Canyons of the Escalante Information and Hiking Guide
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PRELUDE to SEVEN SLOTS: FILLING and SUBSEQUENT MODIFICATION of SEVEN BROAD CANYONS in the NAVAJO SANDSTONE, SOUTH-CENTRAL UTAH by David B
PRELUDE TO SEVEN SLOTS: FILLING AND SUBSEQUENT MODIFICATION OF SEVEN BROAD CANYONS IN THE NAVAJO SANDSTONE, SOUTH-CENTRAL UTAH by David B. Loope1, Ronald J. Goble1, and Joel P. L. Johnson2 ABSTRACT Within a four square kilometer portion of Grand Staircase-Escalante National Monument, seven distinct slot canyons cut the Jurassic Navajo Sandstone. Four of the slots developed along separate reaches of a trunk stream (Dry Fork of Coyote Gulch), and three (including canyons locally known as “Peekaboo” and “Spooky”) are at the distal ends of south-flowing tributary drainages. All these slot canyons are examples of epigenetic gorges—bedrock channel reaches shifted laterally from previous reach locations. The previous channels became filled with alluvium, allowing active channels to shift laterally in places and to subsequently re-incise through bedrock elsewhere. New evidence, based on optically stimulated luminescence (OSL) ages, indicates that this thick alluvium started to fill broad, pre-existing, bedrock canyons before 55,000 years ago, and that filling continued until at least 48,000 years ago. Streams start to fill their channels when sediment supply increases relative to stream power. The following conditions favored alluviation in the study area: (1) a cooler, wetter climate increased the rate of mass wasting along the Straight Cliffs (the headwaters of Dry Fork) and the rate of weathering of the broad outcrops of Navajo and Entrada Sandstone; (2) windier conditions increased the amount of eolian sand transport, perhaps destabilizing dunes and moving their stored sediment into stream channels; and (3) southward migration of the jet stream dimin- ished the frequency and severity of convective storms. -
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 ............................................................................................... -
Relation of Sediment Load and Flood-Plain Formation to Climatic Variability, Paria River Drainage Basin, Utah and Arizona
Relation of sediment load and flood-plain formation to climatic variability, Paria River drainage basin, Utah and Arizona JULIA B. GRAF U.S. Geological Survey, Water Resources Division, 375 S. Euclid, Tucson, Arizona 85719 ROBERT H. WEBB U.S. Geological Survey, 1675 W. Anklam Road, Tucson, Arizona 85745 RICHARD HEREFORD U.S. Geological Survey, Geologic Division, 2255 North Gemini Drive, Flagstaff, Arizona 86001 ABSTRACT sediment load for a given discharge declined fill that rises 1-5 m above the modern channel abruptly in the early 1940s in the Colorado bed. Flood-plain deposits are present in all Suspended-sediment load, flow volume, River at Grand Canyon (Daines, 1949; Howard, major tributaries of the Paria River. The area of and flood characteristics of the Paria River 1960; Thomas and others, 1960; Hereford, flood plains is slightly greater than 20 km2, and were analyzed to determine their relation to 1987a). The decline in suspended-sediment sediment volume is estimated to be about 40 climate and flood-plain alluviation between loads has been attributed to improved land use million m3 (Hereford, 1987c). Typically, flood 1923 and 1986. Flood-plain alluviation began and conservation measures initiated in the 1930s plains are not present in first-order drainage ba- about 1940 at a time of decreasing magnitude (Hadley, 1977). A change in sediment-sampler sins but are present in basins of second and and frequency of floods in winter, summer, type and in methods of analysis have been higher order where the stream channel is uncon- and fall. No floods with stages high enough to discounted as causes for the observed decrease fined and crosses nonresistant bedrock forma- inundate the flood plain have occurred since (Daines, 1949; Thomas and others, 1960). -
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. -
Map Showing Location of Selected Surface-Water Sites and Springs, Escalante River Drainage Basin, Garfield and Kane Counties, Utah By
