DOCSLIB.ORG

Evaluation of the Ground-Water Flow Model for Northern Utah Valley, Utah, Updated To

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Evaluation of the Ground-Water Flow Model for Northern Utah Valley, Utah, Updated To Evaluation of the Ground-Water Flow Model for Northern Utah Valley, Utah, Updated to Conditions through 2002 r e v Riverton i Salt Draper R Lake Valley eek Cr Dry 15 Jordan Alpine Mountains River Fork Highland American Traverse W Camp asatch Williams Cedar Hills Northern American Mt Timpanogos Utah 11,750 feet Eagle Lehi Fork Mountain Valley 89 Pleasant Grove Saratoga Springs River Lindon Provo Range Vineyard Orem Cedar Valley Mountains Provo Utah Lake Lake Provo Bay Springville Hobble 15 Creek Spanish Spanish Fork Fork est River W Mountain 89 Scientific Investigations Report 2006–5064 Prepared in cooperation with the Central Utah Water Conservancy District; Jordan Valley Water Conservancy District representing Draper City; Highland Water Company; Utah Department of Natural Resources, Division of Water Rights; and the municipalities of Alpine, American Fork, Cedar Hills, Eagle Mountain, Highland, Lehi, Lindon, Orem, Pleasant Grove, Provo, Saratoga Springs, and Vineyard U.S. Department of the Interior U.S. Geological Survey Cover: View looking east toward American Fork Canyon in Utah County, Utah, March 2004. Evaluation of the Ground-Water Flow Model for Northern Utah Valley, Utah, Updated to Conditions through 2002 By Susan A. Thiros Prepared in cooperation with the Central Utah Water Conservancy District; Jordan Valley Water Conservancy District representing Draper City; Highland Water Company; Utah Department of Natural Resources, Division of Water Rights; and the municipalities of Alpine, American Fork, Cedar Hills, Eagle Mountain, Highland, Lehi, Lindon, Orem, Pleasant Grove, Provo, Saratoga Springs, and Vineyard Scientific Investigations Report 2006–5064 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Salt Lake City, Utah: 2006 For additional information write to: U.S. Geological Survey Director, USGS Utah Water Science Center 2329 W. Orton Circle Salt Lake City, UT 84119-2047 Email: [email protected] URL: http://ut.water.usgs.gov/ For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS--the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. iii Contents Abstract ............................................................................................................................................................ 1 Introduction...................................................................................................................................................... 1 Purpose and Scope ............................................................................................................................... 3 Description of the Study Area ............................................................................................................. 3 Ground-Water Hydrology ..................................................................................................................... 3 Description of the Model ............................................................................................................................... 5 Update of the Model to Conditions through 2002 ...................................................................................... 8 Performance of the Updated Model ........................................................................................................... 8 Potential Revisions and New Data to Improve the Updated Model .................................................... 15 Summary......................................................................................................................................................... 19 References Cited........................................................................................................................................... 19 Figures Figure 1. Location of northern Utah Valley study area, Utah. ..................................................................... 2 Figure 2. Generalized block diagram showing the basin-fill deposits and ground-water system in northern Utah Valley, Utah. .............................................................................................................. 4 Figure 3. Grid for the model of the ground-water system in northern Utah Valley, Utah ...................... 6 Figure 4. Location of cells simulating recharge and discharge in the model of the ground-water system in northern Utah Valley, Utah. ............................................................................................ 7 Figure 5. Specified ground-water discharge from wells in the updated model of the ground-water system in northern Utah Valley, Utah, 1947–2002. ........................................................................ 9 Figure 6. Location of cells simulating flowing and pumping wells in 1981 and 2002 in the updated model of the ground-water system in northern Utah Valley, Utah. ......................................... 10 Figure 7. Annual streamflow in the American Fork and Provo Rivers and specified recharge to the ground-water system in the updated model of northern Utah Valley, Utah, 1947–2002. ......................................................................................................................................... 11 Figure 8. Location of wells with measured and computed water-level changes in the updated model of the ground-water system in northern Utah Valley, Utah. ......................................... 