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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. -
QUATERNARY GEOLOGIC MAP of AUSTIN 4° X 6° QUADRANGLE, UNITED STATES
QUATERNARY GEOLOGIC MAP OF AUSTIN 4° x 6° QUADRANGLE, UNITED STATES QUATERNARY GEOLOGIC ATLAS OF THE UNITED STATES MAP I-1420 (NH-14) State compilations by David W. Moore and E.G. Wermund, Jr. Edited and integrated by David W. Moore, Gerald M. Richmond and Ann Coe Christiansen 1993 NOTE: This map is the product of collaboration of the Texas Bureau of Economic Geology and the U.S. Geological Survey, and is designed for both scientific and practical purposes. It was prepared in two stages. First, the map and map explanations were prepared by the State compiler. Second, information on the map was integrated with that of adjacent maps, locally supplemented, and related to a uniform map symbol classification by the editors. Map unit descriptions were edited, supplemented, and coordinated with those of other maps of this series so that individual unit descriptions are applicable throughout both this map and all other maps of the series. Problems of mapping or interpretation in different areas were resolved by correspondence to the extent possible; most simply reflect differences in available information or differences in philosophies of mapping and serve to encourage further investigation. Less than forty percent of the surficial deposits of the United States have been mapped and described. Traditionally, mapping of surficial deposits has focused on glacial, alluvial, eolian, lacustrine, marine, and landslide deposits. Slope and upland deposits have been mapped in detail only in restricted areas. However, an enormous amount of engineering construction and many important problems of land use and land management are associated with regions that have extensive slope and upland deposits (colluvium and residuum, for example). -
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 Glimpse of Some of the Geology and Mineral Resources: Sierra Blanca
THE EL.PAS0 GEOLOGICAL SOCIETY I I GUIDEBOOK i FIFTH ANNUAL FIELD TRIP I I I I A GLIMPSE OF SOME OF THE I GEOLOGY AND MINERAL RESOURCES I I SIERRA BLANCA-VAN HORN COUNTRY HUDSPETH AND CULBEWSON COUNTIES TEXAS > APRIL 3, 1971 iii TABLE OF CONTENTS F - The Texas Lineament in Eagle Flat, Texas ------------- 28 INTRODUCTION The Trans Pecos region of West Texas has attracted the attention I it deserves as a source of useful minerals both metallic and nsn- metallic. Because of the preoccupation of the people of Texas with petroleum production, many have overlooked the fact that them have been several important metal mines tn this province and that talc deposi ts are s ti1 l being worked here. Undoubtedly othep economic mineral deposits exist in the region awai ting discovery by intensive geological prospecting. The af'fi cers of the El Paso Geological Society and the field trip leadek hope that this trip will heighten inteest in the finding and developing of mineral deposi ts in Trans Pecos Texas. We welcome all our visitcs~sand know that they will wish to jodn us in thanking all those who made thds trip possible. We wish especially to acknowledge the kindness of the Pioneer Talc Company in showing us through the mill at Allamore and allowlng the group to visdt the Texsla- Talc mine. We also wish to thank Mr. Sandy Neal of Van Haon for per- mission to cross the Neal Ranch on the way to the Hazel Wne. John M. Hills, President El Paso Geological Society EL PAS0 GEOLOGICAL SOCIETY OFFICERS John M. -
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. -
Stormwater Management Program 2013-2018 Appendix A
Appendix A 2012 Texas Integrated Report - Texas 303(d) List (Category 5) 2012 Texas Integrated Report - Texas 303(d) List (Category 5) As required under Sections 303(d) and 304(a) of the federal Clean Water Act, this list identifies the water bodies in or bordering Texas for which effluent limitations are not stringent enough to implement water quality standards, and for which the associated pollutants are suitable for measurement by maximum daily load. In addition, the TCEQ also develops a schedule identifying Total Maximum Daily Loads (TMDLs) that will be initiated in the next two years for priority impaired waters. Issuance of permits to discharge into 303(d)-listed water bodies is described in the TCEQ regulatory guidance document Procedures to Implement the Texas Surface Water Quality Standards (January 2003, RG-194). Impairments are limited to the geographic area described by the Assessment Unit and identified with a six or seven-digit AU_ID. A TMDL for each impaired parameter will be developed to allocate pollutant loads from contributing sources that affect the parameter of concern in each Assessment Unit. The TMDL will be identified and counted using a six or seven-digit AU_ID. Water Quality permits that are issued before a TMDL is approved will not increase pollutant loading that would contribute to the impairment identified for the Assessment Unit. Explanation of Column Headings SegID and Name: The unique identifier (SegID), segment name, and location of the water body. The SegID may be one of two types of numbers. The first type is a classified segment number (4 digits, e.g., 0218), as defined in Appendix A of the Texas Surface Water Quality Standards (TSWQS). -
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. -
