Wolverines in the Western United States Biological
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Final Biological Assessment
REVISED BIOLOGICAL ASSESSMENT Effects of the Modified Idaho Roadless Rule on Federally Listed Threatened, Endangered, Candidate, and Proposed Species for Terrestrial Wildlife, Aquatics, and Plants September 12, 2008 FINAL BIOLOGICAL ASSESSMENT Effects of the Modified Idaho Roadless Rule on Federally Listed Threatened, Endangered, Candidate, and Proposed Species for Terrestrial Wildlife, Aquatics, and Plants Table of Contents I. INTRODUCTION.......................................................................................................................................... 1 II. DESCRIPTION OF THE FEDERAL ACTION .................................................................................................... 3 Purpose and Need..................................................................................................................................3 Description of the Project Area...............................................................................................................4 Modified Idaho Roadless Rule................................................................................................................6 Wild Land Recreation (WLR)...............................................................................................................6 Primitive (PRIM) and Special Areas of Historic and Tribal Significance (SAHTS)..............................7 Backcountry/ Restoration (Backcountry) (BCR)................................................................................10 General Forest, Rangeland, -
Wolverines in Idaho 2014–2019
Management Plan for the Conservation of Wolverines in Idaho 2014–2019 Prepared by IDAHO DEPARTMENT OF FISH AND GAME July 2014 2 Idaho Department of Fish & Game Recommended Citation: Idaho Department of Fish and Game. 2014. Management plan for the conservation of wolverines in Idaho. Idaho Department of Fish and Game, Boise, USA. Idaho Department of Fish and Game – Wolverine Planning Team: Becky Abel – Regional Wildlife Diversity Biologist, Southeast Region Bryan Aber – Regional Wildlife Biologist, Upper Snake Region Scott Bergen PhD – Senior Wildlife Research Biologist, Statewide, Pocatello William Bosworth – Regional Wildlife Biologist, Southwest Region Rob Cavallaro – Regional Wildlife Diversity Biologist, Upper Snake Region Rita D Dixon PhD – State Wildlife Action Plan Coordinator, Headquarters Diane Evans Mack – Regional Wildlife Diversity Biologist, McCall Subregion Sonya J Knetter – Wildlife Diversity Program GIS Analyst, Headquarters Zach Lockyer – Regional Wildlife Biologist, Southeast Region Michael Lucid – Regional Wildlife Diversity Biologist, Panhandle Region Joel Sauder PhD – Regional Wildlife Diversity Biologist, Clearwater Region Ben Studer – Web and Digital Communications Lead, Headquarters Leona K Svancara PhD – Spatial Ecology Program Lead, Headquarters Beth Waterbury – Team Leader & Regional Wildlife Diversity Biologist, Salmon Region Craig White PhD – Regional Wildlife Manager, Southwest Region Ross Winton – Regional Wildlife Diversity Biologist, Magic Valley Region Additional copies: Additional copies can be downloaded from the Idaho Department of Fish and Game website at fishandgame.idaho.gov/wolverine-conservation-plan Front Cover Photo: Composite photo: Wolverine photo by AYImages; background photo of the Beaverhead Mountains, Lemhi County, Idaho by Rob Spence, Greater Yellowstone Wolverine Program, Wildlife conservation Society. Back Cover Photo: Release of Wolverine F4, a study animal from the Central Idaho Winter Recreation/Wolverine Project, from a live trap north of McCall, 2011. -
Hydrogeologic Framework of the Upper Clark Fork River Area: Deer Lodge, Granite, Powell, and Silver Bow Counties R15W R14W R13W R12W By
Montana Bureau of Mines and Geology Montana Groundwater Assessment Atlas No. 5, Part B, Map 2 A Department of Montana Tech of The University of Montana July 2009 Open-File Version Hydrogeologic Framework of the Upper Clark Fork River Area: Deer Lodge, Granite, Powell, and Silver Bow Counties R15W R14W R13W R12W by S Qsf w Qsf Yb Larry N. Smith a n T21N Qsf Yb T21N R Authors Note: This map is part of the Montana Bureau of Mines and Geology (MBMG) a n Pz Pz Groundwater Assessment Atlas for the Upper Clark Fork River Area groundwater Philipsburg ValleyUpper Flint Creek g e Pz Qsf characterization. It is intended to stand alone and describe a single hydrogeologic aspect of the study area, although many of the areas hydrogeologic features are The town of Philipsburg is the largest population center in the valley between the Qsc interrelated. For an integrated view of the hydrogeology of the Upper Clark Fork Area Flint Creek Range and the John Long Mountains. The Philipsburg Valley contains 47o30 the reader is referred to Part A (descriptive overview) and Part B (maps) of the Montana 040 ft of Quaternary alluvial sediment deposited along streams cut into Tertiary 47o30 Groundwater Assessment Atlas 5. sedimentary rocks of unknown thickness. The east-side valley margin was glaciated . T20N Yb t R during the last glaciation, producing ice-sculpted topography and rolling hills in side oo B kf l Ovando c INTRODUCTION drainages on the west slopes of the Flint Creek Range. Prominent benches between ac la kf k B Blac oo N F T20N tributaries to Flint Creek are mostly underlain by Tertiary sedimentary rocks. -
