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112 Appendix B Hydrogeologic and Soils Factors
APPENDIX B HYDROGEOLOGIC AND SOILS FACTORS INFLUENCING LEAKAGE POTENTIAL FROM THE CONCHAS-HUDSON CANAL SYSTEM, ARCH HURLEY CONSERVANCY DISTRICT, QUAY AND SAN MIGUEL COUNTIES, NEW MEXICO by John W. Hawley, Senior Hydrogeologist New Mexico Water Resources Research Institute and John F. Kennedy, GIS Specialist/Hydrogeologist New Mexico Water Resources Research Institute October 2005 INTRODUCTION The following discussion of geology and soils in the Arch Hurley Conservancy District (District) study area introduces the major landscape features (landforms) and surficial geologic units of the Conchas-Hudson Canal system between Conchas Reservoir in San Miguel County and the eastern part of the Tucumcari (irrigation) Project in Quay County. Emphasis is on hydrogeologic and soils factors that influence leakage from not only the canal corridor but also the complex network of laterals, ditches and field- drainage features that characterize irrigated parts of the District. Of particular importance is the historic role played by Project operations (since 1946) in recharge of the shallow- alluvial and bedrock (Entrada Sandstone) aquifer systems of the Tucumcari Metropolitan area. The latter topic was first addressed in detail by Trauger and Bushman (1964) and is only briefly covered here. 112 The geologic setting of the entire study area is the subject of a recent comprehensive review paper that was written specifically for a general audience by Adrian Hunt (Director, New Mexico Museum of Natural History and Science; 1998). Hydrogeologic characteristics of major stratigraphic units exposed or shallowly buried along the canal corridor are summarized in Table B1, which also includes a list of supporting references. Distribution patterns and leakage potential of surficial-geologic units and soils are summarized in Tables B2-B5 in Attachment B1 to this Appendix. -
Sedimentology of Mesa Rica Sandstone in Tucumcari Basin, New Mexico
Circular 157 1977 Sedimentology of Mesa Rica Sandstone in Tucumcari Basin, New Mexico by J. E. Gage and G. B. Asquith New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY documenting New Mexico mineral resources since 1927 Circular 157 New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Sedimentology of Mesa Rica Sandstone in Tucumcari Basin, New Mexico by J. E. Gage and G. B. Asquith SOCORRO 1977 11 Published by Authority of State of New Mexico, NMSA 1953 Sec. 63-1-4 Printed by University of New Mexico Printing Plant, June 1977 Available from New Mexico Bureau of Mines & Mineral Resources, Socorro, NM 87801 Price $2.50 Contents iv 5 Abstract The Mesa Rica Sandstone (Lower Cretaceous) in the Tucumcari Basin of east-central New Mexico represents deposits from a lobate sand-rich delta complex. Log-probability curves of the grain-size distributions when compared to the work of Visher (1969) indicate environments ranging from distributary channels to marine wave deposits. The Mesa Rica delta prograded into the marine Tucumcari Basin from the north as shown by the south-trending to southwest-trending paleocurrent directions, and the decrease in mean grain size and thickness to the southeast, south, and southwest (lobate geometry). Also, a decrease in percent cross stratification to the southeast, south, and southwest (accompanied by an increase in percent bioturbation and burrowing) indicates a transition from predominantly fluvial to predominantly marine conditions. If the Mesa Rica Sandstone is correlative with the lower fluvial interval of the Dakota Sandstone north and northwest of the Tucumcari Basin as suggested by Scott (1970), then the Dakota Sandstone represents the fluvial facies of the Mesa Rica marine delta complex. -
REGIONAL STRATIGRAPHIC CROSS SECTIONS of CRETACEOUS ROCKS from EAST-CENTRAL ARIZONA to the OKLAHOMA PANHANDLE Endorsement by the U.S
