Volcano Overview
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The Science Behind Volcanoes
The Science Behind Volcanoes A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface. Volcanoes are generally found where tectonic plates are diverging or converging. A mid-oceanic ridge, for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by convergent tectonic plates coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust in the interiors of plates, e.g., in the East African Rift, the Wells Gray-Clearwater volcanic field and the Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "Plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so- called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere. -
Chapter 4 Alaska's Volcanic Landforms and Features
Chapter 4 Alaska's Volcanic Landforms and Features Resources • Alaska Volcano Observatory website. (Available at http://www.avo.alaska.edu.) • Brantley, S.R., 1999, Volcanoes of the United States: U.S. Geological Survey General Interest Publication. (Available at http://pubs.usgs.gov/gip/volcus/index.html.) • Miller, T.P., McGimsey, R.G., Richter, D.H., Riehle, J.R., Nye, C.J., Yount, M.E., and Dumoulin, J.A., 1998, Catalog of the historically active volcanoes of Alaska: U.S. Geological Survey Open-File Report 98-0582, 104 p. (Also available at http://www.avo.alaska.edu/downloads/classresults.php?citid=645.) • Nye, C.J., and others, 1998, Volcanoes of Alaska: Alaska Division of Geological and Geophysical Surveys Information Circular IC 0038, accessed June 1, 2010, at . PDF Front (6.4 MB) http://www.dggs.dnr.state.ak.us/webpubs/dggs/ic/oversized/ic038_sh001.PDF and . PDF Back (6.6 MB) http://www.dggs.dnr.state.ak.us/webpubs/dggs/ic/oversized/ic038_sh002.PDF. • Smithsonian Institution, [n.d.], Global volcanism program—Augustine: Smithsonian Institution web page, accessed June 1, 2010, at http://www.volcano.si.edu/world/volcano.cfm?vnum=1103-01- &volpage=photos&phoyo=026071. • Tilling, R.I., 1997, Volcanoes—On-line edition: U.S. Geological Survey General Interest Product. (Available at http://pubs.usgs.gov/gip/volc/.) • U.S. Geological Survey, 1997 [2007], Volcanoes teacher’s guide: U.S. Geological Survey website. (Available at http://erg.usgs.gov/isb/pubs/teachers- packets/volcanoes/. • U.S. Geological Survey, 2010, Volcano Hazards Program—USGS photo glossary of volcanic terms: U.S. -
A Geomorphic Classification System
A Geomorphic Classification System U.S.D.A. Forest Service Geomorphology Working Group Haskins, Donald M.1, Correll, Cynthia S.2, Foster, Richard A.3, Chatoian, John M.4, Fincher, James M.5, Strenger, Steven 6, Keys, James E. Jr.7, Maxwell, James R.8 and King, Thomas 9 February 1998 Version 1.4 1 Forest Geologist, Shasta-Trinity National Forests, Pacific Southwest Region, Redding, CA; 2 Soil Scientist, Range Staff, Washington Office, Prineville, OR; 3 Area Soil Scientist, Chatham Area, Tongass National Forest, Alaska Region, Sitka, AK; 4 Regional Geologist, Pacific Southwest Region, San Francisco, CA; 5 Integrated Resource Inventory Program Manager, Alaska Region, Juneau, AK; 6 Supervisory Soil Scientist, Southwest Region, Albuquerque, NM; 7 Interagency Liaison for Washington Office ECOMAP Group, Southern Region, Atlanta, GA; 8 Water Program Leader, Rocky Mountain Region, Golden, CO; and 9 Geology Program Manager, Washington Office, Washington, DC. A Geomorphic Classification System 1 Table of Contents Abstract .......................................................................................................................................... 5 I. INTRODUCTION................................................................................................................. 6 History of Classification Efforts in the Forest Service ............................................................... 6 History of Development .............................................................................................................. 7 Goals -
NASA Planetary Glossary.Pdf
