New Distributional Records of the Red Squirrel (Tamiasciurus Hudsonicus) in Western New Mexico and Evidence for Its Extirpation from the Zuni Mountains
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An Environmental History of the Middle Rio Grande Basin
United States Department of From the Rio to the Sierra: Agriculture Forest Service An Environmental History of Rocky Mountain Research Station the Middle Rio Grande Basin Fort Collins, Colorado 80526 General Technical Report RMRS-GTR-5 Dan Scurlock i Scurlock, Dan. 1998. From the rio to the sierra: An environmental history of the Middle Rio Grande Basin. General Technical Report RMRS-GTR-5. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 440 p. Abstract Various human groups have greatly affected the processes and evolution of Middle Rio Grande Basin ecosystems, especially riparian zones, from A.D. 1540 to the present. Overgrazing, clear-cutting, irrigation farming, fire suppression, intensive hunting, and introduction of exotic plants have combined with droughts and floods to bring about environmental and associated cultural changes in the Basin. As a result of these changes, public laws were passed and agencies created to rectify or mitigate various environmental problems in the region. Although restoration and remedial programs have improved the overall “health” of Basin ecosystems, most old and new environmental problems persist. Keywords: environmental impact, environmental history, historic climate, historic fauna, historic flora, Rio Grande Publisher’s Note The opinions and recommendations expressed in this report are those of the author and do not necessarily reflect the views of the USDA Forest Service. Mention of trade names does not constitute endorsement or recommendation for use by the Federal Government. The author withheld diacritical marks from the Spanish words in text for consistency with English punctuation. Publisher Rocky Mountain Research Station Fort Collins, Colorado May 1998 You may order additional copies of this publication by sending your mailing information in label form through one of the following media. -
Late Paleozoic Tectonic and Sedimentologic History of the Penasco Uplift, North-Central New Mexico
RICE UNIVERSITY LATE PALEOZOIC TECTONIC AND SEDIMENTOLOGIC HISTORY OF THE PENASCO UPLIFT, NORTH-CENTRAL NEW MEXICO by ROY DONALD ADAMS A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE MASTER OF ARTS APPROVED, THESIS COMMITTEE: 0^ (3- /jtd&i obfe B. Anderson, Chairman Assistant Professor pf Geology KT Rudy R. Schwarzer, Adjunct Assistant Professor of GSology John /E. Warme Professor of Geology Donald R. Baker Professor of Geology Houston, Texas May, 1980 ABSTRACT LATE PALEOZOIC TECTONIC AND SEDIMENTOLOGIC HISTORY OF THE PENASCO UPLIFT, NORTH-CENTRAL NEW MEXICO Roy Donald Adams The Paleozoic Peiiasco Uplift, located on the site of the present Nacimiento Mountains of north-central New Mexico, acted as a sediment source and modifier of regional sedimentation patterns from Middle Pennsylvanian to Early Permian time. The earliest history of the uplift is still poorly defined. Orogenic activity may have started as early as the Late Mississippian, or there may have been quiescence until after deposition of the Morrow-age Osha Canyon Formation and prior to deposition of the Atoka-age Sandia Formation. Coarse, arkosic siliciclastic sediments inter- bedded with fossilferious carbonates in the Madera Formation indicate that by early Desmoinesian time the Peiiasco Uplift had risen sufficiently to expose and erode Precambrian rocks. Paleotransport indicators in the arkosic sediments show transport away from the uplift. Throughout the remainder of the Pennsylvanian, the Peiiasco Uplift was a sediment source. The siliciclastic sediments derived from the Peiiasco Uplift formed a wedge that prograded out onto and interfingered with carbonate sediments of a shallow normal marine shelf. A change in paleotransport directions from northeasterly to southwesterly occurs on the east side of the Peiiasco Uplift and is due to the arrival of a flood of siliciclastic sediments derived from the Uncompahgre-San Luis Uplift to the northeast. -
Water and Natural Resources Committee
