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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. -
Texas Big Bend and the Davis Mountains April 22-29, 2017
Texas Big Bend and the Davis Mountains Participants: Anne, Craig, David, Frank, Hilary, Jan, Joan, Judith, Lori, Linda, Neil, Skip and Stephen April 22-29, 2017 GUIDES Woody Wheeler and Lynn Tennefoss Sunset through "The Window" at Chisos Basin, Big Bend National Park Day One: El Paso to McNary Reservoir, Balmorhea State Park and Fort Davis Appropriately, we started this journey on Earth Day. We departed from El Paso on an unusually cool but sunny day – ideal for travelling. El Paso and its suburbs swiftly gave way to the vast expanses of the Chihuahuan Desert. An hour east, and well into the desert, we exited off the freeway at McNary Reservoir. At the exit underpass, we found a small colony of Cave Swallows searching for nest sites. This was a life bird for many in our group. Nearby, we pulled into the completely unassuming McNary Reservoir. From below it appears to be a scrubby, degraded bank. Upon cresting the bank, however, there is a sizeable reservoir. Here we found Clark’s Grebes performing a small portion of their spectacular mating dance that resembles a synchronized water ballet. Western Grebes were also nearby, as were a variety of wintering waterfowl and an unexpected flock of Willet. Gambel’s Quail perched conspicuously and called loudly from the shore. Just as we were about to depart, Lynn spotted a lone Ruddy Duck bringing our total to 17 species of Gambel's Quail birds at our first stop. We stopped for lunch at a colorful Mexican restaurant in Van Horn that has hosted a number of celebrities over the years. -
Stratigraphy, Paleontology and Correlation of Lower Cretaceous Exposures in Southeastern New Mexico Barry S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/44 Stratigraphy, paleontology and correlation of lower Cretaceous exposures in southeastern New Mexico Barry S. Kues and Spencer G. Lucas, 1993, pp. 245-260 in: Carlsbad Region (New Mexico and West Texas), Love, D. W.; Hawley, J. W.; Kues, B. S.; Austin, G. S.; Lucas, S. G.; [eds.], New Mexico Geological Society 44th Annual Fall Field Conference Guidebook, 357 p. This is one of many related papers that were included in the 1993 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. -
Unsolved Geological Problems in Oklahoma in 1925
136 THE UNIVERSlTY OF OKLAHOMA XXXII. UNSOLVED GEOLQGICAL PROBLEMS IN OKLAHOMA IN 1925 By eha•. N. Gould, Oklahoma Geological Survey Thirty years ago Mr. Joseph A. T~f of the. Unit.ed Statc~ Geological Survey began work'on the coal fields of Indian 'Uddea. 1. A.. The'lUaa Rock of tile HiP PIaiu. BaD. A.-oc. Pet. (ieoI.. .~oI. VII. J'23, p. 12·74. THE OKLAHOMA ACADEMY OF SCIENCE 137 Territory., Twenty-~ive yea~s,ago the writer founded the D.epart ment of Geology at the University of Oklahoma. For more thaa half the in'tervening time there were relatively few working geolo gists in Oklahoma but during the last decade the numb'er has in creased. The exact number o~ 'geologists living in Oklahoma is un known' but. there are somewhere around 300 names registerett irom this state on t,he rolls of American Association of Petroleum Geologists, and this of course does not represent the entire' nunt- I,er of geologists in the state. ', It might appear to the casual observer that300 men, :fome O'! who~ have been wor'king for at least a decade, should hav" ~olved practically all the ge'ological probiems in the state: As early as 1905, when E. G. Woodruff and I were the 'onl)' working geologists in Oklahoma, in order to attempt to outlin!: the magnftude o~ the <£ubject I prepared a list of the probleQ\ll to be solved in 'Oklahoma geology. So far as I know this list was never pu'blished and I am not now able to find it. -