12 Figure 9. Measured water-level change for selected wells during 1981–2003 and computed water-level change for the corresponding model cell and layer in the updated model of the ground-water system in northern Utah Valley, Utah. ..................................................... 13 Figure 10. Computed water-level decline from the end of 1980 to the end of 2001 in layer 5 of the updated model of the ground-water system and measured water-level decline from March 1981 to March 2002 at 14 wells that correspond to layer 5 in northern Utah Valley, Utah ....................................................................................................................................... 16 Figure 11. Measured water-level altitude for selected wells during 1981–2003 and computed water-level altitude for the corresponding cell and layer in the updated model of the ground-water system in northern Utah Valley, Utah. ................................................................ 17 Figure 12. Simulated and specified ground-water recharge and discharge in the updated model of the ground-water system in northern Utah Valley, Utah, 1947–2002.................................. 18 iv Table Table 1. Conceptual ground-water budget for the basin-fill aquifer system in northern Utah Valley, Utah ........................................................................................................................................ 4 Conversion Factors and Datums Multiply By To obtain Length foot (ft) 0.3048 meter (m) mile (mi) 1.609 kilometer (km) Area square mile (mi2) 2.590 square kilometer (km2) Volume acre-foot (acre-ft) 1,233 cubic meter (m3) Flow rate acre-foot per year (acre-ft/yr) 1,233 cubic meter per year (m3/yr) Vertical coordinate information is referenced to the North American Vertical Datum of 1929 (NAVD 29). Horizontal coordinate information is referenced to the North American Datum of 1983 (NAD 83). Altitude, as used in this report, refers to distance above the vertical datum. Evaluation of the Ground-Water Flow Model for Northern Utah Valley, Utah, Updated to Conditions through 2002 By Susan A. Thiros Abstract The ability of the model to adequately simulate cli- matic extremes such as the wetter-than-normal conditions of This report evaluates the performance of a numerical 1982–84 and the drier-than-normal conditions of 1999–2002 model of the ground-water system in northern Utah Valley, indicates that the annual variation of recharge to the ground- Utah, that originally simulated ground-water conditions during water system based on streamflow entering the valley, which 1947–1980 and was updated to include conditions estimated in turn is primarily dependent upon precipitation, is appropri- for 1981–2002. Estimates of annual recharge to the ground- ate but can be improved. The updated transient-state model water system and discharge from wells in the area were added of the ground-water system in northern Utah Valley can be to the original ground-water flow model of the area. improved by making revisions on the basis of currently avail- The files used in the original transient-state model able data and information. of the ground-water flow system in northern Utah Valley were imported into MODFLOW-96, an updated version of MODFLOW. The main model input files modified as part of Introduction this effort were the well and recharge files. Discharge from pumping wells in northern Utah Valley was estimated on an Ground water is the primary source of drinking water in annual
Load more

Recommended publications
  • Characterization of Hydrogeological Properties in Salt Lake Valley, Utah, Using Insar
    Journal of Geophysical Research: Earth Surface RESEARCH ARTICLE Characterization of Hydrogeological Properties 10.1029/2017JF004497 in Salt Lake Valley, Utah, using InSAR Key Points: Xie Hu1 , Zhong Lu1 , and Teng Wang2 • Time series ground deformation over Salt Lake Valley (Utah) has been 1Huffington Department of Earth Sciences, Southern Methodist University, Dallas, TX, USA, 2Earth Observatory of Singapore, obtained from satellite InSAR data • Long-term and seasonal deformation Nanyang Technological University, Singapore observations, and hydrological records help characterize hydrogeological properties Abstract Charactering subsurface aquifer systems is important not only to managing their long-term • Deformation maps and decay viability as a stable water source but also to protecting the residences and infrastructures. In particular, coefficients suggest that surface understanding how aquifer skeletons deform in response to hydraulic head changes requires fl faults disturb groundwater ow and fi fi partition hydrological units hydrogeological parameters such as decay coef cient, storage coef cient, and bulk compressibility. Quantifying these key aquifer properties often requires the analysis of limited water gauge and drilling data. Here we investigate the spatiotemporal correlation between the vertical ground deformation derived by Supporting Information: • Supporting Information S1 ENVISAT Advanced Synthetic Aperture Radar (ASAR) and Sentinel-1A data sets and available hydrological records in order to improve the aquifer characterization under Salt Lake Valley, Utah. Interferometric Correspondence to: synthetic aperture radar results show a clear long-term and seasonal correlation between surface X. Hu, uplift/subsidence and groundwater recharge/discharge, with evidence for the net uplift of 15 mm/year of an [email protected] area southwest of Salt Lake City for six years.
