Feasibility Assessment for the Reintroduction of Fishers in Western Oregon, USA
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Lost in Coos
LOST IN COOS “Heroic Deeds and Thilling Adventures” of Searches and Rescues on Coos River Coos County, Oregon 1871 to 2000 by Lionel Youst Golden Falls Publishing LOST IN COOS Other books by Lionel Youst Above the Falls, 1992 She’s Tricky Like Coyote, 1997 with William R. Seaburg, Coquelle Thompson, Athabaskan Witness, 2002 She’s Tricky Like Coyote, (paper) 2002 Above the Falls, revised second edition, 2003 Sawdust in the Western Woods, 2009 Cover photo, Army C-46D aircraft crashed near Pheasant Creek, Douglas County – above the Golden and Silver Falls, Coos County, November 26, 1945. Photo furnished by Alice Allen. Colorized at South Coast Printing, Coos Bay. Full story in Chapter 4, pp 35-57. Quoted phrase in the subtitle is from the subtitle of Pioneer History of Coos and Curry Counties, by Orville Dodge (Salem, OR: Capital Printing Co., 1898). LOST IN COOS “Heroic Deeds and Thrilling Adventures” of Searches and Rescues on Coos River, Coos County, Oregon 1871 to 2000 by Lionel Youst Including material by Ondine Eaton, Sharren Dalke, and Simon Bolivar Cathcart Golden Falls Publishing Allegany, Oregon Golden Falls Publishing, Allegany, Oregon © 2011 by Lionel Youst 2nd impression Printed in the United States of America ISBN 0-9726226-3-2 (pbk) Frontier and Pioneer Life – Oregon – Coos County – Douglas County Wilderness Survival, case studies Library of Congress cataloging data HV6762 Dewey Decimal cataloging data 363 Youst, Lionel D., 1934 - Lost in Coos Includes index, maps, bibliography, & photographs To contact the publisher Printed at Portland State Bookstore’s Lionel Youst Odin Ink 12445 Hwy 241 1715 SW 5th Ave Coos Bay, OR 97420 Portland, OR 97201 www.youst.com for copies: [email protected] (503) 226-2631 ext 230 To Desmond and Everett How selfish soever man may be supposed, there are evidently some principles in his nature, which interest him in the fortune of others, and render their happiness necessary to him, though he derives nothing from it except the pleasure of seeing it. -
Geologic History of Siletzia, a Large Igneous Province in the Oregon And
Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Wells, R., Bukry, D., Friedman, R., Pyle, D., Duncan, R., Haeussler, P., & Wooden, J. (2014). Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot. Geosphere, 10 (4), 692-719. doi:10.1130/GES01018.1 10.1130/GES01018.1 Geological Society of America Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Downloaded from geosphere.gsapubs.org on September 10, 2014 Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Ray Wells1, David Bukry1, Richard Friedman2, Doug Pyle3, Robert Duncan4, Peter Haeussler5, and Joe Wooden6 1U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025-3561, USA 2Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, 6339 Stores Road, University of British Columbia, Vancouver, BC V6T 1Z4, Canada 3Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East West Road, Honolulu, Hawaii 96822, USA 4College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 CEOAS Administration Building, Corvallis, Oregon 97331-5503, USA 5U.S. Geological Survey, 4210 University Drive, Anchorage, Alaska 99508-4626, USA 6School of Earth Sciences, Stanford University, 397 Panama Mall Mitchell Building 101, Stanford, California 94305-2210, USA ABSTRACT frames, the Yellowstone hotspot (YHS) is on southern Vancouver Island (Canada) to Rose- or near an inferred northeast-striking Kula- burg, Oregon (Fig. -
Little Butte Creek Watershed Assessment
Little Butte Creek Watershed Assessment Little Butte Creek Watershed Council August 2003 Abstract The Little Butte Creek Watershed Assessment has been prepared for the Little Butte Creek Watershed Council with funding from the Oregon Watershed Enhancement Board (OWEB). The Assessment was prepared using the guidelines set forth in the Governor’s Watershed Enhancement Board’s 1999 Oregon Watershed Assessment Manual. The purpose of this document is to assess the current conditions and trends of human caused and ecologic processes within the Little Butte Creek Watershed and compare them with historic conditions. Many important ecological processes within the watershed have been degraded over the last 150 years of human activity. This Assessment details those locations and processes that are in need of restoration as well as those that are operating as a healthy system. The Assessment was conducted primarily at the 5th field watershed level, that of the entire Little Butte Creek Watershed. List and describe field watershed levels below. Where possible, the analyses was refined to the smaller 6th field watershed level, thirteen of which exist within the Little Butte Creek Watershed. The assessment also notes gaps in data and lists recommendations for future research and data collection. It is intended that this document, and the Little Butte Creek Watershed Action Plan be used as guides for future research and watershed protection and enhancement over the next decade. The document was developed using existing data. No new data was collected for this project. Where data was lacking, it was detailed for future work and study. Acknowledgements This assessment was compiled and written by Steve Mason. -
