Geologic and Geochemical Characterization of Cross-Communication Potential Within the Northern Edwards Aquifer System, Texas" (2016)
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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 ................................................................................................................................................... -
Chapter 3 Assessment.Pdf
068 11/15/02 5:05 PM Page 68 TERMS & NAMES READING SOCIAL STUDIES Explain the significance of each of the After You Read following: Review your completed chart. Using 1. Rio Grande the information in each column, Mapping Texas Lands 2. Coastal Plains region write your own definitions for Texas can be divided into 3. North Central Plains region physical geography and human regions of similar landforms, geography. Then, with a partner, 4. Great Plains region climate, and precipitation. discuss the following questions: 5. Mountains and Basins region Which key words reflect the physi- 6. census cal geography and human geogra- phy of your town or city? How has REVIEW QUESTIONS the physical geography had an Mapping Texas Lands (pages 46–50) impact on the human geography? 1. Which is likely to change more GEOGRAPHY over a ten-year period, an area’s physical geography or Physical Human Geography Geography its human geography? Explain. 2. Why do you think average temperatures decrease as Mapping Texas People elevation increases? People are drawn to some Identifying the Four Regions of regions more than others Texas (pages 52–57) because of climate, natural resources, 3. Rank the four regions of Texas or the availability in order from largest to small- of jobs. est. How might life in Texas differ if this order were reversed? 4. Based on your knowledge of CRITICAL THINKING Texas regions, what type of Drawing Conclusions physical geography would you expect to see in northern 1. What do you think is the value Mexico? in eastern New of understanding the physical Mexico? in southern Okla- geography of Texas? Identifying the Four homa? in western Louisiana? Drawing Conclusions Regions of Texas Mapping Texas People (pages 61–67) 2. -
Trammel's Trace on Printed Maps of the 19Th Century
CRHR Research Reports Volume 1 Article 2 2-18-2015 Trammel's Trace on Printed Maps of the 19th Century Kelley A. Snowden Stephen F. Austin State University, [email protected] Follow this and additional works at: https://scholarworks.sfasu.edu/crhr_research_reports Part of the Geography Commons, and the History Commons Tell us how this article helped you. Recommended Citation Snowden, Kelley A. (2015) "Trammel's Trace on Printed Maps of the 19th Century," CRHR Research Reports: Vol. 1 , Article 2. Available at: https://scholarworks.sfasu.edu/crhr_research_reports/vol1/iss1/2 This Article is brought to you for free and open access by SFA ScholarWorks. It has been accepted for inclusion in CRHR Research Reports by an authorized editor of SFA ScholarWorks. For more information, please contact [email protected]. Trammel’s Trace on Printed Maps of the 19th Century Kelley A. Snowden Center for Regional Heritage Research, Stephen F. Austin State University ____________________________________________________________________________________ Trammel’s Trace was a nineteenth century road that traversed East Texas. Recognized today as a historic cartographic feature, this road appeared in different ways on nineteenth century printed published maps over time, and in the mid-to-late nineteenth centu- ry was reduced from a route to a fragment. This study is the first to examine the portrayal of the Trace as a historic cartographic feature, how it was presented to the general public, how its portrayal changed over time, and why it appears on the maps at all. In addition, this study is the first to use geographic information systems (GIS) to analyze the presentation of the Trace on printed, published maps. -
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. -
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. -
Albian Rudist Biostratigraphy (Bivalvia), Comanche Shelf to Shelf Margin, Texas
