Fault-Fin Landscape
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Arches National Park, Moab, Utah
Destination: Arches National Park, Moab, Utah Several years ago I took my first month-long road trip around the American West. Planned stops included Santa Fe and the Grand Canyon among others. I did have a goal to include stops in the western states I hadn’t been to before. I would have picked off Utah with a planned stop at Four Corners while on my way to the Grand Canyon, but my wall calendar had a cool picture of Delicate Arch in southeast Utah’s Arches National Park. I wasn’t at all familiar with Utah’s red rock country at the time, but I really wanted to see Delicate Arch. So I made Arches National Park my Utah destination as I travelled from Santa Fe to the Grand Canyon. Needless to say, I fell in love with Arches and more broadly the entire Colorado Plateau region. I’ve since explored many great destinations in the region, and I’ve been back to Arches several times since that first visit. Arches, after all, is my favorite national park. But I’m not the only one who’s discovered Arches National Park. Visitation has soared, close to doubling in just the last decade. For several months a year, the line to get into the park is long. The campground is routinely full. Parking lots at all the key attractions are often full – and you’re delayed from trying your luck elsewhere by cars blocking the road waiting for parking spots to open. Hiking the main trails are very social affairs rather than quiet wilderness experiences. -
Natural Rock a R C H E S the Director’S
UTAH GEOLOGICAL SURVEY SURVEY NOTES Volume 41, Number 2 May 2009 U t a h ’ s Natural Rock A r c h e s The Director’s Perspective predominantly rising trends since price now close to that of Japan, which ranks minima in late December 2008. second after the U.S. Furthermore, China’s economy is projected to grow by The dramatic price swings from record 8 percent in 2009 despite the global reces- highs during mid- to late 2008 are likely sion. China’s pursuit of a higher standard to make 2008 a historically important of living is rapidly consuming recent sur- year for revenue generated from geologic pluses in commodity supplies caused by commodities extracted in Utah. The graph the global downturn, and may already be below shows the updated, inflation-adjust- contributing to rising base metal prices. ed trends since 1960. The gross revenue Although the U.S. economy may take for 2008 exceeds 2007 by over $1 billion, several years to bounce back from its and hits a new high of close to $10 billion. financial and housing market problems, Half the total is from non-fuel minerals expect to see many commodity prices (primarily copper and molybdenum), and begin to grow again this year. The mining by Richard G. Allis half is from fossil fuels (primarily natural industry has gone from boom to bust in gas). With most commodities now at prices only six months, but perhaps this industry less than half their peak, 2008 is likely to is already on the road to recovery. -
Arches Visitor Guide 2019
National Park Service Visitor Guide U.S. Department of the Interior Arches North Window NPS PHOTO / CHRIS WONDERLY Studying the Fate of Arches BY LOGAN HASTINGS The dynamic landscape of Arches goes beyond a human timescale, but you The crackmeter has since found patterns arches are forming at a similar pace, National Park is like a storybook, telling still have the opportunity to be a part of in the crack’s activity as temperature and which will continue the story of Arches tales of change across this unique space. the story as a visitor. seasons change. The data show that the National Park. This landscape constantly The forces of erosion, water, gravity, crack expands and contracts up to 2.1 changes as the tests of time write each and time have brought the stories of the The pages have now turned to today, and centimeters annually (0.82 inches), yet it arch’s story, from beginning to end. arches to life, and we are often reminded during this chapter we can also begin stays within the same range of movement of how powerful these forces are. In to predict the changes to come. Park from year to year. Even over the course of As you look at each arch, think of 1991, a piece of Landscape Arch tumbled staff are focused on the crack in North one day, the crack moves 0.57 millimeters its timescale compared to your own. to the ground, leaving visitors humbled Window as an indicator of change, now (0.02 inches) on average in response to What tests of time mark your greatest as witnesses to the power of time.The and in the future. -
