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Mountains, Streams, and Lakes of Oklahoma I
Information Series #1, June 1998 Mountains, Streams, and Lakes of OklahomaI Kenneth S. Johnson2 INTRODUCTION valleys, hills, and plains throughout most of the re mainder of Oklahoma (Fig. 1). All the major lakes and Mountains and streams define the landscape of reservoirs of Oklahoma are man-made, and they are Oklahoma (Fig. 1). The mountains consist mainly of important for flood contr()l, water supply, recreation, resistant rock masses that were folded, faulted, and and generation of hydroelectric power. Natural lakes thrust upward in the geologic past (Fig. 2), whereas in Oklahoma are limited to oxbow lakes along major the streams have persisted in eroding less-resistant streams and to playa lakes in the High Plains region rock units and lowering the landscape to form broad of the west. Alphabetical List of20 Lakes with Largest Surface Area (from Oklahoma Water Atlas, Oklahoma Water Resources Board) 1. Broken Bow 11. Lake 0' The Cherokees 2. Canton 12. Oologah 3. Eufaula 13. Robert s. Kerr 4. Fort Gibson 14. Sardis 5. Foss 15. Skiatook 6. Great Salt Plains 16. Tenkiller Ferry ·7. Hudson 17. Texoma 8. Hugo 18. Waurika 9. Kaw 19. Webbers Falls 10. Keystone 20. Wister Modified from Historical Atlas of Oklahoma, by John W. Morris, Charles R. Goins, and Edwin C. 25 McReynolds. Copyright © 1986 by the University I of Oklahoma Press. o 40 80Km Figure 1. Mountains, streams, and principal lakes of Oklahoma. lReprinted from Oklahoma Geology Notes (1993), vol. 53, no. 5, p. 180-188. The Notes article was reprinted and expanded from Oklahoma Almanac, 1993-1994, Oklahoma Department of Lihraries, p. -
Cover for Web.Pmd
Little River National Wildlife Refuge Swamp/Marsh Site McCurtain County Location. This reference wetland is a portion of the Little River stream system. It is located on the east side of the Little River National Wildlife Refuge. Latitude: 33° 57' 44". Longitude: 94° 37' 36". Legal: Sec 7 T7S R26E. General Description. This reference site represents wetlands that border the Little River stream system in McCurtain County. This wetland landform is characterized by long and narrow depressions in broad flood plains and whose origin can be traced to abandoned stream channels. Surface water accumulation is from out-of-bank flooding and/or runoff from adjacent areas. Sediment loading is limited to large flood events. Groundwater tables are 1 to 3 feet above the surface during the winter and early spring. These wetlands range in size from 2 to 80 acres. Vegetative Community. Vegetation is dominated by an overstory of bald cypress. Understory vegetation is limited to the margins of the ponded water and consists of Hercules club, blue beech and buttonbush. In the ponded water, the sites are dominated by stinkweed and bladderworts. When disturbed by 66 drainage or filling, these sites convert to water primrose, smartweed, frog fruit and lizard’s tail. Tree trunks are buttressed and root systems are fluted. Hydrology. The water in these wetlands are provided by frequent floods of long duration and/or groundwater. Water tables range in depth from one to three feet above the surface the with the highest levels occurring during the winter through early summer. Subsurface water typically moves through out the soil profile. -
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. -
Oklahoma Today Spring 1980 Volume 30 No. 2
HONORABLE GEORGE NIGH Great Plains Country Enters The 1980s .....................4 Governor By Sue Carter VOLUME 30 NUMBER 2 SPRING 1980 Mountain Climbers' Paradise: Wichita Mountains Wildlife Refuge. ... 8 By Paul McCl~ng SUE CARTER PAUL E. LEFEBVRE Editor Art and Production BlLL BUSCH Dauntless Gold Seekers of the Wichitas .................... 