    [Show full text]
  • An Integrated Geophysical and Geologic Study of the Paleogene- Age Volcanic Body and Possible Landslide Deposit on the South Slope of the Traverse Mountains, Utah
    Brigham Young University BYU ScholarsArchive Theses and Dissertations 2011-12-08 An Integrated Geophysical and Geologic Study of the Paleogene- Age Volcanic Body and Possible Landslide Deposit on the South Slope of the Traverse Mountains, Utah John C. Hoopes Brigham Young University - Provo Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Geology Commons BYU ScholarsArchive Citation Hoopes, John C., "An Integrated Geophysical and Geologic Study of the Paleogene-Age Volcanic Body and Possible Landslide Deposit on the South Slope of the Traverse Mountains, Utah" (2011). Theses and Dissertations. 2866. https://scholarsarchive.byu.edu/etd/2866 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. An Integrated Geophysical and Geologic Study of the Paleogene-age Volcanic Body and Possible Landslide Deposit on the South Slope of the Traverse Mountains, Utah John C. Hoopes A thesis submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Master of Science Department of Geological Sciences Brigham Young University December 2011 John H. McBride, Chair Eric H. Christiansen Bart J. Kowallis Copyright © 2011 John C. Hoopes All Rights Reserved ABSTRACT An Integrated Geophysical and Geologic Study of the Paleogene-age Volcanic Body and Possible Landslide Deposit on the South Slope of the Traverse Mountains, Utah John C. Hoopes Department of Geological Sciences Master of Science Development of homes, roads, and commercial buildings in northern Utah has grown significantly during the last several decades.
    [Show full text]
  • Stratigraphy and Microfaunas of the Oquirrh Group in the Southern East ...Tintic Mountains, Utah
    Stratigraphy and Microfaunas of the Oquirrh Group in the Southern East ...Tintic Mountains, Utah G E 0 L 0 G I C A L S U R V E Y P R 0 F E S S I 0 N A L P A P E R 1025 Stratigraphy and Microfaunas of the Oquirrh Group in the Southern East rrintic Mountains, Utah By H. T. MORRIS, R. C. DOUGLASS, and R. W. KOPF G E 0 L 0 G I CAL S lJ R V E Y P R 0 FE S S I 0 N A L PAP E R 1025 U N I T E D S T A T E S G 0 V E R N M E N T P R I N T I N G 0 F F I C E , WAS H I N G T 0 N : 1977 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Main en try under title: Morris, Hal Tryon, 1920- Stratigraphy and microfaunas of the Oquirrh Group in the southern East Tintic Mountains, Utah. (Geological Survey Professional Paper 1025) Bibliography: p. 20-22. 1. Geology, Stratigraphic--Pennsylvanian. 2. Geology, Stratigraphic--Permian. 3. Micropaleontology-­ Utah--Tintic Mountains. 4. Geology--Utah--Tintic Mountains. I. Douglass, Raymond Charles, joint author. II. Kopf, Rudolph William. III. Title. IV. Series: United States. Geological Survey. Professional Paper 1025. QE673.M67 551.7'52 77-10492 For -,ale by the Superintendent of Documents, U.S. GoYernment Printing Office \Vashington, D.C.
