Geologic Hazards in British Columbia
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Mantle Flow Through the Northern Cordilleran Slab Window Revealed by Volcanic Geochemistry
Downloaded from geology.gsapubs.org on February 23, 2011 Mantle fl ow through the Northern Cordilleran slab window revealed by volcanic geochemistry Derek J. Thorkelson*, Julianne K. Madsen, and Christa L. Sluggett Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia V5A 1S6, Canada ABSTRACT 180°W 135°W 90°W 45°W 0° The Northern Cordilleran slab window formed beneath west- ern Canada concurrently with the opening of the Californian slab N 60°N window beneath the southwestern United States, beginning in Late North Oligocene–Miocene time. A database of 3530 analyses from Miocene– American Holocene volcanoes along a 3500-km-long transect, from the north- Juan Vancouver Northern de ern Cascade Arc to the Aleutian Arc, was used to investigate mantle Cordilleran Fuca conditions in the Northern Cordilleran slab window. Using geochemi- Caribbean 30°N Californian Mexico Eurasian cal ratios sensitive to tectonic affi nity, such as Nb/Zr, we show that City and typical volcanic arc compositions in the Cascade and Aleutian sys- Central African American Cocos tems (derived from subduction-hydrated mantle) are separated by an Pacific 0° extensive volcanic fi eld with intraplate compositions (derived from La Paz relatively anhydrous mantle). This chemically defi ned region of intra- South Nazca American plate volcanism is spatially coincident with a geophysical model of 30°S the Northern Cordilleran slab window. We suggest that opening of Santiago the slab window triggered upwelling of anhydrous mantle and dis- Patagonian placement of the hydrous mantle wedge, which had developed during extensive early Cenozoic arc and backarc volcanism in western Can- Scotia Antarctic Antarctic 60°S ada. -
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. -
Pliocene and Pleistocene Volcanic Interaction with Cordilleran Ice Sheets, Damming of the Yukon River and Vertebrate Palaeontolo
Quaternary International xxx (2011) 1e18 Contents lists available at SciVerse ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Pliocene and Pleistocene volcanic interaction with Cordilleran ice sheets, damming of the Yukon River and vertebrate Palaeontology, Fort Selkirk Volcanic Group, west-central Yukon, Canada L.E. Jackson Jr. a,*, F.E. Nelsonb,1, C.A. Huscroftc, M. Villeneuved, R.W. Barendregtb, J.E. Storere, B.C. Wardf a Geological Survey of Canada, Natural Resources Canada, 625 Robson Street, Vancouver, BC V6B5J3, Canada b Department of Geography, University of Lethbridge, 4401 University Drive, Lethbridge, Alberta T1K 3M4, Canada c Department of Geography, Thompson Rivers University, Box 3010, 900 McGill Road, Kamloops, BC V2C 5N3, Canada d Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada e 6937 Porpoise Drive, Sechelt, BC V0N 3A4, Canada f Department of Earth Sciences, Simon Fraser University, 8888 University Drive, Burnaby, BC V2C 5N3, Canada article info abstract Article history: Neogene volcanism in the Fort Selkirk area began with eruptions in the Wolverine Creek basin ca. 4.3 Ma Available online xxx and persisted to ca. 3.0 Ma filling the ancestral Yukon River valley with at least 40 m of lava flows. Activity at the Ne Ch’e Ddhäwa eruptive center overlapped with the last stages of the Wolverine Creek eruptive centers. Hyaloclastic tuff was erupted between ca. 3.21 and 3.05 Ma. This eruption caused or was coincident with damming of Yukon River. The first demonstrable incursion of a Cordilleran ice sheet into the Fort Selkirk area was coincident with a second eruption of the Ne Ch’e Ddhäwa eruptive center ca. -
Preliminary Results of Field Mapping, Petrography, and GIS Spatial Analysis of the West Tuya Lava Field, Northwestern British Columbia
Geological Survey of Canada CURRENT RESEARCH 2005-A2 Preliminary results of field mapping, petrography, and GIS spatial analysis of the West Tuya lava field, northwestern British Columbia K. Wetherell, B. Edwards, and K. Simpson 2005 Natural Resources Ressources naturelles Canada Canada ©Her Majesty the Queen in Right of Canada 2005 ISSN 1701-4387 Catalogue No. M44-2005/A2E-PDF ISBN 0-662-41122-6 A copy of this publication is also available for reference by depository libraries across Canada through access to the Depository Services Program's website at http://dsp-psd.pwgsc.gc.ca A free digital download of this publication is available from GeoPub: http://geopub.nrcan.gc.ca/index_e.php Toll-free (Canada and U.S.A.): 1-888-252-4301 All requests for permission to reproduce this work, in whole or in part, for purposes of commercial use, resale, or redistribution shall be addressed