World Heritage Volcanoes a Thematic Study
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Lava Lake Eruptive Processes Quantified with Infrasound and Video at Mount Erebus, Antarctica
LAVA LAKE ERUPTIVE PROCESSES QUANTIFIED WITH INFRASOUND AND VIDEO AT MOUNT EREBUS, ANTARCTICA by Alexander Miller A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geophysics Boise State University August 2016 © 2016 Alexander Miller ALL RIGHTS RESERVED BOISE STATE UNIVERSITY GRADUATE COLLEGE DEFENSE COMMITTEE AND FINAL READING APPROVALS of the thesis submitted by Alexander Miller Thesis Title: Lava Lake Eruptive Processes Quantified with Infrasound and Video at Mount Erebus, Antarctica Date of Final Oral Examination: 04 March 2016 The following individuals read and discussed the thesis submitted by student Alexander Miller, and they evaluated the presentation and response to questions during the final oral examination. They found that the student passed the final oral examination. Jeffrey B. Johnson, Ph.D. Chair, Supervisory Committee Brittany Brand, Ph.D. Member, Supervisory Committee Paul Michaels, Ph.D. Member, Supervisory Committee The final reading approval of the thesis was granted by Jeffrey B. Johnson, Ph.D., Chair of the Supervisory Committee. The thesis was approved for the Graduate College by Jodi Chilson, M.F.A., Coordinator of Theses and Dissertations. The truth is out there. iv ACKNOWLEDGMENTS The author wishes to express gratitude to the Mount Erebus Volcano Observa- tory, efforts of Dr. Philip Kyle, Dr. Richard Aster, Dr. William McIntosh, Jake Anderson, Hugo Ortiz, and the McMurdo personnel. v ABSTRACT A natural laboratory exists at Mount Erebus where strombolian activity from the lava lake is directly observed from the crater rim. Lava lake eruptions occur when pressurized bubble slugs distend the lake surface before bursting within a few tenths of a second. -
Geology and Mineralization of the Sierra Blanca Peaks, Hudspeth County, Texas W
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/31 Geology and mineralization of the Sierra Blanca Peaks, Hudspeth County, Texas W. N. McAnulty, 1980, pp. 263-266 in: Trans Pecos Region (West Texas), Dickerson, P. W.; Hoffer, J. M.; Callender, J. F.; [eds.], New Mexico Geological Society 31st Annual Fall Field Conference Guidebook, 308 p. This is one of many related papers that were included in the 1980 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Conserving Wildlife in African Landscapes Kenya’S Ewaso Ecosystem
Smithsonian Institution Scholarly Press smithsonian contributions to zoology • number 632 Smithsonian Institution Scholarly Press AConserving Chronology Wildlife of Middlein African Missouri Landscapes Plains Kenya’sVillage Ewaso SitesEcosystem Edited by NicholasBy Craig J. M. Georgiadis Johnson with contributions by Stanley A. Ahler, Herbert Haas, and Georges Bonani SERIES PUBLICATIONS OF THE SMITHSONIAN INSTITUTION Emphasis upon publication as a means of “diffusing knowledge” was expressed by the first Secretary of the Smithsonian. In his formal plan for the Institution, Joseph Henry outlined a program that included the following statement: “It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge.” This theme of basic research has been adhered to through the years by thousands of titles issued in series publications under the Smithsonian imprint, com- mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Contributions to Anthropology Smithsonian Contributions to Botany Smithsonian Contributions to History and Technology Smithsonian Contributions to the Marine Sciences Smithsonian Contributions to Museum Conservation Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology In these series, the Institution publishes small papers and full-scale monographs that report on the research and collections of its various museums and bureaus. The Smithsonian Contributions Series are distributed via mailing lists to libraries, universities, and similar institu- tions throughout the world. Manuscripts submitted for series publication are received by the Smithsonian Institution Scholarly Press from authors with direct affilia- tion with the various Smithsonian museums or bureaus and are subject to peer review and review for compliance with manuscript preparation guidelines. -
Review of the Hylomyscus Denniae Group (Rodentia: Muridae) in Eastern Africa, with Comments on the Generic Allocation of Epimys Endorobae Heller
PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON 119(2):293–325. 2006. Review of the Hylomyscus denniae group (Rodentia: Muridae) in eastern Africa, with comments on the generic allocation of Epimys endorobae Heller Michael D. Carleton, Julian C. Kerbis Peterhans, and William T. Stanley (MDC) Department of Vertebrate Zoology, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560-0108, U.S.A., e-mail: [email protected]; (JKP) University College, Roosevelt University, Chicago, Illinois 60605, U.S.A.; Department of Zoology, Division of Mammals, The Field Museum of Natural History, Chicago, Illinois 60605, U.S.A., e-mail: [email protected]; (WTS) Department of Zoology, Division of Mammals, The Field Museum of Natural History, Chicago, Illinois 60605, U.S.A., e-mail: [email protected] Abstract.—The status and distribution of eastern African populations currently assigned to Hylomyscus denniae are reviewed based on morpho- logical and morphometric comparisons. Three species are considered valid, each confined largely to wet montane forest above 2000 meters: H. denniae (Thomas, 1906) proper from the Ruwenzori Mountains in the northern Albertine Rift (west-central Uganda and contiguous D. R. Congo); H. vulcanorum Lo¨nnberg & Gyldenstolpe, 1925 from mountains in the central Albertine Rift (southwestern Uganda, easternmost D. R. Congo, Rwanda, and Burundi); and H. endorobae (Heller, 1910) from mountains bounding the Gregory Rift Valley (west-central Kenya). Although endorobae has been interpreted as a small form of Praomys, additional data are presented that reinforce its membership within Hylomyscus and that clarify the status of Hylomyscus and Praomys as distinct genus-group taxa. The 12 species of Hylomyscus now currently recognized are provisionally arranged in six species groups (H. -
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. -
Volcanic Eruption Impacts Student Worksheet
Volcanic Eruption Impacts Student Worksheet Explosive and Effusive Volcanoes The type of volcanic eruption is largely determined by magma composition. Flux-mediated melting at subduction zones creates a felsic magma with high levels of carbon dioxide and water. These dissolved gases explode during eruption. Effusive volcanoes have a hotter, more mafic magma with lower levels of dissolved gas, allowing them to erupt more calmly (effusive eruption). Sinabung (Indonesia) Mount Sinabung is a stratovolcano located 40 km from the Lake Toba supervolcano in North Sumatra. It lies along the Sunda Arc, where the Indo-Australian plate subducts beneath the Sunda and Burma plates. After 1200 years of dormancy, Sinabung began erupting intermittently in 2010. Major eruptions have occurred regularly since November 2013. In November and December 2015, ash plumes reached 6 – 11 km in height on multiple occasions. Pyroclastic flows and ashfall blanketed the region in January 2014 and lava flows travelled down the south flank, advancing 2.5 km by April 2014. Pyroclastic flows in February 2014 killed 17 people in a town 3 km from the vent. In June 2015, ash falls affected areas 10 – 15 km from the summit on many occasions. A lahar in May 2016, caused fatalities in a village 20 km from Sinabung. Pyroclastic flows occurred frequently throughout 2016 and 2017 Eruption of Sinabung 6 October 2016 Major eruptions occurred in 2018 and 2019. In (Y Ginsu, public domain) February 2018, an eruption destroyed a lava dome of 1.6 million cubic metres. At least 10 pyroclastic flows extended up to 4.9 km and an ash plume rose more than 16 km in altitude. -
Module 7 Igneous Rocks IGNEOUS ROCKS
Module 7 Igneous Rocks IGNEOUS ROCKS ▪ Igneous Rocks form by crystallization of molten rock material IGNEOUS ROCKS ▪ Igneous Rocks form by crystallization of molten rock material ▪ Molten rock material below Earth’s surface is called magma ▪ Molten rock material erupted above Earth’s surface is called lava ▪ The name changes because the composition of the molten material changes as it is erupted due to escape of volatile gases Rocks Cycle Consolidation Crystallization Rock Forming Minerals 1200ºC Olivine High Ca-rich Pyroxene Ca-Na-rich Amphibole Intermediate Na-Ca-rich Continuous branch Continuous Discontinuous branch Discontinuous Biotite Na-rich Plagioclase feldspar of liquid increases liquid of 2 Temperature decreases Temperature SiO Low K-feldspar Muscovite Quartz 700ºC BOWEN’S REACTION SERIES Rock Forming Minerals Olivine Ca-rich Pyroxene Ca-Na-rich Amphibole Na-Ca-rich Continuous branch Continuous Discontinuous branch Discontinuous Biotite Na-rich Plagioclase feldspar K-feldspar Muscovite Quartz BOWEN’S REACTION SERIES Rock Forming Minerals High Temperature Mineral Suite Olivine • Isolated Tetrahedra Structure • Iron, magnesium, silicon, oxygen • Bowen’s Discontinuous Series Augite • Single Chain Structure (Pyroxene) • Iron, magnesium, calcium, silicon, aluminium, oxygen • Bowen’s Discontinuos Series Calcium Feldspar • Framework Silicate Structure (Plagioclase) • Calcium, silicon, aluminium, oxygen • Bowen’s Continuous Series Rock Forming Minerals Intermediate Temperature Mineral Suite Hornblende • Double Chain Structure (Amphibole) -
