Utah G E Ological Mineral Survey
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2014 Utah State Comprehensive Outdoor Recreation Plan 2014 Utah
2014 Utah State Comprehensive Outdoor Recreation Plan UTAH STATE PARKS Division of Utah State Parks and Recreation Planning Section 1594 West North Temple, Ste. 116 P.O. Box 146001 Salt Lake City, UT 84116-6001 (877) UT-PARKS stateparks.utah.gov State of Utah Figure 1. Public land ownership in Utah. ii 2014 SCORP ACKNOWLEDGEMENTS The research and publication of the 2014 Utah State Comprehensive Outdoor Recreation Plan (SCORP) is a product of a team effort. The Utah Department of Natural Resources, Division of Utah State Parks and Recreation, Utah Division of Wildlife Resources, Utah Department of Transportation, Utah Division of Water Resources, Governor’s Office of Planning and Budget, National Park Service (Omaha Regional Office), U.S. Department of Agriculture Forest Service, U.S. Department of the Interior Bureau of Land Management, U.S. Department of the Interior Bureau of Reclamation, Utah League of Cities and Towns, Utah Association of Counties, Utah Recreation and Parks Association, and others provided data, information, advice, recommendations, and encouragement. The 2014 Utah SCORP was completed under contract by BIO-WEST, Inc. (BIO-WEST), with survey work completed by Dan Jones & Associates. Key project contributors include Gary Armstrong, project manager for BIO-WEST, and David Howard, lead survey research associate for Dan Jones & Associates. Susan Zarekarizi of the Division of Utah State Parks and Recreation served as the overall project manager and provided contractor oversight. Additional staff contributing to the project include Sean Keenan of BIO-WEST, and Tyson Chapman and Kjersten Adams of Dan Jones & Associates. The 2014 Utah SCORP represents demand for future recreation facilities as identified in a series of public opinion surveys, special reports, park surveys, federal and local plans, technical reports, and other data. -
B2158 Pt 19 Text Copy
Previous section Volume contents Appendix A Around the Henry Mountains with Charlie Hanks, Some Recollections By Charles B. Hunt1 It was my good fortune in 1935 to be assigned chief of a U.S. Geological Survey field party studying and mapping the geology of the Henry Mountains, Utah (fig. 1). Geolog- ically the area is of great interest because of the classic work done there in 1876 by G.K. Gilbert for the Powell Survey. In the 1930’s the area still was frontier (fig. 2)—a long distance from railroads, paved roads, telephones, stores, or medical services. It was the heart of an area the size of New York State without a railroad, and a third of that area was without any kind of a road. This was not Marlboro country; it was Bull Durham country. The geological work had to be done by pack train (fig. 3); it was about the last of the big pack- train surveys in the West—the end of an era. It was my good fortune also to obtain the services of a veteran horseman who knew that country, Charles R. Hanks of Green River, Utah (fig. 4). Charlie served as packer dur- ing each of our five field seasons there. He had played a leading role in the history of the area; the town of Hanks- ville was named (1885) for his father when a post office was established there. Charlie, an old-time cow puncher, had spent more hours in saddles than he had in chairs, and he had slept more nights on the ground under the stars than he had in bed under a roof. -
The Laccolith-Stock Controversy: New Results from the Southern Henry Mountains, Utah