to: Earth Sciences Sector Information Division, Room 402, 601 Booth Street, Ottawa, Ontario K1A 0E8. Authors’ addresses K. Wetherell ([email protected]) B. Edwards ([email protected]) Department of Geology Dickinson College P.O. Box 1773 Carlisle, Pennsylvania U.S.A. 17013 K. Simpson ([email protected]) 605 Robson Street, Suite 101 Vancouver, British Columbia V6B 5J3 Publication approved by GSC Pacific Original manuscript submitted: 2005-04-21 Final version approved for publication: 2005-05-26 Preliminary results of field mapping, petrography, and GIS spatial analysis of the West Tuya lava field, northwestern British Columbia K. Wetherell, B. Edwards, and K. Simpson Wetherell, K., Edwards, B., and Simpson, K., 2005: Preliminary results of field mapping, petrography, and GIS spatial analysis of the West Tuya lava field, northwestern British Columbia; Geological Survey of Canada, Current Research 2005-A2, 10 p. -
Gazetteer of Yukon
Gazetteer of Yukon Updated: May 1, 2021 Yukon Geographical Names Program Tourism and Culture Yukon Geographical Place Names Program The Yukon Geographical Place Names Program manages naming and renaming of Yukon places and geographical features. This includes lakes, rivers, creeks and mountains. Anyone can submit place names that reflect our diverse cultures, history and landscape. Yukon Geographical Place Names Board The Yukon Geographical Place Names Board (YGPNB) approves the applications and recommends decisions to the Minister of Tourism and Culture. The YGPNB meets at least twice a year to decide upon proposed names. The Board has six members appointed by the Minister of Tourism and Culture, three of whom are nominated by the Council of Yukon First Nations. Yukon Geographical Place Names Database The Heritage Resources Unit maintains and updates the Yukon Geographical Place Names Database of over 6,000 records. The Unit administers the program for naming and changing the names of Yukon place names and geographical features such as lakes, rivers, creek and mountains, approved by the Minister of Tourism and Culture, based on recommendations of the YGPNB. Guiding Principles The YGPNB bases its decisions on whether to recommend or rescind a particular place name to the Minister of Tourism and Culture on a number of principles and procedures first established by the Geographic Names Board of Canada. First priority shall be given to names with When proposing names for previously long-standing local usage by the general unnamed features—those for which no public, particularly indigenous names in local names exist—preference shall be the local First Nation language. -
Examples of Volcanic Mountains in India
Examples Of Volcanic Mountains In India Dionysus is unhistorical and imbrue insubordinately while pejorative Hernando superheats and prefaced. Prophylactic and mothiest Graeme normalize: which Elric is disrespectable enough? Rodrick supping youthfully. Then first need only write definitions for text word. Hundreds of mountain in satellite images in arkansas and volcanically active volcanoes examples above, viscosity of sizes were spewing a location. As discussed in the context of subduction-related volcanism in Chapter 4 the. In contrast, phenomena that occur underground is more difficult to model because fresh are more interacting processes. The thick lava cannot travel far down an slope was the volcano before it cools Composite volcanoes are they found at destructive plate margins Examples of. These examples of india in nevada caldera and volcanically triggered a few places, as volcanic cone, which pushes its final design. Which of tangible success criteria do can still need significant work on? However, after sundown, the team observed red lava fountains spewing from the crater into the atmosphere, and hot lava flows streaming down the slopes of the volcano, it said. Apart from temples at Shiv Kund, halfway to aircraft of asylum from Kultajpur side, exhaust are several temples on the crater portion of first hill. Download tslprb mains question of volcanic in. We employ only skillful and qualified experts who have completed thousands of academic papers for students. Pyroclastic flow at a result of bridge collapse. When the process begins, a valley will develop such as the Great Rift Valley in Africa. Hannover in Hannover, Germany. Basaltic lavas are more fluid than andesites or dacites, which contain more silica. -
Documentation of a Holocene Volcanic Cone in the Tuya-Teslin Volcanic Field, Northern British Columbia
