Sevier River Basin
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UMNP Mountains Manual 2017
Mountain Adventures Manual utahmasternaturalist.org June 2017 UMN/Manual/2017-03pr Welcome to Utah Master Naturalist! Utah Master Naturalist was developed to help you initiate or continue your own personal journey to increase your understanding of, and appreciation for, Utah’s amazing natural world. We will explore and learn aBout the major ecosystems of Utah, the plant and animal communities that depend upon those systems, and our role in shaping our past, in determining our future, and as stewards of the land. Utah Master Naturalist is a certification program developed By Utah State University Extension with the partnership of more than 25 other organizations in Utah. The mission of Utah Master Naturalist is to develop well-informed volunteers and professionals who provide education, outreach, and service promoting stewardship of natural resources within their communities. Our goal, then, is to assist you in assisting others to develop a greater appreciation and respect for Utah’s Beautiful natural world. “When we see the land as a community to which we belong, we may begin to use it with love and respect.” - Aldo Leopold Participating in a Utah Master Naturalist course provides each of us opportunities to learn not only from the instructors and guest speaKers, But also from each other. We each arrive at a Utah Master Naturalist course with our own rich collection of knowledge and experiences, and we have a unique opportunity to share that Knowledge with each other. This helps us learn and grow not just as individuals, but together as a group with the understanding that there is always more to learn, and more to share. -
Beaver City Limits (Approximately)
NPS Form 10-900 (7-81) United States Department off the Interior National Park Service National Register of Historic Places 1982 Inventory Nomination Form See instructions in How to Complete National Register Forms Type all entries complete applicable sections___ ______ 1. Name historic -H4**ertcHtesuure«~-&f Be a ve r tPa pti a4 Archtteetu ra I Properties) and/or common_______________ ' 2. Location street & number Beaver City Limits (Approximately). vicinity of state code 049 county Beaver code 0-1 3. Classification Category Ownership Status Present Use _ district public X occupied X. agriculture museum building(s) private X unoccupied X commercial X park structure x both X work in progress X educational X private residence site Public Acquisition Accessible entertainment X religious obiect in process X yes: restricted X government scientific v fflU I tip 1 e M/ .being considered X yes: unrestricted industrial transportation ~v resource fn no military _J£_ other: multiple 4. Owner of Property name Multiple ownership street & number city, town vicinity of state 5. Location of Legal Description courthouse, registry of deeds, etc. Beayer County Couthouse street & number Center Street a,nd First Ea,st city, town state Utah 6. Representation in Existing Surveys title Utah Historical Sites Survey has this property been determined eligible? __ yes x date 1977-80 federal ^c_state __county __local depository for survey records Utah State Historical Society city, town Salt Lake City state Utah Condition Check one Check one y excellent X deteriorated __ unaltered X original site X altered __ moved date Describe the present and original (if known) physical appearance Beaver City is located in southwestern Utah on the high, Great Basin desert at the foot of the lofty Tushar Mountains that rise over 12,000 feet in elevation. -
Water Resources Development by the U.S. Army Corps of Engineers in Utah
DEVELOPMENT W&M U.S. ARMY CORPS OF ENGINEERS TC SOU TH PACIFIC DIVI SI O N 423 • A15 1977 Utah 1977 M ■ - z//>A ;^7 /WATER RESOURCES DEVELOPMENT ec by THE U.S. ARMY CORPS OF ENGINEERS in UTAH JANUARY 1977 ADDRESS INQUIRIES TO DIVISION ENGINEER U.S. Army Engineer Division South Pacific Corps of Engineers 630 Sansome Street San Fransisco, California 94111 DISTRICT ENGINEER DISTRICT ENGINEER U.S. Army Engineer District U.S. Army Engineer District Los Angeles Corps of Engineers Sacramento Federal Building Corps of Engineers 300 North Los Angeles Street Federal and Courts Building Los Angeles, California 90012 (P.O. Box 2711 650 Capitol Mall Los Angeles, California 90053) Sacramento, California 95814 TO OUR READERS: Throughout history, water has played a dominant role in shaping the destinies of nations and entire civilizations. The early settlement and development of our country occurred along our coasts and water courses. The management of our land and water resources was the catalyst which enabled us to progress from a basically rural and agrarian economy to the urban and industrialized nation we are today. Since the General Survey Act of 1824, the US Army Corps of Engineers has played a vital role in the development and management of our national water resources. At the direction of Presidents and with Congressional authorization and funding, the Corps of Engineers has planned and executed major national programs for navigation, flood control, water supply, hydroelectric power, recreation and water conservation which have been responsive to the changing needs and demands of the American people for 152 years. -
