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Quartz Crystal Deposits of Western Arkansas
Quartz Crystal Deposits of Western Arkansas By A. E. J. ENGEL CONTRIBUTIONS TO ECONOMIC GEOLOGY, 1951 GEOLOGICAL SURVEY BULLETIN 973-E Geology of an important domestic source of quartz for optical and oscillator use UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1952 UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary . GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.50 (paper cover) CONTENTS Page Abstract______-_:________-___-____-___________-___-______-_____ 173 Introduction ____ _________________________________________________ 174 History of mining__________________-__-_-_______----_-_--__-_----_ 175 Production and use of crystals.________^____________________________ 178 Geology--...---.-----.---.--------------------------------------- 186 Stratigraphy.__________-_--___-___----.-_-___---_---_-_-_-_-_- 186 General features.___-___________--_---_------.-_-_-._-__-__ 186 Principal quartz-bearing formations______1_________________ 187 Crystal Mountain sandstone (Ordovician?) _______________ 187 Blakely sandstone (Ordovician)_________________________ 189 Structure___._____--___-_-__-__-__-___-_________-_____________ 192 Structural features of the Ouachita anticlinorium_---_____.____ 192 Fractures controlling the deposition of quartz _________________ 194 Quartz deposits_.________"__________-______________________________ 200 Form, size, and distribution_____-_______.__._______._;________ 200 Classification of -
Ouachita National Recreation Trail Recreation National Ouachita
CRE E AT R I L O A N N T O R I A T I A L N OUACHITA NATIONAL RECREATION TRAIL OUACHITA NATIONAL FOREST ARKANSAS-OKLAHOMA This page intentionally left blank. This page intentionally left blank. CRE E AT R I L O Ouachita National Forest A N N T O R I A T I A Arkansas - Oklahoma L N Ouachita National Recreation Trail (ONRT)--Overview Hiking Biking U.S. Department of Agriculture Forest Service Trail Highlights: This is the longest trail in the Ouachita Length: 192 miles. Southern Region National Forest spanning 192 miles across its entire length. Directions: There are many developed and The U.S. Department of undeveloped access points across the forest, In the west, the trail begins at Talimena State Park on Highway Agriculture (USDA) prohib- OUACHITA 271 near Talihina, Oklahoma. identified on the trail map segments. its discrimination in all its programs and activities on the The eastern boundary is south of Perryville, Arkansas on Trail Information: Unsurfaced. Water is scarce on basis of race, color, national Highway 9. many portions of the trail especially during dry periods. Treat all water before drinking. origin, age, disability, and An additional 32 miles of trail, located on private and other Difficulty Level: Varies. where applicable, sex, marital public lands, extends to Pinnacle Mountain State Park, 15 status, familial status, paren- NATIONA miles west of Little Rock, Arkansas. Site amenities: Recreation areas usually include tal status, religion, sexual ori- campgrounds, picnic areas, swimming, drinking entation, genetic information, Elevations range from 600 to 2,600 feet as the trail passes water, restrooms, and other trails. -
Water Sources
OUACHITA TRAIL Use at your own risk. Even a good source NAVIGATION POINTS Most fixes use NAD27 datum. may be dry under drought conditions. Compiled by Bill Mooney Not all verified. MILE SEC CAMP DESCRIPTION LAT/LON UTM 0 1 Talimena State Park 34.78317 94.95100 15S 321488E 3850732N 0.7 1 Old Military Road Trail 34.78817 94.94018 15S 322488E 3851267N 1.2 1 Wildlife pond on left just up from OT after crossing the yellow blaze trail. 2.4 1 Potato Hills Vista Spur 34.79507 94.92360 15S 324020E 3852004N 5 1 Panorama Vista Spur to left. 34.77740 94.90513 15S 325673E 3850012N 5.8 1 FR#6010. Access point. 34.77043 94.89200 15S 326860E 3849216N Bohannon Creek. Rainy season water 7.3 1 source. hike down creek past camp. several pools of water Deadman's Gap. Access point. Water stash 8 1 point. 34.77210 94.87186 15S 328707E 3849366N 8.7 1 Boardstand Trail 9.4 1 S Rock Garden Shelter 34 46.387 94 46.387 15S 337742E 3849118N wildlife pond 1/4 mile down road from 9.4 shelter Seasonal spring just east of shelter on trail 11.2 Best source of water until 19.9 seasonal 13.4 1 Cedar Branch. Rainy season water source. 16.8 1 S Holson Valley Vista Shelter 34 44.799 94 46.076 15S 338165E 3846174N 16.9 1 Spur right to Holson Valley Vista. Horsethief Springs Trail. Cedar Lake Recreation area five miles to left. Talimena 18.7 1 Scenic Drive spur to right. -
