The Columbia River System Inside Story the Columbia River System Inside Story
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Gills Coulee Creek, 2006 [PDF]
Wisconsin Department of Natural Resources Bureau of Watershed Management Sediment TMDL for Gills Coulee Creek INTRODUCTION Gills Coulee Creek is a tributary stream to the La Crosse River, located in La Crosse County in west central Wisconsin. (Figure A-1) The Wisconsin Department of Natural Resources (WDNR) placed the entire length of Gills Coulee Creek on the state’s 303(d) impaired waters list as low priority due to degraded habitat caused by excessive sedimentation. The Clean Water Act and US EPA regulations require that each state develop Total Maximum Daily Loads (TMDLs) for waters on the Section 303(d) list. The purpose of this TMDL is to identify load allocations and management actions that will help restore the biological integrity of the stream. Waterbody TMDL Impaired Existing Codified Pollutant Impairment Priority WBIC Name ID Stream Miles Use Use Gills Coulee 0-1 Cold II Degraded 1652300 168 WWFF Sediment High Creek 1-5 Cold III Habitat Table 1. Gills Coulee use designations, pollutants, and impairments PROBLEM STATEMENT Due to excessive sedimentation, Gills Coulee Creek is currently not meeting applicable narrative water quality criterion as defined in NR 102.04 (1); Wisconsin Administrative Code: “To preserve and enhance the quality of waters, standards are established to govern water management decisions. Practices attributable to municipal, industrial, commercial, domestic, agricultural, land development, or other activities shall be controlled so that all waters including mixing zone and effluent channels meet the following conditions at all times and under all flow conditions: (a) Substances that will cause objectionable deposits on the shore or in the bed of a body of water, shall not be present in such amounts as to interfere with public rights in waters of the state. -
Northrup Canyon
Northrup Canyon Why? Fine basalt, eagles in season Season: March to November; eagles, December through February Ease: Moderate. It’s about 1 ¾ miles to an old homestead, 3 ½ miles to Northrup Lake. Northrup Canyon is just across the road from Steamboat Rock, and the two together make for a great early or late season weekend. Northrup, however, is much less visited, so offers the solitude that Steamboat cannot. In season, it’s also a good spot for eagle viewing, for the head of the canyon is prime winter habitat for those birds. The trail starts as an old road, staying that way for almost 2 miles as it follows the creek up to an old homestead site. At that point the trail becomes more trail-like as it heads to the left around the old chicken house and continues the last 1 ½ miles to Northrup Lake. At its start, the trail passes what I’d term modern middens – piles of rusted out cans and other metal objects left from the time when Grand Coulee Dam was built. Shortly thereafter is one of my two favorite spots in the hike – a mile or more spent walking alongside basalt cliffs decorated, in places, with orange and yellow lichen. If you’re like me, about the time you quit gawking at them you realize that some of the columns in the basalt don’t look very upright and that, even worse, some have already fallen down and, even more worse, some have not quite finished falling and are just above the part of the trail you’re about to walk. -
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. -
Evaluating Snowmelt Runoff Generation in a Discontinuous Permafrost
Evaluating snowmelt runoff generation in a discontinuous Nordic Hydrology permafrost catchment using stable isotope, hydrochemical and hydrometric data* S.K. Carey1 and W.L. Quinton2 1Department of Geography and Environmental Studies, Carleton University, Ottawa, Ontario, Canada K1S 5B6 Vol 35 No 4 pp 309–324 E-mail: [email protected] 2Department of Geography, Simon Fraser University, Burnaby, British Columbia, Canada V5A 1S6 Received 1 November 2003; accepted in revised form 15 June 2004 Abstract Research on snowmelt runoff generation in discontinuous permafrost subarctic catchments has highlighted the role of: (i) permafrost in restricting deep percolation and sustaining near-surface water tables and (ii) the surface organic layer in rapidly conveying water to the stream. Conceptual models of runoff generation have largely been derived from hydrometric data, with isotope and hydrochemical data having only limited q application in delineating sources and pathways of water. In a small subarctic alpine catchment within the Wolf IWA Publishing 2004 Creek Research Basin, Yukon, Canada, snowmelt runoff generation processes were studied during 2002 using a mixed methods approach. Snowmelt timing varied between basin slopes, with south-facing exposures melting prior to permafrost-underlain north-facing slopes. The streamflow freshet period begain after 90% of snow had melted on the south-facing slope and coincided with the main melt period on the north-facing slope, indicating that contributing areas were largely defined by permafrost distribution. Stable isotope (d18O) and hydrochemical parameters (dissolved organic carbon, specific conductivity, pH) suggest that, at the beginning of the melt period, meltwater infiltrates soil pores and resides in temporary storage. As melt progresses and bare ground appears, thawing of soils and continued meltwater delivery to the slopes allows rapid drainage of this meltwater through surface organic layers. -
