IDAHO ACTION PLAN (V3.0) for Implementing the Department of the Interior Secretarial Order 3362
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AVALANCHE ACCIDENT- Boardman Pass SUBMITTED BY
AVALANCHE ACCIDENT- Boardman Pass SUBMITTED BY: Sawtooth National Forest Avalanche Center LOCATION: 15 Miles northwest of Fairfield, ID DATE: January 28, 2010 SUMMARY: 1 snowmobiler caught, buried and killed SYNOPSIS: On January 28, 2010, a group of five backcountry snowmobilers were riding near Boardman Pass in the Soldier Mountains of southern Idaho. This area is approximately 15 miles northwest of Fairfield, Idaho and is often accessed from the popular Chimney Creek trailhead. Two riders were climbing the west side of Pt. 9538 when a slide started above the uppermost rider. A third rider watched as moving snow overtook the first rider and the second rider turned to the climber’s left and out of the slide. The slide carried the victim over a thousand vertical feet downhill and buried him four to five feet deep next to his snowmachine; the debris continued several hundred vertical feet further downhill. The party quickly regrouped, located the burial site with a beacon and dug deep enough to provide an airway within an estimated 25 minutes. CPR was unsuccessful. The SS-AMu-D3-R2 avalanche was 2 to 3 feet deep, approximately 300ft wide and ran over 1300 vertical feet. Prior to the accident, the Soldier Mountains had received over 3” of Snow Water Equivalent and roughly three feet of snow since January 12. Moderate to strong southerly and westerly winds had accompanied the snowfall, with wind speeds peaking five days before the accident. The mid-January snowfall fell on an unusually weak layer that had been a concern the entire season. A widespread natural avalanche cycle had occurred in much of the advisory area the weekend prior to the accident, and a smaller avalanche had claimed the life of a skier a week earlier; the local and regional press had covered that accident extensively. -
The Pennsylvania State University
The Pennsylvania State University The Graduate School UNDERSTANDING TRAJECTORIES OF LANDSCAPE CHANGE: THE RESPONSES OF A ROCKY MOUNTAIN FOREST-SAGEBRUSH-GRASSLAND LANDSCAPE TO FIRE SUPPRESSION, LIVESTOCK GRAZING, AND CLIMATE A Dissertation in Geography by Catherine T. Lauvaux © 2019 Catherine T. Lauvaux Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy May 2019 The dissertation of Catherine T. Lauvaux was reviewed and approved* by the following: Alan H. Taylor Professor of Geography Dissertation Advisor Chair of Committee Andrew M. Carleton Professor of Geography Erica A.H. Smithwick Professor of Geography Margot Wilkinson Kaye Associate Professor of Forest Ecology Cynthia Ann Brewer Head of the Department of Geography *Signatures are on file in the Graduate School iii ABSTRACT Naturally functioning forest ecosystems have been called gemstones of the Rocky Mountain landscape, and yet, since Euro-American settlement, these forests have been altered by land-use, fire suppression, extreme wildfires, and climate change. Understanding the changes is limited by lack of information about historical conditions. Knowledge of pre-settlement vegetation patterns and disturbance processes may also be useful in predicting and mitigating future ecological impacts. This study uses repeat aerial photography, fire-scar dendrochronology, tree population age structure, and grazing reports to determine fire history and land-use history and the characteristics, timing, and drivers of vegetation change in a forest-sagebrush-grassland mosaic in the Soldier Mountains, Idaho. Fire frequency before 1900 was greater in low-elevation Douglas-fir forests than high- elevation whitebark pine forests (mean interval of 31(±28.8) years vs 66 (±34.4) years). -
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. -
Yellowstone National Park, Submerged Resources Survey
te t/:p--J038 .. } ,' ,, .. ' . ·� . I ; ,· . ' . '/ YEL.LOWSTONE NATIONAL PARK " � ! I '!'' • SUBMERGED RESOURCES SURVEY I ·' I i I \. ,· i .\ I: ··r· 'I I CC®ll®IT' §��IID� YELLOWSTONE NATIONAL PARK a product of the NATIONAL PARK SERVICE SYSTEMWIDE ARCHEOLOGICALINVENTORY PROGRAM YELLOWSTONE NATIONAL PARK Submerged Resources Survey James E. Bradford Archeologist Matthew A. Russell Archeologist Larry E. Murphy Archeologist Timothy G. Smith Geodesist Submerged Resources Center Intermountain Region National Park Service Santa Fe, New Mexico 1999 11 Submerged Resources Center Cultural Resources Management Intermountain Region National Park Service US Department of the Interior 111 TABLE OF CONTENTS LIST OF FIGURES ..................................................................................................................... vii FOREWORD ................................................................................................................................. X ACKNOWLEDGEMENTS .......................................................................................................... xi PART 1: REMOTE SENSING SURVEY ..................................... ............................................ 1 Matthew A. Russell, Larry E. Murphy and Timothy G. Smith INTRODUCTION .... ............................ ................ ........................................... ............. 2 PROBLEM STATEMENT................... ........................................................................ 3 SURVEY DESIGN AND RATIONALE .............. -
