Emery County Pre-Disaster Hazard Mitigation Plan 2018
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High-Resolution Correlation of the Upper Cretaceous Stratigraphy Between the Book Cliffs and the Western Henry Mountains Syncline, Utah, U.S.A
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences 5-2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. Drew L. Seymour University of Nebraska, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Sedimentology Commons, and the Stratigraphy Commons Seymour, Drew L., "HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A." (2012). Dissertations & Theses in Earth and Atmospheric Sciences. 88. http://digitalcommons.unl.edu/geoscidiss/88 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. By Drew L. Seymour A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For Degree of Master of Science Major: Earth and Atmospheric Sciences Under the Supervision of Professor Christopher R. Fielding Lincoln, NE May, 2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH. U.S.A. Drew L. Seymour, M.S. -
EVALUATION REPORT Areas of Critical Environmental Concern Richfield Resource Management Plan
EVALUATION REPORT Areas of Critical Environmental Concern Richfield Resource Management Plan Dirty Devil and Henry Mountains Potential ACECs Richfield Field Office Bureau of Land Management January 2005 Evaluation Report Richfield Field Office EVALUATION REPORT—AREAS OF CRITICAL ENVIRONMENTAL CONCERN—RICHFIELD RMP/DEIS1 BACKGROUND ...........................................................................................................................................................1 The Law: FLPMA................................................................................................................................................1 The Regulation: 43 CFR 1610.7-2 .......................................................................................................................1 The Policy: BLM Manual 1613 ...........................................................................................................................1 EVALUATION PROCESS ..............................................................................................................................................2 Existing ACECs ...................................................................................................................................................2 ACEC Nominations .............................................................................................................................................2 Potential ACECs ..................................................................................................................................................6 -
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. -
Bronco Utah Operations LLC, Emery Underground Mine FSSOB UT0022616 Page 1
Bronco Utah Operations LLC, Emery Underground Mine FSSOB UT0022616 Page 1 FACT SHEET AND STATEMENT OF BASIS BRONCO UTAH OPERATIONS LLC, EMERY UNDERGROUND MINE RENEWAL PERMIT: DISCHARGE & STORM WATER UPDES PERMIT NUMBER: UT0022616 UPDES MULTI-SECTOR STORM WATER GENERAL PERMIT NUMBER: UTR000000 MAJOR INDUSTRIAL FACILITY CONTACTS Person Name: Dan R Baker Position: CEO/President, Bronco Utah Operations LLC Phone Number: (801) 286-2301 Person Name: John C. (Kit) Pappas Position: Environmental Manager Phone Number: (435) 650-7339 DESCRIPTION OF FACILITY Facility Name: Emery Underground Mine Mailing and Facility Address: P.O. Box 527 Emery, Utah 84522 Telephone: 435-650-7339 Actual Address: 3300 North 1200 West Classification (SIC): 1222 - Bituminous Coal Underground Mining (NAICS 212112) Bronco Utah Operations, LLC (Formerly Consol Coal) owns and operates an underground coal mine located 4 miles south of the town of Emery in Emery County, Utah, Township 22 South, Range 6 East. In 2009, the Emery Mine produced about 1.2 million short tons of coal. Production at the mine ceased. The mine has been idle for several years, but recent progress is being made to re-open the mine and resume the mining operation. It is anticipated that within this permit cycle, Emery Underground Mine will be operational. Bronco Utah Operations LLC, Emery Underground Mine FSSOB UT0022616 Page 2 SUMMARY OF CHANGES FROM PREVIOUS PERMIT Biomonitoring requirements have changed to remove Acute WET testing, with the addition of Chronic WET testing being required quarterly. DISCHARGE Over the last 5 years, Emery Mine has only had need to discharged from Outfall 003. There has not been enough accumulated storm water to discharge from any of the storm water settling ponds for over 15 years. -
