Status and Distribution of Barbary Sheep in the Southwest U.S
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Some Effects of Fire on Shrubs and Succulents in a Chihuahuan Desert Community in the Franklin Mountains, El Paso County, Texas Richard D
No. 3 January 1987 Contributed Papers of the SECOND SYMPOSIUM ON RESOURCES OF THE CHIHUAHUAN DESERT REGION United States and Mexico —BOTANICAL BIOLOGY— A. Michael Powell, Editor Some Effects of Fire on Shrubs and Succulents in a Chihuahuan Desert Community in the Franklin Mountains, El Paso County, Texas Richard D. Worthington and Rafael D. Corral THE CHIHUAHUAN DESERT RESEARCH INSTITUTE (CDRI) is a nonprofit scientific and educational organization. Its purpose is the collection and dissemination of information pertaining to the Chihuahuan Desert Region of the United States and Mexico. Memberships are available. Annual dues: Individual, $15; Student, $10; Family and Institutional, $25. The Chihuahuan Desert Research Institute publishes the semiannual magazine Chihuahuan Desert Discovery, which is free to members. Nonmembers and members receive our semiannual bulletin Chihuahuan Desert NewsBriefs. Papers in this series were presented during the Second Symposium on the Resources of the Chihuahuan Desert: United States and Mexico, at Sul Ross State University, Alpine, Texas, on October 20—21, 1983, and have been subjected to peer review. Contributed Papers of the SECOND SYMPOSIUM ON RESOURCES OF THE CHIHUAHUAN DESERT: United States and Mexico is a series by the Chihuahuan Desert Research Institute, Box 1334, Alpine,; Texas 79831; 915—837-8370. Copyright © 1986 by the Chihuahuan Desert Research Institute SOME EFFECTS OF FIRE ON SHRUBS AND SUCCULENTS IN A CHIHUAHUAN DESERT COMMUNITY IN THE FRANKLIN MOUNTAINS, EL PASO COUNTY, TEXAS RICHARD D. WORTHINGTON AND RAFAEL D. CORRAL, DEPARTMENT OF BIOLOGICAL SCIENCES, THE UNIVERSITY OF TEXAS AT EL PASO, EL PASO, TEXAS 79968 ABSTRACT.--On 15 July 1981, a fire burned about 30 ha of Chihua— huan desertscrub community in the Franklin Mountains, El Paso County, Texas. -
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. -
Cultural Resources Overview Desert Peaks Complex of the Organ Mountains – Desert Peaks National Monument Doña Ana County, New Mexico
Cultural Resources Overview Desert Peaks Complex of the Organ Mountains – Desert Peaks National Monument Doña Ana County, New Mexico Myles R. Miller, Lawrence L. Loendorf, Tim Graves, Mark Sechrist, Mark Willis, and Margaret Berrier Report submitted to the Wilderness Society Sacred Sites Research, Inc. July 18, 2017 Public Version This version of the Cultural Resources overview is intended for public distribution. Sensitive information on site locations, including maps and geographic coordinates, has been removed in accordance with State and Federal antiquities regulations. Executive Summary Since the passage of the National Historic Preservation Act (NHPA) in 1966, at least 50 cultural resource surveys or reviews have been conducted within the boundaries of the Desert Peaks Complex. These surveys were conducted under Sections 106 and 110 of the NHPA. More recently, local avocational archaeologists and supporters of the Organ Monument-Desert Peaks National Monument have recorded several significant rock art sites along Broad and Valles canyons. A review of site records on file at the New Mexico Historic Preservation Division and consultations with regional archaeologists compiled information on over 160 prehistoric and historic archaeological sites in the Desert Peaks Complex. Hundreds of additional sites have yet to be discovered and recorded throughout the complex. The known sites represent over 13,000 years of prehistory and history, from the first New World hunters who gazed at the nighttime stars to modern astronomers who studied the same stars while peering through telescopes on Magdalena Peak. Prehistoric sites in the complex include ancient hunting and gathering sites, earth oven pits where agave and yucca were baked for food and fermented mescal, pithouse and pueblo villages occupied by early farmers of the Southwest, quarry sites where materials for stone tools were obtained, and caves and shrines used for rituals and ceremonies. -
Promise Beheld and the Limits of Place
Promise Beheld and the Limits of Place A Historic Resource Study of Carlsbad Caverns and Guadalupe Mountains National Parks and the Surrounding Areas By Hal K. Rothman Daniel Holder, Research Associate National Park Service, Southwest Regional Office Series Number Acknowledgments This book would not be possible without the full cooperation of the men and women working for the National Park Service, starting with the superintendents of the two parks, Frank Deckert at Carlsbad Caverns National Park and Larry Henderson at Guadalupe Mountains National Park. One of the true joys of writing about the park system is meeting the professionals who interpret, protect and preserve the nation’s treasures. Just as important are the librarians, archivists and researchers who assisted us at libraries in several states. There are too many to mention individuals, so all we can say is thank you to all those people who guided us