Provincial Freshet and Flood Status
Dashboard # Provincial Lead Contact: Media Relations contact: Provincial Freshet and Flood Status Manager, River Forecast Centre & Flood Safety Provincial Information Coordination Officer Date: June 24th, 2021, 4:00 pm Freshet 12 - George Roman Tyler Hooper 2021 Water Management Branch, Public Affairs Officer Ministry of Forests, Lands, Natural Resource [email protected] Operations and Rural Development (FLNRORD) 250-213-8172 [email protected] 250-896-2725 Provincial Summary Several streams and rivers are flowing higher this week than seasonal due the unprecedented historic heat resulting in a number of Flood Warnings, Flood Watches and High Streamflow Advisories. In general, stream flows will begin to recede over the next week. The Fraser River is expected to rise into the weekend; however, flows are forecast to remain below their earlier 2021 peaks. Provincial staff, local government staff, First Nations, and other parties continue to monitor the situation and support the implementation of flood emergency preparedness, response, and recovery. The public is advised to stay clear of all fast-flowing rivers and streams and potentially unstable riverbanks during spring high streamflow periods. Weather (Current and Forecast) Temperatures have reduced from the historic heat we recently experienced. As the ridge that resulted in the high temperatures moves east there is increased risk of instability leading to thunder and lightening. Limited precipitation is expected over the next several days. Flood Warnings and Advisories River Conditions and Outlook Flood Warning The historic heat event has led to historic snow melt. Many streams responded to the extreme heat and high elevation snow and glacial • Upper Fraser River melt. -
Power System
HISTORY AND CURRENT STATUS OF THE ELECTRICITY INFRASTRUCTURE IN THE PACIFIC NORTHWEST Kevin Schneider Ph.D., P.E. Chair, Seattle Chapter of the IEEE PES IEEE PES SCHOLARSHIP PLUS INITIATIVE 2 Washington State PES Scholars • Patrick Berg, Seattle University • Parichehr Karimi, University of • Zachary Burrows, Eastern Washington Washington UiUnivers ity • TiTravis Kinney, WhitWashington Sta te UiUnivers ity • Erin Clement, University of Washington • Allan Koski, Eastern Washington University • Anastasia Corman, University of • Kyle Lindgren, University of Washington, Washington • John Martinsen, Washington State • Gwendolyn Crabtree, Washington State University University • Melissa Martinsen, University of • David Dearing, Washington State Washington University • JthJonathan NhiNyhuis, SttlSeattle PifiPacific UiUnivers ity • Terra Donley, Gonzaga University Derek Jared Pisinger, Washington State Gowrylow, Seattle University University • Sanel Hirkic, Washington State University • Douglas Rapier, Washington State • Nathan Hirsch, Eastern Washington University University • Chris Rusnak, Washington State University • John Hofman, Washington State • Kaiwen Sun, University of Washington University • Joshua Wu, Seattle University • • Tracy Yuan, University of Washington 3 OVERVIEW Part 1: The Current Status of the Electricity Infrastructure in the Pacific North west Part 2: How the Current System Evolved Over Time Part 3: Current Challenges and the Path Forward Part 4: Concluding Comments PART 1:: THE CURRENT STATUS OF THE ELECTRICITY INFRASTRUCTURE -
3.2 Flood Level of Risk* to Flooding Is a Common Occurrence in Northwest Oregon
