42EM65, the Temple Mountain Pictograph Panel

Total Page:16

File Type:pdf, Size:1020Kb

42EM65, the Temple Mountain Pictograph Panel Steven J. Manning 42EM65, The Temple Mountain Pictograph Panel The Temple Mountain rock art panel, as it is The location of the Temple Mountain panel has called locally, is a group of large and striking been discussed in several "guide books" darkred pictographs (Figure 1). They are locat- (Barnes 1982:136, Castleton 1984:160, Slifer ed on the north side of South Temple Mountain 2000:126). The content of the panel has also Wash, roughly one mile west of the turnoff to been discussed in the rock art literature on sev- Goblin Valley State Park, which is in the San eral occasions (Gunnerson 1957, Manning Rafael Reef area of central Utah. 1990, Schaafsma 1970, 1971 and Siegrist Because the site can easily be seen from the 1972). paved road it is well known and heavily visited. The Temple Mountain pictographs are excep- The Bureau of Land Management (BLM) rang- tional—more exceptional than is generally ap- er in an information trailer at the turnoff to preciated, especially considering the apparent Goblin Valley said that he personally had over poor condition of the panel. The cliff face is 10,000 visitor contacts the previous year marred by large areas of exfoliated sandstone (2001). These contacts are with people request- (Figure 1). It appears that most of the picto- ing information about the San Rafael Reef area graphs have been destroyed, and the ones that as they drive in from State highway 24. I no- remain are severely damaged. Despite this de- ticed, during the hour I spent visiting with the terioration, the panel contains a great deal of ranger one morning, that only about one out of extremely valuable information, and the re- every ten cars stopped as they passed the trailer; maining images are unique and obviously irre- so 10,000 people is certainly an underestimate placeable. of the number of people visiting the area. One reason that the site is exceptional is that it Perhaps a more accurate picture of visitation appears to contain both Barrier Canyon Style may be obtained from visitor statistics at Goblin and Fremont type images. Of particular signifi- Valley State Park. In 2001, 75,702 people vis- cance is the apparent superimposition1 of ited Goblin Valley (Utah Division of State Fremont over the Barrier Canyon Style Parks statistics). April had the highest visita- (Schaafsma 1971:49, 73, her Figures 71 and tion with 13,000 people. Many of the people 130). The definitiveness of this conclusion, who visit Goblin Valley, and stay overnight, however, and its resulting influence on the Bar- camp in and along the San Rafael Reef where rier Canyon Style and Fremont relationships has there are no camping fees. Additionally, there been previously questioned (Manning 1990:61) are people who come to the area specifically to and is further discussed below. visit the San Rafael Reef and the San Rafael The Temple Mountain panel provided one of Swell. The area is a popular off-road vehicle the principal evidences used by Schaafsma to recreation destination. The road that passes the place the Barrier Canyon Style in the Archaic panel provides vehicular access to the Swell, period, thus preceding the later Fremont Culture and it continues northwest to Interstate 70. (Schaafsma 1971:128-135). This superimposi- Given this information, visitation to the area tion, if it indeed exists, has the potential to de- surrounding the pictographs is probably more termine the relative placement of Fremont and like 100,000 people annually. Barrier Canyon Style images in this panel and 47 Utah Rock Art, Volume 21, 2001 consequently provide information on their rela- Park. Unfortunately, I have no photographs of tive age. The Fremont culture is believed to the panel on that date because of a malfunction- have existed in this area from about A.D. 650- ing camera (or more likely a malfunctioning 700 to about 1200-1250 (Madsen 1989). The camera operator). The oldest photographs I Barrier Canyon Style is generally believed to have were taken at a later visit in 1979 (Figure have been created by Archaic peoples between 1). Since that date, I have visited the panel on about 6,000 B.C. to A.D. 500 (Kelen and Sucec many occasions, and I have made some interest- 1996:13). Schaafsma, however, later suggested ing observations and discoveries, most of which that the date during which the Barrier Canyon have not been discussed previously. The pur- Style was being constructed is more likely lim- pose of this paper is to present this information. ited to a shorter period, i.e., 500 B.C. to A.D. Since that first visit, I have observed changes 500 (Schaafsma 1980:70). occurring to the images within the panel, as I believe that the