Ground-Water Geochemistry of the Albuquerque-Belen Basin, Central New Mexico
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New Mexico New Mexico
NEW MEXICO NEWand MEXICO the PIMERIA ALTA THE COLONIAL PERIOD IN THE AMERICAN SOUTHWEst edited by John G. Douglass and William M. Graves NEW MEXICO AND THE PIMERÍA ALTA NEWand MEXICO thePI MERÍA ALTA THE COLONIAL PERIOD IN THE AMERICAN SOUTHWEst edited by John G. Douglass and William M. Graves UNIVERSITY PRESS OF COLORADO Boulder © 2017 by University Press of Colorado Published by University Press of Colorado 5589 Arapahoe Avenue, Suite 206C Boulder, Colorado 80303 All rights reserved Printed in the United States of America The University Press of Colorado is a proud member of Association of American University Presses. The University Press of Colorado is a cooperative publishing enterprise supported, in part, by Adams State University, Colorado State University, Fort Lewis College, Metropolitan State University of Denver, Regis University, University of Colorado, University of Northern Colorado, Utah State University, and Western State Colorado University. ∞ This paper meets the requirements of the ANSI/NISO Z39.48-1992 (Permanence of Paper). ISBN: 978-1-60732-573-4 (cloth) ISBN: 978-1-60732-574-1 (ebook) Library of Congress Cataloging-in-Publication Data Names: Douglass, John G., 1968– editor. | Graves, William M., editor. Title: New Mexico and the Pimería Alta : the colonial period in the American Southwest / edited by John G. Douglass and William M. Graves. Description: Boulder : University Press of Colorado, [2017] | Includes bibliographical references and index. Identifiers: LCCN 2016044391| ISBN 9781607325734 (cloth) | ISBN 9781607325741 (ebook) Subjects: LCSH: Spaniards—Pimería Alta (Mexico and Ariz.)—History. | Spaniards—Southwest, New—History. | Indians of North America—First contact with Europeans—Pimería Alta (Mexico and Ariz.)—History. -
Geothermal Hydrology of Valles Caldera and the Southwestern Jemez Mountains, New Mexico
GEOTHERMAL HYDROLOGY OF VALLES CALDERA AND THE SOUTHWESTERN JEMEZ MOUNTAINS, NEW MEXICO U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 00-4067 Prepared in cooperation with the OFFICE OF THE STATE ENGINEER GEOTHERMAL HYDROLOGY OF VALLES CALDERA AND THE SOUTHWESTERN JEMEZ MOUNTAINS, NEW MEXICO By Frank W. Trainer, Robert J. Rogers, and Michael L. Sorey U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 00-4067 Prepared in cooperation with the OFFICE OF THE STATE ENGINEER Albuquerque, New Mexico 2000 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey. For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Information Services Water Resources Division Box 25286 5338 Montgomery NE, Suite 400 Denver, CO 80225-0286 Albuquerque, NM 87109-1311 Information regarding research and data-collection programs of the U.S. Geological Survey is available on the Internet via the World Wide Web. You may connect to the Home Page for the New Mexico District Office using the URL: http://nm.water.usgs.gov CONTENTS Page Abstract............................................................. 1 Introduction ........................................ 2 Purpose and scope........................................................................................................................ -
Chapter 4: the Hydrologic System of the Middle Rio Grande Basin
Chapter 4: The hydrologic system of the Middle Rio Grande Basin In discussions of the water resources of an area, the hydrologic system is commonly split into two components for convenience: surface water and ground water. However, in the Middle Rio Grande Basin, as in most other locales, the surface- and ground-water systems are intimately linked through a series of complex interactions. These interactions often make it difficult to recognize the boundary between the two systems. In The Rio Grande is the only river I ever this report, the surface- and ground-water systems are described separately, saw that needed irrigation. –attributed to though one of the goals of the report is to show that they are both parts of Will Rogers the hydrologic system of the Middle Rio Grande Basin and that changes in one often affect the other. As defined earlier, in this report “Middle Rio Grande Basin” refers to the geologic basin defined by the extent of deposits of Cenozoic age along the Rio Grande from about Cochiti Dam to about San Acacia. This definition includes nearly the entire ground-water basin; however, the extent of the surface-water basin is delimited topographically by drainage divides and is consequently somewhat larger than the ground-water basin. Surface-water system The most prominent hydrologic feature in the Middle Rio Grande Basin is the Rio Grande, which flows through the entire length of the basin, generally from north to south. The fifth longest river in the United States, its headwaters are in the mountains of southern Colorado. The Rio Grande is the largest river in New Mexico, with a drainage area of 14,900 square miles where it enters the Middle Rio Grande Basin. -
Cenozoic Thermal, Mechanical and Tectonic Evolution of the Rio Grande Rift
