Acid Deposition in Utah: an Analysis by the Acid Deposition Technical Advisory Committee
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Parker Mountain Adaptive Resources Management Group
2006 ANNUAL REPORT PARKER MOUNTAIN ADAPTIVE RESOURCE MANAGEMENT GROUP (PARM) Cooperators Parker Mountain Grazing Association U. S. Bureau of Land Management U. S. Fish and Wildlife Service U. S. Forest Service U.S.D.A. Farm Services Agency U.S.D.A. Natural Resource Conservation Service U.S.D.A. Wildlife Services Utah Agricultural Experiment Station Utah Department of Agriculture and Food Utah Department of Natural Resources Utah Division of Wildlife Resources Utah Farm Bureau Federation Utah School and Institutional Trust Lands Administration Utah State University, Vice President for Research Utah State University, Vice President for Extension Wayne and Piute County Commissions Prepared by David Dahlgren, Michael Guttery, Michael Monsen, and Terry Messmer Quinney Professorship for Wildlife Conflict Management Jack H. Berryman Institute Department of Wildland Resources Utah State University, Logan Verl Bagley Utah State University Extension Service Wayne and Piute County Extension Office January 2007 -1- Table of Contents Page Introduction .......................................................................................................................3 Background ...........................................................................................................3 Objectives ...............................................................................................................3 Sage-grouse Research .......................................................................................................4 Sage-grouse Biology -
A History of Beaver County, Utah Centennial County History Series
A HISTORY OF 'Beaver County Martha Sonntag Bradley UTAH CENTENNIAL COUNTY HISTORY SERIES A HISTORY OF 'Beaver County Martha Sonntag Bradley The settlement of Beaver County began in February 1856 when fifteen families from Parowan moved by wagon thirty miles north to Beaver Valley. The county was created by the Utah legislature on 31 January 1856, a week before the Parowan group set out to make their new home. However, centuries before, prehistoric peoples lived in the area, obtaining obsidian for arrow and spear points from the Mineral Mountains. Later, the area became home to Paiute Indians. Franciscan Friars Dominguez and Escalante passed through the area in October 1776. The Mormon settlement of Beaver devel oped at the foot of the Tushar Mountains. In 1859 the community of Minersville was es tablished, and residents farmed, raised live stock, and mined the lead deposits there. In the last quarter of the nineteenth century the Mineral Mountains and other locations in the county saw extensive mining develop ment, particularly in the towns of Frisco and Newhouse. Mining activities were given a boost with the completion of the Utah South ern Railroad to Milford in 1880. The birth place of both famous western outlaw Butch Cassidy and inventor of television Philo T. Farnsworth, Beaver County is rich in history, historic buildings, and mineral treasures. ISBN: 0-913738-17-4 A HISTORY OF 'Beaver County A HISTORY OF Beaver County Martha Sonntag Bradley 1999 Utah State Historical Society Beaver County Commission Copyright © 1999 by Beaver County Commission All rights reserved ISBN 0-913738-17-4 Library of Congress Catalog Card Number 98-61325 Map by Automated Geographic Reference Center—State of Utah Printed in the United States of America Utah State Historical Society 300 Rio Grande Salt Lake City, Utah 84101-1182 Contents ACKNOWLEDGMENTS vii GENERAL INTRODUCTION ix CHAPTER 1 Beaver County: The Places That Shape Us . -
1992 Utah Fishing Proclamation