Barrier Canyon Style contin- well as major changes occurring to the envi- ued to be created long past A.D. 500 and cite as ronment surrounding the panel. For example, supporting evidence the existence of panels that the State of Utah allowed an oil and gas explor- fit the current definition of the Barrier Canyon atory well to be drilled directly in front of the Style, but that contain characteristics and imag- panel, i.e., between the cliff face and the main es of objects associated with later periods, such road. This resulted in the destruction of the as, for example, the bow and arrow (Manning vegetation and natural environment surrounding 1990). Additionally, Barrier Canyon Style pet- the panel. The area was left looking much like roglyph panels exist with very little patination, a giant dusty parking lot. Down stream (east of indicating that they are of recent origin (Man- the panel) and on the opposite side of the paved ning, this volume). road a large area was filled with dirt, leveled, Undoubtedly, some of the incongruities and po- and then abandoned. No reclamation of either lemics on the age of the Barrier Canyon Style area was done. These appalling scars stand as exist because of problems intrinsic to the defini- monuments to the indifference and negligence tion and use of the concept of style in ordering of the State of Utah in managing our public prehistoric rock art (Manning 1993) and be- lands. cause no reliable dating techniques currently Also damaging the landscape are large numbers exist for Barrier Canyon Style images. of off-road vehicles using the area. Four The Temple Mountain pictograph panel is also wheelers, often with children and teenagers significant because it contains some of the larg- driving them, have driven over much of the area est prehistoric painted figures in Utah. Their creating a maze of trails. While I was recently large size (one anthropomorph2 is about six feet visiting the panel, two off-road motorcyclists tall) suggests that the creators of these paintings raced up the small drainage east of the site, wanted their images to be easily seen. Their drove directly beneath the panel and continued large size also seems to suggest that these im- up the canyon oblivious to the rock art, the veg- ages were of some exceptional significance to etation they had crushed and the deep furrows their creators. they left behind. Recently the site was on the television news and HISTORY OF OBSERVATIONS AND in the newspapers (Joe Bauman, Deseret News, PREVIOUS DESCRIPTIONS March 29-30, 2000). On or about March 16, 2000, the panel was vandalized. Charcoal was I first visited the panel in the spring of 1971 on used to place drawings beneath the main por- a trip to the Maze area of Canyonlands National tion of the panel and on part of the panel itself 48 Steven J, Manning, The Temple Mountain Pictograph Panel (Figure 2). The source of the charcoal was un- Kenneth Castleton first visited and photo- doubtedly from campfires at the site. This is graphed the site on August 6, 1970, and accord- one reason why camping should be prohibited ing to his notes, he visited it again in April of in the area around the panel. 1973 (Castleton 1978:160161). Castleton de- Becoming thus aware of changes to the panel scribed the panel as follows: and its environment, I became interested in how Unfortunately, part of the cliff face has the panel was surviving the ravages of time and chipped away, thus damaging the figures. the ravages of people, which are certainly the The upper parts of two large red anthropo- most destructive. I have tried, therefore, to lo- morphic figures have been damaged by this cate old photographs of the panel for further weathering. One is a Fremont style figure with very broad shoulders, a tapered trunk, evaluation of these changes. These photo- and no extremities. It largely obscures anoth- graphs, and the changes they illustrate, are dis- er slender figure with "bug eyes". The other, cussed below. a Barrier Canyon Style figure, has a short Obtaining old photographs of the panel has right arm and is holding a snake, much in the proven difficult. Certainly, there must be older same manner as figures in the Head of Sinbad photographs than those discussed here. Perhaps and Horseshoe Canyon. To the left are two animals, one with a rectangular body decorat- publication of this article will lead to the dis- ed by a single white horizontal stripe through covery of older photographs that will yield ad- it. The second larger animal has a small head ditional information about the panel. without horns, a curved tail, and a vertical The site was first recorded by James H. Gun- white stripe through the fore part of the body. nerson, an archaeologist from the University of It resembles a quadruped in Barrier Canyon.