through the catalogs, pulled books and documents for us, and filed them back away after we left. One individual who deserves special mention is Jed Howard of Carlsbad, who provided local insight into the area’s national parks. Through his position with the Southeastern New Mexico Historical Society, he supplied many of the photographs in this book. We sincerely appreciate all of his help. And finally, this book is the product of many sacrifices on the part of our families. This book is dedicated to LauraLee and Lucille, who gave us the time to write it, and Talia, Brent, and Megan, who provide the reasons for writing. Hal Rothman Dan Holder September 1998 i Executive Summary Located on the great Permian Uplift, the Guadalupe Mountains and Carlsbad Caverns national parks area is rich in prehistory and history. -
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. -
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........................................................................ -
Magmatic Activity and Mineralization Along the Capitan, Santa Rita, And
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/60 Magmatic activity and mineralization along the Capitan, Santa Rita, and Morenci lineaments in the Chupadera Mesa area, central New Mexico McLemore, Virginia T., Zimmerer, Matthew, 2009, pp. 375-386 in: Geology of the Chupadera Mesa, Lueth, Virgil; Lucas, Spencer G.; Chamberlin, Richard M.; [eds.], New Mexico Geological Society 60th Annual Fall Field Conference Guidebook, 438 p. This is one of many related papers that were included in the 2009 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. -
Automated Landslide Hazard Detection September 2017
UNM Earth Data Analysis Center New Mexico State Cooperating Technical Partner, FEMA Region 6 FY16-PM-MAS008 Mapping Activity Statement 006 Automated Landslide Hazard Detection September 2017 LiDAR Derived Landslide Products September 2017 Figures and Tables ........................................................................................................................................ ii Table of Abbreviations and Acronyms ......................................................................................................... iii Introduction .................................................................................................................................................. 1 The Study Areas ............................................................................................................................................ 1 The Santa Fe County Study Area ............................................................................................................... 1 Rio Hondo HUC-8 Watershed Study Area ................................................................................................. 3 Landslide Types ............................................................................................................................................. 5 Methodology ................................................................................................................................................. 6 Slope......................................................................................................................................................... -
Hydrobasaluminite and Aluminite in Caves of the Guadalupe Mountains, New Mexico
Victor J. Polyak and Paula Provencio-Hydrobasaluminite and Aluminite in Caves of the Guadalupe Mountains, New Mexico. Journal of Cave and Karst Studies 60(1): 51-57. HYDROBASALUMINITE AND ALUMINITE IN CAVES OF THE GUADALUPE MOUNTAINS, NEW MEXICO VICTOR J. POLYAK Department of Geosciences, Texas Tech University, Lubbock, Texas 79409-1053 USA PAULA PROVENCIO Sandia National Laboratories, Albuquerque, New Mexico 87185 USA Hydrobasaluminite, like alunite and natroalunite, has formed as a by-product of the H2S-H2SO4 speleo- genesis of Cottonwood Cave located in the Guadalupe Mountains of New Mexico. This mineral is found as the major component of white pockets in the dolostone bedrock where clay-rich seams containing kaolinite, dickite, and illite have altered during speleogenesis to hydrobasaluminite, amorphous silica, alunite, and hydrated halloysite (endellite). Gibbsite and amorphous silica are associated with the hydrobasaluminite in a small room of Cottonwood Cave. Opalline sediment on the floor of this room accumulated as the cave passage evolved. Jarosite, in trace amounts, occurs in association with the opalline sediment and most likely has the same origin as hydrobasaluminite and alunite. The hydrobasa- luminite was found to be unstable at 25ºC and 50% RH, converting to basaluminite in a few hours. Basaluminite was not detected in the cave samples. Aluminite has precipitated as a secondary mineral in the same small room where hydrobasaluminite occurs. It comprises a white to bluish-white, pasty to powdery moonmilk coating on the cave walls. The bedrock pockets containing hydrobasaluminite provide the ingredients from which aluminite moonmilk has formed. It appears that recent cave waters have removed alumina and sulfate from the bedrock pock- et minerals and have deposited aluminite and gypsum along the cave wall. -