The laccolith-stock controversy: New results from the southern Henry Mountains, Utah MARIE D. JACKSON* Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland 21218 DAVID D. POLLARD Departments of Applied Earth Sciences and Geology, Stanford University, Stanford, California 94305 ABSTRACT rule out the possibility of a stock at depth. At Mesa, Fig. 1). Gilbert inferred that the central Mount Hillers, paleomagnetic vectors indi- intrusions underlying the large domes are Domes of sedimentary strata at Mount cate that tongue-shaped sills and thin lacco- floored, mushroom-shaped laccoliths (Fig. 3). Holmes, Mount Ellsworth, and Mount Hillers liths overlying the central intrusion were More recently, C. B. Hunt (1953) inferred that in the southern Henry Mountains record suc- emplaced horizontally and were rotated dur- the central intrusions in the Henry Mountains cessive stages in the growth of shallow (3 to 4 ing doming through about 80° of dip. This are cylindrical stocks, surrounded by zones of km deep) magma chambers. Whether the in- sequence of events is not consistent with the shattered host rock. He postulated a process in trusions under these domes are laccoliths or emplacement of a stock and subsequent or which a narrow stock is injected vertically up- stocks has been the subject of controversy. contemporaneous lateral growth of sills and ward and then pushes aside and domes the sed- According to G. K. Gilbert, the central intru- minor laccoliths. Growth in diameter of a imentary strata as it grows in diameter. After the sions are direct analogues of much smaller, stock from about 300 m at Mount Holmes to stock is emplaced, tongue-shaped sills and lacco- floored intrusions, exposed on the flanks of nearly 3 km at Mount Hillers, as Hunt sug- liths are injected radially from the discordant the domes, that grew from sills by lifting and gested, should have been accompanied by sides of the stock (Fig. -
Reconnaissance of the Northwest Rim of the Colorado River Basin
RME -77(Pt. ~ ) / Subject Category :' GEOLOGY 'AND MINERA,LOGY U NI TED STATES ATOMIC ENERGY COMM I SSION RECONN.AISS ...-lliCE OF THE NORTHWEST RIM OF THE COLORADO RIVER BASIN, WAYNE AND GARFIELD COUNTIES, UTAH By Robert C. Ge rhard January 1955 Exploration Division Grand J unct ion Operations Office Grand Junction, Colorado Tech n ic a l In formation Ser v i ce Oak. R i dge Te n nes s ee UNCLASSI FI ED I. REC (o NNA l qSA CE OF THE NORYrI1rJEST Rill OF' THE- COLORA OO RIVER BASIN, .. WAYNE AND GARFIELD COUN TIES, UTAH . .- ABSTRACT About five mont hs ' f:eld work was devoted to examining the Salt Wash and Mossback outcrops i n a 1,0 O-square--mile area along the north-" . west r"JTl of 'thE; Co oraclo River, Wayne and Garfield Counties, Utah.- In the Little Rockies district, oxidized d~posits of vanadium- . _ uranium ore, associated chiefl ; with ca r bonized wood, logs, and plant '. "~. fragments, occur in extremely small lenses in two horizons of the Salt ~~: Wash member of t he Morrison f ormation. Beca use of the small l~ri tic ular : .~. nature of presently known or ebodies, ?hysical ~xploration in t his dist r1c t ~ ~ does not now appear to be econOIll:..ca.J..J.Y f easible. 0 -' • __ - . .. "In the Sout he rn Green River Desert, urap.ium m:i.n era liz~tion a Ssc 'cia ted.} ~ ~'~:' ~ ~' with carbon trash, asphaltite, and copper mi nerals occurs in the lower " -~ .: Mossback channel unit fillino paleochannels cut into the Moenkopi for.mation ~ -:-" .. -
Triangulation in Utah 1871-1934
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 913 TRIANGULATION IN UTAH 1871-1934 J. G. STAACK Chief Topographic Engineer UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1940 Tor sale by the Superintendent of Documents, Washington, D. C. Price 20 cents (paper) CONTENTS Page Introduction ______________________________________________________ 1 Scope of report------__-_-_---_----_------------ --__---__ _ 1 Precision __ _ ________________________ _ __________________ _ ___ 1 Instruments used._ _ _ _ _ _ _ _ _ 2 Station marks___- _ _.__ __ __ _ 2 Datum_-_-_-__ __________________________ ______ ______-___.__ 3 Methods of readjustment..._____.-.__..________.___._._...___.__ 4 Form of results__-.________________________ _.___-_____.______ 5 Arrangement__.______________________________ _ ___ _ ________ 6 Descriptions of stations._______________________________________ 6 Azimuths and distances.__ ____-_.._---_--_________ -____ __ __ ^ 7 Maps.__----__-----_-_---__-_--_-___-_-___-__-__-_-_-___.-.__ 7 Personnel_ _ __-----_-_-_---_---------_--__-____-__-_.--_.___ . 7 Projects 9 Uinta Forest Reserve, 1897-98_ 9 Cottonwood and Park City special quadrangles, 1903____ _ 19 Iron Springs special quadrangle, 1905____________________________ 22 Northeastern Utah, 1909.. -_. 26 Eastern Utah, 1910 - . 30 Logan quadrangle, 1913._________-__-__'_--______-___:_____.____ 42 Uintah County, 1913___-__. 48 Eastern Utah, 1914.. ... _ _ .. 55 Northern Utah, 1915 (Hodgeson)_____-___ __-___-_-_-__-_--. _. 58 Northern Utah, 1915 <Urquhart)_. -