Geology of the Northern Portion of the Fish Lake Plateau, Utah
GEOLOGY OF THE NORTHERN PORTION OF THE FISH LAKE PLATEAU, UTAH DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State - University By DONALD PAUL MCGOOKEY, B.S., M.A* The Ohio State University 1958 Approved by Edmund M." Spieker Adviser Department of Geology CONTENTS Page INTRODUCTION. ................................ 1 Locations and accessibility ........ 2 Physical features ......... _ ................... 5 Previous w o r k ......... 10 Field work and the geologic map ........ 12 Acknowledgements.................... 13 STRATIGRAPHY........................................ 15 General features................................ 15 Jurassic system......................... 16 Arapien shale .............................. 16 Twist Gulch formation...................... 13 Morrison (?) formation...................... 19 Cretaceous system .............................. 20 General character and distribution.......... 20 Indianola group ............................ 21 Mancos shale. ................... 24 Star Point sandstone................ 25 Blackhawk formation ........................ 26 Definition, lithology, and extent .... 26 Stratigraphic relations . ............ 23 Age . .............................. 23 Price River formation...................... 31 Definition, lithology, and extent .... 31 Stratigraphic relations ................ 34 A g e .................................... 37 Cretaceous and Tertiary systems . ............ 37 North Horn formation. .......... -
Hydrology and Effects of Mining in the Quitchupah and Pines Coal-Lease Tracts, Central Utah U.S
HYDROLOGY AND EFFECTS OF MINING IN THE QUITCHUPAH AND PINES COAL-LEASE TRACTS, CENTRAL UTAH U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 90-4084 COVER: Sketch by Charles E. Turner depicting fracturing in the Castlegate Sandstone and the potential for coal mining in the Quitch- upah and Pines coal-lease tracts. HYDROLOGY AND POTENTIAL EFFECTS OF MINING IN THE QUITCHUPAH AND PINES GOAL-LEASE TRACTS, CENTRAL UTAH By S.A. Thiros and G.E. Cordy U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 90-4084 Prepared in cooperation with the U.S. BUREAU OF LAND MANAGEMENT Salt Lake City, Utah 1991 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey, WRD Books and Open-File Reports Section Room 1016 Administration Building Federal Center, Bldg. 810 1745 West 1700 South Box 25425 Salt Lake City, Utah 84104 Denver, Colorado 80225 ii CONTENTS Page Abstract ............................................................. 1 Introduction ......................................................... 2 Purpose and scope ............................................... 2 Methods of investigation ........................................ 2 Ground-water site-numbering system .............................. 5 Acknowledgments ................................................. 5 Physical setting ................................................ 5 Topography -
Utah Scenic Byways Guide
Utah is the place where prehistory intersects with the enduring spirit of the Old West. Wild, adventure-rich places cradle vibrant urban centers. With interstates and airplanes, the world can feel pretty small. On Utah’s designated scenic byways, the world feels grand; its horizons seem infinite. As you drive through Utah, you’ll inevitably encounter many of the state’s scenic byways. In total, Utah’s distinct topography provides the surface for 27 scenic byways, which add up to hundreds of miles of vivid travel experiences wherein the road trip is as memorable as the destination. Utah’s All-American Road: Scenic Byway 12 headlines the network of top roads thanks to landscapes and heritage unlike anywhere else in the nation. All of Utah’s scenic byways are explorative journeys filled with trailheads, scenic overlooks, museums, local flavors and vibrant communities where you can stop for the night or hook up your RV. Not sure where to start? In the following pages, you’ll discover monumental upheavals of exposed rock strata among multiple national and state parks along the All-American Road (pg. 4); dense concentrations of fossils along Dinosaur Diamond (pg. 8); and the blazing red cliffs and deep blue waters of Flaming Gorge–Uintas (pg. 12) — and that’s just in the first three highlighted byways. Your journey continues down two dozen additional byways, arranged north to south. Best of all, these byways access an outdoor adventureland you can hike, fish, bike, raft, climb and explore from sunup to sundown — then stay up to welcome the return of the Milky Way. -
