The Columbia Basin Project
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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. -
Washington Division of Geology and Earth Resources Open File Report
RECONNAISSANCE SURFICIAL GEOLOGIC MAPPING OF THE LATE CENOZOIC SEDIMENTS OF THE COLUMBIA BASIN, WASHINGTON by James G. Rigby and Kurt Othberg with contributions from Newell Campbell Larry Hanson Eugene Kiver Dale Stradling Gary Webster Open File Report 79-3 September 1979 State of Washington Department of Natural Resources Division of Geology and Earth Resources Olympia, Washington CONTENTS Introduction Objectives Study Area Regional Setting 1 Mapping Procedure 4 Sample Collection 8 Description of Map Units 8 Pre-Miocene Rocks 8 Columbia River Basalt, Yakima Basalt Subgroup 9 Ellensburg Formation 9 Gravels of the Ancestral Columbia River 13 Ringold Formation 15 Thorp Gravel 17 Gravel of Terrace Remnants 19 Tieton Andesite 23 Palouse Formation and Other Loess Deposits 23 Glacial Deposits 25 Catastrophic Flood Deposits 28 Background and previous work 30 Description and interpretation of flood deposits 35 Distinctive geomorphic features 38 Terraces and other features of undetermined origin 40 Post-Pleistocene Deposits 43 Landslide Deposits 44 Alluvium 45 Alluvial Fan Deposits 45 Older Alluvial Fan Deposits 45 Colluvium 46 Sand Dunes 46 Mirna Mounds and Other Periglacial(?) Patterned Ground 47 Structural Geology 48 Southwest Quadrant 48 Toppenish Ridge 49 Ah tanum Ridge 52 Horse Heaven Hills 52 East Selah Fault 53 Northern Saddle Mountains and Smyrna Bench 54 Selah Butte Area 57 Miscellaneous Areas 58 Northwest Quadrant 58 Kittitas Valley 58 Beebe Terrace Disturbance 59 Winesap Lineament 60 Northeast Quadrant 60 Southeast Quadrant 61 Recommendations 62 Stratigraphy 62 Structure 63 Summary 64 References Cited 66 Appendix A - Tephrochronology and identification of collected datable materials 82 Appendix B - Description of field mapping units 88 Northeast Quadrant 89 Northwest Quadrant 90 Southwest Quadrant 91 Southeast Quadrant 92 ii ILLUSTRATIONS Figure 1. -
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 -
Washington's Channeled Scabland
t\D l'llrl,. \·· ~. r~rn1 ,uR\fEY Ut,l\n . .. ,Y:ltate" tit1Washington ALBEIT D. ROSEWNI, Governor Department of Conservation EARL COE, Dlnctor DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, Supervisor Bulletin No. 45 WASHINGTON'S CHANNELED SCABLAND By J HARLEN BRETZ 9TAT• PIUHTIHO PLANT ~ OLYMPIA, WASH., 1"511 State of Washington ALBERT D. ROSELLINI, Governor Department of Conservation EARL COE, Director DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, Supervisor Bulletin No. 45 WASHINGTON'S CHANNELED SCABLAND By .T HARLEN BRETZ l•or sate by Department or Conservation, Olympia, Washington. Price, 50 cents. FOREWORD Most travelers who have driven through eastern Washington have seen a geologic and scenic feature that is unique-nothing like it is to be found anywhere else in the world. This is the Channeled Scab land, a gigantic series of deeply cut channels in the erosion-resistant Columbia River basalt, the rock that covers most of the east-central and southeastern part of the state. Grand Coulee, with its spectac ular Dry Falls, is one of the most widely known features of this ex tensive set of dry channels. Many thousands of travelers must have wondered how this Chan neled Scabland came into being, and many geologists also have speculated as to its origin. Several geologists have published papers outlining their theories of the scabland's origin, but the geologist who has made the most thorough study of the problem and has ex amined the whole area and all the evidence having a bearing on the problem is Dr. J Harlen Bretz. Dr. -
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. -
Top 26 Trails in Grant County 2020
