Oklahoma Today Spring 1980 Volume 30 No. 2
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The Civilian Conservation Corps As Means of Social
THE CIVILIAN CONSERVATION CORPS AS MEANS OF SOCIAL CONTROL: A SOUTHWESTERN OKLAHOMA PERSPECTIVE By LEON CHAD KINDER Bachelor of Science Southwestern Oklahoma State University Weatherford, Oklahoma 1993 Master of Education Southwestern Oklahoma State University Weatherford, Oklahoma 1995 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of DOCTOR OF EDUCATION December, 2003 Tueiis 2DD3D K5lc THE CIVILIAN CONSERVATION CORPS AS MEANS OF SOCIAL CONTROL: A SOUTHWESTERN OKLAHOMA PERSPECTIVE Thesis Approved: ,~(l,g ,, Thesis Advisor ~ Dean of the Graduate College 11 PREFACE I wish to express my sincere gratitude to Dr. Lowell Caneday, my dissertation advisor, for the many hours he spent in support of my work. To Dr. Christine Cashel, doctoral committee chair, my deepest appreciation is extended. Thanks is also expressed to the other members of the doctoral committee, Dr. William Bryans, Dr. Colleen Hood, and Dr. Thomas Kuzmic for their time, suggestions, and support given in the development of this project. I also wish to express thanks to my mentor, Dr. Ken Rose, Dean of the School of Professional and Graduate Studies at Southwestern Oklahoma State University, for his assistance and support during my doctoral work. To my wife Gayla, children Natalie and Carson, and members of my extended family a special thanks is given. Thank-you all for your love and support. 111 TABLE OF CONTENTS CHAPTER PAGE I. INTRODUCTION, STATEMENT OF THESIS AND HISTORICAL BACKGROUND ......................................... 1 Introduction and Statement of Thesis ............................ 1 The Great Depression ............................................. .2 The Great Depression in Oklahoma .............................. 3 Hoover's Response to the Great Depression .................. -
Highlights of Lawton, Oklahoma
Highlights of Lawton, Oklahoma The Community The City of Lawton, Oklahoma, founded in 1901, is the fifth largest city in Oklahoma and the county seat of Comanche County, in Southwest Oklahoma. Lawton is located approximately 90 miles southwest of Oklahoma City along Interstate 44. Fort Sill, an active U.S. Army installation, is on the City’s north side and is within the city limits as the result of annexation in the 1990s. Comanche County is home to more than 122,000 residents as of 2017, with Lawton accounting for 94,000 of the countywide population – smaller cities and towns including Cache, Chattanooga. Elgin, Faxon, Fletcher, Geronimo, Indiahoma, Medicine Park, and Sterling make up the remainder. Mild Winters, Warm Summers The mean temperature for the Lawton area is 61.5 degrees. The percentage of sunshine in Lawton ranges from an average of about 60 percent in the winter to nearly 80 percent in the summer, providing a long growing season of 215 days. The July high is around 95 degrees. Summers are generally warm with 95 days of 90 degrees or higher. The winter months are typically mild with an average low temperature in January of 27 degrees. Annual precipitation ranges from about 30 inches in western Comanche County to 33 inches in the east, slightly less than the U.S. average of 39 inches. Annual snowfall averages 3.6 inches while the average U.S. city gets 26 inches of snow per year. Cost of Living Lawton remains a low cost-of-living city relative to both the nation and Oklahoma. -
Four Western Cheilanthoid Ferns in Oklahoma
Oklahoma Native Plant Record 65 Volume 10, December 2010 FOUR WESTERN CHEILANTHOID FERNS IN OKLAHOMA Bruce A. Smith McLoud High School McLoud, Oklahoma 74851 Keywords: arid, distribution, habitat, key ABSTRACT The diversity of ferns in some of the more arid climates of western Oklahoma is surprising. This article examines four Oklahoma cheilanthoid ferns: Astrolepis integerrima, Cheilanthes wootonii, Notholaena standleyi, and Pellaea wrightiana. With the exceptions of A. integerrima and P. wrightiana which occur in Alabama and North Carolina respectively, all four species reach their eastern limits of distribution in Oklahoma. Included in this article are common names, synonyms, brief descriptions, distinguishing characteristics, U.S. and Oklahoma distribution, habitat