 15 AFR Democratic Republic of the Congo Garamba National Park Natural World Heritage in Danger 16 AFR Democratic Republic of the Congo Kahuzi-Biega National Park Natural World Heritage in Danger 17 AFR Democratic Republic of the Congo Okapi Wildlife Reserve Natural World Heritage in Danger 18 AFR Democratic Republic of the Congo Salonga National Park Natural World Heritage in Danger 19 AFR Democratic Republic of the Congo Virunga National Park Natural World Heritage in Danger 20 AFR Democratic -
The Mesa Site: Paleoindians Above the Arctic Circle
U. S. Department of the Interior BLM-Alaska Open File Report 86 Bureau of Land Management BLM/AK/ST-03/001+8100+020 April 2003 Alaska State Office 222 West 7th Avenue Anchorage Alaska 99513 The Mesa Site: Paleoindians above the Arctic Circle Michael Kunz, Michael Bever, Constance Adkins Cover Photo View of Mesa from west with Iteriak Creek in foreground. Photo: Dan Gullickson Disclaimer The mention of trade names or commercial products in this report does not constitute endorsement or recommendation for use by the federal government. Authors Michael Kunz is an Archaeologist, Bureau of Land Management (BLM), Northern Field Office, 1150 University Avenue, Fairbanks, Alaska 99709. Michael Bever is a project supervisor for Pacific Legacy Inc., 3081 Alhambra Drive, Suite 208, Cameron Park, CA 95682. Constance Adkins is an Archaeologist, Bureau of Land Management (BLM), Northern Field Office, 1150 University Avenue, Fairbanks, Alaska 99709. Open File Reports Open File Reports issued by the Bureau of Land Management-Alaska present the results of invento- ries or other investigations on a variety of scientific and technical subjects that are made available to the public outside the formal BLM-Alaska technical publication series. These reports can include preliminary or incomplete data and are not published and distributed in quantity. The reports are available while supplies last from BLM External Affairs, 222 West 7th Avenue #13, Anchorage, Alaska 99513 and from the Juneau Minerals Information Center, 100 Savikko Road, Mayflower Island, Douglas, AK 99824, (907) 364-1553. Copies are also available for inspection at the Alaska Resource Library and Information Service (Anchorage), the USDI Resources Library in Washington, D. -
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..................................................................................................... -
Pskov from Wikipedia, the Free Encyclopedia Coordinates: 57°49′N 28°20′E
Create account Log in Article Talk Read Edit View history Pskov From Wikipedia, the free encyclopedia Coordinates: 57°49′N 28°20′E Pskov (Russian: Псков; IPA: [pskof] ( listen), ancient Russian spelling "Плѣсковъ", Pleskov) is Navigation Pskov (English) a city and the administrative center of Pskov Oblast, Russia, located about 20 kilometers Псков (Russian) Main page (12 mi) east from the Estonian border, on the Velikaya River. Population: 203,279 (2010 [1] Contents Census);[3] 202,780 (2002 Census);[5] 203,789 (1989 Census).[6] - City - Featured content Current events Contents Random article 1 History Donate to Wikipedia 1.1 Early history 1.2 Pskov Republic 1.3 Modern history Interaction 2 Administrative and municipal status Help 3 Landmarks and sights About Wikipedia 4 Climate Community portal 5 Economy Recent changes 6 Notable people Krom (or Kremlin) in Pskov Contact Wikipedia 7 International relations 7.1 Twin towns and sister cities Toolbox 8 References 8.1 Notes What links here 8.2 Sources Related changes 9 External links Upload file Special pages History [edit] Location of Pskov Oblast in Russia Permanent link Page information Data item Early history [edit] Cite this page The name of the city, originally spelled "Pleskov", may be loosely translated as "[the town] of purling waters". Its earliest mention comes in 903, which records that Igor of Kiev married a [citation needed] Print/export local lady, St. Olga. Pskovians sometimes take this year as the city's foundation date, and in 2003 a great jubilee took place to celebrate Pskov's 1,100th anniversary. Create a book Pskov The first prince of Pskov was Vladimir the Great's younger son Sudislav. -
