DOCSLIB.ORG

Hydrology and Simulation of Ground-Water Flow in Juab Valley, Juab County, Utah

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Hydrology and Simulation of Ground-Water Flow in Juab Valley, Juab County, Utah STATE OF UTAH DEPARTMENT OF NATURAL RESOURCES Technical Publication No. 114 HYDROLOGY AND SIMULATION OF GROUND-WATER FLOW IN JUAB VALLEY, JUAB COUNTY, UTAH By Susan A. Thiros, Bernard J. Stolp, Heidi K. Hadley, and Judy I. Steiger U.S. Geological Survey Prepared by the United States Geological Survey in cooperation with the Central Utah Water Conservancy District and the East Juab Water Conservancy District 1996 CONTENTS Abstract 1 Introduction I Purpose and scope....................... 4 Previous studies 4 Acknowledgments 4 Description of the study area 4 Geology 5 Climate g Hydrology......................................................................................................................................................... 11 Surface water 11 Streams 11 Distribution systems 16 Reservoirs......................... 18 Ground water 19 Occurrence.............................................................. 19 Recharge................................ 20 Seepage from streams...................... 20 Seepage from unconsumed irrigation water and distribution systems 20 Infiltration of precipitation 24 Subsurface inflow 24 Flow............................................................................................................................................. 25 Discharge..................................................................................................................................... 25 Wells 25 Springs and seeps.............................................................................................................. 2g Evapotranspiration 30 Subsurface outflow......... 30 Hydrologic properties.................................................................................................................. 30 Water-level fluctuations............................................................................................................... 34 Long-term fluctuations...................................................................................................... 34 Seasonal fluctuations........... 34 Chemical characteristics of water............ 41 Chemical composition 41 Isotopes........................................................................................................................................ 4g Geochemical analyses 50 Simulation of the ground-water system in the unconsolidated basin-fill deposits of Juab Valley................... 53 Model construction..................... 54 Discretization 54 Boundary conditions and data requirements 56 Recharge 57 Discharge.......................................................................................................................... 65 Hydrologic properties 72 Model calibration 73 Calibration parameters 73 Steady-state calibration g2 Transient-state calibration g5 Model sensitivity 93 Model limitations 96 iii CONTENTS-Continued Need for future study........................................................................................................................................ 97 Summary 98 References cited. 99 PLATE IPlate is in pocketI Plate 1. Map showing location of selected hydrologic-data sites and rock-sample site, Juab Valley, Utah, 1935-94 FIGURES 1. Map showing location of Juab Valley study area, Utah 2 2. Diagram showing numbering system used in Utah for hydrologic-data sites 3 3. Map showing generalized geology of the Juab Valley study area, Utah............................................ 6 4. Generalized cross section through the southern part of Juab Valley, Utah 9 5. Graphs showing annual precipitation and cumulative departure from the average annual precipitation, 1931-93, at Nephi, Utah............................................................................................... 10 6. Map showing discharge-measurement sites on Salt Creek, on selected irrigation canals and ditches, and in the West Creek area, Juab Valley, Utah 14 7. Graphs showing estimated average seepage gain or loss for reaches of Salt Creek and selected irrigation canals and ditches, Juab Valley, Utah................................................................................. 17 8. Map showing approximate potentiometric surface in unconsolidated basin-fill deposits in Juab Valley, Utah, March and April 1993 26 9. Map showing areal distribution of transmissivity estimated from specific-capacity values, slug tests, and aquifer tests for unconsolidated basin-fill deposits in Juab Valley, Utah 32 10. Hydrographs showing March or April water levels measured during 1942-94 in four wells in Juab Valley, Utah, and cumulative departure of the annual maximum water content of snow from the 1942-94 average at the Payson Ranger Station snow course 35 11. Hydrographs showing long-term water-level fluctuations during 1935-94 in eight wells in Juab Valley, Utah 36 12. Map showing approximate change in water levels in unconsolidated basin-fill deposits from March-April 1965 to March-April 1993 in Juab Valley, Utah 38 13. Hydrographs showing seasonal water-level fluctuations during 1993-94 in four wells in Juab Valley, Utah 40 14. Hydrographs showing seasonal water-level fluctuations during 1937-38, 1965-66, and (or) 1993-94 in four wells in Juab Valley, Utah........................................................................................ 42 15. Map showing dissolved-solids concentration in water from the Juab Valley study area, Utah, 1951-94 44 16. Graphs showing relation between specific conductance of water and streamflow at gaging stations on Salt Creek, Chicken Creek, and Currant Creek, Juab Valley, Utah 47 17. Graph showing relation between 0180 and oD values for water sampled from selected hydrologic-data sites in Juab Valley, Utah 49 18. Graph showing relation between log calcium and log sulfate activity for water sampled along the hypothesized Chicken Creek drainage flow path in Juab Valley, Utah 52 19. Map showing model grid and location of active cells in the ground-water flow model of Juab Valley, Utah ,.................................................... 