Appendix F – Aquatic Resources
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Relation of Sediment Load and Flood-Plain Formation to Climatic Variability, Paria River Drainage Basin, Utah and Arizona
Relation of sediment load and flood-plain formation to climatic variability, Paria River drainage basin, Utah and Arizona JULIA B. GRAF U.S. Geological Survey, Water Resources Division, 375 S. Euclid, Tucson, Arizona 85719 ROBERT H. WEBB U.S. Geological Survey, 1675 W. Anklam Road, Tucson, Arizona 85745 RICHARD HEREFORD U.S. Geological Survey, Geologic Division, 2255 North Gemini Drive, Flagstaff, Arizona 86001 ABSTRACT sediment load for a given discharge declined fill that rises 1-5 m above the modern channel abruptly in the early 1940s in the Colorado bed. Flood-plain deposits are present in all Suspended-sediment load, flow volume, River at Grand Canyon (Daines, 1949; Howard, major tributaries of the Paria River. The area of and flood characteristics of the Paria River 1960; Thomas and others, 1960; Hereford, flood plains is slightly greater than 20 km2, and were analyzed to determine their relation to 1987a). The decline in suspended-sediment sediment volume is estimated to be about 40 climate and flood-plain alluviation between loads has been attributed to improved land use million m3 (Hereford, 1987c). Typically, flood 1923 and 1986. Flood-plain alluviation began and conservation measures initiated in the 1930s plains are not present in first-order drainage ba- about 1940 at a time of decreasing magnitude (Hadley, 1977). A change in sediment-sampler sins but are present in basins of second and and frequency of floods in winter, summer, type and in methods of analysis have been higher order where the stream channel is uncon- and fall. No floods with stages high enough to discounted as causes for the observed decrease fined and crosses nonresistant bedrock forma- inundate the flood plain have occurred since (Daines, 1949; Thomas and others, 1960). -
West Colorado River Plan
Section 9 - West Colorado River Basin Water Planning and Development 9.1 Introduction 9-1 9.2 Background 9-1 9.3 Water Resources Problems 9-7 9.4 Water Resources Demands and Needs 9-7 9.5 Water Development and Management Alternatives 9-13 9.6 Projected Water Depletions 9-18 9.7 Policy Issues and Recommendations 9-19 Figures 9-1 Price-San Rafael Salinity Control Project Map 9-6 9-2 Wilderness Lands 9-11 9-3 Potential Reservoir Sites 9-16 9-4 Gunnison Butte Mutual Irrigation Project 9-20 9-5 Bryce Valley 9-22 Tables 9-1 Board of Water Resources Development Projects 9-3 9-2 Salinity Control Project Approved Costs 9-7 9-3 Wilderness Lands 9-8 9-4 Current and Projected Culinary Water Use 9-12 9-5 Current and Projected Secondary Water Use 9-12 9-6 Current and Projected Agricultural Water Use 9-13 9-7 Summary of Current and Projected Water Demands 9-14 9-8 Historical Reservoir Site Investigations 9-17 Section 9 West Colorado River Basin - Utah State Water Plan Water Planning and Development 9.1 Introduction The coordination and cooperation of all This section describes the major existing water development projects and proposed water planning water-related government agencies, and development activities in the West Colorado local organizations and individual River Basin. The existing water supplies are vital to water users will be required as the the existence of the local communities while also basin tries to meet its future water providing aesthetic and environmental values. -
Floating the Dirty Devil River
The best water levels and time Wilderness Study Areas (WSA) of year to float the Dirty Devil The Dirty Devil River corridor travels through two The biggest dilemma one faces when planning BLM Wilderness Study Areas, the Dirty Devil KNOW a float trip down the Dirty Devil is timing a WSA and the Fiddler Butte WSA. These WSA’s trip when flows are sufficient for floating. On have been designated as such to preserve their wil- BEFORE average, March and April are the only months derness characteristics including naturalness, soli- YOU GO: that the river is potentially floatable. Most tude, and primitive recreation. Please recreate in a people do it in May or June because of warm- manner that retains these characteristics. Floating the ing temperatures. It is recommended to use a hard walled or inflatable kayak when flows Dirty Devil are 100 cfs or higher. It can be done with “Leave-no-Trace” River flows as low as 65 cfs if you are willing to Proper outdoor ethics are expected of all visitors. drag your boat for the first few days. Motor- These include using a portable toilet when camping ized crafts are not allowed on this stretch of near a vehicle, using designated campgrounds The name "Dirty Devil" tells it river. when available, removing or burying human waste all. John Wesley Powell passed in the back country, carrying out toilet paper, using by the mouth of this stream on Another essential consideration for all visitors camp stoves in the backcountry, never cutting or his historic exploration of the is flash flood potential. -
