Mount St Helens 40 Years On
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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. -
Chapter 15 Comparative Phylogeography of North- Western North America: a Synthesis
Chapter 15 Comparative phylogeography of north- western North America: a synthesis S. J. Brunsfeld,* J. Sullivan,†D. E. Soltis‡and P. S. Soltis§ Introduction Phylogeography is concerned with the principles and processes that determine the geographic distributions of genealogical lineages, within and among closely related species (Avise et al. 1987;Avise 2000).Although this field of study is very new (only a little more than a decade has passed since the term ‘phylogeography’was first coined; see Avise et al. 1987),the scientific literature in this research area is now voluminous. To date, most phylogeographic investigations of natural populations have focused on muticellular animals (Hewitt 1993; Patton et al. 1994; daSilva & Patton 1998; Eizirik et al. 1998;Avise 2000; Hewitt 2000; Schaal & Olsen 2000; Sullivan et al. 2000). This bias is due in large part to the ready availability of population-level genetic markers afforded by the animal mitochondrial genome. The more slowly evolving chloroplast genome,in contrast,often does not provide sufficient variation to reconstruct phylogeny at the populational level (Soltis et al. 1997; Schaal et al. 1998; Schaal & Olsen 2000). Phylogeographic data have accumulated so rapidly for animal taxa that it has been possible to compare phylogeographic structure among codistributed species. In fact, one of the most profound recent contributions of molecular phylogeography is the construction of regional phylogeographic perspec- tives that permit comparisons of phylogeographic structure among codistributed species, and subsequent integration of genealogical data with independent biogeo- graphic and systematic data. Probably the best-known regional phylogeographic analysis for North America involves animals from the southeastern USA (reviewed in Avise 2000). -
GEOLOGIC MAP of the MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE of SOUTHERN WASHINGTON by Wes Hildreth and Judy Fierstein
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2460 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE MOUNT ADAMS VOLCANIC FIELD, CASCADE RANGE OF SOUTHERN WASHINGTON By Wes Hildreth and Judy Fierstein When I climbed Mount Adams {17-18 August 1945] about 1950 m (6400') most of the landscape is mantled I think I found the answer to the question of why men by dense forests and huckleberry thickets. Ten radial stake everything to reach these peaks, yet obtain no glaciers and the summit icecap today cover only about visible reward for their exhaustion... Man's greatest 2.5 percent (16 km2) of the cone, but in latest Pleis experience-the one that brings supreme exultation tocene time (25-11 ka) as much as 80 percent of Mount is spiritual, not physical. It is the catching of some Adams was under ice. The volcano is drained radially vision of the universe and translating it into a poem by numerous tributaries of the Klickitat, White Salmon, or work of art ... Lewis, and Cis pus Rivers (figs. 1, 2), all of which ulti William 0. Douglas mately flow into the Columbia. Most of Mount Adams and a vast area west of it are Of Men and Mountains administered by the U.S. Forest Service, which has long had the dual charge of protecting the Wilderness Area and of providing a network of logging roads almost INTRODUCTION everywhere else. The northeast quadrant of the moun One of the dominating peaks of the Pacific North tain, however, lies within a part of the Yakima Indian west, Mount Adams, stands astride the Cascade crest, Reservation that is open solely to enrolled members of towering 3 km above the surrounding valleys. -
Across the Cascade Range
Series I B> DescriPtive Geology- 4l Bulletin No. 235 \ D, Petrography and Mineralogy, DEPARTMENT'OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES \). WALCOTT, Di HECTOR GEOLOGICAL RECONNAISSANCE ACROSS THE CASCADE RANGE NEAR THE FORTY-NINTH PARALLEL GEORGE OTIS SMITH AND FRANK C. CALKINS WASHINGTON GOVERNMENT PRINTING OFFICE 1904 Trri-o^) SL'BD C 0 N T E N T S. I'lliJO. Letter of transmittal. ---_--_---..-.._-_.____.._-______._....._.._____.._.. 9 Introduction-__-._.__,.__-.----._--._._.__..._....__....---_--__._.__.-.-_- 11 Scope of report ---.--_.____.._______-.--....._---.._...._.__ ._.- 11 Route followed ........................:......................... 12 Geography .............................................................. 12 Topography .......................................................... 12 Primary divisions of the region..--.........-.--.-.--.-.-.. 12 Okanogan Valley .................:.. ............................ 18 Cascade Range ...............:........,..._ ....^......i........ 13 General characteristics..._.....-.....-..----.--.----.-.-..-.. 13 Northern termination.,.---.....-......--.-.............._ 13 Subdivision .............................................. 14 Okanogan Mountains ........................................... 14 Hozonieen Range ............................................ 15 Skagit Mountains....-.... ......-.----....-.-----..-...--.--- 16 Drainage ..................................................... 17 Climate ...................................................... ...... 17 Roads and trails -