    [Show full text]
  • Upper Paleozoic Rocks in the Oquirrh Mountains and Bingham Mining District, Utah
    Upper Paleozoic Rocks in The Oquirrh Mountains and Bingham Mining District, Utah GEOLOGICAL SURVEY PROFESSIONAL PAPER 629 - A Upper Paleozoic Rocks in The Oquirrh Mountains and Bingham Mining District, Utah By E. W. TOOKER and RALPH J. ROBERTS with a section on BIOSTRATIGRAPHY AND CORRELATION By MACKENZIE GORDON, JR. and HELEN M. DUNCAN GEOLOGIC STUDIES OF THE BINGHAM MINING DISTRICT, UTAH GEOLOGICAL SURVEY PROFESSIONAL PAPER 629-A A study of the structures, the lithologic successions, and the fossils of two sequences of rocks of the same age that are juxtaposed by thrust faults UNITED STATES GOVERNMENT PRINTING, OFFICE, WASHINGTON: 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress Catalog Card No. 73-607760 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Price $1 (paper cover) CONTENTS Page Psge Abstract _________________________ Al Biostratigraphy and correlation of the Oquirrh Group and related rocks in the Oquirrh Mountains, Utah, Introduction _________________________ 1 by Mackenzie Gordon, Jr., and Helen M. Duncan __ A38 Acknowledgments ______________________ 2 Rogers Canyon sequence _ _ 39 Geologic setting _____________________ 2 Green Ravine Formation ____________ 40 Previous terminology and recommended changes 5 Lake Point Limestone ______________"_ 42 Revised upper Paleozoic stratigraphy __________ 9 Erda Formation __________________ 46 Kessler Canyon Formation ___________ 48 Rogers Canyon
    [Show full text]
  • Valleys of Utah Lake and Jordan River, Utah
    Water-Supply and Irrigation Paper No. 157 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DlKKCTOK UNDERGROUND WATER IN THE VALLEYS OF UTAH LAKE AND JORDAN RIVER, UTAH BY G. B. RICHARDSON WASHINGTON GOVERNMENT PRINTING OFFICE 1906 CONTENTS. Page. Introduction.......................... 5 Topography and drainage.............. 5 Geology.............................. 7 Literature........................ Descriptive geology of the highlands Late geologic history.............. 11 Tertiary..................... 11 Quaternary.................... 11 Climate.............................. 13 Precipitation.. 14 Temperature.. 15 Wind velocity. 16 Humidity..... 16 Evaporation-.. 17 Summary..... 17 Hydrography...... 18 Streams tributary to Utah Lake and Jorc an River. 18 Utah Lake.................... 23 Jordan River.................. 24 Great Salt Lake................ 25 Underground water.................. 27 General conditions............. 27 Source.................... 27 Distribution............... 29 Quality................... 30 Recovery................. 35 Suggestions................. 38 Occurrence.................... 38 West of Jordan .River........ 38 Divisions of area....... 38 Upland area............ 39 Lowland area.......... 41 East of Jordan River........ 43 Salt Lake City......... 43 South of Salt Lake City. 45 Utah Lake Valley........... 48 Lehi and vicinity. 48 American Fork, Pleasant Grove, and vicinity. 49 Provo and vicinity....... i- 51 Springville and vicinity... 52 Spanish Fork, Payson, and vicinity.
