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Likely to Have Habitat Within Iras That ALLOW Road
Item 3a - Sensitive Species National Master List By Region and Species Group Not likely to have habitat within IRAs Not likely to have Federal Likely to have habitat that DO NOT ALLOW habitat within IRAs Candidate within IRAs that DO Likely to have habitat road (re)construction that ALLOW road Forest Service Species Under NOT ALLOW road within IRAs that ALLOW but could be (re)construction but Species Scientific Name Common Name Species Group Region ESA (re)construction? road (re)construction? affected? could be affected? Bufo boreas boreas Boreal Western Toad Amphibian 1 No Yes Yes No No Plethodon vandykei idahoensis Coeur D'Alene Salamander Amphibian 1 No Yes Yes No No Rana pipiens Northern Leopard Frog Amphibian 1 No Yes Yes No No Accipiter gentilis Northern Goshawk Bird 1 No Yes Yes No No Ammodramus bairdii Baird's Sparrow Bird 1 No No Yes No No Anthus spragueii Sprague's Pipit Bird 1 No No Yes No No Centrocercus urophasianus Sage Grouse Bird 1 No Yes Yes No No Cygnus buccinator Trumpeter Swan Bird 1 No Yes Yes No No Falco peregrinus anatum American Peregrine Falcon Bird 1 No Yes Yes No No Gavia immer Common Loon Bird 1 No Yes Yes No No Histrionicus histrionicus Harlequin Duck Bird 1 No Yes Yes No No Lanius ludovicianus Loggerhead Shrike Bird 1 No Yes Yes No No Oreortyx pictus Mountain Quail Bird 1 No Yes Yes No No Otus flammeolus Flammulated Owl Bird 1 No Yes Yes No No Picoides albolarvatus White-Headed Woodpecker Bird 1 No Yes Yes No No Picoides arcticus Black-Backed Woodpecker Bird 1 No Yes Yes No No Speotyto cunicularia Burrowing -
By Douglas P. Klein with Plates by G.A. Abrams and P.L. Hill U.S. Geological Survey, Denver, Colorado
U.S DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY STRUCTURE OF THE BASINS AND RANGES, SOUTHWEST NEW MEXICO, AN INTERPRETATION OF SEISMIC VELOCITY SECTIONS by Douglas P. Klein with plates by G.A. Abrams and P.L. Hill U.S. Geological Survey, Denver, Colorado Open-file Report 95-506 1995 This report is preliminary and has not been edited or reviewed for conformity with U.S. Geological Survey editorial standards. The use of trade, product, or firm names in this papers is for descriptive purposes only, and does not imply endorsement by the U.S. Government. STRUCTURE OF THE BASINS AND RANGES, SOUTHWEST NEW MEXICO, AN INTERPRETATION OF SEISMIC VELOCITY SECTIONS by Douglas P. Klein CONTENTS INTRODUCTION .................................................. 1 DEEP SEISMIC CRUSTAL STUDIES .................................. 4 SEISMIC REFRACTION DATA ....................................... 7 RELIABILITY OF VELOCITY STRUCTURE ............................. 9 CHARACTER OF THE SEISMIC VELOCITY SECTION ..................... 13 DRILL HOLE DATA ............................................... 16 BASIN DEPOSITS AND BEDROCK STRUCTURE .......................... 20 Line 1 - Playas Valley ................................... 21 Cowboy Rim caldera .................................. 23 Valley floor ........................................ 24 Line 2 - San Luis Valley through the Alamo Hueco Mountains ....................................... 25 San Luis Valley ..................................... 26 San Luis and Whitewater Mountains ................... 26 Southern -
Runoff and Sediment Yield from Proxy Records: Upper Animas Creek Basin, New Mexico
United States Department of Agriculture Runoff and Sediment Yield from Forest Service Proxy Records: Rocky Mountain Research Station Research Paper RMRS-RP-18 Upper Animas Creek Basin, New Mexico June 1999 W. R. Osterkamp Abstract Osterkamp, W. R. 1999. Runoff and sediment yield from proxy records: upper Animas Creek Basin, New Mexico. Res. Pap. RMRS-RP-18. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 50 p. Analyses of water- and sediment-yield records from the Walnut Gulch Experimental Watershed, the San Simon Wash Basin, and the Jornada Experimental Range, combined with observations of regional variations in climate, geology and soils, vegetation, topography, fire frequency, and land-use history, allow estimates of present conditions of water and sediment discharges in the upper Animas Creek Basin, New Mexico. Further, the records are used to anticipate fluxes of water and sediment should watershed conditions change. Results, intended principally for hydrologists, geomorpholo- gists, and resource managers, suggest that discharges of water and sediment in the upper Animas Creek Basin approximate those of historic, undisturbed conditions, and that erosion rates may be generally lower than those of comparison watersheds. If conversion of grassland to shrubland occurs, sediment yields, due to accelerated upland gully erosion, may increase by 1 to 3 orders of magnitude. However, much of the released sediment would likely be deposited along Animas Creek, never leaving the upper Animas Creek Basin. Keywords: runoff, sediment yield, erosion, Animas Creek Author W. R. Osterkamp is a research hydrologist with the U. S. Geological Survey, Water Resources Division, Tucson, AZ. -