Wilderness Study Areas
I ___- .-ll..l .“..l..““l.--..- I. _.^.___” _^.__.._._ - ._____.-.-.. ------ FEDERAL LAND M.ANAGEMENT Status and Uses of Wilderness Study Areas I 150156 RESTRICTED--Not to be released outside the General Accounting Wice unless specifically approved by the Office of Congressional Relations. ssBO4’8 RELEASED ---- ---. - (;Ao/li:( ‘I:I)-!L~-l~~lL - United States General Accounting OfTice GAO Washington, D.C. 20548 Resources, Community, and Economic Development Division B-262989 September 23,1993 The Honorable Bruce F. Vento Chairman, Subcommittee on National Parks, Forests, and Public Lands Committee on Natural Resources House of Representatives Dear Mr. Chairman: Concerned about alleged degradation of areas being considered for possible inclusion in the National Wilderness Preservation System (wilderness study areas), you requested that we provide you with information on the types and effects of activities in these study areas. As agreed with your office, we gathered information on areas managed by two agencies: the Department of the Interior’s Bureau of Land Management (BLN) and the Department of Agriculture’s Forest Service. Specifically, this report provides information on (1) legislative guidance and the agency policies governing wilderness study area management, (2) the various activities and uses occurring in the agencies’ study areas, (3) the ways these activities and uses affect the areas, and (4) agency actions to monitor and restrict these uses and to repair damage resulting from them. Appendixes I and II provide data on the number, acreage, and locations of wilderness study areas managed by BLM and the Forest Service, as well as data on the types of uses occurring in the areas. -
Download It FREE Today! the SKI LIFE
SKI WEEKEND CLASSIC CANNON November 2017 From Sugarbush to peaks across New England, skiers and riders are ready to rock WELCOME TO SNOWTOPIA A experience has arrived in New Hampshire’s White Mountains. grand new LINCOLN, NH | RIVERWALKRESORTATLOON.COM Arriving is your escape. Access snow, terrain and hospitality – as reliable as you’ve heard and as convenient as you deserve. SLOPESIDE THIS IS YOUR DESTINATION. SKI & STAY Kids Eat Free $ * from 119 pp/pn with Full Breakfast for Two EXIT LoonMtn.com/Stay HERE Featuring indoor pool, health club & spa, Loon Mountain Resort slopeside hot tub, two restaurants and more! * Quad occupancy with a minimum two-night Exit 32 off I-93 | Lincoln, NH stay. Plus tax & resort fee. One child (12 & under) eats free with each paying adult. May not be combined with any other offer or discount. Early- Save on Lift Tickets only at and late-season specials available. LoonMtn.com/Tickets A grand new experience has arrived in New Hampshire’s White Mountains. Arriving is your escape. Access snow, terrain and hospitality – as reliable as you’ve heard and as convenient as you deserve. SLOPESIDE THIS IS YOUR DESTINATION. SKI & STAY Kids Eat Free $ * from 119 pp/pn with Full Breakfast for Two EXIT LoonMtn.com/Stay HERE Featuring indoor pool, health club & spa, Loon Mountain Resort slopeside hot tub, two restaurants and more! We believe that every vacation should be truly extraordinary. Our goal Exit 32 off I-93 | Lincoln, NH * Quad occupancy with a minimum two-night stay. Plus tax & resort fee. One child (12 & under) is to provide an unparalleled level of service in a spectacular mountain setting. -
B2158 Pt 08 Text