Recommended publications
  • Geology of U Rani Urn Deposits in Triassic Rocks of the Colorado Plateau Region
    Geology of U rani urn Deposits in Triassic Rocks of the Colorado Plateau Region By W. I. FINCH CONTRIBUTIONS TO THE GEOLOGY OF URANIUM GEOLOGICAL SURVEY BULLETIN 1074-D This report concerns work done on behalf ~1 the U. S. Atomic Energy Commission -Jnd is published with the permission of ~he Commission NITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printin~ Office Washin~ton 25, D. C. CONTENTS Page Abstract---------------------------------------------------------- 125 Introduction__ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 125 History of mining and production ____ ------------------------------- 127 Geologic setting___________________________________________________ 128 StratigraphY-------------------------------------------------- 129 ~oenkopiformation_______________________________________ ~29 Middle Triassic unconformity_______________________________ 131 Chinle formation__________________________________________ 131 Shinarump Inernber____________________________________ 133 ~udstone member------------------------------------- 136 ~oss Back member____________________________________ 136 Upper part of the Chinle formation______________________ 138 Wingate sandstone_________________________________________ 138 lgneousrocks_________________________________________________ 139 Structure_____________________________________________________
    [Show full text]
  • Iidentilica2tion and Occurrence of Uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals from the Colorado Plateaus
    IIdentilica2tion and occurrence of uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals From the Colorado Plateaus c By A. D. WEEKS and M. E. THOMPSON A CONTRIBUTION TO THE GEOLOGY OF URANIUM GEOLOGICAL S U R V E Y BULL E TIN 1009-B For jeld geologists and others having few laboratory facilities.- This report concerns work done on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE- INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan. Director Reprint, 1957 For sale by the Superintendent of Documents, U. S. Government Printing Ofice Washington 25, D. C. - Price 25 cents (paper cover) CONTENTS Page 13 13 13 14 14 14 15 15 15 15 16 16 17 17 17 18 18 19 20 21 21 22 23 24 25 25 26 27 28 29 29 30 30 31 32 33 33 34 35 36 37 38 39 , 40 41 42 42 1v CONTENTS Page 46 47 48 49 50 50 51 52 53 54 54 55 56 56 57 58 58 59 62 TABLES TABLE1. Optical properties of uranium minerals ______________________ 44 2. List of mine and mining district names showing county and State________________________________________---------- 60 IDENTIFICATION AND OCCURRENCE OF URANIUM AND VANADIUM MINERALS FROM THE COLORADO PLATEAUS By A. D. WEEKSand M. E. THOMPSON ABSTRACT This report, designed to make available to field geologists and others informa- tion obtained in recent investigations by the Geological Survey on identification and occurrence of uranium minerals of the Colorado Plateaus, contains descrip- tions of the physical properties, X-ray data, and in some instances results of chem- ical and spectrographic analysis of 48 uranium arid vanadium minerals.
    [Show full text]
  • Appendix L—Acec Evaluations for the Price Resource Management Plan
    Proposed RMP/Final EIS Appendix L APPENDIX L—ACEC EVALUATIONS FOR THE PRICE RESOURCE MANAGEMENT PLAN INTRODUCTION Section 202(c)(3) of the Federal Land Policy and Management Act (FLPMA) requires that priority be given to the designation and protection of areas of critical environmental concern (ACEC). FLPMA Section 103 (a) defines ACECs as public lands for which special management attention is required (when such areas are developed or used or when no development is required) to protect and prevent irreparable damage to important historic, cultural, or scenic values; fish and wildlife resources; or other natural systems or processes or to protect life and safety from natural hazards. CURRENTLY DESIGNATED ACECS BROUGHT FORWARD INTO THE PRICE RMP FROM THE SAN RAFAEL RMP In its Notice of Intent (NOI) to prepare this Resource Management Plan (RMP) (Federal Register, Volume 66, No. 216, November 7, 2001, Notice of Intent, Environmental Impact Statement, Price Resource Management Plan, Utah), BLM identified the 13 existing ACECs created in the San Rafael RMP of 1991. The NOI explained BLM’s intention to bring these ACECs forward into the Price Field Office (PFO) RMP. A scoping report was prepared in May 2002 to summarize the public and agency comments received in response to the NOI. The few comments that were received were supportive of continued management as ACECs. The ACEC Manual (BLM Manual 1613, September 29, 1988) states, “Normally, the relevance and importance of resource or hazards associated with an existing ACEC are reevaluated only when new information or changed circumstances or the results of monitoring establish a need.” The following discussion is a brief review of the existing ACECs created by the San Rafael RMP of 1991 and discussed in the Environmental Impact Statement (EIS).
