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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, -
Selkirk Mountains Grizzly Bear Recovery Area 2015 Research and Monitoring Progress Report
SELKIRK MOUNTAINS GRIZZLY BEAR RECOVERY AREA 2015 RESEARCH AND MONITORING PROGRESS REPORT PREPARED BY WAYNE F. KASWORM, ALEX WELANDER, THOMAS G. RADANDT, JUSTIN E. TEISBERG, WAYNE L. WAKKINEN, MICHAEL PROCTOR, AND CHRISTOPHER SERVHEEN 2016 UNITED STATES FISH AND WILDLIFE SERVICE GRIZZLY BEAR RECOVERY COORDINATOR'S OFFICE UNIVERSITY OF MONTANA, MAIN HALL ROOM 309 MISSOULA, MONTANA 59812 (406) 243-4903 1 Abstract: Idaho Department of Fish and Game (IDFG) captured and monitored a radio collared sample of grizzly bears in the SMGBRZ from 1983 until 2002 to determine distribution, home ranges, cause specific mortality, reproductive rates, and population trend. This effort was suspended in 2003 due to funding constraints and management decisions. In cooperation with IDFG and the Panhandle National Forest (USFS) this effort was reinitiated during 2012 with personnel from the U.S. Fish and Wildlife Service (USFWS). During 2013 the program was expanded with funding from IDFG, USFS, several sources in British Columbia (BC), and USFWS. This cooperative research and monitoring effort was expanded to involve Idaho Department of Lands, the Kalispel Tribe, the Kootenai Tribe of Idaho, and Washington Department of Fish and Wildlife in 2014 Numbers of females with cubs in the Selkirk Mountains grizzly bear recovery zone (SMGBRZ) varied from 0–4 per year and averaged 1.5 per year from 2010–15. Human caused mortality averaged 1.7 bears per year and 0.7 females per year. Ten human caused mortalities during 2010-15 include 4 females (all BC) and 6 males (one US and five BC). Human caused mortalities during 2010-15 were four adult females (one vehicle collision and three under investigation), one adult male (management), and four subadult males (two management, one mistaken identity, and one self-defense). -
CANADA's MOUNTAIN Rocky Mountain Goats
CANADA'S MOUNTAIN Rocky Mountain Goats CANADA'S MOUNTAIN PLAYGROUNDS BANFF • JASPER • WATERTON LAKES • YOHO KOOTENAY ° GLACIER • MOUNT REVELSTOKE The National Parks of Canada ANADA'S NATIONAL PARKS are areas The National Parks of Canada may, for C of outstanding beauty and interest that purposes of description, be grouped in three have been set apart by the Federal Govern main divisions—the scenic and recreational ment for public use. They were established parks in the mountains of Western Canada; the to maintain the primitive beauty of the land scenic, recreational, wild animals, and historic scape, to conserve the native wildlife of the parks of the Prairie Provinces; and the scenic, country, and to preserve sites of national his recreational, and historic parks of Eastern Can toric interest. As recreational areas they pro ada. In these pages will be found descriptions vide ideal surroundings for the enjoyment of of the national parks in the first group—areas outdoor life, and now rank among Canada's which lie within the great mountain regions outstanding tourist attractions. of Alberta and British Columbia. Canada's National Park system teas estab * * * lished in 1SS5, when a small area surrounding mineral hot springs at Banff in the Rocky This publication is compiled in co-operation Mountains was reserved as a public posses with the National Parks Branch, Department sion. From this beginning has been developed of Northern Affairs and National Resources. the great chain of national playgrounds note Additional information concerning these parks stretching across Canada from the Selkirk may be obtained from the Park Superintend Mountains in British Columbia to the Atlantic ents, or from the Canadian Government Travel Coast of Nova Scotia. -
The Effects of Linear Developments on Wildlife
