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Speleogenesis and Delineation of Megaporosity and Karst
Stephen F. Austin State University SFA ScholarWorks Electronic Theses and Dissertations 12-2016 Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas Jon T. Ehrhart Stephen F. Austin State University, [email protected] Follow this and additional works at: https://scholarworks.sfasu.edu/etds Part of the Geology Commons, Hydrology Commons, and the Speleology Commons Tell us how this article helped you. Repository Citation Ehrhart, Jon T., "Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas" (2016). Electronic Theses and Dissertations. 66. https://scholarworks.sfasu.edu/etds/66 This Thesis is brought to you for free and open access by SFA ScholarWorks. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of SFA ScholarWorks. For more information, please contact [email protected]. Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas Creative Commons License This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License. This thesis is available at SFA ScholarWorks: https://scholarworks.sfasu.edu/etds/66 Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas By Jon Ehrhart, B.S. Presented to the Faculty of the Graduate School of Stephen F. Austin State University In Partial Fulfillment Of the requirements For the Degree of Master of Science STEPHEN F. -
Salado Formation Followed
GW -^SZ-i^ GENERAL CORRESPONDENCE YEAR(S): B. QUICK, Inc. 3340 Quail View Drive • Nashville, TN 37214 Phone: (615) 874-1077 • Fax: (615) 386-0110 Email: [email protected] November 12,2002 Mr Roger Anderson Environmental Bureau Chief New Mexico OCD 1220 S. ST. Francis Dr. 1 Santa Fe, NM 87507 Re: Class I Disposal Wells Dear Roger, I am still very interested in getting the disposal wells into salt caverns in Monument approved by OCD. It is my sincere belief that a Class I Disposal Well would be benefical to present and future industry in New Mexico. I suspect that one of my problems has been my distance from the property. I am hoping to find a local company or individuals who can be more on top of this project. In the past conditions have not justified the capital investment to permit, build and operate these wells and compete with surface disposal. Have there been any changes in OCD policy that might effect the permitting of these wells? If so, would you please send me any pretinent documents? Sincerely, Cc: Lori Wrotenbery i aoie or moments rage i uu Ctoraeferiz&MoiHi ©ff Bedded Satt fltoir Storage Caverns Case Stundy from the Midlamdl Basim Susan D. Hovorka Bureau of Economic Geology The University of Texas at Austin AUG1 0R9 9 Environmental Bureau Introduction to the Problem °" Conservation D/ws/on About solution-mined caverns l^Btg*** Geolojy_ofsalt Purpose, scope, and methods of our study Previous work: geologic setting of the bedded salt in the Permian Basin J^rV^W^' " Stratigraphic Units and Type Logs s Midland Basin stratigraphy -
Dissolution of Permian Salado Salt During Salado Time in the Wink Area, Winkler County, Texas Kenneth S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/44 Dissolution of Permian Salado salt during Salado time in the Wink area, Winkler County, Texas Kenneth S. Johnson, 1993, pp. 211-218 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. -
Play Analysis and Digital Portfolio of Major Oil Reservoirs in the Permian Basin
Play Analysis and Digital Portfolio of Major Oil Reservoirs in the Permian Basin: Application and Transfer of Advanced Geological and Engineering Technologies for Incremental Production Opportunities Final Report Reporting Period Start Date: January 14, 2002 Reporting Period End Date: May 13, 2004 Shirley P. Dutton, Eugene M. Kim, Ronald F. Broadhead, Caroline L. Breton, William D. Raatz, Stephen C. Ruppel, and Charles Kerans May 2004 Work Performed under DE-FC26-02NT15131 Prepared by Bureau of Economic Geology John A. and Katherine G. Jackson School of Geosciences The University of Texas at Austin University Station, P.O. Box X Austin, TX 78713-8924 and New Mexico Bureau of Geology and Mineral Resources New Mexico Institute of Mining and Technology Socorro, NM 87801-4681 DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability for responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. iii ABSTRACT The Permian Basin of west Texas and southeast New Mexico has produced >30 Bbbl (4.77 × 109 m3) of oil through 2000, most of it from 1,339 reservoirs having individual cumulative production >1 MMbbl (1.59 × 105 m3). -