U.S. DEPARTMENT OF THE INTERIOR MISCELLANEOUS FIELD STUDIES MAP MF-2382 Version 1.0 U.S. GEOLOGICAL SURVEY SHEET 2 OF 3 D' D" WEST 275 mi (442 km) along the line of section or 220 mi (353 km) end point to end point EAST San Juan Volcanic Field San Luis Valley Sangre De Cristo Raton Basin Mountains Pagosa Springs San Juan Sag COLORADO NEW MEXICO NEW MEXICO OKLAHOMA 27 29.4 mi (47.3 km) 28 10.3 mi (16.6 km) 29 63.5 mi (102 km) 30 24.5 mi (39.4 km) 31 22.5 mi (36.2 km) 32 27 mi (43.4 km) 33 26.2 mi (42.2 km) 34 Samedan Oil Corp. Meridian Oil Co. Waggoner-Baldridge Energy Jake L. Harmon Clark & Perkins Amoco Production Co. Continental Oil Co. Brooks Expl. Co. Brown Fed. No. 1-17 South Park Fed. No. 23-17 Shelly No. 1-10 Cisneros No. 1 Goemmer Land Co. No. 1 Horse Springs Canyon No. 1 No. 3 Towndrow No. 1 Sec. 17, T. 35 N., R. 1 E. Sec. 17, T. 39 N., R. 4 E. Sec. 10, T. 40 N., R. 5 E. Sec. 5, T. 27 S., R. 70 W. Sec. 11, T. 29 S., R. 67 W. Sec. 33, T. 32 S., R. 66 W. Sec. 18, T. 30 N., R. 22 E. Sec. 27, T. 31 N., R. 25 E. KB 8,564 ft KB 10,086 ft KB 8,178 ft KB 7,654 ft KB 6,839 ft KB 7,452 ft KB 7,974 ft KB 8,267 ft SP R GR R EXPLANATION Formation or member contact P resent- ? Contact that rises (uniformly or abruptly) SP R in stratigraphic position Queried where uncertain Tertiary Contact, position is uncertain day ? Unconformity Queried where uncertain erosio ? Time line Queried where uncertain Raton Formation SP Spontaneous-potential curve ? n surface GR Gamma-ray curve TERTIARY Area of fault or unconformity R Resistivity curve at base of Kirtland Shale 2 CRETACEOUS KB Kelly bushing 1 (proj) Projected position of macrofossil from nearest outcrop TERTIARY (see sheet 1 for age ranges of molluscan fossils) mation Borehole depths shown are in thousands of feet below altitude of Kelly CRETACEOUS bushing except for boreholes where igneous sills have been removed. -
Mineral and Energy Resources of the BLM Roswell Resource Area, East-Central New Mexico
U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Mineral and Energy Resources of the BLM Roswell Resource Area, East-central New Mexico by Susan Bartsch-Winkleri, editor Open-File Report 92-0261 1992 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1 Denver, Colorado iMail Stop 937 Federal Center P.O. Box 25046 Denver, Colorado 80225 MINERAL AND ENERGY RESOURCES OF THE BLM ROSWELL RESOURCE AREA, EAST-CENTRAL NEW MEXICO Summary.......................................................................................... 1 Introduction.................................................................................... 1 Location and geography of study area...................................... 1 Purpose and methodology........................................................ 3 Acknowledgements......................................................................... 4 Geology of east-central New Mexico, by Susan Bartsch-Winkler, with a section on Intrusive and extrusive alkaline rocks of the Lincoln County porphyry belt by Theodore J. Armbrustmacher 4 General..................................................................................... 4 Structure................................................................................. 5 Uplifts........................................................................ -
Quay County, New Mexico Barry S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/52 Nearshore fauna of the Tucumcari Formation (Lower Cretaceous, Albian), Quay County, New Mexico Barry S. Kues and Spencer G. Lucas, 2001, pp. 229-249 in: Geology of Llano Estacado, Lucas, Spencer G.;Ulmer-Scholle, Dana; [eds.], New Mexico Geological Society 52nd Annual Fall Field Conference Guidebook, 340 p. This is one of many related papers that were included in the 2001 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. -
Geologic Map of New Mexico, 1:500,000
GEOLOGIC MAP OF NEW MEXICO, 1:500,000 NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES Open File Report No. 408 Orin J. Anderson and Glen E. Jones 1994 1’ 36015I ’ SANTA FE I I I 19 I _”-- 32” ””””” L I” ,. \Iio i . IndexMap to principal s0urCe.s . of data for state geologic map Principal Sources of Data Number at left refers to numbered l"x2" quadrangles shown in above index map. 1. *Thaden,R. E., and Zech, R. S., unpublished geologic mapof the northwest quadrant of New Mexico, 1:500,000: U.S. Geological Survey, Denver, Colorado. 2. Crouse, D. L., Hultgren, M. C., andWoodward, L. A., 1992, Geologyof French Mesa quadrangle, Rio Arriba County, New Mexico: New Mexico Bureau of Mines and Mineral Resources, Geologic Map GM-67, 1:24,000. Manley, K., Scott, G. R., and Wobus, R. A., 1987, Geologic map of the Aztec lox 2" quadrangle, northwestern New Mexico and southern Colorado: U.S. Geological Survey, Map 1-1730, 1:250,000. Smith, R. L., Bailey, R. A., and Ross, C. S., 1970, Geologic map of the Jemez Mountains: U.S. Geological Survey, Map 1-571, 1:125,000. *Thaden, R. E., and Zech, R. S., unpublished geologic map of the northwest quadrant of New Mexico, 1:500,000: U.S. Geological Survey, Denver, Colorado. Woodward, L. A., Gibson, G. G., and McLelland, D., 1976, Geology of the Gallina quadrangle, Rio Arriba County, New Mexico: New Mexico Bureau of Mines and Mineral Resources, GM-39, 1:24,000. Woodward, L. A., McLelland, D., and Kaufman, W. -
