Salmon-Challis NF Fire Plan
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Idaho Mountain Goat Management Plan (2019-2024)
Idaho Mountain Goat Management Plan 2019-2024 Prepared by IDAHO DEPARTMENT OF FISH AND GAME June 2019 Recommended Citation: Idaho Mountain Goat Management Plan 2019-2024. Idaho Department of Fish and Game, Boise, USA. Team Members: Paul Atwood – Regional Wildlife Biologist Nathan Borg – Regional Wildlife Biologist Clay Hickey – Regional Wildlife Manager Michelle Kemner – Regional Wildlife Biologist Hollie Miyasaki– Wildlife Staff Biologist Morgan Pfander – Regional Wildlife Biologist Jake Powell – Regional Wildlife Biologist Bret Stansberry – Regional Wildlife Biologist Leona Svancara – GIS Analyst Laura Wolf – Team Leader & Regional Wildlife Biologist Contributors: Frances Cassirer – Wildlife Research Biologist Mark Drew – Wildlife Veterinarian Jon Rachael – Wildlife Game Manager Additional copies: Additional copies can be downloaded from the Idaho Department of Fish and Game website at fishandgame.idaho.gov Front Cover Photo: ©Hollie Miyasaki, IDFG Back Cover Photo: ©Laura Wolf, IDFG Idaho Department of Fish and Game (IDFG) adheres to all applicable state and federal laws and regulations related to discrimination on the basis of race, color, national origin, age, gender, disability or veteran’s status. If you feel you have been discriminated against in any program, activity, or facility of IDFG, or if you desire further information, please write to: Idaho Department of Fish and Game, P.O. Box 25, Boise, ID 83707 or U.S. Fish and Wildlife Service, Division of Federal Assistance, Mailstop: MBSP-4020, 4401 N. Fairfax Drive, Arlington, VA 22203, Telephone: (703) 358-2156. This publication will be made available in alternative formats upon request. Please contact IDFG for assistance. Costs associated with this publication are available from IDFG in accordance with Section 60-202, Idaho Code. -
Tectonic Alteration of a Major Neogene River Drainage of the Basin and Range
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2016 TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE Stuart D. Parker Follow this and additional works at: https://scholarworks.umt.edu/etd Part of the Tectonics and Structure Commons Let us know how access to this document benefits ou.y Recommended Citation Parker, Stuart D., "TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE" (2016). Graduate Student Theses, Dissertations, & Professional Papers. 10637. https://scholarworks.umt.edu/etd/10637 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. TECTONIC ALTERATION OF A MAJOR NEOGENE RIVER DRAINAGE OF THE BASIN AND RANGE By STUART DOUGLAS PARKER Bachelor of Science, University of North Carolina-Asheville, Asheville, North Carolina, 2014 Thesis Presented in partial fulfillment of the requirements for the degree of Master of Science in Geology The University of Montana Missoula, MT May, 2016 Approved by: Scott Whittenburg, Dean of The Graduate School Graduate School James W. Sears, Committee Chair Department of Geosciences Rebecca Bendick Department of Geosciences Marc S. Hendrix Department of Geosciences Andrew Ware Department of Physics and Astronomy Parker, Stuart, M. S., May, 2016 Geology Tectonic alteration of a major Neogene river drainage of the Basin and Range Chairperson: James W. -
Seasonal Status of the American Pipit in Idaho
SEASONAL STATUS OF THE AMERICAN PIPIT IN IDAHO DANIEL M. TAYLOR, 244 N. 12th, Pocatello,Idaho 83201 In Idaho, the AmericanPipit (Antbus rubescens)has been considered primarilya migrant,either locally common but erratic (Larrison et al. 1967) or uncommonin springand commonin fall (Burleigh1972). Severalother writers(Merriam 1891, Merrill 1898, Newhouse1960, Levy 1962) consid- ered it an abundantfall migrantbut gaveno indicationof actualnumbers. The one (Larrisonet al. 1967) or two (Burleigh1972) winterrecords were from Lewiston.Larrison et al. (1967) suspectedthat pipitsmight breed on someof the state'shigh mountains,while Burleigh(1972) knew of only Merriam's(1891) statementthat they breedin the Salmon River Mountains and a report by L. B. McQueenof breedingin the upper Pahsimeroi drainagenear Borah Peak. This scantinessof breedingevidence may be why the mostrecent A.O.U. checklist(1983) statesthat the AmericanPipit breedslocally on mountaintopsin