Digital Representation of 1:1,000,000-Scale Hydrographic Areas of the Great Basin
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Description and Correlation of Geologic Units, Cross
Plate 2 UTAH GEOLOGICAL SURVEY Utah Geological Survey Bulletin 135 a division of Hydrogeologic Studies and Groundwater Monitoring in Snake Valley and Utah Department of Natural Resources Adjacent Hydrographic Areas, West-Central Utah and East-Central Nevada DESCRIPTION OF GEOLOGIC UNITS SOURCES USED FOR MAP COMPILATION UNIT CORRELATION AND UNIT CORRELATION HYDROGEOLOGIC Alluvial deposits – Sand, silt, clay and gravel; variable thickness; Holocene. Qal MDs Lower Mississippian and Upper Devonian sedimentary rocks, undivided – Best, M.G., Toth, M.I., Kowallis, B.J., Willis, J.B., and Best, V.C., 1989, GEOLOGIC UNITS UNITS Shale; consists primarily of the Pilot Shale; thickness about 850 feet in Geologic map of the Northern White Rock Mountains-Hamlin Valley area, Confining Playa deposits – Silt, clay, and evaporites; deposited along the floor of active Utah, 300–400 feet in Nevada. Aquifers Qp Beaver County, Utah, and Lincoln County, Nevada: U.S. Geological Survey Units playa systems; variable thickness; Pleistocene through Holocene. Map I-1881, 1 pl., scale 1:50,000. D Devonian sedimentary rocks, undivided – Limestone, dolomite, shale, and Holocene Qal Qsm Qp Qea Qafy Spring and wetland related deposits – Clay, silt, and sand; variable thickness; sandstone; includes the Guilmette Formation, Simonson and Sevy Fritz, W.H., 1968, Geologic map and sections of the southern Cherry Creek and Qsm Quaternary Holocene. Dolomite, and portions of the Pilot Shale in Utah; thickness about 4400– northern Egan Ranges, White Pine County, Nevada: Nevada Bureau of QTcs 4700 feet in Utah, 2100–4350 feet in Nevada. Mines Map 35, scale 1:62,500. Pleistocene Qls Qlm Qlg Qgt Qafo QTs QTfs Qea Eolian deposits – Sand and silt; deposited along valley floor margins, includes Hintze, L.H., 1963, Geologic map of Utah southwest quarter, Utah Sate Land active and vegetated dunes; variable thickness; Pleistocene through S Silurian sedimentary rocks, undivided – Dolomite; consists primarily of the Board, scale 1:250,000. -
North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave
North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave http://www.desertusa.com/desert.html In most modern classifications, the deserts of the United States and northern Mexico are grouped into four distinct categories. These distinctions are made on the basis of floristic composition and distribution -- the species of plants growing in a particular desert region. Plant communities, in turn, are determined by the geologic history of a region, the soil and mineral conditions, the elevation and the patterns of precipitation. Three of these deserts -- the Chihuahuan, the Sonoran and the Mojave -- are called "hot deserts," because of their high temperatures during the long summer and because the evolutionary affinities of their plant life are largely with the subtropical plant communities to the south. The Great Basin Desert is called a "cold desert" because it is generally cooler and its dominant plant life is not subtropical in origin. Chihuahuan Desert: A small area of southeastern New Mexico and extreme western Texas, extending south into a vast area of Mexico. Great Basin Desert: The northern three-quarters of Nevada, western and southern Utah, to the southern third of Idaho and the southeastern corner of Oregon. According to some, it also includes small portions of western Colorado and southwestern Wyoming. Bordered on the south by the Mojave and Sonoran Deserts. Mojave Desert: A portion of southern Nevada, extreme southwestern Utah and of eastern California, north of the Sonoran Desert. Sonoran Desert: A relatively small region of extreme south-central California and most of the southern half of Arizona, east to almost the New Mexico line. -
Water Resources of Millard County, Utah
WATER RESOURCES OF MILLARD COUNTY, UTAH by Fitzhugh D. Davis Utah Geological Survey, retired OPEN-FILE REPORT 447 May 2005 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES Although this product represents the work of professional scientists, the Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, stated or implied, regarding its suitability for a particular use. The Utah Department of Natural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users of this product. This Open-File Report makes information available to the public in a timely manner. It may not conform to policy and editorial standards of the Utah Geological Survey. Thus it may be premature for an individual or group to take action based on its contents. WATER RESOURCES OF MILLARD COUNTY, UTAH by Fitzhugh D. Davis Utah Geological Survey, retired 2005 This open-file release makes information available to the public in a timely manner. It may not conform to policy and editorial standards of the Utah Geological Survey. Thus it may be premature for an individual or group to take action based on its contents. Although this product is the work of professional scientists, the Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, expressed or implied, regarding its suitability for a particular use. The Utah Department of Natural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users of this product. -
