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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. -
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. -
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. -
Wayne County, Utah Resource Management Plan
DRAFT Document for Public Review May 1, 2017 WAYNE COUNTY, UTAH RESOURCE MANAGEMENT PLAN 2017 Wayne County Resource Management Plan Page 1 DRAFT Document for Public Review May 1, 2017 Prologue Wayne County is a unique and beautiful place steeped in pioneer heritage and culture. The hearty souls that settled this county and their generations of offspring to follow, have a rich history of making a living utilizing the public lands within it. The early settlers and those that followed, up until the 1970’s, had no idea the government would start locking up land, limiting their access and use of the land. It could be said we have all been naïve while bit by bit land has been taken from our reach and set aside in monuments, parks, recreation areas, wilderness study areas, wilderness characteristic areas, roadless areas, and other designations. All land uses except recreation have been almost entirely eliminated, and that has been limited and controlled to the point that some people are completely prevented from visiting some areas. This elimination of use has severely affected the livelihoods, families, economics, and entire lives of those who have remained and tried to raise families in the county. The slow choking out and change to a seasonal and recreational economy is devastating. As kids move away, farms and ranching operations are sold, houses are sold for second homes or short term rentals, and tourists flock in, good traditional jobs, and families disappear. It can be said that almost everything that sustains life comes from the earth, except sun light. -
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. -
Structural Geologic Evolution of the Colorado Plateau
Geological Society of America 3300 Penrose Place P.O. Box 9140 Boulder, CO 80301 (303) 357-1000 • fax 303-357-1073 www.geosociety.org This PDF file is subject to the following conditions and restrictions: Copyright © 2009, The Geological Society of America, Inc. (GSA). All rights reserved. Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in other subsequent works and to make unlimited copies for noncommercial use in classrooms to further education and science. For any other use, contact Copyright Permissions, GSA, P.O. Box 9140, Boulder, CO 80301-9140, USA, fax 303-357-1073, [email protected]. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. This file may not be posted on the Internet. The Geological Society of America Memoir 204 2009 Structural geologic evolution of the Colorado Plateau George H. Davis Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA Alex P. Bump BP Exploration and Production Technology, Houston, Texas 77079, USA ABSTRACT The Colorado Plateau is composed of Neoproterozoic, Paleozoic, and Mesozoic sedimentary rocks overlying mechanically heterogeneous latest Paleoproterozoic and Mesoproterozoic crystalline basement containing shear zones. The structure of the plateau is dominated by ten major basement-cored uplifts and associated mono- clines, which were constructed during the Late Cretaceous through early Tertiary Laramide orogeny. -
Capitol Reef Wilderness Study