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 91, NO. B6, PAGES 6263-6276, MAY 10, 1986 Cenozoic Thermal, Mechanical and Tectonic Evolution of the Rio Grande Rift PAUL MORGAN1 Departmentof Geosciences,Purdue University,West Lafayette, Indiana WILLIAM R. SEAGER Departmentof Earth Sciences,New Mexico State University,Las Cruces MATTHEW P. GOLOMBEK Jet PropulsionLaboratory, CaliforniaInstitute of Technology,Pasadena Careful documentationof the Cenozoicgeologic history of the Rio Grande rift in New Mexico reveals a complexsequence of events.At least two phasesof extensionhave been identified.An early phase of extensionbegan in the mid-Oligocene(about 30 Ma) and may have continuedto the early Miocene (about 18 Ma). This phaseof extensionwas characterizedby local high-strainextension events (locally, 50-100%,regionally, 30-50%), low-anglefaulting, and the developmentof broad, relativelyshallow basins, all indicatingan approximatelyNE-SW •-25ø extensiondirection, consistent with the regionalstress field at that time.Extension events were not synchronousduring early phase extension and were often temporally and spatiallyassociated with major magmatism.A late phaseof extensionoccurred primarily in the late Miocene(10-5 Ma) with minor extensioncontinuing to the present.It was characterizedby apparently synchronous,high-angle faulting givinglarge verticalstrains with relativelyminor lateral strain (5-20%) whichproduced the moderuRio Granderift morphology.Extension direction was approximatelyE-W, consistentwith the contemporaryregional stress field. Late phasegraben or half-grabenbasins cut and often obscureearly phasebroad basins.Early phase extensionalstyle and basin formation indicate a ductilelithosphere, and this extensionoccurred during the climax of Paleogenemagmatic activity in this zone.Late phaseextensional style indicates a more brittle lithosphere,and this extensionfollowed a middle Miocenelull in volcanism.Regional uplift of about1 km appearsto haveaccompanied late phase extension, andrelatively minor volcanism has continued to thepresent. -
Gravity and Aeromagnetic Studies of the Santo Domingo Basin Area, New Mexico
Gravity and Aeromagnetic Studies of the Santo Domingo Basin Area, New Mexico By V.J.S. Grauch, David A. Sawyer, Scott A. Minor, Mark R. Hudson, and Ren A. Thompson Chapter D of The Cerrillos Uplift, the La Bajada Constriction, and Hydrogeologic Framework of the Santo Domingo Basin, Rio Grande Rift, New Mexico Edited by Scott A. Minor Professional Paper 1720–D U.S. Department of the Interior U.S. Geological Survey Contents Abstract .........................................................................................................................................................63 Introduction...................................................................................................................................................63 Gravity Data and Methods..........................................................................................................................64 Data Compilation .................................................................................................................................64 Estimating Thickness of Basin Fill ...................................................................................................64 Locating Faults From Gravity Data ...................................................................................................66 Aeromagnetic Data and Methods .............................................................................................................69 Data Compilation .................................................................................................................................69 -
Guidebook Contains Preliminary Findings of a Number of Concurrent Projects Being Worked on by the Trip Leaders
TH FRIENDS OF THE PLEISTOCENE, ROCKY MOUNTAIN-CELL, 45 FIELD CONFERENCE PLIO-PLEISTOCENE STRATIGRAPHY AND GEOMORPHOLOGY OF THE CENTRAL PART OF THE ALBUQUERQUE BASIN OCTOBER 12-14, 2001 SEAN D. CONNELL New Mexico Bureau of Geology and Mineral Resources-Albuquerque Office, New Mexico Institute of Mining and Technology, 2808 Central Ave. SE, Albuquerque, New Mexico 87106 DAVID W. LOVE New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801 JOHN D. SORRELL Tribal Hydrologist, Pueblo of Isleta, P.O. Box 1270, Isleta, NM 87022 J. BRUCE J. HARRISON Dept. of Earth and Environmental Sciences, New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 Open-File Report 454C and D Initial Release: October 11, 2001 New Mexico Bureau of Geology and Mineral Resources New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 NMBGMR OFR454 C & D INTRODUCTION This field-guide accompanies the 45th annual Rocky Mountain Cell of the Friends of the Pleistocene (FOP), held at Isleta Lakes, New Mexico. The Friends of the Pleistocene is an informal gathering of Quaternary geologists, geomorphologists, and pedologists who meet annually in the field. The field guide has been separated into two parts. Part C (open-file report 454C) contains the three-days of road logs and stop descriptions. Part D (open-file report 454D) contains a collection of mini-papers relevant to field-trip stops. This field guide is a companion to open-file report 454A and 454B, which accompanied a field trip for the annual meeting of the Rocky Mountain/South Central Section of the Geological Society of America, held in Albuquerque in late April. -