Petrified Wood of Oklahoma: Lap- Lawrence, 455P
2 Petrified Wood In Oklahoma Neil H. Suneson, Geologist IV, Oklahoma Geological Survey Adjunct Professor, ConocoPhillips School of Geology and Geophysics, University of Oklahoma [email protected] / 405.325.7315 Introduction world’s most baffling puzzles, the bane of professional cryp- tologists and amateur sleuths who have spent 15 years trying In the fossil world, petrified wood may be second only to solve it” (www.guardian.co.uk/world/2005/jun/11/dan- to dinosaurs in its fascination to humans, and “wood turned brown.books, acc. 2/27/10). Kryptos is referred to twice to stone” probably has the longer history of the two. In fact, on the dust jacket of the U.S. version of Dan Brown’s novel a fossil cycad was placed in the tomb of the Marzabotto “The Da Vinci Code” (http://en.wikipedia.org/wiki/kryptos, necropolis over 4000 years ago by the ancient Etruscans. It acc. 2/27/10). was accompanied by other funerary objects and thus must have had some special significance. Furthermore, it appears that the trunk of a fossil cycad may have been used by Ne- olithic people as a sharpening stone (Wieland, 1916) and thus may have “the longest known history of any fossil” (from www.plantapalm.com/vce/intro/historicalperspec- tive.htm, acc. 2/27/10). Around 1000 A.D. the Persian as- tronomer, chemist, mathematician, physicist, scientist, theologian, and philosopher Avicenna suggested “that or- ganic materials might be ‘turned into stone by a certain min- eralizing, petrifying power … and this transmutation of the bodies of animals and plants is just as short a step as the transmutation of waters. -
U-Pb Detrital Geochronology and Provenance Comparisons from The
New Mexico Geological Society Downloaded from: https://nmgs.nmt.edu/publications/guidebooks/70 U-Pb Detrital Geochronology and Provenance Comparisons from the Nonmarine Strata of the Dakota Group, Lytle Sandstone, and Morrison Formation in Northeastern New Mexico Samatha R. Bartnik, Brian A. Hampton, and Greg H. Mack, 2019, pp. 55-65 in: Geology of the Raton-Clayton Area, Ramos, Frank; Zimmerer, Matthew J.; Zeigler, Kate; Ulmer-Scholle, Dana, New Mexico Geological Society 70th Annual Fall Field Conference Guidebook, 168 p. This is one of many related papers that were included in the 2019 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. -
ALREFAEI-DISSERTATION-2016.Pdf (11.59Mb)
IMPLICATIONS OF LITHOFACIES ASSOCIATION AND ARCHITECTURE FOR LOW AND HIGH-ACCOMMODATION SYSTEM TRACTS FROM THE SANDSTONE DOMINATED ZONE (THE BARREN SERIES) OF THE CRETACEOUS-PALEOCENE RATON FORMATION, TRINIDAD, COLORADO by YAQOUB Y Y S M ALSAYED ALREFAEI Presented to the Faculty of the Graduate School of The University of Texas at Arlington in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY THE UNIVERSITY OF TEXAS AT ARLINGTON DECEMBER 2016 Copyright © by Yaqoub Y Y S M Alsayed Alrefaei 2016 All Rights Reserved ACKNOWLEDGEMENTS I’m grateful to Dr. Merlynd Nestell, my dissertation committee chairman, and Dr. John Holbrook, my dissertation committee co-chairman, for their unlimited help, assistance, advice and patience. I would also like to thank my committee members, Dr. Andrew Hunt, Dr. John Wickham, and Dr. James Grover, for their participation and help in my thesis. Special thanks to Kuwait University for sponsoring my scholarship and giving me the opportunity to pursue my higher education in the United States of America. Also a special thanks for Larry O'Donnell for his help during the fieldwork and to all of my colleagues for their help and assistance. I would like to dedicate this dissertation to my beloved family especially my parents (Yousef Alrefaei, Mariam Ali) without whom I could not finished it and whose prayers and encouragement sustained me. Most of all, I wish to thank my dear wife Hanan and children Mariam, Yousef and Hashim for their patience, sacrifices, help and endless support. December 16, 2016 iii LIST OF ILLUSTRATIONS Figure Page 1. Models for channelized reservoir shows channel connectivity .................................................... -