MEXICO Las Moras Seco Creek K Er LAVACA MEDINA US HWY 77 Springs Uvalde LEGEND Medina River
Cedar Creek Reservoir NAVARRO HENDERSON HILL BOSQUE BROWN ERATH 281 RUNNELS COLEMAN Y ANDERSON S HW COMANCHE U MIDLAND GLASSCOCK STERLING COKE Colorado River 3 7 7 HAMILTON LIMESTONE 2 Y 16 Y W FREESTONE US HW W THE HIDDEN HEART OF TEXAS H H S S U Y 87 U Waco Lake Waco McLENNAN San Angelo San Angelo Lake Concho River MILLS O.H. Ivie Reservoir UPTON Colorado River Horseshoe Park at San Felipe Springs. Popular swimming hole providing relief from hot Texas summers. REAGAN CONCHO U S HW Photo courtesy of Gregg Eckhardt. Y 183 Twin Buttes McCULLOCH CORYELL L IRION Reservoir 190 am US HWY LAMPASAS US HWY 87 pasas R FALLS US HWY 377 Belton U S HW TOM GREEN Lake B Y 67 Brady iver razos R iver LEON Temple ROBERTSON Lampasas Stillhouse BELL SAN SABA Hollow Lake Salado MILAM MADISON San Saba River Nava BURNET US HWY 183 US HWY 190 Salado sota River Lake TX HWY 71 TX HWY 29 MASON Buchanan N. San G Springs abriel Couple enjoying the historic mill at Barton Springs in 1902. R Mason Burnet iver Photo courtesy of Center for American History, University of Texas. SCHLEICHER MENARD Y 29 TX HW WILLIAMSON BRAZOS US HWY 83 377 Llano S. S an PECOS Gabriel R US HWY iver Georgetown US HWY 163 Llano River Longhorn Cavern Y 79 Sonora LLANO Inner Space Caverns US HW Eckert James River Bat Cave US HWY 95 Lake Lyndon Lake Caverns B. Johnson Junction Travis CROCKETT of Sonora BURLESON 281 GILLESPIE BLANCO Y KIMBLE W TRAVIS SUTTON H GRIMES TERRELL S U US HWY 290 US HWY 16 US HWY P Austin edernales R Fredericksburg Barton Springs 21 LEE Somerville Lake AUSTIN Pecos -
Stratigraphic and Hydrogeologic Framework of Part of the Coastal Plain of Texas
Report 2361 I STRAT~ RAPHIC AND HYDROGEOLOGIC FRAMEr ORK OF PART OF THE COAST, L PLAIN ·OF TEXAS TEXAS DE RTMENT OF WATER RESOURCE~S July 1979 TEXAS DEPARTMENT OF WATER RESOURCES REPORT 236 STRATIGRAPHIC AND HYDROGEOLOGIC FRAMEWORK OF PART OF THE COASTAL PLAIN OF TEXAS By E. T. Baker, Jr. United States Geological Survey This report was prepared by the U.S. Geological Survey under cooperative agreement with the Texas Department of Water Resources. July 1979 TEXAS DEPARTMENT OF WATER RESOURCES Harvey Davis, Executive Director TEXAS WATER DEVELOPMENT BOARD A. L. Black, Chairman John H. Garrett, Vice Chairman Milton Potts Glen E. Roney George W. McCleskey W. O. Bankston TEXAS WATER COMMISSION Felix McDonald, Chairman Dorsey B. Hardeman, Commissioner Joe R. Carroll, Commissioner Authorization for use or reproduction of any original material contained in this publicatiun, i.e., not obtained from other sources, is freely granted. The Department would appreciate acknowledgement. Published and distributed by the Texas Department of Water Resources Post Office Box 13087 Austin, Texas 78711 ii TABLE OF CONTENTS Page ABSTRACT .. INTRODUCTION 3 Acknowledgements 3 Metric Conversions 35 STRATIGRAPHIC FRAMEWORK. 35 General Features of Deposition and Correlation Problems 35 Stratigraphic Units 35 Pre-Miocene 35 Miocene. 36 Post-Miocene 38 HYDROGEOLOGIC FRAMEWORK 38 Catahoula Confining System (Restricted) . 38 Jasper Aquifer ..... 39 Burkeville Confining System 40 Evangeline Aquifer 40 Chicot Aquifer 40 SELECTED REFERENCES 42 TABLE 1. Stratigraphic and Hydrogeologic Framework of Part of the Coastal Plain of Texas ........... 4 FIGURES 1. Index Map Showing Location of Sections. 5 iii TABLE OF CONTENTS-Continued Page 2-15. -
Prize Bridge 1960 •
PRIZE BRIDGE 1960 • Prize Bridges 1960 Steel b1'idges selected tn the annual national competition conducted by the Ame1'ican Insti tute of Steel Const1'uction as the most beautiful b~'idges opened to traffic in 1960. • AMERICAN INSTITUTE OF STEEL CONSTRUCTION, INC. 101 Park Avenue, New York 17, N. Y. • • ~ury of Award A. L. AYDELOTT, AlA A. L. Aydelott and Associates, Architects Memphis, Tennessee THOMAS S. BUECHNER Director The Brooklyn Museum Brooklyn, New YOl'k GLENN W. HOLCOMB President American Society of Civil Engineers Professor, Civil Engineering Oregon State University • Corvallis, Oregon GEORGE LINDSTROM Lundstrom & Skubic, Architects Chicago, Illinois GEOFFREY PLATT, FAIA Architect New York City, New York 'J ; • Beauty in Steel Bridges The enduring beauty of steel bridges is eloquent tribute to the vision and skill of the men who plan, design and build them. The bridge de igner of today is both artist and engineer. He understands the potential for strength and beauty which is inherent in steel structures, and he knows that aesthetic appearance can be achieved at no sacrifice of efficiency or economy. The simple grace of a highway overpass, no less than the majestic sweep of a river crossing reflects a creative integration of structure, func tion and form, skillfully executed in beautiful bridges of steel. To promote a more widespread appreciation of the aesthetics of steel bridges and to honor the architectural excellence of modern bridge design, the American Institute of Steel Construction sponsors an annual Prize Brid'ge Competition. Each year a distinguished Jury of Award, composed of leading art directors, architects and engineers, selects the steel bridges which it judges to be the most beautiful of those opened to traffic in the • United States during the previous year. -
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 ....................................................................................................................