Glossary of Terms Aeolian: Pertaining to wind. Albedo: The ratio of the radiation reflected by a body to the amount incident upon it, often expressed as a percentage, as, the albedo of the Earth is 34%. Angle of illumination: The angle that a ray of electromagnetic energy makes with the plane of a surface (light from directly overhead is at 90¡). Atmosphere: The body of gases surrounding or comprising any planet or other celestial body, held there by gravity. Caldera: Large, circular to subcircular depression associated with a volcanic vent. Calderas result from col- lapse, explosion, or erosion. Cinder cone: A volcanic, conical hill formed by the accumulation of cinders and other pyroclastic materials; slopes are usually greater than 10¡. Contact: A plane or irregular surface between two types or ages of rock. Coriolis effect: The acceleration which a body in motion experiences when observed in a rotating frame. This force acts at right angles to the direction of the angular velocity. Corona: Elliptical, tectonically deformed terrains found on Venus and Miranda. Crater: Circular depression on a surface. Cyclonic storm: Atmospheric disturbance with circulation of winds in a counterclockwise direction in the northern hemisphere and in a clockwise direction in the southern hemisphere. Datum plane: A surface of widespread extent used as a reference for stratigraphic determinations. Density: Measure of the concentration of matter in a substance; mass per unit volume. Deposition: The accumulation of material by physical or chemical sedimentation. Dip: The angle that a surface makes with the horizontal (measured perpendicular to the strike of the surface). Dune: Mound of fine-grained material formed by wind or water Eddy: A temporary current, usually formed at a point at which a current passes some obstruction, or between two adjacent currents flowing in opposite directions, or at the edge of a permanent current. -
Rocks of Augusta, Rockingham Highland, and Bath Counties, Virginia
COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES FIELD TRIP TO THE IGNEOUS ROCKS OF AUGUSTA, ROCKINGHAM HIGHLAND, AND BATH COUNTIES, VIRGINIA ROBERT W. JOHNSON, JR. CHARLES MILTON, AND JOHN M. DENNISON INFORMATION CIRCUI.AR I 6 VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVILLE, VIRGINIA 't971 COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES FIELD TRIP TO THE IGNEOUS ROCKS OF AUGUSTA, ROCKINGHAM, HIGHLAND, AND BATH COUNTIES, VIRGINIA ROBERT W. JOHNSON, JR. CHARLES MILTON, AND JOHN M. DENNISON INFORMATION CIRCULA,R I 6 VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stoie Geologisl CHARLOTTESVILLE, VI RGINIA 1971 CoMMoNWEALTH or VIncrr.rr.l DnrAnt1vrsNr or Puncnesss AND Suppl,y RTCHMoND !97L Portions of this publication may be quoted if credit is given to the Virginia Division of Mineral Resources. It is recomrnended that reference to this repor."t be made in the following form: Johnson, R, W., Jr., Milton, Charles, and Dennison, J. M., 1971, Field trip to the igneous rocks of Augusta, Rockingham, I{ighland, and Bath counties, Virginia: Virginia Division of Mineral Resources Information Circ. 16, 68 p. DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia MARVIN M. SumnnLAND, Director Culnlps A. CnnrsropHERsEN, DeputA Director A. S. RlcnAL, JR., E*ecutiae Assi,stant BOARD Wrllrlu H. KrNc, Burkeville, Chuirman Wrr,r,rAu H. Sraxn,q.cEN, Alexandria, Vi,ce Chairman D. HnNny ALMoND, Richmond Ml.ron T. BENToN, Suffolk Josnps C. Canrnn, Jn., Richmond Aoor,r' U. -
Hawaii Volcanoes National Park Geologic Resources
National Park Service U.S. Department of the Interior Natural Resource Program Center Hawai‘i Volcanoes National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/163 THIS PAGE: Geologists have long been monitoring the volcanoes of Hawai‘i Volcanoes National Park.k. Here lava cascades during the 1969-1971 Mauna Ulu eruption of Kīlauea Vollcano. Note the Mauna Ullu fountain in tthee background. U.S. Geological Survey Photo by J. B. Judd (12/30/1969). ON THE COVER: Continuously erupting since 1983, Kīllaueaauea Vollcanocano continues to shape Hawai‘i Volcanoes National Park. Photo courtesy Lisa Venture/University of Cincinnati. Hawai‘i Volcanoes National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/163 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 December 2009 U.S. Department of the Interior National Park Service Natural Resource Program Center Denver, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
R6 Geomorphology Legend and Glossary
Geomorphology of the Pacific Northwest Legend and Glossary Definitions and Descriptions of Terms Used in the Mapping of Landforms, Landform Groups, and Landform Associations in Region Six, Forest Service Jay S. Noller Oregon State University Corvallis, Oregon Sarah J. Hash Forest Service Bend, Oregon Karen Bennett Forest Service Portland, Oregon December 2013 ver. 0.7 DRAFT Note to the Reader This provisional, draft text presents and briefly describes the terms used in the preparation of a map of landform groups covering all forests within Region Six of the US Forest Service. Formal definition of map units is pending completion of this map and review thereof by all of the forests in Region Six. Map unit names appended to GIS shapefiles