Soldier Mountain Snow Report
Soldier Mountain Snow Report Discoidal or tonetic, Randal never profiles any infrequency! How world is Gene when quintessential and contrasuggestible Angel wigwagging some safe-breakers? Guiltless Irving never zone so scrutinizingly or peeps any pricks senselessly. Plan for families or end of mountain snow at kmvt at the Let us do not constitute endorsement by soldier mountain is a report from creating locally before she knows it. Get in and charming town of the reports and. Ski Report KIVI-TV. Tamarack Resort gets ready for leave much as 50 inches of new. Soldier mountain resort in an issue! See more ideas about snow tubing pocono mountains snow. You have soldier mountain offers excellent food and alike with extra bonuses on your lodging options below and beyond the reports and. Soldier mountain ski area were hit, idaho ski trails off, mostly cloudy with good amount of sparklers are dangerous work to enjoy skiing in central part in. The grin from detention OR who bought Soldier Mountain Ski wax in. Soldier Mountain ski village in Idaho Snowcomparison. Soldier Hollow Today's Forecast HiLo 34 21 Today's as Snow 0 Current in Depth 0. Soldier Mountain Reopen 0211 46 60 base ThuFri 9a-4p. Grazing Sheep in National Forests Hearings Before. Idaho SnowForecast. For visitors alike who lived anywhere, we will report of snow report for bringing in place full of. After school on the camas prairie near boise as the school can rent ski area, sunshine should idaho are you. Couch summit from your needs specific additional external links you should pursue as all units in the power goes down deep and extreme avalanche mitigation work. -
Conservation Status of Least Phacelia (Phaceim Minutissima)
BLM LIBRARY 88049443 G(lSERVmONSlItB^(^ IM^PEIAGELIA fPhaceHa tMmMssima) by Robert K. Moseley (Phacelia minutissima) QK 495 .H88 M674 1995 c.2 W OF LAND MANAGEMENT TECHNICAL BULLETIN NO. 95-7 MARCH 1995 aS 0' ZDO^ 6H ?W3 CONSERVATION STATUS OF LEAST PHACELIA (PHACEIM MINUTISSIMA) by Robert K. Moseley Conservation Data Center February 1995 Idaho Department of Fish and Game 600 South Walnut, P.O. Box 25 Boise, Idaho 83707 Jerry M. Conley, Director % Boise District BLM Idaho Department of Fish and Game Purchase Order No. D050-P4-0268 ABSTRACT Least phacelia (Phacelia minutissima) is a widely distributed, but rarely observed species, known from eight disjunct collection sites in Washington, Oregon, Idaho, and Nevada. Due to the rangewide conservation concern, it was recently added to the list of candidate plants being considered for listing as endangered or threatened under the Endangered Species Act. No systematic survey has been conducted in Idaho. To rectify this paucity of information, I conducted a field survey in the vicinity of all known Idaho sites during 1994, but was unsuccessful in relocating the old collection sites or finding new populations. Recent systematic searches and general floristic inventories in the other three states have also failed to relocate any populations. This report is the status of our knowledge of the distribution and conservation status of least phacelia throughout its range, with an emphasis on Idaho. Because no populations have been seen recently, threats to population and species viability are unknown, although the Oregon population is considered extirpated. Before useful conservation recommendations can be made for leas't phacelia the eight known collections sites must be relocated. -
Appendix E: SWAP Vegetation Conservation Target Abstracts Member National Vegetation Classification Macrogroup/Group Summaries