55 20. Generalized geology and the four layers used in the ground-water flow model of Juab Valley, Utah 56 iv FIGURES-Continued 21. Graph showing depth from the estimated top of the saturated unconsolidated basin-fill deposits, the amount of 1963-93 average annual ground-water discharge to pumped wells in each depth interval, and corresponding model layers in the ground-water flow model of Juab Valley, Utah ..... 57 22-29. Maps showing: 22. Location of specified-flux boundary cells that simulate recharge from nonirrigation-season streamflow, unconsumed irrigation water and distribution-system losses, and irrigation­ season streamflow not included in the unconsumed irrigation water and distribution-system losses component in the ground-water flow model of Juab Valley, Utah.................................... 59 23. Location of specified-flux boundary cells that simulate recharge from subsurface inflow and seepage from ephemeral streams and discharge by subsurface outflow in the ground-water flow model of Juab Valley, Utah.................................................................................................. 66 24. Location of specified-flux boundary cells that simulate discharge to pumped wells in the ground-water flow model of Juab Valley, Utah 67 25. Location of head-dependent flux boundary cells that simulate discharge to flowing wells, springs, seeps, streams, and reservoirs in the ground-water flow model of Juab Valley, Utah... 69 26. Location of head-dependent flux boundary cells that simulate discharge by evapotranspiration in the ground-water flow model of Juab Valley, Utah 71 27. Final distribution of horizontal hydraulic conductivity for layers I through 3 of the ground- water flow model of Juab Valley, Utah........................................................................................ 76 28. Final distribution of transmissivity for layer 4 of the ground-water flow model of Juab Valley, Utah 78 29. Final distribution of vertical hydraulic conductivity for layers I through 4 of the ground- water flow model of Juab Valley, Utah........................................................................................ 81 30. Hydrographs showing water level in selected wells in Juab Valley, Utah 83 31. Map showing potentiometric surface for model layer 3 contoured from water levels computed from the steady-state simulation for 1949 and the difference between model-computed and measured water levels in observation wells, Juab Valley, Utah, March 1950................................... 84 32. Graph showing estimated annual ground-water discharge to pumped wells, length of stress periods, and average annual pumpage for each stress period of the multi-year transient-state simulation, Juab Valley, Utah............................................................................................................. 86 33. Hydrographs showing model-computed and measured water-level change in selected wells in Juab Valley, Utah, for the multi-year transient-state simulation 88 34. Map showing potentiometric surface for model layer 3 contoured from water levels computed from the transient-state simulation for 1964 and the difference between model-computed and measured water levels in observation wells, Juab Valley, Utah, March 1965................................... 90 35. Map showing potentiometric surface for model layer 3 contoured from water levels computed from the transient-state simulation for 1992 and the difference between model-computed and measured
Load more

Recommended publications
  • Nebo Overthrust, Southern Wasatch Mountains, Utah
    GEOLOGY I YOUNG STUDIES f UNIVERSITY Volume 12 December 1965 r' r' CONTENTS Thrusting in the Southern Wasatch Mountains, Utah ........ Michael J. Brady 3 Nebo Overthrust, Southern Wasatch Mountains, Utah ........ B. Allen Black 55 Paleoecologic implications of Strontium, Calcium, and Magnesium in Jurassic rocks near Thistle, Utah .... Button W. Bordine 91 Paleoecology of the Twin Creek Limestone In the Thistle, Utah area .................................... .... .....Ladell R. Bullock 121 Geolo of the Stockton stock and related intmsives, &1e County, Utah ................................................. John L. Lufkin 149 Stratigraphy and rifera of Ordovician rocks near Columbia Iceads, Jasper National Park, Alberta, Canada .............................................................. .. .... J. Keith Rigby 165 Lower Ordovician conodonts and other microfossils from the Columbia Icefields Section, Alberta, Canada ........................... .. .......... R. L. Ethington and D. L. Clark 185 Publications and maps of the Geology Department ........................... .. ..... 207 Brigham Young University Geology Studies Volume 12 - December 1965 Contents Thrusting in the Southern Wasatch Mountains, Utah ........ Michael J. Brady 3 Nebo Overthrust, Southern Wasatch Mountains, Utah ........ B. Allen Black 55 Paleoecologic irriplications of Strontium, Calcium, and Magnesium in Jurassic rocks near Thistle, Utah .... Burton W. Bordine 91 Paleoecology of the Twin Creek Limestone in the Thistle, Utah area ...................................................