information, state abundance, and a dichotomous key to selected cheilanthoids. The Oklahoma Natural Heritage Inventory has determined that all but one (N. standleyi) are species of concern in the state. INTRODUCTION of eastern Oklahoma, while most members of the Pteridaceae occur in Almost half of the ferns in the family western Oklahoma (Taylor & Taylor Pteridaceae are xeric adapted ferns. In 1991). Oklahoma six genera and sixteen species Statewide, the most common species in the family are known to occur. They in the Pteridaceae is Pellaea atropurpurea live on dry or moist rocks and can be (Figure 4), which can be found found in rock crevices, at the bases of throughout the body of the state and boulders, or on rocky ledges. Common Cimarron County in the panhandle. The associated species include lichens, mosses, rarest are Cheilanthes horridula and liverworts, and spike mosses. Two Cheilanthes lindheimeri. Cheilanthes horridula physical characteristics that unite the and Cheilanthes lindheimeri have only been family are the marginal sori (Figure 1) and seen in one county each, Murray and the lack of a true indusium. -
2016 OSAI Visitors Guide
40TH OKLAHOMA SUMMER ARTS INSTITUTE JUNE 11-26, 2016 THE CON- TENTS About OSAI ............................................................ 2 About Quartz Mountain ............................................ 4 The Art Collection .................................................... 6 2016 Students ......................................................... 8 Board Members ....................................................... 10 Artistic Advisory Panels ............................................. 12 Faculty & Staff ......................................................... 16 Volunteers & Partners ................................................ 38 Donors to OAI ......................................................... 40 Endowment Support ................................................. 46 Support OAI ............................................................ 48 1 ABOUT OSAI CELEBRATING 40 YEARS OKLAHOMA SUMMER ARTS INSTITUTE The Oklahoma Summer Arts Institute (OSAI) is an intensive, two-week residential academy for serious, disciplined, and motivated high school students. Students are selected through a competitive, statewide audition process to study with nationally renowned artists in the fields of acting, creative writing, ballet, modern dance, orchestra, chorus, drawing & painting, photography, and film & video. In addition to studying a chosen field for at least six hours a day, students are exposed to a rich variety of art forms and learning experiences. Students and faculty attend and participate in performances, gallery openings, -
Refuge Update
WICHITA MOUNTAINS CLIMBERS COALITION Exposure WMCC Newsletter Volume 10, Fall/Winter 2011 Dedicated to Protecting the Climbing Resources and Natural Environment of the Wichita Mountains After a long hiatus, the WMCC’s Exposure Newsletter, is relaunched, Table of Contents Fixed Anchor Mgmt...........................8 reconnecting our local climbing Refuge Update....................................1 ABC Update........................................9 community and keeping climbers WMCC History...................................2 In Remembrance...............................10 abreast of news, events, and happenings From the Refuge Manager.................4 Tread Lightly......................................11 in the Wichita Mountains. Within this document you will find links to Events Report......................................5 Perspective.........................................12 additional online resources. We hope Quartz Update....................................6 WMCC Membership........................14 you’ll find this updated issue of Announcements..................................7 Purpose and Board...........................14 Exposure both informative and helpful. continue to be managed as it has, to would continue; replacement of fixed Refuge Update “Alternative C” which completely anchors would be allowed and new fixed eliminates rock climbing. However, the anchors would be very limited. The Comprehensive Conservation Plan “Proposed Alternative,” Alternate B, current review process in place would continue to include the WMCC Advisory The U.S. Fish and Wildlife Service is Bolting Committee (ABC) for evaluation working on a long-term management with the Refuge making the final plan for the Wichita Mountains Wildlife approval. Refuge. This plan, called a Comprehensive Conservation Plan The Draft CCP was originally slated to (CCP), will serve as a guide for managing arrive in Fall of 2011 but that date appears the Wichita Mountains Wildlife Refuge to have been pushed back a bit. The Final over the next 15 years. -