    [Show full text]
  • Establishing the Geomorphic Context for Wetland and Riverine Restoration of the San Rafael River
    Final Report Establishing the geomorphic context for wetland and riverine restoration of the San Rafael River NRCS Cooperative Agreement #68-3A75-4-155 Stephen T. Fortney, John C. Schmidt, and David J. Dean Intermountain Center for River Rehabilitation and Restoration Department of Watershed Sciences Utah State University Logan, UT In collaboration with Michael E. Scott Julian Scott Fort Collins Science Center U. S. Geological Survey Fort Collins, CO March 22, 2011 1 Table of Contents I. Introduction 5 II. Purpose 5 III. Study Area 9 IV. Hydrology 11 V. Methods 18 A. Floodplain Stratigraphy 18 B. Repeat Photography: Aerial Imagery and Oblique Ground Photographs 19 C. USGS gage data 21 Reconstructed Cross Sections 21 Rating Relations 22 Time Series of Thalweg Elevation 22 Time Series of Width and Width-to-Depth Ratio 22 Hydraulic Geometry 22 D. Longitudinal Profile 24 E. Additional Activities 24 VI. Results: Channel Transformation on Hatt Ranch 26 Turn of the 20th century 26 1930s and 1940s 29 1950s 33 1960s and 1970s 41 1980s 46 1990s to present 49 Longitudinal Profile 50 VII. Summary 54 A. Channel Transformation on Hatt Ranch 54 B. Restoration and Management Implications 55 VIII. Expenditures 56 IX. Timeline 56 X. References 56 XI. Appendix 59 Table of Figures Figure 1. Oblique ground photos taken near the old Highway 24 bridge 6 Figure 2. Conceptual model of how watershed attributes control channel and floodplain form. 7 Figure 3. Conceptual model of restoration versus rehabilitation 8 Figure 4. Map of the San Rafael River watershed. 10 Figure 5. Map of the study area 11 Figure 6.
    [Show full text]
  • Download Date 06/10/2021 21:27:28
    Taphonomy of fossil plants in the Upper Triassic Chinle Formation. Item Type text; Dissertation-Reproduction (electronic) Authors Demko, Timothy Michael. Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 06/10/2021 21:27:28 Link to Item http://hdl.handle.net/10150/187397 INFORMATION TO USERS I This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print' bleed through, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back of the book. Photographs included in the original manuscript have been reproduced xerographically in this copy.
    [Show full text]
  • San Rafael Swell 3-4 Day
    San Rafael Swell 3-4 Day Zion, Bryce, Canyonlands, Arches, Natural Bridges, Dinosaur, Capital Reef, Grand Staircase... in a state brimming with national parks, it's easy to overlook another national treasure. Utah locals call it 'THE SWELL' a three thousand-foot fold of sandstone and shale on the edge of the Colorado Plateau. Its hidden canyons provided sanctuary to old west outlaw Butch Cassidy. Today the same red-wall canyons are your sanctuary from the everyday grind. You will ride back in time past abandoned mining camps and turn of the century ranches. Stop to explore cowboy camps, prehistoric Indian rock art, we might even see a few dinosaur prints. Your ride ends at the Wedge Overlook, Utah’s ‘Little Grand Canyon’. A thousand feet below, the San Rafael River counts another day in the eons… from above we count ourselves fortunate that such a place exists at all. SAMPLE ITINERARY One of the advantages of a bike trip is the flexibility of the daily itinerary. It can vary widely from one trip to the next based on ​ group desires, Mother Nature, and courtesy for other groups on the trail. The “Swell” is well known for its spectacular scenery and ​ abundance of historical sites. Dispersed camping offers the ultimate opportunity for choose your own adventure exploration of the vast maze of old mining roads and slot canyons. Expect to ride 20-30 miles per day. Day 1: Meet at Holiday River Expeditions headquarters in Green River, Utah. A one and one-half hour van ride takes us to Temple Mountain​ .
