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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. -
Black Elk Peak Mobile Scanning Customers & Services Definitive Elevation Bringing the Goods TRUE ELEVATION BLACK ELK PEAK » JERRY PENRY, PS
MAY 2017 AROUND THE BEND Survey Economics Black Elk Peak Mobile Scanning Customers & services Definitive elevation Bringing the goods TRUE ELEVATION BLACK ELK PEAK » JERRY PENRY, PS Displayed with permission • The American Surveyor • May 2017 • Copyright 2017 Cheves Media • www.Amerisurv.com lack Elk Peak, located in the Black Hills region of South Dakota, is the state’s highest natural point. It is frequently referred to as the highest summit in the United States east of the Rocky BMountains. Two other peaks, Guadalupe Peak in Texas and Sierra Blanca Peak in New Mexico, are higher and also east of the Continental Divide, but they are P. Tuttle used a Green’s mercury barometer, one of the considered south of the Rockies. best instruments of the time to determine elevations on The famed Black Elk Peak was known as Harney high peaks. Tuttle coordinated his measurements with Peak as early as 1855 in honor of General William S. simultaneous readings at the Union Pacific Railroad Harney. This designation lasted for more than 160 depot in Cheyenne, Wyo. The difference between the two years, but the peak was renamed Black Elk Peak on barometer readings, when added to the known sea level August 11, 2016, by the U. S. Board of Geographic elevation at Cheyenne, resulted in elevations of 7369.4’ Names to honor medicine man Black Elk of the Oglala and 7368.4’, varying greatly from the 9700’ elevation Lakota (Sioux). The two names are synonymously used previously obtained by Ludlow. in this article as the same peak. The elevation results of the Newton-Jenney The first attempt to accurately measure the elevation of Expedition were not published until 1880 due to the Black Elk Peak was in 1874 during the Custer Expedition. -
Encounters with the Early Highpointers by Charles
SOME CLOSE (AND NOT SO CLOSE) ENCOUNTERS WITH THE EARLY HIGHPOINTERS BY CHARLES FERIS Many stories can be told of how we got our first inspiration to pursue this hobby of ours, this highpointing. We’ve been inspired in a hundred ways; mine arose during a period of boredom, while in college. Seeking something other than study, I took out a Rand McNally road atlas, and looked at a map of my native state of Illinois, noting the little red dot in the northwest corner of the state. Wow, something neat to do. So while the other kids were off to Florida, off to Charles Mound I went during spring break 1961. Then it hit me; I had already done Mt. Whitney the year before, so why not do all the states. Now I was really excited. The next few years saw me collecting 13 more highpoints in the Midwest and southeast. I went my merry way, never realizing that others might be crazy enough to be pursuing the very same project. At this point I was not aware of the tiny fraternity of early highpointers who were already years before me. I had no idea of the remarkable people I was about to meet. Then in August 1965 a Sierra Club friend of mine in Chicago told me about C. Rowland Stebbins. I had found a kindred soul, one who had already completed the 48. I phoned him immediately. Soon my wife and I were off on the four hour drive to Lansing, Michigan. We arrived to an expansive mansion on Moore’s River Drive atop a bluff overlooking the Grand River. -
Arrowhead • Fall 2008 1 Arrowhead Fall 2008 • Vol
Arrowhead • Fall 2008 1 Arrowhead Fall 2008 • Vol. 15 • No. 4 The Newsletter of the Employees & Alumni Association of the National Park Service Published By Eastern National FROM THE DIRECTOR National Parks Second Century or more than Fa half-century, Commission Established folk singers have been repeating the Old Testament PS Director Mary A. Bomar has experts, park managers and the general conservationists, academics, business lead- advice: “To every Nhailed the establishment of the public over the course of their 12-month ers, policy experts and retired NPS execu- thing there is a National Parks Second Century Commis- effort, culminating in a report with rec- tives. The commission is led by former season.” This is a sion, a nonpartisan citizens group that will ommendations in the fall of 2009. senators Baker and Johnston. season of change provide recommendations for the future Former United States senators Howard “As the National Park Service looks and a season of celebration. of the National Park System. The com- H. Baker, Jr. (R-Tenn.) and J. Bennett ahead to our centennial in 2016,” said Most of the world’s religions rec- mission first met in August at Santa Johnston, Jr. (D-La.) announced the for- Director Bomar, “we appreciate that ognize the lengthening days that Monica Mountains NRA and will meet in mation of the National Parks Second public-spirited citizens step forward to follow the winter solstice as a time four additional national parks by June of Century Commission on Aug. 12. The help chart the course of our parks for of hope and possibility. -