Geology Along a Margin of the Colorado Plateau and Rio Grande Rift, North-Central New Mexico
Geology along a Margin of the Colorado Plateau and Rio Grande rift, north-central New Mexico: roadlog and field-stop discussions to accompany Field-trip#3 of the Rocky Mountain/South-Central sections annual meetingof the Geological Society of America in Albuquerque,New Mexico, April 20-27, 1991 prepared by Mark A. Gonzalez David P. Dethier Department of Geography and Geology Department of Geology University of Denver Williams College Denver, CO 80208 Williamstown, MA 01267 New Mexico Bureauof Mines and Mineral Resources, Open-file Report374. Table of Contents page List of Figures ii List of Tables V. Abstract 1 Introduction 2 Geologic Setting 4 Stop 1: Espaiiola Formation east of EspaiiolaHigh School 11 Stop 2: Mid-Quaternary surfaces and faults along the Embudo fault 18 zone, Arroyo de la Presa Stop 3+ Examination of Quaternary,erosion surfaces, deposits, and 25 the Lava CreekB ash Stop 4: Inset Quaternary depositsin the Colorado Plateau 33 Stop 5: Overview of Pre-Quaternary and Quaternary surfaces 38 Day 2: Neotectonism and ancestral drainage of the rift margin 45 Stop 6: Caiiones fault zone and other rift margin structures 45 Stop 7: Tectonic control on paleo-topography and volcanogenic 50 sediment distribution Stop 8: Late-Quaternary faulting(?) along the Madera Caiion fault 59 zone Stop 9: White Rock Canyon formation and large-scale cycles of base- 63 level change Acknowledgements 68 References 69 i List of Figures Figure 1. Location map showing the location of roadways, field-trip 5 scops, and physiographic and geologic features found in the Espafiola basin and Abiquiu embayment study area and cited in the text. -
The Colorado Plateau Geographic Information System (GIS): an Introduction to the Arcview Project and Data Library
Chapter D National Coal Resource The Colorado Plateau Geographic Assessment Information System (GIS): An Introduction to the ArcView Project and Data Library Click here to return to Disc 1 By Laura R.H. Biewick1 and Tracey J. Mercier2 Volume Table of Contents Chapter D 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* 1 U.S. Geological Survey, Denver, Colorado 80225 2 U.S. Geological Survey contract employee, 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 Introduction .................................................................................................................................................D1 Purpose ................................................................................................................................................. 1 What is the Colorado Plateau Geographic Information System (GIS)?...................................... 1 How Were the Data Collected and Compiled?................................................................................ 4 The Colorado Plateau ArcView Project .................................................................................................... 8 General Discussion ............................................................................................................................ -
Colorado's Little Fish a Guide to the Minnows and Other Lesser Known Fishes in the State of Colorado
Colorado's Little Fish A Guide to the Minnows and Other Lesser Known Fishes in the State of Colorado. By John Woodling Designed and Edited by Russ Bromby Published June, 1985, by the COLORADO DIVISION OF WILDLIFE Department of Natural Resources 6060 Broadway, Denver, CO 80216 Telephone: 303/297-1192 ACKNOWLEDGEMENTS Many people helped in the preparation of this book. Without their aid, comple- tion of the work would have been impossible. To these people I offer my most sincere thanks and appreciation. Charles Bennett, Gerald Bennett, Steve Burge, James Chadwick, Scott Chartier, Larry Finnell, John Goettl, Mike Japhet, Bob Judy, Rick Kahn, Robin Knox, Mike McAllister, Charlie Munger, Dave Ruiter, Jay Sarason, Clee Sealing, Jay Stafford, Roger Trout, Bill Weiler, Bill Wiltzius, Lawrence Zuckerman and others all spent time and effort in locating records, collecting, and in some cases, transporting live fish across large distances. Jim Bennett, Charles Haynes and Dave Miller not only helped locating specimens but reviewed large portions of text. Wilbur BoIdt provided needed assistance in obtaining and maintaining funds to produce this book. Gil Dalrymple, Carol Dreitz and Pat Barnett spent many hours typing the manuscript. Special thanks to Marian Herschopf, whose diligent efforts produced many obscure documents and materials essential to production of this text. PREFACE Colorado's Little Fish is a bit of a misnomer. Some species included in this book attain a length of greater than one foot and weigh in excess of three pounds. Specimens of one fish in the book, the Colorado squawfish, have been recorded up to 65 pounds. -
