Flooding the Grand Canyon: a Phony Issue
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Ellen Tibbetts
boatman’s quarterly review the journal of the Grand Canyon River Guide’s, Inc. • voulme 32 number 3 fall 2019 the journal of Grand Canyon River Guide’s, Prez Blurb • Farewells • Andy Hall • Guide Profile • The Journey • Stanton’s Cave Point Positive • Save the Dates • Glen Canyon Dam and the Colorado River Book Reviews • Eye of Odin • Cooler Research • Whale News boatman’s quarterly review Prez Blurb …is published more or less quarterly by and for GRAND CANYON RIVER GUIDES. REETINGS FROM SALMON IDAHO where I’m GRAND CANYON RIVER GUIDES finishing up my Middle Fork tour. It’s the is a nonprofit organization dedicated to Gtime of the season where we all feel pretty well worked and probably need a vacation before the “dog Protecting Grand Canyon days of August.” I had a guest say recently, “You guides Setting the highest standards for the river profession just have a paid vacation.” I just pointed out, “Yeah, Celebrating the unique spirit of the river community fourteen hours a day, every day.” Anyway, onward… Providing the best possible river experience By now the incident at National Canyon has flowed around the community, of a guest thinking he was left General Meetings are held each Spring and Fall. Our behind and making his way down-river and eventually Board of Directors Meetings are generally held the first losing his life by drowning. This incident points to the Wednesday of each month. All innocent bystanders are fact it is impossible to protect guests totally from their urged to attend. Call for details. own misguided actions, however well-meaning they STAFF may seem to that individual. -
The Little Colorado River Project: Is New Hydropower Development the Key to a Renewable Energy Future, Or the Vestige of a Failed Past?
COLORADO NATURAL RESOURCES, ENERGY & ENVIRONMENTAL LAW REVIEW The Little Colorado River Project: Is New Hydropower Development the Key to a Renewable Energy Future, or the Vestige oF a Failed Past? Liam Patton* Table of Contents INTRODUCTION ........................................................................................ 42 I. THE EVOLUTION OF HYDROPOWER ON THE COLORADO PLATEAU ..... 45 A. Hydropower and the Development of Pumped Storage .......... 45 B. History of Dam ConstruCtion on the Plateau ........................... 48 C. Shipping ResourCes Off the Plateau: Phoenix as an Example 50 D. Modern PoliCies for Dam and Hydropower ConstruCtion ...... 52 E. The Result of Renewed Federal Support for Dams ................. 53 II. HYDROPOWER AS AN ALLY IN THE SHIFT TO CLEAN POWER ............ 54 A. Coal Generation and the Harms of the “Big Buildup” ............ 54 B. DeCommissioning Coal and the Shift to Renewable Energy ... 55 C. The LCR ProjeCt and “Clean” Pumped Hydropower .............. 56 * J.D. Candidate, 2021, University oF Colorado Law School. This Note is adapted From a final paper written for the Advanced Natural Resources Law Seminar. Thank you to the Colorado Natural Resources, Energy & Environmental Law Review staFF For all their advice and assistance in preparing this Note For publication. An additional thanks to ProFessor KrakoFF For her teachings on the economic, environmental, and Indigenous histories of the Colorado Plateau and For her invaluable guidance throughout the writing process. I am grateFul to share my Note with the community and owe it all to my professors and classmates at Colorado Law. COLORADO NATURAL RESOURCES, ENERGY & ENVIRONMENTAL LAW REVIEW 42 Colo. Nat. Resources, Energy & Envtl. L. Rev. [Vol. 32:1 III. ENVIRONMENTAL IMPACTS OF PLATEAU HYDROPOWER ............... -
Theodore Roosevelt Reservoir 1995 Sedimentation Survey
THEODORE ROOSEVELT RESERVOIR 1995 SEDIMENTATION SURVEY 1.FOkTF1Ep02. RESOiJ U.S. Department of the Interior Bureau of Reclamation ERRATA Theodore Roosevelt Reservoir 1995 Sedimentation Survey Page 10, Table 1, item 9: This should read 2,100 feet rather than 2214. Page 12, Table 1, item 47,footnote 1: Modifications to Roosevelt Dam completed in 1995 raised the dam elevation and lowered the spillway sill elevation. The original dam elevation was 2142 and the spiliway elevation (top of radial gates) was 2136. Page 13. Table 2, ,foolnole 7: Computed sediment expressed as a percentage of total computed sediment (182,185 acre-feet). REPORT DOCUMENTATION PAGE FormApproved J 0MB No. 0704-0188 Pubhc reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the cotlection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Washington Headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suit 1204, Arlington VA 22202-4302, and to the Office of Management and Budget, Paper-work Reduction Report (0704-0188), Washington DC 20503. 1. AGENCY USE ONLY (Leave Blank) 2. REPORT DATE 3. REPORT TYPE AND DATES COVERED May 1996 Final 4. TITLE AND SUBTiTLE 5. FUNDING NUMBERS Theodore Roosevelt Reservoir 1995 Sedimentation Survey PR 6. AUTHOR(S) Joe Lyons and Lori Lest 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION Bureau of Reclamation REPORT NUMBER Technical Service Center Denver CO 80225 9. -
