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Presidential Documents Vol
50223 Federal Register Presidential Documents Vol. 61, No. 186 Tuesday, September 24, 1996 Title 3Ð Proclamation 6920 of September 18, 1996 The President Establishment of the Grand Staircase-Escalante National Monument By the President of the United States of America A Proclamation The Grand Staircase-Escalante National Monument's vast and austere land- scape embraces a spectacular array of scientific and historic resources. This high, rugged, and remote region, where bold plateaus and multi-hued cliffs run for distances that defy human perspective, was the last place in the continental United States to be mapped. Even today, this unspoiled natural area remains a frontier, a quality that greatly enhances the monument's value for scientific study. The monument has a long and dignified human history: it is a place where one can see how nature shapes human endeavors in the American West, where distance and aridity have been pitted against our dreams and courage. The monument presents exemplary opportunities for geologists, paleontologists, archeologists, historians, and biologists. The monument is a geologic treasure of clearly exposed stratigraphy and structures. The sedimentary rock layers are relatively undeformed and unobscured by vegetation, offering a clear view to understanding the proc- esses of the earth's formation. A wide variety of formations, some in brilliant colors, have been exposed by millennia of erosion. The monument contains significant portions of a vast geologic stairway, named the Grand Staircase by pioneering geologist Clarence Dutton, which rises 5,500 feet to the rim of Bryce Canyon in an unbroken sequence of great cliffs and plateaus. The monument includes the rugged canyon country of the upper Paria Canyon system, major components of the White and Vermilion Cliffs and associated benches, and the Kaiparowits Plateau. -
Scoping Report: Grand Staircase-Escalante National
CONTENTS 1 Introduction .............................................................................................................................................. 1 2 Scoping Process ....................................................................................................................................... 3 2.1 Purpose of Scoping ........................................................................................................................... 3 2.2 Scoping Outreach .............................................................................................................................. 3 2.2.1 Publication of the Notice of Intent ....................................................................................... 3 2.2.2 Other Outreach Methods ....................................................................................................... 3 2.3 Opportunities for Public Comment ................................................................................................ 3 2.4 Public Scoping Meetings .................................................................................................................. 4 2.5 Cooperating Agency Involvement ................................................................................................... 4 2.6 National Historic Preservation Act and Tribal Consultation ....................................................... 5 3 Submission Processing and Comment Coding .................................................................................... 5 -
Terrestrial Vertebrate Fauna of the Kaiparowits Basin
Great Basin Naturalist Volume 40 Number 4 Article 2 12-31-1980 Terrestrial vertebrate fauna of the Kaiparowits Basin N. Duane Atwood U.S. Forest Service, Provo, Utah Clyde L. Pritchett Brigham Young University Richard D. Porter U.S. Fish and Wildlife Service, Provo, Utah Benjamin W. Wood Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Atwood, N. Duane; Pritchett, Clyde L.; Porter, Richard D.; and Wood, Benjamin W. (1980) "Terrestrial vertebrate fauna of the Kaiparowits Basin," Great Basin Naturalist: Vol. 40 : No. 4 , Article 2. Available at: https://scholarsarchive.byu.edu/gbn/vol40/iss4/2 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. TERRESTRIAL VERTEBRATE FAUNA OF THE KAIPAROWITS BASIN N. Diiane Atwood', Clyde L. Pritchctt', Richard D. Porter', and Benjamin W. Wood' .\bstr^ct.- This report inehides data collected during an investigation by Brighani Young University personnel to 1976, as well as a literature from 1971 review. The fauna of the Kaiparowits Basin is represented by 7 species of salamander, toads, mnphihians (1 5 and 1 tree frog), 29 species of reptiles (1 turtle, 16 lizards, and 12 snakes), 183 species of birds (plus 2 hypothetical), and 74 species of mammals. Geographic distribution of the various species within the basin are discussed. Birds are categorized according to their population and seasonal status. -