severalRocky Mountain states but does not specificallylist Idaho. In this paper I consolidateand enhancewhat is known aboutAmerican Pipit distributionin Idaho with reference to adjacent areas. I present evidenceof additionalbreeding, concentrations of thousandsof fall mi- grants,and the species'regular but erraticwintering in much of southern Idaho.I analyzeChristmas Bird Countdata for patternsin winterdistribu- tion relatedto differencesin weather,elevation, geography, and annual variability. METHODS I gatheredrecent American Pipit recordsfrom a literaturereview and my own fieldnotes for the last 15 years.All ChristmasBird Counts(CBCs) for Idahosince 1978 were included,as well as somefrom adjacentMontana and Washington.Long-term counts from southernIdaho were examined statisticallyin a mannersimilar to that of Lauranceand Yensen(1985) and Dunning and Brown (1982). Weather data were extracted from U.S. EnvironmentalData Servicemonthly reports from eachweather station in or closeto eachCBC. -
Big Lost River Mountain Whitefish and Other Populations of Snake River Basin Mountain Whitefish
Mountain Whitefish Conservation and Management Plan for the Big Lost River Drainage, Idaho Photos: Bart Gamett May 2007 Idaho Department of Fish and Game TABLE OF CONTENTS TABLE OF CONTENTS......................................................................................................... 2 EXECUTIVE SUMMARY....................................................................................................... 3 GOAL........................................................................................................................................ 4 PLAN OBJECTIVES............................................................................................................... 4 Population objectives .......................................................................................................................4 DRAINAGE SUMMARY......................................................................................................... 7 MOUNTAIN WHITEFISH POPULATION .......................................................................... 8 General Species Description............................................................................................................8 Origin ................................................................................................................................................9 Historical Status .............................................................................................................................10 Current Status................................................................................................................................11 -
Job Announcement Rangeland Management Specialist, GS 454-9/11
Job Announcement Rangeland Management Specialist, GS 454-9/11 Region 4 Salmon‐Challis National Forest Lost River Ranger District The Lost River Ranger District is seeking candidates for a Rangeland Management Specialist position. This 800,000+ acre Ranger District has an extensive range program with all the excitement, challenges and gratification that goes along with managing grazing (both cattle and sheep) in some incredible country in south central Idaho. The duty station is Mackay, Idaho, a small town in the gorgeous Lost River Valley, settled between the Lost River and Pioneer Mountain ranges. Interested candidates should go to USAjobs and search for Announcement Number 15-0413-149835G-RCA This job is open from July 14 to July 24, 2015 The Forest will be offering up to $25,000 incentive bonus to the selected applicant with a requirement to stay in place for at least three years. For additional information contact Diane Weaver, District Ranger at 208‐588‐3400 or [email protected] Major Duties: The person selected will serve as the District range and weed program leader, supervising one GS 5/7/9 rangeland management specialist, one range technician and a varying seasonal workforce. They will have responsibility for overall management of 35 allotments, including permit administration and long‐term monitoring; overseeing completion of environmental analysis; implementing decisions regarding grazing authorizations; and coordinating with two counties and Cooperative Weed Management Areas. This position works closely with the fisheries and wildlife biologists, as well as other personnel on the District and across the Forest. This position will oversee an extensive monitoring program associated with grazing and ecosystem management. -
