{DOWNLOAD} Ring of Fire Pdf Free Download
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
AMEC Report Template
BLACKWATER GOLD PROJECT APPLICATION FOR AN ENVIRONMENTAL ASSESSMENT CERTIFICATE / ENVIRONMENTAL IMPACT STATEMENT POTENTIAL EFFECTS OF THE ENVIRONMENT ON THE PROJECT TABLE OF CONTENTS 11 POTENTIAL EFFECTS OF THE ENVIRONMENT ON THE PROJECT ............................. 11-1 11.1 Introduction .............................................................................................................. 11-1 11.2 Information Sources and Methods .......................................................................... 11-2 11.3 Subsidence .............................................................................................................. 11-2 11.4 Landslides/Mass Wasting/Slope Stability ................................................................ 11-3 11.4.1 Baseline ...................................................................................................... 11-3 11.4.2 Potential Effects on the Project and Mitigation ........................................... 11-4 11.4.3 Summary .................................................................................................... 11-5 11.5 Avalanches .............................................................................................................. 11-6 11.5.1 Baseline ...................................................................................................... 11-6 11.5.2 Potential Effects on the Project and Mitigation ........................................... 11-6 11.5.3 Summary ................................................................................................... -
Holocene Tephras in Lake Cores from Northern British Columbia, Canada
935 Holocene tephras in lake cores from northern British Columbia, Canada Thomas R. Lakeman, John J. Clague, Brian Menounos, Gerald D. Osborn, Britta J.L. Jensen, and Duane G. Froese Abstract: Sediment cores recovered from alpine and subalpine lakes up to 250 km apart in northern British Columbia con- tain five previously unrecognized tephras. Two black phonolitic tephras, each 5–10 mm thick, occur within 2–4 cm of each other in basal sediments from seven lakes in the Finlay River – Dease Lake area. The upper and lower Finlay tephras are slightly older than 10 220 – 10 560 cal year B.P. and likely originate from two closely spaced eruptions of one or two large volcanoes in the northern Cordilleran volcanic province. The Finlay tephras occur at the transition between deglacial sediments and organic-rich postglacial mud in the lake cores and, therefore, closely delimit the termination of the Fraser Glaciation in northern British Columbia. Sediments in Bob Quinn Lake, which lies on the east edge of the northern Coast Mountains, contain two black tephras that differ in age and composition from the Finlay tephras. The lower Bob Quinn tephra is 3–4 mm thick, basaltic in composition, and is derived from an eruption in the Iskut River volcanic field about 9400 cal years ago. The upper Bob Quinn tephra is 12 mm thick, trachytic in composition, and probably 7000–8000 cal years old. A fifth tephra occurs as a cryptotephra near the top of two cores from the Finlay River area and is correlated to the east lobe of the White River tephra (ca. -
Cascades Volcano Observatory Monitoring Cascade Volcanoes