Please Pass the Salt: Using Oil Fields for the Disposal of Concentrate from Desalination Plants
FINAL REPORT - June 2005 Please Pass the Salt: Using Oil Fields for the Disposal of Concentrate from Desalination Plants PRESSURE 8 0 % % 0 8 0 500 1,000 1,500 2,000 2,500 3,000 3,500 4,000 6 J l 0 C % % a 0 C 0 J + 6 + J J M 4 JJ J O 4 JJ J JJ J J J g 0 J JJ J J J J S JJ JJ J % % J J J J JJ J 1,000 J JJJJJJ J JJJ J J 0 JJJ J JJJJJ JJJJ J J J J 4 JJJ JJJJJ JJ JJ J J J JJJJJJJJJ JJJJJJJJJ JJ 2 JJJJ JJJ JJ J J 0 J JJJJJ JJ JJJJ J J JJ J JJJJJJJJ J J % % J J JJJJJJJJJJ J JJ 2,000 JJ JJJ JJJJJ J J JJJ J 0 J JJJ JJJJJJJJJ JJJ J J JJ 2 JJ JJJJ J J J J JJJ JJ J J JJ J J J JJJJJ J JJ J J J JJ JJJJJJJJ J JJ J J JJJ J J JJJ J J 3,000 JJ JJ JJ J J J J JJ JJ J JJ J J JJ J J J J J J JJ J J J J J J J J JJ J JJJJ J J J JJ J JJ JJ JJJ JJJ J J JJJ J J J J JJ J JJ J J J J 4,000 J J J JJ JJJJJ J J J J JJJJ J J J J J JJ JJJJJ J J JJJJ DEPTH J J J J JJ JJJJ 5,000 J JJJ JJ JJ 2 JJJJ 0 % J JJ % 0 J JJJJ 2 J J J J 80% N JJJ 80% a JJ JJJ 3 6,000 JJJ J + J J O 4 JJ C 0 % K JJJ % J 0 J JJ H S g 4 JJ J O 60% JJ JJ J 60% M 4 7,000 6 JJ 0 J JJ J J J % % J JJ J J J J J 0 J JJ JJJ J J J J 6 JJJJ J 40% J J J J J J J J J J JJ 40% J J J JJ J JJ JJ J JJ 8,000 J J J J J 8 J J J J J JJJJJJ J J J J J J J 0 J J J J JJ JJ J J J J % J JJ J J J J JJ J JJ JJ J % J J JJJ JJJJ JJJJ J JJ J J J JJJJ JJJ J J 0 J JJJJJJ JJJJJJ J J JJJ J J JJ JJJ JJJJJJJ J JJ J 8 J JJ JJJJ JJJJJJ J JJ JJJ J JJ 20% J J JJJ JJJJJJJJJJ JJ JJJJJJ J J J J J JJJ JJJJJJ JJJJJJJ JJJ J JJJJ J 20% J JJ JJJJ JJJJJJJJJJJJJ J JJJ JJJ JJJJ J JJ JJJJJ JJJJJJJJJJJJJJJJJJJ JJJJJJJ J J J JJJJJJJJJJJJJJJJJJJJJJJJ JJJJJJJJJJ -
GSA Poster 2013 Long
Hydrological and Geochemical Characteristics in the Edwards and Trinity Hydrostratigraphic Units Using Multiport Monitor Wells in the Balcones Fault Zone, Hays County, Central Texas Alan Andrews, Brian Hunt, Brian Smith Purpose Rising-falling K Slug-in K Slug-out K Zone Zone (ft/day) (ft/day) (ft/day) Thickness (ft) Trans ft2/day Stratigraphy 21 0.3 -- -- 35 10 Stratigraphy General Hydrologic ID To better understand the hydrogeological properties of and 20 53 -- -- 70 3700 Eagle Ford/ Hydrostratigraphy Function thickness in feet Lithology Porosity/Permeability Sources Rising-falling K Slug K Zone Transmissivity Qal? confining Zone (ft/day) (ft/day) Thickness (ft) (ft2/day) 19 5 8 6 30 140 40-50 Dense limestone Buda unit (CU) Low 18 3 3 -- 25 84 relationships between the geologic units that make up the Confining Units 14 -- -- 136 -- CU Blue-green to 17 38 -- 44 105 4000 Upper Del Rio 50-60 Upper Confining Unit 13 65 -- 72 13000 137.9’ Fract oyster wakestone yellow-brown clay 16 29 80 19 70 2000 12 2 -- 34 460 145.7’ stylolites and fract I Edwards, Upper and Middle Trinity Aquifers and to compare Georgetown Fm. CU Marly limestone; grnst Low 15 29 105 161 75 2100 40-60 11 4 -- 159 8300 Crystalline limestone; mdst to wkst 14 8 10 3 45 370 Leached and 199.6’ fossil (toucasid) vug Aquifer (AQ) III to milliolid grnst; chert; collapse High 10 0.09 -- 197 50 13 4 2 6 40 160 observed hydrologic properties of formations to generally accept- Collapsed mbrs 230’ solutioned bedding plane 30-80 breccia 9 0.005 -- 97 4 12 0.2 -- -- 85 -- 200 feet Reg. -