    [Show full text]
  • History of the Uinta National Forest
    History of the Uinta National Forest A Century of Stewardship United States Forest Uinta National Provo, Department of Service Forest Utah Agriculture History of the Uinta National Forest A Century of Stewardship Editor: Shaun R. Nelson Contributions By: Loyal Clark Stephanie Hall Rebecca Hirschi Peter Karp Bevan Killpack Lola Murray Debra Tatman Charmaine Thompson Cover photos, clockwise from upper left: Silver Lake Reservoir with Mount Timpanogos in the background, Dan Gull and A. Taylor looking over Ray’s Valley reseeding, 1951, Boy Scouts volunteering at Tibble Fork Reservoir, and Provo Peak Watershed Project meeting at the mouth of Slate Canyon, 1935. Copyright 1997 Uinta National Forest Forward We have no way of knowing who first named the area called the Uinta National Forest. We do know that the word “Uinta” comes from a Native American word meaning “pine tree” or “pine forest.” The forested areas, wonderful streams, meadows, striking mountains and rock formations, along with the native wildlife, fish and plants make this National Forest one of the finest lands that we have in our entire country! We expect the early inhabitants relied very heavily on the natural resources that were produced on the Uinta. Their lives depended on the wild animals, fish, plants, and clean water that came from the Uinta. Products from the Forest were undoubtedly used for clothing, shelter, and heat for warmth and cooking. While little is known about the early people’s use of the Forest, much more is known about the settlers that moved here from the East. These people were very dependent on forest resources to carve out a settlement suitable for their needs.
    [Show full text]
  • Geology Utah of the Mountains
    Geology of the Oquirrh Mountains, Utah by Edwin W. Tooker Open-File Report OF 99-571 1999 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Menlo Park, CA, CONTENTS Page Abstract 7 Introduction 11 Purpose of the report 11 Location, geomorphic features, and access 13 Acknowledgments 15 Geologic setting of north-central Utah 17 Precambrian basement terrane and the Uinta trend 17 Paleozoic depositional basins 20 Jurassic orogeny 22 Cretaceous Sevier orogeny 23 Formation of the Cenozoic Basin and Range province 24 Tertiary igneous activity and ore deposits 25 Uplift in the Oquirrh Mountains along the Uinta trend during the period of igneous activity 26 Quaternary uplift and Pleistocene glaciation 27 Recognition of nappes in the Oquirrh Mountains . 27 Location of the Oquirrh Mountains nappes . 28 Hinterland source of the nappes 29 Movement of the nappes 29 Convergence of nappes in the area of the future Oquirrh Mountains 30 Stratigraphic features of the main nappes 31 Pass Canyon nappe 32 Bingham nappe 33 Rogers Canyon nappe 34 Significance of variations in nappe sedimentary rocks 35 Structural features of nappes 35 Main and secondary folds 36 Faults 37 Sole and imbricate thrusts 37 Tanscurrent or tear faults 38 Tensional and other normal faults of thrust origin 39 Basin and Range normal faults 39 Igneous rocks associated with the nappes 40 Geology, correlation, and economic importance of typical nappe rocks in the Oquirrh Mountains 41 Pass Canyon nappe 42 Stratigraphic characteristics and correlation of sedimentary rocks 44 Dry Fork unit of looker and Roberts (1988) 45 Flood Canyon unit of looker and Roberts (1988) 46 __ _ _ _ _ _ _________ - _ - __ - ___ __ _ _ ____ _____________ ___ _ ______ ___ A*7__j.
