Fill Mead First: a Different Approach to Managing the Colorado River
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Comprehensive Review of the Fill Lake Mead First Initiative
Comprehensive Review of the Fill Lake Mead First Initiative Trevor Carey ECL 290 February 28th, 2018 Lake Powell • Commissioned in 1966, full pool 1980 • 2nd largest man-made reservoir in United States (24.3 MAF) • Important for water storage and power generation for the Western United States USBR (2015) Impacts of Lake Powell and Glen Canyon Dam Fish Mollie & Aviva: Showed the dam almost eliminated sediment flows, decreased river temp. and allowed for a more hospitable environment for non-native fish. Vanessa: Discussed how dams contributed the extirpation of native fish. Water Rights Jesse & Jennifer: Native American’s access to water rights in the upper and lower basin, (Navajo water rights are in the Lake Powell watershed). Sediment Jeff: Sediment regime of the lower basin has been completely altered by impoundment of Lake Powell. Sarah: How dams contributed to changes to riparian ecosystems. Jasmin: Using high flow experiments to redistribute sediment and create beaches Dam Operation Marisa: Citizen science program looking at tidal effects caused by the dam Other Ann: Habitat destruction of the Kanab Ambersnail from high flows Fill Lake Mead First Initiative • Reservoir levels of both Lake Mead & Powell have been hovering around 50% full • Recent studies Barnett and Pierce (2008) and Kirk et al. (2017) showed reservoir levels will continue to decline, and hot drier conditions will be more common • Drain water from Lake Powell to fill Lake Mead • Glen Canyon dam would become a run of the river dam, with additional flood control capacity if needed Data courtesy of water-data.com Goals of FLMF • First proposed by Glen Canyon Institute in 2013 • Identified 3 goals of the initiative: 1. -
Terrestrial Vertebrate Fauna of the Kaiparowits Basin
Great Basin Naturalist Volume 40 Number 4 Article 2 12-31-1980 Terrestrial vertebrate fauna of the Kaiparowits Basin N. Duane Atwood U.S. Forest Service, Provo, Utah Clyde L. Pritchett Brigham Young University Richard D. Porter U.S. Fish and Wildlife Service, Provo, Utah Benjamin W. Wood Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Atwood, N. Duane; Pritchett, Clyde L.; Porter, Richard D.; and Wood, Benjamin W. (1980) "Terrestrial vertebrate fauna of the Kaiparowits Basin," Great Basin Naturalist: Vol. 40 : No. 4 , Article 2. Available at: https://scholarsarchive.byu.edu/gbn/vol40/iss4/2 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. TERRESTRIAL VERTEBRATE FAUNA OF THE KAIPAROWITS BASIN N. Diiane Atwood', Clyde L. Pritchctt', Richard D. Porter', and Benjamin W. Wood' .\bstr^ct.- This report inehides data collected during an investigation by Brighani Young University personnel to 1976, as well as a literature from 1971 review. The fauna of the Kaiparowits Basin is represented by 7 species of salamander, toads, mnphihians (1 5 and 1 tree frog), 29 species of reptiles (1 turtle, 16 lizards, and 12 snakes), 183 species of birds (plus 2 hypothetical), and 74 species of mammals. Geographic distribution of the various species within the basin are discussed. Birds are categorized according to their population and seasonal status. -
A Preliminary Assessment of Archaeological Resources Within the Grand Staircase-Escalante National Monument, Utah
A PRELIMINARY ASSESSMENT OF ARCHAEOLOGICAL RESOURCES WITHIN THE GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT, UTAH by David B. Madsen Common rock art elements of the Fremont and Anasazi on the Colorado Plateau and the Grand Staircase-Escalante National Monument. ,I!! CIRCULAR 95 . 1997 I~\' UTAH GEOLOGICAL SURVEY ." if;~~ 6EPARTMENT OF NATURAL RESOURCES ISBN 1-55791-605-5 STATE OF UTAH Michael O. Leavitt, Governor DEPARTMENT OF NATURAL RESOURCES Ted Stewart, Executive Director UTAH GEOLOGICAL SURVEY M. Lee Allison~ Director UGS Board Member Representing Russell C. Babcock, Jr. (chairman) .................................................................................................. Mineral Industry D. Cary Smith ................................................................................................................................... Mineral Industry Richard R. Kennedy ....................................................................................................................... Civil Engineering E.H. Deedee O'Brien ......................................................................................................................... Public-at-Large C. William Berge .............................................................................................................................. Mineral Industry Jerry Golden ..................................................................................................................................... Mineral Industry Milton E. Wadsworth ............................................................................................... -