University of Nevada Reno Determination of Timing Of
University of Nevada Reno J Determination of Timing of Recharge for Geothermal Fluids in The Great Basin Using Environmental Isotopes and Paleoclimate Indicators A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science, in geology by Paul K. Buchanan 1" April, 1990 i MINES LIBRARY Tti GS Li a (ths The thesis of Paul K. Buchanan is approved by University of Nevada Reno April, 1990 11 ACKNOWLEGEMENTS This study was made possible by grant DE-FG07-88ID12784 from the United States Department of Energy, Geothermal Technology Division, administered by the Idaho Operations Office, Idaho Falls, Idaho. Additional financial assistance from the Nevada Section of the Geothermal Resources Council aided in the completion of this thesis. My thanks go to the Nevada geothermal power industry for allowing fluid sampling of deep powerplant production wells. Specifically, Chevron Resources, Oxbow Geothermal, Ormat Energy Systems, Geothermal Food Processors, Tad's Enterprises, Thermochem Inc., Elko Heat Co. and Elko School District are thanked. Thanks also to Dr. Robert Fournier of the United States Geological Survey for providing data on the Coso geothermal system. Michelle Stickles is to be commended for suffering through the proof reading of the initial drafts of this report. Thanks to my advisor, Jim Carr, and my committee members, Mel Hibbard and Gary Haynes, for taking on this project and putting up with my inconsistent scheduling and "last minute" rush. Special thanks to my cohorts at the Division of Earth Sciences and Mackay School of Mines for their cynical attitudes that helped keep it all in perspec- tive, through both the good and the bad times. -
Episodic Dust Events of Utah's Wasatch
1654 JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY VOLUME 51 Episodic Dust Events of Utah’s Wasatch Front and Adjoining Region W. JAMES STEENBURGH AND JEFFREY D. MASSEY Department of Atmospheric Sciences, University of Utah, Salt Lake City, Utah THOMAS H. PAINTER Jet Propulsion Laboratory, Pasadena, California (Manuscript received 4 January 2012, in final form 4 April 2012) ABSTRACT Episodic dust events cause hazardous air quality along Utah’s Wasatch Front and dust loading of the snowpack in the adjacent Wasatch Mountains. This paper presents a climatology of episodic dust events of the Wasatch Front and adjoining region that is based on surface weather observations from the Salt Lake City International Airport (KSLC), Geostationary Operational Environmental Satellite (GOES) imag- ery, and additional meteorological datasets. Dust events at KSLC—defined as any day [mountain standard time (MST)] with at least one report of a dust storm, blowing dust, and/or dust in suspension with a visi- bility of 10 km or less—average 4.3 per water year (WY: October–September), with considerable in- terannual variability and a general decline in frequency during the 1930–2010 observational record. The distributions of monthly dust-event frequency and total dust flux are bimodal, with primary and secondary maxima in April and September, respectively. Dust reports are most common in the late afternoon and evening. An analysis of the 33 most recent (2001–10 WY) events at KSLC indicates that 11 were associated with airmass convection, 16 were associated with a cold front or baroclinic trough entering Utah from the west or northwest, 4 were associated with a stationaryorslowlymovingfrontorbaroclinictroughwestof Utah, and 2 were associated with other synoptic patterns. -
See for Details and How to Win a Limited Edition Full Curl Rifle
200 Trophy Permits • $5 per Permit Application FEBRUARY 9–12, 2012 Salt Palace Convention Center Salt Lake City 200 Trophy Permits • $5 per Permit Application J AďLY NOW FOR $5 DRAWINGFEBRUARY FOR 200 BIG GAME 9–12, PERMITS 2012 K SpecialSpecial Salt Palace Convention Center Salt Lake City ThanksThanks J AďLY NOW FOR $5 DRAWING FOR 200 BIG GAME PERMITS K toto ourour TitleTitle 2017 AUCTION SponsorsSponsors 5 CATALOG www.AMMOANDMORESTORE.com THOSE WHO MAKE IT HAPPEN Welcome Sportsmen and Sportswomen! Welcome to the 11th Annual Western Hunting & Conservation Expo. Sportsmen for Fish & Wildlife and the Emmett Burroughs – Mule Deer Foundation Founder Sportsmen for Fish & Wildlife Board of Directors Don Peay – Founder Mule Deer Foundation are excited to bring you this very special hunting and conservation show. Your attendance Mule Deer Foundation Board of Directors Dave Woodhouse – Chairman and purchases help ensure the conservation of our wildlife and wild lands and the future of our hunting and sporting Brian Fienhold – Chairman of the Board Kevin Pritchett – Vice Chairman heritage. Thank you for joining us. Bethany Erb – Vice-Chair of the Board Rusty Aiken Ryan Bronson Brayden Richmond We are proud of how far the Expo has grown the past 11 years and this year promises to be spectacular. Our four- CJ Buck Kurt Wood Aaron Oelger day event features over 375 exhibits offering the finest guides, outfitters, professional hunters, artists, taxidermists, Erik Craythorne Jim Steadman jewelers, furriers and purveyors of fine guns, knives, optics, clothing and sporting equipment for the discerning Bob Jacobs sportsman and sportswoman. Kirstie Pike SFW Mission Fulfillment Board Art Reese Troy Justensen – Mission Fulfillment Board Chairman Daniel Harrison Dave Woodhouse – Vice Chairman/Utah Co. -
