Overview of Wheat Movement on the Columbia River Report Prepared August 17, 2016 All Data Based on Five Year Averages (2011-2015)
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Program 2019 Northwest Regional Managers Conference
PROGRAM 2019 NORTHWEST REGIONAL MANAGERS CONFERENCE April 30 – May 3, 2019 ◆ Best Western Plus, Hood River Printed copies of the agenda will be available onsite. All other handouts and presentations will be available online following the conference. Tuesday, April 30 4:00 pm – 6:30 pm Registration Shoreline Lounge 5:00 pm – 6:30 pm Welcome Reception Shoreline Lounge After you check-in at registration, join fellow conference attendees for a drink and some conversation. 6:30 pm Dinner on Own Hood River has many local restaurants. For recommendations, please refer to the “Hood River Attractions” handout available on www.occma.org or sign up to join one of the pre- arranged dinners at Registration. Wednesday, May 1 8:00 am – 5:00 pm Registration Gorge Room 8:00 am – 9:00 am Continental Breakfast Gorge Room 8:00 am – 3:00 pm Sponsor Exhibits Open Gorge Room Our sponsors/vendors will be available during session breaks and meals. Be sure to stop by for a visit. For a full list of sponsors/vendors, please visit www.occma.org. 9:00 am – 9:15 am Welcome Gorge Room OCCMA President Marty Wine of Tigard and WCMA President Cindy Reents of Richland welcome conference attendees to the 2019 Northwest Regional Managers Conference. 9:15 am – 10:30 am When Crisis Hits – Managing Through a Crisis or Significant Gorge Room Event in Your Community {LGMC-3} Facilitator: • Michael Sykes, City Manager, Scappoose, OR Speakers: • Scott Derickson, City Manager, Woodburn, OR • Nick Green, City Manager, John Day, OR • Jeff Hecksel, Hood River County Manager • Steve King, City Manager, Wenatchee, WA PROGRAM 2019 NORTHWEST REGIONAL MANAGERS CONFERENCE April 30 – May 3, 2019 ◆ Best Western Plus, Hood River Forest fires, active shooter and a massive influx of people are the types of events that these panelists have experienced firsthand. -
Lesson 1 the Columbia River, a River of Power
Lesson 1 The Columbia River, a River of Power Overview RIVER OF POWER BIG IDEA: The Columbia River System was initially changed and engineered for human benefit Disciplinary Core Ideas in the 20th Century, but now balance is being sought between human needs and restoration of habitat. Science 4-ESS3-1 – Obtain and combine Lesson 1 introduces students to the River of Power information to describe that energy curriculum unit and the main ideas that they will investigate and fuels are derived from natural resources and their uses affect the during the eleven lessons that make up the unit. This lesson environment. (Clarification Statement: focuses students on the topics of the Columbia River, dams, Examples of renewable energy and stakeholders. Through an initial brain storming session resources could include wind energy, students record and share their current understanding of the water behind dams, and sunlight; main ideas of the unit. This serves as a pre-unit assessment nonrenewable energy resources are fossil fuels and fissile materials. of their understanding and an opportunity to identify student Examples of environmental effects misconceptions. Students are also introduced to the main could include loss of habitat to dams, ideas of the unit by viewing the DVD selection Rivers to loss of habitat from surface mining, Power. Their understanding of the Columbia River and the and air pollution from burning of fossil fuels.) stakeholders who depend on the river is deepened through the initial reading selection in the student book Voyage to the Social Studies Pacific. Economics 2.4.1 Understands how geography, natural resources, Students set up their science notebook, which they will climate, and available labor use to record ideas and observations throughout the unit. -
Snake River 1157 Wildlife Habitat Information to Inform the Plan- Ton, and Northeast Oregon
