Scenic Bywayssouthern Utah’S Best
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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). -
The Geography of Wildfire
Page 14 ZANE GREY EXPLORER AUGUST 2017 The Geography of Wildfire by Dr. Kevin Blake, Professor Emeritus of Geogrophy Kansas State U niversitY STfrR7- The geography of Wildfire ) 6rytz (1917\ is among the most sig- a, C"n.7on -, N nificant in all of Zane Grey's el Ct ,|r F wrld. western romances. lt weaves t/ l-'lors e _ -o1 I l4\. \' L lAeso together four places that 14,. fK.; por.*lls t) ' 'Pl*tequ) shaped Grey's vision of the West more than any oth- !; P /+) t\ er prior to 1917: Lees Ferry (Grey's fictional name is 1^1 Ko"oL Bostil's Ford), the Grand Canyon, Monument Valley, a ;,t u lo is the I and Wild Horse Mesa. Most importantly, this I menf v 3 €-7* book that launched Monument Valley to worldwide t t{ t:: I fame and thus greatly shaped the image of the Fr rd , ril { American West (Blake, 1995; Harvey, 2OLt). o *T"h;s ;: wh"r. , ln this article, I explain the geography of Wildfire by t 7*e flrc-'| s€'-'s /t ljri\'1 0 9, Aoc,umenf following the chronology of the book from Lees Ferry a-f. in a;tlqli*.;.,;"1- (Y _\i ;* iryated to the Grand Canyon, Monument Valley, and finally \ 2( O, 6Lopr oximale i" .65 mlles +o rlne is a story about a wild rP"wcll I I *si - Wild Horse Mesa. Though this I Piaiedu ? rprileqs*. greatest I horse named Wildfire, and is one of Grey's I I Tui.&1} I oo I a horse stories along with Riders of the Purple Soge 4 J 4. -
Bryce Canyon National Park From: Utah Place Names
Bryce Canyon National Park from: Utah Place Names BRYCE CANYON NATIONAL PARK (Garfield County) has a north-northeast by south-southwest orientation and runs parallel to the Sevier River, East Fork. The canyon drainage goes into the Paria River. The spectacularly colorful Pink Cliffs, named by Major Powell's survey party at the center of the National Park, are the east escarpment of the Paunsaugunt Plateau. The Pink Cliffs have been sculptured by water, wind, and gravity into pinnacles, columns, cliffs, castles, and shapes of indescribable form and beauty. The park is not a canyon per se, but the edge of a plateau which can be enjoyed from above or from the depths below. The park was established in 1928 by President Hoover. See Bryce Canyon below for name source. BRYCE CANYON (Garfield County) originates in the center of Bryce Canyon National Park and continues east to the Paria River. It was named for Ebenezer Bryce, a pioneer cattleman who homesteaded there in the fall of 1875. Bibliography: Our Pioneer Heritage, 17 vols. Daughters of the Utah Pioneers. (v17). Creer, Leland Hargrave. The Founding of an Empire: The Exploration and Colonization of Utah, 1776 -1856. Salt Lake City: Bookcraft, 1947. Layton, Stanford J. "Fort Rawlins, Utah: A Question of Mission and Means." Utah Historical Quarterly 42 (Winter 1974): 68-83. Utah, A Guide to the State. Work Projects Administration. Comp. by Utah State Institute of Fine Arts, Salt Lake County Commission. New York: Hastings House, 1941. Woodbury, Angus Munn. A History of Southern Utah and Its National Parks. Salt Lake City: State Historical Society, 1950. -
Report Development
(This page intentionally left blank) Table of Contents Table of Figures ........................................................................ v Table of Tables ....................................................................... vii Executive Summary ................................................................. 1 Introduction .............................................................................. 2 Region 4 VCMQ Objectives .................................................................... 2 Intended Uses ............................................................................................ 3 Business Needs Requirements ............................................................ 3 General Characteristics of the Area ................................................... 4 Partnerships .............................................................................................. 6 Final Products ........................................................................................... 7 Methods ...................................................................................... 8 Project Planning .................................................................................... 10 Vegetation Classification Development ......................................... 10 Vegetation Type Map Units .............................................................................. 11 Structural Characteristics................................................................................. 11 Tree Size Class ......................................................................................................................... -