Tectonic Setting of the Southern Cascade Range As Interpreted from Its Magnetic and Gravity Fields
Tectonic setting of the southern Cascade Range as interpreted from its magnetic and gravity fields RICHARD J. BLAKELY \ ROBERT C. JACHENS > U.S. Geological Survey, Menlo Park, California 94025 ROBERT W. SIMPSON J RICHARD W. COUCH School of Oceanography, Oregon State University, Corvallis, Oregon 97331 ABSTRACT every major volcano of the study area is lo- cated on the perimeter of a local gravitational We have compiled and analyzed aeromag- low. We suggest that the gravity lows reflect netic data from the southern Cascade Range subsidence of low-density volcanic material and compared them with residual gravity relative to denser country rock and that the data from the same region in order to investi- major volcanoes have developed over struc- gate regional aspects of these young volcanic tures at the perimeters of their respective rocks and of basement structures beneath depressions. them. Various constant-level aeromagnetic surveys were mathematically continued up- COMPILATION AND ANALYSIS ward to 4,571 m and numerically mosaicked OF THE DATA into a single compilation extending from lat. 40°10'N to lat. 44°20'N. These data were re- During the past six years, Oregon State duced to the pole, upward continued an addi- University has systematically collected aero- tional 10 km, and compared with a magnetic magnetic data of exceptional quality over the topographic model and with residual gravity entire southern part of the Cascade Range, from data upward continued to the same level. lat. 40°10'N to lat. 44°20'N (Connard, 1979; Several intriguing regional features are sug- Connard and others, 1983; McLain, 1981; Hup- gested by these data. -
Geology of the Northern Part of the Southeast Three Sisters
AN ABSTRACT OF THE THESIS OF Karl C. Wozniak for the degree of Master of Science the Department cf Geology presented on February 8, 1982 Title: Geology of the Northern Part of the Southeast Three Sisters Quadrangle, Oregon Redacted for Privacy Abstract approved: E. M. Taylorc--_, The northern part of the Southeast Three Sisters quadrangle strad- dles the crest of the central High Cascades of Oregon. The area is covered by Pleistocene and Holocene volcanic and volcaniclastic rocks that were extruded from a number of composite cones, shield volcanoes, and cinder cones. The principal eruptive centers include Sphinx Butte, The Wife, The Husband, and South Sister volcanoes. Sphinx Butte, The Wife, and The Husband are typical High Cascade shield and composite vol- canoes whose compositions are limited to basalt and basaltic andesite. South Sister is a complex composite volcano composed of a diverse assem- blage of rocks. In contrast with earlier studies, the present investi- gation finds that South Sister is not a simple accumulation of andesite and dacite lavas; nor does the eruptive sequence display obvious evolu- tionary trends or late stage divergence to basalt and rhyolite. Rather, the field relations indicate that magmas of diverse composition have been extruded from South Sister vents throughout the lifespan of this volcano. The compositional variation at South Sister is. atypical of the Oregon High Cascade platform. This variation, however, represents part of a continued pattern of late Pliocene and Pleistocene magmatic diver- sity in a local region that includes Middle Sister, South Sister, and Broken Top volcanoes. Regional and local geologic constraints combined with chemical and petrographic criteria indicate that a local subcrustal process probably produced the magmas extruded fromSouth Sister, whereas a regional subcrustal process probably producedthe magmas extruded from Sphinx Butte, The Wife, and The Husband. -
The Jackson Volcano