A Preliminary Assessment of Archaeological Resources Within the Grand Staircase-Escalante National Monument, Utah
A PRELIMINARY ASSESSMENT OF ARCHAEOLOGICAL RESOURCES WITHIN THE GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT, UTAH by David B. Madsen Common rock art elements of the Fremont and Anasazi on the Colorado Plateau and the Grand Staircase-Escalante National Monument. ,I!! CIRCULAR 95 . 1997 I~\' UTAH GEOLOGICAL SURVEY ." if;~~ 6EPARTMENT OF NATURAL RESOURCES ISBN 1-55791-605-5 STATE OF UTAH Michael O. Leavitt, Governor DEPARTMENT OF NATURAL RESOURCES Ted Stewart, Executive Director UTAH GEOLOGICAL SURVEY M. Lee Allison~ Director UGS Board Member Representing Russell C. Babcock, Jr. (chairman) .................................................................................................. Mineral Industry D. Cary Smith ................................................................................................................................... Mineral Industry Richard R. Kennedy ....................................................................................................................... Civil Engineering E.H. Deedee O'Brien ......................................................................................................................... Public-at-Large C. William Berge .............................................................................................................................. Mineral Industry Jerry Golden ..................................................................................................................................... Mineral Industry Milton E. Wadsworth ............................................................................................... -
Yanawant: Paiute Places and Landscapes in the Arizona Strip
Yanawant Paiute Places and Landscapes in the Arizona Strip Volume Two OfOfOf The Arizona Strip Landscapes and Place Name Study Prepared by Diane Austin Erin Dean Justin Gaines December 12, 2005 Yanawant Paiute Places and Landscapes in the Arizona Strip Volume Two Of The Arizona Strip Landscapes and Place Name Study Prepared for Bureau of Land Management, Arizona Strip Field Office St. George, Utah Prepared by: Diane Austin Erin Dean Justin Gaines Report of work carried out under contract number #AAA000011TOAAF030023 2 Table of Contents Preface……………………………………………………………………………………………ii i Chapter One: Southern Paiute History on the Arizona Strip………………………………...1 Introduction.............................................................................................................................. 1 1.1 Early Southern Paiute Contact with Europeans and Euroamericans ........................... 5 1.2 Southern Paiutes and Mormons ........................................................................................ 8 1.3 The Second Powell Expedition......................................................................................... 13 1.4 An Onslaught of Cattle and Further Mormon Expansion............................................ 16 1.5 Interactions in the First Half of the 20 th Century ......................................................... 26 Chapter Two: Southern Paiute Place Names On and Near the Arizona Strip 37 Introduction ........................................................................................................................... -
Itineraries from Panguitch, Utah
Itineraries From Panguitch, Utah Day One: Red Canyon / Casto Canyon / Losee Canyon Explore these three canyons that are all part of the Dixie National Forest. Go east from downtown Panguitch and follow Scenic Highway 89 as it bends south (seven miles) to Scenic Byway 12. Turn east (left) on Scenic Byway 12 toward Bryce Canyon National Park. Just over one mile up the road you’ll encounter a dirt road with signs pointing to the trail-heads for both Casto and Losee Canyons. You may venture to these canyons for hiking, mountain biking, ATV riding, or you may continue straight on Scenic Byway 12 to Red Canyon (.5 miles). Here you’ll find a visitor information center with details on how what to see and do in Red Canyon and the surrounding area. Explore side canyons or venture on the paved path that leads to the top of the canyon. This is ideal for people on foot or on a bicycle. The paved trail follows Scenic Byway 12 as it winds to the east, crossing over ravines, and ascending to the Pansaugunt Plateau. The return walk or ride downhill is easy going and very enjoyable. Upon completion of your chosen activities you may return to Panguitch for dining, shopping and lodging. Panguitch, Utah – Itineraries – www.Panguitch.com 1 Day Two: Bryce Canyon National Park Bryce Canyon National Park is actually a series of amphitheaters that run for approximately 20 miles along the eastern rim of the Pansaugunt Plateau. You may venture the full length of this beautifully paved road to the end of the park, stopping at overlooks along the way. -
