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USGS Geologic Investigations Series I-1963, Pamphlet
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I-1963 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE SKYKOMISH RIVER 30- BY 60 MINUTE QUADRANGLE, WASHINGTON By R.W. Tabor, V.A. Frizzell, Jr., D.B. Booth, R.B. Waitt, J.T. Whetten, and R.E. Zartman INTRODUCTION From the eastern-most edges of suburban Seattle, the Skykomish River quadrangle stretches east across the low rolling hills and broad river valleys of the Puget Lowland, across the forested foothills of the North Cascades, and across high meadowlands to the bare rock peaks of the Cascade crest. The quadrangle straddles parts of two major river systems, the Skykomish and the Snoqualmie Rivers, which drain westward from the mountains to the lowlands (figs. 1 and 2). In the late 19th Century mineral deposits were discovered in the Monte Cristo, Silver Creek and the Index mining districts within the Skykomish River quadrangle. Soon after came the geologists: Spurr (1901) studied base- and precious- metal deposits in the Monte Cristo district and Weaver (1912a) and Smith (1915, 1916, 1917) in the Index district. General geologic mapping was begun by Oles (1956), Galster (1956), and Yeats (1958a) who mapped many of the essential features recognized today. Areas in which additional studies have been undertaken are shown on figure 3. Our work in the Skykomish River quadrangle, the northwest quadrant of the Wenatchee 1° by 2° quadrangle, began in 1975 and is part of a larger mapping project covering the Wenatchee quadrangle (fig. 1). Tabor, Frizzell, Whetten, and Booth have primary responsibility for bedrock mapping and compilation. -
Washington Geology, V, 21, No. 2, July 1993
WASHINGTON GEOLOGY Washington Department of Natural Resources, Division of Geology and Earth Resources Vol. 21, No. 2, July 1993 , Mount Baker volcano from the northeast. Bagley Lakes, in the foreground, are on a Pleistocene recessional moraine that is now the parking lot for Mount Baker Ski Area. Just below Sherman Peak, an erosional remnant on the left skyline, is Boulder Glacier. Park and Rainbow Glaciers share the area below the main summit (Grant Peak, 10,778 ft) . Boulder, Park, and Rainbow Glaciers drain into Baker Lake, which is out of the photo on the left. Mazama Glacier forms under the ridge that extends to Hadley Peak on the right. (See related article, p. 3 and Fig. 2, p. 5.) Table Mountain, the flat area just above and to the right of center, is a truncated lava flow. Lincoln Peak is just visible over the right shoulder of Mount Baker. Photo taken in 1964. In This Issue: Current behavior of glaciers in the North Cascades and its effect on regional water supplies, p. 3; Radon potential of Washington, p. 11; Washington areas selected for water quality assessment, p. 14; The changing role of cartogra phy in OGER-Plugging into the Geographic Information System, p. 15; Additions to the library, p. 16. Revised State Surface Minin!Jf Act-1993 by Raymond Lasmanls WASHINGTON The 1993 regular session of the 53rd Le:gislature passed a major revision of the surface mine reclamation act as En GEOLOGY grossed Second Substitute Senate Bill No. 5502. The new law takes effect on July 1, 1993. Both environmental groups and surface miners testified in favor of the act. -
Snohomish County Media Release
Snohomish County Medical Examiner’s Office 9509 29th Ave West, Everett, WA 98204 For information regarding the 530 Slide, please visit our web page at: www.snohomishcountywa.gov/530slideme Media Release www.snohomishcountywa.gov/SCMEOmediareport The next scheduled update is Wednesday, October 29, 2014 at 7:30 AM. October 28, 2014 0730h The Snohomish County Medical Examiner’s Office has completed the examination and identification of a 14-year old female who was involved in the incident at Marysville-Pilchuck High School in Marysville, WA on October 24, 2014. The decedent is Gia C. Soriano of Marysville, WA. The cause of death is gunshot wound of the head. The manner of death is Homicide. For further information, please contact the Snohomish County Sheriff’s Office. October 27, 2014 0730h The Snohomish County Medical Examiner’s Office has completed the examination and identification of a 14-year old female who was involved in the incident at Marysville-Pilchuck High School in Marysville, WA on October 24, 2014. The decedent is Zoe R. Galasso of Marysville, WA. The cause of death is handgun wound of the head. The manner of death is Homicide. For further information, please contact the Snohomish County Sheriff’s Office. The Snohomish County Medical Examiner’s Office has completed the examination and identification of a 15-year old male who was involved in the incident at Marysville-Pilchuck High School in Marysville, WA on October 24, 2014. The decedent is Jaylen R. Fryberg of Marysville, WA. The cause of death is handgun wound of the head. The manner of death is Suicide. -