The Geology of Part of the Snake River Canyon and Adjacent Areas in Northeastern Oregon and Western Idaho
AN ABSTRACT OF THE THESIS OF Tracy Lowell Vallier for the Ph.D. in Geology (Name) (Degree) (Major) Date thesis is presented May 1, 1967 Title THE GEOLOGY OF PART OF THE SNAKE RIVER CANYON AND ADJACENT AREAS IN NORTHEAXERN OREGON AND WESTERN IDAHO Abstract approved Redacted for Privacy (Major professor) The mapped area lies between the Wallowa Mountains of northeastern Oregon and the Seven Devils Mountains of western Idaho. Part of the Snake River canyon is in- cluded. A composite stratigraphic section includes at least 30,000 feet of strata. Pre- Tertiary and Tertiary strata are separated by a profound unconformity. Pre -Tertiary layered rocks are mostly Permian and Triassic volcani- clastic and volcanic flow rocks. At least four pre -Ter- tiary intrusive suites occur. Tertiary rocks are Miocene and Pliocene plateau basalts. Quaternary glacial materi- als and stream deposits locally mantle the older rocks. Permian ( ?) rocks of the Windy Ridge Formation are the oldest rocks and consist of 2,000 to 3,000 feet of keratophyre, quartz keratophyre, and keratophric pyro- clastic rocks. Unconformably ( ?) overlying the Windy Ridge Formation are 8,000 to 10,000 feet of volcaniclastic rocks and minor volcanic flow rocks of the Hunsaker Creek Formation of Middle Permian (Leonardian and Wordian) age. Spilitic flow rocks of the Kleinschmidt Volcanics are interlayered with and in part overlie the Hunsaker Creek Formation and comprise a sequence about 2,000 to 3,000 feet thick. The Paleozoic layered rocks were intruded by the Holbrook - Irondyke intrusives, composed of keratophyre porphyry, quartz keratophyre porphyry, diabase, and gab- bro. -
OUTREACH Region 4 Salmon Challis NF Lost River Ranger District
OUTREACH District Range Technician, GS 455-6/7/8 Region 4 Salmon Challis NF Lost River Ranger District The Lost River Ranger District is seeking candidates for a Range Technician position. This 800,000+ acre Ranger District has an extensive range program with all the excitement, challenges and gratification that goes along with managing grazing (both cattle and sheep) in some incredible country in south central Idaho. The duty station is Mackay, Idaho; a small town in the gorgeous Lost River Valley, settled between the Lost River and Pioneer Mountain ranges. Interested candidates should contact Diane Weaver, District Ranger, Lost River Ranger District for more information. If you wish to be considered for this opportunity please complete the attached outreach form and send it to Diane Weaver at [email protected] by May 6, 2015. Major Duties: The person selected will be responsible for technical work in support of overall management of 35 allotments. Duties will include: inspect and document permittee compliance with range improvement maintenance and livestock distribution; data collection and monitoring annual forage use and impacts; inventory and treat noxious weeds; administer and maintain the district horse program; lead a monitoring and inventory seasonal crew (usually 2-3 students); input data in INFRA data base; and prepare environmental analysis documents for small range improvement projects. This person needs to be experienced with horses, ATVs, GPS, maps, driving in rugged conditions, have some basic botany skills, and able to work with a crew or independently in the field. Salmon-Challis National Forest The Salmon-Challis National Forest covers over 4.3 million acres in east-central Idaho. -
Chronology, Stable Isotopes, and Glaciochemistry of Perennial Ice in Strickler Cavern, Idaho, USA
