Geologic Map of the Fruita Quadrangle, Wayne County, Utah
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Capitol Reef National Park Geologic Resources Inventory Scoping
Geologic Resources Inventory Workshop Summary Capitol Reef National Park September 27-28, 1999 National Park Service Geologic Resources Division and Natural Resources Information Division Version: Draft of November 5, 1999 EXECUTIVE SUMMARY An inventory workshop was held at Capitol Reef NP on September 27-28, 1999 to view and discuss the park’s geologic resources, to address the status of geologic mapping by both the Utah Geological Survey (UGS) and the United States Geological Survey (USGS) for compiling both paper and digital maps, and to assess resource management issues and needs. Cooperators from the NPS Geologic Resources Division (GRD), Natural Resources Information Division (NRID), Capitol Reef NP, UGS, USGS, and Brigham Young University (BYU) were present for the two-day workshop. (See Appendix A, Capitol Reef NP Geological Resources Inventory Workshop Participants, September 27-28, 1999) Z:\Scoping\scoping_summaries\CARE_scoping_summary_19991105.doc Last printed 11/28/2006 12:16:00 PM Page 1 of 18 Capitol Reef NP GRI Workshop Summary: September 27-28, 1999 (cont'd) Day one involved a field trip throughout the northern extent of Capitol Reef NP co-led by USGS geologists Pete Peterson and George Billingsley. Highlights of the field trip can be found at http://www.nature.nps.gov/grd/geology/gri/ut/care/field_trip_care Day two involved a scoping session to present overviews of the NPS Inventory and Monitoring (I&M) program, the Geologic Resources Division, and the ongoing Geologic Resources Inventory (GRI) for Colorado and Utah. Round table discussions involving geologic issues for Capitol Reef NP included interpretation, soils mapping, paleontologic resources, the UGA Millennium 2000 guidebook featuring the geology of Utah's National and State parks, the status of cooperative geologic mapping efforts, sources of available data, geologic hazards, potential future research topics, and action items generated from this meeting. -
Cathedral Valley Loop @
Cathedral Valley Loop @ www.ontdek-amerika.nl Last Update : Januari 27, 2007 Cathedral Valley Loop INLEIDING Cathedral Valley ligt in het uiterste noorden van Capitol Reef National Park, en is alleen via onverharde wegen bereikbaar. Een van de meest opvallende kenmerken is de aanwezigheid van veel schitterende monolieten, dat zijn apart staande rotsen die hoog boven de omgeving uitsteken. Het woord monoliet is afgeleid van de Griekse woorden ‘monos’ (alleen) en ‘lithos’ (gesteente). Je kan het zeer eenzame gebied – er komen hier maar héél weinig bezoekers – bereiken via de Hartnet Road en de Caineville Wash Road, die samen een 58 mijl lange lus vormen. Via diverse korte zijwegen kan je naar een aantal punten rijden die een panoramisch uitzicht bieden over de weidse omgeving. De route valt deels binnen de parkgrenzen; het deel dat niet tot het park behoort wordt beheerd door het Bureau of Landmanagement. De beste jaargetijden om de Cathedral Valley Loop te rijden zijn de lente en de herfst. Tijdens de winter is de weg vaak te slecht, en tijdens de zomer kan het ondraaglijk heet worden. TOESTAND VAN DE WEG In principe is de weg het hele jaar door open. Vierwielaandrijving is meestal niet nodig, maar een hoge bodemvrijheid (high clearance) is wel absoluut noodzakelijk. Bij goede weersomstandigheden is de weg goed berijdbaar, maar bij slecht weer kan de toestand van de weg drastisch veranderen. Regen en sneeuw kunnen delen van de route onbegaanbaar maken. Informeer daarom altijd vooraf bij het Visitor Center in Capitol Reef National Park naar de conditie van de weg én naar de weersvoorspelling. -
West Colorado River Plan
Section 9 - West Colorado River Basin Water Planning and Development 9.1 Introduction 9-1 9.2 Background 9-1 9.3 Water Resources Problems 9-7 9.4 Water Resources Demands and Needs 9-7 9.5 Water Development and Management Alternatives 9-13 9.6 Projected Water Depletions 9-18 9.7 Policy Issues and Recommendations 9-19 Figures 9-1 Price-San Rafael Salinity Control Project Map 9-6 9-2 Wilderness Lands 9-11 9-3 Potential Reservoir Sites 9-16 9-4 Gunnison Butte Mutual Irrigation Project 9-20 9-5 Bryce Valley 9-22 Tables 9-1 Board of Water Resources Development Projects 9-3 9-2 Salinity Control Project Approved Costs 9-7 9-3 Wilderness Lands 9-8 9-4 Current and Projected Culinary