Alumni Newsletter No. 18
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Plate Tectonics, Volcanoes, and Earthquakes / Edited by John P
ISBN 978-1-61530-106-5 Published in 2011 by Britannica Educational Publishing (a trademark of Encyclopædia Britannica, Inc.) in association with Rosen Educational Services, LLC 29 East 21st Street, New York, NY 10010. Copyright © 2011 Encyclopædia Britannica, Inc. Britannica, Encyclopædia Britannica, and the Thistle logo are registered trademarks of Encyclopædia Britannica, Inc. All rights reserved. Rosen Educational Services materials copyright © 2011 Rosen Educational Services, LLC. All rights reserved. Distributed exclusively by Rosen Educational Services. For a listing of additional Britannica Educational Publishing titles, call toll free (800) 237-9932. First Edition Britannica Educational Publishing Michael I. Levy: Executive Editor J. E. Luebering: Senior Manager Marilyn L. Barton: Senior Coordinator, Production Control Steven Bosco: Director, Editorial Technologies Lisa S. Braucher: Senior Producer and Data Editor Yvette Charboneau: Senior Copy Editor Kathy Nakamura: Manager, Media Acquisition John P. Rafferty: Associate Editor, Earth Sciences Rosen Educational Services Alexandra Hanson-Harding: Editor Nelson Sá: Art Director Cindy Reiman: Photography Manager Nicole Russo: Designer Matthew Cauli: Cover Design Introduction by Therese Shea Library of Congress Cataloging-in-Publication Data Plate tectonics, volcanoes, and earthquakes / edited by John P. Rafferty. p. cm.—(Dynamic Earth) “In association with Britannica Educational Publishing, Rosen Educational Services.” Includes index. ISBN 978-1-61530-187-4 ( eBook) 1. Plate tectonics. -
Cassini RADAR Images at Hotei Arcus and Western Xanadu, Titan: Evidence for Geologically Recent Cryovolcanic Activity S
GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L04203, doi:10.1029/2008GL036415, 2009 Click Here for Full Article Cassini RADAR images at Hotei Arcus and western Xanadu, Titan: Evidence for geologically recent cryovolcanic activity S. D. Wall,1 R. M. Lopes,1 E. R. Stofan,2 C. A. Wood,3 J. L. Radebaugh,4 S. M. Ho¨rst,5 B. W. Stiles,1 R. M. Nelson,1 L. W. Kamp,1 M. A. Janssen,1 R. D. Lorenz,6 J. I. Lunine,5 T. G. Farr,1 G. Mitri,1 P. Paillou,7 F. Paganelli,2 and K. L. Mitchell1 Received 21 October 2008; revised 5 January 2009; accepted 8 January 2009; published 24 February 2009. [1] Images obtained by the Cassini Titan Radar Mapper retention age comparable with Earth or Venus (500 Myr) (RADAR) reveal lobate, flowlike features in the Hotei [Lorenz et al., 2007]). Arcus region that embay and cover surrounding terrains and [4] Most putative cryovolcanic features are located at mid channels. We conclude that they are cryovolcanic lava flows to high northern latitudes [Elachi et al., 2005; Lopes et al., younger than surrounding terrain, although we cannot reject 2007]. They are characterized by lobate boundaries and the sedimentary alternative. Their appearance is grossly relatively uniform radar properties, with flow features similar to another region in western Xanadu and unlike most brighter than their surroundings. Cryovolcanic flows are of the other volcanic regions on Titan. Both regions quite limited in area compared to the more extensive dune correspond to those identified by Cassini’s Visual and fields [Radebaugh et al., 2008] or lakes [Hayes et al., Infrared Mapping Spectrometer (VIMS) as having variable 2008]. -
Summary of the Mineral Information Package for the Khanneshin Carbonatite Area of Interest
Chapter 21A. Summary of the Mineral Information Package for the Khanneshin Carbonatite Area of Interest Contribution by Robert D. Tucker, Harvey E. Belkin, Klaus J. Schulz, Stephen G. Peters, and Kim P. Buttleman Abstract The Khanneshin carbonatite is a deeply dissected igneous complex of Quaternary age that rises approximately 700 meters above the flat-lying Neogene sediments of the Registan Desert, Helmand Province, Afghanistan. The complex consists almost exclusively of carbonate-rich intrusive and extrusive igneous rocks, crudely circular in outline, with only three small hypabyssal plugs of leucite phonolite and leucitite outcropping in the southeastern part of the complex. The complex is broadly divisible into a central intrusive vent (or massif), approximately 4 kilometers in