Investigation of perennial ice in Strickler Cavern, Idaho, USA Chronology, stable isotopes, and glaciochemistry of perennial ice in Strickler Cavern, Idaho, USA Jeffrey S. Munroe†, Samuel S. O’Keefe, and Andrew L. Gorin Geology Department, Middlebury College, Middlebury, Vermont 05753, USA ABSTRACT INTRODUCTION in successive layers of cave ice can provide a record of past changes in atmospheric circula- Cave ice is an understudied component The past several decades have witnessed a tion (Kern et al., 2011a). Alternating intervals of of the cryosphere that offers potentially sig- massive increase in research attention focused ice accumulation and ablation provide evidence nificant paleoclimate information for mid- on the cryosphere. Work that began in Antarc- of fluctuations in winter snowfall and summer latitude locations. This study investigated tica during the first International Geophysi- temperature over time (e.g., Luetscher et al., a recently discovered cave ice deposit in cal Year in the late 1950s (e.g., Summerhayes, 2005; Stoffel et al., 2009), and changes in cave Strickler Cavern, located in the Lost River 2008), increasingly collaborative efforts to ex- ice mass balances observed through long-term Range of Idaho, United States. Field and tract long ice cores from Antarctica (e.g., Jouzel monitoring have been linked to weather patterns laboratory analyses were combined to de- et al., 2007; Petit et al., 1999) and Greenland (Schöner et al., 2011; Colucci et al., 2016). Pol- termine the origin of the ice, to limit its age, (e.g., Grootes et al., 1993), satellite-based moni- len and other botanical evidence incorporated in to measure and interpret the stable isotope toring of glaciers (e.g., Wahr et al., 2000) and the ice can provide information about changes compositions (O and H) of the ice, and to sea-ice extent (e.g., Serreze et al., 2007), field in surface environments (Feurdean et al., 2011). -
MAP SHOWING LOCATIONS of MINES and PROSPECTS in the DILLON Lox 2° QUADRANGLE, IDAHO and MONTANA
DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY MAP SHOWING LOCATIONS OF MINES AND PROSPECTS IN THE DILLON lox 2° QUADRANGLE, IDAHO AND MONTANA By JeffreyS. Loen and Robert C. Pearson Pamphlet to accompany Miscellaneous Investigations Series Map I-1803-C Table !.--Recorded and estimated production of base and precious metals in mining districts and areas in the Dillon 1°x2° guadrangle, Idaho and Montana [Production of other commodities are listed in footnotes. All monetary values are given in dollars at time of production. Dashes indicate no information available. Numbers in parentheses are estimates by the authors or by those cited as sources of data in list that follows table 2. <,less than; s.t., short tons] District/area Years Ore Gold Silver Copper Lead Zinc Value Sources name (s. t.) (oz) (oz) (lb) (lb) (lb) (dollars) of data Idaho Carmen Creek 18 70's-190 1 (50,000) 141, 226 district 1902-1980 (unknown) Total (50,000) Eldorado 1870's-1911 17,500 (350 ,000) 123, 226 district 1912-1954 (13,000) (8,000) (300,000) Total (650,000) Eureka district 1880's-1956 (13 ,500) 12,366 (2,680,000) 57,994 (4,000) ( 4,000 ,000) 173 Total (4,000,000) Gibbonsville 1877-1893 (unknown) district 1894-1907 (83,500) (1,670,000) 123, 226 1908-1980 ( <10 ,000) 123 Total (2,000,000) Kirtley Creek 1870's-1890 2,000 40,500 173 district 1890's-1909 (<10,000) 1910-1918 24,300 (500 ,000) 123 1919-1931 (unknown) 1932-1947 2,146 (75 ,000) 173 Total (620,000) McDevitt district 1800's.-1980 (80,000) Total (80,000) North Fork area 1800's-1980 (unknown) Total ( <10 ,000) Pratt Creek 1870's-1900 (50 ,000) district Total (50,000) Sandy Creek 1800 's-1900 (unknown) district 1901-1954 19,613 4,055 4,433 71,359 166,179 (310,000) 17 3, 200 Total (310 ,000) Montana Anaconda Range 1880's-1980 (<100,000) area Total (<100,000) Argenta district 1864-1901 (1 ,500 ,000) 1902-1965 311,796 72,241 562,159 604,135 18,189,939 2,009,366 5,522,962 88 Total (7,000,000) Baldy Mtn. -
Late Quaternary Stratigraphy, Idaho National Laboratory, Eastern Snake River Plain, Idaho
Late Quaternary Stratigraphy, Idaho National Laboratory, Eastern Snake River Plain, Idaho Thomas V. Dechert Paul A. McDaniel Kenneth L. Pierce Anita L. Falen Maynard A. Fosberg Idaho Geological Survey Technical Report 06-1 University of Idaho ISBN 1-55765-512-X Moscow, Idaho 2006 Contents Abstract ........................................................................................................................................ 1 Introduction .................................................................................................................................. 1 Quaternary Geologic Setting ....................................................................................................... 