Water Use 9-12 9-5 Current and Projected Secondary Water Use 9-12 9-6 Current and Projected Agricultural Water Use 9-13 9-7 Summary of Current and Projected Water Demands 9-14 9-8 Historical Reservoir Site Investigations 9-17 Section 9 West Colorado River Basin - Utah State Water Plan Water Planning and Development 9.1 Introduction The coordination and cooperation of all This section describes the major existing water development projects and proposed water planning water-related government agencies, and development activities in the West Colorado local organizations and individual River Basin. The existing water supplies are vital to water users will be required as the the existence of the local communities while also basin tries to meet its future water providing aesthetic and environmental values. -
English Information
National Park Service U.S. Department of the Interior Capitol Reef National Park … the light seems to flow or shine out of the rock rather than to be reflected English from it. – Clarence Dutton, geologist and early explorer of Capitol Reef, 1880s A Wrinkle in the Earth A vibrant palette of color spills across the landscape before bridges, and twisting canyons. Over millions of years geologic forces you. The hues are constantly changing, altered by the play shaped, lifted, and folded the earth, creating this rugged, remote area of light against the towering cliffs, massive domes, arches, known as the Waterpocket Fold. Panorama Point at Sunset Erosion creates waterpockets and potholes that collect The Castle is made of fractured Wingate Sandstone perched upon grey Chinle and red Moenkopi Formations. rainwater and snowmelt, enhancing a rich ecosystem. From the east, the Waterpocket Fold appears as a formidable barrier Capitol Dome reminded early travelers of the US Capitol to travel, much like a barrier reef in an ocean. building and later inspired the name of the park. Creating the Waterpocket Fold Capitol Reef’s defining geologic feature is a wrinkle in Uplift: Between 50 and 70 million years ago, an ancient fault was Earth’s crust, extending nearly 100 miles from Thousand reactivated during a time of tectonic activity, lifting the layers to the Lake Mountain to Lake Powell. It was created over time by west of the fault over 7,000 feet higher than those to the east. Rather three gradual, yet powerful processes—deposition, uplift, than cracking, the rock layers folded over the fault line. -
Geology and Stratigraphy Column
Capitol Reef National Park National Park Service U.S. Department of the Interior Geology “Geology knows no such word as forever.” —Wallace Stegner Capitol Reef National Park’s geologic story reveals a nearly complete set of Mesozoic-era sedimentary layers. For 200 million years, rock layers formed at or near sea level. About 75-35 million years ago tectonic forces uplifted them, forming the Waterpocket Fold. Forces of erosion have been sculpting this spectacular landscape ever since. Deposition If you could travel in time and visit Capitol Visiting Capitol Reef 180 million years ago, Reef 245 million years ago, you would not when the Navajo Sandstone was deposited, recognize the landscape. Imagine a coastal you would have been surrounded by a giant park, with beaches and tidal flats; the water sand sea, the largest in Earth’s history. In this moves in and out gently, shaping ripple marks hot, dry climate, wind blew over sand dunes, in the wet sand. This is the environment creating large, sweeping crossbeds now in which the sediments of the Moenkopi preserved in the sandstone of Capitol Dome Formation were deposited. and Fern’s Nipple. Now jump ahead 20 million years, to 225 All the sedimentary rock layers were laid million years ago. The tidal flats are gone and down at or near sea level. Younger layers were the climate supports a tropical jungle, filled deposited on top of older layers. The Moenkopi with swamps, primitive trees, and giant ferns. is the oldest layer visible from the visitor center, The water is stagnant and a humid breeze with the younger Chinle Formation above it. -
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. -
2014-2015 Annual Report Director Site Manager Administrative Support Michael T