diameter, consisting of coarse-grained sövite and brecciated and agglomeratic barite-ankerite alvikite; a thin marginal zone (less than 1 kilometer wide) of outwardly dipping (5°–45°). Neogene sedimentary strata; and a peripheral apron of volcanic and volcaniclastic strata extending another 3–5 kilometers away from the central intrusive massif. Small satellitic intrusions of biotite-calcite carbonatite, no larger than 400 meters in diameter, crop out on the southern and southeastern margin of the central intrusive massif. In the 1970s several teams of Soviet geologists identified prospective areas of interest for uranium, phosphorus, and light rare earth element (LREE) mineralization in four regions of the carbonatite complex. High uranium concentrations are reported in two regions; the greatest concentrations are confined to silicified shear zones in sandy clay approximately 1.1 kilometers southwest of the peripheral part of the central vent. An area of phosphorus enrichment, primarily occurring in apatite, is present in coarse-grained agglomeratic alvikite, with abundant fenite xenoliths, approximately 750 meters south of the periphery of the central vent. -
Hydrovolcanic Vs Magmatic Processes in Forming Maars and Associated Pyroclasts: the Calatrava -Spain- Case History
1 Hydrovolcanic vs Magmatic Processes in Forming Maars and Associated Pyroclasts: The Calatrava -Spain- Case History F. Stoppa, G. Rosatelli, M. Schiazza and A. Tranquilli Università Gabriele d'Annunzio, Dipartimento di Scienze, Chieti Italy 1. Introduction The Calatrava Volcanic Field (CVF) of Castilla-La Mancha is characterised by numerous monogenetic volcanic centres, that erupted mainly foidites, melilitites and carbonatites (ultra-alkaline rock-association sensu, Le Bas, 1981) carrying abundant mantle xenoliths. At CVF, carbonatites have been described by Bailey et al. (2005) and Stoppa et al. (2011). Along with the volcanic field of Eifel of Germany, Limagne basin of France and Intra-mountain Ultra-alkaline Province (IUP) of Italy, the CVF encompasses the most numerous Pliocene- Quaternary extrusive carbonatites in Western Europe in terms of dimension, number and size of volcanoes (Bailey et al., 2005; Bailey et al., 2006). Similar volcanic fields are Toro- Akole and Bufumbira in Uganda (Bailey & Collier, 2000), the Avon district in Missouri (Callicoat et al., 2008), Mata da Corda in Brazil (Junqueira-Brod et al., 1999) and West Qinling in Gansu Province, China (Yu et al., 2003). In spite of abundant local studies (González Cárdenas et al., 2010; Peinado et al., 2009), the CVF has been mostly neglected by the international audience, although Bailey (2005) outlined the need for a long-term research program on CVF. This work focuses on the role of deep CO2 at CVF, which is considered an intrinsic component of carbonatitic mantle magmatism (Hamilton et al., 1979). Previous, studies of CVF volcanoes considered that the hydrovolcanism is a necessary and sufficient condition to explain the CVF volcanological features, and, as a corollary that the carbonate present in the pyroclastic rocks is remobilised limestones (e.g., López-Ruiz et al., 2002). -
A Simple Classification of Volcanic Rocks Summary Introduction
A Simple Classification of Volcanic Rocks E. A. K. MIDDLEMOST* Summary There is a considerable volume of information on the abundance, distribu- tion and chemical composition of volcanic rocks. In this paper an attempt is made to use these data to construct a simple chemical classification of the volcanic rocks. Silica content is used to divide the rocks into seven major classes; and the major classes are then subdivided using soda, potash, alumina and lime. Introduction At the present time there is a reawakening of interest in the problem of the classification of igneous rocks (STRECr~ISEN, 1965, 1967; IRVINE and BARAaAR, 1971). Much of this interest has been generated by attempts to use electronic computers to store and manip- ulate large volumes of petrological data (CHAYES, 1969b; HUBAUX, 1969; HARRISON and SABINE, 1970). It has also been shown that it is not possible to devise a single comprehensive classification of igneous rocks that can be used in both the fields of petrography and petro- genesis (MIDDLEMOST, 1971). Petrographic classifications are essentially concerned with producing a systematic framework that provides compartments into which rocks can be placed (i.e. JOHANNSEN, 1931). The needs of petrogenesis are different, as this branch of petrology is constantly searching for ways in which to adapt our vocabulary of rock names so that the language we use is able to change in response to new discoveries, or new ways of interpreting old discoveries. * Dept. of Geology and Geophysics, University of Sydney, NSW, Australia. I -- 383 There is a large store of information on the abundance, composi- tion and distribution of igneous rocks. -