Geologic Map of the Kitchen Cove 7.5-Minute Quadrangle, Eddy County, New Mexico by Colin T
Geologic Map of the Kitchen Cove 7.5-Minute Quadrangle, Eddy County, New Mexico By Colin T. Cikoski1 1New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, NM 87801 June 2019 New Mexico Bureau of Geology and Mineral Resources Open-file Digital Geologic Map OF-GM 276 Scale 1:24,000 This work was supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program (STATEMAP) under USGS Cooperative Agreement G18AC00201 and the New Mexico Bureau of Geology and Mineral Resources. New Mexico Bureau of Geology and Mineral Resources 801 Leroy Place, Socorro, New Mexico, 87801-4796 The views and conclusions contained in this document are those of the author and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government or the State of New Mexico. Executive Summary The Kitchen Cove quadrangle lies along the northwestern margin of the Guadalupian Delaware basin southwest of Carlsbad, New Mexico. The oldest rocks exposed are Guadalupian (upper Permian) carbonate rocks of the Seven Rivers Formation of the Artesia Group, which is sequentially overlain by similar strata of the Yates and Tansill Formations of the same Group. Each of these consists dominantly of dolomitic beds with lesser fine-grained siliciclastic intervals, which accumulated in a marine or marginal-marine backreef or shelf environment. These strata grade laterally basinward (here, eastward) either at the surface or in the subsurface into the Capitan Limestone, a massive fossiliferous “reef complex” that lay along the Guadalupian Delaware basin margin and is locally exposed on the quadrangle at the mouths of Dark Canyon and Kitchen Cove. -
Overview of the Geologic History of Cave Development in the Guadalupe Mountains, New Mexico
Carol A. Hill - Overview of the geologic history of cave development in the Guadalupe Mountains, New Mexico. Journal of Cave and Karst Studies 62(2): 60-71. OVERVIEW OF THE GEOLOGIC HISTORY OF CAVE DEVELOPMENT IN THE GUADALUPE MOUNTAINS, NEW MEXICO CAROL A. HILL 17 El Arco Drive, Albuquerque, NM 87123-9542 USA [email protected] The sequence of events relating to the geologic history of cave development in the Guadalupe Mountains, New Mexico, traces from the Permian to the present. In the Late Permian, the reef, forereef, and backreef units of the Capitan Reef Complex were deposited, and the arrangement, differential dolomitization, jointing, and folding of these stratigraphic units have influenced cave development since that time. Four episodes of karsification occurred in the Guadalupe Mountains: Stage 1 fissure caves (Late Permian) developed primarily along zones of weakness at the reef/backreef contact; Stage 2 spongework caves (Mesozoic) developed as small interconnected dissolution cavities during limestone mesogenesis; Stage 3 thermal caves (Miocene?) formed by dissolution of hydrothermal water; Stage 4 sulfuric acid caves (Miocene-Pleistocene) formed by H2S-sulfuric acid dissolution derived hypogenically from hydro- carbons. This last episode is reponsible for the large caves in the Guadalupe Mountains containing gyp- sum blocks/rinds, native sulfur, endellite, alunite, and other deposits related to a sulfuric acid speleoge- netic mechanism. This paper provides an overview of events affecting cave of the Delaware Basin. The Capitan Formation in the Delaware development in the Guadalupe Mountains of New Mexico. Basin is exposed in the northwestern Guadalupe Mountains Table 1 outlines the sequence of karst events, integrated with section, the southwestern Apache Mountains section, and the the regional geology. -
Subsurface Petroleum Geology of Santa Rosa Sandstone (Triassic), Northeast New Mexico
