USGS Fact Sheet 165-97
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1922 Elizabeth T
co.rYRIG HT, 192' The Moootainetro !scot1oror,d The MOUNTAINEER VOLUME FIFTEEN Number One D EC E M BER 15, 1 9 2 2 ffiount Adams, ffiount St. Helens and the (!oat Rocks I ncoq)Ora,tecl 1913 Organized 190!i EDITORlAL ST AitF 1922 Elizabeth T. Kirk,vood, Eclttor Margaret W. Hazard, Associate Editor· Fairman B. L�e, Publication Manager Arthur L. Loveless Effie L. Chapman Subsc1·iption Price. $2.00 per year. Annual ·(onl�') Se,·ent�·-Five Cents. Published by The Mountaineers lncorJ,orated Seattle, Washington Enlerecl as second-class matter December 15, 19t0. at the Post Office . at . eattle, "\Yash., under the .-\0t of March 3. 1879. .... I MOUNT ADAMS lllobcl Furrs AND REFLEC'rION POOL .. <§rtttings from Aristibes (. Jhoutribes Author of "ll3ith the <6obs on lltount ®l!!mµus" �. • � J� �·,,. ., .. e,..:,L....._d.L.. F_,,,.... cL.. ��-_, _..__ f.. pt",- 1-� r�._ '-';a_ ..ll.-�· t'� 1- tt.. �ti.. ..._.._....L- -.L.--e-- a';. ��c..L. 41- �. C4v(, � � �·,,-- �JL.,�f w/U. J/,--«---fi:( -A- -tr·�� �, : 'JJ! -, Y .,..._, e� .,...,____,� � � t-..__., ,..._ -u..,·,- .,..,_, ;-:.. � --r J /-e,-i L,J i-.,( '"'; 1..........,.- e..r- ,';z__ /-t.-.--,r� ;.,-.,.....__ � � ..-...,.,-<. ,.,.f--· :tL. ��- ''F.....- ,',L � .,.__ � 'f- f-� --"- ��7 � �. � �;')'... f ><- -a.c__ c/ � r v-f'.fl,'7'71.. I /!,,-e..-,K-// ,l...,"4/YL... t:l,._ c.J.� J..,_-...A 'f ',y-r/� �- lL.. ��•-/IC,/ ,V l j I '/ ;· , CONTENTS i Page Greetings .......................................................................tlristicles }!}, Phoiitricles ........ r The Mount Adams, Mount St. Helens, and the Goat Rocks Outing .......................................... B1/.ith Page Bennett 9 1 Selected References from Preceding Mount Adams and Mount St. -
Washington Division of Geology and Earth Resources Open File Report 74-1
TEPHRA OF SALMON SPRINGS AGE FROM THE SOUTHEASTERN OLYMPIC PENINSULA, WASHINGTON by R. U. BIRDSEYE and R. J. CARSON North Carolina State University WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 74-1 1974 This report has not been edited or reviewed for conformity with Division of Geology and Earth Resources standards and nomenclature Revised October, 1989 CONTENTS Page Abstract •.•................••......••........•.......•............• 1 Introduction ....................................................... 1 Acknowledgments •••••••••••••••••••••••••••••••••••••••••••••••••••• 1 Pleistocene climate, glaciation, and volcanism ••••••••••••••••••••• 2 The ashes: Their thickness, distribution, and stratigraphic position •••••••••••••••••••••••••••••••••••••••••• 7 Color and texture of the ash ••••••••••••••••••••••••••••••••••••••• 14 Deposition of the ash •••••••••••••••••••••••••••••••••••••••••••••• 14 Atmospheric conditions during deposition of the ash •••••••••••••••• 20 Usefulness of volcanic ash in stratigraphic determination •••••••••• 21 Canel us ion ....•••.•..••••.••..••......•.••••••.••••....•••••...••.. 21 References cited ••••••••••••••••••••••••••••••••••••••••••••••••••• 23 ILLUSTRATIONS Figure 1 - Maximum extent of the Cordilleran ice sheet •••••••••••• 3 Figure 2 - Summary of late Pleistocene events in western Washington ••••••••••••••••••••••••••••••••••••• 4 Figure 3 - Location map showing inferred extent of minimum areas of fallout of volcanic ash from eruptions of Mount Mazama and Glacier Peak ••••••••••••••••••••••• -
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 _____________. -
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 -
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. -
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. -
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. -
Crater Lake National Park Oregon
DEPARTMENT OF THE INTERIOR HUBERT WORK. SECRETARY NATIONAL PARK SERVICE STEPHEN T. MATHER. DIRECTOR RULES AND REGULATIONS CRATER LAKE NATIONAL PARK OREGON PALISADE POINT, MOUNT SCOTT IN THE DISTANCE 1923 Season from July 1 to September 30 THE PHANTOM SHIP. FISHING IS EXCELLENT IN CRATER LAKE. THE NATIONAL PARKS AT A GLANCE. [Number, 19; total area, 11,372 square miles.] Area in National parks in Distinctive characteristics. order of creation. Location. squaro miles. Hot Springs Middle Arkansas li 40 hot springs possessing curative properties- 1832 Many hotels and boarding houses—20 bath houses under public control. Yellowstone Northwestern Wyo 3.348 More geysers than in all rest of world together- 1872 ming. Boiling springs—Mud volcanoes—Petrified for ests—Grand Canyon of the Yellowstone, remark able for gorgeous coloring—Large lakes—Many largo streams and waterfalls—Vast wilderness, greatest wild bird and animal preserve in world— Exceptional trout fishing. Sequoia. Middle eastern Cali 252 The Big Tree National Park—several hundred 1S90 fornia. sequoia trees over 10 feet in diameter, some 25 to 36 feet, hi diameter—Towering mountain ranges- Startling precipices—Mile long cave of delicate beauty." Yosemito Middle eastern Cali 1,125 Valley of world-famed beauty—Lofty chits—Ro 1890 fornia. mantic vistas—Many waterfalls of extraordinary height—3 groves of big trees—High Sierra— Waterwhcol falls—Good trout fishing. General Grant Middle eastern Cali 4 Created to preserve the celebrated General Grant 1S90 fornia. Tree, 3* feet in diameter—6 miles from Sequoia National Park. Mount Rainier ... West central Wash 321 Largest accessible single peak glacier system—28 1899 ington.