    [Show full text]
  • Murray City's Code Banning Pet Stores
    John E. Eining Chiei Murray City's Code Banning Pet Stores Excellence I::; Our Standarcl (BO l I 57"6-(dilO I 1020 E P1r1111 '1·r Roc1d I l)r;ip1'r, UT 84tl20 ORDINANCE NO. --- AN ORDINANCE ENACTING SECTION 6.16.070 OF THE MURRAY CITY MUNICIPAL CODE RELATING TO THE SALE OF DOGS, CATS, AND RABBITS AT PET SHOPS, RETAIL BUSINESSES, OR OTHER COMMERCIAL ESTABLISHMENTS WITHIN MURRAY CITY. PREAMBLE Pet stores, retail businesses, and other commercial establishments selling live animals have traditionally been a sales outlet for young dogs, cats, and rabbits bred in substandard breeding facilities often referred to as "puppy mills", "kitten mills", and "rabbit mills" which mass-produce animals for sale to the public. Animals born and raised at these types of facilities are often subjected to: over­ breeding and inbreeding; minimal to non-existent veterinary care; lack of adequate food, water, and shelter; lack of socialization; lack of adequate space; and the euthanization of unwanted animals. The inhumane conditions in facilities such as these may lead to health and behavioral issues in those animals, which many consumers are unaware of when purchasing animals. These health and behavioral issues, which may not present themselves until years after the purchase of the animals, can impose exorbitant financial and emotional costs on consumers. The Murray City Municipal Council believes that regulating the retail sale of dogs, cats, and rabbits within the City will promote community awareness of animal welfare, and , in turn, will foster a more humane environment in the City. These regulations will also reduce impulse purchases of pets, which can lead to abandonment or mistreatment of the animals once they have outgrown their initial appeal, as well as reduce the costs of sheltering and euthanizing unwanted problem pets.
    [Show full text]
  • Nature and Origin of the East Traverse Mountains Mega-Landslide, Northern Utah (USA)" (2020)
    Brigham Young University BYU ScholarsArchive Theses and Dissertations 2020-12-11 Nature and Origin of the East Traverse Mountains Mega- Landslide, Northern Utah (USA) Rodney Ryan Chadburn Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Physical Sciences and Mathematics Commons BYU ScholarsArchive Citation Chadburn, Rodney Ryan, "Nature and Origin of the East Traverse Mountains Mega-Landslide, Northern Utah (USA)" (2020). Theses and Dissertations. 8771. https://scholarsarchive.byu.edu/etd/8771 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Nature and Origin of the East Traverse Mountains Mega-Landslide, Northern Utah (USA) Rodney Ryan Chadburn A thesis submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Master of Science Jeffrey D. Keith, Chair Eric H. Christiansen Ron A. Harris Department of Geological Sciences Brigham Young University Copyright © 2020 Rodney Ryan Chadburn All Rights Reserved ABSTRACT Nature and Origin of the East Traverse Mountains Mega-Landslide, Northern Utah (USA) Rodney Ryan Chadburn Department of Geological Sciences, BYU Master of Science The East Traverse Mountains are an E-W trending mountain range dividing Utah and Salt Lake valleys in northern Utah. Geologically perplexing, the nature of the East Traverse Mountains has been under investigation for 140 years. Previously, the mountain range was proposed to be a dismembered but still coherent down-faulted block that experienced 4 km of post-thrusting extension within the Charleston-Nebo thrust sheet.
    [Show full text]
  • The Point of the Mountain Phase Two Extended Report
    The Point of the Mountain Phase Two Extended Report 1 The Point of the Mountain Phase Two Extended Report Extended Report Contents Introduction to the Process 3 Phase One 4 Phase Two 6 Scenario Overview 7 The Scenarios Across 8 Topics • Jobs & Economy 10 • Transportation 14 • Community Design 22 • Air Quality 26 • Recreation 29 • Entertainment 31 • Water & Wildlife 33 • Prison Redevelopment 35 Appendix • Consultant Reports and Data A1 • Commission Presentations B1 • Public Meeting Notes C1 • Public Comments D1 2 The Point of the Mountain Phase Two Extended Report Introduction to the Process In the 2016 Legislative Session, the Utah State Legislature passed House Bill 318, which established the Point of the Mountain Development Commission and served as a formal starting point for a process to explore possibilities for the future of the Point of the Mountain through community outreach and expert collaboration. The bill outlines six objectives for the project area and the state as a whole: • maximizing job creation; • ensuring a high quality of life for residents in and surrounding the project area; • strategic residential and commercial growth; • preservation of natural lands and expansion of recreational opportunities; • provision of a variety of community and housing types that match workforce needs; • planning for future transportation infrastructure and other investments to enhance mobility and protect the environment. 3 The Point of the Mountain Phase Two Extended Report Phase One On behalf of the Point of the Mountain Development Commission, the consultant team spent significant time and resources during Phase 1 of the project to compile feedback from industry experts, stakeholders, and the public to create a proposed aspirational vision of what the area could be.