Bivalvia, Late Jurassic) from South America
Author's personal copy Pala¨ontol Z DOI 10.1007/s12542-016-0310-z RESEARCH PAPER Huncalotis, an enigmatic new pectinoid genus (Bivalvia, Late Jurassic) from South America 1 2 Susana E. Damborenea • He´ctor A. Leanza Received: 29 September 2015 / Accepted: 16 March 2016 Ó Pala¨ontologische Gesellschaft 2016 Abstract The extensive outcrops of the Late Jurassic– orientated at right angles to the shell margins. A few speci- Early Cretaceous Vaca Muerta Formation black shales and mens were found on the outside of large calcareous con- marls in the Neuque´n Basin have yielded very few bivalves, cretions within black shales; these are often articulated, and these are not well known. The material described here complete shells, which preserve the original convexity of the was collected in central Neuque´n, from late Tithonian cal- valves. In some cases these articulated shells seem to be careous levels within the black shales, between beds with associated with large ammonite shells, suggesting an epi- Substeueroceras sp. and with Argentiniceras noduliferum byssate (possibly also pseudoplanktonic) lifestyle. (Steuer). The material is referred to the new genus Huncalotis and to the new species H. millaini. The strongly Keywords Late Tithonian Á Neuque´n Basin Á Vaca inequivalve shells, the ligamental area with a triangular Muerta Formation Á Argentina Á Peru Á Bivalvia Á slightly prosocline resilifer, the right valve with ctenolium Pectinoidea Á Pectinidae and a very deep byssal notch, and the lack of radial orna- mentation make the shell of this new genus strikingly similar Kurzfassung Die reichlich zutage tretenden Schwarz- to the Triassic pectinid Pleuronectites. -
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. -
Index of Surface Water Stations in Texas
1 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY I AUSTIN, TEXAS INDEX OF SURFACE WATER STATIONS IN TEXAS Operated by the Water Resources Division of the Geological Survey in cooperation with State and Federal Agencies Gaging Station 08065000. Trinity River near Oakwood , October 1970 UNITED STATES DEPARTMENT OF THE INTERIOR Geological Survey - Water Resources Division INDEX OF SURFACE WATER STATIONS IN TEXAS OCTOBER 1970 Copies of this report may be obtained from District Chief. Water Resources Division U.S. Geological Survey Federal Building Austin. Texas 78701 1970 CONTENTS Page Introduction ............................... ................•.......•...•..... Location of offices .........................................•..•.......... Description of stations................................................... 2 Definition of tenns........... • . 2 ILLUSTRATIONS Location of active gaging stations in Texas, October 1970 .•.•.•.••..•••••..•.. 1n pocket TABLES Table 1. Streamflow, quality, and reservoir-content stations •.•.•... ~........ 3 2. Low-fla.o~ partial-record stations.................................... 18 3. Crest-stage partial-record stations................................. 22 4. Miscellaneous sites................................................. 27 5. Tide-level stations........................ ........................ 28 ii INDEX OF SURFACE WATER STATIONS IN TEXAS OCTOBER 1970 The U.S. Geological Survey's investigations of the water resources of Texas are con ducted in cooperation with the Texas Water Development -
