Oregon State Game Commission Were Consolidated and the Total Catch Determined
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Historical Overview
HISTORIC CONTEXT STATEMENT The following is a brief history of Oregon City. The intent is to provide a general overview, rather than a comprehensive history. Setting Oregon City, the county seat of Clackamas County, is located southeast of Portland on the east side of the Willamette River, just below the falls. Its unique topography includes three terraces, which rise above the river, creating an elevation range from about 50 feet above sea level at the riverbank to more than 250 feet above sea level on the upper terrace. The lowest terrace, on which the earliest development occurred, is only two blocks or three streets wide, but stretches northward from the falls for several blocks. Originally, industry was located primarily at the south end of Main Street nearest the falls, which provided power. Commercial, governmental and social/fraternal entities developed along Main Street north of the industrial area. Religious and educational structures also appeared along Main Street, but tended to be grouped north of the commercial core. Residential structures filled in along Main Street, as well as along the side and cross streets. As the city grew, the commercial, governmental and social/fraternal structures expanded northward first, and with time eastward and westward to the side and cross streets. Before the turn of the century, residential neighborhoods and schools were developing on the bluff. Some commercial development also occurred on this middle terrace, but the business center of the city continued to be situated on the lower terrace. Between the 1930s and 1950s, many of the downtown churches relocated to the bluff as well. -
Willamette Falls Recertification Review Report 2018
Willamette Falls (LIHI # 33) Recertification Review Report Introduction and Overview This report reviews the application submitted by Portland General Electric (applicant) to the Low Impact Hydropower Institute (LIHI) for LIHI recertification for the Willamette Falls Hydroelectric Project (Facility) located on the Willamette River in Clackamas County, Oregon. The Federal Energy Regulatory Commission (FERC) relicensed the project (FERC 2233) in 2005 for the operation and maintenance of the 15.18 megawatt run-of-river project. This application review for recertification was conducted using the new, 2nd Edition Handbook that was published in March 2016. Background: The project is located at river mile 26.5 on the Willamette River within the city limits of Oregon City (to the east) and West Linn (to the west) in north-central Oregon, approximately 10 miles from Portland and 40 miles from the Willamette’s confluence with the Columbia River. The project is located in a populated, industrial urban setting at the site of Willamette Falls, a natural waterfall that marks the head of the tidally influenced lower Willamette River. The applicant has operated hydroelectric facilities at the site since 1889. Willamette Falls (the Falls) is a horseshoe-shaped, 40-foot-high, natural waterfall that marks the head of the tidally influenced lower Willamette River. The general project area has been home to hydroelectric generation for more than 125 years, beginning with PGE’s Station A in 1889 and continuing to this day with PGE’s T.W. Sullivan (TWS) Powerhouse, built in 1895. Multiple paper mills have also operated at the Falls for more than a century. -
Click Here to Download the 4Th Grade Curriculum
