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Baylor Geological Studies
BAYLORGEOLOGICA L STUDIES PAUL N. DOLLIVER Creative thinking is more important than elaborate FRANK PH.D. PROFESSOR OF GEOLOGY BAYLOR UNIVERSITY 1929-1934 Objectives of Geological Training at Baylor The training of a geologist in a university covers but a few years; his education continues throughout his active life. The purposes of train ing geologists at Baylor University are to provide a sound basis of understanding and to foster a truly geological point of view, both of which are essential for continued professional growth. The staff considers geology to be unique among sciences since it is primarily a field science. All geologic research in cluding that done in laboratories must be firmly supported by field observations. The student is encouraged to develop an inquiring ob jective attitude and to examine critically all geological concepts and principles. The development of a mature and professional attitude toward geology and geological research is a principal concern of the department. Frontis. Sunset over the Canadian River from near the abandoned settlement of Old Tascosa, Texas. The rampart-like cliffs on the horizon first inspired the name "Llano Estacado" (Palisaded Plain) among Coronado's men. THE BAYLOR UNIVERSITY PRESS WACO, TEXAS BAYLOR GEOLOGICAL STUDIES BULLETIN NO. 42 Cenozoic Evolution of the Canadian River Basin Paul N. DoUiver BAYLOR UNIVERSITY Department of Geology Waco, Texas Spring 1984 Baylor Geological Studies EDITORIAL STAFF Jean M. Spencer Jenness, M.S., Editor environmental and medical geology O. T. Ph.D., Advisor, Cartographic Editor what have you Peter M. Allen, Ph.D. urban and environmental geology, hydrology Harold H. Beaver, Ph.D. -
Hon. H. A. Beckwith, Chairman Board of Water Engineers 302 West Fifteenth Street Austin, Texas Opinion No
Hon. H. A. Beckwith, Chairman Board of Water Engineers 302 West Fifteenth Street Austin, Texas Opinion No. V-1307 Re: Purposes for which the appropriation to the In- terstate Compact Commis- Bion may be used during the biennium ending Au- gust 31, 1953. Dear Sir: You have requested an opinion of this office re- lating to the purposes for which expenditures may be made from the appropriation to the Interstate Compact Commission in the general anoronriation bill for the biennium ending August 31, 1953.--I-i.@. 426, Acts 52nd Leg., R. S. 1951, ch. 499, p. 1228, at p. 1374. The various statutes pertaining to the Interstate Compact Commission and related agencies will be summarized in chronological order so that your specific questions can be placed in the proper perspective. The Le lslature created the Interstate Compact Commission In 19& 9, and authorized the Governor to appoint an Interstate Compact Commissioner 'to negotiate an agree- ment with each of the affected States respecting the use, control and disposition of'the waters of the Canadian, Red and Sabine Rivers and their tributaries" and to tlmakethe necessary investigations and procure the necessary data for the proper performance of his duties, and may, with the approval of the Governor, employ such clerical, legal, engineering and other assistance as may be necessary in the performance of such duties." H.B. 594, Acts 51st Leg., R.S. 1949, ch. 380, p. 716 (Art. 7466g, V.C.S.) The stat- ute and emergency clause make clear that the Commissioner's duties were the negotiation of agreements and the investi- gating and procuring or data necessary to the negotiations concerning the above-named rivers. -
The Native Fish Fauna of Major Drainages East of The
THE NATIVE FISH FAUNA OF MAJOR DRAINAGES EAST OF THE CONTINENTAL DIVIDE IN NEW MEXICO A Thesis Presented to the Graduate Faculty of Biology Eastern New Mexico University In Partial Fulfillment of the Requirements fdr -the7Degree: Master of Science in Biology by Michael D. Hatch December 1984 TABLE OF CONTENTS Page Introduction Study Area Procedures Results and Discussion Summary Acknowledgements Literature Cited Appendices Abstract INTRODUCTION r (t. The earliest impression of New Mexico's native fish fauna =Ems during the 1850's from naturalists attached to various government survey parties. Without the collections from these and other early surveys, the record of the native fish fauna would be severely deficient because, since that time, some 1 4 native species - or subspecies of fish have become extirpated and the ranges of an additionial 22 native species or subspecies have become severly re- stricted. Since the late Miocene, physiographical changes of drainages have linked New Mexico, to varying degrees, with contemporary ichthyofaunal elements or their progenitors from the Rocky Mountains, the Great Plains, the Chihuahuan Desert, the Mexican Plateau, the Sonoran Desert and the Great Basin. Immigra- tion from these areas contributed to the diversity of the state's native ichthyofauna. Over the millinea, the fate of these fishes waxed and waned in ell 4, response to the changing physical and _chenaca-l-conditions of the surrounding environment. Ultimately, one of the most diverse fish faunas of any of the interior southwestern states developed. Fourteen families comprising 67 species of fish are believed to have occupied New Mexico's waters historically, with strikingly different faunas evolving east and west of the Continental Divide. -