Arches Visitor Guide
National Park Service Park News U.S. Department of the Interior Arches Visitor Guide The official newspaper of Arches National Park Bring this paper to 2014, No. 1 the visitor center desk for travel tips, Make Memories & Leave No Trace or see back page! MY EYES STARE IN WONDER, MY BREATH is a problem that is widespread in many grows deeper and I can’t seem to stop national parks. The process of removing taking pictures. Where I live, the views graffiti takes time, care, and a lot of hard are not as vast, the colors not as vibrant, work. the air not as fresh, and the skyline not formed by magnificent rock towers. I Luckily though, I know that graffiti have come to a national park: a place of is easily prevented and there are such significance it was deemed worthy many other ways we can mark our of special protection. Arches National journey here: a spectacular photo, an Park was created to protect “gigantic unforgettable hike, a quiet moment arches, natural bridges, ‘windows’, of reflection. When I think about the spires, balanced rocks, and other unique National Park Service mission, wind-worn sandstone formations, for the preservation of which is desirable “to preserve unimpaired the because of their educational and scenic natural and cultural resources and value.” I have traveled far for this values of the national park system experience. for the enjoyment, education, and inspiration of this and future As I marvel at this extraordinary generations” landscape, I notice something out of place: someone has “tagged” the rock Examples of graffiti and park staff working hard to remove it. -
Water from Bedrock in the Colorado Plateau of Utah
Utah State Engineer Technical Publication No. 15 WATER FROM BEDROCK IN THE COLORADO PLATEAU OF UTAH by R. D. Feltis Geologist U. S. Geological Survey Prepared by the U. S. Geological Survey in cooperation with THE UTAH OIL AND GAS CONSERVATION COMMISS10N 1966 CONTENTS - (Continued) Page Water from bedrock in the Canyon Lands section-Continued Entrada Sandstone _. .. _. .. _._ .._ _.. .. '2:7 Bluff Sandstone .. __ ._ __.. __ ._ .. __ . .. _._ _ _ _.... '2:7 Morrison Formation .... ._ .. _. __ ._.. __ __ .. _. .__ ..__.._.._..... '2:7 Dakota Sandstone .. _ _ __ _ __.. __ _ _..... 28 Burro Canyon Formation __ __ .. _ _.._ __ _ _.. _..... 28 Mancos Shale .__ _._._ __ __ _ _._ _ __ _..... 28 Ferron Sandstone Member of Mancos Shale _ _. __ .._ _.. __ .__ __ _ 29 Tununk Shale Member of Mancos Shale _._ _ _ _..... 29 Water from bedrock in the High Plateaus section _ _ __ _ 29 Limestones of Paleozoic age ._ _ __.._.._ _.._ _ .._ _... 31 Rocks of NIississippian age .__ .. __ .. __ ._ _ _ _ _... 31 Rocks of Mississippian age and Molas Formation __ _ _.............. 31 Toroweap Formation .. __ .__ .. _._ __ ._._._ __.._ __ _ _ _. __ _._ _... 31 Cedar Mesa Sandstone Member of Cutler Formation .._ _.................. 31 Coconino Sandstone _. __ ._. ._ _ _.._ _ __ _ _._._. -
Guidebook to the Colorado River Part 1: Lee's Ferry to Phantom Ranch In
Brigham Young University Geology Studies Volume 15 - Part 5 - 1968 Studies for Students No. 4 Guidebook to the Colorado River, Part 1: Lee's Ferry to Phantom Ranch in Grand Canyon Nati'onal Park with Notes on Aboriginal Cultures by Ray T.Matheny and on Biological Features by Joseph R. Murphy W. KENNETHHAMBLIN AND J. KEITHRIGBY A Publicacion of the Department of Geology Brigham Young Un~versicy Provo, Utah 84602 Studzes for Students supplements the regular Issue of Bvzgharn Young Unzvev~zty Geology Studzes and 1s Intended as a serles of short papers of general Interest which may serve as guides to the geology of Utah for beginning students and laymen. Distributed 1 October 1968 Second Edition 30 September 1969 Repr~ntedJuly 1970 Reprinted July 1972 Reprinted May 1974 Repr~ntedApr~l 1978 Reprinted April 1982 Reprinted December 1996 Guidebook to the Colorado River, Part 1: Lee's Ferry to Phantom Ranch in Grand Canyon National Park W. KENNETHHAMBLIN AND J. KEITHRIGBY Department of Geology, Brigham Yolrng Univerrity PREFACE A trip down the Colorado River through the Grand Canyon offers the unique opportunity to study close-hand a classic cross section into the earth's crust. Such a trip would not have been practical for students of geology some years ago, but with the innovation of pontoon boats and the establishment of regular float trips through the canyon by experienced boatmen, this trip is now feasible. Experience in taking students down the Colorado River over the past several years as part of their educational program has prompted us to write this guidebook, not only for the geology student but for all interested persons who desire to understand the scenery of the Canyon. -