Geological Survey of Canada CURRENT RESEARCH 2006-A1 Documentation of a Holocene volcanic cone in the Tuya-Teslin volcanic field, northern British Columbia K. Simpson, B. Edwards, and K. Wetherell 2006 CURRENT RESEARCH Natural Resources Ressources naturelles Canada Canada ©Her Majesty the Queen in Right of Canada 2006 ISSN 1701-4387 Catalogue No. M44-2006/A1E-PDF ISBN 0-662-42326-7 A copy of this publication is also available for reference by depository libraries across Canada through access to the Depository Services Program's Web site at http://dsp-psd.pwgsc.gc.ca A free digital download of this publication is available from GeoPub: http://geopub.nrcan.gc.ca/index_e.php Toll-free (Canada and U.S.A.): 1-888-252-4301 Critical reviewers Mark Stasiuk Authors’ addresses K. Simpson ([email protected]) Geological Survey of Canada 605 Robson Street, Suite 101, Vancouver, British Columbia V6B 5J3 B.Edwards ([email protected]) K. Wetherell ([email protected]) Department of Geology, Dickinson College, P.O. Box 1773, Carlisle, Pennsylvania 17013 U.S.A. Publication approved by GSC Pacific, Vancouver Original manuscript submitted: 2005-09-13 Final version approved for publication: 2005-11-03 Correction date: All requests for permission to reproduce this work, in whole or in part, for purposes of commercial use, resale, or redistribution shall be addressed to: Earth Sciences Sector Information Division, Room 402, 601 Booth Street, Ottawa, Ontario K1A 0E8. Documentation of a Holocene volcanic cone in the Tuya-Teslin volcanic field, northern British Columbia K. Simpson, B. Edwards, and K. Wetherell Simpson, K., Edwards, B., and Wetherell, K., 2006: Documentation of a Holocene volcanic cone in the Tuya-Teslin volcanic field, northern British Columbia; Geological Survey of Canada, Current Research 2006-A1, 7 p. -
Distribution, Nature, and Origin of Neogene–Quaternary Magmatism in the Northern Cordilleran Volcanic Province, Canada
Distribution, nature, and origin of Neogene–Quaternary magmatism in the northern Cordilleran volcanic province, Canada Benjamin R. Edwards* Igneous Petrology Laboratory, Department of Earth and Ocean Sciences, James K. Russell } University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada ABSTRACT Cordillera, driven by changes in relative these diverse volcanic rocks in space and time. plate motion between the Pacific and North We then use the compiled petrological and geo- The northern Cordilleran volcanic province American plates ca. 15–10 Ma. chemical data to address the origins of this alka- encompasses a broad area of Neogene to Qua- line magmatism and the structure of the litho- ternary volcanism in northwestern British Keywords: alkaline basalt, Canada, Cordil- sphere beneath the northern Cordilleran volcanic Columbia, the Yukon Territory, and adjacent leran, magmatism, Quaternary, volcanism. province. Specifically, we determine the source eastern Alaska. Volcanic rocks of the north- region characteristics of northern Cordilleran ern Cordilleran volcanic province range in INTRODUCTION volcanic province magmas using trace element age from 20 Ma to ca. 200 yr B.P. and are and isotopic data, and we produce a petrological dominantly alkali olivine basalt and hawai- Neogene to Quaternary magmatism in the image of the lithosphere using phase equilibria ite. A variety of more strongly alkaline rock Cordillera of North America is closely related to calculations for lavas and mantle peridotite types not commonly found in the North the current tectonic configuration between the xenoliths. Results of this analysis provide a basis American Cordillera are locally abundant in North American, Pacific, and Juan de Fuca plates on which to amplify the tectonic model we have the northern Cordilleran volcanic province. -
Aleutian Islands
324 ¢ U.S. Coast Pilot 9, Chapter 7 Chapter 9, Pilot Coast U.S. 180°W 176°W 172°W 168°W 164°W Chart Coverage in Coast Pilot 9—Chapter 7 NOAA’s Online Interactive Chart Catalog has complete chart coverage http://www.charts.noaa.gov/InteractiveCatalog/nrnc.shtml 16011 172°W 176°W 58°N St. Paul Island BERING SEA St. George Island 56°N Unimak Island 16528 16518 16531 16500 16517 54°N S 16515 16433 16435 D L A N 16511 A L E U T I A N I S 16522 16501 16520 Attu Island A 16421 16436 16480 M 16521 16430 U K 16514 T 16487 16490 A 16513 16463 Agattu Island P 16431 A S 16471 S S S 16441 A P 52°N 16432 A 16434 K 16423 Kiska Island T Adak Island I 16465 16486 16420 16442 16450 H C 16467 M A 16462 16440 16460 50°N 16012 26 SEP2021 NORTH PA CIFIC OCEAN 26 SEP 2021 U.S. Coast Pilot 9, Chapter 7 ¢ 325 Aleutian Islands (1) This chapter describes the Aleutian Islands and the 26 51°11.83'N., 179°50.46'W. 31 51°37.86'N., 171°34.53'W. many passes leading from the Pacific Ocean into the 27 52°39.35'N., 178°39.78'W. 32 51°15.27'N., 172°36.40'W. Bering Sea. Also described are the harbors of Dutch 28 53°13.18'N., 173°49.18'W. 33 50°21.63'N., 179°24.20'W. Harbor on Unalaska Island; Kuluk Bay on Adak Island; Massacre Bay on Attu Island; and many other smaller 29 53°02.71'N., 172°51.16'W. -
