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Geophysical Mapping of Mount Bonnell Fault of Balcones Fault Zone
Geophysical mapping of Mount Bonnell fault of Balcones fault zone and its implications on Trinity-Edwards Aquifer interconnection, central Texas, USA Mustafa Saribudak1 Abstract There are up to 1200 ft (365 m) of total displacement across the Geophysical surveys (resistivity, natural potential [self-po- BFZ. Faults generally dip steeply (45–85°), varying primarily tential], conductivity, magnetic, and ground penetrating radar) due to specific rock properties and local stress fields (Ferrill and were conducted at three locations across the Mount Bonnell fault Morris, 2008). in the Balcones fault zone of central Texas. The normal fault has The BFZ includes the Edwards and Trinity aquifers, which hundreds of meters of throw and is the primary boundary between are primary sources of water for south-central Texas communities, two major aquifers in Texas, the Trinity and Edwards aquifers. including the city of San Antonio. The Trinity Aquifer underlies In the near surface, the fault juxtaposes the Upper Glen Rose the Edwards Aquifer through the Balcones fault zone. Formation on the Edwards Plateau, consisting of interbedded The BFZ’s most prominent fault is the Mount Bonnell, with limestone and marly limestone, against the Edwards Group, which a vertical throw of up to 600 ft (183 m) (Figure 1). The fault is mostly limestone, on the eastern down-thrown side (coastal hydrogeologically juxtaposes these Cretaceous carbonate aquifers plain). The Upper Glen Rose member is considered to be the during the Miocene tectonic deformation associated with the Upper Trinity Aquifer and also a confining zone underlying the Balcones fault zone, where the younger Edwards Group limestone Edwards Aquifer. -
USGS Water-Resources Investigations Report 97-4133
HYDROGEOLOGIC FRAMEWORK AND GEOCHEMISTRY OF THE EDWARDS AQUIFER SALINE-WATER ZONE, SOUTH-CENTRAL TEXAS U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 97–4133 FRESHWATER ZONE SALINE-WATER ZONE Prepared in cooperation with the EDWARDS AQUIFER AUTHORITY and SAN ANTONIO WATER SYSTEM HYDROGEOLOGIC FRAMEWORK AND GEOCHEMISTRY OF THE EDWARDS AQUIFER SALINE-WATER ZONE, SOUTH-CENTRAL TEXAS By George E. Groschen and Paul M. Buszka U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 97–4133 Prepared in cooperation with the EDWARDS AQUIFER AUTHORITY and SAN ANTONIO WATER SYSTEM Austin, Texas 1997 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Acting Director Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 8011 Cameron Rd. Box 25286 Austin, TX 78754–3898 Denver, CO 80225–0286 ii CONTENTS Abstract ................................................................................................................................................................................ 1 Introduction .......................................................................................................................................................................... 1 Purpose and Scope ................................................................................................................................................... -
Geologic Resource Evaluation Report, Lyndon B. Johnson
National Park Service U.S. Department of the Interior Natural Resource Program Center Lyndon B. Johnson National Historical Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2008/024 ON THE COVER: The cattle on the LBJ Ranch are descended from the same bloodline as the herd that Lyndon Johnson owned. They look more like 1960s Hereford cattle and so they can be called "history on the hoof." Lyndon B. Johnson National Historical Park Web site (www.nps.gov/lyjo, accessed 1/23/2008). NPS Photo Lyndon B. Johnson National Historical Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2008/024 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 February 2008 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer- reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly- published newsletters. -
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. -
Evaluation of the Depositional Environment of the Eagle Ford
Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School 2012 Evaluation of the depositional environment of the Eagle Ford Formation using well log, seismic, and core data in the Hawkville Trough, LaSalle and McMullen counties, south Texas Zachary Paul Hendershott Louisiana State University and Agricultural and Mechanical College, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Earth Sciences Commons Recommended Citation Hendershott, Zachary Paul, "Evaluation of the depositional environment of the Eagle Ford Formation using well log, seismic, and core data in the Hawkville Trough, LaSalle and McMullen counties, south Texas" (2012). LSU Master's Theses. 863. https://digitalcommons.lsu.edu/gradschool_theses/863 This Thesis is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. EVALUATION OF THE DEPOSITIONAL ENVIRONMENT OF THE EAGLE FORD FORMATION USING WELL LOG, SEISMIC, AND CORE DATA IN THE HAWKVILLE TROUGH, LASALLE AND MCMULLEN COUNTIES, SOUTH TEXAS A Thesis Submitted to the Graduate Faculty of the Louisiana State University Agricultural and Mechanical College in partial fulfillment of the requirements for degree of Master of Science in The Department of Geology and Geophysics by Zachary Paul Hendershott B.S., University of the South – Sewanee, 2009 December 2012 ACKNOWLEDGEMENTS I would like to thank my committee chair and advisor, Dr. Jeffrey Nunn, for his constant guidance and support during my academic career at LSU. -