THE DEPARTMENT OF ENVIRONMENTAL QUALITY Office of Geology P. 0. Box 20307 Volume 18, Number 3 Jackson, Mississippi 39289-1307 September 1997 THE JACKSON VOLCANO David T. Dockery ID, John C. Marble, and Jack Henderson Mississippi Office of Geology INTRODUCTION One of the most interesting geologic features ofMississippi is the Jackson Volcano, which rests only 2900 feet beneath the state's capital city. The volcano's dense core forms one ofthe most prominent structural anomalies found on gravity and magnetic surveys of the state, showing tightly wrapped con tours of increasing gravity and magnetic deflection like a crowded bull's- eye (Figure l ). This igneous complex and the up Iifted formations around it comprise a structure known as the Jackson Dome. Northwest ofthe Jackson Volcano in southern Humphreys County is the Midnight Volcano and the associ ated volcanic terrain ofthe Sharkey Platform . Dense igneous rock below Jackson and Midnight increase the force ofgravity slightly as shown in Figure I. A person tipping the scales at Jackson or Midnight would be slightly heavier than elsewhere in the state (if anyone would like to use that for an excuse). No other capital city or major population center is situated above an extinct volcano, even though the recent movie "Volcano" fictitiously placed Los Angeles, California, above one. Monroe, Louisiana, is Jackson 's sister city in being a close second, as it rests above a volcanic terrain known as the Monroe Uplift. However, the position ofJackson's downtown district above the throat of an extinct Cretaceous volcano seems to be unique. Ifthe Jackson Volcano were to ever vent itself in the future, the Coliseum would be near ground zero. -
Finding My Feet 22 Balancing Act 24
ALUMNI AND FRIENDS // AUTUMN 2016 A fond farewell Baroness Hale reflects on her time as Chancellor Hole in the heart A revolution in medicine The road ahead Your University launches a new strategy A fond farewell ALUMNI AND FRIENDS // AUTUMN 2016 We thank our Chancellor for 13 years at the helm of the University Page 14 Contents Features The road ahead 6 Hole in the heart 10 A fond farewell 14 Letter to my lecturer 20 Finding my feet 22 Balancing act 24 News Latest from Bristol 2 In pictures 4 Listings In memoriam 27 Events 28 4 10 6 Graduation 2016 © Bhagesh Sachania Photography Sachania Bhagesh © 2016 Graduation Autumn 2016 // nonesuch 1 Latest from Bristol bristol.ac.uk/news News In brief Former Bristol academic and Nobel Prize winner Professor Sir Angus Deaton was awarded the University’s highest honour earlier this year, an Honorary Fellowship, for his distinction in the field of economics. His Awards Awards research has had a significant and lasting Writing residency award Queen’s Anniversary Prize impact at Bristol and Playwright Ian McHugh has been named Professor Hugh Brady, Vice-Chancellor around the world. as the first ever recipient of the annual of the University of Bristol, has been Kevin Elyot Award by the University of presented with the Queen’s Anniversary Aircraft engineer and Bristol Theatre Collection. Prize for Higher Education on behalf of Bristol graduate Emma the University. England (MEng 2013) is The award, created in the memory of the renowned flying the flag for women playwright, screenwriter and Bristol drama alumnus, The prize, also presented to Denis Burn (BSc 1975), in engineering after being will support Ian to create a new dramatic work Chair of the Board of Trustees, and Professor named the Best of British inspired by Kevin’s archive, which was donated to Katharine Cashman, leader of Bristol’s Volcanology Engineering at the Semta the collection by his sister following his death in 2014. -
A Tale of Three Sisters: Reconstructing the Holocene Glacial History and Paleoclimate Record at Three Sisters Volcanoes, Oregon, United States
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 2005 A Tale of Three Sisters: Reconstructing the Holocene glacial history and paleoclimate record at Three Sisters Volcanoes, Oregon, United States Shaun Andrew Marcott Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Glaciology Commons Let us know how access to this document benefits ou.y Recommended Citation Marcott, Shaun Andrew, "A Tale of Three Sisters: Reconstructing the Holocene glacial history and paleoclimate record at Three Sisters Volcanoes, Oregon, United States" (2005). Dissertations and Theses. Paper 3386. https://doi.org/10.15760/etd.5275 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. THESIS APPROVAL The abstract and thesis of Shaun Andrew Marcott for the Master of Science in Geology were presented August II, 2005, and accepted by the thesis committee and the department. COMMITTEE APPROVALS: (Z}) Representative of the Office of Graduate Studies DEPARTMENT APPROVAL: MIchael L. Cummings, Chair Department of Geology ( ABSTRACT An abstract of the thesis of Shaun Andrew Marcott for the Master of Science in Geology presented August II, 2005. Title: A Tale of Three Sisters: Reconstructing the Holocene glacial history and paleoclimate record at Three Sisters Volcanoes, Oregon, United States. At least four glacial stands occurred since 6.5 ka B.P. based on moraines located on the eastern flanks of the Three Sisters Volcanoes and the northern flanks of Broken Top Mountain in the Central Oregon Cascades. -