WATER AND NATURAL RESOURCES COMMITTEE 2012 INTERIM FINAL REPORT to the FIFTIETH LEGISLATURE SECOND SESSION New Mexico Legislative Council Service Santa Fe, New Mexico December 2012 WATER AND NATURAL RESOURCES COMMITTEE 2012 REPORT Santa Fe, New Mexico December 2012 2012 LEGISLATIVE INTERIM WATER AND NATURAL RESOURCES COMMITTEE SUMMARY OF WORK The committee scheduled five meetings during the 2012 interim that were held in Las Cruces, Truth or Consequences, Ruidoso, Albuquerque and Santa Fe. Continued drought and major wildfires again dominated the news in 2012. Through November 2012, the average precipitation for New Mexico was near the record lowest value, ranking as the second driest since 1895, as severe to exceptional drought continued across New Mexico, and the average temperature for the state for the year was the highest on record. It was also the second consecutive year during which record-breaking wildfires burned across the state. The lightning-sparked Whitewater-Baldy Complex Fire in the Gila Wilderness burned more than 297,845 acres, which surpassed the area burned by the Las Conchas Fire of 2011, making it the largest wildfire in New Mexico state history. The Little Bear Fire was also started by a lightning strike; it burned 44,330 acres and 254 buildings in Lincoln County after quickly growing out of control due to dry, windy conditions. The city of Ruidoso and the surrounding area will need more than $14 million in the coming years to address the effects of that fire on their drinking water supplies alone. At the committee's joint meeting in August with the Courts, Corrections and Justice Committee, the committees reviewed several legal issues of concern to both committees, including the state's suit against the federal Bureau of Reclamation on its administration of Rio Grande Project water, implementation of the Pecos River Settlement, the status of ongoing adjudications and the need for spaceport liability legislation. -
Butch Cassidy Roamed Incognito in Southwest New Mexico
Nancy Coggeshall I For The New Mexican Hideout in the Gila Butch Cassidy roamed incognito in southwest New Mexico. Hideout in the Gila utch Cassidy’s presence in southwestern New Mexico is barely noted today. Notorious for his successful bank Butch Cassidy roamed and train robberies at the turn of the 20th century, incognito in southwest Cassidy was idealized and idolized as a “gentleman out- New Mexico wilderness Blaw” and leader of the Wild Bunch. He and various members of the • gang worked incognito at the WS Ranch — set between Arizona’s Blue Range and San Carlos Apache Reservation to the west and the Nancy Coggeshall rugged Mogollon Mountains to the east — from February 1899 For The New Mexican until May 1900. Descendants of pioneers and ranchers acquainted with Cassidy tell stories about the man their ancestors knew as “Jim Lowe.” Nancy Thomas grew up hearing from her grandfather Clarence Tipton and others that Cassidy was a “man of his word.” Tipton was the foreman at the WS immediately before Cassidy’s arrival. The ranch sits at the southern end of the Outlaw Trail, a string of accommodating ranches and Wild Bunch hideouts stretching from Montana and the Canadian border into Mexico. The country surrounding the WS Ranch is forbidding; volcanic terrain cleft with precipitously angled, crenelated canyon walls defies access. A “pretty hard layout,” local old-timer Robert Bell told Lou Blachly, whose collection of interviews with pioneers — conducted PROMIENT PLACES - between 1942 and 1953 — are housed at the University of New OUTLAW TRAIL Mexico. What better place to dodge the law? 1. -
Geologic Influences on Apache Trout Habitat in the White Mountains of Arizona