Quaternary Geology and Geomorphology of the Nankoweap Rapids Area, Marble Canyon, Arizona
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2608 U.S. GEOLOGICAL SURVEY QUATERNARY GEOLOGY AND GEOMORPHOLOGY OF THE NANKOWEAP RAPIDS AREA, MARBLE CANYON, ARIZONA By Richard Hereford, Kelly J. Burke, and Kathryn S. Thompson INTRODUCTION sion elsewhere in Grand Canyon {Hereford and oth ers, 1993; Fairley and others, 1994, p. 147-150). The Nankoweap Rapids area along the Colorado River {fig. 1) is near River Mile 52 {that is 52 mi or 83 km downstream of Lees Ferry, Arizona) in Grand Canyon National Park {west bank) and the Navajo METHODS Indian Reservation {east bank). Geologic mapping and [See map sheet for Description of Map Units] related field investigations of the late Quaternary geo morphology of the Colorado River and tributary A variety of methods were used to date the de streams were undertaken to provide information about posits. Radiocarbon dates were obtained from char the age, distribution, and origin of surficial deposits. coal and wood recovered from several of the mapped These deposits, particularly sandy alluvium and closely units (table 1). Several of these dates are not defini related debris-flow sediment, are the substrate for tive as they are affected by extensive animal bur riparian vegetation, which in turn supports the eco rowing in the alluvial deposits that redistributed burnt system of the Colorado River (Carothers and Brown, roots of mesquite trees, giving anomalous dates. The 1991, p. 111-167). late Pleistocene breccia (units be and bf) and re Closure of Glen Canyon Dam {109 km or 68 lated terraces were dated by Machette and Rosholt mi upstream of the study area) in 1963 and subse (1989; 1991) using the uranium-trend method. -
Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California
Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California By Paul Stone, Calvin H. Stevens, Paul Belasky, Isabel P. Montañez, Lauren G. Martin, Bruce R. Wardlaw, Charles A. Sandberg, Elmira Wan, Holly A. Olson, and Susan S. Priest Pamphlet to accompany Scientific Investigations Map 3298 2014 U.S. Department of the Interior U.S. Geological Survey Cover View of Marble Canyon area, California, showing dark rocks of Mississippian Indian Springs Formation and Pennsylvanian Bird Spring Formation overlying light rocks of Mississippian Santa Rosa Hills Limestone in middle distance. View is southeast toward Emigrant Wash and Tucki Mountain in distance. U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2014 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Stone, P., Stevens, C.H., Belasky, P., Montanez, I.P., Martin, L.G., Wardlaw, B.R., Sandberg, C.A., Wan, E., Olson, H.A., and Priest, S.S., 2014, Geologic map and upper Paleozoic stratigraphy of the Marble Canyon area, Cottonwood Canyon quadrangle, Death Valley National Park, Inyo County, California: U.S. Geological Survey Scientific Investigations Map 3298, scale 1:24,000, 59 p., http://dx.doi.org/10.3133/sim3298. -
3.6 Riverflow Issues
AFFECTED ENVIRONMENT & ENVIRONMENTAL CONSEQUENCES CHAPTER 3 3.6 RIVERFLOW ISSUES 3.6.1 INTRODUCTION This section considers the potential effects of interim surplus criteria on three types of releases from Glen Canyon Dam and Hoover Dam. The Glen Canyon Dam releases analyzed are those needed for restoration of beaches and habitat along the Colorado River between the Glen Canyon Dam and Lake Mead, and for a yet to be defined program of low steady summer flows to be provided for the study and recovery of endangered Colorado River fish, in years when releases from the dam are near the minimum. The Hoover Dam releases analyzed are the frequency of flood releases from the dam and the effect of flood flows along the river downstream of Hoover Dam. 3.6.2 BEACH/HABITAT-BUILDING FLOWS The construction and operation of Glen Canyon Dam has caused two major changes related to sediment resources downstream in Glen Canyon and Grand Canyon. The first is reduced sediment supply. Because the dam traps virtually all of the incoming sediment from the Upper Basin in Lake Powell, the Colorado River is now released from the dam as clear water. The second major change is the reduction in the high water zone from the level of pre-dam annual floods to the level of powerplant releases. Thus, the height of annual sediment deposition and erosion has been reduced. During the investigations leading to the preparation of the Operation of Glen Canyon Dam Final EIS (Reclamation, 1995b), the relationships between releases from the dam and downstream sedimentation processes were brought sharply into focus, and flow patterns designed to conserve sediment for building beaches and habitat (i.e., beach/habitat-building flow, or BHBF releases) were identified. -
The Central Arizona Project
