The Columbia Basin Grand Coulee 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 Geology
JULY 1978 VOLUME 6 - NUMBER 3 A PLBLICATION OF THE DEPARTMENT OF NATURAL RESOURCES WASHINGTON GEOWGIC NEWSLETTER BERT L.COLE COMMISSIONER OF PUBLIC LANDS RALPH A BESWICK, Supervisor VAUGHN E. LIVINGSTON,JR.,State Geologist DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGY AND EARTH RESOURCES DEPARTMENT Of NATURAL RESOURCES, DIVISION OF GEOLOGY AND EARTH RESOURCES, OLYMPIA, WASHINGTON, 98504 LOCATION MAP : DIVISION OF GEOLOGY AND EARTH RESOURCES DEPT. SOCIAL AND HEALTH SERVICES t ~ i~L f ...J ~ i ,...... N g a: ~ ~OGY ANO EARTH <t tt RESOURCES D u -, t STATE CAPITOL ... TACOMA S~TILE- IDEPT. HIGHWAYS CITY CENTER FREEWAY EXIT PORTLA~ STATE CAPITOL EXIT Vaughn E. (Ted) Livingston, Jr., Supervisor Geologic Staff J. Eric Schuster, Assistant Supervisor Minerals and Energy Geologists Land Use Geologists Carl McFarland James G. Rigby Allen J. Fiksdal Keith L. Stoffel Clint Milne Glennda B. Tucker Kurt L. 0th berg Gerald W. Thorsen Wayne S. Moen Ellis R. Vonheeder Pamela Palmer Weldon W. Rau Charles W. Walker Regulations and Operations Surface Mined Land Reclamation and Oil and Gos Conservation Act Donald M. Ford, Assistant Supervisor Publications: Library: Laboratory: Secretaries: Loura Broy Connie Manson Arnold W. Bowman Patricia Ames Keith Ikerd Cherie Dunwoody Wonda Walker Kim Summers Pamela Whitlock Mailing address: Deportment of Natural Resources Division of Geology and Earth Resou rces Olympia, WA 98504 (206) 753-6183 ORIGIN OF THE GRAND COULEE AND DRY FALLS by Ted Livingston Washington State hos many interesting geo original terrain until in the Grand Coulee area it was logic features. Among the more outstanding dre the completely buried. During the course of these erup Grand Coulee and Dry Falls . -
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. -
Stormwater Ordinance Leaf & Grass Blowing Into Storm Drains Lafayette
Good & Bad • Stormwater GOOD: Only Rain in the Drain! The water drains to Ordinance the river. Leaf & Grass Blowing into Storm Drains Lafayette BAD: Grass and leaves blown into a storm drain interfere with drainage. Parish Dirt is also being allowed in our waterways. Potential Illicit Discharge Sources: Environmental Quality • Sanitary sewer wastewater. Regulatory Compliance 1515 E. University Ave. • Effluent from septic tanks. Lafayette, LA 70501 Phone: 337-291-8529 • Laundry wastewater. Fax: 337-291-5620 • Improper disposal of auto and household toxics. www.lafayettela.gov/stormwater • Industrial byproduct discharge. Illicit Discharge (including leaf blowing) Stormwater Ordinance Stormwater Runoff Illicit Discharge Please be advised that the Environmental Grass clippings and leaves blown or swept is defined by the EPA as: Quality Division of Lafayette Consolidated into storm drains or into the street harms Any discharge into a municipal separate Government has recently adopted an waterways and our river. Storm drains flow storm sewer that is not composed entirely of into coulees and into the Vermilion River. rainwater and is not authorized by permit. Illicit Discharge (including leaf blowing) Grass clippings in the river rob valuable Stormwater Ordinance oxygen from our Vermilion River. Chapter 34. ENVIRONMENT When leaf and grass clippings enter the Signs of Potential Illicit Discharge Article 5. STORMWATER storm drain, flooding can occur. Only rain must enter the storm drain. When anything • Heavy flow during dry weather. Division 4 Sec. 34-452 but rain goes down the storm drain, it can • Strong odor. It is now in effect and being enforced. You become a drainage problem. may access this ordinance online at Grass clippings left on the ground improve the • Colorful or discolored liquid. -
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. -
Columbia Basin Project Coordinated Water Conservation Plan ‐ Final Draft
COLUMBIA BASIN PROJECT COORDINATED WATER CONSERVATION PLAN ‐ FINAL DRAFT Prepared for East Columbia Basin Irrigation District Quincy-Columbia Basin Irrigation District South Columbia Basin Irrigation District Washington State Department of Ecology Prepared by Anchor QEA, LLC 811 Kirkland Avenue, Suite 200 Kirkland, WA 98033 March 2010 Ecology Publication Number: 10-12-010 COLUMBIA BASIN PROJECT COORDINATED WATER CONSERVATION PLAN – FINAL DRAFT Prepared for East Columbia Basin Irrigation District Quincy-Columbia Basin Irrigation District South Columbia Basin Irrigation District Washington State Department of Ecology Prepared by Anchor QEA, LLC 811 Kirkland Avenue, Suite 200 Kirkland, WA 98033 March 2010 TABLE OF CONTENTS 1 INTRODUCTION ..................................................................................................................1 1.1 Project Goals.....................................................................................................................1 1.2 Columbia Basin Project....................................................................................................1 1.3 Past Water Conservation Studies and Actions ...............................................................2 2 METHODOLOGY..................................................................................................................4 2.1 Identifying Water Conservation Projects.......................................................................4 2.2 Estimating Water Savings................................................................................................4 -
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. -
Tolna Coulee Control Structure Nears Completion