Cascades Volcano Observatory Monitoring Cascade Volcanoes http://volcanoes.usgs.gov/observatories/cvo/cvo_monitoring.html About CVO Monitoring Cascade Volcanoes Volcano Updates Volcano eruption forecasting relies on several disciplines of volcanology. Hazards Active volcanoes are complex natural systems, Monitoring and understanding a volcano's behaviors requires the attention of specialists from many science Seismicity disciplines. It demands a combination of current Deformation knowledge about magma systems, tectonic plate motion, volcano deformation, earthquakes, gases, Volcanic Gas chemistry, volcano histories, processes, and Lahar Detection hazards. Hydrothermal No single tool or technique can adequately monitor or predict volcanic behaviors. Therefore, Innovative Techniques volcanologists rely on an assortment of instruments and techniques to monitor volcanic unrest. This CVO Education requires placement of monitoring instruments both Prepare close to and far away from the primary source of eruptive activity (e.g. in a crater, on the crater rim, Multimedia and on the volcano's flanks). By placing sensitive monitoring instruments at hazardous volcanoes in Regional Volcanism Helicopter dropping off monitoring equipment at Mount St. advance of the unrest, the USGS CVO helps to Helens, Washington. ensure that communities at risk can be forewarned with sufficient time to prepare and implement response plans and mitigation measures. Recommendations for the numbers and types of ground-based sensors were made by an interdisciplinary team of scientists as part of planning for the National Volcano Early Warning System. CVO uses these recommendations to plan monitoring improvements throughout the Cascades. You can watch interviews with volcano scientists (Web Shorts) about their research and monitoring efforts and videos about volcano monitoring techniques in the Multimedia section of this website. -
El Volcán Chiliques Y El" Morar-En-El-Mundo" De Una
Estudios Atacameños ISSN: 0716-0925 [email protected] Universidad Católica del Norte Chile Moyano, Ricardo; Uríbe, Carlos El volcán chiliques y el "morar-en-el-mundo" de una comunidad atacameña del norte de Chile Estudios Atacameños, núm. 43, 2012, pp. 187-208 Universidad Católica del Norte San Pedro de Atacama, Chile Disponible en: http://www.redalyc.org/articulo.oa?id=31526842010 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto EL VOLCÁN CHILIQUES y EL "MORAR-EN-EL MUNDO" DE UNA COMUNIDAD ATACAMEÑA DEL NORTE DE CHILE Ricardo Moyana' y Carlos Uríbe' --+ INTRODUCCIÓN Resumen El volcán Chiliques corresponde a un estrato volcán de En estetrabajosemuestranlosresul tadospreliminares del 5778 rn.s.n.rn., ubicado en la Región de Antofagasta. reconocimiento arqueológico delvolcán Chílíques (2}034'5 /67°42'W /5778 m.s.nm.), desierto deAtacama, nortedeChile. El objetivo fue norte de Chile (23'34'5, 6i42'W) (Figura 1). Esta mon confirmar laexistencia desitiosarqueológicos enlazona, asícomo taña no habría registrado actividad volcánica durante los una posible líneaceque proyectadadesdeelcentroceremonial de últimos 10.000 años, sin embargo, en enero de 2002 Socaire. Los resul tadosconfirman laimportancia delvolcán Chiliques una imagen infrarroja obtenida por ASTER (Advanced como propiciadordefenómenos meteorológicos dentrodelsistema de Spaceborne Thermal Emission and Reflection Radio montañassagradas invocadas para laceremoníade limpia decanalesdel mesdeoctubreenSocaire. Chílíques habríaconstituidoun "axis mund¡' meter) de la NASA, reveló ciertos hotspots en una zona porlassiguientes razones: su forma cónica yvisibilidad permanente cercana al cráter y edificiovolcánico.' desdeotrosadoratorios prehíspánícos. -
Information Circular 41: Origin of Cascade Landscapes