and 12 Watchable Wildlife Units For more information, please contact: Grant County Tourism Commission P.O. Box 37, Ephrata, WA 98823 509.765.7888 • 800.992.6234 In Grant County, Washington TourGrantCounty.com TOP TRAILS Grant County has some of the most scenic and pristine vistas, hiking trails and outdoor 26 recreational opportunities in Washington State. and 12 Watchable Wildlife Units Grant County is known for its varied landscapes on a high desert plateau with coulees, lakes, in Grant County Washington reservoirs, sand dunes, canals, rivers, creeks, and other waterways. These diverse ecosystems Grant County Tourism Commission For Additional copies please contact: support a remarkable variety of fish and PO Box 37 Jerry T. Gingrich wildlife species that contribute to the economic, Ephrata, Washington 98837 Grant County Tourism Commission recreational and cultural life of the County. www.tourgrantcounty.com Grant County Courthouse PO Box 37 Ephrata, WA 98837 No part of this book may be reproduced in (509) 754-2011, Ext. 2931 any form, or by any electronic, mechanical, or other means, without permission in For more information on writing from the Grant County Tourism Grant County accommodations Commission. www.tourgrantcounty.com © 2019, Grant County Tourism Commission Second printing, 10m Trails copy and photographs Book, map and cover design by: provided by: Denise Adam Graphic Design Cameron Smith, Lisa Laughlin, J. Kemble, Veradale, WA 99037 Shawn Cardwell, Mark Amara, (509) 891-0873 Emry Dinman, Harley Price, [email protected] Sebastian Moraga and Madison White Printed by: Rewriting and editing by: Mark Amara Pressworks 2717 N. Perry Street Watchable Wildlife copy and Spokane, Washington 99207 photographs provided by: (509) 462-7627 Washington Department of [email protected] Fish and Wildlife Photograph by Lisa Laughlin CONTENTS CONTENTS Grant County Trails and Hiking Grant County Watchable Wildlife Viewing Upper Grand Coulee Area 1. -
One Thread That Weaves Throughout Our 125-Year History Is That of Innovation
ON THE COVER Summer storms hitting 10 days apart caused extensive damage throughout Avista’s Washington/Idaho service area in 2014, knocking out power to nearly 100,000 customers. Crews and office staff worked around the clock, restoring power quickly and safely, keeping customers informed through traditional and social media channels. 1411 EAST MISSION AVENUE | SPOKANE, WASHINGTON 99202 | 509.489.0500 | AVISTACORP.COM One thread that weaves throughout our 125-year history is that of innovation. A LANDMARK Dear Fellow Shareholder: It’s been a landmark year at Avista for many reasons — we celebrated our milestone 125th anniversary; we sold Ecova, our home-grown energy and sustainability management business; we acquired Alaska Energy and Resources Company (AERC) and its primary subsidiary Alaska Electric Light and Power Company (AEL&P) in Juneau, Alaska; and we continued to make significant progress in achieving our goals of investing in our infrastructure, upgrading our technology and preparing our utility to effectively and efficiently implement 21st century energy delivery. For the first time in a generation, we can consider ourselves close to being a “pure play” utility. None of this would have been possible without our cadre operations were $1.93 per diluted share, with net income of dedicated and knowledgeable employees. There’s a from continuing operations attributable to Avista Corp. confidence that comes with competence, a steadiness that shareholders of $119.8 million for 2014. builds on itself and makes things happen. It’s not flashy, but Our balance sheet and credit ratings remain healthy. the effects speak for themselves. Avista’s employees embody At year-end, Avista Corp. -
Columbia River Treaty History and 2014/2024 Review
U.S. Army Corps of Engineers • Bonneville Power Administration Columbia River Treaty History and 2014/2024 Review 1 he Columbia River Treaty History of the Treaty T between the United States and The Columbia River, the fourth largest river on the continent as measured by average annual fl ow, Canada has served as a model of generates more power than any other river in North America. While its headwaters originate in British international cooperation since 1964, Columbia, only about 15 percent of the 259,500 square miles of the Columbia River Basin is actually bringing signifi cant fl ood control and located in Canada. Yet the Canadian waters account for about 38 percent of the average annual volume, power generation benefi ts to both and up to 50 percent of the peak fl ood waters, that fl ow by The Dalles Dam on the Columbia River countries. Either Canada or the United between Oregon and Washington. In the 1940s, offi cials from the United States and States can terminate most of the Canada began a long process to seek a joint solution to the fl ooding caused by the unregulated Columbia provisions of the Treaty any time on or River and to the postwar demand for greater energy resources. That effort culminated in the Columbia River after Sept.16, 2024, with a minimum Treaty, an international agreement between Canada and the United States for the cooperative development 10 years’ written advance notice. The of water resources regulation in the upper Columbia River U.S. Army Corps of Engineers and the Basin. -