Smutty Alchemy
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2021-01-18 Smutty Alchemy Smith, Mallory E. Land Smith, M. E. L. (2021). Smutty Alchemy (Unpublished doctoral thesis). University of Calgary, Calgary, AB. http://hdl.handle.net/1880/113019 doctoral thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Smutty Alchemy by Mallory E. Land Smith A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY GRADUATE PROGRAM IN ENGLISH CALGARY, ALBERTA JANUARY, 2021 © Mallory E. Land Smith 2021 MELS ii Abstract Sina Queyras, in the essay “Lyric Conceptualism: A Manifesto in Progress,” describes the Lyric Conceptualist as a poet capable of recognizing the effects of disparate movements and employing a variety of lyric, conceptual, and language poetry techniques to continue to innovate in poetry without dismissing the work of other schools of poetic thought. Queyras sees the lyric conceptualist as an artistic curator who collects, modifies, selects, synthesizes, and adapts, to create verse that is both conceptual and accessible, using relevant materials and techniques from the past and present. This dissertation responds to Queyras’s idea with a collection of original poems in the lyric conceptualist mode, supported by a critical exegesis of that work. -
Vmsg Abstract Book
V-VMSG Annual General Meeting 6-8 January 2021 Abstract book CODE OF CONDUCT FOR MEETINGS AND EVENTS The Volcanic & Magmatic Studies Group is a Special Interest Group joint between the Geological Society of London and Mineralogical Society. These learned societies are signatories to the Science Council Declaration on Diversity, Equality and Inclusion. Through their members, the Geological Society of London and Mineralogical Society have a duty in the public interest to provide a safe, productive and welcoming environment for all participants and attendees of meetings, workshops, and events regardless of gender, sexual orientation, gender identity, race, ethnicity, religion, disability, physical appearance, or career level. The Volcanic & Magmatic Studies Group has worked with the Geological Society of London and Mineralogical Society on Code of Conduct policies. These are available from https://www.geolsoc.org.uk/codeofconduct and https://www.minersoc.org/code-of- conduct.html. The Code of Conduct outlined below specifically applies to all participants in Volcanic & Magmatic Studies Group activities, including ancillary events and social gatherings. The Volcanic & Magmatic Studies Group expects all participants -- including, but is not limited to, attendees, speakers, volunteers, exhibitors, staff, service providers and representatives to outside bodies -- to uphold the principles of this Code of Conduct. 1. Behaviour The Volcanic & Magmatic Studies Group aims to provide a constructive, supportive and professionally stimulating environment for all its members. Participants of VMSG meetings and events are expected to behave in a professional manner at all times. 2. Unacceptable Behaviour Harassment and/or sexist, racist, or exclusionary comments or jokes are not appropriate and will not be tolerated. -
Eruptions of Lassen Peak, California, 1914 to 1917
Department of the Interior U.S. GEOLOGICAL SURVEY—REDUCING THE RISK FROM VOLCANO HAZARDS A Sight “Fearfully Grand”—Eruptions of Lassen Peak, California, 1914 to 1917 n May 22, 1915, a large explosive Oeruption at the summit of Lassen Peak, California, the southernmost active volcano in the Cascade Range, devastated nearby areas and rained volcanic ash as far away as 280 miles to the east. This explosion was the most powerful in a series of eruptions during 1914–17 that were the last to occur in the Cascade Range before the 1980 eruption of Mount St. Helens, Washington. A century after the Lassen eruptions, work by U.S. Geological Survey (USGS) scientists in cooperation with the National Park Service is shedding new light on these events. Lassen Peak in Lassen Volcanic National Park, northern California, is the Lassen Peak in northern California produced a series of eruptions during 1914–17. The larg- largest of a group of more than 30 lava domes est of those eruptions, on May 22, 1915, blasted rock fragments and pumice high into the air erupted in that area during the past 300,000 and rained fine volcanic ash as far away as Elko, Nevada, 280 miles (450 km) to the east. This years. These steep-sided accumulations of photograph, taken from the town of Red Bluff, 40 miles (65 km) west of the volcano, shows the volcanic rock were created by the pushing huge eruption column of ash and gas, which rose to a height of more than 30,000 feet (9,000 m). up of lava too viscous to flow away from its (Photograph by R.E.