2 Local Setting ................................................................................................................................ 5 Methodology ................................................................................................................................ 6 Stratigraphic Units ....................................................................................................................... 7 The Surface Complex ............................................................................................................ 7 The Buried Complex .............................................................................................................. 9 Discussion and Conclusions ...................................................................................................... 11 References ................................................................................................................................. -
Abandoned-Inactive Mines on Bitterroot National Forest-Administered Land
Abandoned-Inactive Mines on Bitterroot National Forest-Administered Land Map of the Curlew Mine by Rick Schmidt in MBMG mineral property files Open-File Report MBMG 484 Phyllis A. Hargrave Catherine McDonald Michael D. Kerschen John J. Metesh Robert Wintergerst Prepared for the U.S. Department of Agriculture Forest Service-Region 1 Abandoned-Inactive Mines on Bitterroot National Forest-Administered Land Open-File Report MBMG 484 October 2003 Phyllis A. Hargrave Catherine McDonald Michael D. Kerschen John J. Metesh Robert Wintergerst Prepared for the U.S. Department of Agriculture Forest Service-Region 1 CONTENTS Page LIST OF FIGURES ........................................................... iii LIST OF TABLES ............................................................ iii 1.0 INTRODUCTION ..........................................................1 1.1 Project Objectives ....................................................1 1.2 Abandoned and Inactive Mines Defined . 2 1.3 Health and Environmental Problems at Mines . 2 1.3.1 Acid Mine Drainage ...........................................3 1.3.2 Solubilities of Selected Metals ...................................3 1.3.3 The Use of pH and SC to Identify Problems . 5 1.4 Methodology ........................................................5 1.4.1 Data Sources .................................................5 1.4.2 Pre-Field Screening............................................6 1.4.3 Field Screening ...............................................7 1.4.4 Field Methods ................................................8 -
Big Lost Mountain Whitefish PROSOPIUM WILLIAMSONI Rev
Conservation Success Index: Big Lost Mountain Whitefish PROSOPIUM WILLIAMSONI Rev. 2.0 - 7/2009 SPECIES SUMMARY Idaho has several sinks river drainages that infiltrate completely into the porous volcanic geology of the northern Snake River Plain and, hence, are disconnected from other surface waters. The Big Lost River, the largest of the sinks drainages, has lacked a surface connection to other rivers for at least 10,000 years. Although the Big Lost River formally terminates at the Big Lost River Sinks, the river also loses water at several natural sinks that form a complex subsurface and groundwater system throughout the valley. The mountain whitefish Prosopium williamsoni is native to western North America, including the Big Lost River in northeastern Idaho. It was first described by Charles Girard in 1891. Recent research at the University of Montana determined the mountain whitefish in the Big Lost River to be genetically divergent from other populations, including its parent population in the upper Snake River; genetic isolation times are estimated to be around 166,000 to 330,000 years. Current Populations and Historic Range Map The mountain whitefish in the Big Lost River has experienced drastic declines from its historical distribution and abundance. According to the 2005 Mountain Whitefish Conservation and Management Plan, it occupied only 24% of its historical range, and abundance was 1.5% of historical estimates. Although the mountain whitefish is considered to be a large river fish, little is known about its habitat requirements. As a result, it remains unknown whether the ecology of mountain whitefish in the Big Lost River differs from other populations.