Previous section Volume contents Processes of Laccolithic Emplacement in the Southern Henry Mountains, Southeastern Utah By Marie Jackson1 CONTENTS References Cited............................................................................................................. 27 FIGURES 1. Simplified geologic map of the south Henry Mountains .......................................... 52 2. Interpretive radially oriented cross sections through Mounts Holmes, Ellsworth, and Hillers ................................................................................................................. 54 3. Zijderveldt plots showing the progressive demagnetization of a diorite porphyry sample from sill A in cross section C–C′.................................................................. 56 4. G.K. Gilbert’s concept of laccoliths in Henry Mountains ........................................ 56 5. Structure contour maps and cross sections of Mounts Holmes, Ellsworth, and Hillers, illustrating C.B. Hunt’s concept of relationships between the stocks and uplifts of the beds ............................................................................................... 57 6. Vertical cross sections showing states in growth of central intrusions and domes in the Henry Mountains ................................................................................. 58 A sequence of sedimentary rocks about 4 km thick was New geologic mapping (Jackson and Pollard, 1988) bent, stretched, and uplifted during the growth of three igne- demonstrates that the sedimentary -
Historic, Archived Document Do Not Assume Content Reflects Current
Historic, archived document Do not assume content reflects current scientific knowledge, policies, or practices. BULLETIN No. 23. ' U. S. DEPARTMENT OF AGRICULTURE, DIVISION OF AGROSTOLOGY/ [Grass and Forage Plant Investigation**] STUDIES ON AMEKICAN GRASSES. A REVISION OF THE NORTH AMERICAN SPECIES OF BROMUS OCCURRING NORTH OF MEXICO. CORNELIUS L. SHEAR, Assistant Agrostologist. PREPARED UNDER THE DIRECTION OF F. LAMSON-SCRIBNER, AGROSTOLOGIST. V ISSXJE1D JTTLY 3, 19OO. ¥* WASHINGTON: GOVERNMENT PRINTING OFFICE. 1900, > ' -r '-' ' BULLETIN NO. 23. Agros. 65. U. S. DEPARTMENT OF AGRICULTURE, DIVISION OF AGKQSTOLOGY. [Gra§§ and Forage Plant Investigations.] STUDIES ON AMEKICAN GKASSES. A REVISION OF THE NORTH AMERICAN SPECIES OF BROMUS OCCURRING NORTH OF MEXICO. CORNELIUS L. SHEAR, Assista7it Agrostologist. PREPARED UNDER THE DIRECTION OF F. LAMSON-SCRIBNER, AGROSTOLOGIST. ISSTJIED JULY 3, 19OO. WASHINGTON: GOVERNMENT PRINTING OFFICE. 1900. LETTER OF TRANSMITTAL U. S. DEPARTMENT OF AGRICULTURE, DIVISION OF AGROSTOLOGY, Washington, D. C., April 9, 1900. SIR: I have the honor to transmit herewith the manuscript of a paper entitled A Revision of the North American Species of Bromus Occurring North of Mexico, prepared under my direction by Mr. Cor- nelius L. Shear, assistant agrostologist, and recommend the same for publication as Bulletin No. 23 of this division, under the general title of " Studies on American Grasses." The abundance of good material collected during the past few years in the Rocky Mountains and the Northwest has shown the necessity of a revision of the genus Bromus. Until very recently good specimens from these regions have been few, and their identification has rested in many cases on tradition and misconceptions of the species. -
USGS Miscellaneous Field Studies Map 2329, Pamphlet
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP MF-2329 U.S. GEOLOGICAL SURVEY MAP SHOWING INVENTORY AND REGIONAL SUSCEPTIBILITY FOR HOLOCENE DEBRIS FLOWS AND RELATED FAST-MOVING LANDSLIDES IN THE CONTERMINOUS UNITED STATES By Earl E. Brabb, Joseph P. Colgan, and Timothy C. Best INTRODUCTION Debris flows, debris avalanches, mud flows, and lahars are fast-moving landslides that occur in a wide variety of environments throughout the world. They are particularly dangerous to life and property because they move quickly, destroy objects in their paths, and can strike with little warning. U.S. Geological Survey scientists are assessing debris-flow hazards and developing real-time techniques for monitoring hazardous areas so that road closures, evacuations, or corrective actions can be taken (Highland and others, 1997). According to the classifications of Varnes (1978) and Cruden and Varnes (1996), a debris flow is a type of slope movement that contains a significant