Summary of Us Geological Survey Ground-Water
SUMMARY OF U.S. GEOLOGICAL SURVEY GROUND-WATER- FLOW MODELS OF BASIN-FILL AQUIFERS IN THE SOUTHWESTERN ALLUVIAL BASINS REGION, COLORADO, NEW MEXICO, AND TEXAS By John Michael Kernodle U.S. GEOLOGICAL SURVEY Open-File Report 90-361 Albuquerque, New Mexico 1992 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL |SURVEY Dallas L. Peck, E'irector 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 4501 Indian School Rd. NE, Suite 200 Box 25425 Albuquerque, New Mexico 87110 Denver, Colorado 80225 Foreword The Regional Aquifer-System Analysis Program The Regional Aquifer-System Analysis (RASA) program was started in 1978 after a congressional mandate to develop quantitative appraisals of the major ground-water systems of the United States. The RASA program represents a systematic effort to study a number of the Nation's most important aquifer systems that, in aggregate, underlie much of the country and that represent important components of the Nation's total water supply. In general, the boundaries of these studies are identified by the hydrologic extent of each system, and accordingly transcend the political subdivisions to which investigations have often arbitrarily been limited in the past. The broad objective for each study is to assemble geologic, hydrologic, and geochemical information, to analyze and develop an understanding of the system, and to develop predictive capabilities that will contribute to the effective management of the system. The use of computer simulation is an important element of the RASA studies, both to develop an understanding of the natural, undisturbed hydrologic system and any changes brought about by human activities as well as to provide a means of predicting the regional effects of future pumping or other stresses. -
Major Geologic Structures Between Lordsburg, New Mexico, and Tucson, Arizona Harald D
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/29 Major geologic structures between Lordsburg, New Mexico, and Tucson, Arizona Harald D. Drewes and C. H. Thorman, 1978, pp. 291-295 in: Land of Cochise (Southeastern Arizona), Callender, J. F.; Wilt, J.; Clemons, R. E.; James, H. L.; [eds.], New Mexico Geological Society 29th Annual Fall Field Conference Guidebook, 348 p. This is one of many related papers that were included in the 1978 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. -
Mation to Investigate the Role of Natural and for Which Written
Reconstruction of Precipitation and PDSI from Tree-Ring Chronologies Developed in Mountains of New Mexico, USDA and Sonora, Mexico Item Type text; Proceedings Authors Villanueva-Diaz, Jose; McPherson, Guy R. Publisher Arizona-Nevada Academy of Science Journal Hydrology and Water Resources in Arizona and the Southwest Rights Copyright ©, where appropriate, is held by the author. Download date 24/09/2021 04:36:16 Link to Item http://hdl.handle.net/10150/297002 RECONSTRUCTION OF PRECIPITATION AND PDSI FROM TREE -RING CHRONOLOGIES DEVELOPED IN MOUNTAINS OF NEW MEXICO, USA AND SONORA, MEXICO Jose Villanueva -Diaz and Guy R. McPherson) Long quantitative records of year -by -year meteor- Tertiary volcanic activity was renewed with erup- ological observations are limited or nonexistent in tions of rhyolite, tuffs, and basalt (Arras 1979; the southwestern United States and northern Stone and O'Brian 1990; Wagner 1977). Mexico. Such records are invaluable to researchers The Sierra los Ajos are located in Sonora, Mex- studying paleoclimate dynamics and forcing func- ico (30 °55'N latitude, 109°55W longitude), about tions that influence the climate system. 100 km southwest of the Animas Mountains. The Trees store information on their annual rings main peak rises above 2600 m (COTECOCA 1973) about climates and their effects on the structure (Figure 1). The Sierra los Ajos comprise a complex and composition of local forest ecosystems. There- geologic formation characterized by a heterogene- fore, tree rings have been used as sources of infor- ous lithic composition. Outcrops from Precambri- mation to investigate the role of natural and an and Holocene age are found in these mountains anthropogenic disturbances as well as environ- (Aponte 1974). -