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 ............................................................................................. -
Ouachita National Recreation Trail Recreation National Ouachita
CRE E AT R I L O A N N T O R I A T I A L N OUACHITA NATIONAL RECREATION TRAIL OUACHITA NATIONAL FOREST ARKANSAS-OKLAHOMA This page intentionally left blank. Help Maintain the Ouachita Trail The trail is maintained by volunteer members of FoOT Friends of the Ouachita Trail If you would like to help, contact FoOT at: Email: [email protected] Mail: PO Box 8630 Hot Springs, AR 71910 WWW.FriendsOT.org FoOT is organized exclusively to provide assistance for the maintenance, enhancement and use of the Ouachita National Recreation Trail CRE E AT Ouachita National Forest R I L O A N N T O R I A T I A L Arkansas - Oklahoma N Ouachita National Recreation Trail (ONRT)--Overview Hiking Biking U.S. Department of Agriculture Forest Service Trail Highlights: This is the longest trail in the Ouachita Length: 192 miles. Southern Region National Forest spanning 192 miles across its entire length. Directions: There are many developed and The U.S. Department of In the west, the trail begins at Talimena State Park on Highway undeveloped access points across the forest, Agriculture (USDA) prohib- OUACHITA 271 near Talihina, Oklahoma. identified on the trail map segments. its discrimination in all its programs and activities on the The eastern boundary is south of Perryville, Arkansas on Trail Information: Unsurfaced. Water is scarce on basis of race, color, national Highway 9. many portions of the trail especially during dry periods. Treat all water before drinking. origin, age, disability, and An additional 32 miles of trail, located on private and other Difficulty Level: Varies. -
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. -
Ouachita National Forest Womble Trail
Ouachita National Forest SOUTHERN REGION NATIONAL FORESTS Arkansas - Oklahoma The U.S. Department of Womble Trail Hiking Biking TRAIL Agriculture (USDA) prohibits WOMBLE discrimination in all its programs and activities on the basis of race, color, national Trail Highlights: The Womble Trail stretches over 37 Length: 37.8 miles. origin, age, disability, and miles from Northfork Lake to the Ouachita National Travel time one-way: 2 to 4 days. where applicable, sex, marital Recreation Trail. This trail is considered one of the best status, familial status, parental Trail Information: The trail is unsurfaced and single track trails in this area. Short segments of the trail status, religion, sexual orien- marked with white triangles. meander along the bluffs of the Ouachita River provid- tation, genetic information, ing breathtaking views. Hikers and mountain bikers Access: There are four trailhead parking areas: political beliefs, reprisal, or can combine the Roundtop Trail with the Womble and Round Top Trail on Forest Road D75A, Highway because all or a part of an Ouachita National Recreation Trail (west of Highway 27 south of the bridge crossing Lake Ouachita, individual's income is derived 27) to form an 8-mile loop. North Fork Lake and Highway 298 trail intersec- from any public assistance Surrounding Areas: Visitors can use the short spur tion. program. (Not all prohibited bases apply to all programs.) trails to access three float camps located along the south The trail is also accessible from the three float shore of the Ouachita River: Persons with disabilities who camps and adjacent forest roads. require alternative means for • Rocky Shoals Float Camp (0.3-mile spur) Water: Non-potable.