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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. -
Ground-Water Geochemistry of the Albuquerque-Belen Basin, Central New Mexico
GROUND-WA TER GEOCHEMISTRY OF THE ALBVQVERQVE-BELEN BASIN, CENTRAL NEW MEXICO By Scott K. Anderholm U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 86-4094 Albuquerque, New Mexico 1988 DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information Copies of this report can write to: be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Water Resources Division Books and Open-File Reports Pinetree Office Park Federal Center, Building 810 4501 Indian School Rd. NE, Suite 200 Box 25425 Albuquerque, New Mexico 87110 Denver, Colorado 80225 CONTENTS Page Abstract ............................................................. 1 Introduction ......................................................... 2 Acknowledgments ................................................. 4 Purpose and scope ............................................... 4 Location ........................................................ 4 Climate ......................................................... 6 Previous investigations ......................................... 6 Geology .................................................... 6 Hydrology .................................................. 6 Well-numbering system ........................................... 9 Geology .............................................................. 10 Precambrian rocks ............................................... 10 Paleozoic rocks ................................................. 10 Mesozoic -
Stratigraphic Nomenclature of ' Volcanic Rocks in the Jemez Mountains, New Mexico
-» Stratigraphic Nomenclature of ' Volcanic Rocks in the Jemez Mountains, New Mexico By R. A. BAILEY, R. L. SMITH, and C. S. ROSS CONTRIBUTIONS TO STRATIGRAPHY » GEOLOGICAL SURVEY BULLETIN 1274-P New Stratigraphic names and revisions in nomenclature of upper Tertiary and , Quaternary volcanic rocks in the Jemez Mountains UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director U.S. GOVERNMENT PRINTING OFFICE WASHINGTON : 1969 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 15 cents (paper cover) CONTENTS Page Abstract.._..._________-...______.._-.._._____.. PI Introduction. -_-________.._.____-_------___-_______------_-_---_-_ 1 General relations._____-___________--_--___-__--_-___-----___---__. 2 Keres Group..__________________--------_-___-_------------_------ 2 Canovas Canyon Rhyolite..__-__-_---_________---___-____-_--__ 5 Paliza Canyon Formation.___-_________-__-_-__-__-_-_______--- 6 Bearhead Rhyolite-___________________________________________ 8 Cochiti Formation.._______________________________________________ 8 Polvadera Group..______________-__-_------________--_-______---__ 10 Lobato Basalt______________________________________________ 10 Tschicoma Formation_______-__-_-____---_-__-______-______-- 11 El Rechuelos Rhyolite--_____---------_--------------_-_------- 11 Puye Formation_________________------___________-_--______-.__- 12 Tewa Group__._...._.______........___._.___.____......___...__ 12 Bandelier Tuff.______________.______________... 13 Tsankawi Pumice Bed._____________________________________ 14 Valles Rhyolite______.__-___---_____________.________..__ 15 Deer Canyon Member.______-_____-__.____--_--___-__-____ 15 Redondo Creek Member.__________________________________ 15 Valle Grande Member____-__-_--___-___--_-____-___-._-.__ 16 Battleship Rock Member...______________________________ 17 El Cajete Member____..._____________________ 17 Banco Bonito Member.___-_--_---_-_----_---_----._____--- 18 References . -
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. -
Fire History in the Taos Valley Watersheds, New Mexico, USA