Bibliography of Literature from 1990-1997 Pertaining to Holocene
%LEOLRJUDSK\RIOLWHUDWXUHIURP SHUWDLQLQJWR +RORFHQHDQGIXPDUROLF 3OHLVWRFHQHYROFDQRHVRI $ODVND&DQDGDDQGWKH FRQWHUPLQRXV8QLWHG6WDWHV E\ &KULVWRSKHU-+DUSHO DQG-RKQ:(ZHUW 2SHQ)LOH5HSRUW 7KLVUHSRUWLVSUHOLPLQDU\DQGKDVQRWEHHQUHYLHZHGIRUFRQIRUPLW\ZLWK86*HRORJLFDO6XUYH\ HGLWRULDOVWDQGDUGV$Q\XVHRIWUDGHILUPRUSURGXFWQDPHVLVIRUGHVFULSWLYHSXUSRVHVRQO\DQG GRHVQRWLPSO\HQGRUVHPHQWE\WKH86*RYHUQPHQW 'HSDUWPHQWRIWKH,QWHULRU 86*HRORJLFDO6XUYH\ USGS Cascades Volcano Observatory 5400 MacArthur Blvd. Vancouver WA 98661 86'HSDUWPHQWRIWKH,QWHULRU %UXFH%DEELW6HFUHWDU\ 86*HRORJLFDO6XUYH\ &KDUOHV*URDW'LUHFWRU 7KLVUHSRUWLVRQO\DYDLODEOHLQGLJLWDOIRUPRQWKH:RUOG:LGH:HE 85/KWWSZUJLVZUXVJVJRYRSHQILOH2) Table of Contents Table of Contents..............................................................................................................................3 Illustrations and Tables....................................................................................................... .............8 Introduction..................................................................................................................................9 Methods.........................................................................................................................................9 EndNote© Reference Database.........................................................................................................10 Formatted Version...............................................................................................................................12 Discussion......................................................................................................................................13 -
Yukon Gazetteer May No Be Found on Referenced 1: 50,000 Map
YG Photo Tombstone Range February 2012 Geographical Names Program Heritage Resources Unit Cultural Services Branch Yukon Geographical Place Names Database The Heritage Resources Unit maintains and updates the Yukon Geographical Place Names Database of over 5,000 records. The Unit administers the program for naming and changing the names of Yukon geographical features such as lakes, rivers, creek and mountains, approved by the Minister of Tourism and Culture, based on recommendations of the Yukon Geographical Place Names Board. Mandate The mandate of the Heritage Resources Unit is to ensure that Yukon’s heritage resources are properly planned, researched, managed, protected, developed and interpreted in a manner consistent with the principles of responsible heritage resource management, the Historic Resources Act and Land Claims Heritage Agreements. Principles of Nomenclature The principles of nomenclature which guide the decisions of the Yukon Geographical Place Names Board (YGPNB) on geographical names are summarized as follows: 1. First priority shall be given to names with 5. When proposing names for previously long -standing local usage by the general unnamed features those for which no local public, particularly indigenous names in the names exist, preference shall be given to names local First Nation language. from native languages, names that describe the feature, name associated with historical events, 2. The Board has no jurisdiction over the names and names of people who have made an of municipalities, parks, territorial divisions or important contribution to the area where the other legal bodies that have been created by, or place name is proposed. result from legislation. 6. Geographical names shall be recognizable 3. -
Mafic Volcanism in the Colorado Plateau I Basin-And-Range Transition Zone, Hurricane, Utah
UNLV Theses, Dissertations, Professional Papers, and Capstones 12-1995 Mafic olcanismv in the Colorado Plateau: basin and range transition zone, Hurricane, Utah Alexander Sanchez University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geology Commons, and the Volcanology Commons Repository Citation Sanchez, Alexander, "Mafic olcanismv in the Colorado Plateau: basin and range transition zone, Hurricane, Utah" (1995). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1410. http://dx.doi.org/10.34917/3338134 This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. MAFIC VOLCANISM IN THE COLORADO PLATEAU I BASIN-AND-RANGE TRANSITION ZONE, HURRICANE, UTAH by Alexander Sanchez A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geoscience Department of Geoscience University ofNevada, Las Vegas December, 1995 The thesis of Alexander Sanchez for the degree of Master of Science in Geoscience is approved. Examining Committee Member, David L Weide, Ph.D.