Route to Wichita Mountains Wildlife Refuge, Lawton OK
Route to Wichita Mountains Wildlife Refuge, Lawton OK 147 miles total round trip – approximately 3 hrs not counting stops Attractions: Wichita Mountains Wildlife Refuge Visitors Center Mount Scott Prairie dogs, Buffalo, Longhorns Medicine Park, OK This route takes you north through some of the scenic farm lands of Oklahoma west of the I-44 corridor. You will enter into the Wichita Mountains Wildlife Refuge from the Fort Sill west range area. Stop at the Visitors center and see displays and history of the area. Eastward you can head toward Mount Scott that overlooks Lakes Elmer Thomas and Lawtonka. From Mount Scott you can head east to Medicine Park which is a little community with historical restaurants and shops. Wildlife Refuge From the MPEC, head right (West) on 5 th St and take a right (North) on the I-44 ramp Continue North past Burkburnett to the first exit just north of the OK border. Take the right ramp OK-36 North and you will pass 2 casinos on the left. Left at US-70/OK-36 heading West toward Grandfield, OK Right on OK-36 heading North (N2410 Rd) toward Chattanooga, OK Go through Chattanooga Left on N2430 Rd heading North toward Cache, OK Cross over US-62 continuing North (This is also County Hwy 115) Goes into Refuge Right on OK-49 and will see visitors center on your left. The refuge is large with several nice roads to ride that include roaming buffalo, Prairie dog towns, The Holy City and the small town of Mears which is known for its great hamburgers. -
Cambrian Intermediate-Mafic Magmatism
Lithos 260 (2016) 164–177 Contents lists available at ScienceDirect Lithos journal homepage: www.elsevier.com/locate/lithos Cambrian intermediate-mafic magmatism along the Laurentian margin: Evidence for flood basalt volcanism from well cuttings in the Southern Oklahoma Aulacogen (U.S.A.) Matthew E. Brueseke a,⁎,JasperM.Hobbsa, Casey L. Bulen a, Stanley A. Mertzman b, Robert E. Puckett c, J. Douglas Walker d,JoshFeldmand a Department of Geology, Kansas State University, 108 Thompson Hall, Manhattan, KS 66506, United States b Earth and Environment, Franklin and Marshall College, P.O. Box 3003, Lancaster, PA 17604-3003, United States c 12700 Arrowhead Lane, Oklahoma City, OK 73120, United States d Department of Geology, University of Kansas, Lawrence, KS 66045, United States article info abstract Article history: The Southern Oklahoma Aulocogen (SOA) stretches from southern Oklahoma through the Texas panhandle and Received 24 February 2016 into Colorado and New Mexico, and contains mafic through silicic magmatism related to the opening of Accepted 28 May 2016 the Iapetus Ocean during the early Cambrian. Cambrian magmatic products are best exposed in the Wichita Available online 7 June 2016 Mountains (Oklahoma), where they have been extensively studied. However, their ultimate derivation is still somewhat contentious and centers on two very different models: SOA magmatism has been suggested to Keywords: occur via [1] continental rifting (with or without mantle plume emplacement) or [2] transform-fault related Basalt – Large igneous province magmatism (e.g., leaky strike slip faults). Within the SOA, the subsurface in and adjacent to the Arbuckle Rifting Mountains in southern Oklahoma contains thick sequences of mafic to intermediate lavas, intrusive bodies, Iapetus and phreatomagmatic deposits interlayered with thick, extensive rhyolite lavas, thin localized tuffs, and lesser Southern Oklahoma Aulocogen silicic intrusive bodies. -
Overview of Water and Related Resources Part 2