Snake River 1157 wildlife habitat information to inform the plan- ton, and northeast Oregon. +roughout its long ning decisions for renewable energy. history, volcanoes, flooding, and glaciers have Climate change impacts may be felt in the arid shaped the river and its shores. region; nitrogen deposits, atmospheric carbon +e Snake River plain was created by a volca- dioxide, and other changes will impact the grass- nic hotspot beneath Yellowstone National Park, lands. Climate change may impact the size of the which holds the headwaters and origin of the river. sagebrush areas, for example, which in turn con- Flooding as the glaciers retreated after the ice age stricts grouse and other birds and mammals liv- created the current landscape, including eroded ing in these habitats. canyons and valleys. Mountains and plains are typical terrain along the river. +e Snake River has P J. C more than 20 major tributaries, most of them in the mountains; Hells Canyon is the deepest river Further Reading gorge in North America. Cutright, Paul Russell. Lewis and Clark: Pioneering +e Snake River is home to salmon and steel- Naturalists . Lincoln: University of Nebraska head, which were central to the lives of the Nez Press, 2003. Perce and Shoshone, the dominant tribal nations Petersen, Keith C. River of Life, Channel of Death: before the Europeans came. People have lived Fish and Dams on the Lower Snake . Corvallis: along the Snake River for over 15,000 years. +e Oregon State University Press, 2001. Snake River may have been given its name by the Waring, Gwendolyn. L. A Natural History of Shoshones, as a hand signal made by the Shosho- the Intermountain West: Its Ecological and nes representing fish was misinterpreted by Euro- Evolutionary Story. -
Columbia River Crossing I-5 Immersed Tunnel I-5 Immersed Tunnel Advantages Immersed Tunnel
6 Sections 500 feet long x 170 feet wide 3,000 ft. Columbia River Crossing I-5 Immersed Tunnel I-5 Immersed Tunnel Advantages Immersed Tunnel Navigation clearances Aviation clearances No freeway noise on river front No mile-long elevated bridge ramps dividing Vancouver Aberdeen Casting Basin 165 x 910 feet Baltimore's Fort McHenry Tunnel Completed 1985 1.4 miles 8 lanes – 4 tubes 115,000 vehicles/day I-95 Immersed Tunnel saved Baltimore’s Inner Harbor 1985 1959 freeway plan Vancouver’s Massey Tunnel under Fraser River October 14, 2019 Vancouver’s Fraser River Bridge replaced by Tunnel 10 lanes April 1, 2020 Vancouver’s Columbia River Bridge replaced by Tunnel Øresund Bridge 20 sections x 577ft = 2.2miles & Tunnel 1999 138ft wide Øresund Tunnel Section 20 sections x 577ft =2.2miles 138ft wide Columbia River Tunnel Section 6 sections x 500ft = 0.6miles 170ft wide Immersed Tunnels About six 500 foot immersed tunnel sections could be a simple, elegant, and cost effective solution to the I-5 Columbia River Crossing. The Aberdeen Casting Basin used to build the SR 520 bridge pontoons would be well suited to casting tunnel sections. https://www.wsdot.wa.gov/sites/default/files/2014/11/12/SR520-Factsheet-Pontoons- February2017.pdf In 1985 Baltimore completed the Fort McHenry Immersed Tunnel and saved its famous Inner Harbor from encirclement by I-95 concrete bridge. https://www.baltimorebrew.com/2011/04/29/the-senator-and-the-highway/ Vancouver, Canada rejected a ten lane bridge over the Fraser in favor of an immersed tunnel. https://www.enr.com/blogs/15-evergreen/post/47724-vancouvers-george-massey- tunnel-replacement-may-now-be-a-tunnel-instead-of-a-bridge The 1999 Oresund Bridge & Immersed Tunnel connects Sweden to Denmark. -
The Skagit-High Ross Controversy: Negotiation and Settlement
Volume 26 Issue 2 U.S. - Canada Transboundary Resource Issues Spring 1986 The Skagit-High Ross Controversy: Negotiation and Settlement Jackie Krolopp Kirn Marion E. Marts Recommended Citation Jackie K. Kirn & Marion E. Marts, The Skagit-High Ross Controversy: Negotiation and Settlement, 26 Nat. Resources J. 261 (1986). Available at: https://digitalrepository.unm.edu/nrj/vol26/iss2/6 This Article is brought to you for free and open access by the Law Journals at UNM Digital Repository. It has been accepted for inclusion in Natural Resources Journal by an authorized editor of UNM Digital Repository. For more information, please contact [email protected], [email protected], [email protected]. JACKIE KROLOPP KIRN* and MARION E. MARTS** The Skagit-High Ross Controversy: Negotiation and Settlement SETTING AND BACKGROUND The Skagit River is a short but powerful stream which rises in the mountains of southwestern British Columbia, cuts