m ftroiG wm "t let erkLte^ "IHferae you won't let go ®fl Wfo(B ttrout! The largest fish ever taken on a rod and reel, a 3,427 pound great white shark, was caught on Berkley Trilene — America's best selling fishing Rtf*rlrlctir line! SPORTSCASTLE SANDY PRICE 5600 S. 9th E., Murray 838 E. 9400 S. 730 W. Prive River Rd. 263-3633 571-8812 637-2077 ZCMICENTER CEDAR CITY SUGARHOUSE 2nd Level ZCMI Center 606 S. Main 1171 East 2100 So.. 359-4540 586-0687 487-7726 VERNAL OGDEN CITY MALL ROY 872 W. Main 24th & Washington 5585 So. 1900 W. 789-0536 399-2310 776-4453 FAMILY CENTER PROVO/UNIV. MALL ROCK SPRINGS 5666 S. Redwood Rd. 1300 S. State 1371 Dewar Drive SPORTING GOODS COMPANY 967-9455 224-9115 307-362-4208 ON THE COVER "Snagged"by Luke Frazier, oil, 16"x CONTENTS 20". J99I, To learn more about Frazier and his art work, turn to page 60, INTRODUCTION Strawberry Recreation Area Loyal Clark, US Forest Service 35 One of the most exciting Director's Message Scofield Reservoir/What the Timothy H. Provan, Director Future Holds Kevin Christophereon, things about fishing is its Division of Wildlife Resources 2 unpredictability, You simply Southeast Region Fisheries Manager 37 Utah's 1992 Fishing Season don't kno w when that big Why Rainbow Trout? Bruce Schmidt, Fisheries Chief 3 Joe Valentine, Assistant Fisheries one is going to strike, it Chief (Culture) ........39 could be on your next cast! 1992 FISHING RULES Willard Bay Shad 1992 Fishing Rules: Purpose Thomas D. -
Hydrology and Ground-Water Conditions of the Tertiary Muddy Creek Formation in the Lower Virgin River Basin of Southeastern Neva
HYDROLOGY AND GROUND-WATER CONDITIONS OF THE TERTIARY MUDDY CREEK FORMATION IN THE LOWER VIRGIN RIVER BASIN OF SOUTHEASTERN NEVADA AND ADJACENT ARIZONA AND UTAH Geological Society of America 2002 Rocky Mountain Section Annual Meeting Cedar City, Utah May 10, 2002 FIELD TRIP LEADERS By Michael Johnson, Virgin Valley Water District, Mesquite, NV 89027 500 Riverside Road (702) 346-5731 Gary L. Dixon, Southwest Geology, Inc., Blackfoot, ID 83221 Peter D. Rowley, Geologic Mapping, Inc., New Harmony, UT 84757 Terry C. Katzer, Cordilleran Hydrology, Inc., Reno, NV 89511 Michael Winters, Virgin Valley Water District, Mesquite, Nevada 89027 284 HYDROLOGY AND GROUND-WATER CONDITIONS OF THE TERTIARY MUDDY CREEK FORMATION IN THE LOWER VIRGIN RIVER BASIN OF SOUTHEASTERN NEVADA AND ADJACENT ARIZONA AND UTAH Geological Society of America 2002 Rocky Mountain Section Annual Meeting Cedar City, Utah May 10, 2002 FIELD TRIP LEADERS By Michael Johnson, Virgin Valley Water District, Mesquite, NV 89027 Gary L. Dixon, Southwest Geology, Inc., Blackfoot, ID 83221 Peter D. Rowley, Geologic Mapping, Inc., New Harmony, UT 84757 Terry C. Katzer, Cordilleran Hydrology, Inc., Reno, NV 89511 Michael Winters, Virgin Valley Water District, Mesquite, NV 89027 ABSTRACT The lower Virgin River Basin is a complex structural basin formed by Neogene extension in Nevada, Arizona, and Utah. There is a large volume of ground water in transient storage moving through the basin. Ongoing investigations to characterize the basin have determined that it is one of the deepest in the Basin and Range Province. The estimated depth to basement underlying the carbonate rock may be as great as 5 miles. -
Trail Development in the Lake Mountains, North Oquirrh
U.S. Department of the Interior Bureau of Land Management April 2021 Trail Development in the Lake Mountains, North Oquirrh Management Area and Rose and Yellow Fork Canyons DOI-BLM-UT-W010-2020-0007-EA Environmental Assessment Cost Estimate $ 9,960.00 Salt Lake Field Office 2370 South Decker Lake Boulevard West Valley City, Utah 84119 Phone: (801) 977-4300 Fax: (801) 977i -4397 Table of Contents Chapter 1. Purpose & Need ............................................................................................................ 4 1.1 Background ........................................................................................................................... 4 1.2 Purpose and Need ................................................................................................................. 6 1.2.1 Decision to be Made ...................................................................................................... 6 1.3 Conformance with BLM Land Use Plan(s) .......................................................................... 6 1.4 Relationship to Statutes, Regulations, or Other Plans .......................................................... 7 1.5 Identification of Issues ........................................................................................................ 10 1.5.1 Issues Analyzed in Detail ............................................................................................. 11 1.5.2 Issues Not Analyzed in Detail..................................................................................... -