A History of Fort Bascom in the Canadian River Valley
New Mexico Historical Review Volume 87 Number 3 Article 4 7-1-2012 Boots on the Ground: A History of Fort Bascom in the Canadian River Valley James Blackshear Follow this and additional works at: https://digitalrepository.unm.edu/nmhr Recommended Citation Blackshear, James. "Boots on the Ground: A History of Fort Bascom in the Canadian River Valley." New Mexico Historical Review 87, 3 (2012). https://digitalrepository.unm.edu/nmhr/vol87/iss3/4 This Article is brought to you for free and open access by UNM Digital Repository. It has been accepted for inclusion in New Mexico Historical Review by an authorized editor of UNM Digital Repository. For more information, please contact [email protected], [email protected], [email protected]. Boots on the Ground a history of fort bascom in the canadian river valley James Blackshear n 1863 the Union Army in New Mexico Territory, prompted by fears of a Isecond Rebel invasion from Texas and its desire to check incursions by southern Plains Indians, built Fort Bascom on the south bank of the Canadian River. The U.S. Army placed the fort about eleven miles north of present-day Tucumcari, New Mexico, a day’s ride from the western edge of the Llano Estacado (see map 1). Fort Bascom operated as a permanent post from 1863 to 1870. From late 1870 through most of 1874, it functioned as an extension of Fort Union, and served as a base of operations for patrols in New Mexico and expeditions into Texas. Fort Bascom has garnered little scholarly interest despite its historical signifi cance. -
Oklahoma City's Drinking Water in a Struggling Watershed
Oklahoma City’s Drinking Water Keywords: planning - watershed & strategic, public health, restoration, in a Struggling Watershed stormwater, water quality The Oklahoma City Watershed Organization Name: The North Canadian River—a key component of Oklahoma City’s watershed—runs 441 miles from New Mexico to Central Oklahoma, where it joins the Canadian River and Lake Eufaula. Oklahoma City channels much of the river water into reservoir lakes, including Hefner and Overholser, which together with the other regional lakes, supply drinking water to the city and surrounding neighborhoods. The Oklahoma Water Resources Board, lakes are also stocked with popular fish, and residents use the lakes sub-grantee of the Oklahoma and river for recreational boating and rowing. Like most metropolitan Secretary of Energy and rivers, the North Canadian is highly engineered, its levels controlled Environment according to various demands, including water treatment, recreation, and maintenance of drinking water supplies. About the Organization: The mission of the Oklahoma Water Both Lake Hefner and Lake Overholser have a long history of Resources Board (OWRB) is to eutrophication, a harmful condition characterized by lack of oxygen, protect and enhance the quality of resulting in excessive algal growth and death of wildlife. Eutrophic life for Oklahomans by managing conditions are caused by nutrient-rich runoff from point sources (such and improving the state’s water as factories and sewage treatment plants) and non-point sources (such resources to ensure clean and reliable as stormwater carrying pollutants and agricultural fertilizers). water supplies, a strong economy, and a safe and healthy environment. Location: Oklahoma City, OK Contact Information: Chris Adams, Ph.D. -
North Canadian River Ranch 1,230 + Acres | Woodward County, Woodward, Ok
NORTH CANADIAN RIVER RANCH 1,230 + ACRES | WOODWARD COUNTY, WOODWARD, OK BRYAN PICKENS Partner/Broker Associate 214-552-4417 [email protected] REPUBLICRANCHES.COM NORTH CANADIAN RIVER RANCH The North Canadian River Ranch is an impeccable live-water hunting and recreational trophy property which stands out from other ranches on the market. It has diverse terrain, a terrific lodge on a serene setting complete with a top-notch grass airstrip, and is quiet, remote, and full of game and outdoor opportunities typical for this part of the state. This northwest Oklahoma ranch has an excellent blend of rolling sand hills, grassland meadows and productive cultivated areas, prime habitat for whitetail deer, bob white quail, and rio grande turkeys. Price: $2,850,000 Woodward County 1,230 +/-Acres Luxury log cabin hunting lodge 3 main pastures for cattle 4 water wells Whitetail deer, quail, abundant game 2 fishing ponds 2.3 miles of North Canadian River Improvements: The luxury log cabin hunting lodge was completely remodeled in 2008, complete with a new roof and exterior stone. It has approximately 4,400 sf of living space, and approximately 2,000 sf of porch area. The setup is excellent for large groups or families. 5 bedrooms, each with a full bath. (4 bedrooms + 1 master suite) Stone tile flooring, hand-scraped hardwoods, and granite countertops. Two geo thermal heating/cooling units. Covered porch overlooking the lake to the south. Screened in porch overlooking the lake to the south. High-end appliances and advanced water filtration system. Sprinklered irrigation system for the entire yard. -