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 -
Quantifying the Base Flow of the Colorado River: Its Importance in Sustaining Perennial Flow in Northern Arizona And
1 * This paper is under review for publication in Hydrogeology Journal as well as a chapter in my soon to be published 2 master’s thesis. 3 4 Quantifying the base flow of the Colorado River: its importance in sustaining perennial flow in northern Arizona and 5 southern Utah 6 7 Riley K. Swanson1* 8 Abraham E. Springer1 9 David K. Kreamer2 10 Benjamin W. Tobin3 11 Denielle M. Perry1 12 13 1. School of Earth and Sustainability, Northern Arizona University, Flagstaff, AZ 86011, US 14 email: [email protected] 15 2. Department of Geoscience, University of Nevada, Las Vegas, NV 89154, US 16 3. Kentucky Geological Survey, University of Kentucky, Lexington, KY 40506, US 17 *corresponding author 18 19 Abstract 20 Water in the Colorado River is known to be a highly over-allocated resource, yet decision makers fail to consider, in 21 their management efforts, one of the most important contributions to the existing water in the river, groundwater. This 22 failure may result from the contrasting results of base flow studies conducted on the amount of streamflow into the 23 Colorado River sourced from groundwater. Some studies rule out the significance of groundwater contribution, while 24 other studies show groundwater contributing the majority flow to the river. This study uses new and extant 1 25 instrumented data (not indirect methods) to quantify the base flow contribution to surface flow and highlight the 26 overlooked, substantial portion of groundwater. Ten remote sub-basins of the Colorado Plateau in southern Utah and 27 northern Arizona were examined in detail. -
Projecting Temperature in Lake Powell and the Glen Canyon Dam Tailrace
Projecting Temperature in Lake Powell and the Glen Canyon Dam Tailrace By Nicholas T. Williams1 Abstract factors affecting the magnitude of warming in dam discharges (Bureau of Reclamation, 2007). During the period of warmest river temperatures, the Recent drought in the Colorado River Basin reduced dissolved oxygen content of discharges from the dam declined water levels in Lake Powell nearly 150 feet between 1999 to concentrations lower than any previously observed (fig. 1). and 2005. This resulted in warmer discharges from Glen Operations at Glen Canyon Dam were modified by running Canyon Dam than have been observed since initial filling of turbines at varying speeds, which artificially increased the dis- Lake Powell. Water quality of the discharge also varied from solved oxygen content of discharges; however, these changes historical observations as concentrations of dissolved oxygen also resulted in decreased power generation and possibly dropped to levels previously unobserved. These changes damaged the turbines (Bureau of Reclamation, 2005). The generated a need, from operational and biological resource processes in the reservoir creating the low dissolved oxygen standpoints, to provide projections of discharge temperature content in the reservoir had been observed in previous years, and water quality throughout the year for Lake Powell and but before 2005 the processes had never affected the river Glen Canyon Dam. Projections of temperature during the year below the dam to this magnitude (Vernieu and others, 2005). 2008 were done using a two-dimensional hydrodynamic and As with the warmer temperatures, the low dissolved oxygen water-quality model of Lake Powell. The projections were concentrations could not be explained solely by the reduced based on the hydrological forecast for the Colorado River reservoir elevations. -
The Colorado River a NATURAL MENACE BECOMES a NATIONAL RESOURCE ' '
The Colorado River A NATURAL MENACE BECOMES A NATIONAL RESOURCE ' ' I Comprehensive Report on the Development of ze Water Resources of the Colorado River Basin for rrigation, Power Production, and Other Beneficial Ises in Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming By THE UNITED STATES DEPARTMENT OF THE INTERIOR J . A . Krug, Secretary SPONSORED BY AND PREPARED UNDER THE GENERAL SUPERVISION OF THE BUREAU OF RECLAMATION Michael W. Straus, Commissioner E. A. Morit-, Director, Region 3 ; E. O. Larson, Director, Region 4 MARCH 1 946 1P 'A m 4„ M 1i'leming Library Grand Canyon Colleg P . )x 11097 Contents Page PROPOSED REPORT OF THE SECRETARY OF THE Explorations 46 INTERIOR Settlement 48 Page Population 49 Letter of June 6,1946, from the Acting Commissioner, Chapter III . DIVIDING THE WATER 53 3 Bureau of Reclamation Virgin Conditions 55 REGIONAL DIRECTORS' REPORT Early Development of the River 56 Summary of Conditions in the Early 1920's . 