Quartz Crystal Deposits of Western Arkansas
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Geologic Resources Inventory Report, Hot Springs National Park
National Park Service US Department of the Interior Natural Resource Stewardship and Science Hot Springs National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2013/741 ON THE COVER View from the top of the display spring down to the Arlington Lawn within Hot Springs National Park. THIS PAGE Gulpha Creek flows over Stanley Shale downstream from the Gulpha Gorge Campground. Photographs by Trista L. Thornberry-Ehrlich (Colorado State University) Hot Springs National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2013/741 National Park Service Geologic Resources Division PO Box 25287 Denver, CO 80225 December 2013 US Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. This report received informal peer review by subject-matter experts who were not directly involved in the collection, analysis, or reporting of the data. -
Basin-Centered Gas Systems of the U.S. by Marin A
Basin-Centered Gas Systems of the U.S. By Marin A. Popov,1 Vito F. Nuccio,2 Thaddeus S. Dyman,2 Timothy A. Gognat,1 Ronald C. Johnson,2 James W. Schmoker,2 Michael S. Wilson,1 and Charles Bartberger1 Columbia Basin Western Washington Sweetgrass Arch (Willamette–Puget Mid-Continent Rift Michigan Basin Sound Trough) (St. Peter Ss) Appalachian Basin (Clinton–Medina Snake River and older Fms) Hornbrook Basin Downwarp Wasatch Plateau –Modoc Plateau San Rafael Swell (Dakota Fm) Sacramento Basin Hanna Basin Great Denver Basin Basin Santa Maria Basin (Monterey Fm) Raton Basin Arkoma Park Anadarko Los Angeles Basin Chuar Basin Basin Group Basins Black Warrior Basin Colville Basin Salton Mesozoic Rift Trough Permian Basin Basins (Abo Fm) Paradox Basin (Cane Creek interval) Central Alaska Rio Grande Rift Basins (Albuquerque Basin) Gulf Coast– Travis Peak Fm– Gulf Coast– Cotton Valley Grp Austin Chalk; Eagle Fm Cook Inlet Open-File Report 01–135 Version 1.0 2001 This report is preliminary, has not been reviewed for conformity with U. S. Geological Survey editorial standards and stratigraphic nomenclature, and should not be reproduced or distributed. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U. S. Government. 1Geologic consultants on contract to the USGS 2USGS, Denver U.S. Department of the Interior U.S. Geological Survey BASIN-CENTERED GAS SYSTEMS OF THE U.S. DE-AT26-98FT40031 U.S. Department of Energy, National Energy Technology Laboratory Contractor: U.S. Geological Survey Central Region Energy Team DOE Project Chief: Bill Gwilliam USGS Project Chief: V.F. -
1 STEPHEN ANDREW LESLIE Department of Geology And
STEPHEN ANDREW LESLIE Department of Geology and Environmental Science James Madison University, MSC 6903 Harrisonburg, VA 22807 Phone: (540) 568-6144; Fax: (540) 568-8058 E-mail: [email protected] EDUCATION Ph.D. Geology, The Ohio State University, June 1995 Dissertation: Upper Middle Ordovician conodont biofacies distribution patterns in eastern North America and northwestern Europe: Evaluations using the Deicke, Millbrig and Kinnekulle K-bentonite beds as time planes. M.S. Geology, University of Idaho, May 1990 Thesis: The Late Cambrian-Middle Ordovician Snow Canyon Formation of the Valmy Group, Northeastern Nevada. B.S. Geology, Bowling Green State University, May 1988, Cum Laude Minor in Classical Studies GEOLOGY EMPLOYMENT 7/07-present Department Head and Professor with tenure, Department of Geology and Environmental Science, James Madison University. 7/04-7/06 Department Chair, Department of Earth Sciences, University of Arkansas at Little Rock. 8/02-7/06 Acting Director/Director of the Master of Science in Integrated Science and Mathematics Program, College of Science and Mathematics 8/05 – 7/06 Professor with tenure, Department of Earth Sciences, University of Arkansas at Little Rock. 8/00 -7/05 Associate Professor with tenure, Department of Earth Sciences, University of Arkansas at Little Rock. 8/96 -7/00 Assistant Professor, Department of Earth Sciences, University of Arkansas at Little Rock. 6/95 - 8/96 Postdoctoral Research Scientist at The Ohio State University. 1/95 - 3/96 Lecturer at Otterbein College. 6/95 - 8/95 Lecturer at The Ohio State Univ.-Marion & Marion Correctional Institution 9/94 - 12/94 Lecturer at The Ohio State Univ.-Marion & Marion Correctional Institution 9/93 - 6/94 Doctoral Fellow at The Ohio State University. -
INTRODUCTION. GENERAL GEOGRAPHY and GEOLOGY of the Ridges, but Other Streams in All Parts of the Province Have Cut OUACHITA MOUNTAIN REGION