Preliminary Geologic Map of the Enterprise Quadrangle, Washington and Iron Counties, Utah
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY PRELIMINARY GEOLOGIC MAP OF THE ENTERPRISE QUADRANGLE, WASHINGTON AND IRON COUNTIES, UTAH By H. Richard Blank U.S. Geological Survey, Denver, CO Open-File Report 93-203 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1993 PRELIMINARY GEOLOGIC MAP OF THE ENTERPRISE QUADRANGLE, WASHINGTON AND IRON COUNTIES, UTAH INTRODUCTION This map is the first to be released of 4 contiguous l:24,000-scale geologic map sheets comprising the area known informally as the Bull Valley district of the eastern Bull Valley Mountains. The district contains abundant low-grade contact metasomatic and jaspillitic sediment-hosted iron deposits, and less abundant but higher-grade vein-iron deposits. All are associated with monzonitic hypabyssal magmatism of early Miocene age, including emplacement of the Big Mountain intrusion, which cores the Big Mountain structural and topographic dome in the southeast corner of the Enterprise quadrangle. Numerous iron mining claims in the district were patented in years past but intensive exploration, including diamond drilling, had ceased by about 1960 and no ore has ever been shipped from the district on a commercial basis. Mineral resources of the eastern Bull Valley Mountains and vicinity include gold and silver in addition to iron. The Goldstrike district, about 18 km southwest of the Enterprise quadrangle, is currently an active gold producer; and until recently the Escalante mine, located a few km north of the quadrangle, was an important primary producer of silver. Ground water is doubtless the most significant non-mineral resource in the quadrangle, sustaining a flourishing agricultural industry in the southern Escalante Valley. -
Vestiges May 2004Volume24number5
May May 2016 2006 Volume 36 Volume 26 Number 5 Number 5 Monthly Newsletter of URARA, the Utah Rock Art Research Association Table of Contents Symposium Lodging Information .......... 1 Lake Mountain Video ............................... 7 Horsehoe Canyon Field Trip ................... 3 Rock Art and Public Land in the News . 8 Volunteering at Horseshoe Canyon ....... 3 URARA Board Contacts............................ 8 Lake Mountain Shooting Closure........... 4 Calendar and Field Trip Schedule.......... 9 Site Stewards Needed, Vernal BLM....... 7 Presidents Letter Richard Jenkinson is currently out of internet range while he and Lynn move into new quarters. Symposium Lodging Information Steve Acerson Delta Hotels/Motels Fillmore is 30 miles up the road if addition rooms are needed. Days Inn 527 East Topaz Blvd. Victor Chaudhary contact (435) 864-3882 82 Rooms 79.99/71.99 Mention you are a URARA member for $10. discount Budget Motel 75 South 350 East Mike Patel contact (435) 864-4533 33 Rooms Mention URARA 2BD/$67. 1BD/$62. Deltan Inn 347 East Main (435) 864-5318 14 rooms Diamond D Motor Lodge 234 West Main Campgrounds (435) 864-2041 16 Rooms $35 single, $40 dbl Antelope Valley RV Park 776 West Main, Delta Rancher Motel & Café (435) 864-1813 171 West Main (800) 430-0022 (435) 864-2741 96 spaces RV $32, Tent $15 15 Rooms www.antelopevalleyrvpark.com 1 Vestiges URARA Newsletter Great Gallery, April 9, 2016, Steve Acerson Old Woman Canyon, April 10, 2016, Steve Aceerson 2 | May 2016 Vestiges URARA Newsletter Horsehoe Canyon Field Trip Steve Acerson Again the weather forecast was heavy rains and colder temperatures. -
Fire Ecology and Management of the Major Ecosystems of Southern Utah