GEOLOGIC INFLUENCES ON APACHE TROUT HABITAT IN THE WHITE MOUNTAINS OF ARIZONA JONATHAN W. LONG, ALVIN L. MEDINA, Rocky Mountain Research Station, U.S. Forest Service, 2500 S. Pine Knoll Dr, Flagstaff, AZ 86001; and AREGAI TECLE, Northern Arizona University, PO Box 15108, Flagstaff, AZ 86011 ABSTRACT Geologic variation has important influences on habitat quality for species of concern, but it can be difficult to evaluate due to subtle variations, complex terminology, and inadequate maps. To better understand habitat of the Apache trout (Onchorhynchus apache or O. gilae apache Miller), a threatened endemic species of the White Mountains of east- central Arizona, we reviewed existing geologic research to prepare composite geologic maps of the region at intermediate and fine scales. We projected these maps onto digital elevation models to visualize combinations of lithology and topog- raphy, or lithotopo types, in three-dimensions. Then we examined habitat studies of the Apache trout to evaluate how intermediate-scale geologic variation could influence habitat quality for the species. Analysis of data from six stream gages in the White Mountains indicates that base flows are sustained better in streams draining Mount Baldy. Felsic parent material and extensive epiclastic deposits account for greater abundance of gravels and boulders in Mount Baldy streams relative to those on adjacent mafic plateaus. Other important factors that are likely to differ between these lithotopo types include temperature, large woody debris, and water chemistry. Habitat analyses and conservation plans that do not account for geologic variation could mislead conservation efforts for the Apache trout by failing to recognize inherent differences in habitat quality and potential. -
Museum of New Mexico
MUSEUM OF NEW MEXICO OFFICE OF ARCHAEOLOGICAL STUDIES ARCHAEOLOGY OF THE MOGOLLON HIGHLANDS: SETTLEMENT SYSTEMS AND ADAPTATIONS edited by Yvonne R. Oakes and Dorothy A. Zamora VOLUME 6. SYNTHESIS AND CONCLUSIONS Yvonne R. Oakes Submitted by Timothy D. Maxwell Principal Investigator ARCHAEOLOGY NOTES 232 SANTA FE 1999 NEW MEXICO TABLE OF CONTENTS Figures............................................................................iii Tables............................................................................. iv VOLUME 6. SYNTHESIS AND CONCLUSIONS ARCHITECTURAL VARIATION IN MOGOLLON STRUCTURES .......................... 1 Structural Variation through Time ................................................ 1 Communal Structures......................................................... 19 CHANGING SETTLEMENT PATTERNS IN THE MOGOLLON HIGHLANDS ................ 27 Research Orientation .......................................................... 27 Methodology ................................................................ 27 Examination of Settlement Patterns .............................................. 29 Population Movements ........................................................ 35 Conclusions................................................................. 41 REGIONAL ABANDONMENT PROCESSES IN THE MOGOLLON HIGHLANDS ............ 43 Background for Studying Abandonment Processes .................................. 43 Causes of Regional Abandonment ............................................... 44 Abandonment Patterns in the Mogollon Highlands -
Late Wisconsin Climate Inferences from Rock Glaciers in South-Central
LateWisconsin climatic inlerences from rock glaciers in south-centraland west-central New Mexico andeast-central Arizona byJohn W. Blagbrough, P0 Box8063, Albuquerque, NewMexico 87198 Abstract Inactive rock glaciersof late Wisconsin age occur at seven sites in south-central and west-central New Mexico and in east-centralArizona. They are at the base of steep talus in the heads of canyons and ravines and have surfacefeatures indicating they are ice-cemented (permafrost) forms that moved by the flow of interstitial ice. The rock glaciersindicate zones of alpine permafrost with lower levels that rise from approximately 2,400m in the east region to 2,950 m in the west. Within the zones the mean annual temperaturewas below freezing, and the climatewas marked by much diurnal freezing and thawing resulting in the production of large volumes of talus in favorableterrain. The snow cover was thin and of short duration, which fa- vored ground freezing and cryofraction. The rock glaciers in the east region occur near the late Wisconsin 0'C air isotherm and implv that the mean annual temperature was depressedapproximately 7 to 8'C during a periglacial episodein the late Wisconsin.A dry continental climate with a seasonaldistribution of precipitation similar to that of the present probably prevailed, and timberline former timberlines. may have been depresseda minimum of 1,240m. The rise in elevation of the rock glaciersfrom east to west acrossthe region is attributed to greater snowfall in west-centralNew Mexico and east-centralArizona, which reducedthe inten- sity and depth of ground freezing near the late Wisconsin 0"C air isotherm. -