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. -
Kamchatka Peninsula and Salmon Research with Pro Plus
YSI Environmental Application Note Kamchatka Peninsula: Where the Waters Run Free and Salmon Thrive In Russia’s Far East lies the 1,250 km (780 mile) Kamchatka The habitat on the Kol is nearly ideal for salmon. The salmon run Peninsula. Situated between the Pacific Ocean and the Sea of includes over seven million fish returning to spawn. The fish fill Okhotsk, Kamchatka is home to Steller’s sea-eagles, brown bears, the river channel so fully that some sections block the view to the World Heritage List volcanoes, and a remarkable amount of Pacific river bottom. The Kol also has the world’s first whole-basin refuge salmon (genus Oncorhynchus) that are being studied, protected, and for the conservation of Pacific salmon - the Kol-Kekhta Regional even filmed for television. Experimental Salmon Reserve. Kamchatka may contain the world’s Research greatest diversity of salmonids including Along the Kol’s north bank is the Kol River chinook, chum, coho, seema, pink and Biostation established for the sole purpose sockeye salmon. Rainbow trout and dolly of serving as a binational research station varden char are also highly abundant. between Russia and the U.S. Researchers Biologists estimate at least 20% of all wild are studying the dynamics of the Kol Pacific salmon originates in Kamchatka. ecosystem and addressing the question of the importance of the salmon to the health The life of a salmon is far from easy as a of the entire river’s ecosystem. fish life goes. Millions of fry, roughly five inches long after a few months of growth, While there is no question to the have to navigate close to a hundred miles All six species of Pacific salmon spawn in the importance of the healthy ecosystem on to the sea. -
Explosive Earth
Natural Hazards Explosive Earth One of the most beautiful pictures taken of the Earth is known as the Blue Marble. Taken from space, it is the epitome of serenity. The Earth really looks like a small marble with swirls of blue, white, green and brown, as it floats placidly in the vastness of space. However, the Volcano Variety picture is misleading, for Mother Earth is geologically restless and Based on history of activity often explodes in acts so violent that we call them, natural hazards. Active: These volcanoes are currently erupting, or exhibiting unrest through earthquakes and/or gas emissions. Natural hazards are defined as, “those Volcano Architecture Dormant: These volcanoes are inactive, but have not been so long elements of the physical environment, harmful A volcano constitutes a vent, a pipe, a enough to be declared extinct. to man and caused by forces extraneous to crater, and a cone. him.” The prefix “natural” shows that these Vent: This is the opening through which Extinct: These volcanoes have been exclude phenomenon that are a result of volcanic material is ejected. A central vent inactive in all of recorded history. human action. An event that causes large underlies the summit crater of the volcano. Based on shape numbers of fatalities and/or tremendous loss It is connected to a magma chamber, of property is a “natural disaster.” which is the main storage area for material Volcanic cone: Volcanic cones are among that is finally ejected. the simplest volcano formations. These are Violent Volcano Pipe: This is a passageway through which built up of ejected material around a volcanic One of the most explosively violent events the ejected magma rises to the surface. -
A 100-Year Record of North Pacific Volcanism in an Ice Core from Eclipse Icefield, Yukon Territory, Canada Kaplan Yalcin and Cameron P