through the northern Cascades in a spectacular and once-remote mountain gorge, and empties into Puget Sound approximately sixty miles north of Seattle. The beautiful mountain scenery of the heavily glaciated north Cascades was formally recognized in the United States by the creation of the North Cascades National Park and the Ross Lake National Recreation Area in 1968, and earlier in British Columbia by creation of the E.C. Manning Provincial Park. The Ross Lake Recreation Area covers the narrow valley of the upper Skagit River in Washington and portions of several tributary valleys. It was created as a political and, to environmentalists who wanted national park status for the entire area, controversial, compromise which accom- modated the city of Seattle's Skagit River Project and the then-planned North Cascades Highway. -
History of Snake River Canyon Indicated by Revised Stratigraphy of Snake River Group Near Hagerman and King Hill, Idaho
History of Snake River Canyon Indicated by Revised Stratigraphy of Snake River Group Near Hagerman and King Hill, Idaho GEOLOGICAL SURVEY PROFESSIONAL PAPER 644-F History of Snake River Canyon Indicated by Revised Stratigraphy of Snake River Group Near Hagerman and King Hill, Idaho By HAROLD E. MALDE With a section on PALEOMAGNETISM By ALLAN COX SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 644-F Lavaflows and river deposits contemporaneous with entrenchment of the Snake River canyon indicate drainage changes that provide a basis for improved understanding of the late Pleistocene history UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY W. A. Radlinski, Acting Director Library of Congress catalog-card No. 72-171031 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 40 cents (paper cover) Stock Number 2401-1128 CONTENTS Page page Abstract ___________________________________________ Fl Late Pleistocene history of Snake River_ _ F9 Introduction.______________________________________ 2 Predecessors of Sand Springs Basalt. 13 Acknowledgments --..______-__-____--__-_---__-_____ 2 Wendell Grade Basalt-________ 14 Age of the McKinney and Wendell Grade Basalts. _____ 2 McKinney Basalt. ____---__---__ 16 Correlation of lava previously called Bancroft Springs Bonneville Flood.________________ 18 Basalt_________________________________________ Conclusion___________________________ 19 Equivalence of pillow lava near Bliss to McKinney Paleomagnetism, by Allan Cox_________ 19 Basalt.._________________________ References cited._____________________ 20 ILLUSTRATIONS Page FIGURE 1. Index map of Idaho showing area discussed.______________________________________________________ F2 2. Chart showing stratigraphy of Snake River Group..____________________________._____--___-_-_-_-. -
Forest Plan Amendment No. 30 Clearwater National Forest Latah
Forest Plan AmendmentNo. 30 Clearwater National Forest Latah County, Idaho The purpose of Amendment No. 30 is to changethe water quality objectives in Appendix K of the Clearwater National Forest Plan for Little Boulder Creek, East Fork Potlatch River, and Ruby Creek, plus, add the Potlatch River. Currently the water quality objective for Little Boulder, East Fork Potlatch and Ruby Creek is "Minimum viable" and the fish speciesis listed as rainbow. Minimum Viable does not support the requirements of the Clean Water Act to provide fishable streams. It only provides a minimal population and does not reflect the listing of the species or importance of the area for spawning. Surveys have documented steelhead in Little Boulder, East Fork Potlatph Riyer, and Ruby Creek. Steelheadwas listed as a Threatened Species within the Snake River in 1997. The Potlatch River, a migratory channel for steelhead,had only been listed in Appendix K as a placeholder to indicate the watershed geography. Stream surveys have shown the river to have a C channel and steelheadas the fish species. Spawning occurs in the East Fork Potlatch, and rearing occurs in most of the tributaries of the Potlatch River. Since the Potlatch River is proposed as critical habitat for steelhead,the water quality objective is being changed from "Minimum Viable" to "High Fish" to follow the direction of the Clean Water Act and Endangered SpeciesAct. Also, as part of the high fish standard, threshold levels of sediment for the Potlatch River should not exceed 10 out of 30 years. Since the proposed changes are not significant, adoption of this amendmentwould not significantly change the forest-wide environmental impacts disclosed in the Clearwater National Forest Plan EIS. -