PUBLIC COMMENT DRAFT 11/07/2016 3.2 Flood Level of Risk* to Flooding is a common occurrence in Northwest Oregon. All Flood Hazards jurisdictions in the Planning Area have rivers with high flood risk called Special Flood Hazard Areas (SFHA), except Wood High Village. Portions of the unincorporated area are particularly exposed to high flood risk from riverine flooding. •Unicorporated Multnomah County Developed areas in Gresham and Troutdale have moderate levels of risk to riverine flooding. Preliminary Flood Insurance Moderate Rate Maps (FIRMs) for the Sandy River developed by the Federal Emergency Management Agency (FEMA) in 2016 •Gresham •Troutdale show significant additional risk to residents in Troutdale. Channel migration along the Sandy River poses risk to Low-Moderate hundreds of homes in Troutdale and unincorporated areas. •Fairview Some undeveloped areas of unincorporated Multnomah •Wood Village County are subject to urban flooding, but the impacts are low. Developed areas in the cities have a more moderate risk to Low urban flooding. •None Levee systems protect low-lying areas along the Columbia River, including thousands of residents and billions of dollars *Level of risk is based on the local OEM in assessed property. Though the probability of levee failure is Hazard Analysis scores determined by low, the impacts would be high for the Planning Area. each jurisdiction in the Planning Area. See Appendix C for more information Dam failure, though rare, can causing flooding in downstream on the methodology and scoring. communities in the Planning Area. Depending on the size of the dam, flooding can be localized or extreme and far-reaching. -
Economics of Columbia River Initiative
Economics of Columbia River Initiative Final Report to the Washington Department of Ecology and CRI Economics Advisory Committee. Study Team: Daniel Huppert School of Marine Affairs University of Washington Gareth Green Albers School of Business Seattle University William Beyers Department of Geography University of Washington Andrew Subkoviak Department of Economics University of Washington Andrew Wenzl Department of Geography University of Washington January 12, 2004 Executive Summary i EXECUTIVE SUMMARY The purpose of this study is to review the economic effects of increased water use from the Columbia River in the context of Washington State’s Columbia River Initiative (CRI). The CRI is designed to address the legal, scientific, and political issues related to water use from the mainstem of the Columbia River in Washington State. The economic analysis in this report is one of several kinds of information that will be used to inform the Department of Ecology’s rule- making related to the Columbia River. In addition to this review, the State has contracted with the National Academy of Sciences to consider the relationship between water use and the health of salmon populations. This report focuses on the economic consequences of increased water diversions in the mainstem Columbia river in Washington State, including effects on agricultural production, municipal and industrial water supplies, hydropower generation, flood control, river navigation, commercial and recreational fishing, regional impacts, and passive use values. In addition to gauging these effects, the report includes a summary of issues related to the increased use of market transactions in water rights. The analysis is focused on a series of five “Management Scenarios” developed by the Department of Ecology in consultation with water users. -
Dolen, Timothy P
Historical Development of Durable Concrete for the Bureau of Reclamation Timothy P. Dolen Research Civil Engineer - Senior Technical Specialist Materials Engineering and Research Laboratory Technical Service Center - Denver, Colorado Introduction The Bureau of Reclamation infrastructure stretches across many different climates and environments in the seventeen western states. Many of the dams, spillways, pumping plants, power plants, canals, and tunnels are constructed with concrete. These structures were built from Arizona to Montana, across the plains and in the mountains and deserts. Concrete structures had to remain durable to resist both the design loads and the natural environments of the western climate zones. Many natural environments can be quite destructive to concrete and the earliest Reclamation projects were faced with a variety of durability problems. The state-of-the-art of concrete construction advanced from hand mixing and horse and wagon transporting operations to automated mixing plants, underwater canal construction, and pumping and conveyor placing. This paper first overviews the challenges facing concrete construction in the beginning of the 20th Century. It then traces the Bureau of Reclamation’s role in the development of durable concrete to resist the environments of the west. What is Concrete? Before we begin, we must first understand what is concrete, the most versatile building material. The American Concrete Institute defines concrete as “a composite material that consists essentially of a binding medium within which are embedded particles or fragments of aggregate, usually a combination of fine aggregate and coarse aggregate; in portland-cement concrete, the binder is a mixture of portland cement and water.”1 The earliest concretes date at least as far back as early Roman times including the aqueducts and the historic Pantheon in Rome. -