111ackin I CdrlJ .rc-1J ORIGIN OF CASCADE LANDSCAPES ---=-~--=---------=---- FRONTISPIECE Picket Range in upper Skagit area, Northern Cascade Mountains. Snowfields occupy a former ice-filled cirque. Grass is enroaching on ice-polished rock surfaces. State of Washington DANIEL J. EVANS, Governor Department of Conservation ROY MUNDY, Director DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, SupervisoT Information Circular No. 41 ORIGIN OF CASCADE LANDSCAPES By J. HOOVER MACKIN and ALLENS. CARY STATE PRINTING PLANT, OLYMPIA, WASHINGTON 1965 For sale by Department of Conservation, Olympia, Washington. Price, 50 cents. FOREWORD The Cascade Range has had an important influence on the lives of a great many people ever since man has inhabited the Northwest. The mountains were a barrier to Indian travel; they were a challenge to the westward migration of the early settlers in the area; they posed serious problems for the early railroad builders; and they still constitute an obstruction to east-west travel. A large part of the timber, mineral, and surface water resources of the State come from the Cascades. About 80 percent of the area covered by glaciers in the United States, exclusive of Alaska, is in the Cascades of Washington. This region includes some of the finest mountain scenery in the country and is a popular outdoor recreation area. The Cascade Range is a source of economic value to many, a source of pleasure to many others, and a problem or source of irritation to some. Regardless of their reactions, many people have wondered about the origin of the mountains How and when did the Cascades come into being, and what forces were responsible for the construction job? -This report, "Origin of Cascade Landscapes," gives the answers to these questions. -
Geology of the Hoodoo Mountain Area (NTS 104B/14W)
Geology of the Hoodoo Mountain Area (NTS 104B/14W) by M.G. Mihalynuk1, A. Zagorevski2 and F. Cordey3 KEYWORDS: Hoodoo Mountain, Sphaler Creek, Stikine information is included herein; see Mihalynuk et al. assemblage, Stuhini Group, copper porphyry, Galore (2010, 2011a) for additional unit descriptions and Creek, Dirk prospect, Telena prospect, volcanic-hosted previous work. massive sulphide, Rock and Roll, Andrei Icefield, Iskut River LOCATION AND ACCESS INTRODUCTION Hoodoo Mountain area (NTS 104/14W) can be accessed either via the Bronson airstrip to the immediate Hoodoo Mountain area is located between the south, or via the Espaw camp located at kilometre 91 on enormous copper-gold resource defined at Galore Creek the incomplete Galore Creek access road, immediately and the past-producing gold deposits of the Bronson north of the map area. At the time of our field program, Camp. Reserves at Galore Creek in proven and probable both required air transport from Bob Quinn airstrip categories are 528 Mt grading 0.58% Cu, 0.32 g/t Au and located on Highway 37, approximately 400 km by road 6.02 g/t Ag (Gill et al., 2011). In the Bronson Camp, the from both Smithers and Terrace (Figure 1). Bob Quinn Snip mine produced 32 million grams of gold, 12 million airstrip is 60 km from both Bronson airstrip and Espaw grams silver and nearly 250 000 kilograms copper from Camp. about 1.2 million tonnes between 1991 and 1999; Johnny Mountain produced for less than two years with produced, proven, probable and “possible” categories totalling 0.622 Mt at 19.54 g/t Au (MINFILE, 2011). -
2016 Cascade Volcanoes.Pptx
The Cascade Range Lake Almanor Mt Garibaldi 1 Mt Garibaldi, Brish Columbia 2 hp://volcano.si.edu/Photos/full/027024.jpg Lassen Peak from Lake Almanor, California hps://californiawolves.files.wordpress.com/2015/05/3437400098_5bcbed91d9.jpg 3 Volcanic Activity • Diffuse degassing and fumaroles • Hawaiian eruptions • Lava lakes • Strombolian eruptions • Vulcanian eruptions • Visuvian or sub-plinian eruptions (M‹4) • Plinian eruptions (M=4+) • Pelean eruptions • Hydrovolcanic eruptions 4 5 6 Vent: Any opening at the Earth's surface through which magma erupts or volcanic gases are emied. 