Mount Baker – Studying the Active Volcano in Our Backyard
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Catalog of Earthquake Hypocenters at Alaskan Volcanoes: January 1 Through December 31, 2009
Catalog of Earthquake Hypocenters at Alaskan Volcanoes: January 1 through December 31, 2009 Data Series 531 U.S. Department of the Interior U.S. Geological Survey Catalog of Earthquake Hypocenters at Alaskan Volcanoes: January 1 through December 31, 2009 By James P. Dixon, U.S. Geological Survey, Scott D. Stihler, University of Alaska Fairbanks, John A. Power, U.S. Geological Survey, and Cheryl K. Searcy, U.S. Geological Survey Data Series 531 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Dixon, J.P., Stihler, S.D., Power, J.A., and Searcy, Cheryl, 2010, Catalog of earthquake hypocenters at Alaskan volcanoes: January 1 through December 31, 2009: U.S. Geological -
Mount Baker, Washington
WATER-QUALITY EFFECTS ON BAKER LAKE OF RECENT VOLCANIC ACTIVITY AT MOUNT BAKER, WASHINGTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 1022-B Prepared in cooperation with the State of Washington Department of Ecology Water-Quality Effects on Baker Lake of Recent Volcanic Activity at Mount Baker, Washington By G. C. BORTLESON, R. T. WILSON, and B. L. FOXWORTHY VOLCANIC ACTIVITY AT MOUNT BAKER, WASHINGTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 1022-B Prepared in cooperation with the State of Washington Department of Ecology UNITED STATES GOVERNMENT PRINTING OFFICE:1977 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Bortleson, Gilbert Carl, 1940- Water-quality effects on Baker Lake of recent volcanic activity at Mount Baker, Washington. (Volcanic Activity at Mt. Baker) (Geologic Survey Professional Paper 1022-B) Bibliography: p. 30. Supt.ofDocs.no.: I 19.16:1022-6 1. Water quality-Washington (State)--Baker Lake. 2. Volcanism-Washington (State). 3. Baker, Mount, Wash. I. Wilson, Reed T., joint author. II. Foxworthy, Bruce, La Verne, 1925- joint author. III. Washington (State). Dept. of Ecology. IV. Title. V. Series: Volcanic activity at Mount Baker, Washington. VI. Series: United States Geological Survey Professional Paper 1022-B. TD224.W2B67 363.6'1 77-21097 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03008-0 CONTENTS Conversion factors _________________________. Ill Quality of surface waters draining to Baker Lake ______B16 Abstract__________________________________. Bl Water in Sherman Crater __________________ 16 Introduction ______________________________. 1 Boulder Creek and other streams _____________. -
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. -
Redalyc.ACTIVIDAD ERUPTIVA Y CAMBIOS GLACIARES EN EL
Boletín de Geología ISSN: 0120-0283 [email protected] Universidad Industrial de Santander Colombia Julio-Miranda, P.; Delgado-Granados, H.; Huggel, C.; Kääb, A. ACTIVIDAD ERUPTIVA Y CAMBIOS GLACIARES EN EL VOLCÁN POPOCATÉPETL, MÉXICO Boletín de Geología, vol. 29, núm. 2, julio-diciembre, 2007, pp. 153-163 Universidad Industrial de Santander Bucaramanga, Colombia Disponible en: http://www.redalyc.org/articulo.oa?id=349632018015 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 ACTIVIDAD ERUPTIVA Y CAMBIOS GLACIARES EN EL VOLCÁN POPOCATÉPETL, MÉXICO Julio-Miranda, P. 1; Delgado-Granados, H. 2; Huggel, C.3 y Kääb, A. 4 RESUMEN El presente trabajo, se centra en el estudio del impacto de la actividad eruptiva del volcán Popocatépetl en el área glaciar durante el período 1994-2001. Para determinar el efecto de la actividad eruptiva en el régimen glaciar, se realizaron balances de masa empleando técnicas fotogramétricas, mediante la generación de modelos digitales de elevación (MDE). La compa- ración de MDEs permitió establecer los cambios glaciares en términos de área y volumen tanto temporales como espaciales. Así mismo, los cambios morfológicos del área glaciar fueron determinados con base en la fotointerpretación, de manera que los datos obtenidos por este procedimiento y los obtenidos mediante la comparación de los MDE se relacionaron con la actividad eruptiva a lo largo del periodo de estudio, estableciendo así la relación entre los fenómenos volcánicos y los cambios glaciares. -
Volcanic Event