Plan for the Recovery of Desert Bighorn Sheep in New Mexico 2003-2013
PLAN FOR THE RECOVERY OF DESERT BIGHORN SHEEP IN NEW MEXICO 2003-2013 New Mexico Department of Game and Fish August 2003 Executive Summary Desert bighorn sheep (Ovis canadensis mexicana) were once prolific in New Mexico, occupying most arid mountain ranges in the southern part of the state. Over-hunting, and disease transmission from livestock are 2 primary reasons for the dramatic decline in bighorn sheep numbers throughout the west during the early 1900s. In 1980, desert bighorn were placed on New Mexico’s endangered species list. From 1992-2003, approximately 25% of bighorn were radiocollared to learn causes of mortality driving this species towards extinction. Approximately 85% of all known-cause non-hunter killed radiocollared individuals have been killed by mountain lions. Despite the lack of a native ungulate prey base in desert bighorn range, mountain lion populations remain high, leading to the hypothesis that mountain lions are subsidized predators feeding on exotic ungulates, including cattle. Lack of fine fuels from cattle grazing have resulted in a lack of fire on the landscape. This has lead to increased woody vegetation which inhibits bighorn’s ability to detect and escape from predators. Bighorn numbers in spring 2003 in New Mexico totaled 213 in the wild, and 91 at the Red Rock captive breeding facility. This is in spite of releasing 266 bighorn from Red Rock and 30 bighorn from Arizona between 1979 and 2002. Several existing herds of desert bighorn likely need an augmentation to prevent them from going extinct. The presence of domestic sheep and Barbary sheep, which pose risks to bighorn from fatal disease transmission and aggression, respectively, preclude reintroduction onto many unoccupied mountain ranges. -
U.S. Department of the Interior U.S. Geological Survey
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Prepared in cooperation with New Mexico Bureau of Mines and Mineral Resources 1997 MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO 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. Cover: View looking south to the east side of the northeastern Organ Mountains near Augustin Pass, White Sands Missile Range, New Mexico. Town of White Sands in distance. (Photo by Susan Bartsch-Winkler, 1995.) MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO By SUSAN BARTSCH-WINKLER, Editor ____________________________________________________ U. S GEOLOGICAL SURVEY OPEN-FILE REPORT 97-521 U.S. Geological Survey Prepared in cooperation with New Mexico Bureau of Mines and Mineral Resources, Socorro U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Shaefer, Interim Director For sale by U.S. Geological Survey, Information Service Center Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO Susan Bartsch-Winkler, Editor Summary Mimbres Resource Area is within the Basin and Range physiographic province of southwestern New Mexico that includes generally north- to northwest-trending mountain ranges composed of uplifted, faulted, and intruded strata ranging in age from Precambrian to Recent. -
Newsmac Spring 2020
NewsMAC Spring 2020 NewsMAC Newsletter of the New Mexico Archeological Council P.O. Box 25691 Albuquerque, NM 87125 NewsMAC Spring 2020 (2020-1) Contents PRESIDENT’S WELCOME 1 EDITOR’S INTRODUCTION 2 PROGRESS UPDATE: ANCESTRAL PUEBLO AGRICULTURAL LANDSCAPES PROJECT 3 Kaitlyn E. Davis, Ph.D. Candidate, University of Colorado, Boulder RADIOCARBON DATING OF A THERMAL FEATURE AT A TIPI RING SITE AT THE 4 DEHAVEN RANCH AND PRESERVE Emily J. Brown, Aspen CRM Consulting – NMAC Grant Recipient INVESTIGATIONS ON THE BOX CANYON VILLAGE SITE (LA 4980), AN ANIMAS PHASE VILLAGE IN HIDALGO COUNTY, NM 11 Thatcher A. Rogers, University of New Mexico – NMAC Grant Recipient THE AZOTEA PEAK RING MIDDEN SURVEY: A CULTURAL LANDSCAPE OF SUBSISTENCE AND FEASTING AROUND THE AZOTEA MESA, EDDY COUNTY, NM 16 Ryan Scott Hechler, Statistical Research, Inc. DATA RECOVERY AT SEVEN SITES SOUTH OF SANTA FE FOR NM GAS CO. Kye Miller, PaleoWest 20 SOUTH BY SOUTHWEST: ARCHAEOLOGICAL DICHOTOMIES, ORTHODOXIES, AND 21 HETERODOXIES IN THE MOGOLLON OR WERE THOSE MIGRANTS PROPERLY DOCUMENTED? Marc Thompson 28 REPORT ON 2019 NMAC FALL CONFERENCE: COLLABORATIVE ARCHAEOLOGY, INDIGENOUS ARCHAEOLOGY, AND TRIBAL HISTORIC PRESERVATION IN THE SOUTHWESTERN UNITED STATES Michael Spears NMAC CONTACTS 30 NewsMAC Spring 2020 President’s Welcome Greetings all and welcome to this pandemic issue of NewsMAC. I want to say thank you to Tamara Jager Stewart for volunteering to fill our newsletter editor vacancy this year, and working with our NMAC Past President Kye Miller to get this issue out to the membership during this busy and stressful time for all of us. I hope everyone is healthy and safe, and dealing well with the challenges of teleworking, videoconferencing, and Zoom-meeting fatigue—or the even greater challenges of safely conducting fieldwork during the COVID-19 pandemic. -