Canadian River Basin Bioassessment
Canadian River Basin Bioassessment Sarah Robertson, Melissa Parker, Gordon Linam, Clinton Robertson, Archis Grubh Texas Parks and Wildlife Department, Inland Fisheries Division AND Melissa Casarez University of Texas at Austin, Biodiversity Collections River Studies Report No. 26 Inland Fisheries Division Texas Parks and Wildlife Department Austin, Texas October 2017 TABLE OF CONTENTS Executive Summary .............................................................................................................. 1 Introduction ........................................................................................................................... 2 Study Area ................................................................................................................. 2 Survey and Management History .............................................................................. 2 Study Sites .............................................................................................................................. 4 Canadian River .......................................................................................................... 6 Oxbow Lakes ............................................................................................................. 6 Supplemental Fish Collection Sites ........................................................................... 7 Water Quality and Quantity .................................................................................................... 8 Fish Assemblage .................................................................................................................... -
Canadian River Project, Texas, January 1954, 29-32; Water and Power Resources, Project Data, 108
Canadian River Project Eric A. Stene Bureau of Reclamation 1995 Table of Contents The Canadian River Project......................................................2 Project Location.........................................................2 Historic Setting .........................................................3 Project Authorization.....................................................4 Construction History .....................................................6 Post Construction History ................................................17 Settlement ............................................................18 Uses of Project Water ...................................................19 Conclusion............................................................21 About the Author .............................................................21 Bibliography ................................................................22 Manuscripts and Archival Collections.......................................22 Government Documents .................................................22 Articles...............................................................22 Index ......................................................................24 1 The Canadian River Project The Texas panhandle lies in the southern portion of the "Great American Desert" as the Great Plains were known in the mid-nineteenth century. The consistent shortage of rainwater and runoff forced area residents to rely on groundwater pumping for many years. As area urbanization and industries grew, -
Hydrogeology and Water Quality of the North Canadian River Alluvium, Concho Reserve, Canadian County, Oklahoma______
HYDROGEOLOGY AND WATER QUALITY OF THE NORTH CANADIAN RIVER ALLUVIUM, CONCHO RESERVE, CANADIAN COUNTY, OKLAHOMA__________ By Carol J. Becker U. S. DEPARTMENT OF INTERIOR U.S. GEOLOGICAL SURVEY Open-File Report 97-657 Prepared in cooperation with the Cheyenne and Arapaho Tribes of Oklahoma Oklahoma City, Oklahoma 1998 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY THOMAS J. CASADEVALL, Acting Director Any use of trade names in this publication is for descriptive purposes only and does not impiy endorsement by the U.S. Government. UNITED STATES GOVERNMENT PRINTING OFFICE: OKLAHOMA CITY 1998_____ For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services Water Resources Division Box 25286 202 NW 66th Street, Building 7 Denver, CO 80225-0286 Oklahoma City, OK 73116 CONTENTS Abstract..........................................................^^ Introduction ..........................................._^ Purrwse and Scope................................................^ Acknowledgments..................................................................................^^ Description of stody area...................................................................................................................................» Methods of study................................................................................................................................................. Seismic-Refraction -
Geomorphic Development of the Canadian River Valley, Texas Panhandle: an Example of Regional Salt Dissolution and Subsidence