Geology and Mineral Resources of the Randolph Quadrangle, Utah -Wyoming
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 923 GEOLOGY AND MINERAL RESOURCES OF THE RANDOLPH QUADRANGLE, UTAH -WYOMING BY G. B. RICHARDSON UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1941 For sale by the Superintendent of Documents, Washington, D. O. ......... Price 55 cents HALL LIBRARY CONTENTS Pag* Abstract.____________--__-_-_-___-___-_---------------__----_____- 1 Introduction- ____________-__-___---__-_-_---_-_-----_----- -_______ 1 Topography. _____________________________________________________ 3 Bear River Range._.___---_-_---_-.---.---___-___-_-__________ 3 Bear River-Plateau___-_-----_-___-------_-_-____---___________ 5 Bear Lake-Valley..-_--_-._-_-__----__----_-_-__-_----____-____- 5 Bear River Valley.___---------_---____----_-_-__--_______'_____ 5 Crawford Mountains .________-_-___---____:.______-____________ 6 Descriptive geology.______-_____-___--__----- _-______--_-_-________ 6 Stratigraphy _ _________________________________________________ 7 Cambrian system.__________________________________________ 7 Brigham quartzite.____________________________________ 7 Langston limestone.___________________________________ 8 Ute limestone.__----_--____-----_-___-__--___________. 9 Blacksmith limestone._________________________________ 10 Bloomington formation..... _-_-_--___-____-_-_____-____ 11 Nounan limestone. _______-________ ____________________ 12 St. Charles limestone.. ---_------------------_--_-.-._ 13 Ordovician system._'_____________.___.__________________^__ -
Geologic Map of Ruby Dam Area Southwestern Montana
Geologic Map of Ruby Dam Area Southwestern Montana Compiled and Mapped by Zachary C. St. Jean and Deirdre R. Teeter Montana Bureau of Mines and Geology Open File Report MBMG 488 2004 This report has had preliminary reviews for conformity with Montana Bureau of Mines and Geology’s technical editorial standards. Partial support has been provided by the EDMAP component of the National Cooperative Geological Mapping Program of the U.S. Geological Survey under Contract Number 01HQAG0157. Introduction This project was funded by the EDMAP program of the U. S. Geological Survey. Field studies, including geologic mapping and a gravity and magnetic survey, were conducted during the 2001 field season. These studies were undertaken to gain a better understanding of the geologic structure of the Ruby basin in the area of Ruby Dam in southwest Montana (Figures 1 and 2). Ruby Dam, which impounds Ruby Reservoir, lies within a seismically active region known as the Intermountain Seismic Belt. Delineation and detailed mapping of the Tertiary and Quaternary sediments has helped to understand better the occurrence of Quaternary faulting in the basin. No new faults of Quaternary age were recognized within the field area. However, a fault that offsets Quaternary deposits was newly mapped by the authors in a gravel pit two miles north of the north map boundary. This fault may change previously calculated ground acceleration values at the dam site, and may indicate a greater susceptibility of the dam to seismic activity than previously thought. The geologic map in this report combines previous work that focused on the bedrock of the area with new mapping of the Tertiary and Quaternary deposits by the present authors. -
Rmrs 2008 Rogers P001.Pdf
Forest Ecology and Management 256 (2008) 1760–1770 Contents lists available at ScienceDirect Forest Ecology and Management journal homepage: www.elsevier.com/locate/foreco Lichen community change in response to succession in aspen forests of the southern Rocky Mountains Paul C. Rogers a,*, Ronald J. Ryel b a Western Aspen Alliance, Utah State University, Department of Wildland Resources, 5200 Old Main Hill, Logan, UT 84322, USA b Utah State University, Department of Wildland Resources, 5200 Old Main Hill, Room 108, Logan, UT 84322, USA ARTICLE INFO ABSTRACT Article history: In western North America, quaking aspen (Populus tremuloides) is the most common hardwood in Received 6 July 2007 montane landscapes. Fire suppression, grazing and wildlife management practices, and climate patterns Received in revised form 21 May 2008 of the past century are all potential threats to aspen coverage