Renewable Energy in the National Park Service
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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. -
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. -
Replace Or Modernize?
Payne ES 1896 Draper ES 1953 Miner ES 1900 Shadd ES 1955 Ketcham ES Replace1909 Moten or ES Modernize1955 ? Bell SHS 1910 Hart MS 1956 Garfield ETheS Future191 0of theSharpe District Health of SE Columbia' 1958 s Thomson ES 191Endangered0 Drew ES Old and 195Historic9 Smothers ES 1923 Plummer ES 1959 Hardy MS (Rosario)1928 Hendley ESPublic 195School9 s Bowen ES 1931 Aiton ES 1960 Kenilworth ES 1933 J.0. Wilson ES May196 12001 Anacostia SHS 1935 Watkins ES 1962 Bunker Hill ES 1940 Houston ES 1962 Beers ES 1942 Backus MS 1963 Kimball ES 1942 C.W. Harris ES 1964 Kramer MS 1943 Green ES 1965 Davis ES 1943 Gibbs ES 1966 Stanton ES 1944 McGogney ES 1966 Patterson ES 1945 Lincoln MS 1967 Thomas ES 1946 Brown MS 1967 Turner ES 1946 Savoy ES 1968 Tyler ES 1949 Leckie ES 1970 Kelly Miller MS 1949 Shaed ES 1971 Birney ES 1950 H.D. Woodson SHS 1973 Walker-Jones ES 1950 Brookland ES 1974 Nalle ES 1950 Ferebee-Hope ES 1974 Sousa MS 1950 Wilkinson ES 1976 Simon ES 1950 Shaw JHS 1977 R. H. Terrell JHS 1952 Mamie D. Lee SE 1977 River Terrace ES 1952 Fletche-Johnson EC 1977 This report is dedicated to the memory of Richard L. Hurlbut, 1931 - 2001. Richard Hurlbut was a native Washingtonian who worked to preserve Washington, DC's historic public schools for over twenty-five years. He was the driving force behind the restoration of the Charles Sumner School, which was built after the Civil War in 1872 as the first school in Washington, DC for African- American children. -
Pounding the Pavement the Park 16TH ST
MD. B EA C H 29 D.C. Chevy D MD. R. Chase D.C. N.H. AVE. CONNECTICUT AVE. MILITARY RD. MILITARY RD. 13TH ST. Pounding the Pavement The Park 16TH ST. 1.7 miles ROCK (With Your Boots On) NEBRASKA AVE. CREEK . D R S.D. AVE. FINISH: Fort Reno T Rock Creek N P ARK A Park G R Suburbs Park Tennis E G 400 O RIGGS RD. 409 feet Center R feet in the City G I Iowa and 1 3 miles A A B N V Arkansas r O E o R . avenues a T START: d H Rock Broad Fort Carter The area around Third and Webster 13th and 171 feet Creek Branch C DAVENPORT ST. Br Barron A Washington’s Reno streets shows a diversity of homes. P FORT U streets I T Park Amphi- O L TOTTEN 95 feet 300 highest point is in theatre S . T Fort Reno Park. E . Finish V Fort Otis and A S Endless Totten A Park Place S N N.H. AVE. Park A Northwest 200 feet K FORT RENO PHOTO BY JAMES M. THRESHER — THE WASHINGTON POST; OTHER PHOTOS BY STEVEN GINSBERG — THE WASHINGTON POST R 2 miles IOWA AVE. A Rock . Sherman This old clunker probably hadn’t been on the open road in decades. 200 TENLEYTOWN- DR Creek H Circle AU C Cemetery A E B 5TH ST. Suburbs BUCHANAN ST. Endless Northwest | 2 miles Heart of Rock Creek Endless The in the 29 Petwort h WEBSTER ST the City Cemetery Northwest Park City 13TH ST. -
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 -
Rock Creek Park Visitor Study Summer 1999
Rock Creek Park Visitor Study Summer 1999 Report 112 Visitor Services Project Cooperative Park Studies Unit Rock Creek Park Visitor Study Summer 1999 Margaret Littlejohn Visitor Services Project Report 112 April 2000 Margaret Littlejohn is VSP Coordinator, National Park Service, based at the Cooperative Park Studies Unit, University of Idaho. I thank Mike Meehan, Alyson Vander Stoep, Leigh Blackburn, Sara Kohan and the staff of Rock Creek Park for their assistance with this study. The VSP acknowledges the Public Opinion Lab of the Social and Economic Sciences Research Center, Washington State University, for its technical assistance. Visitor Services Project Rock Creek Park Report Summary • This report describes the results of a visitor study at Rock Creek Park during July 8-14, 1999. A total of 888 questionnaires were distributed to visitors. Visitors returned 564 questionnaires for a 63.5% response rate. • This report profiles Rock Creek Park visitors. A separate appendix contains visitors' comments about their visit. This report and the appendix include summaries of those comments. • Forty percent of the visitors were alone; 25% were with friends and 25% were with family. Forty- three percent of visitor groups were groups of one; 33% were in groups of two. Over one-half of visitors (56%) were aged 26-50; 13% were aged 15 years or younger. • Most visitors (93%) said English is their primary language. Most visitors (94%) said their ethnicity was "not Hispanic or Latino." When asked about their race, visitors responded as follows: White (74%), Black or African American (24%), Asian (3%), Hispanic or Latino (2%), American Indian/Alaska Native (1%) and Native Hawaiian/Pacific Islander (<1%). -
NEVADA CALIF Ecogroup.Indd