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. -
Map Showing Location of Selected Surface-Water Sites and Springs, Escalante River Drainage Basin, Garfield and Kane Counties, Utah By
U.S. DEPARTMENT OF THE INTERIOR PREPARED IN COOPERATION WITH THE SCIENTIFIC INVESTIGATIONS REPORT 2004–5223 U.S. GEOLOGICAL SURVEY U.S. DEPARTMENT OF THE INTERIOR, BUREAU OF LAND MANAGEMENT, GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT Location of selected surface-water sites and springs, Escalante River drainage basin—Plate 1 Wilberg, D.E., and Stolp, B.J., 2004, Seepage Investigation and Selected Hydrologic Data for the Escalante River Drainage Basin, Garfield and Kane Counties, Utah, 1909-2002 111°45' 111°05' 114 ° 113 ° 112 ° 111° 42 ° T. 30 S. T. 31 S. Great 15 Salt 110 ° 109 ° B 41 ° Lake ou Salt Lake City lde r M Provo ou 40 ° nt ain 39 ° Utah Study 38 ° area Garfield County Kane County 37 ° E a s t F o T. 31 S. r k T. 32 S. 21 East Fork Boulder Creek near Boulder EXPLANATION B o u Boundary of study area l d u e s Platea r Aquariu C r Boundary of Grand Staircase-Escalante National Monument e e k Road k e e r C C ir Stream c r e le e C D l 16 38°00' if Surface-water site and number k fs or 22 East Fork Deer Creek near Boulder t F 38°00' as Spring E +35 Mile marker—Labeled every 5 miles T. 32 S. T. 33 S. 12 Dixie National Forest s il n a i Tr a t n p u o Boulder rr o T u B M n i f f i D r e e T. 33 S. -
Busting the Big One Activists Claim That Decommissioning Glen Canyon Dam Will Save Water and Restore a Wild Canyon
BUSTING THE BIG ONE Activists claim that decommissioning Glen Canyon Dam will save water and restore a wild canyon. Are they right? BY Krista LaNGLOIS “I just read n 1963, Glen Canyon was pronounced dead. Glen Can- Meanwhile, Lake Powell may be squandering the very re- yon Dam had submerged its fabled grottoes, Ancestral source it was designed to protect. Every day, water slowly seeps what everyone Puebloan cliff dwellings and slickrock chutes beneath the into the soft, porous sandstone beneath the reservoir and evapo- else had I stagnant water of Lake Powell, and forever altered the rates off its surface into the desert air. When more water flowed in ecology of the Grand Canyon just downstream. the system, this hardly mattered. But in an era where “every drop forgotten.” For wilderness lovers, the 710-foot-tall concrete wall stuck counts,” says Eric Balken, executive director of the nonprofit Glen out of the Colorado River like a middle finger — an insult that Canyon Institute, it calls for a drastic re-evaluation of the Colo- —Jack Schmidt, helped ignite the modern environmental movement. In 1981, rado River’s plumbing. “The Colorado River can no longer sustain watershed scientist the radical group Earth First! faked a “crack” on the dam by two huge reservoirs,” Balken says. “There isn’t enough water.” who evaluated water unfurling a 300-foot-long black banner down the structure’s That’s one reason the Glen Canyon Institute is pushing an savings and loss from Lake Powell front. The Sierra Club’s first executive director, David Brower, audacious proposal called “Fill Mead First,” which calls for the and Lake Mead considered the dam’s construction a personal failure and spent U.S. -
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. -
Fill Mead First: a Technical Assessment1 Executive Summary
Fill Mead First: a technical assessment1 John C. Schmidt2 with contributions from Maggi Kraft3, Daphnee Tuzlak4, and Alex Walker3 White Paper No. 1 Center for Colorado River Studies Quinney College of Natural Resources Utah State University November 10, 2016 Executive Summary The Fill Mead First (FMF) plan would establish Lake Mead reservoir as the primary water storage facility of the main-stem Colorado River and would relegate Lake Powell reservoir to a secondary water storage facility to be used only when Lake Mead is full. The objectives of the FMF plan are to re-expose some of Glen Canyon’s sandstone walls that are now inundated, begin the process of re-creating a riverine ecosystem in Glen Canyon, restore a more natural stream-flow, temperature, and sediment-supply regime of the Colorado River in the Grand Canyon ecosystem, and reduce system-wide water losses caused by evaporation and movement of reservoir water into ground-water storage. The FMF plan would be implemented in three phases. Phase I would involve lowering Lake Powell to the minimum elevation at which hydroelectricity can still be produced (called minimum power pool elevation): 3490 ft asl (feet above sea level). At this elevation, the water surface area of Lake 1 suggested citation: Schmidt, J. C., Kraft, M., Tuzlak, D., and Walker, A. 2016. Fill Mead First: a technical assessment. Logan, Utah State University Quinney College of Natural Resources, Center for Colorado River Studies, white paper no. 1, 80 p., available at <https://qcnr.usu.edu/wats/colorado_river_studies/>. 2 corresponding author; Department of Watershed Sciences, Utah State University, Logan UT 84322-5210; [email protected] 3 graduate student, Department of Watershed Sciences 4 graduate student, Department of Geology 1 Powell is approximately 77 mi2, which is 31% of the surface area when the reservoir is full. -