Lower Snake River Dams Stakeholder Engagement Report
Lower Snake River Dams Stakeholder Engagement Report FINAL DRAFT March 6, 2020 Prepared by: Kramer Consulting Ross Strategic White Bluffs Consulting Contents Executive Summary .......................................................... 1 Opportunities to Increase Understanding .................................... 52 Background and Context ............................................................... 2 Public Comments Related to Agriculture ..................................... 52 Major Findings and Perspectives ................................................... 3 Section 7: Transportation .............................................. 53 Opportunities to Increase Understanding .................................... 12 Context ........................................................................................ 53 Moving Forward ........................................................................... 13 Perspectives ................................................................................ 60 Section 1: Purpose and Scope of Report ..................... 15 Opportunities to Increase Understanding .................................... 62 Background .................................................................................. 15 Public Comments Related to Transportation............................... 62 The Intent of the Report and Engagement Process .................... 15 Section 8: Recreation ..................................................... 64 Methodology................................................................................ -
The Geology of Part of the Snake River Canyon and Adjacent Areas in Northeastern Oregon and Western Idaho
AN ABSTRACT OF THE THESIS OF Tracy Lowell Vallier for the Ph.D. in Geology (Name) (Degree) (Major) Date thesis is presented May 1, 1967 Title THE GEOLOGY OF PART OF THE SNAKE RIVER CANYON AND ADJACENT AREAS IN NORTHEAXERN OREGON AND WESTERN IDAHO Abstract approved Redacted for Privacy (Major professor) The mapped area lies between the Wallowa Mountains of northeastern Oregon and the Seven Devils Mountains of western Idaho. Part of the Snake River canyon is in- cluded. A composite stratigraphic section includes at least 30,000 feet of strata. Pre- Tertiary and Tertiary strata are separated by a profound unconformity. Pre -Tertiary layered rocks are mostly Permian and Triassic volcani- clastic and volcanic flow rocks. At least four pre -Ter- tiary intrusive suites occur. Tertiary rocks are Miocene and Pliocene plateau basalts. Quaternary glacial materi- als and stream deposits locally mantle the older rocks. Permian ( ?) rocks of the Windy Ridge Formation are the oldest rocks and consist of 2,000 to 3,000 feet of keratophyre, quartz keratophyre, and keratophric pyro- clastic rocks. Unconformably ( ?) overlying the Windy Ridge Formation are 8,000 to 10,000 feet of volcaniclastic rocks and minor volcanic flow rocks of the Hunsaker Creek Formation of Middle Permian (Leonardian and Wordian) age. Spilitic flow rocks of the Kleinschmidt Volcanics are interlayered with and in part overlie the Hunsaker Creek Formation and comprise a sequence about 2,000 to 3,000 feet thick. The Paleozoic layered rocks were intruded by the Holbrook - Irondyke intrusives, composed of keratophyre porphyry, quartz keratophyre porphyry, diabase, and gab- bro. -
The Columbia River Gorge: Its Geologic History Interpreted from the Columbia River Highway by IRA A