By A. H. Pur due and H. D. Miser. INTRODUCTION. GENERAL GEOGRAPHY AND GEOLOGY OF THE ridges, but other streams in all parts of the province have cut OUACHITA MOUNTAIN REGION. their courses transverse to the ridges and thus run through LOCATION AND GENERAL RELATIONS OF THE DISTRICT. /Surface features. The Ouachita Mountain region consists of narrow, picturesque water gaps. a mountainous area known as the Ouachita Mountains and of Climate and vegetation. The climate of the region on the The area shown on the maps in this folio, which includes the Athens Plateau, which lies along the southern border of the whole is mild. The cold in winter is not extreme, but the Hot Springs and vicinity, in Arkansas, extends from latitude mountains, most of it in Arkansas. A part of the east end of the heat in summer is at times intense. The rainfall, which is 34° 22' 57" to 34° 37' 57" N. and from longitude 92° 55' 47" Ouachita Mountains is embraced in the Hot Springs district. abundant, commonly reaches a maximum in the late spring to 93° 10' 47" W. and includes one-sixteenth of a "square and early summer and decreases to a minimum late in the degree" of the earth's surface, which in that latitude amounts summer and early in the fall, when in some years there are to 245.83 square miles. It is a little southwest of the center droughts. In spite of the rather poor soil the precipitation of Arkansas, and most of it is in Garland County, but a narrow has produced a heavy forest cover over .the entire region. -
Information Circular 39C FF-OG-OU 017
Information Circular 39C FF-OG-OU 017 STATE OF ARKANSAS ARKANSAS GEOLOGICAL SURVEY BEKKI WHITE, DIRECTOR AND STATE GEOLOGIST INFORMATION CIRCULAR 39C STRUCTURAL AND STRATIGRAPHIC ANALYSIS OF THE SHELL INTERNATIONAL PAPER NO. 1-21 WELL, SOUTHERN OUACHITA FOLD AND THRUST BELT, HOT SPRING COUNTY, ARKANSAS Ted Godo (Shell Exploration & Production Company, Houston, TX) Peng Li (Arkansas Geological Survey, Little Rock, AR) M. Ed Ratchford (Arkansas Geological Survey, Little Rock, AR) 2014 Table of Contents List of Figures, Tables, Plates, and Appendices ................................................................ ii Acknowledgments ............................................................................................................. iii Introduction ........................................................................................................................ 1 Regional Geologic Setting ................................................................................................. 3 Stratigraphic and Structural Test Concept .................................................................... 4 Pre-Drill Reservoirs (Ordovician Sandstone Objectives) ............................................. 7 Pre-Drill Reservoirs (Bigfork Chert Objective) ............................................................ 9 Pre-Drill Structural Setting and Analysis ........................................................................ 12 Pre-Drill Thermal Maturity ............................................................................................. -
Groundwater Vulnerability Map of Oklahoma -- Appendix A
APPENDIX A Description of Hydrogeologic Basins Description of Hydrogeologic Basins A description of the basin definitions, boundaries, and hydrogeology for the hydrogeologic basins is presented below. Table A-1 lists for each basin the names, ages, and codes for the geologic units, as cited in the surficial geology maps in the hydrologic atlases of Oklahoma. The 12 hydrologic atlases are available from the Oklahoma Geological Survey. The digital surficial geology sets from the hydrologic atlases are available on the Internet at http://wwwok.cr.usgs.gov/gis/geology/index.html. The digital surficial geology map of Hydro- logic Atlas 3 does not include the alluvium and terrace deposits. To identify the alluvium and terrace deposits in the Ardmore and Sherman quadrangles, refer to Sheet 1 in Hydrologic Atlas 3 (Hart, 1974). Alluvium and Terrace Deposits Alluvium and terrace deposits are Quaternary in age, and occur along modern and ancient streams throughout the state. They encompass the outcrop of alluvium, terrace deposits, and dune sand. Alluvium and terrace deposits along the major rivers (Salt Fork of the Arkansas, Arkansas, Cimarron, Beaver-North Canadian, Canadian, Washita, North Fork of the Red, and the Red) extend from 1-15 miles from the river banks. Terraces represent older, higher stages of the rivers that have since cut their channels deeper (OWRB, 1995). Alluvium and terrace deposits consist mainly of unconsolidated deposits of gravel, sand, silt, and clay. Along large streams, these deposits consist of clay and silt at the surface, grading down- ward into coarse sand and gravel at the base (Carr and Bergman, 1976). -
Appendix F – Minerals
