Terrestrial Vertebrate Fauna of the Kaiparowits Basin
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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. -
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 -
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 ............................................................................................... -
38-Simpson Et Al (Wahweap Fm).P65
Sullivan et al., eds., 2011, Fossil Record 3. New Mexico Museum of Natural History and Science, Bulletin 53. 380 UPPER CRETACEOUS DINOSAUR TRACKS FROM THE UPPER AND CAPPING SANDSTONE MEMBERS OF THE WAHWEAP FORMATION, GRAND STAIRCASE-ESCALANTE NATIONAL MONUMENT, UTAH, U.S.A. EDWARD L. SIMPSON1, H. FITZGERALD MALENDA1, MATTATHIAS NEEDLE1, HANNAH L. HILBERT-WOLF2, ALEX STEULLET3, KEN BOLING3, MICHAEL C. WIZEVICH3 AND SARAH E. TINDALL1 1 Department of Physical Sciences, Kutztown University, Kutztown, PA 19530; 2 Department of Geology, Carleton College, Northfield, MN, 55057; 3 Central Connecticut State University, Department of Physics and Earth Sciences, New Britain, Connecticut 06050, USA Abstract—Tridactyl tracks were identified in the fluvial strata of the Upper Cretaceous Wahweap Formation in Grand Staircase-Escalante National Monument, southern Utah, U.S.A. An isolated track and a trackway are located within the upper member at the Cockscomb, and an isolated track is in the capping sandstone member at Wesses Canyon. The upper member tracks are tridactyl pes imprints consisting of a longer, blunt digit III and shorter, blunt digits II-IV. This trace corresponds well to an ornithropod dinosaur as the trackmaker. The capping sandstone member track is a tridactyl pes with an elongate digit III and shorter digits II-IV. Claw impressions are present on the terminus of digits II and III. This trace is consistent with the pes impression of a one meter tall theropod. The tracks further highlight the diversity of dinosaurs in the capping sandstone of the Wahweap Formation. INTRODUCTION During the Late Cretaceous, North America, in particular the west- ern United States, was the site of a radiation of new dinosaurian genera. -
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. -
Halls Crossing
National Park Service Glen Canyon National Recreation Area U.S. Department of the Interior Rainbow Bridge National Monument Vol. 10, No. 1, 2014 The official newspaper PHOTO: Bob Moffitt Discover Glen Canyon Welcome! only 13% of Glen Canyon National Recreation overlooks. For spectacular views of the canyon Area. The impounded waters offer unparalleled country, those with 4-wheel drive vehicles Glen Canyon National Recreation Area’s varied water-based recreational opportunities where can visit less accessible areas of the park like expanses of land and water offer more than you can boat, swim, fish, water ski, camp or Alstrom Point or the Burr Trail, which begins you may think. As a unit of the National Park take a boat tour to Rainbow Bridge or Antelope in Glen Canyon and continues into Capitol Reef Service, Glen Canyon preserves and protects Canyon. National Park. over 1.2 million acres for scenic, scientific, and recreational values. Glen Canyon’s vast acreage You may be surprised to know that almost half With such recreational diversity and so many can be divided into three prominent land and of the park is managed as a proposed wilderness places to discover, visitors are often inspired to water areas, each of which offers distinct types area, meaning there is minimal development and return for further exploration. Whether it’s by of experiences for visitors from around the visitors can enjoy a more remote experience. boat, car, or foot, we invite you to experience all globe. that Glen Canyon National Recreation Area has The remainder of the park offers areas that to offer. -
Of Coal in the Kaiparowits Plateau, Southern Utah