11 C~rculat~on and Promotion By Steve Wilson Published hy the Oklahoma Tourism and Recreauon Deparln~enl Delores Buffalo Takes Us To Indian City. ..... BvJoye R. Boulton COMMISSION MEMBERS LT. GOV. SPENCER BERNARD BOB HODDER JIM PATE Wedding at Holy City. ..... Chalrman Oklahoma C~tyV~ce Chalrman Mad111 Secretary By Sheila Samples JAKE J SIMMONS. JR LARRY FIELD Muskogee Guymon Pageantry, Tradition Follow The Artillery Hunt .... BOB HINTON CELlA ROSENBERGER WR DICK STUBBS By Sheila Samples Altus Tulsa Henryetta BILL KELLOW. Dlr ABE L HESSER RON ACREE. Dlr Red Rock Canyon Family Reunion. ...... Tour~smPromollon Plannlng & Development Execut~veD~rector By Judith Wall W D JOHNSON. Dlr ROBERT A PIKE Dlr KEN FLAMING Dlr Adm~n~strat~on State Parks State Lodges Quartz Mountain Resort Fascinates Hikers .................. 25 11 1s Ihe purvose 01 Oklahoma Today lo dovole llself lo Ihe enule stale 01 Oklaho~naand 11s evay poslllve aspecl the scenery culture recreallonal and vls~lorallracllny evenls 11s lndustly nalural and By John Davis man made wonders 11s achievements 11s herrlage 11s presenl and 11s tulure Quartz Visitors Discover The World of Jeff Briley, Naturalist. ...... 27 502 WILL ROGERS BUILDING .Oklahoma C~ty73105 .(405) 521-2496 By Gary Lantz $5 00 Pel Year In U S S9 00 Elsewhere SI 25 Srnyle Copy Copyr~ghl1980 by Oklahoma Today Mayazrne L~lho111 Oklaho~na Restaurant Diners Enjoy Tales Of Oklahoma's First Resort ....... -
TOPOGRAPHIC MAP of OKLAHOMA Kenneth S
Page 2, Topographic EDUCATIONAL PUBLICATION 9: 2008 Contour lines (in feet) are generalized from U.S. Geological Survey topographic maps (scale, 1:250,000). Principal meridians and base lines (dotted black lines) are references for subdividing land into sections, townships, and ranges. Spot elevations ( feet) are given for select geographic features from detailed topographic maps (scale, 1:24,000). The geographic center of Oklahoma is just north of Oklahoma City. Dimensions of Oklahoma Distances: shown in miles (and kilometers), calculated by Myers and Vosburg (1964). Area: 69,919 square miles (181,090 square kilometers), or 44,748,000 acres (18,109,000 hectares). Geographic Center of Okla- homa: the point, just north of Oklahoma City, where you could “balance” the State, if it were completely flat (see topographic map). TOPOGRAPHIC MAP OF OKLAHOMA Kenneth S. Johnson, Oklahoma Geological Survey This map shows the topographic features of Oklahoma using tain ranges (Wichita, Arbuckle, and Ouachita) occur in southern contour lines, or lines of equal elevation above sea level. The high- Oklahoma, although mountainous and hilly areas exist in other parts est elevation (4,973 ft) in Oklahoma is on Black Mesa, in the north- of the State. The map on page 8 shows the geomorphic provinces The Ouachita (pronounced “Wa-she-tah”) Mountains in south- 2,568 ft, rising about 2,000 ft above the surrounding plains. The west corner of the Panhandle; the lowest elevation (287 ft) is where of Oklahoma and describes many of the geographic features men- eastern Oklahoma and western Arkansas is a curved belt of forested largest mountainous area in the region is the Sans Bois Mountains, Little River flows into Arkansas, near the southeast corner of the tioned below. -
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. -
Description of the Coalgate Quadrangle
' *' DESCRIPTION OF THE COALGATE QUADRANGLE. By Joseph A. Taff. GEOGRAPHY. forms of the Ouachita Mountain Range. The a long time the valleys become wide and silted, that at ordinary conditions the stream meanders ridges of the valley region are nearly parallel and the hills are gradually reduced to the level in rivulets or narrow channels. Indeed, its chan GENERAL RELATIONS. with those of the range, but, with the exception of the valleys. nel is so choked with sand that the water does The Coalgate quadrangle is bounded by the of the few isolated mountains which lie in Arkan The surface of the Coalgate quadrangle is of not at any stage of the river flow on the country meridians 96° and 96° 30' and the parallels 34° sas Valley, they have low relief. low relief, and the topographic features indicate rock. During floods, which usually come in 30' and 35°, and thus occupies one- Extentand The Prairie Plains region stretches from the that it has been so for a relatively long period of spring from the headwaters of the river, vast quarter of a square degree of the earth's th1?Juad=f Arkansas Valley and Ozark highland regions time. The larger streams have nearly ceased cut quantities of sands are swept down, shifting for surface. It is 34.4 miles long north rangle> northward and westward across north- Character ting their valleys deeper, and throughout most of mer shoals and channels. Little River, which is and south and 28.5 miles wide, and contains west Indian Territory into Oklahoma their courses are meandering in the deposits of silt tributary to the Canadian, crosses the northwest nearly 980 square miles. -