In Panguitch Lake and Navajo Lake, Utah, from Scales and Opercular Bones
Utah State University DigitalCommons@USU All Graduate Theses and Dissertations Graduate Studies 5-1954 Age and Growth of the Utah Chub, Gila atraria (Girard), in Panguitch Lake and Navajo Lake, Utah, From Scales and Opercular Bones John M. Neuhold Follow this and additional works at: https://digitalcommons.usu.edu/etd Part of the Aquaculture and Fisheries Commons Recommended Citation Neuhold, John M., "Age and Growth of the Utah Chub, Gila atraria (Girard), in Panguitch Lake and Navajo Lake, Utah, From Scales and Opercular Bones" (1954). All Graduate Theses and Dissertations. 3769. https://digitalcommons.usu.edu/etd/3769 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Theses and Dissertations by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. AGE AND GROWTH OF THE UTAH CHUB, Ql1! ATRARIA (GIRARD), IN PANGUITCH LAKE AND NAVAJO LA!E, UTAH, FROM SCALES AND OPERCULAR BONES by John M. Beuhold A thesis submitted in partial fulfillment of the requirements for the degree ot MASTER OF SCIENCE ln Fishery Management UTAH STATE AGRICULTURAL COLLEGE Logan, Utah 1954 ABSTRACT Previous literature indicates the opercular bone as a . useful t ool for the determination of age and growth of fish. The reliability and validity _o f this method is tested for two populations of Utah chub. Age and growth are calculated for 222 Utah chub collected from Panguitch Lake and 212 Utah chub collected from Navajo Lake, southern Utah, in 1952-1953 from both scales and opercular bones. -
The Science Behind Volcanoes
The Science Behind Volcanoes A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface. Volcanoes are generally found where tectonic plates are diverging or converging. A mid-oceanic ridge, for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by convergent tectonic plates coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust in the interiors of plates, e.g., in the East African Rift, the Wells Gray-Clearwater volcanic field and the Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "Plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so- called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere. -
Bryce Canyon National Park
Lees Ferry, Arizona), White (which surround Utah Zion Canyon), Gray and Pink. Most of the Grand Staircase is now contained within the BLM-managed Grand Staircase - Escalante National Monument. The rocks that give Bryce Canyon its distinctive colors are members of the Claron Formation, a mixed Highlights limestone/sandstone layer, and are also found exposed, with similarly intricate forms, in other nearly locations such as Red Canyon and Cedar Breaks. Erosion: Water is responsible for creating the rock shapes in Bryce Canyon National Park. Rain and melting snow flowing down the Pink Cliffs towards the Paria River form ridges, or fins, which subsequently erode into the spires, pinnacles and other shapes (collectively known as ‘hoodoos’) which are left standing. In time these too erode, and the whole process moves very gradually westwards as more of the cliff is slowly worn away. During the long, cold winters, the cliffs are further weakened by freezing water Bryce Canyon National Park expanding in cracks, resulting in more erosion when the ice Bryce Canyon National Park does not contain one main thaws in spring. canyon, but rather a dozen smaller ravines eroded into the east side of a ridge running approximately north-south at Bryce Canyon Trails: As with most national parks, the best the edge of the Paunsaugunt Plateau in southwest Utah. This way to appreciate Bryce Canyon is to explore away from erosion has resulted in thousands of bizarre and fragile rock the main roads. There are various trails both along the rim formations, large and small, in many subtle shades of pink, and down through the formations, but probably the best white, yellow, orange and red, extending in quite a narrow is the Fairyland Loop Trail, an 8 mile, little-used route which band for over 25 miles along the plateau rim. -
Documented by Mcdonald and Harbaugh (1988) Was Used for This Sirrulation