Appendix E: SWAP Vegetation Conservation Target Abstracts Member National Vegetation Classification Macrogroup/Group Summaries Alpine & High Montane Scrub, Grassland & Barrens Cushion plant communities, dense sedge and grass turf, heath and willow dwarf-shrubland, wet meadow, and sparsely-vegetated rock and scree found at and above upper timberline. Topography, wind, rock movement, soil depth, and snow accumulation patterns determine distribution of vegetation types in these short growing season habitats. Alpine Scrub, Forb Meadow & Grassland (M099) M099. Rocky Mountain & Sierran Alpine Scrub, Forb Meadow & Grassland Railroad Ridge RNA, White Cloud Mountains, Idaho © 2006 Steve Rust Rocky Canyon, Lemhi Mountains, Idaho © 2006 Chris Murphy Cushion plant communities, dense turf, dwarf-shrublands, and sparsely-vegetated rock and scree slopes found at and above upper timberline throughout the Rocky Mountains, Great Basin ranges, and Sierra Nevada. Topography (e.g., ridgetops versus lee slopes), wind, rock movement, and snow accumulation patterns produce scoured fell-fields, dry turf, snow accumulation heath sites, runoff-fed wet meadows, and scree communities. Fell-field plants are cushioned or matted, adapted to shallow drought-prone soils where wind removes snow, and are intermixed with exposed lichen coated rocks. Common species include Ross’ avens (Geum rossii), Bellardi bog sedge (Kobresia myosuroides), twinflower sandwort (Minuartia obtusiloba), Idaho Department of Fish & Game, 2016 September 22 886 Appendix E. Habitat Target Descriptions. Continued. cushion phlox (Phlox pulvinata), moss campion (Silene acaulis), and others. Dense low-growing, graminoids, especially blackroot sedge (Carex elynoides) and fescue (Festuca spp.), characterize alpine turf found on dry, but less harsh soil than fell-fields. Dwarf-shrublands occur in snow accumulating areas and are comprised of heath species, such as moss heather (Cassiope), dwarf willows (Salix arctica, S. -
Crustal Thickness and Vp/Vs Ratio of Yellowstone, Eastern Snake River
Scholars' Mine Masters Theses Student Theses and Dissertations Summer 2017 Crustal thickness and Vp/Vs ratio of Yellowstone, Eastern Snake River Plain, Wyoming Province, and the northern Basin and Range Province through receiver function analysis Avikant Dayma Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Geology Commons, and the Geophysics and Seismology Commons Department: Recommended Citation Dayma, Avikant, "Crustal thickness and Vp/Vs ratio of Yellowstone, Eastern Snake River Plain, Wyoming Province, and the northern Basin and Range Province through receiver function analysis" (2017). Masters Theses. 7689. https://scholarsmine.mst.edu/masters_theses/7689 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. CRUSTAL THICKNESS AND 푉푝/푉푠 RATIO OF YELLOWSTONE, EASTERN SNAKE RIVER PLAIN, WYOMING PROVINCE, AND THE NORTHERN BASIN AND RANGE PROVINCE THROUGH RECEIVER FUNCTION ANALYSIS by AVIKANT DAYMA A THESIS Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE AND TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE IN GEOLOGY & GEOPHYSICS 2017 Approved by Stephen Gao, Advisor Kelly Liu Maochen Ge ii 2017 Avikant Dayma All Rights Reserved iii ABSTRACT For decades, numerous studies have been conducted and contradictory results were achieved about the origin and evolution of the Yellowstone supervolcano and the Eastern Snake River Plain. Whether the 640 km long time-progressive chain of rhyolitic calderas was formed due to mantle-plume or a result of lithospheric extension allowing the emergence of melt on the surface is still a debate. -
EES Wyoming-Idaho Spring Field Course Trip Report
EES Wyoming-Idaho Spring Field Course Trip Report In May, 2019, 24 EES students and three wizened professors flew to Salt Lake City for a a 12-day field course in Utah, Idaho and Wyoming (with a brief foray into Montana). After arriving late at night and discovering that Dr D had forgotten his driver’s license, then found it and lost it, then found it, then lost it and then found it again, the group set off on a clockwise route with 3 days of thunderstorms and rain in the forecast. Fortunately, a quick stop at the Great Salt Lake (Antelope Island) went smoothly and we were able to see the pretty lake amidst swarms of flies hovering over microbial mats, with views of the distant Wasatch Range and its impressive faulted mountain front. We then drove north into Idaho and turned west to the City of Rocks in the southern Albion Range. We lucked out with the weather and had a marvelous hike in the heavily jointed and weathered granite landscape leaving the students in happy spirits because we had truly entered a very scenic part of the wild west. We arrived late in Twin Falls, but still had time to peek into the Snake River Canyon and watch base jumpers plunging past flood basalt cliffs. The evening began with a group meal at Idaho Joes with burgers and pie slices for most. A medical incident left some people poorly rested for the next day, but after a brief stop at dramatic Shoshone Falls, we raced up to Craters of the Moon where again, we somehow avoided the rain, (although we watched a tornado) and saw all the main sites of the amazingly raw volcanic landscape of the northern Snake River Plain. -
Henrys Fork Basin Study Final Report 1 1.0 Introduction