Colorado & Utah National Park Tour
Colorado & Utah National Park Tour $2590 Per Person 11 Days / 10 Nights Day 1 - Hays, KS Day 4 - Arches National Park We begin our journey by heading west into Kansas. While driving through the Flint Hills, we’ll see several This morning we head to Canyonlands National Park windfarms and hundreds of miles of prairie and crop where we’ll explore some of the towering buttes and land. You’ll visit the Dwight Eisenhower Library and deep canyons carved out by the Colorado River. In the Museum. There is a vast amount of history in this afternoon we’re off to see the arches at Arches National world-class library. We’ll end today in Hays, KS. Park. We’ll see a few of the 2,000 natural stone arches and bridges. Tonight we end up in Green River, UT. Day 2 - Wings Over the Rockies Museum After breakfast we start our journey to Colorado. We stop at Wings Over the Rockies Air & Space Museum. You’ll see a hangar full of iconic aircraft and military memorabilia. We’ll also visit Downtown Denver and Union Station for some sight seeing and a bite to eat before we settle into our hotel near Golden, CO. Make sure to rest up for the great days ahead. Day 3 - Colorado National Monument This morning we’ll drive west to the Colorado National Monument where you’ll see sheer-walled red rock canyons, towering monoliths and maybe some big horn sheep. Along the way we’ll drive through the Day 5 - Bryce Canyon National Park famous Eisenhower Tunnel. -
The Lost World of Glen Canyon
- r f 1 / I / I / r llS^ *&v . .".•*' : '•.-• - :•:-.*« •••• '•• i^g. i. A large sandstone arch called Galloway Cave existed on the right bank about 2.25 miles upstream from Glen Canyon Dam. River travelers camped here before the turn of the century and seemed always to build their campfires in the same place, at the downstream corner of the arch. Many also left a record of their presence by uniting their names on the wall with a piece of charcoal. This view shows a Nevills river party preparing for dinner on June 11, 1949. Lake Powell covers this site. Photographs, except Fig. 4, are courtesy of author. The Lost World of Glen Canyon BY P. T. REILLY THOUSANDS OF PEOPLE CRUISE THE SURFACE OF Lake Powell never dream ing of the wonders beneath the waters, features that are not likely to be exposed again in our lifetime, nor in those of our children or grandchildren. In fact, they may never be seen again. This photo graphic collection of landforms will serve as a reminder that our world changes as dramatically in the vertical as it does in the horizontal. Mr. Reilly lives in Sun City, Arizona. Readers may wish to refer to the following: Plan and Profile, Colorado River, Lees Ferry, Arizona, to Mouth of Green River, Utah, Sheet B; Navajo Mountain, Utah- Arizona quadrangle; Lake Canyon, Utah quadrangle; and Mancos Mesa, Utah quadrangle. The Lost World of Glen Canyon 123 Lee's Ferry occupies a unique and important position on the Colorado River because the 1921 measurement by the U.S. -
Lee's Ferry Historic District
STATE: Form 10-31/0 UNITED STATES DEPARTMENT OF THE INTERIOR (Oct. 1972) NATIONAL PARK SERVICE Arizona NATIONAL REGISTER OF HISTORIC PLACES Coconino INVENTORY-NOMINATION FORM FOR NPSUSE ONLY FOR FEDERAL PROPERTIES ENTRY DATE. (Type all entries - complete applicable sections) Lees Ferry Sections 13 & 18. T.40N., R.7E. & R.8E. Lees Ferry District, en Canyon NRA Rep.' J . Sam StM>j>r^.»Jj^" V •',.- 3 CATEGORY ACCESSIBLE OWNERSHIP STATUS (Check One) TO THE PUBLIC QJ District [~1 Building Public Acquisition: l Occupied Yes: Q Site |—| Structure f~] Private I I In Process [ | Unoccupied [~~1 Restricted O Object CD Bofh I | Being Considered I | Preservation work ££] Unrestricted in progress CD No PRESENT USE (Check One or Afore as Appropriate) |~~| Agricultural (3 Government Transportation (~~1 Comments [~2fl Commercial F~| Industrial | | Private Residence Other fS | | Educational Q Military I | Religious recreation - jump nff | | Entertainment [~] Museum Scientific point for Hoi oradn U.S. National Park Service.- Glen Canyon National Recreation Area REGIONAL HEADQUARTERS: (It applicable) STREET AND NUMBER: 5 M P.O. Box 1507 O 3 CITY OR TOWN: P) Page Ari zona 11 COURTHOUSE, REGISTRY O-F DEEDS, ETC: Establishing legislation for Glen Canyon National Recreation Arc>a STREET AND NUMBER: CITY OR TOWN: TITLE OF SURVEY: Arcgeological Survey of Glen Canvon DATE OF SURVEY: - ~\ 963 Federal Lxl State [~1 County Local DEPOSITORY FOR SURVEY RECORDS: Utah Statewide Archeolocpcal Survey: Glen Canyon Series STREET AND NUMBER: Department of Anthropology - University of Utah CITY OR TOWN: STATE: CODE Cit Utah. 49 continued on 10-300a Form 10-300o UNITED STATES DEPARTMENT OF THE INTERIOR (July 1969) NATIONAL PARK SERVICE Arizona NATIONAL REGISTER OF HISTORIC PLACES Coconino INVENTORY - NOMINATION FORM FOR NPS USE ONLY ENTRY NUMBER DATE (Continuation Sheet) IS (Number all entries) 6.