2Nd Circular
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Correlating the Electrification of Volcanic Plumes With
Earth and Planetary Science Letters 492 (2018) 47–58 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Correlating the electrification of volcanic plumes with ashfall textures at Sakurajima Volcano, Japan ∗ Cassandra M. Smith a, , Alexa R. Van Eaton b, Sylvain Charbonnier a, Stephen R. McNutt a, Sonja A. Behnke c, Ronald J. Thomas d, Harald E. Edens d, Glenn Thompson a a University of South Florida, School of Geosciences, Tampa, FL, United States of America b U.S. Geological Survey, Cascades Volcano Observatory, Vancouver, WA, United States of America c Los Alamos National Laboratory, Los Alamos, NM, United States of America d New Mexico Institute of Mining and Technology, Department of Physics, Socorro, NM, United States of America a r t i c l e i n f o a b s t r a c t Article history: Volcanic lightning detection has become a useful resource for monitoring remote, under-instrumented Received 7 September 2017 volcanoes. Previous studies have shown that the behavior of volcanic plume electrification responds to Received in revised form 26 March 2018 changes in the eruptive processes and products. However, there has not yet been a study to quantify the Accepted 27 March 2018 links between ash textures and plume electrification during an actively monitored eruption. In this study, Available online 11 April 2018 we examine a sequence of vulcanian eruptions from Sakurajima Volcano in Japan to compare ash textural Editor: T.A. Mather properties (grain size, shape, componentry, and groundmass crystallinity) to plume electrification using Keywords: a lightning mapping array and other monitoring data. -
Ausser Rosen Besteller: Ansprechpartner Für Rückfragen
Alles Ausser Rosen Besteller: Ansprechpartner für Rückfragen: Firmenstempel/Adresse: ggf. abweichende Lieferadresse: Firmenstempel/Adresse: ggf. abweichende Lieferadresse: Alle Felder in dieser Farbe sind vom Kunden bearbeit-/ und ausfüllbar! 'Hinweis in eigener Sache: Die Sortenliste wird laufend aktualisiert und angepasst. Trotz Liste für folgende BildTafeln: nur 1*Ankreuzen sorgfältiger Prüfung können Fehler nicht ausgeschlossen werden, Irrtum vorbehalten. Marken und Warenzeichen gehören den jeweiligen Eigentümern und werden hier ausschließlich UVTop-D A4 hoch (18er-weise) zu Identifikationszwecken benutzt. Die Liste darf im Rahmen einer "nicht ausschließlichen" Nutzungslizenz nur zur Erstellung von UVTop-D A5 hoch (36er-weise) Bestellungen bei GartenMedien (GM) benutzt werden. Jede weitere Verwendung oder Weitergabe ist ausdrücklich untersagt. UVTop-D HxB 21x14 cm*) (36er) Die Verwendung von GM-Bildtafeln/Auszeichnungssystemen ist nur im Zusammenhang mit der Auszeichung "regulärer Ware" gestattet, die mit allen erforderlichen Rechten und Lizenzen, z.B. UVTop-D A5 quer (36er)/opt. Janus mgl. für den Handel und Verkauf ausgestattet ist. Manche Sorten können auch als Infoprint-Etikett kundenbezogen gefertigt werden. Infoprint-Etiketten sind keinerlei Züchter- oder Schutzetikett und UVTOP-D SSG500 (10x16cm, 72er) dürfen nur zur Kennzeichnung freier Sorten, oder zur zusätzlichen Informationsvermittlung und Preisauszeichnung im Zusammenhang mit geschützen Sorten - und dort nur ergänzend zu den UVTOP-D SSG440 (7,9x12,4cm, 112er) vom Züchter vorgeschriebenen Schutzmassnahmen wie Züchter- und/oder Schutzetikett/en eingesetzt werden. Für Etiketten sind weiterhin gesonderte Verträge und Haftungsübernahmen UV-Top-L A4 hoch Bestandteil der Auftragsabwicklung. Die Annahme von Aufträgen kann ohne Angabe von Gründen auch verweigert werden. Mit der Bestellung sichert der Kunde GM die Einhaltung dieser UVTOP-L A5 hoch Bedingungen zu sowie, daß er die Tafeln über den gedachten längeren Zeitraum benutzt und auch im Rahmen seiner Entsorgungslizenzen/-verträge entsorgt. -
Towada-Hachimantai National Park Guide Book