Geophysics, Geology, and Geothermal Leasing Status of the Lightning Dock KGRA, Animas Valley, New Mexico Christian S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/29 Geophysics, geology, and geothermal leasing status of the Lightning Dock KGRA, Animas Valley, New Mexico Christian S. Smith, 1978, pp. 343-348 in: Land of Cochise (Southeastern Arizona), Callender, J. F.; Wilt, J.; Clemons, R. E.; James, H. L.; [eds.], New Mexico Geological Society 29th Annual Fall Field Conference Guidebook, 348 p. This is one of many related papers that were included in the 1978 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. -
Delayed and Rapid Deglaciation of Alpine Valleys in the Sawatch Range, Southern
Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA Joseph P. Tulenko1, William Caffee1, Avriel D. Schweinsberg1, Jason P. Briner1, Eric M. 5 Leonard2. 1. Department of Geology, University at Buffalo, Buffalo, NY 14260, USA 2. Department of Geology, Colorado College, Colorado Springs, CO 80903, USA 10 Abstract We quantify retreat rates for three alpine glaciers in the Sawatch Range of the southern Rocky Mountains following the Last Glacial Maximum using 10Be ages from ice-sculpted, valley-floor bedrock transects and statistical analysis via the BACON program in R. Glacier retreat in the Sawatch Range from at (100%) or near (~83%) Last 15 Glacial Maximum extents initiated between 16.0 and 15.6 ka and was complete by 14.2 – 13.7 ka at rates ranging between 35.6 to 6.8 m a-1. Deglaciation in the Sawatch Range commenced ~2 – 3 kyr later than the onset of rising global CO2, and prior to rising temperatures observed in the North Atlantic region at the Heinrich Stadial 1/Bølling transition. However, deglaciation in the Sawatch Range approximately aligns 20 with the timing of Great Basin pluvial lake lowering. Recent data-modeling comparison efforts highlight the influence of the large North American ice sheets on climate in the western United States, and we hypothesize that recession of the North American ice sheets may have influenced the timing and rate of deglaciation in the Sawatch Range. 1 While we cannot definitively argue for exclusively North Atlantic forcing or North 25 American ice sheet forcing, our data demonstrate the importance of regional forcing mechanisms on past climate records. -
Jaguar Critical Habitat Comments in Response to 71 FR 50214-50242 (Aug
October 19, 2012 Submitted on-line via www.regulations.gov, Docket No. FWS-R2-ES-2012-0042. Re: Jaguar critical habitat comments in response to 71 FR 50214-50242 (Aug. 20, 2012). To Whom it May Concern, The Center for Biological Diversity supports the designation of the entirety of the areas that the Fish and Wildlife Service proposes as critical habitat. However, these areas are not sufficient to conserve the jaguar in the United States. Nor does the Service’s itemization of threats to critical habitat areas cover the array of actions that would in fact destroy or adversely modify them. As we explain in detail in the comments below and through evidence presented in our appended letter of 10/1/2012 on the Recovery Outline for the Jaguar, we request seven principal changes in the final critical habitat designation rule, as follows: 1. The following additional mountain ranges within the current boundary of the Northwestern Recovery Unit (as described in the April 2012 Recovery Outline for the Jaguar) should be designated as critical habitat: in Arizona, the Chiricahua, Dos Cabezas, Dragoon and Mule mountains, and in New Mexico the Animas and adjoining Pyramid mountains. 2. The following additional “sky island” mountain ranges outside of the current boundaries of the Northwestern Recovery Unit should be designated as critical habitat: In New Mexico, the Alama Hueco, Big Hatchet, Little Hatchet, Florida, West and East Potrillo, Cedar and Big Burro mountains; in Arizona, the Galiuro, Santa Teresa, Pinaleno, Whitlock, Santa Catalina and Rincon mountains. Straddling both states, the Peloncillo Mountains north of the current boundaries of the Northwestern Recovery Unit should also be designated 3.