University of New Hampshire University of New Hampshire Scholars' Repository Earth Sciences Scholarship Earth Sciences 1-8-2003 A 100-year record of North Pacific olcanismv in an ice core from Eclipse icefield, ukonY Territory, Canada Kaplan Yalcin University of New Hampshire - Main Campus Cameron P. Wake University of New Hampshire - Main Campus, [email protected] Mark S. Germani MVA, Inc. Follow this and additional works at: https://scholars.unh.edu/earthsci_facpub Recommended Citation Yalcin, K., C. P. Wake, and M. Germani, A 100-year record of North Pacific olcanismv in an ice core from Eclipse Icefield, ukonY Territory, Canada, J. Geophys. Res., 108(D1), 4012, doi:10.1029/2002JD002449, 2003. This Article is brought to you for free and open access by the Earth Sciences at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Earth Sciences Scholarship by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. D1, 4012, doi:10.1029/2002JD002449, 2003 A 100-year record of North Pacific volcanism in an ice core from Eclipse Icefield, Yukon Territory, Canada Kaplan Yalcin and Cameron P. Wake Climate Change Research Center, Institute for the Study of Earth, Oceans, and Space (EOS), University of New Hampshire, Durham, New Hampshire, USA Mark S. Germani MicroMaterials Research, Inc., Burr Ridge, Illinois, USA Received 16 April 2002; revised 16 July 2002; accepted 4 August 2002; published 8 January 2003. [1] A record of regionally significant volcanic eruptions in the North Pacific over the last century has been developed using a glaciochemical record from Eclipse Icefield, Yukon Territory, Canada. -
Worksheet: Volcanoes
Worksheet: Volcanoes Find the most spectacular volcanoes in the world! Purpose: This participation and discussion When pressure builds up, eruptions occur. exercise enables students to discover for Gases and rock shoot up through the opening themselves the notable volcanoes of the world and spill over or fill the air with lava fragments. and some basic information about each. Some volcanoes even exist underwater, along the ocean floor or sea bed. Objectives: Students will be able to: > geographically locate 12 notable volcanoes Activity: Follow these steps: > see images of real active volcanoes > identify key features of volcanic activity 1. Print off the: Skills: Students can demonstrate: - Information Required sheet > Researching - Volcano Locations sheet > Classifying - The 12 Volcano sheets for each group > Communicating - The Volcano Teacher Briefing > Observing > Posing questions 2. Spend 20 minutes engaging students in the formation and types of Volcanoes. (Prepare by Time Required: 45 minutes. reading the Teacher Briefing). Group Size: In small groups of 4. 3. Provide each small group with a set of the 12 volcanoes and challenge the students to: Materials/Preparation: Includes: a) locate each volcano > Access to the internet for each group b) identify the height of each volcano > The following 2 teacher guide sheets c) identify the type of each volcano > A printed copy of the 12 volcanoes to locate and research for each group. 4. Review the students discoveries and > A copy of the Volcano Teacher Briefing accuracy in identifying the information for each volcano. Background: Volcanoes form when magma reaches the Earth’s surface, causing eruptions 5. Use the Information and Location sheets to of lava and ash. -
Features of Heat and Mass Transfer Processes Under the Avachinsky Volcano (Kamchatka)
EGU2020-362 https://doi.org/10.5194/egusphere-egu2020-362 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Features of heat and mass transfer processes under the Avachinsky volcano (Kamchatka) Grigory Kuznetsov1 and Victor Sharapov1,2 1Institute of Geology and Mineralogy SB RAS, Novosibirsk, Russian Federation, ([email protected]) 2Novosibirsk State University, Novosibirsk, Russian Federation, ([email protected]) We investigated the processes beneath the Avacha volcano using mantle peridotite xenoliths the with the EPMA, electronic microscope and ICP methods and numeric modeling of the mass transfer accounting the melt fluid reactions with peridotites The decompression melting processes in peridotites beneath Avachinsky volcano (Kamchatka) are associated with seismic events. After the reactions with the Si, Ca, Na, K from partial melts associated with the subduction related fluids the spinel and orthopyroxene were melted and essentially clinopyroxene veins were formed. Secondary crystals growth in the mantle xenoliths (with melt and