Bibliography of New Mexico Invertebrate Paleontology Barry S
University of New Mexico UNM Digital Repository Earth and Planetary Sciences Faculty and Staff Scholarly Communication - Departments Publications 8-2-2005 Bibliography of New Mexico Invertebrate Paleontology Barry S. Kues Follow this and additional works at: https://digitalrepository.unm.edu/eps_fsp Recommended Citation Kues, Barry S.. "Bibliography of New Mexico Invertebrate Paleontology." (2005). https://digitalrepository.unm.edu/eps_fsp/4 This Book is brought to you for free and open access by the Scholarly Communication - Departments at UNM Digital Repository. It has been accepted for inclusion in Earth and Planetary Sciences Faculty and Staff ubP lications by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. BIBLIOGRAPHY OF NEW MEXICO INVERTEBRATE PALEONTOLOGY Barry S. Kues Department of Earth and Planetary Sciences, MSC03 2040, University of New Mexico, Albuquerque, NM 87131-0001; [email protected] Introduction New Mexico has a rich record of invertebrate fossils, which have been reported in publications since 1848. Several thousand species have been documented from the state, and they represent each of the geologic periods from Cambrian to Neogene. The literature on the invertebrate paleontology of New Mexico is vast. Reference to much of this literature through 1979 was brought together by Kues and Northrop (1981) in a bibliography that included vertebrate and plant as well as invertebrate fossil groups reported in the state. A separate bibliography on vertebrate paleontology was published by Kues and Lucas in 1993, and this has been recently updated by Lewis et al. Much work on New Mexico invertebrate paleontology has been published since 1979, especially by paleontologists associated with the New Mexico Museum of Natural History and Science (which opened in the mid-1980s), the University of New Mexico, and the U. -
Palfacurrents and Depositional Environmmt5 Master
Paleocurrents and Depositional Environments of the Dakota Group (Cretaceous), San Miguel County, New Mexico Item Type text; Thesis-Reproduction (electronic) Authors Bejnar, Craig Russel Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the Antevs Library, Department of Geosciences, and the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author or the department. Download date 10/10/2021 09:59:36 Link to Item http://hdl.handle.net/10150/244084 PALFACURRENTS AND DEPOSITIONAL ENVIRONMMT5 OF THE DAKOTA GROUP (CRETACEOUS), SAN MIGUEL COUNTY, NEW MEXICO by ,Crag Ru.s s el Bejnar A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1975 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of re- quirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests . for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his judg- ment the proposed use of the material is in the interests of scholar- ship. -
Mineral Resources of the Sabinoso Wilderness Study Area, San Miguel County, New Mexico
Mineral Resources of the Sabinoso Wilderness Study Area, San Miguel County, New Mexico U.S. GEOLOGICAL SURVEY BULLETIN 1733-A Chapter A Mineral Resources of the Sabinoso Wilderness Study Area, San Miguel County, New Mexico By ANNE M. LEIBOLD, RICHARD W. SALTUS, V.J.S. GRAUCH, and DAVID A. LINDSEY U.S. Geological Survey CARL L. ALMQUIST U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1733 MINERAL RESOURCES OF WILDERNESS STUDY AREAS- NORTHERN NEW MEXICO DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1987 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Mineral resources of the Sabinoso Wilderness Study Area, San Miguel County, New Mexico. (U.S. Geological Survey bulletin ; 1733)(Mineral resources of wilderness study areas northern New Mexico ; ch. A) Bibliography: p. 1. Mines and mineral resources New Mexico Sabinoso Wilderness. 2. Geology New Mexico Sabinoso Wilderness.. I. Leibold, Anne M. II. Series: Geological Survey bulletin ; 1733. III. Series: Mineral resources of wilderness study areas northern New Mexico ; ch. A. QE75.B9 no. 1733-A 557.3s 87-600221 [TN24.N6] [553'.09789'55] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S. Bureau of Mines to conduct mineral surveys on certain areas to determine the mineral values, if any, that may be present.