    [Show full text]
  • Bureau of Land Management Mineral Potential Report Price Field Office, Utah 2002
    Bureau of Land Management Mineral Potential Report Price Field Office, Utah 2002 1. INTRODUCTION 1.1 PURPOSE AND SCOPE The purpose of this report is to assess the mineral resource occurrence and development potential of all lands managed by the U.S. Bureau of Land Management’s (BLM’s) Price Field Office in Carbon and Emery Counties, Utah. This assessment involved reviewing both published and unpublished data, and selecting pertinent information for use in the report. Identified mineral resources are classified according to the BLM system described in Manual 3031 (BLM, 1985) and Manual 3060 (BLM, 1994). As used in this report, the term mineral includes any earth material that is considered an economic commodity. The Price Field Office is currently revising and combining the Price River Resource Area Management Framework Plan (MFP), and the San Rafael Resource Management Plan (RMP), into a new management plan to be called the Price Field Office RMP. As part of the RMP, the BLM is required to prepare a Mineral Potential Report describing the occurrence and development potential of economic mineral commodities in the planning area. Once complete, this Mineral Potential Report will become incorporated into the broader RMP to provide decision makers with a better understanding of the mineral resources in the area, and the importance of those resources in the context of future land use allocations. Prior to the restructuring of the BLM in the mid-1990’s, the northern portion of the planning area was previously managed as the Price River Resource Area, while the southern area was designated the San Rafael Resource Area.
    [Show full text]
  • Recreation Guide to the San Rafael Area – Moab Area Travel Council - 7/11/06 Page 1
    Recreation Guide to the San Rafael Area – Moab Area Travel Council - 7/11/06 Page 1 include tent pads, picnic tables, toilets, Areas South of 1-70 and fire rings. No drinking water is Recreation Guide to the available. When camping at other areas, 5. Head of Sinbad / Swasey's Cabin San Rafael Area please use existing undeveloped campsites to avoid impacting new areas. Just off 1-70, the Head of Sinbad area invites camping, hiking, and exploring. 2. Wedge Overlook The elements have molded the buff- colored sandstone into pocketed The Wedge Overlook provides a striking watchtowers and other fanciful shapes. Moab Area Travel Council view of the Little Grand Canyon, the San Internet Brochure Series Rafael River, and the Sid's Mountain Members of the Swasey family first Available from: Wilderness Study Area. To protect the grazed livestock in the area in the late fragile resources, notably an endangered 1800's. Today visitors may see the log discovermoab.com cactus species, use of motorized vehicles cabin they built in 1921. Listed on the and mountain bikes is limited to Utah State Register of Historic Sites, the designated roads and camping is limited cabin can be reached from 1-70 from to designated sites. To visit the overlook, ranch exit 129. Head west and south from INTRODUCTION drive from the town of Cleveland south exit 129 for four miles. Turn right and towards the San Rafael Recreation Site. continue for 1.1 miles. Turn right again Continue beyond the Buckhorn Reservoir and travel in a northwesterly direction for The San Rafael Swell, 2,000 square miles just over four miles to the water tank at about four miles.
    [Show full text]
  • Spcoll Energy Tel 328A (F
    SpColl Energy TEl 328A (f/ r.=== UNITED STATES GEOLOGICAL SURVEY TEI-328A / GEOLOGIC ASPECTS OF THE RESOURCE APPRAISAL OF URANIUM DEPOSITS IN PRE-MORRISON FORMATIONS OF THE COLORADO PLATEAU: An Interim Report By W. I. Finch This preliminary report Is released without editorial and technical review for conformity with official standards and nomenclature, to make the information available to interested organizations and to stimulate the search for uranium deposits. May 1953 II ... ,..... , ............. ,,N., '" .. UNITED STATES ATOMIC ENERGY COMMISSION Technical Information Service, Oak Ridge, Te!!nALL~ ~·· ·-- ·--:~ ~~r0-:: Lc~if;;.·~·:;·. GEOLOGY AND MINERALOGY This report has been reproduced direct from copy as submitted to the Technical Information Service. Arrangements for reproduction of this document in whole or in part should be made directly with the author and the organiza­ tion he represents. Such reproduction is encouraged by the United States Atomic Energy Commission. 2 AEC, oak Ridge, Tenn.,-W36235 3 CONTENTS Page c Abstract c 5 Introduction 8 Geologic setting • 10 Stratigraphy c 0 • • 10 Moenkopi formation 0 • • 10 Shinarump conglomerate ' 13 Chinle formation ' ' • • ' • • • 15 Structure and igneous rocks 0 • • 16 Ore deposits , c 0 ' ' . • • • 17 Mineralogy • 0 0 17 Principal uranium minerals 17 Vanadium and copper minerals ' 18 Other minerals ' 18 ,, Types of deposits 0 0 • 18 Vanadium-uranium deposits • 0 19 Copper-uranium deposits 0 ' • 19 Uranium deposits 0 • • • • • 20 Habits of uranium ore deposits 0 0 20 • ' • Guides to ore deposits 0 0 22 ' • Thickening of beds 0 • ' 22 Alteration of mudstone and underlying beds • 23 Carbonaceous material • • • 0 23 Other guides , , 0 • 0 0 • • • • • " 24 Comparison of uranium deposits in Shinarump and Morrison formations 0 .