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. -
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. -
Climbing America's
batical leave in Scandinavia, I finally reached the 5895m summit of Africa’s high- est mountain. In 1986, the year after I climbed Kilimanjaro, Dick Bass, Frank Wells, and Rick Ridgeway published Seven Summits, an account of Bass and Wells’ attempt to climb the highest peak on each of the world’s seven continents. I bought their book and devoured it. Inspired by it, I devised my own climbing goal—to climb at least ‘Three-and-a-Half Summits’: namely, at least three of the six highest of the Seven Summits plus Australia’s Mt Kosciuszko, which is a mere 2228m above sea level (i.e., less than half the height of Antarctica’s Vinson Massif, the sixth-lowest of the Seven Summits), and Kosciuszko can therefore, as a Kiwi I quipped, really only be regarded as a half-summit. I made reasonably quick progress towards achieving my goal. In August 1994, I climbed Russia’s Mt Elbrus, 5642m, the highest mountain in Europe. In December the same year, I summited 6962m-high Cerro Aconcagua in Argentina, the highest mountain in South America (which I like to tell people is ‘the highest mountain in the world outside Asia,’ and then hope their geography is so weak that they don’t realise how huge an exclusion clause those two words, ‘outside Asia’, are). I then decided to have a crack at climbing Denali, and on 6 July 1997 stood proudly on the 6194m-high summit of North America’s high- est peak and held up a t-shirt from Victoria University (which is where I taught political science for many years). -
Birds of the Guadalupe Mountain Region of Western Texas
Number 8 August 20, 1940 OCCASIONAL PAPERS OF THE MUSEUM OF ZOOLOGY LOUISIANA STATE UNIVERSITY Baton Rouge, La. Louisiana State University Press BIRDS OF THE GUADALUPE MOUNTAIN REGION OF WESTERN TEXAS' By Thomas D. Burleigh and George H. Lowery, Jr. Rising from the desert floor amid Mesquite, cactus, and Grease Bush, Guadalupe Peak has the distinction of being the highest point in the big state of Texas — reaching an altitude of 8758 feet above sea level. There, among its high ridges and escarpments in the heart of a Texas desert plain, one finds a beautiful Canadian Transition Zone forest. Dense stands of conifers — Western Yellow Pine and Douglas Fir— along with oaks and maples, combine to make the area a biotic community quite unlike the remainder of Texas. One would judge that such an area would have long since attracted ornithologists. In searching for new Texas birds, certainly the highest point in the state would merit investigation. To the contrary, however, so far as we can determine, only three ornithologists have collected and observed birds there prior to the present study, and then only for an aggregate of sixteen days during late summer. During May, 1939, we collected birds in several localities in the Trans-Pecos area of western Texas. Proceeding from Van Horn, osten sibly for El Paso, we made a brief stop during the afternoon of May 17 in Pine Springs Canyon of the Guadalupe range. Even superficial 1 The present work represents a cooperative study undertaken jointly by the Fish and Wildlife Service, U.S. Department of the Interior, and the Museum of Zoology of the Louisiana State University and Agricultural and Mechanical College. -
Locsec News by Sandy Halby
The Newsletter of Plains and Peaks Mensa, Southern Colorado Volume 28, Issue 11 http://www.plainsandpeaks.us.mensa.org/ DECEMBER 2011 LocSec News by Sandy Halby Hello! All is normal at the Halbys except we’ve Coming up in December – our annual Holiday Brian, Wetzel, Ann, Ginny, Kathie, Deborah, made some adjustments to our “pack.” In mid- Party at the Stagecoach Inn in Manitou Springs. Gary, Tony, Anthony, David, Gary, Steve, Jim, October, we adopted another dog – a New- This is our biggest event of the year and I hope RC, Gia, Kari, Lou, Daniel, Jennie-Jo, Wayne, foundland named Otis. He’s black and not as you can join me, Mike and a bunch of fellow Eryn and anybody I might have missed … and big as Kody, but just as sweet. Otis was a little Mensans for an evening of camaraderie, fun, hugs to all of you… my Mensa friends. nervous at first about all these other dogs, but as and holiday cheer! Be sure to RSVP by the 28th dogs are wont to do, they’re all working it out. of November! From Mike and me: Merry Christmas and Chance is teaching Otis to play and Brinkley is Happy New Year! Hope to see YOU soon at a teaching him how to beg and get on the beds! Then, in January, some of usual events like Give Plains & Peaks Mensa event!! Having four large dogs now leaves no room in In to Beer Pressure, Trivia Night, Mix & Mingle the kitchen during feeding time and when they and Kimball’s. -
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. -
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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