VOLCANIC EVENT DEFINITIONS: Composite Volcano – typically steep-sided, symmetrical cones of large dimension built of alternating layers of lava flows, volcanic ash and tephra. Typical features include a crater at the summit, which contains a central vent or a clustered group of vents connected to a conduit system through which magma from a reservoir deep in the Earth’s crust rises to the surface; sometimes called stratovolcanoes. Debris Flow – fast-moving slurry of rock, mud, and water that looks and behaves like flowing wet concrete; similar to but coarser and less cohesive than a mudflow. Lahar – an Indonesian word describing mudflows and debris flows that originate from the slope of a volcano; pyroclastic flows can generate lahars by rapidly melting snow and ice. Lava – molten rock or magma that erupts, or oozes onto the Earth’s surface. Lava Dome – a mound of hardened lava that forms when viscous lava is erupted slowly and plies up over the vent rather than moving away as a lava flow. Lava Flow – streams of molten rock or magma that erupt relatively non-explosively from a volcano and move slowly downslope. Magma – molten rock located below the surface of the Earth. Mudflow – a fast-moving slurry of rock, mud, and water that looks and behaves like flowing wet concrete; similar to but less coarse and more cohesive than a debris flow. Pyroclastic Flow – a hot, fast-moving avalanche of ash, rock fragments and gas that moves down the sides of a volcano during explosive eruptions or when the steep edge of a dome breaks apart and collapses. -
Unalaska Hazard Mitigation Plan 2018
Unalaska, Alaska Multi-Jurisdictional Hazard Mitigation Plan Update April 2018 Prepared for: City of Unalaska and Qawalangin Tribe of Unalaska City of Unalaska Hazard Mitigation Plan THIS PAGE LEFT BLANK INTENTIONALLY ii City of Unalaska Hazard Mitigation Plan Table of Contents 1. Introduction .......................................................................................................... 1-1 1.1 Hazard Mitigation Planning ..................................................................... 1-1 1.2 Grant Programs with Mitigation Plan Requirements ............................... 1-1 1.2.1 HMA Unified Programs ............................................................... 1-2 2. Community Description ....................................................................................... 2-1 2.1 Location, Geography, and History ........................................................... 2-1 2.2 Demographics .......................................................................................... 2-3 2.3 Economy .................................................................................................. 2-4 3. Planning Process .................................................................................................. 3-1 3.1 Planning Process Overview ..................................................................... 3-1 3.2 Hazard Mitigation Planning Team ........................................................... 3-3 3.3 Public Involvement & Opportunities for Interested Parties to participate ................................................................................................ -
Geology of the Prince William Sound and Kenai Peninsula Region, Alaska
Geology of the Prince William Sound and Kenai Peninsula Region, Alaska Including the Kenai, Seldovia, Seward, Blying Sound, Cordova, and Middleton Island 1:250,000-scale quadrangles By Frederic H. Wilson and Chad P. Hults Pamphlet to accompany Scientific Investigations Map 3110 View looking east down Harriman Fiord at Serpentine Glacier and Mount Gilbert. (photograph by M.L. Miller) 2012 U.S. Department of the Interior U.S. Geological Survey Contents Abstract ..........................................................................................................................................................1 Introduction ....................................................................................................................................................1 Geographic, Physiographic, and Geologic Framework ..........................................................................1 Description of Map Units .............................................................................................................................3 Unconsolidated deposits ....................................................................................................................3 Surficial deposits ........................................................................................................................3 Rock Units West of the Border Ranges Fault System ....................................................................5 Bedded rocks ...............................................................................................................................5 -