2014-2015 Annual Report Director Site Manager Administrative Support Michael T. Stevens, Ph.D. Jason Kudulis (July-February) Annette Harrington Associate Professor of Biology Site Manager Custodial & Associate Director Gina Gilson (May-Present) Maintenance Support Keith White Lesa Dean Associate Professor of Assistant Site Manager Developmental Mathematics Darrell Mensel CRFS Staff CRFS Advisory Board Maria Blevins, Ph.D. Travis Lovell Linda Shelton Assistant Professor Assistant Professor of Instructor of of Communication Art & Visual Communication English & Literature Danny Horns, Ph.D. T. Heath Ogden, Ph.D. Paul Weber, Ph.D. Associate Dean, Assistant Professor Assistant Professor of Physics College of Science & Health of Biology Advisory Board Members are Betsy Lindley, Ph.D. Mary Sowder, Ph.D. Utah Valley University (UVU) faculty Associate Professor of Exercise Associate Professor and staff who serve for ~3 years on Science & Outdoor Recreation of Education a rotating schedule. 2 crfs 2014-2015 annual report Four hundred fifty undergraduates visited Capitol Reef Field Station (CRFS) this year in our busiest year ever. To put this number into context, this rate of visitation places us in the top 15% of field stations nationwide.1 The majority of students who visit CRFS are from UVU. Because of our dual mission, UVU is in the uncommon position of having the field station resources of a comprehensive university while serving a high proportion of community-college-going students CRFS who are often underrepresented at field stations.1 Further, CRFS is one of less than ten field stations run by a university Staff and located in a national park. It’s exciting to be part of such a unique, vibrant, and growing enterprise. -
Episodic Sediment Delivery and Landscape Connectivity in the Mancos Shale Badlands and Fremont River System, Utah, USA
Geomorphology 102 (2008) 242–251 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Episodic sediment delivery and landscape connectivity in the Mancos Shale badlands and Fremont River system, Utah, USA Andrew E. Godfrey 1, Benjamin L. Everitt a, José F. Martín Duque b,⁎ a 170 W. 300 North, Ivins, Utah 84738, USA b Department of Geodynamics, Complutense University, 28040 Madrid, Spain ARTICLE INFO ABSTRACT Article history: The Fremont River drains about 1000 km2 of Mancos Shale badlands, which provide a large percentage of the Accepted 23 May 2007 total sediment load of its middle and lower reaches. Factors controlling sediment movement include: Available online 18 May 2008 weathering that produces thin paralithic soils, mass movement events that move the soil onto locations susceptible to fluvial transport, intense precipitation events that move the sediment along rills and across Keywords: local pediments, and finally Fremont River floods that move the sediment to the main-stem Colorado River. Mancos Shale badlands A forty-year erosion-pin study has shown that down-slope creep moves the weathered shale crust an Erosion Mass movement average of 5.9 cm/yr. Weather records and our monitoring show that wet winters add large slab failures and Connectivity mudflows. Recent sediment-trap studies show that about 95% of sediment movement across pediments is Coupling accomplished by high-intensity summer convective storms. Between 1890 and 1910, a series of large autumn Arroyo cutting floods swept down the Fremont River, eroding its floodplain and transforming it from a narrow and meandering channel to a broad, braided one. -
Geologic Resource Evaluation Report, Capitol Reef National Park
National Park Service U.S. Department of the Interior Natural Resource Program Center Capitol Reef National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2006/005 Capitol Reef National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2006/005 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2006 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. -
Fremont River Watershed Water Quality Management Plan
FFrreemmoonntt RRiivveerr WWaatteerrsshheedd Water Quality Management Plan September 27, 2002 Includes TMDLs for: Johnson Valley Reservoir Forsyth Reservoir Mill Meadow Reservoir UM Creek Upper Fremont River Lower Fremont River i FREMONT RIVER WATERSHED WATER QUALITY MANAGEMENT PLAN TABLE OF CONTENTS 1.0 INTRODUCTION .................................................................................................... 1 1.1 The TMDL Process ........................................................................................ 1 1.2 Utah’s Watershed Approach .......................................................................... 3 2.0 WATERSHED DESCRIPTION ............................................................................... 