Brian Head Peak, Iron County
Brian Head Peak, Iron County Robert F. Biek1 and Peter D. Rowley2 1Utah Geological Survey, P.O. Box 146100, Salt Lake City, UT 84114-6100, [email protected] 2Geologic Mapping Inc., P.O. Box 651, New Harmony, UT 84757 Utah Geosites 2019 Utah Geological Association Publication 48 M. Milligan, R.F. Biek, P. Inkenbrandt, and P. Nielsen, editors Cover Image: Th e type section of the Brian Head Formation (Tbh) is on the ridge just right of center (by the Tbh label). Brian Head peak is capped by the Leach Canyon Formation (Tql), which overlies the Isom Formation (Ti). A modern landslide (Qms) is west and south of the peak. M. Milligan, R.F. Biek, P. Inkenbrandt, and P. Nielsen, editors 2019 Utah Geological Association Publication 48 Presidents Message I have had the pleasure of working with many diff erent geologists from all around the world. As I have traveled around Utah for work and pleasure, many times I have observed vehicles parked alongside the road with many people climbing around an outcrop or walking up a trail in a canyon. Whether these people are from Utah or from another state or country, they all are quick to mention to me how wonderful our geology is here in Utah. Utah Geosites 2019 Utah is at the junction of several diff erent geological provinces. We have the Basin and Range to the west and the Central Utah Utah Geological Association Publication 48 Hingeline and Th rust Belt down the middle. Th e Uinta Mountains M. Milligan, R.F. Biek, P. Inkenbrandt, and P. -
Geologic Resource Evaluation Report, Bryce Canyon National Park
National Park Service U.S. Department of the Interior Natural Resource Program Center Bryce Canyon National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2005/002 Bryce Canyon National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2005/002 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2005 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly-published newsletters. Views and conclusions in this report are those of the authors and do not necessarily reflect policies of the National Park Service. Mention of trade names or commercial products does not constitute endorsement or recommendation for use by the National Park Service. -
1992 Utah Fishing Proclamation
m ftroiG wm "t let erkLte^ "IHferae you won't let go ®fl Wfo(B ttrout! The largest fish ever taken on a rod and reel, a 3,427 pound great white shark, was caught on Berkley Trilene — America's best selling fishing Rtf*rlrlctir line! SPORTSCASTLE SANDY PRICE 5600 S. 9th E., Murray 838 E. 9400 S. 730 W. Prive River Rd. 263-3633 571-8812 637-2077 ZCMICENTER CEDAR CITY SUGARHOUSE 2nd Level ZCMI Center 606 S. Main 1171 East 2100 So.. 359-4540 586-0687 487-7726 VERNAL OGDEN CITY MALL ROY 872 W. Main 24th & Washington 5585 So. 1900 W. 789-0536 399-2310 776-4453 FAMILY CENTER PROVO/UNIV. MALL ROCK SPRINGS 5666 S. Redwood Rd. 1300 S. State 1371 Dewar Drive SPORTING GOODS COMPANY 967-9455 224-9115 307-362-4208 ON THE COVER "Snagged"by Luke Frazier, oil, 16"x CONTENTS 20". J99I, To learn more about Frazier and his art work, turn to page 60, INTRODUCTION Strawberry Recreation Area Loyal Clark, US Forest Service 35 One of the most exciting Director's Message Scofield Reservoir/What the Timothy H. Provan, Director Future Holds Kevin Christophereon, things about fishing is its Division of Wildlife Resources 2 unpredictability, You simply Southeast Region Fisheries Manager 37 Utah's 1992 Fishing Season don't kno w when that big Why Rainbow Trout? Bruce Schmidt, Fisheries Chief 3 Joe Valentine, Assistant Fisheries one is going to strike, it Chief (Culture) ........39 could be on your next cast! 1992 FISHING RULES Willard Bay Shad 1992 Fishing Rules: Purpose Thomas D.