Mollusks from the Pepper Shale Member of the Woodbine Formation Mclennan County, Texas
Mollusks From the Pepper Shale Member of the Woodbine Formation McLennan County, Texas GEOLOGICAL SURVEY PROFESSIONAL PAPER 243-E Mollusks From the Pepper Shale Member of the Woodbine Formation McLennan County, Texas By LLOYD WILLIAM STEPHENSON SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY, 1952, PAGES 57-68 GEOLOGICAL SURVEY PROFESSIONAL PAPER 243-E Descriptions and illustrations of new species offossils of Cenomanian age UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1953 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 25 cents (paper cover) CONTENTS Page Abstract________________________________________________________________ 57 Historical sketch__-___-_-__--__--_l________________-__-_-__---__--_-______ 57 Type section of the Pepper shale member.____________________________________ 58 Section of Pepper shale at Haunted Hill._______________-____-__-___---_------- 58 Systematic descriptions._______.._______________-_-__-_-_-____---__-_-_-_----_ 59 Pelecypoda_ ________________________________________________________ 59 Gastropoda.______-____-_-_____________--_____-___--__-___--__-______ 64 Cephalopoda-_______-_______________________-___--__---_---_-__-— 65 References......___________________________________________________________ 65 Index.__________________________________________________ 67 ILLUSTRATIONS Plate 13. Molluscan fossils, mainly from the Pepper shale__________ -
Late Cretaceous and Tertiary Burial History, Central Texas 143
A Publication of the Gulf Coast Association of Geological Societies www.gcags.org L C T B H, C T Peter R. Rose 718 Yaupon Valley Rd., Austin, Texas 78746, U.S.A. ABSTRACT In Central Texas, the Balcones Fault Zone separates the Gulf Coastal Plain from the elevated Central Texas Platform, comprising the Hill Country, Llano Uplift, and Edwards Plateau provinces to the west and north. The youngest geologic for- mations common to both regions are of Albian and Cenomanian age, the thick, widespread Edwards Limestone, and the thin overlying Georgetown, Del Rio, Buda, and Eagle Ford–Boquillas formations. Younger Cretaceous and Tertiary formations that overlie the Edwards and associated formations on and beneath the Gulf Coastal Plain have no known counterparts to the west and north of the Balcones Fault Zone, owing mostly to subaerial erosion following Oligocene and Miocene uplift during Balcones faulting, and secondarily to updip stratigraphic thinning and pinchouts during the Late Cretaceous and Tertiary. This study attempts to reconstruct the burial history of the Central Texas Platform (once entirely covered by carbonates of the thick Edwards Group and thin Buda Limestone), based mostly on indirect geological evidence: (1) Regional geologic maps showing structure, isopachs and lithofacies; (2) Regional stratigraphic analysis of the Edwards Limestone and associated formations demonstrating that the Central Texas Platform was a topographic high surrounded by gentle clinoform slopes into peripheral depositional areas; (3) Analysis and projection -
Map Showing Geology and Hydrostratigraphy of the Edwards Aquifer Catchment Area, Northern Bexar County, South-Central Texas
Map Showing Geology and Hydrostratigraphy of the Edwards Aquifer Catchment Area, Northern Bexar County, South-Central Texas By Amy R. Clark1, Charles D. Blome2, and Jason R. Faith3 Pamphlet to accompany Open-File Report 2009-1008 1Palo Alto College, San Antonio, TX 78224 2U.S. Geological Survey, Denver, CO 80225 3U.S. Geological Survey, Stillwater, OK 74078 U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Denver, Colorado: 2009 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Clark, A.R., Blome, C.D., and Faith, J.R, 2009, Map showing the geology and hydrostratigraphy of the Edwards aquifer catchment area, northern Bexar County, south- central Texas: U.S. Geological Survey Open-File Report 2009-1008, 24 p., 1 pl. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. 2 Contents Page Introduction……………………………………………………………………….........……..…..4 Physical Setting…………………………………………………………..………….….….….....7 Stratigraphy……………..…………………………………………………………..….…7 Structural Framework………………...……….……………………….….….…….……9 Description of Map Units……………………………………………………….…………...….10 Summary……………………………………………………………………….…….……….....21 References Cited………………………………………….…………………………...............22 Figures 1. -
Pterosaur Distribution in Time and Space: an Atlas 61
Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie B28 DAVID W. E. HONE & ERIC BUFFETAUT (Eds) Flugsaurier: pterosaur papers in honour of Peter Wellnhofer CONTENTS/INHALT Dedication 3 PETER WELLNHOFER A short history of pterosaur research 7 KEVIN PADIAN Were pterosaur ancestors bipedal or quadrupedal?: Morphometric, functional, and phylogenetic considerations 21 DAVID W. E. HONE & MICHAEL J. BENTON Contrasting supertree and total-evidence methods: the origin of the pterosaurs 35 PAUL M. BARRETT, RICHARD J. BUTLER, NICHOLAS P. EDWARDS & ANDREW R. MILNER Pterosaur distribution in time and space: an atlas 61 LORNA STEEL The palaeohistology of pterosaur bone: an overview 109 S. CHRISTOPHER BENNETT Morphological evolution of the wing of pterosaurs: myology and function 127 MARK P. WITTON A new approach to determining pterosaur body mass and its implications for pterosaur fl ight 143 MICHAEL B. HABIB Comparative evidence for quadrupedal launch in pterosaurs 159 ROSS A. ELGIN, CARLOS A. GRAU, COLIN PALMER, DAVID W. E. HONE, DOUGLAS GREENWELL & MICHAEL J. BENTON Aerodynamic characters of the cranial crest in Pteranodon 167 DAVID M. MARTILL & MARK P. WITTON Catastrophic failure in a pterosaur skull from the Cretaceous Santana Formation of Brazil 175 MARTIN LOCKLEY, JERALD D. HARRIS & LAURA MITCHELL A global overview of pterosaur ichnology: tracksite distribution in space and time 185 DAVID M. UNWIN & D. CHARLES DEEMING Pterosaur eggshell structure and its implications for pterosaur reproductive biology 199 DAVID M. MARTILL, MARK P. WITTON & ANDREW GALE Possible azhdarchoid pterosaur remains from the Coniacian (Late Cretaceous) of England 209 TAISSA RODRIGUES & ALEXANDER W. -
April 2014 Midden
The Midden League City Rain Garden by Chris LaChance Galveston Bay Area Chapter - Texas Master Naturalists April 2014 Table of Contents President’s Corner by Maureen Nolan-Wilde, President 2014 Prairie Ponderings 2 Wetland Wanderings 2 In mid-January, current and former board members took part in a planning day at Julie Receives Award 4 Galveston Island State Park. The purpose of the day was to build on the Chapter’s accomplishments, identify opportunities and help plan for the future. 2014 Plant of the Yr. 4 Early People of Texas 6 We developed a “roadmap” that can be used to set goals and focus our efforts for 2014 and beyond. We identified the following areas where we can make immediate Heritage Book Study - 6 improvements: Review Membership 7 Succession planning for key roles (learning exactly what board members and Outreach Survey committee chairs do so that, in the future, this knowledge isn’t lost), Coastal Mammals AT 7 Pelican AT 8 Leveraging current technologies (for example, making better use of the website, social media and tools for sending messages to our members), Diurnal Raptors AT 9 GBA Clan 10 Growing our outreach efforts (such as stewardship and education in schools). WaterSmart Award 12 Since that meeting, we have launched an image database that contains over 1,000 GBAC 1st Camp Out 12 pictures and has been viewed more than 10,200 times. This database, which is easily 2014 Class Fun 14 accessible and can be viewed 24/7, is a great example of using technology to make us more efficient and effective. -
Geological Society of America Bulletin
Downloaded from gsabulletin.gsapubs.org on January 11, 2012 Geological Society of America Bulletin Structural framework of the Edwards Aquifer recharge zone in south-central Texas David A. Ferrill, Darrell W. Sims, Deborah J. Waiting, Alan P. Morris, Nathan M. Franklin and Alvin L. Schultz Geological Society of America Bulletin 2004;116, no. 3-4;407-418 doi: 10.1130/B25174.1 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. -
Geology of the Balcones Fault Zone Along the Growth Corridor of San Antonio, Boerne, Wimberley, and New Braunfels, South-Central Texas
Geology of the Balcones Fault Zone along the Growth Corridor of San Antonio, Boerne, Wimberley, and New Braunfels, South-Central Texas Edward W. Collins Bureau of Economic Geology, The University of Texas at Austin, University Station, Box X, Austin, TX 78713-7508 Extended Abstract The south-central Texas region that encompasses San Antonio, Boerne, Wimberley, and New Braunfels and adjacent areas west of San Antonio and northeast of New Braunfels is undergoing rapid urban growth. It lies within part of the recharge zone of the Edwards aquifer and includes a complex part of the Balcones Fault Zone (Fig. 1). The geology of this region is important to geologists and other professionals involved in planning land use, designing construction projects, and studying the Edwards aquifer. Recharge of the aquifer may be locally enhanced at karst features, faults, and joints. Faulted aquifer strata partly influence regional ground-water flow, and faults locally juxtapose strata having different physical properties, creating potential construction/foundation problems. Geologic maps are some of the most basic and useful sources of information for this geologically critical area of Central Texas. In this study, maps (scale 1:24,000) were prepared for a >1,250 mi2 region; additional mapping west of San Antonio and Boerne is ongoing. Maps have been interpreted using standard field mapping techniques and studying aerial photographs. Compilation and field verification of existing geologic maps of various scales aided map interpretation. This study benefited greatly from the many previous stratigraphic, structural, and mapping studies of the region. The Balcones Fault Zone, one of the main structural features of Central Texas, extends from near Del Rio east-northeastward to San Antonio, where the zone bends northward through New Braunfels, Austin, Georgetown, and Waco and continues toward Dallas.