Bibliography Rec# 5. LeBlanc, R. 1991. The aversive conditioning of a roadside habituated grizzly bear within Banff Park: progress report 1991. 6 pp. road impacts/ grizzly bear/ Ursus arctos/ Banff National Park/ aversive conditions/ Icefields Parkway. Rec# 10. Forman, R.T.T. 1983. Corridors in a landscape: their ecological structure and function. Ekologia 2 (4):375-87. corridors/ landscape/ width. Rec# 11. McLellan, B.N. 1989. Dymanics of a grizzly bear population during a period of industrial resource extraction. III Natality and rate of increase. Can. J. Zool. Vol. 67 :1865-1868. reproductive rate/ grizzly bear/ Ursus arctos/ British Columbia/ gas exploration/ timber harvest. Rec# 14. McLellan, B.N. 1989. Dynamics of a grizzly bear population during a period of industrial resource extraction. II.Mortality rates and causes of death. Can. J. Zool. Vol. 67 :1861-1864. British Columbia/ grizzly bear/ Ursus arctos/ mortality rate/ hunting/ outdoor recreation/ gas exploration/ timber harvest. Rec# 15. Miller, S.D., Schoen, J. 1993. The Brown Bear in Alaska . brown bear/ grizzly bear/ Ursus arctos middendorfi/ Ursus arctos horribilis/ population density/ distribution/ legal status/ human-bear interactions/ management/ education. Rec# 16. Archibald, W.R., Ellis, R., Hamilton, A.N. 1987. Responses of grizzly bears to logging truck traffic in the Kimsquit River valley, British Columbia. Int. Conf. Bear Res. and Manage. 7:251-7. grizzly bear/ Ursus / arctos/ roads/ traffic/ logging/ displacement/ disturbance/ carnivore/ BC/ individual disruption / habitat displacement / habitat disruption / social / filter-barrier. Rec# 20. Kasworm, W.F., Manley, T.L. 1990. Road and trail influences on grizzly bears and black bears in northwest Montana. -
Chipmunks (Genus Tamias) in the Northern Rocky Mountains
Evolution, 57(8), 2003, pp. 1900±1916 PHYLOGEOGRAPHY AND INTROGRESSIVE HYBRIDIZATION: CHIPMUNKS (GENUS TAMIAS) IN THE NORTHERN ROCKY MOUNTAINS JEFFREY M. GOOD,1,2 JOHN R. DEMBOSKI,3 DAVID W. NAGORSEN,4,5 AND JACK SULLIVAN1 1Department of Biological Sciences, Box 443051, University of Idaho, Moscow, Idaho 83844-3051 3Biological Sciences Department, California State Polytechnic University, Pomona, 3801 West Temple Avenue, Pomona, California 91768-4032 4Royal British Columbia Museum, Victoria, British Columbia V8V 1X4, Canada Abstract. If phylogeographic studies are to be broadly used for assessing population-level processes relevant to speciation and systematics, the ability to identify and incorporate instances of hybridization into the analytical frame- work is essential. Here, we examine the evolutionary history of two chipmunk species, Tamias ru®caudus and Tamias amoenus, in the northern Rocky Mountains by integrating multivariate morphometrics of bacular (os penis) variation, phylogenetic estimation, and nested clade analysis with regional biogeography. Our results indicate multiple examples of mitochondrial DNA introgression layered within the evolutionary history of these nonsister species. Three of these events are most consistent with recent and/or ongoing asymmetric introgression of mitochondrial DNA across mor- phologically de®ned secondary contact zones. In addition, we ®nd preliminary evidence where a fourth instance of nonconcordant characters may represent complete ®xation of introgressed mitochondrial DNA via a more ancient hybridization event, although alternative explanations of convergence or incomplete sorting of ancestral polymorphisms cannot be dismissed with these data. The demonstration of hybridization among chipmunks with strongly differentiated bacular morphology contradicts long-standing assumptions that variation within this character is diagnostic of complete reproductive isolation within Tamias. -
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. -
Avalanche Characteristics of a Transitional Snow Climate—Columbia Mountains, British Columbia, Canada
