112 Appendix B Hydrogeologic and Soils Factors
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Mosaic of New Mexico's Scenery, Rocks, and History
Mosaic of New Mexico's Scenery, Rocks, and History SCENIC TRIPS TO THE GEOLOGIC PAST NO. 8 Scenic Trips to the Geologic Past Series: No. 1—SANTA FE, NEW MEXICO No. 2—TAOS—RED RIVER—EAGLE NEST, NEW MEXICO, CIRCLE DRIVE No. 3—ROSWELL—CAPITAN—RUIDOSO AND BOTTOMLESS LAKES STATE PARK, NEW MEXICO No. 4—SOUTHERN ZUNI MOUNTAINS, NEW MEXICO No. 5—SILVER CITY—SANTA RITA—HURLEY, NEW MEXICO No. 6—TRAIL GUIDE TO THE UPPER PECOS, NEW MEXICO No. 7—HIGH PLAINS NORTHEASTERN NEW MEXICO, RATON- CAPULIN MOUNTAIN—CLAYTON No. 8—MOSlAC OF NEW MEXICO'S SCENERY, ROCKS, AND HISTORY No. 9—ALBUQUERQUE—ITS MOUNTAINS, VALLEYS, WATER, AND VOLCANOES No. 10—SOUTHWESTERN NEW MEXICO No. 11—CUMBRE,S AND TOLTEC SCENIC RAILROAD C O V E R : REDONDO PEAK, FROM JEMEZ CANYON (Forest Service, U.S.D.A., by John Whiteside) Mosaic of New Mexico's Scenery, Rocks, and History (Forest Service, U.S.D.A., by Robert W . Talbott) WHITEWATER CANYON NEAR GLENWOOD SCENIC TRIPS TO THE GEOLOGIC PAST NO. 8 Mosaic of New Mexico's Scenery, Rocks, a n d History edited by PAIGE W. CHRISTIANSEN and FRANK E. KOTTLOWSKI NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES 1972 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY STIRLING A. COLGATE, President NEW MEXICO BUREAU OF MINES & MINERAL RESOURCES FRANK E. KOTTLOWSKI, Director BOARD OF REGENTS Ex Officio Bruce King, Governor of New Mexico Leonard DeLayo, Superintendent of Public Instruction Appointed William G. Abbott, President, 1961-1979, Hobbs George A. Cowan, 1972-1975, Los Alamos Dave Rice, 1972-1977, Carlsbad Steve Torres, 1967-1979, Socorro James R. -
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. -
U.S. Geoligical Survey Scientific Investigations Report 2012–5238
Prepared in cooperation with San Miguel County, New Mexico Characterization of the Hydrologic Resources of San Miguel County, New Mexico, and Identification of Hydrologic Data Gaps, 2011 Scientific Investigations Report 2012–5238 U.S. Department of the Interior U.S. Geological Survey Cover: Canadian escarpment rising above the plains, northeastern San Miguel County (photograph by David Lutz). Characterization of the Hydrologic Resources of San Miguel County, New Mexico, and Identification of Hydrologic Data Gaps, 2011 By Anne Marie Matherne and Anne M. Stewart Prepared in cooperation with San Miguel County, New Mexico Scientific Investigations Report 2012–5238 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 This and other USGS information products are available at http://store.usgs.gov/ U.S. Geological Survey Box 25286, Denver Federal Center Denver, CO 80225 To learn about the USGS and its information products visit http://www.usgs.gov/ 1-888-ASK-USGS Any use of trade, product, or firm 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 materials contained within this report. Suggested citation: Matherne, A.M., and Stewart, A.M., 2012, Characterization of the hydrologic resources of San Miguel County, New Mexico, and identification of hydrologic data gaps, 2011: U.S. Geological Survey Scientific Investigations Report 2012–5238, 44 p. -
This File Copyright © the Geological Association of Canada
This File Copyright © The Geological Association of Canada PLEASE RESPECT COPYRIGHT Considerable investment goes into the production of any publication. Recovering that investment helps ensure the publishing program can continue to provide books at reasonable prices, and continue to create publishing opportunities to future authors. This digital file is provided to the Lead Author on condition: * that the digital file remains in the possession of the Author(s), and is not distributed, shared or forwarded in any manner (except for individual study) without prior written approval from GAC®; * that the file is not manipulated in any way; * that it is understood the digital file may not be an exact representation of the original hardcopy text. As such, GAC® will be held blameless for any discrepancy between digital and printed versions; and * that printouts are distributed free of charge to colleagues and students for individual study, and do not appear in coursebooks or other compilation works (digital, printed or otherwise) for which direct or indirect payment is expected without prior arrangement with Access Copyright, the Canadian Copyright agency: Access Copyright The Canadian Copyright Licensing Agency 1 Yonge Street, Suite 800 Toronto, Ontario M5E 1E5 www.accesscopyright.ca Phone: 416-868-1620 Fax: 416-868-1621 Toll-Free: 1-800-893-5777 Email: [email protected] In the paper by Oboh-Ikuenobe et al., Table 1 (p. 206) is missing part B, as follows: Anatomy of epicontinental flooding: Late Albian-Early Cenomanian of the southern -