    [Show full text]
  • The March 16 1992 Magnitude 4.2 Western Traverse Mountains
    THE MARCH 16, 1992 ML 4.2 WESTERN TRAVERSE MOUNTAINS EARTHQUAKE, SALT LAKE COUNTY, UTAH compiled by Gary E. Christenson Utah Geological Survey \ , . 1 (j KM ••. 50' .fl. ~ I '., , , ,e, e , , , • I~ • &. ~ • •• 0 ~\ \ •••• •• • ,1.J • • {~., .. ~ •• "It "': ..... 1, ••••• o .It • • \ • 40' ,""j . '\.~ (e: :r~ o 30'. .......o. • ' ML4.2 • ~ ~·•• o 3/16/92 Q) ·.,,0•• --.•• • • ·1 • • "It • • o • . • . 10 · 50' 40 · OPEN-FILE REPORT 255 October ~ UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES This open-file release makes information available to the public which will not appear in another published form but is col)Sidered to be of value. It may not necessarily conform to formal VOS policy, technical review, or editorial standards, and therefore it may be premature for an individual or group to take action based on the contents of this report. STATE OF UTAH Norman H. Bangerter, Governor DEP ARTMENT OF NATURAL RESOURCES Dee C. Hansen, Executive Director UT AH GEOLOGICAL SURVEY M. Lee Allison, Director Board Member Representing Kenneth R. Poulson, Chainnan ................................ Mineral Industry Lawrence Reaveley ........................................ Civil Engineering Jo Brandt ............................................... Public-at-wge Samuel C. Quigley ......................................... Mineral Industry Russell C. Babcock, Jr. ..................................... Mineral Industry Jerry Golden ............................................. Mineral Industry Milton E. Wadsworth ...................................
    [Show full text]
  • Traverse Mountains From: Utah Place Names
    Traverse Mountains from: Utah Place Names TRAVERSE MOUNTAINS (Salt Lake County). The name reflects the east-west orientation instead of the usual north-south orientation. The Jordan River cuts through the Traverse Mountains at the Point of the Mountain, from Utah Lake into the Great Salt Lake. >T4S,R1W,SLM; 6,331' (1,930m). EXPLANATION OF SYMBOLS... 1. An asterisk (*) following a place name indicates past or present inhabitation. 2. When a series of letters and numbers are present towards the end of an entry after the ">" symbol, the first group indicates section/township/range as closely as can be pinpointed (i.e., S12,T3S,R4W,SLM, or USM). A section equals approximately one square mile, reflecting U.S. Geological Survey topographic map sections. Because Utah is not completely mapped, some entries are incomplete. In this case, whatever information is available will be provided. The second group, when present, is altitude in feet followed by meters in parentheses [i.e., 6,000' (1,829m)]. Altitude is not included with canyons or deserts with varying altitudes. _____________________________________________________________________ SOURCE... Utah Place Names. Salt Lake City, Utah : University of Utah. University of Utah Press, 1990. AUTHOR... Van Cott, John W. USE RESTRICTIONS... The contents of this article may be repurposed for non-commercial, non-profit, educational use. _____________________________________________________________________ Distributed by the Utah Education Network eMedia service: http://www.uen.org/emedia Original digital conversion by UCME: Utah Collections Multimedia Encyclopedia project: http://www.uen.org/ucme File ID = t_005252 A softbound copy of the original book may be purchased online from the University of Utah Press at: http://www.uofupress.com Page 1.
    [Show full text]