Copyright © 2014 The Confederated Tribes of Grand Ronde Community of Oregon. All rights reserved. All materials in this curriculum are copyrighted as designated. Any republication, retransmission, reproduction, or sale of all or part of this curriculum is prohibited. Introduction Welcome to the Grand Ronde Tribal History curriculum unit. We are thankful that you are taking the time to learn and teach this curriculum to your class. This unit has truly been a journey. It began as a pilot project in the fall of 2013 that was brought about by the need in Oregon schools for historically accurate and culturally relevant curriculum about Oregon Native Americans and as a response to countless requests from Oregon teachers for classroom- ready materials on Native Americans. The process of creating the curriculum was a Tribal wide effort. It involved the Tribe’s Education Department, Tribal Library, Land and Culture Department, Public Affairs, and other Tribal staff. The project would not have been possible without the support and direction of the Tribal Council. As the creation was taking place the Willamina School District agreed to serve as a partner in the project and allow their fourth grade teachers to pilot it during the 2013-2014 academic year. It was also piloted by one teacher from the Pleasant Hill School District. Once teachers began implementing the curriculum, feedback was received regarding the effectiveness of lesson delivery and revisions were made accordingly. The teachers allowed Tribal staff to visit during the lessons to observe how students responded to the curriculum design and worked after school to brainstorm new strategies for the lessons and provide insight from the classroom teacher perspective. -
Geologic Map of the Cascade Head Area, Northwestern Oregon Coast Range (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 Minute Quadrangles)
(a-0g) R ago (na. 96-53 14. U.S. DEPARTMENT OF THE INTERIOR , U.S. GEOLOGICAL SURVEY Alatzi2/6 (Of (c,c) - R qo rite 6/6-53y Geologic Map of the Cascade Head Area, Northwestern Oregon Coast Range (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 minute Quadrangles) by Parke D. Snavely, Jr.', Alan Niem 2 , Florence L. Wong', Norman S. MacLeod 3, and Tracy K. Calhoun 4 with major contributions by Diane L. Minasian' and Wendy Niem2 Open File Report 96-0534 1996 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American stratigraphic code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1/ U.S. Geological Survey, Menlo Park, CA 94025 2/ Oregon State University, Corvallis, OR 97403 3/ Consultant, Vancouver, WA 98664 4/ U.S. Forest Service, Corvallis, OR 97339 TABLE OF CONTENTS INTRODUCTION 1 GEOLOGIC SKETCH 2 DESCRIPTION OF MAP UNITS SURFICIAL DEPOSITS 7 BEDROCK UNITS Sedimentary and Volcanic Rocks 8 Intrusive Rocks 14 ACKNOWLEDGMENTS 15 REFERENCES CITED 15 MAP SHEETS Geologic Map of the Cascade Head Area, Northwestern Oregon Coast Range, scale 1:24,000, 2 sheets. Geologic Map of the Cascade Head Area, Northwest Oregon Coast Range (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 minute Quadrangles) by Parke D. Snavely, Jr., Alan Niem, Florence L. Wong, Norman S. MacLeod, and Tracy K. Calhoun with major contributions by Diane L. Minasian and Wendy Niem INTRODUCTION The geology of the Cascade Head (W.W. -
Volcanic Vistas Discover National Forests in Central Oregon Summer 2009 Celebrating the Re-Opening of Lava Lands Visitor Center Inside
Volcanic Vistas Discover National Forests in Central Oregon Summer 2009 Celebrating the re-opening of Lava Lands Visitor Center Inside.... Be Safe! 2 LAWRENCE A. CHITWOOD Go To Special Places 3 EXHIBIT HALL Lava Lands Visitor Center 4-5 DEDICATED MAY 30, 2009 Experience Today 6 For a Better Tomorrow 7 The Exhibit Hall at Lava Lands Visitor Center is dedicated in memory of Explore Newberry Volcano 8-9 Larry Chitwood with deep gratitude for his significant contributions enlightening many students of the landscape now and in the future. Forest Restoration 10 Discover the Natural World 11-13 Lawrence A. Chitwood Discovery in the Kids Corner 14 (August 4, 1942 - January 4, 2008) Take the Road Less Traveled 15 Larry was a geologist for the Deschutes National Forest from 1972 until his Get High on Nature 16 retirement in June 2007. Larry was deeply involved in the creation of Newberry National Volcanic Monument and with the exhibits dedicated in 2009 at Lava Lands What's Your Interest? Visitor Center. He was well known throughout the The Deschutes and Ochoco National Forests are a recre- geologic and scientific communities for his enthusiastic support for those wishing ation haven. There are 2.5 million acres of forest including to learn more about Central Oregon. seven wilderness areas comprising 200,000 acres, six rivers, Larry was a gifted storyteller and an ever- 157 lakes and reservoirs, approximately 1,600 miles of trails, flowing source of knowledge. Lava Lands Visitor Center and the unique landscape of Newberry National Volcanic Monument. Explore snow- capped mountains or splash through whitewater rapids; there is something for everyone. -