Towada-Hachimantai National Park Guide Book 十和田八幡平国立公園 Feel the landscapes of Northern Tohoku that change from season to season in the vast nature 四季それぞれに美しい北東北を自然の中で体感 In Japan, each of the four seasons has its own colour that allows visitors to truly feel its atmosphere. Especially in Tohoku, where winter is crucially rigorous, people wait for the arrival of spring, sing the joys of summer, and appreciate the rich harvests of autumn. There are many things in Tohoku that bring joy to people throughout the year. Towada-Hachimantai National Park is located in the mountainous area of Northern Japan, and lies upon the three prefectures of Northern Tohoku. It is composed of “Towada-Hakkoda Area” , on the northern side that consists of Lake Towada, Oirase Gorge and Hakkoda Mountains and “Hachimantai Area” , on the southern side that consists of Mt. Hachimantai, Mt. Akita-Komagatake and Mt. Iwate. Both areas are very rich in natural resources, such as forests, lakes and marshes, and a wide variety of fauna and flora. There are also many onsen spots where you can immerse your body and soul. 01 Shin-Hakodate-Hokuto Hakodate Airport Oma To Tomakomai Aomori Contents ● Tohoku Shinkansen about 3hr 10 min. Tokyo Station Shin-Aomori Station Towada-Hakkoda Area Shin-Aomori Station Airplane about 1hr 20 min. Haneda Airport Misawa Airport Airplane about 1hr 15 min. Haneda Airport Aomori Airport Tohoku Shinkansen about 1hr 30 min. Sendai Station Shin-Aomori Station Hokkaido / Tohoku Shinkansen about 1hr Shin-Hakodate-Hokuto Station Shin-Aomori Station Highway Bus about 4hr 50 min. Sendai Station Aomori Station Joy of Spring Iwate 04 春の歓喜 Tohoku Shinkansen about 2hr 20 min. -
Systems Analysis of Social Resilience Against Volcanic Risks: Case Studies of Mt
Systems Analysis of Social Resilience against Volcanic Risks: Case Studies of Mt. Merapi, Indonesia and Mt. Sakurajima, Japan by Saut Aritua Hasiholan Sagala A thesis submitted in fulfilment of the requirements of the degree of Doctor of Engineering Supervised by Prof. Norio Okada DEPARTMENT OF URBAN MANAGEMENT GRADUATE SCHOOL OF ENGINEERING Kyoto University August, 2009 Acknowledgements This thesis has benefitted from collaboration with and contribution by many people. Therefore, I want to thank a number of people for their assistance while I was preparing for this thesis and completing my doctoral study in Kyoto University (KU). First of all, I would like to express my gratitude to Prof Norio Okada, my PhD advisor, who has provided a lot of important ideas for the completion of my PhD research. His excellent experiences in research fields and ways of building networks have become my source of inspiration. Finally, Prof Okada has also kindly recommended me to the scholarship provided by Monbukagakusho under Kyoto University - International Doctoral Program which funded my study in Kyoto. The next person I would like to thank is Dr. Muneta Yokomatsu, who are very kind and friendly, but at the same time has been the role model of how a real researcher should be. I have gain many insight during our discussion time. In particular I would like to thank Dr. Yokomatsu for helping me during the field visit to Mt. Sakurajima. Prof Douglas Paton of University of Tasmania has provided an enormous help for my research and has been a great discussion partner in which we have written some research articles which are parts of this thesis. -
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. -
Giant Rhyolite Lava Dome Formation