PDF Linkchapter
Index [Italic page numbers indicate major references] Abajo Mountains, 382, 388 Amargosa River, 285, 309, 311, 322, Arkansas River, 443, 456, 461, 515, Abort Lake, 283 337, 341, 342 516, 521, 540, 541, 550, 556, Abies, 21, 25 Amarillo, Texas, 482 559, 560, 561 Abra, 587 Amarillo-Wichita uplift, 504, 507, Arkansas River valley, 512, 531, 540 Absaroka Range, 409 508 Arlington volcanic field, 358 Acer, 21, 23, 24 Amasas Back, 387 Aromas dune field, 181 Acoma-Zuni scction, 374, 379, 391 Ambrose tenace, 522, 523 Aromas Red Sand, 180 stream evolution patterns, 391 Ambrosia, 21, 24 Arroyo Colorado, 395 Aden Crater, 368 American Falls Lava Beds, 275, 276 Arroyo Seco unit, 176 Afton Canyon, 334, 341 American Falls Reservoir, 275, 276 Artemisia, 21, 24 Afton interglacial age, 29 American River, 36, 165, 173 Ascension Parish, Louisana, 567 aggradation, 167, 176, 182, 226, 237, amino acid ash, 81, 118, 134, 244, 430 323, 336, 355, 357, 390, 413, geochronology, 65, 68 basaltic, 85 443, 451, 552, 613 ratios, 65 beds, 127,129 glaciofluvial, 423 aminostratigraphy, 66 clays, 451 Piedmont, 345 Amity area, 162 clouds, 95 aggregate, 181 Anadara, 587 flows, 75, 121 discharge, 277 Anastasia Formation, 602, 642, 647 layer, 10, 117 Agua Fria Peak area, 489 Anastasia Island, 602 rhyolitic, 170 Agua Fria River, 357 Anchor Silt, 188, 198, 199 volcanic, 54, 85, 98, 117, 129, Airport bench, 421, 423 Anderson coal, 448 243, 276, 295, 396, 409, 412, Alabama coastal plain, 594 Anderson Pond, 617, 618 509, 520 Alamosa Basin, 366 andesite, 75, 80, 489 Ash Flat, 364 Alamosa -
Sulfide/Barite/Fluorite Mineral Deposits, Guadalupe Mountains
Sulfide/barite/fluoritemineraldeposits, Guadalupe Mountains, NewMexico and west Texas byCarol A. Hrl/,Consulting Geologist, 17 ElArco Drive, Albuquerque, NM87123 Abstract along Basinand Rangefault zones(Wood, Rocky Arroyo prospect (Teepeemine, Sulfide/barite/fluorite mineral depos- 1958).The Bird and Bissettmines in the Pitts and Price,fr.) its in the Guada.lupeMountains are sim- Glass Mountains are associatedwith in- The Rocky Arroyo prospect (RA) is in ilar to those elsewhere in the Delaware trusive bodies (King, 1930).Despite var- SEt/c sec. 26 T2lS R24E along Walt Can- Basin: (1) they are all mineralogically iations in location (from Guadalupe yon -1 km (-0.6 mi) south of NM-137 simple (containing pyrite and usually Mountains to Fort Stockton;Fig. 1) and where the road crossesRockv Arroyo. This sphalerite, calcite, dolomite, and some- geologic association (igneous intrusions, prospect, unlike most of the other mineral times barite, fluorite, or galena);(2) most faults, structural and stratigraphic traps), depositsin the GuadalupeMountains, is have sulfur-isotope values ranging from the mineral deposits around the margins 6vS= - 9 to + (3) have not a sulfide deposit. It is a uranium de- 5%o;and most car- of the Delaware Basin appear to be re- bon-orygen-isotope values ranging from posit where uranium (as much as 2.35Vo; 6t:g- - 5 lo - !5%o,61EO: - 3 to - 107oo. lated. Mineralogy in all of the deposits is Waltman, 1954;Mclemore, 1983)as well The deposits are in structural and strat- similar, and sulfur-isotope values of sul- as arsenic,barium, copper, molybdenum, igraphii traps, occupying the same po- fide minerals usually fall within a fairly nickel (Table 1) are concentrated in -9 and sition as many of the cavesin the narrow range of values(6sS: to I5%o, hydrocarbon (thucholite) pellets dissem- Guadalupe Mountains. -
A Geologic Study of the Capulin Volcano National Monument and Surrounding Areas, Union and Colfax Counties, New Mexico
A Geologic Study of the Capulin Volcano National Monument and surrounding areas, Union and Colfax Counties, New Mexico by William O. Sayre and Michael H. Ort New Mexico Bureau of Geology and Mineral Resources, New Mexico Tech Socorro, New Mexico 87801 Open-file Report 541 August, 2011 A geologic study of Capulin Volcano National Monument and surrounding areas Final Report Cooperative Agreement CA7029-2-0017 December 4, 1999 Submitted to: Capulin Volcano National Monument P. O. Box 80 Capulin, New Mexico 88414 Submitted by: William O. Sayre, Ph.D., P.G. College of Santa Fe 1600 St. Michael’s Drive Santa Fe, New Mexico 87505-7634 and Michael H. Ort, Ph.D. Department of Geology PO Box 4099 Northern Arizona University Flagstaff, Arizona 86011 Table of Contents Executive Summary ........................................................................................................ 2 Introduction ..................................................................................................................... 2 Body of Report .............................................................................................................. 17 Discussion and Conclusions ......................................................................................... 22 Recommendations for Future Work .............................................................................. 64 References .................................................................................................................... 65 Appendices…………………………………………………………………………………….