Carnets Geol. 16 (21) Albian rudist biostratigraphy (Bivalvia), Comanche shelf to shelf margin, Texas Robert W. SCOTT 1, 2 2 Yulin WANG 2 Rachel HOJNACKI Yulin WANG 3 Xin LAI 4 Highlights • Barremian-Albian caprinids biostratigraphic zones are revised and integrated with ammonites and benthic foraminifers. • New caprinid rudist species are the key to revising long-held correlations of Albian strata on the Co- manche shelf, Texas. • On the San Marcos Arch, central Texas, the shallow shelf Person Formation is the upper unit of the Fredericksburg Group. • The Person underlies the basal Washita Group sequence boundary Al Sb Wa1 and the Georgetown Formation. Abstract: Rudists were widespread and locally abundant carbonate producers on the Early Cretaceous Comanche Shelf from Florida to Texas, and on Mexican atolls. As members of the Caribbean Biogeogra- phic Province, their early ancestors emigrated from the Mediterranean Province and subsequently evol- ved independently. Comanchean rudists formed biostromes and bioherms on the shelf interior and at the shelf margin. Carbonate stratigraphic units of the Comanche Shelf record rudist evolution during the Barremian through the Albian ages and an established zonal scheme is expanded. This study documents new Albian rudist occurrences from the Middle-Upper Albian Fredericksburg and Washita groups in Central and West Texas. Rudists in cores at and directly behind the shelf margin southeast of Austin and San Antonio, Texas, complement the rudist zonation that is integrated with ammonites and foraminifers. These new rudist data test long-held correlations of the Edwards Group with both the Fredericksburg and Washita groups based solely on lithologies. Rudist and foraminifer biostratigraphy indicate that the Edwards Group is coeval with the Fredericksburg not the Washita Group. -
GEOLOGIC QUADRANGLE MAP NO. 49 Geology of the Pedernales Falls Quadrangle, Blanco County, Texas
BUREAU OF ECONOMIC GEOLOGY THE UNIVERSITY OF TEXAS AT AUSTIN AUSTIN, TEXAS 78712 W. L. FISHER, Director GEOLOGIC QUADRANGLE MAP NO. 49 Geology of the Pedernales Falls Quadrangle, Blanco County, Texas By VIRGIL E. BARNES November 1982 THE UNIVERSITY OF TEXAS AT AUSTIN TO ACCOMPANY MAP-GEOLOGIC BUREAU OF ECONOMIC GEOLOGY QUADRANGLE MAP NO. 49 GEOLOGY OF THE PEDERNALES FALLS QUADRANGLE, BLANCO COUNTY, TEXAS Virgil E. Barnes 1982 CONTENTS General setting .. .. .. ............... 2 Cretaceous System (Lower Cretaceous) . 10 Geologic formations ......... .. ... 2 Trinity Group . 10 Paleozoic rocks ........... .. .. 2 Travis Peak Formation . 10 Cambrian System (Upper Cambrian) . 2 Sycamore Sand . 10 Moore Hollow Group ....... 2 Hammett Shale and Cow Creek Wilberns Formation . ........ 2 Limestone . 10 San Saba Member . .. .... 2 Shingle Hills Formation . 10 Ordovician System (Lower Ordovician) .. 3 Hensen Sand Member . 10 Ellenburger Group . ... .. .... 3 Glen Rose Limestone Member . 10 Tanyard Formation .. ... .... 3 Cenozoic rocks . 11 Threadgill Member ..... ... 3 Quaternary System . 11 Staendebach Member ....... 3 Pleistocene Series . 11 Gorman Formation ...... 4 Terrace deposits . 11 Honeycut Formation ......... 5 Recent Series . 11 Devonian system . .. .... .... 7 Alluvium . 11 Stribling Formation .... .. .. 7 Subsurface geology . 11 Devonian-Mississippian rocks . ...... 8 Mineral resources . 12 Joint fillings ...... ... ... 8 Construction materials . 12 Houy Formation ....... .. .. 8 Building stone . 12 Mississippian System ......... ... -
Changing Patterns and Perceptions of Water Use In
CHANGING PATTERNS AND PERCEPTIONS OF WATER USE IN EAST CENTRAL TEXAS SINCE THE TIME OF ANGLO SETTLEMENT A Dissertation by WENDY WINBORN PATZEWITSCH Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY May 2007 Major Subject: Geography CHANGING PATTERNS AND PERCEPTIONS OF WATER USE IN EAST CENTRAL TEXAS SINCE THE TIME OF ANGLO SETTLEMENT A Dissertation by WENDY WINBORN PATZEWITSCH Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Approved by: Chair of Committee, Jonathan M. Smith Committee Members, Peter J. Hugill Christian Brannstrom Bradford P. Wilcox Head of Department, Douglas J. Sherman May 2007 Major Subject: Geography iii ABSTRACT Changing Patterns and Perceptions of Water Use in East Central Texas Since the Time of Anglo Settlement. (May 2007) Wendy Winborn Patzewitsch, B.A., Trinity University; M.S., Southern Methodist University Chair of Advisory Committee: Dr. Jonathan M. Smith Patterns and perceptions of water use have changed since Anglo settlement in Texas in the early nineteenth century. Change has not been constant, gradual, or linear, but rather has occurred in fits and spurts. This pattern of punctuated equilibrium in water use regimes is the central finding of this dissertation. Water use is examined in terms of built, organizational, and institutional inertias that resist change in the cultural landscape. Change occurs only when forced by crisis and results in water management at an increasing scale. Perception is critical in forcing response to crisis. -
• Approvea Auguet. 1924•