Elliott State Forest: Next Step Considerations for Decoupling From
ELLIOTT STATE FOREST Next Step Considerations for Decoupling from Oregon’s Common School Fund October 2018 An Oregon Consensus Assessment Report to the Oregon Department of State Lands and Oregon State Land Board 1 Assessment Team Peter Harkema, Oregon Consensus Director Brett Brownscombe, Senior Project Manager Amy Delahanty, Project Associate Acknowledgements Oregon Consensus deeply appreciates all those who generously gave their time to inform this assessment and report. About Oregon Consensus Oregon Consensus (OC) was established by state statute as the State of Oregon's program for public policy conflict resolution and collaborative governance. The program provides mediation and other collaborative services to public bodies and stakeholders who are seeking new approaches to challenging public issues. OC conducts assessments and designs and facilitates impartial and transparent collaborative processes that foster balanced participation and durable agreements. OC is housed in the National Policy Consensus Center in the Hatfield School of Government at Portland State University. Contact Oregon Consensus National Policy Consensus Center Hatfield School of Government Portland State University 506 SW Mill Street, Room 720 PO Box 751 Portland, OR 97207-0751 (503) 725-9077 [email protected] www.oregonconsensus.org 2 Contents 1. Introduction .................................................................................................................................................................. 5 1.1. Purpose of report .............................................................................................................................................. -
Medford Area Geology Report
._.. April GEOLOGICAL NE1/lS - w..""'TTER 33 1948 GEOLOGY IN THE MEDFORD AREA. OREGON By Hollis M. Dole* This paper is a review of the geology of part of southwestern Oregon as worked out and mapped by Diller, Winchell, Wells, and Wilkinson.** The area described is of special interest because it affords an opportunity to observe the seldom exposed "basement" rocks of the Cascade Range. The geologic column of this area includes possible Proterozoic, Paleozoic, Mesozoic, and 0-enozoic rocks. The ee-nozoTc -rock-s- are represented in the rocks of the western Cascades and in the sediments and volcanics of Bear Creek and Rogue Ri ver valleys. The Mesozoic rocks occur along the southwestern edge of Bear Creek Valley and in isolated spots on the adjacent foothills. The oldest rocks are to the south and west of Medford in the Klamath geomorphic province, and they, in this area, are called the Siskiyou Mount~ . Old schists are found near the California line almost due south of Medford. These schists undoubtedly are some of the oldest rocks in Oregon, although there is no definite paleontological evidence to prove this. They consist of highly altered, crenulated and folded rocks, the most abundant of which are plagioclase hornblende schists. Sericite and graphitic schists are also common. The plagio clase-hornblende schists are interpreted as highly altered andesite or basalt flows, the sericite schists as altered dacite or rhyolite, and the graphitic schists as altered organic sedimentary rocks. The age of these rocks is Paleozoic or older, and their character indicates both volcanism in Oregon in earliest times and the existence of ancient seas. -
Cordilleran Section Meeting
Vol. 51, No. 4 Cordilleran Section Meeting 15–17 May Portland, Oregon, USA www.geosociety.org/cd-mtg 115th Annual Meeting of the Cordilleran Section Geological Society of America Portland, Oregon, USA 15–17 May 2019 Oregon Convention Center Local Program Committee Meeting Co-chairs . Martin Streck, Jim O’Connor Technical Program . Matt Brunengo, Erick Burns, Anita Grunder Field Trips . Jason McClaughry, Clark Niewendorp, Bob Houston Workshops, Exhibits, and Student Volunteers . Frank Granshaw Sponsorship . Scott Burns GSA Cordilleran Section Officers 2018–2019 Chair . Michael Wells Vice Chair . Jeffrey Lee Past Chair . Susan M . Cashman Secretary and Accounting Officer . Calvin G . Barnes Student Representative . Jason Womer GSA Councilors . Nathan Niemi, Jeff Rubin, Wendy Bohrson Sponsors We are grateful to the following sponsors who have graciously contributed financial and logistical support . Association of Women Geoscientists The Paleontological Society Portland State University NOTICE By registering for this meeting you have acknowledged that you have read and will comply with the GSA Code of Conduct for Events (full code of conduct found on inside back cover) . If you have any concerns about behavior that may violate the Code, please contact: GSA Executive Director, Vicki McConnell, vmconnell@geosociety .org GSA Ethics and Compliance Officer, Nan Stout, gsaeventscode@gmail .com You may also stop by the registration desk or the GSA Bookstore to have the named individuals directly contacted via phone . 50% Total Recovered Fiber 30% Post-Consumer General Information Location about 250 feet west of the Holladay Lobby entrance. The The 115th Annual Meeting of the Cordilleran Section DoubleTree by Hilton Hotel Portland is across the street from of the Geological Society of America will be held at the the Holladay Park MAX station, also served by the Red, Blue, Oregon Convention Center (OCC), Portland, Oregon, and Green Lines. -