Saddlebrooke Hiking Club Hike Database 11-15-2020 Hike Location Hike Rating Hike Name Hike Description
SaddleBrooke Hiking Club Hike Database 11-15-2020 Hike Location Hike Rating Hike Name Hike Description AZ Trail B Arizona Trail: Alamo Canyon This passage begins at a point west of the White Canyon Wilderness on the Tonto (Passage 17) National Forest boundary about 0.6 miles due east of Ajax Peak. From here the trail heads west and north for about 1.5 miles, eventually dropping into a two- track road and drainage. Follow the drainage north for about 100 feet until it turns left (west) via the rocky drainage and follow this rocky two-track for approximately 150 feet. At this point there is new signage installed leading north (uphill) to a saddle. This is a newly constructed trail which passes through the saddle and leads downhill across a rugged and lush hillside, eventually arriving at FR4. After crossing FR4, the trail continues west and turns north as you work your way toward Picketpost Mountain. The trail will continue north and eventually wraps around to the west side of Picketpost and somewhat paralleling Alamo Canyon drainage until reaching the Picketpost Trailhead. Hike 13.6 miles; trailhead elevations 3471 feet south and 2399 feet north; net elevation change 1371 feet; accumulated gains 1214 northward and 2707 feet southward; RTD __ miles (dirt). AZ Trail A Arizona Trail: Babbitt Ranch This passage begins just east of the Cedar Ranch area where FR 417 and FR (Passage 35) 9008A intersect. From here the route follows a pipeline road north to the Tub Ranch Camp. The route continues towards the corrals (east of the buildings). -
Scenic Trips to the Geologic Past No. 4: Southern Zuni Mountains. Zuni
SCENIC TRIPS TO THE GEOLOGIC PAST No. No. 1—Santa Fe, New Mexico, 1968 ($1.00). No. 2—Taos-Red River-Eagle Nest, New Mexico, Circle Drive 1968 ($1.00). No. 3—Roswell-Capitan-Ruidoso and Bottomless Lakes Park, New Mexico, 1967 ($1.00). No. 4—Southern Zuni Mountains, New Mexico, 1971 ($1.50). No. No. 5—Silver City-Santa Rita-Hurley, New Mexico, 1967 ($1.00). No. 6—Trail Guide to the Upper Pecos, New Mexico, 1967 ($1.50). No. 7—High Plains—Northeastern New Mexico, Raton-Capulin Mountain- Clayton, 1967 ($1.50). No. 8—Mosaic of New Mexico's Scenery, Rocks, and History, 1967 ($1.50). No. 9—Albuquerque-Its Mountains, valley, Water, and Volcanoes, 1969 ($1.50). No. 10—Southwestern New Mexico, 1971 ($1.50). Cover: SHALAKO WARRIOR DOLL “Man-made highways and automobiles crisscross this world but hardly penetrate it…” J. FRANK DOBIE Apache Gold and Yaqui Silver SCENIC TRIPS TO THE GEOLOGIC PAST NO. 4 Southern Zuni Mountains Zuni-Cibola Trail BY ROY W. FOSTER PHOTOGRAPHS BY H. L. JAMES SKETCHES BY PATRICIA C. GICLAS 1971 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO 87801 NEW MEXICO STATE BUREAU OF MINES AND MINERAL RESOURCES DON H. BAKER, JR., Director A Division of NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY STIRLING A. COLGATE, President THE REGENTS MEMBERS EX OFFICIO The Honorable Bruce King ...............................Governor of New Mexico Leonard DeLayo .............................Superintendent of Public Instruction APPOINTED MEMBERS William G. Abbott .......................................................................... Hobbs Henry S. Birdseye ................................................................Albuquerque Ben Shantz ................................................................................Silver City Steve S. -
Southwest NM Publication List