    [Show full text]
  • Distribution of the Native Trees of Utah Kimball S
    Brigham Young University Science Bulletin, Biological Series Volume 11 | Number 3 Article 1 9-1970 Distribution of the native trees of Utah Kimball S. Erdman Department of Biology, Slippery Rock State College, Slippery Rock, Pennsylvania Follow this and additional works at: https://scholarsarchive.byu.edu/byuscib Part of the Anatomy Commons, Botany Commons, Physiology Commons, and the Zoology Commons Recommended Citation Erdman, Kimball S. (1970) "Distribution of the native trees of Utah," Brigham Young University Science Bulletin, Biological Series: Vol. 11 : No. 3 , Article 1. Available at: https://scholarsarchive.byu.edu/byuscib/vol11/iss3/1 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 Brigham Young University Science Bulletin, Biological Series by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. MU3. CCy.P. ZOOL. LIBRARY DEC 41970 Brigham Young University HARVARD Science Bulletin UNIVERSITY) DISTRIBUTION OF THE NATIVE TREES OF UTAH by Kimball S. Erdman BIOLOGICAL SERIES—VOLUME XI, NUMBER 3 SEPTEMBER 1970 BRIGHAM YOUNG UNIVERSITY SCIENCE BULLETIN BIOLOGICAL SERIES Editor: Stanley L. Welsh, Department of Botany, Brigham Young University, Provo, Utah Members of the Editorial Board: Tipton, Zoology Vernon J. Feeeon L. Anderson, Zoology Joseph R. Murdock, Botany WiLMER W. Tanner, Zoology Ex officio Members: A. Lester Allen, Dean, College of Biological and Agricultural Sciences Ernest L. Olson, Chairman, University Publications The Brigham Young University Science Bulletin, Biological Series, publishes acceptable papers, particularly large manuscripts, on all phases of biology. Separate numbers and back volumes can be purchased from Pubhcation Sales, Brigham Young University, Provo, Utah.
    [Show full text]
  • Ground Water in Utah's Densely Populated Wasatch Front Area the Challenge and the Choices
    Ground Water in Utah's Densely Populated Wasatch Front Area the Challenge and the Choices United States Geological Survey Water-Supply Paper 2232 Ground Water in Utah's Densely Populated Wasatch Front Area the Challenge and the Choices By DON PRICE U.S. GEOLOGICAL SURVEY WATER-SUPPLY PAPER 2232 UNITED STATES DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1985 For sale by the Branch of Distribution U.S. Geological Survey 604 South Pickett Street Alexandria, VA 22304 Library of Congress Cataloging in Publication Data Price, Don, 1929- Ground water in Utah's densely populated Wasatch Front area. (U.S. Geological Survey water-supply paper ; 2232) viii, 71 p. Bibliography: p. 70-71 Supt. of Docs. No.: I 19.13:2232 1. Water, Underground Utah. 2. Water, Underground Wasatch Range (Utah and Idaho) I. Title. II. Series. GB1025.U8P74 1985 553.7'9'097922 83-600281 PREFACE TIME WAS Time was when just the Red Man roamed this lonely land, Hunted its snowcapped mountains, its sun-baked desert sand; Time was when the White Man entered upon the scene, Tilled the fertile soil, turned the valleys green. Yes, he settled this lonely region, with the precious water he found In the sparkling mountain streams and hidden in the ground; He built his homes and cities; and temples toward the sun; But without the precious water, his work might not be done. .**- ste'iA CONTENTS Page Preface ..................................................... Ill Abstract ................................................... 1 Significance Ground water in perspective ................................ 1 The Wasatch Front area Utah's urban corridor ....................................