Contemporary Seismicity, Faulting, and the State of Stress in the Colorado Plateau
Contemporary seismicity, faulting, and the state of stress in the Colorado Plateau ~:~SGR~~ii;HREY } Woodward-Clyde Consultants, 500 12th Street, Suite JOO, Oakland, California 94607 ABSTRACT west- or northeast-striking planes at shallow with the installation of regional networks by the depths. The contemporary state of stress University of Utah Seismograph Stations The contemporary seismicity of the Colo within the plateau is characterized by approx (UUSS), the Los Alamos National Laboratory rado Plateau based on seismic monitoring in imate northeast-trending extension in con (LANL), and the USGS Albuquerque Seismo the past 30 yr can be characterized as being of trast to the previous belief that the plateau logical Laboratory (ASL) (Fig. 2). Despite the small to moderate magnitude, and contrary to was being subjected to east-west tectonic additional network coverage, however, detec earlier views, of a low to moderate rate of compression. One area of the plateau, the tion of earthquakes smaller than ML 2 within occurrence with earthquakes widely distrib eastern Wasatch Plateau and Book Cliffs, the plateau interior improved only slightly. This uted. Concentrations of earthquakes have may still be characterized by compressive paper presents the results of the first major pro been observed in a few areas of the plateau. stresses; however, the nature of these stresses gram of seismographic studies performed within The most seismically active area of the Colo is not well understood. the Colorado Plateau. This program, initiated by rado Plateau is the eastern Wasatch Plateau Woodward-Clyde Consultants (WCC) in 1979, Book Cliffs, where abundant small-magnitude INTRODUCTION included an extensive program of microearth seismicity is induced by coal mining. -
A History of Water Development in Emery County, Utah
A History of Water Development in Emery County, Utah Edward A. Geary Brigham Young University Department of English Provo, Utah 84602 Emery County is a dramatically varied region in east-central Utah, ranging in elevation from under 4,000 feet in the depths of Labyrinth Canyon on the Green River to well above 10,000 feet on the higher ridges of the Wasatch Plateau to the west. The central part of the county is dominated by the San Rafael Swell, a deeply eroded anticlinal uplift characterized by imposing buttes, rugged canyons, and great mural cliffs. Between the Wasatch Plateau and the San Rafael Swell lies Castle Valley, home to most of the county’s agricultural and industrial development and population. The county’s other developed area is in and around the community of Green River on the eastern border. Emery County is an arid region with an annual average of less than ten inches of precipitation. However, there is significant local variation. The highest levels of the Wasatch Plateau receive more than forty inches of precipita- tion in an average year, most of it in the form of snow during the winter months. The prevailing westerly winds deposit the snow in massive drifts just below the skyline ridge. These snowbanks feed the four major creeks that drain into Castle Valley. There is sufficient moisture on the higher benches of Castle Valley and the San Rafael Swell to support native bunchgrasses and pinion-juniper woodlands. In the lower parts of the county the natural vegetation is desert growth including shadscale, greasewood, prickly pear, and a low saltbush locally known as "Castle Valley clover." No cultivated crops can be grown without irrigation. -
Standards of Quality for Waters of the State (2020) (PDF)