Geological Survey Professional Paper 1022-C
GEOLOGICAL SURVEY PROFESSIONAL PAPER 1022-C POSTGLACIAL VOLCANIC DEPOSITS ATMOUNTBAKER, WASHINGTON AND POTENTIAL HAZARDS FROM FUTURE ERUPTIONS FRONTISPIECE.- East side of Mount Baker. Boulder Creek, in the center of the photograph, flows into Baker Lake. Postglacial Volcanic Deposits at Mount Baker, Washington, and Potential Hazards from Future Eruptions By JACK H. HYDE and DWIGHT R CRANDELL VOLCANIC ACTIVITY AT MOUNT BAKER, WASHINGTON G E 0 L 0 G I CAL SURVEY P R 0 FE S S I 0 N A L PAPER 1 0 2 2 -C An assessment of potential hazards at Mount Baker is based on the volcano's eruptive behavior during the last 10, 000 years UNITED STATES GOVERNMENT PRINTING OFFICE, \Y ASHINGTON : 1978 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director First Printing 1978 Second Printing 1981 Library of Congress Cataloging in Publication Data Hyde, Jack H. J'()stglacial volcanic deposits at Mount Baker. Washington, and potential hazards from future eruptions. (Volcanic activity at Mount Baker, Washington) Geological Survey Professional Paper 1022-C Bibliography: p. 16 Supt. of Docs. No.: I 19.16:1022-C I. Volcanic ash, tuff, etc.-Washington (State)-Baker, Mount. 2. Volcanism-Washington (State)-Baker, Mount. 3. Volcanic activity prediction. I. Crandell, Dwight Raymond, 1923- joint author. II. Title: Postglacial volcanic deposits at Mount Baker, Washington, and potential hazards from future eruptions. III. Series: IV. Series: United States Geological Survey Professional Paper 1022-C. QE46I.H976 55 1.2'2'09797 77-5891 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. -
Geologic Map of the North Cascade Range, Washington by Ralph A
Prepared in cooperation with Washington State Division of Geology and Earth Resources, U.S. National Park Service, and U.S. Forest Service Geologic Map of the North Cascade Range, Washington By Ralph A. Haugerud and Rowland W. Tabor Nontechnical pamphlet to accompany Scientific Investigations Map 2940 Looking south from the North Klawatti Glacier [Mbse]. In the right foreground, the glacier breaks into a heavily crevassed icefall where it descends steeply. Rock in the foreground knob is Eldorado Orthogneiss (unit TKgo), a 90 million-year-old stitching pluton, which here includes numerous dikes of light- colored pegmatite. Mount Buckner on the left skyline and Mount Forbidden hidden in clouds are also eroded from the Eldorado Orthogneiss (photographed in 1987). 2009 U.S. Department of the Interior U.S. Geological Survey CONTENTS Introduction.....................................................................................................................................................1 Using this report ....................................................................................................................................1 Map preparation ...................................................................................................................................1 Major sources of new data .................................................................................................................1 Acknowledgments ................................................................................................................................2 -
Volcanology: Electric Eruption
news & views VOLCANOLOGY Electric eruption On the morning of 24 August, ad 79, Mount Vesuvius in the Bay of Naples, Italy, exploded into activity. The eruption caught the roman occupants of Pompeii and Herculaneum utterly unawares. The cities were rapidly buried by thick ash fall and pyroclastic surges, killing thousands of people. In a letter to the historian Tacitus, Pliny the Younger, an eyewitness and survivor of the eruption, described “frightening dark clouds, rent by lightning twisted and hurled” (http://go.nature.com/gkcLgn). Volcanic lightning has since been documented during many historical eruptions. More recently, spectacular lightning was observed