2008 Portland, UNITED STATES
GGGeeennneeesss,,, BBBrrraaaiiinnn,,, aaannnddd BBBeeehhhaaavvviiiooorrr Tenth Annual Meeting of the International Behavioural and Neural Genetics Society May 5‐9, 2008 University Place Hotel and Conference Center 310 SW Lincoln Street at SW 3rd Avenue, Tel. 503.221.0140 Portland, Oregon USA Sponsored by National Institute on Alcohol Abuse and Alcoholism, National Institutes of Health, USA National Institute of Child Health and Human Development, National Institutes of Health, USA National Institute of Mental Health, National Institutes of Health, USA Exhibitors: Noldus Program Committee: Kari Buck (Chair), John Crabbe, Daniel Goldowitz, Andrew Holmes, Helen Kamens, Charalambos Kyriacou, Richard Nowakowski, Inga Poletaeva, Oliver Stork Local Organizers: Kari Buck, John Crabbe, Tamara Phillips, Mark Rutledge‐Gorman Genes, Brain, and Behavior May 5‐9, 2008 Table of Contents Page Conference Program Schedule at‐a‐Glance 3 Hotel Map of Conference Meeting and Event Locations 3 Portland Downtown Map 4 General Information 5‐6 Accommodation and Emergency Contact Banking and Currency Exchange Cultural, Recreation and Athletic Activities E‐mail and Internet Access Emergency Telephone Numbers Medical and Dental Treatment Name Badge Parking Posters Responsibility Smoking Taxes Transportation in the Portland Area From Portland International Airport (PDX) to University Place Hotel Transportation: Streetcars, Buses, Taxis Tram (Aerial) to Oregon Health & Science University IBANGS Award Winners 7 Conference Program Schedule ‐ Detailed 8‐14 Wineries Tour -
State Highway Department
Description of WOrk of the State Highway Department in the Counties of the State 1923 -1924 BAKER COUNTY There was less activity in highway constructjon in Baker County dur- ing the biennium just past than in previousyears. However, the main trunk line highway known as the Old Oregon Trailwas completed during this period, and some work was doneon the Baker-Cornucopia and the Baker-Unity Highways. The work on the Baker-Cornucopia Highway involved theconstruction of the grade down the Powder River Canyon, which eliminated the high Sparta summit and materially improved existing communicationbetween the Eagle and Pine Valleys and Baker.However, there still remains a very bad section between Middle Bridge and Love Bridge, and the section between Black Bridge and Richland, through the Dry Gulch country, is impassable to automobile traffic during the spring of theyear. On the Baker-Unity Highway the gradeon both sides of Dooley Moun- tain was completed. Those who were forced to travel the old mountain grade, which was narrow, crooked, and in places reacheda gradient of 22 per cent, will appreciate traveling over thenew highway now open to traffic. The total length of grading completed in Baker County during the past biennium was 18.11 miles, of which 8.95 mileswere surfaced. in addition to this work there were 25.90 miles surveyed. The Baker County bond issue of 1918, amounting to $500,000,was in- sufficient to meet the State in cooperating to complete the state highways through the county, and on November 4, 1924,an additional $500,00G was voted to complete the Baker-Cornucopia and the Baker-Unity High- ways. -
THS Newsletter Nov Dec 2010.Pub