Carboniferous Formations and Faunas of Central Montana
Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________ -
Foundation Document Big Bend National Park Texas May 2016 Foundation Document
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Big Bend National Park Texas May 2016 Foundation Document Unpaved road Trail Ruins S A N 385 North 0 5 10 Kilometers T Primitive road Private land within I A Rapids G 0 5 10 Miles (four-wheel-drive, park boundary O high-clearance Please observe landowner’s vehicles only) BLACK GAP rights. M WILDLIFE MANAGEMENT AREA Persimmon Gap O U N T A Stillwell Store and RV Park Graytop I N S Visitor Center on Dog Cany Trail d o a nch R 2627 TEXAS Ra a u ng Te r l i 118 Big Bend Dagger Mountain Stairway Mountain S I National Park ROSILLOS MOUNTAINS E R R A DAGGER Camels D r Packsaddle Rosillos e FLAT S Hump E v i l L I Mountain Peak i E R a C r R c Aqua Fria A i T R B n A Mountain o A e t CORAZONES PEAKS u c lat A L ROSILLOS gger F L S Da O L O A d RANCH ld M R n G a Hen Egg U O E A d l r R i Mountain T e T O W R O CHRI N R STM I A Terlingua Ranch o S L L M O a e O d d n U LA N F a TA L r LINDA I A N T G S Grapevine o d Fossil i a Spring o Bone R R THE Exhibit e Balanced Rock s G T E L E P d PAINT GAP l H l RA O N n SOLITARIO HILLS i P N E N Y O a H EV ail C A r Slickrock H I IN r LL E T G Croton Peak S S Mountain e n Government n o i I n T y u Spring v Roys Peak e E R e le n S o p p a R i Dogie h C R E gh ra O o u G l n T Mountain o d e R R A Panther Junction O A T O S Chisos Mountains r TERLINGUA STUDY BUTTE/ e C BLACK MESA Visitor Center Basin Junction I GHOST TOWN TERLINGUA R D Castolon/ Park Headquarters T X o o E MADERAS Maverick Santa Elena Chisos Basin Road a E 118 -
Pre-Atoka Rocks of Northern Arkansas
Pre-Atoka Rocks of Northern Arkansas GEOLOGICAL SURVEY PROFESSIONAL PAPER 314-H Pre-Atoka Rocks of Northern Arkansas By SHERWOOD E. FREZON and ERNEST E. CLICK SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 314-H Thickness, lithofacies, and geologic history of potential oil and gas producing rocks of Paleozoic age in northern Arkansas UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U. S. Geological Survey Library has cataloged this publication as follows: Frezon, Sherwood Earl, 1921- Pre-Atoka rocks of northern Arkansas, by Sherwood E. Frezon and Ernest E. Glick. Washington, U. S. Govt. Print. Off., 1959. iii, 171-189 p. maps, diagrs., table. 30 cm. (U. S. Geological Sur vey. Professional paper 314-H. Shorter contributions to general geology) Part of illustrative matter fold, col., in pocket. Bibliography: p. 186-187. 1. Geology Arkansas. 2. Rocks, Sedimentary. 3. Geology, Strati- graphic Paleozoic. i. Glick, Ernest Earwood, 1922- joint author, n. Title. (Series: U. S. Geological Survey. Professional paper 314-H. Series: U. S. Geological Survey. Shorter contribu tions to general geology) 551.7209767 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Abstract .__----_ ---_-_._--._---__-_-____ 171 Stratigraphy Continued Page Introduction. ___ ___________________________________ 171 Probable latest Mississippian and early