COVER—Well-developed primary porosity in Santa Rosa sandstone, 800-810 ft, Husky Oil Co. and General Crude Oil Co. No. 1 Hanchett State, Sec. 16, T. 8 N., R. 24 E., Guadalupe County, New Mexico. Circular 193 New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Subsurface petroleum geology of Santa Rosa Sandstone (Triassic), northeast New Mexico by Ronald F. Broadhead New Mexico Bureau of Mines & Mineral Resources SOCORRO 1984 111 Contents A B S T R A C T 5 DOCKUM SEDIMENTOLOGY 13 INTRODUCTION 5 STRUCTURE 15 PETROLEUM METHODS OF INVESTIGATION 5 OCCURRENCES 17 STRATIGRAPHY 9 PETROGRAPHY AND RESERVOIR SAN ANDRES FORMATION (PERMIAN: GE OL O G Y 1 7 LEONARDIAN) 9 LOWER SANDSTONE UNIT OF SANTA ROSA ARTESIA GROUP (PERMIAN: GUADALUPIAN) 9 SANDSTONE 19 Grayburg-Queen unit 9 UPPER SANDSTONE UNIT OF SANTA ROSA Seven Rivers Formation 10 SANDSTONE 19 Yates-Tansill unit 10 CUERVO MEMBER OF CHINLE FORMATION 19 BERNAL FORMATION PETROLEUM POTENTIAL OF SANTA ROSA (PERMIAN: GUADALUPIAN) 10 SANDSTONE AND CUERVO MEMBER OF DOCKUM GROUP (TRIASSIC) 11 CHINLE FORMATION 20 Santa Rosa Sandstone 11 SANTA ROSA SANDSTONE 20 Lower sandstone unit 12 CUERVO MEMBER OF CHINLE Middle mudstone unit 12 FORMATION 21 REFERENCES 21 Upper sandstone unit 12 Chinle Formation 13 Lower shale member 13 Cuervo Sandstone Member 13 Upper shale member 13 Redonda Formation 13 Figures 1—Study area and locations of tar-sand deposits 6 2—Stratigraphic chart of Upper Permian and Triassic rocks in northeast New Mexico 9 3—(in pocket)—East-west -
Outcropping Permian Shelf Formations of Eastern New Mexico Vincent C
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/23 Outcropping Permian shelf formations of eastern New Mexico Vincent C. Kelley, 1972, pp. 72-78 in: East-Central New Mexico, Kelley, V. C.; Trauger, F. D.; [eds.], New Mexico Geological Society 23rd Annual Fall Field Conference Guidebook, 236 p. This is one of many related papers that were included in the 1972 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. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Capitan Reef Complex Structure and Stratigraphy
Capitan Reef Complex Structure and Stratigraphy Report by Allan Standen, P.G. Steve Finch, P.G. Randy Williams, P.G., Beronica Lee-Brand, P.G. Assisted by Paul Kirby Texas Water Development Board Contract Number 0804830794 September 2009 TABLE OF CONTENTS 1. Executive summary....................................................................................................................1 2. Introduction................................................................................................................................2 3. Study area geology.....................................................................................................................4 3.1 Stratigraphy ........................................................................................................................4 3.1.1 Bone Spring Limestone...........................................................................................9 3.1.2 San Andres Formation ............................................................................................9 3.1.3 Delaware Mountain Group .....................................................................................9 3.1.4 Capitan Reef Complex..........................................................................................10 3.1.5 Artesia Group........................................................................................................11 3.1.6 Castile and Salado Formations..............................................................................11 3.1.7 Rustler Formation -
"Geology & Ground-Water Conditions in Southern Lea County, New
ItI *1. I.4 GROUND-WTATER REPORT 6 an4 A.; Geology and Ground-Water 54 Conditions in Southern I Lea County, New Mexico by ALEXANDER NICHOLSON, Jr. C,'I and ALFRLD CLEBSCH, JR. UN!TED STATES GEOLOGICAL SUR'VEY i I I i i I i I' ;it it. STATE BUREAU OF MINES AND MINERAL RESOURCES .t64 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO Contents Page NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY ABSTRACT ............................................. 1 E. J. Workman, President INTRODUCTION ....................................... 2 Location and area ....................................... 2 History and scope of investigation ......................... 2 STATE BUREAU OF MINES AND MINERAL RESOURCES Previous investigations and acknowledgments ............... 4 Well-numbering system ................................. 5 Alvin J. Thompson, Direclor GEOGRAPHY ............... 7 Topography and drainage ................................ 7 Mescalero Ridge and High Plains ....................... 7 THE REGENTS Querecho Plains and Laguna Valley ..................... 9 Grama Ridge area ..................................... 11 MEEMBERS Ex OFFICIO Eunice Plain ......................................... 12 Monument Draw ................................... 12 TheHonorable Edwin L. Mechern ...... Governor of New Mexico Rattlesnake Ridge area ................................ 13 Tom Wiley ............. Superintendent of Public Instruction San Simon Swale ...................................... 13 Antelope Ridge area ................................. -