THiS I) !_i~ c·::r':::::'t.L ~!A~lUS::!UPT IT IlAY 1101 DE COPIED WITHOUT THE AUTHOR'S PEBWISSIOH • Approve a Auguet. 1924• • • TIllS IS A:l O:'I-::::l.L l:'~:lUS:nlrr IT MAY llOT fiE COPIE' WITHour THE AUTHOR'S PEBuISSION THE SOURCE OF THE VIA TER ALONG THE BALCOllES FAULT ESCARl'1lSHT TI1E SOURCE OF TI1E IVA TER ALOIiG TI1E BALCOllES FAULT ESCAlU'1ll':1iT TI1ESDl Presented to the FaoUlty of the Grsduate Sohool of Ths University of Texas in Partial Fulfill ment of the Requirements For the Degree of MASTER OF ARTS By Alfred Knox Tyson, B.A. , Maysfiald, Tsxas Austin, Texas June 1924 235013 PREFACE The subject of this paper wss suggested to the writer by Dr. H. P. Bybee, who has continuously interested himself in the completion of the work. The writer, however, is deep~y appreciative of the time~y suggestions. va~UBb~e dets. and constant wi~~ingness of Professor F. L. Whitney to aid him in the preparation of the work. Dr. F. W. Simonds and Dr. E. P. Schoch a~so furnished suggestions and data which helped the author. Assiatance in determining the analyses of various water samples was rendered by the Division of Industrial Chemistry. Bureau of Economic Geology and Technology. ProfeSBor F. L. Whitney. Mr. W. A. Maley and Mr. E. A. Wendlandt kind~y aided in the preparation of the mapB. Austin. Texas AuguBt.~924. • COllTEllTS CaAPTER I Page Introduction 6 Locetion of Area........................ 6 Topography and drainag•••.•••••••••••••• 7 Climate end rainfall•..•.•••••••••••.••• 8 Balconea Escarpment BS 8 physiographic feature ••..•.••.•....••• 9 CaAPTER II Stratigraphic Geology•.. -
Geologic Summary
View metadata, citation and similar papers at core.ac.uk brought to you by CORE G 4032 provided by UT Digital Repository T3 cs 2005 C6 GEOL MAPS Miscellaneous Map No. 43 eologic Map of the West Half of the Taylor, Texas, 30 x 60 Minute Quadrangle: Central Texas Urban Corridor, Encompassing Round Rock, Georgetown, Salado, Briggs, Liberty Hill, and Leander Edward W. Collins ;;;;;;;;;;;;;;; -!!!!!!!!!!!!!!! Ill - Q. < - :::E ;;;;;;;;;;;;;;; CJ .J - 0 rn w ;;;;;;;;;;;;;;; er c(J -;;;;;;;;;;;;;;; " c(J U) c(J 0 = c() Ill ;;;;;;;;;;;;;;; ::r 0 ~ ...-'! 0 - ru N Ill 0 ;;;;;;;;;;;;;;; M - I- N = M 0 - 'It' -!!!!!!!!!!!!!!! - " Bureau of Economic Geology Scott W. Tinker, Director John A. and Katherine G. Jackson School of Geosciences The University of Texas at Austin Austin, Texas 78713-8924 2005 Miscellaneous Map No. 43 Geologic Map of the West Half of the Taylor, Texas, 30 x 60 Minute Quadrangle: Central Texas Urban Corridor, Encompassing Round Rock, Georgetown, Salado, Briggs, Liberty Hill, and Leander Edward W. Collins Bureau of Economic Geology Scott W. Tinker, Director John A. and Katherine G. Jackson School of Geosciences The University of Texas at Austin Austin, Texas 78713-8924 2005 ( CONTENTS ABSTRACT ....................................................................................................................... l INTRODUCTION ............................................................................................................ 1 Methods ..................................................................................................................... -
Stephenville Curriculum Document Social Studies Grade: 7 Course: Texas History Bundle (Unit) 1 Est
STEPHENVILLE CURRICULUM DOCUMENT SOCIAL STUDIES GRADE: 7 COURSE: TEXAS HISTORY BUNDLE (UNIT) 1 EST. NUMBER OF DAYS 20 UNIT 1 NAME Natural Texas, its people and their government Unit Overview Narrative This is a study of the physical geography of Texas that focuses on location, climate, regions and natural resources. Additionally, students will explore the cultural impact of this environment on the earliest inhabitants of Texas. Geography sets the foundation for how a society defines who it becomes. Generalizations/Enduring Understandings Using geographic tools gives humans a standardized measuring system to an ever changing world. All civilizations have an agreed upon understanding for their social order and structure. Concepts What are the differences between physical and human geography? What are the most important aspects humans look for when settling an area? What are the major concepts that define a culture? What role did geography play in developing the many different cultures of early Native Texans? Guiding/Essential Questions What are some of the ways different societies govern themselves? How is geography studied, measured, and interpreted? What tools are used to interpret geography? How would you explain the ideals of a democratic society? What are the similarities and differences that can be found between the United States’ and Texas’ governments? Learning Targets Formative Assessments Summative Assessments TEKS Specifications (1) History. The student understands traditional Locations- relative and absolute location (longitude and historical points of reference in Texas history. The Latitude) and how they relate to historical events student is expected to: (A) identify the major eras in Texas history, Native Texans- study of tribes and their effect on early Texas.