Magnetostratigraphy of the Upper Triassic Chinle Group of New Mexico: Implications for Regional and Global Correlations Among Upper Triassic Sequences
Magnetostratigraphy of the Upper Triassic Chinle Group of New Mexico: Implications for regional and global correlations among Upper Triassic sequences Kate E. Zeigler1,* and John W. Geissman2,* 1Department of Earth and Planetary Sciences, MSC 03-2040 Northrop Hall, University of New Mexico, Albuquerque, New Mexico 87131, USA 2Department of Earth and Planetary Sciences, MSC 03-2040 Northrop Hall, University of New Mexico, Albuquerque, New Mexico 87131, USA, and Department of Geosciences, ROC 21, University of Texas at Dallas, 800 West Campbell Road, Richardson, Texas 75080-3021, USA ABSTRACT polarity chronologies from upper Chinle graphic correlations (e.g., Reeve, 1975; Reeve and strata in New Mexico and Utah suggest that Helsley, 1972; Bazard and Butler, 1989, 1991; A magnetic polarity zonation for the strata considered to be part of the Rock Point Molina-Garza et al., 1991, 1993, 1996, 1998a, Upper Triassic Chinle Group in the Chama Formation in north-central New Mexico are 1998b, 2003; Steiner and Lucas, 2000). Conse- Basin, north-central New Mexico (United not time equivalent to type Rock Point strata quently, the polarity record of the mudstones and States), supplemented by polarity data from in Utah or to the Redonda Formation of east- claystones, which are the principal rock types in eastern and west-central New Mexico (Mesa ern New Mexico. the Chinle Group, is largely unknown. Redonda and Zuni Mountains, respectively), In our study of Triassic strata in the Chama provides the most complete and continuous INTRODUCTION Basin of north-central New Mexico, we sam- magnetic polarity chronology for the Late pled all components of the Chinle Group, with Triassic of the American Southwest yet avail- The Upper Triassic Chinle Group, prominent a focus on mudstones and claystones at Coyote able. -
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........................................................................ -
Western Portion of the Panhandle of Texas
f B, Descriptive Geology, 114 "Water-Supply and Irrigation Paper No. 191 \ 0, Underground Waters, 68 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR THE GEOLOGY AND WATER RESOURCES WESTERN PORTION OF THE PANHANDLE OF TEXAS CHARLES 1ST. WASHINGTON GOVERNMENT PRINTING OFFICE 1907 CONTENTS. Page. Introduction................................................................ 7 Area covered........................................................... 7 Sources of data. ......................................................... 7 Topography.................................................................. 7 General features....................................................... 7 High Plains.......................................................... 8 Valleys and canyons................................................... 9 Canadian River valley............................................. 9 Palo Duro Canyon.'................................................ 10 Minor stream valleys.............................................. 11 Beaver Creek valley............................................ 11 Coldwater Creek valley......................................... 11 Palo Duro Creek valley.......................................... 12 Carriso and Perico Creek valleys................................. 12 Big Blue Creek valley.......................................... 12 Tierra Blanca Creek valley...................................... 12 Geology.................................................................. 12 General -
GPS=Latitude-Longitude Coordinates from Global Positioning System)