fire Article Surface Fire to Crown Fire: Fire History in the Taos Valley Watersheds, New Mexico, USA Lane B. Johnson 1 and Ellis Q. Margolis 2,* 1 University of Minnesota, Cloquet Forestry Center, 175 University Drive, Cloquet, MN 55720, USA; [email protected] 2 U. S. Geological Survey, Fort Collins Science Center, New Mexico Landscapes Field Station, 301 Dinosaur Trail, Santa Fe, NM 87508, USA * Correspondence: [email protected]; Tel.: +1-505-954-2251 Received: 9 February 2019; Accepted: 8 March 2019; Published: 14 March 2019 Abstract: Tree-ring fire scars, tree ages, historical photographs, and historical surveys indicate that, for centuries, fire played different ecological roles across gradients of elevation, forest, and fire regimes in the Taos Valley Watersheds. Historical fire regimes collapsed across the three watersheds by 1899, leaving all sites without fire for at least 119 years. Historical photographs and quaking aspen (Populus tremuloides Michx.) ages indicate that a high-severity fire historically burned at multiple high-elevation subalpine plots in today’s Village of Taos Ski Valley, with large high-severity patches (>640 ha). Low-severity, frequent (9–29-year median interval) surface fires burned on the south aspects in nearby lower elevation dry conifer forests in all watersheds. Fires were associated with drought during the fire year. Widespread fires commonly burned synchronously in multiple watersheds during more severe drought years, preceded by wet years, including fire in all three watersheds in 1664, 1715, and 1842. In contrast, recent local “large” wildfires have only burned within single watersheds and may not be considered large in a historical context. -
Geology of the Northern Jemez Mountains, North-Central New Mexico Kirt A
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/58 Geology of the northern Jemez Mountains, north-central New Mexico Kirt A. Kempter, Shari A. Kelley, and John R. Lawrence, 2007, pp. 155-168 in: Geology of the Jemez Region II, Kues, Barry S., Kelley, Shari A., Lueth, Virgil W.; [eds.], New Mexico Geological Society 58th Annual Fall Field Conference Guidebook, 499 p. This is one of many related papers that were included in the 2007 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. -
New Mexico Forest and Watershed Restoration Institute Annual Report 2013-2014
New Mexico Forest and Watershed Restoration Institute Annual Report 2013-2014 The New Mexico Forest and Watershed Restoration Institute (FWRI) exists to promote practices that reduce the risk of catastrophic wildfire and enhance ecosystem function. We have pursued this through four program areas: the biology of restoration treatments, or which tree to cut and which to leave, with an emphasis on the need to burn treated areas; the mechanics of treatments, or how to operate safely and efficiently, a program area that was most active 2008-2010 but currently is dormant; support from geographic information systems (GIS) to field work by FWRI and our partners, which usually involves maps; and monitoring, or how to determine if treatments are effective, and is the subject which accounts for most of our partner’s requests for technical assistance. This report is organized into three broad areas: technical assistance and monitoring, restoration- based economic development, and watershed restoration partnerships. These areas are further subivided as needed. This report focuses on the period 1 October 2013 through 30 September 2014, with activities outside of that period mentioned as needed for context. This period was one of transition for FWRI. First, the previous Director, Andy Egan, left in May 2013 to become Dean of Science at a university in Canada, and the FWRI forester stepped in as Interim Director. Second, an employee resigned unexpectedly at the end of September 2013. We took this opportunity to restructure two positions as program directors for restoration monitoring and for collaboration. These positions were advertised in July 2014. In addition, our Administrative Associate missed six months due to a serious illness. -
Geologic Map of the Redondo Peak Quadrangle, Sandoval County,New