Geology of Apache Mountains, Trans-Pecos Texas
GEOLOGY OF APACHE MOUNTAINS, TRANS-PECOS TEXAS John William Wood University of Texas, Ph.D. thesis, 241 p., 10 sections, 6 diagrams, 40 photos, June, 1965. ABSTRACT The Apache Mountains of southeastern Culberson County, Texas, are com- posed of Permian marine rocks deposited over truncated Paleozoic formations along part of the southwest margin of the Delaware Basin. The western sector of the range, a broadly developed half-dome, is dominated by modified horst-and-graben structure superposed on shelf, shelf-margin, and basin facies ranging in age from Leonardian to Ochoan. The eastern two-thirds of the range is an exhumed Guadalupian reef complex, the surface structure of which is the elongate, southeast-plunging Apache anticline. The oldest exposed rocks are Leonardian in age and compose the upper part of the Victorio Peak Limestone. The VictorioPeakcrops out in an isolated ridge at the western end of the range. The siltstone, dolomite, and limestone within the unit probably formed as shallow-watershelf-margin deposits. In the same ridge, the Victorio Peak is conformably overlain by shale, silt stone, and lime- stone of the Cutoff Shale. The age of at least the upper part of the Cutoff is Guadalupian. As a result of uplift, erosion, and subsequent subsidence a tongue of Cherry Canyon basin- facies oversteps trucated Cutoff beds. The Munn Formationcrops out along the western base of the range and makes up the southwestern ridges. The two members of the Munn are composed of dolomite, siltstone, and limestone deposited as shelf and shelf-margin facies. The "backbone" of the Apache Mountains is a southeast trending, massive carbonate lithosome, the Capitan Limestone, which is flanked on the northeast by a fault-line scarp and on the southwest by ridges composed of bedded back- reef dolomite and siltstone of the Seven Rivers, Yates, and Tansill formations. -
Geologic Map of the Carlsbad Caverns 7.5-Minute Quadrangle
NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES A RESEARCH DIVISION OF NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY NMBGMR Open-File Geologic Map 285 Last Modified June 2020 Correlation of Map Units Description of Map Units 104°30'0"W 104°27'30"W 104°25'0"W 104°22'30"W 490000 548000 549000 550000 500000 551000 552000 553000 510000 554000 A 555000 556000 520000 557000 558000 QUATERNARY PERMIAN Capitan Formation 32°15'0"N Py Qy 32°15'0"N Qy Py Qyc Capitan Formation—From a distance this unit exhibits a weekly Qy Py Qy Holocene Ochoan Pcp Pt Py Qyc Qy Py Holo. developed inclined layering that dips southeastward between ~15° and 000 Holocene Sedimentary Deposits Castile Formation Alluvial Alluvial Deposits 3568 Pt Qy Deposits Holocene 4 Holocene Psr Qyc Qyc 000 3568000 30°. This layering is more pronounced closer to the Delaware basin. In Qy Qy Pt Qy 0 Active channel deposits—Predominantly unconsolidated sand and Castile Formation—Composed of alternating regular laminae and thin Py 0 Qyc Pc Qy Pt 0 Qs outcrop, most exposures appear massive and structureless. A faint Qy 4 0 gravel dominated by clasts of carbonate surrounded by a silty to sandy beds of dark-colored and light- colored anhydrite. Layering is mostly 0 e Pt e Qy Psr 8 Qy 02 3 brecciated texture is visible locally where angular clasts of dolomite of n n carbonaceous matrix. Mostly devoid of vegetation though some low contorted and is rarely consistent for more than a few meters. Both 04 03 01 Qyc e 05 04 03 e Qss e e Pt c Py c terraces typically less than 1 m above the active channel contain weak stream-cut exposures and upper surface exposures show abundant all sizes are strongly cemented by different generations of carbonate.