West Colorado River Plan
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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 ............................................................................................... -
Saline Soils and Water Quality in the Colorado River Basin: Natural and Anthropogenic Causes Gabriel Lahue River Ecogeomorphology Winter 2017
Saline soils and water quality in the Colorado River Basin: Natural and anthropogenic causes Gabriel LaHue River Ecogeomorphology Winter 2017 Outline I. Introduction II. Natural sources of salinity and the geology of the Colorado River Basin IIIA. Anthropogenic contributions to salinity – Agriculture IIIB. Anthropogenic contributions to salinity – Other anthropogenic sources IV. Moving forward – Efforts to decrease salinity V. Summary and conclusions Abstract Salinity is arguably the biggest water quality challenge facing the Colorado River, with estimated damages up to $750 million. The salinity of the river has doubled from pre-dam levels, mostly due to irrigation and reservoir evaporation. Natural salinity sources – saline springs, eroding salt-laden geologic formations, and runoff – still account for about half of the salt loading to the river. Consumptive water use for agricultural irrigation concentrates the naturally- occurring salts in the Colorado River water, these salts are leached from the root zone to maintain crop productivity, and the salts reenter the river as agricultural drainage water. Reservoir evaporation represents a much smaller cause of river salinity and most programs to reduce the salinity of the Colorado River have focused on agriculture; these include the lining of irrigation canals, irrigation efficiency improvements, and removing areas with poor drainage from production. Salt loading to the Colorado River has been reduced because of these efforts, but more work will be required to meet salinity reduction targets. Introduction The Colorado River is one of the most important rivers in the Western United States: it provides water for approximately 40 million people and irrigation water for 5.5 million acres of land, both inside and outside the Colorado River Basin (CRBSCF, 2014). -
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). -
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. -
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. -
Preliminary Report on Some Uranium Deposits Along the West Side of the San Rafael Swell, Emery County, Utah
UNITED STATES ATOMIC ENERGY COMMISSION RMO-673 PRELIMINARY REPORT ON SOME URANIUM DEPOSITS ALONG THE WEST SIDE OF THE SAN RAFAEL SWELL, EMERY COUNTY, UTAH By Millard L. Reyner October 1950 SI-7c1 Division of Raw Materials Exploration Branch Technical Information Service, Oak Ridge, T•nn•ss•• ; "N_ ' \ - —rrs1 • „ 6 NOV 1952 METALLURGY AND CERAMICS Reproduced direct from copy a3 submitted to this office. AEC,Oak Ridge,Tenn.,8-13-51--515-W5593 CONTMITS Page Introduction 1 Geography 3 History 4 Regional geology 4 Economic geology 5 General 5 Mineralogy 7 Deposits examined 8 Lone Tree group. 8 Hard Pan group 11 Dalton group 12 Dexter group 12 Clifford Smith claim 16 Wickiup group 17 Gardell Snow's claim 20 Dolly group 20 South Fork group 20 Hertz No. 1 claim 21 Pay Day claim. Green Vein group. and Brown Throne group 21 Dirty Devil group 26 Summary and conclusions 30 iii ILLUSTRATIONS Page Figure 1. Index Map of Utah showing location of area examined. • •••••••• OOOOO ••. 2 Figure 2. Map showing locations of uranium prospects and samples on a mesa 4 miles southwest of the San Rafael River bridge. OOOOO . 9 Figure 3. Sketch showing plan, sections, and samples of the Lone Tree adit .••••• OOOOO 10 Figure 4. Plan and sections of Dalton Group showing sample locations and assays . 13 Figure 5. Plan of adit on Dexter Group showing sample looations and assays. 15 Figure 6. Sketch of Block Mountain showing locations of samples in Wickiup Group•• OOOOOO 18 Figure 7. Sketch showing sample locations and assays in main workings of Wickiup Group on the west side of Block Mountain. -
May Wasatch Mountain Club
MAY WASATCH MOUNTAIN CLUB VOL 63, NO. 5, MAY 1986 HIGHLIGHTS NEW HIKINC f\'.ATINGS THURSDAD EVEN ING H(r-1:S START NEW EQU 1PM£:NT ENVJ EONMENTJ\L REGULATl ONS WASATCH MOUNTAIN CLUB THE RAMBLER, the official publication of the Wasatch Mountain Club is published monthly by and for its members. Persons wishing to become members and receive Earl Cook, Managing Editor THE RAMBLER for two months upon written request to the Membership Director, 168 Production: Carl Cook West, Fifth North, Salt Lake City, Utah, David Vickery 84103 and payment of $3.00. Checks to be made payable to the Wasatch Mountain Club. There is a $10.00 charge for THE RAMBLER (USPS 053-410) is published returned checks. monthly by the WASATCH MOUNTAIN CLUB, Inc., 168 West, 500 North, Salt Lake Membership applicants must participate city, ·uT 841 03. Telephone 363-7150. in at least two Club outdoor or service Subscription rates of $12.00 per year activities, verified by the signatures are paid for by membership dues only. of the activity leader. Yearly dues are Second-class Postage Paid at Salt Lake $15.00 single, $20.00 couple. A $5.00 City, UT. initiation/reinstatement fee is charged. POSTMASTER: Send address changes to THE RAMBLER Membership Director, 168 West, 1985-1986 500 North, Salt Lake City, UT 84103, DIRECTORS President Ann Cheves 355-0304 CHANGE OF ADDRESS: This publication is Secretary Carol Kalm 272-0828 not forwarded by the Post Office. Treasurer John Veranth 278-5826 Change of address should be submitted in Membership Marian Nelson 582-8308 writing to the Membership Director, 168 Boating Gary Tomlinson 571-5555 West, Fifth North, Salt Lake City, Utah, Conservation Mary Gustafason 364-9252 84103, Written correspondence Chris Biltoft 359-5645 regarding the mailing of THE RAMBLER Entertainment Cassie Badowsky 278-51 53 should be directed to the Membership John Colaizzi 571-5555 Director at that address. -