Review of Local and Global Impacts of Volcanic Eruptions and Disaster Management Practices: the Indonesian Example
geosciences Review Review of Local and Global Impacts of Volcanic Eruptions and Disaster Management Practices: The Indonesian Example Mukhamad N. Malawani 1,2, Franck Lavigne 1,3,* , Christopher Gomez 2,4 , Bachtiar W. Mutaqin 2 and Danang S. Hadmoko 2 1 Laboratoire de Géographie Physique, Université Paris 1 Panthéon-Sorbonne, UMR 8591, 92195 Meudon, France; [email protected] 2 Disaster and Risk Management Research Group, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta 55281, Indonesia; [email protected] (C.G.); [email protected] (B.W.M.); [email protected] (D.S.H.) 3 Institut Universitaire de France, 75005 Paris, France 4 Laboratory of Sediment Hazards and Disaster Risk, Kobe University, Kobe City 658-0022, Japan * Correspondence: [email protected] Abstract: This paper discusses the relations between the impacts of volcanic eruptions at multiple- scales and the related-issues of disaster-risk reduction (DRR). The review is structured around local and global impacts of volcanic eruptions, which have not been widely discussed in the literature, in terms of DRR issues. We classify the impacts at local scale on four different geographical features: impacts on the drainage system, on the structural morphology, on the water bodies, and the impact Citation: Malawani, M.N.; on societies and the environment. It has been demonstrated that information on local impacts can Lavigne, F.; Gomez, C.; be integrated into four phases of the DRR, i.e., monitoring, mapping, emergency, and recovery. In Mutaqin, B.W.; Hadmoko, D.S. contrast, information on the global impacts (e.g., global disruption on climate and air traffic) only fits Review of Local and Global Impacts the first DRR phase. -
The Year Without a Summer
The Year Without a Summer In 1816, half a foot of snow fell in New England. That would be Mount Tambora, an active completely unremarkable. Except that it was in one day—in June. stratovolcano that is a peninsula of and the highest That same summer, Mary Shelley spent a chilly vacation holed peak on the island of up indoors—and used the time to write Frankenstein. Crops Sumbawa in Indonesia. failed around the world, plunging Thomas Jefferson into serious Credit: Jialiang Gao (peace-on- debt for the rest of his life. Oats became scarce in Germany, earth.org) via Wikimedia Commons making horse travel expensive—and leading to the invention (CC BY-SA 3.0 [http://creative- of the bicycle. Struggling farmers in China began raising opium, commons.org/licenses/by-sa/3.0]) giving rise to a drug trade that has lasted to modern times. And famine in many areas led to widespread disease, including a cholera outbreak that killed millions. What was the cause of all this chaos? A year earlier, a volcano erupted in Indonesia. Larger than Krakatoa, Vesuvius, or Mount St. Helens, Mount Tambora erupted for 2 weeks straight. Around it, nearly 100,000 people died, buried under thick layers of ash like in Pompeii. Greenhouse-gas emissions from the eruption, which could have warmed the atmosphere, were offset by particulates and sulfur dioxide gas. Ash and dust blocked out the sun temporarily, darkening skies around the world. The sulfur dioxide was longer-lasting, becoming aerosols that reflected the sun’s heat for 3 years! This turned 1816 into “The Year Without a Summer,” as it was called, with long-term global effects. -
Alumni Newsletter No. 22