fluid inclusions) are associated possibly with the fluids appeared due to retrograde boiling of the magma chamber beneath the volcano. The processes of sublimation and recrystallization of Avacha harzburgites was investigated at the facility in the Institute of Nuclear Physics (Novosibirsk, Russia), which generates high-density electron beams and makes it possible to obtain boiling ultrabasic and basic liquids and condensates of magmatic gas on the surface of harzburgite. Results of experiments provides a satisfactory explanation for the observed local heterophase alterations within ultramafic rocks that have experienced multistage deformation beneath volcanoes of the Kamchatka volcanic front. Mathematical model of convective heating and metasomatic reactions in harzburgites were modeled using the Selector PC thermodynamic software. -
2005 Volcanic Activity in Alaska, Kamchatka, and the Kurile Islands: Summary of Events and Response of the Alaska Volcano Observatory
The Alaska Volcano Observatory 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 . The Alaska Volcano Observtory is funded by the U.S. Geological Survey Volcano Hazards Program and the State of Alaska. 2005 Volcanic Activity in Alaska, Kamchatka, and the Kurile Islands: Summary of Events and Response of the Alaska Volcano Observatory Scientific Investigations Report 2007–5269 U.S. Department of the Interior U.S. Geological Survey Cover: Southeast flank of Augustine Volcano showing summit steaming, superheated fumarole jet, and ash dusting on snow. View is toward the northwest with Iniskin Bay in the distance. Photograph taken by Chris Waythomas, AVO/USGS, December 20, 2005. 2005 Volcanic Activity in Alaska, Kamchatka, and the Kurile Islands: Summary of Events and Response of the Alaska Volcano Observatory By R.G. McGimsey, C.A. Neal, J.P. Dixon, U.S. Geological Survey, and Sergey Ushakov, Institute of Volcanology and Seismology The Alaska Volcano Observatory is a cooperative program of the U.S. Geological Survey, University of Alaska Fairbanks Geophysical Institute, and the Alaska Division of Geological and Geophuysical Surveys. The Alaska Volcano Observatory is funded by the U.S. Geological Survey Volcano Hazards Program and the State of Alaska. Scientific Investigations Report 2007–5269 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. -
First Documented Record of Watercock (Gallicrex Cinerea) in Oceania
96 Short note Notornis, 2010, Vol. 57: 96-97 0029-4470 © The Ornithological Society of New Zealand, Inc. SHORT NOTE First documented record of watercock (Gallicrex cinerea) in Oceania DONALD W. BUDEN* Division of Natural Sciences and Mathematics, College of Micronesia-FSM. P.O. Box 159, Kolonia, Pohnpei, Federated States of Micronesia GLENN MCKINLAY C/-55 Albert Road. Devonport, Auckland, New Zealand The watercock (Gallicrex cinerea) breeds from Pratt et al. (1987) listed this species as hypothetical Pakistan, India, and the Maldive Is east to China, in Palau, based on an unconfirmed sighting by R. P. Korea, Japan (Yaeyama Is), the Russian Far Owen that was mentioned in correspondence from East (Primorskiy Teritory, Bol’shoy Pelis I), the Owen to Pratt. Philippines, and Greater Sunda Is (Brazil 1991; Kosrae (5˚19’N, 162˚59’E; 109 km2; 630 m Mackinnon & Phillipps 1993; Taylor 1996; Coates elevation) is the easternmost island in the Caroline Is & Bishop 1997; Grimmett et al. 1999; Smythies & and the Federated States of Micronesia (FSM), in the Davison 1999; Strange 2001; Shimba 2007; Mann west-central Pacific Ocean (Fig. 2). The watercock 2008; Nechaev & Gamova 2009). Birds from the was found in a grassy field just outside Utwe northern part of the range regularly migrate to village at the south end of the island. McKinlay as far south as the Lesser Sundas, (Mackinnon & saw it initially the morning of 1 May, once again Phillipps 1993, 2000; Taylor 1996; Taylor & van Perlo during late afternoon (presumably the same bird), 1998; Strange 2001). A few, probably overshooting and once again during mid-afternoon on 2 May their wintering destination, have been recorded before he left the island the following day.