University of Colorado Law School Colorado Law Scholarly Commons New Sources of Water for Energy Development and Growth: Interbasin Transfers: A Short 1982 Course (Summer Conference, June 7-10) 6-9-1982 The Central Arizona Project Jon Kyl Follow this and additional works at: https://scholar.law.colorado.edu/new-sources-of-water-for-energy- development-and-growth-interbasin-transfers Part of the Agriculture Law Commons, Animal Law Commons, Aquaculture and Fisheries Commons, Biodiversity Commons, Contracts Commons, Energy and Utilities Law Commons, Environmental Law Commons, Hydrology Commons, Law and Economics Commons, Legal History Commons, Legislation Commons, Natural Resource Economics Commons, Natural Resources and Conservation Commons, Natural Resources Law Commons, Natural Resources Management and Policy Commons, Oil, Gas, and Mineral Law Commons, Property Law and Real Estate Commons, State and Local Government Law Commons, Transportation Law Commons, Water Law Commons, and the Water Resource Management Commons Citation Information Kyl, Jon, "The Central Arizona Project" (1982). New Sources of Water for Energy Development and Growth: Interbasin Transfers: A Short Course (Summer Conference, June 7-10). https://scholar.law.colorado.edu/new-sources-of-water-for-energy-development-and-growth-interbasin- transfers/21 Reproduced with permission of the Getches-Wilkinson Center for Natural Resources, Energy, and the Environment (formerly the Natural Resources Law Center) at the University of Colorado Law School. Jon Kyl, The Central Arizona Project, in NEW SOURCES OF WATER FOR ENERGY DEVELOPMENT AND GROWTH: INTERBASIN TRANSFERS (Natural Res. Law Ctr., Univ. of Colo. Sch. of Law 1982). Reproduced with permission of the Getches-Wilkinson Center for Natural Resources, Energy, and the Environment (formerly the Natural Resources Law Center) at the University of Colorado Law School. -
William Martin Little a Thesis Submitted to the Faculty of the In
An engineering and economic feasibility study for diversion of Central Arizona Project waters from alternate sites. Item Type Thesis-Reproduction (electronic); text Authors Little, William Martin,1944- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 26/09/2021 17:22:05 Link to Item http://hdl.handle.net/10150/191503 AN ENGINEERING AND ECONOMIC FEASIBILITY STUDY FOR DIVERSION OF CENTRAL ARIZONA PROJECT WATERS FROM ALTERNATE SITES by William Martin Little A Thesis Submitted to the Faculty of the COMMITTEE ON HYDROLOGY AND WATER RESOURCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1968 STATEMENT BY AUTHOR This thesis has been submitted In partial fulfillment of require- ments for an advanced degree at The University of Arizona and is deposited in the Univeristy Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or In part may be granted by the head of the major department or the Dean of the Graduate College when in his judg- ment the proposed use of the material is in the interests of scholarship. In all other instances, however, permission must be obtained from the author. -
Effects of the Glen Canyon Dam on Colorado River Temperature Dynamics
Effects of the Glen Canyon Dam on Colorado River Temperature Dynamics GEL 230 – Ecogeomorphology University of California, Davis Derek Roberts March 2nd, 2016 Abstract: At the upstream end of the Grand Canyon, the Glen Canyon Dam has changed the Colorado River from a run-of-the-river flow to a deep, summer-stratified reservoir. This change in flow regime significantly alters the temperature regime of the Colorado River. Seasonal temperature variation, once ranging from near to almost , is now limited to 7 . The lack of warm summer temperatures has prevented spawning of endangered 0℃ 30℃ humpback chub in the Colorado River. Implementation of a temperature control device, to − 14℃ allow for warmer summer releases to mitigate negative temperature effects on endangered fish, was considered by the federal government. Ultimately, this proposal was put on indefinite hold by the Bureau of Reclamation and U.S. Fish and Wildlife Service due to concerns of cost and unintended ecological consequences. The low-variability of the current dam-induced Colorado River temperature regime will continue into the foreseeable future. Agencies are reviewing humpback chub conservation efforts outside of temperature control. Keywords: Colorado River, Grand Canyon, Glen Canyon Dam, thermal dynamics 1.0 Introduction Temperature in natural water bodies is a primary driver of both ecological and physical processes. Freshwater plant and animal metabolisms are heavily affected by temperature (Coulter 2014). Furthermore, the thermal structure of a water body has significant impacts on the physical processes that drive ecosystem function (Hodges et al 2000); fluid dynamics drive transport of nutrients, oxygen, and heat. Human action, often the introduction of dams or industrial cooling systems, can alter the natural thermal regimes of rivers and lakes leading to reverberating impacts throughout associated ecosystems. -
Hydroelectric Power -- What Is It? It=S a Form of Energy … a Renewable Resource