during the eruptions of Mount Redoubt in Alaska, USA, in 2009 and Eyjafjallajökull Volcano in Iceland in 2010. The lightning generally occurs within the volcanic plume — a spreading column of ash, rock and hot gases blasted from the volcano vent. Although the details of the processes are poorly understood, volcanic lightning is thought to be triggered by the fragmentation of, and high-speed collisions between, volcanic rocks and ash as they exit the vent, as well as by the interactions between super-cooled water / ALAMY IMAGES © ARCTIC droplets and ice particles in higher, cooler parts of the column. The collisions create positive and negative electrically charged analysed ash deposits collected from The glass spherules mostly formed regions within the volcanic plume that are the Mount Redoubt and Eyjafjallajökull from melting of the smallest individual ash equalized by an electrical discharge that eruptions and found tiny glass spherules grains or from the fusion of several melted creates a lightning flash. (less than 100 μm across), which could ash grains. -
Geologic Map of Washington - Northwest Quadrant
GEOLOGIC MAP OF WASHINGTON - NORTHWEST QUADRANT by JOE D. DRAGOVICH, ROBERT L. LOGAN, HENRY W. SCHASSE, TIMOTHY J. WALSH, WILLIAM S. LINGLEY, JR., DAVID K . NORMAN, WENDY J. GERSTEL, THOMAS J. LAPEN, J. ERIC SCHUSTER, AND KAREN D. MEYERS WASHINGTON DIVISION Of GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 •• WASHINGTON STATE DEPARTMENTOF 4 r Natural Resources Doug Sutherland· Commissioner of Pubhc Lands Division ol Geology and Earth Resources Ron Telssera, Slate Geologist WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere, State Geologist David K. Norman, Assistant State Geologist GEOLOGIC MAP OF WASHINGTON NORTHWEST QUADRANT by Joe D. Dragovich, Robert L. Logan, Henry W. Schasse, Timothy J. Walsh, William S. Lingley, Jr., David K. Norman, Wendy J. Gerstel, Thomas J. Lapen, J. Eric Schuster, and Karen D. Meyers This publication is dedicated to Rowland W. Tabor, U.S. Geological Survey, retired, in recognition and appreciation of his fundamental contributions to geologic mapping and geologic understanding in the Cascade Range and Olympic Mountains. WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 Envelope photo: View to the northeast from Hurricane Ridge in the Olympic Mountains across the eastern Strait of Juan de Fuca to the northern Cascade Range. The Dungeness River lowland, capped by late Pleistocene glacial sedi ments, is in the center foreground. Holocene Dungeness Spit is in the lower left foreground. Fidalgo Island and Mount Erie, composed of Jurassic intrusive and Jurassic to Cretaceous sedimentary rocks of the Fidalgo Complex, are visible as the first high point of land directly across the strait from Dungeness Spit. -
Foundation Document Overview – Lake Clark National Park
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Lake Clark National Park and Preserve Alaska Contact Information For more information about the Lake Clark National Park and Preserve Foundation Document, contact: [email protected] or (907) 644-3626 or write to: Superintendent, Lake Clark National Park and Preserve, 240 West 5th Avenue, Suite 236, Anchorage, AK 99501 Purpose Significance and Fundamental Resources and Values Significance statements express why Lake Clark National Park and Preserve resources and values are important enough to merit national park unit designation. Statements of significance describe why an area is important within a global, national, regional, and systemwide context. These statements are linked to the purpose of the park unit, and are supported by data, research, and consensus. Significance statements describe the distinctive nature of the park and inform management decisions, focusing efforts on preserving and protecting the most important resources and values of the park unit. Fundamental resources and values are those features, systems, processes, experiences, stories, scenes, sounds, smells, or other attributes determined to merit primary consideration during planning and management processes because they are essential to achieving the purpose of the park and maintaining its significance. The purpose of LAKE CLARK NATIONAL PARK AND PRESERVE is to protect a region of dynamic geologic and ecological processes that create scenic mountain landscapes, unaltered