McGill University Alumni Newsletter #22 January 2019 Crystals form the building blocks of much of our world. Studying them closely lets us understand the structure of biomolecules of things like our bones and muscles, medications, and even chocolate. Here are five things you might not know about crystals and crystallography 1. Crystallography takes the prize The father and son combination of father William Henry Bragg and son William Lawrence Bragg first revealed the structure of salt and won the Nobel Prize in Physics in 1915 for their services “in the analysis of crystal structure by means of x-ray.” So far, the Braggs are the only father and son team to receive a Nobel Prize. In fact, crystallography is the science or discipline directly attributable to winning the most Nobel Prizes, taking the award 28 times. X-ray crystallography has developed at a rapid pace in the last 20 years. Scientists first used the technique over 100 years ago when they determined the crystal structure of salt. In essence, the method involves placing a tiny crystal in the path of an x-ray beam. As the x-ray passes through the crystal, the radiation is diffracted into a pattern by the atoms that make up the molecules in the crystal structure. The diffraction pattern is like a fingerprint that identifies not only the nature of the atoms and bonds in the molecules, but also their three-dimensional arrangement. It is the only analytical method that can achieve this level of analysis in such a complete and unambiguous fashion. 2. Around 90 percent of all drugs are crystals That’s because it’s much easier to control the solid state of a crystalline structure—even using a gel would involve crystals that are suspended in a gooey substance to aid the delivery of the drug involved. -
Canadian Mineralogist, 51
785 The Canadian Mineralogist Vol. 51, pp. 785-800 (2013) DOI : 10.3749/canmin.51.5.785 A COMBINED GEOCHEMICAL AND GEOCHRONOLOGICAL INVESTIGATION OF NIOCALITE FROM THE OKA CARBONATITE COMPLEX, CANADA WEI CHEN§, ANTONIO SIMONETTI, AND PETER C. BURNS* Department of Civil & Environmental Engineering & Earth Sciences, 156 Fitzpatrick Hall, University of Notre Dame, Notre Dame IN, 46556 USA ABSTRACT This study is the first to report a detailed geochemical investigation and in situ U-Pb ages for niocalite, which occurs within carbonatite from the Bond Zone area of the Oka Carbonatite Complex (Canada). Niocalite is a Nb-disilicate member of the låvenite−cuspidine group. The major element composition of the niocalite studied here is relatively homogeneous with the average formula of: (Na0.34Fe0.06Mn0.19Mg0.09Ca13.40REE0.15Ti0.02)Σ14.25Nb2.12Ta0.06(Si2O7)4O7.65F2.44. Niocalite is enriched in minor and trace elements [i.e., Ta, Ti, and rare earth elements (REEs) up to 4.35 wt.%], with double- and triple-valenced elements (i.e., Sr, Y, REEs) substituting at different Ca-occupied lattice sites. The chondrite-normalized REE patterns for niocalite are LREE-enriched (~104 times chondrite) and negatively sloped. In addition, niocalite has higher HREE contents compared to those for co-existing apatite from the identical carbonatite sample. This result is expected based on bond valence data because of differing cation sizes. In situ U-Pb ages for niocalite from three carbonatite samples obtained by LA-ICP-MS define a wide range of ages, between ~111 and ~133 Ma. Niocalite from one carbonatite sample yields a bimodal distribution with weighted mean 206Pb/238U ages of 110.1 ± 5.0 Ma and 133.2 ± 6.1 Ma, and overlap those of co-existing apatite for the same sample. -
Adamsite-(Y), a New Sodium–Yttrium Carbonate Mineral
1457 The Canadian Mineralogist Vol. 38, pp. 1457-1466 (2000) ADAMSITE-(Y), A NEW SODIUM–YTTRIUM CARBONATE MINERAL SPECIES FROM MONT SAINT-HILAIRE, QUEBEC JOEL D. GRICE§ and ROBERT A. GAULT Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ANDREW C. ROBERTS Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A 0E8, Canada MARK A. COOPER Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada ABSTRACT Adamsite-(Y), ideally NaY(CO3)2•6H2O, is a newly identified mineral from the Poudrette quarry, Mont Saint-Hilaire, Quebec. It occurs as groups of colorless to white and pale pink, rarely pale purple, flat, acicular to fibrous crystals. These crystals are up to 2.5 cm in length and form spherical radiating aggregates. Associated minerals include aegirine, albite, analcime, ancylite-(Ce), calcite, catapleiite, dawsonite, donnayite-(Y), elpidite, epididymite, eudialyte, eudidymite, fluorite, franconite, gaidonnayite, galena, genthelvite, gmelinite, gonnardite, horváthite-(Y), kupletskite, leifite, microcline, molybdenite, narsarsukite, natrolite, nenadkevichite, petersenite-(Ce), polylithionite, pyrochlore, quartz, rhodochrosite, rutile, sabinaite, sérandite, siderite, sphalerite, thomasclarkite-(Y), zircon