The Tolna Coulee Control Structure Nears Completion FROM THE NORTH DAKOTA STATE WATER COMMISSION The Tolna Coulee Control Strucutre on June 6. Inset shows water elevation measurement on The Tolna Coulee Control Structure prior to completion. structure at the same elvevation as the lakes. In the last part of May, the U.S. more likely. As a result, the Corps Construction of the structure Army Corps of Engineers (Corps), began the design and construction began in the fall of 2011, and was and their contractor, announced of a control structure on Tolna aided by the mild winter. Less than Key Points of the Tolna Coulee Control Structure they had substantially completed Coulee, with input from the Water a year later, the structure is now construction on the Tolna Coulee Commission. ready for operation. • The intent of the Tolna Control Structure is that • Once water begins to flow over the divide, stop control structure. the existing topography, not the structure, will logs in the middle of the structure will be placed The structure is designed Initially, the Corps will control discharge, with the removal of stop logs at an elevation of 1,457’. as the divide erodes. This will allow the lake Tolna Coulee is the natural outlet to permit erosion of the divide, manage operation of the Tolna to lower as it would have without the structure - from Devils Lake and Stump Lake. allowing the lake to lower, as it Coulee Control Structure, which while limiting releases to no more than 3,000 cfs. • If erosion occurs, the stop logs will be removed to As recently as 2011, the lake was would have without the project, will be guided by the “Standing the new lake elevation, with flows not to exceed less than four feet from overflowing while limiting releases to no Instructions To The Project 3,000 cfs. -
Dry Falls Visitor Center Due to the Fact That Many Travelers Saw These Unusual Landforms in the Landscape As They Drove the Coulee Corridor
Interactive Design Approach IMMERSIVE Theater Topo Model The design approach for the exhibits is closely integrated with the Seating architecture. The layering of massive, linear building walls pro- for 50-60 EXHIBIT vides a direction for the design and layout of exhibit components. Gallery Real ‘Today’ erratic OUTDOOR Terrace Building walls are cut open at strategic points to accommodate WITH EXhibits specific exhibits and to allow for circulation. Smaller, wall-panel exhibits are used for supports and dividers. Equipment ‘Volcanic ‘Ice Age Floods’ Room Period’ Approaching the center, visitors are forced to walk around a mas- sive erratic – these huge boulders are seemingly deposited directly Gallery Animal Modelled erratic Lava flow overhead Freestanding time line animal cutouts on the path to the front door. The displaced rock serves as a strong Welcome in floor icon of the violent events that occurred during the Ice Age Floods. Through the Visitor Center’s front doors, visitors are startled to see another massive erratic precariously wedged overhead between W M Retail / cafe the two parallel building walls. Just out of reach it makes an un- usual photo opportunity for visitors who puzzle over how the rock terrace stays in place. From an interpretive standpoint, it is important to Outdoor Classroom realize no actual erratics are present in the Sun Lakes-Dry Falls with Amphitheater State Park landscape. During the floods, water was moving too quickly for erratics to be deposited at Dry Falls - they were car- ried downstream and deposited in the Quincy and Pasco basins many miles away. However, the results of the visioning workshop determined that erratics are an important and exciting flood fea- ture to display at the Dry Falls Visitor Center due to the fact that many travelers saw these unusual landforms in the landscape as they drove the Coulee Corridor. -
Table of Contents
SECTION 32 – Table of Contents 32 Upper Columbia Subbasin Assessment – Terrestrial...................................... 2 32.1 Focal Habitats: Current Distribution, Limiting Factors, and Condition ............................2 32.2 Wildlife of the Upper Columbia Subbasin.......................................................................13 32.3 Summary of Terrestrial Resource Limiting Factors ........................................................19 32.4 Interpretation and Synthesis.............................................................................................21 32-1 32 Upper Columbia Subbasin Assessment – Terrestrial 32.1 Focal Habitats: Current Distribution, Limiting Factors, and Condition Vegetation in the Upper Columbia Subbasin is dominated by interior mixed conifer forest, ponderosa pine forests, eastside interior grasslands, and shrub-steppe habitats. Montane mixed conifer forest, upland aspen forest, and lodgepole pine forests are present in the high elevations along with montane coniferous wetlands. Timber management is an important land use in the Subbasin on Tribal, state, federal, and private timberlands. Agriculture and grazing are other dominant land uses, particularly within the Colville River valley, on the plateaus above Lake Roosevelt, and in the extreme southern portion of the Subbasin. The largest urban areas in the Subbasin boundary include Chewelah, Colville, Kettle Falls, Davenport, and Grand Coulee. Figure 29.4 (Section 29) shows the current distribution of wildlife-habitat types in the Upper -
Irrigation and Streamflow Depletion in Columbia River Basin Above the Dalles, Oregon
Irrigation and Streamflow Depletion in Columbia River Basin above The Dalles, Oregon Bv W. D. SIMONS GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1220 An evaluation of the consumptive use of water based on the amount of irrigation UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1953 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 50 cents (paper cover) CONTENTS Page Abstract................................................................................................................................. 1 Introduction........................................................................................................................... 2 Purpose and scope....................................................................................................... 2 Acknowledgments......................................................................................................... 3 Irrigation in the basin......................................................................................................... 3 Historical summary...................................................................................................... 3 Legislation................................................................................................................... 6 Records and sources for data..................................................................................... 8 Stream