U.S. DEPARTMENT OF THE INTERIOR PREPARED IN COOPERATION WITH THE SCIENTIFIC INVESTIGATIONS REPORT 2004–5223 U.S. GEOLOGICAL SURVEY U.S. DEPARTMENT OF THE INTERIOR, BUREAU OF LAND MANAGEMENT, GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT Location of selected surface-water sites and springs, Escalante River drainage basin—Plate 1 Wilberg, D.E., and Stolp, B.J., 2004, Seepage Investigation and Selected Hydrologic Data for the Escalante River Drainage Basin, Garfield and Kane Counties, Utah, 1909-2002 111°45' 111°05' 114 ° 113 ° 112 ° 111° 42 ° T. 30 S. T. 31 S. Great 15 Salt 110 ° 109 ° B 41 ° Lake ou Salt Lake City lde r M Provo ou 40 ° nt ain 39 ° Utah Study 38 ° area Garfield County Kane County 37 ° E a s t F o T. 31 S. r k T. 32 S. 21 East Fork Boulder Creek near Boulder EXPLANATION B o u Boundary of study area l d u e s Platea r Aquariu C r Boundary of Grand Staircase-Escalante National Monument e e k Road k e e r C C ir Stream c r e le e C D l 16 38°00' if Surface-water site and number k fs or 22 East Fork Deer Creek near Boulder t F 38°00' as Spring E +35 Mile marker—Labeled every 5 miles T. 32 S. T. 33 S. 12 Dixie National Forest s il n a i Tr a t n p u o Boulder rr o T u B M n i f f i D r e e T. 33 S. -
5. Location of Legal Description
FHR-8-300 (11-78) United States Department of the Interior Heritage Conservation and Recreation Service National Register of Historic Places Inventory Nomination Form See instructions in How to Complete National Register Forms Type all entries complete applicable sections_____________. 1. Name historic Ensign-Smith House and/or common Silas Smith House 2. Location street & number 96 Main not for publication city, town Paragonah vicinity of state Utah code 049 county Iron code 021 3. Classification Category Ownership States Present Use _ ^district _kloccupied agriculture museum _ _ building(s) _i^lprivate unoccupied commercial park structure both work in progress educational Lf^private residence site Public Acquisition Accessible entertainment religious object in process V yes: restricted government scientific _ L being considered yes: unrestricted industrial transportation n no military other: 4. Owner of Property name R. J. Reynolds street & number Box 384 city, town Palm Springs vicinity of state CA 92263 5. Location of Legal Description courthouse, registry of deeds, etc. Iron County Courthouse street & number city, town Parowan state Utah 6. Representation in Existing Surveys Utah Historic Sites Survey/ title Iron County Survey______ has this property been determined elegible? yes no date SP rin 9 1981 federal X state county local depository for survey records Utah State Historical Society city, town Lake Ci state Utah 7. Description Condition Check one Check one excellent ^,__ deteriorated .. unaltered X original site _A_ goodC* » -- l<-_ ruins ^ altered __ moved date __ fair __ unexposed Describe the present and original (if known) physical appearance The En sign -Smith house in Paragonah is a long (the front section measures about 50' x 17') 1-1/2 story adobe house. -
Water Quality Monitoring for the Escalante River and Coyote Gulch in Glen Canyon National Recreation Area 2014 Summary Report
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Water Quality Monitoring for the Escalante River and Coyote Gulch in Glen Canyon National Recreation Area 2014 Summary Report Natural Resource Data Series NPS/SCPN/NRDS—2017/1134 ON THE COVER Water quality monitoring site ESC02 on the Escalante River in Glen Canyon National Recreation Area. Photography by SCPN Water Quality Monitoring for the Escalante River and Coyote Gulch in Glen Canyon National Recreation Area 2014 Summary Report Natural Resource Data Series NPS/SCPN/NRDS—2017/1134 Melissa Dyer Stephen A. Monroe Stacy E. Stumpf National Park Service Southern Colorado Plateau Network 525 S. Beaver, Building 20 PO Box 5663 Flagstaff, AZ, 86011-5663 December 2017 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conserva- tion and environmental constituencies, and the public. The Natural Resource Data Series is intended for the timely release of basic data sets and data summaries. Care has been taken to assure accuracy of raw data values, but a thorough analysis and interpretation of the data has not been completed. Consequently, the initial analyses of data in this report are provisional and subject to change. Please direct any data requests to the water resources project manager or the SCPN data manager. -
Aquatic Ecosystems and Invertebrates of the Grand Staircase-Escalante National Monument Cooperative Agreement Number JSA990024 Annual Report of Activities for 2000