INTRODUCTION Hydroelectric Power -- what is it? It=s a form of energy … a renewable resource. Hydropower provides about 96 percent of the renewable energy in the United States. Other renewable resources include geothermal, wave power, tidal power, wind power, and solar power. Hydroelectric powerplants do not use up resources to create electricity nor do they pollute the air, land, or water, as other powerplants may. Hydroelectric power has played an important part in the development of this Nation's electric power industry. Both small and large hydroelectric power developments were instrumental in the early expansion of the electric power industry. Hydroelectric power comes from flowing water … winter and spring runoff from mountain streams and clear lakes. Water, when it is falling by the force of gravity, can be used to turn turbines and generators that produce electricity. Hydroelectric power is important to our Nation. Growing populations and modern technologies require vast amounts of electricity for creating, building, and expanding. In the 1920's, hydroelectric plants supplied as much as 40 percent of the electric energy produced. Although the amount of energy produced by this means has steadily increased, the amount produced by other types of powerplants has increased at a faster rate and hydroelectric power presently supplies about 10 percent of the electrical generating capacity of the United States. Hydropower is an essential contributor in the national power grid because of its ability to respond quickly to rapidly varying loads or system disturbances, which base load plants with steam systems powered by combustion or nuclear processes cannot accommodate. Reclamation=s 58 powerplants throughout the Western United States produce an average of 42 billion kWh (kilowatt-hours) per year, enough to meet the residential needs of more than 14 million people. -
Executive Summary U.S
Glen Canyon Dam Long-Term Experimental and Management Plan Environmental Impact Statement PUBLIC DRAFT Executive Summary U.S. Department of the Interior Bureau of Reclamation, Upper Colorado Region National Park Service, Intermountain Region December 2015 Cover photo credits: Title bar: Grand Canyon National Park Grand Canyon: Grand Canyon National Park Glen Canyon Dam: T.R. Reeve High-flow experimental release: T.R. Reeve Fisherman: T. Gunn Humpback chub: Arizona Game and Fish Department Rafters: Grand Canyon National Park Glen Canyon Dam Long-Term Experimental and Management Plan December 2015 Draft Environmental Impact Statement 1 CONTENTS 2 3 4 ACRONYMS AND ABBREVIATIONS .................................................................................. vii 5 6 ES.1 Introduction ............................................................................................................ 1 7 ES.2 Proposed Federal Action ........................................................................................ 2 8 ES.2.1 Purpose of and Need for Action .............................................................. 2 9 ES.2.2 Objectives and Resource Goals of the LTEMP ....................................... 3 10 ES.3 Scope of the DEIS .................................................................................................. 6 11 ES.3.1 Affected Region and Resources .............................................................. 6 12 ES.3.2 Impact Topics Selected for Detailed Analysis ........................................ 6 13 ES.4 -
Management of the Colorado River: Water Allocations, Drought, and the Federal Role
Management of the Colorado River: Water Allocations, Drought, and the Federal Role Updated March 21, 2019 Congressional Research Service https://crsreports.congress.gov R45546 SUMMARY R45546 Management of the Colorado River: Water March 21, 2019 Allocation, Drought, and the Federal Role Charles V. Stern The Colorado River Basin covers more than 246,000 square miles in seven U.S. states Specialist in Natural (Wyoming, Colorado, Utah, New Mexico, Arizona, Nevada, and California) and Resources Policy Mexico. Pursuant to federal law, the Bureau of Reclamation (part of the Department of the Interior) manages much of the basin’s water supplies. Colorado River water is used Pervaze A. Sheikh primarily for agricultural irrigation and municipal and industrial (M&I) uses, but it also Specialist in Natural is important for power production, fish and wildlife, and recreational uses. Resources Policy In recent years, consumptive uses of Colorado River water have exceeded natural flows. This causes an imbalance in the basin’s available supplies and competing demands. A drought in the basin dating to 2000 has raised the prospect of water delivery curtailments and decreased hydropower production, among other things. In the future, observers expect that increasing demand for supplies, coupled with the effects of climate change, will further increase the strain on the basin’s limited water supplies. River Management The Law of the River is the commonly used shorthand for the multiple laws, court decisions, and other documents governing Colorado River operations. The foundational document of the Law of the River is the Colorado River Compact of 1922. Pursuant to the compact, the basin states established a framework to apportion the water supplies between the Upper and Lower Basins of the Colorado River, with the dividing line between the two basins at Lee Ferry, AZ (near the Utah border).