Appendix F – Minerals The Ouachita National Forest is located in Central Arkansas, within the Ouachita Mountains and the very southern portion of the Arkansas River Valley, and in southeastern Oklahoma in the Ouachita Mountains and the Red River Valley (Idabel, Oklahoma area). The geologic setting of the Forest provides a diversity of energy and non-energy mineral resources. Since approval of the 1986 Land Management Plan, minerals from the Forest, including natural gas, hardrock, and mineral materials, have been used to meet the basic needs of the public, such as providing natural gas fuel for energy sources and heating homes; stone for construction and functional home projects, and road surfacing/maintenance materials. Development of the federal and private minerals underlying the National Forest stimulates the local and national economies by making available the raw materials needed for continued economic development, resulting in increased jobs and spending. The sustainability of the Forest depends on the continued use of mineral resources to meet the public’s demand for such things as fuels and building materials. The role of mineral resources is fundamental to viability of human ecosystems. The goals for management of the Ouachita National Forest were developed in consideration of the other national forests within the Southern Region. Any decisions on projects to implement the Revised Forest Plan will be based on site-specific analysis in compliance with the National Environmental Policy Act (NEPA). These environmental analyses will be appropriately documented according to direction in the Council on Environmental Quality Regulations for Implementing the Procedural Provisions of the National Environmental Policy Act (40 CFR Parts 1500-1508) and the Environmental Policy and Procedures Handbook (FSH 1909.15). -
A Geochemical Analysis of the Arkansas Novaculite And
University of Arkansas, Fayetteville ScholarWorks@UARK Theses and Dissertations 5-2016 A Geochemical Analysis of the Arkansas Novaculite and Comparison to the Siliceous Deposits of the Boone Formation John Byron Scott hiP lbrick University of Arkansas, Fayetteville Follow this and additional works at: http://scholarworks.uark.edu/etd Part of the Geochemistry Commons, and the Geology Commons Recommended Citation Philbrick, John Byron Scott, "A Geochemical Analysis of the Arkansas Novaculite and Comparison to the Siliceous Deposits of the Boone Formation" (2016). Theses and Dissertations. 1520. http://scholarworks.uark.edu/etd/1520 This Thesis is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. A Geochemical Analysis of the Arkansas Novaculite and Comparison to the Siliceous Deposits of the Boone Formation A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology by John Byron Scott Philbrick University of Arkansas Bachelor of Science in Geology, 2014 May 2016 University of Arkansas This thesis is approved for recommendation to the Graduate Council _____________________________________ Walter Manger, PhD Thesis Director _____________________________________ Adriana Potra, PhD Committee Member _____________________________________ Erik Pollock, MS Committee Member _____________________________________ Dr. Doy Zachry, PhD Committee Member Abstract Geochemical analyses of the Arkansas Novaculite, located within core structures of the Ouachita Mountains in west-central Arkansas, and penecontemporaneous chert of the lower Boone Formation, located atop the Springfield Plateau of southwest Missouri, northwest Arkansas, and northeast Oklahoma, have identified a significant concentration of both aluminum and potassium. -
Hydrogeologic Investigation Report of the Kiamichi, Potato Hills, Broken
HYDROLOGIC INVESTIGATION REPORT OF THE KIAMICHI, POTATO HILLS, BROKEN BOW, PINE MOUNTAIN AND HOLLY CREEK MINOR BEDROCK GROUNDWATER BASINS IN SOUTHEASTERN OKLAHOMA by Kent Wilkins OKLAHOMA WATER RESOURCES BOARD Planning & Management Division January 2001 TABLE OF CONTENTS INTRODUCTION ............................................................................................................. 1 PHYSICAL SETTING ...................................................................................................... 1 Location .............................................................................................................. 1 Physiography ...................................................................................................... 3 Climate ................................................................................................................ 3 Land Use ............................................................................................................. 3 GEOLOGIC SETTING .................................................................................................... 4 Regional Structure ............................................................................................. 4 Regional Geology ............................................................................................... 4 GROUNDWATER RESOURCES .................................................................................... 5 Kiamichi Minor Groundwater Basin ................................................................. -