Cold Regions Science and Technology 37 (2003) 255–276 www.elsevier.com/locate/coldregions Avalanche characteristics of a transitional snow climate—Columbia Mountains, British Columbia, Canada Pascal Ha¨gelia,*, David M. McClungb a Atmospheric Science Program, University of British Columbia, 1984 West Mall, Vancouver, British Columbia, Canada V6T 1Z2 b Department of Geography, University of British Columbia, Vancouver, British Columbia, Canada Received 1 September 2002; accepted 2 July 2003 Abstract The focus of this study lies on the analysis of avalanche characteristics in the Columbia Mountains in relation to the local snow climate. First, the snow climate of the mountain range is examined using a recently developed snow climate classification scheme. Avalanche observations made by a large helicopter operator are used to examine the characteristics of natural avalanche activity. The results show that the Columbia Mountains have a transitional snow climate with a strong maritime influence. Depending on the maritime influence, the percentage of natural avalanche activity on persistent weak layers varies between 0% and 40%. Facet–crust combinations, which primarily form after rain-on-snow events in the early season, and surface hoar layers are the most important types of persistent weak layers. The avalanche activity characteristics on these two persistent weak layers are examined in detail. The study implies that, even though the ‘avalanche climate’ and ‘snow climate’ of an area are closely related, there should be a clear differentiation between these two terms, which are currently used synonymously. We suggest the use of the term ‘avalanche climate’ as a distinct adjunct to the description of the snow climate of an area. -
Freeride the Powder-Highway Mit Den Breiten Latten Und Splitboards in Kanadas Grossem Nord-Westen Unterwegs - Abseits Der Pisten Und Auf Tour
Freeride the Powder-Highway Mit den breiten Latten und Splitboards in Kanadas grossem Nord-Westen unterwegs - abseits der Pisten und auf Tour. Mehr Kanada-Feeling geht nicht: Exklusiv für Berg+Tal-Gäste haben wir einen neuen Traumtrip für Freerider und Splitboarder entwickelt. Gemeinsam mit unserem deutschsprachigen kanadischen Splitboardguide Hayden und seinem Freund Ben, ebenfalls kanadischer Skiguide, entdecken Sie das Herzstück der Kanadischen Rockies. Bei diesem Ski-Trip treffen regionale Insider-Tipps auf komfortable Unterkünfte und verbinden sich mit kanadischem Livestyle zu einem Winterabenteuer erster Klasse. Skitouren und Freeride in den Monashees. Hier spielen unsere Local Guides ihren Heimvorteil voll aus und führen Sie zu den besten Gipfel und Abfahrten. Unsere Reise führt über den bekannten "Powder Highway" von Kelowna nach Revelstoke, weiter nach Nelson und nach Rossland. Dabei reihen wir Gebiete aneinander, deren Namen maximalen Touren- und Freeride-Spass garantieren: Revelstoke Ski Resort, Rogers Pass, Whitewater Skiing Area, Selkirk Mountains, Kootenay Pass und die Monashee- und Red Mountains. „Powder Highway“ Freeride & Touren für Skifahrer & Splitboarder in Kanada / Kurs919 Vorgesehener Ablauf der Reise im Kurzprogramm 1. Tag Treffpunkt in Zürich und Direktflug nach Kanada. Abwechslungsreiche Fahrt mit Mietfahrzeugen nach Revelstoke. Übernachtung im komfortablen Best Western Plus Hotel, unserer Basis für die kommenden drei Skitage. 2.-4. Tag Freeride- und Skitouren im riesigen Gebiet von Revelstoke und Rogers Pass. Das Programm legen wir dabei jeden Tag neu fest und passen es den jeweils aktuellen Schnee- und Wetterbedingungen an. Am Nachmittag des 4. Tages reisen wir nach Nelson weiter und besuchen unterwegs die Halcyon Hot Springs. Übernachtung im eleganten Hume Hotel & Spa, Ausgangspunkt für die kommenden drei Skitage. -
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._'_____________.___.__________________^__ -
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. -
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.