Ranch Creek Watershed and Riparian Improvement Project
Ranch Creek Watershed United States Department of and Riparian Improvement Agriculture Forest Service Project Intermountain Region Environmental Assessment Dixie National Forest Escalante Ranger District January 2017 Environmental Assessment Title Page Photo Description: For More Information Contact: Terry DeLay Escalante Ranger District P.O. Box 246 Escalante, UT 84726 Phone: (435) 826-5401 Email: [email protected] Fax: (435) 826-5491 In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD-3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. -
Tribally Approved American Indian Ethnographic Analysis of the Proposed Escalante Valley Solar Energy Zone
Tribally Approved American Indian Ethnographic Analysis of the Proposed Escalante Valley Solar Energy Zone Participating Tribes Confederated Tribes of the Goshute Reservation, Ibapah, Utah Paiute Indian Tribe of Utah, Cedar City, Utah Ethnography and Ethnographic Synthesis For Solar Programmatic Environmental Impact Statement and Solar Energy Study Areas in Portions of Arizona, California, Nevada, and Utah By Richard W. Stoffle Kathleen A. Van Vlack Hannah Z. Johnson Phillip T. Dukes Stephanie C. De Sola Kristen L. Simmons Bureau of Applied Research in Anthropology School of Anthropology University of Arizona October 2011 Solar PEIS Ethnographic Assessment Page 1 ESCALANTE VALLEY The proposed Escalante Valley solar energy zone (SEZ) is located in Iron County, Utah (Figure 1). It is approximately four miles south of Lund, Utah and ten miles east of Beryl, Utah. The SEZ is situated in the Escalante Valley, which is a large, southwest-northeast trending valley in the south-central portion of the Escalante Desert. Figure 1 Google Earth Image of the Escalante Valley SEZ Outlined in Red and SEZ American Indian Study Area The Escalante Valley SEZ American Indian study area extends beyond the boundaries of the SEZ because of the existence of cultural resources in the surrounding landscape. The Escalante Valley SEZ American Indian study area includes plant and animal communities, geological features, water sources, historic events and the trails that would have connected these features. Southern Paiute and Goshute representatives maintain that, in order to understand Numic connections to the SEZ, it must be placed in context with neighboring connected places including the Milford Flats South and Wah Wah Valley SEZs and their associated cultural resources found in the larger study areas. -
Hydrogeology of Spring, Cave, Dry Lake, and Delamar Valleys Impacts
HYDROGEOLOGY OF SPRING, CAVE, DRY LAKE, AND DELAMAR VALLEYS IMPACTS OF DEVELOPING SOUTHERN NEVADA WATER AUTHORITY’S CLARK, LINCOLN, AND WHITE PINE COUNTIES GROUNDWATER DEVELOPMENT PROJECT Presented to the Office of the Nevada State Engineer on behalf of Protestants White Pine County, Great Basin Water Network, et al. June, 2017 Prepared by: _______________________________________________________________ Thomas Myers, Ph.D. Hydrologic Consultant Reno, NV June 28, 2017 Date Table of Contents Summary ................................................................................................................................................. 1 Introduction ............................................................................................................................................ 3 Method of Analysis .................................................................................................................................. 3 Study Area ........................................................................................................................................... 5 Water Rights Applications and Proposed Pumping Scenarios ............................................................... 8 Conceptual Flow Model ..................................................................................................................... 10 White River Flow System ................................................................................................................... 25 Hydrogeologic Properties of Aquifer Systems -
Karen Glasgow