VOLUMB 2 NUMBBI3 NOVBMBBR, 1916 . THE .MINERAL · RESOURCES OF OREGON ' PuLhaLed Monthly By The Oregon Bureau of Mines and Geology Mitchell Point tunnel and viaduct, Columbia River Hi~hway The .. Asenstrasse'' of America The Columbia River Gorge: its Geologic History Interpreted from the Columbia River Highway By IRA A. WILLIAMS 130 Pages 77 Illustrations Entered aa oeoond cl,... matter at Corvallis, Ore., on Feb. 10, l9lt, accordintt to tbe Act or Auc. :U, 1912. .,.,._ ;t ' OREGON BUREAU OF MINES AND GEOLOGY COMMISSION On1cm or THm Co><M188ION AND ExmBIT OREGON BUILDING, PORTLAND, OREGON Orncm or TBm DtBIICTOR CORVALLIS, OREGON .,~ 1 AMDJ WITHY COMBE, Governor HENDY M. PABKB, Director C OMMISSION ABTBUB M. SWARTLEY, Mining Engineer H. N. LAWRill:, Port.land IRA A. WILLIAMS, Geologist W. C. FELLOWS, Sumpter 1. F . REDDY, Grants Pass 1. L. WooD. Albany R. M. BIITT8, Cornucopia P. L. CAI<PBELL, Eugene W 1. KEBR. Corvallis ........ Volume 2 Number 3 ~f. November Issue {...j .· -~ of the MINERAL RESOURCES OF OREGON Published by The Oregon Bureau of Mines and Geology ~•, ;: · CONTAINING The Columbia River Gorge: its Geologic History l Interpreted from the Columbia River Highway t. By IRA A. WILLIAMS 130 Pages 77 Illustrations 1916 ILLUSTRATIONS Mitchell Point t unnel and v iaduct Beacon Rock from Columbia River (photo by Gifford & Prentiss) front cover Highway .. 72 Geologic map of Columbia river gorge. 3 Beacon Rock, near view . ....... 73 East P ortland and Mt. Hood . 1 3 Mt. Hamilton and Table mountain .. 75 Inclined volcanic ejecta, Mt. Tabor. 19 Eagle creek tuff-conglomerate west of Lava cliff along Sandy river. -
Soviet Ready to Negotiate on Settling Berlin Dispute
r - ’ z v » f'.-. :.'o’ .* / THURSDAY, AUGUST 8, 198r FACE EIGHTEEN Arenge Dally Net .PrcM Run iltanrl]ffBter lEnmittg ll^ralb The Weather For the Week Ended Eereeeet of O. S. WMtiMV I - June S, IBSl / CBeodf, foggy M d eeel tm About Town 13,3.30 lew In lew SSm, Bntnriny, i COME TO PINEHCRST FOR Member of the Audit wnmior, elMwan Into In dny or nt The ?lipser Club will hold a pub Bureeu of ObwnlatloB night. High M-f6. lic setback party Saturday night Manchester— A City of Village Charm GOOD/rS'EAR SCRATCH n at 8 o'clock. FRESH BLOCK ISLAND SWORDFISH The Manchester Junior Square VOL. LXXX, NO. 259 (FOURTEEN PAGES) MANCHESTER, CONN., FRIDAY, AUGUST 4, 1961 (CbMsIfled AdvertlelBg en Page U ) 'Dance Club will hold a dance to PRICE FIVE CENTS morrow from 7 to 10 p.m. at the DENT SALE We.«il Side tenni.e court.e. In the event or rain, the dance will be Aim at Pocketbooks SOME ONE OF A KIND-SOME FLOOR /UODELS- held in the recreation building. State News The Rev, Percy F. Smith of ALL BRANDNEW AND FULLY G''*RANTEED - ; New London, former aaeiatant paa- I tor otf South Methodiat Church In Roundup HUGE SAVINGS! Mancheeter, ie aecretary of the East Reds Add Soviet Ready to Negotiate annual four-day Methodiat aaaem- hly acheduled for Aug. 28 to Sept. 1 at Geneva Point' Camp Lake Winnepeaaukee, N.H. The Rev. Prospect Gets Harvey K. Motisley of Bolton, au- Worker Curbs perintendent of the Norwich Dia- trict of the Methodiat Church ia aa- Legal Licpior .■«:.«tant dean. -
2020 EARLY SEASON REPORT Columbia Shuswap Regional District Golden, BC (Area ‘A’) Mosquito Program
2020 EARLY SEASON REPORT Columbia Shuswap Regional District Golden, BC (Area ‘A’) Mosquito Program Submitted by Morrow BioScience Ltd. April 17, 2020 www.morrowbioscience.com Toll Free: 1-877-986-3363 [email protected] TABLE OF CONTENTS Executive Summary ____________________________________________________________ 1 Introduction __________________________________________________________________ 2 Monitoring Methodology _______________________________________________________ 2 Data Management ____________________________________________________________ 4 Education Outreach ____________________________________________________________ 4 Season Forecast _______________________________________________________________ 5 Snowpack ________________________________________________________________________ 5 Weather __________________________________________________________________________ 7 Reporting Schedule ____________________________________________________________ 8 Contacts _____________________________________________________________________ 8 References ___________________________________________________________________ 9 LIST OF TABLES Table 1. Snow basin indices for the Upper Columbia Basin determined by the 1 April 2018, 1 April 2019, and 1 April 2020 bulletins ............................................................................................ 7 LIST OF APPENDICES Appendix I. Frequently Asked Questions (FAQs) regarding Aquabac®, the bacterial larvicide utilized by MBL (a.i., Bacillus thuringiensis var. israelensis) Appendix