Chapter 6 Creosotebush, Blackbrush, and Interior Chaparral Shrublands Matthew L. Brooks, Todd C. Esque, and Tim Duck Introduction Creosotebush Scrub The vegetation, fire regime, and Fire Regime Condi- Introduction tion Class descriptions in this paper apply broadly to the Mojave Desert, Colorado Plateau, and southern Great Low cover (5 to 30 percent) of woody shrubs of Basin of western North America. More detail on these various heights (0.5 to 1.5 m [1.6 to 4.9 ft] character- topics, including estimated percentages within each con- izes Creosotebush scrub (Vasek and Barbour 1995). dition class, is provided for the Mojave-Colorado Plateau It occurs across the warm desert regions of western ecotone spanning southern Nevada, the Arizona Strip North America and is the most common plant assem- northwest of the Grand Canyon, and southwestern Utah, blage in the Mojave Desert (fig. 1) (MacMahon 2000). including the area within the boundaries of the Southern Creosotebush scrub is typically found below 1,500 m Utah Fuel Management Demonstration Project (Hood (4,920 ft) on well-drained alluvial flats and slopes below and others, this volume; www.firelab.org/fep/research/ the blackbrush zone and above the saltbush zone that sufm/home.htm). Fire Regime Condition Classes (FRCC) often occur within valley basins (Vasek and Barbour are an interagency, standardized tool for describing the 1995). It phases into shrub-steppe in regions with high natural range of variation in vegetation, fuels, and fire proportions of summer rainfall, typically encountered regime characteristics for a particular biogeographic in the eastern Mojave Desert and Sonoran Desert. -
United States Department of the Interior
United States Department of the Interior BUREAU OF LAND MANAGEMENT Salt Lake Field Office 2370 S Decker Lake Blvd. West Valley City, UT 84119-2022 http://www.blm.gov/utah In Reply Refer To: 8130/2800 (UTW010) Dear Reader: The Bureau of Land Management (BLM) is preparing an environmental assessment (EA) to analyze the development of non-motorized trails to facilitate outdoor recreation opportunities on BLM-managed lands within three areas (an overview map is enclosed) including: 1) Lake Mountains, Utah County. Approximately 17,250 acres in Township 5 South, Range 1 West; Township 6 South, Range 1 West; Township 7 South, Range 1 West; Township 7 South, Range 1 East; Salt Lake Meridian. 2) North Oquirrh Management Area, Tooele County. Approximately 5,285 acres in Township 1 South, Range 4 West; Township 2 South, Range 4 West; Township 2 South, Range 3 West; Township 3 South, Range 4 West; Township 3 South, Range 3 West Salt Lake Meridian; west of the ridgeline and at elevations lower than approximately 6,200 feet. 3) Rose and Yellow Fork Canyons, Salt Lake County. Approximately 1,520 acres in Township 4 South, Range 2 West; Salt Lake Meridian. The BLM recognizes the importance of providing quality recreation experiences on public lands that are adjacent to growing population centers. The BLM is coordinating with partner organizations in Tooele, Utah, and Salt Lake counties, including, but not limited to, the National Park Service Rivers, Trails and Conservation Assistance Program; Tooele County Trails Committee; Tooele County Health Department; Salt Lake County Parks and Recreation; Bike Utah; Eagle Mountain City; Utah Rock Art Research Association; local mountain biking organizations; other entities and the general public in identifying areas and stipulations for the appropriate construction of new, single-track, non-motorized trails. -
West-Central Utah AVAILABILITY of BOOKS and MAPS of the U.S