United States Department of the Interior OFFICE OF THE SOLICITOR Pacific Southwest Region San Francisco Field Office 333 Bush Street, Suite 775 San Francisco. California 94104 Direct Telephone: (415) 296-3381 Facsimile: (415) 296-3371 E-mail: [email protected] October 28, 2020 Mr. Tim Wilson Nevada Division of Water Resources, State Engineer’s Office 901 South Stewart Street, Suite 2002 Carson City, NV 89701-5250 Re: NPS and BLM Written Testimony on the Proposed Order Designating and Describing the Hamlin Valley Hydrographic Basin (11-196) within Lincoln and White Pine Counties, Nevada. Dear Mr. Wilson: On behalf of the National Park Service and the Bureau of Land Management (the DOI Agencies), I am submitting the DOI Agencies’ joint written testimony on the Nevada State Engineer’s proposed order designating and describing the Hamlin Valley Hydrographic Basin (11-196). The written testimony is submitted in accordance with the instructions noted in the hearing notice for the order. The DOI Agencies appreciate the opportunity to provide written testimony on the proposed order. If you or your staff have any questions regarding this written testimony, please contact me at your convenience. Sincerely, Karen D. Glasgow Field Solicitor-San Francisco Field Office Office of the Solicitor, Department of the Interior Cc (electronic): Forrest Harvey, Peter Fahmy, Jeff Hughes, Gary Karst, James Woolsey, Ben Roberts (NPS) Sarah Peterson, Roy E. Smith (BLM) Erica Anderson (Solicitor) Written Testimony on the Proposed Order Designating and Describing the Hamlin Valley Hydrographic Basin (11-196) within Lincoln and White Pine Counties, Nevada. The National Park Service (NPS) and Bureau of Land Management (BLM Nevada), collectively referred to as the DOI Agencies, thank the Nevada Division of Water Resources (NDWR) for the opportunity to provide written testimony on the proposed order designating and describing the Hamlin Valley Hydrographic Basin (11-196). -
A History of Kane County, Utah Centennial County History Series
A HISTORY OF <Kam County Martha Sonntag Bradley UTAH CENTENNIAL COUNTY HISTORY SERIES A HISTORY OF County Martha Sonntag Bradley Kane County is noted for some of the most beautiful—though often inhospitable—land in Utah and has been home to resourceful humans for thousands of years. It was outside the area of first Mormon settlement and was actually created in the early 1860s before many had moved to the area. After the Black Hawk War, settlers soon moved to favorable locations such as Kanab and Long Valley, establishing towns in the isolated region north of the Arizona Strip with economies based on ranching and timber harvesting. With the improvement of area roads and communications in the twentieth century, more people became aware of the scenic splen dor of the county, and tourism and movie making began to increase, Kanab even be coming known as Utah's Little Hollywood during the heyday of filmmaking. Traditional extractive uses of the land's resources have declined in recent years, but the recent cre ation of the Grand Staircase-Escalante Na tional Monument has brought the promise of increased tourism to the area. It also has sparked opposition from many who had hoped for coal mining development in the region. Issues of control and uses of public lands promise to be debated vigorously as the county enters the new millenium. ISBN: 0-913738-40-9 A HISTORY OF cKgne County A HISTORY OF JOme County Martha Sonntag Bradley 1999 Utah State Historical Society Kane County Commission Copyright © 1999 by Kane County Commission All rights -
Water Resources-Reconnaissance
View of Spring Valley looking northwest from the town site of Osceola I I WATER RESOURCES- RECONNAISSANCE SERIES REPORT 33 I WATER RESOURCES APPRAISAL OF SPRING VALLEY, I WHITE PINE AND LINCOLN COUNTIES, NEVADA By I F. EUGENE RUSH Geologist and I S. A. T. KAZMI Geologist I Prepared Cooperatively by the I Geolagicai Survey, U.S. Department of Interior JULY 1965 I I I WATER RESOURCES - RECONNAISSANCE SERIES I Report 33 I I WATER RESOURCES APPRAISAL OF SPRING VALLEY, WHITE PINE AND LINCOLN COUNTIES, NEVADA I By I F. Eugene Rush Geologist I and S. A. T. Kazmi I Geologist I I I I I a I Prepared cooperatively by the Geological Survey, U. Sr Department of the Interior I September, 1965 I I I I CONTENTS Page I Summary 1 Introduction 2 i Purpose and scope of the study 2 , Location and general features 3 Previous work 3 I Climate 4 I Physiography and drainage 6 Numbering system for wells and springs 7 I General hydrogeologic features 7 I Geomorphic features 7 Lithologic and hydrologic features of the rocks 8 I Hydrology 9 I Precipitation 9 Surface water, by Donald O. Moore 12 I General conditions 12 I Estimated average annual runoff 14 Development 17 I Ground water 18 , Occurrence and movement 18 I Recharge 20 Discharge 22 I Evapotranspiration 22 I Springs 22 Subsurface outflow 24 I I",,,,' Contents - Continued I Page Discharge from wells 24 I Water budget 25 I Perennial yield 26 Storage 27 I Chemical quality of the water 27 , Suitability for agricultural use 27 Water quality and its relation to I the ground-water system 28 Development 29 I References cited 34 I List of previously published reports in this series 37 I I I I ,I I I I I I I TABLES Page I Table 1.