are concatenations of terms defined herein and are meant to be objective descriptors of the landscape within each map unit boundary. These map unit names have yet to undergo a final vetting and culling to reduce complexity, redundancy or obfuscation unintentionally resulting from map creation activities. Any omissions or errors in this draft document are the responsibility of its authors. Rev. 06 on 05December2013 by Jay Noller 2 Geomorphology of the Pacific Northwest – Map Legend Term Description Ancient Volcanoes Landform groups suggestive of a deeply eroded volcano. Typically a central hypabyssal or shallow plutonic rocks are present in central (core) area of the relict volcano. Apron Footslope to toeslope positions of volcanoes to mountain ranges. Synonymous with bajada in an alluvial context. Ballena Distinctively round-topped, parallel to sub-parallel ridgelines and intervening valleys that have an overall fan-shaped or distributary drainage pattern. -
Geology 305 with Terry J. Boroughs
DATE DUE: Name: Ms. Terry J. Boroughs Geology 305 Section: Volcanism Instructions: Read each question carefully before selecting the BEST answer. Use GEOLOGIC vocabulary where applicable! Provide concise, but detailed answers to essay and fill-in questions. TURN IN YOUR 882 –ES SCANTRON AND ANSWER SHEET ONLY! Volcanism: MULTIPLE CHOICE QUESTIONS: 1. Intermediate magmas cool to form: a. basalt b. granite c. rhyolite d. diorite e. andesite 2. Violent volcanic activity is often associated with a. Fissure eruptions c. Shield volcanoes e. answers b. and/or d. b. Resurgent Calderas d. Composite cones f. Cinder cones 3. The most violent volcanic activity is associated with the combined eruption and subsequent collapse of the volcanic structure and is associated with the following type of volcanic structure: a. Fissure eruptions c. Shield volcanoes e. Cinder cones b. Resurgent Calderas d. Composite cones 4. Mount St. Helens is an example of a a. Shield volcano c. Cinder cone e. Composite cone b. Lava dome d. Volcanic neck 5. Felsic lavas cool to form: a. basalt b. granite c. rhyolite d. diorite e. gabbro 6. The Aleutian Islands in Alaska are associated with a. Intraplate volcanism d. Spreading center volcanism b. Subduction zone volcanism e. Intercrustal volcanism c. Geothermal volcanism 7. The Columbia Plateau in the northwestern United States is an excellent example of a. Silica-rich lava flows d. site of former fissure eruptions b. An eroded shield volcano e. both c. and d. c. Flood Basalts 8. A basaltic lava flow with a rough, jagged surface in which the dissolved gasses have escaped, is known as ________________ lava. -
Pre-Field Trip Lecture: O'ahu Volcanism
Pre-field Trip Lecture: O’ahu Volcanism http://www.pelagicos.net/classes_naturalhistory_sp16.htm Two Eroded Shields The study of Hawaiian volcanism hindered by two processes: 1) Erosion of original shields. 2) The overlaying of later volcanic features from rejuvenation period. Two shield volcanoes on O’ahu: Wai’anae: 1227 m (Mt. Ka’ala) Ko’olau: Lacks alkalic cap Rises to 960 m (Mt. Konahaunui) Intense dike complex Two Eroded Shields Both shield volcanoes have suffered from large landslides that removed about half of each volcano. Post-erosional volcanoes are shown on the map above by small "x"s. Wai’anae: Ko’olau: Shield formed between 3.8 and 2.9 MY. Main shield is about 2.7 to 1.8 MY. Caldera located near center of Waianae Caldera located south of Kaneohe Bay. Range and rift zones extend NW and SE. Numerous dikes mark location of a Lava flows of capping-stage about 1.8 MY. rift zone trending to NW and SE. Rocks from the renewed volcanism stage No rocks from capping stage. present but have not been dated. Much of volcano removed by landslide Volcano extensively modified by erosion. Re-shaped by renewed volcanism between 1 MY and 30,000 years ago. Evolution of O’ahu Evolution of O’ahu USGS Map of O’ahu: http://http://pubs.usgs.gov/of/2007/1089/Oahu_2007.pdf USGS Map of O’ahu: http://http://pubs.usgs.gov/of/2007/1089/Oahu_2007.pdf Volcanism on O’ahu Ko‘olau Poko or "short Ko‘olau," is one of two districts (with Ko‘olau Loa or "long Ko‘olau") making up the ko‘olau ("windward”) side of O‘ahu and encompassing the lands and reefs offshore of the northeast-facing slopes of the Ko‘olau volcano Ko’olau Erosion Very large dike complex exposed NE of the crest of the Ko`olau range. -
Volcanoes and Related Basalts of Albuquerque Basin, New Mexico by V