Tualatin Historical Society Newsletter NOVEMBER/DECEMBERJune 20082010 Founded in 1986, the Society’s mission is to preserve, promote and interpret the rich and colorful history of Tualatin Save the Date… Annual Meeting and Potluck November 7 Good old-fashioned The 2010 Lafky-Martinazzi potluck fare and con- Award for exceptional service versation will high- to THS will be revealed dur- “The Valley of the Giants” light the 2010 annual ing the afternoon. Each February, in com- meeting of Tualatin Historical Soci- Come celebrate accomplishments and memoration of the opening ety this Sunday, November 7 at Tu- anticipate activities on the horizon. of the Tualatin Heritage alatin Heritage Center starting at Election of officers for 2011 will also Center in 2006, the Tuala- 1:00 p.m. There will be no regu- be conducted. tin Historical Society lar meeting on November 3. Bring presents a look at some as- You might also be a winner in our pect of Tualatin history. your own table service as well as a drawing for special prizes. All comers The next “look” will take favorite dish to share. Beverages get a ticket. We might also test your us back in time to what will be provided. Tualatin history IQ. Tualatin was like some l5,000 years ago when the Annual THS Wine Tasting and Auction Nets $6500 area was home to giant animals, long extinct, and Despite the heavy rain, a fun eve- was periodically deluged ning was had by all. The event fea- by tumultuous icy floods. It turing Northwest wines, tasty food was the Ice Age, and the and live music from Island Trio presenters will show and helped approximately 100 guests tell the story of our ice-age raise $6500 after expenses to help past and the evidence that THS continue its mission. -
Spawning Areas and Abundance of Chinook Salmon {Oncorhynchus Tshawytscha} in the Columbia River Basin--Past and Present By
UNITED STATES DEPARTMENT OF THE INTERIOR u.S. FISH AND WILDLIFE SERVICE BUREAU OF COMMERCIAL FISHERIES Spawning Areas and Abundance of Chinook Salmon {Oncorhynchus tshawytscha} in The Columbia River Basin--Past and Present By LEONARD A. FULTON United States Fish and Wildlife Service Special Scientific Report- - Fisheries No. 571 Washington, D.C. October 1968 CONTENTS Page Introduction........................ Spring- and summer-run chinook salmon. .. 3 Spawning areas . .. 3 Abundance of spring- and summer- run chinook salmon. 4 Fall-run chinook salmon. 16 Spawning areas . 16 Abundance of fall- run chinook salmon 20 Summary and conclusions 22 Acknowledgments. 23 Literature cited .. 24 Maps .............. .See Map Appendix iii Spawning Areas and Abundance of Chinook Salmon (Oncorhynchus tshawytscha) in The Columbia River Basin--Past and Present By LEONARD A. FULTON, Fishery Biologist Bureau of Commercial Fisheries 'Biological Laboratory Seattle, Washington 98102 ABSTRACT Chinook salmon, the most abundant species of salmon in the Columbia Basin, formerly spawned in nearly a11 tributaries ofthe Columbia River and in many areas of the main river. Over the past 60 years, the construction of dams has inundated, impeded, or blocke.d acces!, to spawning areas. Despite these heavy losses, large areas of spawning grounds in the middle and lower portions of the drainage are sti11 available to chinook salmon. Stream im provements by State and Federal fishery agencies have rehabilitated some areas and have brought others into production for the first time. Important spawning areas are listed and charted in this report according to their past use (before 1965) and present use (1966). Estimates of recent spawning populations in major tributaries and in segments of the main stem are also given. -
Nestucca Sanctuary a Former Jesuit Retreat Pacific City, Oregon
Real Estate Auction Oregon Coast Legacy Property Nestucca Sanctuary A former Jesuit Retreat Pacific City, Oregon Pacific City Kiwanda Beach Nestucca Bay National Wildlife Refuge 93± acre headland peninsula with over one mile of shoreline, ocean and bay views, and location next to Nestucca Bay National Wildlife Refuge SEALED BIDS DUE: December 5, 2012 REALTY MARKETING/NORTHWEST The Opportunity Kiwanda Beach Haystack Rock Pacific City Bob Straub State Park Location of Lodge and Nestucca Bay additional Improvements National Wildlife Refuge, Airport Cannery Hill Unit 88± Acres Gated Entry Access Road Tax Lot 4300 5± Acres