Hiking Withdogs
www.wta.org April 2008 » Washington Trails On Trail « Hiking withDogs Photo by “Sadie’s Driver” Dogs make some of the finest hiking companions. Sadie hikes with her “driver” on the Yellow Aster Butte Trail. Hiking with Your Best Buddy The Northwest is blessed with so many but sometimes that pushed her to the limits. places to venture in the outdoors—no matter Like the time I decided to do a trail run to the what your skill level. And, for some, it’s so top of Mount Dickerman in August. Not real much more enjoyable when you have a four- smart. She collapsed about a mile from the car legged companion to join you. The dogs I have on our way down. The combination of heat and seen on the trail seem so happy to be out roam- insufficient water took its toll. We made it back ing with their humans. fine, but I learned a lesson. Having hiked for a number of years all Some dogs are comfortable rock hopping around Washington and areas in British Colum- and scrambling, but many are not. Sadie could bia, my greatest enjoyment has been with my climb higher and faster than I could, but I al- Sadie’s buddy Sadie. This was a she-devil golden re- ways worried about what would happen when triever who, as a puppy, was a terror! But from she got to the top. Fortunately Sadie was quite Driver Sadie’s Driver lives her very first trip, being on the trail brought out confident on her feet and was cautious enough her best. -
Chapter 3: the Affected Environment
Chapter 3: The Affected Environment 3.0 THE AFFECTED ENVIRONMENT 3.0.1 Introduction Chapter 3 – The Affected Environment describes the physical and biological environment (e.g., water resources, wildlife, etc.) as well as the human environment (e.g., social and economic factors, recreation, etc.), which may be affected by the range of alternatives, as described in Chapter 2 - Alternatives. Much of the information on the affected environment is compiled from detailed technical reports and other analyses prepared by the USFS and consultants. Some of these reports are attached to this FEIS as appendices. All reports are available for review as part of the Analysis File maintained for this project at the MBSNF Supervisor’s Office. References cited in this FEIS are provided in Chapter 5 - References. 3.0.2 Analysis Area The “analysis area” (referred to as the “Study Area” throughout this document) varies by resource area. The Study Area includes all public (USFS) lands as well as private land owned by Ski Lifts, Inc. and other land holders. When discussing individual projects within the Study Area, the following terms are used to distinguish the different locations within the SUP: Summit East, Summit Central, and Summit West, are collectively referred to as “The Summit.” Alpental, when discussed individually, is referred to as “Alpental.” All four ski areas are collectively referred to as “The Summit-at-Snoqualmie.” Figure 3.0-1, Study Area illustrates the boundaries of the Study Area, including The Summit and Alpental. Figure 3.0-2, 5th Field Watersheds illustrates the boundaries of the two 5th field watersheds used in this FEIS analysis: the South Fork Snoqualmie River Watershed (S.F. -
An Overview of the Geology and Geomorphology of the Snoqualmie River Watershed
AN OVERVIEW OF THE GEOLOGY AND GEOMORPHOLOGY OF THE SNOQUALMIE RIVER WATERSHED Prepared by: John Bethel, Geologist Ecological Services Unit Prepared for: Fran Solomon, Ph.D., Senior Ecologist Watershed and Ecological Assessment Team April 2004 Department of Natural Resources and Parks Water and Land Resources Division Capital Projects and Open Space Acquisitions Section 201 South Jackson Street, Suite 600 Seattle, Washington 98104-3855 An Overview of the Geology and Geomorphology of the Snoqualmie River Watershed Prepared by John Bethel, Geologist Ecological Services Unit Prepared for King County Water and Land Resources Division Snoqualmie Watershed Team September 2004 Department of Natural Resources and Parks Water and Land Resources Division Capital Projects and Open Space Acquisitions Section 201 South Jackson Street, Suite 600 Seattle, Washington 98104-3855 King County Executive Ron Sims King County Council Carolyn Edmonds, District 1 Bob Ferguson, District 2 Kathy Lambert, District 3 Larry Phillips, District 4 Dwight Pelz, District 5 Rob