Chapter T National Coal Resource Geologic Overview and Resource Assessment Assessment of Coal in the Kaiparowits Plateau, Southern Utah Click here to return to Disc 1 By Robert D. Hettinger,1 Laura N.R. Roberts,1 Volume Table of Contents Laura R.H. Biewick,1 and Mark A. Kirschbaum1 Chapter T of Geologic Assessment of Coal in the Colorado Plateau: Arizona, Colorado, New Mexico, and Utah Edited by M.A. Kirschbaum, L.N.R. Roberts, and L.R.H. Biewick U.S. Geological Survey Professional Paper 1625–B* Chapter T supersedes U.S. Geological Survey Open-File Report 96-539 1 U.S. Geological Survey, Denver, Colorado 80225 * This report, although in the USGS Professional Paper series, is available only on CD-ROM and is not available separately U.S. Department of the Interior U.S. Geological Survey Contents Abstract........................................................................................................................................................ T1 Introduction ................................................................................................................................................... 2 Purpose and Scope ............................................................................................................................. 2 Methods ................................................................................................................................................ 2 Lithologic and Stratigraphic Data ............................................................................................ 2 -
The Lost World of Glen Canyon
- r f 1 / I / I / r llS^ *&v . .".•*' : '•.-• - :•:-.*« •••• '•• i^g. i. A large sandstone arch called Galloway Cave existed on the right bank about 2.25 miles upstream from Glen Canyon Dam. River travelers camped here before the turn of the century and seemed always to build their campfires in the same place, at the downstream corner of the arch. Many also left a record of their presence by uniting their names on the wall with a piece of charcoal. This view shows a Nevills river party preparing for dinner on June 11, 1949. Lake Powell covers this site. Photographs, except Fig. 4, are courtesy of author. The Lost World of Glen Canyon BY P. T. REILLY THOUSANDS OF PEOPLE CRUISE THE SURFACE OF Lake Powell never dream ing of the wonders beneath the waters, features that are not likely to be exposed again in our lifetime, nor in those of our children or grandchildren. In fact, they may never be seen again. This photo graphic collection of landforms will serve as a reminder that our world changes as dramatically in the vertical as it does in the horizontal. Mr. Reilly lives in Sun City, Arizona. Readers may wish to refer to the following: Plan and Profile, Colorado River, Lees Ferry, Arizona, to Mouth of Green River, Utah, Sheet B; Navajo Mountain, Utah- Arizona quadrangle; Lake Canyon, Utah quadrangle; and Mancos Mesa, Utah quadrangle. The Lost World of Glen Canyon 123 Lee's Ferry occupies a unique and important position on the Colorado River because the 1921 measurement by the U.S. -
Energy and Mineral Resources, Grand Staircase
Circular 93 Utah Geological Survey Illustration Captions View figure: Circular 93 1., 2., 3., 4., 5., 6., 7., 8., 9., 10., 11., 12., 13., 14., 15. A Preliminary Assessment of Energy and Table of Contents 1.Preface Mineral Resources within the Grand 2.Summary 3.Introduction Staircase - Escalante National Monument 4.Geology 5.Kaiparowits Plateau coal Compiled by M. Lee Allison, State Geologist field 6.Oil and Gas Potential Contributors: 7.Tar-sand Resources Robert E. Blackett, Editor 8.Non-fuel Minerals and Thomas C. Chidsey Jr., Oil and Gas Mining David E. Tabet, Coal and Coal-Bed Gas 9.Acknowledgments Robert W. Gloyn, Minerals 10.References Charles E. Bishop, Tar-Sands January 1997 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES CONTENTS PREFACE SUMMARY INTRODUCTION Background Purpose and Scope GEOLOGY Regional Structure Permian through Jurassic Stratigraphy Cretaceous and Tertiary Stratigraphy THE KAIPAROWITS PLATEAU COAL FIELD History of Mining and Exploration Coal Resources Coal Resources on School and Institutional Trust Lands Sulfur Content of Kaiparowits Coal Coal-bed Gas Resources Further Coal Resource Assessments Needed OIL AND GAS POTENTIAL Source Rocks Potential Reservoirs Trapping Mechanisms Exploration and Development Carbon Dioxide Further Oil and Gas Resource Assessments Needed TAR-SAND RESOURCES OF THE CIRCLE CLIFFS AREA NON-FUEL MINERALS AND MINING Manganese Uranium-Vanadium Zirconium-Titanium Gold Copper, Lead and Zinc Industrial and Construction Materials Mining Activity Further Non-Fuel Mineral Resource Assessments Needed ACKNOWLEDGMENTS REFERENCES APPENDIX A: Presidential proclamation APPENDIX B: Summary of the coal resource of Kaiparowits Plateau and its value APPENDIX C: Summary of coal resources on School and Institutional Trust Lands APPENDIX D: Authorized Federal Oil and Gas Leases in the monument ILLUSTRATIONS Figure 1. -
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 ......................................................