Overview of Water and Related Resources Part 2 Natural Resource & Socioeconomic Characteristics n almost endless array of environmental and socioeconomic characteristics -- including climate, geography, geology, minerals, soils, agriculture, wildlife, recreation, archeology, commerce population and employment -- which affect the current and future availability and use of Oklahomas surface and groundwater supplies. A CLIMATE Climate, along with geography, has a profound influence on water resources and hydrologic characteristics in Oklahoma, which lies across two divergent climatic regions. The states relatively long distance from the moderating effect of the oceans and an absence of mountains to the north often allows cold arctic winds to reach Oklahoma during the winter, which is normally short and mild. In the spring, large thunderstorms develop when warm, moist air from the Gulf of Mexico converges with colder northern, humid eastern and dry western air masses, often producing tornadoes and large hail. Summers in Oklahoma are usually long and hot, punctuated by droughts of varying degree and duration. Fall, though often wet, normally features mild days and cool nights. May ranks as the wettest month while January is the driest. Annual rainfall (Figure 7) varies from more than 50 inches in the relatively warm and humid pine forests of the Ouachita Mountains in southeast Oklahoma to approximately 16 inches in the high plains of the western Panhandle where warm days and cool nights predomi- nate. The state-averaged precipitation is 33.5 inches. The temperatures in Oklahoma (Figure 8) vary from approximately 54 to 62 degrees Fahrenheit from west to east with a state average of 60.5 degrees. -
Sample Full Technical Report
Wichita Mountains Wildlife Refuge Comprehensive Alternative Transportation Plan May 2014 DOT-VNTSC-FWS-14-01 Prepared for: U.S. Fish and Wildlife Service Wichita Mountains Wildlife Refuge – Comprehensive Alternative Transportation Plan 1-ii Notice This document is disseminated under the sponsorship of the U.S. Department of Transportation in the interest of information exchange. The U.S. Government assumes no liability for use of the information contained in this document. This report does not constitute a standard, specification, or regulation. The United States Government does not endorse products or manufacturers. Trademarks or manufacturers’ names appear herein only because they are considered essential to the objective of this document. Quality Assurance Statement The U.S. Fish and Wildlife Service provides high-quality information to serve Government, industry, and the public in a manner that promotes public understanding. Standards and policies are used to ensure and maximize the quality, objectivity, utility, and integrity of its information. The U.S. Fish and Wildlife Service periodically reviews quality issues and adjusts its programs and processes to ensure continuous quality improvement. Wichita Mountains Wildlife Refuge – Comprehensive Alternative Transportation Plan 1-iii REPORT DOCUMENTATION PAGE Form Approved OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Washington Headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302, and to the Office of Management and Budget, Paperwork Reduction Project (0704-0188), Washington, DC 20503. -
Wichita Mountains Wildlife Refuge
Alternative Transportation Study: WICHITA MOUNTAINS WILDLIFE REFUGE August 2010 Prepared for: Federal Highway Administration Central Federal Lands Highway Division Lakewood, CO U.S. Fish and Wildlife Service Refuge Roads Program Division of Visitor Services and Communications Albuquerque, NM Prepared by: John A. Volpe National Transportation Systems Center Research and Innovative Technologies Administration U.S. Department of Transportation ACKNOWLEDGMENTS The U.S. Department of Transportation (USDOT) Volpe National Transportation Systems Center (Volpe Center), in coordination with the Federal Highway Administration - Central Federal Lands Highway Division and the U.S. Fish and Wildlife Service (USFWS), prepared this study with Refuge Roads Program funds. The project team included Charlotte Burger, Gabriel Lopez-Bernal, Luis Mejias, and Eric Plosky of the Volpe Center Systems Operations and Assessment Division. The authors wish to thank the numerous organizations and individuals who graciously provided their time, knowledge and guidance in the development of this report. Those of particular note are listed below: Jeff Rupert (U.S. Fish and Wildlife Service, Wichita