University of Florida Thesis Or Dissertation Formatting
UNDERSTANDING CARNIVORAN ECOMORPHOLOGY THROUGH DEEP TIME, WITH A CASE STUDY DURING THE CAT-GAP OF FLORIDA By SHARON ELIZABETH HOLTE A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2018 © 2018 Sharon Elizabeth Holte To Dr. Larry, thank you ACKNOWLEDGMENTS I would like to thank my family for encouraging me to pursue my interests. They have always believed in me and never doubted that I would reach my goals. I am eternally grateful to my mentors, Dr. Jim Mead and the late Dr. Larry Agenbroad, who have shaped me as a paleontologist and have provided me to the strength and knowledge to continue to grow as a scientist. I would like to thank my colleagues from the Florida Museum of Natural History who provided insight and open discussion on my research. In particular, I would like to thank Dr. Aldo Rincon for his help in researching procyonids. I am so grateful to Dr. Anne-Claire Fabre; without her understanding of R and knowledge of 3D morphometrics this project would have been an immense struggle. I would also to thank Rachel Short for the late-night work sessions and discussions. I am extremely grateful to my advisor Dr. David Steadman for his comments, feedback, and guidance through my time here at the University of Florida. I also thank my committee, Dr. Bruce MacFadden, Dr. Jon Bloch, Dr. Elizabeth Screaton, for their feedback and encouragement. I am grateful to the geosciences department at East Tennessee State University, the American Museum of Natural History, and the Museum of Comparative Zoology at Harvard for the loans of specimens. -
Preliminary Geologic Map of the Albuquerque 30' X 60' Quadrangle
Preliminary Geologic Map of the Albuquerque 30’ x 60’ Quadrangle, north-central New Mexico By Paul L. Williams and James C. Cole Open-File Report 2005–1418 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2006 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: Williams, Paul L., and Cole, James C., 2006, Preliminary Geologic Map of the Albuquerque 30’ x 60’ quadrangle, north-central New Mexico: U.S. Geological Survey Open-File Report 2005-1418, 64 p., 1 sheet scale 1:100,000. 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 material contained within this report. ii Contents Abstract.................................................................................................................1 Introduction ...........................................................................................................2 Geography and geomorphology.........................................................................3 -
July 13, 2015 Cons: # 02ENNM00
New Mexico Ecological Services Field Office 2105 Osuna NE Albuquerque, New Mexico 87113 Phone: (505) 346-2525 Fax: (505) 346-2542 July 13, 2015 Cons: # 02ENNM00-2014-F-0266 Maria T. Garcia, Forest Supervisor Santa Fe National Forest 11 Forest Lane Santa Fe, New Mexico 87508 Dear Ms. Garcia: Thank you for your request for formal consultation and conferencing with the U.S. Fish and Wildlife Service (USFWS) pursuant to section 7 of the Endangered Species Act of 1973 (16 U.S.C. § 1531 et seq.), as amended (Act). We began early coordination with you and received a Biological Assessment (BA) (dated June 6, 2014) and supplemental information, which evaluate the impacts of the Southwest Jemez Mountains Restoration Project Santa Fe National Forest Jemez Ranger District Sandoval County, New Mexico (Restoration Project). At issue are potential impacts from the proposed action on the Mexican spotted owl (Strix occidentalis lucida) (MSO) and its critical habitat, the Jemez Mountains salamander (Plethodon neomexicanus) (salamander) and its critical habitat, the New Mexico meadow jumping mouse (Zapus hudsonius luteus) and its proposed critical habitat, and the Rio Grande Cutthroat trout (Oncorhynchus clarki virginalis) (cutthroat trout). You determined that the proposed action “may affect, is likely to adversely affect” the MSO and its designated critical habitat, the salamander and its designated critical habitat, the jumping mouse and its proposed critical habitat. This biological opinion does not rely on the regulatory definition of “destruction or adverse modification” of critical habitat at 50 CFR 402.02. Instead, we have relied upon the statute and the August 6, 2004, Ninth Circuit Court of Appeals decision in Gifford Pinchot Task Force v. -
Frijoles Canyon, the Preservation of a Resource