srATE OF UTAH DEPAR'IMENI' OF NATURAL RESCURCES Tedmical Publication lb. 102 GROUND-WATER HYrROLCGY OF THE UPPER SE.VIER RIVER BASIN, SClJIH-cENrnAL UTAH, AID SIMULATION OF GROUND-WATER F'I.(W IN THE VALLEY-FILL AlJJIFER IN PAN:lliI'ICH VALLEY By Susan A. 'Ihiros am William C. Brothers Prepared by the Uni ted States Geological Survey in cooperation with the Utah Departnent of Natural Resources Division of water Rights 1993 Page Abstract 1 Introduction ••••••• I Purp:>se arrl soope 3 Methods of investigation . 3 Ackoowledgnents 3 Numberi~ system for hydrologic-data sites •••••••••••••• 3 Description of the study area ................................... 4 Geologic setti~ ........................................... 6 Climate .................................................... 8 vegetation . 9 Iarrluse ................................................... 10 Surface-water hydrology .................................... 10 Ground-water hydrology of oonsolidated rocks 11 Ground-water hydrology of the valley-fill aquifer in Panguitch Valley 13 Recharge 14 seepage fran streams 14 seepage fran caIla.1s ••••••••••••••••••••••••••••••••••••••••• 15 seepage fran unconsuned irrigation water ••••••••••••••••• 16 Infiltration of precipitation •••••••••••••••••••••••• 22 seepage fran consolidated rock ....................... 22 Movanent 22 Discharge 23 seepage to the Sevier River and canals ••••••••••••••••••• 23 E.Va]?CJtraIlSpiration . 24 Springs 25 wells 25 Slll:::surfare outfl~ •••••••••..•.••••••.•••••••••••••••••.••• 26 Water-level fluctuations 26 -
Factors Affecting Cottonwood Recruitment in Zion National Park
Factors Affecting Cottonwood Recruitment in Zion National Park Final Report to National Park Service CPCESU, Project number OSU 3 and OSU 4 Cooperative Agreement CA# H1200040002 By William J. Ripple1 and Robert L. Beschta College of Forestry Oregon State University, Corvallis, OR 97331 E-mail: [email protected] Phone: (541) 737-3956 Fax: (541) 737-3049 January 29, 2007 1 Corresponding author 1 Factors Affecting Cottonwood Recruitment in Zion National Park Abstract The strength of top-down forces in terrestrial food webs is highly debated as there are few examples illustrating the role of large mammalian carnivores in structuring biotic and abiotic systems. Based on the results of this study we hypothesize that an increase in human visitation within Zion Canyon of Zion National Park ultimately resulted in a catastrophic regime shift through pathways involving trophic cascades and abiotic environmental changes. Increases in human visitors in Zion canyon apparently reduced cougar (Puma concolor) densities, which subsequently led to higher mule deer (Odocoileus hemionus) densities, higher browsing intensities and reduced recruitment of riparian cottonwood trees (Populus fremontii), increased bank erosion, and reductions in both terrestrial and aquatic species abundance. These results may have broad implications with regard to our understanding of alternative ecosystem states where large carnivores have been removed or are being recovered. Key Words: predator, cottonwood, deer, stream, biodiversity, Leopold 2 Introduction Humans can have a major role in food web dynamics by displacing or extirpating top predators. Over a half century ago, the iconoclast Aldo Leopold was among the first to argue that elimination of large mammalian predators had strong top-down influences on ecosystems (Leopold et al., 1947). -
Our Secret Is Now Yours!
EXPLORE... THREE ADVENTUROUS ZONES Travel Guide Travel The Highlands Capitol Reef East Desert Our secret is now yours! Wayne County, - Utah - USA TABLE OF CONTENTS WELCOME Wayne County, Utah - Capitol Reef Country 1- Cover Calendar of Events 2- Table of Contents April to October - Daily Walks / Capitol Reef Welcome to the scenically diverse region encompassing Wayne County YOUR NEXT GREAT 3- Welcome May Utah’s Capitol Reef Country. - Entrada Institute’s Cowboy Poetry and Music DESTINATION 4- Zones Festival This vacation destination includes mountains, forests, pinnacles, arches, 5- Zones July plateaus, and astounding desert - Torrey Apple Days landscapes. The contrast in elevation 6- Attractions - Capitol Reef Classic – Annual High Desert Bike and terrain makes this area a haven Race. for those seeking solitude or - Bicknell International Film Festival (BIFF) 7- Attractions outdoor adventure. August This region is an excellent multi-day 8- Activities - Women’s Redrock Music Festival vacation destination, central to Utah’s - Wayne County Fair scenic attractions, and easily acces- 9- Guides & Outfitters sible from major cities such as Salt September/October Lake City, Denver, and Las Vegas. 10- Maps - Heritage Star Festival - Wayne Wonderland Air show Unpack once and discover a realm 11- Maps that is conveniently situated be- On Going Events: May - September tween Bryce Canyon, the Grand 12- Hotels / Motels Staircase, Goblin Valley State Park, Capitol Reef National Park: Daily walks and nightly Canyonlands National Park, and amphitheatre programs mid May - September. Lake Powell. 13- Cabins / B&B Check at Visitor Center for Ripple Rock Nature Center schedule. Capitol Reef National Park. You’ll want to reserve several days to 14- Campgrounds (435) 425-3791, ext.