National Register of Historic Places Registration Form
NPS Form 10-900 OMB No. 10024-0018 (Oct. 1990) United States Department of the Interior ,C£$ PftRKSERVIC National Park Service National Register of Historic Places Registration Form This form is for use in nominating or requesting determinations for individual properties and districts. See instructions in How to Complete the National Register of Historic Pla Registration Form (National Register Bulletin 16A). Complete each item by marking "x" in the appropriate box or by entering the information requested. If an item does not ap property being documented, enter "N/A" for "not applicable." For functions, architectural classification, materials, and areas of significance, enter only categories and subcatei instructins. Place additional entries and narrative items on continuation sheets (NPS Form 10-900a). Use a typewriter, word processor, or computer, to complete all items. 1. Name of Property historic name: American Falls Reservoir Flooded Townsite other name/site number: 2. Location street & number American Falls Reservoir [ ] not for publication city or town American Falls ______ [ X ] vicinity state: Idaho code: ID county: Power code: 077 zip code: 83211 3. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act, as amended, I hereby certify that this [X] nomination [ ] request for determination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 -
The Selkirk Mountains : a Guide for Mountain Climbers and Pilgrims
J Presentee) to ^be Xibrar^ of tbe xaniversit^ of Toronto bs Her"bert B. Sampson, K,C, Digitized by the Internet Archive in 2011 with funding from University of Toronto http://www.archive.org/details/selkirkmountainsOOwhee THE Selkirk Mountains A Guide for Mountain Climbers and Pilgrims Information by A. O. WHEELER, F.R.G.S., A.C.C., A.C., A.A.C. vo A- Stovel Company, Engravers, Lithographers and Printers, Winnipeg, Man. Arthur O. Wheeler, First President of Alpine Club — CONTENTS Foreword—A. 0. Wlieeler Page 1 One Word More—Elizabeth Parker 2 The Snowy Selkirks—Elizabeth Parker 3-5 CHAPTER I. The Rocky Mountain System—The Selkirks—Early Explorers Later Histor}'—The Railway—Discovery of Rogers Pass—An Alpine Club—Members of British Association Visit the Selkirks, (1884) —Result of Completion of Railway—Government Surveys (1886) —First Scientific Observations of Illecillewaet Glacier Topographical Survey by William Spotswood Green—The Alpine Club, England, and the Swiss Alpine Club—The Appalachian Mountain Club—Triangulation of Railway Belt—Subsequent Mountaineering Pages 6-32 CHAPTER n. Peaks, Passes and Valleys Reached from Glacier—Glacier Park Swiss Guides—Glacier House—Outfits and Ponies—Places and Peaks of Interest Alphabetically Arranged 33-104 CHAPTER m. The Caves of Cheops (Xakimu Caves) —the Valley of the Caves The Approach to the Caves—Formation and Structure—Descrip- tion of Caves—The Mill Bridge Series—The Gorge Series—The Judgment Hall 106-117 CHAPTER IV. •Golden and the Country of the Upper Columbia—Along the Columbia River between Golden and Beavermouth are Several Points of Interest—the Upper Columbia—Travel by Waterway on the Upper Columbia 119-135 CHAPTER V. -
Effects of Dams on Native Americans in the Columbia River Basin Elliott
Dammed Societies: Effects of Dams on Native Americans in the Columbia River Basin Elliott McGill Senior Capstone Project Faculty Advisors: Dr. Jamie Dolan, Dr. Jeremy Johnson, and Dr. David McCanna McGill 1 Abstract Since dam construction began in the New Deal Era, it has represented a dominance of humankind over nature. These massive structures have harnessed, collected, and distributed electricity from the rivers they hold back and allow humans to reap the benefits of that cycle. One of the areas where dams are particularly apparent is in the Columbia River Basin in the Pacific Northwest region of the United States. While the dams in this region certainly have allowed the area to develop and build by using the electricity collected by these dams, they have also had several negative effects on the tribal people in the region who once fished the mighty Columbia during its populous salmon runs and relied on the salmon for nutritional, economic, and cultural reasons. This project seeks to examine the costs of human advancement when it comes to dams, and will do so by studying three dams located in the Columbia River Basin: The Bonneville Dam, The Dalles Dam, and The Grand Coulee Dam. These dams will be studied using Black’s Theory of Law as a framework to examine the manner in which law was applied to each case. The research finds that although the dams certainly provide a useful resource to the people of the region, it has had negative effects on the Native American people who depended on the river. McGill 2 Introduction When President Franklin D.