    [Show full text]
  • Geology and Uranium Deposits of the Temple Mountain District Emery County, Utah
    Geology and Uranium Deposits of the Temple Mountain District Emery County, Utah By C. C. HAWLEY, D. G. WYANT, and D. B. BROOKS GEOLOGICAL SURVEY BULLETIN 1192 Prepared on behalf of the U.S. Atomic Energy Commission RECEIVED MAY 91966 I.U.J. LIMSVUU. IY. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 196S UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director Library of Congress catalog-card No. GS 65-310. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract__ _____________________________________________________ 1 Introduction._____________________________________________________ 3 Geography _____ _______________________________________ 4 History of mining operations and production._____________________ 6 Previous geologic work_________________________________.___-___ 9 Fieldwork and acknowledgments._______________________________ 12 Analyses._-_________-______-__-_-_-^-___--__-_--____-___-__-__-_- 13 Geology.__.__..________...._______________ 15 Stratigraphy._________________________________________________ 15 Permian System_________________________________________ 15 Triassic and Jurassic Systems.______________________________ 16 Moenkopi Fonnation_________-______-____--______---__ 16 Chinle Formation_________--.__________-____-----__- 18 Temple Mountain and Monitor Butte Members.--..-- 18 Moss Back Member....___________________________ 20 Church Rock Member...__-___------_-_-_ _. 29 Wingate Sandstone_--__-__----_-_-__-_---_---__-------
    [Show full text]
  • Finished Guide.Indd
    The SAN RAFAEL COUNTRY Travel Guide Experience The Roads Less Traveled SAN RAFAEL COUNTRY E M E R Y C O U N T Y ® ®® ® www.sanrafaelcountry.com TABLE OF CONTENTS AREA INFORMATION Emergency Numbers Introduction, Precautions, & Important Info. p. 3 Calendar of Events p. 4 Emery County Sheri! : Emergency 911 San Rafael Country App p. 5 Green River 435-564-8111 Museums & Information Centers p. 6 Castle Dale 435-381-2404 Golf Courses p. 7 State Parks p. 8 & 9 Utah Highway Patrol: Emergency 911 Utah State Route 10 p. 10-12 Green River 435-564-3474 Huntington Canyon p. 13 Miller Flat p. 14 Medical Centers: Green River 435-564-3434 Joe’s Valley p. 15 Castle Dale 435-381-2305 Cleveland - Lloyd Dinosaur Quarry p. 16 Cedar Mountain p. 17 Hospital: Old Rail Road Grade Road p. 18 Price 435-637-4800 Wedge Overlook p. 19 Bureau of Land Management: Cottonwood Wash/Buckhorn Wash p. 20 & 21 Price 435-636-3600 Interstate 70 p. 22 Black Dragon Wash p. 23 Forest Service: Ferron 435-384-2372 Little Wild Horse Road p. 24 Price 435-637-2817 Goblin Valley State Park Road p. 25 Heart of Sinbad Road p. 26 Road Department: Behind the Reef Road p. 27 Green River 435-564-3574 Castle Dale 435-381-2550 McKay Flat/Hondu Arch Road p. 28 Hidden Splendor Road p. 29 Reds Canyon Road p. 30 Rod’s Valley p. 31 Swasey’s Cabin p. 32 Dutchman’s Arch/Head of Sinbad p. 33 Moore Cuto! Road p. 34 Rochester Creek Rock Art p.
    [Show full text]
  • Geologic Resource Evaluation Report, Canyonlands National Park
    National Park Service U.S. Department of the Interior Natural Resource Program Center Canyonlands National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2005/003 Canyonlands National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2005/003 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2005 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.
    [Show full text]