Mountains Wildlife Refuge) Ralph Bryant (U.S. Fish and Wildlife Service, Wichita Mountains Wildlife Refuge) Bruce Booth (U.S. Fish and Wildlife Service, Wichita Mountains Wildlife Refuge) Chip Kimball (U.S. Fish and Wildlife Service, Wichita Mountains Wildlife Refuge) Susan Howell (U.S. Fish and Wildlife Service, Wichita Mountains Wildlife Refuge) Vicki Swier (U.S. Fish and Wildlife Service, Wichita Mountains Wildlife Refuge) Quinton Smith (U.S. Fish and Wildlife Service, Wichita Mountains Wildlife Refuge) Susan Law (Federal Highway Administration, Central Federal Lands Highway Division) Nathan Caldwell (U.S. Fish and Wildlife Service) Robert O'Brien (U.S. -
Ages of Pre-Rift Basement and Synrift Rocks Along the Conjugate Rift and Transform Margins of the Argentine Precordillera and Laurentia
Making the Southern Margin of Laurentia themed issue Ages of pre-rift basement and synrift rocks along the conjugate rift and transform margins of the Argentine Precordillera and Laurentia William A. Thomas1, Robert D. Tucker2, Ricardo A. Astini3, and Rodger E. Denison4 1Geological Survey of Alabama, 420 Hackberry Lane, P.O. Box 869999, Tuscaloosa, Alabama 35486-6999, USA 2U.S. Geological Survey, 12201 Sunrise Valley Drive, National Center, MS 926A, Reston, Virginia 20192, USA 3Laboratorio de Análisis de Cuencas, Universidad Nacional de Córdoba, Avenida Velez Sarsfi eld 1611, Ofi cino 7, 2° Piso, X5016GCA Córdoba, Argentina 415141 Kingstree Drive, Dallas, Texas 75248, USA ABSTRACT with Grenville-age rocks along the conjugate 1996, 1999, 2003; Astini and Thomas, 1999; margins of the Precordillera and Laurentia. Ramos, 2004). The Laurentian origin of the Pre- New geochronologic data from basement Ages from one newly analyzed collection, cordillera terrane is based on a variety of data rocks support the interpretation that the however, are older than those from other from Precambrian basement rocks, Early Cam- Argentine Precordillera (Cuyania) terrane basement rocks in the Precordillera. These brian synrift deposits, and a Cambrian–Ordovi- was rifted from the Ouachita embayment of ages, from granodioritic-granitic basement cian passive-margin carbonate succession (e.g., the Iapetan margin of Laurentia. New data clasts in a conglomerate olistolith in Ordo- Astini et al., 1995; Astini, 1998; Astini and from the Ozark dome show a range of ages vician slope deposits, are 1370 ± 2 Ma and Thomas 1999; Thomas and Astini, 1999, 2003; in two groups at 1466 ± 3 to 1462 ± 1 Ma 1367 ± 5 Ma. -
Teacher's Guide
Destinations OklahomaTeacher's Guide Content for this educational program provided by: CIMC Students of All Ages: Your adventure is about to begin! Within these pages you will become a “Geo-Detective” exploring the six countries of Oklahoma. Yes, countries! Within Oklahoma you’ll be traveling to unique places or regions called “countries.” Maybe you’ve heard of “Green Country” with its forests and specialty crops, or “Red Carpet Country,” named for the red rocks and soil formed during the ancient Permian age. Each region or country you visit will have special interesting themes or features, plus fun and sometimes challenging activities that you will be able to do. You will notice each country or region can be identifi ed by natural, economic, historic, cultural, geographic and geological features. The three maps you see on this page are examples of maps you might need for future Geo-Explorations. As a Geo-Detective having fun with the following activities, you’ll experience being a geographer and a geologist at the same time! So for starters, visit these websites and enjoy your Geo-Adventure: http://education.usgs.gov http://www.ogs.ou.edu http://www.census.gov http://www.travelok.com/site/links.asp Gary Gress, Geographer Neil Suneson, Geologist Oklahoma Alliance for Geographic Education Oklahoma Geological Survey Teachers: PASS Standards met by Destinations Oklahoma are listed on pages 15 – 17. Indian Nations of Oklahoma 1889 - Before and after the Civil War, tribal boundaries were constantly changing due to U.S. government policies. Eventually the Eastern and Western tribes merged into a state called “Oklahoma,” meaning “(land of) red people.” Oklahoma's 10 Geographic Regions - These regions refl ect both physical features (topography) and soils.