7 Vent: Any opening at the Earth's surface through which magma erupts or volcanic gases are emied. Caldera:A large basin-shaped volcanic depression with a diameter many mes larger than included volcanic vents; may range from 2 to 50 km (1 to 30 mi) across. Commonly formed when magma is withdrawn or erupted from a shallow underground magma reservoir. The removal of large volumes of magma may result in loss of structural support for the overlying rock, thereby leading to collapse of the ground and formaon of this type of large depression. Calderas are different from craters, which are smaller, circular depressions created primarily by explosive excavaon of rock during erupons. hps://volcanoes.usgs.gov/vsc/glossary/caldera.html 8 Model of Unzen Volcanic Dome, Japan hp://www.eri.u-tokyo.ac.jp/KOHO/Yoran2003/sec4-5-eng.files/image002.jpg 9 10 Shield Volcanoes Belnap Crater, McKenzie Pass 11 Belnap Crater 12 AA lava flow 13 Medicine Lake Shield volcano 14 15 hp://volcanoes.usgs.gov/volcanoes/medicine_lake/geo_hist_summary.html -
Towards Interactive Global Paleogeographic Maps, New Reconstructions at 60, 40 and 20 Ma
Earth-Science Reviews 214 (2021) 103508 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Towards interactive global paleogeographic maps, new reconstructions at 60, 40 and 20 Ma F. Poblete a,b,*, G. Dupont-Nivet a,c, A. Licht d, D.J.J. van Hinsbergen e, P. Roperch a, M. G. Mihalynuk f, S.T. Johnston g, F. Guillocheau a, G. Baby a, F. Fluteau h, C. Robin a, T.J. M. van der Linden e,i, D. Ruiz c, M.L.J. Baatsen j a G´eosciences Rennes, UMR CNRS 6118, Rennes, 35042 Rennes Cedex, France b Departamento de Geología, Facultad de Ciencias Físicas y Matematicas,´ Universidad de Chile, Chile c Universitat¨ Potsdam, Institute of Geoscience, 14476 Potsdam, Germany d Centre Europ´een de Recherche et d’Enseignement des G´eosciences de l’Environnement (Cerege), UMR CNRS 7330, 13545 Aix-en-Provence, France e Department of Earth Sciences, Utrecht University, Princetonlaan 8a, 3584 CB, Utrecht, the Netherlands f British Columbia Geological Survey, Vancouver, Canada g Department of Earth and Atmospheric Sciences, University of Alberta, Canada h Universit´e de Paris, Institut de physique du globe de Paris, CNRS, F-75005 Paris, France i Thomas van der Linden – LinGeo, Berlin, Germany j IMAU, Utrecht University, Princetonplein 5, 3584CC Utrecht, the Netherlands ARTICLE INFO ABSTRACT Keywords: Paleogeographic maps are essential tools for understanding Earth system dynamics. They provide boundary Paleogeographic maps conditions for climate and geodynamic modelling, for analysing surface processes and biotic interactions. Paleoelevation However, the temporal and spatial distribution of key features such as seaways and mountain belts that govern Cenozoic climate changes and biotic interchange differ between various paleogeographies that require regular updates Eocene-Oligocene transition with new data and models. -
Canadian Volcanoes, Based on Recent Seismic Activity; There Are Over 200 Geological Young Volcanic Centres
Volcanoes of Canada 1 V4 C.J. Hickson and M. Ulmi, Jan. 3, 2006 • Global Volcanism and Plate tectonics Where do volcanoes occur? Driving forces • Volcano chemistry and eruption types • Volcanic Hazards Pyroclastic flows and surges Lava flows Ash fall (tephra) Lahars/Debris Flows Debris Avalanches Volcanic Gases • Anatomy of an Eruption – Mt. St. Helens • Volcanoes of Canada Stikine volcanic belt Presentation Outline Anahim volcanic belt Wells Gray – Clearwater volcanic field 2 Garibaldi volcanic belt • USA volcanoes – Cascade Magmatic Arc V4 Volcanoes in Our Backyard Global Volcanism and Plate tectonics In Canada, British Columbia and Yukon are the host to a vast wealth of volcanic 3 landforms. V4 How many active volcanoes are there on Earth? • Erupting now about 20 • Each year 50-70 • Each decade about 160 • Historical eruptions about 550 Global Volcanism and Plate tectonics • Holocene eruptions (last 10,000 years) about 1500 Although none of Canada’s volcanoes are erupting now, they have been active as recently as a couple of 4 hundred years ago. V4 The Earth’s Beginning Global Volcanism and Plate tectonics 5 V4 The Earth’s Beginning These global forces have created, mountain Global Volcanism and Plate tectonics ranges, continents and oceans. 6 V4 continental crust ic ocean crust mantle Where do volcanoes occur? Global Volcanism and Plate tectonics 7 V4 Driving Forces: Moving Plates Global Volcanism and Plate tectonics 8 V4 Driving Forces: Subduction Global Volcanism and Plate tectonics 9 V4 Driving Forces: Hot Spots Global Volcanism and Plate tectonics 10 V4 Driving Forces: Rifting Global Volcanism and Plate tectonics Ocean plates moving apart create new crust. -