Isotopic Ages and Stratigraphy of Cenozoic Rocks of the Marysvale Volcanic Field and Adjacent Areas, West-Central Utah AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications re leased prior to the current year are listed in the most recent annual "Price and Availability List." Publications that may be listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" may no longer be available. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices listed below. BY MAIL OVER THE COUNTER Books Books and Maps Professional Papers, Bulletins, Water-Supply Papers, Tech Books and maps of the U.S. Geological Survey are available niques of Water-Resources Investigations, Circulars, publications over the counter at the following U.S. Geological Survey offices, all of general interest (such as leaflets, pamphlets, booklets), single of which are authorized agents of the Superintendent of Docu copies of Earthquakes & Volcanoes, Preliminary Determination of ments. Epicenters, and some miscellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from • ANCHORAGE, Alaska-Rm. -
Federal Center, Denver, Colorado 60225
DEPARTMENT OF THE INTFPinp UNITED STATES GEOLOGicSl OPEN FILE REPORT1967 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Special Projects Branch PRELIMINARY GEOLOGIC SECTION FROM PAHUTE MESA, NEVADA TEST SITE, TO ENTERPRISE, UTAH By P. J. Barosh 1967 Ibis report is preliminary and has not been dited or reviewed for conformity with U. :i. Geological Survey standards and nomenclature. Prepared by the Geological Survey for the U.S. Atomic Energy Commission. UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Federal Center, Denver, Colorado 60225 PRELIMINARY GEOLOGIC SECTION FROM PAHUTB MESA, NEVADA TEST SITE, TO ENTERPRISE, UTAH By P. J. Barosh ABSTRACT The 154-mile long geologic cross section trends nearly perpendicular to the structural grain of the Basin-Range province in Nevada, and in Utah extends eastward into the transition zone between the Basin-Range and Colorado Plateau provinces. The structure is characterized by complex thrust faults, involving uppermost Precambrian to lower Mesozoic sedimentary rocks, and normal faults which cut the thick sequence of Tertiary volcanic rocks as well as older rocks. Some of the normal faults are the result of caldera collapse. The principal normal faults trend northerly west of Delamar, Nev., and form north-trending basins and ranges. Farther east the principal faults trend northwesterly, and form a moderately rugged highland rather than distinct basins and ranges* The uppermost Precambrian-Paleozoic strata thin markedly eastward across the region. The pre-Pennsylvanian sedimentary rocks vary from 32,500 feet in thickness at the Nevada Test Site (Harley Barnes, E. N. Rinrichs, F. A. McKeown and P. P. Orkild, written commun., 1963) to 4,500 feet in the Beaver Dam Mountains in western Utah (Cook, 1960). -
Zion National Park, Utah and Pipe Spring National Monument, Arizona
Ethnographic Overview And Assessment: Zion National Park, Utah And Pipe Spring National Monument, Arizona Prepared for Rocky Mountain Regional Office National Park Service Denver, CO 1997 (Revised 2013) ETHNOGRAPHIC OVERVIEW AND ASSESSMENT: ZION NATIONAL PARK, UTAH AND PIPE SPRING NATIONAL MONUMENT, ARIZONA Prepared by Richard W. Stoffle Diane E. Austin David B. Halmo Arthur M. Phillips III With the assistance of Carolyn M. Groessl Maria Banks Maria Porter Bureau of Applied Research in Anthropology The University of Arizona in Tucson And Southern Paiute Consortium Pipe Spring, Arizona Submitted to Rocky Mountain Regional Office National Park Service Denver, Colorado July 1999 1 TABLE OF CONTENTS List of Figures ...........................................................................................................................xi List of Maps ..............................................................................................................................xvi List of Tables ............................................................................................................................xvii Acknowledgements ...................................................................................................................xix CHAPTER ONE STUDY OVERVIEW Introduction ............................................................................................................................1 1.1 Ecological Stewardship .....................................................................................................1