    [Show full text]
  • A History of Juab County, Utah Centennial County History Series
    A HISTORY OF fjuab County Pearl D. Wilson with June McNulty and David Hampshire UTAH CENTENNIAL COUNTY HISTORY SERIES A HISTORY OF JuaB County Pearl D. Wilson with June McNulty and David Hampshire luab County, one of Utah's earliest created counties, sits along the strategic north-south corridor of the state. Prehistoric and Native American Indian cultures roamed there, as did early Spanish priests and explorers, who left an important record of the area. Trappers and traders wandered the mountains and deserts that create stark contrasts in this geo­ graphically diverse county. Mark Twain, an early traveler through parts of luab, penned interesting insights of the county, which contained portions of the Pony Express and Overland Stage routes. Mormon pioneers arrived to establish farms and ranches. This was followed by the build­ ing of railroads and mineral exploration. Rail traffic for a vast region centered in Nephi, labeled "Little Chicago." To the west, the Tintic Mining District rose as one of Utah's richest gold and silver mining areas, attract­ ing a more ethnically diverse population. From majestic Mount Nebo to streams and lakes and the vast sand dunes of west Juab, the county contains many recreational possibili­ ties. Juab County is rich in history, geogra­ phy, and tradition; this book tells its story. ISBN: 0-913738-20-4 A HISTORY OF Juab County A HISTORY OF ffuaB County Pearl D. Wilson with June McNulty and David Hampshire 1999 Utah State Historical Society Juab County Commission Copyright © 1999 by Juab County Commission
    [Show full text]
  • Juab County, Utah Resource Assessment August 2005
    Juab County, Utah Resource Assessment August 2005 This resource assessment is designed to gather and display information specific to Juab County, Utah. This report will highlight the natural and social resources present in the county, detail specific concerns, and be used to aid in resource planning and target conservation assistance needs. This document is dynamic and will be updated as additional information is available through a multi-agency partnership effort. The general observations and summaries are listed first, followed by the specific resource inventories. Contents Observations and Summary Resource Concerns - Air, Plants, Animals Land Use Resource Concerns - Social and Economic Resource Concerns - Soils Survey Results Resource Concerns - Water Footnotes/Bibliography Introduction Juab County was formed in 1852, including portions of what is now Nevada. The size of the county was reduced in 1854 and 1856 along with various other changes through the years until the current borders were set. The first real settlement came in 1851 when Mormon pioneers settled Nephi. They relied mainly on agriculture for their livelihoods. In 1869, silver, gold, copper and other precious metals were discovered in the Tintic region. Many mining towns, such as Diamond, Silver City and Eureka popped up during this era. By 1899, it was considered to be one of the richest mining districts in the entire nation. Mining continued into the mid-1900's with the operations scaling down through the rest of the century. Area: 3,412 square miles; population: 5,817 (in 1990); county seat: Nephi; origin of county name: from the Ute word meaning flat or level plain; principal cities/towns: Nephi (3,515), Mona (584), Eureka (562), Levan (416); economy: agriculture, manufacturing, mining, recreation; points of interest: Historic Tintic Mining District, Little Sahara Recreation Area, Old Pony Express and Stage Route, Yuba Reservoir, Goshute Indian Reservation, Tintic Mining Museum in Eureka, Mount Nebo Wilderness Area, Fish Springs National Wildlife Refuge.