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. -
Volcanoes at Antarctica
ClimateChangeTheFacts.org.au FACT SHEET #4 FIRE AND ICE: VOLCANOES AT ANTARCTICA HOT TAKES Figure 1: Volcanoes of West Antarctica3 1 At West Antarctica, 91 newly discovered volcanoes lie buried kilometres beneath a thick ice sheet. Ronne-Filchner Ice Shelf 2 The ice sheet has co-existed with volcanism for millions 0 of years. 90 W Ellsworth Whitmore South Pole 3 Future volcanism is inevitable but fears it would Land Mountains destabilise the ice sheet and accelerate sea-level rise Mount Takahe are unfounded. Transantarctic Mount Sidley Mountains 135 Mount Cumming 0 E Marie Many people are concerned the (slight) global warming Amundsen Sea Byrd observed over the past 100 years is unnatural and caused Land 80 0 Mount Siple S Ross Ice Shelf by human activity. Some also believe this will accelerate melting of ice sheets and glaciers and cause rapid 0 W Mount Erebus catastrophic sea level rise. However this conclusion is 135 Ross Sea dependent on complex computer models containing many W 0 untested assumptions. A great many of the assumptions the 70 0 1000 km S models need to get right before they are of any use are only 180 very poorly understood. Visible volcanoes Volcanoes hidden beneath ice Some environmentalists believe volcanoes associated with the Not even the large inland volcanoes protruding through the West Antarctic Ice Sheet (WAIS) could magnify the ‘climate WAIS were known to exist before 1940 when first seen from change’ risk to the ice sheet. However close examination of the air. Mount Takahe is so remote it was not visited until the relationship between the volcanoes and the ice shows this 1957. -
29. Evolution of the Southwestern Atlantic Ocean Basin
29. EVOLUTION OF THE SOUTHWESTERN ATLANTIC OCEAN BASIN: RESULTS OF LEG 36, DEEP SEA DRILLING PROJECT The Shipboard Scientific Party1 Together with Wayne Harris, and William V. Sliter INTRODUCTION cores only and will be considered only briefly here. The four successful sites of the leg were drilled on the Leg 36 started in Ushuaia, Argentina, on 4 April Falkland (Malvinas) Plateau and in the Malvinas Outer 1974 and finished in Rio de Janeiro, Brazil, on 22 May Basin. The Falkland Plateau extends eastwards from 1974. It completed the second of three austral summer the continental shelf of the South American continent seasons of drilling planned for Antarctic waters during (Figure 1). The 500-fathom submarine contour lies east Phase III of the Deep Sea Drilling Project. In fact Leg of the Falkland Islands which consist of a meta- 36 brought the Antarctic drilling program of Phase III morphic complex overlain by Paleozoic-Triassic sedi- to an end, because the plan to drill south of Africa dur- mentary strata deformed in the early Mesozoic and cut ing the austral summer of 1974-75 had to be abandoned by mafic dykes (Greenway, 1972). The strata can be for want of a suitable escort vessel. correlated with rocks of comparable age in South The two main objectives of Leg 36 as originally con- America and southern Africa. There is therefore no ceived by the Antarctic Advisory Panel were to in- reason to doubt that the western portion of the plateau vestigate the geologic histories of the Scotia Arc and of at least is underlain by continental crust.