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. -
Lake Roosevelt National Recreation Area Foundation Document Overview
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Lake Roosevelt National Recreation Area Washington Contact Information For more information about the Lake Roosevelt National Recreation Area Foundation Document, contact: [email protected] or (509) 754-7893 or write to: Superintendent, Lake Roosevelt National Recreation Area, 1008 Crest Drive, Coulee Dam, WA 99116 Purpose Significance Significance statements express why Lake Roosevelt National Recreation Area resources and values are important enough to merit national park unit designation. Statements of significance describe why an area is important within a global, national, regional, and systemwide context. These statements are linked to the purpose of the park unit, and are supported by data, research, and consensus. Significance statements describe the distinctive nature of the park and inform management decisions, focusing efforts on preserving and protecting the most important resources and values of the park unit. • Lake Roosevelt National Recreation Area, which includes some of the most publicly accessible shoreline in the Pacific Northwest, offers a wide range of visitor experiences and appropriate recreational opportunities. • Lake Roosevelt National Recreation Area is located within two distinct geologic provinces—the Okanogan Highlands and the Columbia Plateau—and is an outstanding and easily accessible landscape sculpted by a rare combination of sequential geologic processes: volcanism, collision of tectonic plates, continental glaciation, and cataclysmic ice age floods. • Lake Roosevelt National Recreation Area is located at a historic convergence point for numerous Pacific Northwest tribes and contains a central gathering place in their traditional homeland, including the site of the second-largest The purpose of LAKE ROOSEVELT NATIONAL prehistoric and historic Native American fishery on the RECREATION AREA is to protect, conserve, Columbia River. -
Narrow Gauge Politics: Railway Labor, Parties, Race, and the State
Narrow Gauge Politics: Railway Labor, Parties, Race, and the State Daniel Schlozman Assistant Professor Department of Political Science Johns Hopkins University 3400 N. Charles Street Baltimore, MD 21218 (410) 516-5882 [email protected] 1 Workers in the American railroad and air transport industries still belong to unions.1 Fully 65.2 percent of workers in the railroad industry held union membership in 2014; in air transport, the figure was 40.5 percent. Union density is higher among railroad workers than among postal workers or than among public workers in every state but two. A distinct legal regime – a “state within a state”2 – developed to protect white railroaders, and withstood the assaults that have devastated American labor. While workers in the rest of the private sector organize under the National Labor Relations Act, the Railway Labor Act governs labor relations on the railroads and the airlines. Its consensual subgovernment among railroads, white unions, and the state has proven remarkably stable. But that labor-relations regime achieved stability precisely by avoiding large-scale ideological conflict. Rather, at the roots of stability lie political quiescence and racial intransigence in the critical New Deal and Fair Deal era. This paper situates the case of railway labor, comparing rail unions both across time and with other American labor regimes. At the end of the nineteenth century, the state repressed worker militancy (including from railroad workers) in the North and, by the extreme means of Jim Crow, in the