Download Chapter
Table Of Contents Conservation Toolbox............................................................................................................................... 3 Outreach, Education, and Engagement................................................................................................... 4 Voluntary Conservation Programs......................................................................................................... 16 Conservation in Urban Areas.................................................................................................................. 23 Planning and Regulatory Framework..................................................................................................... 30 General References.................................................................................................................................. 50 Conservation Toolbox Everyone has a role in the successful implementation of the Oregon Conservation Strategy. The Conservation Toolbox provides recommendations to support implementation and suggestions for additional information and assistance. Key components of the Conservation Toolbox include: Outreach, Education, and Engagement Conservation in Urban Areas Oregon’s Existing Planning and Regulatory Framework Voluntary Conservation Programs General References: additional resources outside of the references provided in each section Outreach, Education, and Engagement Connecting people to nature is an important element of successful Conservation Strategy implementation. Acquiring -
2019-21 Budget Highlights
2019-21 BUDGET HIGHLIGHTS Legislative Fiscal Office September 2019 State of Oregon Ken Rocco Legislative Fiscal Office Legislative Fiscal Officer 900 Court St. NE, Rm. H-178 Paul Siebert Salem, OR 97301 Deputy Legislative Fiscal Officer 503-986-1828 September 9, 2019 To the Members of the Eightieth Oregon Legislative Assembly: Following is the 2019-21 Budget Highlights, which provides summary information on the legislatively adopted budget; legislative actions affecting the budget; program areas and agencies; state bonding and capital construction; budget notes; information technology; fiscal impact statements; substantive bills with a budget effect; and appendices containing detailed data. We hope you find this resource useful and invite you to call the Legislative Fiscal Office if you have any questions. Ken Rocco Legislative Fiscal Officer Table of Contents Summary of the 2019-21 Legislatively Adopted Budget ............................................................. 1 Summary of Legislative Actions Affecting the Budget ............................................................... 33 Program Area Summaries .......................................................................................................... 58 State Bonding and Capital Construction .................................................................................. 117 Budget Notes ........................................................................................................................... 120 Information Technology.......................................................................................................... -
Re and Os Isotopes of the Central Oregon Cascades and Along the Arc Indicate Variable Homogenization and Mafic Growth in the Deep Crust
Available online at www.sciencedirect.com Geochimica et Cosmochimica Acta 109 (2013) 345–364 www.elsevier.com/locate/gca Re and Os isotopes of the central Oregon Cascades and along the arc indicate variable homogenization and mafic growth in the deep crust Mariek E. Schmidt a,⇑, Anita L. Grunder a,1, Michael C. Rowe a,2, John T. Chesley b,3 a Department of Geosciences, Oregon State University Corvallis, OR 97333, United States b Department of Geosciences, University of Arizona, Tucson, AZ 85721, United States Received 2 May 2012; accepted in revised form 1 February 2013; available online 14 February 2013 Abstract The rhenium–osmium isotopic system has the potential to track the maturation of arc crust at lower crustal levels because the 187Os/188Os in magmas is sensitive to the age and composition of crust with which they interact. We here present Re and Os iso- topic data for a suite of samples from the extensional central Oregon Cascade arc that includes diverse, primitive (high Mg) bas- alts and low- and medium-K basaltic andesites from North Sister and Little Brother volcanoes. The basaltic andesites contain higher 187Os/188Os than the two most common basalt types, calc-alkaline basalt and low-K tholeiites (0.17–0.19 vs. 0.14– 0.15), indicating interaction with mafic crust. The evolution of 187Os/188Os in the deep crust depends on Re partitioning that in turn depends on sulfide and magnetite stability and oxygen fugacity. We estimate bulk mineral-melt partition coefficients for Re to be 4atfO2 QFM and 10 at fO2 +1 to +3 DQFM in keeping with near liquidus phase equilibria at deep crustal conditions (Mercer and Johnston, 2008) and on fO2 of central Oregon primitive magmas (Rowe et al., 2009). -