Report on Biodiversity and Tropical Forests in Indonesia
Report on Biodiversity and Tropical Forests in Indonesia Submitted in accordance with Foreign Assistance Act Sections 118/119 February 20, 2004 Prepared for USAID/Indonesia Jl. Medan Merdeka Selatan No. 3-5 Jakarta 10110 Indonesia Prepared by Steve Rhee, M.E.Sc. Darrell Kitchener, Ph.D. Tim Brown, Ph.D. Reed Merrill, M.Sc. Russ Dilts, Ph.D. Stacey Tighe, Ph.D. Table of Contents Table of Contents............................................................................................................................. i List of Tables .................................................................................................................................. v List of Figures............................................................................................................................... vii Acronyms....................................................................................................................................... ix Executive Summary.................................................................................................................... xvii 1. Introduction............................................................................................................................1- 1 2. Legislative and Institutional Structure Affecting Biological Resources...............................2 - 1 2.1 Government of Indonesia................................................................................................2 - 2 2.1.1 Legislative Basis for Protection and Management of Biodiversity and -
Three-Dimensional Magmatic Architecture of a Buried Shield Volcano
https://doi.org/10.1130/G47941.1 Manuscript received 22 January 2020 Revised manuscript received 24 August 2020 Manuscript accepted 29 August 2020 © 2020 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 12 October 2020 Inside the volcano: Three-dimensional magmatic architecture of a buried shield volcano Faye Walker1*, Nick Schofield1, John Millett1,2, Dave Jolley1, Simon Holford3, Sverre Planke2,4, Dougal A. Jerram4,5 and Reidun Myklebust6 1 Geology and Petroleum Geology, University of Aberdeen, Aberdeen AB24 3UE, UK 2 Volcanic Basin Petroleum Research, Blindernveien 5, N-0361 Oslo, Norway 3 Australian School of Petroleum, University of Adelaide, Adelaide, South Australia 5000, Australia 4 Centre for Earth Evolution and Dynamics (CEED), University of Oslo, N-0315 Oslo, Norway 5 DougalEARTH Ltd., Solihull B91 3NU, UK 6 TGS, Asker N-1386, Norway ABSTRACT its magma chamber have never been imaged in The nature and growth of magmatic plumbing systems are of fundamental importance detail before. to igneous geology. Traditionally, magma chambers have been viewed as rapidly emplaced Magma chambers have traditionally been bodies of molten rock or partially crystallized “magma mush” connected to the surface viewed as large, long-lived, geometrically sim- by a narrow cylindrical conduit (referred to as the “balloon-and-straw” model). Recent ple bodies of molten rock, which are emplaced data suggest, however, that magma chambers beneath volcanoes are formed incrementally rapidly and slowly crystallize to form plutons through amalgamation of smaller intrusions. Here we present the first high-resolution three- (Glazner et al., 2004; Annen et al., 2015; Jerram dimensional reconstruction of an ancient volcanic plumbing system as a large laccolithic and Bryan, 2018; Sparks et al., 2019). -
Sequences of Pleistocene Marine Terraces in the Santa Rosalia Area, Baja California Sur, Mexico