5 2.1 Historic Perspective ....................................................................................... 5 2.2 Climate........................................................................................................... 6 2.3 Geology / Soils............................................................................................... 8 2.4 Land Use / Land Cover ................................................................................ 11 2.5 Hydrology..................................................................................................... 12 2.5.1 Reservoirs ....................................................................................... 12 2.5.2 Subbasins ....................................................................................... 18 2.5.3 Irrigation -
Bowns Point - Boulder Mountain
BOWNS POINT - BOULDER MOUNTAIN Rating: Easy/Moderate Hike Length: 2-3 hours (2.5 miles) Gear: Standard Hiking Gear Maps: LOWER BOWNS RESERVOIR, UT Water: None Season: Late Spring through Fall Waypoints: Trailhead 12S 470070mE 4211917mN N38° 03' 16" W111° 20' 28" Gate 12S 469912mE 4211754mN N38° 03' 11" W111° 20' 35" Gate 2 12S 468674mE 4211605mN N38° 03' 06" W111° 21' 25" Viewpoint 12S 468654mE 4211579mN N38° 03' 05" W111° 21' 26" Hype For the desert aficionado, or enthusiastic leaf peeper, Bowns Point is a must do hike. The point, on the eastern edge of Boulder Mountain, has panoramic views of Capitol Reef National Park, the Henry Mountains, Grand Staircase Escalante National Monument, and the Kaiparowits Plateau. Time your visit for the fall, when the leaves are changing, and you will be rewarded with some of the best colors in Utah. The point was named after the Bowns family. The Bowns family originally ran cattle in Wayne County but was one of the early families to change to sheep. They developed the Sandy Ranch at Notom and ran an estimated 2500-3000 sheep a year in the county. Bowns Reservoir is another reminder of the family name, and the impact they had on the county. I am not sure if they build the original trail to the point, but my hat is off to whoever did. The trail steep, rocky, and would require an enormous amount of work to build. Tags: hike, fall colors, intermediate, access: 4x4 Trailhead Note: Reaching the trailhead requires a 4-wheel drive high clearance vehicle. -
Vascular Flora and Vegetation of Capitol Reef National Park, Utah
Vascular Flora and Vegetation of Capitol Reef National Park, Utah Kenneth D. Heil, J. Mark Porter, Rich Fleming, and William H. Romme Technical Report NPS/NAUCARE/NRTR-93/01 National Park Service Cooperative Park Studies Unit U.S. Department of the Interior at Northern Arizona University National Park Service Cooperative Park Studies Unit Northern Arizona University The National Park Service (NPS) Cooperative Park Studies Unit (CPSU) at Northern Arizona University (NAU) is unique in that it was conceptualized for operation on an ecosystem basis, rather than being restrained by state or NPS boundaries. The CPSU was established to provide research for the 33 NPS units located within the Colorado Plateau, an ecosystem that shares similar resources and their associated management problems. Utilizing the university's physical resources and faculty expertise, the CPSU facilitates multidisciplinary research in NPS units on the Colorado Plateau, which encompasses four states and three NPS regions—Rocky Mountain, Southwest, and Western. The CPSU provides scientific and technical guidance for effective management of natural and cultural resources within those NPS units. The National Park Service disseminates the results of biological, physical, and social science research through the Colorado Plateau Technical Report Series. Natural resources inventories and monitoring activities, scientific literature reviews, bibliographies, and proceedings of techni cal workshops and conferences are also disseminated through this series. Unit Staff Charles van Riper, III, Unit Leader Peter G. Rowlands, Research Scientist Henry E. McCutchen, Research Scientist Mark K. Sogge, Ecologist Charles Drost, Zoologist Elena T. Deshler, Biological Technician Paul R. Deshler, Technical Information Specialist Connie C. Cole, Editor Margaret Rasmussen, Administrative Clerk Jennifer Henderson, Secretary National Park Service Review Documents in this series contain information of a preliminary nature and are prepared primarily for internal use within the National Park Service.