Late Mesozoic Or Early Tertiary Melanges in the Western Cascades of Washington
Washington Division of Geology and Earth Resources Bulletin 77, 1987 129 LATE MESOZOIC OR EARLY TERTIARY MELANGES IN THE WESTERN CASCADES OF WASHINGTON Virgil A. Frizzell, Jr. U.S. Geological Survey 2255 North Gemini Flagstaff, Arizona 86001 Rowland W. Tabor Robert E. Zartman Charles D. Blome U.S. Geological Survey U.S. Geological Survey U.S. Geological Survey 345 Middlefield Road Denver Federal Center Denver Federal Center Menlo Park, California 94025 Denver, Colorado 80225 Denver, Colorado 80225 ABSTRACT Marine rocks west of the Straight Creek fault, from Snoqualmie Pass to the Pilchuck River, are highly deformed and varied in lithology. These rocks, referred to various formations or stratigraphic units by earlier workers, should be considered two lithologically distinct melange belts. Immediately west of the Straight Creek fault from the Weden Creek area to Snoqualmie Pass, the discontinuous melange of the eastern belt consists of strongly hornfelsed rocks including chert, metabasalt, graywacke, argiUite, marble, and ultramafic rocks. Marble near Skykomish yields Permian fusu1inids with Tethyan affinities. Zircons from tonalitic gneiss northwest of Skykomish are 190 million years old, and metagabbro near Snoqualmie Pass is 165 million years old. In the western foothills, the melange of the western belt consists of pervasively sheared argillite and graywacke studded with outcrop- to mountain-scale steep-sided phacoids of chert, limestone, pillow basalt, gabbro, and tonalite; ultramafic rocks are rare. Strikes of bedding and cleavage and trends of small fold axes are mostly north-northwest to north-northeast. Rare macrofossils in foliated sedimentary rocks and radiolarians in chert phacoids are Late Jurassic to Early Cretaceous in age. -
Geology As Destiny: Cold Waters Run Deep in Western Oregon
PNW Pacific Northwest Research Station INSIDE The Geologic Divide . .2 The Allocation Challenge . .3 Dam the Consequences . .4 Land Use, Water, and Time . .4 Municipal Waters and National Forests . .5 FINDINGS issue forty-nine / december 2002 “Science affects the way we think together.” Lewis Thomas GEOLOGY AS DESTINY: COLD WATERS RUN DEEP IN WESTERN OREGON “Geology plays an extremely But a closer look reveals that the state has been blessed with a huge geological IN SUMMARY important and previously backup plan for water supply. unappreciated role in The summer of 2001 brought the “Contrary to popular belief, most summer determining flow regimes.” second-worst drought on record in flow out of the high Cascades is not due to Gordon Grant snowmelt. Instead, the high Cascades form Oregon, resulting in historically low a vast hydrologic sponge that stores many streamflows and reservoir levels, or most of the year, it just doesn’t decades worth of water as deep groundwa- seem like water is a problem in ter,” says Gordon Grant. “Recent analysis stressed aquatic ecosystems, and even F western Oregon. It’s a fixture, for of streamflow patterns, ranging in scale dramatic confrontations between irri- better or for worse. Few people, including from individual mountain streams to larger residents, fully appreciate that the warm, rivers such as the McKenzie, has revealed gators and federal resource agencies dry sunny weather of each summer actu- that geology plays an extremely important in the Klamath basin. These events ally constitutes a pretty reliable drought, and previously unappreciated role in deter- with serious implications for water mining flow regimes.” underscore the critical and growing management. -
Geology of the Central and Northern Parts of the Western Cascade Range in Oregon
Geology of the Central and Northern Parts of the Western Cascade Range in Oregon GEOLOGICAL SURVEY PROFESSIONAL PAPER 449 Prepared in cooperation with the State of Oregon, Departtnent of Geology and Mineral Industries Geology of the Central and Northern Parts of the Western Cascade Range in Oregon By DALLAS L. PECK, ALLAN B. GRIGGS, HERBERT G: SCHLICKER, FRANCIS G. WELLS, and HOLLIS M. DOLE ·~ GEOLOGICAL SURVEY PROFESSIONAL PAPER 449 Prepared in cooperation with the State of Oregon, Department of Geology and Mineral Industries ,... UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director . -~ The U.S. Geological Survey Library catalog card for this publication appears after page 56. For sale by the Superintendent of Documents,. U.S. Government Printing Office · · ·. Washington, D.C. 20402 CONTENTS Page Page Stratigraphy-Continued 1 Abstract------------------------------------------- Sardine Formation-Continued Introduction ______ --------------------------------- 2 Lithology and petrography-Continued Scope of investigation ______ - ___ - __ -------------- 2 Location, accessibility, and culture __ -------------- 2 Pyroclastic rocks __________ -- __ ---------'-- 33 Physical features ______ --_---_-_- ___ -----_------- 3 Age and correlation ____ - _--- __ -------------- 34 Climate and vegetation ___ --- ___ - ___ -----_------- 4 Troutdale Formation _____ ------------------------ 35 Fieldwork and reliability of the geologic