McKenna, District 6 Pete von Reichbauer, District 7 Dow Constantine, District 8 Steve Hammond, District 9 Larry Gossett, District 10 Jane Hague, District 11 David Irons, District 12 Julia Patterson, District 13 Department of Natural Resources and Parks Pam Bissonnette, Director Water and Land Resources Division Daryl Grigsby, Division Director Contributing Staff John Bethel, Geologist Supporting Staff Fran Solomon, Ph.D., Senior Ecologist Terry Butler, Geologist Gino Lucchetti, Senior Ecologist Wendy Gable Collins, Graphic Designer and Cartographer Bob Gilland, Technical Information Processing Specialist AN OVERVIEW OF THE GEOLOGY AND GEOMORPHOLOGY OF THE SNOQUALMIE RIVER WATERSHED Table of Contents 1.0 Introduction..................................................................................................................1 1.1. Purpose and Scope of this Report .......................................................................1 1.2. -
President's Corner
PRESIDENT’S CORNER Elden Altizer It’s been fun seeing the sunny outings of the Basic Class, but even the rain cancelation of Mt. Erie has a message. Knowing when to go home is part of being safe in the hills. I’m looking forward to seeing a happy group of graduates after Mt. Baker. I see more trips by instructors and members are be- ing added to the website trips forum, so look to see what is in the works, or even better, post a trip you’re thinking of leading there. I had the opportunity to be part of the Mountaineer’s advisory council meeting in May. The topic, part of their 2020 Vision, was how to reduce the carbon footprint of the club. It’s encouraging to see the largest climbing club in our area tackle such a difficult subject. Ideas ranged from carpooling, van pooling, energy efficiency of facilities, and increasing plant-based food at club functions. I’m glad that the WAC has changed most of the lights (all?) at Guye Cabin to efficient LED’s, and we should think about what we can do to adopt best practices on this critical issue. I’ve finally made a pilgrimage to the Seattle Central Library, where there’s an almost complete set of bulletins from the beginning of the club. Mike Mahaney had mentioned this long ago when he was the President. I was looking for insight on this 75th anniversary of D-Day, and the war was on the minds of WAC members in the 1940’s. -
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. -
THE WILD CASCADES December 1972 - January 1973 2 the WILD CASCADES
THE WILD CASCADES December 1972 - January 1973 2 THE WILD CASCADES TM TUTS ISSUE... R. &G*UC 6VM0S, WFT6«. (» VeAfLS AS k>ot^THo>fc.>T C*US6*.- UfcTloO <^Pe.€r^exrTAT»y6r, CotTH ^FfiCOUt^ \jb*rJ*& H\» (SfcU.vfc-a \Ki UKSWIUCCTO^, v^.c Se& Pfcc,eg *--7. 9^UM «2jeTo(UoS To ^feATTCfe . P©Ue>/ FHe ^iGr^vPiOrtor CA»oT<-tAo-rcG*oS fceP. Peuu4 MM^e -n>uiMM^r stcotnuc,- •* -*• ** # *f PV/AK-J MJO taTK KCrftfcCr -m*T f*-oSS fctVv^ UOST MOT &fc «r\s«o. SfrAT-n-t QT«^ Coot^ovuuto uK>socoejrFv>v.v>^ U<UVfer MA^crtt- UHLMMO T© ofl-Ofcft. A M6tftAr©<Ui>-| ©^ C*Mv^T«-oCT>ok> UaVhufc- CAK>AOA A*Jb -VWfe O.V KjcGfOTl^TCs- OK* HOUJ TO JT*P TWfc ?0*AfcCT. Sfcfc PAGffeS la-V) Premier David Barrett —Staff photo by COVER DRAWING by Gladys Aravena Richard S. Heyza. December 1972 - January 1973 3 g>m®Mi WM&MSWWW&W W® WMWWMM®W®M^W^®U Stock bids on aching fatewell to the Northwest Three men have held the position of Northwest Conservation Representative since its creation almost 12 years ago. M. Brock Evans leaves this office after 6 years (February 1967 - February 1973) to become the Sierra Club's top lobbyist in Washington, D. C. His predecessor Rodger W. Pegues after 2 short years (February 1965 - February 1967) also left the Northwest for the nation's Capital and went to work for the Director of the National Park Service. The first Representative, J. Michael McCloskey, went to San Francisco, after 3 1/2 years (August 1961 - February 1965) in the office, where he became the Sierra Club's Conservation Director and then Executive Director. -
The Journal of the North Cascades Conservation Council Summer/Fall 2010