    [Show full text]
  • Utah Forest Insect and Disease Conditons Report 2002-2004
    Utah State University DigitalCommons@USU Quinney Natural Resources Research Library, The Bark Beetles, Fuels, and Fire Bibliography S.J. and Jessie E. 2005 Utah Forest Insect and Disease Conditons Report 2002-2004 K Matthews V DeBlander L Pederson P Mocettini D Halsey Follow this and additional works at: https://digitalcommons.usu.edu/barkbeetles Part of the Ecology and Evolutionary Biology Commons, Entomology Commons, Forest Biology Commons, Forest Management Commons, and the Wood Science and Pulp, Paper Technology Commons Recommended Citation Matthews, K., DeBlander, V., Pederson, L., Mocettini, P. and Halsey, D. (2005). Utah forest insect and disease conditons report 2002-2004. USDA Forest Service, State and Private Forestry, Forest Health Protection, Intermountain Region, R4-OFO-TR-05012, 58 pp. This Full Issue is brought to you for free and open access by the Quinney Natural Resources Research Library, S.J. and Jessie E. at DigitalCommons@USU. It has been accepted for inclusion in The Bark Beetles, Fuels, and Fire Bibliography by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. United States Department of Agriculture Forest Service Utah State and Private Forestry Forest Health Forest Insect and Disease Protection Intermountain Region Conditions Report R4-OFO-TR-05-12 2002 - 2004 State of Utah Department of Natural Resources Division of Forestry, Fire and State Lands Butterfly Lake, Mirror Lake Highway Darren Blackford, USFS. FOREST HEALTH SPECIALISTS Forest Health Protection
    [Show full text]
  • W9200094.Pdf
    STATE OF UTAH DEPARTt1EtJT OF tJATURAL RESOURCES Technical Publ ication No. 42 HYDROLOG IC RECOtJNA , SSANCE OF THE tWRTHERN GREAT SALT LAKE DESERT AND SUMMARY HYDROLOGIC RECONNAISSANCE OF NORTHWESTERN UTAH by Jerry C. Stephens, Hydrologist U. S. Geological Survey Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of ~ater Rights 1974 CONTENTS Page Abstract ...........................................•....................... Introduction ••••.•••.••••.••••••••••••••••••••••••••••••••••••••••••••••••• 2 Previous studies and acknowledgments ••••••.•••••••••••••••••••••••••••••••• 3 Hydrologic reconnaissance of the northern Great Salt Lake Desert............................................................ 7 Location and general features •••••••••••.•.••••••••••••••••••.•.•.. 7 Hydrology •••••••••• ................................................ 7 Surface water •• ................................................ 7 Ground water ••••••••••••••••••••••••••••••••••••••••••••••••••• 11 Shallow brine aquifer ••• ................................... 12 Alluvial-fan aquifer ••• .................................... 16 Valley-fill aquifer 20 ot he r aqui fer 5 ••••••••••••••••••••••••••••••••••• 22 Discussion of recharge and discharge estimates ••••••••••••• 23 ~"a te r qua litY••••••• ........................................... 23 Potential for additional water-resources development •• 26 Summary of hydrology of northwestern Utah •••••••••••••••••••••••••••••••••• 26 Surface water .................•..•................................
    [Show full text]
  • County Grants Easement to Transwest After Concerns Are Allayed
    Serving East Juab County - A Nice Place To Live! Volume 117, No. 13 March 27, 2019 Single Copy Price $100 Water from aquifers in Nephi and Mona most likely mix underground By Myrna Trauntvein Times-News Correspondent Does the water from the aquifers in Nephi and Mona mix underground? It is likely that they do be- cause of data from a 1996 study entitled: “Hydrology and Simu- lation of Ground-Water Flow in Juab Valley, Juab County, Utah.” The study was filed with the State of Utah Department of Natural Resources as Techni- cal Publication No. 114 and was written by Susan A. Thi- ros, Bernard J. Stolp, Heidi K. Hadley and Judy I. Steiger and was prepared by the Unit- ed States Geological Survey in cooperation with the Central Utah Water Conservancy Dis- trict and the East Juab Water Conservancy District and is 113 pages long including maps and charts. MONA RESERVOIR ON THE FIRST DAY OF SPRING • This photo taken last Wednesday, the fi rst day of Spring, shows Mount Nebo in “Water discharging from a all it’s winter glory. refl ected in the water of Mona Reservoir as it fi lls during the runoff from this winter’s storms. Photo Mike Davis spring at Burraston Ponds is a mixture of about 70 percent ground water from a hypoth- esized flow path that extends Mona City offi cials want questions answered about down gradient from where Salt Creek enters Juab Valley and 30 percent from a hypothesized Houweling’s operations and plans for the future flow path from the base of the By Myrna Trauntvein man camp and not single fam- toes is projected to pay in the dressed.