Bryce Canyon Geology
National Park Service Bryce Canyon U.S. Department of the Interior Bryce Canyon National Park The Story in the Rocks The geology of Bryce Canyon is a story rich with change and the exciting interaction between nature’s forces. The creation of the unique landscape that makes Bryce Canyon famous began between 35 and 55 million years ago, when much of southern Utah was covered by braided rivers and streams, and later by a system of lakes. However, the story really begins millions of years before. The Top of the Stairs In the preface to Clarence E Dutton’s Report on The oldest rocks exposed at Bryce Canyon are the Geology of the High Plateaus of Utah (1880), from the Lower Cretaceous, when most of North John Wesley Powell wrote “These cliffs are bold America was under water. The Dakota Formation, escarpments hundreds and thousands of feet Tropic Shale, and Straight Cliffs Formation are in altitude - grand steps by which the region is marine sediments associated with the Western terraced.” Powell was describing a series of cliffs Interior Seaway. These rock layers, along with we now know as the Grand Staircase, visible from the slightly younger Wahweap Formation, are the Kaibab Plateau north of the Grand Canyon. the Gray Cliffs, covering a span of time from 100 Each of Powell’s steps represents a different to 75 million years ago, are the fourth step in the period of geologic history, beginning 260 million staircase. The Pink Cliffs of the Claron Formation years ago in the Permian. A low lying set of cliffs are the fifth and final step. -
Role of Fracture Localization in Arch Formation, Arches National Park, Utah
Role of fracture localization in arch formation, Arches National Park, Utah KENNETH M. CRUIKSHANK* 1 Rock Fracture Project and Bailey Willis Geomechanics Laboratory, Department of Geological ATILLA AYDIN J and Environmental Sciences, Stanford University, Stanford, California 94305 ABSTRACT ever, because these processes are not re- themselves participate in arch formation. In stricted to the sites of arches in rock fins. many sites we are able to demonstrate that Spectacular rock fins on the flanks of Salt There must be some factor that locally en- the reason for fracture localization is shearing Valley anticline in southeast Utah are formed hances the effects of erosion within a rather along preexisting discontinuities, together with by erosion along zones of joints. Within a rock small part of a rock fin to produce an arch. the interaction between adjacent sheared fin, arches form where intense fracturing is lo- How erosion is localized within a rock fin to discontinuities. calized. Fracture localization is controlled by form an arch is enigmatic. In the case of nat- shear displacement along existing horizontal or ural bridges (for example, Natural Bridge Geological Setting vertical discontinuities. Horizontal discontinu- National Monument, Southeast Utah), a ities may be shale layers, shale lenses, or bed- river or stream is assumed to be the agent Arches National Park is centered on the ding planes, whereas vertical discontinuities providing localized erosion. Arches within salt-cored Salt Valley anticline (Fig. lb), are usually preexisting joint segments. The Arches National Park, however, are not as- which represents the northwest extent of the roof and overall shape of an arch is controlled sociated with fluvial activity. -
Arches National Park Geologic Resource Evaluation Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Arches National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2004/005 THIS PAGE: Canyon, Arches NP. ON THE COVER: Delicate Arch, Arches NP NPS Photo’s Arches National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2004/005 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 November 2004 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.