The Wild CasCades The Journal of The norTh CasCades ConservaTion CounCil Summer/fall 2010 visit www.northcascades.org • americanalps.blogspot.com/ The Wild CasCades • Summer/Fall 2010 1 The North CasCades ConservaTion COuncil was The Wild CASCades summer/Fall 2010 formed in 1957 “To protect and preserve the North Cascades’ scenic, in This issue scientific, recreational, educational, and wilderness values.” Continuing this mission, NCCC keeps government 3 President’s Report — Marc Bardsley officials, environmental organizations, 4 a special contribution to the NCCC would help and the general public informed about saving the Cascades with social media — Philip Fenner issues affecting the Greater North 5 Forest service proposes illabot road decommissioning — rick Cascades ecosystem. action is pursued McGuire through legislative, legal, and public participation channels to protect the Viewpoint: into the wilds with iceaxe, cellphone and GPs — John S. edwards lands, waters, plants and wildlife. 6 American alps Biodiversity Report released — Jim davis over the past half century the NCCC 7 Researching biodiversity and ecosystem dynamics in our ameri- has led or participated in campaigns can alps — Phillip Zalesky to create the North Cascades National Park Complex, Glacier Peak Wilder- 8 More news from Reiter Forest — Karl Forsgaard ness, and other units of the National 10 Finney aMa Plan disappoints — rick McGuire Wilderness System from the W.o. 12 Margaret Miller returns to Cascade Pass — Tom hammond douglas Wilderness north to the 14 Joe Miller — american hero — Tom hammond alpine lakes Wilderness, the henry M. Jackson Wilderness, the Chelan-Saw- 15 Suggested Revegetation Practices — Margaret M. Miller and Joseph tooth Wilderness, the Wild Sky Wil- W. -
1957
the Mountaineer 1958 COPYRIGHT 1958 BY THE MOUNTAINEERS Entered as second,class matter, April 18, 1922, at Post Office in Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and December by THE MOUNTAINEERS, P. 0. Box 122, Seattle 11, Wash. Clubroom is at 523 Pike Street in Seattle. Subscription price of the current Annual is $2.00 per copy. To be considered for publication in the 1959 Annual articles must be sub, mitted to the Annual Committee before Oct. 1, 1958. Enclose a self-addressed stamped envelope. For further information address The MOUNTAINEERS, P. 0. Box 122, Seattle, Washington. The Mountaineers THE PURPOSE: to explore and study the mountains, forest and water courses of the Northwest; to gather into permanent form the history and traditions of this region; to preserve by the encouragement of protective legislation or otherwise, the natural beauty of Northwest America; to make expeditions into these regions in fulfillment of the above purposes; to encourage a spirit of good fellowship among all lovers of outdoor life. OFFICERS AND TRUSTEES Paul W. Wiseman, President Don Page, Secretary Roy A. Snider, Vice-president Richard G. Merritt, Treasurer Dean Parkins Herbert H. Denny William Brockman Peggy Stark (Junior Observer) Stella Degenhardt Janet Caldwell Arthur Winder John M. Hansen Leo Gallagher Virginia Bratsberg Clarence A. Garner Harriet Walker OFFICERS AND TRUSTEES: TACOMA BRANCH Keith Goodman, Chairman Val Renando, Secretary Bob Rice, Joe Pullen, LeRoy Ritchie, Winifred Smith OFFICERS: EVERETT BRANCH Frederick L. Spencer, Chairman Mrs. Florence Rogers, Secretary EDITORIAL STAFF Nancy Bickford, Editor, Marjorie Wilson, Betty Manning, Joy Spurr, Mary Kay Tarver, Polly Dyer, Peter Mclellan. -
Glaciers a Scientist Observes the Disappearing Glaciers of the Cascades
News & Features ELTO P AURI M Glaciers A scientist observes the disappearing glaciers of the Cascades Easton Glacier, Mount Baker, 2003. The line indicates the former glacier terminus in 1985. Nearly every glacier in the North Cascades is currently in retreat. By Mauri Pelto increased even more in the 1980s and then the glacier will shrink as fast as a culminated in the total disappearance of checkbook facing a high-interest credit Much of the grandeur of Pacific North- the north branch of the glacier in 2001. card . If ablation (which scientists use west mountain ranges stems from the No more does this glacier dominate the to describe melting and evaporation of extensive glacier cover. We often choose headwaters, and its demise will continue a glacier) equals or is greater than accu- our hikes based on scenic geographic to alter the hydrology of the White Chuck mulation, the glacier is in disequilibrium elements, such as waterfalls, glaciers and River headwaters. Why did this glacier and will eventually disappear. alpine lakes. We expect these features disappear? Is this the fate of many Pacific A glacier must consistently have to remain the same, but today glaciers of Northwest glaciers? two-thirds of its surface covered by the the North Cascades are rapidly changing. A Brief History of North previous winter’s snowcover at the end Glaciers are more than just attractive of the summer melt season to endure. If vistas. They are also crucial to the late Cascade Glaciers Glaciers form where snowfall accu- a glacier is consistently nearly snow free summer water supply of many rivers, and it will not survive.