in this region. If aspen-dependent species Accepted 22 May 2008 are losing habitat, this raises concerns about their long-term viability. Though lichens have a rich history as air pollution indicators, we believe that they may also be useful as a metric of community diversity Keywords: associated with habitat change. We established 47 plots in the Bear River Range of northern Utah and Aspen southern Idaho to evaluate the effects of forest succession on epiphytic macrolichen communities. Plots Lichens Diversity were located in a narrow elevational belt (2134–2438 m) to minimize the known covariant effects of Community analysis elevation and moisture on lichen communities. Results show increasing total lichen diversity and a Succession decrease in aspen-dependent species as aspen forests succeed to conifer cover types. -
Structural and Lithological Influences on the Tony Grove Alpine Karst
Utah State University DigitalCommons@USU All Graduate Theses and Dissertations Graduate Studies 5-2016 Structural and Lithological Influences on the onyT Grove Alpine Karst System, Bear River Range, North-Central Utah Kirsten Bahr Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/etd Part of the Geology Commons Recommended Citation Bahr, Kirsten, "Structural and Lithological Influences on the onyT Grove Alpine Karst System, Bear River Range, North-Central Utah" (2016). All Graduate Theses and Dissertations. 5015. https://digitalcommons.usu.edu/etd/5015 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Theses and Dissertations by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. STRUCTURAL AND LITHOLOGICAL INFLUENCES ON THE TONY GROVE ALPINE KARST SYSTEM, BEAR RIVER RANGE, NORTH-CENTRAL UTAH by Kirsten Bahr A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Geology Approved: ______________________________ ______________________________ W. David Liddell, Ph.D. Robert Q. Oaks, Jr, Ph.D. Major Professor Committee Member ______________________________ ______________________________ Thomas E. Lachmar, Ph.D. Mark R. McLellan, Ph.D. Committee Member Vice President for Research and Dean of the School of Graduate Studies UTAH STATE UNIVERSITY Logan, Utah 2016 ii Copyright © Kirsten Bahr 2016 All Rights Reserved iii ABSTRACT Structural and Lithological Influences on the Tony Grove Alpine Karst System, Bear River Range, North-Central Utah by Kirsten Bahr, Master of Science Utah State University, 2016 Major Professor: Dr. W. -
Correlation Chart of Frontier Formation from Greenhorn Range, Southwestern Montana, to Mount Everts in Yellowstone National Park, Wyoming
DEPARTMENT OF THE INTERIOR MISCELLANEOUS FIELD STUDIES U.S. GEOLOGICAL SURVEY MAPMF-2116 PAMPHLET CORRELATION CHART OF FRONTIER FORMATION FROM GREENHORN RANGE, SOUTHWESTERN MONTANA, TO MOUNT EVERTS IN YELLOWSTONE NATIONAL PARK, WYOMING By R.G. Tysdal, T.S. Dyman, D.J. Nichols, and W.A. Cobban INTRODUCTION figure 2, and thickness relationships-for the measured sections are illustrated in figure 3. In discussing The Upper Cretaceous Frontier Formation in stratigraphic relationships, we proceed from eas* to southwestern Montana was deposited in the foreland west, from shelf to foreland basin. All megafossils basin of the Cordillera in the west and shelf facies of reported here, including those in cited references, were the foreland in the east. Lateral and vertical changes identified by co-author W.A. Cobban and are shown in the lithology of the formation reflect both in tables 1 and 2. All palynomorphs, including those depositional environments and regional tectonism. in cited references, were identified by co-author D.J. The measured sections presented here form a 120-km Nichols and are shown in tables 3 and 4. In the (75-mi) transect that is about normal to the axial citation of previous studies, we have attempted to trend of the mid-Cretaceous seaway in which the include all relevant M.S. and Ph. D. theses, but marine rocks of the formation were deposited, and others, of which we are unaware, may exist. about normal to the orogenic trend in the hinterland to the west (fig. 1). During the Late Cretaceous to MEASURED SECTIONS early Tertiary Laramide orogeny, Cretaceous strata in southwestern Montana were deformed and General locations of the measured sections are foreshortened (telescoped) by eastward transport of shown in figure 1, and detailed locations are giver on strata above major thrust faults. -
Environmental Analysis of the Swan Peak Formation in the Bear River Range, North-Central Utah and Southeastern Idaho