275 SEQUENCES OF PLEISTOCENE MARINE TERRACES IN THE SANTA ROSALIA AREA, BAJA CALIFORNlA SUR, MEXICO Luc ORTLIEB Instituto de Geologfa, Univ. Nal. Aut6n. de Mexico & O.R.S.T.O.M. Apdo. Postal 1159 Hermosillo, Sonora, Mexico. ABSTRACT The coastal area near Santa Rosalla and on the eastern flank of the La Re forma volcanic complex, in eastcentral Baja California, presents an exceptional sequence of Pleistocene marine terraces. These remnants of past high stands of sea-level have been studied along 11 traverses roughly perpendicular to the coast line. The shorelines interpreted to correspond to distinct interglacial sea-level are regularly distributed at elevations varying from about + 9 m to + 190 m above mean sea level. A number of nine main shorelines were identified. Since no radio metric dates are yet available, a tentative chronostratigraphy of these features has been inferred from the V28-238 deep-sea core paleoclimatic curve; according to these correlations nine "interglacial" isotopic stages would be represented: one in early Late Pleistocene, six in Middle Pleistocene, and two in late Early Pleistocene. The Santa Rosalla Formation previously attributed to the base of the Pleistocene is thought to be a late Early Pleistocene (about 1 M. y.) inter glacial marine deposit. The vertical motions in the whole coastal area have prob ably been constant during the Quaternary although uplift rates are interpreted to have changed from a near value of 240 mrn/ka to approximately 130 mm/ka , at about 350 000 years B.P. RESUMEN La costa cerca de Santa Rosalfa y de la ladera oriental del complejo volca nico de La Reforma, en el noreste de Baja California Sur, presenta una secuencia excepcional de terrazas marinas pleistocenicas. -
Geohazard Supersites and Natural Laboratories Initiative
Versión 1.0, 14 de octubre de 2015 www.earthobservations.org/gsnl.php Geohazard Supersites and Natural Laboratories Initiative A.1 Proposal Title: Volcano-tectonic Geohazard Interaction within the Nicaraguan Depression Volcanoes: Cosiguina, San Cristóbal, Telica, Cerro Negro, Momotombo, Península de Chiltepe, Masaya and Concepción A.2 Supersite Coordinator Email (Organization only) [email protected] Name: Iris Valeria Surname: Cruz Martínez Position: Director General of Geology and Geophysics Personal website: <In case a personal web page does not exist, please provide a CV below this table> Institución: Instituto Nicaragüense de Estudios Territoriales-INETER- Nicaragua Type of institution Government (Government, Education, other): The institution's web address: https://www.ineter.gob.ni/ Address: Front of Solidarity Hospital City: Managua Postal Code/Postal Code: 2110 Managua, Nicaragua Country: Nicaragua Province, Territory, State or Managua County: Phone number: Tel. +505-22492761 Fax +505-22491082 1 Versión 1.0, 14 de octubre de 2015 A.3 Core Supersite Team Email (Organization only) [email protected] Name: Federico Vladimir Surname: Gutiérrez Corea Position: Director of the Nicaraguan Institute of Territorial Studies-INETER- Nicaragua Personal website: http://www.vlado.es/ http://uni.academia.edu/FedericoVLADIMIRGutierrez/Curriculu mVitae Institution: Nicaraguan Institute of Territorial Studies-INETER-Nicaragua Type of institution Government (Government, Education, others): Institution's web address: https://www.ineter.gob.ni/ -
50156-001: Muara Laboh Geothermal Power Project
Draft Environmental Impact Assessment Report (ANDAL) Project Number: 50156-001 October 2013 INO: Muara Laboh Geothermal Power Project Prepared by PT Greencap NAA Indonesia for PT Supreme Energy Muara Laboh (PT SEML) This environmental impact assessment report is a document of the borrower. The views expressed herein do not necessarily represent those of ADB's Board of Directors, Management, or staff, and may be preliminary in nature. Your attention is directed to the “Term of Use” section of this website. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. Environmental Impact Assessment (ANDAL) Geothermal Development Activities for 250 MW Muara Laboh Geothermal Power Plant in South Solok Regency, West Sumatra Province October, 2013 Environmental Impact Assessment (ANDAL) Geothermal Development Activities for the 250 MW Muara Laboh Geothermal Power Plant (PLTP) in South Solok Regency, West Sumatra Province October, 2013 PREFACE PT Supreme Energy Muara Laboh (PT SEML), a company owned by PT Supreme Energy, GDF Suez (a company domiciled in France), and Sumitomo Corporation (a company domiciled in Japan), plan to conduct "Geothermal Development Activities for the 250 MW Muara Laboh Geothermal Power Plant in South Solok Regency, West Sumatra Province". The planned Geothermal Development Activities generally include the development and operation of geothermal power plant and the construction of supporting facilities. It is expected that the planned activities will give benefits in supporting the policy of Indonesian Government on energy diversification.