APPENDIX: SAMPLE LOCALITIES (DATA ARCHIVE #1) (GPS=latitude-longitude coordinates from Global Positioning System) Santa Rosa (SR): Santa Rosa Sandstone of Dockum Group from Canadian River valley TX (Riggs et al., 1996). Tabular crossbedded to horizontally laminated fluvial sandstone of braided channel system including pebbly horizons resting unconformably on Permian Quartermaster Formation. TRU: Trujillo Formation of Dockum Group from headwaters of Red River TX. Green micaceous fluvial sandstone ~2 m from base of Trujillo Formation (resting on Tecovas Formation) in cliff beside TX Highway 256 ~10 mi east of Silverton TX and 1.2 mi downhill from rest area at eastern edge of caliche caprock on Llano Estacado at lip of its eastern escarpment. GPS (30 m distant from cliff face and 3 m from white line marking south edge of roadway): 34˚ 28.182’ N, 101˚ 05.788’ W. COO: Cooper Canyon Formation of Dockum Group from headwaters of Brazos River TX (from type area in Garza County SW of Post TX) provided by Thomas M. Lehman (Lehman et al., 1992). Currie (CUR): Shinarump Member (or Formation) of Chinle Formation (Stewart, 1980, p. 64) or Group (Lucas and Orchard, 2007) near Currie NV. Craggy knob (off road to Mizpah) of horizontally laminated fluvial sandstone of a locally pebbly channel complex (Gehrels and Dickinson, 1995). GPS (base of outcrop): 40˚ 22.0’ N, 114˚ 47.1’ W. CP4: Gartra Member of Chinle Formation near Vernal UT. Pebbly fluvial sandstone of braided channel complex forming prominent cuesta and exposed in double-sided roadcut on US Highway 191 located 10.7 mi north of its intersection with US Highway 40 in downtown Vernal UT. -
Evaluation of Available Saline Water Resources in New Mexico for The
SERlrrp-232-3597 UC Category: 244 DE89009511 Evaluation pf Available Saline Water Resources in New Mexico for the Production of Microalgae R. Lansford J. Hernandez P. Enis D. Truby C. Mapel August 1990 Prepared under Task No. BF911 01 0 Solar Energy. Research Institute A Division 01 Midwest Research Institute 1617 Cole Boulevard Golden, Colorado 80401-3393 Prepared for the U.S. Department of Energy Contract No. DE-AC02-83CH10093 NOTICE 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 or responsibility for the accuracy. com pleteness, 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 con stitute or imply its endorsement, recommendation. or favoring by the United States government or any agency thereof. The views and opinions 01 authors expressed herein do not necessarily state or reflect those of the United States government or any agency thereof. Printed in the United States of America Available from: National Technical Information Service U.S. Department of Commerce 5285 Port Royal Road Springfield, VA 22161 Price: Microfiche AD1 Printed Copy AD5 Codes are used for pricing all publications. The code is determined by the number of pages in the publication. Information pertaining to the pricing codes can be found in the current issue of the following publications which are generally available in most libraries: Energy Research Abstracts (ERA); Govem ment Reports Announcements and Index (GRA and I); Scientific and Technical Abstract Reports (STAR); and publication NTIS-PR-36D available Irom NTIS at the above address. -
Measured Strati Graphic Sections of Uranium-Bearing Upper Triassic
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Measured strati graphic sections of uranium-bearing Upper Triassic rocks of the Dockum Basin, eastern New Mexico, west Texas, and the Oklahoma Panhandle with brief discussion of stratigraphic problems by Warren I. Finch 1 and James C. Wright* Open-File Report 83-701 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. *Deceased *U.S. Geological Survey, Box 25046, MS 916, Denver Federal Center, Denver, Colorado 80225 1983 CONTENTS Page Statement ............................................................ 1 Measured sections..................................................... 4 New Mexi co....................................................... 4 Guadalupe County............................................ 4 Santa Rosa railroad-cut section........................ 4 Sunshine Mesa-State Route 156 road-cut section......... 9 Quay County................................................. 11 Dripping Triangulation Station section................. 11 Henry Pittman Ranch section............................ 15 Rana Arroyo section.................................... 20 Revuelto Creek-U.S. Route 66 section................... 23 Texas............................................................ 26 Armstrong County............................................ 26 State Route 284 - Pleasant Creek section............... 26 Borden County............................................... 31 Muchakooago Peak -
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.