Utah State University DigitalCommons@USU All Graduate Theses and Dissertations Graduate Studies 5-1969 Environmental Analysis of the Swan Peak Formation in the Bear River Range, North-Central Utah and Southeastern Idaho Philip L. VanDorston Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/etd Part of the Geology Commons Recommended Citation VanDorston, Philip L., "Environmental Analysis of the Swan Peak Formation in the Bear River Range, North-Central Utah and Southeastern Idaho" (1969). All Graduate Theses and Dissertations. 3530. https://digitalcommons.usu.edu/etd/3530 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Theses and Dissertations by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. ENVffiONMENTAL ANALYSIS OF THE SWAN PEAK FORMATION IN THE BEAR RTVER RANGE , NORTH-CENTRAL UTAH AND SOUTHEASTERN IDAHO by Philip L. VanDorston A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Geology UTAH STATE UNIVERSITY Logan, Utah 1969 ACKNOWLEDGMENTS My sincerest appreciation is extended to Dr. Robert Q. Oaks, Jr. , for allowing me to develop the study along the directions I preferred, and for imposing few restrictions on the methodology, approach, and ensuing inter pretations. The assistance of Dr. J . Stewart Williams in identification of many of the fossils collected throughout the study was gratefully recetved. My appreciation is also extended to Dr. Raymond L. Kerns for assistance in obtaining the thin sections used in this study. -
Appendix E: Wild and Scenic Rivers Eligibility Study Process Table of Contents
Appendix E: Wild and Scenic Rivers Eligibility Study Process Table of Contents Introduction .................................................................................................................................................. 2 Relevant Laws, Regulations, and Policy ........................................................................................................ 2 Eligibility Process ........................................................................................................................................... 2 Overview ................................................................................................................................................... 2 Step 1: Identify all free-flowing named streams ....................................................................................... 3 Step 2: Identify the region of comparison for each resource ................................................................... 4 Step 3: Develop evaluation criteria to identify ORVs ............................................................................... 6 Step 4: Evaluate named streams and determine if they are free-flowing and possess ORVs .................. 9 Step 5: Classification of eligible streams ................................................................................................... 9 Step 6: Develop management direction to be included in the proposed action .................................... 12 Public Feedback on Wild and Scenic River Eligibility ............................................................................. -
Proposed Action–Revised Forest Plan, Custer Gallatin National Forest
United States Department of Agriculture Proposed Action–Revised Forest Plan, Custer Gallatin National Forest Forest Service January 2018 In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (for example, Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD-3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. To request a copy of the complaint form, call (866) 632-9992. Submit your completed form or letter to USDA by: (1) mail: U.S. -
Outdoor Alliance Draft EIS Comments (2019)
June 4, 2019 Virginia Kelly Custer Gallatin National Forest P.O. Box 130, (10 E Babcock) Bozeman, MT 59771 Submitted online at https://cara.ecosystem-management.org/Public/CommentInput?project=50185 Re: Comments on the Custer Gallatin National Forest draft EIS Dear Virginia and Forest Planning Team: Thank you for the opportunity to comment on the draft Environmental Impact Statement (DEIS) for the Custer Gallatin forest plan revision. These comments are submitted on behalf of Outdoor Alliance and Outdoor Alliance Montana, a coalition of national and Montana-based advocacy organizations that includes Southwest Montana Climbers Coalition, Montana Backcountry Alliance, Southwest Montana Mountain Bike Association, Western Montana Climbers Coalition, Mountain Bike Missoula, Winter Wildlands Alliance, International Mountain Bicycling Association, American Whitewater, and the American Alpine Club. Our members visit the Custer Gallatin National Forest (CGNF) to hike, mountain bike, fat-tire bike, paddle, climb, backcountry ski, cross- country ski, and snowshoe. Outdoor Alliance is a coalition of ten member-based organizations representing the human powered outdoor recreation community. The coalition includes Access Fund, American Canoe Association, American Whitewater, International Mountain Bicycling Association, Winter Wildlands Alliance, The Mountaineers, the American Alpine Club, the Mazamas, Colorado Mountain Club, and Surfrider Foundation and represents the interests of the millions of Americans who climb, paddle, mountain bike, backcountry