Eastern Sierra Eastern Sierra Humboldt-Toiyabe National Forest Scattered pieces of a national treasure where adventures come together H U M B O L D T - T O I Y A B E N A T I O N A L F O R E S T USDA Department of Agriculture • Forest Service Intermountain Region • Ogden, Utah Bridgeport Ranger District’s Hoover Wilderness in eastern California 23.260.419.01/01 Humboldt-Toiyabe National Forest WHERE ADVENTURES COME TOGETHER Santa Rosa Ranger District’s Santa Rosa Peak Spring Mountains National Recreation Area’s Mummy Mountain Hoover Wilderness he Humboldt-Toiyabe’s spectacular 6.3 million acres make up the largest national forest in the lower 48 states. TTen distinctive ranger districts are scat- tered like an intriguing puzzle across Nevada and a small portion of eastern California. Each piece contains its own unusual features, which offer unlimited rec- reation. The ranger districts vary from hardy “desert scapes” to snow-capped mountains with lush alpine meadows and timbered canyons. A world of discovery Indian Paintbrush awaits those who explore the Forest’s rich historic past. The following page displays the districts and lists numbers and web- sites. Bristlecone pine: one of the oldest known living tree species. Ruby Mountains Ranger District’s Echo Canyon Bridgeport Ranger District’s East Lake in the Hoover Wilderness Contacts . Scattered pieces of a national treasure: Humboldt Toiyabe Headquarters (Sparks) ................................ 775-355-5301 www.fs.fed.us/r4/htnf/ Carson Ranger District (Carson City) .................................. 775-882-2766 bringing it all together . Bridgeport Ranger District (Bridgeport, CA) ..................... -
Mistletoes of North American Conifers
United States Department of Agriculture Mistletoes of North Forest Service Rocky Mountain Research Station American Conifers General Technical Report RMRS-GTR-98 September 2002 Canadian Forest Service Department of Natural Resources Canada Sanidad Forestal SEMARNAT Mexico Abstract _________________________________________________________ Geils, Brian W.; Cibrián Tovar, Jose; Moody, Benjamin, tech. coords. 2002. Mistletoes of North American Conifers. Gen. Tech. Rep. RMRS–GTR–98. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 123 p. Mistletoes of the families Loranthaceae and Viscaceae are the most important vascular plant parasites of conifers in Canada, the United States, and Mexico. Species of the genera Psittacanthus, Phoradendron, and Arceuthobium cause the greatest economic and ecological impacts. These shrubby, aerial parasites produce either showy or cryptic flowers; they are dispersed by birds or explosive fruits. Mistletoes are obligate parasites, dependent on their host for water, nutrients, and some or most of their carbohydrates. Pathogenic effects on the host include deformation of the infected stem, growth loss, increased susceptibility to other disease agents or insects, and reduced longevity. The presence of mistletoe plants, and the brooms and tree mortality caused by them, have significant ecological and economic effects in heavily infested forest stands and recreation areas. These effects may be either beneficial or detrimental depending on management objectives. Assessment concepts and procedures are available. Biological, chemical, and cultural control methods exist and are being developed to better manage mistletoe populations for resource protection and production. Keywords: leafy mistletoe, true mistletoe, dwarf mistletoe, forest pathology, life history, silviculture, forest management Technical Coordinators_______________________________ Brian W. Geils is a Research Plant Pathologist with the Rocky Mountain Research Station in Flagstaff, AZ. -
Fort Dupont Park Historic Resources Study Final Robinson & Associates
Fort Dupont Park Historic Resources Study Final Robinson & Associates, Inc. November 1, 2004 Page 1 ______________________________________________________________________________________ TABLE OF CONTENTS I. LIST OF ILLUSTRATIONS 2 II. PURPOSE AND METHODOLOGY 5 III. SUMMARY OF SIGNIFICANCE 6 IV. HISTORIC CONTEXT STATEMENT 20 1. Pre-Civil War History 20 2. 1861-65: The Civil War and Construction of Fort Dupont 25 3. Post-Civil War Changes to Washington and its Forts 38 4. The Planning and Construction of the Fort Drive 48 5. Creation of Fort Dupont Park 75 6. 1933-42: The Civilian Conservation Corps Camp at Fort Dupont Park 103 7. 1942-45: Antiaircraft Artillery Command Positioned in Fort Dupont Park 116 8. History of the Golf Course 121 9. 1938 through the 1970s: Continued Development of Fort Dupont Park 131 10. Recreational, Cultural, and African-American Family Use of Fort Dupont Park 145 11. Proposals for the Fort Circle Parks 152 12. Description of Fort Dupont Park Landscape Characteristics, Buildings and Structures 155 V. BIBLIOGRAPHY 178 VI. KEY PARK LEGISLATION 191 Fort Dupont Park Historic Resources Study Final Robinson & Associates, Inc. November 1, 2004 Page 2 ______________________________________________________________________________________ I. LIST OF ILLUSTRATIONS Figure 1 Fort Dupont Park is located in the southeast quadrant of Washington, D.C. 7 Figure 2 Fort Dupont Park urban context, 1995 8 Figure 3 Map of current Fort Dupont Park resources 19 Figure 4 Detail of the 1856-59 Boschke Topographical Map 24 Figure 5 Detail