Henrys Fork Basin Study Final Report Produced in partnership with the State of Idaho Water Resource Board U.S. Department of the Interior Idaho Water Resource Board Bureau of Reclamation State of Idaho Pacific Northwest Region Boise, Idaho Snake River Area Office Boise, Idaho January 2015 MISSION OF THE U.S. DEPARTMENT OF THE INTERIOR PROTECTING AMERICA'S GREAT OUTDOORS AND POWERING OUR FUTURE The U.S. Department of the Interior protects America's natural resources and heritage, honors our cultures and tribal communities, and supplies the energy to power our future. MISSION OF THE BUREAU OF RECLAMATION The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound manner in the interest of the American public. Photograph on front cover: Fly fishing, irrigated agriculture, and wildlife habitat are important activities in the Henrys Fork River basin Disclaimer The Henrys Fork Basin Study was funded jointly by the Bureau of Reclamation (Reclamation) and the Idaho Water Resource Board (IWRB), and is a collaborative product of the study participants as identified in Section 1.3, page 5 of this report. The purpose of the study is to assess current and future water supply and demand in the Henrys Fork Basin and adjacent areas that receive water from the basin, and to identify a range of potential strategies to address any projected imbalances. The study is a technical assessment and does not provide recommendations or represent a statement of policy or position of the Bureau of Reclamation, the Department of the Interior, or the funding partners. -
Teton View Regional Plan
for sustainable development MAY 2015 The work that provided the basis for this publication was supported by funding under an award with the U.S. Department of Housing and Urban Development. The substance and findings of the work are dedicated to the public. The author and publisher are solely responsible for the accuracy of the statements and interpretations contained in this publication. Such interpretations do not necessarily reflect the views of the Government. Preface Sustainable communities partnership On June 16, 2009, the U.S. Department of Housing and Urban Development (HUD), the U.S. Department of Transportation (DOT), and the U.S. Environmental Protection Agency (EPA) joined together to help communities nationwide improve access to affordable housing, increase transportation options, and lower transportation costs, all while protecting the environment. This “Sustainable Communities Partnership” identified six livability principles that would form a framework for the variety of funding programs that each agency intended to design over a multi-year period. These principles are: • Provide more transportation choices • Provide equitable, affordable housing • Enhance economic competitiveness • Support existing communities • Coordinate policies and leverage investment • Value communities and neighborhoods The Sustainable Communities Regional Planning Grant program was launched by HUD in 2010 to encourage cities and counties to collaborate on studies related to regional land use, affordable housing, economic development, community vitality, food equity, public transportation and environmental quality. The grants also provided for training and technical assistance for local communities as means to build their resilience for the future. In November 2011, the Western Greater Yellowstone Consortium (Consortium) was awarded a $1.5 million HUD grant and launched its three-year planning process in February 2012. -
Summer in Camas County
S UMMERINSummer in CCamasAMAS CountyC OUNTY S A W T O O T H Ryan SAWTOOTH Glassford Ryan Glassford PeakPeak PeakPeak 11,795 LEGEND r AlturasAlturas 11,795 r WILDERNESS Galena 11,60211,602 e WILDERNESS Galena EGEND e LakeLake L v Peak v Peak i ek 11,170 LAND DESIGNATIONi A R E A reeek 11,170 RR AREA Cr S A W T O O T H C LAND DESIGNATION r e SAWTOOTH s r ke Sawtooth National Recreations Area e ak k e n e v La Galena n v s i L e a e Galena e i r s Sawtooth National Recreatione Area a r Lodge B Sawtooth Wilderness Area e R ur Lodge NATIONAL RECREATION u R t C u MATTINGLY lu O NATIONAL RECREATION MATTINGLY t Closed to motorized and non- Q CREEK l rk k 9090 k A N Sawtooth Wilderness Area— CREEK e Q ee DIVIDE ee r GALENA A e s e U s DIVIDE e GALENA ve o r mechanized vehicles i e i r COEUR Closed to motorized and non- v r COEUR ar SUMMIT e r o i t o L e C SUMMIT A R E A D’ALENE v D’ALENE C h mechanized vehicles C B N B R i AREA B B D Greylock r y o Greylock R O e y r * Mtn e n E k t ROADS AND TRAILSMtn v e l F k o h l i r a n RU o i r r o k Y e * k m o m k ROADS AND TRAILS L l o e F r B m k Paved, Maintained Roads k S T m F e a D e F o S l Y r e Y r o e S ek r N k F a e r and Highways l Y o r E k Paved, Maintained Roads TT Creek k C C e C l e k e TU J J S d F M e l o o Owl w R e Boulder e d N h h TRAIL CREEK id NO N h n O e Boulder r r k and Highways t n O r e TRAIL CREEK Md U h s s r Peak C c Unpaved Maintained Roads i C r o o d SUMMIT M U t n n 181 C UC Peak l o OO ro 181 k k d SUMMIT e u r O o C C r N o c Unpaved Maintained Roads E C N r e