Utah State University DigitalCommons@USU U.S. Government Documents (Utah Regional Elusive Documents Depository) 12-1973 Capitol Reef Wilderness Study United States Deparment of the Interior, National Park Service Follow this and additional works at: https://digitalcommons.usu.edu/elusive_docs Part of the Environmental Monitoring Commons Recommended Citation United States Deparment of the Interior, National Park Service, "Capitol Reef Wilderness Study" (1973). Elusive Documents. Paper 105. https://digitalcommons.usu.edu/elusive_docs/105 This Report is brought to you for free and open access by the U.S. Government Documents (Utah Regional Depository) at DigitalCommons@USU. It has been accepted for inclusion in Elusive Documents by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. wilderness study '" b-703 CAPITOL REEF NATIONAL PARK· UTAH }o' a:u .C~8 W~4 197~ NATIONAL WI LDERNESS STUDY Preliminary - Subject to Change Capitol Reef National Park Utah December 1973 CORRECTION TO WILDERNESS STUDY REPORT for CAPITOL REEF NATIONAL PARK, UTAH June 1974 The lands shown in this report as ~otential wilderness additions total 15,470 acres. ·This correction deletes 13,660 acres of Utah State land, thus the correct potential wilderness additions total 1,810 acres. FINDINGS I\JII\IE UI\JITS WITHIN CAPITOL REEF NATIONAL PARK, TOTALING 181,230 ACRES, HAVE BEEN FOUI\JD SUITABLE FOR WI LDERI\JESS DESIGNATION AND ARE PROPOSED FOR INCLUSION IN THE NATIONAL WILDERNESS PRESERVATION SYSTEM. IN ADDITION, POTENTIAL WI LDERNESS ADDITIONS OF 15,470 ACRES INCLUDING LAND PRESENTLY MINED, LEASED FOR 01 L AND GAS, AND NON-FEDERALLY OWNED, ARE RECOMMEI\IDED FOR INCLUSION IN THE NATIONAL WILDERI\IESS PRESERVATION SYSTEM WHEN THE SECRETARY OF THE INTERIOR DETERMINES THAT THEY QUALIFY. -
Capitol Reef Scenic Byway
Capitol Reef Country Scenic Byway FFoolllllloowwiiinngg UUtttaahh’’’ss SStttaatttee RRoouutttee 2244 fffrroomm HHaannkkssvviiillllllee tttoo LLooaa,,, CCaappiiitttoolll RReeeefff CCoouunntttrryy SScceenniiicc BByywwaayy iiiss aa 6655 mmiiilllee llloonngg hhiiigghhwwaayy ddrriiivvee ttthhaattt llleeaaddss onnee ttthhrroouugghh ttthhee DDiiixxiiiee NNaatttiiioonnaalll FFoorreessttt aanndd CCaappiiitttoolll RReeeefff NNaatttiiioonnaalll PPaarrkk aass wweellllll aass ttthhee sspprraawwllliiinngg SSaann RRaafffaaeelll SSwweellllll aanndd ccoollloorrfffuulll MMaazzee DDiiisstttrriiiccttt oofff CCaannyyoonnlllaannddss NNaatttiiioonnaalll PPaarrkk... AAdddd aann aaddddiiitttiiioonnaalll 1166 mmiiillleess rroouunndd tttrriiipp iiifff yyoouu iiinnccllluuddee ttthhee CCaappiiitttoolll RReeeefff SScceenniiicc RRooaadd ttthhrroouugghh ttthhee NNaatttiiioonnaalll PPaarrkk... 1 Hanksville Located within the heart of Utah’s National parks, Hanksville is a small town which offers the necessary amenities to allow for a comfortable stay to explore the surrounding sights of Lake Powell, Goblin Valley, and Capital Reef. 1. Wolverton Mill 38.366833, -110.717807 The Wolverton Mill is a log structure built by Edwin T. Wolverton in 1921. Functioning to mill wood and crush ore it was one of a handful of mills in the country to do both of these functions. Once located in the Henry Mountains, the mill was disassembled and restored and is now located at the Bureau of Land Management Henry Mountains Field Station (Hanksville Office). www.waterhistory.org/histories/wolverton 2. Factory Butte Special Recreation Area 38.364877, -110.914597 Factory Butte is a popular recreation site for OHV jumping and riding to motorcycling and passenger car touring. These scenic badlands offer a surreal experience of strange mancos-shale peaks and hills. It is also a popular site in the spring to view the wildflowers blooming at Factory Butte. www.blm.gov/visit/factory-butte-recreation-area Capitol Reef National Park Capitol Reef National Park is in south-central Utah, in the heart of red rock country. -