59 Map of Colorado River Basin Facing 9 Between the Upper and Lower Basins 59 Scope and Purpose 9 Between United States and Mexico . 66 Authority for the Report 9 DEVELOPING THE BASIN Cooperation and Acknowledgments 9 Chapter IV. 69 Description of Area 10 Upper Basin 72 Problems of the Basin 11 Labor Force 72 Water Supply 12 Land Ownership and Use 73 Division of Water 13 Soils 73 Future Development of Water Resources 13 Agriculture 73 Table I, Present and Potential Stream Depletions in Minerals and Mining 80 the Colorado River Basin 14 Lumbering 85 Potential Projects 14 Manufacturing 86 Table II, Potential Projects in the Colorado River Transportation and Markets . -
Clear-Water Tributaries of the Colorado River in the Grand Canyon, Arizona: Stream Ecology and the Potential Impacts of Managed Flow by René E
Clear-water tributaries of the Colorado River in the Grand Canyon, Arizona: stream ecology and the potential impacts of managed flow by René E. Henery ABSTRACT Heightened attention to the sediment budget for the Colorado River systerm in Grand Canyon Arizona, and the importance of the turbid tributaries for delivering sediment has resulted in the clear-water tributaries being overlooked by scientists and managers alike. Existing research suggests that clear-water tributaries are remnant ecosystems, offering unique biotic communities and natural flow patterns. These highly productive environments provide important spawning, rearing and foraging habitat for native fishes. Additionally, clear water tributaries provide both fish and birds with refuge from high flows and turbid conditions in the Colorado River. Current flow management in the Grand Canyon including beach building managed floods and daily flow oscillations targeting the trout population and invasive vegetation has created intense disturbance in the Colorado mainstem. This unprecedented level of disturbance in the mainstem has the potential to disrupt tributary ecology and increase pressures on native fishes. Among the most likely and potentially devastating of these pressures is the colonization of tributaries by predatory non-native species. Through focused conservation and management tributaries could play an important role in the protection of the Grand Canyon’s native fishes. INTRODUCTION More than 490 ephemeral and 40 perennial tributaries join the Colorado River in the 425 km stretch between Glen Canyon Dam and Lake Mead. Of the perennial tributaries in the Grand Canyon, only a small number including the Paria River, the Little Colorado River and Kanab Creek drain large watersheds and deliver large quantities of sediment to the Colorado River mainstem (Oberlin et al. -
Glen Canyon Unit, CRSP, Arizona and Utah
Contents Glen Canyon Unit ............................................................................................................................2 Project Location...................................................................................................................3 Historic Setting ....................................................................................................................4 Project Authorization .........................................................................................................8 Pre-Construction ................................................................................................................14 Construction.......................................................................................................................21 Project Benefits and Uses of Project Water.......................................................................31 Conclusion .........................................................................................................................36 Notes ..................................................................................................................................39 Bibliography ......................................................................................................................46 Index ..................................................................................................................................52 Glen Canyon Unit The Glen Canyon Unit, located along the Colorado River in north central -
Bacteria in the Grand Canyon