Presented below are water quality standards that are in effect for Clean Water Act purposes. EPA is posting these standards as a convenience to users and has made a reasonable effort to assure their accuracy. Additionally, EPA has made a reasonable effort to identify parts of the standards that are not approved, disapproved, or are otherwise not in effect for Clean Water Act purposes. R317. Environmental Quality, Water Quality. R317-2. Standards of Quality for Waters of the State. R317-2-1A. Statement of Intent. Whereas the pollution of the waters of this state constitute a menace to public health and welfare, creates public nuisances, is harmful to wildlife, fish and aquatic life, and impairs domestic, agricultural, industrial, recreational and other legitimate beneficial uses of water, and whereas such pollution is contrary to the best interests of the state and its policy for the conservation of the water resources of the state, it is hereby declared to be the public policy of this state to conserve the waters of the state and to protect, maintain and improve the quality thereof for public water supplies, for the propagation of wildlife, fish and aquatic life, and for domestic, agricultural, industrial, recreational and other legitimate beneficial uses; to provide that no waste be discharged into any waters of the state without first being given the degree of treatment necessary to protect the legitimate beneficial uses of such waters; to provide for the prevention, abatement and control of new or existing water pollution; to place first in priority those control measures directed toward elimination of pollution which creates hazards to the public health; to insure due consideration of financial problems imposed on water polluters through pursuit of these objectives; and to cooperate with other agencies of the state, agencies of other states and the federal government in carrying out these objectives. -
Dikes of the Clear Creek Area, Wasatch Plateau, Utah
Utah State University DigitalCommons@USU All Graduate Theses and Dissertations Graduate Studies 5-1976 Dikes of the Clear Creek Area, Wasatch Plateau, Utah William Dennis Thomas Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/etd Part of the Geology Commons Recommended Citation Thomas, William Dennis, "Dikes of the Clear Creek Area, Wasatch Plateau, Utah" (1976). All Graduate Theses and Dissertations. 2113. https://digitalcommons.usu.edu/etd/2113 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Theses and Dissertations by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. DIKES OF THE CLEAR CREEK AREA, WASATCH PLATEAU, UTAH by William Dennis Thomas A thesis submitted .in partial fulfillment of the requirements for the degree of ~~TER OF SCIENCE in Geology Approved: ·:9ajor Professor Committee Member' Committee Member Dean of Graduate Studies UTAH STATE UNIVERSITY Logan, Utah 1976 ii ACKNOWLEDGMENTS The author would like to express thanks to Dr. Donald R. Olsen, Dr. Clyde T. Hardy, and Dr. Peter T. Kolesar for their assistance. Thanks are also due to Dr. Robert Q. Oaks, Jr., and Jerome V. DeGraff for their helpful comments. Mr. DeGraff was also instrumental in helping to gain financial aid for the preparation of thin sections. This aid was supplied by Utah State University and the U. S. Forest Service DEVELOP ECOSYM project. Acknowledgment should be made to EMCO of Clear Creek, Utah, and especially to Mr. Dan Guy for the use of coal mine maps and other helpful information. -
Geology and Oil and Gas Prospects of Part of the San Rafael Swell, Utah
GEOLOGY AND OIL AND GAS PROSPECTS OF PART OF THE SAN RAFAEL SWELL, UTAH By JAMES GILLULY INTRODUCTION Purpose of the report. The purpose of this report is to present an account of the general geologic features of part of the San Rafael Swell, Utah, with especial reference to its oil and gas possibilities. Oil-field experience has shown that upfolds or domes in the rocks are generally more favorable to the accumulation of oil and gas than other structural features. The San Rafael Swell is a feature of this type, and the public lands in the region were accordingly withdrawn from entry pending classification as to their oil possibilities. The discovery in 1923 of helium in gas from a well on the Woodside anti cline, in sec. 12, T. 19 S., R. 13 E., near the north end of the Swell, aroused considerable additional interest because of the probable value of this gas in national defense. Numerous factors affect the accumulation of commercially impor tant bodies of oil and gas. The expense of drilling is very great compared with that of geologic study, and although such study can only rarely be completely decisive in advance of drilling, the data thus obtainable are desirable as a basis for classification of the land. Location and extent of the area. The San Rafael Swell lies in Emery County and northern Wayne County, Utah. The name was doubtless applied in reference to the geologic structure of the region, which is that of a huge swell or dome in the sedimentary rocks. Erosion has carved the Swell into a topography which is very dis tinctive and striking: geographically, as well as geologically, it is a unit.