Ouachita Mountains Ecoregional Assessment December 2003
Ouachita Mountains Ecoregional Assessment December 2003 Ouachita Ecoregional Assessment Team Arkansas Field Office 601 North University Ave. Little Rock, AR 72205 Oklahoma Field Office 2727 East 21st Street Tulsa, OK 74114 Ouachita Mountains Ecoregional Assessment ii 12/2003 Table of Contents Ouachita Mountains Ecoregional Assessment............................................................................................................................i Table of Contents ........................................................................................................................................................................iii EXECUTIVE SUMMARY..............................................................................................................1 INTRODUCTION..........................................................................................................................3 BACKGROUND ...........................................................................................................................4 Ecoregional Boundary Delineation.............................................................................................................................................4 Geology..........................................................................................................................................................................................5 Soils................................................................................................................................................................................................6 -
University of Oklahoma
UNIVERSITY OF OKLAHOMA GRADUATE COLLEGE WISTER AREA FOURCHE MALINE: A CONTESTED LANDSCAPE A DISSERTATION SUBMITTED TO THE GRADUATE FACULTY in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY By SIMONE BACHMAI ROWE Norman, OKlahoma 2014 WISTER AREA FOURCHE MALINE: A CONTESTED LANDSCAPE A DISSERTATION APPROVED FOR THE DEPARTMENT OF ANTHROPOLOGY BY ______________________________ Dr. Lesley RanKin-Hill, Co-Chair ______________________________ Dr. Don Wyckoff, Co-Chair ______________________________ Dr. Diane Warren ______________________________ Dr. Patrick Livingood ______________________________ Dr. Barbara SafiejKo-Mroczka © Copyright by SIMONE BACHMAI ROWE 2014 All Rights Reserved. This work is dedicated to those who came before, including my mother Nguyen Thi Lac, and my Granny (Mildred Rowe Cotter) and Bob (Robert Cotter). Acknowledgements I have loved being a graduate student. It’s not an exaggeration to say that these have been the happiest years of my life, and I am incredibly grateful to everyone who has been with me on this journey. Most importantly, I would like to thank the Caddo Nation and the Wichita and Affiliated Tribes for allowing me to work with the burials from the Akers site. A great big thank you to my committee members, Drs. Lesley Rankin-Hill, Don Wyckoff, Barbara Safjieko-Mrozcka, Patrick Livingood, and Diane Warren, who have all been incredibly supportive, helpful, and kind. Thank you also to the Sam Noble Oklahoma Museum of Natural History, where most of this work was carried out. I am grateful to many of the professionals there, including Curator of Archaeology Dr. Marc Levine and Collections Manager Susie Armstrong-Fishman, as well as Curator Emeritus Don Wyckoff, and former Collection Managers Liz Leith and Dr. -
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.