and an unidentified Na–REE carbonate (UK 91). The transparent to translucent mineral has a vitreous to pearly luster and a white streak. It is soft (Mohs hardness 3) and brittle with perfect {001} and good {100} and {010} cleav- ␣  ␥ ° ° ages. Adamsite-(Y) is biaxial positive, = V 1.480(4), = 1.498(2), = 1.571(4), 2Vmeas. = 53(3) , 2Vcalc. = 55 and is nonpleochroic. Optical orientation: X = [001], Y = b, Z a = 14° (in  obtuse). It is triclinic, space group P1,¯ with unit-cell parameters refined from powder data: a 6.262(2), b 13.047(6), c 13.220(5) Å, ␣ 91.17(4),  103.70(4), ␥ 89.99(4)°, V 1049.1(5) Å3 and Z = 4. -
How Mount Agung's Eruption Can Create the World's Most Fertile Soil
How Mount Agung's eruption can create the world's most fertile soil https://theconversation.com/how-mount-agungs-eruption-can-create-the... Disiplin ilmiah, gaya jurnalistik How Mount Agung’s eruption can create the world’s most fertile soil Oktober 5, 2017 3.58pm WIB Balinese farmers with Mount Agung in the background. Areas with high volcanic activity also have some of the world’s most fertile farmlands. Reuters/Darren Whiteside Mount Agung in Bali is currently on the verge of eruption, and more than 100,000 Penulis people have been evacuated. However, one of us (Dian) is preparing to go into the area when it erupts, to collect the ash. This eruption is likely to be catastrophic, spewing lava and ashes at temperatures up to Budiman Minasny 1,250℃, posing serious risk to humans and their livelihoods. Ash ejected from volcano Professor in Soil-Landscape Modelling, not only affects aviation and tourism, but can also affect life and cause much nuisance to University of Sydney farmers, burying agricultural land and damaging crops. However, in the long term, the ash will create world’s most productive soils. Anthony Reid Emeritus Professor, School of Culture, 1 of 5 10/7/2017, 5:37 AM How Mount Agung's eruption can create the world's most fertile soil https://theconversation.com/how-mount-agungs-eruption-can-create-the... History and Language, Australian National University Dian Fiantis Professor of Soil Science, Universitas Andalas Alih bahasa Bahasa Indonesia English Read more: Bali’s Mount Agung threatens to erupt for the first time in more than 50 years While volcanic soils only cover 1% of the world’s land surface, they can support 10% of the world’s population, including some areas with the highest population densities. -
Th- Ra- Pb Disequilibria. 2 3 Ramananda
ManuscriptView metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Woods Hole Open Access Server 1 Timescales of Magmatic Processes and Eruption Ages of the Nyiragongo 2 volcanics from 238U-230Th-226Ra-210Pb disequilibria. 3 4 Ramananda Chakrabarti 1#*, Kenneth W. W. Sims2, 3, Asish R. Basu1, Mark Reagan4, 5 Jacques Durieux5 6 7 1. Department of Earth and Environmental Sciences, University of Rochester, 8 Rochester, NY-14627 9 10 2. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, 11 Woods Hole, Massachusetts, MA 02543 12 13 3. Dept of Geology and Geophysics, University of Wyoming, Laramie, WY 82071 14 15 4. Department of Geoscience, University of Iowa, Iowa City, Iowa 52242 16 17 5. Deceased, formerly at Unite De Gestion Des Risques Volcaniques, UNDP / 18 UNOPS, Goma - Nord-Kivu - RD Congo 19 20 # Current address: Department of Earth and Planetary Sciences, Harvard University, 21 Cambridge, MA 02138 22 * Corresponding author - email: [email protected] 23 24 Keywords: Silica-undersaturated volcanism, 238U-230Th-226Ra-210Pb series 25 disequilibria, Magma transport and residence time, Carbonate metasomatism, Volcanic 26 hazard assessment. 27 28 29 Abstract 30 The silica-undersaturated Nyiragongo volcanics, located in the East African rift, have 31 globally unique chemical compositions and unusually low viscosities, only higher than 32 carbonatite lavas, for terrestrial silicate magmas. We report 238U-230Th-226Ra-210Pb series 33 disequilibria in 13 recent and prehistoric lava samples from Nyiragongo including those 34 from the 2002 flank eruption and a 2003 lava lake sample. (230Th/238U) ranges from 0.90- 35 0.97 in the recent lavas and from 0.94-1.09 in the prehistoric lavas.