    [Show full text]
  • LCC DEIS Chapter 13 – Ecosystem Resources
    Chapter 13: Ecosystem Resources 13.1 Introduction This chapter describes the ecosystem resources, habitat types, and What is the ecosystem wildlife species in the ecosystem resources impact analysis area and how resources impact analysis these resources would be directly and indirectly affected by the project area? alternatives. The ecosystem resources impact Ecosystem Resources Impact Analysis Area. The ecosystem analysis area extends along resources impact analysis area extends along State Route (S.R.) 210 S.R. 210 from its intersection from its intersection with S.R. 190/Fort Union Boulevard in Cottonwood with S.R. 190/Fort Union Boule- vard in Cottonwood Heights to its Heights to its terminus in the town of Alta, including the Alta Bypass Road terminus in the town of Alta, (for a graphic depiction of the impact analysis area, see Figure 13.3-1, including the Alta Bypass Road. Wildlife Habitat Types in the Ecosystem Resources Impact Analysis Area, It also includes the area around on page 13-7). It also includes the area around the gravel pit adjacent to the gravel pit and the existing Wasatch Boulevard north of Fort Union Boulevard and the existing park- park-and-ride lot at 9400 South and-ride lot at 9400 South and Highland Drive. For wildlife habitat, the and Highland Drive. For wildlife habitat, the impact analysis area impact analysis area includes the entirety of Little Cottonwood Canyon. includes the entirety of Little The areas adjacent to Wasatch Boulevard, the gravel pit, and the park- Cottonwood Canyon. and-ride lot are primarily residential and commercial developments. From North Little Cottonwood Road through the town of Alta, the impact analysis area includes the wildlife, vegetation, and aquatic resources present in addition to a mix of residential and commercial (ski resort) development.
    [Show full text]
  • This Report Is Preliminary and Has Not Been Reviewed for Conformity with the U.S
    DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY NEW INFORMATION RESOURCES OF THE U.S. GEOLOGICAL SURVEY LIBRARY SYSTEM NUMBER 36 Apri1 1989 OPEN-FILE REPORT 89-400-D This report is preliminary and has not been reviewed for conformity with the U.S. Geological Survey editorial standards 1989 Main PAGE American mines handbook. Toronto : Northern Miner Press Ltd., / c!989- S(099) Am437 Geologic map of the Thatcher Mountain quadrangle, Box Elder County, Utah. Salt Lake City, Utah : Utah Geological and Mineral Survey, 1988. M(273)2 T324J Geologic map of the Black Hills area, South Dakota and Wyoming. Reston, Va. : U.S. Geological Survey, 1989. M(200) I no. 1910 Geological fieldwork 1988 : a summary of field activities and current research. Victoria, B.C. : Ministry of Energy, Mines and Petroleum Resources, [1989] 402(180) B777p no.1989-1 Mineral investigations resource map. Washington, D.C. : United States Geological Survey, 1952- M(200) MR Mineral resource assessment map of the Healy quadrangle, Alaska. Reston, Va. : U.S. Geological Survey, 1989. M(200) MF no.2058-A Mineral resources of the central part of the Independence mining district, Park and Sweet Grass Counties, Montana / by Phillip R. Moyle ... [et al.]. Spokane, Wash. : Western Field Operations Center, U.S. Dept. of the Interior, Bureau of Mines, [1989] 402(200) Un34msi no.89-4 Mining in Ecuador. Quito : The Institute. 420(465) qM664 Road log of the Chatham, Randolph and Orange County areas, North Carolina : annual meeting, Carolina Geological Society, November 7-8, 1964. Raleigh : The Society, [1964] G(231) qC22g 1964 SMSS technical monograph.