Preliminary Geologic Map of the Redondo Peak Quadrangle, Sandoval County, New Mexico By Fraser Goff, Jamie N. Gardner, Steven L. Reneau, and Cathy J. Goff January, 2006 New Mexico Bureau of Geology and Mineral Resources Open-file Digital Geologic Map OF-GM 111 Scale 1:24,000 This work was supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program (STATEMAP) under USGS Cooperative Agreement 06HQPA0003 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. GEOLOGIC MAP OF THE REDONDO PEAK 7.5-MINUTE QUADRANGLE, SANDOVAL COUNTY, NEW MEXICO 1:24,000 by Fraser Goff, Jamie N. Gardner, Steven L. Reneau, and Cathy J. Goff INTRODUCTION The Redondo Peak 7.5 minute quadrangle is in Sandoval County and straddles the southern rim of the Valles caldera in the Jemez Mountains, New Mexico (Fig. 1). Topographically, the quadrangle is bounded by Redondo Peak on the north, the Banco Bonito plateau and Cat Mesa on the west, Valle Grande on the northeast, and a series of north-trending canyons and ridges to the south and southeast (San Juan Canyon, Peralta Ridge, etc.). Geologically, the quadrangle consists of three domains: the resurgent dome of Valles caldera in the north; the southern moat of Valles caldera in the center; and a part of the Jemez Mountains volcanic field to the south. -
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 -
Rio Guadalupe Stream Inventory Report Santa Fe National Forest Surveyed: June – July 2004 Forest Fisheries Crew
Rio Guadalupe Stream Inventory Report Santa Fe National Forest Surveyed: June – July 2004 Forest Fisheries Crew Report By Tara Anderson, Fisheries Technician Dylan Hoffman, Fisheries Technician Chuck Dentino, Fisheries Biologist Reviewed By Sean Ferrell Forest Fisheries Biologist Santa Fe National Forest February 2006 Versions of this document were reviewed, edited and approved by the following individual: Bill Britton, Forest Biologist, USDA Forest Service, Santa Fe National Forest Table of Contents Section Page Number Map of the area 3 Introduction 4 Basin Summary 6 Executive Summary 7 Habitat Characteristics 9 Reach by Reach Comparison 12 Tributaries 13 Stream Flow 14 Water Quality 15 Riparian Vegetation 20 Beaver Activity 21 Fisheries 23 Wildlife 25 Stream Improvements 27 Land Use Cultural Resources 27 Timber Harvest 30 Mining 31 Roads 31 Fires 33 Grazing 34 Recreation 35 Recommendation Summary 37 Reach Summaries 40 Reach 1: Private Land: Not Surveyed 41 Reach 2: Above Private Land to the USGS Station Below the Guadalupe Box 42 Reach 3: USGS Station below the Guadalupe Box to Upper End of Guadalupe Box 48 Reach 4: Top of Guadalupe Box to the Bottom of the Upper Box Canyon 54 Reach 5: Bottom of the Upper Box Canyon to the Top of the Upper Box Canyon 64 Appendix A 69 Appendix B 70 Glossary 71 Literature Cited 73 Acknowledgements 76 Map 1. Rio Guadalupe from the headwaters to its confluence with Jemez River and its designated reaches (2004). 3 This document is a specialist report. It is meant to assist managers in understanding current conditions of a stream corridor and possibly how those conditions have developed over a period of time. -
Estimation of Natural Streamflow in the Jemez River at the Boundaries of Indian Lands, Central New Mexico
ESTIMATION OF NATURAL STREAMFLOW IN THE JEMEZ RIVER AT THE BOUNDARIES OF INDIAN LANDS, CENTRAL NEW MEXICO by Edward E. Fischer and John P. Borland U.S. GEOLOGICAL SURVEY WATER-RESOURCES INVESTIGATIONS REPORT 82-4113 Prepared in cooperation with the U.S. BUREAU OF INDIAN AFFAIRS Albuquerque, New Mexico 1983 Cover i__ Upper--The Jemez River downstream from San Ysidro, looking south- southwest. Flow is from right to left. Lower Jemez Canyon Dam. UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information Copies of this report can write to: be purchased from: Open-File Services Section ..District Chief Western Distribution Branch U.S. Geological Survey U.S. Geological Survey Water Resources Division Box 25425, Federal Center 505 Marquette NW, Room 720 Lakewood, Colorado 80225 Albuquerque, New Mexico 87102 (303) 234-5888 ii CONTEHTS Page Abstract 1 Introduction 1 Previous studies 2 Data used 3 Method of study 6 Man-made changes in the basin that could affect flow 7 Irrigation diversions 7 Inter-basin diversion 7 Re s ervo i r s 8 San Gregorio Reservoir 8 Seven Springs State Fish Hatchery 8 Fenton Lake 10 Jemez Canyon Reservoir 10 Water losses due to man-made changes 10 Irrigation diversions 10 Inter-basin diversion 11 Reservoirs 1 1 San Gregorio Reservoir, Seven Springs State Fish Hatchery, and Fenton Lake 11 Jemez Canyon Reservoir - 12 Natural streamflow at the upstream boundary of the Jemez Indian Reservation 13 Natural streamflow at the Jemez-Zia Indian Reservation boundary 13 Natural streamflow at the Zia-Santa Ana Indian Reservation Natural streamflow at the downstream boundary of the Santa Ana .