University of Pennsylvania ScholarlyCommons Theses (Historic Preservation) Graduate Program in Historic Preservation 2002 Frijoles Canyon, the Preservation of a Resource Lauren Meyer University of Pennsylvania Follow this and additional works at: https://repository.upenn.edu/hp_theses Part of the Historic Preservation and Conservation Commons Meyer, Lauren, "Frijoles Canyon, the Preservation of a Resource" (2002). Theses (Historic Preservation). 508. https://repository.upenn.edu/hp_theses/508 Copyright note: Penn School of Design permits distribution and display of this student work by University of Pennsylvania Libraries. Suggested Citation: Meyer, Lauren (2002). Frijoles Canyon, the Preservation of a Resource. (Masters Thesis). University of Pennsylvania, Philadelphia, PA. This paper is posted at ScholarlyCommons. https://repository.upenn.edu/hp_theses/508 For more information, please contact [email protected]. Frijoles Canyon, the Preservation of a Resource Disciplines Historic Preservation and Conservation Comments Copyright note: Penn School of Design permits distribution and display of this student work by University of Pennsylvania Libraries. Suggested Citation: Meyer, Lauren (2002). Frijoles Canyon, the Preservation of a Resource. (Masters Thesis). University of Pennsylvania, Philadelphia, PA. This thesis or dissertation is available at ScholarlyCommons: https://repository.upenn.edu/hp_theses/508 uNivERsmy PENNSYLV^NL^ UBKARIE5 Frijoles Canyon, The Preservation of A Resource Lauren Meyer A THESIS In Historic Preservation -
Geology, Groundwater, and Geologic Hazards in the Albuquerque Basin, New Mexico
GEOLOGY, GROUNDWATER, AND GEOLOGIC HAZARDS IN THE ALBUQUERQUE BASIN, NEW MEXICO Sean D. Connell New Mexico Bureau of Geology and Mineral Resources-Albuquerque Office Problem: Geologic mapping and subsurface studies provide fundamental data for evaluating water resources and natural hazards. The enhancement of understanding of groundwater resources, in particular, is of great concern and value to rapidly growing communities of the semi-arid southwestern United States and northern Mexico. The largest urban center in New Mexico, the Albuquerque-Rio Rancho metropolitan area, lies within the Albuquerque Basin of the Rio Grande rift. Rocks exposed along the margins provide clues to the character of the regional aquifer system. The Santa Fe Group comprises the principal regional aquifer for nearly all communities within the basin. A shallower alluvial aquifer, associated with cutting of the Rio Grande Valley during Quaternary time, is inset against the Santa Fe Group. This shallow aquifer is thin, restricted to the valley floor, and contains water associated with the modern river. It is also highly susceptible to groundwater contamination. The Geologic Map: Fault mapping is critical to effectively managing water resources and evaluating geologic hazards. Faults strongly influence sedimentation and groundwater-flow patterns, they tend to locally compartmentalize aquifers, and are partly responsible for aquifer discharge and recharge zones. Numerous faults have moved repeatedly during Pleistocene time and may pose future earthquake threats. Understanding the connections between sediments and groundwater resources depends on geologic mapping. Diverse depositional environments record different phases of basin development. Dune fields and small streams that drained into playa lakes and mud flats dominated the early phase (lower Santa Fe Group) of deposition. -
Birth and Evolution of the Rio Grande Fluvial
University of New Mexico UNM Digital Repository Earth and Planetary Sciences ETDs Electronic Theses and Dissertations Fall 9-21-2016 Birth and evolution of the Rio Grande fluvial system in the last 8 Ma:Progressive downward integration and interplay between tectonics, volcanism, climate, and river evolution Marisa N. Repasch Follow this and additional works at: https://digitalrepository.unm.edu/eps_etds Part of the Geology Commons, Geomorphology Commons, Hydrology Commons, Other Earth Sciences Commons, Sedimentology Commons, Tectonics and Structure Commons, and the Volcanology Commons Recommended Citation Repasch, Marisa N.. "Birth and evolution of the Rio Grande fluvial system in the last 8 Ma:Progressive downward integration and interplay between tectonics, volcanism, climate, and river evolution." (2016). https://digitalrepository.unm.edu/eps_etds/139 This Thesis is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in Earth and Planetary Sciences ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. Marisa Repasch Candidate Earth and Planetary Sciences Department This thesis is approved, and it is acceptable in quality and form for publication: Approved by the Thesis Committee: Karl Karlstrom Laura Crossey Matt Heizler i BIRTH AND EVOLUTION OF THE RIO GRANDE FLUVIAL SYSTEM IN THE LAST 8 MA: PROGRESSIVE DOWNWARD INTEGRATION AND INTERPLAY BETWEEN TECTONICS, VOLCANISM, CLIMATE, AND RIVER EVOLUTION BY MARISA REPASCH B.S. EARTH AND ENVIRONMENTAL SCIENCES LEHIGH UNIVERSITY 2014 M.S. THESIS Submitted in partial fulfillment of the Requirements for the Degree of Master of Science Earth and Planetary Sciences The University of New Mexico Albuquerque, New Mexico December, 2016 ii ACKNOWLEDGEMENTS First and foremost, I acknowledge my advisor, Karl Karlstrom, for all of the guidance, time, and energy he invested in my research, professional development, and personal well-being.