    [Show full text]
  • Commemorative Booklet
    SEVENTY YEARS OF OHIO STATE UNIVERSITY GEOLOGY IN SANPETE VALLEY, UTAH Ohio State University School of Earth Sciences Columbus, Ohio June 2017 View to northwest from edge of Wasatch Plateau, showing Ephraim, Sanpete Valley, San Pitch Mountains, with Mt Nebo in the distance. [T. Wilson] SEVENTY YEARS OF OHIO STATE UNIVERSITY GEOLOGY IN SANPETE VALLEY, UTAH Ohio State University School of Earth Sciences 70th Geology Field Camp Commemorative Booklet Columbus, Ohio June 2017 [Recall] the fable of Antaeus, the famous giant of antiquity, who was invincible, as long as he had his feet on the ground. But let him be lifted ever so little off the ground, as he was later by Hercules, and his strength vanished, and he was helpless. We geologists, my friends, are exactly in the position of Antaeus. The only thing that has not changed one iota, not only in the sixty years of my own observation, but in the whole nearly 200 years of geology itself, is the vital necessity for field work. … As we push forward, let us ever keep it in mind, like Antaeus, we must forever keep our feet firmly planted on the ground! Edmund M. Spieker, March 20, 1972, addressing faculty and graduating students on the occasion of the departmental celebration of his receiving an honorary Doctor of Science degree from The Ohio State University Ed Spieker, Summer 1963. Photo courtesy S. Zahoni i CONTENTS Introduction…………………………………………………………………………………………………………………………………………………..1 History Significant Dates for Ohio State University Summer Field Geology Courses (1947-2017)………………………………..4
    [Show full text]
  • Geology of the North Canyon Area, Southern Wasatch Mountains, Utah
    NmG UNIVERSITY RESEARCH STUDIES Geology Series Vol. 3 No. 7 July, 1956 GEOLOGY OF THE NORTH CANYON AREA, SOUTHERN WASATCH MOUNTAINS, UTAH by Cleon V. Smith Brigham Young University Departmerit of Geology Pmvo, Utah GEOLOGY OF THE NORTH CANYON AREA, SOUTHERN WASATCH MOUNTAINS, UTAH A thesis submitted to the Faculty of the Department of Geology Br igham Young Univer s ity in partial fulfillment of the requirements for the degree Master of Science by Cleon V. Smith August, 1956 ACKNOWLEDGEMENTS 1' - The writer gratefully acknowledges the assistance of Dr, Harold J. Bissell for help in field work and checking the manuscript, Dr. George H. Hansen for applying ground water information and well logs and Professor Jess R. Bushman for checking the writer's manuscript. The writer is indebted to Dell R. Foutz, for his help in field work and to his brother, Grant B. Smith, for field assistance, The writer expresses sincere appreciation to his wife, Meridee, for her encouragement and cooperation. iii TABLE OF CONTENTS Page ACKNOWLEDGEMENTS . iii LIST OF ILLUSTRATIONS . vi ABSTRACT. .. vii Location and accessibility . 1 Physical features - 1 Field work and laboratory studies . 2 Previous work. 2 GENERAL GEOLOGY Principal features . 3 Sedimentary Rocks . 6 Precambrian System . 6 Big Cottonwood series . 6 Cambrian System. Tintic quartzite . Ophir formation . Teutonic limestone . Dagmar limestone . Herkimer lime stone . Bluebird dolomite . Cole Canyon dolomite . Opex dolomite . Ordovician System 14 Ajax limestone (?) 14 Unconformity at Base of Mississippian . 15 Mississippian System . 15 Gardner dolomite . 15 Pine Canyon limestone . 17 Humbug formatign 19 Quaternary System 19 Landslides . 19 Fans - 19 Alluvium . 21 Igneous Rocks .
    [Show full text]