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. -
Establishing the Geomorphic Context for Wetland and Riverine Restoration of the San Rafael River
Final Report Establishing the geomorphic context for wetland and riverine restoration of the San Rafael River NRCS Cooperative Agreement #68-3A75-4-155 Stephen T. Fortney, John C. Schmidt, and David J. Dean Intermountain Center for River Rehabilitation and Restoration Department of Watershed Sciences Utah State University Logan, UT In collaboration with Michael E. Scott Julian Scott Fort Collins Science Center U. S. Geological Survey Fort Collins, CO March 22, 2011 1 Table of Contents I. Introduction 5 II. Purpose 5 III. Study Area 9 IV. Hydrology 11 V. Methods 18 A. Floodplain Stratigraphy 18 B. Repeat Photography: Aerial Imagery and Oblique Ground Photographs 19 C. USGS gage data 21 Reconstructed Cross Sections 21 Rating Relations 22 Time Series of Thalweg Elevation 22 Time Series of Width and Width-to-Depth Ratio 22 Hydraulic Geometry 22 D. Longitudinal Profile 24 E. Additional Activities 24 VI. Results: Channel Transformation on Hatt Ranch 26 Turn of the 20th century 26 1930s and 1940s 29 1950s 33 1960s and 1970s 41 1980s 46 1990s to present 49 Longitudinal Profile 50 VII. Summary 54 A. Channel Transformation on Hatt Ranch 54 B. Restoration and Management Implications 55 VIII. Expenditures 56 IX. Timeline 56 X. References 56 XI. Appendix 59 Table of Figures Figure 1. Oblique ground photos taken near the old Highway 24 bridge 6 Figure 2. Conceptual model of how watershed attributes control channel and floodplain form. 7 Figure 3. Conceptual model of restoration versus rehabilitation 8 Figure 4. Map of the San Rafael River watershed. 10 Figure 5. Map of the study area 11 Figure 6. -
Our Secret Is Now Yours!
EXPLORE... THREE ADVENTUROUS ZONES Travel Guide Travel The Highlands Capitol Reef East Desert Our secret is now yours! Wayne County, - Utah - USA TABLE OF CONTENTS WELCOME Wayne County, Utah - Capitol Reef Country 1- Cover Calendar of Events 2- Table of Contents April to October - Daily Walks / Capitol Reef Welcome to the scenically diverse region encompassing Wayne County YOUR NEXT GREAT 3- Welcome May Utah’s Capitol Reef Country. - Entrada Institute’s Cowboy Poetry and Music DESTINATION 4- Zones Festival This vacation destination includes mountains, forests, pinnacles, arches, 5- Zones July plateaus, and astounding desert - Torrey Apple Days landscapes. The contrast in elevation 6- Attractions - Capitol Reef Classic – Annual High Desert Bike and terrain makes this area a haven Race. for those seeking solitude or - Bicknell International Film Festival (BIFF) 7- Attractions outdoor adventure. August This region is an excellent multi-day 8- Activities - Women’s Redrock Music Festival vacation destination, central to Utah’s - Wayne County Fair scenic attractions, and easily acces- 9- Guides & Outfitters sible from major cities such as Salt September/October Lake City, Denver, and Las Vegas. 10- Maps - Heritage Star Festival - Wayne Wonderland Air show Unpack once and discover a realm 11- Maps that is conveniently situated be- On Going Events: May - September tween Bryce Canyon, the Grand 12- Hotels / Motels Staircase, Goblin Valley State Park, Capitol Reef National Park: Daily walks and nightly Canyonlands National Park, and amphitheatre programs mid May - September. Lake Powell. 13- Cabins / B&B Check at Visitor Center for Ripple Rock Nature Center schedule. Capitol Reef National Park. You’ll want to reserve several days to 14- Campgrounds (435) 425-3791, ext. -
Ide to I-70 Through Southeastern Utah – Discovermoab.Com - 6/22/07 Page 1
A Guide to I-70 Through Southeastern Utah – discovermoab.com - 6/22/07 Page 1 and increase to Milepost 227 near the Colorado border. Mileage marker posts 2W - Thompson Springs A Guide to I-70 Through (or Mileposts) and Exit numbers Welcome Center Southeastern Utah correspond, and both are used in the Milepost 189 descriptive text which follows. This rest area welcomes westbound Although the scenery is spectacular as visitors with free brochures and maps. viewed from the highway, you are The center, operated by the State of Utah, encouraged to stop at the sites described is open all year. From Memorial Day Moab Area Travel Council below to see even more. Other nearby through Labor Day, personnel are on duty Internet Brochure Series points of interest accessible from 1-70 are from 8 a.m. to 8 p.m. to answer your Available from: briefly noted and located on the map. questions. The rest of the year the center More detailed information on these sights is operated from 9 a.m. to 5 p.m. Indoor discovermoab.com can be obtained by contacting the rest rooms, water, picnic shelters, and a appropriate agencies listed in this public phone are available at all times. brochure. INTRODUCTION Food and fuel are available at Thompson 1W - Harley Dome View Area Springs (Exit 187), which provides access Interstate 70 (1-70) through southeastern Milepost 228 to a panel of Native American rock art in Utah is a journey through fascinating Sego Canyon. To visit this site, follow the landscapes. The route reveals vast deserts, The Harley Dome View Area is located signs from the north side of town.