Aquatic Ecosystems and Invertebrates of the Grand Staircase-Escalante National Monument Cooperative Agreement Number JSA990024 Annual Report of Activities for 2000 Mark Vinson National Aquatic Monitoring Center Department of Fisheries and Wildlife Utah State University Logan, Utah 84322-5210 www.usu.edu/buglab 1 April 2001 i Table of contents Page Foreword ........................................................................... i Introduction ........................................................................ 1 Study area ......................................................................... 1 Long-term repeat sampling sites ........................................................ 2 Methods Locations and physical habitat ................................................... 3 Aquatic invertebrates Qualitative samples...................................................... 3 Quantitative samples ..................................................... 4 Laboratory methods ........................................................... 4 Results Sampling locations............................................................ 5 Habitat types................................................................. 6 Water temperatures ........................................................... 8 Aquatic invertebrates .......................................................... 8 Literature cited..................................................................... 13 Appendices 1. Aquatic invertebrates collected in the major habitats A. Alcove pools ...................................................... -
Seepage Investigation and Selected Hydrologic Data for the Escalante River Drainage Basin, Garfield and Kane Counties, Utah, 1909-2002
Seepage Investigation and Selected Hydrologic Data for the Escalante River Drainage Basin, Garfield and Kane Counties, Utah, 1909-2002 By Dale E. Wilberg and Bernard J. Stolp U.S. GEOLOGICAL SURVEY Scientific Investigations Report 2004-5233 Prepared in cooperation with the U. S. DEPARTMENT OF THE INTERIOR, BUREAU OF LAND MANAGEMENT, GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT Salt Lake City, Utah 2005 U.S. DEPARTMENT OF THE INTERIOR GALE A. NORTON, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 2329 West Orton Circle Building 810 Salt Lake City, Utah 84119 Box 25286, Denver Federal Center http://ut.water.usgs.gov Denver, CO 80225-0286 1-888-ASK-USGS iii CONTENTS Abstract .................................................................................................................................................................................................... 1 Introduction .................................................................................................................................................................................................... 1 Physical Setting and Hydrogeology.................................................................................................................................................. -
Grand Staircase-Escalante National Monument
©Lonely Planet Publications Pty Ltd Grand Staircase-Escalante National Monument Includes ¨ Why Go? Day Hikes . .. 140 The largest park in the Southwest, Grand Staircase-Escalante Overnight Hikes . 144 National Monument (GSENM) features spectacular scenery Driving . 145 in rough-cut wilderness. From the Grand Canyon floor, geo- Cycling . 149 logical strata climb in staircase fashion 3500ft to Bryce Can- yon and the Escalante River canyons. These rock layers tell Sleeping . 149 260 million years of history in a riot of color. The diversity of landscapes is astounding – pink dunes, white cliffs, red canyons, vast slickrock and undulating slot canyons. The monument was established in 1996 by US President Best Hikes Bill Clinton in a controversial designation. Many ranchers and residents were concerned about losing access. Local ¨ Slot Canyons of Dry Fork/ legislators and mining interests were stymied. Environment Coyote Gulch (p142) activists appeared and conflicts ensued. Years later, federal ¨ Willis Creek (p143) versus local control is still a hot issue, though there is also rec- ¨ Lower Calf Creek Falls ognition that the land needs, and deserves, some protection. (p141) ¨ Escalante River Natural Bridge (p140) Driving Distances (miles) Bryce Canyon National Park ¨ Boulder Mail Trail (p144) (Park Entrance) 80 Escalante 30 50 Grand Staircase-Escalante National Monument (Canonville Visitor Center) 65 15 35 Best Drives Kanab 150 75 120 85 ¨ Burr Trail (p145) Grand Canyon North Rim (Park Entrance) 2157145 190 155 0 ¨ Hole-in-the Rock Road (p145) ) ¨ Cottonwood Canyon Road (p147) e b Boulder Bryce Canyon National Park (Park Entrance) Escalant Grand Staircase-Escalante National Monument (Canonville Visitor Center Kana Note: Distances are approximate 137 Entrances PARK POLICIES & REGULATIONS There are no entrance stations; the monument is accessible 24/7.