Sensitive Plant Species
SENSITIVE PLANT SPECIES Barneby Woody Aster (Aster kingii var. barnebyana) Barneby’s woody aster is a member of the sunflower family (Asteraceae) and it grows from a well-developed taproot. There are persistent blackish or dark brown, old leaf bases at the base of the plant. The stems are short (3-12 cm long) and the herbage is covered with glandular hairs. The leaves are basal, 0.8-12 cm long, and oblanceolate to spatulate in shape with 1-10 pronounced teeth. Flowers occur in clusters of 1-5, standing 8-11 mm high. The inner bracts are often purplish and at least the outer tips are bent backward. The ray flowers are white, often fading to pale pink. This plant flowers between August and September. This species is found in mountain mahogany and oak communities on rock outcrops composed of Precambian quartzite. This endemic species of the Canyon Mountains in Millard and Juab Counties, Utah has been reported in 15 element occurrence records as of 2002 (Madsen 2002). These scattered occurrences indicate a total population of 600+ plants. The range of elevation is between 7,500 and 9640. Major associated species are Holodiscus dumosus (Mountain spray), Huechera rubescens (Red alumroot), Symphoricarpos oreophilus (Mountain snowberry), Quercus gambelii (Gambel’s oak), and Eriogonum brevicaule (Shortstem buckwheat) (Franklin 1990). To date there are 15 known occurrences of this species on the Fillmore Ranger District of the Fishlake National Forest (Franklin 1990). Plants are harbored from threats such as livestock grazing by their occurrence on steep rock outcrops. 40 Bicknell milkvetch (Astragalus consobrinus) The Bicknell milkvetch is a member of the pea family (Fabaceae). -
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. -
Beaver County, Utah Resource Management Plan
BEAVER COUNTY, UTAH RESOURCE MANAGEMENT PLAN Beaver County Commissioners Michael F. Dalton, Chair Mark S. Whitney Tammy Pearson Planning & Zoning Commission Darrel Davis, Chairman Kyle Blackner, Administrator Von Christiansen, Attorney Jamie Kelsey, Secretary Steve Kinross Mike Riley Walter Schofield Kolby Blackner Drew Coombs Don Noyes Public Lands Keven Whicker, Public Lands Administrator County Staff Scott Albrecht, Michelle Evans, Tracy McMullin, Heidi Eyre Adopted June 6, 2017 (ordinance 2017-03) Amended December 17, 2019 (ordinance 2019-06) i TABLE OF CONTENTS INTRODUCTION .......................................................................................................................... v LEGAL BASIS FOR COUNTY RESOURCE MANAGEMENT PLANNING .......................... ix SOCIAL-ECONOMIC LINKAGES ............................................................................................. xi CURRENT RESOURCE MANAGEMENT SETTING .............................................................. xv DESIRED RESOURCE MANAGEMENT SETTING .............................................................. xvii 1. LAND USE ............................................................................................................................. 1 2. ENERGY, MINING, MINERAL & GEOLOGICAL RESOURCES .................................... 9 2.1 Mining and Mineral & Geological Resources .................................................................. 9 2.2 Energy Resources ........................................................................................................... -
Triangulation in Utah 1871-1934
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 913 TRIANGULATION IN UTAH 1871-1934 J. G. STAACK Chief Topographic Engineer UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1940 Tor sale by the Superintendent of Documents, Washington, D. C. Price 20 cents (paper) CONTENTS Page Introduction ______________________________________________________ 1 Scope of report------__-_-_---_----_------------ --__---__ _ 1 Precision __ _ ________________________ _ __________________ _ ___ 1 Instruments used._ _ _ _ _ _ _ _ _ 2 Station marks___- _ _.__ __ __ _ 2 Datum_-_-_-__ __________________________ ______ ______-___.__ 3 Methods of readjustment..._____.-.__..________.___._._...___.__ 4 Form of results__-.________________________ _.___-_____.______ 5 Arrangement__.______________________________ _ ___ _ ________ 6 Descriptions of stations._______________________________________ 6 Azimuths and distances.__ ____-_.._---_--_________ -____ __ __ ^ 7 Maps.__----__-----_-_---__-_--_-___-_-___-__-__-_-_-___.-.__ 7 Personnel_ _ __-----_-_-_---_---------_--__-____-__-_.--_.___ . 7 Projects 9 Uinta Forest Reserve, 1897-98_ 9 Cottonwood and Park City special quadrangles, 1903____ _ 19 Iron Springs special quadrangle, 1905____________________________ 22 Northeastern Utah, 1909.. -_. 26 Eastern Utah, 1910 - . 30 Logan quadrangle, 1913._________-__-__'_--______-___:_____.____ 42 Uintah County, 1913___-__. 48 Eastern Utah, 1914.. ... _ _ .. 55 Northern Utah, 1915 (Hodgeson)_____-___ __-___-_-_-__-_--. _. 58 Northern Utah, 1915 <Urquhart)_. -
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).