White-water Researchers Check Bacteria in the Grand Canyon Item Type Article Authors Tunnicliff, Brock; Brickler, Stan; Webster, Guy Publisher College of Agriculture, University of Arizona (Tucson, AZ) Journal Progressive Agriculture in Arizona Rights Copyright © Arizona Board of Regents. The University of Arizona. Download date 27/09/2021 20:42:41 Link to Item http://hdl.handle.net/10150/296209 White -water Researchers Check Bacteria in the Grand Canyon Using river rafts equipped as mobile laboratories is the best way to By Dr. Brock Tunnicliff test water quality in the Colorado River of the Grand Canyon. The and Dr. Stan Brickler, School sharply increased number of boat trips through the canyon since the of Renewable Natural 1960s is the main reason that testing the water there has become impor- Resources, and Guy Webster, tant. Agricultural Communications Based on two years of testing, UA School of Renewable Natural Resources researchers have made recommendations for safer use of river water by boaters. Boaters should treat water from the river and its trib- utaries before drinking it. Drinking straight from the river has been common in past seasons. Boaters also should avoid stirring up bottom sediments. The sediments contain much more bacterial contamination than does the surface water. Stirring up sediments, especially in side- stream pools, can raise the fecal bacteria count in water above the stan- dard maximum for body- contact water use. Photograph: Recreational rafts The UA researchers have explained these recommendations to navigate a stretch of the Colorado River in the lower half of the boatmen from 22 licensed commercial outfitters during National Park Grand Canyon. -
FISH of the COLORADO RIVER Colorado River and Tributaries Between Glen Canyon Dam and Lake Mead
FISH OF THE COLORADO RIVER Colorado River and tributaries between Glen Canyon Dam and Lake Mead ON-LINE TRAINING: DRAFT Outline: • Colorado River • Glen Canyon Dam Adaptive Management Program (GCDAMP) • Native Fishes • Common Non-Native Fishes • Rare Non-Native Fishes • Standardized Sampling Protocol Colorado River: • The Colorado River through Grand Canyon historically hosted one of the most distinct fish assemblages in North America (lowest diversity, highest endemism) • Aquatic habitat was variable ▫ Large spring floods ▫ Cold winter temperatures ▫ Warm summer temperatures ▫ Heavy silt load • Today ▫ Stable flow releases ▫ Cooler temperatures ▫ Predation Overview: • The Glen Canyon Dam Adaptive Management Program was established in 1997 to address downstream ecosystem impacts from operation of Glen Canyon Dam and to provide research and monitoring of downstream resources. Area of Interest: from Glen Canyon Dam to Lake Mead Glen Canyon Dam Adaptive Management Program (Fish) Goals: • Maintain or attain viable populations of existing native fish, eliminate risk of extinction from humpback chub and razorback sucker, and prevent adverse modification to their critical habitat. • Maintain a naturally reproducing population of rainbow trout above the Paria River, to the extent practicable and consistent with the maintenance of viable populations of native fish. Course Purpose: • The purpose of this training course “Fish of the Colorado River” is to provide a general overview of fish located within the Colorado River below Glen Canyon Dam downstream to Lake Mead and linked directly to the GCDAMP. • Also included are brief explanations of management concerns related to the native fish species, as well as species locations. Native Fishes: Colorado River and tributaries between Glen Canyon Dam and Lake Mead Bluehead Sucker • Scientific name: Catostomus discobolus • Status: Species of Special Concern (conservation status may be at risk) • Description: Streamlined with small scales. -
Grand Canyon National Park
To Bryce Canyon National Park, KANAB To St. George, Utah To Hurricane, Cedar City, Cedar Breaks National Monument, To Page, Arizona To Kanab, Utah and St. George, Utah V and Zion National Park Gulch E 89 in r ucksk ive R B 3700 ft R M Lake Powell UTAH 1128 m HILDALE UTAH I L ARIZONA S F COLORADO I ARIZONA F O gin I CITY GLEN CANYON ir L N V C NATIONAL 89 E 4750 ft N C 1448 m RECREATION AREA A L Glen Canyon C FREDONIA I I KAIBAB INDIAN P Dam R F a R F ri U S a PAGE RESERVATION H 15 R i ve ALT r 89 S 98 N PIPE SPRING 3116 ft I NATIONAL Grand Canyon National Park 950 m 389 boundary extends to the A MONUMENT mouth of the Paria River Lees Ferry T N PARIA PLATEAU To Las Vegas, Nevada U O Navajo Bridge M MARBLE CANYON r e N v I UINKARET i S G R F R I PLATEAU F I 89 V E R o V M L I L d I C a O r S o N l F o 7921ft C F 2415 m K I ANTELOPE R L CH JACOB LAKE GUL A C VALLEY ALT P N 89 Camping is summer only E L O K A Y N A S N N A O C I O 89T T H A C HOUSE ROCK N E L E N B N VALLEY YO O R AN C A KAIBAB NATIONAL Y P M U N P M U A 89 J L O C FOREST O K K D O a S U N Grand Canyon National Park- n F T Navajo Nation Reservation boundary F a A I b C 67 follows the east rim of the canyon L A R N C C Y r O G e N e N E YO k AN N C A Road to North Rim and all TH C OU Poverty Knoll I services closed in winter.