U-Pb Detrital Zircon Signature of the Ouachita Orogenic Belt
U-PB DETRITAL ZIRCON SIGNATURE OF THE OUACHITA OROGENIC BELT By PRESTON REEVES McGUIRE Bachelor of Arts, 2014 Western State Colorado University Gunnison, Colorado Submitted to the Graduate Faculty of The College of Science and Engineering Texas Christian University In partial Fulfillment of the requirements for the degree MASTERS OF SCIENCE IN GEOLOGY May 2017 Copyright by Preston Reeves McGuire 2017 Acknowledgements I would like to gratefully acknowledge the help, support, and extreme generosity of all individuals and universities while working on the project. I would first like to thank my graduate advisor, Dr. Xianyang Xie, for giving me this opportunity to study under his guidance. His enthusiasm has kept me motivated and excited about this project during the course of my stay at TCU. I could not have asked for a better advisor who was as dedicated and inspiring as Dr. Xie was. I would also like to thank my other thesis advisors, Dr. Helge Alsleben and Dr. Elizabeth Petrie, for their helpful criticisms and inputs. Their support and critiques during my research were very much appreciated. Secondly, I would like to thank the help of the other geology departments that graciously offered their facilities and assistance in helping me complete this project: Dr. Fan and the University of Texas at Arlington, Dr. William Griffin and the University of Texas at Dallas, and Dr. George Gehrels and Dr. Mark Pecha at the University of Arizona. I would like to thank Dr. William Thomas for his thoughtful input and assistance. Without his input, this project would have been incredibly more difficult. -
Environmental Assessment
Environmental Assessment For Little Fir Watershed Restoration Management Project Montgomery County, Arkansas Responsible Agency: USDA Forest Service Ouachita National Forest Caddo-Womble Ranger District Responsible Official: Gloria Chrismer District Ranger Caddo-Womble Ranger District 1523 Hwy 270 East Mount Ida, AR 71957 (870) 867-2101 For Further Information Contact: Seanna Whisenhunt Caddo-Womble Ranger District 1523 Hwy 270 East Mount Ida, AR 71957 (870) 867-2101 The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or a part of an individual's income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA's TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410 or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. TABLE OF CONTENTS CHAPTER 1 ...................................................................................................................... 1 PURPOSE -
The Oklahoma Geology Notes, Which Had Been a Feature of the Oklahoma Geology Scene Since the Early 40S, but Was Last Published in 2014
VOLUME 75 FALL 2016 STRATIGRAPHIC NOMENCLATURE OF THE OUACHITA MOUNTAINS IN OKLAHOMA: FORMAL, INFORMAL, OBSOLETE, AND INCORRECT or THE GOOD, THE BAD, AND THE UGLY INSIDE ON PAGE 5 OKLAHOMA GEOLOGICAL SURVEY OKLAHOMA GEOLOGICAL SURVEY DR. JEREMY BOAK, Director OGS Geologist Neil Suneson Editor delves into the Good, the Bad, and Ted Satterfield the Ugly of the topic of stratigraphic nomenclature in the Ouachita Mountains. Cartography Manager James Anderson GIS Specialist Russell Standridge Copy Center Manager Richard Murray This publication, printed by the Oklahoma Geological Survey, Norman, Oklahoma, is issued by the Oklahoma Geological Survey as authorized by Title 70, Oklahoma Statutes 1981, Section 3310, and Title 74, Oklahoma Statutes 1981, Sections 231—238 The Oklahoma Geological Survey is a state agency for research and public service, mandated in the State Constitution to study Oklahoma’s land, water, mineral and energy resources and to promote wise Cover: Outcrop of the Wapanucka Limestone use and sound environmental practices. east of Hartshorne, Oklahoma. (Photo by TED SATTERFIELD). 2 FALL 2016 Grateful to be back As the Director of the Oklahoma Geological Survey (OGS), I am very glad to see the revival of the Oklahoma Geology Notes, which had been a feature of the Oklahoma geology scene since the early 40s, but was last published in 2014. This issue, marking the return, introduces a new format, becoming less of a newsletter and more of a scientific publication. From there we proceed, as many geological investigations do, from the surface downward. We start up the Notes again with Neil Sune- son’s take on stratigraphic nomenclature in the Ouachita Mountains.