Tax Lot 400 The 93± acre Nestucca Sanctuary – a former Jesuit retreat -- is one of the largest north coast ocean and bay view properties still available for potential redevelopment as a camp or retreat, for education or commercial recreation uses, within a two-hour drive of Portland. It is located five miles south of Pacific City, next to the Cannery Hill Unit of the Nestucca Bay National Wildlife Refuge, along a spectacular forested headland peninsula with lodge complex and over one mile of shoreline, providing an opportunity to acquire a Pacific Northwest legacy property with seclusion and significant conservation values. Nestucca Bay is considered one of the crown jewels of Oregon’s north coast, formed by the Nestucca and Little Nestucca Rivers and tributaries which support large runs of Chinook and Coho salmon, Nestucca Sanctuary cutthroat trout, and steelhead. R E A L T Y M A R K E T I N G / N O R T H W E S T Portland -
Geophysical and Geochemical Analyses of Selected Miocene Coastal Basalt Features, Clatsop County, Oregon
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1980 Geophysical and geochemical analyses of selected Miocene coastal basalt features, Clatsop County, Oregon Virginia Josette Pfaff Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geochemistry Commons, Geophysics and Seismology Commons, and the Stratigraphy Commons Let us know how access to this document benefits ou.y Recommended Citation Pfaff, Virginia Josette, "Geophysical and geochemical analyses of selected Miocene coastal basalt features, Clatsop County, Oregon" (1980). Dissertations and Theses. Paper 3184. https://doi.org/10.15760/etd.3175 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]. AN ABSTRACT OF THE THESIS OF Virginia Josette Pfaff for the Master of Science in Geology presented December 16, 1980. Title: Geophysical and Geochemical Analyses of Selected Miocene Coastal Basalt Features, Clatsop County, Oregon. APPROVED BY MEMBERS OF THE THESIS COMMITTEE: Chairman Gi lTfiert-T. Benson The proximity of Miocene Columbia River basalt flows to "locally erupted" coastal Miocene basalts in northwestern Oregon, and the compelling similarities between the two groups, suggest that the coastal basalts, rather than being locally erupted, may be the westward extension of plateau -
AN INVENTORY of FILLED LANDS in NESTUCCA RIVER ESTUARY August 1972
AN INVENTORY OF FILLED LANDS IN NESTUCCA RIVER ESTUARY August 1972 ADVISORY COMMITTEE TO THE STATE LAND BOARD Representative Anthony Meeker, Chairman Senator Gordon W. McKay, Vice Chairman Senator Betty Browne Senator George Eivers Representative Paul Hanneman Representative Richard Magruder Representative Rod McKenzie Mr. Patrick Gilroy Mr. Cecil L. Edwards, Executive Assistant Prepared by the Advisory Committees Engineering Staff under the direction of Stanley F. Hamilton, P.E. Staff Engineer Oregon Division of State Lands This report was funded by the Advisory Committee to the State Land Board and a grant from the U.S. Department of Labors Emergency Employment Act of 1971 Nestucca River Basin, located in Tillamook, Yamhill, and Polk counties, Oregon, about 75 miles south of the Columbia River mouth, drains an area on the western slope of the Coast Range. The basin is bounded by the Pacific Ocean on the west, the Tillamook and Trask River divides on the north, the Coast Range divides on the east, and the Neskowin Creek and Salmon River divides on the south. The drainge area of the basin is approximately 317 square miles._?? The major streams of the basin are the Nestucca River and the Little Nestucca River which flow into the Nestucca estuary and then discharge dir- ectly into the Pacific Ocean immediately south of Cape Kiwanda. The Nestucca estuary has a total area of 1000 acresY of which 578 acres are legal tidelands41 Since statehood, the State Land Board has deededsome 299 acres of tide- lands to private owners.!" The navigable length of the Nestucca River / is 6.0 miles and the Little Nestucca River 1.6 miles._ These distances are recorded from the mouth of each river respectively.