Capitol Reef National Park Foundation Document
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Capitol Reef National Park Utah January 2018 Foundation Document B To Goblin Valley SP Paradise Valley a M Lake k O and 70 e il Well Be ch R r n o o R ad a r n c o FISHLAKE h n R d c k i l a NATIONAL FOREST B n s l e a i t t n t Cathedral L i o u S rn R l M Elkho o Junction M M o u ad dd I p y D e To Fremont MONOLITHS s h D s and 72 Gypsum L a 5mi W Sinkhole C P 8km E o A lk T Cr Cathedral D E eek H l R Upper Cathedral Valley E k oad Valley 9mi E h Overlook 14km D S Black Mountain o R E lt r 6308ft Sa n A R 1923m R L T o H a a Elkhorn Road closed Upper rtn F d Hartnet e during winter t R Junction South Desert oa E Overlook d Temple of C a E the Sun thed Neff 14mi ra R 9256ft l C Reservoir 2821m 23km Temple of W r Po the Moon V oo e lk d E e A k L Cr L ee L 15mi Thousand k B L T E 24km e n I Lake Mtn Big h Y ch 11306ft Lake e Dee V 3446m p Ro ad E S O N Lower South U Desert Overlook I ek A re T C a C H a C s H in e a e H M r v e il T l t le i l R n v e e O H n 24 a i t r W t N a n e W C t A a N s h 24 19mi T 31km Hanksville 4295ft To Hite Crossing, E River 1309m 95 Glen Canyon NRA, R 14mi nt and Natural Bridges NM D N 23km mo t re S e o F pr P D r s in e r l g p t e l h O E s i e H B S C l R D Sulp u o Caineville e hur Twin Rocks E a 4600ft C e u d d 10mi C K r 1402m l a R e F e 24 16km Orientation n e B y l a Chimney Rock o k R E a s Pullout n T r 6843ft t e T s e 2085m M Creek p To Bicknell Torrey Visitor Center 7mi e 11km l p and 5500ft i l 70 Orientation v -
Geologic Map of the Fruita Quadrangle, Wayne County, Utah
UTAH GEOLOGICAL SURVEY a division of Utah Department of Natural Resources in cooperation with Plate 1 National Park Service Utah Geological Survey Miscellaneous Publication 07-2 and Brigham Young University Department of Geological Sciences Geologic Map of the Fruita Quadrangle Jpc Qatd Je Ti 1 Qatd1 Qae Js Qmt Qmt Qmt Jms Jcpr Ti Je Jcs Jmb To Cathedral Jcwg Qmt Qmt Jpc Qal Qae Valley Qae Qmtv Je Jmt Jmb Qmt Jmb Je Qatd1 Ti 6000 Jcpr Qatd1 Je Qatd1 Qmt Jpc Jcwb Qatdu Je Je Js Qmt Ti Jmb Jcwb Qatd1 Jms Ti Qatd Qmt Je 1 Ti Qae Jms Ti Qae Jpc Je Qatd1 Qatdu Qatd Ti Je 1 Jmb Qal Jmt Hartnet Road Je Ti Jmb Jcpr Qal Jpc Je Je Jn Je Qae Ti Qatd1 Qatd1 Qatdu Jmb Qatdu Jmb Qatd1 Jmb Qatd1 Jms Kcb Qal Kcb Jcwg Ti Qmtv Jmt Jmb DeepQatd1 Jms Jmt Je Jcpr Jcwb Je Jmb Jpc Ti Qal North Jcpr Jcpr Qatd1 Ti Jcpr Jpc Qatd Kcb Jcwb 1 Jk Ti Jcwg Ti Qatd Jms Je 1 Jms Kcb Kcb Je Jcpr Je Kcb Jn Ti Qal Js Jms 13 Jms Jmt Kcb Blue Jcwb Je Qatd1 Qae Jmt Kcr Kcm W A T E R P O C K E T Jmb Jcpr Qatd1 Kcm Ti Qatd1 Kd Jk Qae Jmb Kd Kcm Kd Jmt 6 Jcpr Qae Ti Qmt 8 Kcb Jpc 11 Qae Jk Qae Qal 5000 8 9 Kcb Kmt 5500 Je Jmb Jmb Qae Qatd1 Jmb Je 10 Jpc Creek 6000 Ti 3000 20 Qatd1 Js Flats Qe Kmt Qmt 10 Jcwg Qatd1 Qatd1 T he No t ch Kcb To Highway 24 Je Jms 2500 Jn Jpc 4000 Jcs Jpc S O U T H Kcm Ti Jmb Kcr 3500 Je Qal Qatd1 Js Kmt 4500 Jcpr 2000 Jcwg Jmb Ti Qae Jmt Qatd1 Qal Jpc Je Qal Jcwg Je Je Jcpr Qal Kcm F L A T S Jms Jmb syncline Qatd Js Kmt Jcwb 1 Qal Kcr Kmt Jpc Jcpr Ti Jcwg Qatd1 Kcb Jcwb F O L D Qatd Qe 1 Qatd1 Kmt Ti Qatd1 Jcwg Jcpr Je Jcwb Ti Jcwg Je Qatd1 Jk Kcr Jpc