Geomorphic development of the Canadian River Valley, Texas Panhandle: An example of regional salt dissolution and subsidence THOMAS C. GUSTAVSON Bureau of Economic Geology, The University of Texas, Austin, Texas 78713 ABSTRACT dian River Valley is primarily the result of regional salt dissolution and subsidence that have been active throughout the late Tertiary and Quater- Development of the Canadian River Valley in the Texas Pan- nary. The Deaf Smith County nuclear waste repository site, one of three handle resulted mostly from regional subsidence following dissolution recently identified sites, is located in the southern part of the study area of Permian bedded salts. Salts of the Clear Fork, Glorieta, San (Fig. 1). Andres, and Seven Rivers Formations have undergone dissolution along the margins of the Palo Duro, Dalhart, and Anadarko Basins. GEOLOGIC SETTING The Canadian River Valley follows a zone of subsidence for >208 km (130 mi) across the High Plains. High solute loads (3,000 ppm Late Paleozoic tectonic movements resulted in the Amarillo Uplift, chloride) in the Canadian River and historical development of sink- the Cimarron Arch and the Bravo Dome, and the adjacent Palo Duro, holes indicate that dissolution and subsidence processes are still active. Dalhart, and Anadarko Basins (Fig. 2) (Birsa, 1977). By middle Permian Evidence that these processes have been active in the region since the time, these basins were essentially filled, and the area evolved into an middle Tertiary includes Pliocene lake sediments and Quaternary extensive marine shelf, covering the northern portion of the Permian basin, terrace alluvium that have been deformed by dissolution-induced sub- where salt and other evaporites accumulated (Dutton and others, 1979; sidence as well as former sinkholes filled with lacustrine sediments of Handford and Dutton, 1980). -
TPWD Strategic Planning Regions
River Basins TPWD Brazos River Basin Brazos-Colorado Coastal Basin W o lf Cr eek Canadian River Basin R ita B l anca C r e e k e e ancar Cl ita B R Strategic Planning Colorado River Basin Colorado-Lavaca Coastal Basin Canadian River Cypress Creek Basin Regions Guadalupe River Basin Nor t h F o r k of the R e d R i ver XAmarillo Lavaca River Basin 10 Salt Fork of the Red River Lavaca-Guadalupe Coastal Basin Neches River Basin P r air i e Dog To w n F o r k of the R e d R i ver Neches-Trinity Coastal Basin ® Nueces River Basin Nor t h P e as e R i ve r Nueces-Rio Grande Coastal Basin Pease River Red River Basin White River Tongue River 6a Wi chita R iver W i chita R i ver Rio Grande River Basin Nor t h Wi chita R iver Little Wichita River South Wichita Ri ver Lubbock Trinity River Sabine River Basin X Nor t h Sulphur R i v e r Brazos River West Fork of the Trinity River San Antonio River Basin Brazos River Sulphur R i v e r South Sulphur River San Antonio-Nueces Coastal Basin 9 Clear Fork Tr Plano San Jacinto River Basin X Cypre ss Creek Garland FortWorth Irving X Sabine River in San Jacinto-Brazos Coastal Basin ity Rive X Clea r F o r k of the B r az os R i v e r XTr n X iityX RiverMesqu ite Sulphur River Basin r XX Dallas Arlington Grand Prai rie Sabine River Trinity River Basin XAbilene Paluxy River Leon River Trinity-San Jacinto Coastal Basin Chambers Creek Brazos River Attoyac Bayou XEl Paso R i c h land Cr ee k Colorado River 8 Pecan Bayou 5a Navasota River Neches River Waco Angelina River Concho River X Colorado River 7 Lampasas -
Canadian River Compact
CANADIAN RIVER COMPACT The state of New Mexico, the state of Texas, and the state of Oklahoma, acting through their commissioners, John H. Bliss, for the state of New Mexico, E. V. Spence for the state of Texas, and Clarence Burch for the state of Oklahoma, after negotiations participated in by Berkeley Johnson, appointed by the president as the representative of the United States of America, have agreed respecting Canadian river as follows: ARTICLE I The major purposes of this compact [this section] are to promote interstate comity; to remove causes of present and future controversy; to make secure and protect present developments within the states; and to provide for the construction of additional works for the conservation of the waters of Canadian river. ARTICLE II As used in this compact: (a) the term "Canadian river" means the tributary of Arkansas river which rises in northeastern New Mexico and flows in an easterly direction through New Mexico, Texas and Oklahoma and includes North Canadian river and all other tributaries of said Canadian river; (b) the term "North Canadian river" means that major tributary of Canadian river officially known as North Canadian river from its source to its junction with Canadian river and includes all tributaries of North Canadian river; (c) the term "commission" means the agency created by this compact for the administration thereof; (d) the term "conservation storage" means that portion of the capacity of reservoirs available for the storage of water for subsequent release for domestic, municipal, irrigation and industrial uses, or any of them, and it excludes any portion of the capacity of reservoirs allocated solely to flood control, power production and sediment control, or any of them.