Kobe University Repository : Kernel タイトル Giant rhyolite lava dome formation after 7.3 ka supereruption at Kikai Title caldera, SW Japan Tatsumi, Yoshiyuki / Suzuki-Kamata, Keiko / Matsuno, Tetsuo / Ichihara, Hiroshi / Seama, Nobukazu / Kiyosugi, Koji / Nakaoka, Reina / 著者 Nakahigashi, Kazuo / Takizawa, Hideaki / Hayashi, Kazuki / Chiba, Author(s) Tatsuro / Shimizu, Satoshi / Sano, Mamoru / Iwamaru, Hikaru / Morozumi, Haruhisa / Sugioka, Hiroko / Yamamoto, Yojiro 掲載誌・巻号・ページ Scientific Reports,8:2753 Citation 刊行日 2018-02-09 Issue date 資源タイプ Journal Article / 学術雑誌論文 Resource Type 版区分 publisher Resource Version © The Author(s) 2018 This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party 権利 material in this article are included in the article’s Creative Commons Rights license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. DOI 10.1038/s41598-018-21066-w JaLCDOI URL http://www.lib.kobe-u.ac.jp/handle_kernel/90004609 -
Volcanic Hazards As Components of Complex Systems: the Case of Japan
Volume 13 | Issue 33 | Number 6 | Article ID 4359 | Aug 17, 2015 The Asia-Pacific Journal | Japan Focus Volcanic Hazards as Components of Complex Systems: The Case of Japan Gregory Smits The past year or so has been a time of the earth’s crust suggested Mt. Fuji is more particularly vigorous volcanic activity in Japan, likely to erupt owing to effects from the 2011 or at least activity that has intruded into public Tōhoku earthquake.3 Well publicized by a press awareness. Perhaps most dramatic was the release on the eve of its publication, mass deadly eruption of Mt. Ontake on September media around the world have reported this 27, 2014, whose 57 fatalities were the first finding, along with speculation regarding volcano-related deaths in Japan since 1991. On possible connections between earthquakes and May 29, 2015, Mt. Shindake, off the southern volcanic eruptions. tip of Kyushu, erupted violently, forcing the evacuation of the island of Kuchinoerabu. That As of June 30, 2015, the Japan Meteorological same day, Sakurajima, located just north in Agency (JMA) designated ten volcanoes in or Kagoshima Bay, erupted more forcefully than near the main Japanese islands as warranting usual. Sakurajima has been erupting in some levels of warning ranging from Mt. Shindake’s fashion almost continuously since 1955, but Level 5 (“Evacuate”), to Level 2 (“Do not since 2006, its activity has become relatively approach the crater”) in seven cases. more vigorous. Indeed, a May 30 Asahi shinbun Sakurajima is at Level 3 (“Do not approach the article characterized these eruptions as “the volcano”), as is Hakoneyama, located near Mt. -
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. -
Origins of the Japanese Languages. a Multidisciplinary Approach”
MASTERARBEIT / MASTER’S THESIS Titel der Masterarbeit / Title of the Master’s Thesis “Origins of the Japanese languages. A multidisciplinary approach” verfasst von / submitted by Patrick Elmer, BA angestrebter akademischer Grad / in partial fulfilment of the requirements for the degree of Master of Arts (MA) Wien, 2019 / Vienna 2019 Studienkennzahl lt. Studienblatt / A 066 843 degree programme code as it appears on the student record sheet: Studienrichtung lt. Studienblatt / Masterstudium Japanologie UG2002 degree programme as it appears on the student record sheet: Betreut von / Supervisor: Mag. Dr. Bernhard Seidl Mitbetreut von / Co-Supervisor: Dr. Bernhard Scheid Table of contents List of figures .......................................................................................................................... v List of tables ........................................................................................................................... v Note to the reader..................................................................................................................vi Abbreviations ....................................................................................................................... vii 1. Introduction ................................................................................................................. 1 1.1. Research question ................................................................................................. 1 1.2. Methodology ........................................................................................................