Southwest New Mexico Publication Inventory Draft Source of Document/Search Purchase Topic Category Keywords County Title Author Date Publication/Journal/Publisher Type of Document Method Price Geology 1 Geology geology, seismic Southwestern NM Six regionally extensive upper-crustal Ackermann, H.D., L.W. 1994 U.S. Geological Survey, Open-File Report 94- Electronic file USGS publication search refraction profiles, seismic refraction profiles in Southwest New Pankratz, D.P. Klein 695 (DJVU) http://pubs.er.usgs.gov/usgspubs/ southwestern New Mexico ofr/ofr94695 Mexico, 2 Geology Geology, Southwestern NM Magmatism and metamorphism at 1.46 Ga in Amato, J.M., A.O. 2008 In New Mexico Geological Society Fall Field Paper in Book http://nmgs.nmt.edu/publications/g $45.00 magmatism, the Burro Mountains, southwestern New Boullion, and A.E. Conference Guidebook - 59, Geology of the Gila uidebooks/59/ metamorphism, Mexico Sanders Wilderness-Silver City area, 107-116. Burro Mountains, southwestern New Mexico 3 Geology Geology, mineral Catron County Geology and mineral resources of York Anderson, O.J. 1986 New Mexico Bureau of Mines and Mineral Electronic file (PDF) NMBGMR search $10.00 for resources, York Ranch SE quadrangle, Cibola and Catron Resources Open File Report 220A, 22 pages. <http://geoinfo.nmt.edu/publicatio CD Ranch, Fence Counties, New Mexico ns/openfile/details.cfml?Volume=2 Lake, Catron, 20A> Cibola 4 Geology Geology, Zuni Salt Catron County Geology of the Zuni Salt Lake 7 1/2 Minute Anderson, O.J. 1994 New Mexico Bureau of Mines and -
Summits on the Air – ARM for the USA (W7A
Summits on the Air – ARM for the U.S.A (W7A - Arizona) Summits on the Air U.S.A. (W7A - Arizona) Association Reference Manual Document Reference S53.1 Issue number 5.0 Date of issue 31-October 2020 Participation start date 01-Aug 2010 Authorized Date: 31-October 2020 Association Manager Pete Scola, WA7JTM Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Document S53.1 Page 1 of 15 Summits on the Air – ARM for the U.S.A (W7A - Arizona) TABLE OF CONTENTS CHANGE CONTROL....................................................................................................................................... 3 DISCLAIMER................................................................................................................................................. 4 1 ASSOCIATION REFERENCE DATA ........................................................................................................... 5 1.1 Program Derivation ...................................................................................................................................................................................... 6 1.2 General Information ..................................................................................................................................................................................... 6 1.3 Final Ascent -
Geohydrology of the San Agustin Basin, Alamosa Creek Basin
Geohydrology of the San Agustin Basin, Alamosa Creek Basin upstream from Monticello Box, and upper Gila Basin in parts of Catron, Socorro, and Sierra Counties, New Mexico By R.G. Myers, J.T. Everheart, and C.A. Wilson U.S. GEOLOGICAL SURVEY WATER-RESOURCES INVESTIGATIONS REPORT 94-4125 Prepared in cooperation with the NEW MEXICO STATE ENGINEER OFFICE Albuquerque, New Mexico 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For additional information Copies of this report can write to: be purchased from: U.S. Geological Survey District Chief Earth Science Information Center U.S. Geological Survey Open-File Reports Section Water Resources Division Box 25286, MS 517 4501 Indian School Rd. NE, Suite 200 Denver Federal Center Albuquerque, New Mexico 87110 Denver, Colorado 80225 CONTENTS Page Abstract.................................................................................................................................................. 1 Introduction........................................................................................................................................... 1 Purpose and scope...................................................................................................................... 3 Location and extent.................................................................................................................... 3 Ctimate....................................^ 3 Previous hydrologic investigations.........................................................................................