Circular 156 1978 Volcanoes and related basalts of Albuquerque Basin, New Mexico by V. C. Kelley and A. M. Kudo New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Circular 156 New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Volcanoes and related basalts of Albuquerque Basin, New Mexico by V. C. Kelley and A. M. Kudo SOCORRO 1978 ii Published by Authority of State of New Mexico, NMSA 1953 Sec. 63-1-4 Printed by University of New Mexico Printing Plant, September, 1978 Available from New Mexico Bureau of Mines & Mineral Resources, Socorro, NM 87801 Price $5.00 Preface This paper results from our mutual interest and current work on basalts of the Albuquerque Basin. Much new work is presented on the petrology and chemistry of the rocks (by Kudo) and on field relationships (by Kelley). Kudo's contribu- tions are a part of his study of basalts in New Mexico and other places in the Rockies. Kelley's contribution is an outgrowth of current study of the stratig- raphy, structure, and geomorphology of the Albuquerque Basin (Kelley, 1977). Parts of this circular appeared in "Guidebook to Albuquerque Basin of the Rio Grande rift" (Kelley and others, 1976). We acknowledge the assistance of: 1) John Husler, for chemical analyses of the rocks, 2) James A. Kasten, who mapped Cerro de Los Lunas and Tome Hill for his master's thesis under Kudo's direction, and 3) Jacques R. Renault, for suggestions on improving the manuscript. -
A Hawaiian Term for Basaltic Lava Flows That Are Typically Rough and Jagged with a Clinkery Surface
‘A‘ā: A Hawaiian term for basaltic lava flows that are typically rough and jagged with a clinkery surface. Agglutinate: Welded, ejected material characterized by glassy material binding the pyroclasts (ejected particles), or “sintered” glassy pyroclasts. Ash: Fine, 4.0 mm (.16 in) to 0.25mm (.01 in) in diameter, unconsolidated pyroclastic (ejected particles) material. Basalt: A dark colored, hard, volcanic rock containing 45% to 54% silica rich minerals (SiO2) which results in low viscosity (resistance to flow). Basalt is erupted at temperatures between 2012 ºF and 2282 ºF. Common minerals in basalt include olivine, pyroxene, and plagioclase. Blister: A blister is formed by the swelling of the crust that occurs as a result of the expansion of gas or vapor beneath a flow; typically about 1 meter (3.3 ft) in diameter and hollow. Block: A solid pyroclastic fragment greater than 64 mm (2.5 in) and up to several meters in diameter, that was ejected from a volcano during an explosive eruption. Bomb: Pyroclastic fragments greater than 64mm (2.5 in) in diameter, that were molten or plastic at the time of ejection. The shape of a bomb is determined by the viscosity of the magma, velocity and length of flight, the rate at which the lava cooled, the rate of expansion of gases, and the type of deformation that occurred upon impact. Breadcrust Breadcrust bombs are characterized by a crust that cooled bomb: during flight and as gases within it continued to expand the crust cracked much like bread rising in an oven. Cinder: Uncemented, glassy, vesicular (holes created by escaping gas bubbles), pyroclastic material. -
Baxter Layout
PREPARED WITH THE SUPPORT OF THE U.S. GEOLOGICAL SURVEY AS PART OF THE MISCELLANEOUS MAP SERIES 2000 STATE GEOLOGIC MAPPING PROGRAM ELEMENT (STATEMAP) OF THE NATIONAL GEOLOGIC MAPPING PROGRAM MAP M-111 Baxter Quadrangle MINNESOTA GEOLOGICAL SURVEY D.L. Southwick, Director ro pe rls pe ro al pe ri ce pe pe CORRELATION OF MAP UNITS pe Fluvial Lacustrine Glacial Eolian ri Paludal rtm pe pe al rtm ce Holocene ri al pe cwlt mlt rls pe ce ro ro pe cwut QUATERNARY ce ri Late pe ro Pleistocene rls Wisconsinan ro pe ro rls rtm pe ri rt ro ce p pe ce DESCRIPTION OF MAP UNITS MAP SYMBOLS pe This map shows the surface distribution of Quaternary sediments in the Baxter quadrangle. Geologic contact—Approximately located. Established from aerial photo- cwut pe It was constructed in part using aerial photographs taken in 1977 (1:80,000 scale), U.S. graphs, geomorphology, soil maps, well logs, borings, and examination ro pe Soil Conservation Service soil-survey maps for Cass, Crow Wing, and Morrison Counties of surficial materials. RL pe ce pe (Arneman and others, 1965; Brug and Gorton, 1994; Richardson and others, 1997), and Kame—Conical hill composed predominantly of sand and gravel. Interpreted ce information from borings made by the U.S. Geological Survey, Minnesota Department of to be a deposit within the confines of supporting ice. When ice melted, Natural Resources, and Minnesota Geological Survey (Southwick and others, 1986). Field gravel and sand assumed angle of repose. Collapsed bedding is common. work was conducted during the summer and fall of 2000 and included observations, Drumlin—Arrow shows inferred direction of ice movement.