proportion of particles larger than 2 mm and that resembles a viscous fluid. Debris avalanches are extremely rapid, tend to be large, and often occur on open slopes rather than down channels. A lahar is a debris flow from a volcano. A mudflow is a flowing mass of predominantly fine-grained material that possesses a high degree of fluidity (Jackson, 1997). In the interest of brevity, the term "debris flow" will be used in this report for all of the rapid slope movements described above. WHAT CAUSES DEBRIS FLOWS? Debris flows in the Appalachian Mountains are often triggered by hurricanes, which dump large amounts of rain on the ground in a short period of time, such as the November 1977 storm in North Carolina (Neary and Swift, 1987) and Hurricane Camille in Virginia (Williams and Guy, 1973). -
The Yellowstone Paleontological Survey
E PALEONT ON O T LO S G W I O C L A L L E National Y Park The Yellowstone Service Department of the Interior Paleontological Survey SURVEY Vincent L. Santucci Yellowstone Center for Resources National Park Service Yellowstone National Park, Wyoming YCR-NR-98-1 1998 How to cite this document: Santucci, V. L. 1998. The Yellowstone Paleontological Survey. Yellowstone Center for Resources, National Park Service, Yellowstone National Park, Wyoming,YCR-NR-98-1. Current address for Vincent L. Santucci is National Park Service, P.O. Box 592, Kemmerer, WY 83101. The Yellowstone Paleontological Survey To Lt. Col. Luke J. Barnett, III “Uncle by blood, brother in spirit!” Vincent L. Santucci Yellowstone Center for Resources National Park Service Yellowstone National Park, Wyoming YCR-NR-98-1 1998 Table of Contents Introduction .................................................................................................... 1 Stratigraphy .................................................................................................... 4 Fossil Chronology........................................................................................... 6 Taxonomy ..................................................................................................... 12 Localities ...................................................................................................... 15 Interpretation ................................................................................................ 19 Paleontological Resource Management....................................................... -
Wasatch Mountain Club SEPTEMBER
Wasatch Mountain Club SEPTEMBER VOLUME 70, NUMBER 9, SEPTEMBER 1993 Printed on 100% Recycled Paper The JR it m b Re r MEMBERSHIP & RAMBLER INFORMATION Managing Editors MEMBERS: If you have moved, please notify the WMC Jean Frances, Christine Allred Membership Director, 888 South 200East,Suite 207, Salt Lake City, UT 84111-4220, of your new address. ADVERTISING: ........ Knick Knickerbocker If you did not receive your RAMBLER, contact the CLASSIFIED ADS: .... Sue de Vall COVER LOGO: .......... Knick Knickerbocker Membership Director to make sure your address is in the MAILING: .................. Christine Allred Club computer correctly. PRODUCTION: .......... Jean Frances and IF YOU WANT TO SUBMIT AN ARTICLE: Articles ..................................... Christine Allred must be typed double spaced or on a floppy disk with a hard copy, also doubled spaced, and received by 6:00 pm on the The office will generally be staffed from 9 am to 15th of the month preceding publication. Drop articles off 2 pm on Tuesdays and Thursdays by Carol Rauba. in the WMC office mail slot (Mon.-Fri.-8 am to 5 pm) or Office phone number-363-7150. mail or deliver to Editors' Blue Box at 5352 Old Trenton Way, Murray, 84123. Pick up of disks at same address but in Red Box. Include your name and phone number on all THE RAMBLER (USPS 053-410) is published monthly by submissions. the WASATCH MOUNTAIN CLUB, Inc., 888 South 200 East, Suite 207, Salt Lake City, UT 84111-4220. Telephone: IF YOU WANT TO SUBMIT A PHOTO: We welcome 363-7150. Subscription rates of $12.00 per year are paid for photos of all kinds: black & white prints, color prints, and by membership dues only.